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This report contains discharge records of 109 gaging stations; stage for 11 gaging stations; stage and contents for 18 lakes and reservoirs; water quality for 109 continuing-record stations; peak stage and discharge only for 121 crest-stage partial-record stations and 6 miscellaneous sites; and water levels of 27 observation wells. 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 Georgia.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrGA851","collaboration":"Prepared in cooperation with the State of Georgia and with other agencies","usgsCitation":"Stokes, W., Hale, T., Pearman, J., and Buell, G.R., 1986, Water resources data for Georgia, water year 1985: U.S. Geological Survey Water Data Report GA-85-1, ix, 389 p., https://doi.org/10.3133/wdrGA851.","productDescription":"ix, 389 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":181632,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/ga-85-1/report-thumb.jpg"},{"id":494964,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/ga-85-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":57619,"text":"wdrFL863B - 1986 - Water resources data, Florida, water year 1986. Volume 3B. Southwest Florida-ground water","interactions":[],"lastModifiedDate":"2024-06-05T21:57:41.342303","indexId":"wdrFL863B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"FL-86-3B","title":"Water resources data, Florida, water year 1986. Volume 3B. Southwest Florida-ground water","docAbstract":"<p>Water resources data for the 1986 water year in Florida consist of continuous or daily discharge for 277 streams, periodic discharge for 38 streams, miscellaneous discharge for 34 streams, continuous or daily stage for 77 streams, periodic stage for 20 streams, peak discharge for 88 streams and peak stage for 69 streams; continuous or daily elevations for 69 lakes, periodic elevations for 72 lakes; continuous ground-water levels for 476 wells, periodic ground-water levels for 1226 wells, and miscellaneous water-level measurements for 1570 wells; quality-of-water data for 188 surface-water sites and 878 wells.</p><p>The data for southwest Florida include continuous or daily discharge for 85 streams, periodic discharge for 21 streams, miscellaneous discharge for 7 streams, continuous or daily stage for 26 streams, periodic stage for 10 streams, peak discharge for 20 streams, and peak stage for 1 stream; continuous elevations for 30 lakes and periodic elevations for 28 lakes; continuous ground-water levels for 25 wells, periodic ground-water levels for 146 wells, and miscellaneous water-level measurements for 722 wells; quality-of-water for 106 surface-water sites and 265 wells.</p><p>These data represent the National Water Data System records collected by the U. S. Geological Survey and cooperating local, state and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL863B","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Fletcher, W., Ogle, J., Oberg, J., and Todd, J., 1986, Water resources data, Florida, water year 1986. Volume 3B. Southwest Florida-ground water: U.S. Geological Survey Water Data Report FL-86-3B, viii, 343 p., https://doi.org/10.3133/wdrFL863B.","productDescription":"viii, 343 p.","costCenters":[],"links":[{"id":429530,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1986/fl-86-3-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181318,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1986/fl-86-3-b/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"southwest Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -83.09853431437669,\n              29.462315841167396\n            ],\n            [\n              -83.09853431437669,\n              26.894131530979593\n            ],\n            [\n              -81.81108718826917,\n              26.894131530979593\n            ],\n            [\n              -81.81108718826917,\n              29.462315841167396\n            ],\n            [\n              -83.09853431437669,\n              29.462315841167396\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fcfda","contributors":{"authors":[{"text":"Fletcher, W.L.","contributorId":97977,"corporation":false,"usgs":true,"family":"Fletcher","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":257530,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ogle, J.K.","contributorId":8898,"corporation":false,"usgs":true,"family":"Ogle","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":257527,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oberg, J.L.","contributorId":54669,"corporation":false,"usgs":true,"family":"Oberg","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":257529,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Todd, J.M.","contributorId":11280,"corporation":false,"usgs":true,"family":"Todd","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":257528,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":57613,"text":"wdrFL853A - 1986 - Water resources data, Florida, water year 1985. Volume 3A: Southwest Florida - surface water","interactions":[],"lastModifiedDate":"2024-07-26T22:35:56.853774","indexId":"wdrFL853A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"FL-85-3A","title":"Water resources data, Florida, water year 1985. Volume 3A: Southwest Florida - surface water","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey, in cooperation with State agencies, obtains a large amount of data pertaining to the water resources of Florida each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled \"Water Resources Data - Florida.\"</p><p>This report series includes records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs, and water levels and water quality of groundwater wells. This volume contains records for continuous daily discharge at 91 gaging stations; periodic discharge at 23 stream sites; miscellaneous discharge at 57 stream sites; continuous daily stage at 30 stream sites; periodic stage at 10 stream sites; peak discharge at 20 stream sites; peak stage at 1 stream site; continuous daily elevations at 50 lakes; periodic elevations at 39 lakes; water quality at 146 surface-water sites and 287 ground-water sites; continuous ground-water elevations at 223 wells; periodic ground-water elevations at 146 wells; and miscellaneous ground-water elevations at 1,477 wells. Locations of these sites are shown on figure 1. 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 Florida.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL853A","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Mycyk, R., Fayard, L., Fletcher, W., and Ogle, J., 1986, Water resources data, Florida, water year 1985. Volume 3A: Southwest Florida - surface water: U.S. Geological Survey Water Data Report FL-85-3A, xiii, 402 p., https://doi.org/10.3133/wdrFL853A.","productDescription":"xiii, 402 p.","costCenters":[],"links":[{"id":431532,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/fl-85-3-a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181629,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/fl-85-3-a/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"southwest Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -83.21925655621072,\n              28.74916638707282\n            ],\n            [\n              -83.21925655621072,\n              26.44946642032781\n            ],\n            [\n              -81.58382669186231,\n              26.44946642032781\n            ],\n            [\n              -81.58382669186231,\n              28.74916638707282\n            ],\n            [\n              -83.21925655621072,\n              28.74916638707282\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd008","contributors":{"authors":[{"text":"Mycyk, R.T.","contributorId":32566,"corporation":false,"usgs":true,"family":"Mycyk","given":"R.T.","affiliations":[],"preferred":false,"id":257513,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fayard, L.D.","contributorId":46571,"corporation":false,"usgs":true,"family":"Fayard","given":"L.D.","affiliations":[],"preferred":false,"id":257514,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fletcher, W.L.","contributorId":97977,"corporation":false,"usgs":true,"family":"Fletcher","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":907099,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ogle, J.K.","contributorId":8898,"corporation":false,"usgs":true,"family":"Ogle","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":257512,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":59958,"text":"mf1235B - 1986 - Complete Bouguer gravity and aeromagnetic maps of the Rattlesnake Roadless Area, Missoula County, Montana","interactions":[],"lastModifiedDate":"2016-08-22T15:18:28","indexId":"mf1235B","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":"1235","chapter":"B","title":"Complete Bouguer gravity and aeromagnetic maps of the Rattlesnake Roadless Area, Missoula County, Montana","docAbstract":"<p>The Rattlesnake Roadless Area was identified by the U.S. Forest Service as a possible addition to the Wilderness System. &nbsp;This 120 square mile area is north of Missoula, Mont. (see index map); Rattlesnake Creek forms the major drainage to the south.