No abstract available.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a25cc","contributors":{"authors":[{"text":"Finn, Carol A. 0000-0002-6178-0405 cfinn@usgs.gov","orcid":"https://orcid.org/0000-0002-6178-0405","contributorId":1326,"corporation":false,"usgs":true,"family":"Finn","given":"Carol","email":"cfinn@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":227765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, W.M.","contributorId":49332,"corporation":false,"usgs":true,"family":"Phillips","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":227766,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, D.L.","contributorId":7681,"corporation":false,"usgs":true,"family":"Williams","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":227764,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":29199,"text":"wri844122 - 1984 - Selenium concentrations in waters tributary to and in the vicinity of the Kesterson National Wildlife Refuge, Fresno and Merced counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri844122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4122","title":"Selenium concentrations in waters tributary to and in the vicinity of the Kesterson National Wildlife Refuge, Fresno and Merced counties, California","docAbstract":"Analyses were made for selenium in waters and other materials of the Kesterson National Wildlife Refuge. Analyses were also made of source agricultural drainage waters from the San Luis Drain discharged into the refuge, and surrounding irrigation supply and return waters. Selenium concentrations range from 140 to 1 ,400 micrograms per liter (microgram/L) in irrigation drain waters supplied to the San Luis Drain. The selenium supplied to the Kesterson National Wildlife Refuge is to a small extent precipitated in sodium sulfate (thenardite) but a higher concentration was found in an alagal mat. Most other waters of the area contain less than detectable < 2 micrograms per liter concentrations of selenium. Oxidation of organic matter and reduction of selenate to selenite were found to be necessary for a quantitative analysis of total selenium. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844122","usgsCitation":"Presser, T.S., and Barnes, I., 1984, Selenium concentrations in waters tributary to and in the vicinity of the Kesterson National Wildlife Refuge, Fresno and Merced counties, California: U.S. Geological Survey Water-Resources Investigations Report 84-4122, iii, 26 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844122.","productDescription":"iii, 26 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159432,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4122/report-thumb.jpg"},{"id":58060,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4122/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7c44","contributors":{"authors":[{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":201132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":201131,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":20368,"text":"ofr84613 - 1984 - January 1984 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr84613","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-613","title":"January 1984 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"Water-level measurements were made, mostly during January 1984, in about 1,450 wells in western and south-central Kansas. The measurements were made in mid-winter when pumping was minimal and water levels had recovered, for the most part, from the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water-level changes from a ' base-reference year ' (predevelopment year), a year of abnormally high rainfall and minimum pumpage (1966 or 1974), and each of 7 consecutive years of measurement (1978-84). The ' base-reference year ' is designated as 1940 for the southwestern area, 1944 for the south-central area, and 1950 for the northwestern and west-central areas. Water levels for the ' base-reference year ' are established by measurements made during that year and by interpretation of maps showing water-level altitudes. Data also are provided for relating the average annual water-level changes, saturated thicknesses of the deposits, and percentage changes in saturated thicknesses.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84613","usgsCitation":"Pabst, M., and Dague, B., 1984, January 1984 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 84-613, iv, 163 p. :ill. ;28 cm., https://doi.org/10.3133/ofr84613.","productDescription":"iv, 163 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0613/report-thumb.jpg"},{"id":49901,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0613/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fb2","contributors":{"authors":[{"text":"Pabst, M.E.","contributorId":17608,"corporation":false,"usgs":true,"family":"Pabst","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":182529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dague, B.J.","contributorId":45723,"corporation":false,"usgs":true,"family":"Dague","given":"B.J.","affiliations":[],"preferred":false,"id":182530,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28919,"text":"wri844160 - 1984 - The ground-water resources in the Ross Barnett Reservoir area, Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri844160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4160","title":"The ground-water resources in the Ross Barnett Reservoir area, Mississippi","docAbstract":"The Ross Barnett Reservoir area occupies about 78 sq mi of a 490 sq mi study area northeast of the City of Jackson, MS. For several years, water use in the area has increased and during 1983 about 0.57 mil gal/day were obtained from groundwater sources. Virtually all groundwater in the area is used for public supplies. The principal aquifers currently used in the area are in the Sparta Sand and Cockfield Formations. The Sparta Sand is the most intensively developed and generally the highest yielding aquifer in the study area. Water level declines have averaged 2 to 3 ft/yr since 1940. The principal source of groundwater recharge to the aquifers is precipitation on outcrops of permeable strata northeast of the area. The base of freshwater is at the base of the Meridian-upper Wilcox aquifer except in the extreme northeast part of the area where the lower Wilcox aquifer contains freshwater. Water from the aquifers is suitable for public supply use without treatment except in a few places where iron concentrations are high, at from 0.10 to 9.3 mg/L. Excessive color is also a problem in the water from some wells in the area. Color was 20 units or greater in 8 of 25 wells sampled. