{"pageNumber":"6672","pageRowStart":"166775","pageSize":"25","recordCount":184900,"records":[{"id":1278,"text":"wsp1576E - 1964 - Availability of ground water in parts of the Acoma and Laguna Indian Reservations, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1576E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1576","chapter":"E","title":"Availability of ground water in parts of the Acoma and Laguna Indian Reservations, New Mexico","docAbstract":"The need for additional water has increased in recent years on the Acoma and Laguna Indian Reservations in west-central New Mexico because the population and per capita use of water have increased; the tribes also desire water for light industry, for more modern schools, and to increase their irrigation program. Many wells have been drilled in the area, but most have been disappointing because of small yields and poor chemical quality of the water. \r\n\r\nThe topography in the Acoma and Laguna Indian Reservations is controlled primarily by the regional and local dip of alternating beds of sandstone and shale and by the igneous complex of Mount Taylor. The entrenched alluvial valley along the Rio San Jose, which traverses the area, ranges in width from about 0.4 mile to about 2 miles. \r\n\r\nThe climate is characterized by scant rainfall, which occurs mainly in summer, low relative humidity, and large daily fluctuations of temperature. Most of the surface water enters the area through the Rio San Jose. The average annual streamflow past the gaging station Rio San Jose near Grants, N. Mex. is about 4,000 acre-feet. Tributaries to the Rio San Jose within the area probably contribute about 1,000 acre-feet per year. At the present time, most of the surface water is used for irrigation. \r\n\r\nGround water is obtained from consolidated sedimentary rocks that range in age from Triassic to Cretaceous, and from unconsolidated alluvium of Quaternary age. The principal aquifers are the Dakota Sandstone, the Tres Hermanos Sandstone Member of the Mancos Shale, and the alluvium. The Dakota Sandstone yields 5 to 50 gpm (gallons per minute) of water to domestic and stock wells. The Tres Hermanos sandstone Member generally yields 5 to 20 gpm of water to domestic and stock wells. Locally, beds of sandstone in the Chinle and Morrison Formations, the Entrada Sandstone, and the Bluff Sandstone also yield small supplies of water to domestic and stock wells. The alluvium yields from 2 gpm to as much as 150 gpm of water to domestic and stock wells. Thirteen test wells were drilled in a search for usable supplies of ground water for pueblo and irrigation supply and to determine the geologic and hydrologic characteristics of the water-bearing material. The performance of six of the test wells suggests that the sites are favorable for pueblo or irrigation supply wells. The yield of the other seven wells was too small or the quality of the water was too poor for development of pueblo or irrigation supply to be feasible. However, the water from one of the seven wells was good in chemical quality, and the yield was large enough to supply a few homes with water. \r\n\r\nThe tests suggest that the water in the alluvium of the Rio San Jose valley is closely related to the streamflow and that it might be possible to withdraw from the alluvium in summer and replenish it in winter. The surface flow in summer might be decreased by extensive pumpage of ground water, but on the other hand, more of the winter flow could be retained in the area by storage in the ground-water reservoir. Wells could be drilled along the axis of the valley, and the water could be pumped into systems for distribution to irrigated farms. The chemical quality of ground water in the area varies widely from one stratigraphic unit to another and laterally within each unit and commonly the water contains undesirably large amounts of sulfate. However, potable water has been obtained locally from all the aquifers. The water of best quality seemingly is in the Tres Hermanos Sandstone Member of the Mancos Shale and in the alluvium north of the Rio San Jose. The largest quantity of water that is suitable for irrigation is in the valley fill along the Rio San Jose. \r\n\r\nIntensive pumping of ground water from aquifers containing water of good quality may draw water of inferior chemical quality into the wells.","language":"ENGLISH","publisher":"United States Government Printing Office,","doi":"10.3133/wsp1576E","usgsCitation":"Dinwiddie, G.A., and Motts, W.S., 1964, Availability of ground water in parts of the Acoma and Laguna Indian Reservations, New Mexico: U.S. Geological Survey Water Supply Paper 1576, iv, 65 p. :ill., map ;24 cm. & 3 maps in pocket., https://doi.org/10.3133/wsp1576E.","productDescription":"iv, 65 p. :ill., map ;24 cm. & 3 maps in