{"pageNumber":"2919","pageRowStart":"72950","pageSize":"25","recordCount":184563,"records":[{"id":80034,"text":"i2698E - 2002 - Backscatter Intensity and Sun-Illuminated Sea Floor Topography of Quadrangles 1 and 2","interactions":[],"lastModifiedDate":"2012-02-10T00:11:39","indexId":"i2698E","displayToPublicDate":"2007-06-19T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2698","subseriesTitle":"GIS","chapter":"E","title":"Backscatter Intensity and Sun-Illuminated Sea Floor Topography of Quadrangles 1 and 2","docAbstract":"The Great South Channel separates the western part of Georges Bank from Nantucket Shoals and is a major conduit for the exchange of water between the Gulf of Maine to the north and the Atlantic Ocean to the south. Water depths range mostly between 65 and 80 m in the region. A minimum depth of 45 m occurs in the east-central part of the mapped area, and a maximum depth of 100 m occurs in the northwest corner. The channel region is characterized by strong tidal and storm currents that flow dominantly north and south. Major topographic features of the seabed were formed by glacial and postglacial processes. Ice containing rock debris moved from north to south, sculpting the region into a broad shallow depression and depositing sediment to form the irregular depressions and low gravelly mounds and ridges that are visible in parts of the mapped area. Many other smaller glacial featuresprobably have been eroded by waves and currents at worksince the time when the region, formerly exposed bylowered sea level or occupied by ice, was invaded by the sea. The low, irregular and somewhat lumpy fabric formed by the glacial deposits is obscured in places by drifting sand and by the linear, sharp fabric formed by modern sand features. Today, sand transported by the strong north-south-flowing tidal and storm currents has formed large, east-west-trending dunes. These bedforms (ranging between 5 and 20 m in height) contrast strongly with, and partly mask, the subdued topography of the older glacial features.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Maps Showing Sea Floor Topography, Sun-Illuminated Sea Floor Topography, and Backscatter Intensity of Quadrangles 1 and 2 in the Great South Channel Region, Western Georges Bank","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/i2698E","collaboration":"Prepared in cooperation with the U.S. National Oceanic and Atmospheric Administration","usgsCitation":"Valentine, P.C., Middleton, T.J., and Fuller, S.J., 2002, Backscatter Intensity and Sun-Illuminated Sea Floor Topography of Quadrangles 1 and 2 (Version 1.0): U.S. Geological Survey IMAP 2698, 1 Sheet: 40 x 57 inches; Also available on CD-ROM, https://doi.org/10.3133/i2698E.","productDescription":"1 Sheet: 40 x 57 inches; Also available on CD-ROM","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192038,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9792,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2698/index.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"25000","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -69.05,40.9 ], [ -69.05,41.13333333333333 ], [ -68.78333333333333,41.13333333333333 ], [ -68.78333333333333,40.9 ], [ -69.05,40.9 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ad9a","contributors":{"authors":[{"text":"Valentine, Page C. 0000-0002-0485-6266 pvalentine@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-6266","contributorId":1947,"corporation":false,"usgs":true,"family":"Valentine","given":"Page","email":"pvalentine@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":291528,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Middleton, Tammie J.","contributorId":27532,"corporation":false,"usgs":true,"family":"Middleton","given":"Tammie","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":291529,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fuller, Sarah J.","contributorId":39878,"corporation":false,"usgs":true,"family":"Fuller","given":"Sarah","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":291530,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70209171,"text":"70209171 - 2002 - Challenges in observational seismology","interactions":[],"lastModifiedDate":"2020-03-20T09:34:06","indexId":"70209171","displayToPublicDate":"2007-03-20T09:32:01","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5944,"text":"International Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Challenges in observational seismology","docAbstract":"

Earthquake seismology became a quantitative scientific discipline after instruments were developed to record seismic waves in the late 19th century (Dewey and Byerly, 1969; Chapter 1 by Agnew). Earthquake seismology is essentially based on field observations. The great progress made in the past several decades was primarily due to increasingly plentiful and high-quality data that are readily distributed. Our ability to collect, process, and analyze earthquake data has been accelerated by advances in electronics, communications, computers, and software (see Chapter 85 edited by Snoke and Garcia-Fernandez).

Instrumental observation of earthquakes has been carried out for a little over 100 years by seismic stations and networks of various sizes, from local to global scales (see Chapter 87 edited by Lahr and van Eck). The observed data have been used, for example, (1) to compute the source parameters of earthquakes, (2) to determine the physical properties of the Earth's interior, (3) to test the theory of plate tectonics, (4) to map active faults, (5) to infer the nature of damaging ground shaking, and (6) to carry out seismic hazard analysis. Construction of a satisfactory theory of the earthquake process has not yet been achieved within the context of physical laws. Good progress, however, has been made in building a physical foundation of the earthquake source process, partly as a result of research directed toward earthquake prediction.

This chapter is intended for a general audience. Technical details are not given, but relevant references and chapters in this Handbook are referred to. The first part of this chapter presents a brief overview of the observational aspects of earthquake seismology, concentrating on instrumental observations of seismic waves generated by earthquakes (i.e., seismic monitoring), and readers are referred to Chapter 49 by Musson and Cecic for noninstrumental observations. A few key developments and practices are summarized by taking a general view, since many national and regional developments have been chronicled in national and institutional reports (see Chapter 79 edited by Kisslinger). In the latter part of this chapter, the nature of seismic monitoring and some challenges in observational seismology are discussed from a personal perspective. Comments of a technical or philosophical nature are given in the Notes at the end of the chapter, and they are referenced by superscript numbers in the text.

