{"pageNumber":"6851","pageRowStart":"171250","pageSize":"25","recordCount":184769,"records":[{"id":70010947,"text":"70010947 - 1959 - Modern instruments for surveying and mapping","interactions":[],"lastModifiedDate":"2026-02-27T15:32:47.503419","indexId":"70010947","displayToPublicDate":"1959-10-23T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Modern instruments for surveying and mapping","docAbstract":"New surveying systems utilizing photogrammetry and electronics speed production of topographic maps.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.130.3382.1059","issn":"00368075","usgsCitation":"Whitmore, G., Thompson, M., and Speert, J.L., 1959, Modern instruments for surveying and mapping: Science, v. 130, no. 3382, p. 1059-1066, https://doi.org/10.1126/science.130.3382.1059.","productDescription":"8 p.","startPage":"1059","endPage":"1066","costCenters":[],"links":[{"id":220874,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"130","issue":"3382","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5c96e4b0c8380cd6fddc","contributors":{"authors":[{"text":"Whitmore, G.D.","contributorId":41588,"corporation":false,"usgs":true,"family":"Whitmore","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":359952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, M.M.","contributorId":78876,"corporation":false,"usgs":true,"family":"Thompson","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":359954,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Speert, J. L.","contributorId":43100,"corporation":false,"usgs":true,"family":"Speert","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359953,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1014250,"text":"1014250 - 1959 - Infectious nature of pancreatic necrosis","interactions":[],"lastModifiedDate":"2026-04-15T17:02:36.647908","indexId":"1014250","displayToPublicDate":"1959-10-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Infectious nature of pancreatic necrosis","docAbstract":"<p><span>To determine if pancreatic necrosis is a communicable disease of trout, lots of eyed brook trout eggs were obtained from four hatcheries. Pancreatic necrosis appeared spontaneously in trout from one of these hatcheries and the other strains were exposed to infection by suspension prepared from diseased fish. In all cases, typical pancreatic necrosis appeared in fish exposed to infection and the control fish remained healthy. Disease was more acute in fry fed brine shrimp nauplii than in those fed beef liver. Mortality data suggest that susceptibility to pancreatic necrosis decreases with the increased age of trout. No treatment for the disease is known, but sanitary measures were effective in preventing its spread.</span></p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1959)88[289:INOPN]2.0.CO;2","usgsCitation":"Snieszko, S.F., Wolf, K., Camper, J., and Pettijohn, L., 1959, Infectious nature of pancreatic necrosis: Transactions of the American Fisheries Society, v. 88, no. 4, p. 289-293, https://doi.org/10.1577/1548-8659(1959)88[289:INOPN]2.0.CO;2.","productDescription":"5 p.","startPage":"289","endPage":"293","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131782,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee934","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":320053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":320054,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Camper, J.E.","contributorId":55782,"corporation":false,"usgs":true,"family":"Camper","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":320056,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pettijohn, L.L.","contributorId":32878,"corporation":false,"usgs":true,"family":"Pettijohn","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":320055,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70010644,"text":"70010644 - 1959 - Time-lapse motion picture technique applied to the study of geological processes","interactions":[],"lastModifiedDate":"2026-02-27T15:44:04.188629","indexId":"70010644","displayToPublicDate":"1959-09-25T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Time-lapse motion picture technique applied to the study of geological processes","docAbstract":"Light-weight, battery-operated timers were built and coupled to 16-mm motion-picture cameras having apertures controlled by photoelectric cells. The cameras were placed adjacent to Emmons Glacier on Mount Rainier. The film obtained confirms the view that exterior time-lapse photography can be applied to the study of slow-acting geologic processes.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.130.3378.795","issn":"00368075","usgsCitation":"Miller, R., and Crandell, D.R., 1959, Time-lapse motion picture technique applied to the study of geological processes: Science, v. 130, no. 3378, p. 795-796, https://doi.org/10.1126/science.130.3378.795.","productDescription":"2 p.","startPage":"795","endPage":"796","costCenters":[],"links":[{"id":219314,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount Rainier","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.09680003106901,\n              47.06480388005761\n            ],\n            [\n              -122.09680003106901,\n              46.489924062549875\n            ],\n            [\n              -121.37770581227939,\n              46.489924062549875\n            ],\n            [\n              -121.37770581227939,\n              47.06480388005761\n            ],\n            [\n              -122.09680003106901,\n              47.06480388005761\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"130","issue":"3378","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb3c6e4b08c986b325fbc","contributors":{"authors":[{"text":"Miller, R. D.","contributorId":92693,"corporation":false,"usgs":true,"family":"Miller","given":"R. D.","affiliations":[],"preferred":false,"id":359341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crandell, D. R.","contributorId":78385,"corporation":false,"usgs":true,"family":"Crandell","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359340,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010966,"text":"70010966 - 1959 - Mummified seal carcasses in the McMurdo Sound region, Antarctica","interactions":[],"lastModifiedDate":"2026-02-27T15:52:29.236893","indexId":"70010966","displayToPublicDate":"1959-09-18T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Mummified seal carcasses in the McMurdo Sound region, Antarctica","docAbstract":"Information was collected on 90 mummified carcasses of the \"crab-eater\" seal in the ice-free areas of the McMurdo Sound region, Antarctica. The carcasses range from relatively well-preserved bodies to merely old, twisted, wind-dissected fragments of tissue. They are hard and dry and lie on the surface of the ground, mostly in valley bottoms. The arid, cold climate is ideal for retarding organic decay. One carcass was dated by radiocarbon analysis and found to be be-tween 1600 and 2600 years old.