{"pageNumber":"4537","pageRowStart":"113400","pageSize":"25","recordCount":184738,"records":[{"id":67192,"text":"i1994 - 1989 - Geologic map of the surficial deposits of the Jackass Flats Quadrangle, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:11:20","indexId":"i1994","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1994","subseriesTitle":"NONE","title":"Geologic map of the surficial deposits of the Jackass Flats Quadrangle, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/i1994","usgsCitation":"Swadley, W.C., and Hoover, D.L., 1989, Geologic map of the surficial deposits of the Jackass Flats Quadrangle, Nye County, Nevada: U.S. Geological Survey IMAP 1994, 1 map :col. ;58 x 46 cm., on sheet 73 x 81 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1994.","productDescription":"1 map :col. ;58 x 46 cm., on sheet 73 x 81 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107241,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10069.htm","linkFileType":{"id":5,"text":"html"},"description":"10069"},{"id":187506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.36749999999999,36.75 ], [ -116.36749999999999,36.8675 ], [ -116.25,36.8675 ], [ -116.25,36.75 ], [ -116.36749999999999,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688813","contributors":{"authors":[{"text":"Swadley, W. C.","contributorId":46940,"corporation":false,"usgs":true,"family":"Swadley","given":"W.","middleInitial":"C.","affiliations":[],"preferred":false,"id":275746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoover, D. L.","contributorId":70388,"corporation":false,"usgs":true,"family":"Hoover","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":275747,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19183,"text":"ofr88324 - 1989 - Suspended-sediment data in the upper Rio Grande De Loiza basin, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:30","indexId":"ofr88324","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-324","title":"Suspended-sediment data in the upper Rio Grande De Loiza basin, Puerto Rico","docAbstract":"Fluvial sediment, a widely recognized pollutant of surface water , is reducing the efficiency and useful life of almost all reservoirs in Puerto Rico. Sediment transported from the upper basin of the Rio Grande de Loiza is eventually deposited in the bottom of Lago Loiza, a water reservoir. Suspended sediment data were collected from 1983 to 1986 from a 208 sq mi area extending from the headwaters of Rio Grande de Loiza to the Lago Loiza. The drainage areas range from 0.82 sq mi to 89.8 sq mi. Results are based on three years of data from a network of five daily- record stations and five partial-record stations. A total of 2 ,114 sediment samples were collected and analyzed during the investigation. Instantaneous concentrations of suspended sediment varied from 0 to 56, 100 mg/L. Instantaneous suspended sediment loads ranged from 0 tons/day to 817,000 tons/day. A total of 152 suspended sediment samples were analyzed for particle size distribution. Suspended sediment in the streams is composed mostly of silt and clay. Sand content ranged from 6 to 80% during high flows. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr88324","usgsCitation":"Guzman-Rios, S., 1989, Suspended-sediment data in the upper Rio Grande De Loiza basin, Puerto Rico: U.S. Geological Survey Open-File Report 88-324, v, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr88324.","productDescription":"v, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0324/report-thumb.jpg"},{"id":48649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0324/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fbf","contributors":{"authors":[{"text":"Guzman-Rios, Senen sgguzman@usgs.gov","contributorId":2853,"corporation":false,"usgs":true,"family":"Guzman-Rios","given":"Senen","email":"sgguzman@usgs.gov","affiliations":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"preferred":true,"id":180459,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15408,"text":"ofr85166 - 1989 - Inventory of interbasin transfers of water in the western conterminous United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:58","indexId":"ofr85166","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"85-166","title":"Inventory of interbasin transfers of water in the western conterminous United States","docAbstract":"Information is presented on the quantity of water transferred from one river basin to another in the western conterminous United States. The information is needed by water system managers and planners to develop water budgets for major river basins, to examine the relative extent of existing interbasin transfers, and to define the importance of transferring water to meet regional water demands. All or parts of 11 major water resources regions and 111 complete subregions comprise the study area; water is exported from 39 of these subregions. The average quantity of water exported annually during 1973-82 was about 12 million acre-feet. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85166","usgsCitation":"Petsch, H., 1989, Inventory of interbasin transfers of water in the western conterminous United States: U.S. Geological Survey Open-File Report 85-166, iii, 45 p. :map ;28 cm., https://doi.org/10.3133/ofr85166.","productDescription":"iii, 45 p. :map ;28 cm.","costCenters":[],"links":[{"id":148000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0166/report-thumb.jpg"},{"id":44362,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0166/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44363,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0166/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4968e4b07f02db59eba4","contributors":{"authors":[{"text":"Petsch, H.E. Jr.","contributorId":46532,"corporation":false,"usgs":true,"family":"Petsch","given":"H.E.","suffix":"Jr.","affiliations":[],"preferred":false,"id":171087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19535,"text":"ofr89485 - 1989 - Alluvial stratigraphy of the Potomac River valley bottom near Petersburg and Moorefield, West Virginia","interactions":[],"lastModifiedDate":"2022-09-19T21:02:30.556795","indexId":"ofr89485","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-485","title":"Alluvial stratigraphy of the Potomac River valley bottom near Petersburg and Moorefield, West Virginia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr89485","usgsCitation":"Jacobson, R., Linton, R.C., and Rubin, M., 1989, Alluvial stratigraphy of the Potomac River valley bottom near Petersburg and Moorefield, West Virginia: U.S. Geological Survey Open-File Report 89-485, Report: 27 p.; 14 Plates: 17.64 × 11.76 inches or smaller, https://doi.org/10.3133/ofr89485.","productDescription":"Report: 27 p.; 14 Plates: 17.64 × 11.76 inches or