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The physical characteristics are the drainage area of the subbasin, the percentage area of the subbasin covered only by lakes, the percentage area of the subbasin covered by both lakes and wetlands, the main-channel length, and the main-channel slope. Stream sites include outlets of subbasins of at least 5 square miles, and locations of U.S. Geological Survey high-flow, and continuous-record gaging stations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ofr2000232","collaboration":"Prepared in cooperation with the Minnesota Department of Transportation","usgsCitation":"Sanocki, C.A., and Fischer, B.C., 2000, Physical characteristics of stream subbasins in the Long Prairie River basin, central Minnesota: U.S. Geological Survey Open-File Report 2000-232, Document: 7 p.; Plate: 38.03 x 27.01 inches, https://doi.org/10.3133/ofr2000232.","productDescription":"Document: 7 p.; Plate: 38.03 x 27.01 inches","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321487,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12211,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://mn.water.usgs.gov/publications/pubs/00-232.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":12212,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://mn.water.usgs.gov/publications/pubs/00-232-plate.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Long Prairie River basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.38330078125, 46.19266555785523 ], [ -95.37300109863281, 46.1912395780416 ], [ -95.37300109863281, 46.18458451637958 ], [ -95.36956787109375, 46.17887953650578 ], [ -95.35102844238281, 46.17364945158338 ], [ -95.34072875976562, 46.17127197581503 ], [ 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,{"id":31176,"text":"ofr00412 - 2000 - Geologic map of the Kingston Range, southern Death Valley, California","interactions":[],"lastModifiedDate":"2015-11-17T14:36:13","indexId":"ofr00412","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-412","title":"Geologic map of the Kingston Range, southern Death Valley, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr00412","usgsCitation":"Calzia, J., Troxel, B., Wright, L., Burchfiel, B., Davis, G.A., and McMackin, M., 2000, Geologic map of the Kingston Range, southern Death Valley, California: U.S. Geological Survey Open-File Report 2000-412, 2 Plates: 56.51 x 40.11 inches and 39.85 x 27.37 inches, https://doi.org/10.3133/ofr00412.","productDescription":"2 Plates: 56.51 x 40.11 inches and 39.85 x 27.37 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":161427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr00412.PNG"},{"id":311387,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2000/0412/plate-2.pdf","text":"Sheet 2","linkFileType":{"id":1,"text":"pdf"}},{"id":311386,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2000/0412/plate-1.pdf","text":"Sheet 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Death Valley, Kingston Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.378173828125,\n              35.49198366469642\n            ],\n            [\n              -116.378173828125,\n              35.93354064249312\n            ],\n            [\n              -115.4937744140625,\n              35.93354064249312\n            ],\n            [\n              -115.4937744140625,\n              35.49198366469642\n            ],\n            [\n              -116.378173828125,\n              35.49198366469642\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69745b","contributors":{"authors":[{"text":"Calzia, J.P.","contributorId":58614,"corporation":false,"usgs":true,"family":"Calzia","given":"J.P.","affiliations":[],"preferred":false,"id":205233,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troxel, B.W.","contributorId":101681,"corporation":false,"usgs":true,"family":"Troxel","given":"B.W.","email":"","affiliations":[],"preferred":false,"id":205235,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wright, L.A.","contributorId":91875,"corporation":false,"usgs":true,"family":"Wright","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":205234,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burchfiel, B.C.","contributorId":30262,"corporation":false,"usgs":true,"family":"Burchfiel","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":205230,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Davis, G. A.","contributorId":44940,"corporation":false,"usgs":true,"family":"Davis","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205231,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McMackin, M.R.","contributorId":51344,"corporation":false,"usgs":true,"family":"McMackin","given":"M.R.","affiliations":[],"preferred":false,"id":205232,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":31169,"text":"ofr00351 - 2000 - Geologic map and database of the Salem East and Turner 7.5 minute quadrangles, Marion County, Oregon: A digital database","interactions":[],"lastModifiedDate":"2022-02-01T20:18:19.696676","indexId":"ofr00351","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-351","title":"Geologic map and database of the Salem East and Turner 7.5 minute quadrangles, Marion County, Oregon: A digital database","docAbstract":"<p>The Salem East and Turner 7.5-minute quadrangles are situated in the center of the Willamette Valley near the western margin of the Columbia River Basalt Group (CRBG) distribution. The terrain within the area is of low to moderate relief, ranging from about 150 to almost 1,100-ft elevation. Mill Creek flows northward from the Stayton basin (Turner quadrangle) to the northern Willamette Valley (Salem East quadrangle) through a low that dissects the Columbia River basalt that forms the Salem Hills on the west and the Waldo Hills to the east. Approximately eight flows of CRBG form a thickness of up to 700 in these two quadrangles. The Ginkgo intracanyon flow that extends from east to west through the south half of the Turner quadrangle is exposed in the hills along the southeast part of the quadrangle.</p><p>Previous geologic mapping by Thayer (1939) and Bela (1981) while providing the general geologic framework did not subdivide the CRBG which limited their ability to delineate structural elements. Reconnaissance mapping of the CRBG units in the Willamette Valley indicated that these stratigraphic units could serve as a series of unique reference horizons for identifying post-Miocene folding and faulting (Beeson and others, 1985,1989; Beeson and Tolan, 1990). Crenna, et al. (1994) compiled previous mapping in the Willamette Valley in a study of the tectonics of the Salem area.</p><p>The major emphasis of this study was to identify and map CRBG units within the Salem East and Turner Quadrangles and to utilize this detailed CRBG stratigraphy to identify and characterize structural features. Water well logs were used to provide better subsurface stratigraphic control. Three other quadrangles (Scotts Mills, Silverton, and Stayton NE) in the Willamette Valley have been mapped in this way (Tolan and Beeson, 1999).</p><p>This area was a lowland area of weathered and eroded marine sedimentary when the Columbia River basalts encroached on this area approximately 15-16 m.y. ago. An incipient Coast Range apparently stopped or diverted the fluid lava flows from moving much farther westward toward the coast at this latitude. It is assumed also that an ancestral Willamette River flowed northward through this low-lying area so that water was present as streams and ponds along the flood plain.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr00351","usgsCitation":"Tolan, T.L., Beeson, M.H., and DuRoss, C., 2000, Geologic map and database of the Salem East and Turner 7.5 minute quadrangles, Marion County, Oregon: A digital database: U.S. Geological Survey Open-File Report 2000-351, 2 Plates: 30.93 x 35.04 inches and 31.73 x 35.20 inches; Readme, https://doi.org/10.3133/ofr00351.","productDescription":"2 Plates: 30.93 x 35.04 inches and 31.73 x 35.20 inches; Readme","additionalOnlineFiles":"Y","costCenters":[{"id":412,"text":"National Cooperative Geologic Mapping Program","active":false,"usgs":true}],"links":[{"id":161020,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr00351.gif"},{"id":2676,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/0351/","linkFileType":{"id":5,"text":"html"}},{"id":281611,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2000/0351/00351ps.tar.gz"},{"id":281612,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2000/0351/00351db.tar.gz"},{"id":281613,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2000/0351/00351db.zip"},{"id":281614,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2000/0351/pdf/README.PDF"},{"id":281610,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2000/0351/pdf/tnrfinal.pdf"},{"id":281615,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2000/0351/pdf/slmfinal.pdf"},{"id":110130,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_34045.htm","linkFileType":{"id":5,"text":"html"},"description":"34045"}],"scale":"24000","projection":"Universal Transverse Mercator projection","country":"United States","state":"Oregon","county":"Marion County","otherGeospatial":"Mill Creek, Willamette Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.0,44.75 ], [ -123.0,45.0 ], [ -122.875,45.0 ], [ -122.875,44.75 ], [ -123.0,44.