{"pageNumber":"380","pageRowStart":"9475","pageSize":"25","recordCount":11386,"records":[{"id":5221191,"text":"5221191 - 1972 - Residues of organochlorine pesticides, polychlorinated biphenyls, and mercury in bald eagle eggs and changes in shell thickness--1969 and 1970","interactions":[],"lastModifiedDate":"2013-03-20T13:07:21","indexId":"5221191","displayToPublicDate":"2010-06-16T12:17:54","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3038,"text":"Pesticides Monitoring Journal","onlineIssn":" 0031-615","printIssn":" 0031-615","active":true,"publicationSubtype":{"id":10}},"title":"Residues of organochlorine pesticides, polychlorinated biphenyls, and mercury in bald eagle eggs and changes in shell thickness--1969 and 1970","docAbstract":"Twenty-three bald eagle eggs collected in Alaska, Maine, Michigan, Minnesota, and Florida during 1969 and 1970 were analyzed for organochlorine pesticides, polychlorinated biphenyls, and mercury.  All eggs contained residues of DDE, dieldrin, PCB's, and mercury.  Average residue concentrations were lowest in eggs from Alaska.  Significant eggshell thinning has occurred among eggs from most major areas sampled.  Some eggs contained DDE residues of the same magnitude as those that produced shell thinning in experimental species.  High dieldrin residues in some eggs could be having an adverse effect on reproductive success.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pesticides Monitoring Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Wiemeyer, S.N., Mulhern, B., Ligas, F., Hensel, R., Mathisen, J., Robards, F., and Postupalsky, S., 1972, Residues of organochlorine pesticides, polychlorinated biphenyls, and mercury in bald eagle eggs and changes in shell thickness--1969 and 1970: Pesticides Monitoring Journal, v. 6, no. 1, p. 50-55.","productDescription":"50-55","startPage":"50","endPage":"55","numberOfPages":"6","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269751,"type":{"id":11,"text":"Document"},"url":"https://biodiversitylibrary.org/page/26094936"}],"volume":"6","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629ef0","contributors":{"authors":[{"text":"Wiemeyer, Stanley N.","contributorId":78279,"corporation":false,"usgs":true,"family":"Wiemeyer","given":"Stanley","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":333244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mulhern, B.M.","contributorId":98683,"corporation":false,"usgs":true,"family":"Mulhern","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":333248,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ligas, F.J.","contributorId":93156,"corporation":false,"usgs":true,"family":"Ligas","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":333247,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hensel, R.J.","contributorId":62313,"corporation":false,"usgs":true,"family":"Hensel","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":333243,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mathisen, J.E.","contributorId":14534,"corporation":false,"usgs":true,"family":"Mathisen","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":333242,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Robards, F.C.","contributorId":91589,"corporation":false,"usgs":true,"family":"Robards","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":333245,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Postupalsky, S.","contributorId":91957,"corporation":false,"usgs":true,"family":"Postupalsky","given":"S.","affiliations":[],"preferred":false,"id":333246,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70047554,"text":"70047554 - 1972 - Hydraulic testing of hole UA-1-HTH-1, Amchitka Island, Alaska","interactions":[],"lastModifiedDate":"2013-09-19T13:11:24","indexId":"70047554","displayToPublicDate":"2009-01-01T09:10:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Hydraulic testing of hole UA-1-HTH-1, Amchitka Island, Alaska","docAbstract":"Total depth of the hole was 1,054 meters (3,458 feet) but, because of borehole erosion and bridging, only about 198 meters (650 feet) of the hole was·hydraulically tested with straddle packers. Some information was obtained on the lower part of the hole by use of the pressure recorders which are used with the straddle packers. The heads below land surface in that part of the hole tested with. straddle packers. ranged from·3.9 meters {12.7 feet) in the ..\ninterval 80.5 to 125. 