Data on geology, topography, hydrology, climate, land use, and vegetation were compiled between October 2000 and September 2001 and assembled into a database for use by local and regional waterresource managers and for future water-resource investigations. The hydrologic data include information on wells, springs, streamflow, water chemistry, and water use. Limitations of the data and additional data needs also were prepared. The roughly 5,000-square-mile Coconino Plateau contains a complex regional aquifer that has become increasingly important as a source of water supply for domestic, municipal, and in-stream uses owing to population growth and development. The flow characteristics of the regional aquifer are poorly understood because the aquifer is deeply buried, which limits exploratory drilling and testing, and because the geologic structure, which controls the occurrence and movement of ground water, is complex. The study area is about 10,300 square miles and, besides containing the entire Coconino Plateau, includes parts of adjacent areas where ground water from the Coconino Plateau discharges. Selected data are presented in tabular or graphical form. All data are available in electronic form.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tucson, AZ","doi":"10.3133/ofr02265","collaboration":"Prepared in cooperation with the City of Williams","usgsCitation":"Bills, D., and Flynn, M., 2002, Hydrogeologic data for the Coconino Plateau and adjacent areas, Coconino and Yavapai counties, Arizona: U.S. Geological Survey Open-File Report 2002-265, Report: vi, 29 p.; Tables, https://doi.org/10.3133/ofr02265.","productDescription":"Report: vi, 29 p.; Tables","numberOfPages":"38","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":287825,"rank":4,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02265.gif"},{"id":287824,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0265/report.pdf"},{"id":296283,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0265/","size":"6.4 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":296284,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0265/ofr02-265_Tables1-7.xls","size":"5.1 MB","linkFileType":{"id":3,"text":"xlsx"}}],"scale":"100000","projection":"Lambert Conformal Conic projection","country":"United States","state":"Arizona","county":"Coconino County, Yavapai County","otherGeospatial":"Coconino Plateau","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.0,35.0 ], [ -113.0,36.5 ], [ -111.0,36.5 ], [ -111.0,35.0 ], [ -113.0,35.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae11c","contributors":{"authors":[{"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":241624,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":241623,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":50499,"text":"ofr02229 - 2002 - Southwest Washington coastal erosion workshop report 2000","interactions":[],"lastModifiedDate":"2018-09-19T17:50:40","indexId":"ofr02229","displayToPublicDate":"2003-03-01T00:00:00","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":"2002-229","title":"Southwest Washington coastal erosion workshop report 2000","docAbstract":"This report is a compilation of abstracts that correspond to oral presentations and posters presented at the fifth principal investigators workshop of the Southwest Washington Coastal Erosion Study. The workshop was held November 15 - 17, 2000 at the Department of Ecology headquarters building in Olympia, WA. For the fourth consecutive year in November, the workshop convened the entire multi-disciplinary group of scientists and engineers working on the Study or on related projects within the Columbia River littoral cell (CRLC) (Figures 1 and 2). The workshop participants are listed in the List of Attendees section towards the end of this report.\n\nThe purpose of this workshop was to bring all Study investigators and associated engineers and scientists together to discuss recent work, ongoing tasks, and future research plans in the CRLC. Investigators were asked to present recent data, preliminary interpretations, and research results to invoke discussion and correlation with parallel scientific efforts. The abstracts compiled in this report represent a wealth of information on the CRLC, but because much of the work is in progress, the reader is advised that the information provided herein is preliminary and subject to change.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02229","collaboration":"Prepared in Cooperation with Washington State Department of Ecology","usgsCitation":"Gelfenbaum, G.R., 2002, Southwest Washington coastal erosion workshop report 2000: U.S. Geological Survey Open-File Report 2002-229, p. 308, https://doi.org/10.3133/ofr02229.","productDescription":"p. 308","additionalOnlineFiles":"N","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":4314,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0229/","linkFileType":{"id":5,"text":"html"}},{"id":176179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0229/report-thumb.jpg"},{"id":86328,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0229/pdf/of02-229.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon;Washington","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.3872,45.6064 ], [ -124.3872,47.4392 ], [ -122.9425,47.4392 ], [ -122.9425,45.6064 ], [ -124.3872,45.6064 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636845","contributors":{"editors":[{"text":"Gelfenbaum, Guy R. 0000-0003-1291-6107 ggelfenbaum@usgs.gov","orcid":"https://orcid.org/0000-0003-1291-6107","contributorId":742,"corporation":false,"usgs":true,"family":"Gelfenbaum","given":"Guy","email":"ggelfenbaum@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":745668,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Gelfenbaum, Guy R. 0000-0003-1291-6107 ggelfenbaum@usgs.gov","orcid":"https://orcid.org/0000-0003-1291-6107","contributorId":742,"corporation":false,"usgs":true,"family":"Gelfenbaum","given":"Guy","email":"ggelfenbaum@usgs.gov","middleInitial":"R.","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":241616,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":50527,"text":"ofr02365 - 2002 - Spatial digital database of the geologic map of Catalina Core Complex and San Pedro Trough, Pima, Pinal, Gila, Graham, and Cochise Counties, Arizona","interactions":[],"lastModifiedDate":"2023-06-23T16:57:46.675816","indexId":"ofr02365","displayToPublicDate":"2003-03-01T00:00:00","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":"2002-365","title":"Spatial digital database of the geologic map of Catalina Core Complex and San Pedro Trough, Pima, Pinal, Gila, Graham, and Cochise Counties, Arizona","docAbstract":"The geologic map of Catalina Core Complex and San Pedro Trough by Dickinson (1992) was digitized for input into a geographic information system (GIS) by the U.S. Geological Survey staff and contractors in 2000-2001.