HomeMy WebLinkAboutSalmon Creek Project - Ferc No. 2307 1981FEDERAL ENERGY REGULATORY COMMISSION
APPLICATION FOR AMENDMENT TO LICENSE
FOR MAJOR PROJECT --EXISTING DAM
SALMON CREEK PROJeCT ~~ FERC NO. 2307
APPLICATION BY:
PREPARED BY:
ALASKA ELECTRIC LIGHT & POWER CO.
JUNEAU, ALASKA
MAY, 1982
TONER & NORDLING, REGISTERED ENGINEERS, INC.
JUNEAU, ALASKA
MAY, 1981
FEDERAL ENERGY REGULATORY COMMISSION
APPLICATION FOR AMENDMENT TO LICENSE
FOR MAJOR PROJECT --EXISTING DAM
SALMON CREEK PROJECT FERC NO. 2307
APPLICATION BY:
PREPARED BY:
ALASKA ELECTRIC LIGHT & POWER CO.
JUNEAU, ALASKA
MAY, 198 2
TONER & NORDLING, REGISTERED ENGINEERS, INC.
JUNEAU, ALASKA
MAY, 1981
At:'"":..:;'/ ED
OCT 2 21982
ALASKA POWER AUTHO:J.!TY
BEFORE THE
FEDERAL ENERGY REGULATORY COMMISSION
APPLICATION FOR AMENDMENT TO LICENSE
FOR MAJOR PROJECT --EXISTING DAM
INITIAL STATEMENT
1. ALASKA ELECTRIC LIGHT AND POWER CO. applies to the
Federal Energy Regulatory Commission for amendment of the
license for FERC Project No. 2307, as described in the
attached exhibits.
2. The locati~n of the project is:
State: Alaska
City & Borough:
Stream:
Juneau
Salmon Creek
3. The exact name and business address of the applicant
are: Alaska Electric Light and Power Co.
134 Franklin Street
Juneau, Alaska 99801
The exact name ..and business address of each person
authorized to act as agent for the applicant in this
application are:
Toner & Nordling, Registered Engineers, Inc.
Box 570
Juneau, Alaska 99802
IS -2
B. G. Hildyard, Consultant
c/o James A. Montgomery, Consulting Engineers, Inc.
2255 Avenida De La Playa
La Jolla, California 92037
4. The applicant is a domestic corporation organized
under the laws of the State of Delaware and duly qualified to
do business in the State of Alaska.
5. The following is a listing of state agencies which
administer the various statutory or regulatory requirements
of the State with respect to projects of this nature:
A. Division of Policy & Planning, Office of the Governor.
Under Alaska Statutes AS 46. 40.010-20 and the Alaska
Administrative Code 6 AAC 80.010-85.900, the State must
determine whether activities having a "direct and
significant impact" on coastal waters are compatible
with State plans for the coastal zone.
B. Alaska Public Utilities Commission.
AS 42.05.010-721 provides for comprehensive regulation
of the services provided by electrical utilities and the
rates charged for those services.
C. Department of Environmental Conservation.
Under 18 AAC 70.081, the department must certify that a
project will comply with Alaska water quality standards.
In addition, under AS 43.03.020, the department in
conjunction with the Department off Fish and Game must
ascertain any impact on runs of anadromous fish.
D. Department of Fish and Game.
IS - 3
Under AS 16.10.020, the Department's approval is
required for any work· impacting on anadromous fish
streams.
E. Department of Natural Resources.
Under 11 AAC 93.150-200, the Department has extensive
regulations covering dam construction. Under AS
46.15.010-270, the Department regulates appropriation of
state waters. Under AS 38.05.330 and regulations
promulgated under 11 AAC 58.300-910, the Department
grants leases and easements that may be needed to use or
cross state lands. Also under AS 41.20.040, AS
41.35.020, AS 41.35.050, AS 41.35.080 and the
regulations promulgated under 11 AAC 16.010-160, the
Department administers and regulates the historic,
prehistoric and archaeological resources of the State.
Under the following headings we have indicated the manner in
which we have complied with the various state laws and
regulations administered by the various departments.
A. Division of Policy & Planning, Office of the Governor.
To comply with the laws and regulations administered by
this agency, we submitted a brief memorandum outlining
the proposed work to be performed under the amendment to
the license. Public notice was posted for thirty days
by the agency to receive comments on the report and the
proposed work. As a result of this action, we have
received a letter from the agency advising that we are
in compliance with the State Coastal Zone Management .
IS - 4
Plan.
B. Alaska Public Utilities Commission.
A copy of the same memorandum was filed with the Alaska
Public Utilities Commission. Their letter in reply
indicates the Commission does not require prior review
and approval of proposed construction by Electric
Utilities. They also express themselves as believing
the project, as outlined, should be in the public
interest.
c. Department of Environmental Conservation.
A copy of the same memorandum was filed with the
Department of Environmental Conservation. Their letter
in reply indicated that a Section 401 Water Quality
Certification would not be required. This was based
upon the fact that the Corps of Engineers was not
exercising jurisdiction over the project and was not
requiring the filing for a Corps of Engineers permit.
They also noted that a Title 16 permit might be required
by the Alaska Department of Fish and Game.
D. Department £! Fish ~ Game.
The same memorandum was filed with the Alaska Department
of fish and Game. Their letter in reply indicated that
they had no objection to the project and that they did
not foresee any major adverse environmental impacts
occurring. They did express concern with the timing of
construction of those portions of the project where work
in the stream would be involved and, ~lso, with erosion
IS - 5
problems that might result from disturbed areas. It is
our intent to confine the instream work as they suggest
and to p:rovide for hydro-seeding of the roadway slopes
and disturbed a:reas under the Construction Contrac~
provisions.
E. Department of Natural Resources.
The same memorandum was filed with the Department of
Natural Resources. Their letter in reply contained the
request by the State Historic Preservation Officer that
a pre-construction cultural resource survey be made. It
also contained a :request, if feasible, that a safe,
recreational trail to Salmon Creek Dam be reestablished.
In response to their first request, we have undertaken a
preconstruct ion cultural resource survey. It wi 11 be
presented here as Exhibit E of this application. With
respect to the reestablishment of a safe trail to the
Dam, the roadway construction being proposed will
provide an exc.ellent recreational trail to the Upper
Powerhouse. From there to the dam, the existing trail
has been brushed out and rehabilitation of certain
sections is planned.
6. We have attached a copy of the memorandum circulated
to all the Federal, State and Municipal Agencies involved.
Copies of all letters received in reply to this memorandum
are also included. This memorandum was circulated to the
following agencies:
Alaska Department of Environmental Conservation
Alaska Department of Fish & Game
IS - 6
As
Alaska Department of Natural Resources, Chief of History
and Archaeology
Alaska Office of Policy Development and Planning, Coastal
Zone Management
Alaska Public Utilities Commission
City and Borough of Juneau
National Marine Fisheries Service
U. s. Army Corps of Engineers
u. S. Department of the Interior, H~ritage Conservation
and Recreation Officer
U. S. Department of the Interior, Regional Environmental
Officer
u. s. Fish and Wildlife Service
evidenced by the replies, we received written
communication from ten of the eleven agencies contacted. We
have had a telephone conversation with personnel of the
Department of the Interior,. Office of Heritage Conservation
and Recreation. We have had no communication with the
Regional Conservation Office of the Department of the
Interior.
IS -7
INITIAL STATEMENT
APPENDIX A
IS - 8
MEMORANDUM
ON
PROPOSED ROAD 7 PIPELINE CONSTRUCTION
LOWER SALMON CREEK REHABILITATION
AEL&P CO. JUNEAU, ALASKA
IS - 9
September 8, 1981
MEMORANDUM
TO: Interested Federal, State and Municipal Agencies
FROM: Toner & Nordling, Registered Engineers, Inc.
SUBJECT: Proposed Road and Pipeline Construction
Lower Salmon Creek Powerhouse Rehabilitation
1. Purpose of the Memorandum.
Under the regulations of the Federal Energy Regulatory
Commission (FERC), the Alaska Electric Light and Power Co.
(AEL&P Co.), when seeking an
operate the Salmon and Annex
amendment to its license to
Creek FERC Project No. 2307,
must consult. with a number of Federal, State and Municipal
agencies prior to submittal of the application for amendment
to their license. This memorandum is intended to provide
these various agencies with the necessary background of
information on the nature and extent of the construction that
is proposed so that the project can be reviewed by them to
determine if it is in general conformity with the various
Federal, State and Municipal laws and regulations that are
applicable to projects of this nature.
2. Histor¥ of the Project.
The Salmon Creek portion of the project, to which the
proposed 1 i cense amendment applies, was constructed by the
Alaska Gastineau Mining Co. during the period 1913 to 1915
IS -10
approxirna tely 2. 5 rni 1 es north of Juneau. The project was
purchased from the Alaska Gastineau Mining Co. and,
subsequently in 1973, by the AEL&P Co.
The Salmon Creek portion of Project 2307 consists of a
constant ang 1e concrete arch darn 167 feet high and having a
crest length of 648 feet. The reservoir formed by the darn
provides 18,000 acre feet of storage at elevation 1172. The
reservoir is connected to Upper Salmon Creek Power House by
4,447 feet of riveted steel penstock which varies in diameter
from 40 inches to 30 inches.
Water from the tailrace of Upper Salmon Creek Power House
can be discharged into a conduit leading to Lower Salmon
Creek Power House or discharged into the stream bed of Salmon
Creek. The conduit connecting the Uppwer Power House to the
Lower Power House consists of a 4' x 5' timber flume 9,876
feet in length. The flume is laid on a 0.25% grade and
terminates in a timber fo rebay. From the fo rebay the water
is conveyed to the Lower Power House by two riveted steel
penstocks, varying from 42 to 30 inches in diameter, 1,625
feet in length.
The flume was reconstructed in 1935 and is supported by
timber mud sills and timber bents, dependent upon the
elevation of the ground surface. Its present condition is
poor and it no longer can be used as an effective conduit to
supply water to the Lower Power House. Also, the penstocks
connecting the forebay to the Lower Power House require
replacement.
IS -11
To aid in construction of the original project, a tramway
was constructed from the beach to a point in the basin below
the dam site. Following completion of construction, this
tramway was utili zed for access and deli very of supplies to
the Upper Power House for many years. In 1966, the tramway
was temporarily rehabilitated to deliver materials and
provide access for the reconstruction of the support
structures of the penstock connecting the reservoir to the
Upper Power House. Subsequently, the tramway has
deteriorated to a point where it is no longer usable.
The general layout of these various structures is
indicated on Sheet 1 (see p. IS -13).
3. Basis for Selection of Road and Pipeline Alternate.
Once a decision was reached to replace the existing flume
and dual penstock system with a new single conduit system to
supply water to the Lower Power House, several alternate
systems to achieve that iesult were considered. The
alternates considered were:
1. Steel pipe flume and steel pipe penstock on existing
flume alignment.
2. Fiberglass Reinforced Pipe (FRP) flume and steel pipe
penstock along existing flume alignment.
3. Timber flume and steep pipe penstock along existing
flume alignment.
4. Semi-circular steel flume and steel pipe penstock a-
long existing flume alignment.
5. Steel pipe pressure penstock along tram alignment.
6. FRP pipe pressure penstock along tram alignment.
Working in conjunction with Mr. Ben G. Hildyard,
IS -12
t --·---
LEGEND
• • • • .. ..... . ..
Existing Flume
Existing Penstock
Proposed Road & Pipeline
NOTE: MAP COPIED FROM U .S .G.S. SHEET JUNEAU B-2
ALASKA ELECTRIC LIGHT & POWER CO.
PROPOSED ROAD & PIPELINE
LOWER SALMON CREEK PROJECT
JUNEAU , ALASKA
SCALE: 1 "= 1 000 ' DATE : 9-15-81
1:63( TONER & NORDL I NG , REG I STERED ENGINEERS . INC.
IS -13 SHE E T 1 0 F 2 ~ )> -~ ~ I ' ____ __._._...._ _____ _
'
Consultant, of James M. Montgomery, Consulting Engineers,
Inc., detailed cost estimates were prepared outlining the
costs of each of the alternates. The summary results of
these estimates are shown in Table 1 {see p. IS -15). The
results of this cost analysis clearly indicate that the most
economic alternate is No. 5, the steel pipe pressure penstock
along the tram alignment.
One other cost factor favoring alternate No. 5 --that
does not appear in the cost analysis {Table 1) is the
maintenance cost. The existing flume alignment traverses
several slide areas that have caused substantial maintenance
and repair work on
buried steel pipe
the existing flume over
along the tram alignment
exposed to these hazards.
the years.
will not
A
be
4. Description of Construction Under Road ~ Pipeline Project.
Under the Road and Pipeline Project, it is proposed to
construct approximately 10,800 feet of roadway from the beach
to the headworks at the Upper Power House. Approximately the
same length of 42" diameter steel pipe will be installed to
connect the headworks with the Lower Power House. The
headworks at the Upper Power House will be of concrete
construction located in the same area as the existing timber
headworks. The headworks wi 11 serve to either divert the
tailrace waters of the Upper Power House into the steel
penstock or divert it into Salmon Creek, as conditions may
require.
All drainage streams feeding into Salmon Creek along the
IS -14
H
CJ)
~
U'l
I I
I I
I . '
ITEM -
'
Remove Existing Flume
Access Road
Tailw9rks
Headworks
Penstock (Flume to PH No. 1)
Construct Flume or Penstock
Subtotal
~
Contingencies
(20\ Penstock-15\ Flume)
..
Total Construction Cost
Engineering & Administration
.. (15\)
Total Project Cost ....
(Mid 1981 Dollars)
Escalation to Mid 1982 (15\)
l_TOTAL PROJECT COST
(Mid 1982 Dollars~
TABLE 1
SUMMARY OF ESTIMATED CONSTRUCTION COST
FOR REHABILITATION OF SALMON CREEK FLUME AND PENSTOCK
(1\ll Cos t:J in Oollflrs)
ALTERNATIVE
Steel Pipe FRP Pipe Timber
Flume Flume Flume Steel Flume
450,000 450,000 450,000 450,000
175,000 175,000 175,000 175,000
40,000 40,000 1301000 130 ,ooo
165,000 165,000 165,000 165,000
185,000 ~85,000 185,000 185,000
2,585,000 2,735,000 2,475,000 2,445,000
3,600,000 3,750,000 3,580.,000 3,550,000
540,000 560,000 535,000 530,000
4,140,000 41310 t 000 4 ,115, 000 4,080,000
I
620,000 645,000 615,000 610,000
4,760,000 4,955,000 . 417 30,000 4,690,000
715,000 745,000 710,000 705,000
5,4 751000 5,700,000 5,440,000 5,395,000
Steel Pipe FRP Pipe
Penstock Penstock
Not Applicable Not Applicable·
790,000 790,000
Not Applicable Not Applicable
'
165,000 165,000
Not Applicable Not Applicable
1,335,000 1,750,000
2,290,000 2 I 70 5, QOO
460,000 540,000
2,750,000 3,245,000
410,000 485,000
3,160,000 3,730,000
475,000 560,000 I
I
I
3,635,000 4,290,000 '
I
roadway alignment wi 11 be cul verted. The· required crossings
of Salmon Creek, anticipated to be two in number, will be
bridged. The bridges will be two span sections utilizing a
center pier to break the span.
From Station 91+50 to Station 94+00 along the road
alignment, the roadway section is in a sidehill cut with the
south s ideslope running down to the edge of Salmon Creek.
Through this section it. is proposed to place rock riprap
along the stream edge to protect the sideslope from erosion
during the periods of-high water flow in Salmon Creek. It is
anticipated that this will require the placement of
approximately 150 cubic yards of rock materials below the
ordinary high water line of Salmon Creek.
Typical construction details for the roadway construction
are shown on Sheet 2 (seep. IS-17).
5. Schedule of Construction.
It is assumed that the amended license application will
be filed by October 1, 1981. In the light of the relatively
minor amendment being requested, relocation of a water
conduit within the project boundaries, the application should
be processed in a nine-month period. With such a timetable,
the road construction should be scheduled for construction in
the latter half of 1982 and the pipeline construction during
the first half of 1983. It is estimated that the road
construction wi 11 take a three to four month period and the
pipeline a two to three month period to construct.
IS -16
l_ ,, __ 1J,Q'
-FINISH GRADE
I
/, ~ -2.0'1!>~·-r----~
, 'f ~~-J!.o'
'ft/11'""'"' w ·+~
42·" PIPE
I ---RIP-RAP El.mANKMENT
EXISTiNG GRADE SALMON CREEK
_ry_e_t_c A !,.. _ __<:;JJ_T__§!~ C T LON WI_ F U_L Ly __ ~!:JR!!~ Q_£!P E
NO SCALE
COVER Fill -~~_; 1-Q'~ t ll O' -l
C,:f' ____ \. I . --~·---Fn,;tsH GRADE
'" ----(T}~-2,~-.
..... -.... 42" PIPE ':r' ..... \ CULVERT
-2~~~~~~~~~~~~-~~-£1''~-;~-;j'~~Ti~.;-;·-;;~-;~tJ1J1r.~-;~-·~~~~~~;;~;~~~~}14~'~, ~-L~~:-s~:~.~
-' '·'\\\\,li~~~~!li{W, ~ ~ -:,N -ST~:~~:LACE ROCK
EXISTING
EXISTING GRADE~ BLANKET TO PREVENT EROSION
T)'J~H~AL FILL Sf=CTION _ _yv I fjALFJ?U.R_!fD_cJ£~
NO SCALE
---------------
\-BORROW EMBANKMENT ~
g~-C.M~. CULVERT
-~~~~~w~~
GRADE __ "\.
DETAIL A-A
NO SCALE IS -
TYPICAL DETAILS
ROADWAY CONSTRUCTION
LOWER SALMON CR. PROJECT
SCALE: AS SHOWN DATE: 9/2/81
TONER & NORDLING .
REGISTERED ENGINEERS INC.
JUNEAU , ALASKA
2
6. Water Resource Utilization.
The various power studies for the Salmon Creek Reservoir
and Upper Power House generation indicate that the maximum
release from the Upper Power House wi 11 be on the order of
6, 5 00 acre feet per month or 110 cubic feet per second. It
was on this basis that the proposed penstock from the Upper
Power House to the Lower Power House was sized.
Under a proposed agreement with the City and Borough of
Juneau, and an existing agreement with the Northern Southeast
Regional Aquaculture Association, the release from the Upper
Power House will be utilized to serve three functions: 1)
the development of hydropower at the Lower Power House; 2)
the provision of a domestic water supply for public use by
the City and Borough of Juneau; and 3) an emergency water
supply for a fish hatcher operated by the Northern Southeast
Regional Aquaculture Association near the mouth of Salmon
Creek in the Twin Lakes Area.
Under these agreements, AEL&P Co. proposes to provide the
City and Borough of Juneau with up to a maximum of 4.64 cubic
feet per second of water per day for development of a
domestic water supply to the area and, under certain
emergency conditions (such as fire) the maximum the water
supply system can handle. Further, it has agreed to supply
the Northern Southeast Regional Aquaculture Association up to
10 cubic feet per second of water during periods of low
stream flow in Salmon Creek when their basic water supply
system cannot provide an adequate water supply for the
IS -18
hatchery. The diversion of the City and Borough supply will
be from the penstock immediately ahead of the Lower Power
House and the diversion of the Northern Southeast Regional
Aquaculture Association supply will be at the headworks at
the Upper Power House.
7. Environmental Impact.
The impact on the environment resulting from construction
of the project will be minor in nature, temporary in
character and almost wholly confined to the constructiori
period. The only long term impact will be on the vegetation
that has to be cleared from the roadway area.
The total roadway area requiring clearing is 19.1 acres.
Of this acreage, approximately 4.8 acres will require removal
of brush only. The remaining · 14. 3 acres wi 11 require the
removal of both brush and timber. The timber wi 11 be a
mixture of virgin timber in areas where the road alignment
varies from the original tram alignment and second growth
timber in the areas along the original tram alignment.
With respect to Air Quality and Noise levels, both wi 11
be impacted during the construction period. This will be
caused by the operation of construction equipment as well as
the drilling and blasting required for the roadway
construction and pipelaying. Upon completion of
construction, the project will have no further impact on Air
Quality or Noise levels.
The stream flow pat terns and the water quality of Salmon
Creek also wi 11 be impacted dud ng the construction period.
IS -19
This should be limited to the period of time the bridge
construction is being accomplished; when the rock riprap for
eros ion control is being placed along the creek edge; and,
when the headworks for diverting the Upper Power House
Tailrace discharge is being replaced. The impact will
consist of increased turbidity in the stream for a short
period and minor interference with stream flow.
It is not anticipated that the project will cause an
increase in erosion in the areai rather, ·by avoiding slide
areas, it should reduce the erosion possibilities in the
area.
With respect to wildlife, the project will cause an
interruption to their use of the habitat. Once construction
has concluded; their use of the habitat should be as free and
uninterrupted as it presently is.
The impact on the fish and aquatic life in Salmon Creek
should be similar in nature but shorter in time that the
impact on the wildlife;
period during which the
again, because of the lesser time
construction will affect their
habitat. The upper reachs of Salmon Creek affected by the
project are not a habitat for anadromous fish.
There are no endangered species in the project area.
Therefore, the project wi 11 have no effect on an endangered
species or their critical habitat.
Finally, it should be noted that the work proposed under
the amended application wi 11 cause far less environmental
impact that would the construction of any of the other
IS -20
alternates which could be constructed along the existing
flume alignment. This is due to the much longer construction
period required for each of these alternates.
8. Recreational Impact.
The Salmon Creek Basin provides recreational facilities
to the Juneau Area mainly in hiking, fishing and berrypicking
opportunities. On a very minor scale, there may be some
hunting in the basin at certain periods of the year.
In recent years, access to the upper reaches of the basin
has been along the existing flume structure. The proposed
construction would very materially improve the pedestrian
access to the basin from the beach to the Upper Power House.
While the completed roadway would permit vehicular traffic
access for four-wheel drive vehicles and cycles, it would not
be the policy of the company to permi~ any vehicle other than
company equipment to utilize the road after completion. To
insure this condition, an effective barrier to vehicular
traffic would be installed at the lower end of the road.
9. Historical ~ Cultural Impact.
There are no known historic structures or sites in or
adjacent to the project site. To the best of local
k~owledge, there are no known artifacts or cultural sites
attributable to the Tlingit-Haida culture in or adjacent to
the project site.
10. Status ~ Project Lands.
All of the lands in the proposed project site are in the
Juneau Townsite Elimination from the Tongass National Forest
IS -21
administered by the U. s. Bureau of Land Management. The use
of these lands have been granted to AEL&P Co. under the
existing license for the operation of FERC Project No. 2307.
IS -22
INITIAL STA'I'EMEt-.'T
APPENDIX B
IS -23
DEPARTMENT OF FISH & t.iAME
October 1 , 1981
Mr. Felix J. Toner
Toner & Nordling, Registered Engineers,
Box 570
Juneau, Alaska 9$9802
Dear Mr. Toner,
Inc.
Re: Lower Salmon Creek Rehabilitation Project
JAYS. HAMMOND, Conrnor
230 S. Franklin Street
Juneau, Alaska 99801
PHONE: 465-4290
As per your request, the Department of Fish and Game has reviewed the
proposed rehabilitation of the lower salmon Creek Hydroelectric project
which consists of replacement of the existing wooden flume with a pipe-
line and access road. In general, we have no objections to the project,
nor do we foresee any major adverse environmental impacts. There are
however, some environmental considerations which must be addressed
during construction of the road and line.
