{"pageNumber":"2617","pageRowStart":"65400","pageSize":"25","recordCount":68827,"records":[{"id":2339,"text":"wsp1424 - 1958 - Ground-water factors affecting drainage in the First Division, Buffalo Rapids Irrigation Project, Prairie and Dawson Counties, Montana, with a section on chemical character of the water","interactions":[],"lastModifiedDate":"2023-11-02T19:06:45.983284","indexId":"wsp1424","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":"1424","title":"Ground-water factors affecting drainage in the First Division, Buffalo Rapids Irrigation Project, Prairie and Dawson Counties, Montana, with a section on chemical character of the water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1424","usgsCitation":"Moulder, E.A., Kohout, F.A., and Jochens, E.R., 1958, Ground-water factors affecting drainage in the First Division, Buffalo Rapids Irrigation Project, Prairie and Dawson Counties, Montana, with a section on chemical character of the water: U.S. Geological Survey Water Supply Paper 1424, Report: vi, 198 p.; 11 Plates: 47.72 x 15.00 inches or smaller, https://doi.org/10.3133/wsp1424.","productDescription":"Report: vi, 198 p.; 11 Plates: 47.72 x 15.00 inches or smaller","costCenters":[],"links":[{"id":422352,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24378.htm","linkFileType":{"id":5,"text":"html"}},{"id":28232,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28231,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28235,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1424/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28234,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28233,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28230,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28229,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28228,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28227,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28226,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28225,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28224,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1424/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138576,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1424/report-thumb.jpg"}],"country":"United States","state":"Montana","county":"Dawson County, Prairie County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -105.15410069946182,\n              46.86536358937272\n            ],\n            [\n              -105.07253102519756,\n              46.769672022650184\n            ],\n            [\n              -104.61515820878664,\n              46.96088488162158\n            ],\n            [\n              -104.62681101939576,\n              47.15141679638268\n            ],\n            [\n              -104.75499193609689,\n              47.16330243885534\n            ],\n            [\n              -105.17449311802797,\n              46.88527789908929\n            ],\n            [\n              -105.15410069946182,\n              46.86536358937272\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce39","contributors":{"authors":[{"text":"Moulder, E. A.","contributorId":78719,"corporation":false,"usgs":true,"family":"Moulder","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kohout, Francis Anthony","contributorId":11200,"corporation":false,"usgs":true,"family":"Kohout","given":"Francis","email":"","middleInitial":"Anthony","affiliations":[],"preferred":false,"id":145045,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jochens, E. R.","contributorId":101250,"corporation":false,"usgs":true,"family":"Jochens","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":887470,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010754,"text":"70010754 - 1958 - Biogeochemistry of the rare-earth elements with particular reference to hickory trees","interactions":[],"lastModifiedDate":"2020-11-12T21:11:22.260526","indexId":"70010754","displayToPublicDate":"1958-01-01T00:00:00","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":"Biogeochemistry of the rare-earth elements with particular reference to hickory trees","docAbstract":"<p>Hickory trees concentrate the rare-earth elements in their leaves to a phenomenal degree and may contain as much as 2300 p.p.m. of total rare earths based on the dry weight of the leaves. The average proportions of the individual elements (atomic percent of the total rare-earth elements) in the leaves are: Y 36, La 16, Ce 14, Pr 2, Nd 20, Sm 1, Eu 0.7, Gd 3, Tb 0.6, Dy 3, Ho 0.7, Er 2, Tm 0.2, Yb 1, and Lu 0.2. The similarity in the proportions of the rare-earth elements in the leaves and in the exchange complex of the soil on which the hickory trees grow indicates that the trees do not fractionate the rare earths appreciably.</p><p>The variation of the rare-earth elements in the leaves and soils can be explained generally in terms of the relative abundance of the cerium group and the yttrium group, except for the element cerium. The large fluctuations in the proportion of cerium [Ce/(La + Nd) atomic ratios of 0.16 to 0.86] correlate with oxidation-reduction conditions in the soil profile. The substitution of dilute H<sub>2</sub>SO<sub>3</sub><span>&nbsp;</span>for dilute HC1 in the determination of available rare-earth elements brings about a large increase in the proportion of cerium that is extracted from an oxygenated subsoil. These relationships strongly suggest that quadrivalent cerium is present in oxygenated subsoil and is less available to plants than the other rare-earth elements that do not undergo such a change in valence.</p><p>A few parts per billion of rare-earth elements have been detected in two samples of ground water.