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8694","contributors":{"authors":[{"text":"Tolan, Terry L.","contributorId":31029,"corporation":false,"usgs":true,"family":"Tolan","given":"Terry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":205206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beeson, Marvin H.","contributorId":67937,"corporation":false,"usgs":true,"family":"Beeson","given":"Marvin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":205208,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DuRoss, Christopher B.","contributorId":64298,"corporation":false,"usgs":true,"family":"DuRoss","given":"Christopher B.","affiliations":[],"preferred":false,"id":205207,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31192,"text":"ofr00488 - 2000 - U. S. Geological Survey Middle Rio Grande basin study: Proceedings of the Fourth annual workshop, Albuquerque, New Mexico, February 15-16, 2000","interactions":[],"lastModifiedDate":"2025-01-13T22:27:32.623271","indexId":"ofr00488","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-488","title":"U. S. Geological Survey Middle Rio Grande basin study: Proceedings of the Fourth annual workshop, Albuquerque, New Mexico, February 15-16, 2000","docAbstract":"<p>This volume contains a collection of short papers that document some of the conclusions and results of on-going investigations related to ground-water resources of the Middle Rio Grande Basin, New Mexico. These results, and additional project reports, were presented at the Fourth Annual Middle Rio Grande Basin workshop convened in Albuquerque during February 2000. The workshop was jointly sponsored by the U.S. Geological Survey and the New Mexico Bureau of Mines and Mineral Resources as a forum for public presentation and discussion of multidisciplinary studies conducted during the previous 4 years. This considerable body of work was undertaken to improve the scientific understanding of factors that control ground-water availability and quality, and to explore land-surface characteristics that have affected the development and use of this valley that currently supports a population in excess of 600,000.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr00488","usgsCitation":"Cole, J.C., 2000, U. S. Geological Survey Middle Rio Grande basin study: Proceedings of the Fourth annual workshop, Albuquerque, New Mexico, February 15-16, 2000: U.S. Geological Survey Open-File Report 2000-488, vi, 51 p., https://doi.org/10.3133/ofr00488.","productDescription":"vi, 51 p.","costCenters":[],"links":[{"id":59700,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0488/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":376761,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/ofr-00-0488/","linkFileType":{"id":5,"text":"html"}},{"id":160863,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0488/report-thumb.jpg"},{"id":466182,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37353.htm","text":"Surface geology and liquefaction susceptibility in the inner Rio Grande Valley near Albuquerque, New Mexico [Chapter T]","linkFileType":{"id":5,"text":"html"}},{"id":401890,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37350.htm","text":"Geochemical characterization of ground water flow in parts of the Santa Fe Group aquifer system, Middle Rio Grande Basin, New Mexico [Chapter C]","linkFileType":{"id":5,"text":"html"}},{"id":466180,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37351.htm","text":"Sedimentary, stratigraphic, and hydrologic consequences of syn-depositional faulting in the Rio Grande rift [Chapter E]","linkFileType":{"id":5,"text":"html"}},{"id":466181,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37352.htm","text":"Subsurface constraints on the hydrogeologic model of the Middle Rio Grande Basin, New Mexico, using airborne time-domain electromagnetic data [Chapter G]","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db6232ee","contributors":{"authors":[{"text":"Cole, J. C.","contributorId":51292,"corporation":false,"usgs":true,"family":"Cole","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":205282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31193,"text":"ofr2000497 - 2000 - A Synopsis of Technical Issues for Monitoring Sediment in Highway and Urban Runoff","interactions":[],"lastModifiedDate":"2012-03-08T17:16:16","indexId":"ofr2000497","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-497","title":"A Synopsis of Technical Issues for Monitoring Sediment in Highway and Urban Runoff","docAbstract":"Accurate and representative sediment data are critical for assessing the potential effects of highway and urban runoff on receiving waters. The U.S. Environmental Protection Agency identified sediment as the most widespread pollutant in the Nation's rivers and streams, affecting aquatic habitat, drinking water treatment processes, and recreational uses of rivers, lakes, and estuaries. Representative sediment data are also necessary for quantifying and interpreting concentrations, loads, and effects of trace elements and organic constituents associated with highway and urban runoff. Many technical issues associated with the collecting, processing, and analyzing of samples must be addressed to produce valid (useful for intended purposes), current, complete, and technically defensible data for local, regional, and national information needs. All aspects of sediment data-collection programs need to be evaluated, and adequate quality-control data must be collected and documented so that the comparability and representativeness of data obtained for highway- and urban-runoff studies may be assessed.\r\n\r\n\r\nCollection of representative samples for the measurement of sediment in highway and urban runoff involves a number of interrelated issues. Temporal and spatial variability in runoff result from a combination of factors, including volume and intensity of precipitation, rate of snowmelt, and features of the drainage basin such as area, slope, infiltration capacity, channel roughness, and storage characteristics. In small drainage basins such as those found in many highway and urban settings, automatic samplers are often the most suitable method for collecting samples of runoff for a variety of reasons. Indirect sediment-measurement methods are also useful as supplementary and(or) surrogate means for monitoring sediment in runoff. All of these methods have limitations in addition to benefits, which must be identified and quantified to produce representative data. Methods for processing raw sediment samples (including homogenization and subsampling) for subsequent analysis for total suspended solids or suspended-sediment concentration often increase variance and may introduce bias. Processing artifacts can be substantial if the methods used are not appropriate for the concentrations and particle-size distributions present in the samples collected.