As stated in your report, there is a block to anadromous fish below the
project area on Salmon Creek. However, below the block there is available
spawning area and the Salmon Creek Hatchery operated by the Northern
Southeast Regional Aquaculture Association does obtain its water supply
from Salmon Creek just upstream of the block. Adult salmon can be
expected to start spawning in lower Salmon Creek from July 15 on into
the fall months. Eggs or fry from the wild stocks can then be expected
in the gravel until around the first of May. In order to prevent adverse
impacts upon the wild stocks, or hatchery operations, there should be no
significant introduction of sedimentation into lower Salmon Creek during
the period July 15 to April 30. To avoid possible sedimentation intro-
duction, we recommend that if at all possible no instream or inwater
work be conducted during the period July 15 to April 30.
In addition, due to the past history of sedimentation problems in the
Salmon Creek watershed, we recommend that any area disturbed by the
project be seeded as soon as practical to prevent erosion.
We hope these comments prove useful and we look forward to working with
you on the project as it develops.
Sincerely,
-~~?~
Richard Reed
Regional Supervisor
Habitat Division
cc:
11•K8l.H
Salmon Creek Hatchery
NMFS
USFWS
Planning Dept. C/B Juneau
IS -24
October 2, 1981
Toner & Nordling
P.O. Box 570
Juneau, Alaska 99802
Dear Mr. Toner:
UNITED STATES DEPARTMENT OF COMMERCE
National Oceanic and Atmospheric Administration
Nationat MaPine FishePies SePViae
P.O. Box 1668
Juneau, Ataska 99802
The National Marine Fisheries Service has reviewed the document Lower
Salmon Creek Rehabilitation Project and offer the following comments for
your consideration:
Overall we can identify few impacts that the project may have on the natural
resources which come under our purview. Our main concerns relate to in-stream
construction and road building adjacent to Salmon Creek. The introduction
of soil materials to the stream during road construction could have a short-
lived yet significant impact on fishery resources. Improper road construction
may cause surface erosion, mass soil movement, and stream channel erosion.
One-half to two-thirds of erosion related water pollution occurs during the
first year after road construction.
We believe it is possible for the anadromous fishes present in the lower
reaches of Salmon Creek to be affected by construction activities upstream
within the project area. Surface runoff could transport sediment from the
disturbed uplands to the stream channel. Once in the stream, sediment could
be transported to spawning and rearing areas located downstream.
Proper engineering design, construction techniques, and road maintenance can
minimize the potential for adverse fishery resource impacts. We recommend the
following measures be considered during project design and construction:
1. In-stream construction include a minimum number of entries
and the briefest time per entry possible.
2. All in-stream construction be restricted, if possible, to the
time period of May 1-July 15.
3. Culverts and related drainage features be installed
as filling for the roadbed progresses.
4. All disturbed areas adjacent to Salmon Creek be revegetated as
soon as possible to prevent erosion.
5. If possible, buffer strips of vegetation between the road and
stream be maintained. These buffer strips will act as sediment
traps and reduce the potential silt discharge to the stream.
IS -25
2
6. Sidecasting of excess material should not be allowed. This
material should be properly placed and compacted in inland
disposal areas.
We appreciate the opportunity to provide comments at this time.
Sincerely,
Robe t W. McVey
Direc or, Alaska
I
J
IS -26
DEPARTMEl'WT OF N&nJRAL RESOIJRCES
October 7, 1981
File Re: 1130-13 (FERC/REA)
Mr. Felix J. Toner
Toner & Nordling
P.O. Box 570
Juneau, AK 99802
DIVISION OF PAiti<S
Subject: Proposed Lower Salmon Creek Rehabilitation Work.
Dear Mr. Toner:
JAYS. HAMMOND, GOVERNOR
619 WAREHOUSE DR., SUITE 210
ANCHORAGE, ALASKA 99501
PHONE: 274-4676
We have reviewed the subject proposal and would like to offer the
following comments:
STATE HISTORIC PRESERVATION OFFICER
Our review indicates that significant historic remains may be adversly
impacted. Specifically, the area in question is the locale of three
Alaska Heritage Resource Survey sites (j's JUN-176, JUN-207, and JUN-
2111, all of which are associated with early historic mining efforts in
Juneau. The proposed flume/dual penstock replacement may cause the
removal of significant historical features associated with one or more
of these sites. Moreover, the proposed road construction, as well as
other proposed work in the area, may also adversly impact significant
cultural resources. Therefore, per EO 11593 a 36 CF 8 a pr~
construction cultural resource survey is re t er~r ny
questions, please contact Ty L. Dilliplan e (2 -6).
State Historic Preservation Officer
STATE PARK PLANNING
If feasible this project should provide for the reestablishment of a
safe recreational trail to Salmon Creek reservoir. Description of trail
attached.
LAND & WATER CONSERVATION FUND GRANT PROGRAM
No comment.
Sincerely,
~ ~ip Dennerlein
· DJ.rector
CD/blh
1o-JnLH AttC\chment
IS -27
United States Department of the Interior
IN REPLY REFER TO:
Mr. Felix J. Toner
Toner & Nordling
Box 570
Juneau, Alaska 99802
Dear Mr. Toner:
FISH AND WILDLIFE SERVICE
P. 0. Box 1287
Juneau, Alaska 99802
October 7, 1981
Re: Lower Salmon Creek
Rehabilitation Project
This responds to your letter of September 21, 1981, which requested
our review of your Lower Salmon Creek Rehabilitation Project. The
project would replace a flume that is in poor condition. The proposed
work would involve construction of about 10,800 feet of roadway and a
similar length of pipeline. Tributary streams would be culverted and
crossings of Salmon Creek would be bridged. A portion of the roadway
would cut into a side slope adjacent to Salmon Creek which would be
stabilized by riprap.
We consider the project to be environmentally acceptable provided that
in-stream work is restricted during periods of salmon migration as
recommended by the Alaska Department of Fish and Game in their letter
to you, dated October 1, 1981. We also recommend that erosion control
measures be implemented to minimize discharge of sediments into Salmon
Creek.
Thank you for the opportunity for early review and comment on the
project.
cc: ADF&G, NMFS, ADEC, USFS, DPDP, Jnu
NPS, EPA, BLM, Anc
SEES, ROES
IS -28
Sincerely yours,
~~c.~
Field Supervisor
DEPARTMENT OF THE ARMY
ALASKA DISTRICT. CORPS OF ENGINEERS
P.O. BOX 7002
REPLY TO
ATTENTION OF,
NPACO-RF-P
Toner & Nordling
Registered Engineers, Inc.
P.O. Box 570
Juneau, Alaska 99802
Dear Mr. Toner:
ANCHORAGE. ALASKA 99510
OCT 08 1981
Reference: Lower Salmon Creek
Rehabilitation Project
A review of your proposed project was made recently by myself and I have
determined that a Department of the Army permit would not be required for
the proposed activity.
Thank you for your interest in our regulatory program.
Sincerely,
we~·
RICHARD C. BORSETTI
Permit Processor
Regulatory Functions Branch
IS -29
· lLH
JAY S. HAMMOND, Governor
ALASKA PUBLIC UTILITIES COMMISSION
1100 MacKay Building
338 Denali Street
Anchorage, Alaska 99501
DEPARTMENT OF COMMERCE AND ECONOMIC DEVELOPMENT
Phone (907) 276-6222
Felix J. Toner, P.E.
Toner & Nordling
Registered Engineers, Inc.
P.O. Box 570
Juneau, Alaska 99802
October 16, 1981
RE: Lower Salmon Creek Rehabilitation Project
Dear Mr. Toner:
Currently the Alaska Public Utilities Commission (Commission)
does not require electric utilities under its jurisdiction to ob-
tain prior review and approval of proposed construction. However,
the Commission is as always concerned that utilities endeavor to
provide service to the public in a cost effective manner and where
possible at the lowest possible cost.
Because the content of your September 21, 1981 communication
has not been the subject of investigation or analysis by the Com-
mission, it is not appropriate for it to endorse the proposed
project. However, it appears to the Commission•s staff that in
this instance the proposed construction is compatible with the
aforementioned goal; and accordingly, the amendment of Alaska
Electric Light & Power Co.'s license to operate the Salmon Creek
Hydroelectric Project should be in the public interest.
Very truly yours,
ALASKA PUBLIC UTILITIES COMMISSION
ohnB.(?~~
RB:kjs
IS -30
Mr. Felix Toner -2-December 14, 1981
If you have any questions regarding this letter or the attached stipulations
p 1 ease contact:
David W. Haas
State-Federal Assistance Coordinator
Division of Policy Development
and Planning
Pouch AW
Juneau, Alaska 99811
Phone: ( 907} 465-3562
Enclosure
cc: Wendy Wolf, OCM
Commissioner McAnerney, C&RA
William Lindsay, FERC
Sincerely,
g~
James M. Sou~
Director
Carlton Laird, City and Borough of Juneau
Waine E. Oien, USF&WS
Bruce Hoffman, DEC
Bruce Bachen, S.E. Regional Aquaculture Association, Inc.
IS -31
ORM NO. CBJ 7
Felix Toner
Toner and Nordling
P.O. Box 570
Juneau, Alaska 99801
THE CITY AND BOROUGH OF JUNEAU
CAPITAl OF ALASKA
155 SOUTH SEWARD ST. JUNEAU, ALASKA 99801
October 22, 1981
Subject: Lower Salmon Creek Rehabilitation Project
Dear Mr. Toner:
Your report on the above project was submitted to our Parks
and Recreation Department and the Planning Department for
review. The recommendations from the Parks and Recreation
Department are as follows:
1. That access be continued for recreation purposes along
the proposed road and within the basin.
2. That a sign be placed at the trailhead depicting the
historical significance of the flume, aerial tram and dam.
The Planning Commission reviewed the proposal as well and has
made the following comments:
1. Public access -The Commission requests that the power
company guarantee pedestrian access along the proposed road
for recreational purposes and that access be limited to
service vehicles and pedestrians.
2. Noise impact on the hospital during construction of roads
and pipeline -It is suggested that noise intensive activi-
ties be scheduled during mid-day.
3. Water quality impacts during the construction period -Road
construction should be scheduled during non-migratory/spawn-
ing stages of the salmon in the lower Salmon Creek.
4. Stream flow -Adequate stream flow should be provided for
fish in the lower Salmon Creek hatchery presently under
construction.
IS -32
Felix Toner
October 22, 1981
Page Two
We are glad to be able to be of assistance on this project. If
there is further information needed, we will try to supply it.
Manager
cc: Steve Gilbertson
IS -33
~ ~
Department Of Energy
Alaska Power Administration
P.O. Box 50
Juneau, Alaska 99802
Mr. William Corbus, Manager
Alaska Electric Light & Power Company
134 Franklin Street
Juneau, AK 99801·
Dear Mr. Corbus:
October 30, 1980
This affirms our earlier conversation on your plans to rehabilitate the
lower Salmon Creek Powerplant. The Alaska Power Administration supports
your efforts in this regard.
Our recent studies, as reported in the Juneau Area Power Market Analysis,
September 1980, indicate requirements exceeding critical year firm
energy capability of the present hydras in the Juneau area system as
early as 1983. This is about three years before we expect Crater Lake
power to be available. Thus, the Salmon Creek rehabilitation will
improve the capability to meet winter loads over the next few years.
The added hydro capacity on your system would also help to minimize use
of oil in the event of outages on the Snettisham transmission line.
The Salmon Creek rehabilitation will result in some loss of revenues
from the Snettisham Project through the 1980's, and this will result in
a slight long-term increase in Snettisham power costs. The reason is
that the system will have surplus hydro energy capability for the next
several years, except for the occasional occurrence of low or critical
water supply conditions in unusually cold winters. We think the benefits
to area power consumers through the Salmon Creek rehabilitation would be
substantially larger than any added costs.
As above, our office concurs in your plans for the Salmon Creek rehabili-
tation.
Sincerely,
/y(~
Robert J. Cross
Administrator
IS -34
..
,.
DEPT. OF ENVIRONMENTAL CONSERVATION
SOUTHEAST REGIONAL OFFICE
November 27, 1981
Toner & Nordling Registered Engineers, Inc.
114 South Franklin Street
Juneau, Alaska 99801
ATTN: Felix Toner
Dear Mr. Toner:
JAYS. HAMM0/10, GOVER/lOR
~BOX 2420 JUNEAU, ALASKA 99803
0 BOX 540, SITKA, ALASKA 99835
0 ROOM203
415 MAIN STREET
KETCHIKAN, A LASKA 99901
The Department of Environmental Conservation has reviewed the proposed road
and pipeline construction plans for AEL&P's lower Salmon Creek rehabilitation
project.
No permit will be required from our Department to do the proposed work. If
an Army Corps of Engineers permit is required, a 401 Water Quality Certification
would be issued. Since the Corps of Engineers has stated they are not exercising
jurisdiction, a 401 Certification will not be required. To my knowledge, the
only authorization required from the plans you submitted is a Title 16 permit
issued by the Alaska Department of Fish and Game.
If I may be of further assistance, please feel free to contact me at 789-3151.
Sincerely,
~dr./J'-rYJ~ .
Bruce H. H~f;;T/', ~ /ryt
Ecologist
IS -35
OWI(;B OF TBB GOVERNOR
DIVISION OF POLICY DEVELOPMENT AND PlANNING
GOVERNMENTAL COORDINATION UNfT
Mr. Felix Toner
Toner & Nordling
P.O. Box 570
Juneau, AK 99802
December 14, 1981
JAY S. HAMMOND, Governor
POUCH AW (MS • 0165)
JUNEAU, ALASKA 99811
PHONE: (907) 465-3562
REGISTERED MAIL
RETURN RECEIPT
REQUESTED
Subject: AEL&P SALMON CREEK RENEWABLE ENERGY REHABILITATION -FERC LICENSE
State I.D. No. AK81100506FP
Dear Mr. Toner:
The Division of Policy Development and Planning (DPOP) in accordance with
Public Laws 92-583 and 94-370 and Alaska Statute 46.40.010, has completed
review of the consistency of the subject proposal with the Alaska Coastal
Management Program (ACMP).
As currently planned, we have found the proposal to be consistent with
the ACMP provided that the proposal is modified according to the attached
stipulation(s).
The purpose of the ACMP consistency review is to balance the potentially
conflicting uses of the coastal zone through the application of ACMP
guidelines and standards to a project's design, construction, and impact
on the coastal zone. If the attached stipulations are not acceptable,
they can in some instances be changed or modified to meet the needs of the
applicant while still ensuring consistency with ACMP. Therefore, we
encourage you to contact us if you desire to enter into mediation over
them. Failure to do so within 30 days of receipt of this letter will be
interpreted as your acceptance of the stipulations.
By copy of this letter, we are advising the Federal Energy Regulatory
Commission that your project, as stipulated, is consistent with the
ACMP.
IS -36
STATE OF ALASKA
DIVISION OF POLICY DEVELOPMENT AND PLANNING
CONSISTENCY DETERMINATION WITH THE ALASKA COASTAL MANAGEMENT PROGRAM
A determination of consistency with the Alaska Coastal Management
Program, as required by 6 AAC 80, has been requested by Alaska Electric
Light and Power Co., 134 Franklin Street, Juneau, Alaska 99801 for
construction of 10,800 feet of culverted roadway which will include two
bridges and a 42" diameter steel pipe buried under the roadway. The
proposed activity is located in Salmon Creek Valley approximately 2.5
miles north of Juneau, Alaska.
This proposed activity, identified as AEL&P Salmon Creek Renewable
Energy Rehabilitation-FERC (State I.D. No. 81100506), requires an
authorization from Federal Energy and Regulatory Commission and is
therefore subject to review for consistency with t~e Alaska Coastal
Management Program, in accordance with Section 307(c)(3)(A) of the
Federal Coastal Zone Management Act.
Having reviewed the application, the Division of Policy Development and
Planning determines that the proposed activity is consistent with the
Guidelines and Standards of the Alaska Coastal Management Program, 6 AAC
80, provided that the applicant complies with the following
stipulation(s):
1. There shall be no instream or inwater construction during the period
of July 15 to April 30. (This stipulation is intended to prevent
adverse impacts on spawning salmon habitat caused by the introduction of
sedimentation into lower Salmon Creek.) 6 AAC 80.130. HABITATS.
Adherence to the above stipulation(s) will ensure that this project will
be consistent with the ACMP standard(s) 6 AAC 80.130. HABITATS as follows:
6 AAC 80.130. HABITATS. (a) Habitats in the coastal area which
are subject to the Alaska coastal management program include
(7) rivers, streams, and lakes; and
(b) The habitats contained in (a) of this section must be managed
so as to maintain or enhance the biological, physical, and chemical
characteristics of the habitat which contribute to its capacity to
support living resources.
(c) In addition to the standard contained in (b) of this section,
the following standards apply to the management of the following
habitats:
IS -37
(7) rivers, streams, and lakes must be managed to protect
natural vegetation, water quality, important fish or wildlife habitat
and natural water flow.
(d) Uses and activities in the coastal area which will not conform
to the standards contained in (b) and (c) of this section may be allowed
by the district or appropriate state agency if the following are
established:
(1) there is a significant public need for the proposed use
or activity;
(2) there is no'feasible prudent alternative to meet the
public need for the proposed use or activity which would conform to the
standards contained in (b) and (c) of this section; and
(3) all feasible and prudent steps to maximize conformance
with the standards contained in (b) and (c) of this section will be
taken.
(e) In applying this section, districts and state agencies may use
appropriate expertise, including regional programs referred to in sec.
30(b) of this chapter.
Authority:
IS -38
AS 44.19.893
AS 46.40.040
EXHIBIT A
EXHIBIT A
APPLICATION FOR AMENDMENT OF LICENSE
FERC LICENSE NO. 2307
ALASKA ELECTRIC LIGHT AND POWER CO.
DESCRIPTION OF EXISTING PROJECT
Project Description. The project consists
hydroelectric developments as described below.
Project Works.
of three
Salmon Creek No. 2 Development: A concrete arch dam 170
feet high with a 648-foot crest (including spillway) on
Salmon Creek, creating a reservoir with a storage
capacity of 19,000 acre-feet, and steel pipe conduit
4,477 feet long varying in diameter from 40 to 30 inches
extending to Powerhouse No. 2, containing two 1,400 KW
generators;
Salmon Creek No. 1 Development: A 4-foot by 5-foot wood
flume 9,8 76 feet long extending from the tail race of
Powerhouse No. 2 to a forebay and two steel penstocks
1,625 feet long varying in diameter from 42 to 30 inches
extending from the forebay to Powerhouse No. 1,
containing two 1,400 KW generators;
Annex Creek Development: A wood-frame buttress
A - 2
dam 25 feet high and 115 feet long on Upper Annex Creek
creating a reservoir with a storage capacity of 23,400
acre-feet; an 8 by 8 foot tunnel 1,418 feet long, the
last 250 feet of which iss lined with a 78 inch diameter
steel liner; and 6,409 feet of 42 inch and 703 feet of
36 inch steel pipe extending to a powerhouse containing
two 1,750 KW generators; and
Interconnected transmission lines consisting of the 1.89
mile line between Powerhouse No. 2 and Powerhouse No. 1;
the 4.17 mile line between Powerhouse No. 1 and "A"
millsite and old steam plant regulating station, and the
16 mile line from the Annex Creek powerhouse to millsite
"A" via Thane, and other necessary appurtenances.
DESCRIPTION OF PROPOSED CHANGES
proposed for construction under the The
amendment
project
to the license consists of the construction of
approximately 10,800 feet of roadway and the installation of
10,800 lineal feet of 42" diameter steel pipe. These items
will replace the wood flume, wood forebay and steel penstocks
that were uti 1 i zed to deliver the discharge from the Upper
Salmon Creek Power House and other sources to the Lower
Salmon Creek Power House. Replacement of the original
conduits was required because of the extensive physical
deterioration of those conduits. In the economic analysis
made when the replacement problem was considered, the roadway
A - 3
and pipeline alternate developed as the most economic
alternate of the six alternates considered. The various
alternates and their estimated costs are indicated in Table
1, which follows.
All of the drainage streams feeding into Salmon Creek
along the roadway alignment will be culverted. The required
crossings of Salmon Creek, anticipated to be two in number,
will be bridged. The bridges wi 11 be two span sections
utilizing a center pier to break the span.
From Station 91 + 50 to Station 94 + 00 along the
roadway alignment, the roadway section is in sidehill cut
with the south s ideslope running down to the edge of Salmon
Creek. Through this section it is proposed to place rock
riprap along the stream edge to protect the sideslope from
erosion during the periods of high water flow in Salmon
Creek. It is anticipated that this will require the
placement of appproximately 150 cubic yards of rock materials
below the ordinary high water line of Salmon Creek.
The general plan layout and typical sections of the
proposed road and pipeline construction are part of Exhibits
F & G of this application. Also, as part of Exhibit G, the
detailed 1 ega 1 description of the R. o. W. across Federal
lands is shown.
permanent R. o.
less.
The total acreage of the land within the
W. boundary will be 24.76 acres, more or
A -4
EXHIBIT B
EXHIBIT B
APPLICATION FOR AMENDMENT OF LICENSE
FERC LICENSE NO. 2307
ALASKA ELECTRIC LIGHT AND POWER CO.
PROJECT OPERATION AND RESOURCE UTILIZATION
This Exhibit B contains a statement of project operation
and resources utilization for the project amendment of
replacing the wooden flume and steel penstock that supplied
water from Powerhouse No. 2 (Upper Powerhouse) to Powerhouse
No. 1 {Lower Powerhouse) with a pressure penstock· extending
from Powerhouse No. 2 to Powerhouse No. 1.
Under the amended project, the overall operation of the
system wi 11 remain virtually the same. Water wi 11 continue
to be stored behind Salmon Creek Dam and conducted to
Powerhouse No. 2 for power generation through the existing
riveted steel penstock. Powerhouse no. 1 will continue to
generate power from the releases through Powerhouses no. 2.
The releases will be transported through a pressure penstock
extending from Powerhouse No. 2. There will be no changes or
revisions in Salmon Creek Dam nor any changes in the
operation of either powerhouse.
B - 2
Also, under a proposed agreement with the City and
Borough of Juneau, AEL&P Co. will provide 4.64 cfs of water
per day for a domestic water supply for the Lemon Creek and
Mendenhall Valley areas. Under such emergency conditions as
fire, the maximum the water supply can accommodate would be
provided. AEL&·P Co. also has an existing agreement with
NSRAA to provide 10 cfs for hatchery operations during
periods of low flow in Salmon Creek, when the NSRAA water
supply system does not provide adequate flows.
The lower powerhouse is not presently operating because
of structural deterioration of the existing flume and
penstock making its capability of carrying water in its
present condition questionable. Once the new pressure
penstock is completed, Powerhouse No. 1 will continue to be
operated as in the past before deterioration of the flume and
penstock. The amount of energy produced will be essentially
the same as in the past.
In order to determine the most feasible and economical
replacement for the wooden flume and penstock, feasibility
studies to determine the cost of replacement and amount of
energy generated were made. Six alternative projects were
studied, they were:
Steel pipe flume and steel pipe penstock on existing
8 - 3
alignment.
FRP pipe flume and steel pipe penstock on existing
alignment.
Timber flume and steel pipe penstock on existing
alignment.
Semi-circular steel flume and steel pipe penstock on
existing alignment.
Steel pipe pressure penstock on tram alignment.
FRP pipe pressure penstock on tram alignment.
