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The network was established to monitor local ground-water levels, to determine drought conditions, and to monitor ground-water-level trends. Drought-warning and drought-emergency water-level triggers were determined for 20 of the 23 wells in the Chester County observation-well network. A statistical test to determine either rising or declining water-level trends was performed on data for all wells in the network. Water-level data from both of these wells showed a rising trend. 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Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070
No abstract available.
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1996 - Mineral and energy resource assessment of the Helena National Forest, west-central Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:09:00","indexId":"ofr96683A","displayToPublicDate":"1998-02-01T00:00:00","publicationYear":"1996","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":"96-683","chapter":"A","title":"Mineral and energy resource assessment of the Helena National Forest, west-central Montana","language":"ENGLISH","doi":"10.3133/ofr96683A","usgsCitation":"Tysdal, R.G., Ludington, S.D., and McCafferty, A.E., 1996, Mineral and energy resource assessment of the Helena National Forest, west-central Montana: U.S. Geological Survey Open-File Report 96-683, 18 maps on 6 sheets :photocopies ;103 x 124 cm. and 52 x 62 cm., on sheets 108 x 150 cm., folded to 25 x 19 cm. +1 text (various pagings : ill., maps ; 28 cm.), https://doi.org/10.3133/ofr96683A.","productDescription":"18 maps on 6 sheets :photocopies ;103 x 124 cm. and 52 x 62 cm., on sheets 108 x 150 cm., folded to 25 x 19 cm. +1 text (various pagings : ill., maps ; 28 cm.)","costCenters":[],"links":[{"id":159893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0683a/report-thumb.jpg"},{"id":19315,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-1_a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19316,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-1_b.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19317,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-2_a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19318,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-2_b.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19319,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-3_a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19320,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-3_b.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19321,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-4_a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19322,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-4_b.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19323,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-5_a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19324,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-5_b.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19516,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-6_a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19517,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0683a/plate-6_b.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59887,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0683a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635813","contributors":{"authors":[{"text":"Tysdal, Russell G.","contributorId":1700,"corporation":false,"usgs":true,"family":"Tysdal","given":"Russell","email":"","middleInitial":"G.","affiliations":[],"preferred":true,"id":206663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ludington, S. D.","contributorId":80682,"corporation":false,"usgs":true,"family":"Ludington","given":"S.","middleInitial":"D.","affiliations":[],"preferred":false,"id":206664,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCafferty, Anne E. 0000-0001-5574-9201 anne@usgs.gov","orcid":"https://orcid.org/0000-0001-5574-9201","contributorId":1120,"corporation":false,"usgs":true,"family":"McCafferty","given":"Anne","email":"anne@usgs.gov","middleInitial":"E.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":206662,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31665,"text":"ofr96700 - 1996 - Geological map of the Catasauqua Quadrangle, Northampton and Lehigh counties, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:09:00","indexId":"ofr96700","displayToPublicDate":"1998-01-10T00:00:00","publicationYear":"1996","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":"96-700","title":"Geological map of the Catasauqua Quadrangle, Northampton and Lehigh counties, Pennsylvania","language":"ENGLISH","doi":"10.3133/ofr96700","usgsCitation":"Drake, A.A., 1996, Geological map of the Catasauqua Quadrangle, Northampton and Lehigh counties, Pennsylvania: U.S. Geological Survey Open-File Report 96-700, 20 p., 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet). , https://doi.org/10.3133/ofr96700.","productDescription":"20 p., 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet). ","costCenters":[],"links":[{"id":159894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0700/report-thumb.jpg"},{"id":59888,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0700/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59889,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0700/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6874ff","contributors":{"authors":[{"text":"Drake, Avery