{"pageNumber":"6654","pageRowStart":"166325","pageSize":"25","recordCount":184681,"records":[{"id":1007578,"text":"1007578 - 1965 - Noteworthy records of reptiles from New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:04:17","indexId":"1007578","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1892,"text":"Herpetologica","active":true,"publicationSubtype":{"id":10}},"title":"Noteworthy records of reptiles from New Mexico","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Herpetologica","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Dixon, J., and Medica, P., 1965, Noteworthy records of reptiles from New Mexico: Herpetologica, v. 21, p. 72-75.","productDescription":"p. 72-75","startPage":"72","endPage":"75","numberOfPages":"4","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696934","contributors":{"authors":[{"text":"Dixon, J.R.","contributorId":106057,"corporation":false,"usgs":true,"family":"Dixon","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":315658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Medica, P.A.","contributorId":77079,"corporation":false,"usgs":true,"family":"Medica","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":315657,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1007577,"text":"1007577 - 1965 - Altitude record for Gerrhonotus kingi","interactions":[],"lastModifiedDate":"2012-02-02T00:04:17","indexId":"1007577","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1892,"text":"Herpetologica","active":true,"publicationSubtype":{"id":10}},"title":"Altitude record for Gerrhonotus kingi","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Herpetologica","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Medica, P., 1965, Altitude record for Gerrhonotus kingi: Herpetologica, v. 21, p. 147-148.","productDescription":"p. 147-148","startPage":"147","endPage":"148","numberOfPages":"2","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686994","contributors":{"authors":[{"text":"Medica, P.A.","contributorId":77079,"corporation":false,"usgs":true,"family":"Medica","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":315656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2902,"text":"wsp1809L - 1965 - Reconnaissance of the ground-water resources in parts of Larimer, Logan, Morgan, Sedgwick, and Weld Counties, Colorado, with a section on the chemical quality of the water","interactions":[],"lastModifiedDate":"2023-11-01T21:23:13.44938","indexId":"wsp1809L","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"L","title":"Reconnaissance of the ground-water resources in parts of Larimer, Logan, Morgan, Sedgwick, and Weld Counties, Colorado, with a section on the chemical quality of the water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1809L","usgsCitation":"Weist, W., and Brennan, R., 1965, Reconnaissance of the ground-water resources in parts of Larimer, Logan, Morgan, Sedgwick, and Weld Counties, Colorado, with a section on the chemical quality of the water: U.S. Geological Survey Water Supply Paper 1809, Report; iv, 24 p.; 1 Plate: 37.50 x 16.00 inches, https://doi.org/10.3133/wsp1809L.","productDescription":"Report; iv, 24 p.; 1 Plate: 37.50 x 16.00 inches","costCenters":[],"links":[{"id":422318,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25011.htm","linkFileType":{"id":5,"text":"html"}},{"id":29581,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29582,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809l/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138383,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809l/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Larimer County, Logan County, Morgan County, Sedgwick County, Weld County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -102.425,\n              41\n            ],\n            [\n              -105.17,\n              41\n            ],\n            [\n              -105.17,\n              40.282\n            ],\n            [\n              -102.425,\n              40.282\n            ],\n            [\n              -102.425,\n              41\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636d2d","contributors":{"authors":[{"text":"Weist, William G.","contributorId":21526,"corporation":false,"usgs":true,"family":"Weist","given":"William G.","affiliations":[],"preferred":false,"id":145983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brennan, Robert","contributorId":105695,"corporation":false,"usgs":true,"family":"Brennan","given":"Robert","email":"","affiliations":[],"preferred":false,"id":887318,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2897,"text":"wsp1811 - 1965 - Hydrology of the Little Plover River basin, Portage County, Wisconsin, and the effects of water resource development","interactions":[],"lastModifiedDate":"2023-04-13T20:54:27.826245","indexId":"wsp1811","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"1811","title":"Hydrology of the Little Plover River basin, Portage County, Wisconsin, and the effects of water resource development","docAbstract":"<p>The Little Plover River basin is in the sand-plain area of central Wisconsin. The basin and the surrounding sand-plain area provide a good fish and wildlife habitat and is a popular locale