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(58)90093-0","usgsCitation":"Robinson, W.O., Bastron, H., and Murata, K.J., 1958, Biogeochemistry of the rare-earth elements with particular reference to hickory trees: Geochimica et Cosmochimica Acta, v. 14, no. 1-2, p. 55-67, https://doi.org/10.1016/0016-7037(58)90093-0.","productDescription":"13 p.","startPage":"55","endPage":"67","numberOfPages":"13","costCenters":[],"links":[{"id":219705,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f159e4b0c8380cd4abeb","contributors":{"authors":[{"text":"Robinson, W. O.","contributorId":56924,"corporation":false,"usgs":true,"family":"Robinson","given":"W.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":359574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bastron, H.","contributorId":20067,"corporation":false,"usgs":true,"family":"Bastron","given":"H.","affiliations":[],"preferred":false,"id":359573,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murata, K. J.","contributorId":18759,"corporation":false,"usgs":true,"family":"Murata","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359572,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010753,"text":"70010753 - 1958 - The water, deuterium, gas and uranium content of tektites","interactions":[],"lastModifiedDate":"2020-08-27T20:38:06.205475","indexId":"70010753","displayToPublicDate":"1958-01-01T00:00:00","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 water, deuterium, gas and uranium content of tektites","docAbstract":"<p>The water content, deuterium concentration of the water, total gas and uranium contents were determined on tektite samples and other glass samples from Texas, Australia, Philippine Islands, Java, French Indo-China, Czechoslovakia, Libyan Desert, Billiton Island, Thailand, French West Africa, Peru, and New Mexico. The water content ranges from 0.24 per cent for the Peru tektite, to 0.0002 per cent for a moldavite. The majority of the tektites have less than 0.05 per cent water, and average 0.005 per cent H<sub>2</sub>O by weight. No other gases were detected, the lower detection limit being about 1 p.p.m. by weight. The deuterium content of the water in tektites is in the same range as that in terrestrial waters, and varies from 0.010 mole per cent to 0.0166 mole per cent deuterium. The uranium content is about from 1 to 3 p.p.m.</p><p>The possible origin of tektites is discussed. The experimental data presented favour their being originally terrestrial, but produced by some catastrophic event. An extra-terrestrial source is not ruled out.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(58)90071-1","usgsCitation":"Friedman, I., 1958, The water, deuterium, gas and uranium content of tektites: Geochimica et Cosmochimica Acta, v. 14, no. 4, p. 316-324, https://doi.org/10.1016/0016-7037(58)90071-1.","productDescription":"8 p.","startPage":"316","endPage":"324","costCenters":[],"links":[{"id":219641,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb1d3e4b08c986b325432","contributors":{"authors":[{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":359571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010755,"text":"70010755 - 1958 - Role of clay minerals in the transportation of iron","interactions":[],"lastModifiedDate":"2020-11-12T21:08:59.390801","indexId":"70010755","displayToPublicDate":"1958-01-01T00:00:00","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":"Role of clay minerals in the transportation of iron","docAbstract":"<p>The clay minerals have iron associated with them in several ways:</p><dl class=\"list\"><dt class=\"list-label\">1.</dt><dd class=\"list-description\"><p>(1) as an essential constituent</p></dd><dt class=\"list-label\">2.</dt><dd class=\"list-description\"><p>(2) as a minor constituent within the crystal lattice where it is in isomorphous substitution and</p></dd><dt class=\"list-label\">3.</dt><dd class=\"list-description\"><p>(3) as iron oxide on the surface of the mineral platelets. Nontronite, “hydromica,” some chlorites, vermiculite, glauconite and chamosite contain iron as an essential constituent. Kaolinite and halloysite have no site within the lattice for iron, but in certain environments iron oxide (goethite or hematite) is intimately associated as a coating on the micelles. Analyses of clay minerals show that the content of Fe<sub>2</sub>O<sub>3</sub><span>&nbsp;</span>varies: 29 per cent (nontronite), 7·3 per cent (griffithite), 4.5 per cent (“hydromica”), 5.5 per cent (chlorite), 4 per cent (vermiculite) and 18 per cent (glauconite). The FeO content is: 40 per cent (chamosite), 7.8 per cent (griffithite), 1–2 per cent (“hydromica”), 3 per cent (glauconite) and 2 per cent (chlorite).</p></dd></dl><p>The iron associated with the clay minerals remains stable in the environment in which the minerals occur, but if either pH or Eh or both are changed the iron may be affected. Change of environment will cause:</p><dl class=\"list\"><dt class=\"list-label\">1.</dt><dd class=\"list-description\"><p>(1) removal of iron by reduction of Fe<sup>3+</sup><span>&nbsp;</span>to Fe<sup>2+</sup>;</p></dd><dt class=\"list-label\">2.</dt><dd class=\"list-description\"><p>(2) ion-exchange reactions;</p></dd><dt class=\"list-label\">3.</dt><dd class=\"list-description\"><p>(3) instability of the crystal lattice.</p></dd></dl><p>Experiments using bacterial activity to produce reducing conditions with kaolinite and halloysite coated with iron oxides and with nontronite in which ferric iron is in the octahedral position within the lattice showed that ferric oxide is removed at Eh +0·215 in fresh water and at Eh +0.098 in sea water. Hematite, goethite, and indefinite iron oxides were removed at different rates. Red ferric oxides were changed to black indefinite noncrystalline ferrous sulphide at Eh −0.020 but reverted to ferric oxide under oxidizing conditions. Nontronite turned bright green under reducing conditions and some of the ferrous iron remained within the lattice on a return to oxidizing conditions. Bacterial activity seems to be necessary for maintaining reducing conditions in the environments studied.