{"pageNumber":"539","pageRowStart":"13450","pageSize":"25","recordCount":16500,"records":[{"id":7237,"text":"ofr82679 - 1983 - Hydrology of area 21, Eastern Coal province, Tennessee, Alabama and Georgia","interactions":[],"lastModifiedDate":"2024-09-24T18:08:13.417331","indexId":"ofr82679","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":"82-679","title":"Hydrology of area 21, Eastern Coal province, Tennessee, Alabama and Georgia","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82679","usgsCitation":"May, V., 1983, Hydrology of area 21, Eastern Coal province, Tennessee, Alabama and Georgia: U.S. Geological Survey Open-File Report 82-679, vi, 92 p., https://doi.org/10.3133/ofr82679.","productDescription":"vi, 92 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":94755,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0679/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":462210,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13802.htm","linkFileType":{"id":5,"text":"html"}},{"id":139837,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0679/report-thumb.jpg"}],"country":"United States","state":"Alabama, Georgia, Tennessee","otherGeospatial":"Eastern Coal Province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.15478515625,\n 34.38877925439021\n ],\n [\n -86.15478515625,\n 35.8356283888737\n ],\n [\n -84.869384765625,\n 35.8356283888737\n ],\n [\n -84.869384765625,\n 34.38877925439021\n ],\n [\n -86.15478515625,\n 34.38877925439021\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604430","contributors":{"authors":[{"text":"May, V.J.","contributorId":71539,"corporation":false,"usgs":true,"family":"May","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":154863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":45935,"text":"ofr82523 - 1983 - Hydrologic quadrangle, Osteen, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:58","indexId":"ofr82523","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":"82-523","title":"Hydrologic quadrangle, Osteen, Florida","language":"ENGLISH","doi":"10.3133/ofr82523","usgsCitation":"Tibbals, C.H., Wood, W., and Snell, L.J., 1983, Hydrologic quadrangle, Osteen, Florida: U.S. Geological Survey Open-File Report 82-523, 3 maps :photocopy ;72 x 55 cm., on sheets 84 x 77 cm., https://doi.org/10.3133/ofr82523.","productDescription":"3 maps :photocopy ;72 x 55 cm., on sheets 84 x 77 cm.","costCenters":[],"links":[{"id":169091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db60568d","contributors":{"authors":[{"text":"Tibbals, C. H.","contributorId":76316,"corporation":false,"usgs":true,"family":"Tibbals","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":232331,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, W.D.","contributorId":31799,"corporation":false,"usgs":true,"family":"Wood","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":232330,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snell, Leonard J.","contributorId":89897,"corporation":false,"usgs":true,"family":"Snell","given":"Leonard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":232332,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19663,"text":"ofr84135 - 1983 - Data for ground-water studies of the San Juan Basin, New Mexico (1982-83)","interactions":[],"lastModifiedDate":"2022-08-29T18:17:29.201772","indexId":"ofr84135","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":"84-135","title":"Data for ground-water studies of the San Juan Basin, New Mexico (1982-83)","docAbstract":"Ground-water data that can be used for futher hydrologic studies in the San Juan structural basin of New Mexico are reported. Descriptions and a location map of 64 observation wells, a list of water levels measured in the observation wells, water-level hydrographs of 32 wells, 15 partial chemical analyses of water samples from wells, and descriptions and a location map of 264 potential observations wells are included. The latter are wells for which good records exist. Their potential for use as observation wells needs to be verified in the field. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84135","usgsCitation":"Klausing, R., and Welder, G.E., 1983, Data for ground-water studies of the San Juan Basin, New Mexico (1982-83): U.S. Geological Survey Open-File Report 84-135, Report: 46 p.; 2 Plates: 19.38 × 21.90 inches and 19.49 × 22.15 inches, https://doi.org/10.3133/ofr84135.","productDescription":"Report: 46 p.; 2 Plates: 19.38 × 21.90 inches and 19.49 × 22.15 inches","costCenters":[],"links":[{"id":49128,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0135/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49127,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0135/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49126,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0135/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152158,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0135/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"San Juan Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109,\n 35\n ],\n [\n -107.333,\n 35\n ],\n [\n -107.333,\n 37\n ],\n [\n -109,\n 37\n ],\n [\n -109,\n 35\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c92f","contributors":{"authors":[{"text":"Klausing, R.L.","contributorId":73205,"corporation":false,"usgs":true,"family":"Klausing","given":"R.L.","affiliations":[],"preferred":false,"id":181295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welder, G. E.","contributorId":100814,"corporation":false,"usgs":true,"family":"Welder","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":181296,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7230,"text":"ofr83264 - 1983 - Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1980","interactions":[],"lastModifiedDate":"2017-06-14T11:15:13","indexId":"ofr83264","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":"83-264","title":"Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1980","docAbstract":"

Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, and Houston. Studies have been completed in the Dallas-Fort Worth and San Antonio areas.