for sport fishing. Good yields may be obtained in the area from irrigated crops, and the irrigated acreage has been increasing rapidly in recent years. Sportsmen and conservationists are concerned about the effects of increased development of the water resources on the streams as trout habitat. In the past, many political and legal conflicts among water users have arisen from erroneous opinions as to the behavior of water. Many of these conflicts would be diminished or eliminated if the participants were cognizant of fundamental hydrologic principles. </p><p>This study was made to demonstrate the extent and nature of the interrelation of ground water and surface water and the fundamental hydrologic principles governing water movement. The study was also made to determine the hydrologic changes that might occur following development, to provide information that might be used as a basis for planning water development, and for drafting legislation that recognizes the relation between ground water and surface water. </p><p>Water has been developed in the Little Plover River basin for industry, for domestic and stock supplies, and for irrigation. Irrigated acreage is increasing in the area, and the use of water for irrigation may alter the hydrology of the basin somewhat. About 4,000-4,500 acres of land within the basin, or 50-60 percent of the basin area, is suitable for irrigated farming, but probably no more than 2,500 acres will be under irrigation in any one year, unless present crop-rotation practices are changed. </p><p>Most of the Little Plover River basin is underlain by from 40 to 100 feet of glacial outwash consisting of highly permeable sand and gravel. The glacial outwash is the main aquifer in the area and is capable of yielding large quantities of water to wells. An aquifer test in the area indicated that the coefficient of transmissibility of the glacial outwash is about 140,000 gallons per day per foot. The specific yield of the outwash is about 20 percent, as determined from water-level and streamfiow data. Morainal deposits occur locally with the glacial outwash. These deposits transmit water readily and do not form barriers to ground water in the outwash. Relatively impermeable crystalline rocks underlie the glacial deposits, and a sandstone ridge of low permeability impedes the movement of ground water from the basin by underflow. </p><p>The glacial outwash and morainal deposits are recharged by infiltration of 9-10 inches of the 31 inches of precipitation that falls on the area in an average year. If it is not withdrawn by wells for consumptive use or by phreatophytes, water that infiltrates the sand and gravel discharges later into the Little Plover River. This ground-water discharge constitutes 90-95 percent of the total flow of the Little Plover River. </p><p>Annual evapotranspiration varies considerably, but generally ranges from 2 to 8 inches less than the potential evapotranspiration of 24 inches. Consumptive use of irrigation water averages about 4 inches per year. Most of the water pumped from wells otherwise would be discharged to the stream, and consumptive use of irrigation water will deplete streamflow by the amount of evapotranspiration. </p><p>Pumping wells have little effect on the water level in the highly permeable sand and gravel. Significant interference between wells would occur only if large capacity wells were within a few tens of feet of each other. </p><p>Ground water and surface water are closely interrelated in the sand-plain area and ground-water withdrawals near the Little Plover River may cause a measurable streamflow depletion. In a test, a well that was pumping about 1,120 gpm (gallons per minute) and that was 300 feet from the stream derived about 30 percent of its flow from the stream after 3 days of pumping. </p><p>For this study, the effects of increased ground-water development were evaluated from a hypothetical development schedule, for which it was assumed that 500 acres were irrigated the first year and that an additional 50 acres were irrigated in each succeeding year for 10 years. It also was assumed that the average annual consumptive-use requirement for irrigation water would be one- third of an acre-foot per acre. Calculations indicate that the maximum monthly rate of depletion due to the consumptive use of 4 inches of ground water per year on 500 acres would be about 0.4 cfs (cubic feet per second) the first year and 0.5 cfs after 10 years of pumping. Other computations indicate that the maximum monthly rate of depletion due to irrigating 500 acres the first year and 50 additional acres each year for 10 years would be about 0.8 cfs. Maximum depletion would occur during the summer months, concurrent with the irrigation withdrawals. </p><p>Because of the close interrelation between ground and surface water, surface- water withdrawals will cause an increased inflow of ground water to the stream and a decline in ground-water levels near the stream. These effects were demonstrated by pumping from the stream. After 29 hours of pumping, a depletion of 1,120 gpm at a site 7,000 feet downstream was about 200 gpm less than the diversion at the pump. Most of the 200 gpm was supplied from the stream-banks, and