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(58)90090-5","usgsCitation":"Carroll, D., 1958, Role of clay minerals in the transportation of iron: Geochimica et Cosmochimica Acta, v. 14, no. 1-2, p. 1-28, https://doi.org/10.1016/0016-7037(58)90090-5.","productDescription":"29 p.","startPage":"1","endPage":"28","costCenters":[],"links":[{"id":219706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505aae4ae4b0c8380cd87075","contributors":{"authors":[{"text":"Carroll, D.","contributorId":84495,"corporation":false,"usgs":true,"family":"Carroll","given":"D.","email":"","affiliations":[],"preferred":false,"id":359575,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009835,"text":"70009835 - 1958 - The next decade in geochemistry","interactions":[],"lastModifiedDate":"2020-11-12T20:51:42.495629","indexId":"70009835","displayToPublicDate":"1958-01-01T00:00:00","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 next decade in geochemistry","docAbstract":"<p>The purpose, associations, functions; and activities of the Geochmical Society are reviewed briefly. Work on the Colorado Plateau uranium deposits is described as an example of what geochemical research, in conjunction with detailed field work, mineralogical studies, and related techniques can contribute to the understanding of a type of deposit. It is pointed out that not only have these studies given a great deal of information about the origin of the ores, but they have brought about directly a manifold increase in production and reserves of uranium in the United States. Indirectly, they aided the discovery of the tremendous deposits of the Blind River area in Ontario.</p><p>It is suggested that similar broad cooperative attacks could not only yield comparable results with other types of mineral deposits, such as laterites and Mississippi Valley type lead-zinc deposits, but could also advance our knowledge and understanding of such diverse problems of geology and cosmology as the origin of granites, origin and geologic implications of meteorites (including tektites), origin and search for petroleum, and geochemical relations and interpretations of natural waters. For each of these problems methods of approach are outlined and for some of them, specific projects and correlative problems are mentioned.</p><p>It is further suggested that the broad cooperative attack needed for most of these problems might be fostered most effectively by a programme comparable to that of the I.G.Y., even though for most types of geochemical research synoptic sampling and observations are not as important as they are for many projects in geophysics.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(58)90078-4","usgsCitation":"Ingerson, E., 1958, The next decade in geochemistry: Geochimica et Cosmochimica Acta, v. 14, no. 3, p. 185-203, https://doi.org/10.1016/0016-7037(58)90078-4.","productDescription":"19 p.","startPage":"185","endPage":"203","numberOfPages":"19","costCenters":[],"links":[{"id":218607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bae19e4b08c986b323f05","contributors":{"authors":[{"text":"Ingerson, E.","contributorId":48305,"corporation":false,"usgs":true,"family":"Ingerson","given":"E.","email":"","affiliations":[],"preferred":false,"id":357251,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2523,"text":"wsp1379 - 1958 - Ground-water resources of the San Luis Valley, Colorado, with a section on an inflow-outflow study of the area","interactions":[],"lastModifiedDate":"2023-04-11T21:42:35.558656","indexId":"wsp1379","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":"1379","title":"Ground-water resources of the San Luis Valley, Colorado, with a section on an inflow-outflow study of the area","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1379","usgsCitation":"Powell, W.J., and Mutz, P.B., 1958, Ground-water resources of the San Luis Valley, Colorado, with a section on an inflow-outflow study of the area: U.S. Geological Survey Water Supply Paper 1379, Report: vii, 284 p.; 12 Plates: 20.00 x 36.88 inches or smaller, https://doi.org/10.3133/wsp1379.","productDescription":"Report: vii, 284 p.; 12 Plates: 20.00 x 36.88 inches or smaller","costCenters":[],"links":[{"id":415607,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24361.htm","linkFileType":{"id":5,"text":"html"}},{"id":247220,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247219,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247218,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28728,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28727,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247221,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28732,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28731,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28730,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28733,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28734,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1379/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28729,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28726,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1379/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138827,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1379/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"San Luis Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -106.333,\n              38\n            ],\n            [\n              -106.333,\n              37.306\n            ],\n            [\n              -105.583,\n              37.306\n            ],\n            [\n              -105.583,\n              38\n            ],\n            [\n              -106.333,\n              38\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a6ce","contributors":{"authors":[{"text":"Powell, William J.","contributorId":62202,"corporation":false,"usgs":true,"family":"Powell","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mutz, Philip B.","contributorId":105285,"corporation":false,"usgs":true,"family":"Mutz","given":"Philip","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":145342,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010560,"text":"70010560 - 1958 - The deuterium content of water in some