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,{"id":55102,"text":"wdrWV931 - 1994 - Water resources data, West Virginia, water year 1993","interactions":[],"lastModifiedDate":"2025-02-19T14:31:01.411309","indexId":"wdrWV931","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WV-93-1","title":"Water resources data, West Virginia, water year 1993","docAbstract":"<p>Water-resources data for the 1993 water year for West Virginia consist of records of stage, discharge, and water quality of streams; contents of reservoirs; and water levels of observations wells. This report contains discharge records for 78 streamflow-gaging stations; stage only records for 11 gaging stations; annual maximum discharge at 2 crest-stage partial-record stations; change in contents for 1 reservoir; water-quality records for 13 stations; and water-level records for 29 observation wells. Locations of these sites are shown on figures 4 and 5. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous sites. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in West Virginia.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWV931","collaboration":"Prepared in cooperation with the State of West Virginia and with other agencies","usgsCitation":"Ward, S., Taylor, B., and Mathes, M., 1994, Water resources data, West Virginia, water year 1993: U.S. Geological Survey Water Data Report WV-93-1, xxii, 331 p., https://doi.org/10.3133/wdrWV931.","productDescription":"xxii, 331 p.","costCenters":[],"links":[{"id":482193,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1993/wv-93-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181095,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1993/wv-93-1/report-thumb.jpg"}],"country":"United States","state":"West 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K.","contributorId":74395,"corporation":false,"usgs":true,"family":"White","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":251373,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brosten, T.M.","contributorId":92669,"corporation":false,"usgs":true,"family":"Brosten","given":"T.M.","email":"","affiliations":[],"preferred":false,"id":251374,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chambers, C. L.","contributorId":48525,"corporation":false,"usgs":true,"family":"Chambers","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":251372,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70017601,"text":"70017601 - 1994 - A pore-pressure diffusion model for estimating landslide-inducing rainfall","interactions":[],"lastModifiedDate":"2024-03-14T00:03:38.493693","indexId":"70017601","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2309,"text":"Journal of Geology","active":true,"publicationSubtype":{"id":10}},"title":"A pore-pressure diffusion model for estimating landslide-inducing rainfall","docAbstract":"<div class=\"col-lg-9 article__content\"><div class=\"article__body show-references \"><div class=\"hlFld-Abstract\"><div class=\"abstractSection abstractInFull\"><p>Many types of landslide movement are induced by large rainstorms, and empirical rainfall intensity/duration thresholds for initiating movement have been determined for various parts of the world. In this paper, I present a simple pressure diffusion model that provides a physically based hydrologic link between rainfall intensity/duration at the ground surface and destabilizing pore-water pressures at depth. The model approximates rainfall infiltration as a sinusoidally varying flux over time and uses physical parameters that can be determined independently. If destabilizing pore pressures can be estimated, then the model enables the development of a stability criterion defining destabilizing rainfall intensity/duration conditions. Using a comprehensive data set from an intensively monitored landslide, I demonstrate that the model is capable of distinguishing movement-inducing rainstorms.</p></div></div></div></div>","language":"English","publisher":"University of Chicago Press","doi":"10.1086/629714","issn":"00221376","usgsCitation":"Reid, M., 1994, A pore-pressure diffusion model for estimating landslide-inducing rainfall: Journal of Geology, v. 102, no. 6, p. 709-717, https://doi.org/10.1086/629714.","productDescription":"9 p.","startPage":"709","endPage":"717","numberOfPages":"9","costCenters":[],"links":[{"id":228567,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"102","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4e0e4b0c8380cd469c1","contributors":{"authors":[{"text":"Reid, M.E.","contributorId":108130,"corporation":false,"usgs":true,"family":"Reid","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":376968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70017576,"text":"70017576 - 1994 - Real-time data collection of scour at bridges","interactions":[],"lastModifiedDate":"2012-03-12T17:19:53","indexId":"70017576","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Real-time data collection of scour at bridges","docAbstract":"The record flood on the Mississippi River during the summer of 1993 provided a rare opportunity to collect data on scour of the streambed at bridges and to test data collection equipment under extreme hydraulic conditions. Detailed bathymetric and hydraulic information were collected at two bridges crossing the Mississippi River during the rising limb, near the peak, and during the recession of the flood. Bathymetric data were collected using a digital echo sounder. Three-dimensional velocities were collected using Broadband Acoustic Doppler Current Profilers (BB-ADCP) operating at 300 kilohertz (kHz), 600 kHz, and 1,200 kHz. Positioning of the data collected was measured using a range-azimuth tracking system and two global positioning systems (GPS). Although differential GPS was able to provide accurate positions and tracking information during approach- and exit-reach data collection, it was unable to maintain lock on a sufficient number of satellites when the survey vessel was under the bridge or near the piers. The range-azimuth tracking system was used to collect position and tracking information for detailed data collection near the bridge piers. These detailed data indicated local scour ranging from 3 to 8 meters and will permit a field-based evaluation of the ability of various numerical models to compute the hydraulics, depth, geometry, and time-dependent development of local scour.","largerWorkTitle":"Proceedings of the Symposium on Fundamentals and Advancements in Hydraulic Measurements and Experimentation","conferenceTitle":"Proceedings of the Symposium on Fundamentals and Advancements in Hydraulic Measurements and Experimentation","conferenceDate":"1 August 1994 through 5 August 1994","conferenceLocation":"Buffalo, NY, USA","language":"English","publisher":"Publ by ASCE","publisherLocation":"New York, NY, United States","isbn":"0784400369","usgsCitation":"Mueller, D.S., and Landers, M.N., 1994, Real-time data collection of scour at bridges, <i>in</i> Proceedings of the Symposium on Fundamentals and Advancements in Hydraulic Measurements and Experimentation, Buffalo, NY, USA, 1 August 1994 through 5 August 1994, p. 104-113.","startPage":"104","endPage":"113","numberOfPages":"10","costCenters":[],"links":[{"id":228893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a959fe4b0c8380cd81b26","contributors":{"authors":[{"text":"Mueller, David S. dmueller@usgs.gov","contributorId":1499,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"dmueller@usgs.gov","middleInitial":"S.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":376902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landers, Mark N. 0000-0002-3014-0480 landers@usgs.gov","orcid":"https://orcid.org/0000-0002-3014-0480","contributorId":1103,"corporation":false,"usgs":true,"family":"Landers","given":"Mark","email":"landers@usgs.gov","middleInitial":"N.