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,{"id":54091,"text":"ofr589 - 1958 - Water supply for Persimmon Gap and Santa Elena ranger stations, Big Bend National Park, Brewster county, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:11:37","indexId":"ofr589","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-9","title":"Water supply for Persimmon Gap and Santa Elena ranger stations, Big Bend National Park, Brewster county, Texas","language":"ENGLISH","doi":"10.3133/ofr589","usgsCitation":"Baker, R.C., 1958, Water supply for Persimmon Gap and Santa Elena ranger stations, Big Bend National Park, Brewster county, Texas: U.S. Geological Survey Open-File Report 58-9, 19 p., https://doi.org/10.3133/ofr589.","productDescription":"19 p.","costCenters":[],"links":[{"id":178277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1958/0009/report-thumb.jpg"},{"id":87828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1958/0009/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0100","contributors":{"authors":[{"text":"Baker, R. C.","contributorId":79084,"corporation":false,"usgs":true,"family":"Baker","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":249186,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55786,"text":"ofr5826 - 1958 - Water resources of the Ashtabula regoin, Ohio","interactions":[],"lastModifiedDate":"2023-12-15T12:15:20.73132","indexId":"ofr5826","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-26","title":"Water resources of the Ashtabula regoin, Ohio","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5826","usgsCitation":"Crawford, L.C., 1958, Water resources of the Ashtabula regoin, Ohio: U.S. Geological Survey Open-File Report 58-26, 7 p., https://doi.org/10.3133/ofr5826.","productDescription":"7 p.","costCenters":[],"links":[{"id":181846,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602e8a","contributors":{"authors":[{"text":"Crawford, L. C.","contributorId":85577,"corporation":false,"usgs":true,"family":"Crawford","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":254239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2399,"text":"wsp1460E - 1958 - Geological and geophysical study of the preglacial Teays Valley in west-central Ohio","interactions":[],"lastModifiedDate":"2023-12-15T22:44:35.683417","indexId":"wsp1460E","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1460","chapter":"E","title":"Geological and geophysical study of the preglacial Teays Valley in west-central Ohio","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1460E","usgsCitation":"Norris, S.E., and Spicer, H.C., 1958, Geological and geophysical study of the preglacial Teays Valley in west-central Ohio: U.S. Geological Survey Water Supply Paper 1460, Report: iii, 34 p.; 2 Plates: 12.00 x 18.00 inches and 17.00 x 13.00 inches, https://doi.org/10.3133/wsp1460E.","productDescription":"Report: iii, 34 p.; 2 Plates: 12.00 x 18.00 inches and 17.00 x 13.00 inches","startPage":"199","endPage":"232","costCenters":[],"links":[{"id":28378,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1460e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28379,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1460e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138960,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1460e/report-thumb.jpg"},{"id":28377,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1460e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":423659,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24390.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Ohio","county":"Champaign County, Clark County, Madison County","otherGeospatial":"Teays Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-83.5514,40.2294],[-83.4942,40.2254],[-83.5024,40.126],[-83.504,40.111],[-83.3747,40.1106],[-83.2797,40.1099],[-83.2063,40.1076],[-83.2123,40.0477],[-83.2616,40.0497],[-83.2627,40.042],[-83.2609,40.0338],[-83.2559,40.0221],[-83.2565,40.0184],[-83.2606,40.013],[-83.2648,40.0098],[-83.266,40.007],[-83.2605,39.998],[-83.2568,39.993],[-83.2531,39.9813],[-83.253,39.9699],[-83.2498,39.955],[-83.2462,39.9514],[-83.2425,39.9469],[-83.2383,39.9428],[-83.2376,39.9347],[-83.2388,39.9306],[-83.2369,39.927],[-83.2351,39.9256],[-83.2524,39.9169],[-83.2436,39.8131],[-83.2499,39.7301],[-83.2525,39.6952],[-83.423,39.7031],[-83.6252,39.7146],[-83.6534,39.7166],[-83.6471,39.7729],[-83.6466,39.7761],[-83.7388,39.7811],[-83.7407,39.7888],[-83.8079,39.7958],[-83.8295,39.7979],[-83.827,39.8224],[-83.9415,39.8288],[-83.94,39.8438],[-84.0059,39.8475],[-84.0245,39.8487],[-84.0539,39.8501],[-84.051,39.8801],[-84.0427,39.9673],[-84.0358,40.0399],[-84.0349,40.0535],[-84.035,40.0558],[-84.0232,40.1838],[-84.0188,40.2274],[-84.0188,40.2297],[-84.0143,40.2737],[-83.9829,40.2714],[-83.9739,40.271],[-83.9546,40.2699],[-83.875,40.2653],[-83.8707,40.2649],[-83.7839,40.2599],[-83.7848,40.2481],[-83.7854,40.2449],[-83.5514,40.2294]]]},\"properties\":{\"name\":\"Champaign\",\"state\":\"OH\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db687525","contributors":{"authors":[{"text":"Norris, Stanley Eugene","contributorId":24772,"corporation":false,"usgs":true,"family":"Norris","given":"Stanley","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":145136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spicer, H. Cecil","contributorId":67075,"corporation":false,"usgs":true,"family":"Spicer","given":"H.","email":"","middleInitial":"Cecil","affiliations":[],"preferred":false,"id":145137,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70194827,"text":"70194827 - 1958 - References on laboratory and equipment methods in ground water hydrology","interactions":[],"lastModifiedDate":"2018-01-10T15:37:36","indexId":"70194827","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"References on laboratory and equipment methods in ground water hydrology","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70194827","usgsCitation":"1958, References on laboratory and equipment methods in ground water hydrology, 18 p., https://doi.org/10.3133/70194827.","productDescription":"18 p.","numberOfPages":"22","costCenters":[],"links":[{"id":350418,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a615b03e4b06e28e9c260d8","contributors":{"compilers":[{"text":"Johnson, A. I.","contributorId":120232,"corporation":false,"usgs":true,"family":"Johnson","given":"A.