\n\nThis digital geospatial database is one of many being created by the U.S. Geological Survey as an ongoing effort to provide geologic information in a geographic information system (GIS) for use in spatial analysis. The resulting digital geologic map database data can be queried in many ways to produce a variety of geologic maps and derivative products. Digital base map data (topography, roads, towns, rivers, lakes, and so forth) are not included; they may be obtained from a variety of commercial and government sources. This database is not meant to be used or displayed at any scale larger than 1:125,000 (for example, 1:100,000 or 1:24,000). The digital geologic map plot files that are provided herein are representations of the database.\n\nThe map area is located in southern Arizona. This report lists the geologic map units, the methods used to convert the geologic map data into a digital format, the ArcInfo GIS file structures and relationships, and explains how to download the digital files from the U.S. Geological Survey public access World Wide Web site on the Internet. The manuscript and digital data review by Lorre Moyer (USGS) is greatly appreciated.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02365","collaboration":"Prepared in cooperation with the University of Arizona","usgsCitation":"Dickinson, W.R., Hirschberg, D., Pitts, G.S., and Bolm, K., 2002, Spatial digital database of the geologic map of Catalina Core Complex and San Pedro Trough, Pima, Pinal, Gila, Graham, and Cochise Counties, Arizona: U.S. Geological Survey Open-File Report 2002-365, Report: 25 p.; 1 Plate: 36.00 inches x 52.00 inches; Readme; Metadata; Database, https://doi.org/10.3133/ofr02365.","productDescription":"Report: 25 p.; 1 Plate: 36.00 inches x 52.00 inches; Readme; Metadata; Database","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":176347,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02365.jpg"},{"id":285177,"rank":5,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0365/"},{"id":285179,"rank":8,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2002/0365/00readme.txt"},{"id":285180,"rank":6,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2002/0365/ccc125k.met"},{"id":285184,"rank":3,"type":{"id":9,"text":"Database"},"url":"https://pubs.usgs.gov/of/2002/0365/ccc125k_db.tar.Z"},{"id":285183,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0365/ccc125k.tar.Z"},{"id":285182,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0365/pdf/ccc125k.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":285178,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0365/pdf/ccc-map.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","projection":"UTM zone 12","country":"United States","state":"Arizona","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.25,32.00 ], [ -111.25,33.75 ], [ -110.00,33.75 ], [ -110.00,32.00 ], [ -111.25,32.00 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6d5a","contributors":{"authors":[{"text":"Dickinson, William R.","contributorId":75064,"corporation":false,"usgs":true,"family":"Dickinson","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":241696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hirschberg, Douglas M.","contributorId":75442,"corporation":false,"usgs":true,"family":"Hirschberg","given":"Douglas M.","affiliations":[],"preferred":false,"id":241697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pitts, G. Stephen","contributorId":23187,"corporation":false,"usgs":true,"family":"Pitts","given":"G.","email":"","middleInitial":"Stephen","affiliations":[],"preferred":false,"id":241695,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bolm, Karen S.","contributorId":13226,"corporation":false,"usgs":true,"family":"Bolm","given":"Karen S.","affiliations":[],"preferred":false,"id":241694,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":69617,"text":"i2767 - 2002 - Geology of the Stegall Mountain 7.5-minute quadrangle, Shannon and Carter Counties, south-central Missouri","interactions":[],"lastModifiedDate":"2012-02-10T00:11:23","indexId":"i2767","displayToPublicDate":"2003-03-01T00:00:00","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":"2767","title":"Geology of the Stegall Mountain 7.5-minute quadrangle, Shannon and Carter Counties, south-central Missouri","docAbstract":" The bedrock exposed in the Stegall Mountain Quadrangle, Missouri, comprises Mesoproterozoic aged volcanic rocks overlain by Late Cambrian and Early Ordovician aged dolomite, sandstone, and chert. The sedimentary rocks are nearly flat-lying except where they drape around knobs of the volcanic rocks or where they are adjacent to faults. The carbonates are karstified and the area contains numerous sinkholes, springs, caves, and losing-streams. \r\n This map is one of several being produced under the U.S. Geological Survey National Cooperative Geologic Mapping Program to provide geologic data applicable to land-use problems in the Ozarks of south-central Missouri. Ongoing and potential industrial and agricultural development in the Ozarks region has presented issues of ground-water quality in karst areas. A National Park in this region (Ozark National Scenic Riverways, Missouri ) is concerned about the effects of activities in areas outside of their stewardship on the water resources that define the heart of this Park. This task applies geologic mapping and karst investigations to address issues surrounding competing land use in south-central Missouri. This task keeps geologists from the USGS associated with the park and allows the Parks to utilize USGS expertise and aid the NPS on how to effectively use geologic maps for Park management. For more information see: http://geology.er.usgs.gov/eespteam/Karst/index.html","language":"ENGLISH","doi":"10.3133/i2767","isbn":"0607889810","usgsCitation":"Harrison, R., Orndorff, R.C., and Weary, D.J., 2002, Geology of the Stegall Mountain 7.5-minute quadrangle, Shannon and Carter Counties, south-central Missouri: U.S. Geological Survey IMAP 2767, 1 map : col. ; 58 x 47 cm., on sheet 101 x 138 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i2767.","productDescription":"1 map : col. ; 58 x 47 cm., on sheet 101 x 138 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":110397,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54510.htm","linkFileType":{"id":5,"text":"html"},"description":"54510"},{"id":187617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6255,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2767/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.25,37 ], [ -91.25,37.1175 ], [ -91.11749999999999,37.1175 ], [ -91.11749999999999,37 ], [ -91.25,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e4cf","contributors":{"authors":[{"text":"Harrison, Richard W. rharriso@usgs.gov","contributorId":544,"corporation":false,"usgs":true,"family":"Harrison","given":"Richard W.","email":"rharriso@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":280739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Orndorff, Randall C. 0000-0002-8956-5803 rorndorf@usgs.gov","orcid":"https://orcid.org/0000-0002-8956-5803","contributorId":2739,"corporation":false,"usgs":true,"family":"Orndorff","given":"Randall","email":"rorndorf@usgs.gov","middleInitial":"C.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":280741,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weary, David J. 0000-0002-6115-6397 dweary@usgs.gov","orcid":"https://orcid.org/0000-0002-6115-6397","contributorId":545,"corporation":false,"usgs":true,"family":"Weary","given":"David","email":"dweary@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":280740,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":47756,"text":"wri024234 - 2002 - Simulation of ground-water flow and evaluation of water-management alternatives in the upper Charles River basin, eastern Massachusetts","interactions":[],"lastModifiedDate":"2025-09-11T13:37:32.812392","indexId":"wri024234","displayToPublicDate":"2003-03-01T00:00:00","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":"2002-4234","title":"Simulation of ground-water flow and evaluation of water-management alternatives in the upper Charles River basin, eastern Massachusetts","docAbstract":"Ground water is the primary source of drinking water for towns in the upper Charles River Basin, an area of 105 square miles in eastern Massachusetts that is undergoing rapid growth. The stratified-glacial aquifers in the basin are high yield, but also are thin, discontinuous, and in close hydraulic connection with streams, ponds, and wetlands. Water withdrawals averaged 10.1 million gallons per day in 1989?98 and are likely to increase in response to rapid growth. These withdrawals deplete streamflow and lower pond levels. A study was conducted to develop tools for evaluating water-management alternatives at the regional scale in the basin. Geologic and hydrologic data were compiled and collected to characterize the ground- and surface-water systems. Numerical flow modeling techniques were applied to evaluate the effects of increased withdrawals and altered recharge on ground-water levels, pond levels, and stream base flow. Simulation-optimization methods also were applied to test their efficacy for management of multiple water-supply and water-resource needs. \r\n\r\nSteady-state and transient ground-water-flow models were developed using the numerical modeling code MODFLOW-2000. The models were calibrated to 1989?98 average annual conditions of water withdrawals, water levels, and stream base flow. Model recharge rates were varied spatially, by land use, surficial geology, and septic-tank return flow. Recharge was changed during model calibration by means of parameter-estimation techniques to better match the estimated average annual base flow; area-weighted rates averaged 22.5 inches per year for the basin. Water withdrawals accounted for about 7 percent of total simulated flows through the stream-aquifer system and were about equal in magnitude to model-calculated rates of ground-water evapotranspiration from wetlands and ponds in aquifer areas. Water withdrawals as percentages of total flow varied spatially and temporally within an average year; maximum values were 12 to 13 percent of total annual flow in some subbasins and of total monthly flow throughout the basin in summer and early fall. \r\n\r\nWater-management alternatives were evaluated by simulating hypothetical scenarios of increased withdrawals and altered recharge for average 1989?98 conditions with the flow models. Increased withdrawals to maximum State-permitted levels would result in withdrawals of about 15 million gallons per day, or about 50 percent more than current withdrawals. Model-calculated effects of these increased withdrawals included reductions in stream base flow that were greatest (as a percentage of total flow) in late summer and early fall. These reductions ranged from less than 5 percent to more than 60 percent of model-calculated 1989?98 base flow along reaches of the Charles River and major tributaries during low-flow periods. Reductions in base flow generally were comparable to upstream increases in withdrawals, but were slightly less than upstream withdrawals in areas where septic-system return flow was simulated. Increased withdrawals also increased the proportion of wastewater in the Charles River downstream of treatment facilities. The wastewater component increased downstream from a treatment facility in Milford from 80 percent of September base flow under 1989?98 conditions to 90 percent of base flow, and from 18 to 27 percent of September base flow downstream of a treatment facility in Medway. In another set of hypothetical scenarios, additional recharge equal to the transfer of water out of a typical subbasin by sewers was found to increase model-calculated base flows by about 12 percent of model-calculated base flows. Addition of recharge equal to that available from artificial recharge of residential rooftop runoff had smaller effects, augmenting simulated September base flow by about 3 