No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83611","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Aeromagnetic map of south-central Alabama: U.S. Geological Survey Open-File Report 83-611, 9 Plates:32.24 × 22.31 inches or smaller, https://doi.org/10.3133/ofr83611.","productDescription":"9 Plates:32.24 × 22.31 inches or smaller","costCenters":[],"links":[{"id":172723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79594,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79593,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79592,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79591,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79590,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79589,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79588,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79587,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79586,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391774,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14133.htm"}],"country":"United States","state":"Alabama","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86,\n 31.5\n ],\n [\n -87,\n 31.5\n ],\n [\n -87,\n 32.833\n ],\n [\n -86,\n 32.833\n ],\n [\n -86,\n 31.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691cc3","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530667,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28441,"text":"wri8242 - 1983 - Magnitude and frequency of flooding on small urban watersheds in the Tampa Bay area, west-central Florida","interactions":[],"lastModifiedDate":"2019-11-26T11:15:19","indexId":"wri8242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-42","title":"Magnitude and frequency of flooding on small urban watersheds in the Tampa Bay area, west-central Florida","docAbstract":"Hydrologic data collected on nine small urban watersheds in the Tampa Bay area of west-central Florida and a method for estimating peak discharges in the study area are described. The watersheds have mixed land use and range in size from 0.34 to 3.45 square miles. Watershed soils, land use, and storm-drainage system data are described. Urban development ranged from a sparsely populated area with open-ditch storm sewers and 19% impervious area to a completely sewered watershed with 61% impervious cover. The U.S. Geological Survey natural-basin and urban-watershed models were calibrated for the nine watersheds using 5-minute interval rainfall data from the Tampa, Florida, National Weather Service rain gage to simulate annual peak discharge for the period 1906-52. A log-Pearson Type III frequency analysis of the simulated annual maximum discharge was used to determine the 2-, 5-, 10-, 25-, 50-, and 100-year flood discharges for each watershed. Flood discharges were related in a multiple-linear regression to drainage area, channel slope, detention storage area, and an urban-development factor determined by the extent of curb and gutter street drainage and storm-sewer system. The average standard error for the regional relations ranged from + or - 32 to + or - 42%. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8242","usgsCitation":"Lopez, M.A., and Woodham, W.M., 1983, Magnitude and frequency of flooding on small urban watersheds in the Tampa Bay area, west-central Florida: U.S. Geological Survey Water-Resources Investigations Report 82-42, vi, 52 p. , https://doi.org/10.3133/wri8242.","productDescription":"vi, 52 p. ","costCenters":[],"links":[{"id":369640,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0042/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0042/report-thumb.jpg"}],"country":"United States","state":"Florida","city":"Tampa Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.6336669921875,\n 27.81478637667891\n ],\n [\n -82.1832275390625,\n 27.81478637667891\n ],\n [\n -82.1832275390625,\n 28.14950321154457\n ],\n [\n -82.6336669921875,\n 28.14950321154457\n ],\n [\n -82.6336669921875,\n 27.81478637667891\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649519","contributors":{"authors":[{"text":"Lopez, M. A.","contributorId":12493,"corporation":false,"usgs":true,"family":"Lopez","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woodham, W. M.","contributorId":72356,"corporation":false,"usgs":true,"family":"Woodham","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":199804,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":47671,"text":"wri834058 - 1983 - Shallow ground water in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado, 1975-77","interactions":[],"lastModifiedDate":"2022-12-05T21:04:03.995944","indexId":"wri834058","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4058","title":"Shallow ground water in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado, 1975-77","docAbstract":"Shallow ground water may limit the location of construction and excavation projects in parts of the Front Range Urban Corridor. A shallow water table occurs from 0 to 50 feet below the land surface principally in the alluvial deposits along the streams and rivers in the Boulder-Fort Collins-Greeley area. This shallow water table underlies approximately 400 square miles and is maintained by natural recharge within the South Platte River basin and by the infiltration of irrigation water that is diverted into the basin from streams and reservoirs in the Colorado and the Laramie River basins. Return flow from irrigation, which is mostly ground water, helps maintain the flow of the South Platte River and its tributaries. The report includes a map from which depth to water table and the direction of ground-water movement can be determined. The map, compiled on a topographic base, shows the areal extent of the saturated materials and the altitude and configuration of the ground-water surface. The water-table contour map was prepared using data from approximately 400 wells. Monitoring of shallow ground-water within the study area shows depths to water have changed only slightly over the last 20 years, except for some seasonal and drought-related fluctuations. Gradients, computed from ground-water measurements, range from 27.7 feet per mile in Lone Tree-Spring Creek valley to 10.3 feet per mile in the South Platte River valley. The shallow ground-water underflow from the major tributaries in the basin is about 29,000 acre-feet per year, and underflow calculated at a cross section near Kersey is about 12,000 acre-feet per year.