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":376901,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58781,"text":"mf2155E - 1994 - Sample locality map and analytical data for potassium-argon ages in the Port Moller, Stepovak Bay, and Simeonof Island quadrangles, Alaska Peninsula","interactions":[],"lastModifiedDate":"2023-01-10T19:17:41.083603","indexId":"mf2155E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2155","chapter":"E","title":"Sample locality map and analytical data for potassium-argon ages in the Port Moller, Stepovak Bay, and Simeonof Island quadrangles, Alaska Peninsula","docAbstract":"<p><span>Potassium-argon age determinations for 84 volcanic, intrusive, and hydrothermally altered rocks from the Port Moller, Stepovak Bay, and Simeonof Island quadrangles are reported here. Of these age determinations, 78 samples were analyzed as part of Alaska Mineral Resource Assessment Program (AMRAP) studies in the Port Moller, Stepovak Bay, and Simeonof Island quadrangles. Age deter- minations for 6 of the samples have been previously published (Burk, 1965; Kienle and Turner, 1976; Wilson and others, 1981). This report consists of a sample location map, analytical data (table 1), and rock descriptions (table 2).</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf2155E","usgsCitation":"Wilson, F.H., Shew, N.B., DuBois, G.D., and Bie, S.W., 1994, Sample locality map and analytical data for potassium-argon ages in the Port Moller, Stepovak Bay, and Simeonof Island quadrangles, Alaska Peninsula: U.S. Geological Survey Miscellaneous Field Studies Map 2155, Report: 18 p.; 1 Plate: 39.0 x 36.2 inches, https://doi.org/10.3133/mf2155E.","productDescription":"Report: 18 p.; 1 Plate: 39.0 x 36.2 inches","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":105277,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5782.htm","linkFileType":{"id":5,"text":"html"},"description":"5782"},{"id":88558,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1994/2155e/report.pdf","text":"Report to Accompany Map MF-2155-E","linkFileType":{"id":1,"text":"pdf"}},{"id":183325,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1994/2155e/report-thumb.jpg"},{"id":88557,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1994/2155e/plate-1.pdf","text":"Map MF-2155-E","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Alaska Peninsula, Port Moller quadrangle, Simeonof Island quadrangle, Stepovak Bay quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -162,\n              54.75\n            ],\n            [\n              -162,\n              56\n            ],\n            [\n              -158.4167,\n              56\n            ],\n            [\n              -158.4167,\n              54.75\n            ],\n            [\n              -162,\n              54.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fde9a","contributors":{"authors":[{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":260777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shew, Nora B. 0000-0003-0025-7220 nshew@usgs.gov","orcid":"https://orcid.org/0000-0003-0025-7220","contributorId":3382,"corporation":false,"usgs":true,"family":"Shew","given":"Nora","email":"nshew@usgs.gov","middleInitial":"B.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":260779,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DuBois, Gregory D.","contributorId":6824,"corporation":false,"usgs":true,"family":"DuBois","given":"Gregory","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":260780,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bie, Scott W.","contributorId":16475,"corporation":false,"usgs":true,"family":"Bie","given":"Scott","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":260778,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":18540,"text":"ofr9484 - 1994 - Operation of hydrologic data-collection stations by the U.S. Geological Survey in 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:07:27","indexId":"ofr9484","displayToPublicDate":"1994-01-01T00:00:00","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":"94-84","title":"Operation of hydrologic data-collection stations by the U.S. Geological Survey in 1993","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9484","usgsCitation":"Condes de la Torre, A., 1994, Operation of hydrologic data-collection stations by the U.S. Geological Survey in 1993: U.S. Geological Survey Open-File Report 94-84, vii, 53 p. :chiefly ill., maps ;28 cm., https://doi.org/10.3133/ofr9484.","productDescription":"vii, 53 p. :chiefly ill., maps ;28 cm.","costCenters":[],"links":[{"id":150730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0084/report-thumb.jpg"},{"id":47891,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af1e4b07f02db6917b4","contributors":{"authors":[{"text":"Condes de la Torre, Alberto","contributorId":73570,"corporation":false,"usgs":true,"family":"Condes de la Torre","given":"Alberto","email":"","affiliations":[],"preferred":false,"id":179304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54630,"text":"wdrKY931 - 1994 - Water Resources Data, Kentucky, Water Year 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:11:36","indexId":"wdrKY931","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"KY-93-1","title":"Water Resources Data, Kentucky, Water Year 1993","language":"ENGLISH","doi":"10.3133/wdrKY931","usgsCitation":"McClain, D., Byrd, F., and Brown, A., 1994, Water Resources Data, Kentucky, Water Year 1993: U.S. Geological Survey Water Data Report KY-93-1, 341 p., https://doi.org/10.3133/wdrKY931.","productDescription":"341 p.","costCenters":[],"links":[{"id":177887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb7d3","contributors":{"authors":[{"text":"McClain, D.L.","contributorId":72402,"corporation":false,"usgs":true,"family":"McClain","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":250958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byrd, F.D.","contributorId":25227,"corporation":false,"usgs":true,"family":"Byrd","given":"F.D.","email":"","affiliations":[],"preferred":false,"id":250956,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, A.C.","contributorId":30276,"corporation":false,"usgs":true,"family":"Brown","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":250957,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":18965,"text":"ofr94100 - 1994 - Compilation of atrazine and selected herbicide data from previous surface-water-quality investigations within the Big Blue River basin, Nebraska, 1983-92","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr94100","displayToPublicDate":"1994-01-01T00:00:00","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":"94-100","title":"Compilation of atrazine and selected herbicide data from previous surface-water-quality investigations within the Big Blue River basin, Nebraska, 1983-92","docAbstract":"Atrazine has been detected in the surface water of the Big Blue River Basin during every month of the year. Recent data (1983-92) documenting the occurrence of atrazine and related herbicides in the surface water of the basin are compiled in this report. In samples analyzed during these studies, atrazine was the herbicide detected most frequently within the basin. Of the 385 samples analyzed, 369 contained atrazine in detectable concentrations with detection levels varying from 0 to 0.1 micrograms per liter. The concentrations of atrazine within the samples varied from 0.5 to 166 micrograms per liter, with a median concentration of 2.7 micrograms per liter. Other herbicides frequently detected in the Big Blue River Basin were alachlor, cyanazine, metolachlor, and simazine, and two metabolites of atrazine, desethylatrazine and deisopropylatrazine. In the 226 samples which alachlor was detected, the concentrations of the herbicide ranged from 0.05 to 56 micrograms per liter, and the median concen- tration was 1.1 micrograms per liter. Cyanazine was detected in 210 of 365 samples collected with con- centrations that ranged from 0.05 to 8.6 micrograms per liter with a median concentration of 0.4 microgram per liter. The maximum concentrations of metolachlor and simazine were 26 and 35 micrograms per liter, respectively. The median concentrations of these herbicides were 1.0 and 0.1 micrograms per liter, respectively. The maximum concentration of desethylatrazine, was 3.7 micrograms per liter, with a median concentration of 1.0 microgram per liter. Deisopropylatrazine, was detected in 152 samples with maximum and median concentrations of 2.6 and 0.6 micrograms per liter, respectively.