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,{"id":34062,"text":"b1395A - 1975 - Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1973","interactions":[],"lastModifiedDate":"2025-04-07T20:06:33.775404","indexId":"b1395A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1395","chapter":"A","title":"Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1973","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1395A","usgsCitation":"Cohee, G.V., and Wright, W., 1975, Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1973: U.S. Geological Survey Bulletin 1395, iii, 68 p., https://doi.org/10.3133/b1395A.","productDescription":"iii, 68 p.","costCenters":[],"links":[{"id":484281,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92678.htm","text":"Proposal of the name, Orangeburg Group, for outcropping beds of Eocene age in Orangeburg County and vicinity, South Carolina","linkFileType":{"id":5,"text":"html"}},{"id":484280,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92677.htm","text":"New and revised stratigraphic names in the western Sacramento Valley, California","linkFileType":{"id":5,"text":"html"}},{"id":484279,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92672.htm","text":"Abandonment of the term Beattyville Shale Member (of the Lee Formation)","linkFileType":{"id":5,"text":"html"}},{"id":96247,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1395a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402538,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92669.htm","text":"Beulah Limestone and Hardscrabble Limestone (Mississippian) of Colorado abandoned","linkFileType":{"id":5,"text":"html"}},{"id":167125,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1395a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6ae2","contributors":{"authors":[{"text":"Cohee, George Vincent","contributorId":98295,"corporation":false,"usgs":true,"family":"Cohee","given":"George","email":"","middleInitial":"Vincent","affiliations":[],"preferred":false,"id":212396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, W.B.","contributorId":101296,"corporation":false,"usgs":true,"family":"Wright","given":"W.B.","affiliations":[],"preferred":false,"id":212397,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34063,"text":"b1405A - 1975 - Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1974","interactions":[],"lastModifiedDate":"2025-04-07T20:11:21.015186","indexId":"b1405A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1405","chapter":"A","title":"Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1974","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1405A","usgsCitation":"Cohee, G.V., and Wright, W., 1975, Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1974: U.S. Geological Survey Bulletin 1405, iii, 36 p., https://doi.org/10.3133/b1405A.","productDescription":"iii, 36 p.","costCenters":[],"links":[{"id":484285,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92679.htm","text":"The Science Hill Sandstone Member of the Warsaw Formation, south-central Kentucky","linkFileType":{"id":5,"text":"html"}},{"id":484284,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92676.htm","text":"Early Miocene age of the Clallam Formation, western Washington","linkFileType":{"id":5,"text":"html"}},{"id":484283,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92674.htm","text":"The Italian Mountain Intrusive Complex, west-central Colorado","linkFileType":{"id":5,"text":"html"}},{"id":61978,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1405a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402547,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92670.htm","text":"The Point Pleasant Tongue of the Clays Ferry Formation, northern Kentucky","linkFileType":{"id":5,"text":"html"}},{"id":167761,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1405a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6ae5","contributors":{"authors":[{"text":"Cohee, George Vincent","contributorId":98295,"corporation":false,"usgs":true,"family":"Cohee","given":"George","email":"","middleInitial":"Vincent","affiliations":[],"preferred":false,"id":212398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, W.B.","contributorId":101296,"corporation":false,"usgs":true,"family":"Wright","given":"W.B.","affiliations":[],"preferred":false,"id":212399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44126,"text":"ofr75223 - 1975 - Ozarks land use data set; Tulsa, Okla., Ark., Mo., Kans.","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"ofr75223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-223","title":"Ozarks land use data set; Tulsa, Okla., Ark., Mo., Kans.","language":"ENGLISH","doi":"10.3133/ofr75223","issn":"ma","usgsCitation":"Loelkes, G.L., Hardin, I., Napier, E., Chambers, M., Jessen, E., and Johnson, R., 1975, Ozarks land use data set; Tulsa, Okla., Ark., Mo., Kans.: U.S. Geological Survey Open-File Report 75-223, 5 maps :acetate ;46 x 76 cm., on sheets 77 x 102 cm., https://doi.org/10.3133/ofr75223.","productDescription":"5 maps :acetate ;46 x 76 cm., on sheets 77 x 102 