\n

The U.S. Geological Survey, in cooperation with the city of Houston, began studies in the Houston metropolitan area in 1964. The program was expanded in 1968 to include collection of water-quality data. The objectives of the Houston urban-hydrology study are as follows:

\n
    \n
  1. To determine, on the basis of historical data and hydro!ogic analyses, the magnitude and frequency of flood peaks and flood volumes.
    2. \n
  2. To determine the effect of urban development on flood peaks and volumes.
    3. \n
  3. To ascertain the variation in water quality for different flow conditions and different seasons.
    4. \n
\n

This report, the seventeenth in a series of reports to be published annually, is primarily applicable to objective 2. The report presents hydrologic data collected in the Houston urban area for the 1980 water year (October 1, 1979 to September 30, 1980).

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr83264","collaboration":"Prepared in cooperation with the City of Houston","usgsCitation":"Liscum, F., Hutchison, J., Bruchmiller, J., and Walther, L., 1983, Hydrologic data for urban studies in the Houston, Texas, metropolitan area, 1980: U.S. Geological Survey Open-File Report 83-264, vi, 272 p., https://doi.org/10.3133/ofr83264.","productDescription":"vi, 272 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":34623,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0264/report.pdf","text":"Report","size":"5.55 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":139939,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0264/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"Houston","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.36819458007811,\n 30.039377605001338\n ],\n [\n -95.42587280273438,\n 30.039377605001338\n ],\n [\n -95.49179077148438,\n 30.03462216002981\n ],\n [\n -95.56320190429686,\n 30.0262995822237\n ],\n [\n -95.62774658203125,\n 30.001327656702326\n ],\n [\n -95.73348999023438,\n 29.969211659636663\n ],\n [\n -95.83648681640624,\n 29.92756435779241\n ],\n [\n -95.87493896484374,\n 29.888280933159265\n ],\n [\n -95.86257934570312,\n 29.80251790576445\n ],\n [\n -95.86944580078125,\n 29.75364773335698\n ],\n [\n -95.8447265625,\n 29.69640358280457\n ],\n [\n -95.79940795898438,\n 29.672542219068987\n ],\n [\n -95.69641113281249,\n 29.630771207229\n ],\n [\n -95.63186645507812,\n 29.60092416008231\n ],\n [\n -95.51513671875,\n 29.57106827738255\n ],\n [\n -95.40252685546875,\n 29.511330027309146\n ],\n [\n -95.28030395507812,\n 29.485034019181064\n ],\n [\n -95.17730712890625,\n 29.482643134466617\n ],\n [\n -95.086669921875,\n 29.499378142743375\n ],\n [\n -94.99740600585938,\n 29.532839863453397\n ],\n [\n -94.95483398437499,\n 29.551955878093022\n ],\n [\n -94.9493408203125,\n 29.604506272365295\n ],\n [\n -94.96719360351562,\n 29.653449050468925\n ],\n [\n -94.9822998046875,\n 29.680894340704334\n ],\n [\n -95.01800537109374,\n 29.71787396585316\n ],\n [\n -95.0372314453125,\n 29.744109309616487\n ],\n [\n -95.06881713867188,\n 29.76556948666697\n ],\n [\n -95.06744384765625,\n 29.797751134173065\n ],\n [\n -95.07705688476562,\n 29.837070205715218\n ],\n [\n -95.10314941406249,\n 29.871610558533725\n ],\n [\n -95.1361083984375,\n 29.925183985247404\n ],\n [\n -95.15396118164062,\n 29.972780616663897\n ],\n [\n -95.14572143554688,\n 29.997759725578906\n ],\n [\n -95.185546875,\n 30.01916538794235\n ],\n [\n -95.2294921875,\n 30.02511058549258\n ],\n [\n -95.2789306640625,\n 30.029866486852946\n ],\n [\n -95.33660888671875,\n 30.032244351965684\n ],\n [\n -95.36819458007811,\n 30.039377605001338\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607a55","contributors":{"authors":[{"text":"Liscum, Fred","contributorId":95463,"corporation":false,"usgs":true,"family":"Liscum","given":"Fred","email":"","affiliations":[],"preferred":false,"id":154840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchison, J.S.","contributorId":104558,"corporation":false,"usgs":true,"family":"Hutchison","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":154842,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bruchmiller, J.P.","contributorId":102490,"corporation":false,"usgs":true,"family":"Bruchmiller","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":154841,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Walther, L.S.","contributorId":93760,"corporation":false,"usgs":true,"family":"Walther","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":154839,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":45934,"text":"ofr82518 - 1983 - Hydrologic quadrangles, Osceola, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:58","indexId":"ofr82518","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":"82-518","title":"Hydrologic quadrangles, Osceola, Florida","language":"ENGLISH","doi":"10.3133/ofr82518","usgsCitation":"Tibbals, C.H., Wood, W., and Snell, L.J., 1983, Hydrologic quadrangles, Osceola, Florida: U.S. Geological Survey Open-File Report 82-518, 3 maps :photocopy ;72 x 55 cm., on sheets 84 x 77 cm., https://doi.org/10.3133/ofr82518.","productDescription":"3 maps :photocopy ;72 x 55 cm., on sheets 84 x 77 cm.","costCenters":[],"links":[{"id":168628,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605646","contributors":{"authors":[{"text":"Tibbals, C. H.","contributorId":76316,"corporation":false,"usgs":true,"family":"Tibbals","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":232328,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, W.D.","contributorId":31799,"corporation":false,"usgs":true,"family":"Wood","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":232327,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snell, Leonard J.","contributorId":89897,"corporation":false,"usgs":true,"family":"Snell","given":"Leonard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":232329,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":17251,"text":"ofr82505 - 1983 - Hydrology of area 13, eastern coal province, Kentucky, Virginia, and West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr82505","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":"82-505","title":"Hydrology of area 13, eastern coal province, Kentucky, Virginia, and West Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82505","usgsCitation":"Kiesler, J., Quinones-Marquez, F., Mull, D.S., and York, K., 1983, Hydrology of area 13, eastern coal province, Kentucky, Virginia, and West Virginia: U.S. Geological Survey Open-File Report 82-505, v, 203 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/ofr82505.","productDescription":"v, 203 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":95398,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0505/report.pdf","size":"27120","linkFileType":{"id":1,"text":"pdf"}},{"id":94519,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015048193166?urlappend=%3Bseq=3"},{"id":149363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0505/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604737","contributors":{"authors":[{"text":"Kiesler, Jay","contributorId":35751,"corporation":false,"usgs":true,"family":"Kiesler","given":"Jay","email":"","affiliations":[],"preferred":false,"id":175608,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quinones-Marquez, Ferdinand","contributorId":79083,"corporation":false,"usgs":true,"family":"Quinones-Marquez","given":"Ferdinand","email":"","affiliations":[],"preferred":false,"id":175610,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mull, D. S.","contributorId":43331,"corporation":false,"usgs":true,"family":"Mull","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":175609,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"York, Karen","contributorId":25580,"corporation":false,"usgs":true,"family":"York","given":"Karen","email":"","affiliations":[],"preferred":false,"id":175607,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":17252,"text":"ofr83223 - 1983 - Hydrology of Area 1, eastern coal province, Pennsylvania [West Branch Susquehanna River, Sinnemahoning Creek, Upper Juniata River, Clearfield Creek]","interactions":[],"lastModifiedDate":"2022-02-07T21:20:37.876385","indexId":"ofr83223","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":"83-223","title":"Hydrology of Area 1, eastern coal province, Pennsylvania [West Branch Susquehanna River, Sinnemahoning Creek, Upper Juniata River, Clearfield Creek]","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 resources-related 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.