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834058","usgsCitation":"Schneider, P.A., 1983, Shallow ground water in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado, 1975-77: U.S. Geological Survey Water-Resources Investigations Report 83-4058, 1 Plate: 41.96 × 31.86 inches, https://doi.org/10.3133/wri834058.","productDescription":"1 Plate: 41.96 × 31.86 inches","costCenters":[],"links":[{"id":161788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410064,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35694.htm","linkFileType":{"id":5,"text":"html"}},{"id":84582,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Boulder, Fort Collins, Greeley","otherGeospatial":"Front Range urban corridor","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.46470339334677,\n 40.68848809489273\n ],\n [\n -105.46470339334677,\n 39.92665986663209\n ],\n [\n -104.58735150676397,\n 39.92665986663209\n ],\n [\n -104.58735150676397,\n 40.68848809489273\n ],\n [\n -105.46470339334677,\n 40.68848809489273\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f420a","contributors":{"authors":[{"text":"Schneider, Paul A. Jr.","contributorId":50183,"corporation":false,"usgs":true,"family":"Schneider","given":"Paul","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":235982,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28663,"text":"wri834003 - 1983 - Water quality at and adjacent to the south Dade County solid-waste disposal facility, Florida","interactions":[],"lastModifiedDate":"2022-01-10T12:42:17.030178","indexId":"wri834003","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4003","title":"Water quality at and adjacent to the south Dade County solid-waste disposal facility, Florida","docAbstract":"A water-quality reconnaissance was conducted at the south Dade County solid-waste landfill near Goulds, Florida, from December 1977 through August 1978. The landfill is located directly on the unconfined Biscayne aquifer, which, in the study area, is affected by saltwater intrusion. Water samples collected from six monitor well sites at two depths and four surface-water sites were analyzed to determine the chemical, physical, and biological conditions of the ground water and surface water of the study area. Results indicated that water quality beneath the landfill was highly variable with location and depth. Leachate was generally more evident in the shallow wells and during the dry-season sampling, but was greatly diluted and dispersed in the deep wells and during the wet season. High concentrations of contaminants were generated primarily in areas of the landfill with the most recent waste deposits. Chloride (limited to the shallow wells and the dry season), alkalinity, ammonia, iron, manganese, lead, phosphorus, and organic nitrogen indicate leachate contamination of the aquifer. Water-quality characteristics in the surface waters were generally only slightly above background levels. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri834003","collaboration":"Prepared in cooperation with Dade County Department of Public Works","usgsCitation":"McKenzie, D., 1983, Water quality at and adjacent to the south Dade County solid-waste disposal facility, Florida: U.S. Geological Survey Water-Resources Investigations Report 83-4003, v, 42 p., https://doi.org/10.3133/wri834003.","productDescription":"v, 42 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":158336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4003/coverthb.jpg"},{"id":57504,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4003/wri834003.pdf","text":"Report","size":"1.77 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 83-4003"}],"country":"United States","state":"Florida","county":"Dade County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.5572509765625,\n 25.591994180254712\n ],\n [\n -79.95574951171875,\n 25.591994180254712\n ],\n [\n -79.95574951171875,\n 26.162833742569937\n ],\n [\n -80.5572509765625,\n 26.162833742569937\n ],\n [\n -80.5572509765625,\n 25.591994180254712\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrOR812","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Water resources data Oregon, water year 1981: Volume 2. 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Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533068,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27663,"text":"wri834121E - 1983 - Map showing outcrops of ash-flow tuffs, Basin and Range Province and vicinity, Trans-Pecos Texas","interactions":[],"lastModifiedDate":"2017-11-21T14:37:32","indexId":"wri834121E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4121","chapter":"E","title":"Map showing outcrops of ash-flow tuffs, Basin and Range Province and vicinity, Trans-Pecos Texas","docAbstract":"This map report is one of a series of geologic and hydrologic maps covering all or parts of the States within the Basin and Range province of the western United States, resulting from work under the U.S. Geological Survey's program for geologic and hydrologic evaluation of the Basin and Range province to identify potentially suitable regions for future study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984) .
The map report on the ash-flow tuffs of Trans-Pecos Texas was prepared from published maps and reports and from recent work in progress by geologists of the Texas Bureau of Economic Geology, and was compiled utilizing the project guidelines of Sargent and Bedinger (1984). The map shows the outcrops and localities of measured thicknesses of the ash-flow tuffs that resulted from silicic volcanism 38 to 28 million years ago (Henry and McDowell, 1982). Locally, however, some thin, inadequately studied tuffs of limited distribution have been excluded from the map. Such tuffs are reported in the \"lower rhyolite\" in the Eagle Mountains (Underwood, 1963), in the southern Davis Mountains (Parker, 1977), within parts of the Shely Group and Morita Ranch Formation in the Chinati Mountains (Cepeda and Henry, 1983) , and in the Rawls Formation in the Bofecillos Mountains (McKnight, 1969). The distribution of most ash-flow tuffs in the northern Davis and Wylie Mountains is not well known. The Chambers Tuff, largely tuffaceous sedimentary rocks, is reported to contain several ash-flow tuffs (Walton, 1972), but their distribution is poorly documented. Metamorphosed ash-flow tuffs of Precambrian age in the Thunderbird Group in the Franklin Mountains (Thomann, 1981) and in the Carrizo Mountain Group near Van Horn (Rudnick , 1983) were not included on the map. In some areas studied in reconnaissance, the definitive lithology of some volcanic units described as lava flows or tuffs has not been determined.