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.130.3377.716","issn":"00368075","usgsCitation":"Pewe, T.L., Rivard, N., and Llano, G., 1959, Mummified seal carcasses in the McMurdo Sound region, Antarctica: Science, v. 130, no. 3377, p. 716-716, https://doi.org/10.1126/science.130.3377.716.","productDescription":"1 p.","startPage":"716","endPage":"716","costCenters":[],"links":[{"id":221083,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"McMurdo Sound region, Antarctica","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -197.16416821250053,\n              -77.08686092688944\n            ],\n            [\n              -197.16416821250053,\n              -77.9860072187833\n            ],\n            [\n              -192.04923168218593,\n              -77.9860072187833\n            ],\n            [\n              -192.04923168218593,\n              -77.08686092688944\n            ],\n            [\n              -197.16416821250053,\n              -77.08686092688944\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"130","issue":"3377","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a60c0e4b0c8380cd71662","contributors":{"authors":[{"text":"Pewe, T. L.","contributorId":35786,"corporation":false,"usgs":true,"family":"Pewe","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rivard, N.R.","contributorId":81186,"corporation":false,"usgs":true,"family":"Rivard","given":"N.R.","email":"","affiliations":[],"preferred":false,"id":359988,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Llano, G.A.","contributorId":56335,"corporation":false,"usgs":true,"family":"Llano","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":359987,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70205258,"text":"70205258 - 1959 - John Day to upper Bear Valley, Field Trip no. 5","interactions":[],"lastModifiedDate":"2019-09-12T10:56:07","indexId":"70205258","displayToPublicDate":"1959-09-12T10:55:56","publicationYear":"1959","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"seriesNumber":"50","title":"John Day to upper Bear Valley, Field Trip no. 5","docAbstract":"<p>No abstract available</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Field guidebook: Geologic trips along Oregon highways","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Oregon Department of Geology and Mineral Industries","usgsCitation":"Wilkinson , W., and Thayer, T.P., 1959, John Day to upper Bear Valley, Field Trip no. 5, chap. <i>of</i> Field guidebook: Geologic trips along Oregon highways, p. 99-102.","productDescription":"4 p.","startPage":"99","endPage":"102","costCenters":[],"links":[{"id":367391,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":367388,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.oregongeology.org/pubs/B/p-B.htm"}],"country":"United States","state":"Oregon","city":"John Day","otherGeospatial":"Upper Bear Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.05883789062501,\n              44.17136989600329\n            ],\n            [\n              -118.90914916992188,\n              44.17136989600329\n            ],\n            [\n              -118.90914916992188,\n              44.42691515712095\n            ],\n            [\n              -119.05883789062501,\n              44.42691515712095\n            ],\n            [\n              -119.05883789062501,\n              44.17136989600329\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wilkinson , William Donald ","contributorId":218871,"corporation":false,"usgs":false,"family":"Wilkinson ","given":"William Donald ","affiliations":[{"id":7198,"text":"Oregon Department Geology and Mineral Industries","active":true,"usgs":false},{"id":6605,"text":"USGS","active":true,"usgs":false}],"preferred":false,"id":770586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thayer, Thomas P","contributorId":218870,"corporation":false,"usgs":false,"family":"Thayer","given":"Thomas","email":"","middleInitial":"P","affiliations":[{"id":6605,"text":"USGS","active":true,"usgs":false},{"id":7198,"text":"Oregon Department Geology and Mineral Industries","active":true,"usgs":false}],"preferred":false,"id":770587,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":37826,"text":"37826 - 1959 - Big game inventory for 1958","interactions":[],"lastModifiedDate":"2014-07-24T10:36:52","indexId":"37826","displayToPublicDate":"1959-09-01T10:36:11","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"411","title":"Big game inventory for 1958","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled in the Bird and Mammal Laboratories, Branch of Wildlife Research, Bureau of Sport Fisheries and Wildlife.","usgsCitation":"U.S. Bureau of Sport Fisheries and Wildlife, 1959, Big game inventory for 1958 (Revises Wildlife Leaflet BS-342 (1952).): Wildlife Leaflet 411, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet BS-342 (1952).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd2a0e4b0824b2d176bcb","contributors":{"authors":[{"text":"U.S. Bureau of Sport Fisheries and Wildlife","contributorId":128149,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Sport Fisheries and Wildlife","id":529746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70160572,"text":"70160572 - 1959 - Mycobacterium fortuitum Cruz from the tropical fish Hyphessobrycon innesi","interactions":[],"lastModifiedDate":"2025-03-03T16:47:14.089398","indexId":"70160572","displayToPublicDate":"1959-09-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2192,"text":"Journal of Bacteriology","active":true,"publicationSubtype":{"id":10}},"title":"Mycobacterium fortuitum Cruz from the tropical fish Hyphessobrycon innesi","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/jb.78.3.392-395.1959","usgsCitation":"Ross, A.J., and Brancato, F., 1959, Mycobacterium fortuitum Cruz from the tropical fish Hyphessobrycon innesi: Journal of Bacteriology, v. 78, no. 3, p. 392-395, https://doi.org/10.1128/jb.78.3.392-395.1959.","productDescription":"4 p.","startPage":"392","endPage":"395","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":488356,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/jb.78.3.392-395.1959","text":"Publisher Index Page"},{"id":312780,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"78","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567bd3bae4b0a04ef491a1ec","contributors":{"authors":[{"text":"Ross, A. J.","contributorId":105267,"corporation":false,"usgs":true,"family":"Ross","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":583172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brancato, F.P.","contributorId":150826,"corporation":false,"usgs":false,"family":"Brancato","given":"F.P.","email":"","affiliations":[],"preferred":false,"id":583173,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211897,"text":"70211897 - 1959 - Chemical composition of argillites of the cobalt series (precambrian) and the problem of soda-rich sediments","interactions":[],"lastModifiedDate":"2020-08-11T16:48:13.547768","indexId":"70211897","displayToPublicDate":"1959-08-11T11:35:58","publicationYear":"1959","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":"Chemical composition of argillites of the cobalt series (precambrian) and the problem of soda-rich sediments","docAbstract":"<p>Two new chemical analyses show that the varved argillites of the Precambrian Cobalt series of Ontario, Canada, contain more Na<sub>2</sub>O than K<sub>2</sub>O and have a Na<sub>2</sub>O/K<sub>2</sub>O ratio higher than most pelitic rocks but similar to that found in many graywackes. Published chemical data substantiate these observations. The Cobalt materials are also low in CaO but otherwise have a composition compatible with their presumed glacial origin.