ground-water levels near the stream declined as much as 0.3 foot. Computations indicated that ground-water inflow, following a streamflow diver- sion that lowered the stage 0.15 foot, would be 0.14 cfs after 5 days and 0.06 cfs after 30 days. </p><p>The demonstration of the quantitative relation between ground water and surface water, as given by this study, should provide a sound basis for planning water development to minimize conflicts of interest. The demonstrations also should provide a basis for drafting legislation that recognizes the interrelation of ground water and surface water. </p><p>Because the geology and the hydrology are relatively uniform throughout the sand plains, many of the methods and hydrologic values determined for this detailed study of the Little Plover River basin may be applied to other basins in the sand-plain area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1811","collaboration":"Prepared in cooperation with the Wisconsin Conservation Department and the University of Wisconsin Geological and Natural History Survey","usgsCitation":"Weeks, E.P., Erickson, D.W., and Holt, C.L., 1965, Hydrology of the Little Plover River basin, Portage County, Wisconsin, and the effects of water resource development: U.S. Geological Survey Water Supply Paper 1811, Report: v, 78 p.; 6 Plates: 21.00 x 18.01 inches or smaller, https://doi.org/10.3133/wsp1811.","productDescription":"Report: v, 78 p.; 6 Plates: 21.00 x 18.01 inches or smaller","numberOfPages":"85","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":415734,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25017.htm","linkFileType":{"id":5,"text":"html"}},{"id":29561,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29559,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29558,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29562,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29560,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29563,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1811/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138378,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1811/report-thumb.jpg"},{"id":29557,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Portage County","otherGeospatial":"Little Plover River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.589,\n              44.554\n            ],\n            [\n              -89.589,\n              44.404\n            ],\n            [\n              -89.367,\n              44.404\n            ],\n            [\n              -89.367,\n              44.554\n            ],\n            [\n              -89.589,\n              44.554\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdc0c","contributors":{"authors":[{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":145973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, Donald W.","contributorId":34900,"corporation":false,"usgs":true,"family":"Erickson","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145974,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holt, Charles Lee Roy Jr.","contributorId":77913,"corporation":false,"usgs":true,"family":"Holt","given":"Charles","suffix":"Jr.","email":"","middleInitial":"Lee Roy","affiliations":[],"preferred":false,"id":145975,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38824,"text":"pp525B - 1965 - Geological Survey research 1965, Chapter B","interactions":[],"lastModifiedDate":"2025-08-25T20:53:03.635437","indexId":"pp525B","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"525","chapter":"B","title":"Geological Survey research 1965, Chapter B","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1965 (Professional Paper 525)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp525B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1965, Geological Survey research 1965, Chapter B: U.S. Geological Survey Professional Paper 525, vi, 195 p., https://doi.org/10.3133/pp525B.","productDescription":"vi, 195 p.","costCenters":[],"links":[{"id":494847,"rank":17,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92899.htm","text":"K-Ar and Rb-Sr ages of biotite from the Middle Jurassic part of the Carmel Formation, Utah","linkFileType":{"id":5,"text":"html"}},{"id":494846,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92898.htm","text":"Correlation of Cretaceous and lower Tertiary rocks near Livingston, Montana with those in other areas in Montana and Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":494845,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30100.htm","text":"Effect of Great Swamp, New Jersey, on streamflow during base-flow periods","linkFileType":{"id":5,"text":"html"}},{"id":494843,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30098.htm","text":"Glacial deposits of Nebraskan and Kansan age in northern Kentucky","linkFileType":{"id":5,"text":"html"}},{"id":494841,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30096.htm","text":"Gold Flat Member of the Thirsty Canyon Tuff - a pantellerite ash-flow sheet in southern Nevada","linkFileType":{"id":5,"text":"html"}},{"id":494840,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30095.htm","text":"The Clinchport thrust fault - a major structural element of