In the Description of Map Units, the general location, caldera source and volume of tuff, isotopic age, if available, lithologic data, and the reference sources for each geologic unit are described. The nomenclature of the geologic units is from published reports and does not necessarily conform to U.S. Geological Survey usage.
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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNV821","collaboration":"Prepared in cooperation with the State of Nevada and with other agencies","usgsCitation":"Frisbie, H., La Camera, R., Riek, M., and Wood, D., 1983, Water resources data for Nevada, water year 1982: U.S. Geological Survey Water Data Report NV-82-1, vi, 360 p., https://doi.org/10.3133/wdrNV821.","productDescription":"vi, 360 p.","costCenters":[],"links":[{"id":184486,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/nv-82-1/report-thumb.jpg"},{"id":492553,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/nv-82-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2cfe","contributors":{"authors":[{"text":"Frisbie, H.R.","contributorId":9717,"corporation":false,"usgs":true,"family":"Frisbie","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":254514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"La Camera, R.J.","contributorId":83932,"corporation":false,"usgs":true,"family":"La Camera","given":"R.J.","affiliations":[],"preferred":false,"id":254515,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Riek, M.M.","contributorId":93972,"corporation":false,"usgs":true,"family":"Riek","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":254517,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wood, D.B.","contributorId":87971,"corporation":false,"usgs":true,"family":"Wood","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":254516,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":17253,"text":"ofr82647 - 1983 - Hydrology of area 2, Eastern Coal Province, Pennsylvania and New York","interactions":[],"lastModifiedDate":"2017-07-07T08:29:10","indexId":"ofr82647","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-647","title":"Hydrology of area 2, Eastern Coal Province, Pennsylvania and New York","docAbstract":"Provisions of the Surface Mining Control and Reclamation Act of 1977 recognized a nationwide need for hydrologic information in mined and potentially mined areas. This report is designed to be useful to mine owners, operators, regulatory authorities, citizens groups, and others by presenting information on existing hydrologic conditions and by identifying additional sources of hydrologic information. General hydrologic information is presented in a brief text accompanied by a map, chart, graph, or other illustration for each of a series of water-resourcesrelated topics. The summation of the topical discussions provides a description of the hydrology of the area. The Eastern Coal Province has been divided into 24 hydrologic study areas which are shown on the cover of this report. The divisions are based on hydrologic factors, location, and size. Hydrologic units (surface drainage basins) or parts of units are combined to form each study area. Study Area 2 covers northwestern Pennsylvania and a small part of southwestern New York. Most exposed bedrock is of Pennsylvanian, Mi;;sissippian, or Devonian ages. Glacial drift covers most of the bedrock in the northwestern part of the area. During 1979, more than 7 million tons of bituminous coal was produced from about 230 mines in Area 2 counties. Over 99 percent of the area's coal production is from surface mining. Streamflow data are available for 18 continuousrecord stations; 1 crest-stage, partial-record station; 1 low-flow, partial-record station; and 65 miscellaneous sites. Water-quality data are available for 78 locations. Streams having the highest median specific conductance, highest median dissolved-solids concentrations, lowest median pH, highest median total-iron concentration, highest median total-manganese concentration, and highest dissolved-sulfate concentrations were found in Clarion County, the leading coal-producing county in the area. Statistics on low flow, mean flow, peak flow, and flow duration for gaging stations can be computed from recorded mean daily flows. Similar statistics can be estimated for ungaged streams by regression and graphical techniques. Five ground-water observation wells are being operated in Area 2. Ground-water levels fluctuate seasonally. Depth to water increases with well depth in upland areas and decreases with well depth in valleys. Well yields in the area range from less than 1 to more than 2,000 gallons per minute. Wells in unconsolidated materials usually have higher yields. Ground-water quality is adequate for most domestic purposes, except locally. Additional water-data information are available through: (1) The National Water Data Exchange, (2) The National Water Data Storage and Retrieva
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82647","usgsCitation":"Herb, W., Brown, D., Shaw, L.C., Stoner, J., and Felbinger, J., 1983, Hydrology of area 2, Eastern Coal Province, Pennsylvania and New York: U.S. Geological Survey Open-File Report 82-647, vi, 159 p. :ill. (some col., some folded), maps (some col., some folded) ;28 cm., https://doi.org/10.3133/ofr82647.","productDescription":"vi, 159 p. :ill. (some col., some folded), maps (some col., some folded) ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":95399,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0647/report.pdf","size":"25882","linkFileType":{"id":1,"text":"pdf"}},{"id":149365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0647/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6021f7","contributors":{"authors":[{"text":"Herb, W.J.","contributorId":16847,"corporation":false,"usgs":true,"family":"Herb","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":175615,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, D.E.","contributorId":91879,"corporation":false,"usgs":true,"family":"Brown","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":175618,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shaw, L. C.","contributorId":21162,"corporation":false,"usgs":true,"family":"Shaw","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":175616,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stoner, J.E.","contributorId":67901,"corporation":false,"usgs":true,"family":"Stoner","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":175617,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Felbinger, J.K.","contributorId":104077,"corporation":false,"usgs":true,"family":"Felbinger","given":"J.K.","affiliations":[],"preferred":false,"id":175619,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":13206,"text":"ofr83221 - 1983 - Hydrology of area 47, Northern Great Plains and Rocky Mountain Coal Provinces, North Dakota, South Dakota, and