Area 1 covers 7,400 square miles of the Eastern Coal Province in part or all of 18 counties in west-central Pennsylvania. The major streams in the area are the West Branch Susquehanna and Juniata Rivers. Area 1 counties produced more than 20,000,000 tons of coal during 1979. About 66,000 acres of disturbed coal land in Area 1 counties are in need of reclamation.

Streamflow data have been collected at 146 locations in the area, and water-quality data have been collected at 123 locations. Interpretations of water quality in this report are generally based on a series of four water-quality samples collected at each of 113 locations during the 1979-80 water years. Water-quality data collected at these sites included: specific conductance; dissolved solids; pH; acidity; alkalinty; total and dissolved iron; total and dissolved manganese; sulfate; and bed-material iron, manganese, coal, and organic carbon. Most sites had benthic invertebrate populations sampled and analyses of bed-material constituents. A smaller set of sites was sampled for common constituents and minor elements.

Streams in Clearfield and Cambria Counties, the two leading coal producers in the area, had median specific conductances and dissolved-solids concentrations three to five times greater than those from other area counties. Clearfield County streams had the lowest median stream pH in the area. Most streams sampled in the area had acidity in excess of alkalinity. Streams in the three major coal producing counties in the area had median total-iron concentrations two to three times higher than those for other area counties, and the same general pattern was found for total manganese. The median sulfate concentration of a county's streams showed a close positive correlation with the amount of coal mined in the county. Iron and coal concentrations in bed material were higher in coal-producing counties, but manganese concentrations in bed material were not higher. Twenty-eight streams did not have a benthic biological community as defined by the Office of Surface Mining. Three-fourths of the sites with no biological community had levels of pH, acidity, iron, manganese, and sulfate indicative of acid mine drainage.

Statistics on low flow, mean flow, peak flow, and flow-duration can be computed from gaging station records for gaged streams. The same statistics can be estimated for ungaged streams through the use of regression or graphical techniques. This information may be useful in preparing and evaluating mine-permit applications.

