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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir510","usgsCitation":"Eisenhuth, H., 1965, Index of surface-water records to December 31, 1963: Part 10. - The Great Basin: U.S. Geological Survey Circular 510, 35 p., https://doi.org/10.3133/cir510.","productDescription":"35 p.","numberOfPages":"42","costCenters":[],"links":[{"id":31067,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0510/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0510/report-thumb.jpg"}],"country":"United States","state":"California, Nevada, Oregon, Utah, Wyoming","otherGeospatial":"Great Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.24658203125,\n 32.676372772089834\n ],\n [\n -115.521240234375,\n 38.26406296833961\n ],\n [\n -115.26855468749999,\n 38.44068226417387\n ],\n [\n -114.76318359375,\n 38.46219172306828\n ],\n [\n -114.7467041015625,\n 38.41055825094609\n ],\n [\n -114.2083740234375,\n 37.54457732085582\n ],\n [\n -114.136962890625,\n 37.58376576718623\n ],\n [\n -114.10400390625,\n 37.6968609874419\n ],\n [\n -114.312744140625,\n 38.53527591154413\n ],\n [\n -114.18090820312499,\n 38.69408504756833\n ],\n [\n -113.8568115234375,\n 38.655488159953\n ],\n [\n -113.6700439453125,\n 37.90953361677018\n ],\n [\n -113.44482421875,\n 37.47485808497102\n ],\n [\n -113.2305908203125,\n 37.431250501793585\n ],\n [\n -113.104248046875,\n 37.448696585910376\n ],\n [\n -111.67053222656249,\n 37.93553306183642\n ],\n [\n -111.2640380859375,\n 38.53527591154413\n ],\n [\n -110.8465576171875,\n 40.22082997283287\n ],\n [\n -110.32470703125,\n 41.75492216766298\n ],\n [\n -110.1708984375,\n 42.439674178149424\n ],\n [\n -111.55517578125,\n 42.52069952914966\n ],\n [\n -112.236328125,\n 41.83682786072714\n ],\n [\n -113.115234375,\n 41.934976500546604\n ],\n [\n -114.49951171875,\n 41.36031866306708\n ],\n [\n -115.75195312499999,\n 41.78769700539063\n ],\n [\n -117.3779296875,\n 42.09822241118974\n ],\n [\n -119.77294921874999,\n 44.32384807250689\n ],\n [\n -120.38818359375,\n 44.040218713142146\n ],\n [\n -120.76171875,\n 44.166444664458595\n ],\n [\n -121.57470703125,\n 44.38669150215206\n ],\n [\n -121.39892578125,\n 43.54854811091286\n ],\n [\n -121.11328124999999,\n 42.89206418807337\n ],\n [\n -120.08056640625,\n 42.74701217318067\n ],\n [\n -119.99267578124999,\n 41.983994270935625\n ],\n [\n -119.99267578124999,\n 41.27780646738183\n ],\n [\n -120.78369140624999,\n 41.244772343082076\n ],\n [\n -121.35498046875,\n 40.84706035607122\n ],\n [\n -120.498046875,\n 40.17887331434696\n ],\n [\n -120.08056640625,\n 39.99395569397331\n ],\n [\n -119.970703125,\n 39.01064750994083\n ],\n [\n -118.85009765625,\n 37.666429212090605\n ],\n [\n -118.10302734374999,\n 36.421282443649496\n ],\n [\n -118.27880859375001,\n 34.994003757575776\n ],\n [\n -118.80615234374999,\n 34.92197103616377\n ],\n [\n -117.46582031249999,\n 34.23451236236987\n ],\n [\n -116.45507812500001,\n 33.815666308702774\n ],\n [\n -116.27929687499999,\n 33.02708758002874\n ],\n [\n -116.03759765625,\n 32.62087018318113\n ],\n [\n -115.24658203125,\n 32.676372772089834\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3a77","contributors":{"authors":[{"text":"Eisenhuth, H.P.","contributorId":38140,"corporation":false,"usgs":true,"family":"Eisenhuth","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":147947,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3158,"text":"wsp1819B - 1965 - Predicted hydrologic effects of pumping from the Lichterman Well Field in the Memphis Area, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1819B","displayToPublicDate":"1994-01-01T00:00:00","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":"1819","chapter":"B","title":"Predicted hydrologic effects of pumping from the Lichterman Well Field in the Memphis Area, Tennessee","docAbstract":"The Lichterman well field is scheduled to go into operation early in 1965 to supplement the municipal water-supply system for the city of Memphis, Tenn. Although the initial rate of withdrawal from the well field will be about 8 mgd (million gallons per day), the ultimate design capacity of the field is 20 mgd. A study of sand samples, drillers' logs, and geophysical logs collected during preliminary test drilling at the site for the Lichterman well field was used as a basis for defining three zones of sand favorable for the construction of high-capacity (1,000 gallons per minute or more) water wells. The three zones occur in the '500-foot' sand and are here designated (in descending order) as zone A, zone B, and zone C. The depth to the top of these zones below land surface has the following ranges: zone A, 125 to 225 feet; zone B, 200 to 350 feet; and zone C, 700 to 775 feet. Zones A and B range from 0 to 100 feet in thickness, and