{"pageNumber":"641","pageRowStart":"16000","pageSize":"25","recordCount":16440,"records":[{"id":32755,"text":"pp403F - 1963 - Mineralogy of selected soils from Guam, with a section on description of soil profiles","interactions":[],"lastModifiedDate":"2025-04-15T16:32:32.419787","indexId":"pp403F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"403","chapter":"F","title":"Mineralogy of selected soils from Guam, with a section on description of soil profiles","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology and hydrology of Guam, Mariana Islands (Professional Paper 403)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp403F","usgsCitation":"Carroll, D., Hathaway, J., and Stensland, C., 1963, Mineralogy of selected soils from Guam, with a section on description of soil profiles: U.S. Geological Survey Professional Paper 403, 53 p., https://doi.org/10.3133/pp403F.","productDescription":"53 p.","costCenters":[],"links":[{"id":60689,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0403f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121586,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0403f/report-thumb.jpg"},{"id":484598,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_44671.htm","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"Guam","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              144.6075439453125,\n              13.213208268446683\n            ],\n            [\n              145.0689697265625,\n              13.213208268446683\n            ],\n            [\n              145.0689697265625,\n              13.7153719325982\n            ],\n            [\n              144.6075439453125,\n              13.7153719325982\n            ],\n            [\n              144.6075439453125,\n              13.213208268446683\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ddb","contributors":{"authors":[{"text":"Carroll, Dorothy","contributorId":38534,"corporation":false,"usgs":true,"family":"Carroll","given":"Dorothy","email":"","affiliations":[],"preferred":false,"id":209103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hathaway, J.C.","contributorId":94280,"corporation":false,"usgs":true,"family":"Hathaway","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":209105,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stensland, C.H.","contributorId":53433,"corporation":false,"usgs":true,"family":"Stensland","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":209104,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32705,"text":"pp475C - 1963 - Short papers in geology and hydrology, Articles 60-121: Geological Survey research 1963","interactions":[],"lastModifiedDate":"2025-01-16T22:13:39.656936","indexId":"pp475C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"475","chapter":"C","title":"Short papers in geology and hydrology, Articles 60-121: Geological Survey research 1963","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1963 (Professional Paper 475)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp475C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Short papers in geology and hydrology, Articles 60-121: Geological Survey research 1963: U.S. Geological Survey Professional Paper 475, vi, 233 p., https://doi.org/10.3133/pp475C.","productDescription":"vi, 233 p.","costCenters":[],"links":[{"id":164177,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0475c/report-thumb.jpg"},{"id":113062,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0475c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":476666,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27962.htm","text":"The Canyon Mountain Complex, Oregon, and the alpine mafic magma stem","linkFileType":{"id":5,"text":"html"}},{"id":476667,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27963.htm","text":"Petrology of rhyolite and basalt, northwestern Yellowstone Plateau","linkFileType":{"id":5,"text":"html"}},{"id":476668,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27964.htm","text":"Modal composition of the Idaho batholith","linkFileType":{"id":5,"text":"html"}},{"id":477014,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28009.htm","text":"Gravity survey of the Island of Hawaii","linkFileType":{"id":5,"text":"html"}},{"id":402168,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27959.htm","text":"Structure of Precambrian crystalline rocks in the northern part of Grand Teton National Park, Wyoming"},{"id":476669,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27960.htm","text":"The Ordovician-Silurian contact in Dubuque County, Iowa","linkFileType":{"id":5,"text":"html"}},{"id":477255,"rank":17,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43318.htm","text":"Revised stratigraphic nomenclature and age of the Tuxedni Group in the Cook Inlet region, Alaska","linkFileType":{"id":5,"text":"html"}},{"id":477256,"rank":18,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43319.htm","text":"Redefinition and correlation of the Ohio Creek Formation (Paleocene) in west-central Colorado","linkFileType":{"id":5,"text":"html"}},{"id":477257,"rank":19,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43320.htm","text":"Fenton Pass Formation (Pleistocene?), Bighorn Basin, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":477258,"rank":20,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43321.htm","text":"Nussbaum alluvium of Pleistocene(?) age at Pueblo, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":477259,"rank":21,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43322.htm","text":"Age of the Murray Shale and Hess Quartzite on Chilhowee Mountain, Blount County, Tennessee","linkFileType":{"id":5,"text":"html"}},{"id":477260,"rank":22,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43323.htm","text":"Movement of waterborne cadmium and hexavalent chromium wastes in South Farmingdale, Nassau County, Long Island, New York","linkFileType":{"id":5,"text":"html"}},{"id":477381,"rank":23,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93409.htm","text":"Tertiary volcanic stratigraphy in the western San Juan