{"pageNumber":"119","pageRowStart":"2950","pageSize":"25","recordCount":37001,"records":[{"id":98973,"text":"ofr20101303 - 2010 - Comprehensive database of wellbore temperatures and drilling mud weight pressures by depth for Judge Digby field, Louisiana","interactions":[],"lastModifiedDate":"2012-02-10T00:10:06","indexId":"ofr20101303","displayToPublicDate":"2010-12-29T00:00:00","publicationYear":"2010","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":"2010-1303","title":"Comprehensive database of wellbore temperatures and drilling mud weight pressures by depth for Judge Digby field, Louisiana","docAbstract":"This document serves as the repository for the unprocessed data used in the investigation of temperature and overpressure relations within the deep Tuscaloosa Formation in Judge Digby field. It is a compilation of all the publicly accessible wellbore temperature and pressure data for Judge Digby field, a prolific natural gas field producing from the Upper Cretaceous lower part of the Tuscaloosa Formation in the Gulf Coast region. This natural gas field is in Pointe Coupee Parish in the southern part of onshore Louisiana.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101303","usgsCitation":"Burke, L., 2010, Comprehensive database of wellbore temperatures and drilling mud weight pressures by depth for Judge Digby field, Louisiana: U.S. Geological Survey Open-File Report 2010-1303, iv, 207 p.; Database XLS, https://doi.org/10.3133/ofr20101303.","productDescription":"iv, 207 p.; Database XLS","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":126056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1303.png"},{"id":14405,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1303/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.58333333333333,30.583333333333332 ], [ -91.58333333333333,30.666666666666668 ], [ -91.5,30.666666666666668 ], [ -91.5,30.583333333333332 ], [ -91.58333333333333,30.583333333333332 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f35","contributors":{"authors":[{"text":"Burke, Lauri 0000-0002-2035-8048","orcid":"https://orcid.org/0000-0002-2035-8048","contributorId":44891,"corporation":false,"usgs":true,"family":"Burke","given":"Lauri","affiliations":[],"preferred":false,"id":307123,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":98972,"text":"ofr20101298 - 2010 - Geochemical data for core and bottom-sediment samples collected in 2007 from Grand Lake O' the Cherokees, northeast Oklahoma","interactions":[],"lastModifiedDate":"2019-08-05T10:03:32","indexId":"ofr20101298","displayToPublicDate":"2010-12-29T00:00:00","publicationYear":"2010","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":"2010-1298","title":"Geochemical data for core and bottom-sediment samples collected in 2007 from Grand Lake O' the Cherokees, northeast Oklahoma","docAbstract":"Grand Lake O' the Cherokees is a large reservoir in northeast Oklahoma, below the confluence of the Neosho and Spring Rivers, both of which drain the Tri-State Mining District to the north. The Tri-State district covers an area of 1,200 mi<sup>2</sup> (3,100 km<sup>2</sup>) and comprises Mississippi Valley-type lead-zinc deposits. A result of 120 years of mining activity is an estimated 75 million tons of processed mine tailings (chat) remaining in the district. Concerns of sediment quality and the possibility of human exposure to cadmium and lead through eating fish have led to several studies of the sediments in the Tri-State district.\r\n\r\nIn order to record the transport and deposition of metals from the Tri-State district by the Spring and Neosho Rivers into Grand Lake O' the Cherokees, the U.S. Geological Survey collected 11 sediment cores and 15 bottom-sediment samples in September 2007. Subsamples from five selected cores and the bottom-sediment samples were analyzed for major and trace elements and forms of carbon.\r\n\r\nThe sediment samples collected from the sediment-water interface had larger average concentrations of zinc, cadmium, and lead than local background. The core collected from the Spring River had the largest concentrations of mining-related elements. A core collected just south of Twin Bridges State Park, at the confluence of the Spring and Neosho Rivers, showed a mixing zone with more mining-related elements coming from the Spring River side. The element zinc showed the most definitive patterns in graphs depicting concentration-versus-depth profiles. A core collected from the main body of the reservoir showed affected sediment down to a depth of 85 cm (33 in). This core and two others appear to have penetrated to below mining-affected sediment.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101298","usgsCitation":"Fey, D.L., Becker, M.F., and Smith, K.S., 2010, Geochemical data for core and bottom-sediment samples collected in 2007 from Grand Lake O' the Cherokees, northeast Oklahoma: U.S. Geological Survey Open-File Report 2010-1298, vi, 20 p., https://doi.org/10.3133/ofr20101298.","productDescription":"vi, 20 p.","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":126055,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1298.png"},{"id":14404,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1298/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.08333333333333,36.4 ], [ -95.08333333333333,36.86666666666667 ], [ -94.63333333333334,36.86666666666667 ], [ -94.63333333333334,36.4 ], [ -95.08333333333333,36.4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae74b","contributors":{"authors":[{"text":"Fey, David L. dfey@usgs.gov","contributorId":713,"corporation":false,"usgs":true,"family":"Fey","given":"David","email":"dfey@usgs.gov","middleInitial":"L.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":307120,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Becker, Mark F.","contributorId":40180,"corporation":false,"usgs":true,"family":"Becker","given":"Mark","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":307121,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Kathleen S. 0000-0001-8547-9804 ksmith@usgs.gov","orcid":"https://orcid.org/0000-0001-8547-9804","contributorId":182,"corporation":false,"usgs":true,"family":"Smith","given":"Kathleen","email":"ksmith@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":307122,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9000523,"text":"ofr20101304 - 2010 - Reducing Uncertainty in the Distribution of Hydrogeologic Units within Volcanic Composite Units of Pahute Mesa Using High-Resolution 3-D Resistivity Methods, Nevada Test Site, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:11:57","indexId":"ofr20101304","displayToPublicDate":"2010-12-28T00:00:00","publicationYear":"2010","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":"2010-1304","title":"Reducing Uncertainty in the Distribution of Hydrogeologic Units within Volcanic Composite Units of Pahute Mesa Using High-Resolution 3-D Resistivity Methods, Nevada Test Site, Nevada","docAbstract":"The U.S. Department of Energy (DOE) and the National Nuclear Security Administration (NNSA) at their Nevada Site Office (NSO) are addressing groundwater contamination resulting from historical underground nuclear testing through the Environmental Management program and, in particular, the Underground Test Area (UGTA) project. From 1951 to 1992, 828 underground nuclear tests were conducted at the Nevada Test Site (NTS) northwest of Las Vegas (DOE UGTA, 2003). Most of these tests were conducted hundreds of feet above the groundwater table; however, more than 200 of the tests were near, or within, the water table. This underground testing was limited to specific areas of the NTS including Pahute Mesa, Rainier Mesa/Shoshone Mountain, Frenchman Flat, and Yucca Flat. Volcanic composite units make up much of the area within the Pahute Mesa Corrective Action Unit (CAU) at the NTS, Nevada. The extent of many of these volcanic composite units extends throughout and south of the primary areas of past underground testing at Pahute and Rainier Mesas. As situated, these units likely influence the rate and direction of groundwater flow and radionuclide transport. Currently, these units are poorly resolved in terms of their hydrologic properties introducing large uncertainties into current CAU-scale flow and transport models. In 2007, the U.S. Geological Survey (USGS), in cooperation with DOE and NNSA-NSO acquired three-dimensional (3-D) tensor magnetotelluric data at the NTS in Area 20 of Pahute Mesa CAU. A total of 20 magnetotelluric recording stations were established at about 600-m spacing on a 3-D array and were tied to ER20-6 well and other nearby well control (fig. 1). The purpose of this survey was to determine if closely spaced 3-D resistivity measurements can be used to characterize the distribution of shallow (600- to 1,500-m-depth range) devitrified rhyolite lava-flow aquifers (LFA) and zeolitic tuff confining units (TCU) in areas of limited drill hole control on Pahute Mesa within the Calico Hills zeolitic volcanic composite unit (VCU), an important hydrostratigraphic unit in Area 20. The resistivity response was evaluated and compared with existing well data and hydrogeologic unit tops from the current Pahute Mesa framework model. In 2008, the USGS processed and inverted the magnetotelluric data into a 3-D resistivity model. We interpreted nine depth slices and four west-east profile cross sections of the 3-D resistivity inversion model. This report documents the geologic interpretation of the 3-D resistivity model. Expectations are that spatial variations in the electrical properties of the Calico Hills zeolitic VCU can be detected and mapped with 3-D resistivity, and that these changes correlate to differences in rock permeability. With regard to LFA and TCU, electrical resistivity and permeability are typically related. Tuff confining units will typically have low electrical resistivity and low permeability, whereas LFA will have higher electrical resistivity and zones of higher fracture-related permeability. If expectations are shown to be correct, the method can be utilized by the UGTA scientists to refine the hydrostratigraphic unit (HSU) framework in an effort to more accurately predict radionuclide transport away from test areas on Pahute and Rainier Mesas.