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":725482,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":70206773,"text":"70206773 - 1958 - The environmental control of sedimentary iron minerals","interactions":[],"lastModifiedDate":"2019-11-21T13:29:44","indexId":"70206773","displayToPublicDate":"1958-11-21T13:22:16","publicationYear":"1958","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 environmental control of sedimentary iron minerals","docAbstract":"<p><span>An Eh-pH stability diagram is developed for hematite, magnetite, siderite, pyrite, and iron sulfide that indicates the relative position of their stability fields in a normal sea water system. With the exception of the magnetite-siderite relationship, Eh is much more critical than pH. In general terms, hematite is stable under oxidizing conditions, siderite and magnetite under intermediate to moderately reducing conditions, pyrite under moderate to strongly reducing conditions, and iron sulfide under still stronger reducing conditions. Because of numerous variables involved the relative positions of the stability fields are stressed rather than their limits on the Eh and pH scales. The inclusion of a magnetite field suggests that magnetite should be much more important as a primary or diagenetic mineral in sedimentary rocks than has been commonly recognized. This is in accord with numerous recent suggestions to that effect. The importance of thermodynamic equilibrium is stressed and it is suggested that differences in rates of formation of the various minerals and the persistence of some metastable phases are among the commonest causes of lack of equilibrium.</span></p>","language":"English","publisher":"Society of Economic Geology","doi":"10.2113/gsecongeo.53.2.123","usgsCitation":"Huber, N., 1958, The environmental control of sedimentary iron minerals: Economic Geology, v. 53, no. 2, p. 123-140, https://doi.org/10.2113/gsecongeo.53.2.123.","productDescription":"18 p.","startPage":"123","endPage":"140","costCenters":[],"links":[{"id":369393,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"2","noUsgsAuthors":false,"publicationDate":"1958-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Huber, N.K.","contributorId":73610,"corporation":false,"usgs":true,"family":"Huber","given":"N.K.","affiliations":[],"preferred":false,"id":775728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168613,"text":"70168613 - 1958 - Low-flow characteristics of Iowa streams","interactions":[],"lastModifiedDate":"2016-02-22T08:37:11","indexId":"70168613","displayToPublicDate":"1958-10-01T09:30:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"9","title":"Low-flow characteristics of Iowa streams","docAbstract":"<p>Study of the occurrence of low flow on interior Iowa streams and the Big Sioux River.</p>","language":"English","publisher":"State of Iowa","publisherLocation":"Des Moines","collaboration":"Prepared cooperatively by the U.S. Geological Survey, Water Resources Division, and the Iowa Natural Resources Council.","usgsCitation":"Schwob, H., 1958, Low-flow characteristics of Iowa streams: Bulletin 9, viii, 111 p.","productDescription":"viii, 111 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,{"id":70009845,"text":"70009845 - 1958 - The solusphere - its inferences and study","interactions":[],"lastModifiedDate":"2024-09-16T22:55:59.544268","indexId":"70009845","displayToPublicDate":"1958-09-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The solusphere - its inferences and study","docAbstract":"<p>Water is a fundamental geologic agent active in rock decomposition, erosion, and synthesis. Solutes in water are of particular interest to geochemists as sources of raw material for synthesis or as products of decomposition. When geochemical studies move from the laboratory into natural environment many variables relating to solute hydrology must be considered.</p><p>As a focal point there has been designed a graphical representation of solute hydrology, the solusphere, which embodies the concepts of land-water occurrence and movement on which are superimposed geologic, biologic, physical, chemical, and cultural processes affecting solutes. The solusphere is demonstrated by passing an imaginary plane through the centre of the earth. This plane intercepts concentric zones designated as rock flowage, saturation, aeration, surface activity, and atmosphere. Transport processes carry solutes within and between zones without alteration or conversion. However, whether stationary or in motion, the water's solute character is constantly subject to (1) alteration processes that change concentration by addition or subtraction of solutes or solvent without loss of solute identities, and (2) conversion processes that change the chemical state and form of solutes.</p><p>The geochemist is concerned with specific conversion processes, but he also must consider transport, alteration, and other conversion processes that are continually modifying the materials with which he is dealing in nature. The solusphere is an attempt to organize processes affecting the chemical quality of land waters into a unified field of science much like the field of marine chemistry.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(58)90083-8","usgsCitation":"Rainwater, F.H., and White, W.F., 1958, The solusphere - its inferences and study: Geochimica et Cosmochimica Acta, v. 14, no. 3, p. 244-249, https://doi.org/10.1016/0016-7037(58)90083-8.","productDescription":"6 p.","startPage":"244","endPage":"249","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":218830,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb045e4b08c986b324d4f","contributors":{"authors":[{"text":"Rainwater, F. H.","contributorId":41402,"corporation":false,"usgs":true,"family":"Rainwater","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":357273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, W. F.","contributorId":80259,"corporation":false,"usgs":true,"family":"White","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":357274,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212509,"text":"70212509 - 1958 - Geology of Kapingamarangi Atoll, Caroline Islands","interactions":[],"lastModifiedDate":"2020-08-18T18:03:02.703072","indexId":"70212509","displayToPublicDate":"1958-08-18T12:40:01","publicationYear":"1958","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":"Geology of Kapingamarangi Atoll, Caroline Islands","docAbstract":"<p><span>Kapingamarangi Atoll of the Caroline Islands consists of a peripheral reef, 1000-4000 feet across, surrounding a nearly circular lagoon which is 5 by 6 nautical miles in area and about 240 feet at maximum depth. Thirty-three islands, most of which are less than half a mile in length, are scattered along the eastern half of the peripheral reef. At least 75 patch reefs, most of which are small, nearly symmetrical mounds, rise to the surface of the lagoon. The peripheral reef and the patch reefs, composed largely of the stony structures of corals and coralline algae, have flat upper surfaces, apparently the result of bevelling by waves during a recent lowering of sea level. The islands on the peripheral reef are formed of partially consolidated stratified sediments composed of clastic limestone particles and the shells of marine animals. These islands are migrating lagoonward across the reef flat because of erosion on the seaward sides