This report on ground-water levels, springs and depth to ground water in the Basin and Range province of southern California (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger (1984). Also included in this report are selected references on pertinent geologic and hydrologic studies of the region. Other map reports in this series contain detailed data on ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834116B","usgsCitation":"Langer, W.H., Moyle, W., Woolfenden, L.R., and Mulvihill, D.A., 1984, Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Southern California: U.S. Geological Survey Water-Resources Investigations Report 83-4116, Report: 6 p.; 2 Plates: 41.09 x 53.96 inches and 41.37 x 53.85 inches, https://doi.org/10.3133/wri834116B.","productDescription":"Report: 6 p.; 2 Plates: 41.09 x 53.96 inches and 41.37 x 53.85 inches","costCenters":[],"links":[{"id":373616,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4116b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4116b/report-thumb.jpg"},{"id":373615,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4116b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54425,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4116b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.87158203125,\n 32.509761735919426\n ],\n [\n -114.14794921875,\n 32.509761735919426\n ],\n [\n -114.14794921875,\n 38.805470223177466\n ],\n [\n -120.87158203125,\n 38.805470223177466\n ],\n [\n -120.87158203125,\n 32.509761735919426\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a5d","contributors":{"authors":[{"text":"Langer, William H. blanger@usgs.gov","contributorId":1241,"corporation":false,"usgs":true,"family":"Langer","given":"William","email":"blanger@usgs.gov","middleInitial":"H.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":false,"id":194526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moyle, W. R.","contributorId":27421,"corporation":false,"usgs":true,"family":"Moyle","given":"W. R.","affiliations":[],"preferred":false,"id":194524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woolfenden, L. R. 0000-0003-3500-4709","orcid":"https://orcid.org/0000-0003-3500-4709","contributorId":36945,"corporation":false,"usgs":true,"family":"Woolfenden","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":194525,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mulvihill, D. A.","contributorId":73644,"corporation":false,"usgs":true,"family":"Mulvihill","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194527,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":25653,"text":"wri834120B - 1984 - Maps showing ground-water levels, springs, and depth to water, Basin and Range Province, Oregon","interactions":[],"lastModifiedDate":"2022-02-04T21:00:44.583569","indexId":"wri834120B","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":"83-4120","chapter":"B","title":"Maps showing ground-water levels, springs, and depth to water, Basin and Range Province, Oregon","docAbstract":"This report on ground-water levels, springs and depth to ground water in the Basin and Range province of Oregon (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger (1984). Also included in this report are selected references on pertinent geologic and hydrologic studies of the region. Other map reports in this series contain detailed data on ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources.
This map report is one of a series of geologic and hydrologic maps of States in the Basin and Range Province. These map reports contain information on ground-water hydrology, ground-water quality, surface distribution of selected rock types, data on tectonic conditions, areal geophysical data, Pleistocene lakes and marshes and natural resources. This information is the basis for a summary report that characterizes the Basin and Range Province. The geologic and hydrologic characterization will be used to evaluate the Province for prospective regions for further study relative to isolation of high-level radioactive waste. (Bedinger, Sargent and Reed, 1984).
This report on ground-water levels, springs, and depth to ground water in the Basin and Range province of Utah (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger (1984) . Also included in this report are selected references on pertinent geologic and hydrologic studies of the region. Other map reports in this series contain detailed data on ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNE831","usgsCitation":"Engel, G., Engberg, R., and Johnson, M., 1984, Water resources data, Nebraska water year 1983: U.S. Geological Survey Water Data Report NE-83-1, viii, 391 p., https://doi.org/10.3133/wdrNE831.","productDescription":"viii, 391 p.","costCenters":[],"links":[{"id":381082,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/ne-83-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1983/ne-83-1/report-thumb.jpg"}],"country":"United 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A.","contributorId":104876,"corporation":false,"usgs":true,"family":"Engberg","given":"R. A.","affiliations":[],"preferred":false,"id":256557,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, M.S.","contributorId":49382,"corporation":false,"usgs":true,"family":"Johnson","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":256556,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26232,"text":"wri844058 - 1984 - Estimation of streamflow for selected sites on the Carson and Truckee rivers in California and Nevada, 1944-80","interactions":[],"lastModifiedDate":"2012-02-02T00:08:32","indexId":"wri844058","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":"84-4058","title":"Estimation of streamflow for selected sites on the Carson and Truckee rivers in California and Nevada, 1944-80","docAbstract":"Daily mean and monthly discharges were estimated for 10 sites on the Carson and Truckee Rivers for periods of incomplete records and for tributary sites affected by reservoir regulation. On the basis of the hydrologic characteristics, stream-flow data for a water year were grouped by month or season for subsequent regression analysis. In most cases, simple linear regressions adequately defined a relation of streamflow between gaging stations, but in some instances a nonlinear relation for several months of the water year was derived. Statistical data are presented to indicate the reliability of the estimated streamflow data. Records of discharges including historical and estimated data for the gaging stations for the water years 1944-80 are presented. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844058","usgsCitation":"Blodgett, J.C., Oltmann, R., and Poeschel, K., 1984, Estimation of streamflow for selected sites on the Carson and Truckee rivers in California and Nevada, 1944-80: U.S. Geological Survey Water-Resources Investigations Report 84-4058, iv, 223 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844058.","productDescription":"iv, 223 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":121907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4058/report-thumb.jpg"},{"id":55031,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4058/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649fe2","contributors":{"authors":[{"text":"Blodgett, J. C.","contributorId":32154,"corporation":false,"usgs":true,"family":"Blodgett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":196026,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oltmann, R.N.","contributorId":69164,"corporation":false,"usgs":true,"family":"Oltmann","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":196027,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poeschel, K.R.","contributorId":98715,"corporation":false,"usgs":true,"family":"Poeschel","given":"K.R.","affiliations":[],"preferred":false,"id":196028,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":17892,"text":"ofr84232 - 1984 - Water-resources investigations of the U.S. Geological Survey in Arkansas; fiscal years 1982 and 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:07:14","indexId":"ofr84232","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":"84-232","title":"Water-resources investigations of the U.S. Geological Survey in Arkansas; fiscal years 1982 and 1983","docAbstract":"During fiscal years 1982 and 1983 there were 22 water resources investigations in progress by the Arkansas District of the U.S. Geological Survey 's Water Resources Division. Investigations that mainly involved data collection included surface water gaging, water level measuring, water quality sampling, sediment sampling and water use inventorying. Interpretive studies included two that were principally of groundwater resources, five that were of surface water flow characteristics, one that was of surface water quality characteristics and six that were interdisciplinary. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84232","usgsCitation":"Louthian, B., 1984, Water-resources investigations of the U.S. Geological Survey in Arkansas; fiscal years 1982 and 1983: U.S. Geological Survey Open-File Report 84-232, iv, 49 p. :maps ;28 cm., https://doi.org/10.3133/ofr84232.","productDescription":"iv, 49 p. :maps ;28 cm.","costCenters":[],"links":[{"id":149115,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0232/report-thumb.jpg"},{"id":47131,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0232/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9ca5","contributors":{"authors":[{"text":"Louthian, B.L.","contributorId":48574,"corporation":false,"usgs":true,"family":"Louthian","given":"B.L.","affiliations":[],"preferred":false,"id":178132,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60972,"text":"mf1694 - 1984 - Seismicity map of the state of Colorado","interactions":[{"subject":{"id":60972,"text":"mf1694 - 1984 - Seismicity map of the state of Colorado","indexId":"mf1694","publicationYear":"1984","noYear":false,"title":"Seismicity map of the state of Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":60973,"text":"mf2036 - 1988 - Seismicity map of the state of Colorado","indexId":"mf2036","publicationYear":"1988","noYear":false,"title":"Seismicity map of the state of Colorado"},"id":1}],"supersededBy":{"id":60973,"text":"mf2036 - 1988 - Seismicity map of the state of Colorado","indexId":"mf2036","publicationYear":"1988","noYear":false,"title":"Seismicity map of the state of Colorado"},"lastModifiedDate":"2017-05-11T13:48:00","indexId":"mf1694","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":"1694","title":"Seismicity map of the state of Colorado","docAbstract":"The data shown on this map and listed in table 1 are for earthquakes that were originally included in a study of seismic risk in the United States (Algermissen, 1969). This data file has been recompiled and updated through 1981. Some revisions of epicenters and intensities in the original file have been made, and intensities have been assigned to earthquakes that previously had none assigned. Only earthquakes that had epicenters within the boundary of the state are listed in table 1, even though earthquakes that had epicenters in bordering states or countries may have been felt or may have caused damage in the state. Intensity values were updated from data sources that were not available at the time or original compilation. Some epicenters were relocated on the basis of new information. The data shown in table 1 represent best estimates of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for the earthquakes that occurred before seismic instruments were universally used.
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Data were collected to calibrate and verify steady-state digital, stream, water-quality models. The models were then used to simulate changes in instream diel-minimum dissolved-oxygen resulting from changes in nutrient loading. The city of Fayetteville proposes to divert part of its projected wastewater-treatment plant discharge to Illinois River. Muddy Fork, Spring Creek, and Osage Creek currently received effluent from the cities of Prairie Grove, Springdale, and Rogers, respectively. The diel-minimum dissolved-oxygen standard for each of these streams is 4.0 mg/L under projected loadings. Data collected indicate that none of the four streams meet Arkansas state standards for diel-minimum dissolved oxygen, total phosphorus, and fecal coliform bacteria. Computed dissolved-oxygen deficits indicate that benthal demand is the principal reason for dissolved-oxygen not meeting standards. Model simulations indicate that Spring Creek and Osage Creek can meet dissolved oxygen standards with stringent effluent limits imposed at the inspecting waste water-treatment plants; Muddy Fork and Illinois River can not. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834092","usgsCitation":"Terry, J.E., Morris, E.E., Petersen, J.C., and Darling, M., 1984, Water-quality assessment of the Illinois River basin, Arkansas: U.S. Geological Survey Water-Resources Investigations Report 83-4092, 435 p. :ill. ;28 cm., https://doi.org/10.3133/wri834092.","productDescription":"435 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":158082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4092/report-thumb.jpg"},{"id":54579,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6f06","contributors":{"authors":[{"text":"Terry, J. 