","language":"English","publisher":"Elsevier","doi":"10.1016/S0074-6142(02)80220-0","usgsCitation":"Lee, W., 2002, Challenges in observational seismology: International Geophysics, v. 81, no. A, p. 269-281, https://doi.org/10.1016/S0074-6142(02)80220-0.","productDescription":"13 p.","startPage":"269","endPage":"281","costCenters":[],"links":[{"id":373408,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"81","issue":"A","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lee, W.H.K.","contributorId":35303,"corporation":false,"usgs":true,"family":"Lee","given":"W.H.K.","affiliations":[],"preferred":false,"id":785229,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":78992,"text":"wdrID012 - 2002 - Water resources data, Idaho, water year 2001, Volume 2. Upper Columbia River Basin and Snake River Basin below King Hill","interactions":[],"lastModifiedDate":"2020-06-04T18:55:17.376545","indexId":"wdrID012","displayToPublicDate":"2006-08-30T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ID-01-2","title":"Water resources data, Idaho, water year 2001, Volume 2. Upper Columbia River Basin and Snake River Basin below King Hill","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrID012","usgsCitation":"O’Dell, I.O., Lehmann, A., Campbell, A., Beattie, S., and Brennan, T., 2002, Water resources data, Idaho, water year 2001, Volume 2. 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Mountain Creek Lake is a reservoir adjacent to the Naval Weapons Industrial Reserve Plant and the former Naval Air Station in Dallas, Texas. The U.S. Geological Survey began studies of water, sediment, and biota in the reservoir in 1994 after a Resource Conservation and Recovery Act Facility Investigation detected concentrations of organic chemicals on both facilities. Additional reservoir bottom sediment samples were collected during December 1999–January 2000 at the request of the Southern Division Naval Facilities Engineering Command to further define the occurrence and distribution of selected constituents and to supplement available data. The U.S. Geological Survey National Water Quality Laboratory analyzed bottom-sediment samples from 16 box cores and 5 gravity cores for major and trace elements, organochlorine pesticides, polychlorinated biphenyls, polycyclic aromatic hydrocarbons, grain size, and cesium-137.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0253","collaboration":"Prepared in cooperation with the Southern Division Naval Facilities Engineering Command","usgsCitation":"Wilson, J.T., 2002, Chemical data for bottom sediment in Mountain Creek Lake, Dallas, Texas, 1999-2000: U.S. Geological Survey Open-File Report 2002-53, iv, 55 p., https://doi.org/10.3133/ofr0253.","productDescription":"iv, 55 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":7049,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr02053/","linkFileType":{"id":5,"text":"html"}},{"id":192736,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":341864,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/ofr02053/pdf/ofr02-053.pdf","text":"Report","size":"27.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Dallas","otherGeospatial":"Mountain Creek Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97,\n 32.7\n ],\n [\n -96.93,\n 32.7\n ],\n [\n -96.93,\n 32.75\n ],\n [\n -97,\n 32.75\n ],\n [\n -97,\n 32.7\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3e9a","contributors":{"authors":[{"text":"Wilson, Jennifer T. 0000-0003-4481-6354 jenwilso@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-6354","contributorId":1782,"corporation":false,"usgs":true,"family":"Wilson","given":"Jennifer","email":"jenwilso@usgs.gov","middleInitial":"T.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70645,"text":"pp1654 - 2002 - Mineral and energy resource assessment of the Gallatin National Forest (exclusive of the Absaroka-Beartooth study area), in Gallatin, Madison, Meagher, Park, and Sweet Grass Counties, south-central Montana","interactions":[],"lastModifiedDate":"2024-01-09T22:10:17.015343","indexId":"pp1654","displayToPublicDate":"2005-06-02T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1654","title":"Mineral and energy resource assessment of the Gallatin National Forest (exclusive of the Absaroka-Beartooth study area), in Gallatin, Madison, Meagher, Park, and Sweet Grass Counties, south-central Montana","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1654","isbn":"0607971855","usgsCitation":"Hammarstrom, J.M., Wilson, A.B., Elliott, J., Van Gosen, B.S., Carlson, R.R., Lee, G.K., Kulik, D.M., M’Gonigle, J.W., and Perry, W.J., 2002, Mineral and energy resource assessment of the Gallatin National Forest (exclusive of the Absaroka-Beartooth study area), in Gallatin, Madison, Meagher, Park, and Sweet Grass Counties, south-central Montana (Version 1.0, use with USGS I-2584): U.S. Geological Survey Professional Paper 1654, 194 p., https://doi.org/10.3133/pp1654.","productDescription":"194 p.","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":424242,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73689.htm","linkFileType":{"id":5,"text":"html"}},{"id":6748,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/2005/1654/","linkFileType":{"id":5,"text":"html"}},{"id":185577,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"5000000","country":"United States","state":"Montana","county":"Gallatin County, Madison County, Meagher County, Park County, Sweet Grass County","otherGeospatial":"Gallatin National Forest","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110.1583,\n 46.2833\n ],\n [\n -111.5917,\n 46.2833\n ],\n [\n -111.5917,\n 44.5\n ],\n [\n -110.1583,\n 44.5\n ],\n [\n -110.1583,\n 46.2833\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.0, use with USGS I-2584","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635810","contributors":{"authors":[{"text":"Hammarstrom, Jane M. 0000-0003-2742-3460 jhammars@usgs.gov","orcid":"https://orcid.org/0000-0003-2742-3460","contributorId":1226,"corporation":false,"usgs":true,"family":"Hammarstrom","given":"Jane","email":"jhammars@usgs.gov","middleInitial":"M.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":891785,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, Anna B. 0000-0002-9737-2614 awilson@usgs.gov","orcid":"https://orcid.org/0000-0002-9737-2614","contributorId":1619,"corporation":false,"usgs":true,"family":"Wilson","given":"Anna","email":"awilson@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282811,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elliott, James E.","contributorId":15595,"corporation":false,"usgs":true,"family":"Elliott","given":"James E.","affiliations":[],"preferred":false,"id":891786,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Van Gosen, Bradley S. 0000-0003-4214-3811 bvangose@usgs.gov","orcid":"https://orcid.org/0000-0003-4214-3811","contributorId":1174,"corporation":false,"usgs":true,"family":"Van Gosen","given":"Bradley","email":"bvangose@usgs.gov","middleInitial":"S.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282810,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carlson, Robert R.","contributorId":71944,"corporation":false,"usgs":true,"family":"Carlson","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":891787,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lee, Gregory K. glee@usgs.gov","contributorId":1220,"corporation":false,"usgs":true,"family":"Lee","given":"Gregory","email":"glee@usgs.gov","middleInitial":"K.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":891788,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kulik, Dolores M.","contributorId":83091,"corporation":false,"usgs":true,"family":"Kulik","given":"Dolores","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":891789,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"M’Gonigle, John W.","contributorId":10397,"corporation":false,"usgs":true,"family":"M’Gonigle","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":891790,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Perry, William J. Jr.","contributorId":32498,"corporation":false,"usgs":true,"family":"Perry","given":"William","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":891791,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":70247,"text":"ds84 - 2002 - Time-of-travel of solute data collected by the Mississippi Department of Environmental Quality for Mississippi streams","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"ds84","displayToPublicDate":"2005-03-18T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84","title":"Time-of-travel of solute data collected by the Mississippi Department of Environmental Quality for Mississippi streams","docAbstract":"This report summarizes the time-of-travel of solutes information for Mississippi streams that is available in the files at the Mississippi Department of Environmental Quality, Office of Pollution Control. The time-of-travel information was tabulated for 112 miles of stream reaches in eight of the ten major drainage basins in the State. The data were collected during studies conducted from 1981 through 1998. Estimation of time-of-travel of solutes is important for environmental studies of streams and may be critical in the event of accidental or other spills of contaminants into a waterway.","language":"ENGLISH","doi":"10.3133/ds84","usgsCitation":"Kerry, J.A., 2002, Time-of-travel of solute data collected by the Mississippi Department of Environmental Quality for Mississippi streams: U.S. Geological Survey Data Series 84, iv, 20 p. report, ill., https://doi.org/10.3133/ds84.","productDescription":"iv, 20 p. report, ill.","costCenters":[],"links":[{"id":6954,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://ms.water.usgs.gov/publications/time_of_travel_ds84.html","linkFileType":{"id":5,"text":"html"}},{"id":191415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699bb4","contributors":{"authors":[{"text":"Kerry, J. Arthur","contributorId":74827,"corporation":false,"usgs":true,"family":"Kerry","given":"J.","email":"","middleInitial":"Arthur","affiliations":[],"preferred":false,"id":282061,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":69629,"text":"i2778 - 2002 - Geologic Map of the Katmai Volcanic Cluster, Katmai National Park, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:13:53","indexId":"i2778","displayToPublicDate":"2004-12-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2778","title":"Geologic Map of the Katmai Volcanic Cluster, Katmai National Park, Alaska","docAbstract":"This digital publication contains all the geologic