volcanic glasses","interactions":[],"lastModifiedDate":"2020-11-12T20:58:57.939243","indexId":"70010560","displayToPublicDate":"1958-01-01T00:00:00","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 deuterium content of water in some volcanic glasses","docAbstract":"<p><span>The deuterium-hydrogen composition (relative to Lake Michigan water = 0.0) of water extractsd from coexisting perlite and obsidian from eleven different localities was determined. The water content of the obsidians is generally from 0.09 to 0.29 per cent by weight, though two samples from near Olancha, California, contain about 0.92 per cent. The relative deuterium concentration is from −4.6 to −12.3 per cent. The coexisting perlite contains from 2.0 to 3.8 per cent of water with a relative deuterium concentration of −3.1 to −16.6 per cent. The deuterium concentration in the perlites is not related to that in the enclosed obsidian. The deuterium concentration in the perlite water is related to the deuterium concentration of the modern meteoric water and the perlite water contains approximately 4 per cent less deuterium than does the groundwater of the area in which the perlites occur. The above relations hold true for perlites from northern New Mexico, east slope of the Sierra Nevada. California Coast Range, Yellowstone Park, Wyoming, and New Zealand. As the water in the obsidian is unrelated to meteoric water, but the enclosing perlite water is related, we believe that this is evidence for the secondary hydration of obsidian to form high water content perlitic glass.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(58)90059-0","usgsCitation":"Friedman, I., and Smith, R.L., 1958, The deuterium content of water in some volcanic glasses: Geochimica et Cosmochimica Acta, v. 15, no. 3, p. 218-228, https://doi.org/10.1016/0016-7037(58)90059-0.","productDescription":"12 p.","startPage":"218","endPage":"228","costCenters":[],"links":[{"id":219080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baaa3e4b08c986b3228e7","contributors":{"authors":[{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":359172,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R. L.","contributorId":93904,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"L.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":359171,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":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":70175995,"text":"70175995 - 1957 - Ground-water levels in observation wells in Kansas, 1956","interactions":[],"lastModifiedDate":"2016-08-23T11:58:16","indexId":"70175995","displayToPublicDate":"2016-02-22T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water levels in observation wells in Kansas, 1956","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Fishel, V., and Mason, B., 1957, Ground-water levels in observation wells in Kansas, 1956: Kansas Geological Survey Bulletin, v. 125, 158 p.","productDescription":"158 p.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327650,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327649,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"125","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dde4b03fd6b7df2d09","contributors":{"authors":[{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":646767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mason, B.J.","contributorId":53029,"corporation":false,"usgs":true,"family":"Mason","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":646768,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175996,"text":"70175996 - 1957 - Ground-water resources of the Ladder Creek area in Kansas, with a section on The chemical quality of water, by R.A. Krieger","interactions":[],"lastModifiedDate":"2017-12-08T12:26:35","indexId":"70175996","displayToPublicDate":"2015-12-22T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water resources of the Ladder Creek area in Kansas, with a section on The chemical quality of water, by R.A. Krieger","language":"English","publisher":"University of Kansas","usgsCitation":"Bradley, E., Johnson, C.R., and Krieger, R.A., 1957, Ground-water resources of the Ladder Creek area in Kansas, with a section on The chemical quality of water, by R.A. Krieger: Kansas Geological Survey Bulletin, v. 126, 194 p. .","productDescription":"194 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327652,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327651,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"126","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dee4b03fd6b7df2d16","contributors":{"authors":[{"text":"Bradley, Edward","contributorId":67071,"corporation":false,"usgs":true,"family":"Bradley","given":"Edward","email":"","affiliations":[],"preferred":false,"id":646769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, C. R.","contributorId":14378,"corporation":false,"usgs":true,"family":"Johnson","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":646770,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Krieger, R. A.","contributorId":11202,"corporation":false,"usgs":true,"family":"Krieger","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":646771,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70160529,"text":"70160529 - 1957 - Some problems of private trout hatchery operators","interactions":[],"lastModifiedDate":"2021-03-23T15:54:05.685952","indexId":"70160529","displayToPublicDate":"2015-12-22T00:00:00","publicationYear":"1957","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":"Some problems of private trout hatchery operators","docAbstract":"<p>Disease, nutritional, and environmental problems in commercial production of trout are discussed, including mortality and age of spawners, copepod and gyrodactylid infections, suitable water temperatures, diseases (especially red mouth and back peel) and inspection of fish. It is concluded that experiences with hatchery procedures have varied greatly and often the commercial trout producer must adjust methods to fit his particular needs and conditions.