</p><p>Albitization of the detrital plagioclase feldspar seems to best account for the low lime and high soda content of these rocks. X-ray data confirm the presence of albite.</p><p>Spectrographic analyses of the argillites are also given.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[593:CCOAOT]2.0.CO;2","usgsCitation":"Pettijohn, F., and Bastron, H., 1959, Chemical composition of argillites of the cobalt series (precambrian) and the problem of soda-rich sediments: GSA Bulletin, v. 70, no. 5, p. 593-599, https://doi.org/10.1130/0016-7606(1959)70[593:CCOAOT]2.0.CO;2.","productDescription":"7 p.","startPage":"593","endPage":"599","costCenters":[],"links":[{"id":377340,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","otherGeospatial":"Ontario","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.18798828125,\n              44.24519901522129\n            ],\n            [\n              -78.50830078125,\n              44.24519901522129\n            ],\n            [\n              -78.50830078125,\n              48.180738507303836\n            ],\n            [\n              -85.18798828125,\n              48.180738507303836\n            ],\n            [\n              -85.18798828125,\n              44.24519901522129\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"70","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pettijohn, F.J.","contributorId":41407,"corporation":false,"usgs":true,"family":"Pettijohn","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":795720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bastron, H.","contributorId":20067,"corporation":false,"usgs":true,"family":"Bastron","given":"H.","affiliations":[],"preferred":false,"id":795721,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211669,"text":"70211669 - 1959 - Role of fluid pressure in mechanics of overthrust faulting: II. Overthrust belt in geosynclinal area of western Wyoming in light of fluid-pressure hypothesis","interactions":[],"lastModifiedDate":"2020-09-17T20:28:50.7545","indexId":"70211669","displayToPublicDate":"1959-08-06T15:09:47","publicationYear":"1959","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":"Role of fluid pressure in mechanics of overthrust faulting: II. Overthrust belt in geosynclinal area of western Wyoming in light of fluid-pressure hypothesis","docAbstract":"<p>Pressures of interstitial fluids significantly greater than the normal hydrostatic pressure are known in many parts of the world. Many occurrences are in thick sections of relatively young sediments; some are in areas that have been intensely deformed. Abnormal fluid pressures in the Gulf Coast region are associated with thick bodies of shale or mudstone, and with high hydraulic gradients across bedding. The rocks there have been buried rather rapidly and are evidently not yet fully compacted. The mechanism by which clay consolidates under pressure affords a quantitative relationship among the variables—depth, strength of clay, and fluid pressure—and this relationship indicates that the Gulf Coast examples agree fairly well with observations on depth and porosity in Paleozoic shales of Oklahoma and Tertiary shales of Venezuela. Critical data are lacking, but permeability clearly decreases tremendously as clay rocks are compacted. This decrease in permeability provides a self-sealing mechanism that greatly retards the escape of pore water from deeply buried clay rocks. The relationship between rate of compaction and the development of abnormal fluid pressures probably applies not only to clay rocks but also to carbonates and possibly to micaceous and chloritic metamorphic rocks. Conditions of geosynclinal deposition are, in general, those most favorable to the development of abnormal fluid pressures.</p><p>The hypothesis that large-scale overthrusting is facilitated by abnormal fluid pressures which, in turn, are associated with geosynclinal deposition is applied to the overthrust belt of western Wyoming and adjacent States. This is a long curving belt of several bedding-plane faults which have an aggregate horizontal displacement across the belt of 50 miles or more. The sedimentary rocks that make up the belt were evidently deposited in a major geosyncline bordered by uplands not far to the west. At any given locality, the rate of deposition of the sediments increased continuously until the beginning of intense deformation and overthrusting. The geosynclinal axis and the bordering uplands probably migrated slowly eastward across the belt. Several lines of indirect evidence suggest that abnormal fluid pressures developed in this region during final stages of rapid geosynclinal sinking and that thick plates of Paleozoic and Mesozoic sedimentary rocks sheared off from the underlying rocks and moved slowly eastward. Rate of movement probably was controlled by erosion of upfolds that arose at the front of each moving plate. The fundamental cause of the lateral stresses that propelled the overthrusts is not known, but it may be examined instructively in the light of the fluid-pressure hypothesis. The thrust sheets might, for example, have slid by simple gravitation down the western limb of the geosyncline on reasonable slopes and not improbable fluid pressure-overburden ratios. Such large-scale slumping of thrust sheets, however, seems to require gaps at the rear of the thrust sheets. The long intermontane valleys of Idaho and Utah may possibly have originated as such gaps or rifts, but no proof has yet been recognized that they were formed in this manner. An alternative possibility, regional compression, requires concentration of the lateral stresses within the upper few miles of the earth's crust; in this general region emplacement of the Idaho batholith seems the most likely source of such superficially concentrated stresses. However, this batholith is so far from the front edge of the overthrust belt that it would require extremely high fluid pressure-overburden ratios over a wide area. Perhaps some combination of the two forces—pushing wide thrust plates down a gentle slope—is the most likely explanation.