All alternatives were sized to deliver 110 cubic feet
per second from Powerhouse No. 2 to Powerhouse No. 1. This
quantity of water represents the maximum average discharge
from Powerhouse No. 2 determined from reservoir operation and
power generation studies for various methods of operation of
Salmon Creek Reservoir and Powerhouse No. 2. The two pipe
flume alternatives were designed to flow full when laid to
the grade of the existing flume. The timber and semi-circu-
lar steel flume alternatives were designed to pass the design
flow with approximately one foot freeboard. The two pressure
penstock alternatives were sized so that the power generation
at Powerhouse No. 1 was approximately the same as that under
the four flume alternatives and to limit the velocity to less
than 15 feet per second.
Estimated costs of the four flume alternatives are very
close to being equal with escalated project costs varying
only approximately 6 percent from the least costly to the
B -4
most costly. Estimated costs of the two types of pressure
penstocks are both appreciably less than any. of the flume
alignments with the steel pipe penstock being the least
costly, being appro xi rna tely 65 percent of the cost of the
flume projects with a savings of· over 1.5 million dollars.
The following table gives the results of the studies. Costs
are escalated to mid-1982 and include contingencies and
engineering and administration.
Project
Steel Pipe Penstock
FRP Pipe Penstock
Steel Flume
Timber Flume
Steel Pipe Flume
FRP Pipe Flume
B -5
Estimated Cost
$ 3,635,000
4,290,000
5,395,000
5,440,000
5,475,000
5,700,000
EXHIBIT C
EXHIBIT C
APPLICATION FOR AMENDMENT OF LICENSE
FERC LICENSE NO. 2307
ALASKA ELECTRIC LIGHT AND POWER CO.
CONSTRUCTION SCHEDULE
The project is scheduled to begin and be completed in
1983. It is estimated that the roadway construction will
cover a three to four month period and the pipeline
installation a two to three month period. With roadway
construction begining in the spring of 1983, the project can
be completed prior to November 15th, 1983, the time at which
work of this character is closed down in the Salmon Creek
basin due to weather.
The basis for delaying the work to 1983 is threefold:
1. Action is being deferred until the results of the
Part 12 examination can be reviewed.
2. Financing and management resources should be devoted
almost wholly to the Transmission and Distribution
system during 1982.
3. The Capital Move election is scheduled for November,
1982. The results ·of this election could have a
c -2
severe impact on the Company's future.
c -3
EXHIBIT D
During
EXHIBIT D
APPLICATION FOR AMENDMENT OF LICENSE
FERC LICENSE NO. 2307
ALASKA ELECTRIC LIGHT AND POWER CO.
STATEMENT OF COSTS AND FINANCING
the studies undertaken to determine the
feasibility of the Lower Salmon Creek Rehabilitation Project,
two methods were considered for operation of the Salmon Creek
Reservoir.
The first method was based on having the maximum water
in storage during the latter part of the year to insure the
reservoir would be full on January 1 of each year. This was
based on the need to have a large amount of water in storage
to be used for power generation in case of an interruption of
power from the Snettisham Project during the critical winter
months. Under this first method, the average annual power to
be generated at the Lower Salmon Creek Powerhouse is
9,730,000 KWH.
The second method is based upon reservoir operation to
provide as much power during the winter months, December
through April. Under this second method of reservoir
operation, the average annual power to be generated at Lower
Salmon Creek Powerhouse is 10,080,000 KWH.
D - 2
The company is proposing to operate the reservoir under
the first method outlined above and the power production
developed under this method is used in calculating the
average annual cost per KWH that will be experienced as a
result of constructing this project. The total production
also is corrected to a value of 9,319,570 KWH to allow for
the 410,430 KWH that will be lost as a result of the water
allotment to the City and Borough of Juneau. In determining
the KWH lost as a result of the use of 4.64 cfs by the City
and Borough of Juneau, a direct ratio of water allotted (4.64
cfs) to water available (110 cfs) was used.
Estimated Project Cost
1. Land rights --Annual Payment
($100/yr. for 20 years)
2. Road Construction --2.03 miles
($ 390,000/mi.)
3. Headworks
4. Pipeline Installation
Contingency --20%
Total Construction Cost
Administration, Legal,
Engineering --15 %
Inflation --15%
Interest during Construction
Total Project Cost --1983
D - 3
$ 2,000
791,700
165,000
1,335,000
458,740
2,752,440
412,866
474,796
258,000
$ 3,898,102
Estimated Average Annual Cost
1. Capital Costs* --semiannual payments
(8.6% for. 20 years)
2. Local Taxes 15 mill rate
(1,200,000 value)
3. Depreciation --30 yr. period
4. Operation & Maintenance, Administrative
and General Expenses
*sased on Total Project Cost reduced
by $ 900,000 Grant from City and
Borough of Juneau
$ 166,700
18,000
129,937
60,000
$ 374,637
Average Annual Cost/KWH based on
producing 9,319,570 KW
374,637 = $ 0.040/KWH
9,319,570
The rna in source of energy and capacity for the Juneau
area is the Snettisharn Hydroelectric Project which is
operated by the Alaska Power Administration, an agency of the
U. s. Government. The area is served by two electric
utilities, the Alaska Electric Light and Power Company (AEL&P
Co.) and the Glacier Highway Electric Association (GHEA), a
rural electric cooperative and a preference customer.
The energy requi rernent for 1980 for the two utilities
was 159,000,000 KWH. The annual requirements of both
utili ties is expected to grow signi fcantly over the next few
years because of the advent of electricity's being
competitive with fuel oil as a source of heat. The firm
annual capacity of Snettisharn is 168,000,000. In addition,
AEL&P Co.'s own hydroelectric facilities (Annex Creek and
Upper Salmon) produced firm annual energy of 37,000,000 K\vH.
On September 12, 1980, the Alaska Power Administration
D - 4
completed a report entitled Juneau Area Power Market Analysis
which was prepared· to support a Congressional requests for
funds to expand the capabi 1 i ty of Snett i sham. Enclosed is
Table 17 from the Analysis which shows that by 1983 the
Juneau area will be partially dependent on diesel generation.
The energy that wi 11 be displaced by the rehabilitation of
Lower Salmon will be diesel. AEL&P Co. would probably add a
combination diesel and oi 1-f ired gas turbine capacity at an
ave rage cost of $ 50 0 per KW. The fixed charge rate on
capital investment would be as follows:
Capital 8.6%
Property Taxes l. 5%
Depreciation 3.3%
Total 13.4%
Assuming a 60% plant factor 1 the average cost per KWH would
be
Capacity Charge
$ 500 X 0.134
o:6o-i 3.65 x 24
Cents/KWH
1.3
Operation and maintenance expense
estimates 1.0
Fuel costs are based upon past
experience of 11 KWH/gallon and a
current cost per gallon of $ 1.101 10.0
Total 12.3
Based upon an annual generation of 9 1 319 1 5 70 KWH from
the Lower Salmon Hydroelectric plant 1 the estimated average
annual cost of obtaining the equivalent amount of power
(capacity and energy) would be
D - 5
9,319,570 KWH X $ 0.123/KWH = $ 1,146,307
The estimated average cost of equivalent power could be
higher depending on escalation of the cost of fuel oil.
AEL&P Co. has a financing commitment by statute from the
State of Alaska for a $ 3,500,000 loan for the rehabilitation
of Lower Salmon. In addition, the City and Borough of Juneau
has agreed to contribute $ 900,000 for the rehabilitation in
return for utilization of some of the water for municipal
water utility. The remaining monies required to complete the
project will come from internally-generated funds. AEL&P Co.
has annual Operating Revenues of at least $ 5,900,420 to meet
the construction costs and the annual operating costs of this
project.
D - 6
EXHIBIT E
EXHIBIT E
APPLICATION FOR AMENDMENT OF LICENSE
FERC LICENSE NO. 2307
ALASKA ELECTRIC LIGHT AND POWER CO.
ENVIRONMENTAL REPORT
HISTORIC AND CULTURAL SURVEY
E -2
· AUTHORSHIP AND ACKNOWLEDGEMENTS
Dan Bishop served as Project Manager of the Salmon Creek
investigation and conducted the assessment of water quality
and streamflow impacts. Dan has extensive experience with
the biology and hydrology of coastal Alaskan streams gained
during eleven years with the u.s. Forest Service and eight
years of land-water resource consultant work in Southeast
Alaska.
quality
He has participated in projects addressing water
control, land planning, salmon habitat and hatchery
siteing, and has managed environmental investigations for
proposed hydroelectric sites near Skagway and on Prince of
Wales Island in Southeast Alaska.
Janice Mills served as Coordinator of the investigation and
participated in water quality, streamflow, wildlife and
fisheries assessments. Ms. Mills is a biology graduate from
the University of California at Berkeley, with two years of
resource development consulting work in Alaska. This
experience includes studies of drilling effluent disposal in
the Beaufort Sea for Sohio Alaska Petroleum Company and
biological effects associated with submarine electrical
transmission for the Alaska Power Administration.
Steve Jacoby, who provided vegetative mapping for the Salmon
Creek drainage, is a forester, graduated from Auburn
University, with five years of forestry experience in
E -3
Southeast Alaska. His experience includes growth and yield
assessment for the U.S. Forest Service, forest inventories
for Sealaska Timber Corporation, and forest-habitat
investigations for the Alaska Department of Fish and Game.
He has provided vegetation inventories for other
hydroelectric project sites in Southeast Alaska.
Tim Moore surveyed the proposed development area for items of
cultural and historical value. He is an archaeology graduate
of California State University, with experience in
archaeologic digs in California and environmentally-related
archaeologic investigations in Southeast Alaska and
elsewhere.
Information and
agencies and
investigation:
consultation was provided by the following
organizations during the Salmon Creek
Alaska Department of Fish and Game
Alaska Department of Environmental Conservation
Alaska Department of Natural Resources
Alaska Electric and Light and Power Company
Alaska State Historical Library
City and Borough of Juneau
Northern Southeast Regional Aquaculture Association
United States Fish and Wildlife Service
United States Geological Survey
E - 4
TABLE OF CONTENTS
INTRODUCTION •
ENVIRONMENTAL SETTING.
Climate •
Topography.
Surficial Geology and Geophysical Conditions.
Soils.
Geophysical Hazards.
Land Use and Demography •
Land Development •
Population •
Floodplains and Flood Events.
Wetlands.
BOTANICAL RESOURCES.
WILDLIFE SPECIES •
FISHERIES.
Natural Fishery •
NSRAA Hatchery.
WATER QUALITY CHARACTERISTICS.
Salmon Creek Reservoir.
Salmon Creek.
WATER QUANTITY AND APPROPRIATIONS.
Salmon Creek Streamflow •
Water Appropriations.
CULTURAL RESOURCES •
Historical Setting.
Description of Tramway Route.
Survey of Cultural Resources •
Field survey •
Tramway.
Lower Powerhouse •
Hoist House Area •
Upper Powerhouse •
Flume.
ENVIRONMENTAL AND CULTURAL IMPACTS AND MITIGATION.
Vegetation.
Wildlife Resources.
Water Quality and Fisheries •
During Construction.
After Construction •
Salmon Creek Streamflow and Related Fisheries •
E - 5
Page
12
13
13
15
19
20
24
25
25
26
26
29
29
32
34
34
37
38
38
• 42
45
45
50
54
54
63
63
64
65
80
82
84
86
88
88
89
89
90
92
93
Cultural Resources.
REFERENCES
E 6
94
96
APPENDICES
A. Persons Contacted During Environmental Investigation
B. Note to Files --Salmon Creek Road-Pipeline
c. Alaska Gastineau Mining Company Streamflow and
Stream Height Records
D. Alaska Historical Library Photographs
E. Informant Data --Cultural Resources Survey
E - 7
Figure 1.
Figure 2.
Figure 3.
Figure 4.
Figure 5.
Figure 6.
Figure 7.
Figure 8.
Figure 9.
Figure 10.
Figure 11.
Figure l2A.
Figure 128.
Figure 13.
Figure 14.
LIST OF FIGURES
Mean monthly precipitation
measured in downtown Juneau for
the period of record 1898-1964 ••
Comparison of annual precipitation
in Upper Salmon Creek drainage and
downtown Juneau for the years
1912-1915 •••••••••
Topography of the proposed road-
pipeline alignment •••••••••
Salmon Creek drainage area
Surficial geology of Salmon Creek.
Zoning map •
Salmon Creek floodplain. . . .
Vegetation map for Salmon Creek
drainage between the Upper and Lower
Powerhouses. • • • • • • • • • • •
USGS water quality sampling sites
in Salmon Creek reservoir and
inflowing streams ••••••••• . . .
Mean water temperature near the mouth
of Salmon Creek for November, 1980
through October, 1981, compared with a
conjectural temperature curve ••••••
Monthly average streamflow measured
at the Salmon Creek Dam site for water
years ending September 30, 1911-1914
Monthly average streamflow diverted
through the flume for water years
ending September 30, 1914-1917 •••
Monthly average stream height measured
in Salmon Creek near the roundhouse,
representing undiverted flows •••
Tramway right-of-way, redrawn from 1914
Tramway map. • •••••••
Tramway construction, Alaska Historical
Library, Emile Gastonguay Collection ••
E -8
16
16
17
18
21
27
27
30
39
44
48
48
48
56
59
Figure 15. Map of Powerhouses, redrawn from 1914
flume and pipeline map . . . . . . . • . 60
Figure 16. Horse Tramway, Alaska Historical
Library, Emile Gastonguay Collection 59
Figure 17. Small locomotive, Alaska Historical
Library, Emile Gastonguay Collection 62
Figure 18. Lower Powerhouse and wharf, Alaska
Historical Library, Emile Gastonguay
Collection . . . . . . . . . . . 62
Figure 19. Lower section of the incline tramway
looking down (west). . . . • . . . 71
Figure 20. Incline tramway looking up (east). 71
Figure 21. Incline tramway looking up (east). . . . 71
Figure 22. Top of incline tramway . . . . . . . 71
Figure 23. Tramway map showing trestle numbers. 73
Figure 24. Moss-covered trestle with debris
below, T-32. . . . . . . . . 75
Figure 25. Debris below trestle, T-37 . • 75
Figure 26. Log trestle, T-6 . . . . . • . 75
Figure 27. Small log trestle, T-24. 75
Figure 28. High trestle bracing for T-7 . . . . • . 77
Figure 29. Bracing for T-26 . . . . 77
Figure 30. Bracing for T-14 . . . 77
Figure 31. Trestle-down T-18. . . . . . . . . 78
Figure 32. Trestle-down T-22. . . . . . 78
Figure 33. Trestle-down T-258 . . . 78
Figure 34. Cross-section of a rail. . 79
Figure 35. Slat rail clamp T-7. . . . . . . 81
Figure 36. Round rail clamp . . . . . . . . . 81
Figure 37. Example of guard rail. • . 81
E - 9
Figure 38.
Figure 39.
Figure 40.
Figure 41.
Figure 42.
Figure 4 3.
Figure 44.
Figure 45.
Figure 46.
Figure 47.
Figure 48.
Example of tie spacing on typical track. 81
Hoist house ••
Hoist drum and cable •
Part of the hoist motor control (in
hoist house) • • • • • •
Upper Powerhouse looking west, down
stream • • • • •
Upper Powerhouse headworks, tramway
spur on left, looking east from bridge
81
83
83
85
in Figure 42 • • • • • • • • • 85
Cribbing along creek, protects flume
area • • . . . . . . . . .
Looking west from flume, tramway
enters Upper Powerhouse clearing
in the center of the photograph.
Break in flume looking west.
Close-up of flume •••
Overflow flume discharge near the
hoist area • • • • • • • • • • • •
E -10
85
85
87
87
87
Table l.
Table 2.
Table 3.
Table 4.
Table 5.
Table 6.
Table 7.
Table 8.
Table 9.
Table 10.
Table 11
Table 12.
Table 13.
LIST OF TABLES
Average monthly mean, minimum and
maximum temperatures in the Juneau
vicinity, based on the years 1941-70
Average monthly minimum and maximum
temperatures recorded at the Salmon
Creek Dam and Upper Powerhouse from
July, 1911 to December, 1915 ••
Characteristics of the surficial
geology of Salmon Creek •••••
Wildlife species associated with the
coastal spruce-hemlock vegetation type
Salmon escapement counts in Salmon Creek
for 1940-80 ••••••••••••
Water quality of Salmon Creek reservoir
and inflowing streams •••••
Water quality of Salmon Creek.
Trace elements in water samples from
Salmon Creek • • • • • • • • • . .
Miscellaneous stream flow measurements
on Salmon Creek •••••••••••
Instantaneous discharge measurements
and stream heights recorded near the
mouth of Salmon Creek, 1980-1981 ••
Appropriation of Salmon Creek water.
Salmon Creek tramway trestles.
Length of Salmon Creek tramway • •
E -11
14
14
22
33
35
39
41
42
50
51
52
66
69
INTRODUCTION
Assessment of environmental, archaeological and cultural
resources in the Salmon Creek drainage system was conducted
to identify potential impacts associ a ted with the proposed
Salmon Creek road-pipeline construction and to recommend
mitigation.
included:
Specific objectives of the investigation
(1) Description of the environmental setting ·of the
Salmon Creek valley and road-pipeline.alignment.
(2) Description and mapping of botanical resources
and relevant terrain features which define wild-
life habitat and will be influenced during clear-
ing of the right-of-way.
(3) Establish potentials of wildlife uses in the Sal-
mon Creek watershed, and consider potential im-
pacts of the proposed development.
(4) Identify present conditions of water quality and
fishery resources in Salmon Creek and identify
potential impacts on these resources incurred
during and after construction.
(5) Evaluate available streamflow data for Salmon
Creek and address potential impacts on water
quality and use patterns.
(6) Identify, describe, photograph, and map sites of
cultural and historical significance along the
road-pipeline alignment through literature re-
E -12
search, field reconnaissance and informant data;
and evaluate potential for archaeological re-
sources in the project area.
(7) Recommend appropriate mitigation measures for
consideration during project design, evaluation,
and construction.
ENVIRONMENTAL SETTING
Climate
Juneau lies within the area of maritime climatic influence
which prevails ever Sou the as t Alaska. Low pressure systems
from the Gulf of Alaska typically produce overcast
conditions, abundant precipitation and moderate temperatures
in the vicinity. However,
generate clear skies and
several days at a time.
high pressures from Interior may
more extreme temperatures for
Rugged terrain, which creates
differential insulation and drainage patterns, exerts a
considerable influence over both temperature and precipation.
Local terrain features can cause distinct microclimates in
close proximity to one another.
Temperatures in the Juneau area are
climatic influences which limit
moderated
daily and
by marine
seasonal
temperature ranges. In Juneau, the average diurnal
temperature range is 6.3°C (43°F) in January and 8.9°C (48°F)
in July. On a seasonal basis, temperatures vary from a
monthly mean of -4.7°C (24°F) in January to 13.2°C (56°F) in
E -13
July. Temperature records for Juneau, collected by the u.s.
Department of Commerce (1979) from 1941 to 1970, are
summarized in Table 1.
Limited temperature data collected by the Alaska Gastineau
Mining Company in the upper Salmon Creek drainage indicate
that, with the exception of the summer months, mean daily
minima are generally warmer and maxima cooler than in the
City of Juneau. (Table 2).
TABLE 1. Average Monthly Mean, Minimum and Maximum Temperatures
in the Juneau Vicinity, Based on the Years 1941-1970
(USDC, 1979)
Mean j.£.£2.
Average Average
Month Minimum j£f]_ Maximum j.£.£2.
January -4.7 -7.9 -1.6
February -2.2 -5.5 1.1
March -0.1 -3.6 3.4
April 3.8 -0.4 8.1
May 8.2 3.4 13.0
June 11.8 6.9 16.7
July 13.2 8.7 17.6
August 12.4 7.9 16.8
September 9.6 5.7 13.4
October 5.4 2.4 8.4
November 0.3 -2.4 2.9
December -2.6 -5.3 0.0
Yearly Average 4.6 0.8 8.3
TABLE 2. Average Monthly Minimum and Maximum Temperatures
Recorded at the Salmon Creek Dam and Upper Powerhouse
from July, 1911, to December, 1915 (Alaska Gastineau
Mining Company Records, 1911-1915)
Month
January
February
Average
Minimum J0 £2.
-7.4
-3.5
E -14
Average
Maximum J 0 £2..
-3.8
0.1
March -3.1 2.6
April 0.3 6.5
May 3.8 13.6
June 6.5 16.7
July 7.9 18.9
August 7.1 15.6
September 5.4 11.5
October 2.9 5.8
November -2.8 1.1
December -4.0 -0.6
Yearly Average 1.1 7.3
Precipitation in the City of Juneau is lightest from February
to June, with an average monthly rainfall of 80 mm (3 in.)
during these months, and increases to a maximum of 325 mm (13
in.) in October (Figure 1}. Mean annual precipitation in
downtown Juneau is 2.31 mm (91 in.), (USGS, 1974). Alaska
Gastineau Mining Company's records of precipitation at the
Salmon Creek Dam and Upper Powerhouse indicate total yearly
precipitation in the upper Salmon Creek drainage is 15 to 35
percent greater than in downtown Juneau (Figure 2). Based on
this relation and a comparison to data from nearby Gold and
Sheep Creeks, annual rainfall in Salmon Creek is estimated at
2,540-3,810 mm (100-150 in.), (USGS, 1974).
Topography
Salmon Creek originates about 5. 6 km ( 3. 5 mi.) northeast of
Juneau and flows \vestwa rd for 8 km ( 5 mi.) before emptying
into the Gastineau Channel. The Salmon Creek drainage basin
ranges in elevation from sea level to 1,504 m (4,935 ft.) at
Observation Peak. Slopes within the basin range from 0 to
E -15
[I)
()) ..c:
\,)
0
1-1
FIGURE 1.
14
12
10
8
6
4
2 50
J F M A M J J A S 0 N D
Mean Monthly Precipitation Measured in Downtown
Juneau for the Period of Record 1898-1964 (USDC,
1979)
150
125
I ------i
Salmon Creek I I .._ ____ t I , ____ --
I 3000
I
I
100 I
I (jJ
(jJ
()) 75 ..c:
\,)
0
~
-----r I
I
1----I Downtown Juneau T
~
())
2000 +-l
()) e:
·r-1
r-i
r-i
50 ·r-1
::8
1000
25
65% 63% 79% 87% 85%
1912 1913 1914 1915 1916
FIGURE 2. Comparison of Annual Precipitation in Upper Salmon
Creek Drainage and Downtown Juneau for the Years
1912-1915 (Alaska Gastineau ~1ining Company Records,
1911-1915)
E -16
F
LOWER
POWERHQUSE
Elev. 30ft.
J
FIGURE 3. Topography of the proposed road-pipeline
alignment.
\
-CONTOUR INTERVAL 40ft. -
SCALE
r · = soo ft.
Compiled and Enlarged
from
U. S.G.S . 1: 24,000 Quadrangle
E -17
I
)
Total drainage are = 24.51 km 2 (9.46 mi 2 )
Subdrainages: 2 mi 2 ) ' t l . 11. 19 ( 4. 32 · Upper km2 .2) South Fork 3.68 km 2 ( 1. 42 ml.2 Lower 9.63 km ( 3. 72 mi )
FIGURE 4. Salmon Creek Drainage Area; Base USGS Juneau (B-2),
Alaska, 1:63 360 (1967).
E -18
over 39° (0 to over 80%) (Figure 3).
The Salmon Creek drainage basin was measured at 24.5 km2
(9.46 mi.2 ) from the USGS topographic map Juneau (8-2),
Alaska. For the purposes of this investigation, the basin is
subdivided into the upper drainage feeding Salmon Creek
Reservoir (4.3 mi. 2 ), the South Fork drainage (1.4 mi. 2 )
and the lower drainage (3. 7 mi. 2 ) (Figure 4). Larger size
estimates for the drainage areas have been reported in
previous publications and have included a more extensive area
near the mouth of Salmon Creek. Earliest estimates (Wilcox,
1917) may have been in error due to inaccurate base maps.
