Water resources data for the 1983 water year for Pennsylvania consist of records of discharge and water quality of streams; contents of lakes and reservoirs; and water levels, and water quality of ground-water wells. This volume contains records for water discharge at 84 stations; contents at 13 lakes and reservoirs, water quality at 18 gaging stations; and water levels at 26 network observation wells. Also included are data for 12 crest-stage, 98 low flow, and 3 water-quality, and 85 ground water-quality partial-record stations. Locations of these sites are shown on figures 7-10. Additional water data were collected at various sites not involved in-the systematic data-collection program and are published as miscellaneous measurements and analysis. These data together with the data in Volumes 1 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Pennsylvania.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrPA832","collaboration":"Prepared in cooperation with the Pennsylvania Department of Environmental Resources, the U.S. Army Corps of Engineers, Baltimore District, The Susquehanna River Basin Commission, and with other State, municipal, and Federal agencies","usgsCitation":"Buchanan, J., Loper, W., Schaffstall, W., and Hainly, R., 1984, Water resources data, Pennsylvania, water year 1983. 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stored on site in rubber-lined and clay-lined pits and in large tanks at the U.S. Department of Energy Feed Materials Production Center (FMPC), where purified uranium and uranium compounds are produced. Water samples collected from off-site domestic and commercial wells in December 1981 and in August 1982, contained concentrations of dissolved uranium that ranged from < 0.4 to 430 micrograms/L (ug/L). The wells whose samples contained unusual concentrations of uranium (> 10 ug/L) lie roughly along a line extending about 2000 ft south from the southern boundary of FMPC. The offsite area affected by these concentrations is probably < 100 acres. It is not possible to determine the exact point of origination of contaminants in the groundwater on the basis of available data. 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Pennsylvanian Cherokee and Marmaton Groups, southeastern Iowa, Missouri, southeastern Kansas, and northeastern Oklahoma: U.S. Geological Survey Open-File Report 84-160, i, 41 p. :map ;28 cm., https://doi.org/10.3133/ofr84160.","productDescription":"i, 41 p. :map ;28 cm.","costCenters":[],"links":[{"id":150488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0160/report-thumb.jpg"},{"id":46603,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c228","contributors":{"authors":[{"text":"Hatch, J. R.","contributorId":14775,"corporation":false,"usgs":true,"family":"Hatch","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":176436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daws, T.A.","contributorId":56651,"corporation":false,"usgs":true,"family":"Daws","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":176439,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lubeck, C.M.","contributorId":26190,"corporation":false,"usgs":true,"family":"Lubeck","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":176437,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pawlewicz, M. J.","contributorId":75111,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"M. J.","affiliations":[],"preferred":false,"id":176440,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Threlkeld, C. N.","contributorId":80271,"corporation":false,"usgs":true,"family":"Threlkeld","given":"C.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":176441,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Vuletich, A.K.","contributorId":43784,"corporation":false,"usgs":true,"family":"Vuletich","given":"A.K.","affiliations":[],"preferred":false,"id":176438,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":27149,"text":"wri834125 - 1984 - Hydrogeology of a low-level radioactive-waste disposal site near Sheffield, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri834125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4125","title":"Hydrogeology of a low-level radioactive-waste disposal site near Sheffield, Illinois","docAbstract":"The Sheffield low-level radioactive-waste facility is located on 20 acres of rolling terrain 3 miles southwest of Sheffield, Illinois. The shallow hydrogeologic system is composed of glacial sediments. Pennsylvania shale and mudstone bedrock isolate the regional aquifers below from the hydrogeologic system in the overlying glacial deposits. Pebbly sand underlies 67 percent of the site. Two ground-water flow paths were identified. The primary path conveys ground water from the site to the east through the pebbly-sand unit; a secondary path conveys ground water to the south and east through less permeable material. The pebbly-sand unit provides an underdrain that eliminates the risk of water rising into the trenches. Digital computer model results indicate that the pebbly-sand unit controls ground-water movement. Tritium found migrating in ground water in the southeast corner of the site travels approximately 25 feet per year. A group of water samples from wells which contained the highest tritium concentrations had specific conductivities, alkalinities, hardness, and chloride, sulfate, calcium, and magnesium contents higher than normal for local shallow ground water. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834125","usgsCitation":"Foster, J., Erickson, J., and Healy, R.W., 1984, Hydrogeology of a low-level radioactive-waste disposal site near Sheffield, Illinois: U.S. Geological Survey Water-Resources Investigations Report 83-4125, viii, 83 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834125.","productDescription":"viii, 83 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2120,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=WRIR&number=83-4125","linkFileType":{"id":5,"text":"html"}},{"id":121965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4125/report-thumb.jpg"},{"id":56030,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4125/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db6246cc","contributors":{"authors":[{"text":"Foster, J.B.","contributorId":12040,"corporation":false,"usgs":true,"family":"Foster","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":197639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, J.R.","contributorId":66689,"corporation":false,"usgs":true,"family":"Erickson","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":197640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Healy, R. W.","contributorId":89872,"corporation":false,"usgs":true,"family":"Healy","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":197641,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":21419,"text":"ofr84277 - 1984 - Disturbance of soil and vegetation by the Johnson Valley-Parker motorcycle race of October 8, 1983, in Wilderness Study Area 304A, California and vicinity","interactions":[],"lastModifiedDate":"2012-02-02T00:07:47","indexId":"ofr84277","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-277","title":"Disturbance of soil and vegetation by the Johnson Valley-Parker motorcycle race of October 8, 1983, in Wilderness Study Area 304A, California and vicinity","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84277","usgsCitation":"Wilshire, H.G., 1984, Disturbance of soil and vegetation by the Johnson Valley-Parker motorcycle race of October 8, 1983, in Wilderness Study Area 304A, California and vicinity: U.S. Geological Survey Open-File Report 84-277, 14 p. :chiefly ill., map ;28 cm., https://doi.org/10.3133/ofr84277.","productDescription":"14 p. :chiefly ill., map ;28 cm.","costCenters":[],"links":[{"id":153885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0277/report-thumb.jpg"},{"id":50989,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0277/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d92d","contributors":{"authors":[{"text":"Wilshire, H. G.","contributorId":36125,"corporation":false,"usgs":false,"family":"Wilshire","given":"H.","middleInitial":"G.","affiliations":[],"preferred":false,"id":184396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55815,"text":"wdrNM831 - 1984 - Water resources data, New Mexico, water year 1983","interactions":[],"lastModifiedDate":"2013-07-09T16:12:05","indexId":"wdrNM831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NM-83-1","title":"Water resources data, New Mexico, water year 1983","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNM831","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Water resources data, New Mexico, water year 1983: U.S. Geological Survey Water Data Report NM-83-1, 540 p., https://doi.org/10.3133/wdrNM831.","productDescription":"540 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":185265,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":270294,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/nm-83-1/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0502,31.3322 ], [ -109.0502,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.0502,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0dce","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":532409,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21411,"text":"ofr84124 - 1984 - Engineering-geologic maps of northern Alaska, Barrow quadrangle","interactions":[],"lastModifiedDate":"2022-03-25T19:26:35.767904","indexId":"ofr84124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-124","title":"Engineering-geologic maps of northern Alaska, Barrow quadrangle","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84124","usgsCitation":"Williams, J., and Carter, L.D., 1984, Engineering-geologic maps of northern Alaska, Barrow quadrangle: U.S. Geological Survey Open-File Report 84-124, Report: iii, 39 p.; 2 Plates: 38.36 × 42.31 inches and 38.40 × 42.03 inches, https://doi.org/10.3133/ofr84124.","productDescription":"Report: iii, 39 p.; 2 Plates: 38.36 × 42.31 inches and 38.40 × 42.03 inches","costCenters":[],"links":[{"id":50983,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0124/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50982,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0124/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50981,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0124/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0124/report-thumb.jpg"},{"id":397626,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13280.htm"}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Barrow quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -157.5,\n 71\n ],\n [\n -154.5,\n 71\n ],\n [\n -154.5,\n 71.5\n ],\n [\n -157.5,\n 71.5\n ],\n [\n -157.5,\n 71\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6026c8","contributors":{"authors":[{"text":"Williams, John R.","contributorId":41832,"corporation":false,"usgs":true,"family":"Williams","given":"John R.","affiliations":[],"preferred":false,"id":184379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, L. D.","contributorId":87959,"corporation":false,"usgs":true,"family":"Carter","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":184380,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10951,"text":"ofr84849 - 1984 - Spectral analysis of aeromagnetic profiles for depth estimation principles, software, and practical application","interactions":[],"lastModifiedDate":"2015-09-07T13:56:32","indexId":"ofr84849","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-849","title":"Spectral analysis of aeromagnetic profiles for depth estimation principles, software, and practical application","docAbstract":"Fourier spectral analysis in recent years has become a widely utilized tool for the processing and interpretation of potential field data. It is particularly well suited to analysis of aeromagnetic maps and profiles, where coverage commonly is of broad scope and statistical treatment is appropriate.
