The heavy precipitation and runoff, suitable storage sites near tidewater, and steep stream gradients are favorable to the development of hydroelectric power on the streams considered in this report. A geologic examination of the sites indicates that their development would not be hindered by any unusual geologic conditions.
On the basis of the 18 years of available stream-flow records for Cascade Creek, it is estimated that 20,800 kilowatts of power could have been generated continuously on Cascade Creek; 13,300 kilowatts on Scenery Creek, and 7,900 kilowatts on Delta Creek. Conditions for power development on Delta Creek are not as favorable as on Cascade Creek or Scenery Creek in view of the size of the structures required in relation to the potential power.
The development of a substantial part of this power would depend upon the creation of new industries as the present power market is very limited. There is a heavy growth of timber near tidewater throughout this part of Alaska, and the utilization of this timber in the manufacture of wood pulp is the most likely industrial possibility.
The Cascade Creek, Scenery Creek, and Delta Creek drainage basins are in rugged mountainous terrain. There is little land in the immediate vicinity suitable for the location of industrial developments and the supporting communities, and the power would have to be transmitted to a more favorable area. A considerable area is available near Point Agassiz on Frederick Sound about 10 air-line miles from the mouth of Scenery Creek and 5 airline miles from the mouth of Delta Creek.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i230","usgsCitation":"Pillmore, C.L., and McQueen, K., 1956, Map of Salt Chuck area, Prince of Wales Island, Alaska showing linear features as seen on aerial photographs: U.S. Geological Survey IMAP 230, Report: 1 p.; 1 Plate: 30.03 x 35.31 inches, https://doi.org/10.3133/i230.","productDescription":"Report: 1 p.; 1 Plate: 30.03 x 35.31 inches","costCenters":[],"links":[{"id":420798,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1396.htm","linkFileType":{"id":5,"text":"html"}},{"id":256095,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0230/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256096,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0230/report-thumb.jpg"},{"id":256094,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0230/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":111150,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/13587","linkFileType":{"id":5,"text":"html"}}],"scale":"12000","country":"United States","state":"Alaska","otherGeospatial":"Prince of Wales Island, Salt Chuck area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -132.4658,\n 55.6833\n ],\n [\n -132.4658,\n 55.5777\n ],\n [\n -132.3761,\n 55.5777\n ],\n [\n -132.3761,\n 55.6833\n ],\n [\n -132.4658,\n 55.6833\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656b77","contributors":{"authors":[{"text":"Pillmore, C. L.","contributorId":46093,"corporation":false,"usgs":true,"family":"Pillmore","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":275153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McQueen, Kathleen","contributorId":66352,"corporation":false,"usgs":true,"family":"McQueen","given":"Kathleen","email":"","affiliations":[],"preferred":false,"id":275154,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":51918,"text":"ofr5676 - 1956 - Chemical character of the public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico, 1954","interactions":[{"subject":{"id":51918,"text":"ofr5676 - 1956 - Chemical character of the public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico, 1954","indexId":"ofr5676","publicationYear":"1956","noYear":false,"title":"Chemical character of the public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico, 1954"},"predicate":"SUPERSEDED_BY","object":{"id":2143,"text":"wsp1460A - 1954 - Chemical character of public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico","indexId":"wsp1460A","publicationYear":"1954","noYear":false,"chapter":"A","title":"Chemical character of public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico"},"id":1}],"supersededBy":{"id":2143,"text":"wsp1460A - 1954 - Chemical character of public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico","indexId":"wsp1460A","publicationYear":"1954","noYear":false,"title":"Chemical character of public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico"},"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr5676","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"56-76","title":"Chemical character of the public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico, 1954","language":"ENGLISH","doi":"10.3133/ofr5676","usgsCitation":"Lohr, E.W., 1956, Chemical character of the public water supplies of the larger cities of Alaska, Hawaii, and Puerto Rico, 1954: U.S. Geological Survey Open-File Report 56-76, 39 p., https://doi.org/10.3133/ofr5676.","productDescription":"39 p.","costCenters":[],"links":[{"id":177523,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e474d","contributors":{"authors":[{"text":"Lohr, E. W.","contributorId":48155,"corporation":false,"usgs":true,"family":"Lohr","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":244474,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71601,"text":"tei577 - 1956 - Summary of reconnaissance for radioactive deposits in Alaska, 1945-1954, and an appraisal of Alaskan uranium possibilities","interactions":[],"lastModifiedDate":"2014-06-19T06:56:36","indexId":"tei577","displayToPublicDate":"1957-01-01T09:47:09","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"577","title":"Summary of reconnaissance for radioactive deposits in Alaska, 1945-1954, and an appraisal of Alaskan uranium possibilities","docAbstract":"In the period 1945-1954 over 100 investigations for radioactive source materials were made in Alaska. The nature of these investigations ranged from field examinations of individual prospects or the laboratory analysis of significantly radioactive samples submitted by prospectors to reconnaissance studies of large districts. In this period no deposits of uranium or thorium that would warrant commercial exploitation were discovered. The investigations, however, disclosed that radioactive materials occur in widely scattered areas of Alaska and in widely diverse environments.