Montana","interactions":[],"lastModifiedDate":"2018-02-16T14:27:38","indexId":"ofr83221","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-221","title":"Hydrology of area 47, Northern Great Plains and Rocky Mountain Coal Provinces, North Dakota, South Dakota, and Montana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83221","usgsCitation":"Crosby, O., and Klausing, R., 1983, Hydrology of area 47, Northern Great Plains and Rocky Mountain Coal Provinces, North Dakota, South Dakota, and Montana: U.S. Geological Survey Open-File Report 83-221, 150 p., https://doi.org/10.3133/ofr83221.","productDescription":"150 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":95115,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0221/report.pdf","size":"34188","linkFileType":{"id":1,"text":"pdf"}},{"id":146750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0221/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ff8","contributors":{"authors":[{"text":"Crosby, O.A.","contributorId":61047,"corporation":false,"usgs":true,"family":"Crosby","given":"O.A.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":167403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klausing, R.L.","contributorId":73205,"corporation":false,"usgs":true,"family":"Klausing","given":"R.L.","affiliations":[],"preferred":false,"id":167404,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9728,"text":"ofr83257 - 1983 - Background hydrologic information in potential lignite mining areas in Mississippi, July 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr83257","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-257","title":"Background hydrologic information in potential lignite mining areas in Mississippi, July 1982","docAbstract":"A water-quality sampling program was initiated in 1980 to determine background hydrologic data in potential lignite mining areas of Mississippi. This report is the third in a planned five-part series to provide data to assess future impacts of mining on small streams. The data indicates that most streams in the study area have a dissolved-solids concentration less than 100 mg/. The major ion concentrations were generally less than 10 mg/. Concentrations of arsenic, cadmium, mercury, and selenium in bottom material samples were below detectable limits. Cobalt, lead, zinc, copper, and chromium concentrations exceeded 10 micro-/g at all sites and maganese exceeded 1000 micro-/g at five sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83257","usgsCitation":"Kalkhoff, S.J., 1983, Background hydrologic information in potential lignite mining areas in Mississippi, July 1982: U.S. Geological Survey Open-File Report 83-257, 25 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83257.","productDescription":"25 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":144227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0257/report-thumb.jpg"},{"id":37473,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0257/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64adb1","contributors":{"authors":[{"text":"Kalkhoff, Stephen J. 0000-0003-4110-1716 sjkalkho@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-1716","contributorId":1731,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"Stephen","email":"sjkalkho@usgs.gov","middleInitial":"J.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true},{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":160198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10272,"text":"ofr83286 - 1983 - A hydrogeochemical survey in east-central Nevada","interactions":[],"lastModifiedDate":"2022-07-22T21:20:44.950179","indexId":"ofr83286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-286","title":"A hydrogeochemical survey in east-central Nevada","docAbstract":"A hydrogeochemical survey utilizing waters from springs and wells was conducted in east-central Nevada. None of the trace elements commonly associated with mineralization were found to be highly anomalous in the study area. Slightly anomalous values for some elements were found in the southern valleys of the study area and in a few scattered areas that contained old mines. Data from this study revealed no new areas of significant mineralization.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83286","usgsCitation":"McHugh, J., Miller, W.R., and Ficklin, W.H., 1983, A hydrogeochemical survey in east-central Nevada: U.S. Geological Survey Open-File Report 83-286, i, 28 p., https://doi.org/10.3133/ofr83286.","productDescription":"i, 28 p.","costCenters":[],"links":[{"id":404396,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13966.htm","linkFileType":{"id":5,"text":"html"}},{"id":38129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0286/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0286/report-thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.49,\n 37.874\n ],\n [\n -114,\n 37.874\n ],\n [\n -114,\n 38.5\n ],\n [\n -114.49,\n 38.5\n ],\n [\n -114.49,\n 37.874\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae468","contributors":{"authors":[{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":161115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. Roger","contributorId":60191,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":161114,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ficklin, Walter H.","contributorId":52565,"corporation":false,"usgs":true,"family":"Ficklin","given":"Walter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161113,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":29065,"text":"wri834198 - 1983 - Effect of the proposed Cooper River rediversion on sedimentation in Charleston Harbor, South Carolina","interactions":[],"lastModifiedDate":"2023-03-07T20:24:09.45803","indexId":"wri834198","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4198","title":"Effect of the proposed Cooper River rediversion on sedimentation in Charleston Harbor, South Carolina","docAbstract":"The rates of sedimentation and of resultant maintenance dredging in Charleston Harbor increased dramatically in the 1940s, following two major modifications to the harbor. One modification, the Santee-Cooper diversion project, caused a twentyfold increase in freshwater inflow to the harbor. The other modification was deepening of the navigation channels in the harbor from 30 to 35 feet below mean low water. After field and model studies indicated that the diversion was the major cause of the increase in the sedimentation rate, plans were made to redivert most of the Santee River water back to its former channel. This report documents a review of existing data and literature that was made to evaluate rediversion as a means of reducing the rate of maintenance dredging. The postrediversion decrease in the rate of maintenance dredging can be estimated only within broad limits because some important questions lack reliable answers. Analysis of available information indicates that rediversion will eventually reduce the rate of maintenance dredging by about 40 to 75 percent. The reduction in the rate of maintenance dredging may be delayed for a decade or more by the gradual removal of accumulated sediment and may be partially offset by the effects of future channel deepening.