Mountains, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":477382,"rank":24,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93410.htm","text":"Nomenclature for lithologic subdivisions of the Mississippian Redwall Limestone, Arizona","linkFileType":{"id":5,"text":"html"}},{"id":476665,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27961.htm","text":"Mississippian rocks in the Laramie Range, Wyoming, and adjacent areas","linkFileType":{"id":5,"text":"html"}},{"id":477012,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28007.htm","text":"Solution breccias of the Minnelusa Formation in the Black Hills, South Dakota and Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":477013,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28008.htm","text":"Gravity survey in the Rampart Range area, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":477015,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28010.htm","text":"Glacial lakes near Concord, Massachusetts","linkFileType":{"id":5,"text":"html"}},{"id":477016,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28011.htm","text":"Formation of ridges through differential subsidence of peatlands of the Sacramento - San Joaquin Delta, California","linkFileType":{"id":5,"text":"html"}},{"id":477017,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28012.htm","text":"Mapping transmissivity of alluvium in the lower Arkansas River valley, Arkansas","linkFileType":{"id":5,"text":"html"}},{"id":477253,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43316.htm","text":"Sediments on the continental margin off eastern United States","linkFileType":{"id":5,"text":"html"}},{"id":477254,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43317.htm","text":"Dark shale unit of Devonian and Mississippian age in northern Wyoming and southern Montana","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fb4","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":529435,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010836,"text":"70010836 - 1963 - Tritium distribution in ground water around large underground fusion explosions","interactions":[],"lastModifiedDate":"2026-02-13T16:54:23.910977","indexId":"70010836","displayToPublicDate":"1963-11-29T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tritium distribution in ground water around large underground fusion explosions","docAbstract":"Tritium will be released in significant amounts from large underground nuclear fusion explosions in the Plowshare Program. The tritium could become highly concentrated in nearby ground waters, and could be of equal or more importance as a possible contaminant than other long-lived fission-product and induced radionuclides. Behavior of tritiated water in particular hydrologic and geologic environments, as illustrated by hypothetical explosions in dolomite and tuff, must be carefully evaluated to predict under what conditions high groundwater concentrations of tritium might occur.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.142.3596.1163","issn":"00368075","usgsCitation":"Stead, F., 1963, Tritium distribution in ground water around large underground fusion explosions: Science, v. 142, no. 3596, p. 1163-1165, https://doi.org/10.1126/science.142.3596.1163.","productDescription":"3 p.","startPage":"1163","endPage":"1165","costCenters":[],"links":[{"id":218957,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"142","issue":"3596","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb86ce4b08c986b327852","contributors":{"authors":[{"text":"Stead, F.W.","contributorId":42653,"corporation":false,"usgs":true,"family":"Stead","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":359759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221113,"text":"70221113 - 1963 - Recharge rates of principal aquifers in Lake County, Indiana","interactions":[],"lastModifiedDate":"2021-06-02T13:56:06.824623","indexId":"70221113","displayToPublicDate":"1963-10-01T08:50:34","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Recharge rates of principal aquifers in Lake County, Indiana","docAbstract":"<p><span>The upper 350 to 400 feet of rocks underlying&nbsp;</span><span class=\"ScopusTermHighlight\">Lake</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">County</span><span>,&nbsp;</span><span class=\"ScopusTermHighlight\">Indiana</span><span>, form a single but complex hydrologic system. The rock units composing this system consist (</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;ascending order) of dolomite, clay till (unit 4), glaciofluvial sand (unit 3), clay till (unit 2), and lacustrine sand, silt, and clay (unit 1). The dolomite and unit 3 form the&nbsp;</span><span class=\"ScopusTermHighlight\">principal</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">aquifers</span><span>&nbsp;and the clay tills, units 4 and 2, the confining layers. The geohydrology of the confining layers controls to a large extent the&nbsp;</span><span class=\"ScopusTermHighlight\">rate</span><span>&nbsp;at which the&nbsp;</span><span class=\"ScopusTermHighlight\">aquifers</span><span>&nbsp;are recharged from local precipitation and, thereby, their potential yield. Unit 4, the dolomite's confining layer, has an estimated average vertical permeability of about 0.003 gpd (gallon per day) per square foot. Under present conditions of head difference, the&nbsp;</span><span class=\"ScopusTermHighlight\">rate</span><span>&nbsp;of&nbsp;</span><span class=\"ScopusTermHighlight\">recharge</span><span>&nbsp;to the dolomite through unit 4 is estimated to average 20,000 gpd per square mile. Unit 2, the confining layer for unit 3, has an average estimated vertical permeability of about 0.007 gpd per square foot. Under present conditions of head difference the&nbsp;</span><span class=\"ScopusTermHighlight\">recharge</span><span>&nbsp;through unit 3's confining layer is estimated to average about 100,000 gpd per square mile. However, these&nbsp;</span><span class=\"ScopusTermHighlight\">rates</span><span>&nbsp;of&nbsp;</span><span class=\"ScopusTermHighlight\">recharge</span><span>&nbsp;can be expected to increase as the head difference across each confining layer increases with extensive development of the&nbsp;</span><span class=\"ScopusTermHighlight\">aquifer</span><span>.