smaller","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":407007,"rank":17,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18950.htm","linkFileType":{"id":5,"text":"html"}},{"id":49008,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49007,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49006,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48998,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48997,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48996,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49009,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0485/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49005,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49004,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49003,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49002,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49001,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49000,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48999,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48995,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0485/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0485/report-thumb.jpg"}],"country":"United States","state":"West Virginia","city":"Moorfield, Petersburg","otherGeospatial":"Potomac River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.5430,\n              38.7610\n            ],\n            [\n              -78.343,\n              38.7610\n            ],\n            [\n              -78.343,\n              39.1960\n            ],\n            [\n              -79.5430,\n              39.1960\n            ],\n            [\n              -79.5430,\n              38.7610\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687837","contributors":{"authors":[{"text":"Jacobson, R. 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,{"id":67194,"text":"i2018 - 1989 - Geologic map of the surficial deposits of the Topopah Spring Quadrangle, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:11:20","indexId":"i2018","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2018","subseriesTitle":"NONE","title":"Geologic map of the surficial deposits of the Topopah Spring Quadrangle, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/i2018","usgsCitation":"Swadley, W.C., and Hoover, D.L., 1989, Geologic map of the surficial deposits of the Topopah Spring Quadrangle, Nye County, Nevada: U.S. Geological Survey IMAP 2018, 1 map :col. ;58 x 46 cm., on sheet 71 x 81 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2018.","productDescription":"1 map :col. ;58 x 46 cm., on sheet 71 x 81 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107252,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10084.htm","linkFileType":{"id":5,"text":"html"},"description":"10084"},{"id":187508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.36749999999999,36.8675 ], [ -116.36749999999999,37 ], [ -116.25,37 ], [ -116.25,36.8675 ], [ -116.36749999999999,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6887f3","contributors":{"authors":[{"text":"Swadley, W. C.","contributorId":46940,"corporation":false,"usgs":true,"family":"Swadley","given":"W.","middleInitial":"C.","affiliations":[],"preferred":false,"id":275750,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoover, D. L.","contributorId":70388,"corporation":false,"usgs":true,"family":"Hoover","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":275751,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19525,"text":"ofr87380 - 1989 - Chemical quality of agricultural drainage water tributary to Kesterson Reservoir, Fresno and Merced counties, California, January and August 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:07:33","indexId":"ofr87380","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"87-380","title":"Chemical quality of agricultural drainage water tributary to Kesterson Reservoir, Fresno and Merced counties, California, January and August 1984","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports Section [distributor],","doi":"10.3133/ofr87380","usgsCitation":"Izbicki, J., 1989, Chemical quality of agricultural drainage water tributary to Kesterson Reservoir, Fresno and Merced counties, California, January and August 1984: U.S. Geological Survey Open-File Report 87-380, v, 45 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87380.","productDescription":"v, 45 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0380/report-thumb.jpg"},{"id":48983,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0380/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3b05","contributors":{"authors":[{"text":"Izbicki, John A. 0000-0003-0816-4408 jaizbick@usgs.gov","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":1375,"corporation":false,"usgs":true,"family":"Izbicki","given":"John A.","email":"jaizbick@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":181060,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31611,"text":"ofr89302 - 1989 - Analytical results and sample locality map of stream-sediment, heavy-mineral-concentrate, and rock samples from the Orejana Canyon (OR-1-78) Wilderness Study Area, Harney County, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:09:07","indexId":"ofr89302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-302","title":"Analytical results and sample locality map of stream-sediment, heavy-mineral-concentrate, and rock samples from the Orejana Canyon (OR-1-78) Wilderness Study Area, Harney County, Oregon","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr89302","usgsCitation":"Erickson, M.S., King, H.D., Tippitt, F.W., and Hageman, P., 1989, Analytical results and sample locality map of stream-sediment, heavy-mineral-concentrate, and rock samples from the Orejana Canyon (OR-1-78) Wilderness Study Area, Harney County, Oregon: U.S. Geological Survey Open-File Report 89-302, 14 p.  :map ;28 cm., https://doi.org/10.3133/ofr89302.","productDescription":"14 p.  :map ;28 cm.","costCenters":[],"links":[{"id":160809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0302/report-thumb.jpg"},{"id":59812,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0302/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0302/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e683","contributors":{"authors":[{"text":"Erickson, M. S.","contributorId":35302,"corporation":false,"usgs":true,"family":"Erickson","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":206537,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":206539,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tippitt, F. W.","contributorId":43782,"corporation":false,"usgs":true,"family":"Tippitt","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":206538,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hageman, P.  L. 0000-0002-3440-2150","orcid":"https://orcid.org/0000-0002-3440-2150","contributorId":27459,"corporation":false,"usgs":true,"family":"Hageman","given":"P.  