pocket.","costCenters":[],"links":[{"id":137528,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1576e/report-thumb.jpg"},{"id":26238,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26239,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26240,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26241,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1576e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65db99","contributors":{"authors":[{"text":"Dinwiddie, George A.","contributorId":21135,"corporation":false,"usgs":true,"family":"Dinwiddie","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":143488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motts, Ward Sundt","contributorId":68708,"corporation":false,"usgs":true,"family":"Motts","given":"Ward","email":"","middleInitial":"Sundt","affiliations":[],"preferred":false,"id":143489,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1320,"text":"wsp1779W - 1964 - Geology and ground-water resources of Richardson County, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1779W","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"W","title":"Geology and ground-water resources of Richardson County, Nebraska","docAbstract":"Richardson County is in the extreme southeast corner of Nebraska. It has an area of 545 square miles, and in 1960 it had a population of 13,903. The county is in the physiographic region referred to as the Dissected Loess-covered Till Prairies. Major drainage consists of the Big Nemaha River, including its North and South Forks, and Muddy Creek. These streams flow southeastward and empty into the Missouri River, which forms the eastern boundary of the county. The climate of Richardson County is subhumid; the normal annual precipitation is about 35 inches. Agriculture is the chief industry, and corn is the principal crop. \r\n\r\nPleistocene glacial drift, loess, and alluvial deposits mantle the bedrock except in the southern and southwestern parts of the county where the bedrock is at the surface. Ground water is obtained from glacial till, fluvioglacial material, terrace deposits, and coarse alluvial deposits, all of Pleistocene age--and some is obtained from bedrock aquifers of Pennsylvanian and Permian age. \r\n\r\nAdequate supplies of ground water are in many places difficult to locate because the water-bearing sands and gravels of Pleistocene age vary in composition and lack lateral persistence. Perched water tables are common in the upland areas and provide limited amounts of water to many of the shallow wells, Very few wells in bedrock yield adequate supplies, as the permeability of the rock is low and water that is more than a few tens of feet below the bedrock surface is highly mineralized. \r\n\r\nRecharge is primarily from local precipitation, and water levels in many wells respond rapidly to increased or decreased precipitation. The quality of the ground water is generally satisfactory for most uses, although all the water is hard, and iron and manganese concentrations, in some areas, are relatively high. Ground water is used mainly for domestic and stock purposes.","language":"ENGLISH","publisher":"U.S. G.P.O,","doi":"10.3133/wsp1779W","usgsCitation":"Emery, P.A., 1964, Geology and ground-water resources of Richardson County, Nebraska: U.S. Geological Survey Water Supply Paper 1779, iv, 29 p. :ill., maps (1 col.) ;24 cm., https://doi.org/10.3133/wsp1779W.","productDescription":"iv, 29 p. :ill., maps (1 col.) ;24 cm.","costCenters":[],"links":[{"id":110017,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24970.htm","linkFileType":{"id":5,"text":"html"},"description":"24970"},{"id":138067,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779w/report-thumb.jpg"},{"id":26359,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779w/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26360,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779w/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26361,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779w/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859b9","contributors":{"authors":[{"text":"Emery, Philip A.","contributorId":43733,"corporation":false,"usgs":true,"family":"Emery","given":"Philip","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":143559,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63371,"text":"gq239 - 1964 - Geology of the Aspen Grove quadrangle, Utah","interactions":[{"subject":{"id":46873,"text":"ofr615 - 1961 - Geologic map of the Aspen Grove quadrangle, Utah","indexId":"ofr615","publicationYear":"1961","noYear":false,"title":"Geologic map of the Aspen Grove quadrangle, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":63371,"text":"gq239 - 1964 - Geology of the Aspen Grove quadrangle, Utah","indexId":"gq239","publicationYear":"1964","noYear":false,"title":"Geology of the Aspen Grove quadrangle, Utah"},"id":1}],"lastModifiedDate":"2021-11-10T19:38:32.770049","indexId":"gq239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"239","title":"Geology