A. Jr.","contributorId":81090,"corporation":false,"usgs":true,"family":"Drake","given":"Avery","suffix":"Jr.","middleInitial":"A.","affiliations":[],"preferred":false,"id":206665,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31666,"text":"ofr96714 - 1996 - Topographic map of the Tithonium Chasma region of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:09:00","indexId":"ofr96714","displayToPublicDate":"1998-01-10T00:00:00","publicationYear":"1996","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":"96-714","title":"Topographic map of the Tithonium Chasma region of Mars","language":"ENGLISH","doi":"10.3133/ofr96714","usgsCitation":"Wu, S., 1996, Topographic map of the Tithonium Chasma region of Mars: U.S. Geological Survey Open-File Report 96-714, One over-size sheet, scale 1:502,000 (1 inch = about 8 miles). , https://doi.org/10.3133/ofr96714.","productDescription":"One over-size sheet, scale 1:502,000 (1 inch = about 8 miles). ","costCenters":[],"links":[{"id":159895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":19518,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0714/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"502000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629beb","contributors":{"authors":[{"text":"Wu, S.-S.","contributorId":51714,"corporation":false,"usgs":true,"family":"Wu","given":"S.-S.","email":"","affiliations":[],"preferred":false,"id":206666,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5046,"text":"fs03296 - 1996 - U.S. Geological Survey programs in New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"fs03296","displayToPublicDate":"1998-01-10T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"032-96","title":"U.S. Geological Survey programs in New York","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/fs03296","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1996, U.S. Geological Survey programs in New York: U.S. Geological Survey Fact Sheet 032-96, [4] p. : ill. (some col.), maps ; 28 cm. ill. (some col.), maps ;, https://doi.org/10.3133/fs03296.","productDescription":"[4] p. : ill. (some col.), maps ; 28 cm. ill. (some col.), maps ;","costCenters":[],"links":[{"id":118443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_032_96.jpg"},{"id":361,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-032-96","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6122b1","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":528420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":49852,"text":"ofr96642 - 1996 - Level II scour analysis for Bridge 25 (BRNATH00290034) on Town Highway 29, crossing Locust Creek, Barnard, Vermont","interactions":[],"lastModifiedDate":"2013-12-05T11:53:37","indexId":"ofr96642","displayToPublicDate":"1997-12-05T07:00:00","publicationYear":"1996","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":"96-642","title":"Level II scour analysis for Bridge 25 (BRNATH00290034) on Town Highway 29, crossing Locust Creek, Barnard, Vermont","docAbstract":"This report provides the results of a detailed Level II analysis of scour potential at structure \nBRNATH00290034 on Town Highway 29 crossing Locust Creek, Barnard, Vermont \n(figures 1-8). A Level II study is a basic engineering analysis of the site, including a \nquantitative analysis of stream stability and scour (U.S. Department of Transportation, \n1993). Results of a Level I scour investigation also are included in Appendix E of this \nreport. A Level I investigation provides a qualitative geomorphic characterization of the \nstudy site. Information on the bridge, gleaned from Vermont Agency of Transportation \n(VTAOT) files, was compiled prior to conducting Level I and Level II analyses and is \nfound in Appendix D.\nThe site is in the Green Mountain section of the New England physiographic province in \ncentral Vermont. The 11.5-mi2\n drainage area is in a predominantly rural and forested basin. \nIn the vicinity of the study site, the surface cover is forest, except for pasture on the \ndownstream right overbank.
\nIn the study area, Locust Creek has an incised, generally straight channel with a slope of \napproximately 0.03 ft/ft, an average channel top width of 64 ft and an average channel \ndepth of 7 ft. The predominant channel bed materials are gravel and cobble with a median \ngrain size (D50) of 89.3 mm (0.293 ft). The geomorphic assessment at the time of the Level \nI and Level II site visit on October 13, 1994 and December 16, 1994, indicated that the \nreach was stable.
\nThe Town Highway 29 crossing of Locust Creek is a 37-ft-long, one-lane bridge consisting \nof one 32-foot concrete span (Vermont Agency of Transportation, written communication, \nAugust 23, 1994). The bridge is supported by vertical, concrete abutments with wingwalls. \nThe channel is skewed approximately 25 degrees to the opening while the opening-skew-to-roadway is 25 degrees. \nThere was no observable scour protection measure at the site. Additional details describing \nconditions at the site are included in the Level II Summary and Appendices D and E.