{"pageNumber":"3952","pageRowStart":"98775","pageSize":"25","recordCount":185134,"records":[{"id":26066,"text":"wri944039 - 1994 - Geologic history and hydrogeologic setting of the Edwards-Trinity aquifer system, west-central Texas","interactions":[],"lastModifiedDate":"2016-08-16T14:08:36","indexId":"wri944039","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-4039","title":"Geologic history and hydrogeologic setting of the Edwards-Trinity aquifer system, west-central Texas","docAbstract":"<p>The Edwards-Trinity aquifer system underlies about 42,000 square miles of west-central Texas. Nearly flat-lying, mostly Comanche (Lower Cretaceous) strata of the aquifer system thin northwestward atop massive pre-Cretaceous rocks that are comparatively impermeable and structurally complex. From predominately terrigenous clastic sediments in the east and fluvialdeltaic (terrestrial) deposits in the west, the rocks of early Trinitian age grade upward into supratidal evaporitic and dolomitic strata, intertidal limestone and dolostone, and shallow-marine, openshelf, and reefal strata of late Trinitian, Fredericksburgian, and Washitan age. A thick, downfaulted remnant of mostly open-marine strata of Eaglefordian through Navarroan age composes a small, southeastern part of the aquifer system.</p>\n<p>The Trinity Group was deposited atop a rolling peneplain of pre-Cretaceous rocks during three predominately transgressive cycles of sedimentation that encroached upon the Llano uplift. The Fredericksburg and Washita Groups were deposited above the Trinity Group mostly in the lee of the Stuart City reef trend, a shelf margin ridge that sheltered depositional environments in the study area. The Washita Group subsequently was covered with thick, mostly fine-grained Gulf strata.</p>\n<p>During late Oligocene through early Miocene time, large-scale normal faulting formed the Balcones fault zone, where the Cretaceous strata were downfaulted, intensively fractured, and differentially rotated within a series of northeasttrending fault blocks. In addition to fracturing the rocks in the fault zone and extending the depth of freshwater diagenesis, the faulting vertically displaced the terrain, which steepened hydraulic gradients and maintained relatively high flow velocities near the surface. A shallow regime of dynamic ground-water flow evolved that promoted dissolution and enhanced the transmissivity of the Edwards Group in the Balcones fault zone. Cementation, recrystallization, and mineral replacement caused by deeper, comparatively sluggish ground-water circulation combined to diminish the transmissivity of the underlying Trinity Group, as well as most Cretaceous strata in the Hill Country, Edwards-Plateau, and Trans-Pecos.</p>\n<p>The Trinity, Fredericksburg, and Washita strata compose a regional aquifer system of three aquifers, whose water-transmitting characteristics generally are continuous in the lateral direction, and two hydraulically tight confining units. The aquifers are the Edwards aquifer in the Balcones fault zone, the Trinity aquifer in the Balcones fault zone and Hill Country, and the Edwards-Trinity aquifer in the Edwards Plateau and Trans-Pecos. The Navarro-Del Rio confining unit overlies the subcrop of the Edwards aquifer, and the Hammett confining unit lies within the updip, basal part of the Trinity aquifer and a small southeastern fringe of the Edwards-Trinity aquifer. The confining units are mostly calcareous mudstone, siltstone, and shale of low-energy terrigenous and openshelf marine depositional environments. The aquifers mainly result from fractures, joint cavities, and porosity caused by the dissolution of evaporites and unstable carbonate constituents.&nbsp;</p>\n<p>Because the diagenetic effects of cementation, recrystallization, and mineral replacement diminish the hydraulic conductivity of most rocks composing the Trinity and Edwards-Trinity aquifers, transmissivity values average less than 10,000 feet squared per day over more than 90 percent of the study area. However, the effects of tectonic fractures and dissolution in the Balcones fault zone cause transmissivity values to average about 750,000 feet squared per day in the Edwards aquifer, which occupies less than 10 percent of the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri944039","usgsCitation":"Barker, R., Bush, P.W., and Baker, E., 1994, Geologic history and hydrogeologic setting of the Edwards-Trinity aquifer system, west-central Texas: U.S. Geological Survey Water-Resources Investigations Report 94-4039, iv, 51 p., https://doi.org/10.3133/wri944039.","productDescription":"iv, 51 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":122736,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4039/report-thumb.jpg"},{"id":54843,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Edwards-Trinity aquifer system","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c717","contributors":{"authors":[{"text":"Barker, R.A.","contributorId":28952,"corporation":false,"usgs":true,"family":"Barker","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":195741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bush, P. W.","contributorId":14826,"corporation":false,"usgs":true,"family":"Bush","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":195740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baker, E.T.","contributorId":11584,"corporation":false,"usgs":true,"family":"Baker","given":"E.T.","email":"","affiliations":[],"preferred":false,"id":195739,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":18222,"text":"ofr94303 - 1994 - Water levels in wells J-11 and J-12, 1989-91, Yucca Mountain area, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:19","indexId":"ofr94303","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-303","title":"Water levels in wells J-11 and J-12, 1989-91, Yucca Mountain area, Nevada","docAbstract":"Water levels have been measured in the Yucca Mountain area, Nevada, since 1981 in order to gain a better understanding of the gound-water flow system in the area. Water level in wells J-11 and J-12 have been periodically measured using calibrated reeled steel tapes since 1989, however, calculation of water-level altitude was not possible prior to 1993 due to missing reference elevations. These elevations were determined in 1993 by the U.S. Geological Survey. During 1989-91, water-level altitudes for well J-11 ranged from 732.09 to 732.40 meters and the mean water-level altitude was 732.19 meters. During 1989-91, water-level altitudes for well J-12 ranged from 727.84 to 728.03 meters, and the mean water-level altitude was 727.95 meters.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94303","usgsCitation":"Boucher, M.S., 1994, Water levels in wells J-11 and J-12, 1989-91, Yucca Mountain area, Nevada: U.S. Geological Survey Open-File Report 94-303, iii, 9 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94303.","productDescription":"iii, 9 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":150314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0303/report-thumb.jpg"},{"id":47584,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0303/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9d01","contributors":{"authors":[{"text":"Boucher, Michelle S.","contributorId":71192,"corporation":false,"usgs":true,"family":"Boucher","given":"Michelle","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":178736,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18436,"text":"ofr93663 - 1994 - Hydrogeology of the Silurian and Devonian carbonate-rock aquifer system in the Midwestern Basins and Arches Region of Indiana, Ohio, Michigan, and Illinois","interactions":[],"lastModifiedDate":"2022-10-06T20:25:31.025205","indexId":"ofr93663","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"93-663","title":"Hydrogeology of the Silurian and Devonian carbonate-rock aquifer system in the Midwestern Basins and Arches Region of Indiana, Ohio, Michigan, and Illinois","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr93663","usgsCitation":"Casey, G.D., 1994, Hydrogeology of the Silurian and Devonian carbonate-rock aquifer system in the Midwestern Basins and Arches Region of Indiana, Ohio, Michigan, and Illinois: U.S. Geological Survey Open-File Report 93-663, Report: iv, 14 p.; 2 Plates: 54.00 × 36.00 inches and 52.00 × 35.00 inches, https://doi.org/10.3133/ofr93663.","productDescription":"Report: iv, 14 p.; 2 Plates: 54.00 × 36.00 inches and 52.00 × 35.00 inches","costCenters":[],"links":[{"id":408058,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16524.htm","linkFileType":{"id":5,"text":"html"}},{"id":47787,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0663/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21522,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1993/0663/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21521,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1993/0663/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0663/report-thumb.jpg"}],"country":"United States","state":"Illinois, Indiana, Michigan, Ohio","otherGeospatial":"Midwestern Basin and Arches Region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89,\n              37\n            ],\n            [\n              -80,\n              37\n            ],\n            [\n              -80,\n              43\n            ],\n            [\n              -89,\n              43\n            ],\n            [\n              -89,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614d27","contributors":{"authors":[{"text":"Casey, George