of the Aspen Grove quadrangle, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq239","usgsCitation":"Baker, A.A., 1964, Geology of the Aspen Grove quadrangle, Utah: U.S. Geological Survey Geologic Quadrangle 239, Report: 9 p.; Plate, https://doi.org/10.3133/gq239.","productDescription":"Report: 9 p.; Plate","costCenters":[],"links":[{"id":249471,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0239/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":252953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0239/report-thumb.jpg"},{"id":102244,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_693.htm","linkFileType":{"id":5,"text":"html"},"description":"693"}],"scale":"24000","country":"United States","state":"Utah","otherGeospatial":"Aspen Grove quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.625,\n              40.3750\n            ],\n            [\n              -111.5,\n              40.3750\n            ],\n            [\n              -111.5,\n              40.5000\n            ],\n            [\n              -111.625,\n              40.5000\n            ],\n            [\n              -111.625,\n              40.3750\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b14e4b07f02db6a47db","contributors":{"authors":[{"text":"Baker, Arthur A.","contributorId":65446,"corporation":false,"usgs":true,"family":"Baker","given":"Arthur","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":268743,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32762,"text":"pp417C - 1964 - Hydrology and hydrogeology of Navajo Lake, Kane County, Utah","interactions":[],"lastModifiedDate":"2025-09-22T18:22:47.332703","indexId":"pp417C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"417","chapter":"C","title":"Hydrology and hydrogeology of Navajo Lake, Kane County, Utah","docAbstract":"<p><span>Navajo Lake, whose entire outflow disappears underground, is on the high Markagurit Plateau where the average annual precipitation is more than 30 inches. It nestles among the headwaters of several streams that flow into arid regions where competition for municipal, industrial, and irrigation water sup- plies is very keen. Several proposals for additional development and use of the water of Navajo Lake have led to controversies and raised questions in regard to the total water supply and its disposition, and to the effect of the proposed projects on existing water rights. This report summarizes the results of an investigation of the water supply of Navajo Lake and the present disposition of that supply.</span></p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp417C","collaboration":"Prepared in cooperation with the Utah Water and Power Board and with the Cedar City Corporation","usgsCitation":"Wilson, M.T., and Thomas, H.E., 1964, Hydrology and hydrogeology of Navajo Lake, Kane County, Utah: U.S. Geological Survey Professional Paper 417, Report: iii, 26 p.; 3 Plates: 25.00 x 30.00 inches or smaller, https://doi.org/10.3133/pp417C.","productDescription":"Report: iii, 26 p.; 3 Plates: 25.00 x 30.00 inches or smaller","numberOfPages":"33","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":495857,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4410.htm","linkFileType":{"id":5,"text":"html"}},{"id":60697,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0417c/plate-3.pdf","text":"Plate 3","size":"2.98 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Sinks and closed depressions in the Navajo Lake region, Garfield, Iron, and Kane Counties, Utah"},{"id":60696,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0417c/plate-2.pdf","text":"Plate 2","size":"2.03 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Effect of basalt eruptions on drainage, Navajo Lake region, Garfield, Iron, and Kane Counties, Utah"},{"id":60695,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0417c/plate-1.pdf","text":"Plate 1","size":"2.81 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geologic map of the Navajo Lake region, Garfield, Iron, and Kane Counties, Utah"},{"id":60698,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0417c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126455,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0417c/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Kane County","otherGeospatial":"Navajo Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.83920288085938,\n              37.49746950215633\n            ],\n            [\n              -112.69569396972656,\n              37.49746950215633\n            ],\n            [\n              -112.69569396972656,\n              37.57669160058646\n            ],\n            [\n              -112.83920288085938,\n              37.57669160058646\n            ],\n            [\n              -112.83920288085938,\n              37.49746950215633\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e88a","contributors":{"authors":[{"text":"Wilson, Milton