{"pageNumber":"1321","pageRowStart":"33000","pageSize":"25","recordCount":46734,"records":[{"id":23591,"text":"ofr95506 - 1995 - Structure of the basins and ranges, Southwest New Mexico, an interpretation of seismic velocity sections","interactions":[],"lastModifiedDate":"2018-10-30T12:43:13","indexId":"ofr95506","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","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":"95-506","title":"Structure of the basins and ranges, Southwest New Mexico, an interpretation of seismic velocity sections","docAbstract":"<p>This report presents a geologic appraisal of seismic velocity sections that profile a total of 790 km in southwest New Mexico west of Las Cruces and south of Lordsburg and Deming. The present work outlines the contribution of these velocity sections to estimating areas favorable for mineral resource occurrences. Seismic refraction surveys are carried out with the initial goal of estimating the subsurface distribution of acoustic compressional velocity (Vp), which may ultimately be interpreted to provide information on lithology, geologic structure, and the occurrence of natural resources. The seismic sections presented here show velocity detail having dimensions of 100's to 1000's of meters to a depth of about 2.5 km, and across a net of traverses that profile most basins well as several ranges in the study area.</p><p>Figure 1 shows the location of the seismic refraction lines. The lines are designated 1, 2, 3, 4, 5, and 7; there is no line 6. The survey covers a broad swath of the southwest Basin and Range Province extending from the Arizona border eastward to the Rio Grande River, and from the Mexican border to about lat. 32° 30' N. Lines 1, 3, and 7 traverse the axis of basins in roughly northsouth directions; the remaining lines 2, 4, and 5 trend east-west and cross various ranges and basins.</p><p>Seismic data that have been collected in this region include deep-crustal refraction traverses by university scientists and commercial seismic reflection profiles acquired for petroleum exploration. Results of deep-crustal refraction studies are reviewed to provide a regional setting for the higher resolution refraction data. Results from seismic reflection will not be discussed. Industry reflection data in the area are not generally available for non-proprietary use. The nearest reflection data publicly available are in the Socorro area, about 80 km north of the present study area (Brown and others, 1980). These data were acquired by the Consortium for Continental Reflection Profiling (COCORP), a public-supported research group, to investigate the possibility of magma beneath part of the Rio Grande valley.</p><p>Up to 1978 there were about 36 deep borings in the region of southwest New Mexico (Thompson and others, 1978). This drilling resulted mainly from an evaluation of petroleum potential of the Pedrogosa basin which is an extensive area of Paleozoic subsidence in Arizona, New Mexico, and Mexico that accumulated about three kilometers of Paleozoic sedimentary rock (Zeller, 1965; Thompson and others, 1978). Of these drill holes, 25 are close enough to the present seismic sections to provide correlations of velocity to lithology, and to provide an estimate of the errors associated with depth-to-interface interpretations. This information is summarized prior to considering the implications of the seismic sections in detail. The major portion of the report centers around two plates: Plate I shows seismic lines and selected drill hole locations superimposed on gravity contours, and Plate II shows velocitysections with drill hole summaries. These plates provide the foundation for developing inferences on buried lithologic, structural, and mineral resources for the region. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95506","issn":"0094-9140","usgsCitation":"Klein, D.P., Abrams, G.A., and Hill, P.L., 1995, Structure of the basins and ranges, Southwest New Mexico, an interpretation of seismic velocity sections: U.S. Geological Survey Open-File Report 95-506, Report: v, 60 p.; 2 Plates: 48.12 x 25.60 inches and 36.96 x 22.82 inches, https://doi.org/10.3133/ofr95506.","productDescription":"Report: v, 60 p.; 2 Plates: 48.12 x 25.60 inches and 36.96 x 22.82 inches","costCenters":[],"links":[{"id":358946,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0506/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0506/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0506/report-thumb.jpg"},{"id":358945,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0506/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"New Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.1,\n              31.3\n            ],\n            [\n              -106.4,\n              31.3\n            ],\n            [\n              -106.4,\n              32.5\n            ],\n            [\n              -109.1,\n              32.5\n            ],\n            [\n              -109.1,\n              31.3\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c178","contributors":{"authors":[{"text":"Klein, Douglas P.","contributorId":50896,"corporation":false,"usgs":true,"family":"Klein","given":"Douglas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":190373,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abrams, Gerda A.","contributorId":78706,"corporation":false,"usgs":true,"family":"Abrams","given":"Gerda","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":190374,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hill, Patricia L. pathill@usgs.gov","contributorId":1327,"corporation":false,"usgs":true,"family":"Hill","given":"Patricia","email":"pathill@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":190372,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":21399,"text":"ofr95360 - 1995 - Description of geophysical-log data base for boreholes and wells in and adjacent to the Albuquerque Basin, New Mexico","interactions":[],"lastModifiedDate":"2022-11-01T18:55:14.423194","indexId":"ofr95360","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","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":"95-360","title":"Description of geophysical-log data base for boreholes and wells in and adjacent to the Albuquerque Basin, New Mexico","docAbstract":"Digital geophysical logs for boreholes and wells in and \r\nadjacent to the Albuquerque Basin area have been entered into a \r\ndata base established by the New Mexico District of the U.S. \r\nGeological Survey and documented as of September 1994. The logs \r\nwere digitized from paper or mylar copies or were collected as \r\ndigital data during the logging of boreholes and wells. The \r\nlocation of these boreholes and wells with digital geophysical \r\nlogs is shown in a map. The 1,020 logs and the types of logs for\r\nthe 186 sites are listed in a table.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95360","usgsCitation":"Wilkins, D.W., 1995, Description of geophysical-log data base for boreholes and wells in and adjacent to the Albuquerque Basin, New Mexico: U.S. Geological Survey Open-File Report 95-360, iv, 16 p., https://doi.org/10.3133/ofr95360.","productDescription":"iv, 16 p.","costCenters":[],"links":[{"id":50968,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0360/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409005,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18459.htm","linkFileType":{"id":5,"text":"html"}},{"id":154193,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0360/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Albuquerque Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.5,\n              35.75\n            ],\n            [\n              -107.5,\n              34.25\n            ],\n            [\n              -106,\n              34.25\n            ],\n            [\n              -106,\n              35.75\n            ],\n            [\n              -107.5,\n              35.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3da1","contributors":{"authors":[{"text":"Wilkins, D. W.","contributorId":97471,"corporation":false,"usgs":true,"family":"Wilkins","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":184358,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21096,"text":"ofr95379 - 1995 - Inventory of biological investigations related to stream water quality in the South Platte River basin, Colorado, Nebraska, and Wyoming, 1891-1994","interactions":[],"lastModifiedDate":"2012-02-02T00:07:53","indexId":"ofr95379","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","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":"95-379","title":"Inventory of biological investigations related to stream water quality in the South Platte River basin, Colorado, Nebraska, and Wyoming, 1891-1994","docAbstract":"An inventory of the biological investigations conducted in the South Platte River Basin from 1891 to 1994 was done as a part of the U.S. Geological Survey's National Water-Quality Assessment (NAWQA) program in the South Platte River Basin. To aid in the sampling design of the biological component of the South Platte NAWQA, sources of water-related studies were compiled from computerized literature searches of biological data bases and by contacting other Federal, State, and local agencies. Biological investigations were categorized by their location in either of two major physiographic provinces-the Southern Rocky Mountains or the Great Plains, or in the transition zone between the mountains and the plains. From this collection of 102 references, five general categories of biological investigations were identified:  algae, invertebrates, fish, habitat characterization, and chemicals in organism tissue. The most abundant literature was on studies of invertebrate and fish communities. Invertebrate studies primarily were conducted in the mountain region. There was limited information on algae, invertebrates in the plains region, flood-plain vegetation in the mountains and transition zone, and chemicals in organism tissue.