{"pageNumber":"4875","pageRowStart":"121850","pageSize":"25","recordCount":184569,"records":[{"id":12063,"text":"ofr86497 - 1986 - Geohydrologic data from Port Royal Sound, Beaufort County, South Carolina","interactions":[],"lastModifiedDate":"2016-12-15T12:37:37","indexId":"ofr86497","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-497","title":"Geohydrologic data from Port Royal Sound, Beaufort County, South Carolina","docAbstract":"Nine offshore wells were drilled through overlying sediments into the Upper Floridan aquifer in Port Royal Sound, South Carolina and the adjacent Atlantic Ocean, to obtain geologic, hydrologic, and water quality data. The Upper Floridan aquifer consists predominantly of light-gray, poorly consolidated, fossiliferous limestone. In the Port Royal Sound area, the Upper Floridan is overlain by olive-gray, medium to course sand and silty sand. Falling-head permeability tests on these overlying clastic sediments indicate permeabilities of 1,100 to 4.3 x 10 to the 7th power centimeters/sec. Other geologic and hydrologic data, including geophysical logs, sieve analyses, and detailed core descriptions were obtained, along with continuous water level records of the wells, tidal records, and barometric pressure records. Water collected from the Upper Floridan aquifer beneath Port Royal Sound and the ocean ranged in concentration of chloride from 54 to 12,000 mg/l. Measured pH ranged from 6.8 to 8.4, and alkalinity ranged from 122 to 368 mg/l as CaC03. Other water quality data obtained include temperature, specific conductance, carbon-13, carbon-14, tritium , deuterium, oxygen-18, dissolved oxygen, dissolved solids, nitrogen species, phosphorus, organic carbon, cyanide, sulfide, calcium, magnesium, sodium, potassium, sulfate, fluoride, silica , bromide, iodide, and selected trace metals. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86497","usgsCitation":"Burt, R., Belval, D., Crouch, M., and Hughes, W., 1986, Geohydrologic data from Port Royal Sound, Beaufort County, South Carolina: U.S. Geological Survey Open-File Report 86-497, 64 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr86497.","productDescription":"64 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":40079,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0497/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144380,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0497/report-thumb.jpg"},{"id":40080,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0497/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40081,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0497/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40082,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0497/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40083,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0497/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40084,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0497/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40085,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0497/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40086,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0497/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40087,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0497/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40088,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0497/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","county":"Beaufort County","otherGeospatial":"Port Royal Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.99945068359375,\n              32.086065193329354\n            ],\n            [\n              -80.99945068359375,\n              32.58500645901216\n            ],\n            [\n              -80.37185668945312,\n              32.58500645901216\n            ],\n            [\n              -80.37185668945312,\n              32.086065193329354\n            ],\n            [\n              -80.99945068359375,\n              32.086065193329354\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8ef7","contributors":{"authors":[{"text":"Burt, R.A.","contributorId":40994,"corporation":false,"usgs":true,"family":"Burt","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":164902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belval, D.L.","contributorId":52186,"corporation":false,"usgs":true,"family":"Belval","given":"D.L.","affiliations":[],"preferred":false,"id":164903,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crouch, Michael","contributorId":79105,"corporation":false,"usgs":true,"family":"Crouch","given":"Michael","email":"","affiliations":[],"preferred":false,"id":164904,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hughes, W.B.","contributorId":92263,"corporation":false,"usgs":true,"family":"Hughes","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":164905,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":14573,"text":"ofr8661 - 1986 - Data on snow chemistry of the Cascade-Sierra Nevada Mountains","interactions":[],"lastModifiedDate":"2018-02-15T13:09:03","indexId":"ofr8661","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-61","title":"Data on snow chemistry of the Cascade-Sierra Nevada Mountains","docAbstract":"Snow chemistry data were measured for solutes found in snow core samples collected from the Cascade-Sierra Nevada Mountains from late February to mid-March 1983. The data are part of a study to assess geographic variations in atmospheric deposition in Washington, Oregon, and California. The constituents and properties include pH and concentrations of hydrogen ion, calcium, magnesium, sodium, potassium, chloride, sulfate, nitrate, fluoride, phosphate, ammonium, iron, aluminum, manganese, copper, cadmium, lead, and dissolved organic carbon. Concentrations of arsenic and bromide were below the detection limit. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8661","usgsCitation":"Laird, L., Taylor, H.E., and Lombard, R., 1986, Data on snow chemistry of the Cascade-Sierra Nevada Mountains: U.S. Geological Survey Open-File Report 86-61, 25 p. :map ;28 cm., https://doi.org/10.3133/ofr8661.","productDescription":"25 p. :map ;28 cm.","costCenters":[],"links":[{"id":146573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0061/report-thumb.jpg"},{"id":43242,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0061/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7f5","contributors":{"authors":[{"text":"Laird, L.B.","contributorId":23522,"corporation":false,"usgs":true,"family":"Laird","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":169671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":169673,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lombard, R.E.","contributorId":25551,"corporation":false,"usgs":true,"family":"Lombard","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":169672,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14457,"text":"ofr86633 - 1986 - Radioactive black sand placer deposits of the Challis 1° x 2° quadrangle, Idaho","interactions":[],"lastModifiedDate":"2021-09-28T20:48:13.121114","indexId":"ofr86633","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-633","title":"Radioactive black sand placer deposits of the Challis 1° x 2° quadrangle, Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86633","usgsCitation":"Kiilsgaard, T.H., and Hall, W., 1986, Radioactive black sand placer deposits of the Challis 1° x 2° quadrangle, Idaho: U.S. Geological Survey Open-File Report 86-633, Report: i, 13 p.; 1 Plate: 26.44 × 21.29 inches, https://doi.org/10.3133/ofr86633.","productDescription":"Report: i, 13 p.; 1 Plate: 26.44 × 21.29 inches","costCenters":[],"links":[{"id":389913,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17103.htm"},{"id":43138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0633/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43137,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0633/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0633/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Challis 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116,\n              44\n            ],\n            [\n              -114,\n              44\n            ],\n            [\n              -114,\n              45\n            ],\n            [\n              -116,\n              45\n            ],\n            [\n              -116,\n              44\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649d9a","contributors":{"authors":[{"text":"Kiilsgaard, T. H.","contributorId":102043,"corporation":false,"usgs":true,"family":"Kiilsgaard","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":169490,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hall, W. E.","contributorId":6431,"corporation":false,"usgs":true,"family":"Hall","given":"W. E.","affiliations":[],"preferred":false,"id":169489,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14510,"text":"ofr86424W - 1986 - Sediment transport characteristics of selected streams in the Susitna River Basin, Alaska, October 1983 to September 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:06:54","indexId":"ofr86424W","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-424","chapter":"W","title":"Sediment transport characteristics of selected streams in the Susitna River Basin, Alaska, October 1983 to September 1984","docAbstract":"The upper reaches of the Susitna River have been considered for development of a large power generation system for south-central Alaska. This report presents a summary and discussion of sediment and hydraulic data obtained from October 1983 to September 1984 at ten sites on the Susitna, Chulitna, Talkeetna, and Yentna Rivers. Sediment data include measurements of suspended sediment and bedload discharge and analyses of particle size distribution of suspended sediment, bed-load, and bed material; hydraulic data include measurements of width, average depth and velocity, and water surface slope. Relations between water and sediment discharge are developed for selected sites. Sediment loads for the 1984 water year were estimated for the Yentna, Chulitna, and Talkeetna Rivers and for four sites on the Susitna River. About 25 million tons of sediment was transported by the Susitna River at Susitna Station during the 1984 water year. The Yentna and Chulitna Rivers contributed more than 20 million tons of sediment to the susitna River. About 90% of suspended material (silt, clay, and sand) transported past upstream sites reached Susitna Station during the same period. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86424W","usgsCitation":"Knott, J.M., Lipscomb, S.W., and Lewis, T.W., 1986, Sediment transport characteristics of selected streams in the Susitna River Basin, Alaska, October 1983 to September 1984: U.S. Geological Survey Open-File Report 86-424, vi, 73 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr86424W.","productDescription":"vi, 73 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":147192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0424w/report-thumb.jpg"},{"id":43201,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0424w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbfe7","contributors":{"authors":[{"text":"Knott, J. M.","contributorId":77909,"corporation":false,"usgs":true,"family":"Knott","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":169580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lipscomb, Stephen W.","contributorId":84753,"corporation":false,"usgs":true,"family":"Lipscomb","given":"Stephen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169581,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewis, Terry W.","contributorId":107296,"corporation":false,"usgs":true,"family":"Lewis","given":"Terry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169582,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":69706,"text":"i1787 - 1986 - Controlled photomosaic of part of the Kasei Valles region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:51","indexId":"i1787","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1787","title":"Controlled photomosaic of part of the Kasei Valles region of Mars","language":"ENGLISH","doi":"10.3133/i1787","isbn":"0607789204","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Controlled photomosaic of part of the Kasei Valles region of Mars: U.S. Geological Survey IMAP 1787, p. (1 sheet); Sheet 26 by 38 inches, https://doi.org/10.3133/i1787.","productDescription":"p. (1 sheet); Sheet 26 by 38 inches","costCenters":[],"links":[{"id":191348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101497,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1787/plate-1.pdf","size":"9388","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a7c3","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":534674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33317,"text":"b1719B - 1986 - Mineral resources of the Battle Creek, Yatahoney Creek, and Juniper Creek Wilderness Study Areas, Owyhee County, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:09:16","indexId":"b1719B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1719","chapter":"B","title":"Mineral resources of the Battle Creek, Yatahoney Creek, and Juniper Creek Wilderness Study Areas, Owyhee County, Idaho","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1719B","usgsCitation":"Goeldner, C.A., Sawlan, M., King, H.D., Winters, R.A., Leszcykowski, A., and Graham, D.E., 1986, Mineral resources of the Battle Creek, Yatahoney Creek, and Juniper Creek Wilderness Study Areas, Owyhee County, Idaho: U.S. Geological Survey Bulletin 1719, v, p. B1-B10, maps ;28 cm., https://doi.org/10.3133/b1719B.","productDescription":"v, p. B1-B10, maps ;28 cm.","costCenters":[],"links":[{"id":163993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1719b/report-thumb.jpg"},{"id":61138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1719b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604771","contributors":{"authors":[{"text":"Goeldner, Carolyn A.","contributorId":103525,"corporation":false,"usgs":true,"family":"Goeldner","given":"Carolyn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":210464,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sawlan, M. G.","contributorId":44933,"corporation":false,"usgs":true,"family":"Sawlan","given":"M. G.","affiliations":[],"preferred":false,"id":210460,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":210462,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Winters, R. A.","contributorId":39401,"corporation":false,"usgs":true,"family":"Winters","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":210459,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Leszcykowski, A. M.","contributorId":78735,"corporation":false,"usgs":true,"family":"Leszcykowski","given":"A. M.","affiliations":[],"preferred":false,"id":210461,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Graham, D. E.","contributorId":95951,"corporation":false,"usgs":true,"family":"Graham","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":210463,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":14591,"text":"ofr86534 - 1986 - Aquifer-nomenclature guidelines","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr86534","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-534","title":"Aquifer-nomenclature