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844160","usgsCitation":"Oakley, W.T., 1984, The ground-water resources in the Ross Barnett Reservoir area, Mississippi: U.S. Geological Survey Water-Resources Investigations Report 84-4160, iv, 32 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844160.","productDescription":"iv, 32 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4160/report-thumb.jpg"},{"id":57791,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602b8d","contributors":{"authors":[{"text":"Oakley, W. T.","contributorId":76331,"corporation":false,"usgs":true,"family":"Oakley","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":200619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2229,"text":"wsp2196C - 1984 - Nutrient and detritus transport in the Apalachicola River, Florida","interactions":[{"subject":{"id":10218,"text":"ofr83130 - 1983 - Nutrient and detritus transport in the Apalachicola River, Florida","indexId":"ofr83130","publicationYear":"1983","noYear":false,"title":"Nutrient and detritus transport in the Apalachicola River, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":2229,"text":"wsp2196C - 1984 - Nutrient and detritus transport in the Apalachicola River, Florida","indexId":"wsp2196C","publicationYear":"1984","noYear":false,"chapter":"C","title":"Nutrient and detritus transport in the Apalachicola River, Florida"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp2196C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2196","chapter":"C","title":"Nutrient and detritus transport in the Apalachicola River, Florida","docAbstract":"The Apalachicola River in northwest Florida flows 172 kilometers southward from Jim Woodruff Dam near the Florida-Georgia border to Apalachicola Bay on the Gulf of Mexico. The basin is composed of two 3,100-squarekilometer subbasins, the Chipola and the Apalachicola. The Apalachicola subbasin includes a 454-square-kilometer bottom-land hardwood flood plain that is relatively undeveloped. The flood plain contains more than 1,500 trees per hectare that annually produce approximately 800 metric tons of litter fall per square kilometer. Spring floods of March and April 1980 carried 35,000 metric tons of particulate organic carbon derived from litter fall into Apalachicola Bay. The estuarine food web is predominantly detrital based and represents an important commercial source of oyster, shrimp, blue crab, and various species of fish. \r\n\r\nThe water budget of the Apalachicola basin is heavily dominated by streamflow. For a 1-year period in 1979-80, 28.6 cubic kilometers of water flowed past the Sumatra gage on the lower river. Eighty percent of this volume flowed into the upper river near Chattahoochee, Fla., and 11 percent was contributed by its major tributary, the Chipola River. Contributions from ground water and overland runoff were less than 10 percent. \r\n\r\nStreamflow increases downstream were accompanied by equivalent increases in nitrogen and phosphorus transport. The nutrients were released to the river by the flood-plain vegetation, but also were subject to recycling. The increase in the amount of organic carbon transport downstream was greater than streamflow increases. The flood plain is an important source of organic carbon, especially in detrital form. \r\n\r\nSeveral methods for measurement of detritus in the river and flood plain were developed and tested. The detritus data from the flood plain added semiquantitative evidence for transport of detritus from the flood plain to the river flow, probably accounting for most of the coarse particulate organic material carried by the river. \r\n\r\nDuring the 1-year period of investigation, June 3, 1979, through June 2, 1980, 2.1 ? 10 5 metric tons of organic carbon were transported from the river basin to the bay. Nitrogen and phosphorus transport during the same period amounted to 2.2 ? 10 4 and 1.7 ? 10 3 metric tons, respectively. On an areal basis, it was calculated that the flood plain contributed 70 grams of organic carbon per square meter per year, 0.4 gram of nitrogen per square meter per year, and 0.5 gram of phosphorus per square meter per year. The flood plain acts as a source of detrital carbon, but for the solutes, nutrient release is approximately balanced by nutrient retention.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2196C","usgsCitation":"Mattraw, H., and Elder, J.F., 1984, Nutrient and detritus transport in the Apalachicola River, Florida: U.S. Geological Survey Water Supply Paper 2196, viii, C62 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2196C.","productDescription":"viii, C62 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":137713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2196c/report-thumb.jpg"},{"id":27983,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2196c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6967b4","contributors":{"authors":[{"text":"Mattraw, Harold C.","contributorId":81878,"corporation":false,"usgs":true,"family":"Mattraw","given":"Harold C.","affiliations":[],"preferred":false,"id":144856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elder, John F.","contributorId":23919,"corporation":false,"usgs":true,"family":"Elder","given":"John","email":"","middleInitial":"F.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":144855,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61516,"text":"mf1568C - 1984 - Geologic map of the Fossil Springs Roadless Area, Yavapai, Gila, and Coconino Counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:10:29","indexId":"mf1568C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1568","chapter":"C","title":"Geologic map of the Fossil Springs Roadless Area, Yavapai, Gila, and Coconino Counties, Arizona","language":"ENGLISH","doi":"10.3133/mf1568C","usgsCitation":"Weir, G.W., and Beard, L.S., 1984, Geologic map of the Fossil Springs Roadless Area, Yavapai, Gila, and Coconino Counties, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1568, Sheet 31 inches x 36 inches, https://doi.org/10.3133/mf1568C.","productDescription":"Sheet 31 inches x 36 inches","costCenters":[],"links":[{"id":106037,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7453.htm","linkFileType":{"id":5,"text":"html"},"description":"7453"},{"id":182376,"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\": [ [ [ -111.61749999999999,34.38444444444444 ], [ -111.61749999999999,34.5 ], [ -111.45083333333334,34.5 ], [ -111.45083333333334,34.38444444444444 ], [ -111.61749999999999,34.38444444444444 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69861e","contributors":{"authors":[{"text":"Weir, G. W.","contributorId":107290,"corporation":false,"usgs":true,"family":"Weir","given":"G.","middleInitial":"W.","affiliations":[],"preferred":false,"id":265858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beard, L. S.","contributorId":29410,"corporation":false,"usgs":true,"family":"Beard","given":"L.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":265857,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26710,"text":"wri834288 - 1984 - Estimates of dissolved and suspended substance yield of stream basins in Michigan","interactions":[],"lastModifiedDate":"2023-01-10T20:15:47.117207","indexId":"wri834288","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4288","title":"Estimates of dissolved and suspended substance yield of stream basins in Michigan","docAbstract":"Water-quality data collected at 20 stations in Michigan were used to develop regression equations relating loads of dissolved and suspended substances to discharge. These equations and mean daily discharge were used to estimate long-term loads, which then were converted to estimates of drainage basin yields. These yields were compared to measured yields and to previous estimates.