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[167:ROFPIM]2.0.CO;2","usgsCitation":"Rubey, W.W., and Hubbert, M.K., 1959, Role of fluid pressure in mechanics of overthrust faulting: II. Overthrust belt in geosynclinal area of western Wyoming in light of fluid-pressure hypothesis: GSA Bulletin, v. 70, no. 2, p. 167-206, https://doi.org/10.1130/0016-7606(1959)70[167:ROFPIM]2.0.CO;2.","productDescription":"40 p.","startPage":"167","endPage":"206","costCenters":[],"links":[{"id":377109,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rubey, William W.","contributorId":16899,"corporation":false,"usgs":true,"family":"Rubey","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":794966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubbert, M. King","contributorId":50197,"corporation":false,"usgs":true,"family":"Hubbert","given":"M.","email":"","middleInitial":"King","affiliations":[],"preferred":false,"id":794967,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211668,"text":"70211668 - 1959 - Minimum age of the lower Devonian Slate near Jackman, Maine","interactions":[],"lastModifiedDate":"2020-08-06T20:02:31.422546","indexId":"70211668","displayToPublicDate":"1959-08-06T14:53:43","publicationYear":"1959","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":"Minimum age of the lower Devonian Slate near Jackman, Maine","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[947:MAOTLD]2.0.CO;2","usgsCitation":"Hurley, P.M., Boucot, A., Albee, A.L., Faul, H., Pinson, W., and Fairbairn, H.W., 1959, Minimum age of the lower Devonian Slate near Jackman, Maine: GSA Bulletin, v. 70, no. 7, p. 947-950, https://doi.org/10.1130/0016-7606(1959)70[947:MAOTLD]2.0.CO;2.","productDescription":"3 p.","startPage":"947","endPage":"950","costCenters":[],"links":[{"id":377106,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hurley, Patrick M.","contributorId":12121,"corporation":false,"usgs":true,"family":"Hurley","given":"Patrick","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":794956,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boucot, A. J.","contributorId":30620,"corporation":false,"usgs":true,"family":"Boucot","given":"A. J.","affiliations":[],"preferred":false,"id":794957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Albee, A. L.","contributorId":77595,"corporation":false,"usgs":true,"family":"Albee","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":794958,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Faul, H.","contributorId":101976,"corporation":false,"usgs":true,"family":"Faul","given":"H.","email":"","affiliations":[],"preferred":false,"id":794959,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pinson, W.H.","contributorId":237001,"corporation":false,"usgs":false,"family":"Pinson","given":"W.H.","email":"","affiliations":[{"id":12444,"text":"Massachusetts Institute of Technology","active":true,"usgs":false}],"preferred":false,"id":794960,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fairbairn, Harold W.","contributorId":22627,"corporation":false,"usgs":true,"family":"Fairbairn","given":"Harold","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":794961,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70211667,"text":"70211667 - 1959 - Role of fluid pressure in mechanics of overthrust faulting: I. Mechanics of fluid-filled porous solids and its application to overthrust faulting","interactions":[],"lastModifiedDate":"2020-09-17T20:26:52.652084","indexId":"70211667","displayToPublicDate":"1959-08-06T14:22:20","publicationYear":"1959","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":"Role of fluid pressure in mechanics of overthrust faulting: I. Mechanics of fluid-filled porous solids and its application to overthrust faulting","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[115:ROFPIM]2.0.CO;2","usgsCitation":"Hubbert, M.K., and Rubey, W.W., 1959, Role of fluid pressure in mechanics of overthrust faulting: I. Mechanics of fluid-filled porous solids and its application to overthrust faulting: GSA Bulletin, v. 70, no. 2, p. 115-166, https://doi.org/10.1130/0016-7606(1959)70[115:ROFPIM]2.0.CO;2.","productDescription":"52 p.","startPage":"115","endPage":"166","costCenters":[],"links":[{"id":378544,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hubbert, M. King","contributorId":50197,"corporation":false,"usgs":true,"family":"Hubbert","given":"M.","email":"","middleInitial":"King","affiliations":[],"preferred":false,"id":794954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubey, William W.","contributorId":16899,"corporation":false,"usgs":true,"family":"Rubey","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":794955,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211666,"text":"70211666 - 1959 - The petroleum potential of the emerged and submerged Atlantic coastal plain of the United States","interactions":[],"lastModifiedDate":"2020-08-06T19:21:22.720799","indexId":"70211666","displayToPublicDate":"1959-08-06T14:02:48","publicationYear":"1959","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The petroleum potential of the emerged and submerged Atlantic coastal plain of the United States","docAbstract":"<p><span>Increasing geological and geophysical information about the Atlantic continental shelf of the United States is changing the basis for judging the area's petroleum potential. No nation can afford to overlook an area that overlies 175,000 cubic miles (730,000 km</span><sup>3</sup><span>) of possibly petroliferous sediments (including the emerged coastal plain), though the first barrel of oil is yet to be produced. Seismic and magnetic surveys indicate that the basement is deeper and more irregular than previously supposed and that a basement ridge may separate the shelf sediments into two major elongate basins parallel to the shelf edge, thus forming possible entrapping structures and possibly restricted depositional basins. Lower Paleozoic clastic rocks found in the subsurface of Georgia and Florida, and which may occur elsewhere in downfaulted basins, could be source beds and reservoir rocks for oil and gas over wide areas. Lower Cretaceous, Upper Jurassic( ?), and Triassic sedimentary rocks recognized in some wells must wedge out updip, and numerous unconformities probably occur. The marine sediments were presumably deposited in or close to shelf areas that possibly contain reefs and are partially bordered by known granite washes; thus both source and reservoir rocks are probably present. It can be expected that petroleum will eventually be discovered beneath the continental shelf and perhaps the emerged coastal plain, but it will not be discovered (economic factors aside) until geologists have projected paleogeographic settings into the sediments beneath the shelf from the data obtained through onshore and submarine geology, drilling, and geophysics.