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94100","usgsCitation":"Frankforter, J., 1994, Compilation of atrazine and selected herbicide data from previous surface-water-quality investigations within the Big Blue River basin, Nebraska, 1983-92: U.S. Geological Survey Open-File Report 94-100, iv, 69 p. :maps ;28 cm., https://doi.org/10.3133/ofr94100.","productDescription":"iv, 69 p. :maps ;28 cm.","costCenters":[],"links":[{"id":151384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0100/report-thumb.jpg"},{"id":48376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0100/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6a9ff2","contributors":{"authors":[{"text":"Frankforter, J.D.","contributorId":80303,"corporation":false,"usgs":true,"family":"Frankforter","given":"J.D.","affiliations":[],"preferred":false,"id":180063,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44358,"text":"ofr946A - 1994 - Principal facts and field data for gravity data in and adjacent to the Reno 1 degree by 2 degrees Quadrangle, Nevada and California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:03","indexId":"ofr946A","displayToPublicDate":"1994-01-01T00:00:00","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":"94-6","chapter":"A","title":"Principal facts and field data for gravity data in and adjacent to the Reno 1 degree by 2 degrees Quadrangle, Nevada and California","language":"ENGLISH","doi":"10.3133/ofr946A","usgsCitation":"Plouff, D., 1994, Principal facts and field data for gravity data in and adjacent to the Reno 1 degree by 2 degrees Quadrangle, Nevada and California: U.S. Geological Survey Open-File Report 94-6, 1 computer disk ; 3 1/2 in. + 1 text (i, 16 p. : map ; 28 cm.), https://doi.org/10.3133/ofr946A.","productDescription":"1 computer disk ; 3 1/2 in. + 1 text (i, 16 p. : map ; 28 cm.)","costCenters":[],"links":[{"id":168046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0006a/report-thumb.jpg"},{"id":81659,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0006a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668da2","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":229636,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19248,"text":"ofr9451 - 1994 - Verification of a national water data base using a geographic information system","interactions":[],"lastModifiedDate":"2017-02-07T09:53:30","indexId":"ofr9451","displayToPublicDate":"1994-01-01T00:00:00","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":"94-51","title":"Verification of a national water data base using a geographic information system","docAbstract":"The National Water Data Exchange (NAWDEX) was developed to assist users of water-resource data in the identification, location, and acquisition of data. The Master Water Data Index (MWDI) of NAWDEX currently indexes the data collected by 423 organizations from nearly 500,000 sites throughout the United Stales. The utilization of new computer technologies permit the distribution of the MWDI to the public on compact disc. In addition, geographic information systems (GIS) are now available that can store and analyze these data in a spatial format. These recent innovations could increase access and add new capabilities to the MWDI. Before either of these technologies could be employed, however, a quality-assurance check of the MWDI needed to be performed. The MWDI resides on a mainframe computer in a tabular format. It was copied onto a workstation and converted to a GIS format. The GIS was used to identify errors in the MWDI and produce reports that summarized these errors. The summary reports were sent to the responsible contributing agencies along with instructions for submitting their corrections to the NAWDEX Program Office. The MWDI administrator received reports that summarized all of the errors identified. Of the 494,997 sites checked, 93,440 sites had at least one error (18.9 percent error rate).","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr9451","usgsCitation":"Harrison, H., 1994, Verification of a national water data base using a geographic information system: U.S. Geological Survey Open-File Report 94-51, iii, 149 p. :ill. ;28 cm., https://doi.org/10.3133/ofr9451.","productDescription":"iii, 149 p. :ill. ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":21528,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0051/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0051/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6024f2","contributors":{"authors":[{"text":"Harrison, H.E.","contributorId":81125,"corporation":false,"usgs":true,"family":"Harrison","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":180556,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54673,"text":"wdrME931 - 1994 - Water resources data, Maine, water year 1993","interactions":[],"lastModifiedDate":"2025-09-12T14:28:53.163624","indexId":"wdrME931","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ME-93-1","title":"Water resources data, Maine, water year 1993","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey, in cooperation with State, Federal, and other local governmental agencies, obtains a large amount of data pertaining to the water resources of Maine each year. These data, accumulated during the many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State.</p><p>Water-resources data for the 1993 water year for Maine consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; water levels of ground-water wells; and precipitation amounts at selected sites. This report contains discharge records for 47 gaging stations, stage records for 1 lake; month-end contents for 17 lakes and reservoirs; water-quality data for 12 gaging stations; water levels for 30 ground-water wells; and daily precipitation totals at 1 site. Additional water data were collected at other sites, not part of the systematic data-collection program, and are published as miscellaneous measurements.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrME931","collaboration":"Prepared in cooperation with the State of Maine and with other agencies","usgsCitation":"Nielsen, J., Higgins, W., and Lippert, R.G., 1994, Water resources data, Maine, water year 1993: U.S. Geological Survey Water Data Report ME-93-1, xiv, 233 p., https://doi.org/10.3133/wdrME931.","productDescription":"xiv, 233 p.","costCenters":[],"links":[{"id":180723,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1993/me-93-1/report-thumb.jpg"},{"id":495326,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1993/me-93-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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G.","contributorId":68356,"corporation":false,"usgs":true,"family":"Lippert","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":251115,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27931,"text":"wri934179 - 1994 - Magnitude and frequency of floods in Alaska and conterminous basins of Canada","interactions":[],"lastModifiedDate":"2018-01-10T10:24:28","indexId":"wri934179","displayToPublicDate":"1994-01-01T00:00:00","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":"93-4179","title":"Magnitude and frequency of floods in Alaska and conterminous basins of Canada","docAbstract":"<p>Equations for estimating the magnitude and frequency of floods at ungaged sites on streams in Alaska and conterminous basins of Canada were developed using multipleregression analyses of basin climatic and physical characteristics and peak-flow statistics from 260 gaged locations in Alaska and 72 gaged locations in Canada. Methods are presented for estimating flood magnitude and frequency at sites on gaged streams. Flood-frequency data based on observed peaks and basin physical and climatic characteristics are given for 332 gaged locations on streams with natural flow. The State of Alaska and conterminous basins of Canada were divided into five flood-frequency areas having similar flood characteristics on the basis of statistical cluster analyses and regional regression analyses. Generalized skew coefficients were determined for each of the five flood-frequency areas using at-site unbiased skew coefficients computed for 82 stations in Alaska having 22 or more annual peaks through the 1987 water year and 31 stations in Canada having 22 or more annual peaks through the 1984 calendar year. A set of equations for estimating peak discharge having recurrence intervals of 2,5,10,25, 50,100, 200, and 500 years was developed for each flood-frequency area. Significant basin characteristics in the equations are drainage area, mean annual precipitation, percentage of lakes and ponds, mean minimum January temperature, mean basin elevation, and percentage of forest. Drainage basin sizes range from 1.02 to 321,000 square miles. Average standard errors of prediction for the equations range from 26 to 77 percent.