</p>\n<p>The rocks in the study area consist mainly of the Helena Formation and the Missoula Group of the Belt Supergroup (Proterozoic Y). &nbsp;Rock units of less importance are diabase sills and dikes of probable Proterozoic Z age, Middle Cambrian rocks, and glacial deposits. &nbsp;Structurally, the study area consists of the Rattlesnake thrust system in the south part and a parautochthonous area broken by vertical faults in the north part.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1235B","isbn":"0607807563","usgsCitation":"Kulik, D.M., 1986, Complete Bouguer gravity and aeromagnetic maps of the Rattlesnake Roadless Area, Missoula County, Montana: U.S. Geological Survey Miscellaneous Field Studies Map 1235, 51.33 x 33.45 inches, https://doi.org/10.3133/mf1235B.","productDescription":"51.33 x 33.45 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1235B.PNG"},{"id":327318,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1235-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"50000","country":"United States","state":"Montana","county":"Missoula County","otherGeospatial":"Rattlesnake Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,46.8675 ], [ -114,47.1175 ], [ -113.75,47.1175 ], [ -113.75,46.8675 ], [ -114,46.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ce4b07f02db6a9587","contributors":{"authors":[{"text":"Kulik, Dolores M.","contributorId":83091,"corporation":false,"usgs":true,"family":"Kulik","given":"Dolores","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":262900,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57610,"text":"wdrFL843B - 1986 - Water resources data, Florida, water year 1984. Volume 3B: Southwest Florida - surface water","interactions":[],"lastModifiedDate":"2024-05-15T19:53:22.462992","indexId":"wdrFL843B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"FL-84-3B","title":"Water resources data, Florida, water year 1984. Volume 3B: Southwest Florida - surface water","docAbstract":"<p>Water resources data for the 1984 water year in Florida consist of continuous or daily discharge for 251 streams, periodic discharge for 32 streams, miscellaneous discharge for 43 streams, continuous or daily stage for 92 streams, periodic stage for 31 streams, peak discharge for 60 streams and peak stage for 37 streams; continuous or daily elevations for 73 lakes, periodic elevations for 82 lakes; continuous ground-water levels for 467 wells, periodic ground-water levels for 539 wells, and miscellaneous water-level measurements for 2,039 wells; quality-of-water data for 200 surface-water sites and 596 wells.</p><p>The data for southwest Florida include continuous or daily discharge for 81 streams, periodic discharge for 15 streams, miscellaneous discharge for 14 streams, peak discharge for 20 streams, continuous or daily stage for 31 streams; continuous elevations for 30 lakes and periodic elevations for 43 lakes; continuous ground-water levels for 231 wells, periodic ground-water levels for 199 wells, and miscellaneous water-level measurements for 799 wells; quality of water for 117 surface-water sites and 289 wells.</p><p>These data represent the National Water Data System records collected by the U. S. Geological Survey and cooperating local, state and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL843B","collaboration":"Prepared in cooperation with the state of Florida and other agencies","usgsCitation":"Mycyk, R., Fayard, L., Fletcher, W., and Ogle, J., 1986, Water resources data, Florida, water year 1984. Volume 3B: Southwest Florida - surface water: U.S. Geological Survey Water Data Report FL-84-3B, ix, 336 p., https://doi.org/10.3133/wdrFL843B.","productDescription":"ix, 336 p.","costCenters":[],"links":[{"id":428751,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/fl-84-3-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181626,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/fl-84-3-b/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Southwest Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.9532582609722,\n              29.151564992353073\n            ],\n            [\n              -82.9532582609722,\n              27.094826423263882\n            ],\n            [\n              -81.56491220628033,\n              27.094826423263882\n            ],\n            [\n              -81.56491220628033,\n              29.151564992353073\n            ],\n            [\n              -82.9532582609722,\n              29.151564992353073\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd01d","contributors":{"authors":[{"text":"Mycyk, R.T.","contributorId":32566,"corporation":false,"usgs":true,"family":"Mycyk","given":"R.T.","affiliations":[],"preferred":false,"id":257502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fayard, L.D.","contributorId":46571,"corporation":false,"usgs":true,"family":"Fayard","given":"L.D.","affiliations":[],"preferred":false,"id":257503,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fletcher, W.L.","contributorId":97977,"corporation":false,"usgs":true,"family":"Fletcher","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":257504,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ogle, J.K.","contributorId":8898,"corporation":false,"usgs":true,"family":"Ogle","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":257501,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":57609,"text":"wdrFL842B - 1986 - Water resources data, Florida, water year 1984. Volume 2B. South Florida ground water","interactions":[],"lastModifiedDate":"2024-05-15T19:39:12.555314","indexId":"wdrFL842B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"FL-84-2B","title":"Water resources data, Florida, water year 1984. Volume 2B. South Florida ground water","docAbstract":"<p>Water resources data for the 1984 water year in Florida consists of continuous or daily discharge for 251 streams, periodic discharge for 32 streams, miscellaneous discharge for 43 stream, continuous or daily stage for 92 streams, periodic stage for 31 streams, peak discharge for 60 streams, and peak stage for 37 streams; continuous or daily elevations for 73 lakes, periodic elevations for 82 lakes; continuous ground water levels for 467 wells, and periodic ground water levels for 539 wells; and miscellaneous water level measurement for 2,039 wells; quality of water data for 200 surface water sites and 596 wells.</p><p>The data for south Florida includes continuous or daily discharge for 74 streams, periodic discharge for 2 streams, peak discharge for 2 streams, continuous or daily stage for 76 streams, and periodic stage for 29 streams; continuous elevation for 18 lakes and periodic elevations for 5 lakes; continuous ground water levels for 180 wells, periodic ground water levels for 130 wells, and miscellaneous water level measurements for 360 wells; quality of water for 40 surface water sites and for 310 wells.