and the growth of beaches and bars on the opposite sides. Soils on the islands are poorly developed and retain much of the texture, structure, and composition of the parent rock or sediment. They consist chiefly of mechanical mixtures of carbonaceous material and lime gravel, lime sand, or lime mud. Phosphorite is present on some islands and is still forming locally where apatite derived from bird guano is reacting with limestones. The tidal fluctuation of ground-water lenses, determined on islands of several sizes, ranges from about 4 to 18 inches. In one very small island where the water is brackish, the rise is much greater. The time lag between tidal movements and the rise and fall of fresh water in the islands ranges from a few minutes on very small islands up to 5 hours on some large ones. This time lag is controlled by the permeability of rocks composing an island and varies from one area to another according to the distribution of rock types. The lagoon contains six concentric belts of bottom sediment; in each, the composition and texture depend on the depth of water in which it occurs. Lime sand and lime gravel derived for the most part from the shells of animals form most of the sediment, but a lime mud covers the bottom of the deepest parts of the lagoon. Waves and currents cause gradation between types of sediment to a depth of about 30 feet, but little mixing was detected at greater depths.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[241:GOKACI]2.0.CO;2","usgsCitation":"McKee, E.D., 1958, Geology of Kapingamarangi Atoll, Caroline Islands: GSA Bulletin, v. 69, no. 3, p. 241-278, https://doi.org/10.1130/0016-7606(1958)69[241:GOKACI]2.0.CO;2.","productDescription":"37 p.","startPage":"241","endPage":"278","costCenters":[],"links":[{"id":377628,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Federated States of Micronesia","otherGeospatial":"Kapingamarangi Atoll, Caroline Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              151.89697265625,\n              0.21972602392080884\n            ],\n            [\n              157.34619140625,\n              0.21972602392080884\n            ],\n            [\n              157.34619140625,\n              5.834616165610059\n            ],\n            [\n              151.89697265625,\n              5.834616165610059\n            ],\n            [\n              151.89697265625,\n              0.21972602392080884\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McKee, Edwin D.","contributorId":60207,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":796633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212095,"text":"70212095 - 1958 - Recent underwater surveys using low-frequency sound to locate shallow bedrock","interactions":[],"lastModifiedDate":"2020-08-14T13:57:52.366945","indexId":"70212095","displayToPublicDate":"1958-08-13T13:27:39","publicationYear":"1958","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":"Recent underwater surveys using low-frequency sound to locate shallow bedrock","docAbstract":"<p>Underwater investigations at Lake Mead, Chicago, Passamaquoddy Bay, and on Long Island established the characteristics of sound waves that can be used in shallow geophysical exploration by the sonar method.</p><p>At Lake Mead the sediments were for the most part clay of high water content which was easily penetrated by low-power sound at a frequency of 14.2 kilocycles. The greatest depth of penetration was 140 feet. Sound having frequencies of 50 and 80 kilocycles did not penetrate. At Chicago, sound at a frequecy of 11 kilocycles and an output power of 800 watts gave a satisfactory delineation of bedrock beneath Lake Michigan. The maximum distance to bedrock was about 135 feet. At Passamaquoddy Bay a sound frequency of 6 kilocycles and about 700 watts of output power gave much better delineation of bedrock. A frequency of 6 kilocycles at the lower output power was much better than 11 kilocycles at higher power. About 250 feet of penetration was attained. Pulsed power was used in each of these investigations. The pulse lengths were long—about 14–25 milliseconds.</p><p>Bedrock was mapped at Lake Mead, Chicago, and Passamaquoddy Bay. The methods of ordinary hydrographic surveying were used for horizontal and vertical positioning. For horizontal positions the ordinary three-point sextant-fix method was used. For vertical positioning, recording gages suitably placed and supplemented by staff gages were used. All data were tied into the third-order control net of the U. S. Coast and Geodetic Survey.</p><p>In connection with a study for a proposed Midwestern waterway, the technical problem was reviewed and the techniques considerably improved. New equipment was built and evaluated on Long Island Sound. It operated with pulsed power at a frequency of 6 kilocycles, and pulse length was controlled and variable from 1 to 9 milliseconds. Output acoustic power was about 2500 watts. With the transducer in ordinary operating positions as much as 400 feet of sediment was penetrated. With the transducer placed directly on the bottom of the water in Huntington Bay about 750 feet of penetration was attained. Several innovations in sonar techniques, which are desirable for sediment exploration, and which give much more detailed information than the earlier equipment are described.</p><p>The techniques required for stratigraphic interpretation of the sound records are described briefly. A method for the determination of sound velocities is discussed. Multiple echoes and other effects complicate the interpretation of records and are explained. The problems of geological control encountered also are mentioned.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[69:RUSULS]2.0.CO;2","usgsCitation":"Smith, W.O., 1958, Recent underwater surveys using low-frequency sound to locate shallow bedrock: GSA Bulletin, v. 69, no. 1, p. 69-98, https://doi.org/10.1130/0016-7606(1958)69[69:RUSULS]2.0.CO;2.","productDescription":"30 p.","startPage":"69","endPage":"98","costCenters":[],"links":[{"id":377501,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"Illinois, Maine, Nevada, New Brunswick, New York","city":"Chicago","otherGeospatial":"Lake Mead, Lake Michigan, Long Island Sound, Passamaquoddy Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n      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           -73.93798828125,\n              40.77430186363723\n            ],\n            [\n              -73.34747314453125,\n              40.88444793903562\n            ],\n            [\n              -73.06182861328125,\n              40.92388970852945\n            ],\n            [\n              -72.59765625,\n              40.96123389519331\n            ],\n            [\n              -72.25433349609375,\n              41.143501411390766\n            ],\n            [\n              -71.817626953125,\n              41.32938883149378\n            ],\n            [\n              -72.4713134765625,\n              41.308760782192856\n            ],\n            [\n              -72.91900634765625,\n              41.29844430929419\n            ],\n            [\n              -73.2183837890625,\n              41.18278832811288\n            ],\n            [\n              -73.49578857421875,\n              41.08142149109681\n            ],\n            [\n              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O.","contributorId":53015,"corporation":false,"usgs":true,"family":"Smith","given":"W.