\r\n\r\nAnalytical methods for determining sediment concentrations include the suspended-sediment\r\nconcentration and the total suspended solids methods. Although the terms suspended-sediment concentration and total suspended solids are often used interchangeably to describe the total concentration of suspended solid-phase material, the analytical methods differ and can produce substantially different results. The total suspended solids method, which commonly is used to produce highway- and urban-runoff sediment data, may not be valid for studies of runoff water quality. Studies of fluvial and highway-runoff sediment data indicate that analyses of samples by the total suspended solids method tends to under represent the true sediment concentration, and that relations between total suspended solids and suspended-sediment concentration are not transferable from site to site even when grain-size distribution information is available. Total suspended solids data used to calculate suspended-sediment loads in highways and urban runoff may be fundamentally unreliable. Consequently, use of total suspended solids data may have adverse consequences for the assessment, design, and maintenance of sediment-removal best management practices. Therefore, it may be necessary to analyze water samples using the suspended-sediment concentration method. Data quality, comparability, and utility are important considerations in collection, processing, and analysis of sediment samples and interpretation of sediment data for highway- and urban-runoff studies. Results from sediment studies must be comparable and readily transf","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr2000497","collaboration":"Prepared in cooperation with the Federal Highway Administration (A Contribution to the National Highway Runoff Data and Methodology Synthesis)","usgsCitation":"Bent, G.C., Gray, J.R., Smith, K.P., and Glysson, G.D., 2000, A Synopsis of Technical Issues for Monitoring Sediment in Highway and Urban Runoff: U.S. Geological Survey Open-File Report 2000-497, viii, 51 p., https://doi.org/10.3133/ofr2000497.","productDescription":"viii, 51 p.","onlineOnly":"Y","costCenters":[{"id":377,"text":"Massachusetts-Rhode Island Water Science Center","active":false,"usgs":true}],"links":[{"id":160357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2705,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://ma.water.usgs.gov/fhwa/ndamsp1.htm","linkFileType":{"id":5,"text":"html"}},{"id":9561,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/ofr00-497/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd496ce4b0b290850ef270","contributors":{"authors":[{"text":"Bent, Gardner C. 0000-0002-5085-3146 gbent@usgs.gov","orcid":"https://orcid.org/0000-0002-5085-3146","contributorId":1864,"corporation":false,"usgs":true,"family":"Bent","given":"Gardner","email":"gbent@usgs.gov","middleInitial":"C.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":205285,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gray, John R. 0000-0002-8817-3701 jrgray@usgs.gov","orcid":"https://orcid.org/0000-0002-8817-3701","contributorId":1158,"corporation":false,"usgs":true,"family":"Gray","given":"John","email":"jrgray@usgs.gov","middleInitial":"R.","affiliations":[{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true}],"preferred":true,"id":205283,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Kirk P. 0000-0003-0269-474X kpsmith@usgs.gov","orcid":"https://orcid.org/0000-0003-0269-474X","contributorId":1516,"corporation":false,"usgs":true,"family":"Smith","given":"Kirk","email":"kpsmith@usgs.gov","middleInitial":"P.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":205284,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Glysson, G. Douglas","contributorId":13607,"corporation":false,"usgs":true,"family":"Glysson","given":"G.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":205286,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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,{"id":31206,"text":"ofr0120 - 2000 - Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:09:05","indexId":"ofr0120","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2001-20","title":"Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 2000","language":"ENGLISH","doi":"10.3133/ofr0120","usgsCitation":"Duerr, A.D., 2000, Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 2000: U.S. Geological Survey Open-File Report 2001-20, 1 map ;72 x 69 cm., folded to 22 x 26 cm., https://doi.org/10.3133/ofr0120.","productDescription":"1 map ;72 x 69 cm., folded to 22 x 26 cm.","costCenters":[],"links":[{"id":160330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":59706,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2001/0020/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682c29","contributors":{"authors":[{"text":"Duerr, A. D.","contributorId":29821,"corporation":false,"usgs":true,"family":"Duerr","given":"A.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":205322,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":31179,"text":"ofr00418 - 2000 - Process classification of coastal land loss between 1932 and 1990 in the Mississippi River delta plain, southeastern Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:09:06","indexId":"ofr00418","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-418","title":"Process classification of coastal land loss between 1932 and 1990 in the Mississippi River delta plain, southeastern Louisiana","language":"ENGLISH","doi":"10.3133/ofr00418","usgsCitation":"Penland, S., Wayne, L., Britsch, L.D., Williams, S.J., Beall, A.D., and Butterworth, V.C., 2000, Process classification of coastal land loss between 1932 and 1990 in the Mississippi River delta plain, southeastern Louisiana: U.S. Geological Survey Open-File Report 2000-418, 1 map :col. ;50 x 90 cm., on sheet 93 x 110 cm., https://doi.org/10.3133/ofr00418.","productDescription":"1 map :col. ;50 x 90 cm., on sheet 93 x 110 cm.","costCenters":[],"links":[{"id":2699,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/openfile/of00-418/ ","linkFileType":{"id":5,"text":"html"}},{"id":160941,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660313","contributors":{"authors":[{"text":"Penland, Shea","contributorId":88401,"corporation":false,"usgs":false,"family":"Penland","given":"Shea","email":"","affiliations":[{"id":5115,"text":"Louisiana State University","active":true,"usgs":false}],"preferred":false,"id":205254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wayne, Lynda","contributorId":22392,"corporation":false,"usgs":true,"family":"Wayne","given":"Lynda","email":"","affiliations":[],"preferred":false,"id":205251,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Britsch, L. D.","contributorId":94707,"corporation":false,"usgs":true,"family":"Britsch","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":205255,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, S. Jeffress 0000-0002-1326-7420 jwilliams@usgs.gov","orcid":"https://orcid.org/0000-0002-1326-7420","contributorId":2063,"corporation":false,"usgs":true,"family":"Williams","given":"S.","email":"jwilliams@usgs.gov","middleInitial":"Jeffress","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":205250,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Beall, Andrew D.","contributorId":46137,"corporation":false,"usgs":true,"family":"Beall","given":"Andrew","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":205252,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Butterworth, Victoria Caridas","contributorId":48219,"corporation":false,"usgs":true,"family":"Butterworth","given":"Victoria","email":"","middleInitial":"Caridas","affiliations":[],"preferred":false,"id":205253,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":31158,"text":"ofr2000233 - 2000 - Physical characteristics of stream subbasins in the Sauk River basin, central Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T10:08:51","indexId":"ofr2000233","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-233","title":"Physical characteristics of stream subbasins in the Sauk River basin, central Minnesota","docAbstract":"<p>Data that describe the physical characteristics of stream subbasins upstream from selected sites on streams in the Sauk River Basin, located in central Minnesota, are presented in this report. The physical characteristics are the drainage area of the subbasin, the percentage area of the subbasin covered only by lakes, the percentage area of the subbasin covered by both lakes and wetlands, the main-channel length, and the main-channel slope. Stream sites include outlets of subbasins of at least 5 square miles, and locations of U.S. Geological Survey high-flow, and continuous-record gaging stations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View","doi":"10.3133/ofr2000233","collaboration":"Prepared in cooperation with the Minnesota Department of Transportation","usgsCitation":"Sanocki, C.A., and Fischer, B.C., 2000, Physical characteristics of stream subbasins in the Sauk River basin, central Minnesota: U.S. Geological Survey Open-File Report 2000-233, Document: 8 p.; Plate: 31.03 x 29.01 inches, https://doi.org/10.3133/ofr2000233.","productDescription":"Document: 8 p.; Plate: 31.03 x 29.01 inches","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321489,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr2000233.JPG"},{"id":12213,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://mn.water.usgs.gov/publications/pubs/00-233.