Aquifers in the area receive most recharge from precipitation on outcrop areas. Highest ground-water levels generally occur in spring, decline during the summer, and begin to rise again during the fall. Water levels in valleys generally show less fluctuation than on hills. Median well yields in the area range from 5 to 50 gallons per minute. Ground-water supplies are obtained from more than 40 formations. Ground-water quality is generally suitable for most uses.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83223","usgsCitation":"Herb, W.J., Brown, D.E., Shaw, L.C., and Becher, A.E., 1983, Hydrology of Area 1, eastern coal province, Pennsylvania [West Branch Susquehanna River, Sinnemahoning Creek, Upper Juniata River, Clearfield Creek]: U.S. Geological Survey Open-File Report 83-223, vi, 89 p., https://doi.org/10.3133/ofr83223.","productDescription":"vi, 89 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":149364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0223/report-thumb.jpg"},{"id":94516,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0223/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.31579589843749,\n 39.87601941962116\n ],\n [\n -77.47558593749999,\n 39.87601941962116\n ],\n [\n -77.47558593749999,\n 41.93088998442502\n ],\n [\n -79.31579589843749,\n 41.93088998442502\n ],\n [\n -79.31579589843749,\n 39.87601941962116\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604b72","contributors":{"authors":[{"text":"Herb, William J.","contributorId":79454,"corporation":false,"usgs":true,"family":"Herb","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":175611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Deborah E.","contributorId":92255,"corporation":false,"usgs":true,"family":"Brown","given":"Deborah","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":175614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shaw, Lewis C.","contributorId":84433,"corporation":false,"usgs":true,"family":"Shaw","given":"Lewis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":175612,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Becher, Albert E.","contributorId":82979,"corporation":false,"usgs":true,"family":"Becher","given":"Albert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":175613,"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":17254,"text":"ofr83545 - 1983 - Hydrology of area 50, Northern Great Plains and Rocky Mountain coal provinces, Wyoming and Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr83545","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":"83-545","title":"Hydrology of area 50, Northern Great Plains and Rocky Mountain coal provinces, Wyoming and Montana","docAbstract":"This report is one of a series designed to characterize the hydrology of drainage basins within coal provinces, nationwide. Area 50 includes all of the Powder River Basin, Wyoming and Montana and the upstream parts of the Cheyenne and Belle Fourche River Basins - a total of 20,676 sq mi. The area has abundant coal (81.2 million tons mined in 1982), but scarce water. The information in the report is intended to describe the hydrology of the ' general area ' of any proposed mine. The report represents a summary of results of the water resources investigations of the U.S. Geological Survey, carried out in cooperation with State and other Federal agencies. Each of more than 50 topics is discussed in a brief text that is accompanied by maps, graphs, and other illustrations. Primary topics in the report are: physiography, economic development, surface-water data networks, surface water quantity and quality, and groundwater. The report also contains an extensive description of sources of additional information. (USGS)","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr83545","usgsCitation":"Lowry, M.E., Wilson, J.F., and and others, 1983, Hydrology of area 50, Northern Great Plains and Rocky Mountain coal provinces, Wyoming and Montana (WRI/OFR): U.S. Geological Survey Open-File Report 83-545, vi, 137 p., https://doi.org/10.3133/ofr83545.","productDescription":"vi, 137 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":149366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0545/report-thumb.jpg"},{"id":46400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0545/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601fc3","contributors":{"authors":[{"text":"Lowry, Marlin E.","contributorId":52552,"corporation":false,"usgs":true,"family":"Lowry","given":"Marlin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":175622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, James F. Jr.","contributorId":23546,"corporation":false,"usgs":true,"family":"Wilson","given":"James","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":175621,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":529009,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25397,"text":"wri834142 - 1983 - Application of digital mapping technology to the display of hydrologic information; a proof-of-concept test in the Fox-Wolf River Basin, Wisconsin","interactions":[],"lastModifiedDate":"2017-03-29T11:04:25","indexId":"wri834142","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":"83-4142","title":"Application of digital mapping technology to the display of hydrologic information; a proof-of-concept test in the Fox-Wolf River Basin, Wisconsin","docAbstract":"The Fox-Wolf River basin in east-central Wisconsin was selected to test concepts for a water-resources information system using digital mapping technology. This basin of 16,800 sq km is typical of many areas in the country. Fifty digital data sets were included in the Fox-Wolf information system. Many data sets were digitized from 1:500,000 scale maps and overlays. Some thematic data were acquired from WATSTORE and other digital data files. All data were geometrically transformed into a Lambert Conformal Conic map projection and converted to a raster format with a 1-km resolution. The result of this preliminary processing was a group of spatially registered, digital data sets in map form. Parameter evaluation, areal stratification, data merging, and data integration were used to achieve the processing objectives and to obtain analysis results for the Fox-Wolf basin. Parameter evaluation includes the visual interpretation of single data sets and digital processing to obtain new derived data sets. In the areal stratification stage, masks were used to extract from one data set all features that are within a selected area on another data set. Most processing results were obtained by data merging. Merging is the combination of two or more data sets into a composite product, in which the contribution of each original data set is apparent and can be extracted from the composite. One processing result was also obtained by data integration. Integration is the combination of two or more data sets into a single new product, from which the original data cannot be separated or calculated. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834142","usgsCitation":"Moore, G.K., Baten, L., Allord, G., and Robinove, C., 1983, Application of digital mapping technology to the display of hydrologic information; a proof-of-concept test in the Fox-Wolf River Basin, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 83-4142, vi, 118 p., https://doi.org/10.3133/wri834142.","productDescription":"vi, 118 p.","numberOfPages":"130","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":123303,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4142/report-thumb.jpg"},{"id":54127,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4142/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aa00","contributors":{"authors":[{"text":"Moore, G. K.","contributorId":67550,"corporation":false,"usgs":true,"family":"Moore","given":"G.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":193517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baten, L.G.","contributorId":74786,"corporation":false,"usgs":true,"family":"Baten","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":193519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allord, G.J.","contributorId":26665,"corporation":false,"usgs":true,"family":"Allord","given":"G.J.","affiliations":[],"preferred":false,"id":193516,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robinove, C.J.","contributorId":68778,"corporation":false,"usgs":true,"family":"Robinove","given":"C.J.","affiliations":[],"preferred":false,"id":193518,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":29330,"text":"wri824081 - 1983 - Limnological study of Shasta Lake, Shasta County, California, with emphasis on the effects of the 1977 drought","interactions":[],"lastModifiedDate":"2012-02-02T00:08:45","indexId":"wri824081","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":"82-4081","title":"Limnological study of Shasta Lake, Shasta County, California, with emphasis on the effects of the 1977 drought","docAbstract":"An intensive limnological study of Shasta Lake was made in conjunction with the California Department of Water Resources during the 1977 drought. Water-quality data were collected from March 1977 through September 1978 at six lake stations and four lake tributary stations. Data collected during and after the drought were compared. Lake water quality is described as a function of lake morphometry, climate, hydrology, and reservoir hydraulics. Results indicate Shasta Lake is a warm monomictic lake. Tributary inflow to the lake and outflow through the dam generate density currents which promote mixing at depth and the development of an extensive metalimnion. During the drought, record low lake levels resulted in the exposure of an extensive nearshore sediment zone. Resuspended sediments caused a deterioration of water quality. The most notable effects, in comparison with post-drought conditions, were decreased light penetration, increased dissolved-solids concentration and specific conductance, decreased dissolved-oxygen concentrations, and elevated nutrient levels. A hypolimnetic anoxic condition was observed at the upstream stations of the lake. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824081","usgsCitation":"Rettig, S., and Bortleson, G.C., 1983, Limnological study of Shasta Lake, Shasta County, California, with emphasis on the effects of the 1977 drought: U.S. Geological Survey Water-Resources Investigations Report 82-4081, vii, 66 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824081.","productDescription":"vii, 66 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4081/report-thumb.jpg"},{"id":58168,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4081/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5220","contributors":{"authors":[{"text":"Rettig, S.A.","contributorId":104105,"corporation":false,"usgs":true,"family":"Rettig","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":201357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bortleson, Gilbert C.","contributorId":57472,"corporation":false,"usgs":true,"family":"Bortleson","given":"Gilbert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9743,"text":"ofr8321 - 1983 - Bryozoan fauna of the Upper Clays Ferry, Kope, and Lower Fairview formations (Edenian, Upper Ordovician) at Moffett Road, northern Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr8321","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":"83-21","title":"Bryozoan fauna of the Upper Clays Ferry, Kope, and Lower Fairview formations (Edenian, Upper Ordovician) at Moffett Road, northern Kentucky","docAbstract":"The geology, water movement, and sediment characteristics in the upstream part of the Spring River basin have been appraised, to assist the U.S. EPA in their study of dioxin contamination in the area. The U.S. Environmental Protection Agency has confirmed that the dioxin compound, TCDD (2,3,7 ,8-tetrachlorodibenzo-p-dioxin), is present in the soils, streambed sediments, and fish in the upstream part of the Spring River Basin. Although the solubility of dioxin is small, it may be moving through the hydrologic system, adsorbed on sediment particles. Water movement in the shallow aquifer generally follows the topography. In upland areas, precipitation recharges the shallow aquifer, then the shallow aquifer water discharges into larger streams. Sediment yields generally are small in the upstream part of the Spring River basin. Suspended sediment discharges for the Spring River at La Russell ranged from 3.0 tons/day at a flow of 79 cu ft/sec, 1.7 times the 7-day 2-yr low flow, to about 1240 tons/day at a flow of 1600 cu ft/sec, 6.7 times the long-term average. Suspended sediment particles in the Spring River and Honey Creek generally were silt and clay (smaller than 0.062 mm). Fine sediments with adsorbed dioxin may be transported out of the area by streamflow, or they may be deposited on flood plains or in downstream impoundments during periods of flooding. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8321","usgsCitation":"Karklins, O.L., 1983, Bryozoan fauna of the Upper Clays Ferry, Kope, and Lower Fairview formations (Edenian, Upper Ordovician) at Moffett Road, northern Kentucky: U.S. Geological Survey Open-File Report 83-21, 56 p. ill. ;28 cm., https://doi.org/10.3133/ofr8321.","productDescription":"56 p. ill. ;28 cm.","costCenters":[],"links":[{"id":144062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0021/report-thumb.jpg"},{"id":37489,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0021/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37490,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0021/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37491,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f26d8","contributors":{"authors":[{"text":"Karklins, Olgerts L.","contributorId":55828,"corporation":false,"usgs":true,"family":"Karklins","given":"Olgerts","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true},{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":160198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7226,"text":"ofr8344 - 1983 - Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1981","interactions":[],"lastModifiedDate":"2017-06-14T10:53:09","indexId":"ofr8344","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":"83-44","title":"Hydrologic data for urban studies in the Austin, Texas, metropolitan area, 1981","docAbstract":"

Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, and Houston. Studies have been completed in the Dallas, Fort Worth, and San Antonio areas.

The Geological Survey, in cooperation with the Texas Department of Water Resources, began hydrologic studies in the Austin urban area in 1954. In cooperation with the city of Austin, the program was expanded in 1975 to include additional streamflow and rainfall gaging stations, and the collection of surface water-quality data. In 1978, the program was expanded to include a ground-water resources study of the South Austin metropolitan area in the Balcones Fault Zone.

The objectives of the Austin urban hydrology study are as follows:

  1. To determine, on the basis of historical data and hydrologic analyses, the magnitude and frequency of flood peaks and flood volume.
  2. To determine the effect of urban development on flood peaks and volume.
  3. To determine the variations in water quality during different seasons and flow conditions in representative watersheds under various types of urban development.
  4. To quantitatively appraise the ground-water resources along the Balcones Fault Zone, the effect of urbanization on the quality and quantity of recharge and discharge, and the extent of contamination in the Edwards aquifer that is is hydrologic circulation with Barton Springs.

This report presents the basic hydroloqic data collected in the Austin urban area for the 1981 water year (Oct. 1, 1980 to Sept. 30, 1981).

Additional explanations of terms related to streamflow, water quality, and other hydrologic data used in this report are defined in the U.S. Geological Survey annual report Water Resources Data for Texas, TX-81-3, 1981.

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E.","contributorId":58254,"corporation":false,"usgs":true,"family":"Smith","given":"A.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":154828,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":7612,"text":"ofr83251 - 1983 - Water resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"ofr83251","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":"83-251","title":"Water resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1983","docAbstract":"Water-resources investigations of the U.S. Geological Survey in Missouri consist of collecting hydrologic data and making interpretive investigations. These data and the results of the investigations are published or released by either the U.S. Geological Survey or by cooperating agencies. This report describes the data-collection activities and investigations in Missouri for the 1983 fiscal year and provides an extensive list of water-resources references for the State of Missouri. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83251","usgsCitation":"Kratzer, W.M., 1983, Water resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1983: U.S. Geological Survey Open-File Report 83-251, ii, 55 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83251.","productDescription":"ii, 55 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0251/report-thumb.jpg"},{"id":35101,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0251/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faf42","contributors":{"authors":[{"text":"Kratzer, Wanietia M.","contributorId":40978,"corporation":false,"usgs":true,"family":"Kratzer","given":"Wanietia","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":156302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10025,"text":"ofr83129 - 1983 - Selective annotated bibliography of ground-water resources, records of wells and springs, and availability of streamflow data on Indian reservations in Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr83129","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":"83-129","title":"Selective annotated bibliography of ground-water resources, records of wells and springs, and availability of streamflow data on Indian reservations in Montana","docAbstract":"A compilation was made, for each of the seven Indian reservations in Montana, of the availability of hydrologic data. The report consists of an annotated bibliography of ground-water resources reports, selected data for wells and springs from the data bases of the U.S. Geological Survey and Montana Bureau of Mines and Geology, and a listing of all sites where streamflow has been measured and water-quality samples collected by the U. S.Geological Survey. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83129","usgsCitation":"Levings, G., and White, M.K., 1983, Selective annotated bibliography of ground-water resources, records of wells and springs, and availability of streamflow data on Indian reservations in Montana: U.S. Geological Survey Open-File Report 83-129, iv, 141 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83129.","productDescription":"iv, 141 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0129/report-thumb.jpg"},{"id":37865,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a00e4b07f02db5f7d29","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":160692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Melvin K. mwhite@usgs.gov","contributorId":1563,"corporation":false,"usgs":true,"family":"White","given":"Melvin","email":"mwhite@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":160691,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29516,"text":"wri834091 - 1983 - Hydrology of the Newberry Volcano caldera, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri834091","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":"83-4091","title":"Hydrology of the Newberry Volcano caldera, Oregon","docAbstract":"Precipitation in the Newberry Caldera is very nearly in balance with evaporation, evapotranspiration, and streamflow. Calcium, magnesium, and bicarbonate ions predominate in the more dilute ground and surface water. Thermal waters from springs and wells have concentrations of 900 milligrams per liter or more and are characterized by high concentrations of sodium and sulfate. Attempts to account for the origin of the hot springs on the basis of mixing relations and isotopic analyses were inconclusive; the springs may represent mixtures of thermal and nonthermal water which are altered by gases rising from sources beneath the caldera floor. Annual recharge to deep aquifers beneath the caldera is probably in the range 2,500 to 6,500 acre-feet. Observations in a Geological Survey drill hole suggest that part of the water may flow to aquifers at depths as much as 1,900 feet beneath the caldera floor. Potential recharge to a postulated geothermal reservoir probably is extremely small. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834091","usgsCitation":"Sammel, E., and Craig, R.W., 1983, Hydrology of the Newberry Volcano caldera, Oregon: U.S. Geological Survey Water-Resources Investigations Report 83-4091, v, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834091.","productDescription":"v, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4091/report-thumb.jpg"},{"id":58356,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601a2f","contributors":{"authors":[{"text":"Sammel, E.A.","contributorId":59480,"corporation":false,"usgs":true,"family":"Sammel","given":"E.A.","affiliations":[],"preferred":false,"id":201648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Craig, R. 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No abstract available.