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":796229,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212081,"text":"70212081 - 1958 - The relation of phosphorites to ground water in Beaufort County, North Carolina","interactions":[],"lastModifiedDate":"2020-08-14T13:59:30.7653","indexId":"70212081","displayToPublicDate":"1958-08-13T12:28:37","publicationYear":"1958","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 relation of phosphorites to ground water in Beaufort County, North Carolina","docAbstract":"<p><span>Recent ground-water studies undertaken by the U.S. Geological Survey in cooperation with the North Carolina Division of Mineral Resources have delineated phosphorite deposits, tentatively regarded as being of middle Miocene age, in Beaufort County. These deposits lie unconforma-bly on limestone of Eocene age and are unconformably overlain by late Miocene marl. The phosphorites, buried beneath strata ranging in thickness from 45 to 250 feet, underlie an area approximating 450 square miles. The total thickness of the phosphorite column throughout the area ranges from several feet to nearly 90 feet. </span></p><p><span>The phosphorite column consists of phosphatic sands and intercalated shell limestones. The sands, composed of pellets of brown sand-size collophane (probably carbonate-fluorapatite) and sand-size, flat-sided angular quartz with some silt, clay, and organic material, have a median diameter between 0.50 and 0.25 mm. Chemical analyses of representative samples of the raw sand show a variation in PaOs content from 8 to 31 percent. The P2O5 content is apparently proportionate to the collophane content throughout the area. Reconstruction of the geologic history suggests that the phosphorites were deposited as chemical precipitates and as in situ replacements in a restricted marine basin where the pH of the water acted as the primary depositional control. </span></p><p><span>Reconstruction of the hydrologic history of the phosphorites indicates that the deposits were preserved under artesian conditions; they were never subjected to alteration under water-table conditions. The absence of postpositional alteration makes this area a potentially classic one for studies of phosphorite genesis. </span></p><p><span>Chemical analyses of artesian waters from the phosphorites and from limestones overlain by phosphorites reveal significantly greater concentrations of iodide and bromide in solution than are present in water from overlying sediments or from underlying limestones not overlain by phosphorites. Such anomalies, if present in other similar terranes, may indicate the presence of buried phosphorites. The depth and size distribution of the material suggest a recovery method utilizing wells constructed to \"pump sand.\"</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.53.1.85","usgsCitation":"Brown, P., 1958, The relation of phosphorites to ground water in Beaufort County, North Carolina: Economic Geology, v. 53, p. 85-101, https://doi.org/10.2113/gsecongeo.53.1.85.","productDescription":"17 p.","startPage":"85","endPage":"101","costCenters":[],"links":[{"id":377499,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","county":"Beaufort","otherGeospatial":"Beaufort  County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.8109130859375,\n              35.46514408578589\n            ],\n            [\n              -76.75048828125,\n              35.84008157153468\n            ],\n            [\n              -77.310791015625,\n              35.91129848822746\n            ],\n            [\n              -77.7667236328125,\n              35.78662688467009\n            ],\n            [\n              -77.8436279296875,\n              35.55010533588552\n            ],\n            [\n              -77.3162841796875,\n              35.28150065789119\n            ],\n            [\n              -76.97021484375,\n              35.28150065789119\n            ],\n            [\n              -76.86035156249999,\n              35.40696093270201\n            ],\n            [\n              -77.27783203125,\n              35.594785665487244\n            ],\n            [\n              -77.14599609375,\n              35.60818490437746\n            ],\n            [\n              -76.8109130859375,\n              35.46514408578589\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"53","noUsgsAuthors":false,"publicationDate":"1958-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Brown, P.M.","contributorId":46324,"corporation":false,"usgs":true,"family":"Brown","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":796226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212070,"text":"70212070 - 1958 - Uranium deposits under conglomeratic sandstone of the Morrison Formation, Colorado and Utah","interactions":[],"lastModifiedDate":"2020-08-14T14:05:19.628286","indexId":"70212070","displayToPublicDate":"1958-08-13T11:40:12","publicationYear":"1958","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":"Uranium deposits under conglomeratic sandstone of the Morrison Formation, Colorado and Utah","docAbstract":"<p><span>In southwestern Colorado and southeastern Utah, strata of conglomeratic sandstone are localized at the base of the Brushy Basin Member of the Morrison Formation of Jurassic age. These discrete lithologic units contain sedimentary structures oriented in a prevailing easterly direction. They are believed to cover about one-third of the underlying Salt Wash Member in southwestern Colorado and southeastern Utah, and they locally rest on ore-bearing sandstone in the Salt Wash Member. Eastward-trending planar cross-stratification and trough cross-stratification and a general westward coarsening of sediments in the conglomeratic sandstone strata suggest that they are the products of stream aggradation from westerly source areas. Uranium-vanadium deposits in the uppermost, almost continuous, layer of sandstone of the Salt Wash Member are classified according to their association with the conglomerate strata. Of the 363 deposits studied in the uppermost sandstone layer of the Salt Wash Member, 101 are known to be directly beneath conglomeratic sandstone strata, 211 are below the projected extension of conglomeratic sandstone strata, 33 are beyond the safe limits of such projection, and 18 are lateral to the margins of conglomeratic sandstone strata. At places, near clusters of deposits in the uppermost sandstone of the underlying Salt Wash Member, conglomeratic sandstone strata of the Brushy Basin Member are also mineralized. It is postulated that ground-water movement during deposition of the Morrison Formation in Late Jurassic time localized the uranium and vanadium. The direction of this ground-water movement is believed to have been related to streams that deposited the conglomeratic strata, so that in the ore-bearing sandstone metal ions contained in the ground water were localized in places of high transmissibility and in the vicinity of decaying organic debris. According to the age of the ores, precipitation of the metals was much later than their localization, probably during Late Cretaceous or early Tertiary time.