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E.","contributorId":93493,"corporation":false,"usgs":true,"family":"Morris","given":"E.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":195258,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petersen, Jim C.","contributorId":43816,"corporation":false,"usgs":true,"family":"Petersen","given":"Jim","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":195255,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Darling, M.E.","contributorId":82355,"corporation":false,"usgs":true,"family":"Darling","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":195256,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":55705,"text":"wdrMO831 - 1984 - Water resources data, Missouri, water year 1983","interactions":[],"lastModifiedDate":"2025-07-18T16:09:31.840177","indexId":"wdrMO831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MO-83-1","title":"Water resources data, Missouri, water year 1983","docAbstract":"Water resources data for the 1983 water year for Missouri consist of records of stage, discharge, and water quality of lakes and reservoirs; contains records for water discharge at 110 gaging stations; stage and contents at 9 lakes and reservoirs; water quality at 24 gaging stations (including 1 lake) and data for 35 crest-stage, and 30 water-quality partial record stations.
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Data collected before construction on a 2.81 sq m (7.28 sq km) agricultural watershed (upper Spring Creek) near Rockford, IL, show that during a 2-year period ending June 30, 1981, 2,890 tons (2,620 Mg) of suspended sediment were transported from the watershed. Of the 2 ,890 tons (2,620 Mg), 2,690 tons (2,440 Mg) or 93.1 % were transported during a storm in a 46.6-hour period of June 13-14, 1981. Runoff from a 0.031 sq m (0.080 sq km) subbasin (Spring Creek tributary) transported 33.9 tons (30.9 Mg) of suspended sediment during a 3.2-hour storm period on June 13, 1981. Regression models relating storm suspended-sediment yields and peak-water discharge per square mile for upper Spring Creek and Spring Creek tributary have average standard errors of 57 and 24 %, respectively. Trace amounts of currently banned pesticides, including Aldrin and DDT, were detected in streambed material samples. Documented sediment yields, chemical quality, and relations between runoff and sediment discharge provide baseline information for future evaluation of hydrologic conditions in the watershed. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824073","usgsCitation":"Allen, H., and Gray, J.R., 1984, Runoff, sediment transport, and water quality in a northern Illinois agricultural watershed before urban development, 1979-81: U.S. Geological Survey Water-Resources Investigations Report 82-4073, vii, 55 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824073.","productDescription":"vii, 55 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4073/report-thumb.jpg"},{"id":54658,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5face6","contributors":{"authors":[{"text":"Allen, H.E. Jr.","contributorId":63054,"corporation":false,"usgs":true,"family":"Allen","given":"H.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":195440,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gray, J. R.","contributorId":63372,"corporation":false,"usgs":true,"family":"Gray","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":195441,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2221,"text":"wsp2197 - 1984 - Ground-water monitoring at Santa Barbara, California: Phase 2 — Effects of pumping on water levels and on water quality in the Santa Barbara ground-water basin","interactions":[{"subject":{"id":10186,"text":"ofr82366 - 1982 - Ground-water monitoring at Santa Barbara, California; Phase 2-effects of pumping on water levels and water quality in the Santa Barbara ground-water basins","indexId":"ofr82366","publicationYear":"1982","noYear":false,"title":"Ground-water monitoring at Santa Barbara, California; Phase 2-effects of pumping on water levels and water quality in the Santa Barbara ground-water basins"},"predicate":"SUPERSEDED_BY","object":{"id":2221,"text":"wsp2197 - 1984 - Ground-water monitoring at Santa Barbara, California: Phase 2 — Effects of pumping on water levels and on water quality in the Santa Barbara ground-water basin","indexId":"wsp2197","publicationYear":"1984","noYear":false,"title":"Ground-water monitoring at Santa Barbara, California: Phase 2 — Effects of pumping on water levels and on water quality in the Santa Barbara ground-water basin"},"id":1}],"lastModifiedDate":"2022-01-04T20:05:24.878393","indexId":"wsp2197","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":"2197","title":"Ground-water monitoring at Santa Barbara, California: Phase 2 — Effects of pumping on water levels and on water quality in the Santa Barbara ground-water basin","docAbstract":"From July 1978 to January 1980, water levels in the southern part of the Santa Barbara ground-water basin declined more than 100 feet. These water-level declines resulted from increases in municipal pumping since July 1978. The increase in municipal pumping was part of a basin-testing program designed to determine the usable quantity of ground water in storage. The pumping, centered in the city less than 1 mile from the coast, has caused water-level declines to altitudes below sea level in the main water-bearing zones. As a result, the ground-water basin would be subject to saltwater intrusion if the study-period pumpage were maintained or increased. \r\n\r\nData indicate that saltwater intrusion has degraded the quality of the water yielded from six coastal wells. During the study period, the six coastal wells all yielded water with chloride concentrations in excess of 250 milligrams per liter, and four of the wells yielded water with chloride concentrations in excess of 1,000 milligrams per liter. \r\n\r\nPrevious investigators believed that saltwater intrusion was limited to the shallow part of the aquifer, directly adjacent to the coast. The possibility of saltwater intrusion into the deeper water-bearing deposits in the aquifer was thought to be remote because an offshore fault truncates these deeper deposits so that they lie against consolidated rocks on the seaward side of the fault. Results of this study indicate, however, that ocean water has intruded the deeper water-bearing deposits, and to a much greater extent than in the shallow part of the