the southern Appalachian Mountains","linkFileType":{"id":5,"text":"html"}},{"id":494839,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30094.htm","text":"Structure of the Timber Mountain caldera, southern Nevada, and its relation to basin-range structure","linkFileType":{"id":5,"text":"html"}},{"id":494838,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30093.htm","text":"Distribution of gravel in the Patuxent Formation in the Beltsville quadrangle, Prince Georges and Montgomery Counties, Maryland","linkFileType":{"id":5,"text":"html"}},{"id":494837,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30092.htm","text":"Low-volatile bituminous coal of Mississippian age on the Lisburne Peninsula, northwestern Alaska","linkFileType":{"id":5,"text":"html"}},{"id":494836,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30091.htm","text":"Suggestions for prospecting for evaporite deposits in southwestern Virginia","linkFileType":{"id":5,"text":"html"}},{"id":494835,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30090.htm","text":"Mercury-bearing antimony deposit between Big Creek and Yellow Pine, central Idaho","linkFileType":{"id":5,"text":"html"}},{"id":494834,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30089.htm","text":"Correlation of zinc abundance with stratigraphic thickness variations in the Kingsport Formation, West New Market area, Mascot - Jefferson City mining district, Tennessee","linkFileType":{"id":5,"text":"html"}},{"id":422317,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30088.htm","text":"Geophysical evidence of a caldera at Bonanza, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":65758,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0525b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120113,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0525b/report-thumb.jpg"},{"id":494844,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30099.htm","text":"Age and origin of the Puget Sound trough in western Washington","linkFileType":{"id":5,"text":"html"}},{"id":494842,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30097.htm","text":"Potassium-argon ages of some plutonic rocks, Tenakee area, Chichagof Island, southeastern Alaska","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db68780d","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":529886,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010598,"text":"70010598 - 1965 - Water analysis","interactions":[],"lastModifiedDate":"2023-03-20T16:01:05.594468","indexId":"70010598","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Water analysis","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60224a016","usgsCitation":"Skougstad, M.W., and Fishman, M., 1965, Water analysis: Analytical Chemistry, v. 37, no. 5, p. 232-260, https://doi.org/10.1021/ac60224a016.","productDescription":"29 p.","startPage":"232","endPage":"260","costCenters":[],"links":[{"id":219097,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"5","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505bc795e4b08c986b32c509","contributors":{"authors":[{"text":"Skougstad, Marvin W.","contributorId":65064,"corporation":false,"usgs":true,"family":"Skougstad","given":"Marvin","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359243,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fishman, Marvin J.","contributorId":87110,"corporation":false,"usgs":true,"family":"Fishman","given":"Marvin J.","affiliations":[],"preferred":false,"id":866865,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1718,"text":"wsp1809I - 1965 - Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61","interactions":[],"lastModifiedDate":"2023-03-13T20:10:12.868331","indexId":"wsp1809I","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"I","title":"Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61","docAbstract":"<p>Artesian water pressure in the deep sandstone aquifer continued to decline throughout most of the Milwaukee-Waukesha area, Wisconsin between 1950 and 1961. Areas of greatest water-level decline were in northeast Waukesha County and in northwest Milwaukee County. The chief cause of the decline was continued heavy pumpage. The major aquifers of southeastern Wisconsin are the Niagara aquifer, which is primarily Niagara Dolomite of Silurian age, and the sandstone aquifer, which consists of sandstones of Cambrian and Ordovician ages. Locally, the glacial sands and gravels ,of Pleistocene age also are important aquifers. In the Milwaukee-Waukesha area, the sandstone aquifer is completely artesian, confined above by the Maquoketa Shale. The Niagara aquifer is generally unconfined. Pumpage from the sandstone aquifer in the Milwaukee-Waukesha area de- creased from about 23.3 million gallons per day in 1950 to about 20.9 million gallons per day in 1961. The principal reason for decreased pumpage was sub- stitution of surface-water supply from Lake Michigan. Between 1950 and 1961, the water-level changes in wells in the sandstone aquifer ranged from plus 10 feet at Town of Lake to minus 98 feet in northwest Milwaukee. Except for a small area near Town of Lake, water levels in wells in the Milwaukee-Waukesha area were lower in 1961 than in 1950. Water-level changes were