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1958)69[403:UDUCSO]2.0.CO;2","usgsCitation":"Phoenix, D.A., 1958, Uranium deposits under conglomeratic sandstone of the Morrison Formation, Colorado and Utah: GSA Bulletin, v. 69, no. 4, p. 403-418, https://doi.org/10.1130/0016-7606(1958)69[403:UDUCSO]2.0.CO;2.","productDescription":"16 p.","startPage":"403","endPage":"418","costCenters":[],"links":[{"id":377497,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Morrison Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.0830078125,\n              37.020098201368114\n            ],\n            [\n              -108.160400390625,\n              37.020098201368114\n            ],\n            [\n              -108.160400390625,\n              39.16414104768742\n            ],\n            [\n              -110.0830078125,\n              39.16414104768742\n            ],\n            [\n              -110.0830078125,\n              37.020098201368114\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"69","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Phoenix, D. A.","contributorId":92665,"corporation":false,"usgs":true,"family":"Phoenix","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":796222,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211928,"text":"70211928 - 1958 - Application of statistical methods to the analysis of ground‐water levels","interactions":[],"lastModifiedDate":"2020-08-11T19:31:46.319712","indexId":"70211928","displayToPublicDate":"1958-08-11T14:23:06","publicationYear":"1958","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":"Application of statistical methods to the analysis of ground‐water levels","docAbstract":"<p><span>Valuable hydrologic information can be obtained from statistical analysis of water‐level trends. The time‐series and the functional‐equation approaches are applied to New Jersey well records representing different hydrologic conditions. The results are valuable as concise summaries of the records, for extrapolating observed data, for interpolating between measurements, and for estimating hydrologic factors such as coefficients of transrnissibility and storage, evapotranspiration, and ground‐water discharge.&nbsp;</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/TR039i001p00075","usgsCitation":"Remson, I., and Randolph, J., 1958, Application of statistical methods to the analysis of ground‐water levels: Eos, Transactions, American Geophysical Union, v. 39, no. 1, p. 75-83, https://doi.org/10.1029/TR039i001p00075.","productDescription":"9 p.","startPage":"75","endPage":"83","costCenters":[],"links":[{"id":377381,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Remson, Irwin","contributorId":89115,"corporation":false,"usgs":true,"family":"Remson","given":"Irwin","email":"","affiliations":[],"preferred":false,"id":795845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randolph, J.R.","contributorId":19532,"corporation":false,"usgs":true,"family":"Randolph","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":795846,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211918,"text":"70211918 - 1958 - Reconnaissance study of erosion and deposition produced by the flood of August 1955 in Connecticut","interactions":[],"lastModifiedDate":"2020-08-11T19:16:55.176465","indexId":"70211918","displayToPublicDate":"1958-08-11T14:08:12","publicationYear":"1958","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":"Reconnaissance study of erosion and deposition produced by the flood of August 1955 in Connecticut","docAbstract":"<p><span>A large area in the valley bottoms in Connecticut was inundated by the flood of August 1955. Relative to the total area flooded that part permanently modified by the flow was surprisingly small. Although great in some places, the distribution of these permanent modifications of channel and flood plain was spotty. Erosion of the channel and valley bottom appears to have been most severe in narrow, steep valleys. Environments of deposition were diverse. They appeared to be related to rate and direction of flow, quantity and size of sediments locally available, and in some cases to the presence of vegetation. Most of the coarse sediment deposited in the valley appears to have been derived from local sources such as valley walls and terraces composed of glacial outwash and till and flood plains containing considerable gravel. Fine sand predominated in most of the sediment deposited. Considering the magnitude of the runoff, the quantity of fine sediment transported or deposited by the flood was small. The maximum observed concentration was 473 parts per million in Scantic River at Broad Brook. Newly deposited fine sediments are thin or absent on the flood plains of many valleys which were beneath 20 ft of slow‐moving flood waters. The paucity of deposition in such ideal depositional environments also indicates that the flow did not have a high concentration of fine sediments. A number of boulders five to seven feet in diameter were moved by flood waters in reaches in which smaller gravels were undisturbed. Severe erosion in the uplands was minor. In this reconnaissance we saw little evidence of newly formed gullies and no areas of severe sheet erosion. This was the case in both woodland and pasture land. Large amounts of subsurface flow and relatively unerodible ground are presumed to be responsible for the absence of erosion.