</p><p>A regionalized mean annual precipitation map for the climatic normal period of 1951-80 was developed for Alaska west of longitude 141° and modified from published maps for southeastern Alaska and conterminous basins of Canada. Maximum known floods at 722 sites in Alaska and conterminous basins of Canada are tabulated.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934179","collaboration":"Prepared in cooperation with the State of Alaska, Department of Transportation and Public Facilities and Federal Highway Administration","usgsCitation":"Jones, S.H., and Fahl, C.B., 1994, Magnitude and frequency of floods in Alaska and conterminous basins of Canada: U.S. Geological Survey Water-Resources Investigations Report 93-4179, Report: v, 122 p.; 2 Plates: 47.47 x 34.36 inches and 47.62 x 34.08 inches, https://doi.org/10.3133/wri934179.","productDescription":"Report: v, 122 p.; 2 Plates: 47.47 x 34.36 inches and 47.62 x 34.08 inches","costCenters":[],"links":[{"id":350411,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4179/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350412,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4179/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4179/report-thumb.jpg"},{"id":56747,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4179/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","projection":"Polyconic projection","country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -179.296875,\n              49.439556958940855\n            ],\n            [\n              -129.7265625,\n              49.439556958940855\n            ],\n            [\n              -129.7265625,\n              71.32895017791999\n            ],\n            [\n              -179.296875,\n              71.32895017791999\n            ],\n            [\n              -179.296875,\n              49.439556958940855\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64953a","contributors":{"authors":[{"text":"Jones, Stanley H.","contributorId":98729,"corporation":false,"usgs":true,"family":"Jones","given":"Stanley","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":198923,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fahl, Charles B.","contributorId":201462,"corporation":false,"usgs":true,"family":"Fahl","given":"Charles","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":198924,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30458,"text":"wri934152 - 1994 - Hydrogeology of Pleistocene glacial deposits and Jurassic \"red beds\" in the central lower peninsula of Michigan","interactions":[],"lastModifiedDate":"2018-11-19T11:59:57","indexId":"wri934152","displayToPublicDate":"1994-01-01T00:00:00","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":"93-4152","title":"Hydrogeology of Pleistocene glacial deposits and Jurassic \"red beds\" in the central lower peninsula of Michigan","docAbstract":"<p>Geologic-log data were used to construct thickness and surface-configuration maps of Jurassic deposits, and a map of general composition of Pleistocene glacial deposits, in the central Lower Peninsula of Michigan. These geologic units form the upper part of a regional system of aquifers and confining units in the Michigan Basin. In the peninsula, most bedrock is covered by glacial deposits that are primarily intercalated glaciofluvial sediments and till; in some areas, lacustrine clay and silt are surficial deposits. Areas of primarily glaciofluvial sediments (aquifer material) or till and lacustrine deposits (confining-unit material) were delineated.</p><p>Jurassic \"red beds\" underlie glacial deposits in the west-central part of the Michigan Basin. These confining deposits (primarily clay, shale, and gypsum) cover 4,000 square miles of salinewater-bearing Pennsylvanian rocks. Contour maps were generated to show general thickness and surface configuration of Jurassic \"red beds.\" Contour maps of \"red beds\" and the map of general composition of glacial deposits were prepared to aid in assessing hydrogeologic and geochemical characteristics of the regional aquifer system.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934152","usgsCitation":"Westjohn, D.B., Weaver, T.L., and Zacharias, K., 1994, Hydrogeology of Pleistocene glacial deposits and Jurassic \"red beds\" in the central lower peninsula of Michigan: U.S. Geological Survey Water-Resources Investigations Report 93-4152, iii, 14 p., https://doi.org/10.3133/wri934152.","productDescription":"iii, 14 p.","costCenters":[],"links":[{"id":359552,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4152/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4152/report-thumb.jpg"}],"country":"United States","state":"Michigan","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db62513d","contributors":{"authors":[{"text":"Westjohn, David B.","contributorId":84401,"corporation":false,"usgs":true,"family":"Westjohn","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":203288,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weaver, Thomas L. tlweaver@usgs.gov","contributorId":2392,"corporation":false,"usgs":true,"family":"Weaver","given":"Thomas","email":"tlweaver@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":203286,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zacharias, K.F.","contributorId":83168,"corporation":false,"usgs":true,"family":"Zacharias","given":"K.F.","email":"","affiliations":[],"preferred":false,"id":203287,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":54461,"text":"wdrCO932 - 1994 - Water Resources Data, Colorado, Water Year 1993. Volume 2. Colorado River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:11:37","indexId":"wdrCO932","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CO-93-2","title":"Water Resources Data, Colorado, Water Year 1993. Volume 2. Colorado River Basin","language":"ENGLISH","doi":"10.3133/wdrCO932","usgsCitation":"Ugland, R., Cochran, B., Hiner, M., and Wilson, E., 1994, Water Resources Data, Colorado, Water Year 1993. Volume 2. Colorado River Basin: U.S. Geological Survey Water Data Report CO-93-2, 404 p., https://doi.org/10.3133/wdrCO932.","productDescription":"404 p.","costCenters":[],"links":[{"id":100383,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1993/co-93-2/report.pdf","size":"27482","linkFileType":{"id":1,"text":"pdf"}},{"id":177266,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1993/co-93-2/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbe2d","contributors":{"authors":[{"text":"Ugland, R.C.","contributorId":14044,"corporation":false,"usgs":true,"family":"Ugland","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":250450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cochran, B.J.","contributorId":75999,"corporation":false,"usgs":true,"family":"Cochran","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":250452,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hiner, M.M.","contributorId":28659,"corporation":false,"usgs":true,"family":"Hiner","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":250451,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, E.A.","contributorId":92334,"corporation":false,"usgs":true,"family":"Wilson","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":250453,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26886,"text":"wri944136 - 1994 - Ground-water levels and directions of flow near the Industrial Excess