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.
","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":30857,"text":"wri004046 - 2000 - Bathymetry and selected perspective views of sea floor north and west of Maui, Hawaii","interactions":[],"lastModifiedDate":"2019-07-15T10:21:02","indexId":"wri004046","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-4046","title":"Bathymetry and selected perspective views of sea floor north and west of Maui, Hawaii","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri004046","usgsCitation":"Gardner, J., Dartnell, P., Mayer, L.A., and Clarke, J., 2000, Bathymetry and selected perspective views of sea floor north and west of Maui, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 2000-4046, 2 Plates: 33.99 x 41.71 inches and 32.43 x 38.04 inches, https://doi.org/10.3133/wri004046.","productDescription":"2 Plates: 33.99 x 41.71 inches and 32.43 x 38.04 inches","costCenters":[{"id":335,"text":"Hawaii Water Science Center","active":false,"usgs":true}],"links":[{"id":160285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2000/4046/report-thumb.jpg"},{"id":365514,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2000/4046/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365515,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2000/4046/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","country":"United States","state":"Hawaii","otherGeospatial":"Maui ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -156.708984375,\n 20.56079574020845\n ],\n [\n -155.7421875,\n 20.56079574020845\n ],\n [\n -155.7421875,\n 21.040927787394494\n ],\n [\n -156.708984375,\n 21.040927787394494\n ],\n [\n -156.708984375,\n 20.56079574020845\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ee4b07f02db64036d","contributors":{"authors":[{"text":"Gardner, J.V.","contributorId":76705,"corporation":false,"usgs":true,"family":"Gardner","given":"J.V.","affiliations":[],"preferred":false,"id":204218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dartnell, Peter 0000-0002-9554-729X pdartnell@usgs.gov","orcid":"https://orcid.org/0000-0002-9554-729X","contributorId":2688,"corporation":false,"usgs":true,"family":"Dartnell","given":"Peter","email":"pdartnell@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":204216,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mayer, L. A.","contributorId":105776,"corporation":false,"usgs":true,"family":"Mayer","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204219,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clarke, J.E.","contributorId":28285,"corporation":false,"usgs":true,"family":"Clarke","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":204217,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"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":31178,"text":"ofr00417 - 2000 - Geomorphic classification of coastal land loss between 1932 and 1990 in the Mississippi River delta plain, southeastern Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"ofr00417","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":"2000-417","title":"Geomorphic classification of coastal land loss between 1932 and 1990 in the Mississippi River delta plain, southeastern Louisiana","language":"ENGLISH","doi":"10.3133/ofr00417","usgsCitation":"Penland, S., Wayne, L., Britsch, L.D., Williams, S.J., Beall, A.D., and Butterworth, V.C., 2000, Geomorphic classification of coastal land loss between 1932 and 1990 in the Mississippi River delta plain, southeastern Louisiana: U.S. Geological Survey Open-File Report 2000-417, 1 map :col. ;50 x 90 cm., on sheet 93 x 110 cm., https://doi.org/10.3133/ofr00417.","productDescription":"1 map :col. ;50 x 90 cm., on sheet 93 x 110 cm.","costCenters":[],"links":[{"id":160341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2698,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/openfile/of00-417/ ","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c52d","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":205248,"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":205245,"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":205249,"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":205244,"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":205246,"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":205247,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":30263,"text":"wri004153 - 2000 - Development, testing, and assessment of regression equations for experimental forecasts of fall-transition-season inflows to the Howard A. Hanson Reservoir, Green River, Washington","interactions":[],"lastModifiedDate":"2013-07-08T13:11:06","indexId":"wri004153","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-4153","title":"Development, testing, and assessment of regression equations for experimental forecasts of fall-transition-season inflows to the Howard A. Hanson Reservoir, Green River, Washington","language":"ENGLISH","publisher":"U.S. Department of the Interior, U.S. Geological Survey ;Information Services [distributor],","doi":"10.3133/wri004153","usgsCitation":"Vaccaro, J.J., 2000, Development, testing, and assessment of regression equations for experimental forecasts of fall-transition-season inflows to the Howard A. Hanson Reservoir, Green River, Washington: U.S. Geological Survey Water-Resources Investigations Report 2000-4153, iii, 30 p. :ill., map ;28 cm., https://doi.org/10.3133/wri004153.","productDescription":"iii, 30 