\nThe techniques developed by earlier workers for map data are readily adapted for depth estimates using aeromagnetic profiles. Three subroutines are presented: \"FRQAN\", which employs the complete Fourier transform to convert field intensity to the frequency domain and then computes the logarithmic energy spectrum; \"CSIZE\", which refines the spectrum to correct for the finite horizontal dimensions of magnetic sources, and \"ENSMTH\", which smooths the spectrum to clarify its decay characteristics. The average depths to sources of ensembles are obtained by manually fitting a straight line to each linear interval of the logarithmic energy-decay curve.
\nIf proper account is taken of the constraints of the method, it is capable of providing depth estimates to within an accuracy of about 10 percent under suitable circumstances. The estimates are unaffected by source magnetization and are relatively insensitive to assumptions as to source shape or distribution. The validity of the method is demonstrated by analyses of synthetic profiles and profiles recorded over Harrat Rahat, Saudi Arabia, and Diyur, Egypt, where source depths have been proved by drilling.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84849","usgsCitation":"Sadek, H., Rashad, S., and Blank, H., 1984, Spectral analysis of aeromagnetic profiles for depth estimation principles, software, and practical application: U.S. Geological Survey Open-File Report 84-849, ii, 56 p. in various pagings :ill. ;28 cm., https://doi.org/10.3133/ofr84849.","productDescription":"ii, 56 p. in various pagings :ill. ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":144197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0849/report-thumb.jpg"},{"id":38721,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0849/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5de7","contributors":{"authors":[{"text":"Sadek, H.S.","contributorId":93915,"corporation":false,"usgs":true,"family":"Sadek","given":"H.S.","affiliations":[],"preferred":false,"id":162260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rashad, S.M.","contributorId":63016,"corporation":false,"usgs":true,"family":"Rashad","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":162259,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blank, H. R.","contributorId":50516,"corporation":false,"usgs":true,"family":"Blank","given":"H. R.","affiliations":[],"preferred":false,"id":162258,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":17805,"text":"ofr84110 - 1984 - United States Government initiatives in the assessment and development of the mineral resources of the Exclusive Economic Zone of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr84110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-110","title":"United States Government initiatives in the assessment and development of the mineral resources of the Exclusive Economic Zone of the United States","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84110","usgsCitation":"Holser, A., McGregor, B., Rowland, R., and Goud, M., 1984, United States Government initiatives in the assessment and development of the mineral resources of the Exclusive Economic Zone of the United States: U.S. Geological Survey Open-File Report 84-110, ii, 22 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84110.","productDescription":"ii, 22 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149193,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0110/report-thumb.jpg"},{"id":47045,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ee53","contributors":{"authors":[{"text":"Holser, A.F.","contributorId":100866,"corporation":false,"usgs":true,"family":"Holser","given":"A.F.","email":"","affiliations":[],"preferred":false,"id":177905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGregor, B.A.","contributorId":57072,"corporation":false,"usgs":true,"family":"McGregor","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":177904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowland, R.W.","contributorId":36153,"corporation":false,"usgs":true,"family":"Rowland","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":177903,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Goud, M.R.","contributorId":11599,"corporation":false,"usgs":true,"family":"Goud","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":177902,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":27180,"text":"wri834082 - 1984 - Ground-water resources of Lanfair and Fenner Valleys and vicinity, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri834082","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4082","title":"Ground-water resources of Lanfair and Fenner Valleys and vicinity, San Bernardino County, California","docAbstract":"Lanfair and Fenner Valleys and vicinity cover about 1,300 square miles in eastern San Bernardino County, California. Average annual precipitation ranges from 3 to 10 inches over the area. Ground water is utilized primarily for stock and domestic purposes, and occurs in the unconsolidated deposits as well as in the highly fractured consolidated rock. Ground-water levels in wells range from 5 to 600 feet below land surface, and well yields range from 3 to 1,200 gallons per minute throughout the study area. Records indicate that water levels are at or near their predevelopment levels. Springs occur along faults and formational contacts and generally discharge less than 5 gallons per minute. Measured ground-water outflow from Lanfair Valley at Piute Spring ranged from 100 to 630 acre-feet per year. Most of the water is of good quality for domestic and stock use. However , water from two wells indicates a concentration of sulfate that is above the recommended limit for drinking water. Water supplies are adequate for present needs. However, large-scale pumping would result in the lowering of the water table and a reduction of the ground water in storage. 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