percent. \r\n\r\nSimulation-optimization methods were applied to an area near Populatic Pond and the confluence of the Mill and Charles Rivers in Franklin,","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024234","usgsCitation":"DeSimone, L., Walter, D.A., Eggleston, J.R., and Nimiroski, M.T., 2002, Simulation of ground-water flow and evaluation of water-management alternatives in the upper Charles River basin, eastern Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 2002-4234, vii, 94 p., https://doi.org/10.3133/wri024234.","productDescription":"vii, 94 p.","costCenters":[],"links":[{"id":170495,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4083,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri024234/index.html","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Massachusetts","otherGeospatial":"upper Charles River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -71.667,\n 42.25\n ],\n [\n -71.667,\n 41.9\n ],\n [\n -71.1958,\n 41.9\n ],\n [\n -71.1958,\n 42.25\n ],\n [\n -71.667,\n 42.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2e4d","contributors":{"authors":[{"text":"DeSimone, Leslie A. 0000-0003-0774-9607 ldesimon@usgs.gov","orcid":"https://orcid.org/0000-0003-0774-9607","contributorId":176711,"corporation":false,"usgs":true,"family":"DeSimone","given":"Leslie A.","email":"ldesimon@usgs.gov","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":236165,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walter, Donald A. 0000-0003-0879-4477 dawalter@usgs.gov","orcid":"https://orcid.org/0000-0003-0879-4477","contributorId":1101,"corporation":false,"usgs":true,"family":"Walter","given":"Donald","email":"dawalter@usgs.gov","middleInitial":"A.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":236164,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eggleston, John R. 0000-0001-6633-3041 jegglest@usgs.gov","orcid":"https://orcid.org/0000-0001-6633-3041","contributorId":3068,"corporation":false,"usgs":true,"family":"Eggleston","given":"John","email":"jegglest@usgs.gov","middleInitial":"R.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":236166,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nimiroski, Mark T.","contributorId":65898,"corporation":false,"usgs":true,"family":"Nimiroski","given":"Mark","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":236167,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70242834,"text":"70242834 - 2002 - Kelp forest ecosystems: Biodiversity, stability, resilience and future","interactions":[],"lastModifiedDate":"2023-04-19T16:50:50.126019","indexId":"70242834","displayToPublicDate":"2003-02-19T11:43:46","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1531,"text":"Environmental Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Kelp forest ecosystems: Biodiversity, stability, resilience and future","docAbstract":"Kelp forests are phyletically diverse, structurally complex and highly productive components of coldwater rocky marine coastlines. This paper reviews the conditions in which kelp forests develop globally and where, why and at what rate they become deforested. The ecology and long archaeological history of kelp forests are examined through case studies from southern California, the Aleutian Islands and the western North Atlantic, well-studied locations that represent the widest possible range in kelp forest biodiversity. Global distribution of kelp forests is physiologically constrained by light at high latitudes and by nutrients, warm temperatures and other macrophytes at low latitudes. Within mid-latitude belts (roughly 40–60° latitude in both hemispheres) well-developed kelp forests are most threatened by herbivory, usually from sea urchins. Overfishing and extirpation of highly valued vertebrate apex predators often triggered herbivore population increases, leading to widespread kelp deforestation. Such deforestations have the most profound and lasting impacts on species-depauperate systems, such as those in Alaska and the western North Atlantic. Globally urchin-induced deforestation has been increasing over the past 2–3 decades. Continued fishing down of coastal food webs has resulted in shifting harvesting targets from apex predators to their invertebrate prey, including kelp-grazing herbivores. The recent global expansion of sea urchin harvesting has led to the widespread extirpation of this herbivore, and kelp forests have returned in some locations but, for the first time, these forests are devoid of vertebrate apex predators. In the western North Atlantic, large predatory crabs have recently filled this void and they have become the new apex predator in this system. Similar shifts from fish- to crab-dominance may have occurred in coastal zones of the United Kingdom and Japan, where large predatory finfish were extirpated long ago. Three North American case studies of kelp forests were examined to determine their long history with humans and project the status of future kelp forests to the year 2025. Fishing impacts on kelp forest systems have been both profound and much longer in duration than previously thought. Archaeological data suggest that coastal peoples exploited kelp forest organisms for thousands of years, occasionally resulting in localized losses of apex predators, outbreaks of sea urchin populations and probably small-scale deforestation. Over the past two centuries, commercial exploitation for export led to the extirpation of sea urchin predators, such as the sea otter in the North Pacific and predatory fishes like the cod in the North Atlantic. The large-scale removal of predators for export markets increased sea urchin abundances and promoted the decline of kelp forests over vast areas. Despite southern California having one of the longest known associations with coastal kelp forests, widespread deforestation is rare. It is possible that functional redundancies among predators and herbivores make this most diverse system most stable. Such biodiverse kelp forests may also resist invasion from non-native species. In the species-depauperate western North Atlantic, introduced algal competitors carpet the benthos and threaten future kelp dominance. There, other non-native herbivores and predators have become established and dominant components of this system. Climate changes have had measurable impacts on kelp forest ecosystems and efforts to control the emission of greenhouse gasses should be a global priority. However, overfishing appears to be the greatest manageable threat to kelp forest ecosystems over the 2025 time horizon. Management should focus on minimizing fishing impacts and restoring populations of functionally important species in these systems.