Theurer","contributorId":182373,"corporation":false,"usgs":false,"family":"Wilson","given":"Milton","email":"","middleInitial":"Theurer","affiliations":[],"preferred":false,"id":209116,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Harold E.","contributorId":36116,"corporation":false,"usgs":true,"family":"Thomas","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":209115,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32758,"text":"pp411F - 1964 - Extending Darcy's concept of ground-water motion","interactions":[],"lastModifiedDate":"2013-06-12T09:53:19","indexId":"pp411F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"411","chapter":"F","title":"Extending Darcy's concept of ground-water motion","docAbstract":"The tensor nature of permeability and its effect in a given ground-water flow regime have been acknowledged by various investigators. The effect on the spread of a given dissolved substance can be qualitatively discussed on the basis of the tensor characteristic of the permeability coefficient. The correlation between the dispersion coefficient and the tensor characteristic is one possible means of defining the flow regime within a given aquifer. Because of the large-scale changes in magnitude and direction of the tensor components of permeability, the concept of a mean line of dispersion may produce a more significant statement on the characteristics of flow than does the present concept of hydraulic potential and the streamline.","language":"ENGLISH","publisher":"United States Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp411F","usgsCitation":"Skibitzke, H., 1964, Extending Darcy's concept of ground-water motion: U.S. Geological Survey Professional Paper 411, v, F6, https://doi.org/10.3133/pp411F.","productDescription":"v, F6","numberOfPages":"12","costCenters":[],"links":[{"id":161217,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0411f/report-thumb.jpg"},{"id":268923,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0411f/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8b0f","contributors":{"authors":[{"text":"Skibitzke, H.E.","contributorId":44528,"corporation":false,"usgs":true,"family":"Skibitzke","given":"H.E.","affiliations":[],"preferred":false,"id":209109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18393,"text":"ofr6430 - 1964 - Determination of ammonium citrate-soluble cobalt in soils and sediments","interactions":[],"lastModifiedDate":"2025-06-10T21:28:55.293236","indexId":"ofr6430","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-30","title":"Determination of ammonium citrate-soluble cobalt in soils and sediments","docAbstract":"<p>A rapid field method for the determination of cold-extractable cobalt in soils and sediments has been developed for use in geochemical prospecting. Readily available cobalt is dissolved by treating the sample with an aqueous ammonium citrate-hydroxylamine hydrochloride solution; the filtered citrate extract is then treated with 2-nitroso1-naphthol to form a pink-colored cobalt complex which is concentrated in a floating organic layer by a 1 to 3 mixture of carbon tetrachloride and cyclohexane. After the organic extract is shaken with potassium cyanide solution to eliminate interference by copper and nickel, the intensity of the pink to red color is estimated by comparison with a standard series.</p><p>A concentration range of 1 to 60 ppm is obtained when a 0.2-g sample is used but this range is varied easily by adjustment of sample size and volume of organic solvent. A minimum of 100 determinations per 8-hour day can be made, and because only simple, readily portable items of equipment are required, the method is adapted to use under rough field conditions, at the sample site if desired.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6430","usgsCitation":"Canney, F.C., and Nowlan, G., 1964, Determination of ammonium citrate-soluble cobalt in soils and sediments: U.S. Geological Survey Open-File Report 64-30, 15 p., https://doi.org/10.3133/ofr6430.","productDescription":"15 p.","costCenters":[],"links":[{"id":490351,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0030/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150944,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0030/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667994","contributors":{"authors":[{"text":"Canney, Frank Cogswell","contributorId":70776,"corporation":false,"usgs":true,"family":"Canney","given":"Frank","email":"","middleInitial":"Cogswell","affiliations":[],"preferred":false,"id":179040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":179041,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61784,"text":"gq356 - 1964 - Geology of the Tell City quadrangle, Kentucky-Indiana","interactions":[],"lastModifiedDate":"2012-02-10T00:10:29","indexId":"gq356","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"356","title":"Geology