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":12214,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://mn.water.usgs.gov/publications/pubs/00-233-plate.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Sauk River basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.58198547363281, 45.66444628645173 ], [ -94.57649230957031, 45.66060720625647 ], [ -94.57855224609375, 45.64812837751117 ], [ -94.59228515625, 45.63996763988405 ], [ -94.59297180175781, 45.62652383350405 ], [ -94.60464477539061, 45.6178796835697 ], [ 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,{"id":31162,"text":"ofr00295 - 2000 - Seafloor characterization offshore of the New York-New Jersey metropolitan area using sidescan-sonar","interactions":[],"lastModifiedDate":"2022-01-10T21:21:59.033458","indexId":"ofr00295","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-295","title":"Seafloor characterization offshore of the New York-New Jersey metropolitan area using sidescan-sonar","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr00295","usgsCitation":"Schwab, W.C., Denny, J.F., Butman, B., Danforth, W.W., Foster, D., Swift, B., Lotto, L.L., Allison, M.A., and Thieler, E., 2000, Seafloor characterization offshore of the New York-New Jersey metropolitan area using sidescan-sonar: U.S. Geological Survey Open-File Report 2000-295, HTML Document, https://doi.org/10.3133/ofr00295.","productDescription":"HTML Document","costCenters":[],"links":[{"id":110120,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_33544.htm","linkFileType":{"id":5,"text":"html"},"description":"33544"},{"id":161119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2671,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/of00-295/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Jersey, New York","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.254,\n              40.0167\n            ],\n            [\n              -73.214,\n              40.0167\n            ],\n            [\n              -73.214,\n              40.617\n            ],\n            [\n              -74.254,\n              40.617\n            ],\n            [\n              -74.254,\n              40.0167\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc658","contributors":{"authors":[{"text":"Schwab, William C. 0000-0001-9274-5154 bschwab@usgs.gov","orcid":"https://orcid.org/0000-0001-9274-5154","contributorId":417,"corporation":false,"usgs":true,"family":"Schwab","given":"William","email":"bschwab@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":205182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Denny, J. 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,{"id":24087,"text":"ofr00203 - 2000 - Assessment of volatile organic compounds in surface water at West Branch Canal Creek, Aberdeen Proving Ground, Maryland, 1999","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr00203","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-203","title":"Assessment of volatile organic compounds in surface water at West Branch Canal Creek, Aberdeen Proving Ground, Maryland, 1999","docAbstract":"The U.S. Geological Survey (USGS) collected 13 surface-water samples and 3 replicates from 5 sites in the West Branch Canal Creek area at Aberdeen Proving Ground from February through August 1999, as a part of an investigation of ground-water contamination and natural attenuation processes. The samples were analyzed for volatile organic compounds, including trichloroethylene, 1,1,2,2-tetrachloroethane, carbon tetrachloride, and chloroform, which are the four major contaminants that were detected in ground water in the Canal Creek area in earlier USGS studies. Field blanks were collected during the sampling period to assess sample bias. Field replicates were used to assess sample variability, which was expressed as relative percent difference. The mean variability of the surface-water replicate analyses was larger (35.4 percent) than the mean variability of ground-water replicate analyses (14.6 percent) determined for West Branch Canal Creek from 1995 through 1996. The higher variability in surface-water analyses is probably due to heterogeneities in the composition of the surface water rather than differences in sampling or analytical procedures. The most frequently detected volatile organic compound was 1,1,2,2- tetrachloroethane, which was detected in every sample and in two of the replicates. The surface-water contamination is likely the result of cross-media transfer of contaminants from the ground water and sediments along the West Branch Canal Creek. The full extent of surface-water contamination in West Branch Canal Creek and the locations of probable contaminant sources cannot be determined from this limited set of data. Tidal mixing, creek flow patterns, and potential effects of a drought that occurred during the sampling period also complicate the evaluation of surface-water contamination.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr00203","issn":"0094-9140","usgsCitation":"Olsen, L., and Spencer, T.A., 2000, Assessment of volatile organic compounds in surface water at West Branch Canal Creek, Aberdeen Proving Ground, Maryland, 1999: U.S. Geological Survey Open-File Report 2000-203, iv, 15 p. :maps ;28 cm., https://doi.org/10.3133/ofr00203.","productDescription":"iv, 15 p. :maps ;28 cm.","costCenters":[],"links":[{"id":156830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1753,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/ofr00203/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6674df","contributors":{"authors":[{"text":"Olsen, Lisa D. ldolsen@usgs.gov","contributorId":2707,"corporation":false,"usgs":true,"family":"Olsen","given":"Lisa D.","email":"ldolsen@usgs.gov","affiliations":[{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true}],"preferred":true,"id":191296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spencer, Tracey A.","contributorId":59477,"corporation":false,"usgs":true,"family":"Spencer","given":"Tracey","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":191297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23822,"text":"ofr2000247 - 2000 - Fish community structure in relation to environmental variables within the Sacramento River basin and implications for the greater Central Valley, California","interactions":[],"lastModifiedDate":"2012-03-08T17:16:14","indexId":"ofr2000247","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-247","title":"Fish community structure in relation to environmental variables within the Sacramento River basin and implications for the greater Central Valley, California","language":"ENGLISH","publisher":"U.S. Department of the Interior, U.S. Geological Survey ; Information Services [distributor],","doi":"10.3133/ofr2000247","issn":"0094-9140","usgsCitation":"May, J., and Brown, L.R., 2000, Fish community structure in relation to environmental variables within the Sacramento River basin and implications for the greater Central Valley, California: U.S. Geological Survey Open-File Report 2000-247, vi, 19 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr2000247.","productDescription":"vi, 19 p. :ill., map ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":14637,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/247/","linkFileType":{"id":5,"text":"html"}},{"id":155103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2cb0","contributors":{"authors":[{"text":"May, Jason T. 0000-0002-5699-2112","orcid":"https://orcid.org/0000-0002-5699-2112","contributorId":14791,"corporation":false,"usgs":true,"family":"May","given":"Jason T.","affiliations":[],"preferred":false,"id":190799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Larry R. 0000-0001-6702-4531 lrbrown@usgs.gov","orcid":"https://orcid.org/0000-0001-6702-4531","contributorId":1717,"corporation":false,"usgs":true,"family":"Brown","given":"Larry","email":"lrbrown@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":190798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24309,"text":"ofr2000238 - 2000 - Physical, chemical, and biological data for selected streams in Chester County, Pennsylvania, 1995-97","interactions":[],"lastModifiedDate":"2017-06-19T12:49:53","indexId":"ofr2000238","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-238","title":"Physical, chemical, and biological data for selected streams in Chester County, Pennsylvania, 1995-97","docAbstract":"Physical, chemical, and biological data were collected at 51 sampling sites in Chester County, Pa., from 1970 through 1997 as part of the Stream Conditions of Chester County Program. This report presents data collected from 43 sites from 1995 through 1997 that constitute a continuation of the program. Physical data include water temperature, instantaneous stream discharge, pH, alkalinity, specific conductance, and dissolved oxygen. Chemical data collected include laboratory determinations of nutrients and major ions in whole water samples and selected metals, pesticides, gross polychlorinated biphenyls (PCB's), gross polychlorinated napthalenes (PCN's), and total carbon in stream-sediment samples. The biological data include benthic-macroinvertebrate populations. The data are presented without interpretation.