aquifer. Apparently the offshore fault is not an effective barrier to saltwater intrusion. \r\n\r\nNo physical barriers are known to exist between the coast and the municipal well field. Therefore, if the pumping rate maintained during the basin-testing program were continued, the degraded water along the coast could move inland and contaminate the municipal supply wells. The time required for the degraded water to move from the coast to the nearest supply well is estimated, using Darcy's equation, to be about 20 years. \r\n\r\nManagement alternatives for controlling saltwater intrusion in the Santa Barbara area include (1) decreasing municipal pumping, (2) increasing the quantity of water available for recharge by releasing surplus water from surface reservoirs to Mission Creek, (3) artificially recharging the basin using injection wells, and (4) locating municipal supply wells farther from the coast and spacing them farther apart in order to minimize drawdown. Continued monitoring of water levels and water quality would enable assessment of the effectiveness of the control measures employed.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2197","usgsCitation":"Martin, P., 1984, Ground-water monitoring at Santa Barbara, California: Phase 2 — Effects of pumping on water levels and on water quality in the Santa Barbara ground-water basin: U.S. Geological Survey Water Supply Paper 2197, iv, 31 p., https://doi.org/10.3133/wsp2197.","productDescription":"iv, 31 p.","costCenters":[],"links":[{"id":27970,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2197/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2197/report-thumb.jpg"},{"id":393873,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25353.htm"}],"country":"United States","state":"California","city":"Santa Barbara","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.82376098632814,\n 34.3955786154917\n ],\n [\n -119.52713012695314,\n 34.3955786154917\n ],\n [\n -119.52713012695314,\n 34.513346401475786\n ],\n [\n -119.82376098632814,\n 34.513346401475786\n ],\n [\n -119.82376098632814,\n 34.3955786154917\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66078d","contributors":{"authors":[{"text":"Martin, Peter pmmartin@usgs.gov","contributorId":799,"corporation":false,"usgs":true,"family":"Martin","given":"Peter","email":"pmmartin@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":144841,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25702,"text":"wri844230 - 1984 - Phenolic contamination in the sand-and-gravel aquifer from a surface impoundment of wood treatment wastes, Pensacola, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:18","indexId":"wri844230","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":"84-4230","title":"Phenolic contamination in the sand-and-gravel aquifer from a surface impoundment of wood treatment wastes, Pensacola, Florida","docAbstract":"Creosote and pentachlorophenol wastewaters discharged to unlined surface impoundments have resulted in groundwater contamination in the vicinity of an industrial site near Pensacola, Florida. Total phenol concentrations of 36,000 microgm/liter have been detected 40 ft below land surface in a test hole 100 ft south of an overflow impoundment but less than 10 microgm/liter 90 ft below land surface. Samples collected in test holes 1,350 ft downgradient from the surface impoundments and 100 ft north of Pensacola Bay, above and immediately below a clay lens, indicate that phenol contaminated groundwater may not be discharging directly into Pensacola Bay. Phenol concentrations exceeding 20 microgm/liter were detected in samples from a drainage ditch discharging directly into Bayou Chico. Microbiological data collected near the test site suggest that an anaerobic methanogenic ecosystem contributes to a reduction in phenol concentrations in groundwater. A laboratory study using bacteria isolated from the study site indicates that phenol, 2-methylphenol, and 3-methylphenol are significantly degraded and that methanogenesis reduces total phenol concentrations in laboratory digestors by 45%. Pentachlorophenol may inhibit methanogenesis at concentrations exceeding 0.45 milligm/liter. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844230","usgsCitation":"Troutman, D., Godsy, E., Goerlitz, D., and Ehrlich, G.G., 1984, Phenolic contamination in the sand-and-gravel aquifer from a surface impoundment of wood treatment wastes, Pensacola, Florida: U.S. Geological Survey Water-Resources Investigations Report 84-4230, iv, 36 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844230.","productDescription":"iv, 36 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123635,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4230/report-thumb.jpg"},{"id":54464,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4230/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686216","contributors":{"authors":[{"text":"Troutman, D.E.","contributorId":66301,"corporation":false,"usgs":true,"family":"Troutman","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":194724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Godsy, E.M.","contributorId":56685,"corporation":false,"usgs":true,"family":"Godsy","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":194723,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":194722,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ehrlich, G. G.","contributorId":89126,"corporation":false,"usgs":true,"family":"Ehrlich","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":194725,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":57264,"text":"wdrIN831 - 1984 - Water resources data, Indiana, water year 1983","interactions":[],"lastModifiedDate":"2014-06-11T13:09:06","indexId":"wdrIN831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"IN-83-1","title":"Water resources data, Indiana, water year 1983","docAbstract":"Water resources data for the 1983 water year for Indiana consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels in wells. This report contains discharge records for 174 gaging stations, stage and contents for 9 lake and reservoirs, releases from 7 flood control reservoirs, water quality for 5 gaging stations, and water levels for 84 observation wells. Also included are 23 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Indiana.