</span></p>","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1963.tb01928.x","usgsCitation":"Rosenshein, J., 1963, Recharge rates of principal aquifers in Lake County, Indiana: Groundwater, v. 1, no. 4, p. 13-20, https://doi.org/10.1111/j.1745-6584.1963.tb01928.x.","productDescription":"8 p.","startPage":"13","endPage":"20","costCenters":[],"links":[{"id":386122,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Indiana","county":"Lake County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.528076171875,\n              41.017210578228436\n            ],\n            [\n              -86.9073486328125,\n              41.017210578228436\n            ],\n            [\n              -86.9073486328125,\n              41.701627343789205\n            ],\n            [\n              -87.528076171875,\n              41.701627343789205\n            ],\n            [\n              -87.528076171875,\n              41.017210578228436\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Rosenshein, J.S.","contributorId":95082,"corporation":false,"usgs":true,"family":"Rosenshein","given":"J.S.","affiliations":[],"preferred":false,"id":816791,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221114,"text":"70221114 - 1963 - The hydraulic geometry of a shallow estuary","interactions":[],"lastModifiedDate":"2021-06-02T14:02:29.569826","indexId":"70221114","displayToPublicDate":"1963-09-01T08:59:12","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"The hydraulic geometry of a shallow estuary","docAbstract":"<p><span>An analogy with entropy production in steady-state systems leads to&nbsp;</span><span class=\"ScopusTermHighlight\">a</span><span>&nbsp;statement that the&nbsp;</span><span class=\"ScopusTermHighlight\">geometry</span><span>&nbsp;of natural waterways is governed by two opposing influences:&nbsp;</span><span class=\"ScopusTermHighlight\">a</span><span>) equal work per unit of area of bed, and b) minimum work done in the system as&nbsp;</span><span class=\"ScopusTermHighlight\">a</span><span>&nbsp;whole. The resulting calculations applied to&nbsp;</span><span class=\"ScopusTermHighlight\">shallow</span><span>, estuaries are verified by field measurements.&nbsp;</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666309493340","usgsCitation":"Langbein, W.B., 1963, The hydraulic geometry of a shallow estuary: International Association of Scientific Hydrology - Bulletin , v. 8, no. 3, p. 84-94, https://doi.org/10.1080/02626666309493340.","productDescription":"11 p.","startPage":"84","endPage":"94","costCenters":[],"links":[{"id":386123,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":816792,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221111,"text":"70221111 - 1963 - Preliminary results of a study of calcium carbonate saturation of ground water in central Florida","interactions":[],"lastModifiedDate":"2021-06-02T12:59:17.848563","indexId":"70221111","displayToPublicDate":"1963-09-01T07:55:41","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Preliminary results of a study of calcium carbonate saturation of ground water in central Florida","docAbstract":"<p><span>The departure of&nbsp;</span><span class=\"ScopusTermHighlight\">ground</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;from equilibrium with calcite is being studied&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">central</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Florida</span><span>. Measurements of pH, temperature, and concentration of bicarbonate made&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the field are used with standard laboratory analyses of&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;samples to calculate an ion activity product (K) for&nbsp;</span><span class=\"ScopusTermHighlight\">calcium</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">carbonate</span><span>. The calculated Kiap is compared with the equilibrium constant (Keq) for calcite to determine the departure from equilibrium. The&nbsp;</span><span class=\"ScopusTermHighlight\">calcium</span><span>&nbsp;concentration is lowest&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the area of the highest piezometric surface. Some of the highest concentrations of bicarbonate are&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the area of low&nbsp;</span><span class=\"ScopusTermHighlight\">calcium</span><span>.&nbsp;</span><span class=\"ScopusTermHighlight\">In</span><span>&nbsp;about half of the area of&nbsp;</span><span class=\"ScopusTermHighlight\">study</span><span>, the&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;is undersaturated with respect to calcite. This indicates that solution of limestone can occur several hundred feet below the&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;table.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666309493336","usgsCitation":"Back, W., 1963, Preliminary results of a study of calcium carbonate saturation of ground water in central Florida: International Association of Scientific Hydrology - Bulletin , v. 8, no. 3, p. 43-51, https://doi.org/10.1080/02626666309493336.","productDescription":"9 p.","startPage":"43","endPage":"51","costCenters":[],"links":[{"id":480368,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666309493336","text":"Publisher Index Page"},{"id":386120,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Florida","otherGeospatial":"central Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.265380859375,\n              27.21555620902969\n            ],\n            [\n              -79.541015625,\n              27.21555620902969\n            ],\n            [\n              -79.541015625,\n              29.516110386062277\n            ],\n            [\n              -83.265380859375,\n              29.516110386062277\n            ],\n            [\n              -83.265380859375,\n              