</span></p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"World Petroleum Congress Proceedings","conferenceTitle":"5th World Petroleum Congress","conferenceDate":"May 30- June 5, 1959","conferenceLocation":"New York, New York","language":"English","publisher":"Energy Institute","usgsCitation":"Johnston, J.E., Trumbull, J., and Eaton, G.P., 1959, The petroleum potential of the emerged and submerged Atlantic coastal plain of the United States, <i>in</i> World Petroleum Congress Proceedings, v. 5, New York, New York, May 30- June 5, 1959, p. 435-444.","productDescription":"10 p.","startPage":"435","endPage":"444","costCenters":[],"links":[{"id":377102,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Johnston, J. E.","contributorId":61487,"corporation":false,"usgs":true,"family":"Johnston","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":794951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trumbull, James","contributorId":92233,"corporation":false,"usgs":true,"family":"Trumbull","given":"James","affiliations":[],"preferred":false,"id":794952,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eaton, G. P.","contributorId":86334,"corporation":false,"usgs":true,"family":"Eaton","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":794953,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70211663,"text":"70211663 - 1959 - The Elk Ridge-White Canyon channel system, San Juan County, Utah: Its effect on uranium distribution","interactions":[],"lastModifiedDate":"2020-08-06T19:53:38.206306","indexId":"70211663","displayToPublicDate":"1959-08-06T12:30:09","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The Elk Ridge-White Canyon channel system, San Juan County, Utah: Its effect on uranium distribution","docAbstract":"<p><span>Reconnaissance in the White Canyon district, San Juan County, Utah, indicates that rocks of the Shinarump member of the Chinle formation of Triassic age were deposited in that district in two different channel systems; sediments deposited in channels of one system were derived from a source to the east and sediments of the other from a source to the south. The channel system containing sediments derived from the east, the Elk Ridge-White C anyon channel system, was apparently formed by a large braided stream that flowed westward from a source in granitic and metamorphic terrane of the ancestral Uncompahgre highland.</span></p><p><span> All known uranium deposits of any consequence in the White Canyon district are confined to the Shinarump member deposited in the Elk Ridge-White Canyon channel system. The nature of the channels and the lithologic characteristics of the rocks filling this system of channels combine to form a much more favorable environment for the localization of uranium deposits than do the channels formed and the rocks deposited by northward-flowing streams. </span></p><p><span>Recognition of channel systems in the White Canyon district suggests that channel systems may be recognized elsewhere in the Shinarump member, and that the Shinarump member on the Colorado Plateau may be composed of rocks deposited in many coalescing channel systems. In addition, study in the White Canyon district indicates that rocks deposited in some of these channel systems are more favorable hosts for uranium deposits than the rocks deposited in others. Recognition and delineation of these ancient channel systems may be-of help in making regional appraisals of ore potential and in the search for new mining districts.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.54.1.119","usgsCitation":"Johnson, H., and Thordarson, W., 1959, The Elk Ridge-White Canyon channel system, San Juan County, Utah: Its effect on uranium distribution: Economic Geology, v. 54, no. 1, p. 119-129, https://doi.org/10.2113/gsecongeo.54.1.119.","productDescription":"11 p.","startPage":"119","endPage":"129","costCenters":[],"links":[{"id":480394,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digital.library.unt.edu/ark:/67531/metadc1050458/","text":"External Repository"},{"id":377099,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","county":"San Juan","otherGeospatial":"Elk 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,{"id":70211661,"text":"70211661 - 1959 - Skip-term summation of sequences","interactions":[],"lastModifiedDate":"2020-08-06T17:22:47.64457","indexId":"70211661","displayToPublicDate":"1959-08-06T12:13:14","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5995,"text":"Mathematics of Computation","onlineIssn":"1088-6842","printIssn":"0025-5718","active":true,"publicationSubtype":{"id":10}},"title":"Skip-term summation of sequences","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"American Mathematical Society","doi":"10.1090/S0025-5718-59-99263-4","usgsCitation":"Roman, I., 1959, Skip-term summation of sequences: Mathematics of Computation, v. 13, p. 117-121, https://doi.org/10.1090/S0025-5718-59-99263-4.","productDescription":"5p.","startPage":"117","endPage":"121","costCenters":[],"links":[{"id":377097,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Roman, Irwin","contributorId":57834,"corporation":false,"usgs":true,"family":"Roman","given":"Irwin","email":"","affiliations":[],"preferred":false,"id":794944,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211659,"text":"70211659 - 1959 - United States Geological Survey field work in south Victoria Land, 1958-59","interactions":[],"lastModifiedDate":"2020-08-06T17:02:13.183712","indexId":"70211659","displayToPublicDate":"1959-08-06T11:56:38","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3095,"text":"Polar Record","active":true,"publicationSubtype":{"id":10}},"title":"United States Geological Survey field work in south Victoria Land, 1958-59","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"Cambridge University Press","doi":"10.1017/S0032247400066808","usgsCitation":"Hamilton, W., and Hayes, P.T., 1959, United States Geological Survey field work in south Victoria Land, 1958-59: Polar Record, v. 9, no. 63, p. 575-575, https://doi.org/10.1017/S0032247400066808.","productDescription":"1 p.","startPage":"575","endPage":"575","costCenters":[],"links":[{"id":377096,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"63","noUsgsAuthors":false,"publicationDate":"2009-10-27","publicationStatus":"PW","contributors":{"authors":[{"text":"Hamilton, W.","contributorId":46683,"corporation":false,"usgs":true,"family":"Hamilton","given":"W.","email":"","affiliations":[],"preferred":false,"id":794942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, P. T.","contributorId":17655,"corporation":false,"usgs":true,"family":"Hayes","given":"P.","email":"","middleInitial":"T.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":794943,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211658,"text":"70211658 - 1959 - Water‐level fluctuations caused by Montana earthquake","interactions":[],"lastModifiedDate":"2020-08-06T16:50:26.274737","indexId":"70211658","displayToPublicDate":"1959-08-06T11:37:47","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Water‐level fluctuations caused by Montana earthquake","docAbstract":"<p><span>The major earthquake of August 17, 1959, near the Montana‐Wyoming border had marked effects on water levels and artesian pressures in wells throughout the United States. Preliminary reports from field offices of the U. S. Geological Survey in 21 states show that water‐level fluctuations were automatically recorded in 136 observation wells. These wells for which records are available, and the maximum double amplitude of the fluctuations, are listed in Table 1.