","language":"English","publisher":"Cambridge University Press","doi":"10.1017/S0376892902000322","usgsCitation":"Steneck, R.S., Graham, M.H., Bourque, B.J., Corbett, D., Erlandson, J.M., Estes, J.A., and Tegner, M.J., 2002, Kelp forest ecosystems: Biodiversity, stability, resilience and future: Environmental Conservation, v. 29, no. 4, p. 436-459, https://doi.org/10.1017/S0376892902000322.","productDescription":"24 p.","startPage":"436","endPage":"459","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":416014,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"4","noUsgsAuthors":false,"publicationDate":"2003-02-19","publicationStatus":"PW","contributors":{"authors":[{"text":"Steneck, Robert S.","contributorId":55211,"corporation":false,"usgs":true,"family":"Steneck","given":"Robert","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":869920,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graham, Michael H.","contributorId":42785,"corporation":false,"usgs":true,"family":"Graham","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":869921,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bourque, Bruce J.","contributorId":12698,"corporation":false,"usgs":true,"family":"Bourque","given":"Bruce","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":869922,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Corbett, Debbie","contributorId":304251,"corporation":false,"usgs":false,"family":"Corbett","given":"Debbie","email":"","affiliations":[],"preferred":false,"id":869923,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Erlandson, Jon M.","contributorId":68114,"corporation":false,"usgs":false,"family":"Erlandson","given":"Jon","email":"","middleInitial":"M.","affiliations":[{"id":7025,"text":"Museum of Natural and Cultural History, University of Oregon","active":true,"usgs":false}],"preferred":false,"id":869924,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Estes, James A. jim_estes@usgs.gov","contributorId":53325,"corporation":false,"usgs":true,"family":"Estes","given":"James","email":"jim_estes@usgs.gov","middleInitial":"A.","affiliations":[{"id":6949,"text":"University of California, Santa Cruz","active":true,"usgs":false},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":869925,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tegner, M. 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Together with the accompanying text file (nesfmf.ps, nesfmf.pdf, nesfmf.txt), it provides current information on the geologic structure and stratigraphy of the area covered. The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The scale of the source maps limits the spatial resolution (scale) of the database to 1:62,500 or smaller.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2403","usgsCitation":"Graymer, R.W., Jones, D.L., and Brabb, E.E., 2002, Geologic map and map database of northeastern San Francisco Bay region, California: Most of Solano County and parts of Napa, Marin, Contra Costa, San Joaquin, Sacramento, Yolo, and Sonoma Counties (Version 1.0): U.S. Geological Survey Miscellaneous Field Studies Map 2403, HTML Document, https://doi.org/10.3133/mf2403.","productDescription":"HTML Document","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":188078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6340,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2002/2403/","linkFileType":{"id":5,"text":"html"}},{"id":110377,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54147.htm","linkFileType":{"id":5,"text":"html"},"description":"54147"}],"scale":"100000","country":"United States","state":"California","county":"Contra Costa County, Napa County, Marin County, Sacramento County, San Joaquin County, Solano County, Sonoma County, Yolo County","otherGeospatial":"northeastern San Francisco Bay region","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.5,38 ], [ -122.5,38.75 ], [ -121.5,38.75 ], [ -121.5,38 ], [ -122.5,38 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4974","contributors":{"authors":[{"text":"Graymer, Russell Walter","contributorId":95759,"corporation":false,"usgs":true,"family":"Graymer","given":"Russell","email":"","middleInitial":"Walter","affiliations":[],"preferred":false,"id":280860,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, David Lawrence","contributorId":11580,"corporation":false,"usgs":true,"family":"Jones","given":"David","email":"","middleInitial":"Lawrence","affiliations":[],"preferred":false,"id":280858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brabb, Earl E.","contributorId":48939,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":280859,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":69675,"text":"mf2411 - 2002 - Surficial Geologic Map of The Loop and Druid Arch Quadrangles, Canyonlands National Park, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:11:22","indexId":"mf2411","displayToPublicDate":"2003-02-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2411","title":"Surficial Geologic Map of The Loop and Druid Arch Quadrangles, Canyonlands National Park, Utah","docAbstract":"This geologic map is a product of a cooperative project between the \r\n U.S. Geological Survey and the U.S. National Park Service to provide \r\n geologic information about this part of Canyonlands National Park, Utah.\r\n This digital map database contains bedrock data from previously published \r\n data that has been modified by the author. New mapping of the surficial \r\n deposits represents the general distribution of surficial deposits of the \r\n Druid Arch and The Loop 7.5-minute quadrangles.