zone C ranges from 10 to 100 feet in thickness. Within the well field proper these zones are expected to react to the stress of pumping as separate hydrologic units, but outside the well field the three zones are expected to react as a single hydrologic unit. \r\n\r\nThe '500-foot' sand in the Germantown-Collierville area is recharged chiefly by precipitation on the outcrop area of the sand to the east, but the evidence indicates that additional recharge is entering the aquifer from the Wolf River. In spite of this additional recharge, water levels in the '500-foot' sand are declining at an average rate of about two-thirds of a foot per year, owing to municipal and industrial pumpage in the Memphis area. However, this decline is not expected to alter the excellent quality of the water in the '500-foot' sand at the site of the Lichterman well field. \r\n\r\nPumping in the Lichterman well field will create a cone of depression in the free-water (piezometric) surface of the '500-foot' sand. The decline in water levels will be directly proportional to the rate of pumping and inversely proportional to the distance from the well field. The resultant changes in hydraulic gradients will alter the direction of ground-water movement in the vicinity of the well field and increase the rate of movement toward the well field from areas of recharge. The lowering of water levels might also accelerate locally the changeover from artesian conditions to semiartesian or water-table conditions in the '500-foot' sand. \r\n\r\nWithin the well field proper, water levels are expected to fluctuate as individual wells are turned on and off to accommodate the demand for water. The presence of clay beds in the aquifer will tend to limit the specific capacity of individual production wells, but could serve to limit interference between wells if adjacent wells are screened in different sections of the aquifer. Interference between wells might also be lessened by pumping those wells having the highest specific capacities for the longest periods of time.","language":"ENGLISH","doi":"10.3133/wsp1819B","usgsCitation":"Nyman, D.J., 1965, Predicted hydrologic effects of pumping from the Lichterman Well Field in the Memphis Area, Tennessee: U.S. Geological Survey Water Supply Paper 1819, 26 p. , https://doi.org/10.3133/wsp1819B.","productDescription":"26 p. ","costCenters":[],"links":[{"id":138860,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819b/report-thumb.jpg"},{"id":30106,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e99e","contributors":{"authors":[{"text":"Nyman, Dale J.","contributorId":28584,"corporation":false,"usgs":true,"family":"Nyman","given":"Dale","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":146347,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3558,"text":"cir497 - 1965 - The Clinch River study--An investigation of the fate of radionuclides released to a surface stream","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir497","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"497","title":"The Clinch River study--An investigation of the fate of radionuclides released to a surface stream","docAbstract":"The Clinch River Study is a multiagency effort to evaluate the physical, chemical, and biological effects of the release to de Clinch River of low-level radioactive wastes from the Oak Ridge National Laboratory. The major radionuclides released are ruthenium-106, cesium-137, cobalt-60, and strontium-90. Hydrologic and biologic studies have indicated that the radiation doses in the river are well below maximum acceptable levels. Radionuclide concentrations in river water have been measured at seven sampling stations on the Clinch and Tennessee Rivers. Mass-balance calculations for 44 weeks of sampling indicate that losses of radionuclides from the water phase to the river-bottom sediments represent only a very small part of the total radioactivity released to the river. \r\n\r\nA study of the Clinch River bottom-sediment cores collected in 1962 has disclosed a recurring pattern of variation in radioactivity with depth which may reflect past events in waste-disposal operations at the laboratory. Current investigations are expected to provide information about the chemical forms in which the major radionuclides exist and the mechanisms by which they were incorporated in the sediments.