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101304","usgsCitation":"Rodriguez, B.D., Sweetkind, D., and Burton, B., 2010, Reducing Uncertainty in the Distribution of Hydrogeologic Units within Volcanic Composite Units of Pahute Mesa Using High-Resolution 3-D Resistivity Methods, Nevada Test Site, Nevada: U.S. Geological Survey Open-File Report 2010-1304, v, 32 p.; Appendices; Figures; Tables   , https://doi.org/10.3133/ofr20101304.","productDescription":"v, 32 p.; Appendices; Figures; Tables   ","numberOfPages":"498","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":126009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1304.png"},{"id":19182,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1304/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.45,37.25 ], [ -116.45,37.28333333333333 ], [ -116.4,37.28333333333333 ], [ -116.4,37.25 ], [ -116.45,37.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63527c","contributors":{"authors":[{"text":"Rodriguez, Brian D. 0000-0002-2263-611X brod@usgs.gov","orcid":"https://orcid.org/0000-0002-2263-611X","contributorId":836,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Brian","email":"brod@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":344202,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sweetkind, Don","contributorId":28725,"corporation":false,"usgs":true,"family":"Sweetkind","given":"Don","email":"","affiliations":[],"preferred":false,"id":344204,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burton, Bethany L. 0000-0001-5011-7862 blburton@usgs.gov","orcid":"https://orcid.org/0000-0001-5011-7862","contributorId":1341,"corporation":false,"usgs":true,"family":"Burton","given":"Bethany L.","email":"blburton@usgs.gov","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":344203,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9000521,"text":"ofr20101309 - 2010 - Improved USGS methodology for assessing continuous petroleum resources using analogs","interactions":[],"lastModifiedDate":"2012-02-02T00:04:48","indexId":"ofr20101309","displayToPublicDate":"2010-12-28T00:00:00","publicationYear":"2010","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":"2010-1309","title":"Improved USGS methodology for assessing continuous petroleum resources using analogs","docAbstract":"The currently used U.S. Geological Survey methodology for assessing continuous (unconventional) petroleum resources of the United States was developed in the 1990s. This methodology poorly incorporates uncertainty about the estimated ultimate recoveries (EURs). This is especially problematic for hypothetical assessment units where this may be the largest source of uncertainty that needs to be reflected in the estimates. An improved methodology estimates the uncertainty of mean EUR directly. It uses analog data that have been compiled from production histories of many developed U.S. continuous assessment units. The analog databases provide a way of estimating the variability of not just EURs but other production parameters useful in assessing continuous resources.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101309","usgsCitation":"Charpentier, R., and Cook, T., 2010, Improved USGS methodology for assessing continuous petroleum resources using analogs: U.S. Geological Survey Open-File Report 2010-1309, 27 p., https://doi.org/10.3133/ofr20101309.","productDescription":"27 p.","numberOfPages":"27","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":126057,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1309.png"},{"id":14406,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1309/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e8a2","contributors":{"authors":[{"text":"Charpentier, Ronald R. charpentier@usgs.gov","contributorId":934,"corporation":false,"usgs":true,"family":"Charpentier","given":"Ronald R.","email":"charpentier@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":344196,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cook, Troy","contributorId":6418,"corporation":false,"usgs":true,"family":"Cook","given":"Troy","affiliations":[],"preferred":false,"id":344197,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9000522,"text":"ofr20101280 - 2010 - CO2calc: A User-Friendly Seawater Carbon Calculator for Windows, Mac OS X, and iOS (iPhone)","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"ofr20101280","displayToPublicDate":"2010-12-28T00:00:00","publicationYear":"2010","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":"2010-1280","title":"CO2calc: A User-Friendly Seawater Carbon Calculator for Windows, Mac OS X, and iOS (iPhone)","docAbstract":"A user-friendly, stand-alone application for the calculation of carbonate system parameters was developed by the U.S. Geological Survey Florida Shelf Ecosystems Response to Climate Change Project in response to its Ocean Acidification Task. The application, by Mark Hansen and Lisa Robbins, USGS St. Petersburg, FL, Joanie Kleypas, NCAR, Boulder, CO, and Stephan Meylan, Jacobs Technology, St. Petersburg, FL, is intended as a follow-on to CO2SYS, originally developed by Lewis and Wallace (1998) and later modified for Microsoft Excel? by Denis Pierrot (Pierrot and others, 2006). Besides eliminating the need for using Microsoft Excel on the host system, CO2calc offers several improvements on CO2SYS, including: An improved graphical user interface for data entry and results Additional calculations of air-sea CO2 fluxes (for surface water calculations) The ability to tag data with sample name, comments, date, time, and latitude/longitude The ability to use the system time and date and latitude/ longitude (automatic retrieval of latitude and longitude available on iPhone? 3, 3GS, 4, and Windows? hosts with an attached National Marine Electronics Association (NMEA)-enabled GPS) The ability to process multiple files in a batch processing mode An option to save sample information, data input, and calculated results as a comma-separated value (CSV) file for use with Microsoft Excel, ArcGIS,? or other applications An option to export points with geographic coordinates as a KMZ file for viewing and editing in Google EarthTM","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101280","collaboration":"Florida Shelf Ecosystems Response to Climate Change Project\r\n","usgsCitation":"Robbins, L.L., Hansen, M.E., Kleypas, J., and Meylan, S., 2010, CO2calc: A User-Friendly Seawater Carbon Calculator for Windows, Mac OS X, and iOS (iPhone): U.S. Geological Survey Open-File Report 2010-1280, iv, 17 p.; PC zip file; Macintosh disk image file; iTunes link , https://doi.org/10.3133/ofr20101280.","productDescription":"iv, 17 p.; PC zip file; Macintosh disk image file; iTunes link ","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":115902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1280.bmp"},{"id":19181,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1280/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9834","contributors":{"authors":[{"text":"Robbins, L. L.","contributorId":71156,"corporation":false,"usgs":true,"family":"Robbins","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":344200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, M. E.","contributorId":71157,"corporation":false,"usgs":true,"family":"Hansen","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":344201,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kleypas, J.A.","contributorId":13221,"corporation":false,"usgs":true,"family":"Kleypas","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":344198,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Meylan, S.C.","contributorId":13964,"corporation":false,"usgs":true,"family":"Meylan","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":344199,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":98968,"text":"ofr20101290 - 2010 - Reconnaissance of Macondo-1 well oil in sediment and tarballs from the northern Gulf of Mexico shoreline, Texas to Florida","interactions":[],"lastModifiedDate":"2012-02-10T00:10:06","indexId":"ofr20101290","displayToPublicDate":"2010-12-23T00:00:00","publicationYear":"2010","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":"2010-1290","title":"Reconnaissance of Macondo-1 well oil in sediment and tarballs from the northern Gulf of Mexico shoreline, Texas to Florida","docAbstract":"Hydrocarbons were extracted and analyzed from sediment and tarballs collected from the northern Gulf of Mexico (nGOM) coast that is potentially impacted by Macondo-1 (M-1) well oil. The samples were analyzed for a suite of diagnostic geochemical biomarkers. Aided by multivariate statistical analysis, the M-1 well oil has been identified in sediment and tarballs collected from Louisiana, Alabama, Mississippi, and Florida. None of the sediment hydrocarbon extracts from Texas correlated with the M-1 well oil. Oil-impacted sediments are confined to the shoreline adjacent to the cumulative oil slick of the Deepwater Horizon oil spill, and no impact was observed outside of this area. ","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101290","collaboration":"A Preliminary Report to the U.S. Coast Guard","usgsCitation":"Rosenbauer, R.J., Campbell, P.L., Lam, A., Lorenson, T., Hostettler, F.D., Thomas, B., and Wong, F.L., 2010, Reconnaissance of Macondo-1 well oil in sediment and tarballs from the northern Gulf of Mexico shoreline, Texas to Florida: U.S. Geological Survey Open-File Report 2010-1290, iii, 7 p.; Figures; Tables; Appendices , https://doi.org/10.3133/ofr20101290.","productDescription":"iii, 7 p.; Figures; Tables; Appendices ","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":126005,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1290.bmp"},{"id":14399,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1290/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96,27 ], [ -96,31 ], [ -82,31 ], [ -82,27 ], [ -96,27 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e836","contributors":{"authors":[{"text":"Rosenbauer, Robert J. brosenbauer@usgs.gov","contributorId":204,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"Robert","email":"brosenbauer@usgs.gov","middleInitial":"J.