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/mf2411","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Billingsley, G.H., Block, D., and Felger, T.J., 2002, Surficial Geologic Map of The Loop and Druid Arch Quadrangles, Canyonlands National Park, Utah (Version 1.0): U.S. Geological Survey Miscellaneous Field Studies Map 2411, Map: 33 x 52 inches; Digital Database; Metadata; ReadMe, https://doi.org/10.3133/mf2411.","productDescription":"Map: 33 x 52 inches; Digital Database; Metadata; ReadMe","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":110378,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54148.htm","linkFileType":{"id":5,"text":"html"},"description":"54148"},{"id":188163,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9542,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2002/2411/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.86749999999999,38 ], [ -109.86749999999999,38.25 ], [ -109.75,38.25 ], [ -109.75,38 ], [ -109.86749999999999,38 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a079","contributors":{"authors":[{"text":"Billingsley, George H.","contributorId":20711,"corporation":false,"usgs":true,"family":"Billingsley","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":280869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Block, Debra L.","contributorId":66351,"corporation":false,"usgs":true,"family":"Block","given":"Debra L.","affiliations":[],"preferred":false,"id":280870,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Felger, Tracey J. 0000-0003-0841-4235 tfelger@usgs.gov","orcid":"https://orcid.org/0000-0003-0841-4235","contributorId":1117,"corporation":false,"usgs":true,"family":"Felger","given":"Tracey","email":"tfelger@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":280868,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":69583,"text":"i2738 - 2002 - Geologic and aeromagnetic maps of the Fossil Ridge area and vicinity, Gunnison County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:32","indexId":"i2738","displayToPublicDate":"2003-02-01T00:00:00","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":"2738","title":"Geologic and aeromagnetic maps of the Fossil Ridge area and vicinity, Gunnison County, Colorado","docAbstract":"This data set includes a GIS geologic map database \r\nof an Early Proterozoic metavolcanic and metasedimentary terrane \r\nextensively intruded by Early and Middle Proterozoic granitic \r\nplutons. Laramide to Tertiary deformation and intrusion of \r\n\r\nfelsic plutons have created numerous small mineral deposits that \r\nare described in the tables and are shown on the figures in the \r\naccompanying text pamphlet. Also included in the pamphlet are \r\nnumerous chemical analyses of igneous and meta-igneous bodies of \r\nall ages in tables and in summary geochemical diagrams. The text \r\npamphlet also contains a detailed description of map units and \r\ndiscussions of the aeromagnetic survey, igneous and metmorphic \r\nrocks, and mineral deposits. The printed map sheet and browse \r\ngraphic pdf file include the aeromagnetic map of the study area, \r\nas well as figures and photographs.\r\n Purpose:\r\n This GIS geologic map database is provided to facilitate \r\nthe presentation and analysis of earth-science data for this \r\nregion of Colorado. This digital map database may be displayed \r\nat any scale or projection. However, the geologic data in this \r\ncoverage are not intended for use at a scale other than 1:30,000. \r\nSupplemental useful data accompanying the database are extensive \r\ngeochemical and mineral deposits data, as well as an aeromagnetic \r\nmap.","language":"ENGLISH","doi":"10.3133/i2738","isbn":"0607959509","usgsCitation":"DeWitt, E., Zech, R.S., Chase, C., Zartman, R., Kucks, R., Bartelson, B., Rosenlund, G., and Earley, D., 2002, Geologic and aeromagnetic maps of the Fossil Ridge area and vicinity, Gunnison County, Colorado: U.S. Geological Survey IMAP 2738, 1 map : col. ; 77 x 85 cm., on sheet 101 x 137 cm., folded in envelope 30 x 24 cm. + 1 pamphlet (42 p. ; 28 cm.), https://doi.org/10.3133/i2738.","productDescription":"1 map : col. ; 77 x 85 cm., on sheet 101 x 137 cm., folded in envelope 30 x 24 cm. + 1 pamphlet (42 p. ; 28 cm.)","costCenters":[],"links":[{"id":110396,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54509.htm","linkFileType":{"id":5,"text":"html"},"description":"54509"},{"id":193139,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6212,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i-2738/","linkFileType":{"id":5,"text":"html"}}],"scale":"30000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.75,38.416666666666664 ], [ -106.75,38.784166666666664 ], [ -106.45083333333334,38.784166666666664 ], [ -106.45083333333334,38.416666666666664 ], [ -106.75,38.416666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a829a","contributors":{"authors":[{"text":"DeWitt, Ed","contributorId":65081,"corporation":false,"usgs":true,"family":"DeWitt","given":"Ed","affiliations":[],"preferred":false,"id":280658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zech, R. S.","contributorId":51289,"corporation":false,"usgs":true,"family":"Zech","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":280656,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chase, C.G.","contributorId":102965,"corporation":false,"usgs":true,"family":"Chase","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":280659,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":280652,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kucks, R.P.","contributorId":53758,"corporation":false,"usgs":true,"family":"Kucks","given":"R.P.","affiliations":[],"preferred":false,"id":280657,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bartelson, Bruce","contributorId":31845,"corporation":false,"usgs":true,"family":"Bartelson","given":"Bruce","email":"","affiliations":[],"preferred":false,"id":280654,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Rosenlund, G.C.","contributorId":26014,"corporation":false,"usgs":true,"family":"Rosenlund","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":280653,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Earley, Drummond III","contributorId":49880,"corporation":false,"usgs":true,"family":"Earley","given":"Drummond","suffix":"III","email":"","affiliations":[],"preferred":false,"id":280655,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":69616,"text":"i2761 - 2002 - Atlas of natural hazards in the Hawaiian coastal zone","interactions":[],"lastModifiedDate":"2023-04-24T18:28:25.984558","indexId":"i2761","displayToPublicDate":"2003-02-01T00:00:00","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":"2761","title":"Atlas of natural