27.21555620902969\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Back, William","contributorId":59007,"corporation":false,"usgs":true,"family":"Back","given":"William","email":"","affiliations":[],"preferred":false,"id":816789,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221093,"text":"70221093 - 1963 - Hydrologic bench marks to distinguish the effects of climate vs. man","interactions":[],"lastModifiedDate":"2021-06-01T19:42:25.484388","indexId":"70221093","displayToPublicDate":"1963-07-01T14:39:43","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Hydrologic bench marks to distinguish the effects of climate vs. man","docAbstract":"<p><span>There is a vital need for&nbsp;</span><span class=\"ScopusTermHighlight\">hydrologic</span><span>&nbsp;data representing various environments that are free from the&nbsp;</span><span class=\"ScopusTermHighlight\">effects</span><span>&nbsp;of&nbsp;</span><span class=\"ScopusTermHighlight\">man</span><span>'s activities. Without such data hydrologists will be stymied in distinguishing&nbsp;</span><span class=\"ScopusTermHighlight\">hydrologic</span><span>&nbsp;changes caused by&nbsp;</span><span class=\"ScopusTermHighlight\">man</span><span>&nbsp;from those caused by&nbsp;</span><span class=\"ScopusTermHighlight\">climate</span><span>. To provide this background information, the U. S. Geological Survey is planning a nationwide&nbsp;</span><span class=\"ScopusTermHighlight\">hydrologic</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">bench</span><span>‐</span><span class=\"ScopusTermHighlight\">mark</span><span>&nbsp;program in which runoff, transport of sediment, precipitation, changes in vegetation, fluctuations in ground water, and other&nbsp;</span><span class=\"ScopusTermHighlight\">hydrologic</span><span>&nbsp;events will be studied in locales unaffected by the works of&nbsp;</span><span class=\"ScopusTermHighlight\">man</span><span>. The knowledge gained in operating these&nbsp;</span><span class=\"ScopusTermHighlight\">bench</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">marks</span><span>&nbsp;will be invaluable in statistical appraisals of&nbsp;</span><span class=\"ScopusTermHighlight\">hydrologic</span><span>&nbsp;data wherein a part of the record is affected by&nbsp;</span><span class=\"ScopusTermHighlight\">man</span><span>'s activities.</span></p>","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01918.x","usgsCitation":"Wilson, H., 1963, Hydrologic bench marks to distinguish the effects of climate vs. man: Groundwater, v. 1, no. 3, p. 13-14, https://doi.org/10.1111/j.1745-6584.1963.tb01918.x.","productDescription":"2 p.","startPage":"13","endPage":"14","costCenters":[],"links":[{"id":386073,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Wilson, H.D. Jr.","contributorId":51370,"corporation":false,"usgs":true,"family":"Wilson","given":"H.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":816734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221084,"text":"70221084 - 1963 - Some aspects of chemical equilibrium in ground water","interactions":[],"lastModifiedDate":"2021-06-01T18:51:47.135535","indexId":"70221084","displayToPublicDate":"1963-07-01T13:48:46","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Some aspects of chemical equilibrium in ground water","docAbstract":"<p><span>The influence of individual factors such as geologic and hydrologic characteristics of environment, biologic activity&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;soil, and pollutants on&nbsp;</span><span class=\"ScopusTermHighlight\">ground</span><span>‐</span><span class=\"ScopusTermHighlight\">water</span><span>&nbsp;composition is discussed.&nbsp;</span><span class=\"ScopusTermHighlight\">Aspects</span><span>&nbsp;of&nbsp;</span><span class=\"ScopusTermHighlight\">chemical</span><span>&nbsp;equilibria&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">ground</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">water</span><span>, sorption reactions, carbonate equilibria, chemistry of iron, and factors altering equilibria are presented.</span></p>","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01924.x","usgsCitation":"Hem, J., 1963, Some aspects of chemical equilibrium in ground water: Groundwater, v. 1, no. 3, p. 30-34, https://doi.org/10.1111/j.1745-6584.1963.tb01924.x.","productDescription":"5 p.","startPage":"30","endPage":"34","costCenters":[],"links":[{"id":386058,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":816713,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009998,"text":"70009998 - 1963 - Applications of geohydrologic concepts in geology","interactions":[],"lastModifiedDate":"2020-11-19T18:23:16.28895","indexId":"70009998","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Applications of geohydrologic concepts in geology","docAbstract":"<p>Subsurface water, an active agent in many geologic proceses, must be considered in interpreting geologic phenomena. Principles of the occurrence, distribution, and movement of subsurface waters are well established and readily applicable. In many interpretations in geologic literature, geohydrologic principles have been employed realistically, but in many others these principles have been either ignored or violated.</p><p>Explanations of genesis of underclays and associated deposits afford some examples wherein principles of movement and activity of vadose and ground water have been ignored and others in which they have been used advantageously. Postulates stating that waters percolate downward from swamp areas do not allow for the usual movement of subsurface water in such environments. The idea that sediments were leached by vadose water after uplift satisfies the geohydrologic requirements.</p><p>Weathering and solution form porous and permeable zones subjacent to unconformities in dense rocks such as carbonates and granites; this illustrates the geohydrologic and economic significance of unconformities. Examples are Mohawkian carbonate aquifers of northern Illinois and oil-bearing limestones of Mississippian age of eastern Montana.