guidelines","docAbstract":"Guidelines and recommendations for naming aquifers are presented to assist authors of geohydrological reports in the United States Geological Survey, Water Resources Division. The hierarchy of terms that is used for water- yielding rocks from largest to smallest is aquifer system, aquifer, and zone. If aquifers are named, the names should be derived from lithologic terms, rock-stratigraphic units, or geographic names. The following items are not recommended as sources of aquifer names: time-stratigraphic names, relative position, alphanumeric designations, depositional environment, depth of occurrence, acronyms, and hydrologic conditions. Confining units should not be named unless doing so clearly promotes understanding of a particular aquifer system. Sources of names for confining units are similar to those for aquifer names, i.e. lithologic terms, rock-stratigraphic units or geographic names. Examples of comparison charts and tables that are used to define the geohydrologic framework are included. Aquifers are defined in 11 hypothetical examples that characterize geohydrologic settings throughout the country. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86534","usgsCitation":"Laney, R., and Davidson, C., 1986, Aquifer-nomenclature guidelines: U.S. Geological Survey Open-File Report 86-534, vi, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr86534.","productDescription":"vi, 46 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":148209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0534/report-thumb.jpg"},{"id":43259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0534/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679ef8","contributors":{"authors":[{"text":"Laney, R. L.","contributorId":83889,"corporation":false,"usgs":true,"family":"Laney","given":"R. L.","affiliations":[],"preferred":false,"id":169706,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davidson, C.B.","contributorId":54215,"corporation":false,"usgs":true,"family":"Davidson","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":169705,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21282,"text":"ofr86416W - 1986 - Observation-well network in Illinois, 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:07:58","indexId":"ofr86416W","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-416","chapter":"W","title":"Observation-well network in Illinois, 1984","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86416W","usgsCitation":"Voelker, D.C., 1986, Observation-well network in Illinois, 1984: U.S. Geological Survey Open-File Report 86-416, iv, 108 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86416W.","productDescription":"iv, 108 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":155180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0416w/report-thumb.jpg"},{"id":50833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0416w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69650e","contributors":{"authors":[{"text":"Voelker, D. C.","contributorId":36572,"corporation":false,"usgs":true,"family":"Voelker","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":184137,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14630,"text":"ofr86154 - 1986 - Geology of the petroleum and coal deposits in the North China basin, eastern China","interactions":[{"subject":{"id":14630,"text":"ofr86154 - 1986 - Geology of the petroleum and coal deposits in the North China basin, eastern China","indexId":"ofr86154","publicationYear":"1986","noYear":false,"title":"Geology of the petroleum and coal deposits in the North China basin, eastern China"},"predicate":"SUPERSEDED_BY","object":{"id":34912,"text":"b1871 - 1989 - Geology of petroleum and coal deposits in the North China Basin, Eastern China","indexId":"b1871","publicationYear":"1989","noYear":false,"title":"Geology of petroleum and coal deposits in the North China Basin, Eastern China"},"id":1}],"supersededBy":{"id":34912,"text":"b1871 - 1989 - Geology of petroleum and coal deposits in the North China Basin, Eastern China","indexId":"b1871","publicationYear":"1989","noYear":false,"title":"Geology of petroleum and coal deposits in the North China Basin, Eastern China"},"lastModifiedDate":"2025-09-30T15:31:05.043471","indexId":"ofr86154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-154","title":"Geology of the petroleum and coal deposits in the North China basin, eastern China","docAbstract":"<p>The North China basin evolved initially from a rifted intracratonic graben system on the east-central Sino-Korean platform during the Jurassic and Cretaceous Yanshanian orogeny. The basin reached its maximum stage of development in the Neogene owing to rift reactivation by the Himalayan orogeny. As indicated by geophysical data, extensional rifting within the basin is still active today.</p>","language":"English","publisher":"U. S. 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,{"id":14642,"text":"ofr86108 - 1986 - Spectral whitening in the frequency domain","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr86108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-108","title":"Spectral whitening in the frequency domain","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86108","usgsCitation":"Lee, M.W., 1986, Spectral whitening in the frequency domain: U.S. Geological Survey Open-File Report 86-108, i, 15 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86108.","productDescription":"i, 15 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":148225,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0108/report-thumb.jpg"},{"id":43364,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0108/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5ece","contributors":{"authors":[{"text":"Lee, Myung W.","contributorId":84358,"corporation":false,"usgs":true,"family":"Lee","given":"Myung","middleInitial":"W.","affiliations":[],"preferred":false,"id":169783,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15533,"text":"ofr86587 - 1986 - Spectral reflectance of vegetation in the Idaho Cobalt District; potential for exploration using remote sensing","interactions":[],"lastModifiedDate":"2012-02-02T00:06:58","indexId":"ofr86587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-587","title":"Spectral reflectance of vegetation in the Idaho Cobalt District; potential for exploration using remote sensing","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86587","usgsCitation":"Purdy, T.L., Milton, N., and Eiswerth, B.A., 1986, Spectral reflectance of vegetation in the Idaho Cobalt District; potential for exploration using remote sensing: U.S. Geological Survey Open-File Report 86-587, 9 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr86587.","productDescription":"9 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":148181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0587/report-thumb.jpg"},{"id":44491,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0587/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5c86","contributors":{"authors":[{"text":"Purdy, T. L.","contributorId":53812,"corporation":false,"usgs":true,"family":"Purdy","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171283,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Milton, N.M.","contributorId":29415,"corporation":false,"usgs":true,"family":"Milton","given":"N.M.","email":"","affiliations":[],"preferred":false,"id":171282,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eiswerth, B. A.","contributorId":55851,"corporation":false,"usgs":true,"family":"Eiswerth","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":171284,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14703,"text":"ofr86487 - 1986 - Hydrologic data for urban studies in the Houston metropolitan area, Texas, 1983","interactions":[],"lastModifiedDate":"2017-06-14T11:20:52","indexId":"ofr86487","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-487","title":"Hydrologic data for urban studies in the Houston metropolitan area, Texas, 1983","docAbstract":"<p>Hydro!ogic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in the Austin and Houston areas, and have been completed in the Dallas-Fort Worth and San Antonio areas.