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The Geological Survey began its water-resources investigations in New York in 1895. To meet the objectives of assessing New York's water resources, the Geological Survey (1) monitors the quantity and quality of surface and ground water, (2) conducts investigations of the occurrence, availability, and chemical quality of water in specific areas of the State, (3) develops methods and techniques of data-collection and interpretation, (4) provides scientific guidance to the research community, to Federal, State, and local governments, and to the public, and (5) disseminates data and results of research through reports, maps, news releases, conferences, and workshops. \r\n\r\nMany of the joint hydrologic investigations are performed by the Geological Survey in cooperation with State, county, and nonprofit organizations. The data collection network in New York includes nearly 200 gaging stations and 250 observation wells; chemical quality of water is measured at 260 sites. Data collected at these sites are published annually and are filed in the WATSTORE computer system. Some of the interpretive studies performed by the Geological Survey in New York include (1) determining the suitability of ground-water reservoirs for public-water supply in urban areas, (2) assessing geohydrologic impacts of leachate from hazardous waste sites on stream and ground-water quality, (3) evaluating the effects of precipitation quality and basin characteristics on streams and lakes, and (4) developing digital models of the hydrology of aquifers to simulate ground-water flow and the interaction between ground water and streams.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83270","usgsCitation":"Wiltshire, D.A., 1983, The U.S. Geological Survey's water resources program in New York: U.S. Geological Survey Open-File Report 83-270, 15 p. ;27 cm., https://doi.org/10.3133/ofr83270.","productDescription":"15 p. ;27 cm.","costCenters":[],"links":[{"id":139857,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0270/report-thumb.jpg"},{"id":35074,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0270/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6498d8","contributors":{"authors":[{"text":"Wiltshire, Denise A.","contributorId":78717,"corporation":false,"usgs":true,"family":"Wiltshire","given":"Denise","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156237,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29754,"text":"wri834202 - 1983 - Hydrology of an abandoned coal-mining area near McCurtain, Haskell County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri834202","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":"83-4202","title":"Hydrology of an abandoned coal-mining area near McCurtain, Haskell County, Oklahoma","docAbstract":"Water quality was investigated from October 1980 to May 1983 in an area of abandoned coal mines in Haskell county, Oklahoma. Bedrock in the area is shale, siltstone, sandstone, and the McAlester (Stigler) and Hartshorne coals of the McAlester Formation and Hartshorne Sandstone of Pennsylvanian age. The two coal beds, upper and lower Hartshorne, associated with the Hartshorne Sandstone converge or are separated by a few feet or less of bony coal or shale in the McCurtain area. Many small faults cut the Hartshorne coal in all the McCurtain-area mines. The main avenues of water entry to and movement through the bedrock are the exposed bedding-plane openings between layers of sandstone, partings between laminae of shale, fractures and joints developed during folding and faulting laminae of shale, fractures and joints developed during folding and faulting of the brittle rocks, and openings caused by surface mining--the overburden being shattered and broken to form spoil. Water-table conditions exist in bedrock and spoil in the area. Mine pond water is in direct hydraulic connections with water in the spoil piles and the underlying Hartshorne Sandstone.\r\nSulfate is the best indicator of the presence of coal-mine drainage in both surface and ground water in the Oklahoma coal field. Median sulfate concentrations for four sites on Mule Creek ranged from 26 to 260 milligrams per liter. Median sulfate concentrations increased with increased drainage from unreclaimed mined areas. The median sulfate concentration in Mule Creek where it drains the reclaimed area is less than one-third of that at the next site downstream where the stream begins to drain abandoned (unreclaimed) mine lands.\r\n\r\nWater from Mule Creek predominantly is a sodium sulfate type. Maximum and median values for specific conductance and concentrations of calcium, magnesium, sodium, sulfate, chloride, dissolved solids, and alkalinity increase as Mule Creek flows downstream and drains increasing areas of abandoned (unreclaimed) mining lands. Constituent concentrations in Mule Creek, except those for dissolved solids, iron, manganese, and sulfate, generally do not exceed drinking-water limits. Reclamation likely would result in decreased concentrations of dissolved solids, calcium, magnesium, sodium, sulfate, and alkalinity in Mule Creek in the vicinity of the reclaimed area.\r\n\r\nGround water in the area is moderately hard to very hard alkaline water with a median pH of 7.2 to 7.6. It predominately is a sodium sulfate type and, except for dissolved solids, iron manganese, and sulfate, constituent concentrations generally do not exceed drinking-water limits. Ground-water quality would likely be unchanged by reclamation.\r\n\r\nThe quality of water in the two mine ponds is quite similar to that of the shallow ground water in the area. Constituents in water from both ponds generally do not exceed drinking-water limits and the water quality is unlikely to be changed by reclamation in the area.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834202","usgsCitation":"Slack, L.J., 1983, Hydrology of an abandoned coal-mining area near McCurtain, Haskell County, Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 83-4202, v, 117 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834202.","productDescription":"v, 117 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4202/report-thumb.jpg"},{"id":58548,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4202/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58549,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4202/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e2ef3","contributors":{"authors":[{"text":"Slack, L. J.","contributorId":44157,"corporation":false,"usgs":true,"family":"Slack","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28692,"text":"wri834016 - 1983 - Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri834016","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":"83-4016","title":"Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico","docAbstract":"Geohydrologic data have been collected in the Los Medanos area at the U.S. Department of Energy 's proposed Waste Isolation Pilot Plant (WIPP) site in southeastern New Mexico since 1975 as part of an intensive study evaluating the feasibility of storing defense-associated nuclear wastes within the bedded salt of the Salado Formation of Permian age. Drilling and hydrologic testing have identified three principal water-producing zones above the salt, including the Rustler-Salado Formational contact and the Culebra and Magenta Dolomite Members of the Permian Rustler Formation. Below the bedded salt there is another water-bearing zone, the channel sandstones of the Bell Canyon formation of the Permian Delaware Mountain Group. Most data collected from 33 hydrologic test holes indicate that the water-bearing zones are characterized by low transmissivities and contain slightly saline to briny water. Data collected from drill-stem tests in the Bell Canyon Formation indicate the channel sandstones have hydraulic conductivities ranging from 0.02 to 0.36 feet per day grade vertically and laterally into siltstones and shales of very low permeability. The Rustler Formation contains the principal water-producing zones identified at the WIPP site. The Rustler-Salado formational contact has the least transmissivity, ranging from 0.00003 to 0.003 feet squared per day. The Culebra Dolomite is the most productive unit at the WIPP site with transmissivities ranging from 0.001 to 73 feet squared per day; the greater values result from fracturing in the dolomite created by dissolution of underlying halite. Minute vertical permeabilities prevent movement of water between hydrologic units. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834016","usgsCitation":"Mercer, J.W., 1983, Geohydrology of the proposed Waste Isolation Pilot Plant site, Los Medanos area, southeastern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 83-4016, viii, 121 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834016.","productDescription":"viii, 121 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4016/report-thumb.jpg"},{"id":57535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8824","contributors":{"authors":[{"text":"Mercer, Jerry W.","contributorId":32534,"corporation":false,"usgs":true,"family":"Mercer","given":"Jerry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10156,"text":"ofr83143 - 1983 - Hydrologic data from the Johnson Brook phosphorus loading study, Kennebec County, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr83143","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":"83-143","title":"Hydrologic data from the Johnson Brook phosphorus loading study, Kennebec County, Maine","docAbstract":"Streamflow, water quality, and precipitation data collected during the 1980 and 1981 water years are reported. The purpose was to document changes in total phosphorus loads resulting from a change in agricultural waste management practices in the Johnson Brook watershed in Maine. Streamflow data include mean-daily discharges for the period May 12, 1980, through September 30, 1981, and instantaneous discharges determined during water quality sampling. Water quality data for the period March 1980 to September 1981 include total phosphorus concentrations determined from samples collected using cross-sectional depth-integrating sampling techniques and from samples collected using a pumping sampler. Suspended sediment concentrations, and water temperature and specific conductance values are also included. The precipitation data are daily totals for the period October 1980 through September 1981. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83143","usgsCitation":"Maloney, T.J., Dominie, D.R., and Nichols, W.J., 1983, Hydrologic data from the Johnson Brook phosphorus loading study, Kennebec County, Maine: U.S. Geological Survey Open-File Report 83-143, iv, 27 p. maps ;28 cm., https://doi.org/10.3133/ofr83143.","productDescription":"iv, 27 p. maps ;28 cm.","costCenters":[],"links":[{"id":144281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0143/report-thumb.jpg"},{"id":38000,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db60784b","contributors":{"authors":[{"text":"Maloney, Thomas J.","contributorId":35736,"corporation":false,"usgs":true,"family":"Maloney","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":160907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dominie, David R.","contributorId":11227,"corporation":false,"usgs":true,"family":"Dominie","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160905,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nichols, William J.","contributorId":20752,"corporation":false,"usgs":true,"family":"Nichols","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":160906,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7782,"text":"ofr83677 - 1983 - Hydrology of the Jasper (Miocene) Aquifer in the Southeast Texas coastal plain","interactions":[],"lastModifiedDate":"2025-09-23T16:51:31.349837","indexId":"ofr83677","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":"83-677","title":"Hydrology of the Jasper (Miocene) Aquifer in the Southeast Texas coastal plain","docAbstract":"