hazards in the Hawaiian coastal zone","docAbstract":"The purpose of this report is to communicate to citizens and regulatory authorities the history and relative intensity of coastal hazards in Hawaii. This information is the key to the wise use and management of coastal resources. The information contained in this document,we hope,will improve the ability of Hawaiian citizens and visitors to safely enjoy the coast and provide a strong data set for planners and managers to guide the future of coastal resources. \n\nThis work is largely based on previous investigations by scientific and engineering researchers and county, state, and federal offices and agencies. The unique aspect of this report is that, to the extent possible, it assimilates prior efforts in documenting Hawaiian coastal hazards and combines existing knowledge into a single comprehensive coastal hazard data set. This is by no means the final word on coastal hazards in Hawaii. Every hazardous phenomenon described here, and others such as slope failure and rocky shoreline collapse, need to be more carefully quantified, forecast, and mitigated. Our ultimate goal, of course, is to make the Hawaiian coast a safer place by educating the people of the state, and their leaders, about the hazardous nature of the environment. In so doing, we will also be taking steps toward improved preservation of coastal environments, because the best way to avoid coastal hazards is to avoid inappropriate development in the coastal zone.\n\nWe have chosen maps as the medium for both recording and communicating the hazard history and its intensity along the Hawaiian coast.Two types of maps are used: 1) smallscale maps showing a general history of hazards on each island and summarizing coastal hazards in a readily understandable format for general use, and 2) a large-scale series of technical maps (1:50,000) depicting coastal sections approximately 5 to 7 miles in length with color bands along the coast ranking the relative intensity of each hazard at the adjacent shoreline.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2761","usgsCitation":"Fletcher, C.H., Grossman, E., Richmond, B.M., and Gibbs, A.E., 2002, Atlas of natural hazards in the Hawaiian coastal zone: U.S. Geological Survey IMAP 2761, 182 p., https://doi.org/10.3133/i2761.","productDescription":"182 p.","costCenters":[],"links":[{"id":416173,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51546.htm","linkFileType":{"id":5,"text":"html"}},{"id":6254,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2761/","linkFileType":{"id":5,"text":"html"}},{"id":281727,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/i2761/i2761.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":187530,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2761/report-thumb.jpg"}],"scale":"50000","country":"United States","state":"Hawaii","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -159.7842,\n 18.9008\n ],\n [\n -159.7842,\n 22.2333\n ],\n [\n -154.8003,\n 22.2333\n ],\n [\n -154.8003,\n 18.9008\n ],\n [\n -159.7842,\n 18.9008\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6692de","contributors":{"authors":[{"text":"Fletcher, Charles H. III","contributorId":30300,"corporation":false,"usgs":true,"family":"Fletcher","given":"Charles","suffix":"III","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":280737,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grossman, Eric E.","contributorId":40677,"corporation":false,"usgs":true,"family":"Grossman","given":"Eric E.","affiliations":[],"preferred":false,"id":280738,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richmond, Bruce M. 0000-0002-0056-5832 brichmond@usgs.gov","orcid":"https://orcid.org/0000-0002-0056-5832","contributorId":2459,"corporation":false,"usgs":true,"family":"Richmond","given":"Bruce","email":"brichmond@usgs.gov","middleInitial":"M.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":280735,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gibbs, Ann E. 0000-0002-0883-3774 agibbs@usgs.gov","orcid":"https://orcid.org/0000-0002-0883-3774","contributorId":2644,"corporation":false,"usgs":true,"family":"Gibbs","given":"Ann","email":"agibbs@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":280736,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":53702,"text":"ofr02306L - 2002 - Municipal GIS database of Guatemala; 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Program use can be appropriate if all or most ground water in the basin discharges to the stream and if a streamflow-gaging station at the downstream end of the basin measures all or most outflow. Ground-water pumpage and the regulation and diversion of streamflow should be negligible. More information about the application of the method is included in Rutledge, 1997, pages 2-3. The program can be used in conjunction with ground-water-level data. If a well is open to the surficial aquifer, observed water-level rises in the well can be used to evaluate the timing of recharge. Such evaluation is most effective if there are numerous water-level observation wells in the basin. Water levels in observation wells can also be used to evaluate the rate of ground-water discharge estimated by the PULSE program. The results of such an evaluation may be problematic, however, because the relation between ground-water level and ground-water discharge may not be unique. Departures from the linear model of recession occur because of areal variation in transmissivity and because of the longitudinal component of ground-water flow (parallel to the stream). If the PULSE program is used to estimate ground-water recharge, the recession index should not be obtained from periods of extreme low flow, and the calibration process should include plotting flow on the linear scale in addition to plotting flow on the log scale.","language":"ENGLISH","doi":"10.3133/ofr02455","usgsCitation":"Rutledge, A.T., 2002, User guide for the PULSE program: U.S. Geological Survey Open-File Report 2002-455, p. 34, illus., 16 refs, https://doi.org/10.3133/ofr02455.","productDescription":"p. 34, illus., 16 refs","costCenters":[],"links":[{"id":175490,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4377,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr02-455/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486ce4b07f02db50b72e","contributors":{"authors":[{"text":"Rutledge, A. T.","contributorId":38532,"corporation":false,"usgs":true,"family":"Rutledge","given":"A.