</p>\n<p>The U.S. Geological Survey, in cooperation with the city of Houston, began studies in the Houston metropolitan area in 1964. The program was expanded in 1968 to include collection of water-quality data. The objectives of the Houston urban-hydrology study are as follows:</p>\n<ol>\n<li>To determine, on the basis of historical data and hydrologic analyses, the magnitude and frequency of flood peaks and flood volumes.</li>\n<li>To determine the effect of urban development on flood peaks and volumes.</li>\n<li>To ascertain the variation in water quality for different flow conditions and different seasons.</li>\n</ol>\n<p>This report, the twentieth in a series of reports to be published annually, is primarily applicable to objective No. 2. The report presents hydrologic data collected in the Houston urban area for the 1983 water year (October 1, 1982, to September 30, 1983).</p>\n<p>A report by Johnson and Sayre (1973) utilized records collected from 1965 to 1969 to study the effects of urbanization on floods in the Houston area. That report also summarized various basin parameters. A report by Waddell, Massey, and Jennings (1979) presented data on runoff from the Houston area and computed concentrations and loads of selected water-quality constituents discharged to Galveston Bay. The study utilized a variation of the \"STORM\" model developed by the Hydrologic Engineering Center of the U.S. Army Corps of Engineers. A report prepared by Li scum and Massey (1980) presented a technique for estimating the magnitude and frequency of floods in the Houston area from drainage areas, bank-full conveyance, and percentage )f urban development.</p>\n<p>A definition of terms related to streamflow, water quality, and other hydrologic data, as used in this report, are defined in \" U.S. Geological Survey, Water-resources data for Texas, water year 1983, volume 2.\"</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr86487","collaboration":"Prepared in cooperation with the City of Houston","usgsCitation":"Liscum, F., 1986, Hydrologic data for urban studies in the Houston metropolitan area, Texas, 1983: U.S. Geological Survey Open-File Report 86-487, viii, 287 p., https://doi.org/10.3133/ofr86487.","productDescription":"viii, 287 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":14711,"text":"ofr86200 - 1986 - BASIC program to reduce audio-magnetotelluric data and calculate apparent resistivity","interactions":[],"lastModifiedDate":"2012-02-02T00:06:58","indexId":"ofr86200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-200","title":"BASIC program to reduce audio-magnetotelluric data and calculate apparent resistivity","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86200","usgsCitation":"Long, C.L., and Pierce, H.A., 1986, BASIC program to reduce audio-magnetotelluric data and calculate apparent resistivity: U.S. Geological Survey Open-File Report 86-200, 17 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86200.","productDescription":"17 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":148128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0200/report-thumb.jpg"},{"id":43476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0200/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ae21","contributors":{"authors":[{"text":"Long, C. L.","contributorId":98699,"corporation":false,"usgs":true,"family":"Long","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":169890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, H. A.","contributorId":99951,"corporation":false,"usgs":true,"family":"Pierce","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":169891,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14705,"text":"ofr86417 - 1986 - Laboratory measurements of velocity-dependent frictional strength","interactions":[],"lastModifiedDate":"2012-02-02T00:07:03","indexId":"ofr86417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-417","title":"Laboratory measurements of velocity-dependent frictional strength","docAbstract":"Water levels, location, depths, and aquifers tapped are given for 113 observation wells in Michigan. Tabulated data include extremes of water levels for 1985 and for the period of record, pumpage of most major groundwater users in the state, and water quality data from selected wells. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86417","usgsCitation":"Lockner, D., and Byerlee, J., 1986, Laboratory measurements of velocity-dependent frictional strength: U.S. Geological Survey Open-File Report 86-417, 84 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86417.","productDescription":"84 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":147607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0417/report-thumb.jpg"},{"id":43473,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0417/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47fde4b07f02db4c98dc","contributors":{"authors":[{"text":"Lockner, D.A. 0000-0001-8630-6833","orcid":"https://orcid.org/0000-0001-8630-6833","contributorId":85603,"corporation":false,"usgs":true,"family":"Lockner","given":"D.A.","affiliations":[],"preferred":false,"id":169879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byerlee, J.D.","contributorId":69982,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.D.","affiliations":[],"preferred":false,"id":169878,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61018,"text":"mf1867 - 1986 - Map showing landslides in California that have caused fatalities or at least $1,000,000 in damages from 1906 to 1984","interactions":[],"lastModifiedDate":"2016-08-23T10:03:24","indexId":"mf1867","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1867","title":"Map showing landslides in California that have caused fatalities or at least $1,000,000 in damages from 1906 to 1984","docAbstract":"<p>Understanding where landslide processes in California have been most severe is helpful in determining priorities for landslide mapping, mitigation measures, and preparedness planning. Although a few studies of landslide damage and fatalities have been published (see sources of data 12, 17, 34, 36, 40), and many more reports mention landslide damage and fatalities incidentally, our map is the first to show where the problem is most severe for the entire state.