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":160467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2000/4153/report-thumb.jpg"},{"id":274642,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2000/4153/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dd7a","contributors":{"authors":[{"text":"Vaccaro, J. J.","contributorId":48173,"corporation":false,"usgs":true,"family":"Vaccaro","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202956,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29329,"text":"wri20004102 - 2000 - Suspended sediment in the Indiana Harbor Canal and the Grand Calumet River, northwestern Indiana, May 1996-June 1998","interactions":[],"lastModifiedDate":"2022-12-16T19:38:06.047806","indexId":"wri20004102","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-4102","title":"Suspended sediment in the Indiana Harbor Canal and the Grand Calumet River, northwestern Indiana, May 1996-June 1998","docAbstract":"Suspended-sediment samples and streamflow data were collected from May 1996 through June 1998 at three sites in the Grand Calumet River Basin - Indiana Harbor Canal at East Chicago, the east branch of the Grand Calumet River at Gary, and the west branch of the Grand Calumet River at Hammond. Sample analysis allowed for retention of sediments of 0.0015 millimeters or larger.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri20004102","collaboration":"Prepared in cooperation with the US Army Corps of Engineers","usgsCitation":"Renn, D.E., 2000, Suspended sediment in the Indiana Harbor Canal and the Grand Calumet River, northwestern Indiana, May 1996-June 1998: U.S. Geological Survey Water-Resources Investigations Report 2000-4102, v, 52 p., https://doi.org/10.3133/wri20004102.","productDescription":"v, 52 p.","startPage":"1","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1996-05-01","temporalEnd":"1998-06-30","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":159219,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410642,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_34801.htm","linkFileType":{"id":5,"text":"html"}},{"id":12874,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/2000/wri00-4102/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Indiana","otherGeospatial":"Indiana Harbor Canal, Grand Calumet River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.563,\n 41.583\n ],\n [\n -87.563,\n 41.6667\n ],\n [\n -87.25,\n 41.6667\n ],\n [\n -87.25,\n 41.583\n ],\n [\n -87.563,\n 41.583\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fae49","contributors":{"authors":[{"text":"Renn, Danny E.","contributorId":14808,"corporation":false,"usgs":true,"family":"Renn","given":"Danny","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":201355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29238,"text":"wri004103 - 2000 - Sensitivity of ground water to contamination in Lawrence County, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri004103","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-4103","title":"Sensitivity of ground water to contamination in Lawrence County, South Dakota","docAbstract":"Ground-water supplies in Lawrence County, South Dakota, can be contaminated by agricultural, urban, suburban, commercial, and industrial land uses. To address this issue, the U.S. Geological Survey in cooperation with Lawrence County and the City of Spearfish mapped the sensitivity of ground water to contamination in Lawrence County.\r\n\r\nSensitivity of ground water to contamination was determined by delineating hydrogeologic settings with common hydrogeologic characteristics as described in the DRASTIC method, developed by the U.S. Environmental Protection Agency and the National Water Well Association. Within the framework of 11 hydrogeologic settings, sensitivity to contamination was ranked for six intrinsic hydrogeologic characteristics: (1) aquifer media, (2) unsaturated media (3) hydraulic conductivity, (4) recharge rate, (5) depth to water, and (6) land-surface slope. The rating conventions of DRASTIC were modified to provide a relative ranking of hydrogeologic characteristics without assignment of a combined numerical score. Soil characteristics were not included as a map layer because detailed digital data were not available; however, the general distribution of two soil characteristics were shown.\r\n\r\nA total of 956 polygons were delineated and assigned a sensitivity-unit code that represented unique groups of sensitivity rank for the six intrinsic hydrogeologic characteristics. The polygons were created by overlaying and intersecting maps that describe the geology, precipitation, land-surface elevation, and depth to water using a geographic information system. Thirty drainage areas upstream from potential streamflow-loss zones were delineated to describe an additional mechanism of transport of potential contamination. The sensitivity of ground water to contamination was presented on a 1:100,000-scale map with code and label explanations. Limitations of the sensitivity map are described to facilitate appropriate use of the map as a screening tool to compare sensitivity to contamination.","language":"ENGLISH","publisher":"U.S. Department of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri004103","usgsCitation":"Putnam, L.D., 2000, Sensitivity of ground water to contamination in Lawrence County, South Dakota: U.S. Geological Survey Water-Resources Investigations Report 2000-4103, iv, 55 p. :ill. (some col.), maps (some col.) ;28 cm.; 2 over-size sheets, scale 