D.","contributorId":105689,"corporation":false,"usgs":true,"family":"Casey","given":"George","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":179116,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31747,"text":"ofr94346 - 1994 - Approximate changes in water levels in wells completed in the Chicot and Evangeline aquifers, 1977-94 and 1993-94, and measured compaction, 1973-93, in the Houston-Galveston region, Texas","interactions":[],"lastModifiedDate":"2022-09-06T19:19:50.514771","indexId":"ofr94346","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-346","title":"Approximate changes in water levels in wells completed in the Chicot and Evangeline aquifers, 1977-94 and 1993-94, and measured compaction, 1973-93, in the Houston-Galveston region, Texas","docAbstract":"<p>This report is one in a series of reports that depict water-level changes since 1977 and compaction of subsurface material since 1973. &nbsp;The report was prepared in cooperation with the City of Houston and the Harris-Galveston Coastal Subsidence District, and presents maps showing the approximate changes in water levels in wells completed in the Chicot and Evangeline aquifers, 1977-94 and 1993-94 (figs. 1-4), extensometer site locations (fig. 5), and measured compaction, 1973-93 (fig. 6), in the Houston-Galveston region. &nbsp;Water-level change maps were prepared previously by Kasmarek and others (1993). &nbsp;The Houston-galveston region includes Harris and Galveston Counties and adjacent parts of Brazoria, Fort Bend, Waller, Montgomery, Liberty, and Chambers Counties.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94346","usgsCitation":"Kasmarek, M.C., Coplin, L., and Santos, H.X., 1994, Approximate changes in water levels in wells completed in the Chicot and Evangeline aquifers, 1977-94 and 1993-94, and measured compaction, 1973-93, in the Houston-Galveston region, Texas: U.S. Geological Survey Open-File Report 94-346, 6 Plates: 23.00 x 18.00 inches, https://doi.org/10.3133/ofr94346.","productDescription":"6 Plates: 23.00 x 18.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":160395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr94346.PNG"},{"id":406259,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12504.htm","linkFileType":{"id":5,"text":"html"}},{"id":21594,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0346/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21593,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0346/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21592,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0346/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21595,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0346/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21591,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0346/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21590,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0346/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"Galveston, Houston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.7403564453125,\n              29.14496502116881\n            ],\n            [\n              -94.603271484375,\n              29.14496502116881\n            ],\n            [\n              -94.603271484375,\n              30.0381887651539\n            ],\n            [\n              -95.7403564453125,\n              30.0381887651539\n            ],\n            [\n              -95.7403564453125,\n              29.14496502116881\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679c1f","contributors":{"authors":[{"text":"Kasmarek, Mark C. 0000-0003-2808-2506 mckasmar@usgs.gov","orcid":"https://orcid.org/0000-0003-2808-2506","contributorId":1968,"corporation":false,"usgs":true,"family":"Kasmarek","given":"Mark","email":"mckasmar@usgs.gov","middleInitial":"C.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":206862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coplin, L.S.","contributorId":49366,"corporation":false,"usgs":true,"family":"Coplin","given":"L.S.","affiliations":[],"preferred":false,"id":206860,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Santos, Horacio X.","contributorId":97159,"corporation":false,"usgs":true,"family":"Santos","given":"Horacio","email":"","middleInitial":"X.","affiliations":[],"preferred":false,"id":206861,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31746,"text":"ofr94345 - 1994 - Approximate changes in water levels in wells completed in the Chicot and Evangeline aquifers, 1990-94 and 1993-94, in Fort Bend County and adjacent areas, Texas","interactions":[],"lastModifiedDate":"2016-08-25T11:55:19","indexId":"ofr94345","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-345","title":"Approximate changes in water levels in wells completed in the Chicot and Evangeline aquifers, 1990-94 and 1993-94, in Fort Bend County and adjacent areas, Texas","docAbstract":"<p>Measurements of water levels from wells completed in the Chicot and Evangeline aquifers were used to construct maps showing approximate changes of water levels in Fort Bend County and adjacent areas during 1990-94 and 1993-94.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94345","usgsCitation":"Coplin, L., and Santos, H.X., 1994, Approximate changes in water levels in wells completed in the Chicot and Evangeline aquifers, 1990-94 and 1993-94, in Fort Bend County and adjacent areas, Texas: U.S. Geological Survey Open-File Report 94-345, 4 over-size sheets , https://doi.org/10.3133/ofr94345.","productDescription":"4 over-size sheets ","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":160394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a1be","contributors":{"authors":[{"text":"Coplin, L.S.","contributorId":49366,"corporation":false,"usgs":true,"family":"Coplin","given":"L.S.","affiliations":[],"preferred":false,"id":206858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Santos, H. X.","contributorId":69611,"corporation":false,"usgs":true,"family":"Santos","given":"H.","email":"","middleInitial":"X.","affiliations":[],"preferred":false,"id":206859,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19578,"text":"ofr94520 - 1994 - Selected ground-water data, and results of aquifer tests for the Upper Floridan aquifer, Brunswick, Glynn County, Georgia, area","interactions":[],"lastModifiedDate":"2017-01-04T11:52:12","indexId":"ofr94520","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-520","title":"Selected ground-water data, and results of aquifer tests for the Upper Floridan aquifer, Brunswick, Glynn County, Georgia, area","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94520","usgsCitation":"Jones, L.E., and Maslia, M.L., 1994, Selected ground-water data, and results of aquifer tests for the Upper Floridan aquifer, Brunswick, Glynn County, Georgia, area: U.S. Geological Survey Open-File Report 94-520, v, 107 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94520.","productDescription":"v, 107 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":49050,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0520/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152013,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0520/report-thumb.jpg"}],"country":"United States","state":"Georgia","county":"Glynn County","city":"Brunswick","otherGeospatial":"Upper Floridan aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.0404052734375,\n              30.70878122625409\n            ],\n            [\n              -82.02941894531249,\n              31.739846973355032\n            ],\n            [\n              -81.1065673828125,\n              31.751525328078905\n            ],\n            [\n              -81.13471984863281,\n              30.70878122625409\n            ],\n            [\n              -82.0404052734375,\n              30.70878122625409\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa2a8","contributors":{"authors":[{"text":"Jones, L. Elliott 0000-0002-7394-2053 lejones@usgs.gov","orcid":"https://orcid.org/0000-0002-7394-2053","contributorId":44569,"corporation":false,"usgs":true,"family":"Jones","given":"L.","email":"lejones@usgs.gov","middleInitial":"Elliott","affiliations":[],"preferred":false,"id":181153,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maslia, Morris L.","contributorId":71952,"corporation":false,"usgs":true,"family":"Maslia","given":"Morris","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":181154,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18768,"text":"ofr94499 - 1994 - Flood magnitude and frequency of Pochack Creek at two sites, at Pennsauken Township, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr94499","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-499","title":"Flood magnitude and frequency of Pochack Creek at two sites, at Pennsauken Township, New Jersey","docAbstract":"Six methods were used to estimate the magnitude and frequency of floods at Pochack Creek at the down- stream end of the culvert on United States Route 130 and at a second site about 1,600 feet upstream at Pennsauken Township, New Jersey. Flood magnitude and frequency calculated by the six methods, as well as drainage-basin characteristics, are included in this report. The 100-year-flood estimates for the culvert site range from 280 cubic feet per second to 2,600 cubic feet per second. The 100-year-flood estimates for the upstream site range from 216 cubic feet per second to 1,800 cubic feet per second. Flood magni- tude and frequency estimates obtained by using the New Jersey Department of Environmental Protection Special Report 38 method fall within the range of values estimated by using the U.S. Geological Survey transfer method with data collected from three nearby crest-stage gages.