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir497","usgsCitation":"Pickering, R., Carrigan, P., and Parker, F., 1965, The Clinch River study--An investigation of the fate of radionuclides released to a surface stream: U.S. Geological Survey Circular 497, iv, 12 p. :ill., graphs, map ;26 cm., https://doi.org/10.3133/cir497.","productDescription":"iv, 12 p. :ill., graphs, map ;26 cm.","costCenters":[],"links":[{"id":138411,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0497/report-thumb.jpg"},{"id":30577,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0497/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f51e","contributors":{"authors":[{"text":"Pickering, R.J.","contributorId":103253,"corporation":false,"usgs":true,"family":"Pickering","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":147157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carrigan, P.H.","contributorId":85160,"corporation":false,"usgs":true,"family":"Carrigan","given":"P.H.","affiliations":[],"preferred":false,"id":147156,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parker, F.L.","contributorId":79455,"corporation":false,"usgs":true,"family":"Parker","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":147155,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3983,"text":"cir511 - 1965 - Index of surface-water records to December 31, 1963--Part 11, Pacific slope basins in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir511","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"511","title":"Index of surface-water records to December 31, 1963--Part 11, Pacific slope basins in California","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir511","usgsCitation":"Eisenhuth, H., 1965, Index of surface-water records to December 31, 1963--Part 11, Pacific slope basins in California: U.S. Geological Survey Circular 511, 50 p. :ill., map ;26 cm., https://doi.org/10.3133/cir511.","productDescription":"50 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":117207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0511/report-thumb.jpg"},{"id":31068,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0511/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3a7e","contributors":{"authors":[{"text":"Eisenhuth, H.P.","contributorId":38140,"corporation":false,"usgs":true,"family":"Eisenhuth","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":147948,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3038,"text":"wsp1610C - 1965 - Waterpower resources in Nehalem River basin, Oregon","interactions":[{"subject":{"id":16685,"text":"ofr59131 - 1959 - Waterpower resources in Nehalem River basin, Oregon, with geology of dam and reservoir sites","indexId":"ofr59131","publicationYear":"1959","noYear":false,"title":"Waterpower resources in Nehalem River basin, Oregon, with geology of dam and reservoir sites"},"predicate":"SUPERSEDED_BY","object":{"id":3038,"text":"wsp1610C - 1965 - Waterpower resources in Nehalem River basin, Oregon","indexId":"wsp1610C","publicationYear":"1965","noYear":false,"chapter":"C","title":"Waterpower resources in Nehalem River basin, Oregon"},"id":1}],"lastModifiedDate":"2023-01-03T22:05:42.967225","indexId":"wsp1610C","displayToPublicDate":"1994-01-01T00:00:00","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":"1610","chapter":"C","title":"Waterpower resources in Nehalem River basin, Oregon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1610C","usgsCitation":"Young, L.L., Colbert, J.L., Gaskill, D.L., and Piper, A., 1965, Waterpower resources in Nehalem River basin, Oregon: U.S. Geological Survey Water Supply Paper 1610, Report: v, 58 p.; 4 Plates: 26.00 x 19.77 inches or smaller, https://doi.org/10.3133/wsp1610C.","productDescription":"Report: v, 58 p.; 4 Plates: 26.00 x 19.77 inches or smaller","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":411302,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24799.htm","linkFileType":{"id":5,"text":"html"}},{"id":29879,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1610c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29878,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1610c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29881,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1610c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29880,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1610c/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29877,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1610c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139299,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1610c/report-thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Nehalem River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -123.81382726717416,\n 46.09485688632233\n ],\n [\n -123.81382726717416,\n 45.71849428512374\n ],\n [\n -123.041131977578,\n 45.71849428512374\n ],\n [\n -123.041131977578,\n 46.09485688632233\n ],\n [\n -123.81382726717416,\n 46.09485688632233\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485aa","contributors":{"authors":[{"text":"Young, Loyd L.","contributorId":14805,"corporation":false,"usgs":true,"family":"Young","given":"Loyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colbert, Jesse