directly related to the pumpage pattern and pump- age changes. Increased pumpage at Waukesha and in northwest Milwaukee and continued heavy pumpage at Wauwatosa caused widespread water-level declines in northeast Waukesha County and in northwest Milwaukee County. Locally, decreased pumpage at West Milwaukee allowed limited recovery of water levels since 1957. Estimates of pumpage through the year 1975 indicate a pumpage decrease in the middle 1960's, followed by an increase in the late 1960's and early 1970's. Additional conversion to surface-water supply in Milwaukee County will account for most pumpage decreases. Increased pumpage is most likely in Waukesha County where the population is expanding rapidly and an adequate surface-water supply is not readily accessible. The westward shift of the pumpage pattern may cause an additional water-level decline of about 50 feet at Waukesha but will permit water levels to recover about 100 feet at West Allis by 1975. Partial or complete conversion to surface-water supplies by municipalities that depend entirely on water from the sandstone aquifer would allow greater use of the sandstone aquifer by isolated suburban developments and industries.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1809I","collaboration":"Prepared in cooperation with the University of Wisconsin, Geological and Natural History Survey","usgsCitation":"Green, J.H., and Hutchinson, R.D., 1965, Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61: U.S. Geological Survey Water Supply Paper 1809, Report: iii, 19 p. ; 2 Plates: 19.50 x 24.00 inches and 18.50 x 24.00 inches, https://doi.org/10.3133/wsp1809I.","productDescription":"Report: iii, 19 p. ; 2 Plates: 19.50 x 24.00 inches and 18.50 x 24.00 inches","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":26806,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136940,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809i/report-thumb.jpg"},{"id":26805,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26804,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414041,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25008.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wisconsin","city":"Milwaukee, Waukesha","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -88.82011978710044,\n              43.6048598948214\n            ],\n            [\n              -88.82011978710044,\n              42.619688745253114\n            ],\n            [\n              -87.76500461016991,\n              42.619688745253114\n            ],\n            [\n              -87.76500461016991,\n              43.6048598948214\n            ],\n            [\n              -88.82011978710044,\n              43.6048598948214\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673ff","contributors":{"authors":[{"text":"Green, J. H.","contributorId":43312,"corporation":false,"usgs":true,"family":"Green","given":"J.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":144010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchinson, R. D.","contributorId":99112,"corporation":false,"usgs":true,"family":"Hutchinson","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":144011,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175584,"text":"70175584 - 1965 - Oregon ground-water levels, 1964","interactions":[],"lastModifiedDate":"2016-08-17T11:35:47","indexId":"70175584","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Oregon ground-water levels, 1964","docAbstract":"<p>No abstract available.</p>","language":"English","usgsCitation":"Sceva, J.E., and DeBow, R., 1965, Oregon ground-water levels, 1964: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326657,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b53e4b03bcb0104bc2e","contributors":{"authors":[{"text":"Sceva, Jack E.","contributorId":79086,"corporation":false,"usgs":true,"family":"Sceva","given":"Jack","email":"","middleInitial":"E.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":645760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeBow, Robert","contributorId":173757,"corporation":false,"usgs":false,"family":"DeBow","given":"Robert","email":"","affiliations":[],"preferred":false,"id":645761,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175593,"text":"70175593 - 1965 - Selected ground water data in the Eola-Amity Hills area, northern Willamette Valley, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T12:04:25","indexId":"70175593","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Selected ground water data in the Eola-Amity Hills area, northern Willamette Valley, Oregon","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\">Occurrence, quality, and availability of <span class=\"searchword\">ground</span> <span class=\"searchword\">water</span> differ considerably from place to place in the <span class=\"searchword\">Eola</span>-<span class=\"searchword\">Amity</span> <span class=\"searchword\">Hills</span> <span class=\"searchword\">area</span> because of the highly diversified geologic and hydrologic conditions. A table relates the geologic situation to the availability of <span class=\"searchword\">ground</span> <span class=\"searchword\">water</span> for four areas--<span class=\"searchword\">Eola</span>-<span class=\"searchword\">Amity</span> <span class=\"searchword\">Hills</span>, east and west <span class=\"searchword\">valley</span> plains, and <span class=\"searchword\">Willamette</span> River flood plain. Tables show well and spring records, drillers' logs, and chemical analyses of <span class=\"searchword\">ground</span> <span class=\"searchword\">water</span>. The final interpretive report will be published by the U.S. Geological Survey.