Salmon Creek Dam retains 21.7 hm 3 (17,585 acre-feet) water at
a spillway elevation of 357 m (1,171 ft.) (USGS, 19774),
although the water is seldom held at this high level. From
the spillway elevation, Salmon Creek falls 221 m (725 ft.) in
a distance of 1,364 m (4,477 ft.) (Thomson, 1919). The
stream course then becomes quite flat for a distance of
nearly 3.2 km (2 mi.) (Wollenberg, 1911). Upstream from the
remains of the Wagner diversion dam (0.7 mi. above the mouth)
is an alluvial flat caused by infilling. In the 1.1 km (0.7
mi.) below the Wagner dam, the stream falls about 70 m (230
ft.) to tidewater in a steep (5.7%), fast, turbulent flow
(Environaid, 1979). The stream flattens to form a 15 m-wide
(SO ft.) alluvial channel for a short distance before
entering the Gastineau Channel.
Surficial Geology and Geophysical Conditions
E -19
Soils
The surficial geology of Salmon Creek drainage was
characterized and mapped by Miller (1972) and ten major soil
associations were distinguished in the region (Figure 5,
Table 3). Exposed geologic units in the basin include
unconsolidated sediments and metamorphic rock.
Unconsolidated sediments
glacial, deltaic and
consist of mass-wasting, alluvial,
marine deposits (Miller, 1972).
Metamorphic rocks include primarily quartzite, schist, slate,
migmatic, phyllite and marble (Ford and Brew, 1973).
In the lower drainage, old deltaic deposits appear as loose,
sandy gravels interbedded with compact layers of marine
diamicton, in which fossilized shells are evident. Upvalley
from the deltaic deposits, late glacial-outwash deposits of
variable composition (primarily silty-sand to cobble-sized
soils of local bedrock material) wind around bedrock
outcrops. Soils are intergraded with colluvial material,
marine til and weathered greenschist, greenstone and granitic
bedrock. Rubble deposits and debris flows (along the
drainage slopes) generally originate in upslope colluvium and
bedrock zones and represent potentially unstable chutes.
An extensive rock slide-avalanche deposit is notable on the
north side of Salmon Creek near the present stream crossing.
Blocks of bedrock 1.5 m to 1.8 m (5-6 ft.) across cover the
surface for a distance of 610 m (2,000 ft.) at the slide
terminus. The deposit (now covered by the mature trees)
evidently came from a scarred area on the lower slopes of
E -20
bedrock
modern alluvium
rubble deposit
colluvium
SOIL TYPES
older delta deposits
debris flow
late glacial outwash
rockslide-avalanche
undifferentiated landslide
talus
FIGURE 5. Surficial Geology of Salmon Creek (from Miller, 1972),
E -21
TABLE 3.
Li:thology
Topographic
Form
Thickness
Characteristics of the Surficial Geology of Salmon Creek
(from Miller, 1972)
Modern Rubble
Bedrock Alluvium Deposits Colluvium Older Delta
Layered greenstone,
graywacke, slate,
greenschist
Steep slopes
Holocene
Vll.rTable;sand---x---~iigular -DroCKs--or---Variable -;--derl ved Deltaic fossfli-
pebble to gravel; locally derived from underlying and ferous silty &
slate, greenstone, slate, greenstone & nearby upslope clayey sandy gravel;
flow breccia & metavolcanics & deposits with compacted
granite granite boulders marine tills
Broad plliTiis ~----Along stream ---------r;ower slopes of most -To 500-ftelev:-on
point bars among channels hills evenly sloped
larger streams surfaces
Vll.riable; from a Tew Generally-less--tl.i9.I!-·variable to more than Variable to more
inches to several ft 20 ft 15 ft than 30 ft
Drainage Infiltration slow; Infiltration rapid; Excellent lnfiltra-Infiltration rapid; Infiltration rapid.
Erodabi 11 ty
surface runoff rapid runoff fair to poor tion & drainage runoff variable; in sand & gravel,
seeps common slow in till;
springs common
ResiStant-; b1.1t"ls Easily eroded by Eroded only by Easily eroded by
subject to weathering lateral scour from torrential runoff flowing water where
streams vegetation removed
Easily eroO:ed by
sheet wash & streams
Slope Goi:)(f-to excel1ent-;-Generally poor; Poor, especially in Poor to marginal; Nil
Stability except on steepest slumps likely in slopes of excava-slumping common
Physical
Properties
slopes cuts tions
Fractures parll.lle_l___ Generally loose and Rock fragments in· Loose; lies near
to & joint sets saturated point-to-point angle of repose on
perpendicular to contact; voids filled steeper slopes; low
strike of bedding partly by smaller density; generally
rocks weathered
Loose sandy-gravel
gravelly sand with
boulders, dense
marine till inter-
bedded
N
N
til
t<:l
N w
TABLE 3.
Map Symbol
Age
Lithology
Topographic
Form
Thickness
Drainage
Erodability
Slope
Stability
Physical
Properties
(Continued)
Debris Flow
fl
Clayey silty sand or
sand & sandy gravel
tatetliiiCial
Outwash
P-leistocene
Holocene
Rockslide
ra
Holocene
Silty-sand to pebble Rubbly debris.
& cobble; of green-including large
II
schist, greenstone & blocks of local rock
granitic rock types
tlndffferent:Iated
Landslide
Qsl
Holocene
Varfiiblelllix of rock,
soil and surficial
materials
Band of rubble, -To--6()(f ff elevation Along north slope . Along -north slope
bulbous to fan-shaped above Salmon Creek above Salmon Creek
Gimerally5t01(fft, Variable from 10 to -Less than20f_t ____ F_r_om a.~-tew ft to
locally !5 ft 100 ft mor~ t_h!IJ!_:lQ___ft_
Fdr to good; rntn=-1ntTrtrat1onraiJia;-· --uenerany~good-Infiltration good
tration generally runoff slow
slower than in parent
soil
Easily eroded by
flowing water
Gen-erally iiil.st:able
Generally dense &
firm deposits with
clayey silty sand
matrix
Easily -eroded by
streams
NoCeiislly eroded Highly variable
FII.Trto gooaTil ___ ----poor;exciiva t1orimay-Gerierally poor
slopes less than 350 change equilibrium
of deposit
Loose, vadabTe Large, unbr-oken-~ Loose arid porous
texture dense fragments
Talus
ta
Late Holocene
Variable; micaceous
greenschist, green-
stone & metavolcanics
Steep slopes; J()0-350
common
Variable; from a few
ft to more than 10 ft
Excellent in coarse
talus, poor in fines
Little~erosiori in
coarse talus,
moderate in fines
Very unstable
Loose angular
Blackerby Ridge.
Geophysical Hazards
Geophysical hazards within the urban Juneau area have been
identified for the City and Borough for comprehensive
planning and zoning purposes (DMJM, 1972). Five major
earthquake faults were identified within 160 km (100 mi.) of
Juneau, four of which are historically inactive. The
Fairweather-Queen Charlotte fault (100 mi. west of Juneau in
the Gulf of Alaska) has been the site of numerous quakes in
recent times. It is reasonable to assume that if Juneau
experienced an earthquake during seismic activity at this
site, the combination of steep slopes and loosely structured
soils in Salmon Creek would facilitate soil creep, slumping,
rock avalanches and landslides. The response of the Salmon
Creek Dam to a seismic occurrence has also been investigated
by the Corps of Engineers (USEPA, 1976}.
Faulting in the Salmon Creek drainage basin is limited to two
inferred strike faults with two major oblique faults south of
the basin (Sainsbury, 1953). Net displacement and relative
movement of the faults are unknown, but are expected to be
small.
A more pertinent geological hazard in the Salmon Creek
drainage is the potential for mass-wasting occurrences.
Evidence of active land movement is apparent in Salmon Creek
in the form of previous rockslides, debris and rubble slides,
and soil creep. Hazard classification systems applied in the
Juneau area have been based on (1) history of mass-wasting
E -24
occurrences, ( 2) presence of V-notched channels or gullies,
{l) slope gradient, and {4) area of extent affected by
landslide. Although maps of hazardous zones in Salmon Creek
have been developed (Miller, 1972; DMJM, 1972), they are not
available at a scale which is useful for evaluating the
specific project area.
Land Use And Demography
Land Development
All of the lands in the proposed project corridor are within
the Juneau Townsite El imi nation from the Tong ass National
Forest, administered by the U.S. Bureau of Land Management.
The City and Borough of Juneau zoning for· the lower portions
of Salmon Creek Valley is shown on Figure 6. The area is
zoned for residential, commercial, industrial and public
facilities development. In actuality, the zoning areas are
"open-ended" and extend up the drainage to the townsite
boundary; however, de facto application of zoning is
generally limited to the developable portions of the lower
drainage. The road-pipeline development proposed by AEL&P
Co. is consistent with the City and Borough's intent to zone
for industrial activity within the Salmon Creek area.
Existing land use along the road-pipeline alignment is all
related to AEL&P Co.'s hydroelectric generation activities.
Structures at the upper terminus include the Upper
Powerhouse, caretaker's residence, tailrace, inoperable flume
E -25
and headworks, and several utility buildings. At the lower
terminus, structures include the Lower Powerhouse, warehouse -.
and three four-room cottages which are used as AEL&P Co.
employee housing. Along the route, land development is
restricted to the historic development of the tramway, flume,
associated structures (all are inoperable), and a
transmission line which delivers power from the Upper Salmon
Creek Powerhouse to the AEL&P Co. transmission system.
Population
Juneau has experienced a dramatic population surge since
Statehood due to the great increase in government in the
State Capital. The 1960 census showed a population of 9,745
for the combined City and Borough, and the value ncreased to
13,556 at the 1970 count (City and Borough of Juneau, 1977).
Current population recorded during the 1980 census is 19,528
(USDC, 1981), up 44 percent since the previous decennial
census and double the 1960 count.
A 1975 population estimate for the Norway Point to Vanderbilt
Hill subregion, which includes the proposed development site
at Salmon Creek, was given as 393. Assuming a continually
increasing population in the Juneau area, a projected
population of 848 was estimated in the year 1995 for this
subregion (Homan Associates, 1974).
Floodplains and Flood Events
The u.s. Army Corps of Engineers, Alaska District, defined
floodplain and flood event estimates for the Salmon Creek fan
E -26
J.,
LAKE
.:-------:..-:.. ·:::.-=:. ==----=--.::.,.
GASTINEAU CHANNEL
Legend
RML Multi-Family Residential District (Low Density)
R7 Residential District
CWR Residential-Waterfront Commercial District
C Commercial
I Industrial
FIGURE 6. Zoning Map (City and Borough of Juneau, Planning
Department)
FIGURE 7. ·Salmon Creek Floodplain (from City and Borough of
Juneau, Planning Department)
E -27
between the beach and 430 m (1,400 ft.) upstream (Figure 7).
The Corps of Engineers estimates an Intermediate Regional
Flood (IRF) would discharge 3,200 cfs, with the water level
reaching an elevation of 7 m (23 ft.) above the Glacier
Highway Bridge, and 7.8 m (25.5 ft.) at a apoint 180M (600
ft.) upstream from the bridge. An IRF is a flood which,
based on statistical analysis of past hydrologic records, is
expected to occur once every 100 years, or which has the
probability of occurrence of 1 percent each year. Within the
defined floodplain, a 15 m (50 ft.) wide buffer on each side
of the stream is recommended for adequate flood protrection
(U.S. corps of Engineers, 1969).
The proposed road-pipeline alignment does not transect the
defined Salmon Creek floodplain, but does parallel the stream
for approximately 2.4 km (1.5 mi.) further upstream and
crosses Salmon Creek at two locations. There are no
estimates for h igh-wa te r levels or streamflows which would
occur at these upstream locations during an IRF. The
relatively steep slopes of the drainage walls should
effectively contain swelling waters.
Although the failure of the Salmon Creek Dam presents only a
remote possibility, such an occurrence (i.e., resulting from
seismic activity) would pose severe flooding danger for the
entire Salmon Creek Valley. The Corps of Engineers estimates
that if the dam failed, a 3.7 m (12 ft.) wall of water would
flow over the Glacier Highway for three minutes (U.S. Corps
of Engineers, 1969). No statistical probability of such an
E -28
event occurring has been estimated.
Wetlands
The proposed construction of a road and pipeline in the
Salmon Creek drainage does not involved any alteration of or
fill in the wetlands bordering Gastineau Channel. The U.S.
Army Corps of Engineers Alaska District, which is responsible
for permitting activities which affect Alaskan wetlands,
determined a permit was not required under Section 404 of the
Clean Water Act for the proposed project.
BOTANICAL RESOURCES
A survey of the vegetation along the proposed Salmon Creek
road-pipeline alignment ws conducted November 9-14, 1981, by
Steve Jacoby, a party to this investigation. Black.and white
aerial photography (scale 1 in. = 400 ft.) was acquired and
used for interpretation of vegetation types along the
existing tram route. Field time was spent verifying photo
interpretive work, inspecting forest condition, identifying
understory vegetation and field mapping topographic detail.
A road survey map prepared by Toner & Nordling, Registered
Engineers, Inc., was applied as the base map for the
vegetation mapping displayed in this text (Figure 8).
Coastal western hemlock-Sitka spruce (Tsuga heterophyll-Picea
sitchensis) forest makes up the overall vegetative cover of
the area within the approximate two-mile proposed road
corridor, and is found throughout the entire Salmon Creek
E -29
) "~~ ( " . ' ...:;;: _, i i "' Q) "' E 0 Q) V\.
....:• c
Q)
"' E
0 E .....
Cl) ..... 2 -:;; c
t )(A 2 0' :::> -~ 0 .'!! ..... .. -o w 0 0 Q) Q) ..... "'' "' -o Q) Q) !: "' Q) 0 ~ a. ..... 0 0 "' ..... -o ~ Q) c
Q) Ol ..2
-" :::> 0 .....
..... ...0 0
.....
E .Q..
0 0 ..... E
w _J <{ u (/) I I : ,... ..... 0 0 ("'') I ILl
drainage system.
The existing tram route alignment is completely forested by a
mixed age forest of old growth and even-aged second growth.
A even-aged second growth forest (approximately 65 years old)
of western hemlock-Sitka spruce exists along the tram route
between the Lower and Upper Powerhouse~. This second growth
condition is particularly evident on the south side of the·
tram and is influenced by early logging in conjunction with
construction activities in the upper Salmon Creek area and
with initial clearing for both the tram and flume. Old
growth residuals occur within the second growth forest and
influence forest canopy, age structure and understory
vegetation characteristics. Where clearing disturbances were
minimal, as on the north side of the tram, the second growth
forest is less .evident and old growth dominates.
Throughout the tram route, common understory plants of the
hemlock-spruce forest include devil's club (Oplopanax
horridus), salmonberry (Rubus
(Ribes bracteosum), blueberry
cranberry (Viburnum ebule).
spectabilis),
(Vaccinium .§.EE_.)
stink currant
and high-bush
Several small landslide sites along the tram route have
caused continual disturbances, promoting the establishment of
red alder (Alnus rubra) and native grasses. Red alde.r is
also found in rna ture form, commonly mixed with hemlock and
spruce, along the first quarter mile of the tram route.
The vegetation immediately around the Upper Powerhouse site
is influenced by clearing at the time of initial construction
E -31
of power facilities. There remains today approximately two
acres of clearing in the vicinity of the powerhouse turbine
facility, tailraces, flume intake, caretaker's residence and
several utility buildings. Ground vegetation is primarily
grasses, salmonberry and high-bush cranberry, along with
young growth western hemlock and Sitka spruce.
WILDLIFE SPECIES
The Salmon Creek drainage provides habitat for wildlife
species which commonly occur in a spruce-hemlock vegetation
type. A list of species associated with this habitat type is
provided in Table 4, although no formal wildlife surveys have
been conducted in the area.
Primary species which are likely to occur in the Salmon Creek
drainage include black bear (Ursus americanus), porcupine
(Erethizon dorsatum), red squirrel (Tamiasciurus hudsonicus),
and other small mammals, blue grouse (Dendragapus obscurus),
ptarmigan (Lagopus spp.) and migratory waterfowl (personal
communication, Dave Zimmerman, Alaska Department of Fish and
Game). Moutain goats (Oreamnos amedcanus) move into the
drainage from the surrounding ridges during winter, and Sitka
black-tailed deer (Odocoileus hemionus sitkensis) and
wolverine (Gulo luscus) probably occur occasionally.
Lazzette Ohman (Salmon Creek area resident, 1923-1937)
recalls seeing very few deer in the vicinity.
With the exception of bald eagles, there are no reported rare
or endangered animal species or critical habitat types within
E -32
TABLE 4·. Wildlife Species Associated with the Coastal Spruce-
Hemlock Vegetation Type (from City and Borough of
Juneau, 197lf')
MAMMALS(l)
Masked shrew
Dusky shrew
Keen myotis bat
Silver-haired bat
Little brown bat
Red squirrel
Northern flying squirrel
Deer mouse
Northern bog lemming
Red-backed vole
Meadow vole
Long-tailed vole
Mountain goat
.!ll.!Y2.§. ( 2 )
Great blue heron
Goshawk
Sharp-shinned hawk
Red-tailed hawk
Rough-legged hawk
Golden eagle
Bald eagle
Peregrine falcon
Merlin
American kestrel
Blue grouse
Willow ptarmigan
Rock ptarmigan
Solitary sandpiper
Band-tailed pigeon
Mourning dove
Screech owl
Great horned owl
Hawk owl
Great gray owl
Pygmy owl
Boreal owl
Saw-whet owl
Common flicker
Yellow-bellied sapsucker
Black swift
Vau.x's swift
Hairy woodpecker
Downy woodpecker
Hammond's flycatcher
Northern three-toed
woodpecker
Alder flycatcher
Western flycatcher
Western wood pewee
Olive-sided flycatcher
all Swallow species
Gray jay
Steller's jay
Black-billed magpie
Common raven
Northwestern crow
Bushy-tailed wood rat
Porcupine
Coyote
Gray wolf
Black bear
Brown bear
Marten
Short-tailed weasel
Least weasel
Wolverine
Lynx
Sitka bl.ack-tailed deer
Black-capped chickadee
Chestnut-backed chickadee
Red-breasted nuthatch
Brown creeper
Winter wren
American robin
Varied thrush
Hermit thrush
Swainson's thrush
Gray-checked thrush
Golden-crowned kinglet
Ruby-crowned kinglet
Bohemian waxwing
Northern shrike
Starling
Warbling vireo
Orange-crowned warbler
Yellow warbler
Yellow-rumped warbler
Townsend's warbler
Northern water thrush
MacGillvray's warbler
Wilson's warbler
American redstart
Rusty blackbird
Pine grosbeak
Gray-crowned rosy finch
Hoary redpoll
Common redpoll
Pine siskin
Red crossbill
White-winged crossbill
Dark-eyed junco
Tree sparrow
Chipping sparrow
Harris' sparrow
White-crowned sparrow
Golden-crowned sparrow
Fox sparrow
Lincoln's sparrow
Song sparrow
{1) Edited by S. Forrest Blau, Habitat Biologist, Alaska Department
of Fish and Game, September, 1978.
{2) U.S. Forest Service and Alaska Department of Fish and Game,
1973. Birds of Southeast Alaska -A Checklist.
E -33
the project area (USEPA, 1976). There are no identified
eagle nesting sites in the vicinity (personal communication,
Phil Schempf, u.s. Fish and Wildlife Service); however, bald
eagles feed on pink and chum salmon at the mouth of Salmon
Creek during the late-summer runs.
FISHERIES
Natural Fishery
Salmon Creek supports anad romous chum (Onco rphynchus keta) ,
pink (.Q_. gorbuscha), and coho salmon (.Q_. kisutch) and Dolly
Varden (Sal vel i nus malma) in the short sect ion below the 6 m
( 20 Ft.) falls near the mouth; and Dolly Varden and brook
trout (~. fontinalis) in the reservoir. Resident fish are
reported in Salmon Creek between the falls and reserve i r.
Below the falls, a 15 m (50 ft.) wide spawning reach contains
good bank cover and a sand and gravel streambed sui table for
spawning. Escapement counts of pink and chum salmon are
available for the years 1940-1980 (Table 5). Prior to 1960,
chum escapement typically exceeded 1,000 to 1,500 fish and
the chum run was the dominant salmon run in Salmon Creek.
Since 1960, chum escapement counts have declined and the pink
run has become dominant. Based on stream observations in
1980 and a weir count for part of the 1981 season, NSRAA
personnel estimate the natural chum run (beginning July 15)
numbered approximately 150 in 1980 and 375 in 1981.
run (beginning August 1) numbered approximately
E -34
The pink
3,000 to
TABLE 5. Escapement Counts in Salmon Creek for 1940-1980
(Reed and Armstrong, 1972; ADF7G, Comm~ Fish, 1981).
"P" indicates species present, * indicates inter-
tidal count included.
Fish Observed Length o!
~ .....~?.!.!!!_ Chum ~ Surve;)::(mi)
1940 9-21 p p
1951 7-20 150 0.2
8-08 400 0.2
8-18 1470 500 0.2
1952 8-02 p 0.2
1953 8-01 p 0 ·0.2
8-24 p 0 0.2
8-28 p 0 0.2
1954 7-20 150
8-17 1000
1955 8-19 2500 2.0
1957 7-20 1500 0.5
9-10 2500
1958 8-22 1000 225
1959 8-05 1500 0.2
1960 8-12 1175 30 0.6
9-01 320 600 Length
1961 7-25 500 Length
1962 8-17 269 99 Length
1963 8-08 325 Length
1964 9-04 32 365 Length
1965 8-18 200 Length
1967 8-11 150 20 Length
8-30 300 0.2
1968 8-12 80 730* Length
8-14 2400* Length
1969 8-12 70 280 Length
8-28 8 347 Length
1971 8-27 70 108 Length
1972 8-01 170 Length
8-11 50 Length
9-08 211 Length
1973 8-08 172 437 Length
1974 8-14 20 150 Tidal
1975 8-08 60 115 Length
8-21 105 285 Length
1976 7-29 85 0.3
8-03 168 50 0.2
8-17 44 0.2
10-27 (25 coho) 0.3
1977 7-22 38 Length
8-03 475 630 1.0
8-04 40* 825* 0.7
8-10 130 2300 Length
1978 7-27 73* 0.2
8-03 74 0.1
8-17 22 472* 0.3
1979 7-23 61 19* 1.0
8-07 3589* 0.2
8-21 3760* 0.5
1980 7-25 36 ( 1 coho) 0.7
8-20 300* 0.1
8-21 l4 496* 0.5
E -35
4,000 in 1980 and 6,000 in 1981.
Coho salmon are occasionally· observed during escapement
counts in Salmon Creek but there is not a significant
spawning run in the stream.
Dolly Varden spawning in lower Salmon Creek is presumed to be
limited (personal communication, Dick Marriott, ADF&G).
Dollys which spawn in nearby systems typically "nose into"
Salmon Creek\for several weeks at a time while ranging widely
in local saltwaters each summer. Dollys cou1d be expected to
occur in Salmon Creek from July into early September.
Reed and Armstrong (1972) evaluated the overall rearing
potential of lower Salmon Creek as poor. Limited rearing
areas include two large pools just below the falls, a smaller
pool behind a log jam further downstream, and some undercut
banks areas. A survey of potential rearing areas in 1970
revealed an anadromous Dolly Varden population (lengths
103-145 mm, age 2 years).