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrIN831","collaboration":"Prepared in cooperation with the State of Indiana and with other agencies","usgsCitation":"Miller, R.L., Hoggatt, R., and Nell, G., 1984, Water resources data, Indiana, water year 1983: U.S. Geological Survey Water Data Report IN-83-1, xiv, 292 p., https://doi.org/10.3133/wdrIN831.","productDescription":"xiv, 292 p.","numberOfPages":"309","temporalStart":"1982-10-01","temporalEnd":"1983-09-30","costCenters":[],"links":[{"id":288334,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288333,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/in-83-1/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb92c","contributors":{"authors":[{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":256508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoggatt, R.E.","contributorId":96751,"corporation":false,"usgs":true,"family":"Hoggatt","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":256509,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nell, G.E.","contributorId":45960,"corporation":false,"usgs":true,"family":"Nell","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":256507,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":57277,"text":"wdrNHVT831 - 1984 - Water resources data, New Hampshire and Vermont water year 1983","interactions":[],"lastModifiedDate":"2020-05-07T12:14:28.408537","indexId":"wdrNHVT831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"NH-VT-83-1","title":"Water resources data, New Hampshire and Vermont water year 1983","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNHVT831","usgsCitation":"Blackey, F., Cotton, J.E., and Toppin, K., 1984, Water resources data, New Hampshire and Vermont water year 1983: U.S. Geological Survey Water Data Report NH-VT-83-1, vii, 145 p., https://doi.org/10.3133/wdrNHVT831.","productDescription":"vii, 145 p.","costCenters":[],"links":[{"id":185011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2000/nh-vt-83-1/report-thumb.jpg"},{"id":374507,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2000/nh-vt-83-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Hampshire, Vermont","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.3447265625,\n 42.68243539838623\n ],\n [\n -70.68603515625,\n 42.68243539838623\n ],\n [\n -70.68603515625,\n 45.213003555993964\n ],\n [\n -73.3447265625,\n 45.213003555993964\n ],\n [\n -73.3447265625,\n 42.68243539838623\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb3f9","contributors":{"authors":[{"text":"Blackey, F.E.","contributorId":51797,"corporation":false,"usgs":true,"family":"Blackey","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":256559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cotton, J. E.","contributorId":52976,"corporation":false,"usgs":true,"family":"Cotton","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":256560,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Toppin, K. W.","contributorId":35776,"corporation":false,"usgs":true,"family":"Toppin","given":"K. W.","affiliations":[],"preferred":false,"id":256558,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":48777,"text":"ofr82508 - 1984 - Fluoride, Nitrate, and Dissolved-Solids Concentrations in Ground Waters of Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:10:10","indexId":"ofr82508","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":"82-508","title":"Fluoride, Nitrate, and Dissolved-Solids Concentrations in Ground Waters of Washington","docAbstract":"This study provides basic data on ground-water quality throughout the State. It is intended for uses in planning and management by agencies and individuals who have responsibility for or interest in, public health and welfare. It also provides a basis for directing future studies of ground-water quality toward areas where ground-water quality problems may already exist. The information presented is a compilation of existing data from numerous sources including: the Washington Departments of Ecology and Social and Health Services, the Environmental Protection Agency, as well as many other local, county, state and federal agencies and private corporations. Only data on fluoride, nitrate, and dissolved-solids concentrations in ground water are presented, as these constituents are among those commonly used to determine the suitability of water for drinking or other purposes. They also reflect both natural and man-imposed effects on water quality and are the most readily available water-quality data for the State of Washington. The percentage of wells with fluoride, nitrate, or dissolved-solids concentrations exceeding U.S. Environmental Protection Agency Primary and Secondary Drinking Water Regulations were about 1, about 3, and about 3, respectively. Most high concentrations occurred in widely separated wells. Two exceptions were: high concentrations of nitrate and dissolved solids in wells on the Hanford Department of Energy Facility and high concentrations of nitrate in the lower Yakima River basin. (USGS)","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr82508","collaboration":"Prepared in cooperation with the State of Washington Department of Ecology","usgsCitation":"Lum, W.E., and Turney, G.L., 1984, Fluoride, Nitrate, and Dissolved-Solids Concentrations in Ground Waters of Washington (WRI/OFR 82-508): U.S. Geological Survey Open-File Report 82-508, 4 Sheets (3 maps and 1 data sheet; each sheet 21 x 27 inches), https://doi.org/10.3133/ofr82508.","productDescription":"4 Sheets (3 maps and 1 data sheet; each sheet 21 x 27 inches)","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":169477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":85602,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0508/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85603,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0508/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85604,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0508/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85605,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0508/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125,45 ], [ -125,49 ], [ -116,49 ], [ -116,45 ], [ -125,45 ] ] ] } } ] }","edition":"WRI/OFR 82-508","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de650","contributors":{"authors":[{"text":"Lum, W. E. II","contributorId":81504,"corporation":false,"usgs":true,"family":"Lum","given":"W.","suffix":"II","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":238227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turney, Gary L.","contributorId":72446,"corporation":false,"usgs":true,"family":"Turney","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":238226,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44469,"text":"wri854095 - 1984 - Geohydrology of the valley-fill aquifer in the Bath area, Lower Cohocton River, Steuben