\r\n\r\nChester County is undergoing urbanization as agricultural land is converted to residential developments, commercial areas, and industrial and corporate parks. The major goal of the Stream Conditions of Chester County Program is to further the understanding of stream changes in response to urbanization.\r\n","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2000238","issn":"0094-9140","collaboration":"Prepared in cooperation with the Chester County Water Resources Authority\r\n","usgsCitation":"Reif, A.G., 2000, Physical, chemical, and biological data for selected streams in Chester County, Pennsylvania, 1995-97: U.S. Geological Survey Open-File Report 2000-238, iv, 147 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr2000238.","productDescription":"iv, 147 p. :ill., map ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":156251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7641,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/238/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685a88","contributors":{"authors":[{"text":"Reif, Andrew G. 0000-0002-5054-5207 agreif@usgs.gov","orcid":"https://orcid.org/0000-0002-5054-5207","contributorId":2632,"corporation":false,"usgs":true,"family":"Reif","given":"Andrew","email":"agreif@usgs.gov","middleInitial":"G.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":191669,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31170,"text":"ofr00356 - 2000 - Geologic map of the Wildcat Lake 7.5' quadrangle, Kitsap and Mason Counties, Washington","interactions":[],"lastModifiedDate":"2023-11-06T15:31:21.339206","indexId":"ofr00356","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-356","title":"Geologic map of the Wildcat Lake 7.5' quadrangle, Kitsap and Mason Counties, Washington","docAbstract":"<p>The Wildcat Lake quadrangle lies in the forearc of the Cascadia subduction zone, about 20-km east of the Cascadia accretionary complex exposed in the Olympic Mountains (Tabor and Cady, 1978),and about 100-km west of the axis of the Cascades volcanic arc. The quadrangle lies near the middle of the Puget Lowland, which typically has elevations less than 600 feet (183 m), but on Gold Mountain, in the center of the quadrangle, the elevation rises to 1761 feet (537 m). This anomalously high topography also provides a glimpse of the deeper crust beneath the Lowland. Exposed on Green and Gold Mountains are rocks related to the Coast Range basalt terrane. This terrane consists of Eocene submarine and subaerial tholeiitic basalt of the Crescent Formation, which probably accreted to the continental margin in Eocene time (Snavely and others, 1968). The Coast Range basalt terrane may have originated as an oceanic plateau or by oblique marginal rifting (Babcock and others, 1992), but its subsequent emplacement history is complex (Wells and others, 1984). In southern Oregon, onlapping strata constrain the suturing to have occurred by 50 Ma; but on southern Vancouver Island where the terrane-bounding Leech River fault is exposed, Brandon and Vance (1992) concluded suturing to North America occurred in the broad interval between 42 and 24 Ma. After emplacement of the Coast Range basalt terrane, the Cascadia accretionary complex,exposed in the Olympic Mountains west of the quadrangle,developed by frontal accretion and underplating (e.g., Clowes and others, 1987). The Seattle basin, part of which lies to the north of Green Mountain, also began to develop in late Eocene time due to forced flexural subsidence along the Seattle fault zone (Johnson and others, 1994). Domal uplift of the accretionary complex beneath the Olympic Mountains occurred after approximately 18 million years ago (Brandon and others, 1998). Ice-sheet glaciation during Quaternary time reshaped the topography of the quadrangle, and approximately two-thirds of the map area is covered with Quaternary deposits related to the last glaciation. Geophysical studies and regional mapping indicate the Seattle fault lies north of Green Mountain. This fault produced a large earthquake about 1000 years ago and may pose a significant earthquake hazard (Bucknam and others, 1992; Atwater and Moore, 1992; Karlin and Abella,1992; Schuster and others, 1992; Jacoby and others, 1992). We found no evidence of Holocene faulting in the Wildcat Lake quadrangle.</p><p><br></p><p>Geologic mapping within and marginal to the quadrangle began with Willis (1898), who described glacial deposits in Puget Sound. Weaver (1937) correlated volcanic rocks in the quadrangle to the Eocene Metchosin Volcanics on Vancouver Island. Sceva (1957), Garling and Moleenar (1965), and Deeter (1978) all focused on mapping and understanding the Quaternary stratigraphy of the Kitsap Peninsula, but they also examined bedrock in the quadrangle. Reeve (1979) was the first to examine the igneous rocks on Green and Gold Mountains in some detail, and Clark (1989) significantly improved Reeve's (1979) mapping. Clark's (1989) mapping was conducted soon after extensive logging on the mountains. A surficial geologic map of the Seattle 1:100,000-scale quadrangle, which includes the Wildcat Lake 1:24,000-scale quadrangle, was published by Yount and others (1993). Yount and Gower (1991) also published a bedrock geologic map of the Seattle quadrangle. Geologic mapping for this report was conducted by Haeussler in the spring and summer of 1998 and in the winter of 1999. We could not substantially improve upon the bedrock mapping of Clark (1989) and thus it is incorporated into this map. Well data in the southeastern corner of the map area also helped to constrain the surficial mapping (Geomatrix Consultants, 1997). In addition, 1995 vintage 1:12,000-scale aerial photographs were used in mapping Quaternary deposits. Geologic time scale is that of Berggeren and others (1995).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr00356","usgsCitation":"Haeussler, P.J., and Clark, K.P., 2000, Geologic map of the Wildcat Lake 7.5' quadrangle, Kitsap and Mason Counties, Washington: U.S. Geological Survey Open-File Report 2000-356, Report: 14 p.; 1 Plate: 37.89 x 34.67 inches; Metadata, https://doi.org/10.3133/ofr00356.","productDescription":"Report: 14 p.; 1 Plate: 37.89 x 34.67 inches; Metadata","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":125447,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2000_356.jpg"},{"id":391428,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_34290.htm"},{"id":2677,"rank":5,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/0356/","linkFileType":{"id":5,"text":"html"}},{"id":281618,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2000/0356/of00-356.ps"},{"id":281617,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2000/0356/pdf/of00-356.pdf"}],"scale":"24000","projection":"Universal Transverse Mercator projection","datum":"1927 North American datum","country":"United States","state":"Washington","county":"Kitsap County, Mason County","otherGeospatial":"Gold Mountain, Olympic Mountains,  Wildcat Lake quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.875,47.5 ], [ -122.875,47.625 ], [ -122.75,47.625 ], [ -122.75,47.5 ], [ -122.875,47.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4823e4b07f02db4e25ae","contributors":{"authors":[{"text":"Haeussler, Peter J. 0000-0002-1503-6247 pheuslr@usgs.gov","orcid":"https://orcid.org/0000-0002-1503-6247","contributorId":503,"corporation":false,"usgs":true,"family":"Haeussler","given":"Peter","email":"pheuslr@usgs.gov","middleInitial":"J.