Equations were developed for each station that express the relation between load and discharge (L = aQb) for 19 substances and properties. Fifty percent of the equations had standard errors of 22 percent or less; 90 percent of the equations had standard errors of 80 percent or less. Regression exponents indicate that the load increases as discharge increases in all cases, but for about two-thirds of the substances or properties, the increase is less rapid than that of discharge. Seventy-eight percent of the nitrogen, phosphorus, and sediment loads, taken as a group, increase more rapidly than discharge. Concentrations of about 63 percent of the substances or properties decrease as discharge increases, however.
Although comparative data for most drainage basins are scant, yields estimated by use of regression equations did not differ appreciably from measured values at locations where comparison was possible.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri834288","usgsCitation":"Cummings, T., 1984, Estimates of dissolved and suspended substance yield of stream basins in Michigan: U.S. Geological Survey Water-Resources Investigations Report 83-4288, v, 57 p., https://doi.org/10.3133/wri834288.","productDescription":"v, 57 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":411660,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35908.htm","linkFileType":{"id":5,"text":"html"}},{"id":118682,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4288/report-thumb.jpg"},{"id":55580,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4288/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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R.","affiliations":[],"preferred":false,"id":196863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20363,"text":"ofr84222 - 1984 - High-resolution seismic profile data from the U.S. Atlantic continental slope off New England, between Lydonia and Oceanographer canyons","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr84222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-222","title":"High-resolution seismic profile data from the U.S. Atlantic continental slope off New England, between Lydonia and Oceanographer canyons","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84222","usgsCitation":"O’Leary, D.W., and Aaron, J.M., 1984, High-resolution seismic profile data from the U.S. Atlantic continental slope off New England, between Lydonia and Oceanographer canyons: U.S. Geological Survey Open-File Report 84-222, 3 p. :ill. ;28 cm., https://doi.org/10.3133/ofr84222.","productDescription":"3 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153139,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0222/report-thumb.jpg"},{"id":49895,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0222/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68884c","contributors":{"authors":[{"text":"O’Leary, Dennis W.","contributorId":63396,"corporation":false,"usgs":true,"family":"O’Leary","given":"Dennis","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":182520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aaron, John M.","contributorId":10031,"corporation":false,"usgs":true,"family":"Aaron","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":182519,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1726,"text":"wsp1757P - 1984 - A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images","interactions":[{"subject":{"id":9261,"text":"ofr80565 - 1981 - A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images","indexId":"ofr80565","publicationYear":"1981","noYear":false,"title":"A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images"},"predicate":"SUPERSEDED_BY","object":{"id":1726,"text":"wsp1757P - 1984 - A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images","indexId":"wsp1757P","publicationYear":"1984","noYear":false,"chapter":"P","title":"A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1757P","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1757","chapter":"P","title":"A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1757P","usgsCitation":"Grolier, M.J., Tibbitts, G.C., and Ibrahim, M.M., 1984, A qualitative appraisal of the hydrology of the Yemen Arab Republic from Landsat images: U.S. Geological Survey Water Supply Paper 1757, v, P70 p. :ill., maps (1 col.) ;24 cm.; 1 plate in pocket, https://doi.org/10.3133/wsp1757P.","productDescription":"v, P70 p. :ill., maps (1 col.) ;24 cm.; 1 plate in pocket","costCenters":[],"links":[{"id":136974,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1757p/report-thumb.jpg"},{"id":26832,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757p/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1757p/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8777","contributors":{"authors":[{"text":"Grolier, Maurice J.","contributorId":98292,"corporation":false,"usgs":true,"family":"Grolier","given":"Maurice","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":144028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tibbitts, G. Chase Jr.","contributorId":30601,"corporation":false,"usgs":true,"family":"Tibbitts","given":"G.","suffix":"Jr.","email":"","middleInitial":"Chase","affiliations":[],"preferred":false,"id":144026,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ibrahim, Mohammed Mukred","contributorId":47759,"corporation":false,"usgs":true,"family":"Ibrahim","given":"Mohammed","email":"","middleInitial":"Mukred","affiliations":[],"preferred":false,"id":144027,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9587,"text":"ofr84826 - 1984 - Lithologic logs of auger holes and analytical data for auger samples from the Four Notch, Graham Creek, and Chambers Ferry Roadless Areas, Walker, Angelina, Jasper, and Sabine Counties, eastern Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr84826","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-826","title":"Lithologic logs of auger holes and analytical data for auger samples from the Four Notch, Graham Creek, and