</p><p>These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, state, and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL842B","collaboration":"Prepared in cooperation with the State of Florida and other agencies.","usgsCitation":"Haire, W., Price, C., and Sonenshein, R., 1986, Water resources data, Florida, water year 1984. Volume 2B. South Florida ground water: U.S. Geological Survey Water Data Report FL-84-2B, viii, 373 p., https://doi.org/10.3133/wdrFL842B.","productDescription":"viii, 373 p.","costCenters":[],"links":[{"id":428746,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/fl-84-2-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181625,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/fl-84-2-b/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"South Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.40791292493894,\n              27.885758231914238\n            ],\n            [\n              -82.40791292493894,\n              24.79916690623361\n            ],\n            [\n              -79.81507461368825,\n              24.79916690623361\n            ],\n            [\n              -79.81507461368825,\n              27.885758231914238\n            ],\n            [\n              -82.40791292493894,\n              27.885758231914238\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd015","contributors":{"authors":[{"text":"Haire, W.J.","contributorId":47341,"corporation":false,"usgs":true,"family":"Haire","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":257499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, C.","contributorId":12910,"corporation":false,"usgs":true,"family":"Price","given":"C.","affiliations":[],"preferred":false,"id":257498,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sonenshein, R.","contributorId":71251,"corporation":false,"usgs":true,"family":"Sonenshein","given":"R.","email":"","affiliations":[],"preferred":false,"id":257500,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":12719,"text":"ofr86102 - 1986 - Stratigraphic Analysis Techniques System (STRATS) user's manual","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr86102","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":"86-102","title":"Stratigraphic Analysis Techniques System (STRATS) user's manual","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86102","usgsCitation":"Boger, L., 1986, Stratigraphic Analysis Techniques System (STRATS) user's manual: U.S. Geological Survey Open-File Report 86-102, 24 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86102.","productDescription":"24 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":145720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0102/report-thumb.jpg"},{"id":41132,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0102/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b10f2","contributors":{"authors":[{"text":"Boger, L.W.","contributorId":58648,"corporation":false,"usgs":true,"family":"Boger","given":"L.W.","affiliations":[],"preferred":false,"id":166597,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57608,"text":"wdrFL841A - 1986 - Water resources data, Florida, water year 1984. Volume 1A: Northeast Florida - surface water","interactions":[],"lastModifiedDate":"2024-06-05T22:00:38.759141","indexId":"wdrFL841A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"FL-84-1A","title":"Water resources data, Florida, water year 1984. Volume 1A: Northeast Florida - surface water","docAbstract":"<p>Water resources data for the 1984 water year in Florida consist of continuous or daily discharge for 251 streams, periodic discharge for 32 streams, miscellaneous discharge for 43 streams, continuous or daily stage for 92 streams, periodic stage for 31 streams, peak discharge for 60 streams and peak stage for 37 streams; continuous or daily elevations for 73 lakes, periodic elevations for 82 lakes; continuous ground-water levels for 467 wells, periodic ground-water levels for 539 wells, and miscellaneous water-level measurements for 2,039 wells; quality-of-water data for 200 surface-water sites and 596 wells.</p><p>The data for northeast Florida include continuous or daily discharge for 65 streams, periodic discharge for 7 streams, miscellaneous discharge for 21 streams, continuous or daily stage for 37 streams, peak discharge for 15 streams and peak stage for 8 streams; continuous or daily elevations for 22 lakes, periodic elevations for 33 lakes; continuous ground-water levels for 31 wells, periodic ground-water levels for 90 wells, and miscellaneous water-level measurements for 563 wells; quality-of-water data for 15 surface-water sites and 45 wells.</p><p>These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, state and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL841A","collaboration":"Prepared in cooperation with the State of Florida and other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Water resources data, Florida, water year 1984. Volume 1A: Northeast Florida - surface water: U.S. Geological Survey Water Data Report FL-84-1A, xiii, 227 p., https://doi.org/10.3133/wdrFL841A.","productDescription":"xiii, 227 p.","costCenters":[],"links":[{"id":181624,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/fl-84-1-a/report-thumb.jpg"},{"id":429531,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/fl-84-1-a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"northeast Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.87053199169145,\n              30.59386571948582\n            ],\n            [\n              -81.87053199169145,\n              28.20717152179637\n            ],\n            [\n              -79.98790000108694,\n              28.20717152179637\n            ],\n            [\n              -79.98790000108694,\n              30.59386571948582\n            ],\n            [\n              -81.87053199169145,\n              30.59386571948582\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd013","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":533162,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57606,"text":"wdrFL841B - 1986 - Water resources data for Florida, water year 1984. Volume 1B: Northeast Florida - Ground water","interactions":[],"lastModifiedDate":"2024-05-14T16:38:09.408109","indexId":"wdrFL841B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"FL-84-1B","title":"Water resources data for Florida, water year 1984. Volume 1B: Northeast Florida - Ground water","docAbstract":"<p>Water resources data for the 1984 water year in Florida consist of continuous or daily discharge for 251 streams, periodic discharge for 32 streams, miscellaneous discharge for 43 streams, continuous or daily stage for 92 streams, periodic stage for 31 streams, peak discharge for 60 streams and peak stage for 37 streams; continuous or daily elevations for 73 lakes, periodic elevations for 82 lakes; continuous ground-water levels for 467 wells, periodic ground-water levels for 539 wells, and miscellaneous water-level measurements for 2,039 wells; quality-of-water data for 200 surface-water sites and 596 wells.</p><p>The data for northeast Florida include continuous or daily discharge for 65 streams, periodic discharge for 7 streams, miscellaneous discharge for 21 streams, continuous or daily stage for 37 streams, peak discharge for 15 streams and peak stage for 8 streams; continuous or daily elevations for 22 lakes, periodic elevations for 33 lakes; continuous ground-water levels for 31 wells, periodic ground-water levels for 90 wells, and miscellaneous water-level measurements for 563 wells; quality-of-water data for 15 surface-water sites and 45 wells.</p><p>These data represent the National Water Data System records collected by the U. S. Geological Survey and cooperating local, state and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL841B","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Water resources data for Florida, water year 1984. Volume 1B: Northeast Florida - Ground water: U.S. Geological Survey Water Data Report FL-84-1B, ix, 168 p., https://doi.org/10.3133/wdrFL841B.","productDescription":"ix, 168 p.","costCenters":[],"links":[{"id":428697,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/fl-84-1-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181516,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/fl-84-1-b/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Northeast Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.41501449894756,\n              30.690995437172703\n            ],\n            [\n              -82.41501449894756,\n              28.78769532384071\n            ],\n            [\n              -80.69718200343857,\n              28.78769532384071\n            ],\n            [\n              -80.69718200343857,\n              30.690995437172703\n            ],\n            [\n              -82.41501449894756,\n              30.690995437172703\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd034","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":533161,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61558,"text":"mf1183J - 1986 - Geochemical maps showing distribution and abundance of manganese in two fractions of stream-sediment concentrates, Silver City 1 degree by 2 degrees Quadrangle, New Mexico and Arizona","interactions":[],"lastModifiedDate":"2016-08-23T10:45:06","indexId":"mf1183J","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":"1183","chapter":"J","title":"Geochemical maps showing distribution and abundance of manganese in two fractions