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95379","usgsCitation":"Tate, C.M., and Ortiz-Zayas, J.R., 1995, Inventory of biological investigations related to stream water quality in the South Platte River basin, Colorado, Nebraska, and Wyoming, 1891-1994: U.S. Geological Survey Open-File Report 95-379, iii, 12 p. ill., map ;28 cm., https://doi.org/10.3133/ofr95379.","productDescription":"iii, 12 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":154549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0379/report-thumb.jpg"},{"id":19375,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0379/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64865a","contributors":{"authors":[{"text":"Tate, Cathy M. cmtate@usgs.gov","contributorId":3438,"corporation":false,"usgs":true,"family":"Tate","given":"Cathy","email":"cmtate@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":183831,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ortiz-Zayas, Jorge R.","contributorId":81932,"corporation":false,"usgs":true,"family":"Ortiz-Zayas","given":"Jorge","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":183832,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17511,"text":"ofr95567 - 1995 - Preliminary digital geologic map database of the Nevada Test Site area, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr95567","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","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":"95-567","title":"Preliminary digital geologic map database of the Nevada Test Site area, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95567","usgsCitation":"Sawyer, D.A., Wahl, R.R., Cole, J.C., Minor, S., Laczniak, R.J., Warren, R., Engle, C.M., and Vega, R., 1995, Preliminary digital geologic map database of the Nevada Test Site area, Nevada: U.S. Geological Survey Open-File Report 95-567, 62 p. ill. ;28 cm. +1 map (col., photocopy ; 75 x 78 cm., on sheet 92 x 142 cm.), https://doi.org/10.3133/ofr95567.","productDescription":"62 p. ill. ;28 cm. +1 map (col., photocopy ; 75 x 78 cm., on sheet 92 x 142 cm.)","costCenters":[],"links":[{"id":1063,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr-95-0567/","linkFileType":{"id":5,"text":"html"}},{"id":149411,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0567/report-thumb.jpg"},{"id":46660,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0567/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4d8","contributors":{"authors":[{"text":"Sawyer, David A. dsawyer@usgs.gov","contributorId":1262,"corporation":false,"usgs":true,"family":"Sawyer","given":"David","email":"dsawyer@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":176666,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wahl, R. R.","contributorId":27462,"corporation":false,"usgs":true,"family":"Wahl","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":176668,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cole, J. C.","contributorId":51292,"corporation":false,"usgs":true,"family":"Cole","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":176670,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minor, S.A.","contributorId":65047,"corporation":false,"usgs":true,"family":"Minor","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":176671,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Laczniak, R. J.","contributorId":46104,"corporation":false,"usgs":true,"family":"Laczniak","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":176669,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Warren, R.G.","contributorId":6037,"corporation":false,"usgs":true,"family":"Warren","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":176667,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Engle, C. M.","contributorId":91880,"corporation":false,"usgs":true,"family":"Engle","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":176673,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Vega, R.G.","contributorId":76323,"corporation":false,"usgs":true,"family":"Vega","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":176672,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":21507,"text":"ofr95357 - 1995 - Data on ground-water levels and ground-water/surface-water relations in the Great Miami River and Little Miami River valleys, southwestern Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:07:49","indexId":"ofr95357","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","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":"95-357","title":"Data on ground-water levels and ground-water/surface-water relations in the Great Miami River and Little Miami River valleys, southwestern Ohio","docAbstract":"Hydrogeologic data were collected in September, October, and November 1993 to define the ground-water levels and the ground-water/surface-water relations in the vicinity of Dayton, Ohio. In this report, water levels are listed for 678 wells completed in sand and gravel. Data from 101 streamflow measurements made at selected sites along the Great Miami, Stillwater, Mad, and Little Miami Rivers and their tributaries during 2-day gain-loss study also are listed. Surface-water altitudes were determined at 11 stream-gaging stations and 39 other streamflow measurement sites. Discharge data for measurements made at 30 storm-sewer outfalls are given. Streamflow and discharge data obtained during the study were used to calculate the gain or loss of streamflow along 16 selected reaches of the Great Miami, Stillwater, Mad, and Little Miami Rivers. Streambed-conductivity data obtained by use of seepage meters at nine different sites also are given.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Sciences Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95357","usgsCitation":"Yost, W.P., 1995, Data on ground-water levels and ground-water/surface-water relations in the Great Miami River and Little Miami River valleys, southwestern Ohio: U.S. Geological Survey Open-File Report 95-357, iv, 63 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr95357.","productDescription":"iv, 63 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":153765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0357/report-thumb.jpg"},{"id":51080,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0357/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c852","contributors":{"authors":[{"text":"Yost, William P.","contributorId":57093,"corporation":false,"usgs":true,"family":"Yost","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":184561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33117,"text":"b1988K - 1995 - Summary of chemical analyses and 40Ar/39Ar age-spectra data for Eocene volcanic rocks from the central part of the Northeast Nevada volcanic field","interactions":[{"subject":{"id":33117,"text":"b1988K - 1995 - Summary of chemical analyses and 40Ar/39Ar age-spectra data for Eocene volcanic rocks from the central part of the Northeast Nevada volcanic field","indexId":"b1988K","publicationYear":"1995","noYear":false,"chapter":"K","title":"Summary of chemical analyses and 40Ar/39Ar age-spectra data for Eocene volcanic rocks from the central part of the Northeast Nevada volcanic field"},"predicate":"IS_PART_OF","object":{"id":33239,"text":"b1988 - 1992 - Evolution of sedimentary basins: Eastern Great Basin","indexId":"b1988","publicationYear":"1992","noYear":false,"title":"Evolution of sedimentary basins: Eastern Great Basin"},"id":1}],"isPartOf":{"id":33239,"text":"b1988 - 1992 - Evolution of sedimentary basins: Eastern Great Basin","indexId":"b1988","publicationYear":"1992","noYear":false,"title":"Evolution of sedimentary basins: Eastern Great Basin"},"lastModifiedDate":"2017-08-09T13:57:33","indexId":"b1988K","displayToPublicDate":"1995-12-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1988","chapter":"K","title":"Summary of chemical analyses and 40Ar/39Ar age-spectra data for Eocene volcanic rocks from the central part of the Northeast Nevada volcanic field","language":"ENGLISH","doi":"10.3133/b1988K","usgsCitation":"Brooks, W.E., Thorman, C.H., Snee, L., Nutt, C.J., Potter, C.J., and Dubiel, R.F., 1995, Summary of chemical analyses and 40Ar/39Ar age-spectra data for Eocene volcanic rocks from the central part of the Northeast Nevada volcanic field: U.S. Geological Survey Bulletin 1988, p. K1-K33, illus. incl. sect., 7 tables, geol. sketch maps, 43 refs, https://doi.org/10.3133/b1988K.","productDescription":"p. K1-K33, illus. incl. sect., 7 tables, geol. sketch maps, 43 refs","costCenters":[],"links":[{"id":161430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1988k/report-thumb.jpg"},{"id":60918,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1988k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69936f","contributors":{"authors":[{"text":"Brooks, William E.","contributorId":104061,"corporation":false,"usgs":true,"family":"Brooks","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":209934,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thorman, Charles H. cthorman@usgs.gov","contributorId":254,"corporation":false,"usgs":false,"family":"Thorman","given":"Charles","email":"cthorman@usgs.gov","middleInitial":"H.","affiliations":[{"id":7065,"text":"USGS emeritus","active":true,"usgs":false}],"preferred":false,"id":209929,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snee, Lawrence W.","contributorId":81534,"corporation":false,"usgs":true,"family":"Snee","given":"Lawrence W.","affiliations":[],"preferred":false,"id":209933,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nutt, Constance J. cnutt@usgs.gov","contributorId":1781,"corporation":false,"usgs":true,"family":"Nutt","given":"Constance","email":"cnutt@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":209932,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Potter, Christopher J. 0000-0002-2300-6670 cpotter@usgs.gov","orcid":"https://orcid.org/0000-0002-2300-6670","contributorId":1026,"corporation":false,"usgs":true,"family":"Potter","given":"Christopher","email":"cpotter@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":209930,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dubiel, Russell F. 0000-0002-1280-0350 rdubiel@usgs.gov","orcid":"https://orcid.org/0000-0002-1280-0350","contributorId":1294,"corporation":false,"usgs":true,"family":"Dubiel","given":"Russell","email":"rdubiel@usgs.gov","middleInitial":"F.