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":307105,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Pamela L.","contributorId":76719,"corporation":false,"usgs":true,"family":"Campbell","given":"Pamela","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":307110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lam, Angela","contributorId":37312,"corporation":false,"usgs":true,"family":"Lam","given":"Angela","email":"","affiliations":[],"preferred":false,"id":307109,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lorenson, T.D. tlorenson@usgs.gov","contributorId":2622,"corporation":false,"usgs":true,"family":"Lorenson","given":"T.D.","email":"tlorenson@usgs.gov","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":false,"id":307107,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hostettler, Frances D. fdhostet@usgs.gov","contributorId":3383,"corporation":false,"usgs":true,"family":"Hostettler","given":"Frances","email":"fdhostet@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":307108,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Thomas, Burt","contributorId":95454,"corporation":false,"usgs":true,"family":"Thomas","given":"Burt","affiliations":[],"preferred":false,"id":307111,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wong, Florence L. 0000-0002-3918-5896 fwong@usgs.gov","orcid":"https://orcid.org/0000-0002-3918-5896","contributorId":1990,"corporation":false,"usgs":true,"family":"Wong","given":"Florence","email":"fwong@usgs.gov","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":307106,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":98971,"text":"ofr20101271 - 2010 - Bird migration patterns in the arid southwest-Final report","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"ofr20101271","displayToPublicDate":"2010-12-23T00:00:00","publicationYear":"2010","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":"2010-1271","title":"Bird migration patterns in the arid southwest-Final report","docAbstract":"To ensure full life-cycle conservation, we need to understand migrant behavior en route and how migrating species use stopover and migration aerohabitats. In the Southwest, birds traverse arid and mountainous landscapes in migration. Migrants are known to use riparian stopover habitats; we know less about how migrant density varies across the Southwest seasonally and annually, and how migrants use other habitat types during migratory stopover. Furthermore, we lack information about migrant flight altitudes, speeds, and directions of travel, and how these patterns vary seasonally and annually across the Southwest.\r\n\r\nUsing weather surveillance radar data, we identified targets likely dominated by nocturnally migrating birds and determined their flight altitudes, speeds, directions over ground, and variations in abundance. Migrating or foraging bats likely are present across the region in some of these data, particularly in central Texas. We found that migrants flew at significantly lower altitudes and significantly higher speeds in spring than in fall. In all seasons migrants maintained seasonally appropriate directions of movement. We detected significant differences in vertical structure of migrant densities that varied both geographically within seasons and seasonally within sites. We also found that in fall there was a greater and more variable passage of migrants through the central part of the borderlands (New Mexico and west Texas); in spring there was some suggestion of greater and more variable passage of migrants in the eastern borderlands (central and south Texas). Such patterns are consistent with the existence of at least two migration systems through western North America and the use of different migration routes in spring and fall for at least some species.\r\n\r\nUsing radar data and satellite land cover data, we determined the habitats with which migrants are associated during migration stopover. There were significant differences in bird densities among habitat types at all sites in at least one season. Upland forest habitat in parts of Arizona and New Mexico supported high migrant densities, especially in fall. Developed habitats in areas with little upland forest habitat also supported high migrant densities. Scrub/shrub and grassland habitats supported low to intermediate migrant densities, but because these habitat types dominate the region, they may support large numbers of migratory birds. This may be especially true for species that do not use forested habitats during migration.\r\n\r\nTarget identity remains a challenge for radar-based studies. Presence of bats in the data complicates interpretation of some observations, particularly from central Texas. Based on our results it is simplistic to: (1) consider the arid west as a largely inhospitable landscape in which there are only relatively small oases of habitat that provide the resources needed by all migrants; (2) think of western riparian and upland forest habitat as supporting the majority of migrants in all cases; or (3) consider a particular habitat type unimportant migrant stopover habitat based solely on migrant densities. ","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101271","collaboration":"In cooperation with University of Southern Mississippi, U.S Fish and Wildlife Service, Sonoran Joint Venture, and Lannan Foundation","usgsCitation":"Ruth, J.M., Felix, R.K., and Dieh, R.H., 2010, Bird migration patterns in the arid southwest-Final report: U.S. Geological Survey Open-File Report 2010-1271, vi, 51 p., https://doi.org/10.3133/ofr20101271.","productDescription":"vi, 51 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":126735,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1271.png"},{"id":14403,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1271/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af2e4b07f02db691952","contributors":{"authors":[{"text":"Ruth, Janet M. 0000-0003-1576-5957 janet_ruth@usgs.gov","orcid":"https://orcid.org/0000-0003-1576-5957","contributorId":1408,"corporation":false,"usgs":true,"family":"Ruth","given":"Janet","email":"janet_ruth@usgs.gov","middleInitial":"M.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":307117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Felix, Rodney K.","contributorId":22753,"corporation":false,"usgs":true,"family":"Felix","given":"Rodney","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":307118,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dieh, Robert H.","contributorId":50130,"corporation":false,"usgs":true,"family":"Dieh","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":307119,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":98965,"text":"ofr20101273 - 2010 - Vegetation and substrate on aeolian landscapes in the Colorado River corridor, Cataract Canyon, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:05","indexId":"ofr20101273","displayToPublicDate":"2010-12-22T00:00:00","publicationYear":"2010","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":"2010-1273","title":"Vegetation and substrate on aeolian landscapes in the Colorado River corridor, Cataract Canyon, Utah","docAbstract":"Vegetation and substrate data presented in this report characterize ground cover on aeolian landscapes of the Colorado River corridor through Cataract Canyon, Utah, in Canyonlands National Park. The 27-km-long Cataract Canyon reach has undergone less anthropogenic alteration than other reaches of the mainstem Colorado River. Characterizing ecosystem parameters there provides a basis against which to evaluate future changes, such as those that could result from the further spread of nonnative plant species or increased visitor use. Upstream dams have less effect on the hydrology and sediment supply in Cataract Canyon compared with downstream reaches in Grand Canyon National Park. For this reason, comparison of these vegetation and substrate measurements with similar data from aeolian landscapes of Grand Canyon will help to resolve the effects of Glen Canyon Dam operations on the Colorado River corridor ecosystem. \r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101273","usgsCitation":"Draut, A.E., and Gillette, E.R., 2010, Vegetation and substrate on aeolian landscapes in the Colorado River corridor, Cataract Canyon, Utah: U.S. Geological Survey Open-File Report 2010-1273, iv, 21 p.; Tables; Downloads: Spreadsheet of Tables 1-14, https://doi.org/10.3133/ofr20101273.","productDescription":"iv, 21 p.; Tables; Downloads: Spreadsheet of Tables 1-14","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":126152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1273.gif"},{"id":14396,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1273/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.16666666666667,37.833333333333336 ], [ -110.16666666666667,38.25 ], [ -109.83333333333333,38.25 ], [ -109.83333333333333,37.833333333333336 ], [ -110.16666666666667,37.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602678","contributors":{"authors":[{"text":"Draut, Amy E.","contributorId":92215,"corporation":false,"usgs":true,"family":"Draut","given":"Amy","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":307100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gillette, Elizabeth R.","contributorId":71519,"corporation":false,"usgs":true,"family":"Gillette","given":"Elizabeth","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":307099,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":98967,"text":"ofr20101275 - 2010 - Streamflow, water quality, and constituent loads and yields, Scituate Reservoir drainage area, Rhode Island, water year 2009","interactions":[],"lastModifiedDate":"2012-03-08T17:16:13","indexId":"ofr20101275","displayToPublicDate":"2010-12-22T00:00:00","publicationYear":"2010","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":"2010-1275","title":"Streamflow, water quality, and constituent loads and yields, Scituate Reservoir drainage area, Rhode Island, water year 2009","docAbstract":"Streamflow and water-quality data were collected by the U.S. Geological Survey (USGS) or the Providence Water Supply Board (PWSB), Rhode Island's largest drinking-water supplier. Streamflow was measured or estimated by the USGS following standard methods at 23 streamgage stations; 13 of these stations were also equipped with instrumentation capable of continuously monitoring specific conductance and water temperature. Streamflow and concentrations of sodium and chloride estimated from records of specific conductance were used to calculate loads of sodium and chloride during water year (WY) 2009 (October 1, 2008, to September 30, 2009). Water-quality samples also were collected at 37 sampling stations by the PWSB and at 14 monitoring stations by the USGS during WY 2009 as part of a long-term sampling program; all stations are in the Scituate Reservoir drainage area. Water-quality data collected by PWSB are summarized by using values of central tendency and are used, in combination with measured (or estimated) streamflows, to calculate loads and yields (loads per unit area) of selected water-quality constituents for WY 2009.