</p>","language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","doi":"10.1577/1548-8659(1957)87[374:SPOPTH]2.0.CO;2","usgsCitation":"Rucker, R.R., 1957, Some problems of private trout hatchery operators: Transactions of the American Fisheries Society, v. 87, no. 1, p. 374-379, https://doi.org/10.1577/1548-8659(1957)87[374:SPOPTH]2.0.CO;2.","productDescription":"6 p.","startPage":"374","endPage":"379","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312714,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567a7432e4b0a04ef490fcc9","contributors":{"authors":[{"text":"Rucker, Robert R.","contributorId":69615,"corporation":false,"usgs":true,"family":"Rucker","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":583265,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175993,"text":"70175993 - 1957 - The hydraulic properties of the Ordovician rocks at Pittsburg, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T11:46:33","indexId":"70175993","displayToPublicDate":"2015-10-12T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"The hydraulic properties of the Ordovician rocks at Pittsburg, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Stramel, G., 1957, The hydraulic properties of the Ordovician rocks at Pittsburg, Kansas: Kansas Geological Survey Bulletin, v. 127, no. 5.","productDescription":"25 p. ","startPage":"178","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327647,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327646,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"127","issue":"5","edition":"153","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73f5e4b03fd6b7df2dbd","contributors":{"authors":[{"text":"Stramel, G.J.","contributorId":47768,"corporation":false,"usgs":true,"family":"Stramel","given":"G.J.","affiliations":[],"preferred":false,"id":646765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175994,"text":"70175994 - 1957 - Development of a balanced stream-gaging program for Kansas","interactions":[],"lastModifiedDate":"2016-08-23T11:53:52","indexId":"70175994","displayToPublicDate":"2015-10-12T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5189,"text":"Kansas Water Resources Board Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Development of a balanced stream-gaging program for Kansas","language":"English","publisher":"State of Kansas Water Resources Board","usgsCitation":"Furness, L., 1957, Development of a balanced stream-gaging program for Kansas: Kansas Water Resources Board Bulletin, v. 4, 50.","productDescription":"50","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327648,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73b9e4b03fd6b7df2c89","contributors":{"authors":[{"text":"Furness, L.W.","contributorId":16908,"corporation":false,"usgs":true,"family":"Furness","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":646766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70160589,"text":"70160589 - 1957 - Histopathology of fish. V. Gill disease","interactions":[],"lastModifiedDate":"2016-01-04T09:54:13","indexId":"70160589","displayToPublicDate":"2015-08-12T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Histopathology of fish. V. Gill disease","docAbstract":"<p>Possibly&nbsp;no&nbsp;single&nbsp;disease accounts for greater annual mortality than gill disease. Apparently endemic in many hatcheries, the disease is&nbsp;characterized by periodic sharp upsurges which are sometimes correlated with rising water temperatures, excessive foreign matter in the water (Wales and Evins 1937), or borderline nutritional conditions.</p>","language":"English","publisher":"Department of Commerce, Bureau of Fisheries","doi":"10.1577/1548-8659(1957)19[7:HOF]2.0.CO;2","usgsCitation":"Department of Commerce, Bureau of Fisheries, 1957, Histopathology of fish. V. Gill disease: Progressive Fish-Culturist, v. 19, no. 1, p. 7-13, https://doi.org/10.1577/1548-8659(1957)19[7:HOF]2.0.CO;2.","productDescription":"7 p.","startPage":"7","endPage":"13","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312805,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567bd3bce4b0a04ef491a200"}
,{"id":70047631,"text":"70047631 - 1957 - Ground-water reconnaissance of six Eskimo villages in the Kobuk-Noatak area, Alaska","interactions":[{"subject":{"id":56103,"text":"ofr57117 - 1957 - Ground-water reconnaissance of six Eskimo villages in the Kobuk-Noatak area, Alaska","indexId":"ofr57117","publicationYear":"1957","noYear":false,"title":"Ground-water reconnaissance of six Eskimo villages in the Kobuk-Noatak area, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70047631,"text":"70047631 - 1957 - Ground-water reconnaissance of six Eskimo villages in the Kobuk-Noatak area, Alaska","indexId":"70047631","publicationYear":"1957","noYear":false,"title":"Ground-water reconnaissance of six Eskimo villages in the Kobuk-Noatak area, Alaska"},"id":1}],"lastModifiedDate":"2013-08-15T13:28:02","indexId":"70047631","displayToPublicDate":"2013-01-01T13:24:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":140,"text":"Water Hydrological Data","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"4","title":"Ground-water reconnaissance of six Eskimo villages in the Kobuk-Noatak area, Alaska","language":"English","publisher":"Alaska Department of Health","publisherLocation":"Juneau, AK","usgsCitation":"Waller, R., 1957, Ground-water reconnaissance of six Eskimo villages in the Kobuk-Noatak area, Alaska: Water Hydrological Data 4.","costCenters":[],"links":[{"id":276645,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.45,51.21 ], [ 172.45,71.39 ], [ -129.99,71.39 ], [ -129.99,51.21 ], [ 172.45,51.21 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520df866e4b08494c3cb05e3","contributors":{"authors":[{"text":"Waller, Roger M.","contributorId":90353,"corporation":false,"usgs":true,"family":"Waller","given":"Roger M.","affiliations":[],"preferred":false,"id":482585,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040305,"text":"70040305 - 1957 - The ground water resources