of stream-sediment concentrates, Silver City 1 degree by 2 degrees Quadrangle, New Mexico and Arizona","docAbstract":"<p><span>These maps (Maps A and B) show the distribution and abundance of&nbsp;maganese in the nonmagnetic and magnetic fractions&nbsp;of heavy-mineral concentrates from stream sediments collected in the Silver City 1</span><sup><span>o</span></sup><span>&nbsp;x 2</span><span><sup>o</sup>&nbsp;</span><span>quadrangle, New Mexico and Arizona. Geochemical maps showing the distribution and abundance of 10 other selected key elements and the mineral fluorite in the Silver City quadrangle are also part of this folio (Watts and Hassemer, 1980; Watts and others 1986a-i). These maps contribute to the assessment of mineral resources within Silver City&nbsp;1</span><sup><span>o</span></sup><span>&nbsp;x 2</span><span><sup>o</sup>&nbsp;</span><span>quadrangle by (1) showing regional patterns of elements enriched in heavy-mineral concentrates, thereby providing clues to regional patterns of mineralization; (2) showing new areas containing enriched metals, not previously known from mining activity; and (3) providing supportive data to the interpretive and summary maps (Watts and Hassmer, 1986) and the mineral resource assessment (Richter and others, 1983). Background information that pertains to published components of the Silver City Folio is also available (Richter and others, in press).&nbsp;</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1183J","usgsCitation":"Watts, K., Hassemer, J.R., Forn, C.L., and Siems, D.F., 1986, Geochemical maps showing distribution and abundance of manganese in two fractions of stream-sediment concentrates, Silver City 1 degree by 2 degrees Quadrangle, New Mexico and Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1183, 45.30 x 39.71 inches, https://doi.org/10.3133/mf1183J.","productDescription":"45.30 x 39.71 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1183J.PNG"},{"id":327618,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1183-J/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Arizona, New Mexico","city":"Silver City","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110,32 ], [ -110,33 ], [ -108,33 ], [ -108,32 ], [ -110,32 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adfd0","contributors":{"authors":[{"text":"Watts, Kenneth C.","contributorId":101180,"corporation":false,"usgs":true,"family":"Watts","given":"Kenneth C.","affiliations":[],"preferred":false,"id":266038,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hassemer, Jerry R.","contributorId":173451,"corporation":false,"usgs":false,"family":"Hassemer","given":"Jerry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":266036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forn, Carl L.","contributorId":173452,"corporation":false,"usgs":false,"family":"Forn","given":"Carl","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":266037,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Siems, David F.","contributorId":100835,"corporation":false,"usgs":true,"family":"Siems","given":"David","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":266039,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29074,"text":"wri844189 - 1986 - Temperature of ground water at Philadelphia, Pennsylvania, 1979- 1981","interactions":[],"lastModifiedDate":"2017-06-20T09:50:00","indexId":"wri844189","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":"84-4189","title":"Temperature of ground water at Philadelphia, Pennsylvania, 1979- 1981","docAbstract":"<p>Anthropogenic heat production has undoubtedly caused increased ground-water temperatures in many parts of Philadelphia, Pennsylvania, as shown by temperatures of 98 samples and logs of 40 wells measured during 1979-81. Most sample temperatures were higher than 12.6 degrees Celsius (the local mean annual air temperature), and many logs depict cooling trends with depth (anomalous gradients). Heating of surface and shallow-subsurface materials has likely caused the elevated temperatures and anomalous gradients. Solar radiation on widespread concrete and asphalt surfaces, fossil-fuel combustion, and radiant losses from buried pipelines containing steam and process chemicals are believed to be the chief sources of heat. Some heat from these and other sources is transferred to deeper zones, mainly by conduction. Temperatures in densely urbanized areas are commonly highest directly beneath the land surface and decrease progressively with depth. Temperatures in sparsely urbanized areas generally follow the natural geothermal gradient and increase downward at about that same rate.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844189","usgsCitation":"Paulachok, G.N., 1986, Temperature of ground water at Philadelphia, Pennsylvania, 1979- 1981: U.S. Geological Survey Water-Resources Investigations Report 84-4189, iv, 14 p., https://doi.org/10.3133/wri844189.","productDescription":"iv, 14 p.","numberOfPages":"20","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":159451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri844189.jpg"},{"id":310283,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4189/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennslyvania","city":"Philadelphia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.2460479736328,\n              39.8607360278182\n            ],\n            [\n              -75.2460479736328,\n              40.06178210817461\n            ],\n            [\n              -75.01739501953125,\n              40.06178210817461\n            ],\n            [\n              -75.01739501953125,\n              39.8607360278182\n            ],\n            [\n              -75.2460479736328,\n              39.8607360278182\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685802","contributors":{"authors":[{"text":"Paulachok, Gary N. gnpaulac@usgs.gov","contributorId":3500,"corporation":false,"usgs":true,"family":"Paulachok","given":"Gary","email":"gnpaulac@usgs.gov","middleInitial":"N.","affiliations":[],"preferred":true,"id":200911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30258,"text":"wri864096 - 1986 - Evaluation of the matrix exponential for use in ground-water-flow and solute-transport simulations; theoretical framework","interactions":[],"lastModifiedDate":"2012-02-02T00:09:02","indexId":"wri864096","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":"86-4096","title":"Evaluation of the matrix exponential for use in ground-water-flow and solute-transport simulations; theoretical framework","docAbstract":"It is possible to obtain analytic solutions to the groundwater flow and solute transport equations if space variables are discretized but time is left continuous. From these solutions, hydraulic head and concentration fields for any future time can be obtained without ' marching ' through intermediate time steps. This analytical approach involves matrix exponentiation and is referred to as the Matrix Exponential Time Advancement (META) method. Two algorithms are presented for the META method, one for symmetric and the other for non-symmetric exponent matrices. A numerical accuracy indicator, referred to as the matrix condition number, was defined and used to determine the maximum number of significant figures that may be lost in the META method computations. The relative computational and storage requirements of the META method with respect to the time marching method increase with the number of nodes in the discretized problem. The potential greater accuracy of the META method and the associated greater reliability through use of the matrix condition number have to be weighed against this increased relative computational and storage requirements of this approach as the number of nodes becomes large. For a particular number of nodes, the META method may be computationally more efficient than the time-marching method, depending on the size of time steps used in the latter. A numerical example illustrates application of the META method to a sample ground-water-flow problem. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864096","usgsCitation":"Umari, A., and Gorelick, S., 1986, Evaluation of the matrix exponential for use in ground-water-flow and solute-transport simulations; theoretical framework: U.S. Geological Survey Water-Resources Investigations Report 86-4096, iv, 33 p. :ill. ;28 cm., https://doi.org/10.3133/wri864096.","productDescription":"iv, 33 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4096/report-thumb.jpg"},{"id":59047,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4096/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa32c","contributors":{"authors":[{"text":"Umari, A.M.","contributorId":96300,"corporation":false,"usgs":true,"family":"Umari","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":202948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gorelick, S.M.","contributorId":21589,"corporation":false,"usgs":true,"family":"Gorelick","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":202947,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26445,"text":"wri864073 - 1986 - General surface- and ground-water quality in a coal-resource area near Durango, southwestern Colorado","interactions":[],"lastModifiedDate":"2023-01-06T21:15:32.451149","indexId":"wri864073","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":"86-4073","title":"General surface- and ground-water quality in a coal-resource area near Durango, southwestern Colorado","docAbstract":"<p>A general description of surface and groundwater quality in a coal-resource area near Durango, southwestern Colorado is given. Dissolved-solids concentrations were less than 1,000 mg/l in streams, except in the Alkali Gulch, Basin Creek, and Carbon Junction Canyon drainage basins. Median concentrations of dissolved boron, iron, manganese, and zinc were less than 35 microg/l; median concentrations of dissolved lead and selenium were less than 1 microg/l.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864073","usgsCitation":"Butler, D.L., 1986, General surface- and ground-water quality in a coal-resource area near Durango, southwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 86-4073, Report: iv, 53 p.; 1 Plate: 46.80 x 19.55 inches, https://doi.org/10.3133/wri864073.","productDescription":"Report: iv, 53 p.; 1 Plate: 46.80 x 19.55 inches","costCenters":[],"links":[{"id":55268,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4073/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118686,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4073/report-thumb.jpg"},{"id":55267,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4073/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":110168,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36529.htm","linkFileType":{"id":5,"text":"html"},"description":"36529"}],"country":"United States","state":"Colorado","city":"Durango","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.25,\n              37.375\n            ],\n            [\n              -108.333,\n              37.375\n            ],\n            [\n              -108.333,\n              37.125\n            ],\n            [\n              -107.25,\n              37.125\n            ],\n            [\n              -107.25,\n              37.375\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6af967","contributors":{"authors":[{"text":"Butler, D. L.","contributorId":36967,"corporation":false,"usgs":true,"family":"Butler","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196403,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61520,"text":"mf1581B - 1986 - Geochemical map of the North Fork John Day River Roadless Area, Grant County, Oregon","interactions":[],"lastModifiedDate":"2016-08-23T10:39:47","indexId":"mf1581B","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":"1581","chapter":"B","title":"Geochemical map of the North Fork John Day River Roadless Area, Grant County, Oregon","docAbstract":"<p><span>The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and submitted to the President&nbsp;and the Congress. This report presents the analytical results of a geochemical survey of the North Fork John Day River Roadless Area&nbsp;(B6253) in the Umatilla and Wallowa-Whitman&nbsp;National Forests, Grant County, Oregon. The North Fork John Day River Roadless Area was classified&nbsp;as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</span></p>\n<p><span>The North Fork John Day River Roadless Area comprised 21,210 acres in the&nbsp;Umatilla and Wallowa-Whitman&nbsp;National Forests, Grant County, Oregon, about 30 miles northwest of Baker, Oregon. The irregularly shaped area extends for about 1 mile on both sides of a 25-mile segment of the North Fork John Day River from Big Creek on the west to North Fork John Day Campground on the east. Most of the roadless area is in the northern half of the Desolation Butte 15-minute quadrangle. The eastern end of the area is in parts of the Granite and Trout Meadows 7&frac12;-minute quadrangles.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1581B","usgsCitation":"Evans, J.G., 1986, Geochemical map of the North Fork John Day River Roadless Area, Grant County, Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1581, 36.58 x 25.48 inches, https://doi.org/10.3133/mf1581B.","productDescription":"36.58 x 25.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":182476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1581b.PNG"},{"id":327606,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1581-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Grant County","otherGeospatial":"North Fork John Day River Roadless Area, Umatilla National Forest, Wallowa-Whitman National Forest","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.66666666666667,44.833333333333336 ], [ -118.66666666666667,45 ], [ -118.41666666666667,45 ], [ -118.41666666666667,44.833333333333336 ], [ -118.66666666666667,44.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae1f7","contributors":{"authors":[{"text":"Evans, James G. jevans@usgs.gov","contributorId":2396,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"jevans@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":265863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28945,"text":"wri854296 - 1986 - Flood-depth frequency relations for streams in Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri854296","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":"85-4296","title":"Flood-depth frequency relations for streams in Alabama","docAbstract":"Equations were defined for estimating the depth of water for floods having recurrence intervals of 2, 5, 10, 25, 50, 100, and 200 years on rural and urban streams in Alabama. Multiple regression analyses were made using the ' maximum RSQUARE improvement ' procedures. The dependent variable was the flood depth and the independent variables were 10 basin and climatic characteristics. For rural streams, drainage area size (0.44 to 1,344 sq mi) was the only statistically significant independent variable tested to estimate flood depths in six different hydrologic areas. Other variables affecting flood depth relations are reflected in the equation constant and coefficient for each hydrologic area. These account for differences in geologic and topographic characteristics. For urban streams, drainage area size (0.16 to 83.5 sq mi) and percent impervious area (8.3% to 42.9%) of the basin were the most significant independent variables tested to estimate flood depths. For most streams where the drainage area is &gt; 1,344 sq mi, the drainage basin extends into more than one hydrologic area and the equations presented would not apply. Flood profile data and gaging station records are available from the U.S. Geological Survey for use in estimating flood depths for these large streams. Flood routing and historic flood profiles are also available for many of the large streams which have flood regulation. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854296","usgsCitation":"Olin, D., 1986, Flood-depth frequency relations for streams in Alabama: U.S. Geological Survey Water-Resources Investigations Report 85-4296, iv, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854296.","productDescription":"iv, 46 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121566,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4296/report-thumb.jpg"},{"id":57821,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4296/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a0e4b07f02db494602","contributors":{"authors":[{"text":"Olin, D.A.","contributorId":106905,"corporation":false,"usgs":true,"family":"Olin","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":200659,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28864,"text":"wri854316 - 1986 - Effect of bank protection measures, Stehekin River, Chelan County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri854316","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":"85-4316","title":"Effect of bank protection measures, Stehekin River, Chelan County, Washington","docAbstract":"An investigation of the lower Stehekin River was conducted to study the effects on flood elevations and velocities from four bank protection and flood prevention measures that are being contemplated as a means of reducing erosional losses of river bank property. These measures are: bank armoring, armored revetment levees, spur dikes, and redevelopment of old cutoff channels. The banks at seven study sites could be armored without adverse effect on the flood velocities and elevations. The largest increases due to armoring--up to 1.6 ft/sec in velocity and 1 ft in elevation--occurred in the vicinity of sites 5, 6, and 7 where the gradient of the river channel is about 50 ft/mi and the velocities are high to begin with (about 6 to 13 ft/sec). The use of a levee in conjunction with armoring on the northeast bank from sites 5 to 7 would increase the velocities as much as 2.8 ft/sec and increase the elevation as much as 1 ft, but it would also provide some flood protection to the east bank, which is frequently inundated. Spur dikes were considered a practical alternative only at site 3, where reduced bank erosion may occur without aggravating flood inundation or erosion elsewhere. The rerouting of flood flow through an old cutoff channel near site 1 increased the velocity by 3.2 ft/sec and the elevation by 1 ft for the 100-year flood; however, it would move floodwater away from residential property where bank erosion is a problem. The few other old channels that shortcut river bends where much erosion occurs are apparently already part of the channel during floods. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854316","usgsCitation":"Nelson, L.M., 1986, Effect of bank protection measures, Stehekin River, Chelan County, Washington: U.S. Geological Survey Water-Resources Investigations Report 85-4316, iv, 22 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854316.","productDescription":"iv, 22 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4316/report-thumb.jpg"},{"id":57742,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4316/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6256b7","contributors":{"authors":[{"text":"Nelson, L. M.","contributorId":39773,"corporation":false,"usgs":true,"family":"Nelson","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200525,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29086,"text":"wri854218 - 1986 - Organic compounds in ground water near a sanitary landfill in the Town of Brookhaven, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:49","indexId":"wri854218","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":"85-4218","title":"Organic compounds in ground water near a sanitary landfill in the Town of Brookhaven, Long Island, New York","docAbstract":"Landfill leachate and groundwater near the Brookhaven landfill site were analyzed for volatile, acid-extractable, and base/neutral-extractable organic compounds classified by EPA as ' priority pollutants, ' and for dissolved organic carbon (DOC) and inorganic constituents. Thirteen priority pollutants were detected, including benzene, chlorobenzene, ethyl benzene, and naphthalene. The most commonly detected priority pollutant, benzene, was found in the landfill leachate and in five groundwater samples. The concentration of ethyl benzene was the highest of all organic compounds detected--55 micrograms/L (ug/L) in the leachate. Three samples downgradient from the site contained detectable levels of priority pollutants; two of these from wells 2000 ft downgradient from the site, contained trace amounts of chloroform, and the other, from a well 500 ft downgradient, contained four priority pollutants in concentrations totaling less than 20 ug/L. DOC concentrations ranged from 410 mg/L in the leachate to 0.8 mg/L, which is considered background level for groundwater upgradient of the landfill site. Samples from downgradient wells contained less than 8 mg/L DOC except at two wells 500 ft from the site, which contained 21 and 16 mg/L. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854218","usgsCitation":"Pearsall, K., and Wexler, E.J., 1986, Organic compounds in ground water near a sanitary landfill in the Town of Brookhaven, Long Island, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4218, iv, 22 p. :ill., map ;28 cm., https://doi.org/10.3133/wri854218.","productDescription":"iv, 22 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":119731,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4218/report-thumb.jpg"},{"id":57940,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4218/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6910d0","contributors":{"authors":[{"text":"Pearsall, K.A.","contributorId":70800,"corporation":false,"usgs":true,"family":"Pearsall","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":200926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wexler, E. J.","contributorId":104931,"corporation":false,"usgs":true,"family":"Wexler","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200927,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26437,"text":"wri864343 - 1986 - Planning report for the Edwards-Trinity Regional Aquifer-System analysis in central Texas, southeast Oklahoma, and southwest Arkansas","interactions":[],"lastModifiedDate":"2017-05-31T16:10:00","indexId":"wri864343","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":"86-4343","title":"Planning report for the Edwards-Trinity Regional Aquifer-System analysis in central Texas, southeast Oklahoma, and southwest Arkansas","docAbstract":"<p>The Edwards-Trinity regional aquifer system supplies more than 0.78 million acre-feet per year (700 million gallons per day) of water for central Texas and small adjacent parts of southeast Oklahoma and southwest Arkansas. The system consists of three major aquifers and at least three minor aquifers in predominantly Cretaceous rocks, which together have an areal extent of about 80,000 square miles. The major aquifers are the Edwards-Trinity (Plateau) in west-central Texas, the Edwards (Balcones Fault Zone) in south-central Texas, and the Trinity in north-central Texas, southeast Oklahoma, and southwest Arkansas. Current (1986) and future concerns about the aquifer system involve the ever-increasing demand for water, most of which is associated with rapid population increase. Decreases in or elimination of spring discharges and encroachment of water from downdip salinewater zones into updip freshwater zones are of primary concern in the area underlain by ttie Edwards (Balcones Fault Zone) aquifer. Water-level declines of several hundred feet in the Trinity aquifer are a serious concern in some metropolitan areas.</p>\n<p>The Edwards-Trinity regional aquifer-system analysis project, begun in October 1985 and scheduled to be completed by October 1991, is one of a series of similar projects being conducted nationwide. The project is intended to define the hydrogeologic framework, and to describe the geochemistry and groundwater flow of the aquifer system in order to provide a better understanding of the system's long-term water-yielding potential. A multidisciplinary approach will be used in which computer-based digital simulation of flow in the system will be the principal method of hydrogeologic investigation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri864343","usgsCitation":"Bush, P.W., 1986, Planning report for the Edwards-Trinity Regional Aquifer-System analysis in central Texas, southeast Oklahoma, and southwest Arkansas: U.S. Geological Survey Water-Resources Investigations Report 86-4343, iv, 15 p., https://doi.org/10.3133/wri864343.","productDescription":"iv, 15 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":55243,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4343/report.pdf","text":"Report","size":"564.79 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     ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6850ea","contributors":{"authors":[{"text":"Bush, Peter W.","contributorId":57820,"corporation":false,"usgs":true,"family":"Bush","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196391,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29000,"text":"wri864052 - 1986 - Geophysical well-log analysis of fractured crystalline rocks at East Bull Lake, Ontario, Canada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri864052","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":"86-4052","title":"Geophysical well-log analysis of fractured crystalline rocks at East Bull