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94499","usgsCitation":"Dunne, P., 1994, Flood magnitude and frequency of Pochack Creek at two sites, at Pennsauken Township, New Jersey: U.S. Geological Survey Open-File Report 94-499, iv, 11 leaves :map ;28 cm., https://doi.org/10.3133/ofr94499.","productDescription":"iv, 11 leaves :map ;28 cm.","costCenters":[],"links":[{"id":150937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0499/report-thumb.jpg"},{"id":48127,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0499/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef019","contributors":{"authors":[{"text":"Dunne, Paul","contributorId":86794,"corporation":false,"usgs":true,"family":"Dunne","given":"Paul","email":"","affiliations":[],"preferred":false,"id":179708,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18766,"text":"ofr94500 - 1994 - Flood magnitude and frequency of Chandlers Run at two sites, at Pennsauken Township, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr94500","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-500","title":"Flood magnitude and frequency of Chandlers Run at two sites, at Pennsauken Township, New Jersey","docAbstract":"Six methods were used to estimate the magnitude and frequency of floods at Chandlers Run at the culvert on New Jersey Route 612, and at a second site about 2,100 feet upstream, at New Jersey Route 70 at Pennsauken Township, New Jersey. Flood magnitude and frequency calculated by the six methods, as well as drainage-basin characteristics, are included in this report. The 100-year-flood estimates for the culvert site on Route 612 range from 268 cubic feet per second to 2,050 cubic feet per second. The 100-year-flood estimates for the upstream site at Route 70 range from 246 cubic feet per second to 2,320 cubic feet per second. Flood magnitude and frequency estimates obtained by using the New Jersey Department of Environmental Protection Special Report 38 method and other pre- viously published estimates fall within the range of values estimated by using the U.S. Geological Survey transfer method with data collected from three nearby crest-stage gages.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94500","usgsCitation":"Dunne, P., 1994, Flood magnitude and frequency of Chandlers Run at two sites, at Pennsauken Township, New Jersey: U.S. Geological Survey Open-File Report 94-500, iv, 12 leaves :map ;28 cm., https://doi.org/10.3133/ofr94500.","productDescription":"iv, 12 leaves :map ;28 cm.","costCenters":[],"links":[{"id":150935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0500/report-thumb.jpg"},{"id":48125,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0500/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef022","contributors":{"authors":[{"text":"Dunne, Paul","contributorId":86794,"corporation":false,"usgs":true,"family":"Dunne","given":"Paul","email":"","affiliations":[],"preferred":false,"id":179705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19585,"text":"ofr94706W - 1994 - Water-quality conditions and streamflow gain and loss of the South Prong of Spavinaw Creek basin, Benton County, Arkansas","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr94706W","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-706","chapter":"W","title":"Water-quality conditions and streamflow gain and loss of the South Prong of Spavinaw Creek basin, Benton County, Arkansas","docAbstract":"A study of the South Prong of Spavinaw Creek Basin conducted baween July 14 and July 23. 1993. described the surface- and ground-water quality of the basin and the streamflow gain and loss. Water samples were collected from 10 sites on the mainstem of the South Prong of Spavinaw Creek and from 4 sites on tributaries during periods of low to moderate streamflow (less than 11 cubic feet per second). Water samples were collected from 4 wells and 10 springs located in the basin.\r\n\r\nIn 14 surface-water samples, nitrite plus nitrate concentrations ranged from 0.75 to 4.2 milligrams per liter as nitrogen (mg/L). Orthophosphorus concentrations ranged from 0 03 to O. 15 mg/L as phosphorus. Fecal coliform bacteria counts ranged from 61 to 1,400 colonies per 100 milliliters (col/lOO mL), with a median of 120 col/100 mL. Fecal streptococci bacteria counts ranged from 70 to greater than 2,000 col/100 mL with a median of 185 col/lOO mL. Analysis for selected metals collected at one surface-water sites indicates that concentrations were usually below the reporting limit.\r\n\r\nDiel dissolved oxygen concentrations and temperatures were measured at an upstream and downstream site on the mainstem of the stream. At the upstream site, dissolved oxygen concentrations ranged from 7.2 to 83 mg/L and temperatures ranged from 15.5 to 17.0 C. Dissolved oxygen concentrations were higher and temperature values were lower at lhe upstream site, which is located close to two springs that produce all of the flow at that site.\r\n\r\nDissolved nitrite plus nitrate was present in all four wells sampled in the basin with concentrations ranging from 0.04 to 3.5 mg/L as nitrogen. Orthophosphorus was present in concentrations ranging from less than 0.01 to 0.07 mg/L as phosphorus. Volatile organic compound analyses in two wells indicate that toluene was present in both wells and chloroform was present in one well. All other volatile organic compounds were found to be below the reporting limits. Analysis for common constituents and selected metals indicated that fluoride concentrations in one well exceeded the U.S. Environmental Protection Agency's primary maximum contamination levels for drinking water.\r\n\r\nAnalyses of water samples collected from springs indicate that nitrite plus nitrate concen- trations ranged from 0.43 to 3.9 mg/L as nitrogen. Dissolved ammonia plus organic nitrogen concentrations ranged from less than 0.20 to 0.64 mg/L as nitrogen. Dissolved ammonia plus organic nitrogen concentrations ranged from less than 0.20 to 0.64 mg/L at nitrogen. Orthophosphorus concentrations ranged from 0.02 to 0.09 mg/L as phosphorus. Fecal coliform bacteria counts ranged from less than 3 to more than 2,000 col/100 mL, with a median of 370 col/100 mL. Fecal streptococci bacteria counts ranged from less than 4 to greater than 2,000 col/100 mL with a median of 435 col/100 mL.\r\n\r\nStreamflow in nine reaches of the mainstream increased an average of 20 percent. Six losing reaches were identified during the study, one located on the mainstem and the other five located on tributaries to the mainstem.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94706W","collaboration":"Prepared in cooperation with the Arkansas Department of Pollution Control and Ecology","usgsCitation":"Joseph, R.L., and Green, W.R., 1994, Water-quality conditions and streamflow gain and loss of the South Prong of Spavinaw Creek basin, Benton County, Arkansas: U.S. Geological Survey Open-File Report 94-706, iv, 16 p., https://doi.org/10.3133/ofr94706W.","productDescription":"iv, 16 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":151678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0706w/report-thumb.jpg"},{"id":49055,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0706w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.66666666666667,36.083333333333336 ], [ -94.66666666666667,36.583333333333336 ], [ -93.83333333333333,36.583333333333336 ], [ -93.83333333333333,36.083333333333336 ], [ -94.66666666666667,36.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e488ee4b07f02db51e5c6","contributors":{"authors":[{"text":"Joseph, Robert L. rljoseph@usgs.gov","contributorId":3482,"corporation":false,"usgs":true,"family":"Joseph","given":"Robert","email":"rljoseph@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":181165,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, W. Reed","contributorId":87886,"corporation":false,"usgs":true,"family":"Green","given":"W.","email":"","middleInitial":"Reed","affiliations":[],"preferred":false,"id":181166,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16977,"text":"ofr94714 - 1994 - Circum-North Pacific tectonostratigraphic terrane map","interactions":[],"lastModifiedDate":"2022-07-22T19:13:20.313093","indexId":"ofr94714","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-714","title":"Circum-North Pacific tectonostratigraphic terrane map","docAbstract":"<p>The companion tectonostratigraphic terrane and overlap assemblage of map the Circum-North Pacific presents a modern description of the major geologic and tectonic units of the region. The map illustrates both the onshore terranes and overlap volcanic assemblages of the region, and the major offshore geologic features. The map is the first collaborative compilation of the geology of the region at a scale of 1:5,000,000 by geologists of the Russian Far East, Japanese, Alaskan, Canadian, and U.S.A. Pacific Northwest. The map is designed to be a source of geologic information for all scientists interested in the region, and is designed to be used for several purposes, including regional tectonic analyses, mineral resource and metallogenic analyses (Nokleberg and others, 1993, 1994a), petroleum analyses, neotectonic analyses, and analyses of seismic hazards and volcanic hazards. This text contains an introduction, tectonic definitions, acknowledgments, descriptions of postaccretion stratified rock units, descriptions and stratigraphic columns for tectonostratigraphic terranes in onshore areas, and references for the companion map (Sheets 1 to 5).