1:100,000, https://doi.org/10.3133/wri004103.","productDescription":"iv, 55 p. :ill. (some col.), maps (some col.) ;28 cm.; 2 over-size sheets, scale 1:100,000","costCenters":[],"links":[{"id":2370,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri004103/","linkFileType":{"id":5,"text":"html"}},{"id":159374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e1388","contributors":{"authors":[{"text":"Putnam, Larry D. ldputnam@usgs.gov","contributorId":990,"corporation":false,"usgs":true,"family":"Putnam","given":"Larry","email":"ldputnam@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":201197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23129,"text":"ofr2000245 - 2000 - Interim report on the scientific investigations in the Animas River watershed, Colorado to facilitate remediation decisions by the U.S. Bureau of Land Management and the U.S. Forest Service, March 29, 2000 meeting, Denver, Colo.","interactions":[],"lastModifiedDate":"2022-02-03T22:13:45.742285","indexId":"ofr2000245","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":"2000-245","title":"Interim report on the scientific investigations in the Animas River watershed, Colorado to facilitate remediation decisions by the U.S. Bureau of Land Management and the U.S. Forest Service, March 29, 2000 meeting, Denver, Colo.","docAbstract":"INTRODUCTION\r\nThe joint U.S. Department of the Interior and U.S. Department of Agriculture Abandoned Mine Lands\r\nInitiative (AMLI) was developed as a collaborative effort between the Federal land management agencies (FLMA,\r\nthat is the U.S. Bureau of Land Management and the U.S. Forest Service) and the U.S. Geological Survey (USGS)\r\nin 1996. The stated goal of the AML Initiative was to develop a strategy for gathering and communicating the\r\nscientific information needed to develop effective and cost-efficient remediation of abandoned mines within the\r\nframework of a watershed. Four primary objectives of the AMLI are to:\r\n1. Provide the scientific information needed (in the short-term) by the FLMAs to make decisions related to the\r\ndesign and implementation of cleanup actions,\r\n2. Develop a multi-disciplined, multi-division approach that integrates geologic, hydrologic, geochemical and\r\necological information into a knowledge base for sound decision making,\r\n3. Transfer technologies developed within the scientific programs of the USGS to the field and demonstrate\r\ntheir suitability to solve real, practical problems, and\r\n4. Establish working relationships among involved members of land management and regulatory agencies\r\nwithin the framework of a watershed approach to the cleanup of abandoned mines.\r\nLong-term process-based research, including development of analytical tools, is recognized as being critical to the\r\nlong-term success in remediating watersheds impacted by historical mining activities (AML 5-year plan,\r\nhttp://amli.usgs.gov/amli).\r\nIn a meeting of Federal agencies (U.S. Bureau of Land Management [BLM], U.S. Bureau of Reclamation\r\n[BOR], U.S. National Park Service [NPS], U.S. Forest Service [USFS], the U.S. Environmental Protection Agency\r\n[EPA], the U.S. Fish and Wildlife Service [F&WS]), and State agencies (Colorado Division of Public Health and\r\nEnvironment, Colorado Division of Mines and Geology), several watersheds were examined within the state whose\r\nwater quality was presumed to be impacted by historical mining activities. The Animas River watershed (fig. 1) was\r\nselected by the State and Federal agencies as one of two watersheds in the U.S. to be studied in detail by the USGS\r\nin the AML Initiative. Beginning in October 1997, each of the four Divisions of the USGS (Water Resources,\r\nGeologic, Biological Resources, and National Mapping) initiated a collaborative integrated science study of the\r\nwatershed. Funds were provided from USGS base funding to each of the four Divisions in response to the priorities\r\nset by Congressional action and within the flexibility provided by the budgetary framework funding individual\r\nresearch programs. The AML Initiative provides for a five-year focused scientific effort in the two watersheds with\r\nfinal synthesis of the scientific results from each to be published in 2001. Publications are released on the AML web\r\nsite on a regular basis (http://amli.usgs.gov/amli).\r\nOn March 29, 2000, the USGS hosted a meeting for the BLM and USFS to discuss remediation options that\r\nwere under consideration for the summer of 2000. The purpose of this report is to provide an overview of the\r\nscientific rational provided by the USGS to meet objective one above, and to summarize our preliminary\r\ninterpretations of our data. Additional information from sites on private lands have been collected by the State of\r\nColorado, EPA, and the ARSG. Unfortunately, these data have not been fully supplied to the USGS so our\r\nconclusions are based only upon our data. These interpretations provide science-based constraints on possible\r\nremediation options to be considered by the FLMA, the State, and local property owners in the Animas River\r\nwatershed. The report is presented in outline format to facilitate discussion of remediation options at the March 29,\r\n2000 meeting. Not all historical mining sites within the watershed are on public lands. This should not be construed\r\nto be a final report of the USGS","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2000245","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2000, Interim