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","usgsCitation":"Price, D., and Johnson, N.A., 1965, Selected ground water data in the Eola-Amity Hills area, northern Willamette Valley, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326670,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Willamette Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b58e4b03bcb0104bc68","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":645787,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Nyra A.","contributorId":173771,"corporation":false,"usgs":false,"family":"Johnson","given":"Nyra","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":645788,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175590,"text":"70175590 - 1965 - Add to e-Shelf \t Records of wells, water levels and chemical quality of water in Baker Valley, Baker County, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T11:47:07","indexId":"70175590","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Add to e-Shelf \t Records of wells, water levels and chemical quality of water in Baker Valley, Baker County, Oregon","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\"><span class=\"searchword\">Records</span> from 135 representative <span class=\"searchword\">wells</span>, and <span class=\"searchword\">chemical</span> analyses of <span class=\"searchword\">water</span> from 49 <span class=\"searchword\">wells</span> and 2 springs are tabulated. Drillers' logs of representative <span class=\"searchword\">wells</span> comprise most of the report.</span></p>","largerWorkType":{"id":2,"text":"Article"},"usgsCitation":"Ducret, G., and Anderson, D., 1965, Add to e-Shelf \t Records of wells, water levels and chemical quality of water in Baker Valley, Baker County, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326663,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","county":"Baker","otherGeospatial":"Baker Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58abce4b03bcb0104bb55","contributors":{"authors":[{"text":"Ducret, G.L. Jr.","contributorId":107703,"corporation":false,"usgs":true,"family":"Ducret","given":"G.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":645780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, D.B.","contributorId":47762,"corporation":false,"usgs":true,"family":"Anderson","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":645781,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5220445,"text":"5220445 - 1965 - Results of woodcock wing collections, 1959 to 1962","interactions":[],"lastModifiedDate":"2025-02-07T17:11:17.308989","indexId":"5220445","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Results of woodcock wing collections, 1959 to 1962","docAbstract":"<p>During hunting seasons from 1959 to 1962, age and sex determined from 45,444 wings were used to measure annual productivity of woodcocks (<i>Philohela minor</i>). Age of birds was determined by pattern and color of secondaries and by wear on primaries. Sex was determined by width and length of primaries. Overall age ratios, weighted by kill estimates, were the same each year and indicated no change in annual productivity. Immature sex ratios in the combined kill were nearly even each year, but kill of adult females was much larger than kill of adult males. The difference in sex ratios between immatures and adults thus suggests higher mortality of males than females after the first hunting season. Since woodcocks are promiscuous, an unbalanced adult sex ratio in favor of females probably does not reduce productivity. There are, however, factors affecting reliability of information deduced from wing collections, and further research is necessary to answer questions on differential vulnerability and mortality rates.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3798641","usgsCitation":"Martin, F., Geis, A.D., and Stickel, W.H., 1965, Results of woodcock wing collections, 1959 to 1962: Journal of Wildlife Management, v. 29, no. 1, p. 121-131, https://doi.org/10.2307/3798641.","productDescription":"11 p.","startPage":"121","endPage":"131","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197852,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut, Louisiana, Maine, Massachusetts, Michigan, New Hampshire, New York, Pennsylvania, Vermont, 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,{"id":70197584,"text":"70197584 - 1964 - Subdivision of the San Lorenzo Formation (Eocene and Oligocene) west-central California","interactions":[],"lastModifiedDate":"2023-02-01T14:31:27.84101","indexId":"70197584","displayToPublicDate":"2018-06-12T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Subdivision of the San Lorenzo Formation (Eocene and Oligocene) west-central California","docAbstract":"<p>The San Lorenzo Formation was for many years considered synonymous with Oligocene Series. The formation name was extended, incorrectly in most cases, to rocks as far north as British Columbia and as far south as southern California. The formation in its type area was never adequately studied, resulting in fallacious concepts of its faunas and erroneous correlations.