cm.","costCenters":[],"links":[{"id":162430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689fe5","contributors":{"authors":[{"text":"Loelkes, G. L. (compiler)","contributorId":60593,"corporation":false,"usgs":true,"family":"Loelkes","given":"G.","suffix":"(compiler)","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hardin, I.L.","contributorId":57028,"corporation":false,"usgs":true,"family":"Hardin","given":"I.L.","email":"","affiliations":[],"preferred":false,"id":229195,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Napier, E.C.","contributorId":59770,"corporation":false,"usgs":true,"family":"Napier","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":229196,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chambers, M.J.","contributorId":93009,"corporation":false,"usgs":true,"family":"Chambers","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":229199,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jessen, Eldon","contributorId":59771,"corporation":false,"usgs":true,"family":"Jessen","given":"Eldon","email":"","affiliations":[],"preferred":false,"id":229197,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Johnson, R.A.","contributorId":93864,"corporation":false,"usgs":true,"family":"Johnson","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":229200,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":44123,"text":"ofr75106 - 1975 - Velocity sections in Raft River, Idaho, geothermal area from seismic refraction","interactions":[],"lastModifiedDate":"2022-12-29T21:26:45.955185","indexId":"ofr75106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-106","title":"Velocity sections in Raft River, Idaho, geothermal area from seismic refraction","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75106","usgsCitation":"Ackermann, H.D., 1975, Velocity sections in Raft River, Idaho, geothermal area from seismic refraction: U.S. Geological Survey Open-File Report 75-106, 2 p., https://doi.org/10.3133/ofr75106.","productDescription":"2 p.","costCenters":[],"links":[{"id":411196,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15093.htm","linkFileType":{"id":5,"text":"html"}},{"id":81504,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0106/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162427,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0106/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Raft River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113.285,\n              42.17\n            ],\n            [\n              -113.491,\n              42.17\n            ],\n            [\n              -113.491,\n              42.052\n            ],\n            [\n              -113.285,\n              42.052\n            ],\n            [\n              -113.285,\n              42.17\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db60229d","contributors":{"authors":[{"text":"Ackermann, Hans D.","contributorId":44539,"corporation":false,"usgs":false,"family":"Ackermann","given":"Hans","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":229191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1046,"text":"wsp2039A - 1975 - Chemical quality and temperature of water in Flaming Gorge Reservoir, Wyoming and Utah, and the effect of the reservoir on the Green River","interactions":[],"lastModifiedDate":"2017-09-03T14:21:30","indexId":"wsp2039A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"2039","chapter":"A","title":"Chemical quality and temperature of water in Flaming Gorge Reservoir, Wyoming and Utah, and the effect of the reservoir on the Green River","docAbstract":"<p>The major tributaries to Flaming Gorge Reservoir contribute an average of about 97 percent of the total streamflow and 82 percent of the total load of dissolved solids. The Green River is the largest tributary, and for the 1957-72 water years it contributed 81 percent of the total streamflow and 70 percent of the total load of dissolved solids. The principal constituents in the tributary streamflow are calcium and sulfate during periods of lowest flow and calcium and bicarbonate during periods of highest flow.</p><p>Flaming Gorge Dam was closed in November 1962, and the most significant load changes of chemical constituents due to the net effect of inflow, outflow, leaching, and chemical precipitation in the reservoir have been load changes of sulfate and bicarbonate. The average increase of dissolved load of sulfate in the reservoir for the 1969-72 water years was 110,000 tons (99,790 t) per year, which was 40,000 tons (36,287 t) per year less than for the 1963-66 water years. The average decrease of dissolved load of bicarbonate in the reservoir for 1969-72 was 40,000 tons (36,287 t) per year, which was the same as the decrease for 1963-66.</p><p>Anaerobic conditions were observed in the deep, uncirculated part of the reservoir near the dam during the 1971 and 1972 water years, and anaerobic or near-anaerobic conditions were observed near the confluence of the Blacks Fork and Green River during the summers of 1971 and 1972.</p><p>The water in Flaming Gorge Reservoir is in three distinct layers, and the upper two layers (the epilimnion and the metalimnion) mixed twice during each of the 1971-72 water years. The two circulation periods were in the spring and fall. The water in the deepest layer (the hypolimnion) did not mix with the waters of the upper zones because the density difference was too great and because the deep, narrow shape of the basin probably inhibits mixing.