</p><p>The flushing effects of meteoric water and other hydrodynamic factors active during erosion periods are important elements in the genesis and concentration of brines. Explanation of the origin and occurrence of brines must include consideration of the geohydrologic environments throughout their geologic history.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(63)90031-3","usgsCitation":"Maxey, G.B., and Hackett, J.E., 1963, Applications of geohydrologic concepts in geology: Journal of Hydrology, v. 1, no. 1, p. 35-45, https://doi.org/10.1016/0022-1694(63)90031-3.","productDescription":"11 p.","startPage":"35","endPage":"45","numberOfPages":"11","costCenters":[],"links":[{"id":218768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ecc7e4b0c8380cd4949e","contributors":{"authors":[{"text":"Maxey, G. B.","contributorId":76458,"corporation":false,"usgs":true,"family":"Maxey","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":357622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hackett, J. E.","contributorId":72119,"corporation":false,"usgs":true,"family":"Hackett","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":357621,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010491,"text":"70010491 - 1963 - Implications of the minor element content of some major streams of the world","interactions":[],"lastModifiedDate":"2020-11-19T18:13:37.174725","indexId":"70010491","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"Implications of the minor element content of some major streams of the world","docAbstract":"<p>Of 15 or more minor elements in the world's principal river waters only aluminum, iron, manganese, barium and strontium range much over<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>100 &amp;#x3BC;g</mtext><mtext>l</mtext></math>\"><span class=\"MJX_Assistive_MathML\">100 μgl</span></span></span>. (parts per billion). Most minor elements range at or below<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>100 &amp;#x3BC;g</mtext><mtext>1</mtext></math>\"><span class=\"MJX_Assistive_MathML\">100 μg1</span></span></span>. and have median (or middle) values of 10 micrograms per liter or less. Significant areal differences in minor element content are found in the river waters. For example, Atlantic Coastal river waters in the aggregate are slightly more enriched in concentrations of silver, chromium, manganese, molybdenum, nickel, strontium and titanium, and slightly deficient in barium and lithium when compared with median values for North America. Median values of ratios<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Ba</mtext><mtext>Sr</mtext></math>\"><span class=\"MJX_Assistive_MathML\">BaSr</span></span></span>,<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Ni</mtext><mtext>Cr</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NiCr</span></span></span><span>&nbsp;</span>and<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-5-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Ni</mtext><mtext>Cu</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NiCu</span></span></span><span>&nbsp;</span>are reasonably consistent (within a factor of two) in principal drainage from North America. Noteworthy are consistent median ratios of<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-6-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Ni</mtext><mtext>Cu</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NiCu</span></span></span><span>&nbsp;</span>for large rivers of United States, but the ratio tends to be slightly greater in global northern latitudes than in southern latitudes. Median values for aluminum, barium, copper, lead, molybdenum and silver in North American runoff are of the same order as published world averages for ocean water.</p><p>Hydrologic and geochemical aspects of continental runoff are strongly implied in observations of minor element content of large rivers. Evidence to date is that median values of<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-7-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Ba</mtext><mtext>Sr ratios</mtext></math>\"><span class=\"MJX_Assistive_MathML\">BaSr ratios</span></span></span><span>&nbsp;</span>are relatively uniform in global river waters. There is real danger in oversimplifying chemical systems in broad assessments of lower reaches of large drainage basins because individual hydrologic and chemical events upstream are largely obscured.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(63)90069-3","usgsCitation":"Durum, W.H., and Haffty, J., 1963, Implications of the minor element content of some major streams of the world: Geochimica et Cosmochimica Acta, v. 27, no. 1, p. 1-11, https://doi.org/10.1016/0016-7037(63)90069-3.","productDescription":"11 p.","startPage":"1","endPage":"11","numberOfPages":"11","costCenters":[],"links":[{"id":219306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a392fe4b0c8380cd6182c","contributors":{"authors":[{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haffty, J.","contributorId":93187,"corporation":false,"usgs":true,"family":"Haffty","given":"J.","affiliations":[],"preferred":false,"id":359051,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70190792,"text":"70190792 - 1963 - Selected hydrologic data, Tooele Valley, Tooele County, Utah","interactions":[],"lastModifiedDate":"2017-09-14T11:09:23","indexId":"70190792","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"7","title":"Selected hydrologic data, Tooele Valley, Tooele County, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during the period 1958-63 by the U.S. Geological Survey in cooperation with the Utah State Engineer as part of the investigation of ground-water conditions in Tooele Valley, Tooele County, Utah. Additional data, collected prior to this study, can be found in the reports listed in the bibliography, and in the Water-Supply Papers of the Geological Survey listed at the beginning of table 2. The interpretive material will be published in a companion report by Joseph S. Gates.