L.","affiliations":[],"preferred":false,"id":206536,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":31612,"text":"ofr89326 - 1989 - Evolution of the Rodalquilar caldera complex and associated gold-alunite deposits, Cabo de Gata volcanic field, southeastern Spain","interactions":[],"lastModifiedDate":"2012-02-02T00:09:05","indexId":"ofr89326","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-326","title":"Evolution of the Rodalquilar caldera complex and associated gold-alunite deposits, Cabo de Gata volcanic field, southeastern Spain","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr89326","usgsCitation":"Rytuba, J.J., Arribas, A., Cunningham, C.G., McKee, E., Smith, J., and Arribas, A., 1989, Evolution of the Rodalquilar caldera complex and associated gold-alunite deposits, Cabo de Gata volcanic field, southeastern Spain: U.S. Geological Survey Open-File Report 89-326, 18 p.  ill. ;28 cm., https://doi.org/10.3133/ofr89326.","productDescription":"18 p.  ill. ;28 cm.","costCenters":[],"links":[{"id":160213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0326/report-thumb.jpg"},{"id":59814,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0326/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f96d4","contributors":{"authors":[{"text":"Rytuba, James J. jrytuba@usgs.gov","contributorId":3043,"corporation":false,"usgs":true,"family":"Rytuba","given":"James","email":"jrytuba@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":206540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arribas, Antonio Jr.","contributorId":14419,"corporation":false,"usgs":true,"family":"Arribas","given":"Antonio","suffix":"Jr.","affiliations":[],"preferred":false,"id":206541,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cunningham, C. G.","contributorId":76741,"corporation":false,"usgs":true,"family":"Cunningham","given":"C.","middleInitial":"G.","affiliations":[],"preferred":false,"id":206545,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McKee, E.H.","contributorId":20736,"corporation":false,"usgs":true,"family":"McKee","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":206542,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Smith, James G.","contributorId":44534,"corporation":false,"usgs":true,"family":"Smith","given":"James G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":206544,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Arribas, Antonio Sr.","contributorId":22781,"corporation":false,"usgs":true,"family":"Arribas","given":"Antonio","suffix":"Sr.","email":"","affiliations":[],"preferred":false,"id":206543,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":57300,"text":"wdrAZ881 - 1989 - Water resources data, Arizona, water year 1988","interactions":[],"lastModifiedDate":"2023-02-06T20:24:13.538639","indexId":"wdrAZ881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"AZ-88-1","title":"Water resources data, Arizona, water year 1988","docAbstract":"<p>Water resources data for the 1988 water year for Arizona consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; measurements of ground-water levels; and quality of water from selected wells. Also included are discharge data for crest-stage partial-record stations and water-quality data for partial-record stations. Locations of the gaging stations are shown in figures 4, 6, and 7, and of water-quality stations in figures 5 and 6. Additional water data were collected at various sites, which are not part of the systematic data-collection program, and are published as miscellaneous measurements or miscellaneous water-quality analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Arizona.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAZ881","collaboration":"Prepared in cooperation with the State of Arizona and with other agencies","usgsCitation":"Boner, F.C., Garrett, W.B., and Konieczki, A., 1989, Water resources data, Arizona, water year 1988: U.S. Geological Survey Water Data Report AZ-88-1, xi, 391 p., https://doi.org/10.3133/wdrAZ881.","productDescription":"xi, 391 p.","costCenters":[],"links":[{"id":412758,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1988/az-88-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181990,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1988/az-88-1/report-thumb.jpg"}],"country":"United 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,{"id":25934,"text":"wri894065 - 1989 - Stratigraphy of the unsaturated zone at the radioactive waste management complex, Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri894065","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4065","title":"Stratigraphy of the unsaturated zone at the radioactive waste management complex, Idaho National Engineering Laboratory, Idaho","docAbstract":"A complex sequence of layered basalt flows, cinders, and sediment underlies the Radioactive Waste Management Complex at the Idaho National Engineering Laboratory in southeastern Idaho. Wells drilled to 700 ft penetrate a sequence of 10 basalt-flow groups and 7 major sedimentary interbeds that range in age from about 100,000 to 600,000 years old. The 10 flow groups consist of 22 separate lava flows and flow-units. Each flow group is made up of from one to five petrographically similar flows that erupted from common source areas during periods of less than 200 years. Sedimentary interbeds consist of fluvial, lacustrine, and wind-blown deposits of clay, silt, sand, and gravel that accumulated during periods of volcanic inactivity ranging from thousands to hundreds of thousands of years. Flows and sediment are unsaturated to a depth of about 600 ft. Flows and sediment below a depth of 600 ft are saturated and make up the uppermost part of the Snake River Plain aquifer. The areal extent of flow groups and interbeds was determined from well cuttings, cores, geophysical logs, potassium-argon ages, and geomagnetic properties. Stratigraphical control was provided by four sequential basalt flows near the base of the unsaturated zone that have reversed geomagnetic polarity and high emission of natural gamma radiation compared to other flows. Natural gamma logs were used as a primary correlation tool. Natural-gamma emissions, which are generally uniform in related, petrographically similar flows, increase or decrease between petrographically dissimilar flows of different age and source. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCopies of this report can be purchased from Books and Open-File Reports Section,","doi":"10.3133/wri894065","usgsCitation":"Anderson, S.R., and Lewis, B.D., 1989, Stratigraphy of the unsaturated zone at the radioactive waste management complex, Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 89-4065, v, 54 p. :ill ;28 cm., https://doi.org/10.3133/wri894065.","productDescription":"v, 54 p. :ill ;28 cm.","costCenters":[],"links":[{"id":158056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4065/report-thumb.jpg"},{"id":54691,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5492","contributors":{"authors":[{"text":"Anderson, S. R.","contributorId":93518,"corporation":false,"usgs":true,"family":"Anderson","given":"S.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":195508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, B. D.","contributorId":85965,"corporation":false,"usgs":true,"family":"Lewis","given":"B.