report on the scientific investigations in the Animas River watershed, Colorado to facilitate remediation decisions by the U.S. Bureau of Land Management and the U.S. Forest Service, March 29, 2000 meeting, Denver, Colo. (Version 1.0): U.S. Geological Survey Open-File Report 2000-245, 34 p., https://doi.org/10.3133/ofr2000245.","productDescription":"34 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":155693,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":395418,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_26998.htm"},{"id":9154,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2000/ofr-00-0245/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Denver","otherGeospatial":"Animas River watershed","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.8,37.773 ], [ -107.8,37.954 ], [ -107.517,37.954 ], [ -107.517,37.773 ], [ -107.8,37.773 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e094d","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":529108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22990,"text":"ofr00202 - 2000 - Rocky intertidal resources monitoring handbook, Cabrillo National Monument, Point Loma, San Diego, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:51","indexId":"ofr00202","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":"2000-202","title":"Rocky intertidal resources monitoring handbook, Cabrillo National Monument, Point Loma, San Diego, California","language":"ENGLISH","publisher":"U.S. Department of the Interior, U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr00202","issn":"0094-9140","usgsCitation":"Engle, J.M., and Davis, G.E., 2000, Rocky intertidal resources monitoring handbook, Cabrillo National Monument, Point Loma, San Diego, California: U.S. Geological Survey Open-File Report 2000-202, iv, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr00202.","productDescription":"iv, 34 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0202/report-thumb.jpg"},{"id":52379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0202/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ccbb","contributors":{"authors":[{"text":"Engle, John M.","contributorId":82728,"corporation":false,"usgs":true,"family":"Engle","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":189247,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Gary E.","contributorId":73235,"corporation":false,"usgs":true,"family":"Davis","given":"Gary","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":189246,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":23107,"text":"ofr99417 - 2000 - Bathymetry of west-central Florida","interactions":[],"lastModifiedDate":"2017-02-08T12:06:14","indexId":"ofr99417","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":"99-417","title":"Bathymetry of west-central Florida","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr99417","issn":"0094-9140","usgsCitation":"Gelfenbaum, G., and Guy, K.K., 2000, Bathymetry of west-central Florida: U.S. Geological Survey Open-File Report 99-417, 1 computer optical disc :col. maps. ;4 3/4 in. in plastic box 13 x 15 x 1 cm., https://doi.org/10.3133/ofr99417.","productDescription":"1 computer optical disc :col. maps. ;4 3/4 in. in plastic box 13 x 15 x 1 cm.","costCenters":[],"links":[{"id":156542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334969,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0417/ofr99417.zip","linkFileType":{"id":6,"text":"zip"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e192","contributors":{"authors":[{"text":"Gelfenbaum, Guy","contributorId":79844,"corporation":false,"usgs":true,"family":"Gelfenbaum","given":"Guy","affiliations":[],"preferred":false,"id":189447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guy, Kristy K. kguy@usgs.gov","contributorId":3546,"corporation":false,"usgs":true,"family":"Guy","given":"Kristy","email":"kguy@usgs.gov","middleInitial":"K.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":189446,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26833,"text":"wri004163 - 2000 - Probability of detecting atrazine/desethyl-atrazine and elevated concentrations of nitrate plus nitrate as nitrogen in ground water in the Idaho part of the western Snake River Plain","interactions":[],"lastModifiedDate":"2022-09-30T18:41:52.908609","indexId":"wri004163","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-4163","title":"Probability of detecting atrazine/desethyl-atrazine and elevated concentrations of nitrate plus nitrate as nitrogen in ground water in the Idaho part of the western Snake River Plain","docAbstract":"As ground water continues to provide an ever-growing proportion of Idaho?s drinking water, concerns about the quality of that resource are increasing. Pesticides (most commonly, atrazine/desethyl-atrazine, hereafter referred to as atrazine) and nitrite plus nitrate as nitrogen (hereafter referred to as nitrate) have been detected in many aquifers in the State. To provide a sound hydrogeologic basis for atrazine and nitrate management in southern Idaho—the largest region of land and water use in the State—the U.S. Geological Survey produced maps showing the probability of detecting these contaminants in ground water in the upper Snake River Basin (published in a 1998 report) and the western Snake River Plain (published in this report). The atrazine probability map for the western Snake River Plain was constructed by overlaying ground-water quality data with hydrogeologic and