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":209931,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70216585,"text":"70216585 - 1995 - Effects of a 2 x CO2 climate on two large lake systems: Pyramid Lake, Nevada, and Yellowstone Lake, Wyoming","interactions":[],"lastModifiedDate":"2020-11-27T18:26:13.210991","indexId":"70216585","displayToPublicDate":"1995-11-25T13:28:55","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1844,"text":"Global and Planetary Change","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Effects of a 2 × CO<sub>2</sub> climate on two large lake systems: Pyramid Lake, Nevada, and Yellowstone Lake, Wyoming","title":"Effects of a 2 x CO2 climate on two large lake systems: Pyramid Lake, Nevada, and Yellowstone Lake, Wyoming","docAbstract":"<p>The possible effects of trace-gas induced climatic changes on Pyramid and Yellowstone Lakes are assessed using a model of lake temperature. The model is driven by<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>3</mtext><mtext>1</mtext><mtext>2</mtext></math>\"><span class=\"MJX_Assistive_MathML\">312</span></span></span><span>&nbsp;</span>years of hourly meteorological data obtained directly from the output of double-CO<sub>2</sub><span>&nbsp;</span>experiments (2 × CO<sub>2</sub>) conducted with a regional climate model nested in a general circulation model. The regional atmospheric model is the climate version of the National Center for Atmospheric Research/Pennsylvania State University mesoscale model, MM4.</p><p>Average annual surface temperature of Pyramid Lake for the 2 × CO<sub>2</sub><span>&nbsp;</span>climate is 15.5 ± 5.4°C (±1 σ), 2.8°C higher than the control. Annual overturn of the lake ceases as a result of these higher temperatures for the 2 × CO<sub>2</sub><span>&nbsp;</span>climate. Evaporation increases from 1400 mm yr<sup>−1</sup><span>&nbsp;</span>in the control to 1595 mm yr<sup>−1</sup><span>&nbsp;</span>in the 2 × CO<sub>2</sub><span>&nbsp;</span>simulation, but net water supplied to the Pyramid Lake basin increases from −6 mm yr<sup>−1</sup><span>&nbsp;</span>in the control to +27 mm yr<sup>−1</sup><span>&nbsp;</span>in the 2 × CO<sub>2</sub><span>&nbsp;</span>simulation due to increased precipitation.</p><p>For the open water periods, the average annual surface temperature of Yellowstone Lake is 13.2 ± 5.1°C for the 2 × CO<sub>2</sub><span>&nbsp;</span>climate, a temperature 1.6°C higher than the control. The annual duration of ice cover on the lake is 152 days in the 2 × CO<sub>2</sub><span>&nbsp;</span>simulation, a reduction of 44 days relative to the control. Warming of the lake for the 2 × CO<sub>2</sub><span>&nbsp;</span>climate is mostly confined to the near-surface. Simulated spring overturn for the 2 × CO<sub>2</sub><span>&nbsp;</span>climate occurs earlier in the year and fall overturn later than in the control. Evaporation increases from 544 mm yr<sup>−1</sup><span>&nbsp;</span>to 600 mm yr<sup>−1</sup><span>&nbsp;</span>in the 2 × CO<sub>2</sub><span>&nbsp;</span>simulation, but net water supplied to the Yellowstone Lake basin increases from +373 mm yr<sup>−1</sup><span>&nbsp;</span>in the control to +619 mm yr<sup>−1</sup><span>&nbsp;</span>due to increased precipitation. The effects of these climatic changes suggest possible deterioration of water quality and productivity in Pyramid Lake and possible enhancement of productivity in Yellowstone Lake.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0921-8181(94)00019-A","usgsCitation":"Hostetler, S.W., and Giorgino, M.L., 1995, Effects of a 2 x CO2 climate on two large lake systems: Pyramid Lake, Nevada, and Yellowstone Lake, Wyoming: Global and Planetary Change, v. 10, no. 1, p. 43-54, https://doi.org/10.1016/0921-8181(94)00019-A.","productDescription":"12 p.","startPage":"43","endPage":"54","costCenters":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":380812,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada, Wyoming","otherGeospatial":"Pyramid Lake, Nevada, and Yellowstone Lake, Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.8004150390625,\n              39.79376521264885\n            ],\n            [\n              -119.278564453125,\n              39.79376521264885\n            ],\n            [\n              -119.278564453125,\n              40.23550866893913\n            ],\n            [\n              -119.8004150390625,\n              40.23550866893913\n            ],\n            [\n              -119.8004150390625,\n              39.79376521264885\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.64056396484375,\n              44.21764696919354\n            ],\n            [\n              -110.10772705078125,\n              44.21764696919354\n            ],\n            [\n              -110.10772705078125,\n              44.63543682256858\n            ],\n            [\n              -110.64056396484375,\n              44.63543682256858\n            ],\n            [\n              -110.64056396484375,\n              44.21764696919354\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hostetler, S. W. 0000-0003-2272-8302","orcid":"https://orcid.org/0000-0003-2272-8302","contributorId":42911,"corporation":false,"usgs":true,"family":"Hostetler","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":805687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Giorgino, Mary L. giorgino@usgs.gov","contributorId":2242,"corporation":false,"usgs":true,"family":"Giorgino","given":"Mary","email":"giorgino@usgs.gov","middleInitial":"L.","affiliations":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":805688,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70246360,"text":"70246360 - 1995 - Fault healing inferred from time dependent variations in source properties of repeating earthquakes","interactions":[],"lastModifiedDate":"2023-07-06T12:26:39.165471","indexId":"70246360","displayToPublicDate":"1995-11-15T06:56:47","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Fault healing inferred from time dependent variations in source properties of repeating earthquakes","docAbstract":"<p><span>We analyze two sets of repeating earthquakes on the Calaveras fault to estimate in-situ rates of fault strengthening (healing). Earthquake recurrence intervals&nbsp;</span><i>t<sub>r</sub></i><span>&nbsp;range from 3 to 803 days. Variations in relative moment and duration are combined to study changes in stress drop, rupture dimension, rupture velocity, and particle velocity as a function of&nbsp;</span><i>t<sub>r</sub></i><span>. Healing rates and source variations are compared with predictions of laboratory-derived friction laws. Two interpretations of event duration τ are used: one in which τ is given by the ratio of slip to particle velocity and one in which it scales as rupture dimension divided by rupture velocity. Our data indicate that faults strengthen during the interseismic period. We infer that source dimension decreases with&nbsp;</span><i>t<sub>r</sub></i><span>&nbsp;due to aseismic creep within the region surrounding the repeating events. Stress drop increases 1–3MPa per decade increase in&nbsp;</span><i>t<sub>r</sub></i><span>, which represents an increase of a factor of 2–3 relative to events with&nbsp;</span><i>t<sub>r</sub></i><span>&nbsp;between 10 and 100 days. This rate of fault healing is consistent with extrapolations of laboratory measurements of healing rates if fault strength is high, on order of 60MPa, and stress drop is roughly 10% of this value.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95GL03076","usgsCitation":"Marone, C., Vidale, J.E., and Ellsworth, W.L., 1995, Fault healing inferred from time dependent variations in source properties of repeating earthquakes: Geophysical Research Letters, v. 22, no. 22, p. 3095-3098, https://doi.org/10.1029/95GL03076.","productDescription":"4 p.","startPage":"3095","endPage":"3098","costCenters":[],"links":[{"id":418706,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Calaveras Fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.4052173911836,\n              36.689160402516464\n            ],\n            [\n              -121.0187556020827,\n              36.689160402516464\n            ],\n            [\n              -121.0187556020827,\n              37.40239566504556\n            ],\n            [\n              -122.4052173911836,\n              37.40239566504556\n            ],\n            [\n              -122.4052173911836,\n              36.689160402516464\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"22","issue":"22","noUsgsAuthors":false,"publicationDate":"2012-12-07","publicationStatus":"PW","contributors":{"authors":[{"text":"Marone, Chris","contributorId":7426,"corporation":false,"usgs":false,"family":"Marone","given":"Chris","email":"","affiliations":[],"preferred":false,"id":876962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vidale, John E.","contributorId":48850,"corporation":false,"usgs":true,"family":"Vidale","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":876963,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellsworth, William L. ellsworth@usgs.gov","contributorId":787,"corporation":false,"usgs":true,"family":"Ellsworth","given":"William","email":"ellsworth@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":876964,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70048798,"text":"70048798 - 1995 - Historical Landsat data comparisons: illustrations of the Earth's changing surface","interactions":[],"lastModifiedDate":"2014-06-02T05:49:32","indexId":"70048798","displayToPublicDate":"1995-11-05T15:45:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Historical Landsat data comparisons: illustrations of the Earth's changing surface","docAbstract":"<p>The U.S. Geological Survey's (USGS) EROS Data Center (EDC) has managed the Landsat data archive for more than two decades. This archive provides a rich collection of information about the Earth's land surface. Major changes to the surface of the planet can be detected, measured, and analyzed using Landsat data. The effects of desertification, deforestation, pollution, cataclysmic volcanic activity, and other natural and anthropogenic events can be examined using data acquired from the Landsat series of Earth-observing satellites. The information obtainable from the historical and current Landsat data play a key role in studying surface changes through time.