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Off.,","doi":"10.3133/b1187","usgsCitation":"Sainsbury, C., and MacKevett, E., 1965, Quicksilver deposits of southwestern Alaska a description of the quicksilver mines and prospects, with special emphasis on the structural controls of ore deposition: U.S. Geological Survey Bulletin 1187, vi, 89 p. :illus., maps (8 fold. col. in pocket) ;24 cm., https://doi.org/10.3133/b1187.","productDescription":"vi, 89 p. :illus., maps (8 fold. col. in pocket) ;24 cm.","costCenters":[],"links":[{"id":166677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1187/report-thumb.jpg"},{"id":63620,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1187/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63621,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1187/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63622,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1187/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63623,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1187/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63624,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1187/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63625,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1187/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63626,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1187/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63627,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1187/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63628,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a049","contributors":{"authors":[{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":215102,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacKevett, E.M. Jr.","contributorId":58613,"corporation":false,"usgs":true,"family":"MacKevett","given":"E.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":215101,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70112253,"text":"70112253 - 1965 - Photointerpretation of Alaskan post-earthquake photography","interactions":[],"lastModifiedDate":"2017-03-27T13:40:15","indexId":"70112253","displayToPublicDate":"1990-06-12T09:35:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3051,"text":"Photogrammetric Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Photointerpretation of Alaskan post-earthquake photography","docAbstract":"

Aerial photographs taken after the March 27, 1964, Good Friday, Alaskan earthquake were examined stereoscopically to determine effects of the earthquake in areas remote from the towns, highways, and the railroad. The two thousand black and white photographs used in this study were taking in April, after the earthquake, by the U. S. Coast & Geodetic Survey and were generously supplied to the U. S. Geological Survey. Part of the photographs, at a scale of 1/24,000, provide blanket coverage of approximately 2,000 square miles of land area north and west of Prince William Sound, including parts of the mainland and some of the adjacent islands. The epicenter of the earthquake, near the head of Unakwik Inlet, is located in this area. The rest of the photographs, at scales ranging from 1/17,000 to 1/40,000, cover isolated strips of the coastline of the mainland and nearby islands in the general area of Prince William Sound.

\n
\n

Figure 1 shows the area of new photo coverage used in this study. The objective of the study was to determine quickly whether geological features resulting from the earthquake, such as faults, changes in shoreline, cracks in surficial material, pressure ridges in lake ice, fractures in glaciers and lake ice, and rock slides and avalanches, might be identifiable by photointerpretation. The study was made without benefit of comparisons with older, or pre-earthquake photography, which was not readily available for immediate use.

","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Hackman, R., 1965, Photointerpretation of Alaskan post-earthquake photography: Photogrammetric Engineering, v. 31, no. 4, p. 604-610.","productDescription":"7 p.","startPage":"604","endPage":"610","numberOfPages":"7","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288442,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150.0122,59.6906 ], [ -150.0122,61.8408 ], [ -144.9482,61.8408 ], [ -144.9482,59.6906 ], [ -150.0122,59.6906 ] ] ] } } ] }","volume":"31","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc05e4b0e83db6d08f77","contributors":{"authors":[{"text":"Hackman, R.J.","contributorId":95086,"corporation":false,"usgs":true,"family":"Hackman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":686346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70197612,"text":"70197612 - 1965 - Ordovician, Silurian, and Devonian biostratigraphy of east-central Alaska","interactions":[],"lastModifiedDate":"2023-02-01T14:25:21.059833","indexId":"70197612","displayToPublicDate":"1965-12-31T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Ordovician, Silurian, and Devonian biostratigraphy of east-central Alaska","docAbstract":"

A predominantly shale and chert sequence has been mapped from the Canadian border at Latitude 65°00′ N. to the Nation River about 25 miles northwest. It has Ordovician and Silurian graptolites in the lower half, and Middle Devonian corals and Upper Devonian spores in the upper half.

The lower half of the sequence consists of about 400 to 900 feet of predominantly dark gray graptolitic shale with lesser amounts of grayish black laminated chert. This unit has been traced by Green and Roddick from the international border southeastward into the Dawson area of the Yukon Territory and northeastward into the Ogilvie and Richardson Mountains where it has been mapped by Jackson & Lenz, Norris, and others as the Road River Formation. In the Tatonduk-Nation Rivers area the Road River Formation rests disconformably on a sequence of Middle and Upper Cambrian limestone that locally may include Lower Ordovician (Tremadoc) beds at its top. The sequence of graptolite faunas from the Road River Formation in Alaska is essentially the same as the graptolite zones established by Elles and Wood in Great Britain. All the standard series of the Ordovician and Silurian are probably represented in the formation with the exception of the Tremadoc and possibly the Arenig and Wenlock.