</p><p>The San Lorenzo Formation has been subdivided into the Twobar Shale Member of Narizian (late Eocene) age and Rices Mudstone Member of Rufugian and Zemorrian (Eocene and Oligocene) age. Faunas and lithology suggest that the older member was deposited slowly in a bathyal, open-sea environment, whereas the Rices Mudstone Member seems to have been deposited rapidly in a restricted basin. Glauconite at the contact of the members suggests a stratigraphic break in the depositional sequence.</p><p>Most, perhaps all, of the so-called characteristic San Lorenzo mollusks are from the upper (Zemorrian) part of the Rices Mudstone Member, or from the overlying Vaqueros Sandstone. The \"transitional sandstone\" of Arnold is Vaqueros, not San Lorenzo.</p><p>Subdivision of the San Lorenzo Formation and the discovery of glauconitic marker beds provide additional stratigraphic control in an oil province characterized by poor exposures.</p>","language":"English","publisher":"American Association of Petroleum Geologists","publisherLocation":"Tulsa, OK","doi":"10.1306/BC743D21-16BE-11D7-8645000102C1865D","usgsCitation":"Brabb, E.E., 1964, Subdivision of the San Lorenzo Formation (Eocene and Oligocene) west-central California: American Association of Petroleum Geologists Bulletin, v. 48, no. 5, p. 670-679, https://doi.org/10.1306/BC743D21-16BE-11D7-8645000102C1865D.","productDescription":"10 p.","startPage":"670","endPage":"679","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":354982,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Lorenzo Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.45677512208947,\n              37.38122044720332\n            ],\n            [\n              -122.45677512208947,\n              36.95089653986274\n            ],\n            [\n              -121.96980337303017,\n              36.95089653986274\n            ],\n            [\n              -121.96980337303017,\n              37.38122044720332\n            ],\n            [\n              -122.45677512208947,\n              37.38122044720332\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"48","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brabb, Earl E.","contributorId":8545,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":737846,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179736,"text":"70179736 - 1964 - Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part II: Technical report","interactions":[],"lastModifiedDate":"2017-09-06T17:19:54","indexId":"70179736","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"3-II","title":"Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part II: Technical report","docAbstract":"<p>During the 1960 and 1961 water years an annual load of about 2 million tons of dissolved minerals was contributed to the Great Salt Lake area by surficial sources. Almost 60 percent of this load was sodium and chloride. Of the six units contributing to the lake area, three - the Bear River, the Jordan River, and the unit comprising drains and sewage canals – contributed about three-fourths of the runoff and of the load. The water type of these tributaries ranged from bicarbonate in the headwaters to sulfate and chloride near the mouths; the dissolved-solids concentrations were higher in the downstream reaches than in the headwaters.</p>","language":"English","publisher":"Utah Geological and Minerological Society","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with The College of Mines and Mineral Industries, University of Utah, Salt Lake City, Utah","usgsCitation":"Hahl, D.C., and Langford, R., 1964, Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part II: Technical report: Utah Geological and Mineralogical Survey Water-Resources Bulletin 3-II, 40 p.","productDescription":"40 p.","numberOfPages":"44","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333226,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345530,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70179734","text":"Part I: Selected hydrologic data"},{"id":345529,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-3part2.