0. meters (264- to 410 feet), the uppermost zone tested with straddle packers, to 5.1 meters (18.6 feet) in the interval 227.4 to 278.6 meters (.746 to 914 feet), the lowermost part of the hole tested with straddle packers. The composite static water level obtained following a pumping test.was 5.5 meters (18,0 feet). The composite head below 278.6 meters (914 feet), determined from a pressure recorder, was about 12.2 meters (40 feet). The head distribution. indicates a decreasing· head with depth. Water samples were collected from two intervals for chemical, radiochemical, and C-14 analysis. The unadjusted age of water in the interval 183.5 to 234.7 meters (602 to 770. feet) was determined to be 8,410 years, and for the interval 227.4 to 278.6 meters (746 to 914 feet) was 17,880 years. After adjustment the.ages of the waters may be less; however, they would still be. in the thousands of years and the relative difference probably would still be real.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/70047554","usgsCitation":"Ballance, W.C., and Dinwiddie, G., 1972, Hydraulic testing of hole UA-1-HTH-1, Amchitka Island, Alaska, 27 p., https://doi.org/10.3133/70047554.","productDescription":"27 p.","numberOfPages":"32","costCenters":[],"links":[{"id":277872,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047554/report.pdf"},{"id":276298,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047554/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 178.6158,51.3092 ], [ 178.6158,51.6665 ], [ 179.4688,51.6665 ], [ 179.4688,51.3092 ], [ 178.6158,51.3092 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03efe4b0026c2bc11b96","contributors":{"authors":[{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":482395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dinwiddie, G.A.","contributorId":49798,"corporation":false,"usgs":true,"family":"Dinwiddie","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":482394,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039440,"text":"70039440 - 1972 - Channel erosion surveys along proposed TAPS route, Alaska, July 1971","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039440","displayToPublicDate":"2008-11-18T14:45:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Channel erosion surveys along proposed TAPS route, Alaska, July 1971","docAbstract":"The U.S. Geological Survey has the threefold responsibility along the proposed route of the Trans-Alaska Pipeline System (TAPS): to investigate possible hydroloqic hazards to the pipeline, to investigate possible impacts of the pipeline on water resources, and to develop a better understanding of Arctic hydrology. Because the proposed pipeline route lies within many stream channels, one of the obvious hydrologic hazards is channel erosion. It was considered a major hazard in a report by Hadley (1969) after a short reconnaissance of the proposed pipeline route and also in a national assessment of water resources by the Water Resources Council (1968). The U.S. Department of Interior has also recognized the channel erosion problems in considering the environmental impacts of TAPS and has stipulated conditions for their control (U.S. Dept. of Interior, 1972a, b). The Alyeska Pipeline Service Company (APSC), who would build and operate TAPS, has described methods for complying with the Department of Interior stipulations for channel and erosion control (APSC, 1971).","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039440","usgsCitation":"Childers, J.M., 1972, Channel erosion surveys along proposed TAPS route, Alaska, July 1971, 79 p., https://doi.org/10.3133/70039440.","productDescription":"79 p.","numberOfPages":"87","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":261578,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039440/report.pdf"},{"id":261579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039440/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173,54.666666666666664 ], [ 173,71.83333333333333 ], [ -130,71.83333333333333 ], [ -130,54.666666666666664 ], [ 173,54.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f452e4b0c8380cd4bc79","contributors":{"authors":[{"text":"Childers, Joseph M.","contributorId":14379,"corporation":false,"usgs":true,"family":"Childers","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":466241,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010171,"text":"70010171 - 1972 - Middle pleistocene mollusks from St. Lawrence Island and their significance for the paleo-oceanography of the Bering Sea","interactions":[],"lastModifiedDate":"2025-07-11T16:07:00.57417","indexId":"70010171","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Middle pleistocene mollusks from St. Lawrence Island and their significance for the paleo-oceanography of the Bering Sea","docAbstract":"<p>Drift, evidently of Illinoian age, was deposited on St. Lawrence Island at the margin of an ice cap that covered the highlands of the Chukotka Peninsula of Siberia and spread far eastward on the continental shelf of northern Bering Sea. Underlying the drift on the northwestward part of the island are mollusk-bearing beds deposited during the Kotzebuan Transgression.