</p>\n<br/>\n<p>This document provides an overview of the Landsat program and illustrates the application of the data to monitor changes occurring on the surface of the Earth. To reveal changes that have taken place within the past 20 years, pairs and triplicates of images were constructed from the Landsat multispectral scanner (MSS) and thematic mapper (TM) sensors. Landsat MSS data provide a historical record of the Earth's land surface from the early 1970's to the early 1990's. Landsat TM data provide land surface information from the early 1980's to the present.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70048798","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Historical Landsat data comparisons: illustrations of the Earth's changing surface, 45 p., https://doi.org/10.3133/70048798.","productDescription":"45 p.","numberOfPages":"48","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":287916,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287915,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70048798/report.pdf"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -180.0,-90.0 ], [ -180.0,90.0 ], [ 180.0,90.0 ], [ 180.0,-90.0 ], [ -180.0,-90.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"527a2187e4b051792d019547","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27557,"text":"wri954052 - 1995 - Estimated natural ground-water recharge, discharge, and budget for the Dixie Valley area, west-central Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri954052","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-4052","title":"Estimated natural ground-water recharge, discharge, and budget for the Dixie Valley area, west-central Nevada","docAbstract":"The Dixie Valley area includes seven valleys in west-central Nevada (Dixie, Fairview, Stingaree, Cowkick, Eastgate, Pleasant, and Jersey Valleys; total, 2,380 square miles). Dixie Valley receives surface-water and ground-water flow from Stingaree, Cowkick, Eastgate, Pleasant, and Jersey Valleys and subsurface flow from Fairview Valley, which is a topographically closed basin.  The relation between precipitation and altitude was re-evaluated for the Dixie Valley area using new data, and empirical estimates of recharge were revised accordingly. The revised estimate of total recharge is 23,000 acre-feet per  Re-evaluation of ground-water discharge focused on Dixie Valley as the largest basin in the study area. Phreatophytic vegetation was mapped and partitioned into nine zones on the basis of species composition and foliage density. For woody phreatophytes, annual evapotranspiration rates of 0.7 cubic feet of water per cubic foot of foliage for greasewood and 1.1 cubic feet of water per cubic foot of foliage for rabbitbrush were adapted from lysimeter studies near Winnemucca, Nevada. These rates were multiplied by the foliage density of the respective phreatophytes in each zone to estimate a specific rate for that zone. Rates for salt-grass (0.5 to 0.8 foot per year) and the playa surface (0.1 to 0.3 foot per year) were based on a range of rates. used in other recent studies in western and central Nevada. These rates were multiplied by the areas of the zones to produce estimates of the annual volume of ground water discharged. The discharge estimated for Dixie Valley is between 17,000 and 28,000 acre-feet per year. The revised discharge estimate for the entire Dixie Valley area is between 20,000 and 31,000 acre-feet per year.  The revised ground-water budget for the entire Dixie Valley study area has a total recharge of about 23,000 acre-feet per year. This is within the range of estimates of natural discharge--from 20,000 to 31,000 acre-feet per year. For Dixie Valley alone, the total recharge of about 8,900 acre-feet per year and the estimated subsurface inflow from tributary areas of about 11,000 acre-feet per year produce an estimated total inflow of about 20,000 acre-feet per year. This compares with the discharge estimate of 17,000 to 28,000 acre-feet per year.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Information Services [distributor],","doi":"10.3133/wri954052","usgsCitation":"Harrill, J., and Hines, L., 1995, Estimated natural ground-water recharge, discharge, and budget for the Dixie Valley area, west-central Nevada: U.S. Geological Survey Water-Resources Investigations Report 95-4052, iv, 12 p. :ill., col. map ;28 cm., https://doi.org/10.3133/wri954052.","productDescription":"iv, 12 p. :ill., col. map ;28 cm.","costCenters":[],"links":[{"id":123547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4052/report-thumb.jpg"},{"id":56414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a0fc","contributors":{"authors":[{"text":"Harrill, J. R.","contributorId":10417,"corporation":false,"usgs":true,"family":"Harrill","given":"J. R.","affiliations":[],"preferred":false,"id":198319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hines, L.B.","contributorId":49406,"corporation":false,"usgs":true,"family":"Hines","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":198320,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23180,"text":"ofr95623 - 1995 - Digital release of stream-sediment, heavy-mineral-concentrate, and other geochemical data collected in the McCarthy 1 degree x 3 degrees Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2013-09-17T15:07:16","indexId":"ofr95623","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-623","title":"Digital release of stream-sediment, heavy-mineral-concentrate, and other geochemical data collected in the McCarthy 1 degree x 3 degrees Quadrangle, Alaska","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr95623","issn":"0094-9140","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"George, S., 1995, Digital release of stream-sediment, heavy-mineral-concentrate, and other geochemical data collected in the McCarthy 1 degree x 3 degrees Quadrangle, Alaska: U.S. Geological Survey Open-File Report 95-623, 1 computer disk ;3 1/2 in. +1 text (11 p. ; 28 cm.), https://doi.org/10.3133/ofr95623.","productDescription":"1 computer disk ;3 1/2 in. +1 text (11 p. ; 28 cm.)","costCenters":[],"links":[{"id":154964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0623/report-thumb.jpg"},{"id":52502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0623/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":277689,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1995/0623/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a8b5","contributors":{"authors":[{"text":"George, S.L.","contributorId":45342,"corporation":false,"usgs":true,"family":"George","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":189592,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20819,"text":"ofr94711W - 1995 - Hydrologic data from the lower Cedar River Basin, Iowa, 1989-91","interactions":[],"lastModifiedDate":"2019-12-08T13:11:21","indexId":"ofr94711W","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"94-711","chapter":"W","title":"Hydrologic data from the lower Cedar River Basin, Iowa, 1989-91","docAbstract":"<p>Hydrologic data were collected from May 1989 through July 1991 from the Cedar River and the adjacent alluvial aquifer. The data were collected during various flow regimes of the river to evaluate the movement of agricultural chemicals between surface water and ground water. Water-quality samples from 34 surface-water sites and 95 ground-water sites were analyzed for 11 herbicides, 2 dealkylated atrazine metabolites, and nitrate. Specific conductance, pH, water temperature, and dissolved oxygen were measured at the time of sampling. Discharge and water-quality data from two seepage investigations were collected to identify gaining and losing reaches of the river and to help delineate where agricultural chemicals enter the river. Ancillary data on ground-water levels and river stage also were collected.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr94711W","usgsCitation":"Schulmeyer, P., Barnes, K., and Squillace, P.J., 1995, Hydrologic data from the lower Cedar River Basin, Iowa, 1989-91: U.S. Geological Survey Open-File Report 94-711, iv, 116 p., https://doi.org/10.3133/ofr94711W.","productDescription":"iv, 116 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":50401,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0711w/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153390,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0711w/report-thumb.jpg"}],"country":"United States","state":"Iowa","otherGeospatial":"Lower Cedar River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.34857177734375,\n              41.37474755643594\n            ],\n            [\n              -91.329345703125,\n              41.33763822308113\n            ],\n            [\n              -91.241455078125,\n              41.29431726315258\n            ],\n            [\n              -91.16455078125,\n              41.279870545327114\n            ],\n            [\n              -91.14257812499999,\n              41.335575973123895\n            ],\n            [\n              -91.08489990234375,\n              41.395354710280166\n            ],\n            [\n              -91.03271484375,\n              41.45301999377133\n            ],\n         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-91.5216064453125,\n              41.52297326747377\n            ],\n            [\n              -91.49414062499999,\n              