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":205209,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, Kenneth P.","contributorId":65513,"corporation":false,"usgs":true,"family":"Clark","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":205210,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21935,"text":"ofr00205 - 2000 - Measurement of ridge-spreading movements (Sackungen) at Bald Eagle Mountain, Lake County, Colorado, II: Continuation of the 1975-1989 measurements using a Global Positioning System in 1997 and 1999","interactions":[],"lastModifiedDate":"2022-02-22T20:41:37.277636","indexId":"ofr00205","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-205","title":"Measurement of ridge-spreading movements (Sackungen) at Bald Eagle Mountain, Lake County, Colorado, II: Continuation of the 1975-1989 measurements using a Global Positioning System in 1997 and 1999","docAbstract":"Measurements of ridge-spreading movements at Bald Eagle Mountain in north-central Colorado were reported in USGS Open-File Report 90-543 for the years 1975-1989. Measurements were renewed in 1997 and 1999 using the Global Positioning System (GPS). Movements are generally away from a ridge-top graben and appear to be concentrated along 3 or 4 trenches with uphill facing scarps that are parallel with slope contours. A point just below the lowest trench has moved the most? a total of 8.3 cm horizontally and slightly downward from 1977 to 1999 relative to an assumed stable point on the periphery of the graben. Movements from 1997 to 1999 are less than 1 cm or within the error of measurement.","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr00205","usgsCitation":"Varnes, D., Coe, J.A., Godt, J., Savage, W.Z., and Savage, J.E., 2000, Measurement of ridge-spreading movements (Sackungen) at Bald Eagle Mountain, Lake County, Colorado, II: Continuation of the 1975-1989 measurements using a Global Positioning System in 1997 and 1999: U.S. Geological Survey Open-File Report 2000-205, 23 p., https://doi.org/10.3133/ofr00205.","productDescription":"23 p.","costCenters":[],"links":[{"id":396277,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_26321.htm"},{"id":51410,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0205/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":1280,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/ofr-00-0205/","linkFileType":{"id":5,"text":"html"}},{"id":155891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0205/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Lake County","otherGeospatial":"Bald Eagle Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.48944854736328,\n              39.229327808005706\n            ],\n            [\n              -106.42112731933594,\n              39.229327808005706\n            ],\n            [\n              -106.42112731933594,\n              39.273992339346364\n            ],\n            [\n              -106.48944854736328,\n              39.273992339346364\n            ],\n            [\n              -106.48944854736328,\n              39.229327808005706\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db6111bc","contributors":{"authors":[{"text":"Varnes, David J.","contributorId":86322,"corporation":false,"usgs":true,"family":"Varnes","given":"David J.","affiliations":[],"preferred":false,"id":186312,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coe, J. A.","contributorId":8867,"corporation":false,"usgs":true,"family":"Coe","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":186309,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godt, J. W.","contributorId":76732,"corporation":false,"usgs":true,"family":"Godt","given":"J. W.","affiliations":[],"preferred":false,"id":186311,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Savage, W. Z.","contributorId":106481,"corporation":false,"usgs":true,"family":"Savage","given":"W.","email":"","middleInitial":"Z.","affiliations":[],"preferred":false,"id":186313,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Savage, J. E.","contributorId":37365,"corporation":false,"usgs":true,"family":"Savage","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":186310,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":21638,"text":"ofr00470 - 2000 - Borehole velocity measurements and geological conditions at thirteen sites in the Los Angeles, California region","interactions":[],"lastModifiedDate":"2012-02-02T00:07:56","indexId":"ofr00470","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-470","title":"Borehole velocity measurements and geological conditions at thirteen sites in the Los Angeles, California region","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr00470","issn":"0566-8174","usgsCitation":"Gibbs, J., Tinsley, J.C., Boore, D., and Joyner, W.B., 2000, Borehole velocity measurements and geological conditions at thirteen sites in the Los Angeles, California region: U.S. Geological Survey Open-File Report 2000-470, 118 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr00470.","productDescription":"118 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":154252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0470/report-thumb.jpg"},{"id":51195,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0470/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6029ab","contributors":{"authors":[{"text":"Gibbs, James F.","contributorId":95880,"corporation":false,"usgs":true,"family":"Gibbs","given":"James F.","affiliations":[],"preferred":false,"id":185011,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tinsley, J. C.","contributorId":65827,"corporation":false,"usgs":true,"family":"Tinsley","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":185009,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boore, D.M. 0000-0002-8605-9673","orcid":"https://orcid.org/0000-0002-8605-9673","contributorId":64226,"corporation":false,"usgs":true,"family":"Boore","given":"D.M.","affiliations":[],"preferred":false,"id":185008,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Joyner, W. B.","contributorId":70746,"corporation":false,"usgs":true,"family":"Joyner","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":185010,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":21808,"text":"ofr017 - 2000 - Geochemistry of sulfur in the Florida Everglades: 1994 through 1999","interactions":[],"lastModifiedDate":"2021-12-17T20:41:07.707071","indexId":"ofr017","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2001-7","title":"Geochemistry of sulfur in the Florida Everglades: 1994 through 1999","docAbstract":"In this report, we present data on the geochemistry of sulfur in sediments and in surface water, groundwater, and rainwater in the Everglades region in south Florida. The results presented here are part of a larger study intended to determine the roles played by the cycling of carbon, nitrogen, phosphorus, and sulfur in the ecology of the south Florida wetlands. The geochemistry of sulfur in the region is particularly important because of its link to the production of toxic methylmercury through processes mediated by sulfate reducing bacteria.\r\n\r\nSediment cores were collected from the Everglades Agricultural Area (EAA), Water Conservation Areas (WCAs) 1A and 2A, from Lake Okeechobee, and from Taylor Slough in the southern Everglades. Water collection was more widespread and includes surface water from WCAs 1A, 2A, 3A, 2B, the EAA, Taylor Slough, Lake Okeechobee, and the Kissimmee River. Groundwater was collected from The Everglades Nutrient Removal Area (ENR) and from WCA 2A. Rainwater was collected at two month intervals over a period of one year from the ENR and from WCA 2A. Water was analyzed for sulfate concentration and sulfate sulfur stable isotopic ratio (34S/32S). Sediment cores were analyzed for total sulfur concentration and/or for concentrations of sulfur species (sulfate, organic sulfur, disulfides, and acid volatile sulfides (AVS)) and for their stable sulfur isotopic ratio.\r\n\r\nResults show a decrease in total sulfur content (1.57 to 0.61 percent dry weight) with depth in two sediment cores collected in WCA 2A, indicating that there has been an increase in total sulfur content in recent times. A sediment core from the center of Lake Okeechobee shows a decrease in total sulfur content with depth (0.28 to 0.08 percent dry weight). A core from the periphery of the lake (South Bay) likewise shows a decrease in total sulfur content with depth (1.00 to 0.69 percent dry weight), however, the overall sulfur content is greater than that near the center at all depths. This suggests input of sulfur in recent times, especially near the lake margins. Sediments show a general decrease in sulfur concentration with depth, probably because of increases in sulfur input to the marshes in recent times. Regional differences in the concentrations and stable isotopic ratios of sulfate sulfur in surface water show that sulfur contamination to the northern Everglades likely originates from canals draining the EAA.