</p><p>The depletion of flow in the Green River downstream from Flaming Gorge Dam between closure of the dam and the end of the 1972 water year was 4,500,000 acre-feet (5,550.8 hm<sup>3</sup>). Of this total, water stored in the reservoir accounted for 3,500,000 acre-feet (4,317.2 hm<sup>3</sup>), evaporation consumed 700,000 acre-feet (863.4 hm<sup>3</sup>), and 300,000 acre-feet (370.0 hm<sup>3</sup>) went into bank storage.</p><p>The net load of dissolved solids added to the river system during the 1963-72 water years, due to leaching and chemical precipitation, was 1,730,000 tons (1,569,421 t). The leaching rate was 200,000 tons (181,436 t) per year for 1963-68,115,000 tons (104,326 t) per year for 1969-70 and 150,000 tons (136,077 t) per year for 1971-72. It appears that the leaching rates should decrease in the future since the reservoir level in 1972 was near maximum pool level.</p><p>The most significant increase in concentration of the chemical constituents in the water below the reservoir involved the sulfate ion, which increased from about 115 milligrams per litre (42 percent of the anions) in 1957 to about 200 milligrams per litre (54 percent), in 1972. But the highest concentration, about 290 milligrams per litre (58 percent), occurred in 1963, immediately after closure of the dam.</p><p>Prior to closure of the dam, the average monthly temperature of the Green River below the damsite ranged from 0<span class=\"_Tgc\">°</span>C to 19.5<span class=\"_Tgc\">°</span>C as compared to 3.5<span class=\"_Tgc\">°</span>C to 10.0<span class=\"_Tgc\">°</span>C after closure.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2039A","usgsCitation":"Bolke, E., and Waddell, K.M., 1975, Chemical quality and temperature of water in Flaming Gorge Reservoir, Wyoming and Utah, and the effect of the reservoir on the Green River: U.S. Geological Survey Water Supply Paper 2039, Report: iv, 26 p.; 1 Plate: 42.70 in. x 24.66 in., https://doi.org/10.3133/wsp2039A.","productDescription":"Report: iv, 26 p.; 1 Plate: 42.70 in. x 24.66 in.","numberOfPages":"31","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":137909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2039a/report-thumb.jpg"},{"id":25710,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2039a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":246958,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2039a/plate-1.pdf","size":"5519","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Flaming Gorge Dam","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486ce4b07f02db50b473","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":143087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, Kidd M.","contributorId":20720,"corporation":false,"usgs":true,"family":"Waddell","given":"Kidd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":143086,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62599,"text":"gq1294 - 1975 - Geologic map of the Avon SE quadrangle, Iron County, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:48","indexId":"gq1294","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1294","title":"Geologic map of the Avon SE quadrangle, Iron County, Utah","language":"ENGLISH","doi":"10.3133/gq1294","usgsCitation":"Mackin, J.H., and Rowley, P.D., 1975, Geologic map of the Avon SE quadrangle, Iron County, Utah: U.S. Geological Survey Geologic Quadrangle 1294, 1 map., https://doi.org/10.3133/gq1294.","productDescription":"1 map.","costCenters":[],"links":[{"id":107721,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10829.htm","linkFileType":{"id":5,"text":"html"},"description":"10829"},{"id":248759,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1294/report.pdf","size":"67","linkFileType":{"id":1,"text":"pdf"}},{"id":254069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1294/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.36749999999999,37.75 ], [ -113.36749999999999,37.8675 ], [ -113.25,37.8675 ], [ -113.25,37.75 ], [ -113.36749999999999,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0fe4b07f02db6a0736","contributors":{"authors":[{"text":"Mackin, J. Hoover","contributorId":18388,"corporation":false,"usgs":true,"family":"Mackin","given":"J.","email":"","middleInitial":"Hoover","affiliations":[],"preferred":false,"id":267597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowley, Peter D.","contributorId":27435,"corporation":false,"usgs":true,"family":"Rowley","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":267598,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":16237,"text":"ofr75593 - 1975 - Petrochemistry of skarn in the Copper Canyon porphyry copper deposits, Lander County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:05","indexId":"ofr75593","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-593","title":"Petrochemistry of skarn in the Copper Canyon porphyry copper deposits, Lander County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr75593","usgsCitation":"Theodore, T., and