anthropogenic data in a geographic information system (GIS). A data set was produced in which each well had corresponding information on land use, geology, precipitation, soil characteristics, regional depth to ground water, well depth, water level, and atrazine use. These data were analyzed by logistic regression using a statistical software package. Several preliminary multivariate models were developed and those that best predicted the detection of atrazine were selected. The multivariate models then were entered into a GIS and the probability maps were produced. Land use, precipitation, soil hydrologic group, and well depth were significantly correlated with atrazine detections in the western Snake River Plain. These variables also were important in the 1998 probability study of the upper Snake River Basin. The effectiveness of the probability models for atrazine might be improved if more detailed data were available for atrazine application. A preliminary atrazine probability map for the entire Snake River Plain in Idaho, based on a data set representing that region, also was produced. In areas where this map overlaps the 1998 map of the upper Snake River Basin, the two maps show broadly similar probabilities of detecting atrazine. Logistic regression also was used to develop a preliminary statistical model that predicts the probability of detecting elevated nitrate in the western Snake River Plain. A nitrate probability map was produced from this model. Results showed that elevated nitrate concentrations were correlated with land use, soil organic content, well depth, and water level. Detailed information on nitrate input, specifically fertilizer application, might have improved the effectiveness of this model.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri004163","collaboration":"Prepared in cooperation with Idaho State Department of Agriculture","usgsCitation":"Donato, M.M., 2000, Probability of detecting atrazine/desethyl-atrazine and elevated concentrations of nitrate plus nitrate as nitrogen in ground water in the Idaho part of the western Snake River Plain: U.S. Geological Survey Water-Resources Investigations Report 2000-4163, Report: iv, 25 p.; 1 Plate: 24 x 35 inches, https://doi.org/10.3133/wri004163.","productDescription":"Report: iv, 25 p.; 1 Plate: 24 x 35 inches","numberOfPages":"31","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":262324,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2000/4163/plate-1.pdf"},{"id":407729,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_33863.htm","linkFileType":{"id":5,"text":"html"}},{"id":262326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2000/4163/report-thumb.jpg"},{"id":262325,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2000/4163/report.pdf"}],"country":"United States","state":"Idaho","otherGeospatial":"western Snake River Plain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.133,\n 42.55\n ],\n [\n -114.927,\n 42.55\n ],\n [\n -114.927,\n 44.867\n ],\n [\n -117.133,\n 44.867\n ],\n [\n -117.133,\n 42.55\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655fb2","contributors":{"authors":[{"text":"Donato, Mary M.","contributorId":30962,"corporation":false,"usgs":true,"family":"Donato","given":"Mary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":197087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26830,"text":"wri004203 - 2000 - Pesticides in surface water measured at select sites in the Sacramento River basin, California, 1996-1998","interactions":[],"lastModifiedDate":"2023-01-10T19:09:32.999343","indexId":"wri004203","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-4203","title":"Pesticides in surface water measured at select sites in the Sacramento River basin, California, 1996-1998","docAbstract":"Pesticides were measured in one urban stream, one agricultural stream, one site on the Sacramento River, and one large flood control channel over a period of 18 months during 1996-1998. All sites were located within the Sacramento River Basin of California. Measurements were made on 83 pesticides or pesticide transformation products by either gas chromatography/mass spectrometry or by high performance liquid chromatography with ultraviolet light spectrometry. Some pesticides were detected frequently at the agricultural stream and downstream in the Sacramento River and at the flood control channel of the Sacramento River. These were pesticides related to rice farming (molinate, carbofuran, thiobencarb, and bentazon); herbicides used both agriculturally or for roadside maintenance (diuron, simazine, and metolachlor); or insecticides used on orchards and row corps (diazinon and chlorpyrifos). No pesticide concen-trations above enforceable water quality criteria were measured at either the agricultural site or the Sacramento River sites. In contrast to the agricul-tural site, insecticides used for household, lawn, or garden maintenance were the most frequently detected pesticides at the urban site. Diazinon, an organophosphate insecticide, exceeded recom-mended criteria for the protection of aquatic life, and the diazinon levels were frequently above known toxic levels for certain zooplankton species at the urban site. Because of the low discharge of the urban stream, pesticide concentrations were greatly diluted upon mixing with Sacramento River water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri004203","usgsCitation":"Domagalski, J.L., 2000, Pesticides in surface water measured at select