map information used to publish U.S. Geological Survey Geologic Investigations Map Series I-2778 (Hildreth and Fierstein, 2003). This is a geologic map of the Katmai volcanic cluster on the Alaska Peninsula (including Mount Katmai, Trident Volcano, Mount Mageik, Mount Martin, Mount Griggs, Snowy Mountain, Alagogshak volcano, and Novarupta volcano), and shows the distribution of ejecta from the great eruption of June, 1912 at Novarupta. Widely scattered erosional remnants of volcanic rocks, unrelated to but in the vicinity of the Katmai cluster, are also mapped. Distribution of glacial deposits, large landslides, debris avalanches, and surficial deposits are a snapshot of an ever-changing landscape.","language":"ENGLISH","doi":"10.3133/i2778","usgsCitation":"Hildreth, W., and Fierstein, J., 2002, Geologic Map of the Katmai Volcanic Cluster, Katmai National Park, Alaska: U.S. Geological Survey IMAP 2778, map, 62 by 43 inches + 45 p. pamphlet, https://doi.org/10.3133/i2778.","productDescription":"map, 62 by 43 inches + 45 p. pamphlet","costCenters":[],"links":[{"id":110497,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_68329.htm","linkFileType":{"id":5,"text":"html"},"description":"68329"},{"id":191651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6283,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2778/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a84d9","contributors":{"authors":[{"text":"Hildreth, Wes","contributorId":15996,"corporation":false,"usgs":true,"family":"Hildreth","given":"Wes","email":"","affiliations":[],"preferred":false,"id":280762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fierstein, Judy","contributorId":88337,"corporation":false,"usgs":true,"family":"Fierstein","given":"Judy","email":"","affiliations":[],"preferred":false,"id":280763,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44593,"text":"wri20024053 - 2002 - Louisiana ground-water map no. 13: Hydrogeology and potentiometric surface of the Sparta aquifer in northern Louisiana, October 1996","interactions":[],"lastModifiedDate":"2023-11-27T20:37:42.713965","indexId":"wri20024053","displayToPublicDate":"2004-11-01T02:00:00","publicationYear":"2002","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":"2002-4053","title":"Louisiana ground-water map no. 13: Hydrogeology and potentiometric surface of the Sparta aquifer in northern Louisiana, October 1996","docAbstract":"This report describes the thickness and areal extent of the Sparta aquifer, identifies sands within the fresh-water extent of the aquifer, and presents data and a map that illustrate the generalized potentiometric surface (water levels) during October 1996. The report includes a detailed geophysical log, structure contour maps, hydrogeologic sections, and hydrographs of water levels in selected wells. The potentiometric surface-map can be used for determining direction of ground-water flow, hydraulic gradients, and the effects of withdrawals on the aquifer.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri20024053","collaboration":"Prepared in cooperation with the Louisiana Department of Transportation and Development, Public Works and Water Resources Division, Water Resources Section","usgsCitation":"Brantly, J.A., Seanor, R.C., and McCoy, K.L., 2002, Louisiana ground-water map no. 13: Hydrogeology and potentiometric surface of the Sparta aquifer in northern Louisiana, October 1996: U.S. Geological Survey Water-Resources Investigations Report 2002-4053, 3 Plates: 28.00 x 24.00 inches, https://doi.org/10.3133/wri20024053.","productDescription":"3 Plates: 28.00 x 24.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"links":[{"id":422978,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51838.htm","linkFileType":{"id":5,"text":"html"}},{"id":99308,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2002/4053/plate-1_sheet_3.pdf","text":"Sheet 3","linkFileType":{"id":1,"text":"pdf"}},{"id":99307,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2002/4053/plate-1_sheet_2.pdf","text":"Sheet 2","linkFileType":{"id":1,"text":"pdf"}},{"id":14048,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri02-4053/","linkFileType":{"id":5,"text":"html"}},{"id":99306,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2002/4053/plate-1_sheet_1.pdf","text":"Sheet 1","linkFileType":{"id":1,"text":"pdf"}},{"id":120551,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4053/report-thumb.jpg"},{"id":99305,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4053/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Louisiana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94,\n 31\n ],\n [\n -94,\n 33\n ],\n [\n -91.33333333333333,\n 33\n ],\n [\n -91.33333333333333,\n 31\n ],\n [\n -94,\n 31\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640f0e","contributors":{"authors":[{"text":"Brantly, Jeffrey A. jbrantly@usgs.gov","contributorId":5405,"corporation":false,"usgs":true,"family":"Brantly","given":"Jeffrey","email":"jbrantly@usgs.gov","middleInitial":"A.","affiliations":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230057,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seanor, Ronald C. 0000-0001-5735-5580 rcseanor@usgs.gov","orcid":"https://orcid.org/0000-0001-5735-5580","contributorId":3731,"corporation":false,"usgs":true,"family":"Seanor","given":"Ronald","email":"rcseanor@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":230056,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCoy, Kaycee L.","contributorId":32228,"corporation":false,"usgs":true,"family":"McCoy","given":"Kaycee","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":230058,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":50639,"text":"ofr02209 - 2002 - Seismicity maps of the Santa Rosa 1° x 2° quadrangle, California for the period 1969-1995","interactions":[],"lastModifiedDate":"2021-12-30T19:28:24.853987","indexId":"ofr02209","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2002","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":"2002-209","title":"Seismicity maps of the Santa Rosa 1° x 2° quadrangle, California for the period 1969-1995","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02209","usgsCitation":"Priess, J.S., Walter, S.R., and Oppenheimer, D.H., 2002, Seismicity maps of the Santa Rosa 1° x 2° quadrangle, California for the period 1969-1995 (Version 1.0): U.S. Geological Survey Open-File Report 2002-209, HTML Document, https://doi.org/10.3133/ofr02209.","productDescription":"HTML Document","costCenters":[],"links":[{"id":170180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4131,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-209/","linkFileType":{"id":5,"text":"html"}},{"id":110528,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_69596.htm","linkFileType":{"id":5,"text":"html"},"description":"69596"}],"country":"United States","state":"California","otherGeospatial":"Santa Rosa 1° x 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.8,\n 38\n ],\n [\n -122,\n 38\n ],\n [\n -122,\n 39\n ],\n [\n -123.8,\n 39\n ],\n [\n -123.8,\n 38\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa927","contributors":{"authors":[{"text":"Priess, Jeroen S.","contributorId":105172,"corporation":false,"usgs":true,"family":"Priess","given":"Jeroen","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":241998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walter, Stephen R.","contributorId":34954,"corporation":false,"usgs":true,"family":"Walter","given":"Stephen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":241997,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oppenheimer, David H. oppen@usgs.gov","contributorId":1112,"corporation":false,"usgs":true,"family":"Oppenheimer","given":"David","email":"oppen@usgs.gov","middleInitial":"H.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":241996,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44602,"text":"wri024088 - 2002 - Louisiana ground-water map no. 14: Potentiometric surface, January 2001, and water-level changes, June 2000 to January 2001, of the Chicot aquifer system in southwestern Louisiana","interactions":[],"lastModifiedDate":"2023-06-08T18:49:46.971925","indexId":"wri024088","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2002","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":"2002-4088","title":"Louisiana ground-water map no. 14: Potentiometric surface, January 2001, and water-level changes, June 2000 to January 2001, of the Chicot aquifer system in southwestern Louisiana","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024088","usgsCitation":"Lovelace, J.K., Fontenot, J.W., and Frederick, C.P., 2002, Louisiana ground-water map no. 14: Potentiometric surface, January 2001, and water-level changes, June 2000 to January 2001, of the Chicot aquifer system in southwestern Louisiana: U.S. Geological Survey Water-Resources Investigations Report 2002-4088, 2 Plates: 27.00 × 24.00 inches, https://doi.org/10.3133/wri024088.","productDescription":"2 Plates: 27.00 × 24.00 inches","costCenters":[],"links":[{"id":173652,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94344,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://wise.er.usgs.gov/dp/pdfs/WRI_02-4088.pdf","text":"Plates 1 & 2","linkFileType":{"id":1,"text":"pdf"}},{"id":396272,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52700.htm"}],"country":"United States","state":"Louisiana","otherGeospatial":"Chicot aquifer system","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.636474609375,\n 29.554345125748267\n ],\n [\n -91.53259277343749,\n 29.554345125748267\n ],\n [\n -91.53259277343749,\n 31.067050772707812\n ],\n [\n -93.636474609375,\n 31.067050772707812\n ],\n [\n -93.636474609375,\n 29.554345125748267\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db6439f9","contributors":{"authors":[{"text":"Lovelace, J. K.","contributorId":64279,"corporation":false,"usgs":true,"family":"Lovelace","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":230077,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fontenot, J. W.","contributorId":43836,"corporation":false,"usgs":true,"family":"Fontenot","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":230076,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frederick, C. P. 0000-0003-1762-519X pfreder@usgs.gov","orcid":"https://orcid.org/0000-0003-1762-519X","contributorId":6515,"corporation":false,"usgs":true,"family":"Frederick","given":"C.","email":"pfreder@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":false,"id":230075,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":39987,"text":"wri024116 - 2002 - Simulation of hydrodynamics, temperature, and dissolved oxygen in Beaver Lake, Arkansas, 1994-1995","interactions":[],"lastModifiedDate":"2012-02-02T00:10:53","indexId":"wri024116","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2002","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":"2002-4116","title":"Simulation of hydrodynamics, temperature, and dissolved oxygen in Beaver Lake, Arkansas, 1994-1995","docAbstract":"The tailwaters of Beaver Lake and other White River reservoirs support a cold-water trout fishery of significant economic yield in northwestern Arkansas. The Arkansas Game and Fish Commission has requested an increase in existing minimum flows through the Beaver Lake dam to increase the amount of fishable waters downstream. Information is needed to assess the impact of additional minimum flows on temperature and dissolved-oxygen qualities of reservoir water above the dam and the release water. A two-dimensional, laterally averaged hydrodynamic, thermal and dissolved-oxygen model was developed and calibrated for Beaver Lake, Arkansas. The model simulates surface-water elevation, currents, heat transport and dissolved-oxygen dynamics. The model was developed to assess the impacts of proposed increases in minimum flows from 1.76 cubic meters per second (the existing minimum flow) to 3.85 cubic meters per second (the additional minimum flow). Simulations included assessing (1) the impact of additional minimum flows on tailwater temperature and dissolved-oxygen quality and (2) increasing initial water-surface elevation 0.5 meter and assessing the impact of additional minimum flow on tailwater temperatures and dissolved-oxygen concentrations. The additional minimum flow simulation (without increasing initial pool elevation) appeared to increase the water temperature (<0.9 degrees Celsius) and decrease dissolved oxygen concentration (<2.2 milligrams per liter) in the outflow discharge. Conversely, the additional minimum flow plus initial increase in pool elevation (0.5 meter) simulation appeared to decrease outflow water temperature (0.5 degrees Celsius) and increase dissolved oxygen concentration (<1.2 milligrams per liter) through time. However, results from both minimum flow scenarios for both water temperature and dissolved oxygen concentration were within the boundaries or similar to the error between measured and simulated water column profile values.","language":"ENGLISH","doi":"10.3133/wri024116","usgsCitation":"Haggard, B., and Green, W.R., 2002, Simulation of hydrodynamics, temperature, and dissolved oxygen in Beaver Lake, Arkansas, 1994-1995: U.S. Geological Survey Water-Resources Investigations Report 2002-4116, 21 p., https://doi.org/10.3133/wri024116.","productDescription":"21 p.","costCenters":[],"links":[{"id":171337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3671,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://ar.water.usgs.gov/LOCAL_REPORTS/WRIR_02-4116.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699cec","contributors":{"authors":[{"text":"Haggard, Brian","contributorId":81548,"corporation":false,"usgs":true,"family":"Haggard","given":"Brian","email":"","affiliations":[],"preferred":false,"id":222759,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, W. Reed","contributorId":87886,"corporation":false,"usgs":true,"family":"Green","given":"W.","email":"","middleInitial":"Reed","affiliations":[],"preferred":false,"id":222760,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":53430,"text":"wri024132 - 2002 - Ground-Water Resource Assessment in the Rio Grande de Manati Alluvial Plain, Rio Arriba Saliente Area, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:11:58","indexId":"wri024132","displayToPublicDate":"2004-11-01T00:00:00","publicationYear":"2002","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":"2002-4132","title":"Ground-Water Resource Assessment in the Rio Grande de Manati Alluvial Plain, Rio Arriba Saliente Area, Puerto Rico","docAbstract":"The alluvial aquifer within a 160-acre area of the Rio Grande de Manati alluvial plain was investigated to evaluate its potential as a water-supply source for the Barrios Rio Arriba Saliente and Pugnado Afuera, municipio of Manati, Puerto Rico. Analysis of well boring samples and the results of electric resistivity surveys indicate that the average thickness of the unconsolidated alluvial deposits in the study area is about 100 to 110 feet. The alluvium is a mixture of sand and gravel, which generally has a porosity of 0.2 to 0.35. Short-duration pump tests in small-diameter piezometers indicate that the alluvial aquifer has a hydraulic conductivity of about 200 feet per day and a transmissivity of about 7,900 feet squared per day. \r\n\r\nAnalyses of water levels in piezometers, combined with stage measurements at a series of surveyed reference points along the Rio Grande de Manati channel, indicate that the water-table gradient in the alluvial aquifer is about 0.001, and that ground-water flow is generally from south to north, in the general direction of river flow. The water-table data indicate that the Rio Grande de Manati is the principal source of ground-water recharge to the alluvial aquifer in the study area. Because base flow for the Rio Grande de Manati is usually greater than 44 cubic feet per second, a continuous withdrawal rate of 0.5 to 1.0 cubic foot per second (225 to 450 gallons per minute) from a production well is possible. \r\n\r\nChemical analysis of a ground-water sample indicates that the alluvial aquifer water meets U.S. Environmental Protection Agency secondary standards for selected constituents. Bacteriological analysis of ground-water samples indicates that the ground water contains little or no fecal coliform or fecal streptococcus bacteria. Although long-term data from upstream of the study area indicate high levels of fecal coliform and fecal streptococcus prior to 1996, bacteriological analyses of Rio Grande de Manati water samples obtained during the present study indicate that fecal coliform and fecal streptococcus concentrations are within the standards for surface water intended for use (or with the potential for use) as a raw source of public water supply in Puerto Rico. \r\n\r\nIf a production well were constructed in the study area, it would be located close to the river channel (within 500 to 800 feet). Pumping from the porous and permeable alluvial aquifer close to the river channel could substantially enhance recharge from the Rio Grande de Manati channel to the aquifer. Enhanced recharge could shorten travel times for ground water in the aquifer, which might not allow sufficient time to attenuate bacteria and viruses. Travel times for bacteria moving from the river channel to a hypothetical production well were estimated using the numerical transport model MODFLOW/MT3DMS with an uncalibrated model of the alluvial aquifer. The model assumes a well pumping at 1 cubic foot per second. The transport of particles from the river to the well is most sensitive to the porosity of the aquifer and the pumping rate of the well. Sensitivity analysis indicates that a decrease in pumpage will increase the time of travel for particles to move from the river to the pumping well. The model indicates that the leading edge of a plume would reach the production well in about 40 days assuming a porosity of 0.20, 60 days assuming a porosity of 0.275, and about 70 days assuming a porosity of 0.35. If the well were moved 50 feet further from the river, the leading edge of the plume would reach the well in about 50 days assuming a porosity of 0.20 and about 70 days assuming a porosity of 0.275. These estimates are considered worse case estimates because no decay rate was included in the simulation, and because the hypothetical well was located in the center of the alluvial plain rather than further eastward, away from the river channel.","language":"ENGLISH","doi":"10.3133/wri024132","usgsCitation":"Torres-Gonzalez, S., Gómez-Gómez, F., and Warne, A.G., 2002, Ground-Water Resource Assessment in the Rio Grande de Manati Alluvial Plain, Rio Arriba Saliente Area, Puerto Rico (Online only): U.S. Geological Survey Water-Resources Investigations Report 2002-4132, 35 p., https://doi.org/10.3133/wri024132.","productDescription":"35 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":5213,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pr.water.usgs.gov/public/online_pubs/wri02_4132/index.html","linkFileType":{"id":5,"text":"html"}},{"id":180714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d532","contributors":{"authors":[{"text":"Torres-Gonzalez, Sigfredo sttorres@usgs.gov","contributorId":3997,"corporation":false,"usgs":true,"family":"Torres-Gonzalez","given":"Sigfredo","email":"sttorres@usgs.gov","affiliations":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gómez-Gómez, Fernando","contributorId":31366,"corporation":false,"usgs":true,"family":"Gómez-Gómez","given":"Fernando","affiliations":[],"preferred":false,"id":247575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warne, Andrew G.","contributorId":9714,"corporation":false,"usgs":true,"family":"Warne","given":"Andrew","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":247574,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":39866,"text":"fs12802 - 2002 - NWISWeb: New Site for the Nation's Water Data","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"fs12802","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"128-02","title":"NWISWeb: New Site for the Nation's Water Data","language":"ENGLISH","doi":"10.3133/fs12802","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2002, NWISWeb: New Site for the Nation's Water Data: U.S. Geological Survey Fact Sheet 128-02, 2 p., https://doi.org/10.3133/fs12802.","productDescription":"2 p.","costCenters":[],"links":[{"id":120300,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_128_02.jpg"},{"id":3578,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/fs-128-02/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4503","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":529927,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":50087,"text":"fs11202 - 2002 - Fractured-rock aquifers, understanding an increasingly important source of water","interactions":[],"lastModifiedDate":"2023-03-30T14:21:52.330419","indexId":"fs11202","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"112-02","title":"Fractured-rock aquifers, understanding an increasingly important source of water","docAbstract":"