Blake, D.W., 1975, Petrochemistry of skarn in the Copper Canyon porphyry copper deposits, Lander County, Nevada: U.S. Geological Survey Open-File Report 75-593, 14 leaves :ill., maps ;27 cm., https://doi.org/10.3133/ofr75593.","productDescription":"14 leaves :ill., maps ;27 cm.","costCenters":[],"links":[{"id":148898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881e7","contributors":{"authors":[{"text":"Theodore, Ted G.","contributorId":57840,"corporation":false,"usgs":true,"family":"Theodore","given":"Ted G.","affiliations":[],"preferred":false,"id":172470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blake, David W.","contributorId":49229,"corporation":false,"usgs":true,"family":"Blake","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":172469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":36339,"text":"b1313E - 1975 - Automatic interpretation of Schlumberger sounding curves, using modified Dar Zarrouk functions","interactions":[],"lastModifiedDate":"2012-02-02T00:09:41","indexId":"b1313E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1313","chapter":"E","title":"Automatic interpretation of Schlumberger sounding curves, using modified Dar Zarrouk functions","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1313E","usgsCitation":"Zohdy, A.A., 1975, Automatic interpretation of Schlumberger sounding curves, using modified Dar Zarrouk functions: U.S. Geological Survey Bulletin 1313, 39 p. ;24 cm., https://doi.org/10.3133/b1313E.","productDescription":"39 p. ;24 cm.","costCenters":[],"links":[{"id":166951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1313e/report-thumb.jpg"},{"id":64286,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1313e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668098","contributors":{"authors":[{"text":"Zohdy, Adel A. R.","contributorId":61799,"corporation":false,"usgs":true,"family":"Zohdy","given":"Adel","email":"","middleInitial":"A. R.","affiliations":[],"preferred":false,"id":216161,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35403,"text":"b1395I - 1975 - Marine trace fossils in the Upper Jurassic Bluff Sandstone, southeastern Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:09:47","indexId":"b1395I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1395","chapter":"I","title":"Marine trace fossils in the Upper Jurassic Bluff Sandstone, southeastern Utah","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1395I","usgsCitation":"O'Sullivan, R., and Maberry, J.O., 1975, Marine trace fossils in the Upper Jurassic Bluff Sandstone, southeastern Utah: U.S. Geological Survey Bulletin 1395, iii, p. I1-I12, ill. ;24 cm., https://doi.org/10.3133/b1395I.","productDescription":"iii, p. I1-I12, ill. ;24 cm.","costCenters":[],"links":[{"id":96909,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1395i/report.pdf","size":"2290","linkFileType":{"id":1,"text":"pdf"}},{"id":164947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1395i/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eb8e","contributors":{"authors":[{"text":"O'Sullivan, Robert Brett","contributorId":26695,"corporation":false,"usgs":true,"family":"O'Sullivan","given":"Robert Brett","affiliations":[],"preferred":false,"id":214572,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maberry, John O.","contributorId":87134,"corporation":false,"usgs":true,"family":"Maberry","given":"John","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":214573,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61259,"text":"mf677 - 1975 - Photointerpretive map of landslides and surficial deposits of northernmost Napa County, California","interactions":[],"lastModifiedDate":"2018-12-18T13:26:10","indexId":"mf677","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"677","title":"Photointerpretive map of landslides and surficial deposits of northernmost Napa County, California","docAbstract":"<p>This map shows various types of landslide deposits, scarps, and related topographic features, in addition to other types of surficial deposits, in northernmost Napa County, California.&nbsp; It was prepared by viewing overlapping vertical aerial photographs with a stereoscope.&nbsp; This method allows the geologist to see a three-dimensional model of the terrain to be analyzed and thereby permits him to map the distribution and infer the nature and origin of various landforms.&nbsp; Interpretations were checked by low altitude air reconnaissance in January 1975, but the deposits and features shown on this map have not been checked on the ground.&nbsp; They do, however, represent a consensus of judgment by both authors.