</p>\n<br>\n<p>This map is the result of extensive geologic mapping and \nassociated tectonic studies in the Russian Far East, Hokkaido \nIsland of Japan, Alaska, the Canadian Cordillera, and the \nU.S.A. Pacific Northwest in the last few decades. Geologic \nmapping suggests that most of this region can be interpreted as \na collage of fault-bounded tectonostratigraphic terranes that \nwere accreted onto continental margins around the Circum-\n. orth Pacific mainly during the Mesozoic and Cenozoic (Fujita \nand ewberry, 1983; 1987; Parfenov, 1984, 1991; Howell, \n1985; Watson and Fujita, 1985; Parfenov and Natal'in, 1984; \nJones and others. 1987; Monger and Berg, 1987, Fujita and \nCook. 1990; Zonenshain and others. 1990; Natal'in, 1991, \n1993; Moore and others, 1992; Silberling and others, 1992; \nNokleberg and others. 1992, 1993, 1994a; Parfenov and \nothers. 1993; Plaflcer and Berg, 1994; Tabor, 1994).</p>\n<br>\n<p>This map is the result of extensive geologic mapping and \nassociated tectonic studies in the Russian Far East, Hokkaido \nIsland of Japan, Alaska, the Canadian Cordillera, and the \nU.S.A. Pacific Northwest in the last few decades. Geologic \nmapping suggests that most of this region can be interpreted as \na collage of fault-bounded tectonostratigraphic terranes that \nwere accreted onto continental margins around the Circum-\n. orth Pacific mainly during the Mesozoic and Cenozoic (Fujita \nand ewberry, 1983; 1987; Parfenov, 1984, 1991; Howell, \n1985; Watson and Fujita, 1985; Parfenov and Natal'in, 1984; \nJones and others. 1987; Monger and Berg, 1987, Fujita and \nCook. 1990; Zonenshain and others. 1990; Natal'in, 1991, \n1993; Moore and others, 1992; Silberling and others, 1992; \nNokleberg and others. 1992, 1993, 1994a; Parfenov and \nothers. 1993; Plaflcer and Berg, 1994; Tabor, 1994).</p> \n<br>\n<p>On the companion map and in the descriptions bel?w· \nterranes are interpreted according to inferred tectonic \nenvironments. These environments are (I) cratonai; (2) \npassive continental margin; (3) metamorphosed continental \nmargin; (4) continental-margin arc; (5) island arc; (6) oceanic \ncrust, seamount, and ophiolite; (7) accretionary wedge and \nsubduction zone: (8) turbidite basin; and (9) metamorphic for \nterranes that are too highly-deformed and metamorphosed to \nde~ermine the original tectonic environment. For terranes with \ncomplex geologic histories, the chosen color indicates the \ntectonic environment most prevalent during this history of the \nterrane. The tectonic environments inf~rred for igneous rocks \nare both temporal and genetic. The temporal environments are \npreaccretion and postaccretion. The genetic environments are \nsubduction-related, rift-related, and collisional (anatectic)-\nrelated.</p> \n<br>\n<p>In addition to terranes, the map also depicts postaccretion \nunits that include: (I) Cenozoic and Mesozoic overlap \nassemblages of sedimentary and volcanic rocks that are \ndeposited across two or more terranes that formed generally\nafter accretion of most terranes in the region; (2) Cenozoic and \nMesozoic basinal deposits that occur within a terrane or on the \ncraton; (3) plutonic rocks. The postaccretion igneous units are \nidentified by age-lithologic abbreviations and by name. These \noverlap assemblages and basinal deposits formed mainly \nduring sedimentation and magmatism that occurred after \naccretion of terranes to each other or to a continental margin. \nOverlap assemblages provide minimum ages on the timing of \naccretion of terranes. Some Cenozoic and Mesozoic overlap \nassemblages and basinal deposits, as well as fragments of \nterranes, are extensively offset by movement along \npostaccretion faults. In addition, in onshore areas, the map \ndepicts major preaccretion plutonic rocks that are limited to \nindividual terranes. and in offshore areas. the map depicts \nmajor oceanic plates,-ocean floor magnetic lineations. oceanic \nspreading ridges, and seamounts.</p> \n<br>\n<p>The map consists of five sheets. Sheets I and 2 depict, at a \nscale of I :5.000.000. the tectonostratigraphic terranes. \npreaccretion plutonic rocks, and postaccretion Cenozoic and \nMesozoic overlap sedimentary, volcanic. and plutonic \nassemblages, and basinal deposits for the Circum- orth Pacific \nincluding the Russian Far East, northern Hokkaido Island of \nJapan, Alaska. the Canadian Cordillera, part of the U.S.A. \nPacific Northwest. and adjacent offshore areas. Sheet 3 \nprovides the list of map units for Sheets I and 2. Sheet 4 is a \nindex map showing generalized onshore terranes and overlap \nassemblages for onshore parts of the Circum-North Pacific at a \nscale of I: I 0,000,000. Sheet 4 is a guide to the more \ncomplicated onshore features depicted on Sheets I and 2. Sheet \n5 is an index map showing the major geographic regions for \nthe Circum-North Pacific. </p>\n<br>\n<p>Significant differences exist between the representation of \nonshore and offshore geology on Sheets I and 2. These are: (I) \ncompared to the onshore part of the map, the offshore part is \ndepicted in a more schematic fashion because of more limited \ndata and because the offshore terranes and early Cenozoic and \nolder overlap assemblages generally are obscured by extensive \nlate Cenozoic sedimentary cover that is not shown unless \nthicker than two kilometers; (2) marginal contacts of offshore \nCenozoic and Cretaceous sedimentary basins do not match \ncontacts of onshore Cenozoic and Cretaceous sedimentary units \nbecause offshore basins are limited to those regions with \nsediment thicknesses greater than two kilometers; (3) \nstratigraphic columns, included at the end of this explanation. \nare provided only for onshore terranes because the geology of \noffshore terranes is generally less well-known; and (4) for \nsimplicity, the major onshore Cenozoic sedimentary basins are \ngenerally not defined and described separately because the \nonshore part of the map is designed to emphasize terranes and \noverlap volcanic assemblages that are crucial for both for \ntectonic and metallogenic analyses published elsewhere \n(Nokleberg and others, 1993, 1994a).</p>\n<br>\n<p>Several key geologic sources were used in the compilation \nof the map. For Alaska. the basic outcrop pattern for the map is \nfrom Beikman (1980), Gehrels and Berg (1992, 1994). Barker \nand others ( 1994). Brew (1994), and Moli-Stalcup and others \n( 1994b). The distribution of terranes is from Jones and others \n(1987) and Monger and Berg (1987), with modification by \nGrantz and other (1991 ). Worall (199 1 ), okleberg and others \n(1993, 1994a), the cited references, and the Alaskan co-authors \nof this report. For the Canadian Cordillera. the basic outcrop \npattern is from Monger and Berg ( 1987), Wheeler and other \n(1988). and Wheeler and McFeeley ( 1991) with modifications \nby the Canadian authors. For the northern part of the Russian \nFar East. the basic outcrop pattern is from So unov (1985) with \nmodifications by the Russian authors. For the outhern part of \nthe Russian Far East, the basic outcrop pattern is from Krasny \n(1991) and Bazhanov and Oleinik ( 1986) with modification \nby the Russian authors. The Russian Far East part of the map is \nthe first attempt to define and delineate terranes in that region. \nIn their compilation. the Russian authors utilized the \nmethodology of U.S.A. and Canadian geologists. Because this \nmap is the first attempt to display the terranes. Cenozoic and \nMesozoic overlap assemblages. basinal deposit , and plutonic \nbelts of the Russian Far East. the Russian author will \nappreciate constructive sugge tions for improving the map.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94714","collaboration":"Prepared in collaboration with Russian Academy of Sciences, Geological Survey of Canada, Alaska Division of Geological and Geophysical Surveys, Russian Committee on Geology, Michigan State University, Exxon Production Research Company, University of Alaska, Geological Survey of Japan","usgsCitation":"Nokleberg, W.J., Parfenov, L.M., Monger, J.W., Baranov, B., Byalobzhesky, S.G., Bundtzen, T., Feeney, T.D., Fujita, K., Gordey, S.P., Grantz, A., Khanchuk, A.I., Natal’in, B.A., Natapov, L.M., Norton, I.O., Patton, W.W., Plafker, G., Scholl, D.W., Sokolov, S.D., Sosunov, G.M., Stone, D., Tabor, R.W., Tsukanov, N.V., Vallier, T.L., and Wakita, K., 1994, Circum-North Pacific tectonostratigraphic terrane map: U.S. Geological Survey Open-File Report 94-714, Report: 221 p.; 5 Plates: 49.97 x 36.00 inches and smaller, https://doi.org/10.3133/ofr94714.","productDescription":"Report: 221 p.; 5 Plates: 49.97 x 36.00 inches and smaller","numberOfPages":"222","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":286641,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404382,"rank":8,"type":{"id":36,"text":"NGMDB Index 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,{"id":20742,"text":"ofr94254 - 1994 - Deconvolution of continuous borehole temperature logs : example from the Greenland GISP2 icecore hole","interactions":[],"lastModifiedDate":"2012-02-02T00:07:40","indexId":"ofr94254","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-254","title":"Deconvolution of continuous borehole temperature logs : example from the Greenland GISP2 icecore hole","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94254","usgsCitation":"Saltus, R.W., and Clow, G., 1994, Deconvolution of continuous borehole temperature logs : example from the Greenland GISP2 icecore hole: U.S. Geological Survey Open-File Report 94-254, 42 p, https://doi.org/10.3133/ofr94254.","productDescription":"42 p","costCenters":[],"links":[{"id":152362,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0254/report-thumb.jpg"},{"id":50297,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0254/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672608","contributors":{"authors":[{"text":"Saltus, R. W.","contributorId":85588,"corporation":false,"usgs":true,"family":"Saltus","given":"R.","middleInitial":"W.","affiliations":[],"preferred":false,"id":183168,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clow, G.D.","contributorId":46112,"corporation":false,"usgs":true,"family":"Clow","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":183167,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20786,"text":"ofr93495 - 1994 - Quantity and quality of base flow and stormwater runoff in Independence, Missouri, October 1991 to February 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:07:39","indexId":"ofr93495","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"93-495","title":"Quantity and quality of base flow and stormwater runoff in Independence, Missouri, October 1991 to February 1993","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-file Reports Section [distributor],","doi":"10.3133/ofr93495","usgsCitation":"Schalk, G.K., 1994, Quantity and quality of base flow and stormwater runoff in Independence, Missouri, October 1991 to February 1993: U.S. Geological Survey Open-File Report 93-495, v, 69 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr93495.","productDescription":"v, 69 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0495/report-thumb.jpg"},{"id":50337,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0495/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64adc1","contributors":{"authors":[{"text":"Schalk, Gregg K.","contributorId":66250,"corporation":false,"usgs":true,"family":"Schalk","given":"Gregg","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":183249,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26168,"text":"wri934003 - 1994 - Ground-water flow and quality, and geochemical processes, in Indian Wells Valley, Kern, Inyo, and San Bernardino counties, California, 1987-88","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri934003","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"93-4003","title":"Ground-water flow and quality, and geochemical processes, in Indian Wells Valley, Kern, Inyo, and San Bernardino counties, California, 1987-88","docAbstract":"An existing water-quality data base for the 300- square-mile Indian Wells Valley was updated by means of chemical and isotopic analysis of ground water. The wide range in measured concentrations of major ions and of minor constituents such as fluoride, borate, nitrate, manganese, and iron is attributed to geochemical reactions within lacustrine deposits of the valley floor. These reactions include sulfate reduction accompanied by generation of alkalinity, precipitation of carbonates, exchange of aqueous alkaline-earth ions for sodium on clays, and dissolution of evaporite minerals. Differences in timing and location of recharge, which originates primarily in the Sierra Nevada to the west, and evapotranspiration from a shallow water table on the valley floor result in a wide range in ratios of stable hydrogen and oxygen isotopes. As ground water moves from alluvium into lustrine deposits of the ancestral China Lake, dissolved-solids concen- trations increase from about 200 to more than 1,000 milligrams per liter; further large increases to several thousand milligrams per liter occur beneath the China Lake playa. Historical data show an increase during the past 20 years in dissolved- solids concentration in several wells in the principal pumping areas at Ridgecrest and between Ridgecrest and Inyokern. The increase apparently is caused by induced flow of saline ground water from nearby China, Mirror, and Satellite Lakes. A simplified advective-transport model calculates ground-water travel times between parts of the valley of at least several thousand years, indi- cating the presence of old ground water. A local ground-water line and an evaporation line estimated using isotopic data from the China Lake area inter- sect at a delta-deuterium value of about -125 permil. This indicates that late Pleistocene recharge was 15 to 35 permil more negative than current recharge.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-File Reports Section [distributor],","doi":"10.3133/wri934003","usgsCitation":"Berenbrock, C., and Schroeder, R.A., 1994, Ground-water flow and quality, and geochemical processes, in Indian Wells Valley, Kern, Inyo, and San Bernardino counties, California, 1987-88: U.S. Geological Survey Water-Resources Investigations Report 93-4003, vi, 59 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934003.","productDescription":"vi, 59 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4003/report-thumb.jpg"},{"id":54956,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4003/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce7c","contributors":{"authors":[{"text":"Berenbrock, Charles","contributorId":30598,"corporation":false,"usgs":true,"family":"Berenbrock","given":"Charles","email":"","affiliations":[],"preferred":false,"id":195929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schroeder, R. A.","contributorId":15554,"corporation":false,"usgs":true,"family":"Schroeder","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195928,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27705,"text":"wri944250 - 1994 - Refining 1970's Land-Use Data With 1990 Population Data to Indicate New Residential Development","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri944250","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-4250","title":"Refining 1970's Land-Use Data With 1990 Population Data to Indicate New Residential Development","docAbstract":"A procedure using a geographic information system was developed to define urban land use representative of the 1990's by overlaying U.S. Bureau of the Census 1990 population density at the block group level on 1970's digital land-use data from 1:250,000-and 1: 100,000scale maps. Any area having a population density of 1,000 or more people per square mile is re-classified as &quot;urban&quot; land use in the derivative product. The procedure was applied to 20 study units of the National Water-Quality Assessment program to provide what are considered reasonable indications of urbanization that has occurred since the 1970's.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri944250","usgsCitation":"Hitt, K.J., 1994, Refining 1970's Land-Use Data With 1990 Population Data to Indicate New Residential Development: U.S. Geological Survey Water-Resources Investigations Report 94-4250, vi, 15 p., https://doi.org/10.3133/wri944250.","productDescription":"vi, 15 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":158517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11621,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri944250/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635169","contributors":{"authors":[{"text":"Hitt, Kerie J.","contributorId":54565,"corporation":false,"usgs":true,"family":"Hitt","given":"Kerie","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21307,"text":"ofr94654B - 1994 - Digital bedrock geologic map of the Plymouth quadrangle, Vermont","interactions":[],"lastModifiedDate":"2023-11-20T21:45:15.144599","indexId":"ofr94654B","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-654","chapter":"B","title":"Digital bedrock geologic map of the Plymouth quadrangle, Vermont","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94654B","collaboration":"The USGS does not support this software or answer technical questions for the software associated with the publication.","usgsCitation":"Walsh, G.J., and Ratcliffe, N.M., 1994, Digital bedrock geologic map of the Plymouth quadrangle, Vermont: U.S. Geological Survey Open-File Report 94-654, 2 Computer Disks, https://doi.org/10.3133/ofr94654B.","productDescription":"2 Computer Disks","costCenters":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":277714,"rank":2,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1994/0654b/application.zip","linkFileType":{"id":6,"text":"zip"}},{"id":154328,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":108244,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12573.htm","linkFileType":{"id":5,"text":"html"},"description":"12573"}],"country":"United States","state":"Vermont","otherGeospatial":"Plymouth quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -72.75,\n              43.625\n            ],\n            [\n              -72.75,\n              43.5\n            ],\n            [\n              -72.625,\n              43.5\n            ],\n            [\n              -72.625,\n              43.625\n            ],\n            [\n              -72.75,\n              43.