Ground water is one of the Nation's most important natural resources. It provides drinking water to communities, supports industry and agriculture, and sustains streams and wetlands. A long record of contributions exists in understanding ground-water movement in sand and gravel aquifers; historically, these aquifers were easily accessible and the first to be investigated. With increased demand for water, communities are looking to fractured-rock aquifers, where water moves through fractures in the rock. Fractures, however, may not always convey or store large quantities of water. Understanding ground-water flow through fractured-rock aquifers is an area of ground-water research that will have increasing importance to our Nation over the coming years. Many areas of the United States rely on fractured-rock aquifers for water supply. In addition, areas experiencing population growth in the Northeast, Southeast, and mountainous regions of the West are likely to rely heavily on water supplies from fractured-rock aquifers. Finding water for thirsty communities, however, is not the only societal issue requiring an understanding of ground-water flow in fractured rock. Land-use practices affect water quality in fractured-rock aquifers, particularly where ground water flows rapidly through fractures. Fractured rock aquifers also are viewed as potential repositories for radioactive and other types of waste, where it is desirable for the ground water to be inaccessible or move at a very slow rate.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs11202","usgsCitation":"Shapiro, A.M., 2002, Fractured-rock aquifers, understanding an increasingly important source of water: U.S. Geological Survey Fact Sheet 112-02, 2 p., https://doi.org/10.3133/fs11202.","productDescription":"2 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":414959,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0112/fs11202.pdf","text":"Report","size":"2.25 MB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 112-02"},{"id":125124,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0112/coverthb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ce4b07f02db6a945e","contributors":{"authors":[{"text":"Shapiro, Allen M. 0000-0002-6425-9607 ashapiro@usgs.gov","orcid":"https://orcid.org/0000-0002-6425-9607","contributorId":2164,"corporation":false,"usgs":true,"family":"Shapiro","given":"Allen","email":"ashapiro@usgs.gov","middleInitial":"M.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":240746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":50740,"text":"fs02102 - 2002 - The Atchafalaya Basin : river of trees","interactions":[],"lastModifiedDate":"2012-02-02T00:11:17","indexId":"fs02102","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"021-02","title":"The Atchafalaya Basin : river of trees","language":"ENGLISH","doi":"10.3133/fs02102","usgsCitation":"Demas, C.R., Brazelton, S.R., and Powell, N.J., 2002, The Atchafalaya Basin : river of trees: U.S. Geological Survey Fact Sheet 021-02, 1 sheet : col. ill., col. map ; 28 cm., https://doi.org/10.3133/fs02102.","productDescription":"1 sheet : col. ill., col. map ; 28 cm.","costCenters":[],"links":[{"id":94357,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://la.water.usgs.gov/publications/pdfs/FS-021-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_021_02.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db68284d","contributors":{"authors":[{"text":"Demas, Charles R.","contributorId":36121,"corporation":false,"usgs":true,"family":"Demas","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":242198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brazelton, Sebastian R.","contributorId":56621,"corporation":false,"usgs":true,"family":"Brazelton","given":"Sebastian","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":242199,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Powell, Nancy J.","contributorId":98801,"corporation":false,"usgs":true,"family":"Powell","given":"Nancy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":242200,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":50088,"text":"fs11302 - 2002 - Investigation of the geology and hydrology of the Coconino Plateau of northern Arizona: a project of the Arizona Rural Watershed Initiative","interactions":[],"lastModifiedDate":"2014-06-13T17:23:18","indexId":"fs11302","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"113-02","title":"Investigation of the geology and hydrology of the Coconino Plateau of northern Arizona: a project of the Arizona Rural Watershed Initiative","docAbstract":"