Lane","contributorId":9239,"corporation":false,"usgs":true,"family":"Colbert","given":"Jesse","email":"","middleInitial":"Lane","affiliations":[],"preferred":false,"id":146191,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gaskill, David L.","contributorId":53369,"corporation":false,"usgs":true,"family":"Gaskill","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146193,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Piper, Arthur M.","contributorId":65060,"corporation":false,"usgs":true,"family":"Piper","given":"Arthur M.","affiliations":[],"preferred":false,"id":146194,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":4204,"text":"cir501 - 1965 - Index of surface-water records to December 31, 1963--Part 1, North Atlantic slope basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:45","indexId":"cir501","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"501","title":"Index of surface-water records to December 31, 1963--Part 1, North Atlantic slope basins","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir501","usgsCitation":"Anderson, B., and Ham, C., 1965, Index of surface-water records to December 31, 1963--Part 1, North Atlantic slope basins: U.S. Geological Survey Circular 501, 73 p. :ill., map ;26 cm., https://doi.org/10.3133/cir501.","productDescription":"73 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":118193,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0501/report-thumb.jpg"},{"id":31318,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0501/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3a6f","contributors":{"authors":[{"text":"Anderson, B.A.","contributorId":73581,"corporation":false,"usgs":true,"family":"Anderson","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":148401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ham, C.B.","contributorId":73582,"corporation":false,"usgs":true,"family":"Ham","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":148402,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3960,"text":"cir499 - 1965 - Selected references on saline ground-water resources of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir499","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"499","title":"Selected references on saline ground-water resources of the United States","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir499","usgsCitation":"Feth, J.H., 1965, Selected references on saline ground-water resources of the United States: U.S. Geological Survey Circular 499, 30 p. ;26 cm., https://doi.org/10.3133/cir499.","productDescription":"30 p. ;26 cm.","costCenters":[],"links":[{"id":122956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0499/report-thumb.jpg"},{"id":31048,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0499/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f82d6","contributors":{"authors":[{"text":"Feth, John Henry Frederick","contributorId":37310,"corporation":false,"usgs":true,"family":"Feth","given":"John","email":"","middleInitial":"Henry Frederick","affiliations":[],"preferred":false,"id":147898,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3039,"text":"wsp1787 - 1965 - Ground-water conditions and storage in the Central Sevier Valley, Utah","interactions":[{"subject":{"id":52149,"text":"ofr60161 - 1960 - Ground-water areas and well logs, Central Sevier Valley, Utah","indexId":"ofr60161","publicationYear":"1960","noYear":false,"title":"Ground-water areas and well logs, Central Sevier Valley, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3039,"text":"wsp1787 - 1965 - Ground-water conditions and storage in the Central Sevier Valley, Utah","indexId":"wsp1787","publicationYear":"1965","noYear":false,"title":"Ground-water conditions and storage in the Central Sevier Valley, Utah"},"id":1},{"subject":{"id":52226,"text":"ofr6226 - 1962 - Records of selected wells and springs, chemical analyses of ground water, water-level measurements of selected wells, selected drillers' logs of wells, and logs of test holes, Central Sevier Valley, Sanpete, Sevier, and Piute Counties, Utah","indexId":"ofr6226","publicationYear":"1962","noYear":false,"title":"Records of selected wells and springs, chemical analyses of ground water, water-level measurements of selected wells, selected drillers' logs of wells, and logs of test holes, Central Sevier Valley, Sanpete, Sevier, and Piute Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3039,"text":"wsp1787 - 1965 - Ground-water conditions and storage in the Central Sevier Valley, Utah","indexId":"wsp1787","publicationYear":"1965","noYear":false,"title":"Ground-water conditions and storage in the Central Sevier Valley, Utah"},"id":2},{"subject":{"id":52308,"text":"ofr6314 - 1963 - Records of selected wells and