</p><p>A comparison of mollusk faunas from St. Lawrence Island, Chukotka Peninsula, and Kotzebue Sound suggests that the present northward flow through Bering and Anadyr Straits was reversed during the Kotzebuan Transgression. Cold arctic water penetrated southward and southwestward bringing an arctic fauna to the Gulf of Anadyr. Warmer Pacific water probably entered eastern Bering Sea, passed eastward and northeastward around eastern and northern St. Lawrence Island, and then became entrained in the southward currents that passed through Anadyr Strait.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(72)90033-6","issn":"00335894","usgsCitation":"Hopkins, D., Rowland, R., and Patton, W.W., 1972, Middle pleistocene mollusks from St. Lawrence Island and their significance for the paleo-oceanography of the Bering Sea: Quaternary Research, v. 2, no. 2, p. 119-134, https://doi.org/10.1016/0033-5894(72)90033-6.","productDescription":"16 p.","startPage":"119","endPage":"134","costCenters":[],"links":[{"id":219670,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"St. Lawrence Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -172.62707116583636,\n              64.0488182952663\n            ],\n            [\n              -172.62707116583636,\n              62.80972983412474\n            ],\n            [\n              -168.38785991048877,\n              62.80972983412474\n            ],\n            [\n              -168.38785991048877,\n              64.0488182952663\n            ],\n            [\n              -172.62707116583636,\n              64.0488182952663\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"2","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"505a56eae4b0c8380cd6d8f7","contributors":{"authors":[{"text":"Hopkins, D.M.","contributorId":103646,"corporation":false,"usgs":true,"family":"Hopkins","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":358193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowland, R.W.","contributorId":36153,"corporation":false,"usgs":true,"family":"Rowland","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":358192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patton, W. W. Jr.","contributorId":11231,"corporation":false,"usgs":true,"family":"Patton","given":"W.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":358191,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010180,"text":"70010180 - 1972 - Influence of grounding ice on the Arctic shelf of Alaska","interactions":[],"lastModifiedDate":"2025-04-16T23:14:25.067807","indexId":"70010180","displayToPublicDate":"2003-04-02T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Influence of grounding ice on the Arctic shelf of Alaska","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id7\" class=\"abstract author\"><div id=\"aep-abstract-sec-id8\"><p>Alaska's Beaufort Sea shelf is characterized by small-scale relief with an average amplitude of 1–2 m and wavelength of 50–100 m. Diving observations confirm that much of the bottom roughness reflects the action of grounded ice. Except for areas in the shadow of islands, bars, and offshore bathymetric highs, the entire shelf surface from the beach to at least the 75-m contour is now or has been modified by ice gouging. Ice contact with the bottom is more common, and rates of sedimentation higher on the inner shelf than on the outer shelf; the density of gouge features is about equal in both areas. Therefore, the chances are that an area of gouging on the inner shelf contains younger gouges than a similar area on the outer shelf.</p><p>When ice grounds, it becomes an important agent in the sedimentary and morphologic environment of the Arctic shelf, directly by deforming bottom deposits and secondarily by affecting the current regime near the sediment/ice contact. While bulldozing action and rafting do not seem to contribute significantly to the direct transport of sediment, re-suspension of bottom material during bulldozing, which makes sediment available for transport, may be significant.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(72)90014-X","issn":"00253227","usgsCitation":"Reimnitz, E., Barnes, P., Forgatsch, T., and Rodeick, C., 1972, Influence of grounding ice on the Arctic shelf of Alaska: Marine Geology, v. 13, no. 5, p. 323-334, https://doi.org/10.1016/0025-3227(72)90014-X.","productDescription":"12 p.","startPage":"323","endPage":"334","costCenters":[],"links":[{"id":218631,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -146.44775390625,\n              69.89256519285392\n            ],\n            [\n              -145.04150390625,\n              69.89256519285392\n            ],\n            [\n              -145.04150390625,\n              70.18510275498964\n            ],\n            [\n              -146.44775390625,\n              70.18510275498964\n            ],\n            [\n              -146.44775390625,\n              