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834198","usgsCitation":"Patterson, G.G., 1983, Effect of the proposed Cooper River rediversion on sedimentation in Charleston Harbor, South Carolina: U.S. Geological Survey Water-Resources Investigations Report 83-4198, vi, 65 p., https://doi.org/10.3133/wri834198.","productDescription":"vi, 65 p.","costCenters":[],"links":[{"id":413781,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49178.htm","linkFileType":{"id":5,"text":"html"}},{"id":57927,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4198/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119735,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4198/report-thumb.jpg"}],"country":"United States","state":"South Carolina","otherGeospatial":"Charleston Harbor, Cooper River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.1667,\n 33.5\n ],\n [\n -80.1667,\n 32.6667\n ],\n [\n -79.75,\n 32.6667\n ],\n [\n -79.75,\n 33.5\n ],\n [\n -80.1667,\n 33.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6866ea","contributors":{"authors":[{"text":"Patterson, G. G.","contributorId":40242,"corporation":false,"usgs":true,"family":"Patterson","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":200890,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26430,"text":"wri834093 - 1983 - Major geochemical processes related to the hydrology of the Madison aquifer system and associated rocks in parts of Montana, South Dakota, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:32","indexId":"wri834093","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4093","title":"Major geochemical processes related to the hydrology of the Madison aquifer system and associated rocks in parts of Montana, South Dakota, and Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri834093","usgsCitation":"Busby, J., Lee, R.W., and Hanshaw, B., 1983, Major geochemical processes related to the hydrology of the Madison aquifer system and associated rocks in parts of Montana, South Dakota, and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 83-4093, ix, 180 p. :ill., maps ;41 cm., https://doi.org/10.3133/wri834093.","productDescription":"ix, 180 p. :ill., maps ;41 cm.","costCenters":[],"links":[{"id":110161,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35719.htm","linkFileType":{"id":5,"text":"html"},"description":"35719"},{"id":158113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4093/report-thumb.jpg"},{"id":55222,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55223,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55224,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55225,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55226,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55227,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55228,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55229,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55230,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55231,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55232,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55233,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55234,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55235,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55236,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55237,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55238,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4093/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55239,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4093/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649764","contributors":{"authors":[{"text":"Busby, J.F.","contributorId":105300,"corporation":false,"usgs":true,"family":"Busby","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":196379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, R. W.","contributorId":86757,"corporation":false,"usgs":true,"family":"Lee","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196378,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":196377,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10564,"text":"ofr821013 - 1983 - Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","interactions":[{"subject":{"id":10564,"text":"ofr821013 - 1983 - Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","indexId":"ofr821013","publicationYear":"1983","noYear":false,"title":"Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":2420,"text":"wsp2227 - 1987 - Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico","indexId":"wsp2227","publicationYear":"1987","noYear":false,"title":"Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico"},"id":1}],"supersededBy":{"id":2420,"text":"wsp2227 - 1987 - Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico","indexId":"wsp2227","publicationYear":"1987","noYear":false,"title":"Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico"},"lastModifiedDate":"2022-09-07T15:44:24.905824","indexId":"ofr821013","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-1013","title":"Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","docAbstract":"An evaluation of the water resources of the Zuni Tribal lands in west-central New Mexico was made to determine the yield, variability, and quality of water available to the Pueblo of Zuni. This study is needed to aid in orderly development of these resources.
Rocks of Permian to Quaternary age supply stock, irrigation, and domestic water to the Zuni Indians. The Glorieta Sandstone and San Andres Limestone (Glorieta-San Andres aquifer) of Permian age and sandstones in the Chinle Formation of Triassic age provide most of this water supply.
Water in the Glorieta-San Andres aquifer is confined by minimal-permeability shales and is transmitted through the aquifer along interconnected solution channels and fractures. Water-level and water-quality information indicate greater hydraulic conductivities along the southern boundaries of Zuni Tribal lands.
Well yields from the Glorieta-San Andres aquifer are as much as 150 gallons per minute and aquifer transmissivity ranges from 30 to 1,400 feet squared per day. Long-term, water-level declines of as much as 29 feet have been measured near pumping centers at Black Rock. Multiple-well aquifer tests are needed to further define aquifer properties (storage, transmissivity, and leakage from confining units) and the effects of well design on well yields. Dissolved-solids concentrations in water from the aquifer ranged from 331 to 1,068 milligrams per liter. Calcium and sulfate are the predominant ions.