of the Tell City quadrangle, Kentucky-Indiana","language":"ENGLISH","doi":"10.3133/gq356","usgsCitation":"Spencer, F.D., 1964, Geology of the Tell City quadrangle, Kentucky-Indiana: U.S. Geological Survey Geologic Quadrangle 356, 1 map :col. ;76 x 87 cm., https://doi.org/10.3133/gq356.","productDescription":"1 map :col. ;76 x 87 cm.","costCenters":[],"links":[{"id":102368,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_817.htm","linkFileType":{"id":5,"text":"html"},"description":"817"},{"id":248076,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0356/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252736,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0356/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.86749999999999,37.8675 ], [ -86.86749999999999,38 ], [ -86.75,38 ], [ -86.75,37.8675 ], [ -86.86749999999999,37.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e480","contributors":{"authors":[{"text":"Spencer, Frank Darwyn","contributorId":22330,"corporation":false,"usgs":true,"family":"Spencer","given":"Frank","email":"","middleInitial":"Darwyn","affiliations":[],"preferred":false,"id":266361,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62151,"text":"gq347 - 1964 - Geology of the Lancer quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:28","indexId":"gq347","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"347","title":"Geology of the Lancer quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq347","usgsCitation":"Rice, C., 1964, Geology of the Lancer quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 347, 1 map :col. ;58 x 46 cm., on sheet 80 x 84 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq347.","productDescription":"1 map :col. ;58 x 46 cm., on sheet 80 x 84 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102360,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_809.htm","linkFileType":{"id":5,"text":"html"},"description":"809"},{"id":248342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0347/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":253237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0347/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.75,37.6175 ], [ -82.75,37.75 ], [ -82.61749999999999,37.75 ], [ -82.61749999999999,37.6175 ], [ -82.75,37.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f607","contributors":{"authors":[{"text":"Rice, Charles L.","contributorId":61801,"corporation":false,"usgs":true,"family":"Rice","given":"Charles L.","affiliations":[],"preferred":false,"id":266993,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61575,"text":"gq259 - 1964 - Geology of the Livingston quadrangle, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:10:28","indexId":"gq259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"259","title":"Geology of the Livingston quadrangle, Montana","language":"ENGLISH","doi":"10.3133/gq259","usgsCitation":"Roberts, A.E., 1964, Geology of the Livingston quadrangle, Montana: U.S. Geological Survey Geologic Quadrangle 259, 1 map :col. ;58 x 40 cm., on sheet 74 x 69 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq259.","productDescription":"1 map :col. ;58 x 40 cm., on sheet 74 x 69 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102264,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_713.htm","linkFileType":{"id":5,"text":"html"},"description":"713"},{"id":247885,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0259/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":252310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0259/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.61749999999999,45.6175 ], [ -110.61749999999999,45.75 ], [ -110.5,45.75 ], [ -110.5,45.6175 ], [ -110.61749999999999,45.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67eafd","contributors":{"authors":[{"text":"Roberts, Albert Eugene","contributorId":77126,"corporation":false,"usgs":true,"family":"Roberts","given":"Albert","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":266086,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61781,"text":"gq315 - 1964 - Geology of parts of the Rockport and Lewisport quadrangles, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:29","indexId":"gq315","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"315","title":"Geology of parts of the Rockport and Lewisport quadrangles, Kentucky","language":"ENGLISH","doi":"10.3133/gq315","usgsCitation":"Spencer, F.D., 1964, Geology of parts of the Rockport and Lewisport quadrangles, Kentucky: U.S. Geological Survey Geologic Quadrangle 315, 1 map :col. ;66 x 89 cm., https://doi.org/10.3133/gq315.","productDescription":"1 map :col. ;66 x 89 cm.","costCenters":[],"links":[{"id":102327,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_776.htm","linkFileType":{"id":5,"text":"html"},"description":"776"},{"id":248073,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0315/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0315/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.03416666666666,37.8675 ], [ -87.03416666666666,37.9675 ], [ -86.86749999999999,37.9675 ], [ -86.86749999999999,37.8675 ], [ -87.03416666666666,37.