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells as shown in the tables and figures. From table I he can note such things as depth, diameter, water level, yield, drawdown, use of water, temperature of water, and depth of perforations. By comparing the depth of perforations with the drillers' logs in table 3 he can note the type of material that yields water to the wells. Table 2 and figures 2, 3, and 4 show the historic fluctuations and trends of water levels in the vicinity. From table 4 he can note the chemical quality of the water from wells in the vicinity. Table 5 shows the amount of water discharged during 1962 from the pumped wells. If the reader decides from his examination that conditions are favorable he can place an application to drill a well with the State Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Gates, J., 1963, Selected hydrologic data, Tooele Valley, Tooele County, Utah: Utah Basic-Data Report 7, 23 p.","productDescription":"23 p.","numberOfPages":"28","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345757,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-140&Title=Basic+Data+Report+7"}],"country":"United States","state":"Utah","county":"Tooele County","otherGeospatial":"Tooele Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953be4b091459a578236","contributors":{"authors":[{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":710417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190795,"text":"70190795 - 1963 - Selected hydrologic data, Jordan Valley, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2017-09-14T11:34:00","indexId":"70190795","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"4","title":"Selected hydrologic data, Jordan Valley, Salt Lake County, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during the period 1956-59 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation of Ground-water conditions in the Jordan Valley, Utah. The interpretive material Will be published in a companion report by T. lendell Marine and Don Price.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site in plate 1 and examine the records of nearby wells as shown in the tables. From table 2 he can note the type of material that yields water to wells in the vicinity; from table l he can note (1) the depth and diameter of wells in the vicinity and the yield of some of those wells, and (2) the depth to water or the feet of water pressure in the vicinity; from table 1 and plate 1 he can note the location of springs; from tables 3 and l, he can note the chemical quality of the water from wells and springs and from surface sources in the vicinity; and from table l he can find the use made of the well and spring water. If the reader decides from his examination that conditions are favorable, he can place an application to drill a well with the State Engineer. &nbsp;If the State Engineer believes that unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Marine, I.W., and Price, D., 1963, Selected hydrologic data, Jordan Valley, Salt Lake County, Utah: Utah Basic-Data Report 4, 30 p.","productDescription":"30 p.","numberOfPages":"33","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345764,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345763,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-080&Title=Basic+Data+Report+4"}],"country":"United States","state":"Utah","county":"Salt Lake Valley","otherGeospatial":"Jordan Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ae4b091459a57822d","contributors":{"authors":[{"text":"Marine, I. Wendell","contributorId":49339,"corporation":false,"usgs":true,"family":"Marine","given":"I.","email":"","middleInitial":"Wendell","affiliations":[],"preferred":false,"id":710421,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":710422,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70190787,"text":"70190787 - 1963 - Selected hydrologic data, Pavant Valley, Millard County, Utah","interactions":[],"lastModifiedDate":"2017-09-14T10:46:05","indexId":"70190787","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"5","title":"Selected hydrologic data, Pavant Valley, Millard County, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during the period 1959-62 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation of ground-water conditions in Pavant Valley in Millard County, Utah. The interpretive material will be published in a companion report by Reed W. Mower.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate l and examine the records of nearby wells as shown in the tables. From tables l and 3 he can note the type of material that yields water to wells in the vicinity; from table 1 he can note (1) the depth and diameter of wells in the vicinity and the yield of some of those wells, and (2) the depth to water or the feet of water pressure in the vicinity; from table 2 he can note the historic fluctuations and trends of water levels in the vicinity; from table 4 he can note the chemical quality of the water from wells in the vicinity; and from table l he can find the use made of the well water. If the reader decides from his examination that conditions are favorable, he can place an application to drill a well with the State Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, Utah","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Mower, R.W., 1963, Selected hydrologic data, Pavant Valley, Millard County, Utah: Utah Basic-Data Report 5, 20 p.","productDescription":"20 p.","numberOfPages":"25","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345748,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":345747,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-100&Title=Basic+Data+Report+5"}],"country":"United States","state":"Utah","county":"Millard County","otherGeospatial":"Pavant Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953be4b091459a57823a","contributors":{"authors":[{"text":"Mower, Reed W.","contributorId":32503,"corporation":false,"usgs":true,"family":"Mower","given":"Reed","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":710403,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32753,"text":"pp403C - 1963 - Petrology of the volcanic rocks of Guam, with a section on trace elements in the volcanic rocks of Guam","interactions":[],"lastModifiedDate":"2025-04-15T16:24:21.582891","indexId":"pp403C","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"403","chapter":"C","title":"Petrology