41.413895564677304\n            ],\n            [\n              -91.42822265625,\n              41.380930388318\n            ],\n            [\n              -91.34857177734375,\n              41.37474755643594\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607725","contributors":{"authors":[{"text":"Schulmeyer, P.M.","contributorId":17208,"corporation":false,"usgs":true,"family":"Schulmeyer","given":"P.M.","affiliations":[],"preferred":false,"id":183307,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, K.K.","contributorId":99164,"corporation":false,"usgs":true,"family":"Barnes","given":"K.K.","email":"","affiliations":[],"preferred":false,"id":183308,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Squillace, P. J.","contributorId":8878,"corporation":false,"usgs":true,"family":"Squillace","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":183306,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23183,"text":"ofr95625 - 1995 - Digital release of stream-sediment, heavy-mineral-concentrate, soil, and other geochemical data collected in the Nabesna 1 degree x 3 degrees Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2013-09-17T15:05:21","indexId":"ofr95625","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-625","title":"Digital release of stream-sediment, heavy-mineral-concentrate, soil, and other geochemical data collected in the Nabesna 1 degree x 3 degrees Quadrangle, Alaska","language":"ENGLISH","publisher":"U.S. Department of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr95625","issn":"0094-9140","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"George, S., 1995, Digital release of stream-sediment, heavy-mineral-concentrate, soil, and other geochemical data collected in the Nabesna 1 degree x 3 degrees Quadrangle, Alaska: U.S. Geological Survey Open-File Report 95-625, 1 computer disk ;3 1/2 in. +1 text (10 p. ; 28 cm.), https://doi.org/10.3133/ofr95625.","productDescription":"1 computer disk ;3 1/2 in. +1 text (10 p. ; 28 cm.)","costCenters":[],"links":[{"id":156069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0625/report-thumb.jpg"},{"id":52505,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0625/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":277685,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1995/0625/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a5b6","contributors":{"authors":[{"text":"George, S.L.","contributorId":45342,"corporation":false,"usgs":true,"family":"George","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":189595,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27131,"text":"wri954085 - 1995 - User's manual for ANNIE, version 2, a computer program for interactive hydrologic data management","interactions":[],"lastModifiedDate":"2012-02-02T00:08:41","indexId":"wri954085","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-4085","title":"User's manual for ANNIE, version 2, a computer program for interactive hydrologic data management","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954085","usgsCitation":"Flynn, K., Hummel, P., Lumb, A., and Kittle, J., 1995, User's manual for ANNIE, version 2, a computer program for interactive hydrologic data management: U.S. Geological Survey Water-Resources Investigations Report 95-4085, iv, 211 p. :ill. ;28 cm., https://doi.org/10.3133/wri954085.","productDescription":"iv, 211 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":158734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4085/report-thumb.jpg"},{"id":55991,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4085/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603deb","contributors":{"authors":[{"text":"Flynn, K.M.","contributorId":57503,"corporation":false,"usgs":true,"family":"Flynn","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":197605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hummel, P.R.","contributorId":73642,"corporation":false,"usgs":true,"family":"Hummel","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":197607,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lumb, A.M.","contributorId":70019,"corporation":false,"usgs":true,"family":"Lumb","given":"A.M.","affiliations":[],"preferred":false,"id":197606,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kittle, J.L. Jr.","contributorId":89574,"corporation":false,"usgs":true,"family":"Kittle","given":"J.L.","suffix":"Jr.","affiliations":[],"preferred":false,"id":197608,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":19941,"text":"ofr94506 - 1995 - Pesticides in the atmosphere; distribution, trends, and governing factors","interactions":[],"lastModifiedDate":"2013-05-22T15:26:15","indexId":"ofr94506","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"94-506","title":"Pesticides in the atmosphere; distribution, trends, and governing factors","docAbstract":"A comprehensive review of existing literature on the occurrence and distribution of pesticides in the atmosphere of the United States and adjoining Canadian provinces showed that the atmosphere is an important part of the hydrologic cycle that acts to distribute and deposit pesticides in areas far removed from their application sites. A compilation of existing data shows that pesticides have been detected in the atmosphere throughout the nation. Most of the available information on pesticides in the atmosphere is from small-scale, short-term studies that seldom lasted more than one year. Only two national-scale, multi-year studies were done since the late 1960's that analyzed for a wide variety of pesticides in air that were in current use at the time. Another large-scale study was done during 1990-91, but was limited to the midwestern and northeastern United States and only analyzed for two classes of herbicides in wet deposition. Most of the pesticides analyzed for were detected in either air or rain, and represent about 25 percent of the total number of insecticides, herbicides, and fungicides in current use. The geographical distribution of studies, and the type of sampling and analysis were highly variable with most of the historical study efforts concentrated in the Great Lakes area and California. Air and rain were the main atmospheric matrices sampled, but pesticides were also detected in fog and snow. Reported pesticide concentrations in air and rain were frequently positively correlated to their regional agricultural use. Deviations from this relation could usually be explained by non-agricultural use of pesticides, sampling and analytical difficulties, and environmental persistence. High concentrations of locally used pesticides were found to occur seasonally, usually in conjunction with spring planting of row crops and warm temperatures, but high concentrations also occurred during winter months in those areas where dormant orchards were sprayed. The environmentally more persistent pesticides were detected in the atmosphere at low concen- trations throughout the year. Deposition of airborne pesticides can have significant effects on water quality, but neither the nature of nor the magnitude of these effects can be determined with certainty on the basis of the type of data currently available. The lack of consistent, long-term regional and national monitoring and study of pesticides in atmospheric matrices severely limits assessment capability.","language":"ENGLISH","publisher":"U.S. Geological Survey ;Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94506","usgsCitation":"Majewski, M.S., and Capel, P.D., 1995, Pesticides in the atmosphere; distribution, trends, and governing factors: U.S. Geological Survey Open-File Report 94-506, xiii, 191 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94506.","productDescription":"xiii, 191 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0506/report-thumb.jpg"},{"id":272568,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0506/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697904","contributors":{"authors":[{"text":"Majewski, Michael S. majewski@usgs.gov","contributorId":440,"corporation":false,"usgs":true,"family":"Majewski","given":"Michael","email":"majewski@usgs.gov","middleInitial":"S.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":181770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Capel, Paul D. 0000-0003-1620-5185 capel@usgs.gov","orcid":"https://orcid.org/0000-0003-1620-5185","contributorId":1002,"corporation":false,"usgs":true,"family":"Capel","given":"Paul","email":"capel@usgs.gov","middleInitial":"D.","affiliations":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":181771,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18383,"text":"ofr95519 - 1995 - Use and presentation of Magellan quantitative data in Venus mapping","interactions":[],"lastModifiedDate":"2012-02-02T00:07:33","indexId":"ofr95519","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-519","title":"Use and presentation of Magellan quantitative data in Venus mapping","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95519","usgsCitation":"Campbell, B.A., 1995, Use and presentation of Magellan quantitative data in Venus mapping: U.S. Geological Survey Open-File Report 95-519, iv, 32 p. ill. ;28 cm., https://doi.org/10.3133/ofr95519.","productDescription":"iv, 32 p. ill. ;28 cm.","costCenters":[],"links":[{"id":151491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0519/report-thumb.jpg"},{"id":47728,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0519/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6051f8","contributors":{"authors":[{"text":"Campbell, Bruce A.","contributorId":39813,"corporation":false,"usgs":true,"family":"Campbell","given":"Bruce","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179023,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19683,"text":"ofr95305 - 1995 - Hydrologic data for the Usquepaug-Queen River basin, Rhode Island","interactions":[],"lastModifiedDate":"2012-02-02T00:07:38","indexId":"ofr95305","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-305","title":"Hydrologic data for the Usquepaug-Queen River basin, Rhode Island","docAbstract":"The Usquepaug-Queen River ground-water reservoir in Rhode Island is part of the stratified-drift aquifer along the Usquepaug-Queen River and its tributaries. The thickest, most permeable parts of the aquifer form the Usquepaug-Queen River ground-water reservoir. The 36.1-square mile study area comprises parts of Washington and Kent counties, and includes parts of the towns of Exeter, North Kingstown, Richmond, South Kingstown, and West Greenwich. The report presents geologic and hydrologic information needed for the prediction and management of hydrologic effects of proposed ground-water development. The report describes aquifer lithology, provides historical data on water-level and aquifer-storage changes, provides information on ground-water quality, and presents natural flow characteristics and water quality of streams in the Usquepaug-Queen River area. The data includes 275 ground-water sites; lithologic logs of 66 ground-water sites; water levels for 43 ground- water sites; chemical analyses of 36 ground-water sites; stream discharge measurements from the continuous-record gaging station on the Usquepaug- Queen River; discharge measurements at 10 partial- record stations in the area; chemical analyses of 17 stream sites; and the data from 14 slug tests conducted at ground-water sites.