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1867","usgsCitation":"Taylor, F., and Brabb, E.E., 1986, Map showing landslides in California that have caused fatalities or at least $1,000,000 in damages from 1906 to 1984: U.S. Geological Survey Miscellaneous Field Studies Map 1867, Plate: 40.87 x 50.33 inches, https://doi.org/10.3133/mf1867.","productDescription":"Plate: 40.87 x 50.33 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326123,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1867.JPG"},{"id":327549,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1867/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,33 ], [ -124,42 ], [ -115,42 ], [ -115,33 ], [ -124,33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a92e4b07f02db657794","contributors":{"authors":[{"text":"Taylor, Fred","contributorId":50165,"corporation":false,"usgs":true,"family":"Taylor","given":"Fred","affiliations":[],"preferred":false,"id":264842,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brabb, E. E.","contributorId":43780,"corporation":false,"usgs":true,"family":"Brabb","given":"E.","middleInitial":"E.","affiliations":[],"preferred":false,"id":264841,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25442,"text":"wri864051 - 1986 - Determination of geohydrologic framework and extent of d- water contamination using surface geophysical techniques at Picatinny Arsenal, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:18","indexId":"wri864051","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4051","title":"Determination of geohydrologic framework and extent of d- water contamination using surface geophysical techniques at Picatinny Arsenal, New Jersey","docAbstract":"Seismic-refraction, electric-resistivity sounding, and electromagnetic conductivity techniques were used to determine the geohydrologic framework and extent of groundwater contamination at Picatinny Arsenal in northern New Jersey. The area studied encompasses about 4 sq mi at the southern end of the Arsenal. The bedrock surface beneath the glacial sediments was delineated by seismic-refraction techniques. Data for 12 seismic lines were collected using a 12-channel engineering seismograph. Competent bedrock crops out on both sides of the valley, but is about 290 ft below land surface in the deepest part of the topographic valley. Where the exposed bedrock surface forms steep slopes on the valley side, it remains steep below the valley fill. Likewise, gentle bedrock valley slopes have gentle subsurface slopes. The deepest part of the bedrock valley is along the southern extension of the Green Pond fault. The electric-resistivity sounding technique was used to determine the sediment types. Data were collected from four sites using the offset Wenner electrode configuration. Below the surface layer, the sediments have apparent and computed resistivity values of 120 to 170 ohm-meters. These values correspond to a saturated fine-grained sediment such as silt or interbedded sand and clay. Groundwater contamination was by electromagnetic conductivity techniques using transmitting and receiving coils separated by 32.8 ft and 12 ft. Thirteen sites have apparent conductivity values exceeding 15 millimhos/m. Of these, seven sites indicate groundwater contamination from a variety of sources including a sanitary landfill, pyrotechnic testing ground, burning area, former domestic sewage field, salt storage facility, hazardous waste disposal lagoon, sewage treatment plant, and fertilizer storage shed. Three areas underlain by clay or muck are interpreted to be free of contamination. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864051","usgsCitation":"Lacombe, P., 1986, Determination of geohydrologic framework and extent of d- water contamination using surface geophysical techniques at Picatinny Arsenal, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 86-4051, v, 31 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864051.","productDescription":"v, 31 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4051/report-thumb.jpg"},{"id":54172,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4051/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54173,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4051/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54174,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4051/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54175,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4051/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54176,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4051/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54177,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4051/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667691","contributors":{"authors":[{"text":"Lacombe, Pierre","contributorId":28274,"corporation":false,"usgs":true,"family":"Lacombe","given":"Pierre","affiliations":[],"preferred":false,"id":193711,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26958,"text":"wri864344 - 1986 - Sediment-data sources and estimated annual suspended-sediment loads of rivers and streams in Colorado","interactions":[],"lastModifiedDate":"2021-12-21T20:55:50.903688","indexId":"wri864344","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4344","title":"Sediment-data sources and estimated annual suspended-sediment loads of rivers and streams in Colorado","docAbstract":"Sources of sediment data collected by several government agencies through water year 1984 are summarized for Colorado. The U.S. Geological Survey has collected suspended-sediment data at 243 sites; these data are stored in the U.S. Geological Survey 's water data storage and retrieval system. The U.S. Forest Service has collected suspended-sediment and bedload data at an additional 225 sites, and most of these data are stored in the U.S. Environmental Protection Agency 's water-quality-control information system. Additional unpublished sediment data are in the possession of the collecting entities. Annual suspended-sediment loads were computed for 133 U.S. Geological Survey sediment-data-collection sites using the daily mean water-discharge/sediment-transport-curve method. Sediment-transport curves were derived for each site by one of three techniques: (1) Least-squares linear regression of all pairs of suspended-sediment and corresponding water-discharge data, (2) least-squares linear regression of data sets subdivided on the basis of hydrograph season; and (3) graphical fit to a logarithm-logarithm plot of data. The curve-fitting technique used for each site depended on site-specific characteristics. Sediment-data sources and estimates of annual loads of suspended, bed, and total sediment from several other reports also are summarized. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864344","usgsCitation":"Elliott, J.G., and DeFeyter, K.L., 1986, Sediment-data sources and estimated annual suspended-sediment loads of rivers and streams in Colorado: U.S. Geological Survey Water-Resources Investigations Report 86-4344, Report: vii, 148 p.; 2 Plates: 26.86 × 21.85 inches and 26.94 × 22.40 inches, https://doi.org/10.3133/wri864344.","productDescription":"Report: vii, 148 p.; 2 Plates: 26.86 × 21.85 inches and 26.94 × 22.40 inches","costCenters":[],"links":[{"id":55844,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4344/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55843,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4344/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55845,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4344/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4344/report-thumb.jpg"},{"id":393252,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36657.htm"}],"country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.039306640625,\n              37.01132594307015\n            ],\n            [\n              -102.06298828125,\n              37.01132594307015\n            ],\n            [\n              -102.06298828125,\n              41.00477542222947\n            ],\n            [\n              -109.039306640625,\n              41.00477542222947\n            ],\n            [\n              -109.039306640625,\n              37.01132594307015\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499fe4b07f02db5bd219","contributors":{"authors":[{"text":"Elliott, J. G.","contributorId":45341,"corporation":false,"usgs":true,"family":"Elliott","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":197315,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeFeyter, K. L.","contributorId":53425,"corporation":false,"usgs":true,"family":"DeFeyter","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197316,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25887,"text":"wri844119 - 1986 - Geohydrology and potential for artificial recharge in the western part of the U.S. Marine Corps Base, Twentynine Palms, California, 1982-83","interactions":[],"lastModifiedDate":"2018-02-14T17:30:40","indexId":"wri844119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"84-4119","title":"Geohydrology and potential for artificial recharge in the western part of the U.S. Marine Corps Base, Twentynine Palms, California, 1982-83","docAbstract":"<p>A recent gravity survey indicates that sedimentary deposits in the Deadman Lake area of the Twentynine Palms Marine Corps Base, California, are as much as 10,500 feet thick. These deposits fill an ancient valley in the bedrock complex. This valley is alined east-west in the Surprise Spring area and north-south in the Deadman Lake area.