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr017","issn":"0566-8174","usgsCitation":"Bates, A.L., Orem, W., Harvey, J., and Spiker, E., 2000, Geochemistry of sulfur in the Florida Everglades: 1994 through 1999: U.S. Geological Survey Open-File Report 2001-7, v, 54 p., https://doi.org/10.3133/ofr017.","productDescription":"v, 54 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":393056,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_34815.htm"},{"id":153976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0007/report-thumb.jpg"},{"id":51300,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0007/report.pdf","text":"Report","size":"8.8 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2001-7"}],"country":"United States","state":"Florida","otherGeospatial":"Florida Everglades","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.97448730468749,\n              24.943728712051445\n            ],\n            [\n              -79.99969482421875,\n              24.943728712051445\n            ],\n            [\n              -79.99969482421875,\n              26.45090222367262\n            ],\n            [\n              -81.97448730468749,\n              26.45090222367262\n            ],\n            [\n              -81.97448730468749,\n              24.943728712051445\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa67b","contributors":{"authors":[{"text":"Bates, Anne L. 0000-0002-4875-4675 abates@usgs.gov","orcid":"https://orcid.org/0000-0002-4875-4675","contributorId":2789,"corporation":false,"usgs":true,"family":"Bates","given":"Anne","email":"abates@usgs.gov","middleInitial":"L.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":185774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Orem, W. 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,{"id":23623,"text":"ofr00431 - 2000 - Report of the River Master of the Delaware River for the period December 1, 1997 to November 30, 1998, with a section on water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr00431","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-431","title":"Report of the River Master of the Delaware River for the period December 1, 1997 to November 30, 1998, with a section on water quality","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr00431","issn":"0094-9140","usgsCitation":"Krejmas, B.E., Harkness, W.E., Carswell, W., and Darling, H.L., 2000, Report of the River Master of the Delaware River for the period December 1, 1997 to November 30, 1998, with a section on water quality: U.S. Geological Survey Open-File Report 2000-431, vi, 93 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr00431.","productDescription":"vi, 93 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":154911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0431/report-thumb.jpg"},{"id":52900,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0431/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633b39","contributors":{"authors":[{"text":"Krejmas, Bruce E.","contributorId":102501,"corporation":false,"usgs":true,"family":"Krejmas","given":"Bruce","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":190439,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harkness, William E.","contributorId":43797,"corporation":false,"usgs":true,"family":"Harkness","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":190438,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carswell, William J. Jr. carswell@usgs.gov","contributorId":1787,"corporation":false,"usgs":true,"family":"Carswell","given":"William J.","suffix":"Jr.","email":"carswell@usgs.gov","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":false,"id":190436,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Darling, Hugh L. hdarling@usgs.gov","contributorId":4681,"corporation":false,"usgs":true,"family":"Darling","given":"Hugh","email":"hdarling@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":190437,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":22763,"text":"ofr00383 - 2000 - Evaluation of geophysical logs, Phase II, November 1998 to May 1999, at Crossley Farms Superfund Site, Berks County, Pennsylvania","interactions":[],"lastModifiedDate":"2023-08-30T20:27:00.410784","indexId":"ofr00383","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-383","title":"Evaluation of geophysical logs, Phase II, November 1998 to May 1999, at Crossley Farms Superfund Site, Berks County, Pennsylvania","docAbstract":"<p>Between November 1998 and May 1999, geophysical logging was conducted in 29 boreholes at the Crossley Farms Superfund Site, Hereford Township, Berks County, Pa., to determine the fluidproducing zones, fluid-receiving zones, zones of vertical borehole flow, and casing depth. The wells range in depth from 96 to 500 feet below land surface. Gamma logs only were collected in three bedrock wells. The geophysical logging determined the placement of well screens and packers, which allow monitoring and sampling of water-bearing zones in the fractured bedrock so that the horizontal and vertical distribution of contaminated ground water migrating from known sources could be determined. Geophysical logging included collection of caliper, video, fluid-temperature, fluid-resistivity, single-point-resistance, natural-gamma, fluid-flow, and acoustic-televiewer logs. Caliper and video logs were used to locate fractures, joints, and weathered zones. Inflections on fluidtemperature and fluid-resistivity logs indicated possible water-bearing fractures, and flowmeter measurements verified these locations. Single-point-resistance and natural-gamma logs provided information on stratigraphy. After interpretation of geophysical, video logs, and drillers notes, 24 of the wells were reconstructed such that water levels can be monitored and water samples collected from discrete water-bearing fractures in each well. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr00383","usgsCitation":"Conger, R.W., 2000, Evaluation of geophysical logs, Phase II, November 1998 to May 1999, at Crossley Farms Superfund Site, Berks County, Pennsylvania: U.S. Geological Survey Open-File Report 2000-383, vi, 56 p., https://doi.org/10.3133/ofr00383.","productDescription":"vi, 56 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":156957,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0383/report-thumb.jpg"},{"id":52198,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0383/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420331,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_34836.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Crossley Farms Superfund Site","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.517,\n              40.444\n            ],\n            [\n              -75.517,\n              40.404\n            ],\n            [\n              -75.473,\n              40.404\n            ],\n            [\n              -75.473,\n              40.444\n            ],\n            [\n              -75.517,\n              40.444\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fadb2","contributors":{"authors":[{"text":"Conger, Randall W. rwconger@usgs.gov","contributorId":2086,"corporation":false,"usgs":true,"family":"Conger","given":"Randall","email":"rwconger@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":188831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31260,"text":"ofr01116 - 2000 - Programs for using Newmark's method to model slope performance during earthquakes","interactions":[],"lastModifiedDate":"2026-06-26T16:00:24.907689","indexId":"ofr01116","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2001-116","title":"Programs for using Newmark's method to model slope performance during earthquakes","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01116","usgsCitation":"Jibson, R.W., and Jibson, M.W., 2000, Programs for using Newmark's method to model slope performance during earthquakes (Version 1.0): U.S. Geological Survey Open-File Report 2001-116, 1 computer optical disc : ill. ; 4 3/4 in., https://doi.org/10.3133/ofr01116.","productDescription":"1 CD-ROM","costCenters":[],"links":[{"id":506184,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0116/ofr01116.zip","text":"CD-ROM","linkFileType":{"id":6,"text":"zip"}},{"id":160780,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e048","contributors":{"authors":[{"text":"Jibson, Randall