&nbsp;</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/TR040i004p00346","usgsCitation":"Da Costa, J.A., 1959, Water‐level fluctuations caused by Montana earthquake: Eos, Transactions, American Geophysical Union, v. 40, no. 4, p. 346-346, https://doi.org/10.1029/TR040i004p00346.","productDescription":"1 p.","startPage":"346","endPage":"346","costCenters":[],"links":[{"id":377095,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Da Costa, Jose Alves","contributorId":76291,"corporation":false,"usgs":true,"family":"Da Costa","given":"Jose","email":"","middleInitial":"Alves","affiliations":[],"preferred":false,"id":794941,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211620,"text":"70211620 - 1959 - Turtleback faults of Death Valley, California: A reinterpretation","interactions":[],"lastModifiedDate":"2020-08-05T14:04:42.405619","indexId":"70211620","displayToPublicDate":"1959-08-04T15:23:13","publicationYear":"1959","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":"Turtleback faults of Death Valley, California: A reinterpretation","docAbstract":"<p><span>Turtlebacks are smooth, curved surfaces, which form north-northwestward-plunging elongate domes on the east side of Death Valley. These surfaces are roughly parallel to bedding or foliation of anticlines in Precambrian schist, gneiss, and marble. Late Cenozoic fan and playa deposits are faulted over these surfaces along the turtleback faults. Previously the turtleback faults have been interpreted as part of&nbsp;</span><span class=\"ScopusTermHighlight\">a</span><span>&nbsp;thrust fault, perhaps the Amargosa thrust fault, that was arched after thrusting. They are interpreted here as individual normal faults younger than the thrust fault and, contrary to previous interpretations, much younger than the formation of the anticlines in the Precambrian rocks. The tectonic history of this unusual&nbsp;</span><span class=\"ScopusTermHighlight\">area</span><span>&nbsp;is here considered to include the following events: (1) Precambrian folding of the Precambrian rocks; (2) post-Paleozoic and pre-middle(?) Tertiary Amargosa thrusting; (3) uplift and erosion of Paleozoic strata and the Amargosa thrust fault, down to the folded Precambrian rocks in the Black Mountains block; (4) Middle (?) Tertiary rhyolite extrusions and the accumulation of later Tertiary fan and playa deposits; (5) Pliocene or Pleistocene uplift of the Black Mountains relative to Death Valley, along the Black Mountains fault system, with consequent removal of support for the Tertiary deposits on the turtleback surfaces, and the development of the turtleback faults by normal faulting, or sliding, of the Tertiary sedimentary rocks down the turtleback surfaces toward Death Valley; and, (6) Pleistocene to Recent renewal of movement on the Black Mountains fault system.&nbsp;</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[1497:TFODVC]2.0.CO;2","usgsCitation":"Drewes, H., 1959, Turtleback faults of Death Valley, California: A reinterpretation: GSA Bulletin, v. 70, no. 12, p. 1497-1508, https://doi.org/10.1130/0016-7606(1959)70[1497:TFODVC]2.0.CO;2.","productDescription":"12 p.","startPage":"1497","endPage":"1508","costCenters":[],"links":[{"id":377025,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Death Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.09228515624999,\n              35.47856499535729\n            ],\n            [\n              -115.5047607421875,\n              35.47856499535729\n            ],\n            [\n              -115.5047607421875,\n              36.328402729422656\n            ],\n            [\n              -117.09228515624999,\n              36.328402729422656\n            ],\n            [\n              -117.09228515624999,\n              35.47856499535729\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"70","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Drewes, Harald","contributorId":52567,"corporation":false,"usgs":true,"family":"Drewes","given":"Harald","affiliations":[],"preferred":false,"id":794803,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211619,"text":"70211619 - 1959 - Yellowstone Park area, Wyoming: A possible modern Lopolith","interactions":[],"lastModifiedDate":"2020-08-05T14:06:41.987219","indexId":"70211619","displayToPublicDate":"1959-08-04T15:13:09","publicationYear":"1959","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":"Yellowstone Park area, Wyoming: A possible modern Lopolith","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[225:YPAWAP]2.0.CO;2","usgsCitation":"Hamilton, W., 1959, Yellowstone Park area, Wyoming: A possible modern Lopolith: GSA Bulletin, v. 70, no. 2, p. 225-228, https://doi.org/10.1130/0016-7606(1959)70[225:YPAWAP]2.0.CO;2.","productDescription":"4 p.","startPage":"225","endPage":"228","costCenters":[],"links":[{"id":377024,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana, Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.258544921875,\n              43.59630591596548\n            ],\n            [\n              -108.97338867187499,\n              43.59630591596548\n            ],\n            [\n              -108.97338867187499,\n              45.22074260255366\n            ],\n            [\n              -111.258544921875,\n              45.22074260255366\n            ],\n            [\n              -111.258544921875,\n              43.59630591596548\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"70","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hamilton, W.","contributorId":46683,"corporation":false,"usgs":true,"family":"Hamilton","given":"W.","email":"","affiliations":[],"preferred":false,"id":794802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211618,"text":"70211618 - 1959 - Chemistry of granophyres from Wichita Lopolith, Oklahoma","interactions":[],"lastModifiedDate":"2020-08-05T14:09:37.143222","indexId":"70211618","displayToPublicDate":"1959-08-04T14:55:45","publicationYear":"1959","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":"Chemistry of granophyres from Wichita Lopolith, Oklahoma","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[1119:COGFWL]2.0.CO;2","usgsCitation":"Hamilton, W., 1959, Chemistry of granophyres from Wichita Lopolith, Oklahoma: GSA Bulletin, v. 70, no. 8, p. 1119-1126, https://doi.org/10.1130/0016-7606(1959)70[1119:COGFWL]2.0.CO;2.","productDescription":"8 p.","startPage":"1119","endPage":"1126","costCenters":[],"links":[{"id":377023,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","otherGeospatial":"Wichita Lopolith","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99.9591064453125,\n              33.87041555094183\n            ],\n            [\n              -96.74011230468749,\n              33.87041555094183\n            ],\n            [\n              -96.74011230468749,\n              35.303918565311704\n            ],\n            [\n              -99.9591064453125,\n              35.303918565311704\n            ],\n            [\n              -99.9591064453125,\n              33.87041555094183\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"70","issue":"8","edition":"70","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hamilton, Warren","contributorId":14819,"corporation":false,"usgs":true,"family":"Hamilton","given":"Warren","affiliations":[],"preferred":false,"id":794801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211616,"text":"70211616 - 1959 - Cenozoic history of the Bering land bridge","interactions":[],"lastModifiedDate":"2020-08-05T14:12:30.324557","indexId":"70211616","displayToPublicDate":"1959-08-04T14:37:39","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Cenozoic history of the Bering land bridge","docAbstract":"<p><span>The seaway between the Pacific and Arctic basins has often been a land route between Siberia and Alaska.