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":195507,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26186,"text":"wri894160 - 1989 - Sedimentation of Lake Taneycomo, Missouri, 1913-1987","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri894160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4160","title":"Sedimentation of Lake Taneycomo, Missouri, 1913-1987","docAbstract":"On the basis of the data from a sedimentation survey done by the U.S. Department of Agriculture, Soil Conservation Service, during 1935 and data collected by the U.S. Geological Survey during 1987, the volume of sediment accumulated in Lake Taneycomo from 1913 to 1935 and 1913 to 1987 was determined. Table Rock Dam, built directly upstream from Lake Taneycomo during 1958, eliminated about 92% of the 4,644-sq mi basin from contributing sediment directly to the lake. Cesium-137 isotope was used as a tracer in the sediment to determine the quantity of deposition in the lake after Table Rock Dam was completed. The relation between cross-sectional area and distance upstream from the dam (curve method) was used to determine the 1913 (original), the 1935, and the 1987 volumes of Lake Taneycomo. A total of 910,000,000 cu ft of sediment accumulated between 1913 and 1935, 42% of the original volume of the lake. A total of 1 ,066,000,000 cu ft of sediment accumulated between 1913 and 1987 , 49% of the original volume. Lake Taneycomo seems to be functioning as an alluvial river, responding to the new energy gradient established by the spillway at Ozark Beach Dam, and later to changes in the sediment load. The upper two-thirds of the lake seems to have been scoured after Table Rock Dam greatly decreased the sediment load to the lake. The cesium-137 analysis indicated that sediment is still accumulating in the lower reaches of the lake, with measured accumulation generally ranging from 0.2 to 2.6 ft. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-file report [distributor],","doi":"10.3133/wri894160","usgsCitation":"Berkas, W., 1989, Sedimentation of Lake Taneycomo, Missouri, 1913-1987: U.S. Geological Survey Water-Resources Investigations Report 89-4160, vii, 80 p. :ill. ;28 cm., https://doi.org/10.3133/wri894160.","productDescription":"vii, 80 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":157615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4160/report-thumb.jpg"},{"id":54984,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a1ee","contributors":{"authors":[{"text":"Berkas, W.R.","contributorId":59808,"corporation":false,"usgs":true,"family":"Berkas","given":"W.R.","affiliations":[],"preferred":false,"id":195956,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55702,"text":"wdrMO881 - 1989 - Water resources data, Missouri, water year 1988","interactions":[],"lastModifiedDate":"2019-11-22T14:18:47","indexId":"wdrMO881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"MO-88-1","title":"Water resources data, Missouri, water year 1988","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrMO881","usgsCitation":"Waite, L., Davis, J.V., Reed, H., Hatten, D., and Perkins, T., 1989, Water resources data, Missouri, water year 1988: U.S. Geological Survey Water Data Report MO-88-1, x, 290 p., https://doi.org/10.3133/wdrMO881.","productDescription":"x, 290 p.","costCenters":[],"links":[{"id":369476,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1988/mo-88-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1988/mo-88-1/report-thumb.jpg"}],"country":"United States","state":"Missouri","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.7568359375,\n              35.94243575255426\n            ],\n            [\n              -89.14306640625,\n              35.94243575255426\n            ],\n            [\n              -89.14306640625,\n              40.56389453066509\n            ],\n            [\n              -95.7568359375,\n              40.56389453066509\n            ],\n            [\n              -95.7568359375,\n              35.94243575255426\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f1119","contributors":{"authors":[{"text":"Waite, L.A.","contributorId":40995,"corporation":false,"usgs":true,"family":"Waite","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":254060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Jerri V. jdavis@usgs.gov","contributorId":99149,"corporation":false,"usgs":true,"family":"Davis","given":"Jerri","email":"jdavis@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":false,"id":254062,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, H.L.","contributorId":14886,"corporation":false,"usgs":true,"family":"Reed","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":254058,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hatten, D.O.","contributorId":29057,"corporation":false,"usgs":true,"family":"Hatten","given":"D.O.","email":"","affiliations":[],"preferred":false,"id":254059,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Perkins, T.J.","contributorId":76815,"corporation":false,"usgs":true,"family":"Perkins","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":254061,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":14982,"text":"ofr89553A - 1989 - A telemetry-based data-acquisition system; Part I, The remote data-acquisition transmitter","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr89553A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-553","chapter":"A","title":"A telemetry-based data-acquisition system; Part I, The remote data-acquisition transmitter","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89553A","usgsCitation":"Miller, G., 1989, A telemetry-based data-acquisition system; Part I, The remote data-acquisition transmitter: U.S. Geological Survey Open-File Report 89-553, ii, 172 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89553A.","productDescription":"ii, 172 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":148244,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0553a/report-thumb.jpg"},{"id":43792,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0553a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5b68","contributors":{"authors":[{"text":"Miller, G.K.","contributorId":43793,"corporation":false,"usgs":true,"family":"Miller","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":170364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14983,"text":"ofr89553B - 1989 - A telemetry-based data-acquisition system; Part 2, the data-acquisition reciever","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr89553B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-553","chapter":"B","title":"A telemetry-based data-acquisition system; Part 2, the data-acquisition reciever","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89553B","usgsCitation":"Miller, G., 1989, A telemetry-based data-acquisition system; Part 2, the data-acquisition reciever: U.S. Geological Survey Open-File Report 89-553, i, 90 leaves ;28 cm., https://doi.org/10.3133/ofr89553B.","productDescription":"i, 90 leaves ;28 cm.","costCenters":[],"links":[{"id":148245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0553b/report-thumb.jpg"},{"id":43793,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0553b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5b60","contributors":{"authors":[{"text":"Miller, G.K.","contributorId":43793,"corporation":false,"usgs":true,"family":"Miller","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":170365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26323,"text":"wri894094 - 1989 - Contrasts of vegetation, soils, microclimates, and geomorphic processes between north- and