County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:04:55","indexId":"wri854095","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":"85-4095","title":"Geohydrology of the valley-fill aquifer in the Bath area, Lower Cohocton River, Steuben County, New York","docAbstract":"The Bath valley-fill aquifer, southern New York, composed of outwash, ice-contact, and ice-disintegration sand and gravel, is highly productive and is in many areas in hydraulic contact with the Cohocton River. Potential well yields range 50 to more than 1,000 gallons per minute. Most of the aquifer is under shallow water-table conditions and vulnerable to surface contamination. Thickness ranges from 20 to 40 feet. Buried aquifers are present locally. The aquifer system underlies an area containing only a few small communities and therefore is not heavily pumped. Geohydrologic data are compiled on six maps at 1:24,000 scale and on a sheet of geologic sections. The maps depict surficial geology, soil-infiltration capacity, potentiometric surface, aquifer thickness, well yields, and land use. This map report set is one in a series of four that depict selected aquifers in Wester New York. It supplements a series that is being done by the U.S. Geological Survey in cooperation with State agencies. The maps are based largely on published reports, data filled in several State agencies, and some additional field data collection. (USGS)","language":"ENGLISH","doi":"10.3133/wri854095","usgsCitation":"Pagano, T.S., Terry, D., Shaw, M., and Ingram, A., 1984, Geohydrology of the valley-fill aquifer in the Bath area, Lower Cohocton River, Steuben County, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4095, 6 maps and 1 section on 7 sheets ; 92 x 117 cm. and 104 x 115 cm., folded in envelope 39 x 30 cm., https://doi.org/10.3133/wri854095.","productDescription":"6 maps and 1 section on 7 sheets ; 92 x 117 cm. and 104 x 115 cm., folded in envelope 39 x 30 cm.","costCenters":[],"links":[{"id":134840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81806,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4095/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81807,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4095/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81808,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4095/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81809,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4095/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81810,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4095/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81811,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4095/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81812,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4095/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a87d0","contributors":{"authors":[{"text":"Pagano, Timothy S.","contributorId":9628,"corporation":false,"usgs":true,"family":"Pagano","given":"Timothy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":229825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terry, D.B.","contributorId":107249,"corporation":false,"usgs":true,"family":"Terry","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":229827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shaw, M.L.","contributorId":70358,"corporation":false,"usgs":true,"family":"Shaw","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":229826,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ingram, A.W.","contributorId":8433,"corporation":false,"usgs":true,"family":"Ingram","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":229824,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":48838,"text":"ofr83852 - 1984 - Description and evaluation of the information transfer workshop series \"Coal hydrology in Virginia\"","interactions":[],"lastModifiedDate":"2012-02-02T00:10:05","indexId":"ofr83852","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":"83-852","title":"Description and evaluation of the information transfer workshop series \"Coal hydrology in Virginia\"","docAbstract":"A series of workshops was conducted in September, 1982, by staff of the Virginia Office, Mid-Atlantic District of the U.S.-Geological Survey for the benefit of coal operators, consultants, and resource managers in the coal-producing area of southwest Virginia. The purpose of the workshop series was to present hydrologic information and data by the U.S. Geological Survey collected during four years of study of the. coal hydrology of Virginia. The workshop series was held one day a week for three weeks at two locations within southwest Virginia in order to reduce travel time and overnight travel costs for participants. Results of an independently conducted questionnaire indicate the series was a success. The report summarizes the workshop preparation, organization, and presentation, and gives general conclusions and suggestions for those interested in conducting workshops.","language":"ENGLISH","doi":"10.3133/ofr83852","usgsCitation":"Hufschmidt, P.W., 1984, Description and evaluation of the information transfer workshop series \"Coal hydrology in Virginia\": U.S. Geological Survey Open-File Report 83-852, 23 p. ill., map ; 28 cm., https://doi.org/10.3133/ofr83852.","productDescription":"23 p. ill., map ; 28 cm.","costCenters":[],"links":[{"id":162746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0852/report-thumb.jpg"},{"id":85671,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0852/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db44","contributors":{"authors":[{"text":"Hufschmidt, Peter W.","contributorId":85185,"corporation":false,"usgs":true,"family":"Hufschmidt","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":238394,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20655,"text":"ofr84242 - 1984 - Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report No. 3","interactions":[],"lastModifiedDate":"2012-02-02T00:07:47","indexId":"ofr84242","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":"84-242","title":"Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report No. 3","docAbstract":"Rainfall and discharge data collected at 21 urban hydrology sites in Tennessee from July 1977 to September 1983 are summarized. These rainfall-runoff data will be used to calibrate a U.S. Geological Survey Rainfall-Runoff Model. The results of the model calibrations will then be used to develop reliable methods for determining the magnitude and frequency of floods on small streams in Tennessee where urbanization is a factor. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84242","usgsCitation":"Robbins, C.H., 1984, Effects of urbanization on the magnitude and frequency of floods on small streams in Tennessee; basic data report No. 3: U.S. Geological Survey Open-File Report 84-242, iii, 32 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84242.","productDescription":"iii, 32 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":1138,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr84-242","linkFileType":{"id":5,"text":"html"}},{"id":153982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fdfe","contributors":{"authors":[{"text":"Robbins, C. H.","contributorId":54210,"corporation":false,"usgs":true,"family":"Robbins","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":183010,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44461,"text":"wri854040 - 1984 - Geohydrology of the valley-fill aquifer in the Cohocton area, upper Cohocton River, Steuben County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"wri854040","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":"85-4040","title":"Geohydrology of the valley-fill aquifer in the Cohocton area, upper Cohocton River, Steuben County, New York","docAbstract":"The Cohocton valley-fill aquifer, composed of outwash, kame, and alluvial sand and gravel, is highly productive and is in hydraulic contact with the Cohocton River. Potential well yields range from 50 to more than 1,000 gallons per minute. Most of the aquifer is under shallow water-table conditions and vulnerable to surface contamination. Thickness ranges from 20 to 100 feet. The aquifer lies in an area containing only small communities and therefore is not heavily pumped. Geohydrologic data are compiled on six maps at 1:24,000 scale and in geologic sections. The maps depict surficial geology, soil-infiltration capacity, potentiometric surface, aquifer thickness, well yields, and land use. The maps are designed to help planners evaluate developments that may affect the aquifer, particularly potential contamination sources. This set is one in a series of four that depict selected aquifers in western New York. It supplements a series that is being done by the U.S. Geological Survey in cooperation with State agencies. The maps are based largely on published reports, file data in several State agencies, and field notes. (USGS)","language":"ENGLISH","doi":"10.3133/wri854040","usgsCitation":"Terry, D.B., Pagano, T.S., Shaw, M.L., and Ingram, A.W., 1984, Geohydrology of the valley-fill aquifer in the Cohocton area, upper Cohocton River, Steuben County, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4040, 6 maps and 1 section on 7 sheets ; 61 x 89 cm. and 101 x 94 cm., https://doi.org/10.3133/wri854040.","productDescription":"6 maps and 1 section on 7 sheets ; 61 x 89 cm. and 101 x 94 cm.","costCenters":[],"links":[{"id":162058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81782,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81783,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4040/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81784,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4040/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81785,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4040/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81786,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4040/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81787,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4040/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81788,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4040/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a87d5","contributors":{"authors":[{"text":"Terry, David B.","contributorId":102045,"corporation":false,"usgs":true,"family":"Terry","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":229812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pagano, Timothy S.","contributorId":9628,"corporation":false,"usgs":true,"family":"Pagano","given":"Timothy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":229809,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shaw, Martha L.","contributorId":28287,"corporation":false,"usgs":true,"family":"Shaw","given":"Martha","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229811,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ingram, Arlynn W.","contributorId":10015,"corporation":false,"usgs":true,"family":"Ingram","given":"Arlynn","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":229810,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":25449,"text":"wri834160 - 1984 - A digital model for streamflow routing by convolution methods","interactions":[],"lastModifiedDate":"2012-02-02T00:08:19","indexId":"wri834160","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":"83-4160","title":"A digital model for streamflow routing by convolution methods","docAbstract":"U.S. Geological Survey computer model, CONROUT, for routing streamflow by unit-response convolution flow-routing techniques from an upstream channel location to a downstream channel location has been developed and documented. Calibration and verification of the flow-routing model and subsequent use of the model for simulation is also documented. Three hypothetical examples and two field applications are presented to illustrate basic flow-routing concepts. Most of the discussion is limited to daily flow routing since, to date, all completed and current studies of this nature involve daily flow routing. However, the model is programmed to accept hourly flow-routing data. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/wri834160","usgsCitation":"Doyle, W., Shearman, H., Stiltner, G., and Krug, W., 1984, A digital model for streamflow routing by convolution methods: U.S. Geological Survey Water-Resources Investigations Report 83-4160, vi, 136 p. :ill., charts ;28 cm., https://doi.org/10.3133/wri834160.","productDescription":"vi, 136 p. :ill., charts ;28 cm.","costCenters":[],"links":[{"id":124901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4160/report-thumb.jpg"},{"id":54183,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aed4c","contributors":{"authors":[{"text":"Doyle, W.H. Jr.","contributorId":59029,"corporation":false,"usgs":true,"family":"Doyle","given":"W.