\r\n\r\nThe largest tributary to the reservoir (the Ponaganset River, which was monitored by the USGS) contributed a mean streamflow of about 27 cubic feet per second (ft3/s) to the reservoir during WY 2009. For the same time period, annual mean1 streamflows measured (or estimated) for the other monitoring stations in this study ranged from about 0.50 to 17 ft3/s. Together, tributary streams (equipped with instrumentation capable of continuously monitoring specific conductance) transported about 1,400,000 kilograms (kg) of sodium and 2,200,000 kg of chloride to the Scituate Reservoir during WY 2009; sodium and chloride yields for the tributaries ranged from 10,000 to 64,000 kilograms per square mile (kg/mi2) and from 15,000 to 110,000 kg/mi2, respectively.\r\n\r\nAt the stations where water-quality samples were collected by the PWSB, the median of the median chloride concentrations was 21.7 milligrams per liter (mg/L), median nitrite concentration was 0.001 mg/L as N, median nitrate concentration was 0.02 mg/L as N, median orthophosphate concentration was 0.09 mg/L as P, and median concentrations of total coliform and Escherichia coli (E. coli) bacteria were 61 and 16 colony forming units per 100 milliliters (CFU/100 mL), respectively. The medians of the median daily loads (and yields) of chloride, nitrite, nitrate, orthophosphate, and total coliform and E. coli bacteria were 190 kg/d (61 kg/d/mi2), 12 g/d (4.5 g/d/mi2), 93 g/d (32 g/d/mi2), 420 g/d (290 g/d/mi2), 6,200 million colony forming units per day (CFU?106/d) (2,600 CFU?106/d/mi2), and 1,100 CFU?106/d (340 CFU?106/d/mi2), respectively.\r\n\r\n  1The arithmetic mean of the individual daily mean discharges for the year noted or for the designated period. \r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101275","collaboration":"Prepared in cooperation with the Providence Water Supply Board \r\n","usgsCitation":"Breault, R., and Smith, K.P., 2010, Streamflow, water quality, and constituent loads and yields, Scituate Reservoir drainage area, Rhode Island, water year 2009: U.S. Geological Survey Open-File Report 2010-1275, iv, 24 p. , https://doi.org/10.3133/ofr20101275.","productDescription":"iv, 24 p. ","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2008-10-01","temporalEnd":"2009-09-30","costCenters":[{"id":544,"text":"Rhode Island Water Science Center","active":false,"usgs":true}],"links":[{"id":116277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1275.bmp"},{"id":14398,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1275/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.83333333333333,41.666666666666664 ], [ -71.83333333333333,41.916666666666664 ], [ -71.5,41.916666666666664 ], [ -71.5,41.666666666666664 ], [ -71.83333333333333,41.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4bd0","contributors":{"authors":[{"text":"Breault, Robert F. 0000-0002-2517-407X rbreault@usgs.gov","orcid":"https://orcid.org/0000-0002-2517-407X","contributorId":2219,"corporation":false,"usgs":true,"family":"Breault","given":"Robert F.","email":"rbreault@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":307104,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Kirk P. 0000-0003-0269-474X kpsmith@usgs.gov","orcid":"https://orcid.org/0000-0003-0269-474X","contributorId":1516,"corporation":false,"usgs":true,"family":"Smith","given":"Kirk","email":"kpsmith@usgs.gov","middleInitial":"P.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":307103,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":98964,"text":"ofr20101283 - 2010 - Development of monitoring protocols to detect change in rocky intertidal communities of Glacier Bay National Park and Preserve","interactions":[],"lastModifiedDate":"2012-02-02T00:04:46","indexId":"ofr20101283","displayToPublicDate":"2010-12-22T00:00:00","publicationYear":"2010","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":"2010-1283","title":"Development of monitoring protocols to detect change in rocky intertidal communities of Glacier Bay National Park and Preserve","docAbstract":"Glacier Bay National Park and Preserve in southeastern Alaska includes extensive coastlines representing a major proportion of all coastlines held by the National Park Service. The marine plants and invertebrates that occupy intertidal shores form highly productive communities that are ecologically important to a number of vertebrate and invertebrate consumers and that are vulnerable to human disturbances. To better understand these communities and their sensitivity, it is important to obtain information on species abundances over space and time. During field studies from 1997 to 2001, I investigated probability-based rocky intertidal monitoring designs that allow inference of results to similar habitat within the bay and that reduce bias. Aerial surveys of a subset of intertidal habitat indicated that the original target habitat of bedrock-dominated sites with slope less than or equal to 30 degrees was rare. This finding illustrated the value of probability-based surveys and led to a shift in the target habitat type to more mixed rocky habitat with steeper slopes. Subsequently, I investigated different sampling methods and strategies for their relative power to detect changes in the abundances of the predominant sessile intertidal taxa: barnacles -Balanomorpha, the mussel Mytilus trossulus and the rockweed Fucus distichus subsp. evanescens. I found that lower-intensity sampling of 25 randomly selected sites (= coarse-grained sampling) provided a greater ability to detect changes in the abundances of these taxa than did more intensive sampling of 6 sites (= fine-grained sampling). Because of its greater power, the coarse-grained sampling scheme was adopted in subsequent years. This report provides detailed analyses of the 4 years of data and evaluates the relative effect of different sampling attributes and management-set parameters on the ability of the sampling to detect changes in the abundances of these taxa. The intent was to provide managers with information to guide design choices for intertidal monitoring. I found that the coarse-grained surveys, as conducted from 1998 to 2001, had power ranging from 0.68 to 1.0 to detect 10 percent annual changes in the abundances of these predominant sessile species. The information gained through intertidal monitoring would be useful in assessing changes due to climate (including ocean acidification), invasive species, trampling effects, and oil spills.\r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101283","collaboration":"Prepared in cooperation with the National Park Service\r\n","usgsCitation":"Irvine, G.V., 2010, Development of monitoring protocols to detect change in rocky intertidal communities of Glacier Bay National Park and Preserve: U.S. Geological Survey Open-File Report 2010-1283, vi, 29 p.; Figures; Tables; Appendices; Downloads: Report Body; Appendix A; Appendix B; Appendix C; Appendix D; Appendix E, https://doi.org/10.3133/ofr20101283.","productDescription":"vi, 29 p.; Figures; Tables; Appendices; Downloads: Report Body; Appendix A; Appendix B; Appendix C; Appendix D; Appendix E","additionalOnlineFiles":"Y","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":126153,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1283.jpg"},{"id":14395,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1283/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de70","contributors":{"authors":[{"text":"Irvine, Gail V. girvine@usgs.gov","contributorId":2368,"corporation":false,"usgs":true,"family":"Irvine","given":"Gail","email":"girvine@usgs.gov","middleInitial":"V.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":307098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":98966,"text":"ofr20101247 - 2010 - Internet-based interface for STRMDEPL08","interactions":[],"lastModifiedDate":"2012-03-08T17:16:13","indexId":"ofr20101247","displayToPublicDate":"2010-12-22T00:00:00","publicationYear":"2010","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":"2010-1247","title":"Internet-based interface for STRMDEPL08","docAbstract":"The core of the computer program STRMDEPL08 that estimates streamflow depletion by a pumping well with one of four analytical solutions was re-written in the Javascript software language and made available through an internet-based interface (web page). In the internet-based interface, the user enters data for one of the four analytical solutions, Glover and Balmer (1954), Hantush (1965), Hunt (1999), and Hunt (2003), and the solution is run for constant pumping for a desired number of simulation days. Results are returned in tabular form to the user. For intermittent pumping, the interface allows the user to request that the header information for an input file for the stand-alone executable STRMDEPL08 be created. The user would add the pumping information to this header information and run the STRMDEPL08 executable that is available for download through the U.S. Geological Survey. Results for the internet-based and stand-alone versions of STRMDEPL08 are shown to match.\r\n\r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101247","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency\r\n","usgsCitation":"Reeves, H.W., and Asher, A., 2010, Internet-based interface for STRMDEPL08: U.S. Geological Survey Open-File Report 2010-1247, iv, 7 p.; Appendix, https://doi.org/10.3133/ofr20101247.","productDescription":"iv, 7 p.; Appendix","additionalOnlineFiles":"N","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":126151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1247.gif"},{"id":14397,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1247/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0799","contributors":{"authors":[{"text":"Reeves, Howard W. 0000-0001-8057-2081 hwreeves@usgs.gov","orcid":"https://orcid.org/0000-0001-8057-2081","contributorId":2307,"corporation":false,"usgs":true,"family":"Reeves","given":"Howard","email":"hwreeves@usgs.gov","middleInitial":"W.