Landfill, Uniontown, Ohio, March 1994","interactions":[],"lastModifiedDate":"2018-04-12T12:33:03","indexId":"wri944136","displayToPublicDate":"1994-01-01T00:00:00","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":"94-4136","title":"Ground-water levels and directions of flow near the Industrial Excess Landfill, Uniontown, Ohio, March 1994","docAbstract":"<p>Industrial Excess Landfill (IEL), a U.S. Environmental Protection Agency Superfund site, is a closed landfill in northeastern Ohio. In March 1994, personnel from the U.S. Geological Survey, Ohio Environmental Protection Agency, and PRC Environmental Management, Inc., measured water levels in 149 wells in the area. Surface-water altitudes were measured at 13 staff gages, and water levels were measured in 9 piezometers associated with the gages. The data show that the regional pattern of ground-water flow generally is from east to west, but it is locally altered by ground-water mounds that reflect the hummocky terrain. At the landfill, regional flow is altered by two ground-water mounds one in the southeastern corner of the site and one just to the north. The relatively small ground-water mound at the landfill causes ground water to flow radially away from the southeastern corner of the landfill. Ground water that flows to the east and south flows toward Metzger Ditch, whereas flow to the west is consistent with the regional direction of ground-water flow. Ground-water flow northward from IEL is diverted east or west by the southerly component of flow from the larger ground-water mound north of IEL. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944136","usgsCitation":"Dumouchelle, D.H., and Bair, E.S., 1994, Ground-water levels and directions of flow near the Industrial Excess Landfill, Uniontown, Ohio, March 1994: U.S. Geological Survey Water-Resources Investigations Report 94-4136, Report: iv, 17 p.; 3 Plates: 25.74 x 26.48 inches or smaller, https://doi.org/10.3133/wri944136.","productDescription":"Report: iv, 17 p.; 3 Plates: 25.74 x 26.48 inches or smaller","costCenters":[],"links":[{"id":353354,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4136/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353355,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4136/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":353356,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4136/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55777,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4136/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124183,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4136/report-thumb.jpg"}],"country":"United States","state":"Ohio","city":"Uniontown","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.41361111,\n              40.96527778\n            ],\n            [\n              -81.39916667,\n              40.96527778\n            ],\n            [\n              -81.39916667,\n              40.97916667\n            ],\n            [\n              -81.41361111,\n              40.97916667\n            ],\n            [\n              -81.41361111,\n              40.96527778\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668ed3","contributors":{"authors":[{"text":"Dumouchelle, Denise H. ddumouch@usgs.gov","contributorId":1847,"corporation":false,"usgs":true,"family":"Dumouchelle","given":"Denise","email":"ddumouch@usgs.gov","middleInitial":"H.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":197187,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bair, E. Scott","contributorId":194772,"corporation":false,"usgs":false,"family":"Bair","given":"E.","email":"","middleInitial":"Scott","affiliations":[],"preferred":false,"id":197186,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30349,"text":"wri934213 - 1994 - Methods for estimating streamflow at mountain fronts in southern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri934213","displayToPublicDate":"1994-01-01T00:00:00","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":"93-4213","title":"Methods for estimating streamflow at mountain fronts in southern New Mexico","docAbstract":"The infiltration of streamflow is potential recharge to alluvial-basin aquifers at or near mountain fronts in southern New Mexico. Data for 13 streamflow-gaging stations were used to determine a relation between mean annual stream- flow and basin and climatic conditions. Regression analysis was used to develop an equation that can be used to estimate mean annual streamflow on the basis of drainage areas and mean annual precipi- tation. The average standard error of estimate for this equation is 46 percent. Regression analysis also was used to develop an equation to estimate mean annual streamflow on the basis of active- channel width. Measurements of the width of active channels were determined for 6 of the 13 gaging stations. The average standard error of estimate for this relation is 29 percent. Stream- flow estimates made using a regression equation based on channel geometry are considered more reliable than estimates made from an equation based on regional relations of basin and climatic conditions. The sample size used to develop these relations was small, however, and the reported standard error of estimate may not represent that of the entire population. Active-channel-width measurements were made at 23 ungaged sites along the Rio Grande upstream from Elephant Butte Reservoir. Data for additional sites would be needed for a more comprehensive assessment of mean annual streamflow in southern New Mexico.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934213","usgsCitation":"Waltemeyer, S., 1994, Methods for estimating streamflow at mountain fronts in southern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 93-4213, iv, 17 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934213.","productDescription":"iv, 17 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4213/report-thumb.jpg"},{"id":59140,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4213/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a4dd","contributors":{"authors":[{"text":"Waltemeyer, S. D.","contributorId":65857,"corporation":false,"usgs":true,"family":"Waltemeyer","given":"S. D.","affiliations":[],"preferred":false,"id":203099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27534,"text":"wri944011 - 1994 - Hydrogeologic framework and preliminary simulation of ground-water flow in the Mimbres Basin, southwestern New Mexico","interactions":[],"lastModifiedDate":"2022-01-05T22:46:01.698594","indexId":"wri944011","displayToPublicDate":"1994-01-01T00:00:00","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":"94-4011","title":"Hydrogeologic framework and preliminary simulation of ground-water flow in the Mimbres Basin, southwestern New Mexico","docAbstract":"<p>The bolson-fill aquifer, the major water-yielding unit in the Mimbres Basin, southwestern New Mexico, ranges in thickness from 0 to about 3,700 feet. Recharge to the bolson-fill aquifer occurs by infiltration of ephemeral streams that cross the basin margin, infiltration from precipitation and streamflow, ground-water underflow from adjacent basins, and infiltration of springflow from adjacent bedrock units within the basin. Ground water generally flows southward from the northern highland areas of the basin. Ground-water discharge consists of pumpage from wells, transpiration by plants, outflow to playas and springs in the Los Muertos Basin in Mexico, discharge to the Mimbres River, and ground-water flow to the Mesilla Basin near Mason Draw. Before 1910, ground-water recharge and discharge were approximately equal; by 1975, however, about 75 percent of the 146,000 acre-feet withdrawn annually was ground water, most of it from aquifer storage. </p><p>The transmissivity of the bolson-fill aquifer determined from aquifer tests and specific-capacity data ranges from 10 to 50,000 feet squared per day. Hydraulic conductivity, calculated from saturated thickness and transmissivity, ranges from 0.03 to 800 feet per day, with median values of about 18 feet per day in the Deming area and 6 feet per day elsewhere. Reported storage-coefficient values representing confined parts of the aquifer range from 0.00036 to 0.0036, and those representing unconfined parts of the aquifer range from 0.02 to 0.24. </p><p>Water quality in the north and central parts of the Mimbres Basin is suitable for most uses. Due to its large salinity and alkalinity, some of the ground water in the south and southeastern areas of the bolson-fill aquifer may not be suitable for irrigation or domestic use. </p><p>A preliminary two-dimensional digital model was constructed to evaluate ground-water flow in the bolson-fill aquifer. The model was divided into zones of uniform hydraulic conductivity corresponding to the major structural elements of the basin. For simulation purposes, hydraulic conductivity in the central part of the basin ranged from 2.2 to 4.4 feet per day, whereas locally along the edges of the aquifer less certain values ranged from 0.003 to 62 feet per day Analysis of the results of this predevelopment model indicated that use of the mountain-front recharge method overestimates total recharge and that evapotranspiration is substantial. The simulated total inflow was about 55 percent of that estimated in a water budget for the Mimbres Basin.