</span></p>","language":"English","publisher":"Wiley","doi":"10.1029/TR039i001p00001","usgsCitation":"Wolman, M.G., and Eiler, J., 1958, Reconnaissance study of erosion and deposition produced by the flood of August 1955 in Connecticut: Eos, Transactions, American Geophysical Union, v. 39, no. 1, p. 1-14, https://doi.org/10.1029/TR039i001p00001.","productDescription":"14 p.","startPage":"1","endPage":"14","costCenters":[],"links":[{"id":377372,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"39","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wolman, M. Gordon","contributorId":85163,"corporation":false,"usgs":true,"family":"Wolman","given":"M.","email":"","middleInitial":"Gordon","affiliations":[],"preferred":false,"id":795803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eiler, J.P.","contributorId":238011,"corporation":false,"usgs":false,"family":"Eiler","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":795804,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70211916,"text":"70211916 - 1958 - Technique for the extraction and partial chemical analysis of fluid-filled inclusions from minerals","interactions":[],"lastModifiedDate":"2020-08-11T18:54:58.544298","indexId":"70211916","displayToPublicDate":"1958-08-11T13:47:36","publicationYear":"1958","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":"Technique for the extraction and partial chemical analysis of fluid-filled inclusions from minerals","docAbstract":"<p><span>A method has been developed for the extraction and limited chemical analysis of the materials in solution in the fluid from the very minute fluid-filled inclusions such as commonly occur in whitish or milky quartz. The method may also be applied, with some reservations, to a variety of other minerals. As the amounts of substances in the fluid are small compared with possible contaminants, great care is needed in sample purification and cleaning; an electrolytic method has been found to be the only satisfactory final cleaning step. Following this, the inclusions are opened by ball milling of the cleaned sample, with deionized water, in an alumina ball mill using alumina grinding media. The ions present in the resultant slurry are separated from the ground quartz by electrodialysis and analyzed. Other methods, such as the decrepitation of a sample in an absorption train, are used to estimate the amount of H2O and CO2 in the inclusions. The most significant part of the analytical work has been to determine the ratios between the alkali metals. </span></p><p><span>The materials in solution in the fluid-filled inclusions from 11 samples of quartz have been analyzed by the ball milling-electrodialysis method. Although there are large differences between samples, the average weights of the alkali metal ions found, for all samples, in milligrams per kilogram of quartz, are: Li+-0.92, Na+-99, K+-133, Rb+-0.45, Cs+-0.38 (atomic ratios, in the same sequence: 0.03/1.00/0.79/0.001/0.0007). In addition, 27 to 193 milligrams of CI\", and 5 to 140 milligrams of SOr were found, per kilogram of quartz. H2O and COa were determined on only one sample. Six of the samples were from gold-quartz veins in the Grass Valley district, California. In these six the Na+/K+ ratios were all very similar, but the amounts of Li+, Rb+ and Cs+ found varied greatly. Although there are serious limitations to this and to all other techniques developed, it is felt that the results presented are sufficiently encouraging to warrant further study and possible application to specific geologic problems, such as the identification of epochs of quartz deposition</span></p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/gsecongeo.53.3.235","usgsCitation":"Roedder, E., 1958, Technique for the extraction and partial chemical analysis of fluid-filled inclusions from minerals: Economic Geology, v. 53, no. 3, p. 235-269, https://doi.org/10.2113/gsecongeo.53.3.235.","productDescription":"35 p.","startPage":"235","endPage":"269","costCenters":[],"links":[{"id":377367,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"3","noUsgsAuthors":false,"publicationDate":"1958-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Roedder, Edwin","contributorId":25571,"corporation":false,"usgs":true,"family":"Roedder","given":"Edwin","affiliations":[],"preferred":false,"id":795801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211913,"text":"70211913 - 1958 - Limestone aquifers of Maryland","interactions":[],"lastModifiedDate":"2020-08-11T18:08:28.465533","indexId":"70211913","displayToPublicDate":"1958-08-11T13:02:12","publicationYear":"1958","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":"Limestone aquifers of Maryland","docAbstract":"<p><span>Limestone rocks are an important source of ground water in the Piedmont and Appalachian areas of Maryland. The major limestone aquifers are the Cockeysville and Wakefield marbles and the Silver Run, Tomstown, Frederick, Grove, Waynesboro, Elbrook, Conococheague, Beekmantown, Stones River, Tonoloway, Helderberg and Greenbrier formations. Drilled and dug wells and springs are common sources of water supply in the limestone areas. The depths of 298 limestone wells range from 8.7 to 1,800 feet and average about 150 feet. The yields of these wells range from 0.1 to 575 gpm. Specific capacities, or yield per foot of drawdown, range in 137 wells from 0.1 to 43 gpm per foot. Springs are common in the limestone areas and their flow varies widely at different times. Most of the known springs are of the 5th magnitude or lower, and therefore have a mean flow of less than 100 gpm. The quality of water from the limestone aquifers is satisfactory for most purposes, but is commonly hard and slightly alkaline. The limestone aquifers are large essentially untapped ground-water reservoirs whose hydrologic character is only partially understood.&nbsp;</span></p>","language":"English","publisher":"GeoScienceWorld","doi":"10.2113/gsecongeo.53.6.722","usgsCitation":"Otton, E.G., and Richardson, C.A., 1958, Limestone aquifers of Maryland: Economic Geology, v. 53, no. 6, p. 722-736, https://doi.org/10.2113/gsecongeo.53.6.722.","productDescription":"15 p.","startPage":"722","endPage":"736","costCenters":[],"links":[{"id":377358,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Limestone aquifers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.508056640625,\n              38.762650338334154\n            ],\n            [\n              -75.59692382812499,\n              38.762650338334154\n            ],\n            [\n              -75.59692382812499,\n              39.76632525654491\n            ],\n            [\n              -79.508056640625,\n              39.76632525654491\n            ],\n            [\n              -79.508056640625,\n              38.762650338334154\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"53","issue":"6","noUsgsAuthors":false,"publicationDate":"1958-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Otton, Edmond G.","contributorId":96989,"corporation":false,"usgs":true,"family":"Otton","given":"Edmond","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":795797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richardson, Claire A.","contributorId":33299,"corporation":false,"usgs":true,"family":"Richardson","given":"Claire","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":795798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175839,"text":"70175839 - 1958 - Correlation of ground-water levels and air