springs, chemical analyses of ground water, water-level measurements of selected wells, selected drillers' logs of wells, and logs of test holes, Central Sevier Valley, Sanpete, Sevier, and Piute Counties, Utah","indexId":"ofr6314","publicationYear":"1963","noYear":false,"title":"Records of selected wells and springs, chemical analyses of ground water, water-level measurements of selected wells, selected drillers' logs of wells, and logs of test holes, Central Sevier Valley, Sanpete, Sevier, and Piute Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3039,"text":"wsp1787 - 1965 - Ground-water conditions and storage in the Central Sevier Valley, Utah","indexId":"wsp1787","publicationYear":"1965","noYear":false,"title":"Ground-water conditions and storage in the Central Sevier Valley, Utah"},"id":3}],"lastModifiedDate":"2017-09-06T16:06:56","indexId":"wsp1787","displayToPublicDate":"1994-01-01T00:00:00","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":"1787","title":"Ground-water conditions and storage in the Central Sevier Valley, Utah","docAbstract":"The central Sevier Valley, in the central part of Utah, extends from the town of Kingston to the Yuba Dam and from the Tushar and Valley Mountains and the Pavant Range to the Sevier, Fishlake, Wasatch, and Gunnison Plateaus. A geologic and hydrologic investigation of the valley was made to determine the relation between surface water and ground water and to determine if ground water can be used for irrigation supplies without affecting existing water uses. During the investigation, data were collected for about 700 wells and 26 springs. Monthly water-level measurements were made at 93 observation wells, and automatic recording gages were maintained at 6 additional wells. Chemical analyses were made of water collected from 68 wells and springs. Test holes were drilled at 21 sites to determine the thickness and hydrologic properties of the waterbearing materials. Consumption of ground water by vegetation was estimated on the basis of area and applied rates of evapotranspiration.
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1965 - Index of surface-water records to December 31, 1963--Part 14, Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir514","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"514","title":"Index of surface-water records to December 31, 1963--Part 14, Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir514","usgsCitation":"Eisenhuth, H., 1965, Index of surface-water records to December 31, 1963--Part 14, Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Circular 514, 28 p. :ill. ;26 cm., https://doi.org/10.3133/cir514.","productDescription":"28 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":120866,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0514/report-thumb.jpg"},{"id":31071,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0514/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f314a","contributors":{"authors":[{"text":"Eisenhuth, H.P.","contributorId":38140,"corporation":false,"usgs":true,"family":"Eisenhuth","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":147951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15688,"text":"ofr65138 - 1965 - The validity of geologic projection, a successful example: the Straight Creek Tunnel pilot bore, Colorado","interactions":[{"subject":{"id":15688,"text":"ofr65138 - 1965 - The validity of geologic projection, a successful example: the Straight Creek Tunnel pilot bore, Colorado","indexId":"ofr65138","publicationYear":"1965","noYear":false,"title":"The validity of geologic projection, a successful example: the Straight Creek Tunnel pilot bore, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":25017,"text":"pp815 - 1974 - Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado","indexId":"pp815","publicationYear":"1974","noYear":false,"title":"Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado"},"id":1}],"supersededBy":{"id":25017,"text":"pp815 - 1974 - Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado","indexId":"pp815","publicationYear":"1974","noYear":false,"title":"Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado"},"lastModifiedDate":"2018-09-10T09:59:50","indexId":"ofr65138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-138","title":"The validity of geologic projection, a successful example: the Straight Creek Tunnel pilot bore, Colorado","docAbstract":"Projection of details of surface geology to depth prior to construction has met with only limited success in many tunneling operations. in the Straight Creek Tunnel pilot bore good results were obtained by making predictions of the extent and kinds but not the exact locations of conditions that could be expected at tunnel level based on a statistical study of surface features.