south-facing slopes on Green Mountain near Denver, Colorado","interactions":[],"lastModifiedDate":"2019-08-20T12:25:19","indexId":"wri894094","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4094","title":"Contrasts of vegetation, soils, microclimates, and geomorphic processes between north- and south-facing slopes on Green Mountain near Denver, Colorado","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri894094","usgsCitation":"Branson, F.A., and Shown, L.M., 1989, Contrasts of vegetation, soils, microclimates, and geomorphic processes between north- and south-facing slopes on Green Mountain near Denver, Colorado: U.S. Geological Survey Water-Resources Investigations Report 89-4094, v, 18 p. , https://doi.org/10.3133/wri894094.","productDescription":"v, 18 p. ","costCenters":[],"links":[{"id":157654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4094/report-thumb.jpg"},{"id":366724,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4094/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Denver","otherGeospatial":"Green Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.19203186035155,\n              39.678126804900295\n            ],\n            [\n              -105.14911651611328,\n              39.678126804900295\n            ],\n            [\n              -105.14911651611328,\n              39.71537404178252\n            ],\n            [\n              -105.19203186035155,\n              39.71537404178252\n            ],\n            [\n              -105.19203186035155,\n              39.678126804900295\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69859c","contributors":{"authors":[{"text":"Branson, Farrel Allen","contributorId":53823,"corporation":false,"usgs":true,"family":"Branson","given":"Farrel","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":196180,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shown, Lynn M.","contributorId":7326,"corporation":false,"usgs":true,"family":"Shown","given":"Lynn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":196179,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60923,"text":"mf2071A - 1989 - Geochemical maps showing the distribution and abundance of selected elements in stream-sediment samples, Solomon and Bendeleben 1° x 3° quadrangles, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2021-11-08T19:16:33.493326","indexId":"mf2071A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"2071","chapter":"A","title":"Geochemical maps showing the distribution and abundance of selected elements in stream-sediment samples, Solomon and Bendeleben 1° x 3° quadrangles, Seward Peninsula, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2071A","usgsCitation":"Smith, S., King, H.D., and O’Leary, R.M., 1989, Geochemical maps showing the distribution and abundance of selected elements in stream-sediment samples, Solomon and Bendeleben 1° x 3° quadrangles, Seward Peninsula, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 2071, 14 p., https://doi.org/10.3133/mf2071A.","productDescription":"14 p.","costCenters":[],"links":[{"id":179782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1989/2071a/report-thumb.jpg"},{"id":105223,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5671.htm","linkFileType":{"id":5,"text":"html"},"description":"5671"},{"id":88901,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1989/2071a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Seward PeninsulaSolomon and Bendeleben 1° x 3° quadrangles","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -165,64.25 ], [ -165,66 ], [ -162,66 ], [ -162,64.25 ], [ -165,64.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf1f","contributors":{"authors":[{"text":"Smith, S.C.","contributorId":16833,"corporation":false,"usgs":true,"family":"Smith","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":264623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":264625,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Leary, R. M.","contributorId":44894,"corporation":false,"usgs":true,"family":"O’Leary","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":264624,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":33416,"text":"b1702D - 1989 - Mineral resources of the Muggins Mountains Wilderness Study Area, Yuma County, Arizona","interactions":[],"lastModifiedDate":"2025-05-14T19:40:56.793448","indexId":"b1702D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1702","chapter":"D","title":"Mineral resources of the Muggins Mountains Wilderness Study Area, Yuma County, Arizona","language":"ENGLISH","publisher":"U.S. G.P.O. ; For sale by the Books and Open-File Reports Section, U.S. Geological Survey,","doi":"10.3133/b1702D","usgsCitation":"Smith, D., Tosdal, R., Pitkin, J.A., Kleinkopf, M.D., and Wood, R., 1989, Mineral resources of the Muggins Mountains Wilderness Study Area, Yuma County, Arizona: U.S. Geological Survey Bulletin 1702, v, p. D1-D16, ill. ;28 cm., https://doi.org/10.3133/b1702D.","productDescription":"v, p. D1-D16, ill. ;28 cm.","costCenters":[],"links":[{"id":251832,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1702d/report-thumb.jpg"},{"id":247394,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1702d/report.pdf","size":"4063","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a1c4","contributors":{"authors":[{"text":"Smith, David B. 0000-0001-8396-9105 dsmith@usgs.gov","orcid":"https://orcid.org/0000-0001-8396-9105","contributorId":1274,"corporation":false,"usgs":true,"family":"Smith","given":"David B.","email":"dsmith@usgs.gov","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":210965,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tosdal, R. M.","contributorId":54982,"corporation":false,"usgs":true,"family":"Tosdal","given":"R. M.","affiliations":[],"preferred":false,"id":210968,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pitkin, J. A.","contributorId":85194,"corporation":false,"usgs":true,"family":"Pitkin","given":"J.","middleInitial":"A.","affiliations":[],"preferred":false,"id":210969,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kleinkopf, M. D.","contributorId":10036,"corporation":false,"usgs":true,"family":"Kleinkopf","given":"M.","middleInitial":"D.","affiliations":[],"preferred":false,"id":210966,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wood, R. H.","contributorId":31722,"corporation":false,"usgs":true,"family":"Wood","given":"R. H.","affiliations":[],"preferred":false,"id":210967,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":26053,"text":"wri884033 - 1989 - Hydrologic effects of pumpage from the Denver basin bedrock aquifers of northern El Paso County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri884033","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4033","title":"Hydrologic effects of pumpage from the Denver basin bedrock aquifers of northern El Paso County, Colorado","docAbstract":"The Denver groundwater basin underlies a 6,700 sq-mi area in eastern Colorado. To assess current conditions of the four bedrock aquifers in the basin, water levels, streamflow gain and loss, and other data were collected. Current aquifer conditions in the southern part of the basin and likely response to various 100-year