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":307101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Asher, A. Jeremiah","contributorId":34098,"corporation":false,"usgs":true,"family":"Asher","given":"A. Jeremiah","affiliations":[],"preferred":false,"id":307102,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9000519,"text":"ofr20101006 - 2010 - Geophysical and sampling data from the inner continental shelf: Northern Cape Cod Bay, Massachusetts","interactions":[],"lastModifiedDate":"2017-11-10T18:26:01","indexId":"ofr20101006","displayToPublicDate":"2010-12-22T00:00:00","publicationYear":"2010","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":"2010-1006","title":"Geophysical and sampling data from the inner continental shelf: Northern Cape Cod Bay, Massachusetts","docAbstract":"The U.S. Geological Survey (USGS) and the Massachusetts Office of Coastal Zone Management (CZM) have cooperated to map approximately 480 km2 of the inner continental shelf in northern Cape Cod Bay, MA. This report contains geophysical and sampling data collected by the USGS during five research cruises between 2006 and 2008. The geophysical data include (1) swath bathymetry from interferometric sonar, (2) acoustic backscatter from interferometric and sidescan sonars, and (3) subsurface stratigraphy and structure from seismic-reflection profilers. The seafloor sampling data include sediment samples, photographs, and video tracklines. These spatial data support research on the influence that sea-level change and sediment supply have on coastal evolution and help identify the type, distribution, and quality of subtidal marine habitats within the coastal zone of Massachusetts.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101006","usgsCitation":"Andrews, B., Ackerman, S.D., Baldwin, W.E., and Barnhardt, W., 2010, Geophysical and sampling data from the inner continental shelf: Northern Cape Cod Bay, Massachusetts: U.S. Geological Survey Open-File Report 2010-1006, HTML Page and DVD/CD Rom; PDF: iv, 7 p.; Figures; Appendices, https://doi.org/10.3133/ofr20101006.","productDescription":"HTML Page and DVD/CD Rom; PDF: iv, 7 p.; Figures; Appendices","numberOfPages":"19","additionalOnlineFiles":"Y","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":126007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1006.bmp"},{"id":19180,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1006/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","geographicExtents":"{\"crs\": {\"type\": \"name\", \"properties\": {\"name\": \"urn:ogc:def:crs:OGC:1.3:CRS84\"}}, \"geometry\": {\"type\": \"Polygon\", \"coordinates\": [[[-70.1341037750243, 41.95104789733888], [-70.4096186705684, 41.95154055278067], [-70.50489807128906, 41.929197311401474], [-70.59550666809083, 41.96906852722178], [-70.5973510870749, 41.97991037474872], [-70.5879332917579, 41.986537712194135], [-70.58897971345982, 41.998048350914765], [-70.63153419600297, 42.0399052189901], [-70.64330863952637, 42.06887245178229], [-70.59966278076172, 42.08695030212412], [-70.53343772888182, 42.093832015991325], [-70.27768516540526, 42.09016227722178], [-70.26380271816402, 42.08609683315666], [-70.22901064801272, 42.0373683146205], [-70.2007572620618, 42.0206255673903], [-70.15401709271117, 41.955049807405885], [-70.13692553824713, 41.956096229107686], [-70.13679885864252, 42.04490470886237], [-70.1330777347764, 41.954507150169185], [-70.1128253936767, 41.95272636413572], [-70.1341037750243, 41.95104789733888]]]}, \"properties\": {\"extentType\": \"Custom\", \"code\": \"\", \"name\": \"\", \"notes\": \"\", \"promotedForReuse\": false, \"abbreviation\": \"\", \"shortName\": \"\", \"description\": \"\"}, \"bbox\": [-70.64330863952637, 41.929197311401474, -70.1128253936767, 42.09390449523937], \"type\": \"Feature\", \"id\": \"3091914\"}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c1cd","contributors":{"authors":[{"text":"Andrews, Brian D.","contributorId":54180,"corporation":false,"usgs":true,"family":"Andrews","given":"Brian D.","affiliations":[],"preferred":false,"id":344194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ackerman, Seth D. 0000-0003-0945-2794 sackerman@usgs.gov","orcid":"https://orcid.org/0000-0003-0945-2794","contributorId":178676,"corporation":false,"usgs":true,"family":"Ackerman","given":"Seth","email":"sackerman@usgs.gov","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":344193,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baldwin, Wayne E. 0000-0001-5886-0917 wbaldwin@usgs.gov","orcid":"https://orcid.org/0000-0001-5886-0917","contributorId":1321,"corporation":false,"usgs":true,"family":"Baldwin","given":"Wayne","email":"wbaldwin@usgs.gov","middleInitial":"E.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":344192,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barnhardt, Walter A.","contributorId":80656,"corporation":false,"usgs":true,"family":"Barnhardt","given":"Walter A.","affiliations":[],"preferred":false,"id":344195,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":9000518,"text":"ofr20101324 - 2010 - Great Basin Integrated Landscape Monitoring Pilot Summary Report","interactions":[],"lastModifiedDate":"2012-02-10T00:11:57","indexId":"ofr20101324","displayToPublicDate":"2010-12-21T00:00:00","publicationYear":"2010","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":"2010-1324","title":"Great Basin Integrated Landscape Monitoring Pilot Summary Report","docAbstract":"The Great Basin Integrated Landscape Monitoring Pilot project (GBILM) was one of four regional pilots to implement the U.S. Geological Survey (USGS) Science Thrust on Integrated Landscape Monitoring (ILM) whose goal was to observe, understand, and predict landscape change and its implications on natural resources at multiple spatial and temporal scales and address priority natural resource management and policy issues. The Great Basin is undergoing rapid environmental change stemming from interactions among global climate trends, increasing human populations, expanding and accelerating land and water uses, invasive species, and altered fire regimes. GBLIM tested concepts and developed tools to store and analyze monitoring data, understand change at multiple scales, and forecast landscape change. The GBILM endeavored to develop and test a landscape-level monitoring approach in the Great Basin that integrates USGS disciplines, addresses priority management questions, catalogs and uses existing monitoring data, evaluates change at multiple scales, and contributes to development of regional monitoring strategies. GBILM functioned as an integrative team from 2005 to 2010, producing more than 35 science and data management products that addressed pressing ecosystem drivers and resource management agency needs in the region. This report summarizes the approaches and methods of this interdisciplinary effort, identifies and describes the products generated, and provides lessons learned during the project.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101324","usgsCitation":"Finn, S.P., Kitchell, K., Baer, L.A., Bedford, D.R., Brooks, M.L., Flint, A.L., Flint, L.E., Matchett, J., Mathie, A., Miller, D., Pilliod, D., Torregrosa, A.A., and Woodward, A., 2010, Great Basin Integrated Landscape Monitoring Pilot Summary Report: U.S. Geological Survey Open-File Report 2010-1324, iv, 21 p.; Tables; Figures; Appendices, https://doi.org/10.3133/ofr20101324.","productDescription":"iv, 21 p.; Tables; Figures; Appendices","additionalOnlineFiles":"N","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":203749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":19179,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1324/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122,34 ], [ -122,44 ], [ -112,44 ], [ -112,34 ], [ -122,34 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9a8","contributors":{"authors":[{"text":"Finn, Sean P.","contributorId":106623,"corporation":false,"usgs":true,"family":"Finn","given":"Sean","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":344191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kitchell, Kate","contributorId":69694,"corporation":false,"usgs":true,"family":"Kitchell","given":"Kate","email":"","affiliations":[],"preferred":false,"id":344190,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baer, Lori Anne 0000-0003-1908-979X labaer@usgs.gov","orcid":"https://orcid.org/0000-0003-1908-979X","contributorId":4429,"corporation":false,"usgs":true,"family":"Baer","given":"Lori","email":"labaer@usgs.gov","middleInitial":"Anne","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":344188,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bedford, David R. dbedford@usgs.gov","contributorId":3852,"corporation":false,"usgs":true,"family":"Bedford","given":"David","email":"dbedford@usgs.gov","middleInitial":"R.","affiliations":[{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":344187,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Brooks, Matthew L. 0000-0002-3518-6787 mlbrooks@usgs.gov","orcid":"https://orcid.org/0000-0002-3518-6787","contributorId":393,"corporation":false,"usgs":true,"family":"Brooks","given":"Matthew","email":"mlbrooks@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":344180,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Flint, Alan L. 0000-0002-5118-751X aflint@usgs.gov","orcid":"https://orcid.org/0000-0002-5118-751X","contributorId":1492,"corporation":false,"usgs":true,"family":"Flint","given":"Alan","email":"aflint@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":344182,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Flint, Lorraine E. 0000-0002-7868-441X lflint@usgs.gov","orcid":"https://orcid.org/0000-0002-7868-441X","contributorId":1184,"corporation":false,"usgs":true,"family":"Flint","given":"Lorraine","email":"lflint@usgs.gov","middleInitial":"E.