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96642","collaboration":"Prepared in cooperation with Vermont Agency of Transportation and Federal Highway Administration","usgsCitation":"Ivanoff, M.A., and Weber, M.A., 1996, Level II scour analysis for Bridge 25 (BRNATH00290034) on Town Highway 29, crossing Locust Creek, Barnard, Vermont: U.S. Geological Survey Open-File Report 96-642, iv, 50 p., https://doi.org/10.3133/ofr96642.","productDescription":"iv, 50 p.","numberOfPages":"54","costCenters":[],"links":[{"id":162731,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr96642.PNG"},{"id":279273,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0642/report.pdf"}],"country":"United States","state":"Vermont","city":"Barnard","otherGeospatial":"Locust Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.671,43.6925 ], [ -72.671,43.7109 ], [ -72.6462,43.7109 ], [ -72.6462,43.6925 ], [ -72.671,43.6925 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a807b","contributors":{"authors":[{"text":"Ivanoff, Michael A.","contributorId":27105,"corporation":false,"usgs":true,"family":"Ivanoff","given":"Michael","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":240365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weber, Matthew A.","contributorId":41483,"corporation":false,"usgs":true,"family":"Weber","given":"Matthew","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":240366,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31997,"text":"ofr96255 - 1996 - Wetland and peat resource map of the Sandown 7.5-minute quadrangle, New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:09:09","indexId":"ofr96255","displayToPublicDate":"1997-12-01T00:00:00","publicationYear":"1996","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":"96-255","title":"Wetland and peat resource map of the Sandown 7.5-minute quadrangle, New Hampshire","language":"ENGLISH","doi":"10.3133/ofr96255","usgsCitation":"Jackson, J., and Cameron, C., 1996, Wetland and peat resource map of the Sandown 7.5-minute quadrangle, New Hampshire: U.S. Geological Survey Open-File Report 96-255, One over-size sheet, scale 1:24,000 (1 inch = 2,000 feet). , https://doi.org/10.3133/ofr96255.","productDescription":"One over-size sheet, scale 1:24,000 (1 inch = 2,000 feet). ","costCenters":[],"links":[{"id":160680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":60153,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0255/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e49c5","contributors":{"authors":[{"text":"Jackson, J.C.","contributorId":104503,"corporation":false,"usgs":true,"family":"Jackson","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":207420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cameron, C. C.","contributorId":94299,"corporation":false,"usgs":true,"family":"Cameron","given":"C. C.","affiliations":[],"preferred":false,"id":207419,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23535,"text":"ofr96678 - 1996 - Alaska resource data file: Demarcation Point quadrangle","interactions":[],"lastModifiedDate":"2025-03-27T17:19:23.004445","indexId":"ofr96678","displayToPublicDate":"1997-12-01T00:00:00","publicationYear":"1996","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":"96-678","title":"Alaska resource data file: Demarcation Point quadrangle","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96678","issn":"0094-9140","usgsCitation":"Kelley, J., 1996, Alaska resource data file: Demarcation Point quadrangle: U.S. Geological Survey Open-File Report 96-678, 14 p., https://doi.org/10.3133/ofr96678.","productDescription":"14 p.","costCenters":[],"links":[{"id":1612,"rank":3,"type":{"id":18,"text":"Project Site"},"url":"https://doi.org/10.5066/P96MMRFD","linkFileType":{"id":5,"text":"html"}},{"id":156081,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0678/report-thumb.jpg"},{"id":52823,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0678/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389039,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37188.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Demarcation Point quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -144.0,\n 69.0\n ],\n [\n -141.0,\n 69.0\n ],\n [\n -141.0,\n 70.0\n ],\n [\n -144.0,\n 70.0\n ],\n [\n -144.0,\n 69.0\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab2e4b07f02db66ee3d","contributors":{"authors":[{"text":"Kelley, John S.","contributorId":23560,"corporation":false,"usgs":true,"family":"Kelley","given":"John S.","affiliations":[],"preferred":false,"id":190278,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24386,"text":"ofr9694 - 1996 - Computer program for aggregation of probabilistic assessments of mineral resources","interactions":[],"lastModifiedDate":"2013-09-17T14:21:47","indexId":"ofr9694","displayToPublicDate":"1997-12-01T00:00:00","publicationYear":"1996","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":"96-94","title":"Computer program for aggregation of probabilistic assessments of mineral resources","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9694","issn":"0094-9140","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Root, D.H., Scott, W., and Selner, G., 1996, Computer program for aggregation of probabilistic assessments of mineral resources (QuickBasic 4.50.): U.S. Geological Survey Open-File Report 96-94, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr9694.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":157157,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":277644,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1996/0094/application.zip"}],"edition":"QuickBasic 4.50.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a78b6","contributors":{"authors":[{"text":"Root, D. H.","contributorId":74019,"corporation":false,"usgs":true,"family":"Root","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":191825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, W.A. Jr.","contributorId":60267,"corporation":false,"usgs":true,"family":"Scott","given":"W.