temperatures in the winter and spring in Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T10:16:49","indexId":"70175839","displayToPublicDate":"1958-06-17T12:45:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5181,"text":"Technical Paper","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"1","title":"Correlation of ground-water levels and air temperatures in the winter and spring in Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Minnesota Department of Conservation, Division of Waters","publisherLocation":"St. Paul, MN","usgsCitation":"Schneider, R., 1958, Correlation of ground-water levels and air temperatures in the winter and spring in Minnesota: Technical Paper 1, 17 p.","productDescription":"17 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,{"id":5220584,"text":"5220584 - 1958 - Aspergillosis in waterfowl","interactions":[],"lastModifiedDate":"2025-07-25T15:39:28.787199","indexId":"5220584","displayToPublicDate":"1958-06-16T12:18:25","publicationYear":"1958","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Aspergillosis in waterfowl","docAbstract":"<p>No abstract available.</p>","conferenceTitle":"Twenty-third North American Wildlife Conference","conferenceDate":"March 3-5, 1958","conferenceLocation":"St. Louis, MO","language":"English","publisher":"Wildlife Management Institute","usgsCitation":"Herman, C.M., and Sladen, W.J., 1958, Aspergillosis in waterfowl, Twenty-third North American Wildlife Conference, St. Louis, MO, March 3-5, 1958, p. 187-191.","productDescription":"5 p.","startPage":"187","endPage":"191","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":492912,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wildlifemanagement.institute/conference/transactions/1958","linkFileType":{"id":5,"text":"html"}},{"id":196157,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672b46","contributors":{"authors":[{"text":"Herman, Carlton M.","contributorId":88718,"corporation":false,"usgs":true,"family":"Herman","given":"Carlton","email":"","middleInitial":"M.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":332052,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sladen, William J.L.","contributorId":85676,"corporation":false,"usgs":false,"family":"Sladen","given":"William","email":"","middleInitial":"J.L.","affiliations":[],"preferred":false,"id":332051,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221451,"text":"70221451 - 1958 - The thermal regime of an Arctic lake","interactions":[],"lastModifiedDate":"2021-06-16T13:22:04.639707","indexId":"70221451","displayToPublicDate":"1958-06-16T08:20:30","publicationYear":"1958","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":"The thermal regime of an Arctic lake","docAbstract":"<p>Much of the Arctic coastal plain in Alaska is covered by shallow lakes. Those in the Barrow area, which are believed to be representative of most of the lakes in the coastal plain, are generally either two to three feet or six to nine feet deep. The shallow lakes can often provide a suitable summer water supply, but only the deeper lakes provide a significant water supply throughout the year.</p><p>The water in the individual lakes is in an essentially isothermal state during the ice-free period that lasts from late June until September. The maximum temperature recorded in a lake near Barrow in 1954 was about 12°C. When ice formation begins, the temperature of the body of water as a whole may be only a few tenths of a degree above 0°C. Once the lake surface is iced over, the water temperatures may rise rapidly as much as 2°C, apparently owing to radiated heat received through the ice. The heating is terminated by a sudden cooling that coincides with the covering of the ice by a thin blanket of snow. This cooling is followed in turn by a second warming of the bottom and near-bottom water that takes place gradually over a period of weeks. The bottom sediments beneath the lake are the source of heat. The magnitude of the second rise and the time during which it takes place depend on the distance from shore and the depth of water. A gradual cooling takes place during the balance of the winter. Permafrost underlies the shallow lakes but an unfrozen basin several hundred feet deep may extend beneath the deeper lakes.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR039i002p00278","usgsCitation":"Brewer, M.C., 1958, The thermal regime of an Arctic lake: Eos, Transactions, American Geophysical Union, v. 39, no. 2, p. 278-284, https://doi.org/10.1029/TR039i002p00278.","productDescription":"7 p.","startPage":"278","endPage":"284","costCenters":[],"links":[{"id":386528,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Brewer, Max C.","contributorId":260352,"corporation":false,"usgs":false,"family":"Brewer","given":"Max","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":817750,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170553,"text":"70170553 - 1958 - Operator's manual on the visual-accumulation tube method for sedimentation analysis of sands","interactions":[],"lastModifiedDate":"2018-03-05T12:25:42","indexId":"70170553","displayToPublicDate":"1958-06-01T13:45:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":66,"text":"Report","active":false,"publicationSubtype":{"id":1}},"chapter":"K","title":"Operator's manual on the visual-accumulation tube method for sedimentation analysis of sands","docAbstract":"<p>The visual-tube method for sedimentation analysis of sands was developed as a part of the general investigation titled \"A Study of Methods Used in Measurement and Analysis of Sediment Loads in Streams.\"&nbsp;The method is one answer to the need for a simple, rapid, and inexpensive means of determining the sedimentation-size frequency analysis of sand samples containing particles less than one millimeter in size. For analysis of coarser sands see the Appendix, Section 13, Report No. 11 \"The Development and Calibration of the Visual-Accumulation-Tube\" is available for those who have further interest in this analysis.</p>\n<p>The personnel who will be operating these units may have little or no previous knowledge of either the principles involved or the details of opera.ting procedure. This manual is intended as an aid to them in setting up the apparatus, learning the analytical procedure, interpreting the results, and understanding the primary principles encountered.</p>","language":"English","publisher":"Federal Interagency Sedimentation Project","publisherLocation":"Minneapolis, MN","usgsCitation":"Colby, V., and Witzgman, F., 1958, Operator's manual on the visual-accumulation tube method for sedimentation analysis of sands: Report, 30 p.","productDescription":"30 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320511,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":320510,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://water.usgs.gov/fisp/docs/Report_K.