Overlying the Road River Formation is a formation, 200 to 800 feet thick, consisting predominantly of thinly bedded and laminated light gray to black chert and siliceous shale that is here named the McCann Hill Chert. This new formation disconformably overlies the Road River Formation, and its lower boundary is at the base of a distinctive limestone and shale member. The basal limestone and shale member of the McCann Hill Chert contains a remarkably varied fauna including corals, brachiopods, trilobites, conodonts, ostracods, and fish of Eifelian (early Middle Devonian) age. Spores from the upper part of the formation resemble those from the overlying Nation River Formation and indicate a Late Devonian age. The McCann Hill Chert is conformably overlain by the Nation River Formation—a thick succession of inter-bedded graywacke, chert conglomerate, and silty shale of Late Devonian age.

In the vicinity of Jones Ridge, only 7 miles north of exposures of the Road River Formation, Upper Cambrian limestone is overlain by a pure limestone section containing Ordovician, Middle Devonian, and perhaps Silurian shelly faunas contemporaneous with the Road River Formation and the thinner basal limestone and shale member of the McCann Hill Chert. The rapid change from graptolitic shale to limestone probably reflects changes in conditions of sedimentation, but could be a result of thrust faulting.

The Tatonduk-Nation Rivers area seems to lie in a transitional zone between an early Paleozoic eugeosynclinal belt south of the Yukon River and a contemporaneous miogeosynclinal belt along the Porcupine River. One puzzling feature of the lower Paleozoic sequence in the Tatonduk-Nation Rivers area is its thinness in contrast to the much thicker volcanic and detrital sequence on the south and the considerably thicker carbonate sequence on the north.

","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/A6633526-16C0-11D7-8645000102C1865D","usgsCitation":"Churkin, M., and Brabb, E.E., 1965, Ordovician, Silurian, and Devonian biostratigraphy of east-central Alaska: American Association of Petroleum Geologists Bulletin, v. 49, no. 2, p. 172-185, https://doi.org/10.1306/A6633526-16C0-11D7-8645000102C1865D.","productDescription":"14 p.","startPage":"172","endPage":"185","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355007,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Nation-Tatonduk Rivers area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -142.38695878694335,\n 65.46836165464507\n ],\n [\n -142.38695878694335,\n 64.62502455781637\n ],\n [\n -141.00230856836862,\n 64.62502455781637\n ],\n [\n -141.00230856836862,\n 65.46836165464507\n ],\n [\n -142.38695878694335,\n 65.46836165464507\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"49","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Churkin, Michael Jr.","contributorId":62566,"corporation":false,"usgs":true,"family":"Churkin","given":"Michael","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":737908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brabb, Earl E.","contributorId":8545,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":737909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70222078,"text":"70222078 - 1965 - Biota of a late glacial rocky mountain pond","interactions":[],"lastModifiedDate":"2021-07-16T13:23:47.276661","indexId":"70222078","displayToPublicDate":"1965-07-16T08:15:55","publicationYear":"1965","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":"Biota of a late glacial rocky mountain pond","docAbstract":"

The sediments of a late glacial sag pond in Huerfano Park, south-central Colorado, have yielded a varied biota consisting of vertebrates, terrestrial and fresh-water mollusks, sponges, and pollen. Wood from the sediments has a radiocarbon age of 9600 ± 200 years. The vertebrate fauna contains the tooth of a prairie dog and the remains of frog, salamander, snake, and fish—all characteristic of present-day montane lakes and ponds and their margins in Colorado. The mollusks are all living species, and the fauna is dominated by gastropods. With the exception of one form (Vitrina alaskana Dall), whose known range does not extend as far south as Huerfano Park, the fauna is not significantly different from the mollusks living in the area today. The sediments also contain an abundant and unusually diversified sponge fauna in which as many as six species may be represented. A pollen spectrum from the sediments is composed of arboreal pollen characteristic of the present-day Transition Zone flora which, in Colorado, grows on the upper edge of the Great Plains and all of the foothills belt.