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":344181,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Matchett, J.R.","contributorId":11535,"corporation":false,"usgs":true,"family":"Matchett","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":344189,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Mathie, Amy amathie@usgs.gov","contributorId":2542,"corporation":false,"usgs":true,"family":"Mathie","given":"Amy","email":"amathie@usgs.gov","affiliations":[],"preferred":true,"id":344184,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Miller, David M. 0000-0003-3711-0441 dmiller@usgs.gov","orcid":"https://orcid.org/0000-0003-3711-0441","contributorId":1707,"corporation":false,"usgs":true,"family":"Miller","given":"David M.","email":"dmiller@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":344183,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Pilliod, David S. 0000-0003-4207-3518 dpilliod@usgs.gov","orcid":"https://orcid.org/0000-0003-4207-3518","contributorId":161,"corporation":false,"usgs":true,"family":"Pilliod","given":"David S.","email":"dpilliod@usgs.gov","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":false,"id":344179,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Torregrosa, Alicia A. 0000-0001-7361-2241 atorregrosa@usgs.gov","orcid":"https://orcid.org/0000-0001-7361-2241","contributorId":3471,"corporation":false,"usgs":true,"family":"Torregrosa","given":"Alicia","email":"atorregrosa@usgs.gov","middleInitial":"A.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":344186,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Woodward, Andrea 0000-0003-0604-9115 awoodward@usgs.gov","orcid":"https://orcid.org/0000-0003-0604-9115","contributorId":3028,"corporation":false,"usgs":true,"family":"Woodward","given":"Andrea","email":"awoodward@usgs.gov","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":344185,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":98928,"text":"ofr20101259 - 2010 - Helicopter electromagnetic and magnetic geophysical survey data, portions of the North Platte and South Platte Natural Resources Districts, western Nebraska, May 2009","interactions":[{"subject":{"id":98031,"text":"ofr20091110 - 2009 - Helicopter Electromagnetic and Magnetic Geophysical Survey Data for Portions of the North Platte River and Lodgepole Creek, Nebraska, June 2008","indexId":"ofr20091110","publicationYear":"2009","noYear":false,"title":"Helicopter Electromagnetic and Magnetic Geophysical Survey Data for Portions of the North Platte River and Lodgepole Creek, Nebraska, June 2008"},"predicate":"SUPERSEDED_BY","object":{"id":98928,"text":"ofr20101259 - 2010 - Helicopter electromagnetic and magnetic geophysical survey data, portions of the North Platte and South Platte Natural Resources Districts, western Nebraska, May 2009","indexId":"ofr20101259","publicationYear":"2010","noYear":false,"title":"Helicopter electromagnetic and magnetic geophysical survey data, portions of the North Platte and South Platte Natural Resources Districts, western Nebraska, May 2009"},"id":1}],"lastModifiedDate":"2017-05-22T10:58:20","indexId":"ofr20101259","displayToPublicDate":"2010-12-14T00:00:00","publicationYear":"2010","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":"2010-1259","title":"Helicopter electromagnetic and magnetic geophysical survey data, portions of the North Platte and South Platte Natural Resources Districts, western Nebraska, May 2009","docAbstract":"This report is a release of digital data from a helicopter electromagnetic and magnetic survey that was conducted during June 2009 in areas of western Nebraska as part of a joint hydrologic study by the North Platte Natural Resource District (NRD), South Platte NRD, and U.S. Geological Survey (USGS). Flight lines for the survey totaled 937 line kilometers (582 line miles). The objective of the contracted survey, conducted by Fugro Airborne, Ltd., is to improve the understanding of the relation between surface-water and groundwater systems critical to developing groundwater models used in management programs for water resources. A unique aspect of the survey is the flight line layout. One set of flight lines was flown in a zig-zag pattern extending along the length of the previously collected airborne data. The success of this survey design depended on a well-understood regional hydrogeologic framework and model developed by the Cooperative Hydrologic Study of the Platte River Basin and the airborne geophysical data collected in 2008. Resistivity variations along lines could be related to this framework. In addition to these lines, more traditional surveys consisting of parallel flight lines, separated by about 400 meters were carried out for three blocks in the North Platte NRD, the South Platte NRD and in the area of Crescent Lakes. These surveys helped to establish the spatial variations of the resistivity of hydrostratigraphic units. An additional survey was flown over the Crescent Lake area. The objective of this survey, funded by the USGS Office of Groundwater, was to map shallow hydrogeologic features of the southwestern part of the Sand Hills that contain a mix of fresh to saline lakes.\r\n","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101259","collaboration":"Prepared in cooperation with the North Platte and South Platte Natural Resource Districts\r\n","usgsCitation":"Smith, B.D., Abraham, J., Cannia, J.C., Minsley, B., Deszcz-Pan, M., and Ball, L., 2010, Helicopter electromagnetic and magnetic geophysical survey data, portions of the North Platte and South Platte Natural Resources Districts, western Nebraska, May 2009 (Version 1.1: December 10, 2010; Revised May 15, 2017): U.S. Geological Survey Open-File Report 2010-1259, Report: 33 p.; Downloads Directory, https://doi.org/10.3133/ofr20101259.","productDescription":"Report: 33 p.; Downloads Directory","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2009-05-01","temporalEnd":"2009-05-31","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":126117,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1259.bmp"},{"id":341526,"rank":5,"type":{"id":28,"text":"Dataset"},"url":"https://pubs.usgs.gov/of/2010/1259/downloads/","text":"Downloads Directory","linkFileType":{"id":5,"text":"html"},"linkHelpText":"Contains: associated data files. Refer to the Readme and Metadata files for more information."},{"id":341525,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1259/downloads/REPORT/OF10-1259.pdf","text":"Report","size":"3.6 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":341189,"rank":4,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/2010/1259/versionHist.txt","size":"1 kB"},{"id":14351,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1259/","linkFileType":{"id":5,"text":"html"}}],"projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.5,41 ], [ -104.5,42.5 ], [ -101.5,42.5 ], [ -101.5,41 ], [ -104.5,41 ] ] ] } } ] }","edition":"Version 1.1: December 10, 2010; Revised May 15, 2017","revisedDate":"2017-05-15","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635d8c","contributors":{"authors":[{"text":"Smith, B. D.","contributorId":71123,"corporation":false,"usgs":true,"family":"Smith","given":"B.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":306962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abraham, J.D.","contributorId":20686,"corporation":false,"usgs":true,"family":"Abraham","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":306959,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cannia, J. C.","contributorId":105258,"corporation":false,"usgs":true,"family":"Cannia","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":306964,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minsley, B. J.","contributorId":52107,"corporation":false,"usgs":true,"family":"Minsley","given":"B. J.","affiliations":[],"preferred":false,"id":306961,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Deszcz-Pan, M.","contributorId":102422,"corporation":false,"usgs":true,"family":"Deszcz-Pan","given":"M.","email":"","affiliations":[],"preferred":false,"id":306963,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ball, L.B.","contributorId":37683,"corporation":false,"usgs":true,"family":"Ball","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":306960,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":9000510,"text":"ofr20101229 - 2010 - Unintended consequences of biofuels production?The effects of large-scale crop conversion on water quality and quantity","interactions":[],"lastModifiedDate":"2012-03-08T17:16:40","indexId":"ofr20101229","displayToPublicDate":"2010-12-13T00:00:00","publicationYear":"2010","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":"2010-1229","title":"Unintended consequences of biofuels production?The effects of large-scale crop conversion on water quality and quantity","docAbstract":"In the search for renewable fuel alternatives, biofuels have gained strong political momentum. In the last decade, extensive mandates, policies, and subsidies have been adopted to foster the development of a biofuels industry in the United States. The Biofuels Initiative in the Mississippi Delta resulted in a 47-percent decrease in cotton acreage with a concurrent 288-percent increase in corn acreage in 2007. Because corn uses 80 percent more water for irrigation than cotton, and more nitrogen fertilizer is recommended for corn cultivation than for cotton, this widespread shift in crop type has implications for water quantity and water quality in the Delta. Increased water use for corn is accelerating water-level declines in the Mississippi River Valley alluvial aquifer at a time when conservation is being encouraged because of concerns about sustainability of the groundwater resource. Results from a mathematical model calibrated to existing conditions in the Delta indicate that increased fertilizer application on corn also likely will increase the extent of nitrate-nitrogen movement into the alluvial aquifer. Preliminary estimates based on surface-water modeling results indicate that higher application rates of nitrogen increase the nitrogen exported from the Yazoo River Basin to the Mississippi River by about 7 percent. Thus, the shift from cotton to corn may further contribute to hypoxic (low dissolved oxygen) conditions in the Gulf of Mexico.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Welch, H.L., Green, C.T., and Coupe, R.H., 2009. The fate and transport of nitrate through the unsaturated zone at a site in northwestern Mississippi in Geological Society of America 2009 Annual Meeting, Proceedings: Geological Society of America Abstracts with Programs, volume 41, number 7, p. 29. Green, C.T., Welch, H., and Coupe, R., 2009. Multi-tracer analysis of vertical nitrate fluxes in the Mississippi River Valley alluvial aquifer, in Eos Transactions of the American Geophysical Union, 90 (52), Fall meeting, Abstract H31C-0799.","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101229","usgsCitation":"Welch, H.L., Green, C.T., Rebich, R.A., Barlow, J.R., and Hicks, M.B., 2010, Unintended consequences of biofuels production?The effects of large-scale crop conversion on water quality and quantity: U.S. Geological Survey Open-File Report 2010-1229, 6 p., https://doi.org/10.3133/ofr20101229.","productDescription":"6 p.","numberOfPages":"6","additionalOnlineFiles":"N","costCenters":[{"id":394,"text":"Mississippi Water Science Center","active":true,"usgs":true}],"links":[{"id":126043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1229.jpg"},{"id":19172,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1229/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.25,32.5 ], [ -91.25,35 ], [ -85.75,35 ], [ -85.75,32.5 ], [ -91.25,32.