69.89256519285392\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b3de4b0c8380cd62358","contributors":{"authors":[{"text":"Reimnitz, E.","contributorId":61557,"corporation":false,"usgs":true,"family":"Reimnitz","given":"E.","affiliations":[],"preferred":false,"id":358221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, P.","contributorId":73331,"corporation":false,"usgs":true,"family":"Barnes","given":"P.","affiliations":[],"preferred":false,"id":358222,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forgatsch, T.","contributorId":15335,"corporation":false,"usgs":true,"family":"Forgatsch","given":"T.","email":"","affiliations":[],"preferred":false,"id":358219,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rodeick, C.","contributorId":19280,"corporation":false,"usgs":true,"family":"Rodeick","given":"C.","affiliations":[],"preferred":false,"id":358220,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":59234,"text":"mf397 - 1972 - Metallic mineral resources map of the Seldovia Quadrangle, Alaska","interactions":[{"subject":{"id":13087,"text":"ofr6949 - 1969 - Metallic mineral resources map of the Seldovia Quadrangle, Alaska","indexId":"ofr6949","publicationYear":"1969","noYear":false,"title":"Metallic mineral resources map of the Seldovia Quadrangle, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":59234,"text":"mf397 - 1972 - Metallic mineral resources map of the Seldovia Quadrangle, Alaska","indexId":"mf397","publicationYear":"1972","noYear":false,"title":"Metallic mineral resources map of the Seldovia Quadrangle, Alaska"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:16","indexId":"mf397","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"397","title":"Metallic mineral resources map of the Seldovia Quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/mf397","isbn":"0607797894","usgsCitation":"Cobb, E.H., 1972, Metallic mineral resources map of the Seldovia Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 397, map ;47 x 71 cm. on sheet 59 x 90 cm. fold. in envelope 25 x 31 cm.; Reprinted 1979, https://doi.org/10.3133/mf397.","productDescription":"map ;47 x 71 cm. on sheet 59 x 90 cm. fold. in envelope 25 x 31 cm.; Reprinted 1979","costCenters":[],"links":[{"id":185331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":111286,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/13186","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -153,59 ], [ -153,60 ], [ -150,60 ], [ -150,59 ], [ -153,59 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db6284bd","contributors":{"authors":[{"text":"Cobb, E. H.","contributorId":71971,"corporation":false,"usgs":true,"family":"Cobb","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":261629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48113,"text":"ofr7345 - 1972 - Flood surveys along proposed TAPS route, Alaska, July 1971","interactions":[],"lastModifiedDate":"2023-07-10T17:02:33.23188","indexId":"ofr7345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"73-45","title":"Flood surveys along proposed TAPS route, Alaska, July 1971","docAbstract":"<p>The U.S. Geological Survey has a threefold responsibility along the proposed route of the Trans-Alaska Pipeline System (TAPS): to investigate possible hydrologic hazards to the pipeline, to investigate possible impacts of the pipeline system on water resources, and to develop a better understanding of Arctic hydrology. One of the major hazards to the proposed pipeline and its associated roads and facilities is flooding. Floods could inundate or erode foundations of structures, could cause pipeline rupture resulting in oil spillage, or could increase erosion especially where natural floodways have been altered by clearing, excavation, and other construction activities. The primary damage to the environment from accelerated flood erosion could be the degradation of water quality and its detrimental effects on fish and other organisms. Consequently, information on floods along the pipeline corridor is vitally needed to assess possible environmental damages and to aid in the design and management of the pipeline and associated facilities. This report presents a description of existing flood information and a description of flood surveys at 13 sites along the northern segment of the proposed TAPS route from Prudhoe Bay to the Salcha River. A similar report is planned for the southern segment of the TAPS route.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7345","usgsCitation":"Childers, J.M., 1972, Flood surveys along proposed TAPS route, Alaska, July 1971: U.S. Geological Survey Open-File Report 73-45, 16 p., https://doi.org/10.3133/ofr7345.","productDescription":"16 p.","costCenters":[],"links":[{"id":418826,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162203,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0045/report-thumb.jpg"}],"country":"United 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