</span></p>","language":"English","publisher":"AAAS","doi":"10.1126/science.129.3362.1519","usgsCitation":"Hopkins, D., 1959, Cenozoic history of the Bering land bridge: Science, v. 129, no. 3362, p. 1519-1528, https://doi.org/10.1126/science.129.3362.1519.","productDescription":"10 p.","startPage":"1519","endPage":"1528","costCenters":[],"links":[{"id":377022,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia, United States","state":"Alaska, Siberia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -170.09033203125,\n              65.4217295985527\n            ],\n            [\n              -167.36572265625,\n              65.4217295985527\n            ],\n            [\n              -167.36572265625,\n              66.24031184756058\n            ],\n            [\n              -170.09033203125,\n              66.24031184756058\n            ],\n            [\n              -170.09033203125,\n              65.4217295985527\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"129","issue":"3362","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hopkins, David M.","contributorId":37409,"corporation":false,"usgs":true,"family":"Hopkins","given":"David M.","affiliations":[],"preferred":false,"id":794800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211615,"text":"70211615 - 1959 - Froth veins, formed by immiscible hydrothermal fluids, in Mercury deposits, California","interactions":[],"lastModifiedDate":"2020-08-05T14:14:40.599277","indexId":"70211615","displayToPublicDate":"1959-08-04T14:22:35","publicationYear":"1959","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":"Froth veins, formed by immiscible hydrothermal fluids, in Mercury deposits, California","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[661:FVFBIH]2.0.CO;2","usgsCitation":"Bailey, E.H., 1959, Froth veins, formed by immiscible hydrothermal fluids, in Mercury deposits, California: GSA Bulletin, v. 70, no. 5, p. 661-664, https://doi.org/10.1130/0016-7606(1959)70[661:FVFBIH]2.0.CO;2.","productDescription":"4 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 \"}}]}","volume":"70","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bailey, E. H.","contributorId":44509,"corporation":false,"usgs":true,"family":"Bailey","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":794794,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211614,"text":"70211614 - 1959 - History of Imuruk Lake, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2020-08-05T14:17:27.877505","indexId":"70211614","displayToPublicDate":"1959-08-04T14:00:21","publicationYear":"1959","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":"History of Imuruk Lake, Seward Peninsula, Alaska","docAbstract":"<p><span>A study of Imuruk Lake, a large, shallow lake&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;north-central Seward Peninsula, Alaska, illuminates the climatic history of northwestern Alaska and the tectonic history of central Seward Peninsula during Pleistocene and Recent time. Special interest attaches to the older lake sediments, because they contain evidence concerning the climate, fauna, and flora that existed&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the vicinity of Bering Strait at a time when the Bering land bridge was open and when animal and plant populations were being exchanged between the eastern and western hemispheres. </span></p><p><span>The lake is 8 miles long and less than 10 feet deep; bottom sediments consisting of reworked wind-blown silt bury a rolling bedrock topography of much greater relief. Analysis of the hydrologic regime indicates that much of the water draining into the lake is lost by evaporation; smaller quantities are lost by discharge through the outlet, the Kugruk River, and by leakage into the lava flows along the lake shore. Changes&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the duration and temperature of the summer ice-free season would result&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;changes&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the amount of water lost by evaporation and thus&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;appreciable changes&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;lake level. </span></p><p><span>Imuruk Lake occupies an initial low area on basaltic lava flows of Quaternary age, but the initial low area has been modified by faulting and now lies&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;a poorly defined graben. Topographic evidence confirmed by study of lacustrine terraces indicates that until recently Imuruk Lake drained westward into the Noxapaga River instead of eastward into the Kugruk River. A history of repeated warping of the lake basin, on which is superimposed a history of oscillating lake level which is due to changes&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;climate, is recorded by three systems of abandoned shore-line features found along the shores: a warped shore cliff of probable Illinoian age, a double set of warped terraces of probable Wisconsin age, and a low, horizontal terrace of Recent age. Bones of bison, horse, and mammoth were found&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;peaty sediments containing many twigs but no large wood; their presence indicates that these mammals, at least, were capable of surviving&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;a tundra environment during cold stages of the Pleistocene epoch and at a time when the Bering land bridge was&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;existence nearby. </span></p><p><span>The sediments filling the deeper parts of the bedrock basin of Imuruk Lake probably contain an uninterrupted pollen record that reflects vegetation changes&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;central Seward Peninsula beginning&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;middle Illinoian time and terminating a few thousand years ago. Core drilling and pollen analysis of these sediments would greatly amplify our understanding of late Pleistocene events&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span> the vicinity of the Bering land bridge.