</p><p>Ground-water development between 1930 and 1985 was simulated using storage-coefficient values of 0.01 and 0.02 for the Gila Conglomerate, 0.04 to 0.17 for bolson-fill deposits, and 0.001 for bolson fill capped with lacustrine clay. The simulated transient water budget indicated that most of the water pumped by 1985 came from storage, and lesser but substantial amounts came from reductions in evapotranspiration.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944011","collaboration":"Prepared in cooperation with the New Mexico State Engineer Office","usgsCitation":"Hanson, R.T., McLean, J., and Miller, R.S., 1994, Hydrogeologic framework and preliminary simulation of ground-water flow in the Mimbres Basin, southwestern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 94-4011, Report: viii, 118 p.; 2 Plates: 25.71 x 41.06 inches and 24.73 x 32.84 inches, https://doi.org/10.3133/wri944011.","productDescription":"Report: viii, 118 p.; 2 Plates: 25.71 x 41.06 inches and 24.73 x 32.84 inches","costCenters":[],"links":[{"id":393947,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47924.htm"},{"id":56393,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4011/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4011/report-thumb.jpg"},{"id":351629,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4011/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":351628,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4011/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"New Mexico","otherGeospatial":"Mimbres Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.5,\n              31.75\n            ],\n            [\n              -107,\n              31.75\n            ],\n            [\n              -107,\n              33.25\n            ],\n            [\n              -108.5,\n              33.25\n            ],\n            [\n              -108.5,\n              31.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627b59","contributors":{"authors":[{"text":"Hanson, R. T.","contributorId":91148,"corporation":false,"usgs":true,"family":"Hanson","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":198275,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McLean, J. S.","contributorId":48589,"corporation":false,"usgs":true,"family":"McLean","given":"J. S.","affiliations":[],"preferred":false,"id":198273,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, Ryan S.","contributorId":49005,"corporation":false,"usgs":false,"family":"Miller","given":"Ryan","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":198274,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4854,"text":"ds13 - 1994 - International phase of ocean drilling: Seismic Line 1 demultiplexed data, Cape Hatteras to Mid-Atlantic Ridge","interactions":[],"lastModifiedDate":"2024-03-19T14:56:34.297583","indexId":"ds13","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"13","title":"International phase of ocean drilling: Seismic Line 1 demultiplexed data, Cape Hatteras to Mid-Atlantic Ridge","docAbstract":"<h1>Introduction</h1><p>This CD-ROM is part of a 39 disc collection containing the demultiplexed seismic data from a 3400 km-long multichannel seismic-reflection profile extending from Cape Hatteras, N.C., to the rift valley of the Mid-Atlantic Ridge. The data were collected in 1974 as part of the International Phase of Ocean Drilling (IPOD) which was jointly funded by the U.S. Geological Survey (USGS) and the National Science Foundation's Deep Sea Drilling Project (DSDP).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds13","isbn":"0607624302","usgsCitation":"Zihlman, F.N., Abston, C., Taylor, D.J., Agena, W., and Oliver, H.L., 1994, International phase of ocean drilling: Seismic Line 1 demultiplexed data, Cape Hatteras to Mid-Atlantic Ridge: U.S. Geological Survey Data Series 13, Document: 165 p.; Raw Data: CD-ROM, https://doi.org/10.3133/ds13.","productDescription":"Document: 165 p.; Raw Data: CD-ROM","costCenters":[],"links":[{"id":363274,"rank":3,"type":{"id":19,"text":"Raw Data"},"url":"https://pubs.usgs.gov/dds/dds13/index.html","text":"International Phase of Ocean Drilling Seismic Line 1 Demultiplexed Data Cape Hatteras to Mid-Atlantic Ridge","linkFileType":{"id":5,"text":"html"}},{"id":354482,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds13/ds13.pdf","text":"Report","size":"215 KB","linkFileType":{"id":1,"text":"pdf"},"description":"DS 13"},{"id":139942,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76,24.318055555555556 ], [ -76,35 ], [ -64,35 ], [ -64,24.318055555555556 ], [ -76,24.318055555555556 ] ] ] } } ] }","contact":"<p><a href=\"https://woodshole.er.usgs.gov/\" data-mce-href=\"https://woodshole.er.usgs.gov/\">Coastal and Marine Geology Program</a><br> U.S. Geological Survey<br> 384 Woods Hole Road<br> Woods Hole, MA 02543</p>","tableOfContents":"<ul><li>Readme</li><li>Introduction&nbsp;<br></li><li>DOS&nbsp;Software Installation</li><li>Minimal System Requirements</li><li>Disclaimer</li><li>Documentation Files Explanation</li><li>Data</li><li>Oblogs</li><li>Navigation</li><li>Software</li><li>Acknowledgments</li><li>References</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e089b","contributors":{"authors":[{"text":"Zihlman, F. N.","contributorId":16819,"corporation":false,"usgs":true,"family":"Zihlman","given":"F.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":149945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abston, C. C.","contributorId":30617,"corporation":false,"usgs":true,"family":"Abston","given":"C. C.","affiliations":[],"preferred":false,"id":149946,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, D. J.","contributorId":50849,"corporation":false,"usgs":true,"family":"Taylor","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":149947,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Agena, Warren F.","contributorId":67079,"corporation":false,"usgs":true,"family":"Agena","given":"Warren F.","affiliations":[],"preferred":false,"id":149948,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Oliver, H. L.","contributorId":87130,"corporation":false,"usgs":true,"family":"Oliver","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":149949,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70135099,"text":"70135099 - 1994 - Large-scale deformation related to the collision of the Aleutian Arc with Kamchatka","interactions":[],"lastModifiedDate":"2021-01-15T21:49:55.594288","indexId":"70135099","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3524,"text":"Tectonics","active":true,"publicationSubtype":{"id":10}},"title":"Large-scale deformation related to the collision of the Aleutian Arc with Kamchatka","docAbstract":"<p><span>The far western Aleutian Island Arc is actively colliding with Kamchatka. Westward motion of the Aleutian Arc is brought about by the tangential relative motion of the Pacific plate transferred to major, right-lateral shear zones north and south of the arc. Early geologic