of Putnam County, New York","interactions":[],"lastModifiedDate":"2012-10-12T17:16:08","indexId":"70040305","displayToPublicDate":"2012-01-01T13:12:50","publicationYear":"1957","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":"GW-37","title":"The ground water resources of Putnam County, New York","language":"English","publisher":"New York State Water Power and Control Commission Bulletin","publisherLocation":"Albany, NY","usgsCitation":"Grossman, I., 1957, The ground water resources of Putnam County, New York: Bulletin GW-37, 78 p., 2 Plates.","productDescription":"78 p., 2 Plates","numberOfPages":"78","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262566,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e5071fe4b0e8fec6ce9ecf","contributors":{"authors":[{"text":"Grossman, I.G.","contributorId":52574,"corporation":false,"usgs":true,"family":"Grossman","given":"I.G.","email":"","affiliations":[],"preferred":false,"id":468027,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220727,"text":"5220727 - 1957 - Chemicals and wildlife","interactions":[],"lastModifiedDate":"2012-02-02T00:15:07","indexId":"5220727","displayToPublicDate":"2010-06-16T12:18:25","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2810,"text":"National Agricultural Chemicals Association News and Pesticide Review","active":true,"publicationSubtype":{"id":10}},"title":"Chemicals and wildlife","docAbstract":"Short paper that reviews some of the facts about effects of insecticides on wildlife and states principles that should be followed for maximum safety in treatment. These principles include minimal doses, good ground-to-plane control to avoid overdoses, and least possible pollution of water areas. ","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"National Agricultural Chemicals Association News and Pesticide Review","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"reprinted 1958 in Alabama Conservation 29(5):6-7.","usgsCitation":"DeWitt, J., and Springer, P.F., 1957, Chemicals and wildlife: National Agricultural Chemicals Association News and Pesticide Review, v. 16, no. 1, p. 13-14.","productDescription":"13-14","startPage":"13","endPage":"14","numberOfPages":"2","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198214,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e336b","contributors":{"authors":[{"text":"DeWitt, J.B.","contributorId":89080,"corporation":false,"usgs":true,"family":"DeWitt","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":332302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Springer, P. F.","contributorId":56590,"corporation":false,"usgs":false,"family":"Springer","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":332301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221066,"text":"5221066 - 1957 - An ecological study of waterfowl areas in central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:14:44","indexId":"5221066","displayToPublicDate":"2010-06-16T12:18:25","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3637,"text":"Transactions of the North American Wildlife Conference","active":true,"publicationSubtype":{"id":10}},"title":"An ecological study of waterfowl areas in central Florida","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the North American Wildlife Conference","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Sincock, J., and Powell, J.A., 1957, An ecological study of waterfowl areas in central Florida: Transactions of the North American Wildlife Conference, v. 52, p. 220-236.","productDescription":"220-236","startPage":"220","endPage":"236","numberOfPages":"17","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684b32","contributors":{"authors":[{"text":"Sincock, J.L.","contributorId":89994,"corporation":false,"usgs":true,"family":"Sincock","given":"J.L.","affiliations":[],"preferred":false,"id":332961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, J. A.","contributorId":69916,"corporation":false,"usgs":false,"family":"Powell","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":332960,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5230060,"text":"5230060 - 1957 - Waterfowl banding in the Canadian prairie provinces","interactions":[],"lastModifiedDate":"2012-02-02T00:15:26","indexId":"5230060","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"36","title":"Waterfowl banding in the Canadian prairie provinces","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Low, S., 1957, Waterfowl banding in the Canadian prairie provinces: Special Scientific Report  - Wildlife 36, 30.","productDescription":"30","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":92254,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486702?urlappend=%3Bseq=39"},{"id":202883,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c30e","contributors":{"authors":[{"text":"Low, S.H.","contributorId":105001,"corporation":false,"usgs":true,"family":"Low","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":343444,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56081,"text":"ofr5781 - 1957 - Ground water of the Columbia Basin","interactions":[],"lastModifiedDate":"2026-01-21T17:11:04.138834","indexId":"ofr5781","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1957","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":"57-81","title":"Ground water of the Columbia Basin","docAbstract":"Part of the water that infiltrates from the surface reaches a zone of saturation whence it percolates toward the outlet and thereby is delayed in its course to the sea. This ground water is one form of natural storage which has different degrees of effect on stream flow in different segments of the Columbia River basin. As a whole the Columbia River receives a substantial part of its base flow from the discharge of ground water. The inflow from ground water differs materially in each of the six general terrain areas, which are described briefly below.