The Jasper (Miocene) aquifer is one of several important hydrologic units in the Gulf Coastal Plain. Because the Jasper aquifer underlies shallower aquifers in many areas, regional water withdrawals from the Jasper are not significant; however, it is capable of yielding 3,000 gallons per minute (200 liters per second) or more of water to wells in certain areas. The Jasper is underlain by the Catahoula confining system (restricted) and overlain by the Burkeville confining system. The Evangeline and Chicot aquifers, in turn, overlie the Burkeville and also are prolific water-yielding aquifers.

The ground-water hydrology of the Jasper aquifer in an area of about 20,000 square miles (52,000 square kilometers) was simulated by a two-dimensional digital model using a steady-state approach. The model represents hydrologic conditions prior to development by wells, when natural recharge equaled natural discharge. The model's grid pattern of 15 x 24 nodes varies from a dimension of 5 by 10 miles (8 by 16 kilometers) in the outcrop to 10 by 10 miles (16 by 16 kilometers) in the artesian section downdip from the outcrop.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83677","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Baker, E., 1983, Hydrology of the Jasper (Miocene) Aquifer in the Southeast Texas coastal plain: U.S. Geological Survey Open-File Report 83-677, Report: viii, 68 p.; 17 Plates: 20.28 x 10.58 inches or smaller, https://doi.org/10.3133/ofr83677.","productDescription":"Report: viii, 68 p.; 17 Plates: 20.28 x 10.58 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":495911,"rank":19,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0677/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35261,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35260,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35259,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35258,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35268,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35267,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35266,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35264,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35263,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35262,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35257,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35256,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35255,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35254,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35253,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35252,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35265,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0677/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141254,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0677/report-thumb.jpg"}],"country":"United 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