Vertical variation in the sediment types and the enclosed biota makes it possible to recreate the changing depositional environment and local climate throughout the life of the pond. The basal sediments, interbedded marl and clastic materials, are interpreted as indicating deposition during alternating wet and dry periods. A bed of nearly pure calcium carbonate marl, which reaches a thickness of 2 feet, forms the middle stratigraphic unit. It is highly fossiliferous and is thought to have been deposited during a warm dry period with relatively mild winters. The uppermost stratigraphic unit is a gray carbonaceous clay which filled the basin as vegetation encroached upon the lake and the lake itself was reduced to a marsh.

Because of the radiocarbon age and the reconstruction of the climate based upon faunal and sedimentological changes, the lower two stratigraphic units are thought to correlate with the Lubbock Subpluvial, and the uppermost unit, the gray carbonaceous clay, with the early part of the Yellow House Interval as described in the Llano Estacado, New Mexico.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1965)76[1203:BOALGR]2.0.CO;2","usgsCitation":"Kauffman, E., and McCulloch, D.S., 1965, Biota of a late glacial rocky mountain pond: GSA Bulletin, v. 76, no. 11, p. 1203-1232, https://doi.org/10.1130/0016-7606(1965)76[1203:BOALGR]2.0.CO;2.","productDescription":"30 p.","startPage":"1203","endPage":"1232","costCenters":[],"links":[{"id":387223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Huerfano 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\"}}]}","volume":"76","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kauffman, E.G.","contributorId":77676,"corporation":false,"usgs":true,"family":"Kauffman","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":819447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCulloch, David S. dmccullo@usgs.gov","contributorId":3100,"corporation":false,"usgs":true,"family":"McCulloch","given":"David","email":"dmccullo@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":819448,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010602,"text":"70010602 - 1965 - Tectonic deformation associated with the 1964 Alaska earthquake","interactions":[],"lastModifiedDate":"2026-02-11T15:00:12.272329","indexId":"70010602","displayToPublicDate":"1965-06-25T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tectonic deformation associated with the 1964 Alaska earthquake","docAbstract":"