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5781","usgsCitation":"Newcomb, R.C., 1957, Ground water of the Columbia Basin: U.S. Geological Survey Open-File Report 57-81, 7 p., https://doi.org/10.3133/ofr5781.","productDescription":"7 p.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":287212,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0081/report.pdf"},{"id":287213,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1957/0081/report-thumb.jpg"}],"country":"Canada, United States","state":"Alberta, British Columbia, Idaho, Montana, Oregon, Washington","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.39,41.15 ], [ -123.39,52.45 ], [ -111.04,52.45 ], [ -111.04,41.15 ], [ -123.39,41.15 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d6e5","contributors":{"authors":[{"text":"Newcomb, R. C.","contributorId":77907,"corporation":false,"usgs":true,"family":"Newcomb","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":254741,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56080,"text":"ofr5780 - 1957 - An automatic suspended-sediment sampler","interactions":[],"lastModifiedDate":"2014-05-15T09:05:54","indexId":"ofr5780","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1957","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":"57-80","title":"An automatic suspended-sediment sampler","docAbstract":"The automatic suspended-sediment sampler was originally designed to obtain a suspended-sediment\nsample from a single point in a stream or reservoir during a rise in stage. The\nsampler was intended to be used during periods when manually-operated standard samplers\ncould not be used. If the sampling site is remote from the field office or is inaccessible during\nstorm periods or if no notification can be obtained concerning a stream rise, an adequate\nsampling program may be difficult to maintain. Having full knowledge of the many limitations\nand inadequacies of this automatic sampler, personnel of several of the Quality of Water\nBranch offices believe that, for many types of sediment transport and for specific sampling\nsites, samples obtained with the automatic sampler are preferable to a complete lack of\nsamples.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington D.C.","doi":"10.3133/ofr5780","usgsCitation":"Mundorff, J.C., 1957, An automatic suspended-sediment sampler: U.S. Geological Survey Open-File Report 57-80, 7 p., https://doi.org/10.3133/ofr5780.","productDescription":"7 p.","costCenters":[],"links":[{"id":287210,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0080/report.pdf"},{"id":287211,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1957/0080/report-thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.8,24.5 ], [ -124.8,49.383333 ], [ -66.95,49.383333 ], [ -66.95,24.5 ], [ -124.8,24.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684a94","contributors":{"authors":[{"text":"Mundorff, James C.","contributorId":23408,"corporation":false,"usgs":true,"family":"Mundorff","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":254740,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23995,"text":"ofr5778 - 1957 - Water levels in observation wells in Santa Barbara County, California, in 1956","interactions":[],"lastModifiedDate":"2014-05-15T07:36:06","indexId":"ofr5778","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1957","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":"57-78","title":"Water levels in observation wells in Santa Barbara County, California, in 1956","docAbstract":"Investigation of the ground-water resources of Santa Barbara County was continued during 1956 by the Geological Survey in cooperation with the Santa Barbara County Water Agency. Monthly water-level recorders were operated. Earlier measurements, covering the period 1941 through 1953, have been published in Geological Survey water-Supply Papers; those for 1954 and 1955 are in press and have been released locally in duplicated form. Water-Supply Paper 1068 contains tabulated descriptions of 2,246 wells in existence in 1942 in the various ground-water basins of the county. The same publication contains also many water-level measurements made prior to 1942 by the city of Santa Barbara, Santa Maria Valley Water Conservation District, San Joaquin Power Division of the Pacific Gas and Electric Co., Union Sugar Co., Union Oil Co., and other organizations and individuals. Comprehensive reports on the geology and ground-water resources of the Santa Ynez River basin (Upson and Thomasson, 1951), the south-coast basins (Upson, 1951), the Santa Maria Valley area (Worts, 1951), and the Cuyama Valley (Upson and Worts, 1951) have been published as Water-Supply Papers 1107, 1108, 1000, and 1110-B respectively. A report on stream runoff and ground-water storage capacity of the Santa Ynez River valley (Troxell and Wilson, 1952) was released to the open file in October 1952. A report appraising the ground-water resources of the Santa Ynez River valley (Wilson, 1957) was released to the open file in October 1956.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5778","issn":"0094-9140","usgsCitation":"Muir, K.S., and Merritt, P., 1957, Water levels in observation wells in Santa Barbara County, California, in 1956: U.S. Geological Survey Open-File Report 57-78, 77 p., https://doi.org/10.3133/ofr5778.","productDescription":"77 p.","costCenters":[],"links":[{"id":287195,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0078/report.pdf"},{"id":287196,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1957/0078/report-thumb.jpg"}],"country":"United States","state":"California","county":"Santa Barbara County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.6729,33.4625 ], [ -120.6729,35.1147 ], [ -119.0275,35.1147 ], [ -119.0275,33.4625 ], [ -120.6729,33.4625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9d70","contributors":{"authors":[{"text":"Muir, K. S.","contributorId":53764,"corporation":false,"usgs":true,"family":"Muir","given":"K.