The Salmon Creek Reservoir supports a small natural
population of Dolly Varden and a successfully planted stock
of brook trout. The trout population originated from a plant
of 13,150 fish in 1927 (Wadman, 1962) and has maintained a
healthy population of a few thousand fish (personal
communication, Dick Marriott, ADF&G). Alaska Department of
Fish and Game monitors the trout population periodically, but
is not involved in stock enhancement. However, an
examination of fish by ADF&G several years ago indicated that
the condition class was good and growth rates normal
E -36
(Envi ronaid, 1979).
fishery for anglers.
NSRAA Hatchery
The reservoir provides a good local
Northern Southeast Regional Aquaculture Association has
operated a private-nonprofit hatchery for churn, pink and coho
salmon near the mouth of Salmon Creek since 1980. A coho
rearing facility will begin oepration at Twin Lakes, just
north of the mouth of Salmon Creek, in late 1981. Operations
water for both facilities is withdrawn from Salmon Creek.
The following information was provided by Greg Young, NSRAA
Salmon Creek Hatchery.
Salmon Creek Hatchery incubated and released 1.3 million churn
and 100,000 pink salmon in 1980. Stocks increased. to 3.5
million churn and 2.25 million pinks in 1981, and NSRAA plans
to maintain this level for three more seasons. The hatchery
is currently permitted to incubate a combined churn and pink
stock of 6 million eggs. Application has been made to
increase incubation to 40 million pink and churn eggs, with
20-40 million fish reared for short periods of time.
The coho salmon program began in 1981 with 150-200,000 eggs.
NSRAA plans to increase coho incubation to 150-300,000 eggs
within 3 years. The permitted levels of 800,000 coho eggs
and 500,000 srnolt should be achieved with 6 to 9 years. Coho
will be reared in vertical raceways at the Twin Lakes
facility for about a year before their release.
At the levels proposed for incubation and rearing, the Salmon
E -37
Creek hatchery and Twin Lakes rearing facility would produce
annual runs of 400,000 returning chum and pinks, and 50,000
coho.
WATER QUALITY CHARACTERISTICS
Salmon Creek f1 ow is classified by the Alaska Department of
Environmental Conversation (DEC) as suitable for all
potential freshwater uses, including (1) water supply for
drinking and food processing, agriculture,
industrial uses, (2) water recreation, and
aquaculture
( 3) growth
and
and
propagation of fish, shellfish, other aquatic life and
wildlife including waterfowl and fur-bearers (ADEC, 1979).
Salmon Creek Reservoir
Water quality sampling sites established in the reservoir and
at two inflowing streams by USGS (Figure 9) were monitored
for seasonal changes in water quality (USGS, 1974).
Temperature profiles were obtained at each site in the
reservoir and chemical, bacteriological and dissolved oxygen
analyses conducted (Table 6).
Temperature profiles for the reservoir in late-summer and
late-winter indicate surface temperatures are higher than
near-bottom temperatures in summer and are lower in winter.
A distinct summer thermocline was not detected, perhaps due
to the continual mixing resulting from surface wind action.
The water in Salmon Creek reservoir and inflowing streams is
E -38
TABLE 6. Water Quality of Salmon Creek Reservoir and Inflowing Streams
(from USGS, 1974). Concentrations in mgjl.
Ia"""'-s-.1• i!IT:~!!92 loti-Coadlaeil•:l.tr
_!!!!,_ !!!!!! !! !!! £! !I ~ ! !!2!!:1 £!13 !i!4 £! n ft'ltnt• !!!! !!! Total £!!:!! iu.Da•! 2!! Color
--12 I 10.5 1.3 0 5.2 0.1 0.1 0.1 17 0 4.1 0.2 O.l. .02 10.5 22 18 2 40 7.2 0
II t.O 1.4 0 8.2 .8 .. .I 15 0 4.5 .2 .1 .OS 10.1 21 18 I 31 7.1 0
18 1.0 1.5 .010 5.4 ·.8 .• 1.0 14 0 ••• .2 .1 .OS u.o 21 18 5 38 1.1 0
110 1.0 1.1 0 8.2 .I • 4 .. 18 0 5.4 .2 0 .09 11.5 24 11 5 40 7.2 0
11-7-12 0 -1.1 .OliO 0 8.2 .. .II .. 22 0 I. 1 .4 0 .01 21 11 0 .. 1.0
3-20-73 1 o.o 2.1 .009 0 1.0 .. .8 .. 11 0 8.2 .• 0 .17 13 21 20 5 •• 7.1 0
10 0.0 2.0 .020 0 7.2 .. .8 .9 21 0 8.8 .1 0 .11 14 30 21 4 51 7.8 ' 24.5 .5 2.2 .009 0 T.t ,1 .8 1.0 25 0 1.1 •• 0 .15 1 34 23 2 58 1.0 0
8 3-20-73 1 o.o 2.0 • 009 0 ••• .I .I .. 1t 0 a.T .• 0 .II 13 27 11 4 41 1. 3 0
:10 .5 1.1 .020 0 1.0 .7 .5 .I 21 0 1.0 .3 0 .13 12 21 20 3 •• 7.5 0
53.5 1.0 l. 7 .001 0 1.8 .7 .s .. 20 0 e.o .3 0 .13 11 21 Ul 3 47 7.5 5
111 0.0 1.1 .020 0 7.1 ·' .4 .. 28 0 1.2 .a o .13 13 31 11 0 so ,,, 0
e --Tll 1110 s.o 2.1 0 1.0 .1 .a .. 18 0 5.4 .1 0 • 14 10.1 24 II 5 .. 7.1 5
c 5-20-13 1 o.o 2.0 .040 0 7.1 .. •• 1.0 21 0 1.2 .1 0 .14 u :Ill 21 4 50 7.1
10 •• 1.1 .001 0 7.4 .1 .a .. I! 0 1.3 .a o .14 13 ,. 11 4 51 7.2 ••• 1.0 1.8 .040 0 1.8 .1 .a .. 21 0 1.1 .1 0 .11 12 21 10 3 41 7.2
D -.n I 10.0 1.8 • ou 8.1 .8 .5 .. 10 0 4.8 .2 .1 .02 10.3 211 II I tt 7.3
11 7.0 1.3 .010 4.8 .. .4 .. 14 0 4.3 .I .1 .Oil 10.1 20 14 3 31 7.1
1211 a.o 1.7 .020 1.0 .1 .a t.o 11 0 8.1 .1 0 .14 11 14 11 s 43 1.0
D 11-7-11 0 -1.7 .040 0 1.2 .. .1 .I If 0 a.e ·• ·o .1111 28 11 2 .. T.t ., 5-22-12 10 -2.1 .040.8.1 •• 1.0 .. 10 0 1.5 .4 0 .UI 21 n 51 ••• 0
48 .010 1.7 • 1 .I .. 21 20 50 1.7
0, 5-22-11 10 .040 e.e .I 1.2 .I 20 0 n l 53 e.t
21 .020 e.l .1 1.2 .I , 0 ..:. Jl. 3 51 8.1
1-4-12 -1.1 8.o .1 •• 1.0 18 0 4.1 .2 .1 24 18 42 7.1 0
11·1·11 -2.5 .070 0 7.3 .. •• 1.0 21 0 8.5 •• 0 .01 31 D .. 1.0 0
11-7-12 -••• .oio 0 l.ll .. .1 .. 11 0 ••• • 7 0 .n .. IS 0 31 1.2
600 1200 FEET
I 00 2 00 300 METRES
FIGURE 9. USGS (1974) Water Quality Sampling Sites in Salmon
Creek Reservoir and Inflowing Streams
E 39
basically a calc i urn bicarbonate type of excellent quality
(USGS, 197 4) and meets the requirements for freshwater uses
(including domestic) recommended by the State of Alaska
(ADEC, 1979; USEPA, 1976). Reservoir water supports a viable
stock of brook trout and Dolly Varden within the impoundment,
and provides for successful growth and propagation of wild
and hatchery fish stocks downstream. The City and Borough of
Juneau plans to implement a water quality sampling program in
the reservoir in 1982 to supplement available water quality
data (personal communication, George Porter, Department of
Engineering, City and Borough of Juneau.
Bacteriological samples collected from the reservoir by the
USGS (1974) showed 0.0 bacterial count for 88 percent of the
samples and 2.2 .organisms per 100 ml in the remaining 12
percent. The presence of more than one coliform bacteria per
100 ml in several samples would require further check
sampling if the reservoir is to supply drinking water (ADECm
1978).
Dissolved oxygen levels in Salmon Creek reservoir ranged from
7 to 14 mg/1 during USGS (1974) sampling indicating that a
condition exists which contributes to the elimination of
organic impurities in impoundment waters. Although the
reservoir site was not cleared prior to filling in 1915,
annual fluctuations of reservoir storage has helped to
eliminate accumulation of impurities from organic
decomposition.
E -40
TABLE 7. Water Quality of Salmon Creek (from USGS, 1969; 1974)
Concentrations (mg/1)
Sample Temp
~ Date (°C) Si02 ~ Mo Ca MK Na ! HC0 3 ~ so4. Cl !
3 2-22-73 2.0 2.5 0.02 0 8.8 0.9 0.6 0.8 30 0 5.9 1.5 0
4 8-29-50 2.0 0.20 -9.0 1.5 21 -12.0 0.1
4 11-22-66 1.1 2.0 0.04 -7.2 1.2 20 6.7 1.4
4 3-15-68 1.5 2.9 9.2· 0.9 0.6 0.7 28 0 5.0 0.7 0.1
4 6-26-68 6.0 2.2 6.6 0.7 0.5 0.6 24 0 4.6 0.2 0
4 2-22-73 2.0 2.9 0.04 0 9.0 0.7 0.8 0.7 32 0 4.8 1.8 0
Hardness
Sample Non-Conductivity
Site ~ Nitrate DO OS~ Carb (umhos2 E.!! Color
3 2-22-73 0.22 14 37 26 1 60 7.0 1
4 8-29-50 -44 29 12 68 7.3
4 11-22-66 0.10 -30 23 7 48 7.4
4 3-15-68 -35 27 4 60 7.1 5
4 6-26-68 -28 20 50 6.8 5
4 2-22-73 0.14 13 37 25 0 61 6.8 2
E -41
Salmon Creek
The quality of water collected by USGS (1969: 1974} near the
Upper Powerhouse (sample site 3} and at the mouth of Salmon
Creek (sample site 4} is similar to reservoir water quality
and is within standards established by DEC for all freshwater
uses. Water chemistry data for Salmon Creek is presented in
Table 7.
Trace element levels detected in Salmon Creek water are
presented in Table 8. Silver, antimony, arsenic, cadmium,
lead and molybdenum levels are low and are within standards
set for aquatic life criteria and domestic use by DEC (1979}
and USEPA (1976, l980a-d}.
When compared to general freshwater aquatic life criteria
established by the USEPA (1976; 1980e), levels of copper
(.002-.005 mg/1} and zinc (,018, .050 mg/1} border on the
edge of concern for physiological effects. However, the
healthy condition of propagating wild and hatchery stocks of
pink and chum salmon indicate naturally occurring copper and
zinc levels are probably not detrimental to aquatic organisms
in Salmon Creek.
TABLE 8. Trace Elements in Water Samples from Salmon Creek
(USGS, 1974; Environaid, 1979)
Sample Metal Concentrations (mg/ 1)
Site Date ~ An As Cd Cn Mo Pb Zn
3 2-22-73 0 .005 .002
4 2-22-73 .003 .004 0
4 3-22-73 .006 .002 .003
4 6--79 <.002 0.12 <.005 <. 002 .004 .05 <.010 .018
4 11--79 .050
E -42
A continuous record of water temperature for Salmon Creek
exists only for the year November, 1980, through October,
1981 (NSRAA, Stream Data Log, 1980-81). Mean monthly
temperatures for this period (Figure lOA) range from 1. 43°C
(34.6°F) in December, 1980, to 9.77°C (49.6°F) in August,
1981. However, mild winter temperatures experienced in the
Juneau vicinity in 1980-81 likely caused water temperatures
to be uncharacteristically high between November and April.
A conjectural annual water temperature curve developed for
Salmon Creek by Environaid (1979), is shown in Figure lOB.
The curve is based on records for Cabin Creek (1952-53), Deer
Mountain Hatchery (1975-76) and Beaver Falls Hatchery
(1975-76) and indicates a probable seasonal range of 0°C
(32°F) in winter to 10°C (50°F) in summer. Needle ice may
occur from chilling of turbulent waters during the winter.
A bacteriological sample collected from near the mouth of
Salmon Creek in October, 1979, and analyzed by the Alaska
Department of Fish and Game Fish Pathology Laboratory showed
a total coliform count of 50 colonies/lOOrnl and a fecal
coliform count of 0 colonies/100 ml (Environaid, 1979) .This
result concurs with the USGS (1974) observation that Salmon
Creek water showed higher coliform counts than reservoir
water. Salmon Creek water is within the maximum requirement
of 20 FC/100 ml set for most freshwater uses (ADEC, 1979),
but would regui re further checking before use as a drinking
water source (ADEC, 1978).
E -43
10
9 -I C,) 8 I 0
'-' I
7 I Q) I ~ I ;:I
6 I +-I
CIS
' A
I
~ I
Q) 5 ' I 0. \ I s \ I Q) 4 ' ... E-< \ .... .... .... ~ 3 \ /
Q) ' / ........ ;/
+-I ... ,..,
CIS 2 ' ill:
1
N D J F M A M J J A s 0
FIGURE 10. Mean Water Temperature Near the Mouth of Salmon Creek
for November, 1980, through 1981 (A) Compared with a
Conjectural Temperature Curve (B)
E -44
Salmon Creek carries a significant natural suspended sediment
load composed of silt to sand-sized fractions derived from
the streambed and from sediments introduced from eroding
streambanks and landslides. Suspended sediment
concentrations are particularly elevated
rainstorms and resulting high velocity flows.
(3.25 in.) rainfall on October 8-10, 1979, was
during fall
An 8. 25 em
observed to
produce eleva ted turbidity and sediment loads in the stream
(Envi ronaid, 1979). Although the sediment load has not been
quantified nor size-classes determined, NSRAA personnel
attest to the significant load of silt and sand-sized
particles which are suspended in the water withdrawn from
Salmon Creek for hatchery operations
WATER QUANTITY AND APPROPRIATIONS
Salmon Creek Streamflow
No continuous historical record of streamflow exists for the
Salmon Creek drainage; data which are
recorded under varying conditions
waters. The
available have
of impoundment
Alaska Department
been
and
of diversion of drainage
Natural Resources (DNR) has asked the Division of Geological
and Geophysical Surveys (DGGS) to collect current stream
guage data beginning in spring of 1982. For the purposes of
this investigation, available records of streamflow have been
compiled and summarized.
Because runoff data for Salmon Creek has not been
E -45
consistently collected, the USGS ( 19 7 4) estimated flow from
the upper drainage by analogy to Gold and Sheep Creeks, which
share the same hydrologic setting as Salmon Creek. By
applying this method to records from 1950-1970, the estimated
annual flow generated in the upper subdrainage of Salmon
Creek was calculated as 33,800 acre-feet, or 46.8 cfs
averaged annual flow.
This daily flow estimate compares well with limited
historical records of streamflow measurements taken at the
Salmon Creek dam site in 1911-1914, prior to dam completion
(Figure 11). Averaged annual flows of 56.7 cfs and 62.3 cfs
are given for 1912 and 1913, respectively. On a seasonal
basis from 1911 to 1914, flow from the upper subdrainage
varied from an average of 14.0 cfs for the winter months
(December-March) to 108.1 cfs during summer (June-September).
In the early years of operation, Alaska Gastineau Mining
Company recorded flow values of water shunted through the
flume and penstock to the Lower Powerhouse facility. Figure
12A illustrates flow measurements taken "in the flume near
the penstock" just below the headworks at the Upper
Powerhouse in the years 1914-1917 (Wilcox, 1917). The flow
included combined runoff from the upper drainage and 80
percent of the South Fork drainage. Since measurements were
taken in the flume, they represented all the water diverted
from Salmon Creek for power generation at the Lower
Powerhouse. Average annual flows of 100.0 cfs, 80.4 cfs and
81.5 cfs were diverted during the years 1914-1916,
E -46
respectively. Flows diverted through the flume (Figure 12A)
averaged 150 cfs in summer and 23 cfs in winter, compared
with the 110 cfs summer flow and 40-50 cfs winter flow,
anticipated to be carried in the proposed pipeline. Several
low flow values measured in winter in the flume are much
smaller than flows used by the Lower Powerhouse turbine (ie.
March, 1916; January, March, 1917). Examination of climatic
records for 1916 and 1917 gave no explanation for these low
values.
Concurrent with the above records,
Company measured stream height in
Alaska Gastineau Mining
"Salmon Creek near the
Roundhouse", below the point of flume diversion. Records for
1914-1916 represent water which was not diverted into the
flume, but continued down the natural Salmon Creek drainage
to the mouth (Figure 12B). This documentation was necessary
in those years to demonstrate that sufficient water remained
in the stream for use by the Wagner mining operation, 1.1 km
(0. 7 mi.) upstream from the mouth of Salmon Creek (personal
communication, David Stone, AEL&P.). Undiverted water
included the entire North Fork flow and 20 percent of South
Fork water. Unfortunately, streamflow ratings are not
available for the stream height values recorded at this
location in Salmon Creek. Nevertheless, it is apparent that
water in the upper Salmon Creek channel was routinely drawn
down to less than 2.5 em (1 in.) depth during the winter
months under diverson practices illustrated in Figure 12A.
Between 1963 and 1973, USGS (1974) collected miscellaneous
E -47
20.0
17.5
150 .-.
Ul ....
<:) 125
~ ..... .... e
ell
Ql
"' 75 ...
a2
50
25
M J J J
l9ll 1-9!2 1fl13 191'4
FIGURE 11. Monthly Average Streamflow (cfs) Measured at the
Salmon Creek Dam Site for Water Years Ending
September 30, 1911-1914 (Wilcox, 1917)
2l!O 50
50
I
I
I
I
I
I
I I
I I
I ! • r
I I -' ' t-_,_r
' ~..,
I
I
: f"\--,
I I I
I t :
L! ;
,__.._~
0 N P J F Y A Y J J A S 0 N 0 J F Y A'M J J A S 0 N D J F Y A H J J A S 0 N D J F I
1914 1915 1911! 11917
40
...
30 f.
10
.... .. ..
FIGURE 12 A. Monthly Average Streamflow (cfs) Diverted Through
the Flume for Water Years Ending September 30, 1914-
1917 (Wilcox, 1917)
B. Monthly Average Streamheight (in) Measured in
"Salmon Creek Near Roundhouse," Representing
Undiverted Flows (Gastineau Mining Company Records,
1914-1916) --------
E -48
discharge measurements on Salmon Creek which gave an
indication of undiverted runoff at certain times of year
(Table 9). Nearly all measurements were taken near the mouth
of the stream and may or may not include spillage from the
reservoir or from the deteriorating flume. On February 28,
197 3, two measurements were made on Salmon Creek when flume
·leakage was considered neg 1 ig i ble due to icing and there was
no spillage from the reservoir. Near the Upper Powerhouse
undiverted streamflow was 6.9 cfs; near the mouth a discharge
of 24.1 cfs was measured, indicating a gain of 17 cfs from
tri bu tad es entering Salmon Creek in the lower subd ra i nage.
This value is the single recorded datum which assesses the
separate contribution of the lower subdrainage tributaries to
the total runoff of Salmon Creek. Lower subdrainage runoff
will be the primary component of flows available to water
users at the lower reaches of Salmon Creek during total, or
near total, divers ion of upper subdra in age and South Fork
water.
The lower Salmon Creek subdrainage, excluding both the Salmon
Creek reservoir and South Fork drainage areas, totals about
2 . 2) 9.6 km (3.7 m1. • During periods of winter drought
(January-March) this subdrainage will approach low flows of 0
to 2.0 cfs, based on analogy to flows measured in nearby Gold
and Fish Creeks. The lowest flow measured in lower Salmon
Creek (at 5,500 ft. above mouth, on January 13, 1969) was 1.4
cfs. On the same date, Gold Creek's mean daily flow ws 3.5
cfs and Fish Creek's (on Douglas Island) was 4. 7 cfs. Low
E -49
flows of record for Gold Creek and Fish Creek are 0 cfs and
1.0 cfs, respectively.
TABLE 9. Miscellaneous Streamflow Measurements on Salmon Creek
(USGS , 1 9 7 4)
Streamflow
Date Location (cfs)
9-4-63 50 ft. upstream from mouth 27.7
9-10-63 50 ft. upstream from mouth 77.9
9-12-63 200 ft. upstream from mouth 197.0
9-13-:-63 200 ft. upstream from mouth 139.0
3-15-63 200 ft. upstream from mouth 22.1
6-26-68 200 ft. upstream from mouth 120.0
8-22-68 150 ft. upstream from mouth 14.8
1-13-69 5,500 ft. upstream from mouth 1.4
2-2 3-7 3 500 ft. upstream from mouth 24.1
2-23-73 25 ft. below bridge at
Upper Powerhouse 6.9
A log of instantaneous discharge measurements for Salmon
Creek, measured weekly, has been kept at the NSRAA hatchery
for the years 1980 and 1981 (Table 10). Flow measurements
represent total Salmon Creek runoff without diversion of
water from the channel. The lowest recorded winter value was
36.6 cfs on December 26, 1980. It is presumed that the
majority, if not all, of this flow represents water released
through single-turbine operation from the tailrace of the
Upper Powerhouse; this also indicates that flows contributed
to Salmon Creek from the lower subdrainage during cold winter
droughts may be very low. With respect to the resident trout
fishing in Salmon Creek below the Upper Power House, the pro-
posed project will alter the winter streamflow characteris-
tics of the Lower Salmon Creek Basin compared to those which
have been in existence since 1972. With the installation of
the pipeline from the Upper Salmon Creek Power House to the
E --50
TABLE 10. Instantaneous Discharge Measurements and Stream Heights
Recorded Near the Uouth of Salmon Creek (NSRAA Stream
Data Log, 1980-81)
Discharge Stream
Date (cfs) Height (ft)
10-26-80 101.0 2.32
11-1-80 86.8 2.26
11-21-80 95.7 2.28
11-28-80 125.7 2.44
12-2-80 54.9 2.00
12-12-80 42.0 l. 89
12-26-80 36.6 l. 85
1-10-81 73.3 2.22
l-19-81 130.0 2.46
1-26-81 98.9 2.32
2-2-81 88.2 2.26
2-9-81 49.8 2.20
2-16-81 84.2 2.24
2-23-81 51.1 2.08
3-2-81 85.9 2.24
3-9-81 94.0 2.26
3-16-81 102.5 2.32
3-23-81 94.0 2.28
3-30-81 90.0 2.28
4-6-81 84.8 2.26
4-13-81 84.3 2.22
4-20-81 91.6 2.26
4-27-81 83.8 2.20
5-4-81 78.1 2.18
5-11-81 90.1 2.26
5-18-81 71.2 2.16
5-26-81 130.4 2.48
6-1-81: 130.5 2.54
6-8-81 48.5 2.05
6-15-81 38.5 1. 92
6--81 116.6 2.44
7-13-81 103.2 2.38
7-27-81 150.8 2.50
8-3-81 218.1 2.60
9-1-81 22.8 l. 72
E -51
to such conditions will not affect it materially.
Water Appropriations
Salmon Creek waters are currently serving four major
purposes: (1) development of hydroelectric power at AEL&P
Co. facilities, (2) provision of limited public water supply
for the City and Borough of Juneau, ( 3) provision of an
operations water supply for the NSRAA hatchery facilities
near the mouth of Salmon Creek and in the Twin Lakes area,
and ( 4) rna i ntenance of natural anadromous fishery habitat in
the lower reaches of Salmon Creek.