mapping of Cape Kamchatka (a promontory of Kamchatka along strike with the Aleutian Arc) revealed many similarities to the geology of the Aleutian Islands. Later studies support the notion that Cape Kamchatka is the farthest west Aleutian &ldquo;island&rdquo; and that it has been accreted to Kamchatka by the process of arc-continent collision. Deformation associated with the collision onshore Kamchatka includes gravimetrically determined crustal thickening and formation of a narrow thrust belt of intensely deformed rocks directly west of Cape Kamchatka. The trend of the thrust faults is concave toward the collision zone, indicating a radial distribution of maximum horizontal compressive stress. Offshore, major crustal faults trend either oblique to the Kamchatka margin or parallel to major Aleutian shear zones. These offshore faults are complex, accommodating both strike-slip and thrust displacements as documented by focal mechanisms and seismic reflection data. Earthquake activity is much higher in the offshore region within a zone bounded to the north by the northernmost Aleutian shear zone and to the west by an apparent aseismic front. Analysis of focal mechanisms in the region indicate that the present-day arc-continent &ldquo;contact zone&rdquo; is located directly east of Cape Kamchatka. In modeling the dynamics of the collision zone using thin viscous sheet theory, the rheological parameters are only partially constrained to values of&nbsp;</span><i>n</i><span>&nbsp;(the effective power law exponent) &ge; 3 and&nbsp;</span><i>Ar</i><span>(the Argand number) &le; 30. These values are consistent with a forearc thermal profile of Kamchatka, previously determined from heat flow modeling. The thin viscous sheet modeling also indicates that onshore thrust faulting is a consequence, not only of compressive stresses resulting from the west directed collision, but also of sediment-induced coupling of the subducting Pacific plate.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/94TC00428","usgsCitation":"Geist, E.L., and Scholl, D.W., 1994, Large-scale deformation related to the collision of the Aleutian Arc with Kamchatka: Tectonics, v. 13, no. 3, p. 538-560, https://doi.org/10.1029/94TC00428.","productDescription":"23 p.","startPage":"538","endPage":"560","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":296534,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Russia","otherGeospatial":"Kamchatka Peninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              164.3115234375,\n              62.2679226294176\n            ],\n            [\n              154.8193359375,\n              56.80087831233043\n            ],\n            [\n              154.3359375,\n              49.03786794532644\n            ],\n            [\n              164.3994140625,\n              55.7765730186677\n            ],\n            [\n              164.3115234375,\n              62.2679226294176\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","issue":"3","noUsgsAuthors":false,"publicationDate":"2010-07-26","publicationStatus":"PW","scienceBaseUri":"54882b57e4b02acb4f0c8c3b","contributors":{"authors":[{"text":"Geist, Eric L. 0000-0003-0611-1150","orcid":"https://orcid.org/0000-0003-0611-1150","contributorId":15543,"corporation":false,"usgs":true,"family":"Geist","given":"Eric","email":"","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":526826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scholl, David W. 0000-0001-6500-6962 dscholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6500-6962","contributorId":3738,"corporation":false,"usgs":true,"family":"Scholl","given":"David","email":"dscholl@usgs.gov","middleInitial":"W.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":526827,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4884,"text":"ds18A - 1994 - National geochemical data base: National uranium resource evaluation data for the conterminous United States","interactions":[],"lastModifiedDate":"2024-11-15T14:22:23.183742","indexId":"ds18A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"18","chapter":"A","title":"National geochemical data base: National uranium resource evaluation data for the conterminous United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds18A","issn":"1088-1018","isbn":"0607624345","usgsCitation":"Hoffman, J.D., Buttleman, K.P., MAPPER display software by Ambroziak, R.A., and MAPPER 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,{"id":20662,"text":"ofr94152 - 1994 - Geologic features of the sea bottom around a municipal sludge dumpsite near 39 degrees N., 73 degrees W., offshore New Jersey and New York","interactions":[],"lastModifiedDate":"2022-09-20T20:54:07.768688","indexId":"ofr94152","displayToPublicDate":"1994-01-01T00:00:00","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":"94-152","title":"Geologic features of the sea bottom around a municipal sludge dumpsite near 39 degrees N., 73 degrees W., offshore New Jersey and New York","docAbstract":"The sea-floor of a dumpsite area offshore New York and New Jersey (Deep-water dumpsite 106) was studied using detailed bathymetry, sidescan-sonar images, subbottom profiles, bottom photographs, and bottom-sediment samples. These data show that this continental rise area contains deposits of submarine landslides and pathways of sediment gravity flows. Images of the sea floor obtained with a deep-towed high-resolution sidescan sonar system show offshore-trending furrowed surfaces over parts of the area. If such furrows are old, one might expect them to have been obliterated by sediment resuspension and redeposition due to the mostly gentle contour-parallel bottom currents that are measured in the present day. While most of the sea-floor features were probably formed during Pleistocene or early Holocene (glacial or early post-glacial) times, our information suggests that vigorous present-day episodes of offshore-directed transport may continue to occur, at unknown intervals.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94152","usgsCitation":"Robb, J.M., 1994, Geologic features of the sea bottom around a municipal sludge dumpsite near 39 degrees N., 73 degrees W., offshore New Jersey and New York (Online version 1.0): U.S. Geological Survey Open-File Report 94-152, 42 p., https://doi.org/10.3133/ofr94152.","productDescription":"42 p.","costCenters":[],"links":[{"id":407092,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12464.htm","linkFileType":{"id":5,"text":"html"}},{"id":50188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0152/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":1140,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/of94-152/","linkFileType":{"id":5,"text":"html"}},{"id":154015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0152/report-thumb.jpg"}],"country":"United States","state":"New Jersey, New York","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.25,\n              38.5833\n            ],\n            [\n              -71.833,\n              38.5833\n            ],\n            [\n              -71.833,\n              39.167\n            ],\n            [\n              -73.25,\n              39.167\n            ],\n            [\n              -73.25,\n              38.5833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Online version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a605a","contributors":{"authors":[{"text":"Robb, James M.","contributorId":60225,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":183022,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29158,"text":"wri934141 - 1994 - Water resources of Hot Springs County, Wyoming","interactions":[],"lastModifiedDate":"2017-12-14T09:17:42","indexId":"wri934141","displayToPublicDate":"1994-01-01T00:00:00","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":"93-4141","title":"Water resources of Hot Springs County, Wyoming","docAbstract":"<p>The wells and springs inventoried in Hot Springs County most commonly had been completed in or issued from the Quaternary alluvium, Quaternary terrace deposits, Fort Union and Mesaverde Formations, Cody Shale, and the Frontier and Chugwater Formations. The largest discharges measured were from the Quaternary terrace deposits (400 gallons per minute) and the Phosphoria Formation (1,000 gallons per minute). Discharges from all other geologic units varied, but most wells and springs yielded 50 gallons per minute or less.