Chambers Ferry Roadless Areas, Walker, Angelina, Jasper, and Sabine Counties, eastern Texas","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84826","usgsCitation":"Houser, B.B., 1984, Lithologic logs of auger holes and analytical data for auger samples from the Four Notch, Graham Creek, and Chambers Ferry Roadless Areas, Walker, Angelina, Jasper, and Sabine Counties, eastern Texas: U.S. Geological Survey Open-File Report 84-826, i, 20 p. ;28 cm., https://doi.org/10.3133/ofr84826.","productDescription":"i, 20 p. ;28 cm.","costCenters":[],"links":[{"id":142901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0826/report-thumb.jpg"},{"id":37312,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0826/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6355c1","contributors":{"authors":[{"text":"Houser, B. B.","contributorId":46092,"corporation":false,"usgs":true,"family":"Houser","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":159955,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28717,"text":"wri844116 - 1984 - Cost-effectiveness of the US Geological Survey stream-gaging program in central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri844116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4116","title":"Cost-effectiveness of the US Geological Survey stream-gaging program in central Florida","docAbstract":"In the Red Oak area, Oklahoma, water in shale bedrock occurs in bedding planes and fractures and is confined. Wells probably yield less than 5 gallons per minute. Ground water is a sodium or mixed cation carbonate/bicarbonate type with dissolved-solids concentrations ranging from about 300 to 700 milligrams per liter. No relationship between water chemistry and well depth or location is apparent. Brazil Creek flows 1 cubic foot per second or less about 25 percent of the time and has no flow about 15 percent of the time. Water in Brazil Creek is a mixed cation carbonate/bicarbonate type. Dissolved-solids concentrations upstream from old and recent mines ranged from 30 to 100 milligrams per liter whereas concentrations downstreams from the mines ranged from 50 to 600 milligrams per liter. Excessive levels of cadmium, chromium, lead, and mercury at times preclude use of water from Brazil and Rock Creeks for public supply. Maximum suspended-sediment discharge, in tons per day, was 2,500 for Brazil Creek and 3,300 for Rock Creek. Silt-clay particles with diameters less than 0.062 millimeter were the dominant sediment size. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844116","usgsCitation":"Miller, R.A., Anderson, W., and Heath, R., 1984, Cost-effectiveness of the US Geological Survey stream-gaging program in central Florida: U.S. Geological Survey Water-Resources Investigations Report 84-4116, vi, 89 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844116.","productDescription":"vi, 89 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4116/report-thumb.jpg"},{"id":57549,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4116/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680e15","contributors":{"authors":[{"text":"Miller, R. A.","contributorId":95090,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Warren","contributorId":7712,"corporation":false,"usgs":true,"family":"Anderson","given":"Warren","affiliations":[],"preferred":false,"id":200279,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heath, R.C.","contributorId":49408,"corporation":false,"usgs":true,"family":"Heath","given":"R.C.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":200280,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9387,"text":"ofr84847 - 1984 - Principal facts for gravity stations in and near the Madison and Gallatin Divide Roadless Areas, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr84847","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-847","title":"Principal facts for gravity stations in and near the Madison and Gallatin Divide Roadless Areas, Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84847","usgsCitation":"Hassemer, J., and Kaufmann, H.E., 1984, Principal facts for gravity stations in and near the Madison and Gallatin Divide Roadless Areas, Montana: U.S. Geological Survey Open-File Report 84-847, 32 p. :ill. ;28 cm., https://doi.org/10.3133/ofr84847.","productDescription":"32 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":142757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0847/report-thumb.jpg"},{"id":37107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0847/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f4d","contributors":{"authors":[{"text":"Hassemer, J. H.","contributorId":12488,"corporation":false,"usgs":true,"family":"Hassemer","given":"J. H.","affiliations":[],"preferred":false,"id":159585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaufmann, H. E.","contributorId":40215,"corporation":false,"usgs":true,"family":"Kaufmann","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159586,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4195,"text":"cir913 - 1984 - Water-level and water-quality changes in Great Salt Lake, Utah, 1847-1983","interactions":[],"lastModifiedDate":"2017-02-22T12:05:09","indexId":"cir913","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"913","title":"Water-level and water-quality changes in Great Salt Lake, Utah, 1847-1983","docAbstract":"The surface level of Great Salt Lake, Utah, fluctuates continuously, primarily in response to climatic factors. During 1847-1982 the lake surface fluctuated between a low of about 4,191 feet and a high of about 4,212 feet above sea level but showed no net change. From September 18, 1982, to June 30, 1983, however, the lake rose 5.2 feet-from about 4,200 to about 4,205 feet above sea level-which is the greatest seasonal rise ever recorded. That rise resulted from considerably greater than average rainfall in 1982, greater than average snowfall during the autumn of 1982 through the spring of 1983, and unseasonably cool weather during that spring.