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95305","usgsCitation":"Kliever, J.D., 1995, Hydrologic data for the Usquepaug-Queen River basin, Rhode Island: U.S. Geological Survey Open-File Report 95-305, iv, 68 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr95305.","productDescription":"iv, 68 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":152427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0305/report-thumb.jpg"},{"id":19361,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0305/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49166,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0305/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db608204","contributors":{"authors":[{"text":"Kliever, John D.","contributorId":46976,"corporation":false,"usgs":true,"family":"Kliever","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":181328,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16948,"text":"ofr95514 - 1995 - Cerro Prieto geothermal field, Mexico; chemical analyses and other data for 58 samples collected in 1977-1979","interactions":[],"lastModifiedDate":"2019-06-05T08:03:38","indexId":"ofr95514","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-514","title":"Cerro Prieto geothermal field, Mexico; chemical analyses and other data for 58 samples collected in 1977-1979","docAbstract":"<p>This report releases the results of selected chemical analyses by the USGS of fluids collected from geothennal power production wells at the Cerro Prieto Geothennal Field, Mexico. Cerro Prieto, the world's largest producing hot-water geothennal field, is located 32 km southeast of Mexicali, Baja California. Comision Federal de Electricidad de Mexico (CFE) gave permission for, and assisted in, sample collection. Data collection and reported analyses was made by the U.S. Geological Survey. Data collected in 1977 and 1978 where published previously by Ball and Jenne (1983) which was about half the data given here. This report also includes samples collected in 1979 which were not previously released. These activities, including this data release, are supported by the U.S. Department of Energy.</p><p>Analyses given in the following section were made by James W. Ball and E.A. Jenne. The data have been reviewed with the assistance of Cathy Janik, USGS, Menlo Park. Some, but not all, details from Ball and Jenne (1983) concerning collection, and preservation and analytical procedures are repeated here. Nehring and Trusdell (1977) also provide an outline of some of the issues involved in the difficult task of collecting samples from geothermal wells. The initial intent of the study was to provide basic data for use in determining how these fluids should be managed either in disposal or in reinjection. Some of the hot, corrosive brines were separated as two-phase (water and steam) samples under pressure using a coiled condenser tube submerged in an ice/water mixture (called \"condensed\" samples). It is not known if these were total flow samples. Other samples were collected from the brine sampling valve of the separators (called \"flashed\" samples). Analyses given in the following section area sorted by (1) well number, (2) date, and (3) sample type(s).</p><p>Analysis was by a Spectraspan III d.c. argon plasma emission spectrometer with a Spectraject III torch (Ball and Jenne, 1983). Elements were determined in two groups using interchangeable cassettes. Group one included B, Mn, Cu, Zn, Si, Zr, Be, Mn, Sr, Ti, Ca, Fe, Ba, K, Na, Rb, and Al. Group two included As, Se, Bi, Zn, Cd, Sb, Cu, Ni, Hg, Mo, Co, Cr, Fe, V, Tl, Li, and Pb. Ball and Jenne (1983) noted that analysis of B, Ca, Mg, Ba, and Sr generally gave precise results. Movement of the plasma or grating was observed to affect sensitivity over short time periods even while the instrument was carefully standardized and optimized. Sensitivity was also a function of sample concentration. All samples at the time of analysis contained a white precipitate (perhaps colloidal silica) thus the reported concentrations may not accurately represent the concentrations present at the time of collection (Ball and Jenne, 1983). Additional details about specific elements are given in the section on \"Evaluation of data\" (Bliss, this volume) following the data table.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95514","usgsCitation":"1995, Cerro Prieto geothermal field, Mexico; chemical analyses and other data for 58 samples collected in 1977-1979: U.S. Geological Survey Open-File Report 95-514, iii, 75 p., https://doi.org/10.3133/ofr95514.","productDescription":"iii, 75 p.","numberOfPages":"78","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":150231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0514/report-thumb.jpg"},{"id":46057,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0514/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6e5f","contributors":{"editors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":759394,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":18017,"text":"ofr95142 - 1995 - Results of geophysical surveys of glacial deposits near a former waste-disposal site, Nashua, New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:07:23","indexId":"ofr95142","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-142","title":"Results of geophysical surveys of glacial deposits near a former waste-disposal site, Nashua, New Hampshire","docAbstract":"Geophysical investigations were done near a former waste-disposal site in Nashua, New Hampshire to determine the thickness and infer hydraulic characteristics of the glacial sediments that underlie the area. Approximately 5 miles of ground- penetrating radar (GPR) data were collected in the study area by use of dual-80 Megahertz antennas. Three distinct radar-reflection signatures were evident from the data and are interpreted to represent (1) glacial lake-bottom sediments, (2) coarse sand and gravel and (or) sandy glacial till, and (3) bedrock. The GPR signal penetrated as much as 70 feet of sediment in coarse-grained areas, but penetration depth was generally less than 40 feet in extensive areas of fine-grained deposits. Geologic features were evident in many of the profiles. Glacial-lake-bottom sediments were the most common features identified. Other features include deltas deposited in glacial Lake Nashua and lobate fans of sediment deposited subaqueously at the distal end of deltaic sediments. Cross-bedded sands were often identifiable in the deltaic sediments. Seismic-refraction data were also collected at five of the GPR data sites. In most cases, depths to the water table and to the till and (or) bedrock surface indicated by the seismic-refraction data compared favorably with depths calculated from the GPR data. Test holes were drilled at three locations to determine the true depths to radar reflectors and to determine the types of geologic material represented by the various reflectors.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95142","usgsCitation":"Ayotte, J., and Dorgan, T.H., 1995, Results of geophysical surveys of glacial deposits near a former waste-disposal site, Nashua, New Hampshire: U.S. Geological Survey Open-File Report 95-142, iv, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95142.","productDescription":"iv, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151230,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0142/report-thumb.jpg"},{"id":47263,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0142/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaee4b07f02db66c812","contributors":{"authors":[{"text":"Ayotte, Joseph D. jayotte@usgs.gov","contributorId":1802,"corporation":false,"usgs":true,"family":"Ayotte","given":"Joseph D.","email":"jayotte@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":178382,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dorgan, Tracy H.","contributorId":10447,"corporation":false,"usgs":true,"family":"Dorgan","given":"Tracy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":178383,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18019,"text":"ofr95363 - 1995 - Geohydrology of the Flints Pond Aquifer, Hollis, New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:07:23","indexId":"ofr95363","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-363","title":"Geohydrology of the Flints Pond Aquifer, Hollis, New Hampshire","docAbstract":"Flints pond has been subjected to accelerated eutrophication as a result of watershed development (building of new homes and conversion of summer cottages into permanent homes) since the 1930's. Ground-water flow is the primary recharge and discharge mechanism for Flints Pond. The