In accordance with the Alaska Water Use Act of 1966 (Alaska
Statutes 46.15.101-270}, the Alaska Department of Natural
Resources (DNR} is responsible for appropriating and
adjudicating rights to the use of Salmon Creek's water.
Total consumptive ground and surface water appropriations on
Salmon Creek presently total 189.4 cfs (Table 11}.
TABLE 11. Appropriation of Salmon Creek water, indicating
user, certification or permit number and quantity
of allocation.
User
Alaska Electric Light & Power Co.
Alaska Electric Light & Power Co.
City & Borough of Juneau
City & Borough of Juneau
Joseph Henri
Joseph Henri
Northern Southeast Regional
Aquaculture Association
Total
Certification of
Permit ADL 1
45780-C
51675-C
62230-P
62326-P
100508-C
100920-P
101041-P
Quantity
(cfs)
70
105
9
0.1*
<O.l*
0.2*
5
189.4
*Three groundwater withdrawals are included as well depths
are shallow and would be influenced by surface flow.
AEL&P Co. has a water appropriation of 175 cfs dating back to
E -52
water rights secured by the Alaska Gastineau Mining Company.
·For the purposes of road and pipeline design, an anticipated
maximum flow of 110 cfs was used. Typically, flows carried
in the pipeline wi 11 reach 110 cfs during summer months (two
·turbine operation) and will be reduced to 40 to 50 cfs in
winter (single turbine operation) (personal communication,
Corry Hildenbrand, AEL&P Co.). Water piped from the Upper
Powerhouse will be primarily used to generate hydroelectrici-
ty at the Lower Powerhouse. However, under a proposed
agreement with the City and Borough of Juneau, AEL&P Co. will
provide 4.64 cfs of water per day for a domestic water supply
for the Lemon Creek and Mendenhall Valley areas. Under such
emergency conditions as fire, the maximum the water supply
system can accommodate would be provided. AEL&P Co. also has
an existing agreement with NSRAA to provide 10 cfs for
hatchery operations during periods of low flow in Salmon
Creek, when the NSRAA water supply system does not provide
adequate flows.
With regard to other Salmon Creek users, the City and Borough
of Juneau has leased its surface water rights (9cfs) to NSRAA
for fish hatchery and other public water supply purposes.
The use of 3 cfs can be reclaimed by the City and Borough
with 2 years prior notice to the Association.
NSRAA has an outstanding application (ADL# 102820) with DNR
for an allocation of 15 cfs to supplement their present
appropriation (5 cfs). A decision on this application may be
delayed until additional streamflow data is obtained for
E -53
Salmon Creek.
CULTURAL RESOURCES
Historical Setting
The discovery of gold in the Juneau area in 1880 began over
60 years of large scale mining ventures in the area. Once
the placer ground (freegold, no milling required} and high
grade ores played out, attention turned to the extensive
deposits of low grade gold ore in the Juneau area. The major
mining companies operating in the area were the Treadwell
Complex (Douglas Island}, Alaska Gastineau Mining Company
(Perseverance Mines, Silver Bow Basin, east of Juneau) and
the Alaska-Juneau Gold Mining Company (Silver Bow Basin).
Many innovative processes were perfected to allow the miners
and mills to mine and extract ore from large tonnages of
rock, a necessity to make a profit on low grade ore. The
availability of low cost power became critical as the size of
the operation grew. The rugged mountains and high rainfall
made hydroelectric power generation a logical choice and
feasibility investigations were conducted for most of the
creeks in the area.
Salmon Creek, 5.6 km (3.5 mi.) north of Juneau, was
investigated as a power source by several of the major mining
companies. In 1907, a large scale map of Salmon Creek was
prepared by C. E. Davidson, probably an employee of Alaska
Treadwell Gold Mining Company and a complete report on
E -54
feasibility and costs of hydroelectric power from Salmon
Harry Wollenberg in 1909-10. Creek was produced by
Wollenberg later became the Chief Engineer for Construction
of the Salmon Creek Power Project, working for Mr. Bartlett
Thane, General Manager of the Alaska Gastineau Mining Company
(Stone, 1980}. The Alaska Gastineau Mining Company
eventually secured control of the Salmon Creek property and
water rights in 1911 and, by 1912, made preparations to
construct the area's first year-round hydroelectric power
plant at the Salmon Creek site (Stone, 1980}. The generated
power would supply the new Alaska Gastineau Mill at Thane.
The Salmon Creek project called for the construction of a
concrete dam, an upper and lower powerhouse, a wooden flume
and a steel penstock for routing water from the dam to the
powerhouses.
To pro vi de for access and transportation of supplies into
Salmon Creek valley during construction of these
hydroelectric facilities, Wollenberg (1909) suggested a
narrow planked tramway to be built using lumber cut by a mill
located in the Salmon Creek drainage (Figure 13).
Preliminary work on the tramway started in early 1912, and
dates on photographs obtained from the Alaska State
Historical Library indicate that construction of the tramway
and flume was well underway by early summer, 1912 (Figure 14,
Appendix D). The tramway was odgi nally designed to use
horses for power and stables were constructed in the vicinity
of the powerhouses {Figure 15). The Horse Tramway was
E -55
I I
~ Jl
II Jl
J
E -56
tO -
E
0
I'(
00
Q) 'II
d :..__
tJ
(./)
0
E -57
lO
<r ---+
0
E -58
FIGURE 14. Tramway Construction, Alaska Historical
Library, Emile Gastonguay Collection
FIGURE 16. Horse Tramway, Alaska Historical
Library, Emile Gastonguay Collection
E -59
FIGUR£ 15.
Redrct.wn From Nt4 Flume.
a.nd Pipeline Map
Sca.le: I"= 305 trt (Joofl:)
0 4 Rt><>,., G.tf~e.
0 4 Roo, C:.lla.!Je
PoWGR JIOVSE N~ I CAMP
POWE/t J.IOUSE N!! Z CAMP
E -60
probably designed for relatively light duty, but was ample to
supply early stages of construction (Figure 16). The
originial cost estimate for the horse tram was $ 10,000.00,
but expense records (dated.December 31, 1914, Section C.6.2.)
indicate costs eventually rose to $ 16,539.27 for material
and labor.
Prior to the
Salmon Creek
tram. The
start of concrete
Dam, the tramway was
lumber, structural
construction work at the
upgraded to a locomotive
members and rails were
upgraded, as the system had to be capable of carrying
numberous heavy loads of cement. The small gas engine shown
in Figure 17 was transported from Seward City (later known as
Comet, located just north of Berners Bay) to Salmon Creek,
and was later used on the Annex Creek Power Project (Stone,
1980). While the little engine probably saw its fair share
of runs on the tramway, a larger locomotive was used to move
heavy loads of cement bags. The first concrete was poured at
the dam site on July 25, 1913 and the dam was finished within
a year (Stone , 1 9 8 0) •
With the dam completed, the heavy-duty rolling stock was put
to work elsewhere. Eventually, a Model A Ford fitted with
rail wheels was used to transport work crews and supplies
along the tramway.
The Gastineau holdings (including the Salmon Creek
facilities) were purchased by the Alaska Juneau (A-J) Gold
Mining Company in 1935. In 1936, the A-J rebuilt the Lower
Powerhouse, which had burned in 1922, and the flume between
E -61
FIGURE 17 .. Small Locomotive, Alaska Historical
Library, Emile Gastonguay Collection
f
FIGURE 18. Lower Powerhouse and Wharf, Alaska
Historical Library, Emile Gastonguay
Collection
E -62
the Upper and Lower Powerhouses (Stone, 1980).
AEL&P Co. purchased the A-J holdings in 1973 and continues to
maintain and use the Upper Powerhouse for power generation.
In 1974, the operation of the Lower Powerhouse stopped.
Helicopters are used to transport personnel and supplies to
the Upper Powerhouse site and the tramway is now obsolete.
The tramway continues to be a popular recreational access
route into Salmon Creek Bas in. However, although the route
pro vi de easy access to the bas in, the deteri orating wooden
structures present an increasingly hazardous access.
Description of Tramway Route and Associated Structures
The cultural
documentation
Survey of Cultural Resources
resources survey was approached
of historical structures and other
as a
cultural
resources within the proposed project area. There was no
evidence which suggested the existence of archaeological
features along the route and within the confines of the
proposed road-pipeline project, and no such features were
observed during the cultural resources survey effort.
A review of historical registers indicates ·that although no
.cultural features in the Salmon Creek drainage ar-e included
in the National Register of Historic Places (Alaska Division
of Parks, 1976), three sites associated with historic mining
efforts in Juneau have been identified by the Alaska Heritage
Resource Survey (sites JUN 176, JUN 207 and JUN 211). Site
E -63
descriptions provided by Mr. Greg Dixon (Alaska Department of
Natural Resources) are as follows: { l) Salmon Creek
Powerhouse Site I 1, including the Lower Powerhouse, two mile
wooden flume, two Pel ton wheels and three wooden homes; ( 2)
Salmon Creek Powerhouse Site I 2, including the Upper
Powerhouse, one mile steel penstock, two Pelton wheels, two
wooden houses and one bunkhouse; and ( 3) Salmon Creek
damsite, including the concrete arch dam and associated
tramway and timberframe hoist house.
In accordance with requests made by the Alaska State Historic
Preservation officer, the following cultural resources survey
"' ..
was implemented to assess impacts on these and other
historical structures resulting from road-pipeline
construction.
Field Survey
The cultural resources survey was completed between November
ll and 25, 1981, by Tim Moore, party to this investigation.
Survey efforts focused primarily on descriptive and
photographic documentation of historic structures which would
be removed or significantly altered during proposed road
construction {specifically, the tramway and hoist house
sites). Consideration was also given to other structures
identified to be of historical significance, including the
Lower Powerhouse site, the Upper Powerhouse site and the
flume. The historic concrete arch dam at the head of Salmon
Creek was considered to be outside of the area of proposed
E -64
construction impqct.
Historic structures were described, measured and, when
marginal winter light exposures permitted, photographed.
Photographs were taken with TRI-X black and white film and a
35 mm SLR camera, using both 58 mm and 35 mm lenses.
Trestles were assigned a numerical designation (indicated as
T-jf) to aid in field recording (Table 12). The center point
of each trestle was tied into a recent survey and field map
provided by Toner & Nordling, Registered Engineers, Inc.
This recent survey seems to correspond to the original 1914
right-of-way survey for distances and alignment (Figure 13).
Trestle construction, condition, height and length were
recorded. Characteristics of the track which were noted
included condition, width, length and description of the
switch areas.
Tramway
The tramway originally began at the edge of Gastineau Channel
and travelled eastward up the Salmon Creek drainage to the
Salmon Creek Dam. The entire route contains two major
inclines and a spur to the Upper Powerhouse (Table 13).
Also, originally, there was a 152m (500 ft.) wharf out into
the Channel, with a 61 m (120 ft.) length of track (Figures
15 and 18). An incline tramway with steel wire assist (to a
hoist facility) brought materials up the first incline to the
start of the locomotive tramway. The locomotive tramway was
constructed on a slight grade. Near the Upper Powerhouse the
E -65
main line continues to the Dam and a spur goes to the
powerhouse. Between the Lower and Upper Powerhouses the
tramway contains 38 trestles, ranging from 3m (10 ft.) to 63
m (210 ft.) in length (Table 12).
TABLE 12.
Trestle !
T-1
T-2
T-3
T-4
au on log
T-5
T-6
T-7
T-8
T-9
T-10
T-11
Salmon Creek Tramway Trestles
Length Midpoint
14.6 m (48 ft.) 23 + 50
13.4 m (44 ft.) 25 + 00
6.1 m ( 20 ft.) 26 + 33
38.1 m (125 ft.) 29 + 00
sills,
4.6 m ( 15 ft.)
15.2 m (50 ft.) 30 + 60
53.3 m (175ft.) 31 + 45
24.1 m (79ft.) 34 + 00
4.6 m (15 ft.) 35 + 50
4.6 m (15ft.) 36 + 10
15.5 m (51 ft.) 37 + 44
E -66
Remarks
Down; estimated 1.5
m high when upright.
East end falling
down; 1 m high.
Same age deck as T-
3; 1 m high.
Three timbers under
deck; 12 supports,
5 m high.
Small, 1 m high.
Two logs, diameter
75 to 100 em; no
decking or rails
(Figure 26).
Long trestle: north
end 32 + 32, 39 m.
Two sections: 39 m,
13.5 m newer; Deck-
ing 6.5 x 29.5 em
and 6.5 x 14.5 em
{newer), 12m high
(Figures 28 & 35).
Seven supports, log
sills, 4 m high.
Height 1 m.
Delapidated, cut
timber sill; 1 m
high.
Log and cut timber
T-12
T-13
T-14
T-15
T-16
T-17
double track
T-18
T-19
T-20
T-21
4 2. 7 m ( 14 0 ft. ) 38 + 6 0
64.0 m (210 ft.) 40 + 40
32.9 m (108ft.) 42 +52
4.6 m (15 ft.) 45 + 00
3.0 m (10ft.) 45 + 80
24.7 m (81 ft.) 46 + 90
47 + 52
22.9 m (75 ft.) 48 + 60
33.5 m (110 ft. 50 + 00
25.6 m (84ft.) 51 +50
22.3 m (73ft.) 52+ 65
E -67
sill; noted rebuild-
ing; poor shape in
general.
Along cliff; old
trestle & rail be-
low; Decking 6.5 x
29.5 em; 2 timbers,
13 supports; 12 m
high; fair shape.
West section down,
length 40.5 m;
Center section up,
1 ength 6 m; East
section down, length
16.5 m; All cut tim-
ber; center-section
rests on a small
rock ridge.
Moss-covered tres-
tle; 9 supports; 4
m high; slide area,
trestle has been
wiped out in past
(Figure 30).
Height 1 m.
Hillside slumping;
trestle in mud; may
have always been
low.
Down; slide area; 7
m high.
Known as guard rail.
Down; hanging track
(Figure 31).
Down; log sill under.
east end rails.
Deck i n g 6 • 5 em x
29.5 em; 6 supports,
3.5 m high.
Down; track on big
1 og sills ; t r. e e
across trestle des-
troyed it.
T-22
T-23
T-24
T-25a
T-25b
T-26
T-27
T-28
T-30
T-31
T-32
T-33
T-34
T-35
59.1 m {194ft.) 56+ 10
6.4 m (21 ft.) 61 + 70
10.0 m (33ft.) 63 + 10
27. 4 m { 9 0 ft.) 65 + 36
40.2 m (132ft.)
50.6 m (166ft.) 70 + 85
36.3 m (119 ft.) 73 + 60
19.5 m (64ft.) 84 + 50
33.5 m (110ft.)
27.7 m (91 ft.} 86 + 35
33.5 m (110ft.} 88 + 40
24.4 m {80ft.) 90 + 40
24.4 m (80ft.) 92 + 90
33.5 m (110ft.) 94 + 10
16.8 m (55 ft.) 95 + 00
E -68
Down section, length
51.3 m; east end up
7.8 m; old construc-
tion material below
(Figure 32).
Wide plank top; in
mud over swamp area.
Old, rough-looking;
1 m high (Figure
2 7).
Up; 3 m high.
Down; old building
material, log sill
for supports & logs
unaer rails (Figure
3 3).
Seventeen supports;
6 m high (Figure
2 9) •
Old, going down in
spots ; 1 m h i g h •
Down.
Salmon Creek cros-
sing; small track.
Down; larger track.
Tree; down due to
break center; 1 m
high.
Mossy; old trestle
was set on logs
(Figure 24).
Height 1 m.
West section, up
(16.5 m); East sec-
tion down (16.5 m).
Two logs; modern
cable handrail;
small track starts
on east end; 3 m
T-36
T-37
T-38
NOTES:
18.9 m (62ft.) 96 + 00
33.5 m (110 ft.) 97 + 20
4.6 m (15 ft.) 101 + 00
high.
Low trestle; 1 m.
Good shape; old ma-
terial below; 2 m
high (Figure 25).
Small; 1 m.
A small trestle or bridge crosses the overflow flume at 22 +
75, before T-1.
Several small, wooden, track supports were noted but were not
counted as trestles.
TABLE 13. Length of Salmon Creek Tramway
Section
Tramway on Wharf
Lower incline
Locomotive Tramway
1) Lower incline (top) to
upper incline bottom
2) Lower incline to Upper
Powerhouse
3) Spur to Upper Powerhouse
Upper Incline (at Dam)
Width of Right-of-Way
The above information was taken from:
Length
61.0 m (200 ft.)
590.0 m (1936 ft.)
4. 0 km ( 2. 57 mi • )
2. 81 km ( l. 7 8 mi • )
450.0 m (1475 ft.)
301.0 m (989ft.)
30.5 m (100 ft.)
Application for Right-of-Way
Salmon Creek Tramway
Alaska Gastineau Mining Company
Juneau, Alaska
December 1, 1914
E -69
The initial section of the tramway, east of the Lower
Powerhouse, involved a steel wire assist up a 581 m (1936
ft.) incline to a hoist facility. Approximately the lower
third of the tramway on the incline has been pushed aside by
a tractor to form a primitive road (Figure 19) • At the top
of the newly-formed road, the proposed road wi 11 follow the
hillside to the west of the incline to reduce the amount of
grade, and will rejoin the tramway near the hoist house.
Evidence of an old primitive road exists along the proposed
road route, probably part of the pre-tramway construction
access.
Most of the tram on this incline has deteriorated and fallen
down. The foot trail travels on the tramway through a middle
section which is still somewhat supported (Figure 20).
However, the trai 1 above and below this section travels to
the south of the old tram route on a newly-brushed path. The
final grade of the incline has fallen down completely (Figure
21). At several locations along the incline, one or two
steel rollers are placed in the center of the rails to keep
the cable from cutting the ties and supports. Each roller
contained four channels for the cable and the center grooves
show cable scoring.
The incline tramway terminates at the top of the ridge near
the hoist house (Figure 22) (see Section entitled Hoist House
Area). From this point, the locomotive tramway continues at
a slight grade eastward to the Salmon Creek Dam, with a spur
to the Upper Powerhouse.
E -70
FIGURE 19. Lower section of the Incline
Tramway looking down (west)
FIGURE 21. Incline Tramway
looking up (east)
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FIGURE 20. Incline Tramway
looking up (east)
FIGURE 22. Ton of Incline
Tramway
Th~ section of the locomotive tram which will be affected by
the proposed project is the section between the hoist house
and the Upper Powerhouse (Figure 13). This section is 4 km
(2,57 mi.) in length and contains 38 trestles (10 are down,
Tables 12 and 13, Figure 23). The proposed roadway will
follow the tramway for the most part, but may deviate in
areas with long trestles where the r-oad wi 11 mor-e closely
follow the topogr-aphy.
Cultural and histor-ical materials obser-ved within the tramway
cor-ridor included the overflow flume crossing, trestles,
remains of earlier construction discards and stumps with
spring board notches. Spring boards provided a platform for
tree fallers sawing with cross-cut saws.
During the constr-uction of the tr-amway, small r-oads,
construction camps, a stable and sawmill were located along
the r.oute. No evidence of these featur-es were noted in the
cour-se of the sur-vey. The amount of disturbance they caused
has pr.obably been obscur-ed or-destr-oyed by natural pr-ocesses.
Accor-ding to Mr-. William Byington, a for-mer. A-J mining
engineer, the sawmill which pr-oduced cut lumber for-the
project was pr-obably located just west of the point where the
tr.amway crosses Salmon Cr-eek (Figur-e 23, T-29). Dudng his
wor-k with the A-J, Byington observed piles of slash and
sawdust hear this area. Photographs of the sawmill operation
ar-e located in the Alaska State Historical library photograph
collection, PCA-119 (Appendix D).
The 1914 Right-of-Way map shows a stable located 140 m (470
E -72
~
~ SALMON CREEK
I \ I I ) fs I I \ ., i
f/2. -~ -!.
I i i .
r
. I
Tl8
\
.I \ '
LOWER ?OW£RHOU5E
~ ~ T~l
0
+-
~
N
·,
'\
UPPER
fi&URE Z3.
------
...,.-. -· -·--
0
T f'U.M Route.
"Br.tdse or Tres1\e. (Existing)
StreaMS
lnterM\treNt Streo..MS
1'5l 4?7m
i '' == \52 m (500ft.)
E -73
ft.) south of the Upper Powerhouse, but no evidence of the
structure was noted in the area.
The most striking features along the tramway route are the
trestles. Of the 28 standing trestles, many are in very poor
shape and some are beginning to fall down. Many of the more
decayed trestles have lumber, plywood or broken planks on the
decking under the rails. The decking on some of the trestles
appears to be unsafe for foot travel. Nearly every trestle
'has evidence of a predecessor below it. Rotting timbers,
logs, plants, ties and rail were observed beneath most
trestles (Figures 24 and 25). Mr. Byington was of the
opinion that none of the original trestles were still in
place. Based on his experience in maintaining wood
structures in the a rea, he felt that the combination of wet
weather and untreated wood resulted in fairly rapid
deterioration. Also, as a result of damp weather and forest
cover, moss growth on the trestles is quite common and
probably helps promote decay.
The use of spruce logs in trestle construction and as sills
for support foundations appears to have been common in the
earlier trestles. The logs used for sills were often large
and were completely buried to deter the decay process. Many
of the supports appear to go directly into the soil and it is
not possible to determine the type of foundation. It is
possible the log sill is more common than it appears. In
several of the down trestles it was noted that a log or cut
timber was placed under the track for bedding. Again, it was
E -74
tiJ
--..!
lJ1 FIGURE 24. Moss covered trestle
with debris below T-32
~
' • .g)-~ .... ·:-~ ·.:-.,..~~.~~ ... ::'--,...~-::-··-·.;,......,.....--.,.. .~'1-·' f.~ttl",#{,_, ··~ .... :...'f'-=:. .. •;f=·~~~:_"";t~~jjiill'jt.~"" ..... ~ .. T ' "t ~, ~.·J~
,, ..:;.~ ... ~~·\-· ·;·,.1·.,.~~~--,·,::-;t·"'··~~. '--·J!i.~;·; .. >'.. . ' ' --~ ~--F.~r>-:-;: .. \~.. .. ~.· 1; ~ L . ~J' •• ~:o:l;::.-· .·=r •... ~. • . ~~· ~--; ~-; .... ~... '!t , ... ~-..... ., .. ;-,' -~..-· .... .:-· _· .. ;;:·. ~~~~~-="' , . . . ..,, .. •, : . ..-... 1.._ -;--(,;'/nl_~¥~•, ~~I• • ~ .... 0'~ \.•~ .._ ~ .... ·,..~~~ ,._::-':~' ',..,o: I_ ~,H•.£~~ ...... t~
FIGURE 26. Log Trestle T-6
. I
FIGURE 25. Debris below a trestle T-37
FIGURE 27. Small Log Trestle T-24
• 11
often impossible to determine if a bedding log or timber was
placed under the rail. An example of discarded cut lumber
and logs is seen in Figure 24 and 25. Examples of using logs
in the construction of trestles is seen in T-6 and T-22
(Figure 26 and 27), although these were not the only trestles
which incorporated logs as supports. Saw cut lumber was more
commonly used in later trestle construction. Larger timbers
were used for the vert i ca 1 supports, cross-caps, and beams
under the decking and rails. Planks were used for cross
bracing
trestle,
bracing
between the supports and decking. The higher the
the heavier and more complex the amount of cross
(Figures 28, 29 and 30). The dimensions of most
lumber were quite uniform, but in several cases deck planks
were of a different size and appeared to be a different age
(judged by degree of decay and moss cover). Examples of some
of the trestles that have fallen down can be seen in Figures
31, 32 and 33. The large log under the rail can be seen in
Figure 33 (T-25b).