Man's activities have had a lesser, but still important effect on the lake level. The lake surface would have been about 5 feet higher in 1983 had there been no consumptive use of water owing to man's activities in the lake basin since 1847. The lake has been divided into two parts by a railroad causeway since 1959. The causeway restricts natural circulation, resulting in a difference of salinity and surface level of the lake across the causeway. The difference in surface level between the two parts of the lake varies both seasonally and annually and was as much as 3.25 feet in 1983.
The water budget for the Great Salt Lake can be expressed as:
Inflow = Outflow ± Storage change
The average annual inflow for 1931-76 was about 2.9 million acre-feet-about 1.9 million acre-feet from surface water, about 900,000 acre-feet from direct precipitation, and about 75,000 acre-feet from ground water. The average annual outflow for the same period, all by evaporation, also was about 2.9 million acre-feet. There was no net change in storage during the period.
The famed buoyancy of the brine in Great Salt Lake results from a dissolved-mineral content of almost 5 billion tons. More than 2 million additional tons have been added to the lake annually in recent years. The major dissolved ions in the brine are chloride, sulfate, sodium, magnesium, and potassium.
Prior to completion of the railroad causeway, the salinity of the brine varied inversely with the lake level. Since the causeway divided the lake into two parts, the salinity of the brine in the north part has been relatively constant at or close to saturation. The salinity of the brine in the south part has 1 continued to change inversely with the lake level, but the salinity has been less than it would have been without the causeway.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir913","usgsCitation":"Arnow, T., 1984, Water-level and water-quality changes in Great Salt Lake, Utah, 1847-1983: U.S. Geological Survey Circular 913, iv, 22 p., https://doi.org/10.3133/cir913.","productDescription":"iv, 22 p.","numberOfPages":"28","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":31309,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0913/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0913/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.3349609375,\n 40.538851525354666\n ],\n [\n -111.8023681640625,\n 40.538851525354666\n ],\n [\n -111.8023681640625,\n 41.82454867985508\n ],\n [\n -113.3349609375,\n 41.82454867985508\n ],\n [\n -113.3349609375,\n 40.538851525354666\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e782d","contributors":{"authors":[{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":148384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4314,"text":"cir938 - 1984 - U. S. Geological Survey highlights in marine research","interactions":[],"lastModifiedDate":"2018-03-13T17:38:08","indexId":"cir938","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"938","title":"U. S. Geological Survey highlights in marine research","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir938","usgsCitation":"1984, U. S. Geological Survey highlights in marine research: U.S. Geological Survey Circular 938, v, 176 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir938.","productDescription":"v, 176 p. :ill., maps ;27 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":31424,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0938/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0938/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696542","contributors":{"editors":[{"text":"Clarke, Samuel H.","contributorId":42958,"corporation":false,"usgs":true,"family":"Clarke","given":"Samuel H.","affiliations":[],"preferred":false,"id":730997,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":26724,"text":"wri844349 - 1984 - Finite-element simulation of ground-water flow in the vicinity of Yucca Mountain, Nevada-California","interactions":[],"lastModifiedDate":"2023-03-07T21:51:56.728644","indexId":"wri844349","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4349","title":"Finite-element simulation of ground-water flow in the vicinity of Yucca Mountain, Nevada-California","docAbstract":"A finite-element model of the groundwater flow system in the vicinity of Yucca Mountain at the Nevada Test Site was developed using parameter estimation techniques. The model simulated steady-state ground-water flow occurring in tuffaceous, volcanic , and carbonate rocks, and alluvial aquifers. Hydraulic gradients in the modeled area range from 0.00001 for carbonate aquifers to 0.19 for barriers in tuffaceous rocks. Three model parameters were used in estimating transmissivity in six zones. Simulated hydraulic-head values range from about 1,200 m near Timber Mountain to about 300 m near Furnace Creek Ranch. Model residuals for simulated versus measured hydraulic heads range from -28.6 to 21.4 m; most are less than +/-7 m, indicating an acceptable representation of the hydrologic system by the model. Sensitivity analyses of the model 's flux boundary condition variables were performed to assess the effect of varying boundary fluxes on the calculation of estimated model transmissivities. Varying the flux variables representing discharge at Franklin Lake and Furnace Creek Ranch has greater effect than varying other flux variables.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844349","usgsCitation":"Czarnecki, J., and Waddell, R.K., 1984, Finite-element simulation of ground-water flow in the vicinity of Yucca Mountain, Nevada-California: U.S. Geological Survey Water-Resources Investigations Report 84-4349, Report: iv, 38 p.; 2 Plates: 31.1 x 46.30 inches and 30.87 x 42.19 inches, https://doi.org/10.3133/wri844349.","productDescription":"Report: iv, 38 p.; 2 Plates: 31.1 x 46.30 inches and 30.87 x 42.19 inches","costCenters":[],"links":[{"id":413793,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36183.htm","linkFileType":{"id":5,"text":"html"}},{"id":55598,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4349/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55597,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4349/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126893,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4349/report-thumb.jpg"},{"id":55599,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4349/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Nevada","otherGeospatial":"Yucca Mountain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116,\n 37.062\n ],\n [\n -116.883,\n 37.062\n ],\n [\n -116.883,\n 36.217\n ],\n [\n -116,\n 36.217\n ],\n [\n -116,\n 37.062\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef805","contributors":{"authors":[{"text":"Czarnecki, J.B.","contributorId":51768,"corporation":false,"usgs":true,"family":"Czarnecki","given":"J.B.","affiliations":[],"preferred":false,"id":196893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, R. K.","contributorId":25560,"corporation":false,"usgs":true,"family":"Waddell","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":196892,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28723,"text":"wri834256 - 1984 - Effects of three phosphate industrial sites on ground-water quality in central Florida, 1979 to 1980","interactions":[],"lastModifiedDate":"2025-01-13T17:49:39.065886","indexId":"wri834256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4256","title":"Effects of three phosphate industrial sites on ground-water quality in central Florida, 1979 to 1980","docAbstract":"Geologic, hydrologic, and water quality data and information on test holes collected in the vicinity of gypsum stack complexes at two phosphate chemical plants and one phosphatic clayey waste disposal pond at a phosphate mine and beneficiation plant in central Florida are presented. The data were collected from September 1979 to October 1980 at the AMAX Phosphate, Inc. chemical plant, Piney Point; the USS Agri-Chemicals chemical plant, Bartow; and the International Minerals and Chemical Corporation Clear Springs mine, Bartow. Approximately 5,400 field and laboratory water quality determinations on water samples collected from about 100 test holes and 28 surface-water , 5 rainfall, and other sampling sites at phosphate industry beneficiation and chemical plant waste disposal operations are tabulated. Maps are included to show sampling sites. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834256","usgsCitation":"Miller, R.L., and Sutcliffe, H., 1984, Effects of three phosphate industrial sites on ground-water quality in central Florida, 1979 to 1980: U.S. Geological Survey Water-Resources Investigations Report 83-4256, x, 184 p., https://doi.org/10.3133/wri834256.","productDescription":"x, 184 p.","costCenters":[],"links":[{"id":57552,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4256/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122657,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4256/report-thumb.jpg"},{"id":466126,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35886.htm","text":"USSAC and IMC plant sites","linkFileType":{"id":5,"text":"html"}},{"id":466125,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35885.htm","text":"AMAX plant site","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -81.47943871799596,\n 28.219395941025553\n ],\n [\n -82.49798608995513,\n 28.219395941025553\n ],\n [\n -82.49798608995513,\n 27.382784530994\n ],\n [\n -81.47943871799596,\n 27.382784530994\n ],\n [\n -81.47943871799596,\n 28.219395941025553\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db6100a2","contributors":{"authors":[{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200291,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sutcliffe, Horace Jr.","contributorId":96725,"corporation":false,"usgs":true,"family":"Sutcliffe","given":"Horace","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":200292,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":46411,"text":"ofr84331 - 1984 - Measured sections of late Paleozoic and Mesozoic rocks, Mount Michelson Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:04:59","indexId":"ofr84331","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-331","title":"Measured sections of late Paleozoic and Mesozoic rocks, Mount Michelson Quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/ofr84331","usgsCitation":"Detterman, R.L., 1984, Measured sections of late Paleozoic and Mesozoic rocks, Mount Michelson Quadrangle, Alaska: U.S. Geological Survey Open-File Report 84-331, 1 map and 17 stratigraphic sections on 2 sheets :photocopy ;sheets 101 x 108 cm., https://doi.org/10.3133/ofr84331.","productDescription":"1 map and 17 stratigraphic sections on 2 sheets :photocopy ;sheets 101 x 108 cm.","costCenters":[],"links":[{"id":135862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21004,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0331/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21005,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0331/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610e05","contributors":{"authors":[{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":233232,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61993,"text":"mr91 - 1984 - Map showing occurrences of lead minerals in Alaska","interactions":[{"subject":{"id":45907,"text":"ofr8373 - 1982 - Occurrences of lead minerals in Alaska","indexId":"ofr8373","publicationYear":"1982","noYear":false,"title":"Occurrences of lead minerals in Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":61993,"text":"mr91 - 1984 - Map showing occurrences of lead minerals in Alaska","indexId":"mr91","publicationYear":"1984","noYear":false,"title":"Map showing occurrences of lead minerals in Alaska"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:36","indexId":"mr91","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"91","title":"Map showing occurrences of lead minerals in Alaska","language":"ENGLISH","doi":"10.3133/mr91","usgsCitation":"Cobb, E.H., 1984, Map showing occurrences of lead minerals in Alaska: U.S. Geological Survey Mineral Investigations Resource Map 91, 1 map :col. ;80 x 104 cm., on sheet 94 x 122 cm., https://doi.org/10.3133/mr91.","productDescription":"1 map :col. ;80 x 104 cm., on sheet 94 x 122 cm.","costCenters":[],"links":[{"id":180579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260444,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/91/plate-1.pdf"}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -172,51.25 ], [ -172,71 ], [ -130,71 ], [ -130,51.25 ], [ -172,51.