</p><p>Water levels in the Ames Dry Lake area of the Surprise Spring subbasin have changed little between earliest measurements in 1952-53 and in 1982. Water levels in three Marine Corps Base supply wells in the same subbasin near Surprise Spring declined an average of 78 feet during the past 30 years. Water levels in the same timespan in Deadman subbasin and water quality in the base supply wells, drilled in 1952-53 and 1978, have remained virtually unchanged.</p><p>Ground water in storage, suitable for domestic use, in the top 200 feet of saturated sediments in Surprise Spring subbasin was estimated to be 810,000 acre-feet in the early 1950's. About 60,000 acre-feet of this has been removed, mostly for use at the Marine Corps Base, which leaves about 750,000 acre-feet of recoverable water of good quality still stored in the 200-foot interval considered. For planning purposes, it would be safe to use a conservative figure of 300,000 acre-feet for storage in the Deadman subbasin, which contains water having fluoride concentrations greater than the U.S. Environmental Protection Agency's standards for drinking water.</p><p>Three sites in the general area of the present well fields seem favorable for recharging the ground-water system in the Surprise Spring subbasin. Further exploration of these sites is suggested.</p>","language":"English","publisher":"U.S.Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/wri844119","collaboration":"Prepared in cooperation with the U.S. Marine Corps, Department of the Navy","usgsCitation":"Akers, J.P., 1986, Geohydrology and potential for artificial recharge in the western part of the U.S. Marine Corps Base, Twentynine Palms, California, 1982-83: U.S. Geological Survey Water-Resources Investigations Report 84-4119, Report: iv, 18 p.; 2 Plates: 32.07 x 35.21 inches and 32.18 x 34.70 inches, https://doi.org/10.3133/wri844119.","productDescription":"Report: iv, 18 p.; 2 Plates: 32.07 x 35.21 inches and 32.18 x 34.70 inches","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":54649,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4119/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Ground-water-level contours, 1982; well locations, and potential recharge areas; U.S. Marine Corps Base, Twentynine Palms, California"},{"id":54650,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4119/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120070,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4119/report-thumb.jpg"},{"id":54648,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4119/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Configuration of surface on bedrock complex at base of sediments, and area used for estimating ground-water storage, U.S. Marine Corps Base, Twentynine Palms, California"}],"country":"United States","state":"California","city":"Twentynine Palms","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.5,\n              34.5\n            ],\n            [\n              -116.2,\n              34.5\n            ],\n            [\n              -116,\n              34.25\n            ],\n            [\n              -116,\n              34.08333\n            ],\n            [\n              -116.25,\n              34.08333\n            ],\n            [\n              -116.25,\n              34.16667\n            ],\n            [\n              -116.5,\n              34.16667\n            ],\n            [\n              -116.5,\n              34.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8cac","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195425,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26955,"text":"wri854118 - 1986 - Hydraulic geometry and streamflow of channels in the Piceance Basin, Rio Blanco and Garfield Counties, Colorado","interactions":[],"lastModifiedDate":"2023-01-05T20:44:28.001337","indexId":"wri854118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4118","title":"Hydraulic geometry and streamflow of channels in the Piceance Basin, Rio Blanco and Garfield Counties, Colorado","docAbstract":"<p>The influence of streamflow and basin characteristics on channel geometry was investigated at 18 perennial and ephemeral stream reaches in the Piceance basin of northwestern Colorado. Results of stepwise multiple regression analyses indicated that the variabilities of mean bankfull depth (D) and bankfull cross-sectional flow area (Af) were predominantly a function of bankfull discharge (QB), and that most of the variability in channel slopes (S) could be explained by drainage area (DA). None of the independent variables selected for the study could account for a large part of the variability in bankfull channel width (W).&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854118","usgsCitation":"Elliott, J.G., and Cartier, K.D., 1986, Hydraulic geometry and streamflow of channels in the Piceance Basin, Rio Blanco and Garfield Counties, Colorado: U.S. Geological Survey Water-Resources Investigations Report 85-4118, iv, 28 p., https://doi.org/10.3133/wri854118.","productDescription":"iv, 28 p.","costCenters":[],"links":[{"id":411450,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36283.htm","linkFileType":{"id":5,"text":"html"}},{"id":55841,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4118/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123093,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4118/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Garfiled County, Rio Blanco County","otherGeospatial":"Piceance basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.667,\n              39.316\n            ],\n            [\n              -107.771,\n              39.316\n            ],\n            [\n              -107.771,\n              40.167\n            ],\n            [\n              -108.667,\n              40.167\n            ],\n            [\n              -108.667,\n              39.316\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a286","contributors":{"authors":[{"text":"Elliott, J. G.","contributorId":45341,"corporation":false,"usgs":true,"family":"Elliott","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":197311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cartier, K. D.","contributorId":9236,"corporation":false,"usgs":true,"family":"Cartier","given":"K.