Most of the rails on the locomotive section of the tramway
are intact, with the exception of areas where slides have
washed out or buried the line. There were
different size of rails used on the .tramway.
at least two
The two sizes
which were noted are shown in Figure 34. The larger rail was
noted only on the tramway section from T-30 to just east of
T-35. Rails were spaced at approximately 99.5 em (40 in.)
with some variation attributed to loose spikes or shifting
ties. In many places the correct spacing was maintained by
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t'l
FIGURE 28. High Trestle Bracing T-7 FIGURE 29. Bracing T-26
-...I
-...I
FIGURE 30. Bracing T-14
FIGURE 31. Trestle-down T-18
FIGURE 32. Trestle-down T-22 FIGURE 33. Trestle-down T-25B
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!4---4. 8 em (6.oc.rn)~
f
1.5c.m (2.0 em)
i
8.5cm (B.8cm)
~ ... ~---8.8c.TY) ( 9.8 ern)
F i~ u re. 3 4. Cross section of ra. i Is.
Actuo...l sice -numbers rn pa.rentheses
are d i men 5 ion 5 of 1 a. rj e r-
ra.i Js.
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metal clamps. There were two types of clamp n6ted, a painted
flat clamp (Figure 3 5) and an older looking "turn-buckle"
type (Figure 36). The clamp or spacer shown in Figure 35 is
located on the eastern turn of T-7. Most clamps seemed to be
placed on turnss or in wet areas. Mr. Byington indicated the
turns were the most likely spot for cars to derail. In
problem areas, a guard rail was installed outside of the main
rail to prevent derailing (Figure 37).
The tie spacing seemed to be highly variable and no "average"
distance was determined (Figure 38). Maximum spacing was
approximately 1m ( 37 in.). The random spacing may indicate
that ties have been replaced, added or rotted out. However,
many are buried and are preserved much like a mud sill would
be.
There are several places where the tramway track is no longer
in place. The most common breaks are due to the failure of a
trestle, but mud and debris slides and wash-outs have also
removed sections.
Lower Powerhouse
The Lower Powerhouse facilities have undergone considerable
change and disturbance since they were constructed. Several
of the buildings, the wharf and tramway spurs are no longer
present. It appears that structures west of the Lower
Powerhouse and all the track are gone. Since 1914, the
shoreline has changed due to filling and construction of a
four-1 ane expressway which now transects the area. A large,
surfaced parking lot, containing a shed, portable office and
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t%J
00 ......
FIGURE 35. Flat Rail Clamp T-7
FIGURE 37. Example of Guard Rail
FIGURE 36. Round Rail Clamp
FIGURE 38. Example of Tie Spacing and
Typical Track
"
transmission line equipment,· now stands at the location of
the old office and warehouse (Figure 15).
The Lower Powerhouse burned in 1922, was rebuilt in 1936 by
the A-J, and continued to produce power until 1974. Water
entered the powerhouse vi a two 7 5-100 em ( 30-40 in.) riveted
steel penstocks coming down some 488 m (1625 ft.) from the
forebay at the end of the flume. Both penstocks appear to be
rusty and pitted, making them unserviceable.
Hoist House Area
The hoist house is located at the upper end of the incline
tramway. At the upper terminus of the incline there is a
short section of platform which leads into the locomotive
t r a mw a y sect i on ( F i g u r e 2 2) • In the a rea t h ere i s a shed
housing the hoist and controls, a second storage shed, and
two sections of track that forms a switch yard. The hoist
house is a 4.4 m x 6.2 m (14.5 ft. x 20ft.) structure
constructed of wood and corrugated roofing material (Figure
39). Three electrical wires run from the main transmission
line to the front of the building. These powered three large
transformers which, in turn, powered the electric motor on
the hoists. The large drum of steel cable (Figure 40) and
drive gears were moved by a large 75 hp electric motor. The
hoist was made by "Washington Iron Works, Seattle, U.S.A.
(No. 293) ". The motor, rheostatic controller and resistor
bank (Figure 41) are all made by "Westinghouse, Pittsbtggh,
PA". It is assumed that all of this equipment has been in
place since construction.
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[']
00 w
FIGURE 39. Hoist House
. r· l.i.:·,~"
FIGURE 40. Hoist Drum and Cable
, I
FIGURE 41. Part of Hoist Motor
Control (in Hoist
House)
,,
A second ·3m x 4.2 m (10 ft. x 14 ft.) frame building
completely covered with corrugated roofing is located 6 m (20
ft.) southwest of the hoist building. Two wires supplied
electricity to this shed. The shed appears to have been used
for storage as its one window is covered and there is no
chimney hole.
Two short spurs and three switches are located to the south
of the tramway in the vicinity of the hoist house and shed.
The two curved spurs form one line near its terminus (Figure
23). This switch area and a similar one located near the
Upper Powerhouse were used to turn the locomotive around for
return trips.
There is some debris scattered around the hoist house area.
Material from the tramway's operation period include cut
lumber, corrugated metal, rails, 5 gallon oil cans, 55 gallon
drums, and two wooden cars with rai 1 road wheels. Ins ide the
hoist house there is a scattering of old machine parts and
miscellaneous debris. More recent material sea tt ered about
the area included a car seat, .22 shells, as well as food and
beverage containers.
Upper Powerhouse
Just below the Upper Powerhouse is a "turn-around"
track, which is similar to the one at the hoist area.
spur
This
spur was longer and apparently went across the creek to the
"Roundhouse" (Figure 15). The Roundhouse may be the large
building pictured in Figure 42. After the two spurs of the
turn-around join, the single track goes through a small,
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t>J
co
l11
'I
Ll ..... ~" :.._-
-~
FIGURE 42. Upper Powerhouse Camp
Looking West--Down Stream
FIGURE 44. Cribbing Along Creek Protects
Flume Area
FIGURE 43. Upper Powerhouse Headwork Tramway
Open on Left--Looking East From
Bridge in Figure 42.
FIGURE 45. Looking West From Flume Tramway
Enters the Upper Powerhouse Clearing
in the Center o f t he Photograph
' I
corrugated metal-covered frame shed 5m x 3. 5 m (16 ft. x 11
ft.) and ends at the edge of the creek. Figures 43, 44 and
45 show the area near the Upper Powerhouse where the pipeline
will be placed.
The proposed project will require a change in the headworks
just below the Upper Powerhouse area include a large building
constructed over the creek (possibly the Roundhouse in Figure
15) , two sma 11 houses on the south side of the creek, and a
large residence (not shown on Figure 15), Powerhouse facility
and maintenance shop on the north side of the creek.
Flume
The flume was not the focus of this surv~y; however, a brief
survey was conducted along the flume route. The original
flume was 1. 2 m x 1. 8 m ( 4 ft. x 6 ft.) and was completely
r e bu i 1 t as a 1 • 2 m x 1 • 8 m ( 4 f t • x 5 f t • ) structure in 1 9 3 6 •
The flume continued to receive maintenance and carry water
diverted from Salmon Creek until the early 1970's.
There is one section of flume that is completely
caused the deteriorated. At this location, flume leakage
bedrock to be washed clean and a large mass of soil and trees
to slide to the level of the tramway. Some of the
construction techniques used to support the flume can be seen
in Figure 47, which was photographed at the section of flume
which is down.
There are several
sagging or moving,
support failure.
places where the flume appears to be
and these are probably early signs of
The flume decking contains numerous holes
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t:tJ
I .
00
-...J
FIGURE 46. Break in Flume
Looking West
FIGURE 47. Close-Up of Flume
FIGURE 48. Over.flow Flume Discharge Near
the Hoist Area
I
where planks have rotted. The overflow flume that drained
excess water from the fore bay is in poor shape. Figure 48
shows the end of the overflow just below the tramway.
ENVIRONMENTAL AND CULTURAL IMPACTS AND MITIGATION
Vegetation
A total of 19.1 acres will require clearing during road and
pipeline construction. Of this acreage, approximately 4.8
acres will require removal of brush only. The remainin9 14.3
acreas will require remova 1 of both brush and timber. Such
an impact may be considered short-term since removal of
vegetation adjacent to the road bed will be followed by
regrowth of residual plant species and invasion by species
adapted to partially open conditions. Pioneer species will
include both herbaceous plants and young growth hemlock and
spruce.
Both second growth and old growth timber will be removed
during road construction. Care should be taken in the
remova 1 of this standing timber so as to minimize damage to
remaining trees and to avoid felling trees into the stream
channel.
Revegetation of cleared areas with native plant species or
compatible, introduced species would be an effective
m~tigation practice in areas where soil destabilization may
occur due to slow natural revegetation.
E -88
Wildlife Resources
Increased noise and activity in the Salmon Creek drainage
during road-pipeline construction will be the primary impact
on wildlife species. Habitat use patterns will undoubtedly
be altered during construction in response to these
disturbances. Following proj~ct completion, limited vehicle
use and probable increases in pedestrian traffic may raise
noise and activity levels in Salmon Creek over present
conditions. Nevertheless, wildlife will have unrestricted
access within the drainage and impact~ of the road on habitat
use should be minimal.
Improved pedestrian access to the Salmon Creek drainage may
result in increased hunting pressure, especially of mountain
goats which occasionally enter the area. The Alaska
Department of Fish & Game monitors goat populations in the
vicinity and increased hunting pressure would be addressed by
ADF&G regulatory policies.
The gravel roadbed may be used as a gravel source by gizzard
birds. An attraction of blue grouse to gravel logging raods
has been documented elsewhere in Southeast Alaska (personal
communication, Dave Zimmerman, ADF&G).
Water Quality ~ Fisheries
Potential water quality impacts are limited to additional
sediment loading of the occasionally turbid stream during and
after road construction. Water quality standards outlined by
the State of Alaska (ADEC, 1979) indicate that outs ide of a
E -89
variance provided during construction, (1) no measurable
sediments over natural conditions is in suspended
for a domestic water
increase
allowed
loads should not interfere
source, (2) imposed sediment
with established water supply
treatment, and (3) fine sediments in spawning
increase ever natural condi t i ens by more than
weight.
beds may not
5 percent by
Although anadromous fish do not occur in Salmon Creek near
sites of in-stream and stream-side construction, adverse
effects on water quality from upstream construction may
affect downstream habitats. Natural spawning, incubation and
rearing areas and the NSRAA hatchery may be affected by water
quality changes elsewhere in the drainage.
During Construction
In-stream construction in Salmon Creek's channel will include
(1) a single-pier, supported bridge at location 85+00, (2)
rock riprap along the northern streambank between 91+50 and
94+00, and (3) a bridge-headworks installation at the Upper
Powerhouse. An examination of the streambed at these sites
indicated water quality impacts during construction may be
limited, due to the conditions outlined below.
At the proposed 85+00 bridge site, the stream runs largely on
bedrock overlain by coarse alluvial material. Bedrock
outcrops are exposed in several locations and sediment
disturbance during pier placement should be minimal. Rapid
resettlement of the coarser, heavier streambed materials
should help to reduce the area of impact, although some
E -90
increase in concentrations of suspended fines will occur
downstream.
Coarse-sized streambed materials present at the headworks and
riprap locations will also help to minimize sediments
effects. The placement of rock riprap is intended to protect
a long, stream-side cut and fill section from erosion during
high water flow in Salmon Creek.
Impact considerations could be addressed by minimizing
in-stream construction activities during spawning and
incubation of wild and hatchery stocks. If this mitigation
measure is adopted, construction with in the stream channel
should be scheduled between May 1 and July 15.
Construction on slopes adjacent to Salmon Creek and in
tributary drainage paths has the potential for introduction
of sediment to the stream and degradation of water quality.
The following pr inc i pl es and practices may be employed to
mitigate water quality impacts associ a ted with stream-s ide
construction:
(1) Schedule road building operations on stream-side
slopes and in drainage paths during drier weather
to avoid erosion of disturbed, unstabilized soil by
natural torrential runoff.
(2) Minimize equipment operation in tributary drainage
paths.
( 3) Install culverts and bridges concurrent with estab-
lishment of road subgrades.
(4) Apply road surfacing during drier weather to avoid
E -91
runoff of fine sediments from newly-laid surface
material.
After Construction
Naturally-occurring landslips and unstable drainage paths
present along sections of the proposed road-pipeline route
indicate a potential for slope stability problems after
project completion.
a balanced cut-fill
jeopardized by the
In several locations the risk of losing
roadbed is high and water quality is
possibility of excessive erosion and
slumping into or adjacent to Salmon Creek.
During an initial slope stability assessment (Appendix B) and
further field consultation with an engineering and soils
specialist, the road section between locations 38+00 and
52+00 was identified as a particularly critical area.
Primary soil material within this section is derived from
weathered greenschist, with colluvial soil and glacial marine
till also present. Steep slope gradients and active drainage
paths combine with the loosely structured soils to decrease
slope stability within this section.
The nature of unstable soil conditions in Salmon Creek is not
such that road development is not feasible. However, the
following upgraded construction and design techniques may be
appropriate in select areas to provide for roadbed integrity
and protection of water quality:
(1) Use of maximum bedrock support through cut
rather than fill techniques.
(2) Exposure of minimal surface overburden above
E -92
cut slopes.
(3) Removal of unstable overburden beneath the
roadbed and fill materials.
(4) Establishment of well-drained conditions in
fill and roadbed material.
(5) Disposal of excavated soil and rock at loca-
tions which are not subject to slumping or
erosion into Salmon Creek.
(6) Rapid stabilization of disturbed surface
areas by seeding or revegetation.
Salmon Creek Streamflow and Related Fisheries
Return to a flow pattern where discharges from the Upper
Powerhouse and possibly the South Fork are once again
conducted directly to the Lower Powerhouse will reduce flows
in Salmon Creek. During most conditions, the 3. 7 square
miles of drainage below the dam will be sufficient to
maintain the few trout residing between the Upper Powerhouse
and the lower falls. Periods of winter drought will reduce
flow below the dam to low volumes and emergency releases of
water from the Upper Powerhouse for hatchery operations
downstream will also help to maintain resident fish in the
stream.
Hatchery water is removed from Salmon Creek above the lower
falls. Part of this flow is returned to the creek adjacent
to the hatchery, and the remainder of withdrawn water is
E -93
piped into rearing facilities at Twin Lakes. In times of low
flows, about one hundred fifty yards of Salmon Creek between
the falls and the hatchery will be partially or largely
dewatered, but this section of streambed is upstream of
almost all gravel spawning habitat~ Minimum return of
hatchery water back to the stream during winter periods when
drought conditions are most likely, is presently about 2
c.f.s. and will in future years, with large fish production,
probably equal or exceed the minimum instream flow of 3
c.f.s. recommended by ADF&G. One or more of the following
measures may be necessary during certain winter low flow
periods to provide adequate hatchery water and to protect
fishery values:
(l) Emergency release of water from the tailrace
below the Upper Powerhouse. The present agree-
ment provides for up to 10 cfs emergency release.
(2) Installations which provide for obtaining un-
chlorinated water from the tailrace could in-
terconnect with the hatchery water system near
the rearing facility at Twin Lakes.
{3) Recirculation of waters within the NSRAA hatchery.
Cultural Resources
The Salmon Creek Tramway, both the incline and locomotive
sections, are no longer serviceable and would require
complete rebuilding to make them usable. The deterioration
of the wooden structures of the tramway has reached the point
E -94
where structural failures will increase. Many of the
trestles are no longer safe for foot traffic because of
rotten decking and/or failing supports.
Using both field observation and informant data, it was
determined that mos.t, if not all, of the trestles have been
replaced or rebuilt at least once since their original
construction. It is also probable that some replacement,
repair, and upgrading has occurred on the track·and roadbed.
The information used to evaluate the cultural significance of
the tramway included the 1912-13 construction data, present
condition of the trestles and tramway, and evidence of
rebuilding over the years. Evaluation of these features
indicated that the
significant cultural
While the tramway
remains of the tramway are not a
resource that should be preserved.
did play an important role in the
development of the Salmon Creek hydroelectric facilities, the
main structures (Salmon Creek Dam and the
powerhouses) remain, while the non-maintained, wooden,
historical structures are rapidly deteriorating.
E -95
REFERENCES
Alaska Department of Environmental Conservation, 19 78.
Title 18. Environmental Conservation,, Chapter 80,
Dr inking Water.
A;taska Department of Environmental Conservation, 1979.
Water Quality Standards, Alaska Water Pollution
Conrol Program, 34 p.
Alaska Electric Light and Power Company files:
Application for Right-of-Way Salmon Creek Flume and
Pipeline. Alaska Gastineau Mining Company, Juneau,
Alaska, October 12, 1914 (MAP).
Application for Right-of-Way Salmon Creek TRamway,
Alaska Gastineau Mining Company, Juneau, Alaska,
December l, 1914 (MAP).
Expense Records Salmon Cereek
General Transsportation Department,
December 31, 1914.
Power Division
Thane, Alaska,
City and Borough of Juneau, Planning Department, 19 77.
Juneau Coastal Management Program: Phase I.
Interim Report, 84 p.
City and Borough of Juneau, Planning Department, 19 79.
Juneau Coastal Management Program, Final Report -
Hearing Draft, p. 13-18, 9.
Daniel, Mann, Johnson & Mendenhall, 1972.
Geophysical hazards investigation for the City and
Borough of Juneau, Summary Report, 92 p.
Environaid, 1979. Salmon Creek-Potential as a water
source for an NSRAA hatchery. Prepared for NSRAA,
5 p. (Unpublished).
Ford, A. B. and D. A. Brew, 1973. Preliminary geologic
and metamorphic isograd map of the Juneau B-2
quadrangle, Alaska: USGS MF, Map 527.
Homan Associates, 1974. Capital City Economic Base
Study.
Miller, R.D., 1972. Surficial geology of the Juneau
urban area and vicinity, Alaska, with emphasis on
earthquakes and other geologic hazards, USGS
open-file report # 517, 108 p.
E -96
Reed, R. D. and R. H. Armstrong,
sport fishery -Juneau area,
Fish and Game, Federal Aid
Project, Project F-9-3, 105 p.
1972. Dolly Varden
Alaska Department of
in Fish Restoration
Sainsbury, C. L., 1953. Geology of the Mount Olds -
Clark Peak area, Juneau vicinity, Alaska. Colorado
University, unpublished thesis, 48 p.
Stone, D. and B. Stone, 1980. Hard Rock Gold, Juneau,
Alaska.
Thomson, R. H., 1919. Upon certain water power in
Southeastern Alaska, report to Messrs. E. B.
Cadwel·l and Company of New York City, New York.
AEL&P Co., file copy (Unpublished).
u. s. Army Corps of Engineers, Alaska District, 1969.
u.
Special flood hazard information report, Salmon
Creek, Juneau, Alaska.
s. Department of Commerce, Bureau of the
1981. 1980 Census of Population and
Advanced Reports, Alaska, PHC 80-V-3.
Census,
Housing,
U. s. Department of Commerce, National Oceanic and
Atmospheric Administration, 1979. Local
climatological data: Annual summary with
comparative data, Juneau, Alaska.
u.
u.
u.
u.
S. Environmental Protection Agency, 1976.
Creek Interceptor, City and Borough of
Juneau, Alaska. Final Environmental
Statement, EPA-910/9-76-018, 151 p.
s. Environmental
water quality
440/5-80-020.
s. Environmental
Protect ion Agency , 19 8 0 a •
criteria for antimony.
Protection Agency, 1980b.
Salmon
Juneau,
Impact
Ambient
EPA
Ambient
water quality criteria for arsenic, EPA
440/4-80-221.
s. Environmental Protection Agency, 1980c. Ambient
water quality criteria for cadmium, EPA
440/5-80-025.
u. s. Environmental Protection Agency, 1980d. Ambient
water quality criteria for silver, EPA 440/5-80-
071.
U.S. Environmental Protection Agency, 1980e. Ambient
water quality criteria for zinc, EPA 440/5-80-079.
E -97
U. S. Geological Survey, 1969. Hydrological data of the
Juneau Borough, Alaska, 77 p.
U. s. Geological Survey, 1974. Hydrologic investiga-
tions of Salmon Creek Reservoir and drainage Basin
near Juneau, Alaska, 22 p.
Wadman, R. D., 1962. Inventory and cataloguing of the
sport fish and sport fish waters in upper Southeast
Alaska. Alaska Department of Fish and Game,
Federal Aid in Fish Restoration, Annual Report of
Progress, 1961-62, Project F-5-R-3, 3:21-29.
Wilcox, J. A., 1917. Salmon Creek power project, power
output, plant efficiencies and hydrographic data.
Letter to Mr. B. L. Thane, Manager, Alaska
Gastineau Mining Company, Juneau, Alaska, 29 p.,
AEL&P Co. file copy (Unpublished).
Wollenberg, H. L., 1911. Report on Salmon Creek Power
Project. September 23, 1909, Supplement March 5,
1910. AEL&P Co. files (Unpublished).
E -98
APPENDIX A: Persons Contacted During the Environmental
Investigation
G. o. Balding --u. s. Geological Survey
Ron Bolton --Planning Department, City & Borough
of Juneau
Corry Hildenbrand --Alaska Electric Light & Power
Company
Ken Imamura --Commercial Fisheries Division,
Alaska Department of Fish & Game
Tim Maguire --Planning Department, C&BJ
Dick Marriott Sport Fish Division, ADF&G
George Porter Public Works Department, C&BJ
Rich Reed --Habitat Section, ADF&G
Phil Schempf --u. s. Fish & Wildlife Service
David Stone --AEL&P Co.
Doug Swanston
Sara Thompson
u. s. Forest Service
Alaska Department of Natural
Resources
Alex Viteri --Alaska Department of Environmental
Conservation
Greg Young Salmon Creek Hatchery, Northern
Southeast Aquaculture Association
Dave Zimmerman --Game Division, ADF&G
E -99
APPENDIX 8:
November 11, 1981
NOTE TO FILES: Salmon Creek Road-Pipeline
FROM: Daniel M. Bishop
Environaid
Today Janice Mills and I walked up Salmon Creek to examine unstable
slopes and drainage paths along the route of the old tram. We did
this to evaluate the possible effects of the proposed road-pipeline
construction and installation upon the water quality of Salmon
Creek.
We systematically identified locations of respective slides-unstable
slopes along the tramway route, using the topographic survey
information provided by Toner & Nordling. Slopes were measured at
slide paths and soil-rock types were noted. This procedure was
continued until we reached the washed-out tram section at about
Station 45 (on north side of Creek, about 1/4 mile upstream from
bridge crossing).. .This was the last area examined. A tabular
summary of this examination is given below:
Location
38+00
to
39+00
39+00
to
40+00
40+00
to
42+00
Location,
base of
slope to
streambed
feet
50 -100
ca. 100
Slide
path
sloEe
%
60-80
50
Soil
Rock
1Y.E!:.
rotten
schist
schist,
so i 1 rna t • 1
weathered
schist
schist
E -100
Remarks,
Evaluation of
Water Quality
Hazard
Old trestle intact
but little water
flow; If roadbed
is cut into rock
with minimal side
casting, water
quality hazard may
be minimized.
Trestle broken by
old slide. Water
in. chute. Risk to
water quality, pipe
(if filled without
special measures).
Avoid problems by
benching on rock??
42+00 at stream 50-60 colluvial Risk to water qual-
to soil over ity, pipe (if
43+00 schist and filled without spe-
glacial till . , c1a..1. measures).
(rna rine)
46+00 200 55 colluvial Evidence of soil
to soil over creep along much of
47+00 probable tram route in this
till area. Sliding ap-
pears (from recent
alder growth) to
have occurred in
last decade. High
risk to water qual-
i ty.