Alaska's Good Friday earthquake of 27 March 1964 was accompanied by vertical tectonic deformation over an area of 170,000 to 200,000 square kilometers in south-central Alaska. The deformation included two major northeast-trending zones of uplift and subsidence situated between the Aleutian Trench and the Aleutian Volcanic Arc; together they are 700 to 800 kilometers long and from 150 to 250 kilometers wide. The seaward zone is one in which uplift of as much as 10 meters on land and 15 meters on the sea floor has occurred as a result of both crustal warping and local faulting. Submarine uplift within this zone generated a train of seismic sea waves with half-wave amplitudes of more than 7 meters along the coast near the source. The adjacent zone to the northwest is one of subsidence that averages about 1 meter and attains a measured maximum of 2.3 meters. A second zone of slight uplift may exist along all or part of the Aleutian and Alaska ranges northwest of the zone of subsidence.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.148.3678.1675","issn":"00368075","usgsCitation":"Plafker, G., 1965, Tectonic deformation associated with the 1964 Alaska earthquake: Science, v. 148, no. 3678, p. 1675-1687, https://doi.org/10.1126/science.148.3678.1675.","productDescription":"13 p.","startPage":"1675","endPage":"1687","costCenters":[],"links":[{"id":219101,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Aleutian Trench","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -179.9,\n 52.89848022223302\n ],\n [\n -179.9,\n 50.34742724365566\n ],\n [\n -165.90072947118094,\n 52.38515601893195\n ],\n [\n -157.1802921694297,\n 54.89759776829018\n ],\n [\n -155.36618380411227,\n 56.73058764922936\n ],\n [\n -158.829392131228,\n 58.11065126044281\n ],\n [\n -172.99044772182424,\n 53.805294237333726\n ],\n [\n -179.9,\n 52.89848022223302\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 179.9,\n 52.84464206876427\n ],\n [\n 172,\n 54.15161662224946\n ],\n [\n 172,\n 51.89469832853055\n ],\n [\n 179.9,\n 50.32814578749236\n ],\n [\n 179.9,\n 52.84464206876427\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"148","issue":"3678","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba44ce4b08c986b320232","contributors":{"authors":[{"text":"Plafker, George 0000-0003-3972-0390","orcid":"https://orcid.org/0000-0003-3972-0390","contributorId":36603,"corporation":false,"usgs":true,"family":"Plafker","given":"George","affiliations":[],"preferred":false,"id":359251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010596,"text":"70010596 - 1965 - Alaskan glaciers: Recent observations in respect to the earthquake-advance theory","interactions":[],"lastModifiedDate":"2026-02-10T21:31:56.04714","indexId":"70010596","displayToPublicDate":"1965-04-16T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Alaskan glaciers: Recent observations in respect to the earthquake-advance theory","docAbstract":"Preliminary aerial photographic studies indicate that the Alaskan earthquake produced some rockfalls but no significant snow and ice avalanches on glaciers. No rapid, short-lived glacier advances (surges) are conclusively associated with this earthquake. Recent evidence fails to support the earthquake-advance theory of Tarr and Martin.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.148.3668.366","issn":"00368075","usgsCitation":"Post, A., 1965, Alaskan glaciers: Recent observations in respect to the earthquake-advance theory: Science, v. 148, no. 3668, p. 366-368, https://doi.org/10.1126/science.148.3668.366.","productDescription":"3 p.","startPage":"366","endPage":"368","costCenters":[],"links":[{"id":219095,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr_66108_1965","usgsCitation":"Detterman, R.L., and Reed, B.L., 1965, Results of stream-sediment sampling in the Iliamna quadrangle, Alaska: U.S. Geological Survey Open-File Report 66-108, 1 Plate, https://doi.org/10.3133/ofr_66108_1965.","productDescription":"1 Plate","costCenters":[],"links":[{"id":150700,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Iliamna quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -154.4424328729158,\n 59.944283762313574\n ],\n [\n -154.4424328729158,\n 59.48877183724298\n ],\n [\n -152.92195351827567,\n 59.48877183724298\n ],\n [\n -152.92195351827567,\n 59.944283762313574\n ],\n [\n -154.4424328729158,\n 59.944283762313574\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605600","contributors":{"authors":[{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":179529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, Bruce L.","contributorId":19928,"corporation":false,"usgs":true,"family":"Reed","given":"Bruce","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":179528,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3855,"text":"cir491 - 1964 - Alaska's Good Friday earthquake, March 27, 1964, a preliminary geologic evaluation","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"cir491","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"491","title":"Alaska's Good Friday earthquake, March 27, 1964, a preliminary geologic evaluation","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir491","usgsCitation":"Grantz, A., Plafker, G., and Kachadoorian, R., 1964, Alaska's Good Friday earthquake, March 27, 1964, a preliminary geologic evaluation: U.S. Geological Survey Circular 491, 35 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir491.","productDescription":"35 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":117884,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1964/0491/report-thumb.jpg"},{"id":30931,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1964/0491/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688389","contributors":{"authors":[{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":147729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":147730,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kachadoorian, Reuben","contributorId":24336,"corporation":false,"usgs":true,"family":"Kachadoorian","given":"Reuben","email":"","affiliations":[],"preferred":false,"id":147731,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":6095,"text":"pp443 - 1964 - Quaternary geology of the Kenai Lowland and glacial history of the Cook Inlet region, Alaska","interactions":[],"lastModifiedDate":"2017-03-09T13:07:07","indexId":"pp443","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"443","title":"Quaternary geology of the Kenai Lowland and glacial history of the Cook Inlet region, Alaska","docAbstract":"

The Kenai Lowland is part of the Cook Inlet Lowland physiographic subprovince that borders Cook Inlet, a major marine reentrant along the Pacific Ocean coastline of south-central Alaska. The Cook Inlet Lowland occupies a structural trough underlain by rocks of Tertiary age and mantled by Quaternary deposits of varying thicknesses. The bordering high alpine mountains—the Aleutian and Alaska Ranges to the northwest and north and the Talkeetna, Chugach, and Kenai Mountains to the northeast and southeast—are underlain by rocks of Mesozoic and older ages.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp443","usgsCitation":"Karlstrom, T., 1964, Quaternary geology of the Kenai Lowland and glacial history of the Cook Inlet region, Alaska: U.S. Geological Survey Professional Paper 443, Report: iv, 69 p.; 7 Plates: 36.00 x 32.50 inches or smaller, https://doi.org/10.3133/pp443.","productDescription":"Report: iv, 69 p.; 7 Plates: 36.00 x 32.50 inches or smaller","costCenters":[],"links":[{"id":140804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":264504,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0443/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264505,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0443/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264506,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0443/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264507,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0443/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104460,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4440.htm","linkFileType":{"id":5,"text":"html"},"description":"4440"},{"id":337206,"rank":10,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0443/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":337207,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0443/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":337208,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0443/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":337209,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0443/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6517b7","contributors":{"authors":[{"text":"Karlstrom, Thor N. V.","contributorId":77929,"corporation":false,"usgs":true,"family":"Karlstrom","given":"Thor N. V.","affiliations":[],"preferred":false,"id":152102,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7812,"text":"ofr649 - 1964 - Preliminary report on tests of the application of geophysical methods to Arctic ground water problems","interactions":[],"lastModifiedDate":"2023-11-20T23:37:43.02624","indexId":"ofr649","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-9","title":"Preliminary report on tests of the application of geophysical methods to Arctic ground water problems","docAbstract":"