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":191115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Merritt, P.M.","contributorId":45344,"corporation":false,"usgs":true,"family":"Merritt","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":191114,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14401,"text":"ofr5760 - 1957 - Records available to September 30, 1956, on use of water in the Delaware Basin Project area","interactions":[],"lastModifiedDate":"2014-05-21T08:30:12","indexId":"ofr5760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-60","title":"Records available to September 30, 1956, on use of water in the Delaware Basin Project area","docAbstract":"<p>The purpose of this report is to summarize data on the use of water in the Delaware Basin Project area (fig. 2) and to list the principal data sources that are available in published form. The tables and bibliography will assist Geological Survey personnel  assigned to the Delaware Basin Project in evaluating the scope and deficiencies of previous studies of the basin. Information is also given on the use of water by public supplies in the New York-New Jersey region comprising the New York City Metropolitan Area and in the remaining north-central and south-eastern parts of New Jersey. These regions may depend increasingly on water from the Delaware River basin for part of their public supplies.</p>\n<br>\n<p>The Geological Survey has the responsibility for appraising and describing the water resources of the Nation as a guide to use, development, control, and conservation of these resources. Cooperative Federal-State water-resources investigations in the Delaware Basin States have been carried on the the Geological Survey for more than 50 years. In July 1956 the Survey began the \"Delaware Basin Project,\" a hydrologic study of the Delaware River basin in order to: 1) Determine present status and trends in water availability, quality, and use, 2) assess and improve the adequacy of the Survey's basic water data program in the basin, 3) interpret and evaluate the water-resources data in terms of past and possible future water-use and land-use practices, and 4) disseminate promptly the results of this investigation for the benefit of all interested agencies and the general public. The Geological Survey is working closely with the U.S. Corps of Engineers and other cooperating Federal and State agencies in providing water data which will contribute to the present coordinated investigation aimed at developing a plan for long-range water development in the Delaware River basin.</p>\n<br>\n<p>Estimates of quantities of water used are given for water withdrawn from streams and aquifers during calendar year 1955, as compiled or estimated from publications and manuscripts prepared between 1950 and 1956. All quantities are given in millions of gallons per day (mgd). The source of the water used, ground or surface, and the type of use to which is was put -- public supply, industrial supply, irrigation, or rural use -- is given. Use of water for hydroelectric power was not compiled for this report. Most tables in this report do not subdivide withdrawals into fresh and saline water; however, most supplies are fresh, except some of those withdrawn directly from the Delaware River downstream from Philadelphia, Pa. All quantities are expressed as an average rate for a full year and are lower, therefore, than rates resulting from the increased demand for water during the summer for air conditioning and supplemental irrigation.</p>\n<br>\n<p>The primary emphasis of this study was to get an over-all picture of water use throughout large parts of the basin. Therefore, publications relating to a dingle city or county, other than New York City, seldom were used; revisions and refinement based on such sources of information are best made by the field personnel most familiar with locally filed publications and published data. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington D.C.","doi":"10.3133/ofr5760","usgsCitation":"Kammerer, J., 1957, Records available to September 30, 1956, on use of water in the Delaware Basin Project area: U.S. Geological Survey Open-File Report 57-60, ii, 33 p., https://doi.org/10.3133/ofr5760.","productDescription":"ii, 33 p.","numberOfPages":"37","costCenters":[],"links":[{"id":287385,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287384,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0060/report.pdf"}],"country":"United States","state":"Delaware","otherGeospatial":"Delaware Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.0,39.0 ], [ -76.0,42.0 ], [ -75.0,42.0 ], [ -75.0,39.0 ], [ -76.0,39.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63579e","contributors":{"authors":[{"text":"Kammerer, John C.","contributorId":53815,"corporation":false,"usgs":true,"family":"Kammerer","given":"John C.","affiliations":[],"preferred":false,"id":169392,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4558,"text":"wsp1385 - 1957 - Surface water supply of the United States, 1955, Part III-A, Ohio River basin, Ohio River basin except Cumberland and Tennessee River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:51","indexId":"wsp1385","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"1385","title":"Surface water supply of the United States, 1955, Part III-A, Ohio River basin, Ohio River basin except Cumberland and Tennessee River basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1385","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1957, Surface water supply of the United States, 1955, Part III-A, Ohio River basin, Ohio River basin except Cumberland and Tennessee River basins: U.S. Geological Survey Water Supply Paper 1385, xii, 581 p. ;23 cm., https://doi.org/10.3133/wsp1385.","productDescription":"xii, 581 p. ;23 cm.","costCenters":[],"links":[{"id":139818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1385/report-thumb.jpg"},{"id":31615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1385/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696248","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528255,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}