48+00 200 65 schist, Soil slumping evi-
soil is dent in area. Risk
weathered to water quality.
schist
50+80-99 100 70 rotten schist Trestle intact.
to Slide path con tin-
52+00 ues to level of
streambed. High
risk to ·water
quality.
77+00 at stream 45-50 colluvial Originates below
soil over flume, where bed-
marine till rock shows. Drai-
nage and construe-
tion measures can
minimize risk.
82+00 at stream 50 Recent local slid-
ing with concentra-
ted stormflow. Can
be handled to min-
mize further risk.
95+00 at stream Near At toe of Good roadbed mater-
verti-old (500 ial likely unless
cal yrs.+) till hidden under-
to slide of neath. Do not
stream large rocks, foresee continued
boulders risk to water qual-
ity.
Summary: The road-pipeline route between about 38+00 and 52+00
involves numerous sect i osn of unstable slopes. In several
locations, the risk is high of losing the road-pipeline using
balanced cut-fill construction. Accordingly, risk of degrading
E -101
water quality would be high.
My guess is that the schist bedrock encountered along the route will
be fast-weathering if used as rock fill. If this is true, such
material might later prove unstable if used on slopes.
It should also be noted that Salmon Creek's bed and streambanks show
ample evidence of natural sediment load.
E -102
APPENDIX C: Alaska Gastineau Mining Company Streamflow and Stream
Height Records for:
C-1) Salmon Creek Dam Site, 1911-1914.
C-2) "In flume near penstock," 1914-1917.
C-3) "In Salmon Cr~ek near roundhouse," 1914-1917.
E -103
APPENDIX D: Alaska Historical Library Photographs
All are Winter and Pond photographs from the Emile Gastonguay
collection.
Figure 18:
Figure 17:
Figure 14:
Figure 16:
PCA-119-14. Powerhouse No. 1, looking east.
PCA-119-40. Small gas engine on Salmon Creek
tramway.
PCA-119-70. Trestle building and construction
camp.
PCA-119-88. Horse Car on the tramway.
Many pictures on the PCA-119 series microfiche show both
tramway and flume construction, from digging the bed to the
final wood work. Dates on most of the prints help provide a
time-frame of work. However, with vegetation changes, it is
difficult to identify the exact location of the photographs.
The library also holds some of the Alaska Electric Light and
Power Company collection of historical photographs.
E -104
APPENDIX E: Informant Data -Cultural Resources Survey
Throughout the course of the cultural resources survey
valuable information and help was given to the author. The
assistance was an important part of the project's success.
The following informants deserve due credit and a warm thank
you.
Byington, William -586-3557 -Thane
Ret ired A-J
tramway and
Byington is
cheerfully
Mining Engineer. Worked on Salmon CReek
flume after the purchase by the A-J. Mr.
a valuable source of information and he
provides good, accurate answers. The
following is a summary of information collected during
conversations with Mr. Byington.
Mr. Byington doubted any trestles were original due to
the use of untreated lumber. Trams were thought to be
original, he did not know of upgrading. The Model A
Ford reportedly went to the bottom of the hill each
night, which presented a vandalism problem. He could
not remember the exact name of track clamps used to stop
track spreading on corners; some were bought, some were
made. Double tracks were used as guard rails, primarily
on sharp turns. Double track cars gave best
flexibility. No recall of the tin building located at
upper switch yard. Mr. Byington remembers the stable
E -105
across the creek; they stored lumber for the flume
repairs there during his years with the A-J. He also
remembered seeing piles of slash and sawdust on the
north side of Salmon Creek near the tram crossing at
T-29. Mr. Byington thought the flume was rebuilt a
different size when the A-J replaced it in 1936,
although it carried about the same amount of water. In
the last years, the flume was kept half-full to relieve
the pressure and water was kept in the f1 ume to reduce
leakage. Sawdust was thrown into the flume to help plug
leaks and a power increase was noted. Ice buildups
during winter broke bracing and toppled a section of the
flume. The Model A was used to haul men up the drainage
but not down, as a company rule. Mr. Byington once had
the cable break and rode the Model A to the bottom --a
very fast ride!
Ohman, Gunnar and Lazzette -586-9403 -Juneau
Laz ze t te 1i ved in the Salmon Creek area in the 1920's
and 30's. She provided information about horses in the
area, the powerhouse, the road alignment and Warner's
Mining operations. She also talked of the Natives
coming out from town to catch and process salmon. She
recalled the location of local fishing on the point near
the present KJNO communication complex. It was also
learned that the lower incline tramway corridor provided
excellent blueberry picking.
E -106
Gunnar recalled the condition of the tramway from hiking
over it to go fishing at the reservoir. He remembers
good fishing and good hiking.
Stone, David-AEL&P Co., Author of Hard Rock~·
Mr. Stone and his employers, Alaska Electric Light and
Power Company, provided much help and information to the
author. Mr. Stone is currently curator of a vast,
historical collection of reports, maps, ledgers,
letters, books, photographs, and other memorabilia of
the Gastineau and A-J mining operations. The entire
collection is being preserved and stored in the original
vaults which are now owned by AEL&P Co. On my several
visits to his office, Mr. Stone was always willing to
stop working to locate research material or to share his
research material and insights on the operation of the
Salmon Creek power projects.
E -107
APPENDIX F
MEMORANDUM
ON
RECREATIONAL USES OF SALMON CREEK BASIN
AND PROJECT IMPACT ON THOSE USES
Historically, the Salmon Creek basin provides recreational
facilities to the Juneau Community in the area of hiking, fishing
and berry picking opportunities. On a very minor scale there are
hunting opportunities in the basin at certain periods of the year.
Access to the Lower Basin in the past has been mainly along the
tram and flume structures that are schedule~ for replacement under
this project. Access to the Upper Basin has been by trail and
along the pipeline from the Upper Salmon Creek Powerhouse to the
Salmon Creek Reservoir. -This latter area will not be impacted by
the project construction.
During the period of the project construction there will be a
definite impact on the recreational pedestrian access to both the
Lower and Upper Basins. This will be due to the efforts of the
construction contractor to keep the project area clear of the
general public in the interest of safety. The period of time
during which this condition will be experienced will be but a few
months and, given the topography of the basin, there is no
alternate access that can be provided that will mitigate this
temporary condition.
Upon completion of the project, access to and through the
Lower Basin will be improved very materially and should lead to an
increase in use by pedestrian-oriented members of the public.
This could also lead to an increase in the amount of vandalism
that may occur in the Salmon Creek Basin. Because of this
possibility as well as to insure the comfort and safety of
pedestrian traffic using the roadway, it is proposed that
vehicular traffic,· other . than liscensee service equipment and
emergency vehicles, be barred from using the roadway. This latter
condition was also requested by the City and Borough of Juneau
under their comments on the project.
That our description of both the present and future
E -109
recreational uses of the area is reasonable is borne out by a
recently completed recreational study of the City and Borough of
Juneau and the recommendations contained therein. The study was
titled "JUNEAU AREA RECREATION PLAN" and was conducted as a
cooperative effort by the following agencies:
Juneau Parks and Recreation Department
U. s. Forest Service
Alaska Dept. of Transportation and Public Facilities
Alaska Coastal Zone Management Program
Alaska Department of Environmental Conservation
Alaska Department of Fish and Game
Alaska Division of Parks, Department of Natural Resources
The study proposes no changes be made in the facilities presently
available to the public in the Salmon Creek Basin. In a phone
conversation with Bob Bosworth of the Alaska Division of Parks, we
were told thay had considered placement of camping units or cabins
at the reservoir site but had discarded the idea because of the
remoteness of the site as well as the past history of vandalism.
E -110
EXHIBIT F
EXHIBIT F
APPLICATION FOR AMENDMENT OF LICENSE
FERC LICENSE NO. 2307
ALASKA ELECTRIC LIGHT AND POWER CO.
GENERAL DESIGN DRAWINGS
The drawings required for submittal under Exhibit F have
been developed on one standard sheet. On it are set forth
the general layout of the project and a series of typical
sections indicating the construction methods and practices
that will be utilized in constructing the roadway and
installing the pipeline.
The drawing is labelled "Exhibit F" and is attached
hereto.
F -2
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LOWER POWERHOUSE
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S .33 55'26" E-314.35' -~
(RECORD: S 33°55' E -314 .82' )
M S 96 8
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COR . NO . 7
uss 3824
ALL IN T41S, R67E CRM
( PROTRACTED SECTION_$ l
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SCALE DETAIL OF SURVEY TIE
500 1000 FEET NO SCALE • --------------
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~' 1. RO .W. TO BE 50 ' IN WIOTH ON EACH
S lO E OF AOADWA Y CENTERLINE .
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2. CENTERLIN E DESCRIPTION OF ROADWAY IS
A T TACHED TO A PPLICATION AS • ATTACHMENT NO . 1 •
3 . ALL LANDS TRAVERSED BY THE PROPOSED ROAD AND
PIPELINE ARE FEDERAL LANDS ADMINISTERED BY THE
BUREAU OF LANO MANAGMENT. MS 955 AND MS 968
ARE MINING CLAIMS HELD BY LOCATION.
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PLATE 1. PLAN -PROFILE
KEUFFEL a. ESSER CO.
'
---------------BORROW EMBANKM E NT
~ C .M.P . CULV E RT
-\ ''O"'J~.%:~~;zt.4
EXISTIN G '::: AAOE -~ ..
DETAIL A-A
NO SCALE
(!
2 "X6"
4"X4"
0' 1 .0'
---FINISH GRAD E
EXISTING GRADE
,
TYPICAL CUT SECTION WI FULLY BURIED PIPE
NO SCALE
1 1 .o ' 1 , .0'
COVER FILL .
-FINISH GRADE
R l r-RAP EMBA N KMENT
SA LM O N C R EEK
1 .0 'I.
ROW EMBANKMENT .7
............---C .M .P . C UL VERT
' ' -.
EXISTING GRADE
ON STEEP SLOPES PLACE ROCK
BLANKET TO PREVENT EROSION
TYPICAL FILL SECTION W/ HALF BURIED PIPE
NO SCALE
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SMALL S T REAM ..
BRIDGE DETAILS
SCALE: 1 "=10 '
DECK 3" X 12" S1S1E TREATED TIMBER
CAP 12" X 14" TREATED TIMBER
iTRINGERS 12" W.F . ® 27#
I· 20 · I
~LASKA ELECTRIC LIGHT & POWER CO .
2 "X4'" JUNEAU, ALASKA
'
EXHIBIT ' LOWER SALMON CREEK REHABILITATION PROJECT
GENERAL PLAN & CONSTRUCTION DETAILS F
TONER & NORDLING, REGISTERED ENGINEERS, INC.
JUNEAU, ALASKA
3" X 12"
( ' 1--. =::::,J
~-,=;-._ 3"X8 " BOLT TO 12' W.F. 1-------------,r-----------T-------------t
3"X 10" BOLT TO 12" W .F.
DETAIL B-B
NO SCALE
DATE : 6-4-82 SCALE: I" = 500' DR . NO . SC-8 181
EXHIBIT G
EXHIBIT G
APPLICATION FOR AMENDMENT OF LICENSE
FERC LICENSE NO. 2307
ALASKA ELECTRIC LIGHT AND POWER CO.
The standard sheet attached as Exhibit G indicates the
layout of the project with respect to the Federal Lands
involved. The R. 0. W. required for construction of the
project has been applied for from the Bureau of Land
Management. In the case of the Salmon Creek area the Federal
lands in that area are all within the limits of the Juneau
Townsite Elimination and are administered by the Bureau of
Land Management.
In our conversations with the Bureau of Land Management
personnel while preparing the application for a Right of Way,
we were advised that the actual granting of the Right of Way
would be keyed to the granting of an amendment to the license
by FERC. They indicated that this was a policy normally
followed by the Bureau of Land Management in such matters.
The legal description of the Right of Way applied for is
as follows:
CENTERLINE DESCRIPTION OF PROPOSED ROAD RIGHT OF WAY
PROPOSED LOWER SALMON CREEK POWER PROJECT
Beginning at Sta. 0+00, from whence Cor. No. 7 of USS 2133
bears N 6° 19' 57" E, 457.22 ft. distant; thence N 21° 56' E,
1,038.36 ft. to PC10+38.36; thence a+ong a 30° curve to the
G - 2
left with a central angle of 28° 24', an arc length of 94.67
ft. to PT11+33.03; thence N 6° 28' W, 304.91 ft. to
PC 14+3 7. 94; thence along as 30° curve to the left with a
central angle of 16° 46' , an arc length of 55.8 9 ft. to
PT14+93.83; thence N 23° 14' w, 106.02 ft. to PC15+99.85;
thence alon~ a 91.6758° curve to the right with a central
angle of 93 11', an arc length of 101.64 ft. to PT17+0l.49;
thence N 69° 57' E, 284.12 ft. to PC19+85.61; thence along a
30° curve to the· right with a central angle of 36° 12', an
arc length of 120.61 ft. to PT21+06.22; thence S 73° 52' E,
43.78 ft. to POT21+50 (POT19+81.53 stationing ahead); thence
S 73° 52' E, 430.20 ft. to PC24+1l. 74; thence along a 12°
curve to the left with a central angle of 47° 55', an arc
length of 399.31 ft. to PT28+11.05; thence N 58° 13' E,
132.96 ft. to PC29+44.01; thence along a 9.1628° curve to the
right with a central angle of 9° 49', an arc length of 107.14
ft. to PT30+51.15; thence along a 92.4333° curve to the left
with a central angle of 104° 28', an arc length of 113.02 ft.
to PT31+64.17; thence N 36° 26' W, 35.91 ft. to PC32+00.08;
thence along a 40° curve to the right with a central angle of
42° 06', an arc length of 105.25 ft. to PT33+05.33; thence N
5° 40' E, 179.38 ft. to PC34+84.71 (PC34+71.08 stationing
ahead); thence along a 20° curve to the right with a central
angle of 31° 33', an arc length of 157.75 ft. to PT36+28.83;
thence N 37° 13' E, 22.66 ft. to PC36+51.49; thence along a
91.6667° curve to the right with a central angle of 91° 09',
an arc length of 99.44 ft to PT37+50.93; thence along an
88.5333° curve to the left with a central angle of 67° 37',
an arc length of 76.37 ft. to PT38+27.30; thence along a 47°
curve to the right with a central angle of 24° 14', an arc
length of 51.56 ft. to PT38+78.86; thence N 83° 59' E, 10.89
ft. to PC38+8 9. 7 5; thence along a 10° curve to the left with
a central angle of 11° 40', an arc length of 116.67 ft. to
PT40+06.42; thence N 72° 19' E, 6.26 ft. to PC40+12.68;
thence along a 40° curve to the right with a central angle of
40° 02', an arc length of 100.08 ft. to PT41+12. 76; thence S
67° 39' E, 72.31 ft. to PC41+85.07 (PC41+68.35 stationing
ahead); thence along a 20° curve to the left with a central
angle of 23° 53', an arc length of 119.42 ft. to PT42+87.77;
thence N 88° 28' E, 88.45 ft. to PC43+76.22; thence along a
30° curve to the left with a central angle of 61° 42', an arc
length of 205.67 ft. to PT45+81.89; thence N 26° 46' E, 2.69
ft. to PC45+84.58; thence along a 22.5333° curve to the right
with a central angle of 17° 57', an arc length of 79.66 ft.
to PT46+64.24; thence N 44° 43' E, 512.79 ft. to PC51+77.03;
thence along a 30° curve to the·right with a central angle of
41° OS', an arc length of 136.94 ft. to PT53+13.97; thence N
85° 48 1 E, 19.41 ft. to PC53+33.38; thence along a 120 curve
to the right with a central angle of 15° 37', an arc length
of 130.14 ft. to PT54+63.52; thence S 78° 35' E, 122.41 ft.
to PC55+85.93; thence along a 20° curve to the right with a
central angle of 30° 55', an arc length of 154.58 ft. to
PT57+40.51; thence S 47° 40' E, 95.32 ft. to PC58+35.83;
thence along a 40° curve to the right with a central angle of
G - 3
30° 08', an arc length of 75.33 ft. to PT59+ll.l6; thence S
170 32' E, 146.16 ft. to PC60+57.32; thence along a 4QO curve
·to the left with a central angle of 71° 15', an arc length of
178.13 ft. to PT62+35.45; thence S 88° 47' E, 98.97 ft. to
PC63+34.42; thence along a 15° curve to the left with a
central angle of 23° 40', an arc length of 157.78 ft. to
PT64+92.20; thence N 67° 33' E, 104.91 ft. to PC65+97.ll;
thence along a 15° curve to the left with a central angle of
26° 36', an arc length of 177.33 ft. to PT67+74.44; thence N
40° 57' E, 198.43 ft. to PC69+72.87; thence along a 30° curve
to the left with a central angle of 37° 29', an arc length of
124.94 ft. to PT70+97.81; thence N 3° 28' E, 24.07 ft. to
PC71+21.88; thence along al5° curve to the right with a
central angle of 15° 19', an arc length of 102.11 ft. to
PT72+23.99; thence N 18° 47' E, 10.26 ft. to PC72+34.25;
thence along a 25° curve to the right with a central angle of
31° 10'. an arc length of 124.67 ft. to PT73+58.92; thence N
49° 57' E, 88.62 ft. to PC74+47.54; thence along a 46.8167°
curve to the left with a central angle of 28° 50', an arc
length of 61.59 ft. to PT75+09.13; thence along a 34° curve
to the right with a central angle of 52° 24', an arc length
of 154.12 ft. to PT76+63.25; thence N 73° 31' E, 23.91 ft. to
PC7 6+87 .16; thence along a 14° curve to the left with a
central angle of 11° 31', an arc length of 82.26 ft. to
PT77+69.42; thence N 62° E, 9.01 ft. to PC77+78.43; thence
along a 36° curve to the right with a central angle of 50°
43', an arc length of 140.88 ft. to PT79+19.31; thence S 67°
17' E, 52.38 ft. to PC79+71. 69; thence along a 30° curve to
the left with a central angle of 43° 16', an arc length of
144.22 ft. to PT81+15.91; thence N 69° 27' E, 69.76 ft. to
PC81+85.67 (PC81+77.07 stationing ahead); thence along a 20°
curve to the left with a central angle of 14° 31', an arc
length of 72.58 ft. to PT82+49.65; thence N 54° 56' E, 39.41
ft. to PC82+89.06; thence along a 70.1833° curve to the left
with a central angle of 52°. 51', an arc length of 74.24 ft.
to PC83+63. 30; thence N 2° 05' E, 89.21 ft. to PC84+52. 51
(PC84+43. 77 stationing ahead); thence along a 15° curve to
the right with a central angle of 20° 46', an arc length of
138.44 ft. to PT85+82.21; thence N 22° 51' E, 67.67 ft. to
PC86+49. 88; thence along a 25° curve to the right with a
central angle of 29° 16', an arc length of 117.07 ft. to
PT87+66.95; thence N 52° 07' E, 32.23 ft. to PC87+99.18;
thence along a 30° curve to the right with a central angle of
22° 14', an arc length of 74.11 ft. to PT88+73.29; thence N
74° 21' E, 47.23 ft. to PC89+20.53; thence along a 10° curve
to the left with a central angle of 12° 13', an arc length of
122.17 ft. to PT90+42.69; thence N 62° 08' E, 115.39 ft. to
PC91+58. 08; thence along an 18° curve to the right with a
central angle of 34° 35', an arc length of 192.13 ft. to
PT93+50.21; thence S 83° 17' E, 31.78 ft. to PC 93+81.99;
thence along a 10° curve to the left with a central angle of
23° 03', an arc distance of 230.50 ft. to PT96+12.49; thence
N 73° 40' E, 247.84 ft. to PC98+60.33; thence along a 15°
curve to the right with a central angle of 31° 40', an arc
G -4
length of 211.11 ft. to PT100+71.44; thence S 740 40' E,
357.23 ft. to PC104+28.67; thence along a 100 curve to the
left with a central angle of 170 54', an arc length of 179.00
ft. to PT106+07.67; thence N 87° 26' E, 178.03 ft. to
POT107+85.70; and containing in all 24.76 Acres, more or
less.
G - 5
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CONC. MON.
MS 968
BLM MON .
1~ uss 3824
50' 0
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~~~
;; DETAIL OF SURVEY TIE SCALE
500 0 500 1000 FEET
NO SCALE ------------- -
0+00
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N.B.:
I
1. R .O.W. TO BE 50' IN WIDTH ON EACH
SIDE OF ROADWAY CENTERLINE.
-
2 . CENTERLINE DESCRIPTION OF ROADWAY IS
ATTACHED TO APPLICATION AS • ATTACHMENT NO. 1 '
3. ALL LANDS TRAVERSED BY THE PROPOSED ROAD AND
PIPELINE ARE FEOJERAL LANDS ADMINISTERED BY THE
BUREAU OF LAND MANAGMENT. MS 955 AND MS 968
ARE MINING CLAIMS HELD BY LOCATION.
"' N
"'
I~ I ~~~~ 1~ I l~ I 01~
--t-
~¢~ PLATE 1, PLAN-PROFILE
1(1'11FFI'1 .t I'COCOI'O rn
_,. ---------------\ BORROW EMBANKMENT ~
~ C.M.P. CULVERT ~-~'%hit'Q~WkW
EXISTING ( AAOE
DETAIL A-A
NO SV#\Ll::
......
,~'
0'
-2-0%
2.o •
)#?"' ·~
42" PIPE_)-J
11.0'
~-~-FINISH GRADE
2.0%-.....
I
EXISTING GRADE __;
~
RIP -RAP EMBANK*'eNT
SALMON CREEK
fli'W'i)
TYPICAL CUT SECTION W/ FULLY BURIED PIPE j 3.o•,
NO SCALE
11.0' 1 , .0'
COVER FILL
1.0 ' -:f2 I \1-FINISH GR ADE
..
,
~~ ~: .. :1-P~~_---2.0%~
~BO~ROW EMBANKMENT
(
Q
\\
\\
I I;
I; c
~~ .7 '· .,
,\\ J?
EXISTING GRADE
'/ "' ,------C.M.P. CULVERT
\ ~SMALL STREAM
\
-'S-
..
ON STEEP SLOPES PLACE ROCK
BLANKET TO PREVENT EROSION
~~~~ --
TYPICAL FILL SECTION W/ HALF BURIED PIPE
NO SCALE
t -til
I I
II I I: '
I I ~
B
50'
iJ
ll
_j
,
\
~
BRIDGE DETAILS
SCALE: 1''=10'
DECK 3" X 12" S1S1E TREATED TIMBER
CAP 12" X 14" TREATED TIMBER
tTRINGERS 12" W.F. e 27 ..
20· 1
(i---_ --,::-_:-::--_-_ -==-=----,--.---~~-I' M·~< 41 II II 1t jf 41 ~ 16 j~
I 42" PIPE>
a·· -\
2 "X6"~
I
4"X4 "
2"X4"
3" X 12"
CLASS (A) PRESSURE
TREATED CREOSOTE PILIIIG·
AL ASKA ELECTRIC LIGHT & POWER CO.
.JUNEAU, ALASKA
• LOWER SALMON CREEK REHABILITATION PROJECT
GENERAL PROJECT MAP
,7~;-;-,~'
EXHIBIT
G
TONER & NORDLING, REGISTERED ENGINEERS, INC .
.JUNEAU , ALASKA
3"X8" BOLT TO 1 2• W.F. 1--------------r-------------.... --------------f
3"X10" BOLT TO 12" W.F.
DETAIL B-B
NO SCALE
DATE: 6-4-82 SCALE : I" = 500' OR. NO . SC-8182