pumping scenarios were analyzed using a digital finite-difference model. Simulated predevelopment flow through the bedrock aquifers was about 59 cu ft/sec. Water level changes between 1978 and 1985, likely caused by variations in precipitation and in pumping and by lowering of the water table in the overlying Black Squirrel Creek alluvial aquifer, ranged from rises of more than 40 ft to declines of as much as 80 ft. In 1985, pumping from the bedrock aquifers was about 56 cu ft/sec. Simulations indicate that 43% of the pumpage came from a decrease in volume of groundwater in storage; 37% came from induced recharge and captured discharge. The remaining 20% came from a transient high rate of recharge from precipitation. A baseline 100-yr simulation, beginning in 1985, indicated minimal drawdowns for constant pumping at 1985 rates in the southern part of the basin. Other simulations indicated that the pumpage required to supply the needs of the projected population would be accompanied by drawdowns of as much as 1,300 ft and by large decreases in amount of groundwater in storage. Pumpage from a hypothetical well field, located where the aquifers are thickest , and from the aquifers underlying Colorado Springs also was simulated. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884033","usgsCitation":"Banta, E.R., 1989, Hydrologic effects of pumpage from the Denver basin bedrock aquifers of northern El Paso County, Colorado: U.S. Geological Survey Water-Resources Investigations Report 88-4033, vi, 84 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884033.","productDescription":"vi, 84 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4033/report-thumb.jpg"},{"id":54829,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54830,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4033/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54831,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4033/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54832,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4033/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54833,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4033/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54834,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606e8d","contributors":{"authors":[{"text":"Banta, E. R.","contributorId":63038,"corporation":false,"usgs":true,"family":"Banta","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":195720,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25494,"text":"wri894146 - 1989 - Evaluation of field sampling and preservation methods for strontium-90 in ground water at the Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"wri894146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4146","title":"Evaluation of field sampling and preservation methods for strontium-90 in ground water at the Idaho National Engineering Laboratory, Idaho","docAbstract":"Water from four wells completed in the Snake River Plain aquifer was sampled as part of the U.S. Geological Survey 's quality assurance program to evaluate the effect of filtration and preservation methods on strontium-90 concentrations in groundwater at the Idaho National Engineering Laboratory. Water from each well was filtered through either a 0.45-micrometer membrane or a 0.1-micrometer membrane filter; unfiltered samples also were collected. Two sets of filtered and two sets of unfiltered samples was preserved in the field with reagent-grade hydrochloric acid and the other set of samples was not acidified. For water from wells with strontium-90 concentrations at or above the reporting level, 94% or more of the strontium-90 is in true solution or in colloidal particles smaller than 0.1 micrometer. These results suggest that within-laboratory reproducibility for strontium-90 in groundwater at the INEL is not significantly affected by changes in filtration and preservation methods used for sample collections. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri894146","usgsCitation":"Cecil, L., Knobel, L., Wegner, S., and Moore, L., 1989, Evaluation of field sampling and preservation methods for strontium-90 in ground water at the Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 89-4146, iv, 24 p. :ill. ;28 cm., https://doi.org/10.3133/wri894146.","productDescription":"iv, 24 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":118888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4146/report-thumb.jpg"},{"id":54216,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4146/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faddd","contributors":{"authors":[{"text":"Cecil, L.D.","contributorId":62616,"corporation":false,"usgs":true,"family":"Cecil","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":193923,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knobel, L.L.","contributorId":83115,"corporation":false,"usgs":true,"family":"Knobel","given":"L.L.","affiliations":[],"preferred":false,"id":193924,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wegner, S.J.","contributorId":36950,"corporation":false,"usgs":true,"family":"Wegner","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":193922,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moore, L.L.","contributorId":108145,"corporation":false,"usgs":true,"family":"Moore","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":193925,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26371,"text":"wri894152 - 1989 - Geology and ground-water resources of the San Carlos Indian Reservation, Gila, Graham, and Pinal counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:32","indexId":"wri894152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4152","title":"Geology and ground-water resources of the San Carlos Indian Reservation, Gila, Graham, and Pinal counties, Arizona","docAbstract":"The San Carlos Indian Reservation includes about 2,900 sq mi in east- central Arizona. Relatively impermeable pre-Tertiary rocks are exposed in about 23% of the reservation and underlie water-bearing Tertiary and quaternary basin fill and Quaternary stream alluvium in much of the southern part of the reservation. About 9,000 members of the San Carlos Apache Tribe live on the reservation and rely on groundwater to meet public supply, irrigation, and other needs. Basin fill is widespread in the valley of the San Carlos and Gila Rivers and consists of fine sand, silt, limestone, clay, and pyroclastic volcanics that may attain a total maximum thickness of more than 3,200 ft in the reservation. Quaternary stream alluvium overlies the basin fill along many streams and washes. Stream alluvium consists of poorly sorted, unconsolidated, gravelly, muddy, sand; and sandy gravel and reaches a maximum thickness of 100 ft along the San Carlos and Gila Rivers. The volume of recoverable water stored in the basin fill to a depth of 1,200 ft is estimated to be about 20 million acre-ft. The volume of recoverable water stored in the stream alluvium on the reservation is estimated to be more than 100,000 acre-ft. The stream alluvium along the San Carlos River supplies most of the water used for drinking. Water throughout much of the reservation is suitable for most uses except for that in the alluvium along the Gila River, which contains large concentrations of dissolved solids. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894152","usgsCitation":"Brown, J.G., 1989, Geology and ground-water resources of the San Carlos Indian Reservation, Gila, Graham, and Pinal counties, Arizona: U.S. Geological Survey Water-Resources Investigations Report 89-4152, v, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri894152.","productDescription":"v, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":110254,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47240.htm","linkFileType":{"id":5,"text":"html"},"description":"47240"},{"id":122881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4152/report-thumb.jpg"},{"id":55163,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4152/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55164,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4152/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55165,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6835de","contributors":{"authors":[{"text":"Brown, J. G.","contributorId":28263,"corporation":false,"usgs":true,"family":"Brown","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":196273,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26231,"text":"wri884211 - 1989 - Relation of ground-water quality to land use in the Philadelphia, Pennsylvania-Camden, New Jersey area","interactions":[],"lastModifiedDate":"2022-08-29T18:40:14.749232","indexId":"wri884211","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4211","title":"Relation of ground-water quality to land use in the Philadelphia, Pennsylvania-Camden, New Jersey area","docAbstract":"The distributions of common dissolved constituents, trace metals, and volatile organic compounds in ground water near Philadelphia, Pennsylvania, and Camden, New Jersey, are influenced by local geology and land use. Many common dissolved constituents are more concentrated in ground water beneath urban and industrial areas than in water beneath suburban and undeveloped and agricultural areas. Industrial and urban land uses commonly are situated in the outcrop of the aquifer where vulnerability of ground water to contamination is increased by the lack of overlying confining strata. Ground water beneath undeveloped and agricultural lands is least affected by trace metal or volatile organic contamination, but differences in water quality as related to other land-use categories are less clear and vary according to the chemical constituent considered.\r\n\r\n      Only about 20 percent of all water samples contained detectable concentrations of trace metals or volatile organic compounds; as a result, determinations of relations between water quality and land use are difficult. Variations in detection limits further complicated data interpretation. The proportion of water samples in which concentrations of constituents were below detection compared to water samples in which concentrations were present in detectable amounts is the most useful statistic in determining relations based on trace-metal or volatile organic-compound data. Iron and Manganese concentrations are elevated in water throughout the Coastal Plain aquifer in Pennsylvania, but the elevated concentrations cannot be adequately explained on the basis of land use alone.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884211","usgsCitation":"Blickwedel, R.S., and Wood, C.R., 1989, Relation of ground-water quality to land use in the Philadelphia, Pennsylvania-Camden, New Jersey area: U.S. Geological Survey Water-Resources Investigations Report 88-4211, vi, 58 p., https://doi.org/10.3133/wri884211.","productDescription":"vi, 58 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":405825,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47110.htm","linkFileType":{"id":5,"text":"html"}},{"id":55030,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4211/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4211/report-thumb.jpg"}],"country":"United States","state":"New Jersey, Pennsylvania","city":"Camden, Philadelphia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.42938232421875,\n              39.70296052957233\n            ],\n            [\n              -74.84161376953125,\n              39.70296052957233\n            ],\n            [\n              -74.84161376953125,\n              40.143189742924406\n            ],\n            [\n              -75.42938232421875,\n              40.143189742924406\n            ],\n            [\n              -75.42938232421875,\n              39.70296052957233\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606740","contributors":{"authors":[{"text":"Blickwedel, Ray S.","contributorId":23984,"corporation":false,"usgs":true,"family":"Blickwedel","given":"Ray","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":196024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, C. R.","contributorId":100386,"corporation":false,"usgs":true,"family":"Wood","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":196025,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25130,"text":"cir930H - 1989 - International strategic minerals inventory summary report; natural graphite","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"cir930H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"930","chapter":"H","title":"International strategic minerals inventory summary report; natural graphite","docAbstract":"Natural graphite is a crystalline mineral of pure carbon which normally occurs in the form of platelet-shaped crystals. It has important properties, such as chemical inertness, low thermal expansion, and lubricity, that make it almost irreplaceable for certain uses such as refractories and steelmaking. Graphite ore types are crystalline (flake and lump} or 'amorphous' (cryptocrystalline}. Refractory applications use the largest total amount of natural graphite, while the most important use of crystalline graphite is in crucibles for handling molten metals. All graphite deposits being mined today are found in the following metamorphic environments: (1) contact metamorphosed coal generally is a source of amorphous graphite; (2)disseminated crystalline flake graphite comes from syngenetic metasediments; and (3) crystalline lump graphite is found in epigenetic veins in high-grade metamorphic regions. Graphite may also occur as a trace mineral in ultrabasic rocks and pegmatites, but these are economically insignificant. The world's identified economically exploitable resources of crystalline graphite in major deposits are estimated to be about 9.7 million metric tons of concentrate. In-place resources of amorphous graphite are about 11.5 million metric tons. Of these, less than 2 percent of the crystalline ore and less than 1 percent of the amorphous ore are in western industrial countries. World mining production of natural graphite rose from 347,000 metric tons in 1973 to 659,000 metric tons in 1986, while the proportion produced by central economy countries increased from about 50 percent for the period from 1973 to 1978 to more than 64 percent in 1979 to 1986. It is estimated that crystalline flake graphite accounts for at least 180,000 metric tons of total annual world mining production of natural graphite, and amorphous graphite makes up the rest.