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6836bc","contributors":{"authors":[{"text":"Spencer, Frank Darwyn","contributorId":22330,"corporation":false,"usgs":true,"family":"Spencer","given":"Frank","email":"","middleInitial":"Darwyn","affiliations":[],"preferred":false,"id":266358,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17931,"text":"ofr642 - 1964 - Synopsis of ground-water conditions on the San Francisco Plateau near Flagstaff, Coconino County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:07:20","indexId":"ofr642","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-2","title":"Synopsis of ground-water conditions on the San Francisco Plateau near Flagstaff, Coconino County, Arizona","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr642","usgsCitation":"Akers, J.P., Cooley, M.E., and Dennis, P., 1964, Synopsis of ground-water conditions on the San Francisco Plateau near Flagstaff, Coconino County, Arizona: U.S. Geological Survey Open-File Report 64-2, iii, 27 p. :maps., https://doi.org/10.3133/ofr642.","productDescription":"iii, 27 p. :maps.","costCenters":[],"links":[{"id":150084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687d64","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":178224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooley, M. E.","contributorId":89868,"corporation":false,"usgs":true,"family":"Cooley","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":178225,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dennis, P.E.","contributorId":73627,"corporation":false,"usgs":true,"family":"Dennis","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":178223,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":62092,"text":"gq320 - 1964 - Geology of the Fairdealing quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:31","indexId":"gq320","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"320","title":"Geology of the Fairdealing quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq320","usgsCitation":"Wolfe, E.W., 1964, Geology of the Fairdealing quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 320, 1 map., https://doi.org/10.3133/gq320.","productDescription":"1 map.","costCenters":[],"links":[{"id":102333,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_782.htm","linkFileType":{"id":5,"text":"html"},"description":"782"},{"id":248289,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0320/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":253183,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0320/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.25,36.75 ], [ -88.25,36.8675 ], [ -88.11749999999999,36.8675 ], [ -88.11749999999999,36.75 ], [ -88.25,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db68058a","contributors":{"authors":[{"text":"Wolfe, Edward W.","contributorId":79878,"corporation":false,"usgs":true,"family":"Wolfe","given":"Edward","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":266903,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60403,"text":"mf290 - 1964 - Geology of the Devils Slide quadrangle, Morgan and Summit Counties, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:25","indexId":"mf290","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"290","title":"Geology of the Devils Slide quadrangle, Morgan and Summit Counties, Utah","language":"ENGLISH","doi":"10.3133/mf290","usgsCitation":"Mullens, T.E., and Laraway, W., 1964, Geology of the Devils Slide quadrangle, Morgan and Summit Counties, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 290, 1 map ;58 x 44 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf290.","productDescription":"1 map ;58 x 44 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104061,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2710.htm","linkFileType":{"id":5,"text":"html"},"description":"2710"},{"id":183240,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.61749999999999,4.168611111111112 ], [ -111.61749999999999,41 ], [ -111.5,41 ], [ -111.5,4.168611111111112 ], [ -111.61749999999999,4.168611111111112 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f86","contributors":{"authors":[{"text":"Mullens, T. E.","contributorId":34573,"corporation":false,"usgs":true,"family":"Mullens","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":263690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laraway, W.H.","contributorId":81552,"corporation":false,"usgs":true,"family":"Laraway","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":263691,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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