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d56d","contributors":{"authors":[{"text":"Walsh, Gregory J. 0000-0003-4264-8836 gwalsh@usgs.gov","orcid":"https://orcid.org/0000-0003-4264-8836","contributorId":873,"corporation":false,"usgs":true,"family":"Walsh","given":"Gregory","email":"gwalsh@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":184184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ratcliffe, Nicholas M. 0000-0002-7922-5784 nratclif@usgs.gov","orcid":"https://orcid.org/0000-0002-7922-5784","contributorId":4167,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"Nicholas","email":"nratclif@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":184185,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31754,"text":"ofr94654A - 1994 - Digital bedrock geologic map of the Plymouth quadrangle, Vermont","interactions":[],"lastModifiedDate":"2023-11-20T21:50:25.24008","indexId":"ofr94654A","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-654","chapter":"A","title":"Digital bedrock geologic map of the Plymouth quadrangle, Vermont","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94654A","usgsCitation":"Walsh, G.J., and Ratcliffe, N.M., 1994, Digital bedrock geologic map of the Plymouth quadrangle, Vermont: U.S. Geological Survey Open-File Report 94-654, 2 Plates: 29.07 x 32.15 inches and 28.10 x 32.22 inches, https://doi.org/10.3133/ofr94654A.","productDescription":"2 Plates: 29.07 x 32.15 inches and 28.10 x 32.22 inches","costCenters":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":108245,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12573.htm","linkFileType":{"id":5,"text":"html"},"description":"12573"},{"id":160399,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"Vermont","otherGeospatial":"Plymouth quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -72.75,\n              43.625\n            ],\n            [\n              -72.75,\n              43.5\n            ],\n            [\n              -72.625,\n              43.5\n            ],\n            [\n              -72.625,\n              43.625\n            ],\n            [\n              -72.75,\n              43.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b462b","contributors":{"authors":[{"text":"Walsh, Gregory J. 0000-0003-4264-8836 gwalsh@usgs.gov","orcid":"https://orcid.org/0000-0003-4264-8836","contributorId":873,"corporation":false,"usgs":true,"family":"Walsh","given":"Gregory","email":"gwalsh@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":206875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ratcliffe, Nicholas M. 0000-0002-7922-5784 nratclif@usgs.gov","orcid":"https://orcid.org/0000-0002-7922-5784","contributorId":4167,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"Nicholas","email":"nratclif@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":206876,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19091,"text":"ofr94385 - 1994 - Hydrologic data collection at Crowders Creek and Steele Creek, York County, South Carolina, 1991-92","interactions":[],"lastModifiedDate":"2017-01-04T11:17:30","indexId":"ofr94385","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-385","title":"Hydrologic data collection at Crowders Creek and Steele Creek, York County, South Carolina, 1991-92","docAbstract":"Rapid industrial and urban growth is anticipated in the vicinity of Crowders Creek near Clover, S.C., and Steele Creek near Fort Mill, S.C. These subbasins are in the Catawba River Basin in York County, S.C. To obtain baseline information on these basins prior to urbanization, gaging stations 02145642 (Crowders Creek near Clover, S.C.) and 021467801 (Steele Creek near Fort Mill, S.C.) were established to collect streamflow and water-quality data. Continuous stream-stage and streamflow data were collected during the periods of March 23, 1991 to September 30, 1992, and May 29, 1991 to September 30, 1992, for stations 02145642 and 021467801, respectively. Average streamflows for stations 02145642 and 021467801 for the study period were 80.5 cubic feet per second and 28.6 cubic feet per second, respectively. Water-quality data were collected on four separate occasions at each gage site; two samplings during low-flow events and two samplings during high-flow events. Fecal coliform concentrations exceeded minimum standards for freshwater with other physical and chemical constituents meeting South Carolina Department of Health and Environmental Control standards.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94385","usgsCitation":"Gissendanner, J.W., 1994, Hydrologic data collection at Crowders Creek and Steele Creek, York County, South Carolina, 1991-92: U.S. Geological Survey Open-File Report 94-385, iv, 18 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94385.","productDescription":"iv, 18 p. :ill., map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":151053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0385/report-thumb.jpg"},{"id":48529,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0385/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","county":"York County","city":"Fort Mill","otherGeospatial":"Crowders Creek, Steele Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.6448974609375,\n              34.6060845921693\n            ],\n            [\n              -81.6448974609375,\n              35.4382955473967\n            ],\n            [\n              -80.321044921875,\n              35.4382955473967\n            ],\n            [\n              -80.321044921875,\n              34.6060845921693\n            ],\n            [\n              -81.6448974609375,\n              34.6060845921693\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f832","contributors":{"authors":[{"text":"Gissendanner, John W.","contributorId":26710,"corporation":false,"usgs":true,"family":"Gissendanner","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":180296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25942,"text":"wri934224 - 1994 - Ground-water quality and trends at two industrial wastewater-injection sites in northwestern Florida, 1975-91","interactions":[],"lastModifiedDate":"2020-02-25T17:54:52","indexId":"wri934224","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"93-4224","title":"Ground-water quality and trends at two industrial wastewater-injection sites in northwestern Florida, 1975-91","docAbstract":"Industrial wastewater from two synthetic-fiber manufacturing plants has been injected into the Lower Floridan aquifer near Pensacola, Florida, since 1963, and near Milton, Florida, since 1975. Trend analysis of selected water-quality characteristics in water from four monitoring wells at each of these plants indicates that injected wastewater has affected ground-water quality in the Lower Floridan aquifer, which contains nonpotable water, up to 1.5 miles from the injection wells at the plant near Pensacola and at least 0.3 mile from the injection wells at the plant near Milton. No evidence for upward seepage of injected wastewater through the overlying Bucatunna Clay to the Upper Floridan aquifer was found at either of the plants.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934224","usgsCitation":"Andrews, W., 1994, Ground-water quality and trends at two industrial wastewater-injection sites in northwestern Florida, 1975-91: U.S. Geological Survey Water-Resources Investigations Report 93-4224, iv, 25 p., https://doi.org/10.3133/wri934224.","productDescription":"iv, 25 p.","costCenters":[],"links":[{"id":118880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_93_4224.jpg"}],"country":"United States","state":"Florida","city":"Milton, Pensacola","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.40997314453125,\n              30.36102635890718\n            ],\n            [\n              -86.95816040039062,\n              30.36102635890718\n            ],\n            [\n              -86.95816040039062,\n              30.705239001430183\n            ],\n            [\n              -87.40997314453125,\n              30.705239001430183\n            ],\n            [\n              -87.40997314453125,\n              30.36102635890718\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673b8","contributors":{"authors":[{"text":"Andrews, W. J. 0000-0003-4780-8835","orcid":"https://orcid.org/0000-0003-4780-8835","contributorId":56261,"corporation":false,"usgs":true,"family":"Andrews","given":"W. J.","affiliations":[],"preferred":false,"id":195522,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26076,"text":"wri904095 - 1994 - Interactions of metallic substances and acidic ground water in the New Jersey Coastal Plan","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"wri904095","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"90-4095","title":"Interactions of metallic substances and acidic ground water in the New Jersey Coastal Plan","docAbstract":"Four ancillary studies were undertaken in support of an investigation into the extent and distribution of corrosive ground water in the Kirkwood- Cohansey aquifer system of southern New Jersey.The ancillary studies were (1) analysis of tap-water samples for metals and the acquisition of metal data from a county study, (2) leaching experiments in which copper pipe with various types of solder were exposed to a variety of ground-water types, (3) analysis of pipe-scale deposits on plumbing from houses with wells that tap the Kirkwood-Cohansey aquifer system, and (4) measurement of corrosion rates for carbon steel and copper exposed to shallow ground water from the Kirkwood-Cohansey aquifer system.  The results studies indicate that substantial concentrations of lead, copper, and zinc can leach from plumbing materials exposed to corrosive water from the Kirkwood-Cohansey aquifer system, and that leaching appears more pronounced during the summer than during the winter. The leaching experiments indicate that the corrosiveness of water, as estimated by the calculation of a corrosion index (the Aggressive Index), is related to the concentration of trace metals in the leachate.Further, although the leaching of lead-bearing solders produced lead concentrations in leachate above the Primary Drinking Water Criterion in effect at the time of the study (50 micrograms per liter), no potentially toxic levels of metals were leached from lead-free solders, although copper concentrations in some leachate samples were in excess of the Secondary Drinking Water Criterion of 1,000 micrograms per liter.   