\nMany igneous rocks throughout Alaska are weakly radioactive because of uranium- and thorium-bearing accessory minerals, such as allanite, apatite, monazite, sphene, xenotime, and zircon; more rarely the radioactivity of these rocks is due to thorianite or thorite and their uranoan varieties. The felsic rocks, for example, granites and syenites, are generally more radioactive than the mafic igneous rocks. Pegmatites, locally, have also proved to be radioactive, but they have little commercial significance. No primary uranium oxide minerals have been found yet in Alaskan vein deposits, except, perhaps, for a mineral tentatively identified as pitchblende in the Hyder district of southeastern Alaska. However, certain occurrences of secondary uranium minerals, chiefly those of the uranite group, on the Seward Peninsula, in the Russian Mountains, and in the vicinity of Kodiak suggest that pitchblende-type ores may occur at depth beneath zones of alteration. Thorite-bearing veins have been discovered on Prince of Wales Island in southeastern Alaska.
\nAlthough no deposits or carnotite-type minerals have been found in Alaska, several samples containing such minerals have been submitted by Alaskan prospectors. Efforts to locate the deposits from which these minerals were obtained have been unsuccessful, but review of available geologic data suggests that several Alaskan areas are potentially favorable for carnotite-type deposits. The chief of these areas is the Alaska Peninsula-Cook Inlet area which encompasses most of the reported occurrences of the prospectors' carnotite-type samples.
\nAlaska is also potentially favorable for the occurrence of large bodies of the very low-grade uraniferous sedimentary rocks, such as phosphorites and black shales. This type of deposit, however, has not received much study because of the emphasis on the search for bonanza-type high-grade ores. Uraniferous phosphorites similar to those of Idaho, Montana, and Wyoming occur in northern Alaska on the north flank of the Brooks Range; black shales comparable to the uraniferous shales of the Chattanooga formation of southeastern United States have been noted along the Yukon River near the international boundary.
\nPlacer deposits in Alaska have some small potential for the production of the radioactive elements as byproducts of gold- and tin-placer mining. the placer area believed to have the relatively greatest potential in Alaska lies in the Kahiltna River valley where concentrates are known to contain such commercial minerals as ilmenite, cassiterite, platinum, and gold in addition to uranothorianite and monazite.