The water resources of the Coconino Plateau in northern Arizona are under increasing demand as a result of development. The population of this arid region continues to grow, and the number of visitors to the many national and state parks and monuments in the region has increased annually. The sustainability, protection, and maintenance of springs and seeps and associated riparian habitat on the Coconino Plateau are major issues that have broad public and governmental support.

\n
\n

Regional stakeholders agree that an improved understanding of the regional hydrogeologic system is needed to address the concerns of water supply and ground-water sustainability. The base of information required to adequately describe the hydrogeology of the Coconino Plateau currently does not exist. Hydrogeologic data is most abundant for large population centers like Flagstaff and Sedona, but is sparse for less populated areas like Williams, Tusayan, Valle, and Cameron. There are still large parts of the Coconino Plateau for which there is no basic geologic or hydrologic information available. In order to develop a hydrogeologic framework for the Coconino Plateau, a comprehensive effort is needs to compile existent data and collect additional data to fill in data gaps and reinforce limited information.

\n
\n

In 1999, the U.S. Geological Survey (USGS) began an assessment of the hydrogeology of the Coconino Plateau in cooperation with the Arizona Department of Water Resources (ADWR) as part of the Rural Watershed Initiative, a program established by the State of Arizona and managed by the ADWR. Assessments also are underway in the upper-middle Verde River watershed (Woodhouse and others, 2002) to the south and in the Mogollon Highlands to the southeast (Parker and Flynn, 2000).