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":191824,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Selner, G.I.","contributorId":13229,"corporation":false,"usgs":true,"family":"Selner","given":"G.I.","affiliations":[],"preferred":false,"id":191823,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31696,"text":"ofr96623 - 1996 - Potentiometric Surface of the Lower Patapsco Aquifer in Southern Maryland, September 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"ofr96623","displayToPublicDate":"1997-12-01T00:00:00","publicationYear":"1996","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":"96-623","title":"Potentiometric Surface of the Lower Patapsco Aquifer in Southern Maryland, September 1995","docAbstract":"A map showing the potentiometric surface of the lower Patapsco aquifer in the Patapsco Formation of Cretaceous age in southern Maryland during September 1995 was prepared from water-level measurements in 69 wells. The potentiometric surface was 87 feet above sea level near the northwestern boundary and outcrop area of the aquifer in topographically high areas of Anne Arundel County. From this high area, the potentiometric surface declined to the south and southeast toward large well fields at Crofton, Severndale, Arnold, Annapolis, Waldorf, LaPlata, Indian Head, and Morgantown. The ground-water levels reached 18 feet below sea level at Crofton, 62 feet below sea level at Severndale, 26 feet below sea level at Arnold, more than 20 feet below sea level near Annapolis, 160 feet below sea level in the Waldorf area, nearly 100 feet below sea level at LaPlata, more than 110 feet below sea level at Indian Head, and 75 feet below sea level at the Morgantown powerplant.","language":"ENGLISH","doi":"10.3133/ofr96623","usgsCitation":"Curtin, S.E., Andreasen, D., and Mack, F., 1996, Potentiometric Surface of the Lower Patapsco Aquifer in Southern Maryland, September 1995: U.S. Geological Survey Open-File Report 96-623, 1 map : photocopy ; 20 x 17 cm., on sheet 28 x 22 cm., https://doi.org/10.3133/ofr96623.","productDescription":"1 map : photocopy ; 20 x 17 cm., on sheet 28 x 22 cm.","costCenters":[],"links":[{"id":160002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0623/report-thumb.jpg"},{"id":59928,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0623/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aee46","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":206766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":206767,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mack, Frederick K.","contributorId":95858,"corporation":false,"usgs":true,"family":"Mack","given":"Frederick K.","affiliations":[],"preferred":false,"id":206768,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31697,"text":"ofr96624 - 1996 - The difference between the potentiometric surfaces of the Aquia aquifer of September 1982 and September 1995 in southern Maryland","interactions":[],"lastModifiedDate":"2022-07-22T19:52:01.659969","indexId":"ofr96624","displayToPublicDate":"1997-12-01T00:00:00","publicationYear":"1996","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":"96-624","title":"The difference between the potentiometric surfaces of the Aquia aquifer of September 1982 and September 1995 in southern Maryland","docAbstract":"A map showing the net change in the potentiometric surface of the Aquia aquifer in the Aquia Formation of Paleocene age in southern Maryland was based on water levels measured in 66 wells from September 1982 to September 1995 and shows that the decline of the potentiometric surface during the 13-year period was 20 to 30 feet in most of the area. The decline was more than 50 feet in the Lexington Park area and more than 60 feet at Solomons Island.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96624","usgsCitation":"Curtin, S.E., Andreasen, D., and Mack, F., 1996, The difference between the potentiometric surfaces of the Aquia aquifer of September 1982 and September 1995 in southern Maryland: U.S. Geological Survey Open-File Report 96-624, 1 Plate: 8.56 × 11.00 inches, https://doi.org/10.3133/ofr96624.","productDescription":"1 Plate: 8.56 × 11.00 inches","costCenters":[],"links":[{"id":404387,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18659.htm","linkFileType":{"id":5,"text":"html"}},{"id":59929,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0624/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0624/report-thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Aquia aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.336,\n 38\n ],\n [\n -76,\n 38\n ],\n [\n -76,\n 39.25\n ],\n [\n -77.336,\n 39.25\n ],\n [\n -77.336,\n 38\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668563","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":206769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":206770,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mack, Frederick K.","contributorId":95858,"corporation":false,"usgs":true,"family":"Mack","given":"Frederick K.","affiliations":[],"preferred":false,"id":206771,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31998,"text":"ofr96272 - 1996 - Offshore gas hydrate sample database with an overview and preliminary analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"ofr96272","displayToPublicDate":"1997-12-01T00:00:00","publicationYear":"1996","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":"96-272","title":"Offshore gas hydrate sample database with an overview and preliminary analysis","docAbstract":"Synopsis -- A database of offshore gas hydrate samples was constructed from published observations and measurements. More than 90 samples from 15 distinct regions are represented in 13 data categories. This database has permitted preliminary description of gas hydrate (chiefly methane hydrate) tendencies and associations with respect to their geological environment.