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.2305908203125,\n              40.59727063442024\n            ],\n            [\n              -113.2305908203125,\n              41.795888098191426\n            ],\n            [\n              -111.81884765624999,\n              41.795888098191426\n            ],\n            [\n              -111.81884765624999,\n              40.59727063442024\n            ],\n            [\n              -113.2305908203125,\n              40.59727063442024\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d2","contributors":{"authors":[{"text":"Hahl, D. C.","contributorId":57436,"corporation":false,"usgs":true,"family":"Hahl","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":658475,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langford, R.H.","contributorId":59426,"corporation":false,"usgs":true,"family":"Langford","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":658476,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179723,"text":"70179723 - 1964 - Geology and ground-water resources of the Jordan Valley, Utah","interactions":[],"lastModifiedDate":"2017-09-06T17:26:29","indexId":"70179723","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"7","title":"Geology and ground-water resources of the Jordan Valley, Utah","docAbstract":"<p>The Jordan Valley occupies about 400 square miles in the central part of Salt Lake County in north-central Utah. Salt Lake City, the capital of Utah, is in the northeastern part of the valley. The valley is at the eastern margin of the Basin and range physiographic province, and it is bounded on the northeast, east, south, and west by mountain ranges. The valley is drained by the Jordan River which enters through a water gap in the mountains to the south, flows north, and empties into the Great Salt Lake, which forms the northwestern border of the valley.</p>","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Marine, I.W., and Price, D., 1964, Geology and ground-water resources of the Jordan Valley, Utah: Utah Geological and Mineralogical Survey Water-Resources Bulletin 7, 67 p.","productDescription":"67 p.","numberOfPages":"79","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333200,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333199,"rank":2,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70179625","text":"Utah State Engineer Water Circular 1"},{"id":333198,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-7.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Jordan Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.22122192382812,\n              40.72540497175607\n            ],\n            [\n              -112.10861206054688,\n              40.693134153308065\n            ],\n            [\n              -112.13470458984375,\n              40.59935608796518\n            ],\n            [\n              -112.08663940429688,\n              40.54093880017256\n            ],\n            [\n              -112.09899902343749,\n              40.51901917108279\n            ],\n            [\n              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Wendell","contributorId":49339,"corporation":false,"usgs":true,"family":"Marine","given":"I.","email":"","middleInitial":"Wendell","affiliations":[],"preferred":false,"id":658436,"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":658437,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70180001,"text":"70180001 - 1964 - Developing a state water plan: Ground-water conditions in Utah, spring of 1964","interactions":[],"lastModifiedDate":"2017-01-23T11:29:18","indexId":"70180001","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1964","docAbstract":"<p>This report is the first in a series of annual reports which will describe ground-water conditions in Utah. It was prepared cooperatively by the U.S. Geological Survey and the Utah Water and Power Board and was designed to provide the data for interested parties, such as legislators, administrators, and planners to keep abreast of changing ground-water conditions in the state. Because this report is the first of the series, it necessarily includes certain background and descriptive information which gives a broad general picture of ground-water conditions. Subsequent reports will discuss only changes that have taken place during the previous year.</p><p>Many of the data used in the preparation of the report were collected by the Geological Survey in cooperation with the Utah State Engineer during past and continuing programs. The well-location map and some statistical information about numbers of wells in the State were prepared by digital computer from the Utah Resources Information System, University of Utah, utilizing records which were compiled largely from the files of the Utah State Engineer. R.E. Marsell, geological consultant to the Utah Water and Power Board, first suggested that this report be prepared.</p>","language":"English","publisher":"Utah Water and Power Board","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Arnow, T., Butler, R., Mower, R.W., Gates, J., Cordova, R., Carpenter, C., Bjorklund, L., Feltis, R., Robinson, G., and Sandberg, G.W., 1964, Developing a state water plan: Ground-water conditions in Utah, spring of 1964: Cooperative Investigations Report 2, 104 p.","productDescription":"104 p.","numberOfPages":"208","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333666,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333665,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-201"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58863a15e4b0cad700058b71","contributors":{"authors":[{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":659661,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butler, R.G.","contributorId":60706,"corporation":false,"usgs":true,"family":"Butler","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":659662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mower, R. 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