saturated thickness, transmissive properties, and altitude of the water table were determined by use of surface geophysics, test drilling, and aquifer-test data. Information on the geohydrology of the adjacent Flints Pond aquifer can be used in developing a water and nutrient budget for the pond-aquifer system. Ground-penetrating-radar surveys were done over more than 4 miles of the study area and on Flints Pond. Three distinct reflection signatures were commonly identifiable on the radar profiles: (1) thin, relatively flat-lying, continuous reflectors that represent fine-grained lacustrine sediment; (2) subparallel to hummocky and chaotic, coarse-grained reflectors that possibly represent coarse-grained ice-contact deposits or deltaic sediments in a lacustrine environment; and (3) sharply diffracted, fine-grained, chaotic reflectors that represent till and (or) till over bedrock. The saturated thickness of the aquifer exceeds 90 feet in the northern end of the study area and averages 30 to 50 feet in the southern and eastern parts. The saturated thickness of the western part is generally less than 10 feet. Test borings were completed at 19 sites and 13 wells (6 of which were nested pairs) were installed in various lithologic units. A water-table map, constructed from data collected in November 1994, represents average water-table conditions in the aquifer. Horizontal hydraulic conductivities calculated from single-well aquifer test data for stratified drift range from 2.8 to 226 feet per day. Hydraulic conductivities were quantitatively correlated with the reflector signatures produced with ground-penetrating radar so that transmissivities could be inferred for areas where well data were unavailable but where ground- penetrating-radar surveys were done. A saturated- thickness and transmissivity map for the aquifer shows that transmissivities exceeds 3,000 feet squared per day in the southern and east-central parts of the aquifer. Transmissivity ranges from 1,000 to 2,000 feet squared per day in the northern part of the aquifer and is generally less than 1,000 feet squared per day in the western part.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95363","usgsCitation":"Ayotte, J., and Dorgan, T.H., 1995, Geohydrology of the Flints Pond Aquifer, Hollis, New Hampshire: U.S. Geological Survey Open-File Report 95-363, v, 23 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr95363.","productDescription":"v, 23 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":151252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0363/report-thumb.jpg"},{"id":47266,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0363/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89c1","contributors":{"authors":[{"text":"Ayotte, Joseph D. jayotte@usgs.gov","contributorId":1802,"corporation":false,"usgs":true,"family":"Ayotte","given":"Joseph D.","email":"jayotte@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":178385,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dorgan, Tracy H.","contributorId":10447,"corporation":false,"usgs":true,"family":"Dorgan","given":"Tracy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":178386,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16920,"text":"ofr95291 - 1995 - Benthic macrofauna data for San Francisco Bay, California, September 1986","interactions":[],"lastModifiedDate":"2020-05-01T14:34:41.168578","indexId":"ofr95291","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-291","title":"Benthic macrofauna data for San Francisco Bay, California, September 1986","docAbstract":"<p>Benthic macrofauna were collected during September 1986 to evaluate locations for long-term monitoring stations as part of the U.S. Geological Survey Regional Effects Monitoring Program in San Francisco Bay, California. Three to ten replicate samples were collected with a modified Van Veen sampler (0.05 m<sup>2</sup> area) at ten locations. One box core sample (0.06 m<sup>2</sup> area) was collected at seven to the ten locations. Six of the box core samples were split into an upper 10 cm sample and a deeper sample before analysis. Macrofauna specimens were identified to the lowest possible taxon, usually genus and species, then counted. An average of 88 percent of the benthic macrofauna specimens were identified to the species level. The fraction identified varied among stations from 54 to 98 percent. Nematodes and oligochaetes accounted for most of the unidentified specimens. Relative to the total number of species identified in five replicates at each location, an average of 90 percent of the species were collected with three replicates. In general, species with high to moderate abundances were present in all replicates, and species collected only after three or more replicates averaged less than one specimen per replicate. Results from the box cores showed that the dominant species were most abundant in the upper 10 cm, the depth of sediment that can be adequately sampled with a modified Van Veen sampler. On the basis of the number of species and their abundances at each location, seven of the ten locations were selected for sampling in the regular program, which began in March 1987.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95291","usgsCitation":"Schemel, L.E., Thompson, J., Harmon, J., and Yost, B.T., 1995, Benthic macrofauna data for San Francisco Bay, California, September 1986: U.S. Geological Survey Open-File Report 95-291, iii, 33 p. , https://doi.org/10.3133/ofr95291.","productDescription":"iii, 33 p. ","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":46032,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0291/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0291/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.98645019531249,\n              37.38761749978395\n            ],\n            [\n              -121.83288574218749,\n              37.38761749978395\n            ],\n            [\n              -121.83288574218749,\n              38.21660403859855\n            ],\n            [\n              -122.98645019531249,\n              38.21660403859855\n            ],\n            [\n              -122.98645019531249,\n              37.38761749978395\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a3ae4b07f02db61dffb","contributors":{"authors":[{"text":"Schemel, Laurence E. lschemel@usgs.gov","contributorId":4085,"corporation":false,"usgs":true,"family":"Schemel","given":"Laurence","email":"lschemel@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":174185,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, J.K.","contributorId":103300,"corporation":false,"usgs":true,"family":"Thompson","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":174188,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harmon, J.G.","contributorId":90753,"corporation":false,"usgs":true,"family":"Harmon","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":174187,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yost, B. T.","contributorId":19178,"corporation":false,"usgs":true,"family":"Yost","given":"B.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":174186,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":31735,"text":"ofr95590 - 1995 - Digital aeromagnetic anomaly data from eastern-most Guyana","interactions":[],"lastModifiedDate":"2017-11-29T08:53:54","indexId":"ofr95590","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-590","title":"Digital aeromagnetic anomaly data from eastern-most Guyana","docAbstract":"<p>The Center for Inter-American Mineral Resource Investigations (CIMRI) supported distribution and analysis of geoscientific and mineral resource related information concerning Latin America. CIMRI staff digitized aeromagnetic data for eastern-most Guyana as part of a preliminary regional assessment of minerals in the Guyana Shield, South America. The data were digitized from 145 aeromagnetic contour maps at a scale of 1:50,000 and merged into a single digital data set. The data were used to examine the Precambrian shield, greenstone belts, and other tectonic boundaries as well as explore ideas concerning mineral deposits within the area. A subset of these digital data were presented to the Guyanan government during early 1995 (Pierce, 1994). This Open-File report, consisting of this text and seven (7) 3.5\" IBM-PC compatible ASCII magnetic disks, makes the digital data available to the public. Information regarding the source of data and subsequent processing is included below. </p><p>The data were collected in Guyana by two contractors at different times. The first data were collected from 1962 to 1963. These data are several aeromagnetic surveys covering parts of 12 quadrangles funded by the United Nations and flown by Aero Service Corporation. The second and more extensive data set was collected from 1971 to 1972 by the Canadian International Development Agency flown by Terra Surveys Ltd. under a contract with the Geological Survey of Guyana. The Guyana Government published the data as contour maps that are available in Georgetown through the Guyana Government. Coverage extends from about 2°45*N to 8°30*N latitude and from 60°0'W to 57°0'W longitude (see Figure 1.). The contour maps were digitized at points where the magnetic contours intersect the flight lines. </p><p>The data files include XYZ ASCII files, XYZ binary files, ASCII grids, and binary \"standard USGS\" grids. There are four grids consisting of the following data types: </p><ul><li>unprotected raw data grid</li><li>unprotected residual or International Geomagnetic Reference Field (IGRF) removed grid</li><li>UTM projected residual (IGRF removed) grid</li><li>UTM projected residual with a second order surface removed</li></ul><p>These data files were transferred to 3.5\" 1.44 megabyte floppy disks readable on IBM-compatible personal computers. These data are also available from the Department of Commerce National Geophysical Data Center. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95590","usgsCitation":"Pierce, H.A., Backjinski, N., and Manes, J., 1995, Digital aeromagnetic anomaly data from eastern-most Guyana: U.S. Geological Survey Open-File Report 95-590, Report: 12 p.; 1 Diskette ZIP file, https://doi.org/10.3133/ofr95590.","productDescription":"Report: 12 p.; 1 Diskette ZIP file","costCenters":[],"links":[{"id":349498,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/0590/ofr95590.zip","text":"Diskette","linkFileType":{"id":6,"text":"zip"}},{"id":59954,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0590/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0590/report-thumb.jpg"}],"country":"Guyana","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d5f4","contributors":{"authors":[{"text":"Pierce, Herbert A. hpierce@usgs.gov","contributorId":5995,"corporation":false,"usgs":true,"family":"Pierce","given":"Herbert","email":"hpierce@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":false,"id":206840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Backjinski, Natalka","contributorId":14475,"corporation":false,"usgs":true,"family":"Backjinski","given":"Natalka","email":"","affiliations":[],"preferred":false,"id":206838,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manes, John-James","contributorId":35375,"corporation":false,"usgs":true,"family":"Manes","given":"John-James","email":"","affiliations":[],"preferred":false,"id":206839,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20325,"text":"ofr95281 - 1995 - Reassessment of hydrogeologic data and refinement of a regional ground-water-flow model for the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:07:34","indexId":"ofr95281","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-281","title":"Reassessment of hydrogeologic data and refinement of a regional ground-water-flow model for the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95281","usgsCitation":"Olimpio, J.R., and Harte, P.T., 1995, Reassessment of hydrogeologic data and refinement of a regional ground-water-flow model for the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire: U.S. Geological Survey Open-File Report 95-281, iv, 40 p. :maps ;28 cm., https://doi.org/10.3133/ofr95281.","productDescription":"iv, 40 p. :maps ;28 cm.","costCenters":[],"links":[{"id":152525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0281/report-thumb.jpg"},{"id":49855,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0281/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648678","contributors":{"authors":[{"text":"Olimpio, Joseph R.","contributorId":57878,"corporation":false,"usgs":true,"family":"Olimpio","given":"Joseph","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":182453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harte, Philip T. 0000-0002-7718-1204 ptharte@usgs.gov","orcid":"https://orcid.org/0000-0002-7718-1204","contributorId":1008,"corporation":false,"usgs":true,"family":"Harte","given":"Philip","email":"ptharte@usgs.gov","middleInitial":"T.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":182452,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003112,"text":"1003112 - 1995 - Applying computer simulation models as learning tools in fishery management","interactions":[],"lastModifiedDate":"2025-03-27T23:22:45.976903","indexId":"1003112","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Applying computer simulation models as learning tools in fishery management","docAbstract":"<p><span>Computer models can be powerful tools for addressing many problems in fishery management, but uncertainty about how to apply models and how they should perform can lead to a cautious approach to modeling. Within this approach, we expect models to make quantitative predictions but only after all model inputs have been estimated from empirical data and after the model has been tested for agreement with an independent data set. I review the limitations to this approach and show how models can be more useful as tools for organizing data and concepts, learning about the system to be managed, and exploring management options. Fishery management requires deciding what actions to pursue to meet management objectives. Models do not make decisions for us but can provide valuable input to the decision‐making process. When empirical data are lacking. preliminary modeling with parameters derived from other sources can help determine priorities for data collection. When evaluating models for management applications, we should attempt to define the conditions under which the model is a useful, analytical tool (its domain of applicability) and should focus on the decisions made using modeling results, rather than on quantitative model predictions. I describe an example of modeling used as a learning tool for the yellow perch&nbsp;</span><i>Perca flavescens</i><span>&nbsp;fishery in Green Bay, Lake Michigan.</span></p>","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8675(1995)015<0736:ACSMAL>2.3.CO;2","usgsCitation":"Johnson, B., 1995, Applying computer simulation models as learning tools in fishery management: North American Journal of Fisheries Management, v. 15, no. 4, p. 736-747, https://doi.org/10.1577/1548-8675(1995)015<0736:ACSMAL>2.3.CO;2.","productDescription":"12 p.","startPage":"736","endPage":"747","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":134371,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","city":"Green Bay","otherGeospatial":"Lake Michigan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -88.05690415586561,\n              44.72484196720393\n            ],\n            [\n              -88.05690415586561,\n              44.49016875094597\n            ],\n            [\n              -87.80828937178602,\n              44.49016875094597\n            ],\n            [\n              -87.80828937178602,\n              44.72484196720393\n            ],\n            [\n              -88.05690415586561,\n              44.72484196720393\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"15","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a3dc","contributors":{"authors":[{"text":"Johnson, Barry L.","contributorId":95009,"corporation":false,"usgs":true,"family":"Johnson","given":"Barry L.","affiliations":[],"preferred":false,"id":312757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18041,"text":"ofr94454 - 1995 - Simulation of hydrodynamics and solute transport in the Pamlico River estuary, North Carolina","interactions":[],"lastModifiedDate":"2017-01-04T11:19:38","indexId":"ofr94454","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"94-454","title":"Simulation of hydrodynamics and solute transport in the Pamlico River estuary, North Carolina","docAbstract":"An investigation was conducted to characterize flow, circulation, and solute transport in the Pamlico River estuary, North Carolina. The study included a detailed field-measurement program and the calibration, validation, and application of a physically realistic numerical model of hydro- dynamics and transport. Water level, salinity, water temperature, wind speed and direction, and current data were collected during March 1988 through September 1992, and were used to characterize physical conditions in the estuary. Data from pre- existing streamflow gaging stations and meteoro- logical stations were also used. A two-dimensional vertically averaged hydrodynamic and solute transport model was applied to the 48-kilometer study reach. The model domain was discretized into 5,620 separate 200- by 200-meter computational cells. Model calibration was achieved through adjustment of parameters for June 14-30, 1991. Data from selected periods in 1989 and 1991 were used for model validation. Water levels used for model calibration and validation ranged from -0.052 to 0.698 meter; salinities ranged from 0.1 to 13.1 parts per thousand; and wind speeds ranged from calm to 22 meters per second. The model was tested for stratified and unstratified conditions. Simulated and observed data were used to evaluate model performance. The calibrated model was applied for selected periods in 1989 and 1991. Instantaneous flows were simulated at each boundary and at mid- estuary. Circulation patterns were characterized using vector plots, particle tracking, and solute transport. Particle tracks showed that materials released at mid-estuary may remain in the system for 25 days or longer.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94454","usgsCitation":"Bales, J., and Robbins, J.C., 1995, Simulation of hydrodynamics and solute transport in the Pamlico River estuary, North Carolina: U.S. Geological Survey Open-File Report 94-454, vi, 85 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94454.","productDescription":"vi, 85 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":47285,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0454/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0454/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Pamlico River estuary","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.29156494140625,\n              35.137879119634185\n            ],\n            [\n              -77.29156494140625,\n              35.74205383068037\n            ],\n            [\n              -76.124267578125,\n              35.74205383068037\n            ],\n            [\n              -76.124267578125,\n              35.137879119634185\n            ],\n            [\n              -77.29156494140625,\n              35.137879119634185\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f230d","contributors":{"authors":[{"text":"Bales, Jerad","contributorId":47390,"corporation":false,"usgs":true,"family":"Bales","given":"Jerad","affiliations":[],"preferred":false,"id":178424,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robbins, Jeanne C. 0000-0001-7804-0764 jrobbins@usgs.gov","orcid":"https://orcid.org/0000-0001-7804-0764","contributorId":1586,"corporation":false,"usgs":true,"family":"Robbins","given":"Jeanne","email":"jrobbins@usgs.gov","middleInitial":"C.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":178423,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}