Analyses of pipe-scale deposits indicate the formation of iron oxide coatings on some copper-pipe interiors exposed to untreated well water.   Treated water from a public-supply system precipitated copper carbonate and copper chloride minerals. Corrosion rates measured for copper exposed to corrosive water from the Kirkwood-Cohansey aquifer system were slow (less than 0.0254 millimeters per year). Carbon-steel corrosion rates were faster; the fastest rate (0.229 millimeters per year) was measured in oxygen-saturated water.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri904095","usgsCitation":"Barringer, J.L., 1994, Interactions of metallic substances and acidic ground water in the New Jersey Coastal Plan: U.S. Geological Survey Water-Resources Investigations Report 90-4095, vi, 68 p. :ill., map ;28 cm., https://doi.org/10.3133/wri904095.","productDescription":"vi, 68 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4095/report-thumb.jpg"},{"id":54848,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4095/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4930e4b07f02db581757","contributors":{"authors":[{"text":"Barringer, J. L.","contributorId":13994,"corporation":false,"usgs":true,"family":"Barringer","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195760,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20589,"text":"ofr9436 - 1994 - Trihalomethane and nonpurgeable total organic-halide formation potentials for the Mississippi River and some of its tributaries, September-October 1991","interactions":[],"lastModifiedDate":"2012-02-02T00:07:43","indexId":"ofr9436","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-36","title":"Trihalomethane and nonpurgeable total organic-halide formation potentials for the Mississippi River and some of its tributaries, September-October 1991","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9436","usgsCitation":"Rathbun, R.E., and Bishop, L., 1994, Trihalomethane and nonpurgeable total organic-halide formation potentials for the Mississippi River and some of its tributaries, September-October 1991: U.S. Geological Survey Open-File Report 94-36, vi, 53 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr9436.","productDescription":"vi, 53 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":153302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0036/report-thumb.jpg"},{"id":50107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624669","contributors":{"authors":[{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":182897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bishop, L.M.","contributorId":32191,"corporation":false,"usgs":true,"family":"Bishop","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":182896,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32782,"text":"ofr94504 - 1994 - Hydrologic data for the alluvium and terrace deposits of the Cimarron River from Freedom to Guthrie, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"ofr94504","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-504","title":"Hydrologic data for the alluvium and terrace deposits of the Cimarron River from Freedom to Guthrie, Oklahoma","docAbstract":"Ground water in the Quaternary alluvium and terrace deposits associated with the Cimarron River in northwestern Oklahoma is used extensively for irrigation, municipal, stock, and domestic supplies. The data in this report were collected as part of an investigation to provide State water managers with the quantitative knowledge necessary to manage the ground-water resource effectively. The investigation was conducted by the U.S. Geological Survey in cooperation with the Oklahoma Geological Survey. The information presented in this report include data collected in the field from 1985 through 1989, and unpublished data compiled from files of the U.S. Geological Survey and the Oklahoma Water Resources Board. Data include well and test-bole records, consisting of ground-water levels, depth of wells, principal aquifer, and primary use of water. Water levels include continuous, daily, monthly, and periodic measure- ments for selected wells. Concentrations of common chemical constituents, selected trace elements, organic analyses, and tritium analyses of water samples from wells completed in the Cimarron River alluvium and terrace deposits and Permian geologic units are reported. Winter and summer base-flow discharge measurements of the Cimarron River and its Tributaries are presented together with water-quality data from the measuring sites. Continuous water-level and precipitation-gage data are presented graphically. Locations of data- collection sites are shown on plates.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94504","usgsCitation":"Adams, G.P., Bergman, D.L., Pruitt, D., May, J., and Kurklin, J., 1994, Hydrologic data for the alluvium and terrace deposits of the Cimarron River from Freedom to Guthrie, Oklahoma: U.S. Geological Survey Open-File Report 94-504, vi, 231 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94504.","productDescription":"vi, 231 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":161327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0504/report-thumb.jpg"},{"id":60725,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0504/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db6080ce","contributors":{"authors":[{"text":"Adams, Gregory P.","contributorId":13095,"corporation":false,"usgs":true,"family":"Adams","given":"Gregory","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":209154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergman, D. L.","contributorId":93038,"corporation":false,"usgs":true,"family":"Bergman","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":209157,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pruitt, D.J.","contributorId":79756,"corporation":false,"usgs":true,"family":"Pruitt","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":209156,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"May, J.E.","contributorId":7741,"corporation":false,"usgs":true,"family":"May","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":209153,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kurklin, J. K.","contributorId":59032,"corporation":false,"usgs":true,"family":"Kurklin","given":"J. K.","affiliations":[],"preferred":false,"id":209155,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":19245,"text":"ofr94109 - 1994 - Experimental drawdown study, Lower Granite Reservoir, north-central Idaho, March 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:31","indexId":"ofr94109","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-109","title":"Experimental drawdown study, Lower Granite Reservoir, north-central Idaho, March 1992","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94109","usgsCitation":"Harper, R., and Lipscomb, S.W., 1994, Experimental drawdown study, Lower Granite Reservoir, north-central Idaho, March 1992: U.S. Geological Survey Open-File Report 94-109, vi, 622 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94109.","productDescription":"vi, 622 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":151672,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0109/report-thumb.jpg"},{"id":48707,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0109/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f92d4","contributors":{"authors":[{"text":"Harper, R.W.","contributorId":36104,"corporation":false,"usgs":true,"family":"Harper","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":180550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lipscomb, Stephen W.","contributorId":84753,"corporation":false,"usgs":true,"family":"Lipscomb","given":"Stephen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":180551,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27344,"text":"wri944101 - 1994 - Hydrology and water quality of Whitewater and Rice lakes in southeastern Wisconsin, 1990-91","interactions":[],"lastModifiedDate":"2015-10-26T12:22:03","indexId":"wri944101","displayToPublicDate":"1995-09-01T00:00:00","publicationYear":"1994","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":"94-4101","title":"Hydrology and water quality of Whitewater and Rice lakes in southeastern Wisconsin, 1990-91","docAbstract":"<p>The hydrology and water quality of Whitewater and Rice Lakes was studied by the U.S. Geological Survey during November 15, 1990November 14, 1991, in cooperation with the Whitewater-Rice Lakes Management District, Walworth County, Wis. Whitewater and Rice Lakes are small, shallow lakes; surface areas are 697 and 162 acres and mean depths are 8.4 feet and 5.8 feet, respectively. Although both lakes have surface outlets, water levels were below the dam crests during the study, and no water left the lake through the outlets. The drainage basin of Whitewater Lake is 10.9 square miles and that of Rice Lake is 11.8 square miles; but, because of large amounts of depressional areas, only 1.4 square miles and 0.2 square mile, respectively, contribute surface runoff to the lakes. Whitewater Lake is an artificial lake created in 1947 by the damming of three smaller lakes. Rice Lake is an artificial lake created in 1954 by the damming of Whitewater Creek, which drains Whitewater Lake. Maintaining the lake levels at the elevations of their dam crests has been difficult since the lakes were created. For most years, water levels were below the lakes' dam crests.