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":197310,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25889,"text":"wri854178 - 1986 - Ground water in the Long Meadow area and its relation with that in the General Sherman Tree area, Sequoia National Park, California","interactions":[],"lastModifiedDate":"2018-02-15T12:01:33","indexId":"wri854178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4178","title":"Ground water in the Long Meadow area and its relation with that in the General Sherman Tree area, Sequoia National Park, California","docAbstract":"<p>Westward movement of ground water from the Long Meadow area of Sequoia National Park, California, to the General Sherman Tree area is prevented by an eastward hydraulic gradient and low fracture permeability of a granodiorite ridge separating the two areas. Clay beds present in the alluvium in the Long Meadow area would hinder, but not preclude, recharge to the ground-water system beneath Long Meadow from streams. </p><p>A dependable ground-water supply of about 50 gallons per minute (72,000 gallons per day) can be developed from the Long Meadow area. The withdrawal of this quantity of ground water from the Long Meadow area should not affect ground or surface water in the General Sherman Tree area. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/wri854178","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Akers, J.P., 1986, Ground water in the Long Meadow area and its relation with that in the General Sherman Tree area, Sequoia National Park, California: U.S. Geological Survey Water-Resources Investigations Report 85-4178, Report: iv, 15 p.; 1 Plate: 20.19 x 17.62 inches, https://doi.org/10.3133/wri854178.","productDescription":"Report: iv, 15 p.; 1 Plate: 20.19 x 17.62 inches","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":121514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4178/report-thumb.jpg"},{"id":54651,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4178/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Long Meadow Area, Sequoia National Park, California, showing locations of test-hole, stream-measuring, and water-sampling sites"},{"id":54652,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4178/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Sequoia National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.75456809997559,\n              36.572319932849254\n            ],\n            [\n              -118.71500015258789,\n              36.572319932849254\n            ],\n            [\n              -118.71500015258789,\n              36.599542913631645\n            ],\n            [\n              -118.75456809997559,\n              36.599542913631645\n            ],\n            [\n              -118.75456809997559,\n              36.572319932849254\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d999","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26216,"text":"wri864007 - 1986 - Regionalization of winter low-flow characteristics of Tennessee streams","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri864007","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4007","title":"Regionalization of winter low-flow characteristics of Tennessee streams","docAbstract":"Procedures were developed for estimating winter (December-April) low flows at ungaged stream sites in Tennessee based on surface geology and drainage area size. One set of equations applies to West Tennessee streams, and another set applies to Middle and East Tennessee streams. The equations do not apply to streams where flow is significantly altered by the activities of man. Standard errors of estimate of equations for West Tennessee are 22% - 35% and for middle and East Tennessee 31% - 36%. Statistical analyses indicate that summer low-flow characteristics are the same as annual low-flow characteristics, and that winter low flows are larger than annual low flows. Streamflow-recession indexes, in days per log cycle of decrease in discharge, were used to account for effects of geology on low flow of streams. The indexes in Tennessee range from 32 days/log cycle for clay and shale to 350 days/log cycle for gravel and sand, indicating different aquifer characteristics of the geologic units that contribute to streamflows during periods of no surface runoff. Streamflow-recession rate depends primarily on transmissivity and storage characteristics of the aquifers, and the average distance from stream channels to basin divides. Geology and drainage basin size are the most significant variables affecting low flow in Tennessee streams according to regression analyses. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864007","usgsCitation":"Bingham, R., 1986, Regionalization of winter low-flow characteristics of Tennessee streams: U.S. Geological Survey Water-Resources Investigations Report 86-4007, v, 88 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864007.","productDescription":"v, 88 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4007/report-thumb.jpg"},{"id":55012,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4007/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55013,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4007/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55014,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602d47","contributors":{"authors":[{"text":"Bingham, R.H.","contributorId":37301,"corporation":false,"usgs":true,"family":"Bingham","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":195999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58818,"text":"mf1885 - 1986 - Preliminary geologic map of the Bear Hole Quadrangle, Big Horn County, Montana, and Big Horn and Sheridan counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:16","indexId":"mf1885","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"1885","title":"Preliminary geologic map of the Bear Hole Quadrangle, Big Horn County, Montana, and Big Horn and Sheridan counties, Wyoming","language":"ENGLISH","doi":"10.3133/mf1885","usgsCitation":"Agard, S., 1986, Preliminary geologic map of the Bear Hole Quadrangle, Big Horn County, Montana, and Big Horn and Sheridan counties, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 1885, 1 map ;58 x 41 cm., on sheet 71 x 74 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1885.","productDescription":"1 map ;58 x 41 cm., on sheet 71 x 74 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":106249,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7766.htm","linkFileType":{"id":5,"text":"html"},"description":"7766"},{"id":184581,"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\": [ [ [ -108,45 ], [ -108,45.1175 ], [ -107.86749999999999,45.1175 ], [ -107.86749999999999,45 ], [ -108,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bd22","contributors":{"authors":[{"text":"Agard, S.S.","contributorId":28668,"corporation":false,"usgs":true,"family":"Agard","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":260902,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25686,"text":"wri864075 - 1986 - Occurrence and availability of ground water in the Athens region, northeastern Georgia","interactions":[],"lastModifiedDate":"2017-01-24T12:01:42","indexId":"wri864075","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4075","title":"Occurrence and availability of ground water in the Athens region, northeastern Georgia","docAbstract":"A study was conducted to assess the occurrence and availability of groundwater in the crystalline rocks of the Piedmont area in northeastern Georgia and to determine whether groundwater is a viable alternative or supplemental source for industrial, public and private supplies. The area is underlain by a variety of metamorphic and igneous rocks. The quantity of water that a rock unit can supply to wells is determined by the number, capacity, and interconnection of the secondary openings. Of an estimated 10,000 successful wells drilled in the Athens Region, 972 wells are reported by drilling contractors to supply from 20 to 300 gal/min. Studies of well sites revealed that high yielding wells can be developed only where the water bearing units have undergone significant increases in secondary permeability. This occurs mainly in association with (1) contact zones between rock units of contrasting character, (2) contact zones within multilayered rock units, (3) fault zones, (4) stress-relief fractures, and (5) shear zones. Groundwater may be a viable alternative or supplemental source for industrial, public, and private supplies in much of the Athens Region. In 1980, groundwater made up 38% (18 million gal/day) of the total water used in the area. Yields of 20 to more than 200 gal/min are obtained from wells throughout most of the region, and the water is generally of good chemical quality and is suitable for drinking and many other uses. Concentrations of dissolved constituents are fairly consistent throughout the area. Except for iron, manganese, and fluoride, dissolved constituents rarely exceed drinking water standards. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864075","usgsCitation":"Radtke, D.B., Cressler, C., Perlman, H., Blanchard, H., McFadden, K., and Brooks, R., 1986, Occurrence and availability of ground water in the Athens region, northeastern Georgia: U.S. Geological Survey Water-Resources Investigations Report 86-4075, v, 79 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864075.","productDescription":"v, 79 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":54448,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4075/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54449,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4075/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123390,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4075/report-thumb.jpg"}],"country":"United States","state":"Georgia","city":"Athens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.5013427734375,\n              32.89342578969234\n            ],\n            [\n              -84.5013427734375,\n              34.63772760271713\n            ],\n            [\n              -81.93603515625,\n              34.63772760271713\n            ],\n            [\n              -81.93603515625,\n              32.89342578969234\n            ],\n            [\n              -84.5013427734375,\n              32.89342578969234\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649606","contributors":{"authors":[{"text":"Radtke, D. B.","contributorId":72821,"corporation":false,"usgs":true,"family":"Radtke","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":194660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cressler, C.W.","contributorId":37302,"corporation":false,"usgs":true,"family":"Cressler","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":194658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Perlman, H.A.","contributorId":84406,"corporation":false,"usgs":true,"family":"Perlman","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":194661,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blanchard, H.E. Jr.","contributorId":57888,"corporation":false,"usgs":true,"family":"Blanchard","given":"H.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":194659,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McFadden, K.W.","contributorId":22766,"corporation":false,"usgs":true,"family":"McFadden","given":"K.W.","email":"","affiliations":[],"preferred":false,"id":194657,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brooks, Rebekah","contributorId":6457,"corporation":false,"usgs":true,"family":"Brooks","given":"Rebekah","email":"","affiliations":[],"preferred":false,"id":194656,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":26215,"text":"wri854191 - 1986 - Regionalization of low-flow characteristics of Tennessee streams","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri854191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4191","title":"Regionalization of low-flow characteristics of Tennessee streams","docAbstract":"Procedures for estimating 3-day 2-year, 3-day 10-year, 3-day 20-year, and 7-day 10-year low flows at ungaged stream sites in Tennessee are based on surface geology and drainage area size. One set of equations applies to west Tennessee streams, and another set applies to central and east Tennessee streams. The equations do not apply to streams where flow is significantly altered by activities of man. Standard errors of estimate of equations for west Tennessee are 24 to 32% and for central and east Tennessee 31 to 35%. Streamflow recession indexes, in days/log cycle, are used to account for effects of geology of the drainage basin on low flow of streams. The indexes in Tennessee range from 32 days/log cycle for clay and shale to 350 days/log cycle for gravel and sand, indicating different aquifer characteristics of the geologic units that sustain streamflows during periods of no surface runoff. Streamflow recession rate depends primarily on transmissivity and storage characteristics of the aquifers, and the average distance from stream channels to basin divides. Geology and drainage basin size are the most significant variables affecting low flow in Tennessee streams according to regression analyses. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854191","usgsCitation":"Bingham, R., 1986, Regionalization of low-flow characteristics of Tennessee streams: U.S. Geological Survey Water-Resources Investigations Report 85-4191, iv, 63 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854191.","productDescription":"iv, 63 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2110,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri85-4191","linkFileType":{"id":5,"text":"html"}},{"id":158058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":55010,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4191/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55011,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4191/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c41f","contributors":{"authors":[{"text":"Bingham, R.H.","contributorId":37301,"corporation":false,"usgs":true,"family":"Bingham","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":195998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14979,"text":"ofr86256 - 1986 - Magnetic tape format for the USGS ocean bottom seismometer","interactions":[],"lastModifiedDate":"2020-07-16T18:08:27.900984","indexId":"ofr86256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-256","title":"Magnetic tape format for the USGS ocean bottom seismometer","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86256","usgsCitation":"Miller, G., and Dodd, J.E., 1986, Magnetic tape format for the USGS ocean bottom seismometer: U.S. Geological Survey Open-File Report 86-256, i, 9 p., https://doi.org/10.3133/ofr86256.","productDescription":"i, 9 p.","costCenters":[],"links":[{"id":148143,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0256/report-thumb.jpg"},{"id":43789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0256/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649384","contributors":{"authors":[{"text":"Miller, G.K.","contributorId":43793,"corporation":false,"usgs":true,"family":"Miller","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":170360,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dodd, J. E.","contributorId":57867,"corporation":false,"usgs":true,"family":"Dodd","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":170361,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}