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ef17","contributors":{"authors":[{"text":"Welch, Heather L. 0000-0001-8370-7711 hllott@usgs.gov","orcid":"https://orcid.org/0000-0001-8370-7711","contributorId":552,"corporation":false,"usgs":true,"family":"Welch","given":"Heather","email":"hllott@usgs.gov","middleInitial":"L.","affiliations":[{"id":105,"text":"Alabama Water Science Center","active":true,"usgs":true}],"preferred":true,"id":344159,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, Christopher T. 0000-0002-6480-8194 ctgreen@usgs.gov","orcid":"https://orcid.org/0000-0002-6480-8194","contributorId":1343,"corporation":false,"usgs":true,"family":"Green","given":"Christopher","email":"ctgreen@usgs.gov","middleInitial":"T.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":344160,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rebich, Richard A. 0000-0003-4256-7171 rarebich@usgs.gov","orcid":"https://orcid.org/0000-0003-4256-7171","contributorId":2315,"corporation":false,"usgs":true,"family":"Rebich","given":"Richard","email":"rarebich@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":344161,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barlow, Jeannie R.B.","contributorId":33965,"corporation":false,"usgs":true,"family":"Barlow","given":"Jeannie","email":"","middleInitial":"R.B.","affiliations":[],"preferred":false,"id":344163,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hicks, Matthew B. 0000-0001-5516-0296 mhicks@usgs.gov","orcid":"https://orcid.org/0000-0001-5516-0296","contributorId":3778,"corporation":false,"usgs":true,"family":"Hicks","given":"Matthew","email":"mhicks@usgs.gov","middleInitial":"B.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":344162,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":9000512,"text":"ofr20101308 - 2010 - Procedures for conducting underwater searches for invasive mussels (Dreissena sp.)","interactions":[],"lastModifiedDate":"2012-02-02T00:15:49","indexId":"ofr20101308","displayToPublicDate":"2010-12-13T00:00:00","publicationYear":"2010","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":"2010-1308","title":"Procedures for conducting underwater searches for invasive mussels (Dreissena sp.)","docAbstract":"Zebra mussels (Dreissena polymorpha) were first detected in the Great Lakes in 1988. They were likely transported as larvae or young adults inside the ballast tanks of large ocean-going ships originating from Europe. Since their introduction, they have spread throughout the Eastern, Midwestern, and Southern United States. In 2007, Quagga mussels (Dreissena rostriformis bugensis) were found in the Western United States in Lake Mead, Nevada; part of the Lower Colorado River Basin. State and Federal managers are concerned that the mussels (hereafter referred to as dreissenid mussels or mussels) will continue to spread to the Columbia River Basin and have a major impact on the region?s ecosystem, water delivery infrastructure, hydroelectric projects, and the economy. The transport and use of recreational watercraft throughout the Western United States could easily result in spreading mussels to the Columbia River Basin. The number of recreational watercraft using Lake Mead can range from 350 to 3,500 a day (Bryan Moore, National Park Service, oral commun., June 21, 2008). Because recreational watercrafts are readily moved around and mussels may survive for a period of time when they are out of the water, there is a high potential to spread mussels from Lake Mead to other waterways in the Western United States. Efforts are being made to prevent the spread of mussels; however, there is great concern that these efforts will not be 100 percent successful. When prevention efforts fail, early detection of mussels may provide an opportunity to implement rapid response management actions to minimize the impact. Control and eradication efforts are more likely to be successful if they are implemented when the density of mussels is low and the area of infestation is small. Once the population grows and becomes established, the mussels are extremely difficult, if not impossible, to control. Although chemicals may be used to kill the mussels, the chemicals that are currently available also can kill other aquatic life. Early implementation of containment and eradication efforts requires getting reliable information to confirm the location of the infestation. One way to get this information is through the use of properly trained SCUBA divers. This document provides SCUBA divers with the necessary information to conduct underwater searchers for mussels. However, using SCUBA divers to search for mussels over a large geographic area is relatively expensive and inefficient. Early detection monitoring methods can be used to optimize the use of SCUBA divers. Early detection monitoring can be accomplished by collecting water samples or deploying artificial settlement substrates (fig. 1). Water samples are used to look for free-swimming larval mussels (called veligers). Because the veligers cannot be identified with the naked eye, the water samples are sent to a laboratory where they are examined under a microscope and/or analyzed using molecular techniques to detect veligers. To detect the presences of adult mussels, artificial substrates are deployed and periodically retrieved to determine if mussels have settled on the substrate. If veligers or adults are identified, SCUBA divers can be deployed to confirm the presence of mussels.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101308","collaboration":"Prepared in cooperation with the U.S. Fish and Wildlife Service","usgsCitation":"Adams, N., 2010, Procedures for conducting underwater searches for invasive mussels (Dreissena sp.): U.S. Geological Survey Open-File Report 2010-1308, iv, 30 p.; Appendices, https://doi.org/10.3133/ofr20101308.","productDescription":"iv, 30 p.; Appendices","numberOfPages":"44","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":126071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1308.jpg"},{"id":19173,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1308/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6608e6","contributors":{"authors":[{"text":"Adams, Noah","contributorId":91604,"corporation":false,"usgs":true,"family":"Adams","given":"Noah","affiliations":[],"preferred":false,"id":344164,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":98925,"text":"ofr20101265 - 2010 - Geologic map of the White Hall quadrangle, Frederick County, Virginia, and Berkeley County, West Virginia","interactions":[],"lastModifiedDate":"2022-04-14T21:56:46.974717","indexId":"ofr20101265","displayToPublicDate":"2010-12-11T00:00:00","publicationYear":"2010","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":"2010-1265","title":"Geologic map of the White Hall quadrangle, Frederick County, Virginia, and Berkeley County, West Virginia","docAbstract":"The White Hall 7.5-minute quadrangle is located within the Valley and Ridge province of northern Virginia and the eastern panhandle of West Virginia. The quadrangle is one of several being mapped to investigate the geologic framework and groundwater resources of Frederick County, Va., as well as other areas in the northern Shenandoah Valley of Virginia and West Virginia. All exposed bedrock outcrops are clastic and carbonate strata of Paleozoic age ranging from Middle Cambrian to Late Devonian. Surficial materials include unconsolidated alluvium, colluvium, and terrace deposits of Quaternary age, and local paleo-terrace deposits possibly of Tertiary age. The quadrangle lies across the northeast plunge of the Great North Mountain anticlinorium and includes several other regional folds. The North Mountain fault zone cuts through the eastern part of the quadrangle; it is a series of thrust faults generally oriented northeast-southwest that separate the Silurian and Devonian clastic rocks from the Cambrian and Ordovician carbonate rocks and shales. Karst development in the quadrangle occurs in all of the carbonate rocks. Springs occur mainly near or on faults. Sinkholes occur within all of the carbonate rock units, especially where the rocks have undergone locally intensified deformation through folding, faulting, or some combination.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20101265","usgsCitation":"Doctor, D.H., Orndorff, R.C., Parker, R., Weary, D.J., and Repetski, J.E., 2010, Geologic map of the White Hall quadrangle, Frederick County, Virginia, and Berkeley County, West Virginia: U.S. Geological Survey Open-File Report 2010-1265, 1 Plate: 46.00 × 42.00 inches; Downloads Directory, https://doi.org/10.3133/ofr20101265.","productDescription":"1 Plate: 46.00 × 42.00 inches; Downloads Directory","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":126115,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1265.gif"},{"id":398792,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_94646.htm"},{"id":14347,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1265/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","projection":"Polyconic projection","country":"United States","state":"Virginia, West Virginia","county":"Berkeley County, Frederick County","otherGeospatial":"White Hall quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.25,\n              39.25\n            ],\n            [\n              -78.125,\n              39.25\n            ],\n            [\n              -78.125,\n              39.375\n            ],\n            [\n              -78.25,\n              39.375\n            ],\n            [\n              -78.25,\n              39.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9e2","contributors":{"authors":[{"text":"Doctor, Daniel H. 0000-0002-8338-9722 dhdoctor@usgs.gov","orcid":"https://orcid.org/0000-0002-8338-9722","contributorId":2037,"corporation":false,"usgs":true,"family":"Doctor","given":"Daniel","email":"dhdoctor@usgs.gov","middleInitial":"H.