W. 0000-0003-3399-0875 jibson@usgs.gov","orcid":"https://orcid.org/0000-0003-3399-0875","contributorId":2985,"corporation":false,"usgs":true,"family":"Jibson","given":"Randall","email":"jibson@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":205507,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jibson, Matthew W.","contributorId":69199,"corporation":false,"usgs":true,"family":"Jibson","given":"Matthew","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":205508,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22086,"text":"ofr00492 - 2000 - Quantifying submarine groundwater discharge to Indian River Lagoon, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:07:51","indexId":"ofr00492","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-492","title":"Quantifying submarine groundwater discharge to Indian River Lagoon, Florida","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr00492","issn":"0094-9140","usgsCitation":"Swarzenski, P.W., Martin, J., Cable, J., Lindenberg, M., Boynton, B., Bowker, R., and Sigua, G., 2000, Quantifying submarine groundwater discharge to Indian River Lagoon, Florida: U.S. Geological Survey Open-File Report 2000-492, 4 p. :col. ill., col. maps ;28 cm., https://doi.org/10.3133/ofr00492.","productDescription":"4 p. :col. ill., col. maps ;28 cm.","costCenters":[],"links":[{"id":153779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0492/report-thumb.jpg"},{"id":51528,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0492/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a86e4b07f02db64dbcd","contributors":{"authors":[{"text":"Swarzenski, Peter W. 0000-0003-0116-0578 pswarzen@usgs.gov","orcid":"https://orcid.org/0000-0003-0116-0578","contributorId":1070,"corporation":false,"usgs":true,"family":"Swarzenski","given":"Peter","email":"pswarzen@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":187006,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, J.B.","contributorId":32923,"corporation":false,"usgs":true,"family":"Martin","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":187009,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cable, J.E.","contributorId":25963,"corporation":false,"usgs":true,"family":"Cable","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":187008,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lindenberg, M.K.","contributorId":56254,"corporation":false,"usgs":true,"family":"Lindenberg","given":"M.K.","affiliations":[],"preferred":false,"id":187012,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Boynton, Betsy bboynton@usgs.gov","contributorId":3360,"corporation":false,"usgs":true,"family":"Boynton","given":"Betsy","email":"bboynton@usgs.gov","affiliations":[],"preferred":true,"id":187007,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bowker, Rita","contributorId":33733,"corporation":false,"usgs":true,"family":"Bowker","given":"Rita","email":"","affiliations":[],"preferred":false,"id":187010,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sigua, G.C.","contributorId":52994,"corporation":false,"usgs":true,"family":"Sigua","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":187011,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":24643,"text":"ofr00389 - 2000 - 20th century U.S. mineral prices decline in constant dollars","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"ofr00389","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-389","title":"20th century U.S. mineral prices decline in constant dollars","docAbstract":"Price indexes developed by the U.S. Geological Survey (USGS) indicate that the long-term constant dollar price of key U.S. mineral raw materials declined over the last century, even though the need for mineral raw materials increased during the same period. Technologies and reduced production costs have allowed mineral production to remain profitable, while lower priced mineral products from domestic and foreign sources helped fuel growth in other sectors of the economy.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr00389","issn":"0094-9140","usgsCitation":"Sullivan, D.E., Sznopek, J.L., and Wagner, L.A., 2000, 20th century U.S. mineral prices decline in constant dollars: U.S. Geological Survey Open-File Report 2000-389, 8 p., https://doi.org/10.3133/ofr00389.","productDescription":"8 p.","costCenters":[],"links":[{"id":157539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1910,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/openfile/of00-389/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4929e4b0b290850eeed0","contributors":{"authors":[{"text":"Sullivan, Daniel E.","contributorId":62198,"corporation":false,"usgs":true,"family":"Sullivan","given":"Daniel","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":192310,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sznopek, John L.","contributorId":23936,"corporation":false,"usgs":true,"family":"Sznopek","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":192309,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wagner, Lorie A.","contributorId":95457,"corporation":false,"usgs":true,"family":"Wagner","given":"Lorie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":192311,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31194,"text":"ofr00502 - 2000 - Digital airborne time domain electromagnetic data from surveys over Cochiti Pueblo, Rio Puerco, and Rio Rancho, New Mexico","interactions":[],"lastModifiedDate":"2020-03-25T12:58:34","indexId":"ofr00502","displayToPublicDate":"2001-06-01T00:00:00","publicationYear":"2000","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":"2000-502","title":"Digital airborne time domain electromagnetic data from surveys over Cochiti Pueblo, Rio Puerco, and Rio Rancho, New Mexico","docAbstract":"<p>The Albuquerque-Santa Fe region is rapidly growing. The Santa Fe Group aquifer in the Middle Rio Grande Basin (MRGB) is the main source of municipal water for the greater Albuquerque metropolitan area and is more limited than previously thought (Thorn et al., 1993). The MRGB, as defined hydrologically and used here, is the area within the Rio Grande Valley extending from Cochiti Dam downstream to the community of San Acacia (Figure 1). Because approximately 600,000 people (40 percent of the population of New Mexico) live in the study area (Bartolino, 1999), water shortfalls could have serious consequences for the state. Future growth and land management in the region depends on accurate assessment and protection of the region’s groundwater resources. An important issue in understanding the ground water resources is a better understanding of the hydrogeology of the Santa Fe Group, the sedimentary deposits that fill the Rio Grande rift and contain the principal groundwater aquifers. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr00502","usgsCitation":"Deszcz-Pan, M., Rodriguez, B.D., Doucette, J.P., Godbout, M., Williams, J.M., Sawyer, D., Stone, B., Grauch, V., and Geoterrex-Dighem, 2000, Digital airborne time domain electromagnetic data from surveys over Cochiti Pueblo, Rio Puerco, and Rio Rancho, New Mexico: U.S. Geological Survey Open-File Report 2000-502, CD-ROM, https://doi.org/10.3133/ofr00502.","productDescription":"CD-ROM","costCenters":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":160358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2706,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/ofr-00-0502/","linkFileType":{"id":5,"text":"html"}}],"country":"United States ","state":"New Mexico","city":"Cochiti Pueblo, Rio Puerco, Rio Rancho","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.74316406249999,\n              35.06597313798418\n            ],\n            [\n              -104.61181640625,\n              35.06597313798418\n            ],\n            [\n              -104.61181640625,\n              36.87962060502676\n            ],\n            [\n              -106.74316406249999,\n              36.87962060502676\n            ],\n            [\n              -106.74316406249999,\n              35.06597313798418\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4607","contributors":{"authors":[{"text":"Deszcz-Pan, Maria 0000-0002-6298-5314 maryla@usgs.gov","orcid":"https://orcid.org/0000-0002-6298-5314","contributorId":1263,"corporation":false,"usgs":true,"family":"Deszcz-Pan","given":"Maria","email":"maryla@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":205287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodriguez, B. 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