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":241850,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":50540,"text":"ofr2002402 - 2002 - Data on surface-water, streambed-interstitial water, and bed-sediment quality for selected locations in the small arms impact area of central Fort Gordon, Georgia, September 4-6, 2001","interactions":[],"lastModifiedDate":"2023-03-22T19:46:48.256192","indexId":"ofr2002402","displayToPublicDate":"2003-02-01T00:00:00","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":"2002-402","title":"Data on surface-water, streambed-interstitial water, and bed-sediment quality for selected locations in the small arms impact area of central Fort Gordon, Georgia, September 4-6, 2001","docAbstract":"In September 2001, the U.S. Geological Survey, in cooperation with the Environmental and Natural Resources Management Office of the U.S. Army Signal Center and Fort Gordon (U.S. Department of the Army), conducted a chemical assessment of surface water, streambed-interstitial water, and bed sediments within the small arms impact area of Fort Gordon Military Installation. The study was conducted in support of the development of an Integrated Natural Resources Management Plan (INRMP) for Fort Gordon, Georgia. An effective INRMP ensures that natural resources conservation measures and U.S. Army activities on the military base are integrated and consistent with Federal requirements to manage military installations on an ecosystem basis. \r\n\r\nFiltered water samples were collected from five sites along South Prong Creek and three sites along Marcum Branch Creek for chemical analyses of major ions, nutrients, and selected trace elements. On-site measurements of pH, temperature, specific conductance, and dissolved oxygen were made at the eight sites. Filtered water collected showed varying concentrations in both surface- and streambed-interstitial water. Bed-sediment samples collected from South Prong Creek contain elevated levels of arsenic, barium, beryllium, cadmium, chromium, cobalt, copper, iron, lead, manganese, nickel, selenium, vanadium, and total organic carbon relative to previous concentrations (McConnell and others, 2000). Bed-sediment samples collected from Marcum Branch Creek contain elevated levels of beryllium, copper, lead, manganese, mercury, selenium, and total organic carbon relative to previous concentrations (McConnell and others, 2000).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2002402","usgsCitation":"Priest, S., Stamey, T.C., and Lawrence, S.J., 2002, Data on surface-water, streambed-interstitial water, and bed-sediment quality for selected locations in the small arms impact area of central Fort Gordon, Georgia, September 4-6, 2001: U.S. Geological Survey Open-File Report 2002-402, iv, 15 p., https://doi.org/10.3133/ofr2002402.","productDescription":"iv, 15 p.","temporalStart":"2001-09-04","temporalEnd":"2001-09-06","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":175729,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4352,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr02-402/","linkFileType":{"id":5,"text":"html"}},{"id":414568,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_53954.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","otherGeospatial":"Fort Gordon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.2319,\n 33.4161\n ],\n [\n -82.2319,\n 33.3606\n ],\n [\n -82.1472,\n 33.3606\n ],\n [\n -82.1472,\n 33.4161\n ],\n [\n -82.2319,\n 33.4161\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7e2","contributors":{"authors":[{"text":"Priest, Sheryln","contributorId":70468,"corporation":false,"usgs":true,"family":"Priest","given":"Sheryln","email":"","affiliations":[],"preferred":false,"id":241744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stamey, Timothy C. tcstamey@usgs.gov","contributorId":4770,"corporation":false,"usgs":true,"family":"Stamey","given":"Timothy","email":"tcstamey@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":241743,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lawrence, Stephen J. slawrenc@usgs.gov","contributorId":1885,"corporation":false,"usgs":true,"family":"Lawrence","given":"Stephen","email":"slawrenc@usgs.gov","middleInitial":"J.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241742,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":53687,"text":"ofr02307A - 2002 - Municipal GIS database of El Salvador; Volume 1, Berlin, El Salvador","interactions":[],"lastModifiedDate":"2012-02-02T00:11:42","indexId":"ofr02307A","displayToPublicDate":"2003-02-01T00:00:00","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":"2002-307","chapter":"A","title":"Municipal GIS database of El Salvador; Volume 1, Berlin, El Salvador","language":"ENGLISH","doi":"10.3133/ofr02307A","usgsCitation":"Chirico, P., Hearn, P., Bartolomei, O.R., and Tanner, S., 2002, Municipal GIS database of El Salvador; Volume 1, Berlin, El Salvador (1st edition): U.S. Geological Survey Open-File Report 2002-307, 1 CD-ROM : maps ; 4 3/4 in. , https://doi.org/10.3133/ofr02307A.","productDescription":"1 CD-ROM : maps ; 4 3/4 in. ","costCenters":[],"links":[{"id":177396,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"1st edition","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48de","contributors":{"authors":[{"text":"Chirico, Peter G.","contributorId":27086,"corporation":false,"usgs":true,"family":"Chirico","given":"Peter G.","affiliations":[],"preferred":false,"id":248084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hearn, P.P.","contributorId":18380,"corporation":false,"usgs":true,"family":"Hearn","given":"P.P.","affiliations":[],"preferred":false,"id":248083,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartolomei, Ovidio Rivero","contributorId":102134,"corporation":false,"usgs":true,"family":"Bartolomei","given":"Ovidio","email":"","middleInitial":"Rivero","affiliations":[],"preferred":false,"id":248086,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tanner, S.D.","contributorId":37810,"corporation":false,"usgs":true,"family":"Tanner","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":248085,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}