Water in sandstones of the Chinle Formation is confined by adjacent shales and is transmitted along interconnected fractures. Well yields range from 5 to 125 gallons per minute and aquifer transmissivity ranges from 40 to 1,400 feet squared per day. Water-level declines of as much as 27 feet have been measured near Zuni Village. Dissolved-solids concentrations in water from the aquifer ranged from 215 to 1,980 milligrams per liter. Sodium and bicarbonate are the predominant ions.
Other sources of ground water are used primarily for livestock watering by means of windmills, with the exception of buried alluvial channel deposits along the Rio Pescado. These deposits provide domestic and irrigation water through springs and wells to Pescado and Black Rock.
The Bidahochi Formation of Miocene and Pliocene age could potentially provide an additional supply of water chemically suitable for most uses. Seismic-reflection techniques are being used to locate buried channels eroded in the rocks underlying the Bidahochi Formation. These buried channels may contain thicker sections of saturated sands and gravels that could be developed for stock and domestic use.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821013","collaboration":"Prepared in cooperation with the Pueblo of Zuni","usgsCitation":"Orr, B.R., 1983, Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico: U.S. Geological Survey Open-File Report 82-1013, Report: 179 p.; 2 Plates: 23.21 x 19.52 inches and 20.83 x 30.61 inches, https://doi.org/10.3133/ofr821013.","productDescription":"Report: 179 p.; 2 Plates: 23.21 x 19.52 inches and 20.83 x 30.61 inches","costCenters":[],"links":[{"id":406315,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1013/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406314,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1013/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406313,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1013/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1013/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Cibola County, McKinley County","otherGeospatial":"Zuni Tribal Lands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.061279296875,\n 34.134541681937364\n ],\n [\n -107.0068359375,\n 34.134541681937364\n ],\n [\n -107.0068359375,\n 35.96022296929667\n ],\n [\n -109.061279296875,\n 35.96022296929667\n ],\n [\n -109.061279296875,\n 34.134541681937364\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f03be","contributors":{"authors":[{"text":"Orr, Brennon R.","contributorId":18747,"corporation":false,"usgs":true,"family":"Orr","given":"Brennon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43846,"text":"ofr83107 - 1983 - Land use and land cover and associated maps for Williams, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:11:04","indexId":"ofr83107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-107","title":"Land use and land cover and associated maps for Williams, Arizona","language":"ENGLISH","doi":"10.3133/ofr83107","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use and land cover and associated maps for Williams, Arizona: U.S. Geological Survey Open-File Report 83-107, maps :photocopy ;45 x 67 cm., https://doi.org/10.3133/ofr83107.","productDescription":"maps :photocopy ;45 x 67 cm.","costCenters":[],"links":[{"id":168053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae676","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11003,"text":"ofr81918 - 1983 - Geothermal resources of the western arm of the Black Rock Desert, northwestern Nevada: Part I, geology and geophysics","interactions":[],"lastModifiedDate":"2022-10-17T15:30:14.608693","indexId":"ofr81918","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"81-918","title":"Geothermal resources of the western arm of the Black Rock Desert, northwestern Nevada: Part I, geology and geophysics","docAbstract":"Studies of the geothermal potential of the western arm of the Black Rock Desert in northwestern Nevada included a compilation of existing geologic data on a detailed map, a temperature survey at 1-meter depth, a thermal-scanner survey, and gravity and seismic surveys to determine basin geometry. The temperature survey showed the effects of heating at shallow depths due to rising geothermal fluids near the known hot spring areas. Lower temperatures were noted in areas of probable near-surface ground-water movement. The thermal-scanner survey verified the known geothermal areas and showed relatively high-temperature areas of standing water and ground-water discharge. The upland areas of the desert were found to be distinctly warmer than the playa area, probably due to low thermal diffusivity resulting from low moisture content. The surface geophysical surveys indicated that the maximum thickness of valley-fill deposits in the desert is about 3,200 meters. Gravity data further showed that changes in the trend of the desert axis occurred near thermal areas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81918","usgsCitation":"Schaefer, D.H., Welch, A., and Mauzer, D.K., 1983, Geothermal resources of the western arm of the Black Rock Desert, northwestern Nevada: Part I, geology and geophysics: U.S. Geological Survey Open-File Report 81-918, Report: v, 37 p.; 4 Plates: 21.24 × 35.96 inches or smaller, https://doi.org/10.3133/ofr81918.","productDescription":"Report: v, 37 p.; 4 Plates: 21.24 × 35.96 inches or smaller","costCenters":[],"links":[{"id":144063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0918/report-thumb.jpg"},{"id":38767,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0918/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38768,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0918/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38769,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0918/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38770,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0918/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38771,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0918/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":408004,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12207.