of the volcanic rocks of Guam, with a section on trace elements in the volcanic rocks of Guam","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology and hydrology of Guam, Mariana Islands (Professional Paper 403)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp403C","usgsCitation":"Stark, J.T., and Tracey, J.I., 1963, Petrology of the volcanic rocks of Guam, with a section on trace elements in the volcanic rocks of Guam: U.S. Geological Survey Professional Paper 403, iv, 32 p., https://doi.org/10.3133/pp403C.","productDescription":"iv, 32 p.","costCenters":[],"links":[{"id":415898,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_44668.htm","linkFileType":{"id":5,"text":"html"}},{"id":119255,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0403c/report-thumb.jpg"},{"id":60687,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0403c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"otherGeospatial":"Guam","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              144.6075439453125,\n              13.213208268446683\n            ],\n            [\n              145.0689697265625,\n              13.213208268446683\n            ],\n            [\n              145.0689697265625,\n              13.7153719325982\n            ],\n            [\n              144.6075439453125,\n              13.7153719325982\n            ],\n            [\n              144.6075439453125,\n              13.213208268446683\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687c6d","contributors":{"authors":[{"text":"Stark, J. T.","contributorId":62650,"corporation":false,"usgs":true,"family":"Stark","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":209101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, J. I. Jr.","contributorId":17205,"corporation":false,"usgs":true,"family":"Tracey","given":"J.","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":209100,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1149,"text":"wsp1669C - 1963 - Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water","interactions":[{"subject":{"id":52076,"text":"ofr6029 - 1960 - A preliminary report of the geology and ground-water resources of Upper Black Earth Creek Basin, Wisconsin, with a section on surface water","indexId":"ofr6029","publicationYear":"1960","noYear":false,"title":"A preliminary report of the geology and ground-water resources of Upper Black Earth Creek Basin, Wisconsin, with a section on surface water"},"predicate":"SUPERSEDED_BY","object":{"id":1149,"text":"wsp1669C - 1963 - Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water","indexId":"wsp1669C","publicationYear":"1963","noYear":false,"chapter":"C","title":"Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water"},"id":1}],"lastModifiedDate":"2023-11-27T21:46:12.820397","indexId":"wsp1669C","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"C","title":"Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water","docAbstract":"<p>The upper Black Earth Creek drainage basin has an area of 46 square miles and is in Dane County in south-central Wisconsin. The oldest rock exposed in the valley walls is the sandstone of Late Cambrian age. Dolomite of the Prairie du Chien Group of Ordovician age overlies the sandstone and forms the. resistant cap on the hills. The St. Peter Sandstone, Platteville and Decorah Formations, and Galena Dolomite, all Ordovician in age, form a narrow belt along the southern boundary of the area. Outwash and alluvium of Pleistocene and Recent age fill the valleys. The eastern half of the area was glaciated and is covered with till. The sandstone of Late Cambrian age and the sand and gravel of the outwash deposits are hydraulically connected. Ground water occurs under unconfined (water-table) conditions in the western unglaciated part of the basin and under artesian conditions beneath the till locally in the eastern part. The source of most of the ground water is direct infiltration of precipitation; however, some ground water enters the area as underflow from the south. About 7 inches of the 30 inches of average annual precipitation recharges the ground-water reservoir. The ground water generally moves toward Black Earth Creek where it is discharged. Some ground water moves out of the basin as underflow beneath the valley of Black Earth Creek, and some is discharged by evapotranspiration or is withdrawn by pumping from wells. Water levels in shallow nonartesian wells respond rapidly to precipitation. The effect of precipitation on water levels in artesian wells is slower and more subdued. Water levels are generally highest in spring and lowest in fall and winter. The flow of upper Black Earth Creek is derived mostly from ground-water discharge, except during short periods of and immediately after precipitation when most of the flow is derived from surface runoff. The runoff from upper Black Earth Creek basin decreased from an average of 8.72 inches per square mile of drainage area in 1955 to 5.55 inches in 1958; the decrease reflects the generally decreasing precipitation and declining water levels in the basin during that period. On July 10, 1958, the discharge from the basin was 0.367 cubic feet per second per square mile, and the greatest discharge was 0.84 cubic feet per second per square mile from the southwest subbasin. The ground water has an average temperature of about 50°F. It is a calcium magnesium bicarbonate type water and is very hard.