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf677","usgsCitation":"Wright, R.H., and Reid, G., 1975, Photointerpretive map of landslides and surficial deposits of northernmost Napa County, California: U.S. Geological Survey Miscellaneous Field Studies Map 677, 37.41 x 29.59 inches, https://doi.org/10.3133/mf677.","productDescription":"37.41 x 29.59 inches","costCenters":[],"links":[{"id":360470,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0677/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":187182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0677/report-thumb.jpg"}],"country":"United States","state":"California","county":"Napa County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.41666666666667,38.75 ], [ -122.41666666666667,38.8675 ], [ -122.25,38.8675 ], [ -122.25,38.75 ], [ -122.41666666666667,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685dc5","contributors":{"authors":[{"text":"Wright, Robert H.","contributorId":69180,"corporation":false,"usgs":true,"family":"Wright","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":265274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reid, G.O.","contributorId":6530,"corporation":false,"usgs":true,"family":"Reid","given":"G.O.","email":"","affiliations":[],"preferred":false,"id":265273,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3125,"text":"wsp2171 - 1975 - Ground-water levels in the United States, 1969-73, Southeastern states","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"wsp2171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"2171","title":"Ground-water levels in the United States, 1969-73, Southeastern states","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2171","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Ground-water levels in the United States, 1969-73, Southeastern states: U.S. Geological Survey Water Supply Paper 2171, 250 p. :illus., https://doi.org/10.3133/wsp2171.","productDescription":"250 p. :illus.","costCenters":[],"links":[{"id":94729,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2171/report.pdf","size":"18147","linkFileType":{"id":1,"text":"pdf"}},{"id":139458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2171/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667536","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":528101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25965,"text":"wri7514 - 1975 - Water-quality assessment of the Indiana Dunes National Lakeshore, 1973-74","interactions":[],"lastModifiedDate":"2018-11-19T12:18:53","indexId":"wri7514","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"75-14","title":"Water-quality assessment of the Indiana Dunes National Lakeshore, 1973-74","docAbstract":"<p>The Indiana Dunes National Lakeshore is underlain by unconsolidated lake and glacial deposits which have been divided into three units. Unit 1 is comprised mostly of sand and, in the western part of the National Lakeshore, is capable of yielding more than 500 gallons per minute (32 litres per second) to properly constructed wells. Unit 2, a silt till below unit 1, has little potential as a source of water for public supplies within the National Lakeshore area. Unit 4, a clay till under unit 2, is capable of yielding from 10 to 65 gallons per minute (0.6 to 4 litres per second) throughout the National Lakeshore.</p><p>Precipitation samples collected at the National Lakeshore had average inorganic ion concentrations ranging from 0 to 7.0 milligrams per litre. Streams in the National Lakeshore generally had a specific conductance ranging from 300 to 600 micromhos, a pH ranging from 6.5 to 8.1, and a dissolved oxygen concentration near saturation (7.7 to 12.9 milligrams per litre). The hogs and marshlands generally contained water with a specific conductance ranging from 40 to 150 micromhos, a pH ranging from 5.0 to 6.5, and dissolved oxygen ranging from 0.2 to 4.0 milligrams per litre. Most surface waters tended to have calcium and bicarbonate as the dominant ion pair. Exceptions include some inter-dunal ponds and certain watercourses and areas of Pinhook Bog. Ground-water chemical quality varied with depth and location but not with time during a 6-month interval. Ground water was usually a calcium magnesium bicarbonate type and moderately to very hard (71 to 390 milligrams per litre).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7514","usgsCitation":"Arihood, L.D., 1975, Water-quality assessment of the Indiana Dunes National Lakeshore, 1973-74: U.S. Geological Survey Water-Resources Investigations Report 75-14, iv, 56 p., https://doi.org/10.3133/wri7514.","productDescription":"iv, 56 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":359561,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0014/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1975/0014/report-thumb.jpg"}],"country":"United States","state":"Indiana","otherGeospatial":"Indiana Dunes National 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,{"id":56454,"text":"wdrAL741 - 1975 - Water resources data for Alabama, water year 1974; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:17","indexId":"wdrAL741","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AL-74-1","title":"Water resources data for Alabama, water year 1974; Part 1, Surface water records","language":"ENGLISH","doi":"10.3133/wdrAL741","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources data for Alabama, water year 1974; Part 1, Surface water records: U.S. Geological Survey Water Data Report AL-74-1, 163 p., https://doi.org/10.3133/wdrAL741.","productDescription":"163 p.","costCenters":[],"links":[{"id":185120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f78fa","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":532635,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14958,"text":"ofr75312 - 1975 - Availability of ground water in Marion County, Indiana","interactions":[],"lastModifiedDate":"2021-12-30T18:42:52.900204","indexId":"ofr75312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","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":"75-312","title":"Availability of ground water in Marion County, Indiana","docAbstract":"<p>County constitute the most extensive aquifers in the county. Four areally distinct sand and gravel aquifers were mapped in the drift during the course of this study. The aquifer of greatest economic importance consists of sand and gravel deposits of glacial-outwash origin which coincide with the courses of the White River and Fall Creek. Ground water in this aquifer is generally unconfined. Three thin, areally discontinuous, sheetlike deposits of sand and gravel situated one above the other occur in the till-plain area of the county. These deposits coalesce in some areas, but generally are separated by beds of silt and clay of varying thickness which cause the ground water in the till-plain aquifers to be semiconfined.</p>\n<p>The uppermost 100 feet (30 metres) or so of limestone and (or) dolomite underlying the glacial drift constitutes an aquifer of secondary importance in the county. This aquifer is separated from the unconsolidated aquifers either by silt and clay or by shale.</p>\n<p>The present movement of ground water through these aquifers is generally toward the White River, Fall Creek, Eagle Creek or Buck Creek. Based on seepage data, water levels in the aquifers in April and May 1974, and subsequent electric-analog-model analysis, discharge of ground water by seepage into the streams in the glacial outwash averages about 42 cubic feet per day per foot (3.9 cubic metres per day per metre) of channel length.</p>\n<p>A four-layer electric-analog model incorporating the geometry and hydraulic characteristics of the aquifers, the confining beds and the stream- aquifer connection was constructed to determine the feasibility and hydrologic results of proposed plans for future ground-water development.</p>\n<p>Three large well fields were simulated in the model of the glacial-outwash aquifer, with pumping nodes situated so as to take advantage both of high transmissivity areas in the aquifer, and of recharge from the streams.</p>\n<p>A series of model experiments were carried out to test the capacity of the aquifers to sustain increases in pumpage. In all of these, a new equilibrium was established within 6 years of simulated pumpage. In two of these experiments, water levels in the discharging wells were allowed to draw down to approximately half of the saturated thickness of the glacial-outwash aquifer. At this drawdown limit, the total discharge of wells in the system was found to be 59 million gallons per day (2.6 cubic second) assuming that the streams were fully connected to the upper third of the glacial-outwash aquifer. In two other experiments, discharging wells were allowed to drawdown an average of two-thirds of the saturated thickness of the glacial-outwash aquifer. At this limit, the total discharge was found to be 72 million gallons per day (3.2 cubic metres per second) using the conservative stream-aquifer connection, and 103 million gallons per day (4.5 cubic metres per second) assuming a full connection. Some dewatering of the aquifer was associated with the 72 million gallons per day (3.2 cubic metres per second) discharge. In all experiments, the amount that could be pumped from the confined aquifers without disturbing existing domestic wells was found to be small.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr75312","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources, Division of Water","usgsCitation":"Meyer, W.R., Reussow, J.P., Gillies, D.C., and Shampine, W., 1975, Availability of ground water in Marion County, Indiana: U.S. Geological Survey Open-File Report 75-312, viii, 87 p., https://doi.org/10.3133/ofr75312.","productDescription":"viii, 87 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":145968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0312/report-thumb.jpg"},{"id":391894,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15147.htm"},{"id":393663,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0312/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Marion County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.9369,39.9272],[-85.9379,39.87],[-85.9541,39.8696],[-85.9518,39.6969],[-85.9523,39.638],[-86.248,39.6335],[-86.3268,39.6318],[-86.3281,39.8526],[-86.328,39.8662],[-86.325,39.8662],[-86.3267,39.9238],[-86.2967,39.9246],[-86.2757,39.925],[-86.2385,39.9259],[-85.9801,39.9269],[-85.9411,39.9272],[-85.9369,39.9272]]]},\"properties\":{\"name\":\"Marion\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f8f","contributors":{"authors":[{"text":"Meyer, William R.","contributorId":73618,"corporation":false,"usgs":true,"family":"Meyer","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":170320,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reussow, J. 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