</p>\n<p>Ground water, precipitation, and evaporation are important components in the hydrologic budgets of the lakes. For Whitewater Lake, ground water was the dominant source of water, accounting for 57 percent of the inflow budget; precipitation accounted for 26 percent. Ground water also dominated the outflow, accounting for 81 percent of the outflow budget. The remaining 19 percent of the outflow budget was evaporation. For Rice Lake, precipitation was the dominant source of water, accounting for 88 percent of the inflow budget; ground water accounted for 8 percent. Evaporation dominated the outflow budget, at 70 percent, whereas ground water accounted for 30 percent.</p>\n<p>The external phosphorus budget for Whitewater Lake showed that shoreline drainage was the largest source of phosphorus to the lake42 percent of the total input of 558 pounds. Other sources of phosphorus were septic systems, 19 percent of the total; precipitation, 18 percent; a spring inlet at base flow, 13 percent; and ground water, 8 percent. The external phosphorus budget for Rice Lake showed that shoreline drainage also was the largest source of phosphorus to the lake-59 percent of the total input of 63 pounds; other sources were precipitation, 38 percent of the total; and ground water, 3 percent. Application of Vollenweider's phosphorus loading model fairly accurately predicted the lakes' spring turnover phosphorus concentrations and suggested that the external loading of phosphorus would result in mesotrophic to eutrophic conditions for Whitewater Lake and mesotrophic conditions for Rice Lake. Dillon and Rigler's model further suggested additional phosphorus from internal recycling was required to result in the high chlorophyll-a concentrations experienced in both systems during summer. Internal recycling of phosphorus in addition to external loading seems to also cause waterquality problems in both lakes. The amount of phosphorus recycled from the lake sediments was estimated from a mass-balance approach for April 1-November 14, 1991. For Whitewater Lake, the internal load of 582 pounds was slightly greater than the annual external load of 558 pounds. For Rice Lake, the internal load of 295 pounds far exceeded the annual external load of 63 pounds.</p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944101","collaboration":"Prepared in cooperation with the Whitewater-Rice Lakes Management District","usgsCitation":"Goddard, G., and Field, S.J., 1994, Hydrology and water quality of Whitewater and Rice lakes in southeastern Wisconsin, 1990-91: U.S. Geological Survey Water-Resources Investigations Report 94-4101, v, 36 p., https://doi.org/10.3133/wri944101.","productDescription":"v, 36 p.","numberOfPages":"41","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":56207,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4101/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4101/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Walworth County","otherGeospatial":"Rice Lake, Whitewater Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.65486145019531,\n              42.84777884235988\n            ],\n            [\n              -88.55941772460938,\n              42.805728711206285\n            ],\n            [\n              -88.66756439208984,\n              42.71069600569494\n            ],\n            [\n              -88.71700286865234,\n              42.66703805067892\n            ],\n            [\n              -88.81553649902344,\n              42.718768102606354\n            ],\n            [\n              -88.76850128173828,\n              42.77196720401213\n            ],\n            [\n              -88.67408752441406,\n              42.85004420475656\n            ],\n            [\n              -88.65486145019531,\n              42.84777884235988\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bcaed","contributors":{"authors":[{"text":"Goddard, Gerald","contributorId":54202,"corporation":false,"usgs":true,"family":"Goddard","given":"Gerald","affiliations":[],"preferred":false,"id":197951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Field, S. J.","contributorId":50540,"corporation":false,"usgs":true,"family":"Field","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197950,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17795,"text":"ofr94539 - 1994 - U.S. Geological Survey protocol for the collection and processing of surface-water samples for the subsequent determination of inorganic constituents in filtered water","interactions":[],"lastModifiedDate":"2021-05-28T17:38:17.869004","indexId":"ofr94539","displayToPublicDate":"1995-08-01T00:00:00","publicationYear":"1994","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":"94-539","title":"U.S. Geological Survey protocol for the collection and processing of surface-water samples for the subsequent determination of inorganic constituents in filtered water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94539","usgsCitation":"Horowitz, A.J., Demas, C.R., Fitzgerald, K.K., Miller, T.L., and Rickert, D.A., 1994, U.S. Geological Survey protocol for the collection and processing of surface-water samples for the subsequent determination of inorganic constituents in filtered water: U.S. Geological Survey Open-File Report 94-539, vi, 57 p., https://doi.org/10.3133/ofr94539.","productDescription":"vi, 57 p.","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":47036,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0539/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0539/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612209","contributors":{"authors":[{"text":"Horowitz, Arthur J. 0000-0002-3296-730X horowitz@usgs.gov","orcid":"https://orcid.org/0000-0002-3296-730X","contributorId":1400,"corporation":false,"usgs":true,"family":"Horowitz","given":"Arthur","email":"horowitz@usgs.gov","middleInitial":"J.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":177869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Demas, C. R.","contributorId":77178,"corporation":false,"usgs":true,"family":"Demas","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":177873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fitzgerald, K. K.","contributorId":34501,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"K.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":177870,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, T. L.","contributorId":54557,"corporation":false,"usgs":true,"family":"Miller","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":177872,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rickert, D. A.","contributorId":53773,"corporation":false,"usgs":true,"family":"Rickert","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":177871,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":17501,"text":"ofr953 - 1994 - Preliminary analysis of integrated stratigraphic data from the South Venice corehole, Sarasota County, Florida","interactions":[],"lastModifiedDate":"2020-03-27T07:02:41","indexId":"ofr953","displayToPublicDate":"1995-08-01T00:00:00","publicationYear":"1994","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":"95-3","title":"Preliminary analysis of integrated stratigraphic data from the South Venice corehole, Sarasota County, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr953","usgsCitation":"Brewster-Wingard, G.L., Weedman, S., Scott, T., Edwards, L.E., and Green, R., 1994, Preliminary analysis of integrated stratigraphic data from the South Venice corehole, Sarasota County, Florida: U.S. Geological Survey Open-File Report 95-3, 129 p., https://doi.org/10.3133/ofr953.","productDescription":"129 p.","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":149121,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0003/report-thumb.jpg"},{"id":46652,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida ","county":"Sarasota County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.6611328125,\n              27.19112839142226\n            ],\n            [\n              -82.2821044921875,\n              27.19112839142226\n            ],\n            [\n              -82.2821044921875,\n              27.464413510962768\n            ],\n            [\n              -82.6611328125,\n              27.464413510962768\n            ],\n            [\n              -82.6611328125,\n              27.19112839142226\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acae4b07f02db67cd65","contributors":{"authors":[{"text":"Brewster-Wingard, G. Lynn","contributorId":17626,"corporation":false,"usgs":true,"family":"Brewster-Wingard","given":"G.","email":"","middleInitial":"Lynn","affiliations":[],"preferred":false,"id":176612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weedman, S.D.","contributorId":23961,"corporation":false,"usgs":true,"family":"Weedman","given":"S.D.","affiliations":[],"preferred":false,"id":176614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scott, T.M.","contributorId":66694,"corporation":false,"usgs":true,"family":"Scott","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":176615,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":176611,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Green, R.C.","contributorId":22373,"corporation":false,"usgs":true,"family":"Green","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":176613,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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