\r\n\r\nGas hydrates have been recovered from offshore sediment worldwide and from total depths (water depth plus subseabed depth) ranging from 500 m to nearly 6,000 m. Samples have come from subbottom depths ranging from 0 to 400 m. Various physiographic provinces are represented in the data set including second order landforms such as continental margins and deep-sea trenches, and third order forms such as submarine canyons, continental slopes, continental margin ridges and intraslope basins. There is a clear association between fault zones and other manifestations of local, tectonic-related processes, and hydrate-bearing sediment.\r\n\r\nSamples of gas hydrate frequently consist of individual grains or particles. These types of hydrates are often further described as inclusions or disseminated in the sediment. Moreover, hydrates occur as a cement, as nodules, or as layers (mostly laminae) or in veins. The preponderance of hydrates that could be characterized as 2- dimensional (planar) were associated with fine sediment, either as intercalated layers or in fractures. Hydrate cements were commonly associated with coarser sediment.\r\n\r\nHydrates have been found in association with grain sizes ranging from clay through gravel. More hydrates are associated with the more abundant finer-grained sediment than with coarser sediment, and many were discovered in the presence of both fine (silt and clay) and coarse sediment.\r\n\r\nThe thickness of hydrate zones (i. e., sections of hydrate-bearing sediment) varies from a few centimeters to as much as 30 m. In contrast, the thickness of layers of pure hydrate or the dimensions of individual hydrate grains were most often characterized in terms of millimeters or centimeters, although a pure hydrate layer discovered in the Middle America Trench off Guatemala was as much as 3-4-m-thick. The data suggest that grains, or thin veins or laminae of pure gas hydrate may be ubiquitous in many hydrate zones but that typically they may only comprise a minor component of the thicker zones.\r\n\r\nIn more than 80 percent of the hydrate samples the methane was of biogenic origin. The methane in the remainder was either classified as (or may be at least part) thermogenic. Each site where thermogenic gas was identified is characterized by faults or other manifestions of a dynamic geological environment (e.g., diapirs, mud volcanoes, gas seeps).\r\n\r\nEvery sample in the database came from within the zone of theoretical methane hydrate stability, as determined on the basis of assumed regional pressure and temperature gradients. Most show that they were situated --- expressed in terms of depth --- well above the phase boundary and about 70% of the samples were located more than 100 m above the assumed regional position of that boundary. The calculated subseabed positions of the phase boundaries and the BSRs (bottom simulating reflector) are essentially identical. This may be taken as general corroboration of the regional phase boundary calculations and the concept of the BSR.\r\n\r\nThree provocative aspects of marine gas hydrates have been disclosed by the database: \r\n\r\ngas hydrates are frequently situated at much shallower subseabed depths than the assumed contemporary position of the regional phase boundary \r\n\r\nhydrates are often found in areas typified by faults or other indicators of a dynamic geological environment \r\n\r\nzones of gas hydrate-bearing sediment tend to be tens of centimeters to tens of meters thick but the hydrate within the thicker zones tends to be only a minor constituent. \r\n\r\nWhether existing as dispersed particles, cements, or pure layers or vein","language":"ENGLISH","doi":"10.3133/ofr96272","usgsCitation":"Booth, J.S., Rowe, M.M., and Fisher, K.M., 1996, Offshore gas hydrate sample database with an overview and preliminary analysis: U.S. Geological Survey Open-File Report 96-272, 17 p., 1 over-size sheet :col. ill.;28 cm., https://doi.org/10.3133/ofr96272.","productDescription":"17 p., 1 over-size sheet :col. ill.;28 cm.","costCenters":[],"links":[{"id":160681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3301,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1996/of96-272/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d6e","contributors":{"authors":[{"text":"Booth, James S.","contributorId":93477,"corporation":false,"usgs":true,"family":"Booth","given":"James","email":"","middleInitial":"S.