sites in the Sacramento River basin, California, 1996-1998: U.S. Geological Survey Water-Resources Investigations Report 2000-4203, vi, 24 p., https://doi.org/10.3133/wri004203.","productDescription":"vi, 24 p.","costCenters":[],"links":[{"id":158183,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411644,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_34376.htm","linkFileType":{"id":5,"text":"html"}},{"id":2105,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://ca.water.usgs.gov/archive/reports/wrir004203/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Sacramento River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -123,\n 41.733\n ],\n [\n -123,\n 38.033\n ],\n [\n -120,\n 38.033\n ],\n [\n -120,\n 41.733\n ],\n [\n -123,\n 41.733\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688221","contributors":{"authors":[{"text":"Domagalski, Joseph L. 0000-0002-6032-757X joed@usgs.gov","orcid":"https://orcid.org/0000-0002-6032-757X","contributorId":1330,"corporation":false,"usgs":true,"family":"Domagalski","given":"Joseph","email":"joed@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":197082,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53098,"text":"ofr2000232 - 2000 - Physical characteristics of stream subbasins in the Long Prairie River basin, central Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T10:07:52","indexId":"ofr2000232","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":"2000-232","title":"Physical characteristics of stream subbasins in the Long Prairie River basin, central Minnesota","docAbstract":"Data that describe the physical characteristics of stream subbasins upstream from selected sites on streams in the Long Prairie 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.
","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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May–October 1994 and 1995","docAbstract":"The Metropolitan Atlanta area has been undergoing a period of rapid growth and development. The population in the 10-county metropolitan area almost doubled from about 1.5 million people in 1970 to 2.9 million people in 1995 (Atlanta Regional Commission, written commun., 2000). Residential, commercial, and other urban land uses more than tripled during the same period (Frick and others, 1998). The Chattahoochee River is the most utilized water resource in Georgia. The rapid growth of Metropolitan Atlanta and its location downstream of the headwaters of the drainage basin make the Chattahoochee River a vital resource for drinking-water supplies, recreational opportunities, and wastewater assimilation. In 1978, the U.S. Congress declared the natural, scenic, recreation, and other values of 48 miles of the Chattahoochee River from Buford Dam to Peachtree Creek to be of special national significance. To preserve this reach of the Chattahoochee River, the U.S. Congress created the Chattahoochee River National Recreational Area (CRNRA), which includes the Chattahoochee River downstream from Buford Dam to the mouth of Peachtree Creek and a series of park areas adjacent to the river in northern Metropolitan Atlanta Even with this protection, waters of the Chattahoochee River and many of its tributaries in Metropolitan Atlanta did not meet water-quality standards set for designated uses during 1994 and 1995 (fig. 1 and table 1). Much of the degradation of water quality has been associated with areas undergoing rapid urban growth and sprawling suburban development. The resulting conversion of mostly forested land to urban land has multiple adverse effects on water quality. Degradation of water quality may be caused by a number of factors including an increase in nutrient concentrations, sediment and sedimentbound contaminant concentrations (e.g., metals and pesticides) (Frick and others, 1998), and fecal-coliform bacteria concentrations (Center for Watershed Protection, 1999). The presence of fecal-coliform bacteria in streams and rivers indicates that contamination by fecal material from human or animal sources has occurred and contact with these waters can result in exposure to pathogenic bacteria often associated with fecal contamination. During 1994 and 1995, elevated concentrations of fecal-coliform bacteria were the most common reason that the Chattahoochee River and tributaries did not meet their designated uses of drinking-water supply, recreation, and fishing. According to the Georgia Department of Natural Resources (1997), during 1994 and 1995, 67 of 77 stream reaches assessed in Metropolitan Atlanta did not meet or only partially met water-quality requirements for designated uses. Excessive concentrations of fecal-coliform bacteria were a contributing factor in 63 of the 67 streams that did not meet or only partially met designated uses. High concentrations of fecal-coliform bacteria have the potential to reduce the recreational value of the river and pose a continued threat, with unknown health risks, to humans that come in contact with the water while fishing, boating, rafting, wading, and swimming.