\n
\n

Each study has as its objectives: (1) the collection, compilation, and evaluation of all existing geologic, hydrologic, and related data pertaining to the study area and the creation of a database that is readily accessible to the public and (2) the development of an understanding of the hydrogeologic framework, which is the relation between hydrologic and geologic properties, that can be used for water-resources management purposes and that will support the development of conceptual and interpretive models that can be used to evaluate the effects of climate and water use on regional water resources.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs11302","collaboration":"Prepared in cooperation with the Arizona Department of Water Resources","usgsCitation":"Flynn, M., and Bills, D., 2002, Investigation of the geology and hydrology of the Coconino Plateau of northern Arizona: a project of the Arizona Rural Watershed Initiative: U.S. Geological Survey Fact Sheet 113-02, 4 p., https://doi.org/10.3133/fs11302.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":288603,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288602,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/0113-02/report.pdf"}],"country":"United States","state":"Arizona","otherGeospatial":"Coconino Plateau","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.2018,34.4884 ], [ -113.2018,36.9257 ], [ -110.8575,36.9257 ], [ -110.8575,34.4884 ], [ -113.2018,34.4884 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47c8e4b07f02db4ab7e1","contributors":{"authors":[{"text":"Flynn, Marilyn E. meflynn@usgs.gov","contributorId":1039,"corporation":false,"usgs":true,"family":"Flynn","given":"Marilyn E.","email":"meflynn@usgs.gov","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":240747,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bills, Donald J. djbills@usgs.gov","contributorId":4180,"corporation":false,"usgs":true,"family":"Bills","given":"Donald J.","email":"djbills@usgs.gov","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":false,"id":240748,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32738,"text":"fs05102 - 2002 - Glacial ice cores reveal a record of natural and anthropogenic atmospheric mercury deposition for the last 270 years","interactions":[],"lastModifiedDate":"2025-03-06T15:02:59.720942","indexId":"fs05102","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"051-02","displayTitle":"Glacial Ice Cores Reveal A Record of Natural and Anthropogenic Atmospheric Mercury Deposition for the Last 270 Years","title":"Glacial ice cores reveal a record of natural and anthropogenic atmospheric mercury deposition for the last 270 years","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs05102","usgsCitation":"Krabbenhoft, D.P., and Schuster, P.F., 2002, Glacial ice cores reveal a record of natural and anthropogenic atmospheric mercury deposition for the last 270 years: U.S. Geological Survey Fact Sheet 051-02, 2 p., https://doi.org/10.3133/fs05102.","productDescription":"2 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":60657,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0051/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123169,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0051/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a720","contributors":{"authors":[{"text":"Krabbenhoft, David P. 0000-0003-1964-5020 dpkrabbe@usgs.gov","orcid":"https://orcid.org/0000-0003-1964-5020","contributorId":1658,"corporation":false,"usgs":true,"family":"Krabbenhoft","given":"David","email":"dpkrabbe@usgs.gov","middleInitial":"P.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true}],"preferred":true,"id":209068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schuster, Paul F. 0000-0002-8314-1372 pschuste@usgs.gov","orcid":"https://orcid.org/0000-0002-8314-1372","contributorId":1360,"corporation":false,"usgs":true,"family":"Schuster","given":"Paul","email":"pschuste@usgs.gov","middleInitial":"F.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":209067,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32736,"text":"fs04202 - 2002 - Effects of Urbanization on Stream Ecosystems","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"fs04202","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"042-02","title":"Effects of Urbanization on Stream Ecosystems","language":"ENGLISH","doi":"10.3133/fs04202","usgsCitation":"Couch, C., and Hamilton, P., 2002, Effects of Urbanization on Stream Ecosystems: U.S. Geological Survey Fact Sheet 042-02, NA, https://doi.org/10.3133/fs04202.","productDescription":"NA","costCenters":[],"links":[{"id":121750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_042_02.jpg"},{"id":3315,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/fs04202/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624e0a","contributors":{"authors":[{"text":"Couch, Carol","contributorId":74426,"corporation":false,"usgs":true,"family":"Couch","given":"Carol","affiliations":[],"preferred":false,"id":209062,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamilton, Pixie","contributorId":105351,"corporation":false,"usgs":true,"family":"Hamilton","given":"Pixie","affiliations":[],"preferred":false,"id":209063,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32739,"text":"fs05202 - 2002 - WaterWatch - Maps and graphs of current water resources conditions","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"fs05202","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"052-02","title":"WaterWatch - Maps and graphs of current water resources conditions","language":"ENGLISH","doi":"10.3133/fs05202","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2002, WaterWatch - Maps and graphs of current water resources conditions: U.S. Geological Survey Fact Sheet 052-02, NA, https://doi.org/10.3133/fs05202.","productDescription":"NA","costCenters":[],"links":[{"id":3318,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/fs-052-02/","linkFileType":{"id":5,"text":"html"}},{"id":119246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_052_02.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c4d","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":529443,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44603,"text":"wri024089 - 2002 - Trace elements and organic compounds in bed sediment from selected streams in southern Louisiana, 1998","interactions":[],"lastModifiedDate":"2012-02-02T00:10:27","indexId":"wri024089","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2002","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":"2002-4089","title":"Trace elements and organic compounds in bed sediment from selected streams in southern Louisiana, 1998","docAbstract":"Bed-sediment samples from 21 selected streams in southern Louisiana were collected and analyzed for the presence of trace elements and organic compounds during 1998 as part of the U.S. Geological Survey National Water-Quality Assessment Program. Concentrations of selected trace elements and organic compounds were compared on the basis of sediment-quality criteria, land use, and grain size; concentrations of selected trace elements also were compared with concentrations from previous studies. Concentrations of seven selected trace elements and 21 organic compounds were evaluated with sediment-quality criteria established by the Canadian Council of Ministers of the Environment. Concentrations of selected trace elements and organic compounds were highest at sites draining urban and agricultural areas and may result from cumulative effects of relatively high percentages of fine-grained material, iron, and organic material. Concentrations exceeding sediment-quality criteria for the protection of aquatic life occurred most frequently at Bayou Grosse Tete at Rosedale and Bayou Lafourche below weir at Thibodaux. Exceedance of Interim Sediment Quality Guidelines occurred most frequently for arsenic and chromium. Trace-element concentrations in fine-grained samples were compared with concentrations in bulk samples and were determined to be significantly different, and concentrations were generally higher in finegrained sediment. Shapiro-Wilk, paired t-test, and Wilcoxon rank sum statistical procedures, with an alpha of 0.05, were used to compare concentrations of 21 trace elements, total organic carbon, and total carbon in finegrained and bulk sediment samples for 19 sites. Significant differences were determined between fine-grained and bulk sediment samples for aluminum, barium, beryllium, chromium, copper, iron, lithium, nickel, phosphorus, selenium, titanium, and zinc concentrations. Of 133 paired concentrations, 69 percent were greater in fine-grained samples, and 23 percent were greater in bulk samples. Comparisons with data from previous studies indicate increases by more than 20 percent in concentrations of antimony at Bayou Lafourche below weir at Thibodaux, arsenic and chromium at Tickfaw River at Liverpool, lead at Bayou Lafourche below weir at Thibodaux, and zinc at Bayou Lafourche below weir at Thibodaux and Vermilion River at Perry. Historic comparisons also indicate decreases by more than 20 percent in concentrations of chromium at Bayou des Cannes near Eunice and mercury at Mermentau River at Mermentau.","language":"ENGLISH","doi":"10.3133/wri024089","usgsCitation":"Skrobialowski, S.C., 2002, Trace elements and organic compounds in bed sediment from selected streams in southern Louisiana, 1998: U.S. Geological Survey Water-Resources Investigations Report 2002-4089, vi, 39 p. : col. maps ; 28 cm., https://doi.org/10.3133/wri024089.","productDescription":"vi, 39 p. : col. maps ; 28 cm.","costCenters":[],"links":[{"id":173653,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94340,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://la.water.usgs.gov/publications/pdfs/WRI_02-4089.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4893e4b07f02db520fbc","contributors":{"authors":[{"text":"Skrobialowski, Stanley C. 0000-0001-8627-0279 sski@usgs.gov","orcid":"https://orcid.org/0000-0001-8627-0279","contributorId":1402,"corporation":false,"usgs":true,"family":"Skrobialowski","given":"Stanley","email":"sski@usgs.gov","middleInitial":"C.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":230078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32682,"text":"fs07602 - 2002 - Monitoring and Assessing our Nation's Water Quality","interactions":[],"lastModifiedDate":"2012-02-02T00:09:14","indexId":"fs07602","displayToPublicDate":"2004-10-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"076-02","title":"Monitoring and Assessing our Nation's Water Quality","language":"ENGLISH","doi":"10.3133/fs07602","usgsCitation":"Mallard, G.E., and Hamilton, P.A., 2002, Monitoring and Assessing our Nation's Water Quality: U.S. Geological Survey Fact Sheet 076-02, NA, https://doi.org/10.3133/fs07602.","productDescription":"NA","costCenters":[],"links":[{"id":119353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_076_02.bmp"},{"id":3224,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/fs-076-02/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627a02","contributors":{"authors":[{"text":"Mallard, Gail E.","contributorId":46556,"corporation":false,"usgs":true,"family":"Mallard","given":"Gail","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":208920,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamilton, Pixie A. pahamilt@usgs.gov","contributorId":1068,"corporation":false,"usgs":true,"family":"Hamilton","given":"Pixie","email":"pahamilt@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":208919,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":69614,"text":"i2756 - 2002 - Northern Everglades, Florida, satellite image map","interactions":[],"lastModifiedDate":"2025-08-18T20:48:40.608266","indexId":"i2756","displayToPublicDate":"2004-09-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2756","title":"Northern Everglades, Florida, satellite image map","docAbstract":"These satellite image maps are one product of the USGS Land Characteristics from Remote Sensing project, funded through the USGS Place-Based Studies Program with support from the Everglades National Park. The objective of this project is to develop and apply innovative remote sensing and geographic information system techniques to map the distribution of vegetation, vegetation characteristics, and related hydrologic variables through space and over time. The mapping and description of vegetation characteristics and their variations are necessary to accurately simulate surface hydrology and other surface processes in South Florida and to monitor land surface changes. As part of this research, data from many airborne and satellite imaging systems have been georeferenced and processed to facilitate data fusion and analysis. These image maps were created using image fusion techniques developed as part of this project.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2756","usgsCitation":"Thomas, J., and Jones, J., 2002, Northern Everglades, Florida, satellite image map: U.S. Geological Survey IMAP 2756, 1 Plate: 52.43 x 39.95 inches, https://doi.org/10.3133/i2756.","productDescription":"1 Plate: 52.43 x 39.95 inches","costCenters":[],"links":[{"id":187528,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2756/report-thumb.jpg"},{"id":6253,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2756/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","country":"United States","state":"Florida","otherGeospatial":"Northern Everglades","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.13333333333334,25.916666666666668 ], [ -80.13333333333334,26.716666666666665 ], [ -80.01666666666667,26.716666666666665 ], [ -80.01666666666667,25.916666666666668 ], [ -80.13333333333334,25.916666666666668 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696cb6","contributors":{"authors":[{"text":"Thomas, Jean-Claude","contributorId":58307,"corporation":false,"usgs":true,"family":"Thomas","given":"Jean-Claude","affiliations":[],"preferred":false,"id":280732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, John 0000-0001-6117-3691 jwjones@usgs.gov","orcid":"https://orcid.org/0000-0001-6117-3691","contributorId":2220,"corporation":false,"usgs":true,"family":"Jones","given":"John","email":"jwjones@usgs.gov","affiliations":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true},{"id":37786,"text":"WMA - Observing Systems Division","active":true,"usgs":true}],"preferred":true,"id":280731,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":39979,"text":"wri20024092 - 2002 - Estimates of recharge to unconfined aquifers and leakage to confined aquifers in the seven-county metropolitan area of Minneapolis-St. Paul, Minnesota","interactions":[],"lastModifiedDate":"2024-04-22T21:13:32.981208","indexId":"wri20024092","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2002","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":"2002-4092","title":"Estimates of recharge to unconfined aquifers and leakage to confined aquifers in the seven-county metropolitan area of Minneapolis-St. Paul, Minnesota","docAbstract":"