Lake, Ontario, Canada","docAbstract":"Various conventional geophysical borehole measurements were made in conjunction with measurements using a recently designed, low-frequency, acoustic-waveform probe and slow velocity flowmeter for characterization of a fractured mafic intrusion in southern Ontario, Canada. Conventional geophysical measurements included temperature, caliper, gamma, acoustic, single-point resistance, and acoustic televiewer logs. Hole stability problems prevented the use of neutron and gamma-gamma logs, because these logs require that a radioactive source be lowered into the borehole. Measurements were made in three boreholes as much as 850 m deep and penetrating a few tens of meters into granitic basement. All rocks within the mafic intrusion were characterized by minimal gamma radiation and acoustic velocities of about 6.9 km/sec. The uniformity of the acoustic velocities and the character of acoustic-waveform logs made with a conventional high-frequency logging source correlated with the density of fractures evident on televiewer logs. Sample intervals of high-frequency waveform logs were transformed into interpretations of effective fracture opening using a recent model for acoustic attenuation in fractured rocks. The new low-frequency sparker source did not perform as expected at depths below 250 m because of previously unsuspected problems with source firing under large hydrostatic heads. A new heat-pulse, slow velocity flowmeter was used to delineate in detail the flow regime indicated in a general way by temperature logs. The flowmeter measurements indicated that water was entering 2 of the boreholes at numerous fractures above a depth of 200 m, with flow in at least 2 of the boreholes exiting through large isolated fractures below a depth of 400 m. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864052","usgsCitation":"Paillet, F.L., and Hess, A., 1986, Geophysical well-log analysis of fractured crystalline rocks at East Bull Lake, Ontario, Canada: U.S. Geological Survey Water-Resources Investigations Report 86-4052, vi, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864052.","productDescription":"vi, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4052/report-thumb.jpg"},{"id":57867,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b368","contributors":{"authors":[{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, A.E.","contributorId":71979,"corporation":false,"usgs":true,"family":"Hess","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":200764,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28856,"text":"wri844144 - 1986 - Investigation of the need for discharge adjustments for unsteady flow at selected gaging stations on streams in Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri844144","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":"84-4144","title":"Investigation of the need for discharge adjustments for unsteady flow at selected gaging stations on streams in Tennessee","docAbstract":"Measured discharges made during rising or falling stages generally require adjustments to refine constant-stage rating curves (stage-discharge relations) for gaged sites. Measurements at 42 gaging stations on Tennessee streams were selected for adjustment. Two methods, generally accepted by the U.S. Geological Survey, were tested: (1) the slope method adjusts the discharge for changing slope during the measurement, and (2) the storage method adjusts for change in channel storage. Both methods are related to the rate of change in stage. The initial results of the storage method of adjustments were unsatisfactory because of uncertainty in determining channel storage at each site, and a specific trend in the results could not be defined. Consequently, the storage method of adjustment was deleted from successive analyses. Maximum adjustments in measured discharge using the slope method were less than 5 percent at 28 of the 42 stations and less than 10 percent at 39 of the 42 stations used in the analyses. The adjustments were small because most of the measurements were made during nearly stable stage. Adjustments of measurements made during stage changes of several feet per hour could be considerably larger than 10 percent. Stage records at 10 stations showed that maximum change in stage during rises were considerably higher than the change in stage observed during the measurements. Large adjustments are usually required for a short period of time on the rising side of a hydrograph and smaller adjustments are required for a longer period of time on the falling side. Maximum adjustments in discharge using the slope method were less than 5 percent at three of the 10 stations and less than 30 percent at eight of the 10 stations used in the analyses. The mean discharge for the adjusted and unadjusted hydrographs are about the same. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844144","usgsCitation":"Neely, B., and Bingham, R., 1986, Investigation of the need for discharge adjustments for unsteady flow at selected gaging stations on streams in Tennessee: U.S. Geological Survey Water-Resources Investigations Report 84-4144, iv, 21 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844144.","productDescription":"iv, 21 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":2339,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri844144","linkFileType":{"id":5,"text":"html"}},{"id":123970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_84_4144.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4284","contributors":{"authors":[{"text":"Neely, B.L.","contributorId":90344,"corporation":false,"usgs":true,"family":"Neely","given":"B.L.","affiliations":[],"preferred":false,"id":200513,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingham, R.H.","contributorId":37301,"corporation":false,"usgs":true,"family":"Bingham","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":200512,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33559,"text":"b1678 - 1986 - Sea-floor observations and subbottom seismic characteristics of OAK and KOA craters, Enewetak Atoll, Marshall Islands","interactions":[],"lastModifiedDate":"2018-09-18T19:23:33","indexId":"b1678","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":"1678","title":"Sea-floor observations and subbottom seismic characteristics of OAK and KOA craters, Enewetak Atoll, Marshall Islands","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1678","usgsCitation":"1986, Sea-floor observations and subbottom seismic characteristics of OAK and KOA craters, Enewetak Atoll, Marshall Islands: U.S. Geological Survey Bulletin 1678, 257 p. (published as one volume) ill., maps ;28 cm., https://doi.org/10.3133/b1678.","productDescription":"257 p. (published as one volume) ill., maps ;28 cm.","costCenters":[],"links":[{"id":167118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1678/report-thumb.jpg"},{"id":61449,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1678/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc56d","contributors":{"editors":[{"text":"Folger, David W.","contributorId":78349,"corporation":false,"usgs":true,"family":"Folger","given":"David W.","affiliations":[],"preferred":false,"id":745442,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":26820,"text":"wri874009 - 1986 - U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1983, 1984, and 1985","interactions":[{"subject":{"id":70194908,"text":"70194908 - 1986 - Beatty, Nevada: A section in <i>U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1983, 1984, and 1985 (WRI 87-4009)</i>","indexId":"70194908","publicationYear":"1986","noYear":false,"title":"Beatty, Nevada: A section in <i>U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1983, 1984, and 1985 (WRI 87-4009)</i>"},"predicate":"IS_PART_OF","object":{"id":26820,"text":"wri874009 - 1986 - U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1983, 1984, and 1985","indexId":"wri874009","publicationYear":"1986","noYear":false,"title":"U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1983, 1984, and 1985"},"id":1}],"lastModifiedDate":"2018-01-29T14:59:12","indexId":"wri874009","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":"87-4009","title":"U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1983, 1984, and 1985","docAbstract":"<p>The report summarizes progress on geologic and hydrologic research related to the disposal of radioactive wastes. The research is described according to whether it is related most directly to: (1) high-level and transuranic wastes, (2) low-level wastes, or (3) uranium mill tailings. Included is research applicable to the identification and geohydrologic characterization of waste-disposal sites, to investigations of specific sites where wastes have been stored, and to studies of regions or environments where waste-disposal sites might be located. A significant part of the activity is concerned with techniques and methods for characterizing disposal sites and studies of geologic and hydrologic processes related to the transport and (or) retention of waste radionuclides.