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db654903","contributors":{"authors":[{"text":"Cobb, Edward Huntington","contributorId":13629,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":266661,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28748,"text":"wri844065 - 1984 - Availability and chemistry of ground water on the Bruneau Plateau and adjacent eastern plain in Twin Falls County, south-central Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri844065","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4065","title":"Availability and chemistry of ground water on the Bruneau Plateau and adjacent eastern plain in Twin Falls County, south-central Idaho","docAbstract":"The Bruneau plateau in south-central Idaho consists of about 889 ,600 acres of potentially irrigable land. About 112,200 of these acres have been developed for agriculture; 11,200 acres are irrigated with ground water, and the remaining acreage is irrigated with water from the Snake and Bruneau rivers and Salmon Falls Creek. On the basis of present usage, about 158,000 acre-feet of water per year are needed to develop an additional 63,000 acres. About 438,000 acre-feet per year are needed to irrigate existing and newly developed lands in dry years when streamflow in the Snake River at Milner Dam is inadequate to meet appropriated needs. Pumping lifts of about 400-600 feet and low well yields on the Bruneau plateau probably preclude large-scale irrigation development solely from local ground-water resources. However, supplemental sources of irrigation water are available from a perched-water aquifer, a thermal aquifer, and the regional aquifer adjacent to the plateau. About 100,000-115,000 acre-feet per year of water probably could be withdrawn from the perched and regional aquifers and conveyed to the plateau without serious impact on local ground-water resources. The amount of water that could be safely withdrawn from the thermal aquifer was not determined. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844065","usgsCitation":"Moffatt, R.L., and Jones, M., 1984, Availability and chemistry of ground water on the Bruneau Plateau and adjacent eastern plain in Twin Falls County, south-central Idaho: U.S. Geological Survey Water-Resources Investigations Report 84-4065, vi, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844065.","productDescription":"vi, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4065/report-thumb.jpg"},{"id":57597,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4065/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57598,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4065/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57599,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655e5b","contributors":{"authors":[{"text":"Moffatt, R. L.","contributorId":79889,"corporation":false,"usgs":true,"family":"Moffatt","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200331,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, M.L.","contributorId":88731,"corporation":false,"usgs":true,"family":"Jones","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":200332,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28749,"text":"wri844345 - 1984 - Conceptual hydrologic model of flow in the unsaturated zone, Yucca Mountain, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri844345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4345","title":"Conceptual hydrologic model of flow in the unsaturated zone, Yucca Mountain, Nevada","docAbstract":"The unsaturated volcanic tuffs beneath Yucca Mountain, Nevada, are being evaluated as a host rock for a potential repository for high-level radioactive waste. A conceptual hydrologic model is proposed to describe the flow of fluids through these rocks. Thickness of the unsaturated zone is about 500 to 750 meters and consists of three welded units interlayered with two nonwelded units. Compared to nonwelded units, welded units have low matrix porosities and permeabilities, high fracture densities, and high bulk hydraulic conductivities. The principal repository area is bounded by normal fault zones. Of the average annual precipitation of 150 millimeters per year, 0.5 to 4.5 millimeters per year becomes net infiltration. Percolation through the matrix of the welded units is principally vertical and is less than 1 millimeter per year. Percolation through nonwelded units occurs both vertically and laterally and has variable rates (0.1 to 100 millimeters per year). Fracture flow is predominant in the uppermost welded unit during intense pulses of infiltration, but is insignificant in the welded unit that forms the potential host rock. Lateral flow in the upper nonwelded unit, enhanced by existence of a capillary barrier, probably is the factor controlling the low fluxes in the host rock and relatively high fluxes in the structural features. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844345","usgsCitation":"Montazer, P., and Wilson, W., 1984, Conceptual hydrologic model of flow in the unsaturated zone, Yucca Mountain, Nevada: U.S. Geological Survey Water-Resources Investigations Report 84-4345, iv, 55 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844345.","productDescription":"iv, 55 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4345/report-thumb.jpg"},{"id":57600,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4345/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64a9ac","contributors":{"authors":[{"text":"Montazer, P.M.","contributorId":93946,"corporation":false,"usgs":true,"family":"Montazer","given":"P.M.","affiliations":[],"preferred":false,"id":200333,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, W.E.","contributorId":100831,"corporation":false,"usgs":true,"family":"Wilson","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":200334,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4116,"text":"cir905 - 1984 - Vertical crustal movements in Southern California, 1974 to 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"cir905","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"905","title":"Vertical crustal movements in Southern California, 1974 to 1978","docAbstract":"An extensive resurvey of most of the first-order leveling network in southern California, known as the Southern California Releveling Program (SCRP), was carried out during the first 5 months of 1978. The primary scientific purpose of these measurements was to rapidly update the vertical control record throughout a recently uplifted region of southern California in order to more thoroughly document the vertical component of tectonic movement and to provide a reliable base for comparison with future levelings. Analyses of historic first-order leveling results have clearly demonstrated that a broad crustal upwarping, largely contained within a region consisting of the Transverse Ranges province and an area along the intervening section of the San Andreas fault system, had developed between about 1959 and 1974. Unfortunately, there is strong evidence that parts of the 1978 SCRP data are