&nbsp;</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[1033:HOILSP]2.0.CO;2","usgsCitation":"Hopkins, D., 1959, History of Imuruk Lake, Seward Peninsula, Alaska: GSA Bulletin, v. 70, no. 8, p. 1033-1046, https://doi.org/10.1130/0016-7606(1959)70[1033:HOILSP]2.0.CO;2.","productDescription":"14 p.","startPage":"1033","endPage":"1046","costCenters":[],"links":[{"id":377018,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Imuruk Lake, Seward Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -168.57421875,\n              64.09140752262307\n            ],\n            [\n              -160.048828125,\n              64.09140752262307\n            ],\n            [\n              -160.048828125,\n              66.75724984139227\n            ],\n            [\n              -168.57421875,\n              66.75724984139227\n            ],\n            [\n              -168.57421875,\n              64.09140752262307\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"70","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hopkins, David M.","contributorId":37409,"corporation":false,"usgs":true,"family":"Hopkins","given":"David M.","affiliations":[],"preferred":false,"id":794793,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211612,"text":"70211612 - 1959 - Granitization, migmatization, and fusion in the northern Entiat Mountains, Washington","interactions":[],"lastModifiedDate":"2020-08-04T18:22:41.865181","indexId":"70211612","displayToPublicDate":"1959-08-04T13:07:53","publicationYear":"1959","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":"Granitization, migmatization, and fusion in the northern Entiat Mountains, Washington","docAbstract":"<p><span>A tabular quartz diorite complex extends along the&nbsp;</span><span class=\"ScopusTermHighlight\">Entiat</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Mountains</span><span>, which form a southeast-trending spur of the&nbsp;</span><span class=\"ScopusTermHighlight\">Northern</span><span>&nbsp;Cascade&nbsp;</span><span class=\"ScopusTermHighlight\">Mountains</span><span>. The country rocks of the complex are biotite gneiss, probably derived from arkosic sedimentary rocks, and hornblende schist, probably derived from basic volcanic rocks. Their present mineral composition is typical of the upper epidote amphibolite and amphibolite facies of regional metamorphism.</span></p><p><span> During regional metamorphism the biotite gneiss was granitized to biotite-quartz diorite gneiss and the hornblende schist to hornblende-quartz diorite gneiss. The metamorphic origin of these quartz diorite gneisses involving relatively little replacement is shown by their chemical and mineralogical similarity to the original biotite gneiss and hornblende schist, by their enclosing long, thin, undisturbed layers of country rocks, and by their association with migmatites formed by metamorphic processes. Here and there&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the quartz diorite gneisses massive rocks with hypidiomorphic granular \"igneous\" textures have formed principally by recrystallization, and these features are associated with small-scale swirling of the foliation and some intrusive features, which show that the gneiss was rendered plastic and mobile during&nbsp;</span><span class=\"ScopusTermHighlight\">granitization</span><span>. </span></p><p><span>Migmatites containing replacement bodies and secretions of leucocratic quartz diorite occur&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the biotite gneiss and&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;most of the rocks of the complex - particularly&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the biotite-quartz diorite gneiss. During the formation of the complex, the felsic material contained&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the leucocratic rocks, principally sodium, potassium, and silicon, was generated by metamorphic differentiation. </span></p><p><span>During the&nbsp;</span><span class=\"ScopusTermHighlight\">granitization</span><span>, anatectic magmas were formed by&nbsp;</span><span class=\"ScopusTermHighlight\">fusion</span><span>&nbsp;of hornblende-quartz diorite gneiss, and some similar magma intruded from below. Melting without metamorphic differentiation is indicated by the chemical similarity between the anatectic quartz diorite and the parent hornblende-quartz diorite gneiss. Smearing out of inclusions and crystals and the tabular, sill-like nature of the bodies indicate that&nbsp;</span><span class=\"ScopusTermHighlight\">fusion</span><span>&nbsp;may have been triggered by differential movement and shearing. The anatectic rocks contain inclusions of hornblende schist that survived both the&nbsp;</span><span class=\"ScopusTermHighlight\">granitization</span><span>&nbsp;to hornblende-quartz diorite and the&nbsp;</span><span class=\"ScopusTermHighlight\">fusion</span><span>. Crystallization differentiation of the anatectic magmas yielded potassium-rich pegmatites and local granodioritic masses. Regional metamorphism continued after the anatectic magmas&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the sills had solidified; felsic metamorphic differentiates occur&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;leucocratic quartz diorite that partly replaces the borders of the sills. The leucocratic material was plastic and facilitated differential movement between the sill and its walls.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[827:GMAFIT]2.0.CO;2","usgsCitation":"Crowder, D.F., 1959, Granitization, migmatization, and fusion in the northern Entiat Mountains, Washington: GSA Bulletin, v. 70, no. 7, p. 827-878, https://doi.org/10.1130/0016-7606(1959)70[827:GMAFIT]2.0.CO;2.","productDescription":"52 p.","startPage":"827","endPage":"878","costCenters":[],"links":[{"id":377016,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Entiat Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.48681640624999,\n              46.92025531537451\n            ],\n            [\n              -119.46533203125,\n              46.92025531537451\n            ],\n            [\n              -119.46533203125,\n              48.60385760823255\n            ],\n            [\n              -121.48681640624999,\n              48.60385760823255\n            ],\n            [\n              -121.48681640624999,\n              46.92025531537451\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"70","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Crowder, D. F.","contributorId":120036,"corporation":false,"usgs":true,"family":"Crowder","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":794789,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211611,"text":"70211611 - 1959 - Water analysis","interactions":[],"lastModifiedDate":"2020-08-04T18:02:32.856752","indexId":"70211611","displayToPublicDate":"1959-08-04T12:52:48","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Water analysis","docAbstract":"<p><span>No abstract available.</span></p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60148a015","usgsCitation":"Thatcher, L.L., and Kiser, R., 1959, Water analysis: Analytical Chemistry, v. 31, no. 4, p. 776-789, https://doi.org/10.1021/ac60148a015.","productDescription":"14 p.","startPage":"776","endPage":"789","costCenters":[],"links":[{"id":377015,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Thatcher, L. L.","contributorId":23271,"corporation":false,"usgs":true,"family":"Thatcher","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":794787,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kiser, R.T.","contributorId":94659,"corporation":false,"usgs":true,"family":"Kiser","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":794788,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}