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571f3fd6e4b071321fe56a70","contributors":{"authors":[{"text":"Colby, V.C.","contributorId":168886,"corporation":false,"usgs":false,"family":"Colby","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":627599,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witzgman, F.W.","contributorId":168892,"corporation":false,"usgs":false,"family":"Witzgman","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":627600,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047833,"text":"70047833 - 1958 - Design of irrigation ponds using pond and ground-water storage","interactions":[{"subject":{"id":15625,"text":"ofr5795 - 1957 - The design of irrigation ponds using pond and ground-water storage","indexId":"ofr5795","publicationYear":"1957","noYear":false,"title":"The design of irrigation ponds using pond and ground-water storage"},"predicate":"SUPERSEDED_BY","object":{"id":70047833,"text":"70047833 - 1958 - Design of irrigation ponds using pond and ground-water storage","indexId":"70047833","publicationYear":"1958","noYear":false,"title":"Design of irrigation ponds using pond and ground-water storage"},"id":1}],"lastModifiedDate":"2026-03-12T16:06:31.085115","indexId":"70047833","displayToPublicDate":"1958-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3620,"text":"Transactions of the ASAE","active":true,"publicationSubtype":{"id":10}},"title":"Design of irrigation ponds using pond and ground-water storage","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"American Society of Agricultural and Biological Engineers","doi":"10.13031/2013.41217","usgsCitation":"Remson, I., and Randolph, J., 1958, Design of irrigation ponds using pond and ground-water storage: Transactions of the ASAE, v. 1, no. 1, p. 0065-0067, https://doi.org/10.13031/2013.41217.","productDescription":"3 p.","startPage":"0065","endPage":"0067","costCenters":[],"links":[{"id":277009,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521c78e5e4b01458f7842928","contributors":{"authors":[{"text":"Remson, Irwin","contributorId":89115,"corporation":false,"usgs":true,"family":"Remson","given":"Irwin","email":"","affiliations":[],"preferred":false,"id":483097,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randolph, J.R.","contributorId":19532,"corporation":false,"usgs":true,"family":"Randolph","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":483096,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3029,"text":"wsp1370A - 1958 - Floods of June 1954 in Iowa","interactions":[],"lastModifiedDate":"2023-03-23T19:09:03.740959","indexId":"wsp1370A","displayToPublicDate":"1958-01-01T00:00:00","publicationYear":"1958","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1370","chapter":"A","title":"Floods of June 1954 in Iowa","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1370A","usgsCitation":"Yost, I.D., 1958, Floods of June 1954 in Iowa: U.S. Geological Survey Water Supply Paper 1370, viii, 106 p., https://doi.org/10.3133/wsp1370A.","productDescription":"viii, 106 p.","costCenters":[],"links":[{"id":414644,"rank":3,"type":{"id":36,"text":"NGMDB Index 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,{"id":1000102,"text":"1000102 - 1958 - Relationship between Secchi disc readings and light penetration in Lake Huron","interactions":[],"lastModifiedDate":"2016-02-08T14:13:40","indexId":"1000102","displayToPublicDate":"1958-01-01T00:00:00","publicationYear":"1958","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":"Relationship between Secchi disc readings and light penetration in Lake Huron","docAbstract":"<p><span>Fifty-seven paired photometer and Secchi disc measurements made at 18 stations in Saginaw Bay and Lake Huron support the view that a counter-clockwise current usually occurs in the Bay with more transparent Lake Huron water flowing in along the northwest shore and less transparent Bay water flowing out along the southeast shore. The average percentage transmission of surface light intensity, at the Secchi disc depth, was 14.7 percent. Discrepancies in the relationship of disc readings to percentage transmission of surface light are related to the condition of the sky and sea. It is suggested that these discrepancies can best be explained on the basis of the spectral sensitivity of the human eye and its response to surface glare.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1957)87[73:RBSDRA]2.0.CO;2","usgsCitation":"Beeton, A.M., 1958, Relationship between Secchi disc readings and light penetration in Lake Huron: Transactions of the American Fisheries Society, v. 87, p. 73-79, https://doi.org/10.1577/1548-8659(1957)87[73:RBSDRA]2.0.CO;2.","productDescription":"7 p.","startPage":"73","endPage":"79","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":486792,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1577/1548-8659(1957)87[73:rbsdra]2.0.co;2","text":"Publisher Index Page"},{"id":128470,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634829","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":308082,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010455,"text":"70010455 - 1958 - Potassium bromide method of infrared sampling","interactions":[],"lastModifiedDate":"2020-08-27T20:48:41.078158","indexId":"70010455","displayToPublicDate":"1958-01-01T00:00:00","publicationYear":"1958","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":"Potassium bromide method of infrared sampling","docAbstract":"In the preparation of potassium bromide pressed windows for use in the infrared analysis of solids, severe grinding of the potassium bromide powder may produce strong absorption bands that could interfere seriously with the spectra of the sample. These absorption bands appear to be due to some crystal alteration of the potassium bromide as a result of the grinding process. They were less apt to occur when the coarser powder, which had received a relatively gentle grinding, was used. Window blanks prepared from the coarser powders showed smaller adsorbed water peaks and generally higher over-all transmittance readings than windows pressed from the very fine powders.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60144a014","usgsCitation":"Milkey, R., 1958, Potassium bromide method of infrared sampling: Analytical Chemistry, v. 30, no. 12, p. 1931-1933, https://doi.org/10.1021/ac60144a014.","productDescription":"3 p.","startPage":"1931","endPage":"1933","numberOfPages":"3","costCenters":[],"links":[{"id":218870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"12","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a7ea9e4b0c8380cd7a686","contributors":{"authors":[{"text":"Milkey, R.G.","contributorId":89125,"corporation":false,"usgs":true,"family":"Milkey","given":"R.G.","affiliations":[],"preferred":false,"id":358966,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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