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":207423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowe, Mary M.","contributorId":11259,"corporation":false,"usgs":true,"family":"Rowe","given":"Mary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":207421,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fisher, Kathleen M.","contributorId":43397,"corporation":false,"usgs":true,"family":"Fisher","given":"Kathleen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":207422,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31678,"text":"ofr96719 - 1996 - Preliminary bedrock geologic map of the Vermont part of the 7.5 x 15 minute Mount Ascutney and Springfield quadrangles, Windsor County, Vermont","interactions":[],"lastModifiedDate":"2022-03-28T21:13:51.191526","indexId":"ofr96719","displayToPublicDate":"1997-12-01T00:00:00","publicationYear":"1996","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":"96-719","title":"Preliminary bedrock geologic map of the Vermont part of the 7.5 x 15 minute Mount Ascutney and Springfield quadrangles, Windsor County, Vermont","docAbstract":"Bedrock in the Vermont part of the Mount Ascutney and Springfield quadrangles consists largely of, from west to east, Middle Proterozoic gneisses in the core of the Chester Dome, pre-Silurian metasedimentary, metavolcanic, and meta-igneous rocks as a cover sequence immediately above the dome, Silurian and Devonian metasedimentary and metavolcanic rocks of the Connecticut Valley sequence, and Ordovician to Silurian and Devonian metasedimentary rocks informally referred to as the New Hampshire sequence. In addition, the rocks are intruded by granitic dikes of the Devonian New Hampshire Plutonic Suite and, at Mount Ascutney, the Cretaceous White Mountain Plutonic - Volcanic Suite. The primary purpose of this report is to present preliminary results on the stratigraphic and structural relationships in the Connecticut Valley and New Hampshire sequence rocks.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96719","usgsCitation":"Walsh, G., Armstrong, T.R., and Ratcliffe, N.M., 1996, Preliminary bedrock geologic map of the Vermont part of the 7.5 x 15 minute Mount Ascutney and Springfield quadrangles, Windsor County, Vermont: U.S. Geological Survey Open-File Report 96-719, 36 p., https://doi.org/10.3133/ofr96719.","productDescription":"36 p.","costCenters":[],"links":[{"id":121672,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_96_719.jpg"},{"id":13689,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1996/719/","linkFileType":{"id":5,"text":"html"}},{"id":392419,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18688.htm"}],"scale":"24000","country":"United States","state":"Vermont","county":"Windsor County","otherGeospatial":"7.5 x 15 minute Mount Ascutney and Springfield quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.5,\n 43.375\n ],\n [\n -72.375,\n 43.375\n ],\n [\n -72.375,\n 43.5\n ],\n [\n -72.5,\n 43.5\n ],\n [\n -72.5,\n 43.375\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c938","contributors":{"authors":[{"text":"Walsh, G. J. 0000-0003-4264-8836","orcid":"https://orcid.org/0000-0003-4264-8836","contributorId":47409,"corporation":false,"usgs":true,"family":"Walsh","given":"G. J.","affiliations":[],"preferred":false,"id":206685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, T. R.","contributorId":91528,"corporation":false,"usgs":true,"family":"Armstrong","given":"T.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":206687,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ratcliffe, N. M.","contributorId":80691,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"N.","middleInitial":"M.","affiliations":[],"preferred":false,"id":206686,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31698,"text":"ofr96625 - 1996 - The difference between the potentiometric surfaces of the Magothy Aquifer of September 1975 and September 1995 in southern Maryland","interactions":[],"lastModifiedDate":"2022-08-03T19:19:36.134667","indexId":"ofr96625","displayToPublicDate":"1997-12-01T00:00:00","publicationYear":"1996","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":"96-625","title":"The difference between the potentiometric surfaces of the Magothy Aquifer of September 1975 and September 1995 in southern Maryland","docAbstract":"A map showing the net change in the poentiometric surface of the Magothy aquifer in the Magothy Formation of Cretaceous age in southern Maryland from September 1975 to September 1995 was based on water-level measurements in 67 wells. The map shows that the decline of the potentiometric surface during the 20-year period ranged from 2 to 21 feet in the northernmost part of the study area. The decline was greater than 40 feet in parts of southern Prince Georges County, 75 feet at Waldorf, and 28 feet at the Chalk Point powerplant.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96625","usgsCitation":"Curtin, S.E., Andreasen, D., and Mack, F., 1996, The difference between the potentiometric surfaces of the Magothy Aquifer of September 1975 and September 1995 in southern Maryland: U.S. Geological Survey Open-File Report 96-625, 1 p., https://doi.org/10.3133/ofr96625.","productDescription":"1 p.","costCenters":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"links":[{"id":59930,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0625/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0625/report-thumb.jpg"},{"id":404759,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18660.