</p><p>Water-quality samples collected from springs that issued from the Absaroka Volcanic Supergroup, the Bighorn Dolomite, and the Flathead Sandstone had the lowest dissolved-solids concentrations, which ranged from 58 to 265 milligrams per liter, and the least variable water types. Water from the volcanic rocks was a sodium bicarbonate type; whereas, water from the Flathead Sandstone was a calcium bicarbonate type. Water types for all the other aquifers varied from sampling site to sampling site; however, water samples from the Fort Union Formation and the Cody Shale were consistently of the sodium sulfate type. </p><p>The effect of oil- and gas-development at Hamilton Dome on thermal spring discharges at Hot Springs State Park near Thermopolis was studied. The estimated drawdown from 1918, when the Hamilton Dome oil field was discovered, to 1988 was made using drill-stem data from previous studies. Drawdown at Big Spring in the Park was estimated to be less than 3 feet on the basis of recent oil- and water-production data, previous modeling studies, and the estimated water-level drawdown of 330 feet in wells at the Hamilton Dome oil field.</p><p>Streams originating in the Plains region of the county, such as Middle Fork Owl Creek, are ephemeral or intermittent; whereas, streams originating in the mountains, such as Gooseberry Creek, are perennial. Average annual runoff across the county ranges from 0.26 inches at a representative streamflow-gaging station near Worland in the plains region to 5.4 inches in the Owl Creek Mountains and southeastern Absaroka Range.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934141","usgsCitation":"Plafcan, M., and Ogle, K.M., 1994, Water resources of Hot Springs County, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 93-4141, Report: v, 90 p.; 2 Plates: 16.50 x 26.44 inches and 25.78 x 17.71 inches, https://doi.org/10.3133/wri934141.","productDescription":"Report: v, 90 p.; 2 Plates: 16.50 x 26.44 inches and 25.78 x 17.71 inches","costCenters":[],"links":[{"id":349978,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4141/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58034,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4141/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58035,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4141/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159178,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4141/report-thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Hot Springs County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {\n        \"stroke\": \"#555555\",\n        \"stroke-width\": 2,\n        \"stroke-opacity\": 1,\n        \"fill\": \"#555555\",\n        \"fill-opacity\": 0.5\n      },\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.36065673828125,\n              43.42898792344155\n            ],\n            [\n              -107.61383056640625,\n              43.42898792344155\n            ],\n            [\n              -107.61383056640625,\n              44.10336537791152\n            ],\n            [\n              -109.36065673828125,\n              44.10336537791152\n            ],\n            [\n              -109.36065673828125,\n              43.42898792344155\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ac70","contributors":{"authors":[{"text":"Plafcan, Maria","contributorId":20338,"corporation":false,"usgs":true,"family":"Plafcan","given":"Maria","email":"","affiliations":[],"preferred":false,"id":201050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ogle, Kathy Muller","contributorId":8896,"corporation":false,"usgs":true,"family":"Ogle","given":"Kathy","email":"","middleInitial":"Muller","affiliations":[],"preferred":false,"id":201051,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28994,"text":"wri944044 - 1994 - Analysis of the results of hydraulic-fracture stimulation of two crystalline bedrock boreholes, Grand Portage, Minnesota","interactions":[],"lastModifiedDate":"2019-12-08T13:45:43","indexId":"wri944044","displayToPublicDate":"1994-01-01T00:00:00","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":"94-4044","title":"Analysis of the results of hydraulic-fracture stimulation of two crystalline bedrock boreholes, Grand Portage, Minnesota","docAbstract":"Hydraulic fracture-stimulation procedures typical of those provided by contractors in the water-well industry were applied to two boreholes in basaltic and gabbroic rocks near Grand Portage, Minnesota.These boreholes were considered incapable of supplying adequate ground water for even a single household although geophysical logs showed both boreholes were intersected by many apparently permeable fractures. Tests made before and after stimulation indicated that the two boreholes would produce about 0.05 and 0.25 gallon per minute before stimulation, and about 1.5 and 1.2 gallons per minute after stimulation. These increases would be enough to obtain adequate domestic water supplies from the two boreholes but would not furnish enough water for more than a single household from either borehole. Profiles of high-resolution flow made during pumping after stimulation indicated that the stimulation enhanced previously small inflows or stimulated new inflow from seven fractures or fracture zones in one borehole and from six fractures or fracture zones in the other.Geophysical logs obtained after stimulation showed no specific changes in these 13 fractures that could be related to stimulation other than the increases in flow indicated by the flowmeter logs. The results indicate that the stimulation has increased inflow to the two boreholes by improving the connectivity of favorably orientated fractures with larger scale flow zones in the surrounding rocks. Three of four possible diagnostics related to measured pressure and flow during the stimulation treatments were weakly correlated with the increases in production associated with each treatment interval. These correlations are not statistically significant on the basis of the limited sample of 16 treatment intervals in two boreholes, but the results indicate that significant correlations might be established from a much larger data set.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri944044","usgsCitation":"Paillet, F.L., and Olson, J.D., 1994, Analysis of the results of hydraulic-fracture stimulation of two crystalline bedrock boreholes, Grand Portage, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 94-4044, vi, 45 p., https://doi.org/10.3133/wri944044.","productDescription":"vi, 45 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":95740,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4044/report.pdf","size":"4377","linkFileType":{"id":1,"text":"pdf"}},{"id":159176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4044/report-thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Grand Portage","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.62663650512694,\n              47.97084701460957\n            ],\n            [\n              -89.51608657836914,\n              47.97084701460957\n            ],\n            [\n              -89.51608657836914,\n              48.01978346615275\n            ],\n            [\n              -89.62663650512694,\n              48.01978346615275\n            ],\n            [\n              -89.62663650512694,\n              47.97084701460957\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680065","contributors":{"authors":[{"text":"Paillet, Fredrick L.","contributorId":78780,"corporation":false,"usgs":true,"family":"Paillet","given":"Fredrick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, James D.","contributorId":34969,"corporation":false,"usgs":true,"family":"Olson","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":200751,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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