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada","otherGeospatial":"Black Rock Desert","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.542,\n 40.584\n ],\n [\n -118.825,\n 40.584\n ],\n [\n -118.825,\n 41.521\n ],\n [\n -119.542,\n 41.521\n ],\n [\n -119.542,\n 40.584\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ad41","contributors":{"authors":[{"text":"Schaefer, Donald H.","contributorId":77507,"corporation":false,"usgs":true,"family":"Schaefer","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":162358,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mauzer, Douglas K.","contributorId":44922,"corporation":false,"usgs":true,"family":"Mauzer","given":"Douglas","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":162357,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":57348,"text":"wdrOR811 - 1983 - Water resources data Oregon, water year 1981: Volume 1. Eastern Oregon","interactions":[],"lastModifiedDate":"2020-09-25T16:22:15.514316","indexId":"wdrOR811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"OR-81-1","title":"Water resources data Oregon, water year 1981: Volume 1. Eastern Oregon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrOR811","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Water resources data Oregon, water year 1981: Volume 1. 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Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27120,"text":"wri834236 - 1983 - PHRQINPT, an interactive computer program for constructing input data sets to the geochemical simulation program PHREEQE","interactions":[],"lastModifiedDate":"2018-03-21T15:28:23","indexId":"wri834236","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4236","title":"PHRQINPT, an interactive computer program for constructing input data sets to the geochemical simulation program PHREEQE","docAbstract":"PHRQINPT is a FORTRAN 77 program which facilitates formulation of the input data file to PHREEQE (Parkhurst, Thorstenson, and Plummer, 1980). PHRQINPT runs interactively and contains many features to help the user construct the input data set. This report describes these features and gives instructions on the use and implementation of PHRQINPT. A listing of the program and the two accompanying data sets are given in the attachments, along with two examples. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834236","usgsCitation":"Fleming, G., and Plummer, N., 1983, PHRQINPT, an interactive computer program for constructing input data sets to the geochemical simulation program PHREEQE: U.S. Geological Survey Water-Resources Investigations Report 83-4236, iii, 111 p. ;28 cm., https://doi.org/10.3133/wri834236.","productDescription":"iii, 111 p. ;28 cm.","costCenters":[],"links":[{"id":119985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4236/report-thumb.jpg"},{"id":55984,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4236/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689e60","contributors":{"authors":[{"text":"Fleming, G.W.","contributorId":81937,"corporation":false,"usgs":true,"family":"Fleming","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":197589,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":197588,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10874,"text":"ofr83353 - 1983 - Summary of environmental geologic studies in the Mid-Atlantic outer continental shelf area; results of 1978-1979 field seasons","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr83353","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-353","title":"Summary of environmental geologic studies in the Mid-Atlantic outer continental shelf area; results of 1978-1979 field seasons","docAbstract":"Because of the need for knowledge of an offshore area that is undergoing exploration for oil and gas resources, since 1975 the U.S. Bureau of Land Management (BLM) has funded studies of the environmental characteristics of the Mid-Atlantic Outer Continental Shelf. This volume briefly summarizes a final report to the BLM on the results of U.S. Geological Survey investigations stemming from data acquired during 1978 and 1979. The parent final report contains complete accounts of those investigations. The subjects of the studies range from the geologic effects of water currents and their capabilities of erosion and transportation, to delineation of potentially hazardous geologic characteristics of the area. Nine specific studies address the complexities of water currents, the nature of materials suspended in the sea waters, rates of mixing-in of material deposited on the bottom, and the sites of probable deposition of such materials, as well as sites and mechanisms of possible submarine landsliding or unstable bottom (engineering characteristics) of the Continental Slope and shelf.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83353","usgsCitation":"Robb, J.M., 1983, Summary of environmental geologic studies in the Mid-Atlantic outer continental shelf area; results of 1978-1979 field seasons: U.S. Geological Survey Open-File Report 83-353, 40 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83353.","productDescription":"40 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0353/report-thumb.jpg"},{"id":38651,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0353/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69931e","contributors":{"authors":[{"text":"Robb, James M.","contributorId":60225,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":162115,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29224,"text":"wri824065 - 1983 - Numerical simulation of ground-water flow in lower Satus Creek Basin, Yakima Indian Reservation, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri824065","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4065","title":"Numerical simulation of ground-water flow in lower Satus Creek Basin, Yakima Indian Reservation, Washington","docAbstract":"A multilayer numerical model of steady-state ground-water flow in lower Satus Creek basin was constructed, calibrated using time-averaged data, and used to estimate the long-term effects of proposed irrigation-water management plans on ground-water levels in the area. Model computations showed that irrigation of new lands in the Satus uplands would raise ground-water levels in lower Satus Creek basin and thereby increase the size of the waterlogged areas. The model also demonstrated that pumping water from wells, reducing the amount of irrigation water used in the lowlands, and stopping leakage from Satus No. 2 and 3 Pump Canals were all effective methods to alleviate present waterlogging in some parts of the basin and to counteract some of the anticipated ground-water-level rises that would be caused by irrigating the uplands. The proposed changes in water use affected model-computed ground-water levels most in the eastern part of the basin between Satus No. 2 and No. 3 Pump Canals. The effects on ground-water levels in the western part of the basin between Satus Creek and Satus No. 2 Pump Canal were smaller. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824065","usgsCitation":"Prych, E., 1983, Numerical simulation of ground-water flow in lower Satus Creek Basin, Yakima Indian Reservation, Washington: U.S. Geological Survey Water-Resources Investigations Report 82-4065, xi, 89 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824065.","productDescription":"xi, 89 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4065/report-thumb.jpg"},{"id":58077,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4065/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58078,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69680c","contributors":{"authors":[{"text":"Prych, E. A.","contributorId":36163,"corporation":false,"usgs":true,"family":"Prych","given":"E. A.","affiliations":[],"preferred":false,"id":201175,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7078,"text":"ofr83697 - 1983 - Data for ground-water test hole near Butte City, Central Valley aquifer project, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr83697","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-697","title":"Data for ground-water test hole near Butte City, Central Valley aquifer project, California","docAbstract":"This report provides preliminary data for the third of seven test holes drilled as part of the Central Valley Aquifer Project which is part of the National Regional Aquifer Systems Analysis Program. The test hole was drilled in the SW 1/4 NE 1/4 sec. 32, T. 19 N., R. 1 W., Glenn County, California, about one-half mile south of the town of Butte City. Drilled to a depth of 1,432 feet below land surface, the hole is cased to a depth of 82 feet and equipped with three piezometer tubes to depths of 592 feet, 968 feet, and 1,330 feet. A 5-foot well screen is at the bottom of each piezometer. Each screened interval has a cement plug above and below it to isolate it from other parts of the aquifer , and the well bore is filled between the plugs with sediment. Nine cores and 49 sidewall cores were recovered. Laboratory tests were made for mineralogy, hydraulic conductivity, porosity , consolidation, grain-size distribution, Atterberg limits, X-ray diffraction, and chemical quality of water. Geophysical and thermal gradient logs were made. The hole is sampled periodically for chemical analysis and measured for water level in the three tapped zones. This report presents methods used to obtain field samples, laboratory procedures, and the data obtained. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83697","usgsCitation":"French, J.J., Page, R.W., and Bertoldi, G., 1983, Data for ground-water test hole near Butte City, Central Valley aquifer project, California: U.S. Geological Survey Open-File Report 83-697, v, 59 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83697.","productDescription":"v, 59 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0697/report-thumb.jpg"},{"id":34404,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0697/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34405,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0697/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c91e","contributors":{"authors":[{"text":"French, James J.","contributorId":103651,"corporation":false,"usgs":true,"family":"French","given":"James","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":154197,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bertoldi, G.L.","contributorId":11605,"corporation":false,"usgs":true,"family":"Bertoldi","given":"G.L.","affiliations":[],"preferred":false,"id":154196,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7924,"text":"ofr83147 - 1983 - Water quality of the Potomac River at Chain Bridge at Washington, D.C.; hydrologic-data report, 1978 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr83147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-147","title":"Water quality of the Potomac River at Chain Bridge at Washington, D.C.; hydrologic-data report, 1978 water year","docAbstract":"Water quality data are presented, measured at the Potomac River at Chain Bridge at Washington, D.C. for the 1978 water year. Samples were generally collected twice a week and more frequently during periods of high flow. The samples were analyzed for nitrogen, phosphorus, silica and suspended sediments. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83147","usgsCitation":"Blanchard, S.F., 1983, Water quality of the Potomac River at Chain Bridge at Washington, D.C.; hydrologic-data report, 1978 water year: U.S. Geological Survey Open-File Report 83-147, 14 p. map ;28 cm., https://doi.org/10.3133/ofr83147.","productDescription":"14 p. map ;28 cm.","costCenters":[],"links":[{"id":140720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0147/report-thumb.jpg"},{"id":35489,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0147/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6697b5","contributors":{"authors":[{"text":"Blanchard, Stephen F.","contributorId":54966,"corporation":false,"usgs":true,"family":"Blanchard","given":"Stephen","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":156842,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41855,"text":"ofr83529 - 1983 - Approximate altitude of water levels in wells in the Chicot and Evangeline aquifers in the Houston area, Texas, spring 1983","interactions":[],"lastModifiedDate":"2016-08-11T12:29:31","indexId":"ofr83529","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-529","title":"Approximate altitude of water levels in wells in the Chicot and Evangeline aquifers in the Houston area, Texas, spring 1983","docAbstract":"The purpose of this report, which was prepared in cooperation with the City of Houston, the Harris-Galveston Coastal Subsidence District, and Texas Department of Water Resources, is to show the altitudes of water levels in wells in the Chicot and Evangeline aquifers in the Houston, Texas, metropolitan area. The maps are based on water-level measurements in spring of 1983 in about 500 wells.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83529","usgsCitation":"Strause, J.L., 1983, Approximate altitude of water levels in wells in the Chicot and Evangeline aquifers in the Houston area, Texas, spring 1983: U.S. Geological Survey Open-File Report 83-529, Report: 2 p.; 2 Plates: 15.52 x 11.10 inches and 16.05 x 11.28 inches, https://doi.org/10.3133/ofr83529.","productDescription":"Report: 2 p.; 2 Plates: 15.52 x 11.10 inches and 16.05 x 11.28 inches","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":173336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0529/report-thumb.jpg"},{"id":79575,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0529/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79576,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0529/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79577,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0529/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a237","contributors":{"authors":[{"text":"Strause, Jeffrey L.","contributorId":61420,"corporation":false,"usgs":true,"family":"Strause","given":"Jeffrey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225627,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}