Successful predictions were made regarding percentages of rock types, linear feet of faulted and sheared rocks, and attitudes of foliation and fractures, including faults and joints. Predicted rock loads and final swell pressures in gouge and altered rocks agreed well with actual measurements. Ground water flows were encountered in expected amounts, but criteria for estimations proved to be unsound.
Estimates were made of the amount of temporary support, footage of exploratory feeler holes, and amounts of grouting and provided a sound basis for estimating total tunneling coats.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65138","usgsCitation":"Robinson, C., and Lee, F.T., 1965, The validity of geologic projection, a successful example: the Straight Creek Tunnel pilot bore, Colorado: U.S. Geological Survey Open-File Report 65-138, Report: 65 p.; 14 Appendices; 1 Table, https://doi.org/10.3133/ofr65138.","productDescription":"Report: 65 p.; 14 Appendices; 1 Table","costCenters":[],"links":[{"id":357184,"rank":17,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1965/0138/table-1.pdf","text":"Table 1","linkFileType":{"id":1,"text":"pdf"}},{"id":357183,"rank":16,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-10.pdf","text":"Appendix 10","linkFileType":{"id":1,"text":"pdf"}},{"id":357175,"rank":8,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-5a.pdf","text":"Appendix 5a","linkFileType":{"id":1,"text":"pdf"}},{"id":357176,"rank":9,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-5b.pdf","text":"Appendix 5b","linkFileType":{"id":1,"text":"pdf"}},{"id":357177,"rank":10,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-5c.pdf","text":"Appendix 5c","linkFileType":{"id":1,"text":"pdf"}},{"id":357173,"rank":6,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-3.pdf","text":"Appendix 3","linkFileType":{"id":1,"text":"pdf"}},{"id":357178,"rank":11,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-6a.pdf","text":"Appendix 6a","linkFileType":{"id":1,"text":"pdf"}},{"id":357179,"rank":12,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-6b.pdf","text":"Appendix 6b","linkFileType":{"id":1,"text":"pdf"}},{"id":147899,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0138/report-thumb.jpg"},{"id":357169,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0138/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":357170,"rank":3,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-1.pdf","text":"Appendix 1","linkFileType":{"id":1,"text":"pdf"}},{"id":357171,"rank":4,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-2a.pdf","text":"Appendix 2a","linkFileType":{"id":1,"text":"pdf"}},{"id":357174,"rank":7,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-4.pdf","text":"Appendix 4","linkFileType":{"id":1,"text":"pdf"}},{"id":357172,"rank":5,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-2b.pdf","text":"Appendix 2b","linkFileType":{"id":1,"text":"pdf"}},{"id":357180,"rank":13,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-7.pdf","text":"Appendix 7","linkFileType":{"id":1,"text":"pdf"}},{"id":357181,"rank":14,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-8.pdf","text":"Appendix 8","linkFileType":{"id":1,"text":"pdf"}},{"id":357182,"rank":15,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/1965/0138/appendix-9.pdf","text":"Appendix 9","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Straight Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.97824096679688,\n 39.64482503525421\n ],\n [\n -105.84365844726562,\n 39.64482503525421\n ],\n [\n -105.84365844726562,\n 39.7240885773337\n ],\n [\n -105.97824096679688,\n 39.7240885773337\n ],\n [\n -105.97824096679688,\n 39.64482503525421\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f14d","contributors":{"authors":[{"text":"Robinson, Charles Sherwood 0000-0002-7623-2380","orcid":"https://orcid.org/0000-0002-7623-2380","contributorId":71163,"corporation":false,"usgs":true,"family":"Robinson","given":"Charles Sherwood","affiliations":[],"preferred":false,"id":171554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Fitzhugh T.","contributorId":82272,"corporation":false,"usgs":true,"family":"Lee","given":"Fitzhugh","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":171555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14973,"text":"ofr65180 - 1965 - Hot brines and recent iron deposits in deeps of the Red Sea","interactions":[],"lastModifiedDate":"2018-06-22T11:00:45","indexId":"ofr65180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-180","title":"Hot brines and recent iron deposits in deeps of the Red Sea","docAbstract":"Sedimentary iron and heavy-metal deposits of undetermined size have been found in the middle of the Red Sea some 2000 meters below the surface of the sea. This discovery has been made from the Research Vessel Atlantis II, which is still at sea engaged in a series of oceanographic investigations which ultimately will end in November 1965, after the ship has circumnavigated the globe. The discovery is significant because the environment and the processes controlling deposition of heavy metals are observable and appear to be still active.