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri20004139","usgsCitation":"Gregory, M.B., and Frick, E.A., 2000, Fecal-coliform bacteria concentrations in streams of the Chattahoochee River National Recreation Area, Metropolitan Atlanta, Georgia, May–October 1994 and 1995: U.S. Geological Survey Water-Resources Investigations Report 2000-4139, 8 p., https://doi.org/10.3133/wri20004139.","productDescription":"8 p.","temporalStart":"1994-05-01","temporalEnd":"1995-10-31","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393886,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_33342.htm"},{"id":9251,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri004139/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","city":"Atlanta","otherGeospatial":"Chattahoochee River National Recreation Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.26489257812499,\n 33.51391942394942\n ],\n [\n -84.67437744140625,\n 33.02017899916362\n ],\n [\n -83.56201171875,\n 34.129994745824746\n ],\n [\n -84.16900634765625,\n 34.49976628863743\n ],\n [\n -85.26489257812499,\n 33.51391942394942\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6e07","contributors":{"authors":[{"text":"Gregory, M. Brian","contributorId":105772,"corporation":false,"usgs":true,"family":"Gregory","given":"M.","email":"","middleInitial":"Brian","affiliations":[],"preferred":false,"id":198091,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frick, Elizabeth A.","contributorId":98714,"corporation":false,"usgs":true,"family":"Frick","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198090,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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":"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.
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).
","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":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","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":29355,"text":"wri004135 - 2000 - Methods for estimating low-flow statistics for Massachusetts streams","interactions":[],"lastModifiedDate":"2012-02-02T00:08:49","indexId":"wri004135","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-4135","title":"Methods for estimating low-flow statistics for Massachusetts streams","docAbstract":"Methods and computer software are described in this report for determining flow duration, low-flow frequency statistics, and August median flows. These low-flow statistics can be estimated for unregulated streams in Massachusetts using different methods depending on whether the location of interest is at a streamgaging station, a low-flow partial-record station, or an ungaged site where no data are available. Low-flow statistics for streamgaging stations can be estimated using standard U.S. Geological Survey methods described in the report. The MOVE.1 mathematical method and a graphical correlation method can be used to estimate low-flow statistics for low-flow partial-record stations. The MOVE.1 method is recommended when the relation between measured flows at a partial-record station and daily mean flows at a nearby, hydrologically similar streamgaging station is linear, and the graphical method is recommended when the relation is curved. Equations are presented for computing the variance and equivalent years of record for estimates of low-flow statistics for low-flow partial-record stations when either a single or multiple index stations are used to determine the estimates. The drainage-area ratio method or regression equations can be used to estimate low-flow statistics for ungaged sites where no data are available. The drainage-area ratio method is generally as accurate as or more accurate than regression estimates when the drainage-area ratio for an ungaged site is between 0.3 and 1.5 times the drainage area of the index data-collection site. Regression equations were developed to estimate the natural, long-term 99-, 98-, 95-, 90-, 85-, 80-, 75-, 70-, 60-, and 50-percent duration flows; the 7-day, 2-year and the 7-day, 10-year low flows; and the August median flow for ungaged sites in Massachusetts. Streamflow statistics and basin characteristics for 87 to 133 streamgaging stations and low-flow partial-record stations were used to develop the equations. The streamgaging stations had from 2 to 81 years of record, with a mean record length of 37 years. The low-flow partial-record stations had from 8 to 36 streamflow measurements, with a median of 14 measurements. All basin characteristics were determined from digital map data. The basin characteristics that were statistically significant in most of the final regression equations were drainage area, the area of stratified-drift deposits per unit of stream length plus 0.1, mean basin slope, and an indicator variable that was 0 in the eastern region and 1 in the western region of Massachusetts. The equations were developed by use of weighted-least-squares regression analyses, with weights assigned proportional to the years of record and inversely proportional to the variances of the streamflow statistics for the stations. Standard errors of prediction ranged from 70.7 to 17.5 percent for the equations to predict the 7-day, 10-year low flow and 50-percent duration flow, respectively. The equations are not applicable for use in the Southeast Coastal region of the State, or where basin characteristics for the selected ungaged site are outside the ranges of those for the stations used in the regression analyses. A World Wide Web application was developed that provides streamflow statistics for data collection stations from a data base and for ungaged sites by measuring the necessary basin characteristics for the site and solving the regression equations. Output provided by the Web application for ungaged sites includes a map of the drainage-basin boundary determined for the site, the measured basin characteristics, the estimated streamflow