12.07.2015 Views

Electrical Power for Valdez and the Copper River Basin-1981

Electrical Power for Valdez and the Copper River Basin-1981

Electrical Power for Valdez and the Copper River Basin-1981

SHOW MORE
SHOW LESS
  • No tags were found...

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

alternative has been estimated to provide sufficient energy to <strong>the</strong> studyarea until about 1995. When <strong>the</strong> power generated from <strong>the</strong> PRT terminates,an intertie with <strong>the</strong> Anchorage-Fairbanks area may be feasible.C. AFFECTED ENVIRONMENT1. Physicala. General: Two specific sites are possible <strong>for</strong> development; <strong>the</strong>Lowe <strong>River</strong> flats <strong>and</strong> Allison Creek.The proposed PRT site lies at <strong>the</strong> head of Port <strong>Valdez</strong> on <strong>the</strong> south sideof Lowe <strong>River</strong>. The valley is of glacial origin <strong>and</strong> is filled with outwashaeposits of <strong>the</strong> <strong>Valdez</strong> <strong>and</strong> Corbin glaciers. The site is bounded on<strong>the</strong> north by <strong>the</strong> Lowe <strong>River</strong>, <strong>and</strong> south by <strong>the</strong> Chugach Mountains.Allison Lake is located on <strong>the</strong> south side of Port <strong>Valdez</strong>, directly acrossfrom <strong>the</strong> present city of <strong>Valdez</strong>, filling approximately one half of aglacier <strong>for</strong>med hanging valley. Allison Creek, which originates atAllison Lake, decends 1,360 feet in 2-1/4 miles to Port <strong>Valdez</strong>. It is anextremely high graaient stream <strong>for</strong> <strong>the</strong> first 2 miles with <strong>the</strong> lastquarter mile leveling considerably.The area is underlain geologically by <strong>the</strong> late Cretaceous Valaez Group, aseries of metagraywackes, shales <strong>and</strong> slates with occasional beds ofpillow basalt. This is indicative of a rapid, unsorted deposition in anocean environment. The beds are highly disturbed <strong>and</strong> no regionalstructures have yet been defined.The Port <strong>Valdez</strong> area is located in Seismic Zone 4, approximately 46 mileseast of <strong>the</strong> epicenter of <strong>the</strong> 27 March 1964 earthquake. Prior to 1964,<strong>the</strong>re were approximately 70 earthquakes, magnitude 5 or greater, in <strong>the</strong><strong>Valdez</strong> vicinity.Excluding <strong>the</strong> 1964 earthquake, magnitude 5 earthquakes have averagedapproximately one per year. Magnitude 8 or greater events have occurredthree times this century, consequently, <strong>the</strong>re is a good probability of alarge earthquake occurring during <strong>the</strong> life of <strong>the</strong> project.There has been no evidence of ruptures in area bedrock. Most destructionin port <strong>Valdez</strong> has been causea by tsunami <strong>and</strong> submarine mass movement ofunconsolidated Lower <strong>River</strong> delta deposits.The site <strong>for</strong> <strong>the</strong> proposed powerhouse (Alternate #2) is located at <strong>the</strong> 100foot elevation. <strong>Power</strong>house Alternate #1, located on delta deposits at<strong>the</strong> 20 foot elevation has been dismissed from fur<strong>the</strong>r consideration. Thedelta deposits would make good foundation material <strong>for</strong> a small surfacepowerplant; however, <strong>the</strong> area may be subject to tsunami to an elevationof +85 MLLW. During slide induced sea waves, runup at Anderson Bay, 7miles west of Allison Creek, was measured at 70 feet. Measurements atShoup Bay (Cliff Marine) on <strong>the</strong> north side of <strong>the</strong> arm show a runup of 170feet. No runup measurements were made at Jackson Point or Fort Liscum,but <strong>the</strong> cannery at Jackson Point was destroyed.EIS-3

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!