\nThe possibilities of the natural fluids--water and petroleum--have not yet been tested in Alaska to any great extent. Studies of fluids are in progress to determine whether they may be used to discover and define areas potentially favorable for the occurrence of uraniferous lodes.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei577","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Wedow, H., 1956, Summary of reconnaissance for radioactive deposits in Alaska, 1945-1954, and an appraisal of Alaskan uranium possibilities: U.S. Geological Survey Trace Elements Investigations 577, Report: 111 p.; Plate: 19.12 x 13.83 inches, https://doi.org/10.3133/tei577.","productDescription":"Report: 111 p.; Plate: 19.12 x 13.83 inches","numberOfPages":"112","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":288869,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0577/report.pdf"},{"id":288868,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0577/plate-1.pdf"},{"id":288870,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.45,51.21 ], [ 172.45,71.39 ], [ -129.99,71.39 ], [ -129.99,51.21 ], [ 172.45,51.21 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae784ae4b0abf75cf2d03c","contributors":{"authors":[{"text":"Wedow, Helmuth Jr.","contributorId":14374,"corporation":false,"usgs":true,"family":"Wedow","given":"Helmuth","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":284456,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220709,"text":"70220709 - 1956 - Wind-induced stone tracks, Prince of Wales Island, Alaska","interactions":[],"lastModifiedDate":"2021-05-25T13:47:59.278681","indexId":"70220709","displayToPublicDate":"1956-05-25T08:43:20","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Wind-induced stone tracks, Prince of Wales Island, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1956)67[1659:WSTPOW]2.0.CO;2","usgsCitation":"Sainsbury, C., 1956, Wind-induced stone tracks, Prince of Wales Island, Alaska: GSA Bulletin, v. 67, no. 12, p. 1659-1660, https://doi.org/10.1130/0016-7606(1956)67[1659:WSTPOW]2.0.CO;2.","productDescription":"2 p.","startPage":"1659","endPage":"1660","costCenters":[],"links":[{"id":385926,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Wales Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -133.87939453125,\n 54.60389191417926\n ],\n [\n -131.72607421875,\n 54.60389191417926\n ],\n [\n -131.72607421875,\n 56.206703980680814\n ],\n [\n -133.87939453125,\n 56.206703980680814\n ],\n [\n -133.87939453125,\n 54.60389191417926\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"67","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":816434,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048293,"text":"tem357 - 1956 - Radiometric traverse along the Yukon River from Fort Yukon to Ruby, Alaska, 1949","interactions":[],"lastModifiedDate":"2014-03-04T13:37:08","indexId":"tem357","displayToPublicDate":"1956-01-01T14:07:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"357","title":"Radiometric traverse along the Yukon River from Fort Yukon to Ruby, Alaska, 1949","docAbstract":"In 1949, a radiometric traverse was made of rocks exposed along the banks of and near the Yukon River about Fort Yukon to Ruby, Alaska. Granitic rocks of Tertiary age and of Devonian or Carboniferous age and sandstone beds of Cretaceous age gave the highest readings obtained in the field. Other rock types examined were greenstone of Devonian or Carboniferous age and metamorphic rocks of Devonian and pre-Devonian age, sedimentary rocks, and liginite of Tertiary age, and alluvial deposits of Quaternary age. The most radioactive sample, from Melozitna River canyon, contained only 0.017 percent equivalent uranium.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem357","collaboration":"The report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"White, M., Stevens, J.M., and Matzko, J., 1956, Radiometric traverse along the Yukon River from Fort Yukon to Ruby, Alaska, 1949: U.S. Geological Survey Trace Elements Memorandum 357, 14 p., https://doi.org/10.3133/tem357.","productDescription":"14 p.","numberOfPages":"17","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277930,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0357/report-thumb.jpg"},{"id":283236,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0357/report.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"Yukon River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155.7095,64.6876 ], [ -155.7095,66.0817 ], [ -148.8671,66.0817 ], [ -148.8671,64.6876 ], [ -155.7095,64.6876 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523c1cf9e4b024b60d407385","contributors":{"authors":[{"text":"White, Max G.","contributorId":22426,"corporation":false,"usgs":true,"family":"White","given":"Max G.","affiliations":[],"preferred":false,"id":484256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stevens, John M.","contributorId":18746,"corporation":false,"usgs":true,"family":"Stevens","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":484255,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Matzko, John J.","contributorId":79459,"corporation":false,"usgs":true,"family":"Matzko","given":"John J.","affiliations":[],"preferred":false,"id":484257,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":39752,"text":"pp305A - 1956 - Core tests and test wells, Oumalik area, Alaska, with paleontology of test wells and core tests in the Oumalik area, Alaska","interactions":[],"lastModifiedDate":"2023-11-27T22:19:57.786548","indexId":"pp305A","displayToPublicDate":"1956-01-01T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"305","chapter":"A","title":"Core tests and test wells, Oumalik area, Alaska, with paleontology of test wells and core tests in the Oumalik area, Alaska","docAbstract":"No abstract available.
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