statistics, and 90-percent prediction intervals for the estimates. An equation is provided for combining regression and correlation estimates to obtain improved estimates of the streamflow statistics for low-flow partial-record stations. An equation is also provided for combining regression and drainage-area ratio estimates to obtain improved e","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri004135","usgsCitation":"Ries, K., and Friesz, P.J., 2000, Methods for estimating low-flow statistics for Massachusetts streams: U.S. Geological Survey Water-Resources Investigations Report 2000-4135, v, 81 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri004135.","productDescription":"v, 81 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2295,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri004135","linkFileType":{"id":5,"text":"html"}},{"id":159425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a1ab","contributors":{"authors":[{"text":"Ries, Kernell G. III kries@usgs.gov","contributorId":1913,"corporation":false,"usgs":true,"family":"Ries","given":"Kernell G.","suffix":"III","email":"kries@usgs.gov","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":false,"id":201398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friesz, Paul J. 0000-0002-4660-2336 pfriesz@usgs.gov","orcid":"https://orcid.org/0000-0002-4660-2336","contributorId":1075,"corporation":false,"usgs":true,"family":"Friesz","given":"Paul","email":"pfriesz@usgs.gov","middleInitial":"J.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":201397,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26592,"text":"wri004198 - 2000 - Occurrence of fecal coliform bacteria in selected streams in Wyoming, 1990-99","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri004198","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-4198","title":"Occurrence of fecal coliform bacteria in selected streams in Wyoming, 1990-99","docAbstract":"The U.S. Geological Survey (USGS), in cooperation with the Wyoming Department of Environmental Quality (WDEQ), is collecting water samples for analysis of fecal coliform bacteria at 18 stream sites as part of a statewide network. Contamination by bacteria of fecal origin in streams where contact recreation is a designated water use is a concern because of potential public-health risk from the presence of enteric pathogens. Fecal coliform concentrations are temporally and spatially variable in Wyoming streams-concentrations ranged from less than 1 to 45,000 colonies per 100 milliliters of water during 1990-99. Fecal coliform concentrations were less than the water-quality criterion of 400 colonies per 100 milliliters in 83 percent of the samples, indicating fecal coliform contamination is not a widespread problem in these Wyoming streams. However, 14 of the 18 monitoring sites had at least one sample in which the fecal coliform concentration exceeded 400 colonies per 100 milliliters at some time during the 10-year period. Fecal coliform concentrations generally are higher during April through September than during October through March. The higher concentrations coincide with the time period when the public-health risk is higher because summer months are when contact recreation use is more likely occurring. Fecal coliform concentrations were positively correlated with discharge and stream temperature and generally were negatively correlated with pH, specific conductance, and dissolved oxygen.","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/wri004198","usgsCitation":"Clark, M.L., and Norris, J.R., 2000, Occurrence of fecal coliform bacteria in selected streams in Wyoming, 1990-99: U.S. Geological Survey Water-Resources Investigations Report 2000-4198, 8 p., https://doi.org/10.3133/wri004198.","productDescription":"8 p.","costCenters":[],"links":[{"id":157346,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1984,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri004198","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692269","contributors":{"authors":[{"text":"Clark, Melanie L. mlclark@usgs.gov","contributorId":1827,"corporation":false,"usgs":true,"family":"Clark","given":"Melanie","email":"mlclark@usgs.gov","middleInitial":"L.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":196671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norris, Jodi R.","contributorId":43746,"corporation":false,"usgs":true,"family":"Norris","given":"Jodi","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":196672,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29622,"text":"wri004178 - 2000 - Geohydrology and water quality at Shanghai Spring and solid-waste management units at the Fort Leonard Wood Military Reservation, Missouri, 1995-98","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri004178","displayToPublicDate":"2001-07-01T00:00:00","publicationYear":"2000","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":"2000-4178","title":"Geohydrology and water quality at Shanghai Spring and solid-waste management units at the Fort Leonard Wood Military Reservation, Missouri, 1995-98","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri004178","usgsCitation":"Schumacher, J., and Imes, J.L., 2000, Geohydrology and water quality at Shanghai Spring and solid-waste management units at the Fort Leonard Wood Military Reservation, Missouri, 1995-98: U.S. Geological Survey Water-Resources Investigations Report 2000-4178, vi, 163 p. :ill. 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