Seismic refraction and electrical resistivity surveys were made during the summer and fall of 1952 in the Tanana Valley near Fairbanks, Alaska, as part of the studies of the application of geophysical techniques to ground-water problems in Alaska instigated in 1951 by the U.S. Army Engineer Research and Development Laboratories. Work centered around the highway junctions at Fairbanks, Big Delta, and Tok. It was found that both survey methods defined the horizontal extent of the frozen ground and both were capable of determining the depth to the top of the permafrost but neither regularly yielded reliable information on the material beneath the top of the permafrost. The greatest need at present is for a thorough examination of data obtained in the field seasons of 1948 and 1952. Two fundamental theoretical investigations are desirable: (1) examination of the attenuation of longitudinal waves traveling through a thin layer, and (2) further development of the theoretical multilayer resistivity interpretation of problems in which the second layer has a very high resistivity. Further field work should include: (1) tests of the U.S. Geological Survey's new shallow-reflection seismograph; (2) a brief test of electromagnetic equipment; (3) additional resistivity measurements with commutated current; and (4) both seismic and resistivity measurements in areas where the bedrock possesses different physical properties from the schist usually found in interior Alaska. It is doubtful that geophysical techniques are sufficiently developed to be valuable for use by Army personnel in prospecting for ground water in areas of thick permafrost.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr649","collaboration":"Prepared in 1954 in cooperation with U.S. Department of the Army, Engineer Research and Development Laboratories","usgsCitation":"Barnes, D., and MacCarthy, G.R., 1964, Preliminary report on tests of the application of geophysical methods to Arctic ground water problems: U.S. Geological Survey Open-File Report 64-9, iii, 32 p., https://doi.org/10.3133/ofr649.","productDescription":"iii, 32 p.","costCenters":[],"links":[{"id":422762,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0009/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140402,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0009/report-thumb.jpg"}],"country":"United 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One composite frequency curve is applied to the entire study region. This curve relates floods of various magnitudes at any site within the region to probable recurrence intervals (from 1.1 to 50 years) for those floods. Flood magnitudes are reduced to dimensionless form by expressing them as a ratio to mean annual flood. Magnitudes of mean annual floods vary with the flood-producing characteristics of stream basins. On the basis of the limited data available, drainage-area size is found to be the only significant factor affecting the magnitude of the mean annual flood. Trial and error groupings of gaging-station records show that the region can be split into three hydrologic areas: one curve defines the relation within each area between mean annual flood and drainage area. These three curves in combination with the composite flood-frequency curve permit, for natural-flow conditions at any site, the determination of flood magnitude for a given recurrence interval, or the determination of recurrence interval for a flood of known magnitude.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/cir493","collaboration":"Prepared in cooperation with the Alaska State Highway Department and the U.S. Bureau of Public Roads","usgsCitation":"Berwick, V.K., Childers, J.M., and Kuentzel, M., 1964, Magnitude and frequency of floods in Alaska south of the Yukon River: U.S. Geological Survey Circular 493, Report: iii, 15 p.; 1 Map: 19.27 x 16.80 inches, https://doi.org/10.3133/cir493.","productDescription":"Report: iii, 15 p.; 1 Map: 19.27 x 16.80 inches","numberOfPages":"19","costCenters":[],"links":[{"id":122497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0493/report-thumb.jpg"},{"id":31254,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0493/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271065,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0493/plate-1.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"Yukon River","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":"4f4e4a80e4b07f02db649542","contributors":{"authors":[{"text":"Berwick, Vernon Kenneth","contributorId":50806,"corporation":false,"usgs":true,"family":"Berwick","given":"Vernon","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":148292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Childers, Joseph M.","contributorId":14379,"corporation":false,"usgs":true,"family":"Childers","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":148291,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kuentzel, M.A.","contributorId":84248,"corporation":false,"usgs":true,"family":"Kuentzel","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":148293,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2876,"text":"wsp1779D - 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