contaminated by the effects of intrasurvey tectonic deformation, limited surficial failures, and, less certainly, magnetically induced systematic error associated with the use of automatic levels. However, any distortions in leveling results caused by these or other factors are not so serious as to render the SCRP data useless. In fact, the bulk of these data can be accepted at face value, and most of the remaining data can be incorporated with some caution to augment the more reliable parts of the network. The evaluation of the 1978 leveling is based on a combination of circuit-misclosures, local timing of the field observations, analysis of profiles of apparent height changes derived from comparisons with previous levelings, and an analysis of the position and orientation of the various routes in relation to the regional structural grain and the gradients of differential vertical motion established by previous investigations. Comparisons of the 1978 SCRP results with the latest of the previous surveys along each route retained in the analysis show that all but about one-third of the uplift established by leveling data from 1959 to the combined 1974/76 survey period had relaxed by early 1978 through tectonic subsidence. Subsequent limited relevelings along several of the 1978 routes show that rapid tectonic subsidence probably continued through at least early 1979. Despite the pronounced down-to-the-northeast (northeastward) tilt that developed between 1976 and early 1978, the overall shape of the uplift was well preserved. Results of repeated trilateration surveys since 1971 demonstrate that a remarkably uniform and nearly monotonic negative dilatational strain-change trend reversed abruptly between 1977 and 1979. The change from tectonic up to tectonic subsidence is associated with this reversal in horizontal strain accumulation. The reversal in strain trend was expressed as a cessation of the essentially uniaxial north-south contraction, which had been accumulating at about 2? 10 -7/yr (or 0.2 ?strain/yr), accompanied by onset of uniaxial east-west \r\nextension at about 5 ? 10 -7/yr (or 0.5 ?strain/yr). Minor earthquakes and occasional swarms of moderate earthquakes were particularly abundant during 1978 and 1979 in conspicuously mobile regions such as the eastern Transverse Ranges and the Salton Trough, areas respectively characterized by nearly complete collapse of the previous maximum uplift and by a dramatic enhancement of the previously identified tectonic subsidence.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir905","usgsCitation":"Burford, R.O., and Gilmore, T.D., 1984, Vertical crustal movements in Southern California, 1974 to 1978: U.S. Geological Survey Circular 905, iii, 22 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir905.","productDescription":"iii, 22 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":124535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0905/report-thumb.jpg"},{"id":31217,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0905/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6020dd","contributors":{"authors":[{"text":"Burford, Robert O.","contributorId":52560,"corporation":false,"usgs":true,"family":"Burford","given":"Robert","middleInitial":"O.","affiliations":[],"preferred":false,"id":148231,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilmore, Thomas D.","contributorId":64235,"corporation":false,"usgs":true,"family":"Gilmore","given":"Thomas","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":148232,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4334,"text":"cir932 - 1984 - Interlaboratory comparison of mineral constituents in a sample from the Herrin (No. 6) coal bed from Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir932","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"932","title":"Interlaboratory comparison of mineral constituents in a sample from the Herrin (No. 6) coal bed from Illinois","docAbstract":"Approximately 20 kg of the Herrin (No. 6) coal was collected from a strip mine in St. Clair County, Ill. A 10-kg portion was ground to -60 mesh, homogenized, and riffled into 128 splits of 70-80 g each. Homogeneity of these splits was confirmed by moisture, ash, and sulfur analyses of six randomly selected splits. Results of these analyses were within the ASTM (American Society for Testing and Materials) guidelines for interlaboratory precision. Splits of the Herrin (No. 6) coal were then transmitted to more than 30 laboratories for analysis. \r\n\r\nLow-temperature plasma oxidation was used to isolate inorganic matter for quantitative chemical and mineralogical analysis. Despite a wide variation in ashing conditions, only minor variations in ash yields were obtained; these variations were attributed to differences in operating temperature and moisture content. Mineralogical analyses of low-temperature ash (LTA) concentrates prepared by five different laboratories indicated variations within the limits of analytical error. The mean values, in weight percent, for the major minerals are as follows: calcite, 9; quartz, 20; pyrite, 23; kaolinite, 14; and illite+mixed-layer clays, 31. Normative mineralogical calculations and Fourier transform infrared analysis (FTIR) yielded results similar to those obtained from X-ray diffraction (XRD). Choosing appropriate mineral standards was found to be critical for the proper use of analytical techniques such as XRD and FTIR. \r\n\r\nGood interlaboratory agreement was obtained for most major, minor, and trace elements despite differences in analytical procedures and in the type of sample analyzed (coal, high-temperature ash, or LTA). Discrepancies between analyses for zinc, strontium, manganese, and iron may be attributed to sampling inhomogeneity problems. Mossbauer spectroscopy showed that approximately 44 percent of the pyritic sulfur was lost through weathering in the first year after preparation of the interlaboratory sample. Szomolnokite and possibly coquimbite and jarosite were also identified. Scanning electron microscopy studies indicated ubiquitous pyrite framboids and, less commonly, euhedral crystals, skeletal grains, irregularly shaped particles, and vein fillings. Minor accessory minerals such as rare-earth phosphates and possibly silicates, zircon, barium sulfate, titanium oxide, and sphalerite were also found. The textural evidence indicates that the minerals in the banded material are detrital whereas the minerals occurring as vein and pore fillings are authigenic. 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