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/wri874009","usgsCitation":"Dinwiddie, G., and Trask, N., 1986, U.S. Geological Survey research in radioactive waste disposal - Fiscal years 1983, 1984, and 1985: U.S. Geological Survey Water-Resources Investigations Report 87-4009, vi, 109 p., https://doi.org/10.3133/wri874009.","productDescription":"vi, 109 p.","costCenters":[],"links":[{"id":55702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4009/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4009/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6121be","contributors":{"authors":[{"text":"Dinwiddie, G.A.","contributorId":49798,"corporation":false,"usgs":true,"family":"Dinwiddie","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":197062,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trask, N.J.","contributorId":31729,"corporation":false,"usgs":true,"family":"Trask","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":197061,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4295,"text":"cir978 - 1986 - Geologic studies in Alaska by the U.S. Geological Survey during 1985","interactions":[{"subject":{"id":70180235,"text":"70180235 - 1986 - Later Paleozoic and Early Jurassic fossil ages from the McHugh Complex: A section in <i> Geologic studies in Alaska by the U.S. Geological Survey during 1985 Circular 978</i>","indexId":"70180235","publicationYear":"1986","noYear":false,"title":"Later Paleozoic and Early Jurassic fossil ages from the McHugh Complex: A section in <i> Geologic studies in Alaska by the U.S. Geological Survey during 1985 Circular 978</i>"},"predicate":"IS_PART_OF","object":{"id":4295,"text":"cir978 - 1986 - Geologic studies in Alaska by the U.S. Geological Survey during 1985","indexId":"cir978","publicationYear":"1986","noYear":false,"title":"Geologic studies in Alaska by the U.S. Geological Survey during 1985"},"id":1}],"lastModifiedDate":"2022-06-28T20:53:45.716836","indexId":"cir978","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"978","title":"Geologic studies in Alaska by the U.S. Geological Survey during 1985","docAbstract":"This circular contains short reports about many of the geologic studies carried out in Alaska by the U.S. Geological Survey and cooperating agencies in 1985. The topics cover a wide range in scientific and economic interest. Separate bibliographic listings of published reports are included. 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,{"id":26410,"text":"wri864064 - 1986 - Availability of water for irrigation in the South Fork Solomon River Valley, Webster Reservoir to Waconda Lake, north-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:34","indexId":"wri864064","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":"86-4064","title":"Availability of water for irrigation in the South Fork Solomon River Valley, Webster Reservoir to Waconda Lake, north-central Kansas","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864064","usgsCitation":"Burnett, R.D., and Reed, T., 1986, Availability of water for irrigation in the South Fork Solomon River Valley, Webster Reservoir to Waconda Lake, north-central Kansas: U.S. Geological Survey Water-Resources Investigations Report 86-4064, vi, 89 p. :ill., maps ;28 cm.; 4 over-size sheets, https://doi.org/10.3133/wri864064.","productDescription":"vi, 89 p. :ill., maps ;28 cm.; 4 over-size sheets","costCenters":[],"links":[{"id":119096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4064/report-thumb.jpg"},{"id":55199,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4064/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55200,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4064/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55201,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4064/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55202,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4064/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55203,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4064/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d753","contributors":{"authors":[{"text":"Burnett, Robert D.","contributorId":78778,"corporation":false,"usgs":true,"family":"Burnett","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":196340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, Thomas B.","contributorId":76704,"corporation":false,"usgs":true,"family":"Reed","given":"Thomas B.","affiliations":[],"preferred":false,"id":196339,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30244,"text":"wri854320 - 1986 - Quality of ground water in the Columbia Basin, Washington, 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri854320","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":"85-4320","title":"Quality of ground water in the Columbia Basin, Washington, 1983","docAbstract":"Groundwater from 188 sites in the Columbia Basin of central Washington was sampled and analyzed in 1983 for pH, specific conductance, and concentrations of fecal coliform bacteria, major dissolved ions, and dissolved iron, manganese, and nitrate. Twenty of the samples were also analyzed for concentrations of dissolved trace metals including aluminum, arsenic, barium, cadmium, chromium, copper, lead, mercury, selenium, silver, and zinc. The predominant water types were sodium bicarbonate and calcium bicarbonate. The sodium bicarbonate water samples had higher pH, fluoride, and sodium:adsorption ratio values than samples with other water types. Dissolved solids concentrations were generally between 250 and 500 mg/L. Iron and manganese concentrations were usually &lt; 10 micrograms/L (ug/L). Most trace metal concentrations were also &lt; 10 ug/L except for barium and zinc, which had maximum concentrations of 170 and 600 ug/L, respectively. Nitrate concentrations were &lt; 1.0 mg/L in water from more than half the wells sampled. Concentrations exceeded 1.0 mg/L in large areas of Lincoln, eastern Adams, Franklin and southern Grant Counties. No fecal coliform bacteria were detected. U.S. EPA drinking water regulations were exceeded in several samples, most commonly involving pH and concentrations of fluoride, nitrate, and dissolved solids in samples from Adams and Grant Counties. Generally, the historical data lead to similar conclusions about the quality of groundwater in the Columbia Basin region. However , historical samples had higher dissolved solids concentrations in Douglas County. Historical samples also included fewer sodium bicarbonate type waters in the region as a whole than the 1983 samples. These differences may be due to inconsistencies in data collection or analytical methods. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854320","usgsCitation":"Turney, G.L., 1986, Quality of ground water in the Columbia Basin, Washington, 1983: U.S. Geological Survey Water-Resources Investigations Report 85-4320, v, 172 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854320.","productDescription":"v, 172 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4320/report-thumb.jpg"},{"id":59026,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4320/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59027,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4320/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59028,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4320/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59029,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4320/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59030,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4320/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59031,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4320/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c043","contributors":{"authors":[{"text":"Turney, G. L.","contributorId":95070,"corporation":false,"usgs":true,"family":"Turney","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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