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":193741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shearman, H.O.","contributorId":40630,"corporation":false,"usgs":true,"family":"Shearman","given":"H.O.","email":"","affiliations":[],"preferred":false,"id":193739,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stiltner, G.J.","contributorId":56668,"corporation":false,"usgs":true,"family":"Stiltner","given":"G.J.","affiliations":[],"preferred":false,"id":193740,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Krug, W.O.","contributorId":77964,"corporation":false,"usgs":true,"family":"Krug","given":"W.O.","email":"","affiliations":[],"preferred":false,"id":193742,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":746,"text":"wsp2229 - 1984 - Test well DO-CE 88 at Cambridge, Dorchester County, Maryland","interactions":[{"subject":{"id":7572,"text":"ofr821015 - 1982 - Test well DO-CE 88 at Cambridge, Dorchester County, Maryland","indexId":"ofr821015","publicationYear":"1982","noYear":false,"title":"Test well DO-CE 88 at Cambridge, Dorchester County, Maryland"},"predicate":"SUPERSEDED_BY","object":{"id":746,"text":"wsp2229 - 1984 - Test well DO-CE 88 at Cambridge, Dorchester County, Maryland","indexId":"wsp2229","publicationYear":"1984","noYear":false,"title":"Test well DO-CE 88 at Cambridge, Dorchester County, Maryland"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp2229","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":"2229","title":"Test well DO-CE 88 at Cambridge, Dorchester County, Maryland","docAbstract":"Test well DO-CE 88 at Cambridge, Maryland, penetrated 3,299 feet of unconsolidated Quaternary, Tertiary and Cretaceous sediments and bottomed in quartz-monzonite gneiss. The well was drilled to provide data for a study of the aquifer system of the northern Atlantic Coastal Plain. Twenty-one core samples were collected. Six sand zones were tested for aquifer properties and sampled for ground-water chemistry. Point-water heads were measured at seven depths. Environmental heads (which ranged from - 18.33 to + 44.16 feet relative to sea level)indicate an upward component of flow. A temperature log showed a maximum temperature of 41.9 degrees Celsius and a mean temperature gradient of 0.00838 degrees Celsius per foot. \r\n\r\nThe water analyses delineated the freshwater-saltwater transition zone between 2,650 and 3,100 feet. The ground water changes progressively downward from a sodium bicarbonate to a sodium chloride character. Clays in the analyzed core samples belong to the montmorillonite and kaolinite groups, and mean cation exchange capacity ranged from 8.3 to 38.9 milliequivalents per 100 grams. \r\n\r\nVertical and horizontal hydraulic conductivities measured in cores ranged from 1.5 x 10 6 to 1.3 feet per day and from 7.3 x 10 -6 to 1.3 feet per day, respectively, but the most permeable sands were not cored. Porosity was 1.5 percent in the quartz monzonite bedrock and ranged from 22.4 to 41 percent in the overlying sediments. Transmissivities from aquifer tests ranged from 25 to 850 feet squared per day; horizontal hydraulic conductivities ranged from.2.5 to 85 feet squared per day, and intrinsic permeabilities ranged from 0.8 to 23 micrometers squared. \r\n\r\nFossils identified in core samples include palynomorphs, dinoflagellates, and foraminifers.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2229","usgsCitation":"Trapp, H., Knobel, L.L., Meisler, H., and Leahy, P.P., 1984, Test well DO-CE 88 at Cambridge, Dorchester County, Maryland: U.S. Geological Survey Water Supply Paper 2229, iv, 48 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2229.","productDescription":"iv, 48 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":136383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2229/report-thumb.jpg"},{"id":25315,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2229/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684b62","contributors":{"authors":[{"text":"Trapp, Henry Jr.","contributorId":6034,"corporation":false,"usgs":true,"family":"Trapp","given":"Henry","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":142673,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knobel, LeRoy L.","contributorId":76285,"corporation":false,"usgs":true,"family":"Knobel","given":"LeRoy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142675,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":142674,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Leahy, P. Patrick","contributorId":80648,"corporation":false,"usgs":true,"family":"Leahy","given":"P.","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":142676,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":8781,"text":"ofr84134 - 1984 - Water-level hydrographs for observation wells in Virginia, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr84134","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":"84-134","title":"Water-level hydrographs for observation wells in Virginia, 1982","docAbstract":"Water-well data for 1982 are presented from 147 observation wells in Virginia. Historical data from two wells are also included. A description of each observation well is provided that gives the well location, site identification number, hydrologic unit, owner, aquifer, well characteristics, general remarks, period of record, and extreme measurements for the period of record. A hydrograph for the period of record is presented for each well. The method and frequency of water-level measurements at each well are presented in tabular format. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84134","usgsCitation":"Farrington, S., Carrington, N., and Daniels, W., 1984, Water-level hydrographs for observation wells in Virginia, 1982: U.S. Geological Survey Open-File Report 84-134, iv, 167 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84134.","productDescription":"iv, 167 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143435,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0134/report-thumb.jpg"},{"id":36347,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0134/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36348,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0134/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7828","contributors":{"authors":[{"text":"Farrington, Stephen","contributorId":87803,"corporation":false,"usgs":true,"family":"Farrington","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":158318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carrington, Natalie","contributorId":96954,"corporation":false,"usgs":true,"family":"Carrington","given":"Natalie","email":"","affiliations":[],"preferred":false,"id":158319,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Daniels, W.V. Jr.","contributorId":43225,"corporation":false,"usgs":true,"family":"Daniels","given":"W.V.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":158317,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}