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir930H","usgsCitation":"Krauss, U., Schmidt, H., Taylor, H., and Sutphin, D.M., 1989, International strategic minerals inventory summary report; natural graphite: U.S. Geological Survey Circular 930, v. :ill. ;26 cm.; 29 p., https://doi.org/10.3133/cir930H.","productDescription":"v. :ill. ;26 cm.; 29 p.","costCenters":[],"links":[{"id":124484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1989/0930h/report-thumb.jpg"},{"id":54110,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1989/0930h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cde4b07f02db544d63","contributors":{"authors":[{"text":"Krauss, U.H.","contributorId":47404,"corporation":false,"usgs":true,"family":"Krauss","given":"U.H.","email":"","affiliations":[],"preferred":false,"id":193269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmidt, H.W.","contributorId":103710,"corporation":false,"usgs":true,"family":"Schmidt","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":193271,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, H.A. Jr.","contributorId":100024,"corporation":false,"usgs":true,"family":"Taylor","given":"H.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":193270,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sutphin, D. M.","contributorId":27424,"corporation":false,"usgs":true,"family":"Sutphin","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":193268,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":56236,"text":"wdrOK871 - 1989 - Water resources data, Oklahoma, water year 1987","interactions":[],"lastModifiedDate":"2025-03-14T19:12:08.998152","indexId":"wdrOK871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"OK-87-1","title":"Water resources data, Oklahoma, water year 1987","docAbstract":"<p>Water resources data for the 1987 water year for Oklahoma consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes or reservoirs. This report contains discharge records for 123 gaging stations; stage and contents for 30 lakes or reservoirs; water quality for 38 gaging stations and 3 lakes. Also included are 5 partial-record stations. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Oklahoma.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrOK871","collaboration":"Prepared in cooperation with the State of Oklahoma and with other agencies","usgsCitation":"Hauth, L., Walters, D., Coffey, T., and White, D., 1989, Water resources data, Oklahoma, water year 1987: U.S. Geological Survey Water Data Report OK-87-1, viii, 324 p., https://doi.org/10.3133/wdrOK871.","productDescription":"viii, 324 p.","costCenters":[],"links":[{"id":483379,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1987/ok-87-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174534,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1987/ok-87-1/report-thumb.jpg"}],"country":"United 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,{"id":18122,"text":"ofr89251 - 1989 - Ground-water resources of the Central Valley of California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr89251","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-251","title":"Ground-water resources of the Central Valley of California","language":"ENGLISH","publisher":"Department of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr89251","usgsCitation":"Bertoldi, G.L., 1989, Ground-water resources of the Central Valley of California: U.S. Geological Survey Open-File Report 89-251, 2 p. :map ;28 cm., https://doi.org/10.3133/ofr89251.","productDescription":"2 p. :map ;28 cm.","costCenters":[],"links":[{"id":149233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0251/report-thumb.jpg"},{"id":47476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0251/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65aa30","contributors":{"authors":[{"text":"Bertoldi, Gilbert L.","contributorId":60208,"corporation":false,"usgs":true,"family":"Bertoldi","given":"Gilbert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":178587,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26204,"text":"wri884225 - 1989 - Water resources of Sedgwick County, Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri884225","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4225","title":"Water resources of Sedgwick County, Kansas","docAbstract":"Hydrologic data from streams, impoundments, and wells are interpreted to: (1) document water resources characteristics; (2) describe causes and extent of changes in water resources characteristics; and (3) evaluate water resources as sources of supply. During 1985, about 134,200 acre-ft of water (84% groundwater) were used for public (42%), irrigation, (40%), industrial (14%), and domestic (4%) supplies. Streamflow and groundwater levels are related directly to precipitation, and major rivers are sustained by groundwater inflow. Significant groundwater level declines have occurred only in the Wichita well field. The Arkansas and Ninnescah Rivers have sodium chloride type water; the Little Arkansas River, calcium bicarbonate type water. Water quality characteristics of water in small streams and wells depend primarily on local geology. The Wellington Formation commonly yields calcium sulfate type water; Ninnescah Shale and unconsolidated deposits generally yield calcium bicarbonate type water. Sodium chloride and calcium sulfate type water in the area often have dissolved-solids concentrations exceeding 1,000 mg/L. Water contamination by treated sewage effluent was detected inparts of the Arkansas River, Little Arkansas River, and Cowskin Creek. Nitrite plus nitrate as nitrogen contamination was detected in 11 of 101 wells; oilfield brine was detected in the Wichita-Valley Center Floodway, Prairie Creek, Whitewater Creek, and 16 of 101 wells; and agricultural pesticides were detected in 8 of 14 impoundments and 5 of 19 wells. Generally, the water is acceptable for most uses. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884225","usgsCitation":"Bevans, H., 1989, Water resources of Sedgwick County, Kansas: U.S. Geological Survey Water-Resources Investigations Report 88-4225, viii, 119 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884225.","productDescription":"viii, 119 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119109,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4225/report-thumb.jpg"},{"id":54997,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4225/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54998,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4225/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54999,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4225/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69964f","contributors":{"authors":[{"text":"Bevans, H.E.","contributorId":102892,"corporation":false,"usgs":true,"family":"Bevans","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":195976,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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