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Maryland","otherGeospatial":"Magothy Aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.336,\n 38\n ],\n [\n -76,\n 38\n ],\n [\n -76,\n 39.25\n ],\n [\n -77.336,\n 39.25\n ],\n [\n -77.336,\n 38\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668556","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":206772,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":206773,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mack, Frederick K.","contributorId":95858,"corporation":false,"usgs":true,"family":"Mack","given":"Frederick K.","affiliations":[],"preferred":false,"id":206774,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31694,"text":"ofr96621 - 1996 - Potentiometric Surface of the Magothy Aquifer in Southern Maryland, September 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"ofr96621","displayToPublicDate":"1997-12-01T00:00:00","publicationYear":"1996","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":"96-621","title":"Potentiometric Surface of the Magothy Aquifer in Southern Maryland, September 1995","docAbstract":"A map showing the potentiometric surface of the Magothy aquifer in the Magothy Formation of Cretaceous age in southern Maryland during September 1995 was prepared from water-level measurements in 92 wells. The potentiometric surface was highest near the northwestern boundaryand outcrop area of the aquifer in topographically high areas of Anne Arundel and Prince Georges Counties. Regionally, the potentiometric surface sloped gently downward towards the southeast and the local gradients were directed toward the centers of three cones of depression that have developed in response to pumping. These cones were centeredaround well fields in the Annapolis, Waldorf, and Chalk Point areas. Ground-water levels were as low as 63 feet below sea level in the Waldorf area, more than 50 feet below sea level at Chalk Point, and almost 20 feet below sea level near Annapolis.","language":"ENGLISH","doi":"10.3133/ofr96621","usgsCitation":"Curtin, S.E., Andreasen, D., and Mack, F., 1996, Potentiometric Surface of the Magothy Aquifer in Southern Maryland, September 1995: U.S. Geological Survey Open-File Report 96-621, 1 map : photocopy ; 20 x 17 cm., on sheet 28 x 22 cm., https://doi.org/10.3133/ofr96621.","productDescription":"1 map : photocopy ; 20 x 17 cm., on sheet 28 x 22 cm.","costCenters":[],"links":[{"id":159915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0621/report-thumb.jpg"},{"id":59926,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0621/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e489","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":206760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":206761,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mack, Frederick K.","contributorId":95858,"corporation":false,"usgs":true,"family":"Mack","given":"Frederick K.","affiliations":[],"preferred":false,"id":206762,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31695,"text":"ofr96622 - 1996 - Potentiometric Surface of the Upper Patapsco Aquifer in Southern Maryland, September 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"ofr96622","displayToPublicDate":"1997-12-01T00:00:00","publicationYear":"1996","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":"96-622","title":"Potentiometric Surface of the Upper Patapsco Aquifer in Southern Maryland, September 1995","docAbstract":"A map showing the potentiometric surface of the upper Patapsco aquifer in the Patapsco Formation of Cretaceous age in southern Maryland during September 1995 was prepared from water-level measurements in 42 wells. The potentiometric surface was nearly 120 feet above sea level near the northwestern boundary and outcrop area of the aquifer in topographically high areas of Anne Arundel County, and 55 feet above sea level in a similar setting in Prince Georges County. From these high areas, the potentiometic surface declined to the south and southeast toward large well fields in the Annapolis and Waldorf areas and at the Chalk Point powerplant. Ground-water levels reached nearly 30 feet below sea level in the Annapolis area, 113 feet below sea level southwest of Waldorf, and more than 30 feet below sea level at the Chalk Point powerplant.","language":"ENGLISH","doi":"10.3133/ofr96622","usgsCitation":"Curtin, S.E., Andreasen, D., and Mack, F., 1996, Potentiometric Surface of the Upper Patapsco Aquifer in Southern Maryland, September 1995: U.S. Geological Survey Open-File Report 96-622, 1 map : photocopy ; 20 x 17 cm., on sheet 28 x 22 cm., https://doi.org/10.3133/ofr96622.","productDescription":"1 map : photocopy ; 20 x 17 cm., on sheet 28 x 22 cm.","costCenters":[],"links":[{"id":159929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0622/report-thumb.jpg"},{"id":59927,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0622/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683200","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":206763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":206764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mack, Frederick K.","contributorId":95858,"corporation":false,"usgs":true,"family":"Mack","given":"Frederick K.","affiliations":[],"preferred":false,"id":206765,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1664,"text":"wsp2381F - 1996 - Analysis of Nonpoint-Source Ground-Water Contamination in Relation to Land Use: Assessment of Nonpoint-Source Contamination in Central Florida","interactions":[],"lastModifiedDate":"2012-09-12T17:16:23","indexId":"wsp2381F","displayToPublicDate":"1997-11-01T01:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2381","chapter":"F","title":"Analysis of Nonpoint-Source Ground-Water Contamination in Relation to Land Use: Assessment of Nonpoint-Source Contamination in Central Florida","docAbstract":"In central Florida, activities that might affect the quality of ground water include disposal of stormwater through drainage wells, citrus cultivation, and mining and processing of phosphate ore. Possible effects of these and other land-use activities include high concentrations of nitrogen compounds and the pesticide bromacil in the citrus area, and high concentrations of most of the major-dissolved constituents and some organic compounds in the mining area.