The environment of the deposits can be breiefly described as an isolated sub-marine pool of brine having a pH as low as 5.3, a temperature of 56° c. and a salt content of about 310 grams per liter (at 20° c). Shipboard oxygen determinations and the indicated presence of H2S, divalent iron and divalent manganese in the water suggest that the environment is anaerobic. This hot, dense brine is trapped in a local depression of the Red Sea median valley. (Atlantis II Deep). The iron deposits, consisting largely of hydrous iron oxides, are found in the same depression. Brines from the Discovery Deep (21° 17 1 N, 38° 02'E) (1), a few miles southwest of the Atlantis II Deep (21°21 1 N, 38 ° 04'E), have a pH of 6.2 and a temperature of 44.7° c, and are also associated with iron-bearing sedirnents. The Discovery and Atlantis II brine pools both extend about 150 meters above the bottom. A few miles south of the: Discovery Deep another depression of greater depth has been reported (2) containing essentially normal Red Sea water. Deeps several hundred miles to the north (Sta. 540) and south (Sta. 545) were investigated and contained no brine. One of these (Sta. 545) is known to contain normal sediments.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr65180","usgsCitation":"Miller, A., Densmore, C., Degens, E., Hathaway, J., Manheim, F., McFarlin, P., Pocklington, R., and Jokela, A., 1965, Hot brines and recent iron deposits in deeps of the Red Sea: U.S. Geological Survey Open-File Report 65-180, 19 p., https://doi.org/10.3133/ofr65180.","productDescription":"19 p.","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":148138,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":355188,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0180/ofr1965180.pdf","text":"Report","size":"2.65 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1965-180"}],"geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 32.3876953125,\n 29.53522956294847\n ],\n [\n 34.8486328125,\n 24.5271348225978\n ],\n [\n 37.4853515625,\n 19.31114335506464\n ],\n [\n 39.7265625,\n 15.326571801420842\n ],\n [\n 43.3740234375,\n 12.683214911818666\n ],\n [\n 43.59375,\n 12.811801316582619\n ],\n [\n 42.6708984375,\n 16.594081412718474\n ],\n [\n 40.693359375,\n 19.518375478601566\n ],\n [\n 38.7158203125,\n 21.3303150734318\n ],\n [\n 38.7158203125,\n 23.443088931121785\n ],\n [\n 37.3095703125,\n 24.647017162630366\n ],\n [\n 36.6943359375,\n 26.03704188651584\n ],\n [\n 35.4638671875,\n 28.110748760633534\n ],\n [\n 34.1015625,\n 27.994401411046148\n ],\n [\n 33.22265625,\n 28.729130483430154\n ],\n [\n 32.51953125,\n 29.80251790576445\n ],\n [\n 32.3876953125,\n 29.53522956294847\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Coastal and Marine Geology Program
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384 Woods Hole Road
Woods Hole, MA 02543