Recharge to unconfined aquifers in the seven-county Twin Cities metropolitan area of Minnesota was estimated by five methods. Mean recharge estimated as a percentage (27 percent) of precipitation ranged from 7.7 to 8.3 in./yr across the study area. The median recharge estimated from automated analyses of streamflow-recession displacements for seven basins ranged from 1.2 to 12.2 in./yr. Median recharge estimated from graphical analyses of groundwater level fluctuations for 11 wells ranged from 4.5 to 13.6 in./yr. Recharge estimated by age dating of shallow ground water at a nested well site was 8.8 in./yr. Minimal ground-water recharge estimated by statistical analyses of watershed characteristics (geologic data and streamflow records) ranged from less than 0.1 to 5.6 in./yr.

\n

Leakage, considered recharge to confined aquifers, in the seven-county Twin Cities metropolitan area was estimated by two methods. Leakage estimated by analyses of ground-water level fluctuations for 11 wells ranged from 3.2x10-3 to 1.1x10-2 in./yr. Leakage estimated by analyses of vertical-hydraulic gradients based on application of the Darcy flow equation for seven nested well sites ranged from 4.6x10-5 to 1.1x10-1 in./yr.

\n

Recharge estimates, which generally varied within 10 in./yr for each of the methods, generally were largest based on the precipitation, ground-water level fluctuation, and age dating of shallow ground water methods, slightly smaller based on the streamflow-recession displacement method, and smallest based on the watershed characteristics method. Leakage, which was less than 1 in./yr, varied within 1 order of magnitude based on the ground-water level fluctuation method and as much as 4 orders of magnitude based on analyses of vertical-hydraulic gradients.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/wri20024092","collaboration":"Prepared in cooperation with Anoka, Carver, Dakota, Hennepin, Ramsey, Scott, and Washington Counties and the Minnesota Board of Soil and Water Conservation","usgsCitation":"Ruhl, J.F., Kanivetsky, R., and Shmagin, B., 2002, Estimates of recharge to unconfined aquifers and leakage to confined aquifers in the seven-county metropolitan area of Minneapolis-St. Paul, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 2002-4092, iv, 32 p., https://doi.org/10.3133/wri20024092.","productDescription":"iv, 32 p.","numberOfPages":"38","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":428022,"rank":3,"type":{"id":36,"text":"NGMDB Index 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