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wsp2381F","usgsCitation":"German, E.R., 1996, Analysis of Nonpoint-Source Ground-Water Contamination in Relation to Land Use: Assessment of Nonpoint-Source Contamination in Central Florida: U.S. Geological Survey Water Supply Paper 2381, 2 p. online; vi, 60 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2381F.","productDescription":"2 p. online; vi, 60 p. :ill., maps ;28 cm.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":138536,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":10438,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://fl.water.usgs.gov/publications/Abstracts/wsp2381_german.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680bd8","contributors":{"authors":[{"text":"German, Edward R.","contributorId":85567,"corporation":false,"usgs":true,"family":"German","given":"Edward","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21584,"text":"ofr96505C - 1996 - Analytical results and sample locality maps of stream-sediment, panned concentrate, stream-water, and soil samples from the Stuyahok study area, part of Holy Cross A-4 and A-5 quadrangles, Alaska","interactions":[],"lastModifiedDate":"2018-07-07T17:43:40","indexId":"ofr96505C","displayToPublicDate":"1997-11-01T00:00:00","publicationYear":"1996","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":"96-505","chapter":"C","title":"Analytical results and sample locality maps of stream-sediment, panned concentrate, stream-water, and soil samples from the Stuyahok study area, part of Holy Cross A-4 and A-5 quadrangles, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr96505C","usgsCitation":"Bailey, E., Keith, W.J., Bickerstaff, D., Dempsey, D., and Miller, M.L., 1996, Analytical results and sample locality maps of stream-sediment, panned concentrate, stream-water, and soil samples from the Stuyahok study area, part of Holy Cross A-4 and A-5 quadrangles, Alaska: U.S. Geological Survey Open-File Report 96-505, 44 p. :maps ;28 cm. +1 computer disk (3 1/2 in.), https://doi.org/10.3133/ofr96505C.","productDescription":"44 p. :maps ;28 cm. +1 computer disk (3 1/2 in.)","costCenters":[],"links":[{"id":154048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0505c/report-thumb.jpg"},{"id":51167,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0505c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acae4b07f02db67cd0d","contributors":{"authors":[{"text":"Bailey, E. A.","contributorId":100399,"corporation":false,"usgs":true,"family":"Bailey","given":"E. A.","affiliations":[],"preferred":false,"id":184768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keith, W. J.","contributorId":41827,"corporation":false,"usgs":true,"family":"Keith","given":"W.","middleInitial":"J.","affiliations":[],"preferred":false,"id":184764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bickerstaff, D P.","contributorId":69181,"corporation":false,"usgs":true,"family":"Bickerstaff","given":"D P.","affiliations":[],"preferred":false,"id":184766,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dempsey, David","contributorId":65106,"corporation":false,"usgs":true,"family":"Dempsey","given":"David","affiliations":[],"preferred":false,"id":184765,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Miller, Marti L. 0000-0003-0285-4942 mlmiller@usgs.gov","orcid":"https://orcid.org/0000-0003-0285-4942","contributorId":561,"corporation":false,"usgs":true,"family":"Miller","given":"Marti","email":"mlmiller@usgs.gov","middleInitial":"L.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":184767,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":38089,"text":"ofr95615B - 1996 - Analytical results, sample locations, and other information for stream-sediment, soil, heavy-mineral-concentrate, and rock samples used in mineral resource studies of Coronado National Forest and adjacent areas, southeastern Arizona and southwestern New Mexico","interactions":[],"lastModifiedDate":"2025-02-28T17:21:00.095973","indexId":"ofr95615B","displayToPublicDate":"1997-11-01T00:00:00","publicationYear":"1996","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":"95-615","chapter":"B","title":"Analytical results, sample locations, and other information for stream-sediment, soil, heavy-mineral-concentrate, and rock samples used in mineral resource studies of Coronado National Forest and adjacent areas, southeastern Arizona and southwestern New Mexico","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95615B","usgsCitation":"Nowlan, G., and Chaffee, M., 1996, Analytical results, sample locations, and other information for stream-sediment, soil, heavy-mineral-concentrate, and rock samples used in mineral resource studies of Coronado National Forest and adjacent areas, southeastern Arizona and southwestern New Mexico: U.S. Geological Survey Open-File Report 95-615, 1 CD-ROM, https://doi.org/10.3133/ofr95615B.","productDescription":"1 CD-ROM","costCenters":[],"links":[{"id":165099,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":482662,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/0615-b/ofr95615B.zip","text":"Disc","linkFileType":{"id":6,"text":"zip"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c3bb","contributors":{"authors":[{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":218837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chaffee, M.A.","contributorId":108049,"corporation":false,"usgs":true,"family":"Chaffee","given":"M.A.","affiliations":[],"preferred":false,"id":218838,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}