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States (Water-Supply Paper 1669)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1669C","collaboration":"Prepared in cooperation with the Wisconsin Geological and Natural History Survey","usgsCitation":"Cline, D.R., and Busby, M., 1963, Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water: U.S. Geological Survey Water Supply Paper 1669, Report: iv, 27 p.; 5 Plates:18.00 x 15.65 inches or smaller, https://doi.org/10.3133/wsp1669C.","productDescription":"Report: iv, 27 p.; 5 Plates:18.00 x 15.65 inches or smaller","numberOfPages":"32","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":25944,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137643,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669c/report-thumb.jpg"},{"id":25940,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25939,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":422984,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24862.htm","linkFileType":{"id":5,"text":"html"}},{"id":25941,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25943,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669c/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25942,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669c/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Dane County","otherGeospatial":"Black Earth Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.81494903564453,\n              43.04079076668198\n            ],\n            [\n              -89.81494903564453,\n              43.21193220073775\n            ],\n            [\n              -89.52999114990234,\n              43.21193220073775\n            ],\n            [\n              -89.52999114990234,\n              43.04079076668198\n            ],\n            [\n              -89.81494903564453,\n              43.04079076668198\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc7d5","contributors":{"authors":[{"text":"Cline, Denzel R.","contributorId":87910,"corporation":false,"usgs":true,"family":"Cline","given":"Denzel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Busby, Mark W.","contributorId":83099,"corporation":false,"usgs":true,"family":"Busby","given":"Mark W.","affiliations":[],"preferred":false,"id":143259,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047838,"text":"70047838 - 1962 - Data on wells in the Edwards Air Force Base area, California","interactions":[{"subject":{"id":52083,"text":"ofr6041 - 1960 - Appendix A \"Tables of basic data for wells on Edwards Air Force Base,\"; Appendix B \"Tables of basic data for areas outside Edwards Air Force Base\"","indexId":"ofr6041","publicationYear":"1960","noYear":false,"title":"Appendix A \"Tables of basic data for wells on Edwards Air Force Base,\"; Appendix B \"Tables of basic data for areas outside Edwards Air Force Base\""},"predicate":"SUPERSEDED_BY","object":{"id":70047838,"text":"70047838 - 1962 - Data on wells in the Edwards Air Force Base area, California","indexId":"70047838","publicationYear":"1962","noYear":false,"title":"Data on wells in the Edwards Air Force Base area, California"},"id":1}],"lastModifiedDate":"2013-08-26T17:09:35","indexId":"70047838","displayToPublicDate":"2013-01-01T16:17:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"91-6","title":"Data on wells in the Edwards Air Force Base area, California","docAbstract":"The data presented In this report were collected by the U.S. Geological Survey as a phase of the investigation of ground-water geology and hydrology of the Edwards Air Force Base area. The study was made in cooperation with the Department of the Air Force but also was coincident with the U.S. Geological Survey investigation of water wells and general hydrologic conditions throughout much of the desert region of southern California. The overall study of general hydrologic conditions in the desert is part of a cooperative program with the California Department of Water Resources.","language":"English","publisher":"California Department of Water Resources","publisherLocation":"Sacramento, CA","collaboration":"Prepared by United States Department of Interior Geological Survey","usgsCitation":"Dutcher, L., Bader, J., and Hiltgen, W., 1962, Data on wells in the Edwards Air Force Base area, California: Bulletin 91-6, 209 p.; Maps: 2 Sheets.","productDescription":"209 p.; Maps: 2 Sheets","numberOfPages":"236","costCenters":[],"links":[{"id":277019,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047838.png"},{"id":277018,"type":{"id":11,"text":"Document"},"url":"https://www.water.ca.gov/waterdatalibrary/docs/historic/Bulletins/Bulletin_91/Bulletin_91-6__1962.pdf"}],"country":"United States","state":"California","otherGeospatial":"Edwards Air Force Base","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.058539,34.776789 ], [ -118.058539,35.014831 ], [ -117.753877,35.014831 ], [ -117.753877,34.776789 ], [ -118.058539,34.776789 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521c78e4e4b01458f7842924","contributors":{"authors":[{"text":"Dutcher, L.C.","contributorId":42191,"corporation":false,"usgs":true,"family":"Dutcher","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":483109,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bader, J. S.","contributorId":65830,"corporation":false,"usgs":true,"family":"Bader","given":"J. S.","affiliations":[],"preferred":false,"id":483110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hiltgen, W.J.","contributorId":8929,"corporation":false,"usgs":true,"family":"Hiltgen","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":483108,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68696,"text":"ha47 - 1962 - Floods at Fremont, Ohio","interactions":[],"lastModifiedDate":"2012-02-10T00:11:25","indexId":"ha47","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"47","title":"Floods at Fremont, Ohio","language":"ENGLISH","doi":"10.3133/ha47","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1962, Floods at Fremont, Ohio: U.S. Geological Survey Hydrologic Atlas 47, 1 map :col. ;on sheet 72 x 84 in folder 30 x 24.  (Contour interval 5 feet.  30 by 31 inches)), https://doi.org/10.3133/ha47.","productDescription":"1 map :col. ;on sheet 72 x 84 in folder 30 x 24.  (Contour interval 5 feet.  30 by 31 inches))","costCenters":[],"links":[{"id":188097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90418,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.18333333333334,41.25 ], [ -83.18333333333334,41.3675 ], [ -83.05,41.3675 ], [ -83.05,41.25 ], [ -83.18333333333334,41.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7280","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":534516,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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