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":306953,"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":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},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":306955,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parker, Ronald A.","contributorId":70350,"corporation":false,"usgs":true,"family":"Parker","given":"Ronald A.","affiliations":[],"preferred":false,"id":306956,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"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":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":306952,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Repetski, John E. 0000-0002-2298-7120 jrepetski@usgs.gov","orcid":"https://orcid.org/0000-0002-2298-7120","contributorId":2596,"corporation":false,"usgs":true,"family":"Repetski","given":"John","email":"jrepetski@usgs.gov","middleInitial":"E.","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":306954,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":98921,"text":"ofr20061260G - 2010 - Surficial geologic map of the Heath-Northfield-Southwick-Hampden 24-quadrangle area in the Connecticut Valley region, west-central Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:04:46","indexId":"ofr20061260G","displayToPublicDate":"2010-12-09T00:00:00","publicationYear":"2010","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":"2006-1260","chapter":"G","title":"Surficial geologic map of the Heath-Northfield-Southwick-Hampden 24-quadrangle area in the Connecticut Valley region, west-central Massachusetts","docAbstract":"The surficial geologic map layer shows the distribution of nonlithified earth materials at land surface in an area of 24 7.5-minute quadrangles (1,238 mi2 total) in west-central Massachusetts. Across Massachusetts, these materials range from a few feet to more than 500 ft in thickness. They overlie bedrock, which crops out in upland hills and as resistant ledges in valley areas. The geologic map differentiates surficial materials of Quaternary age on the basis of their lithologic characteristics (such as grain size and sedimentary structures), constructional geomorphic features, stratigraphic relationships, and age. Surficial materials also are known in engineering classifications as unconsolidated soils, which include coarse-grained soils, fine-grained soils, and organic fine-grained soils. Surficial materials underlie and are the parent materials of modern pedogenic soils, which have developed in them at the land surface. Surficial earth materials significantly affect human use of the land, and an accurate description of their distribution is particularly important for assessing water resources, construction aggregate resources, and earth-surface hazards, and for making land-use decisions. This work is part of a comprehensive study to produce a statewide digital map of the surficial geology at a 1:24,000-scale level of accuracy. This report includes explanatory text, quadrangle maps at 1:24,000 scale (PDF files), GIS data layers (ArcGIS shapefiles), metadata for the GIS layers, scanned topographic base maps (TIF), and a readme.txt file. \r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061260G","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Office of the State Geologist and Executive Office of Energy and Environmental Affairs\r\n\r\n","usgsCitation":"Stone, J.R., and DiGiacomo-Cohen, M.L., 2010, Surficial geologic map of the Heath-Northfield-Southwick-Hampden 24-quadrangle area in the Connecticut Valley region, west-central Massachusetts: U.S. Geological Survey Open-File Report 2006-1260, Text: iv, 14 p.; Appenix; Links to: Explanatory text; quadrangle maps; GIS data layers; metadata; scanned topographic base maps; readme.txt  , https://doi.org/10.3133/ofr20061260G.","productDescription":"Text: iv, 14 p.; Appenix; Links to: Explanatory text; quadrangle maps; GIS data layers; metadata; scanned topographic base maps; readme.txt  ","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":126771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2006_1260_g.jpg"},{"id":14343,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1260/G/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688f62","contributors":{"authors":[{"text":"Stone, Janet Radway jrstone@usgs.gov","contributorId":1695,"corporation":false,"usgs":true,"family":"Stone","given":"Janet","email":"jrstone@usgs.gov","middleInitial":"Radway","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":306943,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DiGiacomo-Cohen, Mary L.","contributorId":45253,"corporation":false,"usgs":true,"family":"DiGiacomo-Cohen","given":"Mary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":306944,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9000507,"text":"ofr20101300 - 2010 - Framework for ecological monitoring on lands of Alaska National Wildlife Refuges and their partners","interactions":[],"lastModifiedDate":"2017-12-11T11:52:09","indexId":"ofr20101300","displayToPublicDate":"2010-12-08T00:00:00","publicationYear":"2010","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":"2010-1300","title":"Framework for ecological monitoring on lands of Alaska National Wildlife Refuges and their partners","docAbstract":"<p>National Wildlife Refuges in Alaska and throughout the U.S. have begun developing a spatially comprehensive monitoring program to inform management decisions, and to provide data to broader research projects. In an era of unprecedented rates of climate change, monitoring is essential to detecting, understanding, communicating and mitigating climate-change effects on refuge and other resources under the protection of U.S. Fish and Wildlife Service, and requires monitoring results to address spatial scales broader than individual refuges. This document provides guidance for building a monitoring program for refuges in Alaska that meets refuge-specific management needs while also allowing synthesis and summary of ecological conditions at the ecoregional and statewide spatial scales.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101300","usgsCitation":"Woodward, A., and Beever, E.A., 2010, Framework for ecological monitoring on lands of Alaska National Wildlife Refuges and their partners: U.S. Geological Survey Open-File Report 2010-1300, vi, 52 p.; Appendices, https://doi.org/10.3133/ofr20101300.","productDescription":"vi, 52 p.; Appendices","numberOfPages":"94","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":126080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1300.bmp"},{"id":19171,"rank":200,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1300/","linkFileType":{"id":5,"text":"html"}},{"id":308123,"rank":201,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2010/1300/pdf/ofr20101300.pdf","text":"Report","size":"6 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-162.255031,54.978353],[-162.30058,54.832594],[-162.41737,54.877491],[-162.255031,54.978353]]],[[[-160.0179,55.15613],[-159.889174,55.287138],[-159.905365,55.164689],[-159.816419,55.178051],[-160.183466,54.91568],[-160.191392,55.108574],[-160.0179,55.15613]]],[[[-159.455311,55.061452],[-159.328791,54.980598],[-159.426615,54.942266],[-159.455311,55.061452]]],[[[-161.718614,55.154166],[-161.608634,55.116906],[-161.862504,55.127598],[-161.718614,55.154166]]],[[[-160.506927,55.32773],[-160.486174,55.193617],[-160.806009,55.12567],[-160.797147,55.381521],[-160.344369,55.362962],[-160.330722,55.261045],[-160.506927,55.32773]]],[[[-160.21178,55.455862],[-160.141834,55.387154],[-160.27997,55.395905],[-160.21178,55.455862]]],[[[-165.790523,54.171758],[-165.714198,54.120815],[-166.098255,54.103538],[-166.002465,54.213629],[-165.790523,54.171758]]],[[[-165.523466,54.299895],[-165.405377,54.212837],[-165.629725,54.132558],[-165.681458,54.236914],[-165.523466,54.299895]]],[[[-162.801865,54.48944],[-162.588883,54.450064],[-162.611891,54.368077],[-162.86005,54.425452],[-162.801865,54.48944]]],[[[-170.286318,57.128169],[-170.311707,57.219122],[-170.161647,57.229656],[-170.286318,57.128169]]],[[[178.785825,51.633434],[179.462765,51.376176],[178.634021,51.623981],[178.785825,51.633434]]],[[[-176.762478,51.867878],[-176.789558,51.957211],[-176.603598,51.997056],[-176.543309,51.838624],[-176.268243,51.785498],[-176.930952,51.59247],[-176.918065,51.788003],[-176.762478,51.867878]]],[[[-177.800647,51.778294],[-177.909185,51.596671],[-178.172666,51.839985],[-177.615311,51.85508],[-177.800647,51.778294]]],[[[-177.360408,51.727533],[-177.631523,51.696844],[-177.099266,51.936119],[-177.13096,51.762772],[-177.360408,51.727533]]],[[[177.601645,52.016377],[177.235523,51.87326],[177.661607,52.112746],[177.601645,52.016377]]],[[[179.758993,51.946595],[179.649484,51.87367],[179.482464,51.982834],[179.758993,51.946595]]],[[[-174.301818,52.278949],[-174.408277,52.289872],[-174.185347,52.417788],[-173.989415,52.325275],[-174.177679,52.233638],[-174.090169,52.139119],[-175.27485,52.018619],[-174.301818,52.278949]]],[[[-173.602446,52.153773],[-173.019588,52.097881],[-173.511915,52.031278],[-174.04675,52.122403],[-173.602446,52.153773]]],[[[173.587554,52.476785],[173.769503,52.512072],[173.725696,52.356579],[173.3955,52.402647],[173.587554,52.476785]]],[[[172.763366,52.823656],[172.469022,52.911337],[173.107249,52.993228],[173.421682,52.845477],[172.763366,52.823656]]],[[[-168.211705,53.256184],[-169.041338,52.839348],[-168.617143,53.260985],[-168.366519,53.252024],[-168.315847,53.481729],[-167.816998,53.517947],[-167.872879,53.36736],[-168.211705,53.256184]]],[[[-166.728918,54.003111],[-166.57509,53.879236],[-166.373689,54.01003],[-166.210964,53.933557],[-166.547438,53.749404],[-166.119922,53.855048],[-166.111317,53.776856],[-166.656234,53.487119],[-167.798984,53.284757],[-167.102305,53.515077],[-167.16164,53.605909],[-167.041245,53.707929],[-166.779991,53.719126],[-167.141966,53.826932],[-166.728918,54.003111]]],[[[-169.553937,56.608682],[-169.473138,56.601741],[-169.75575,56.591922],[-169.553937,56.608682]]],[[[-165.721389,60.16962],[-165.539367,59.965175],[-166.157071,59.748886],[-167.111785,59.989349],[-167.421489,60.205431],[-166.847438,60.213592],[-166.124379,60.414253],[-165.697326,60.297238],[-165.721389,60.16962]]],[[[-173.052751,60.515252],[-172.951862,60.605671],[-172.269754,60.333887],[-172.595895,60.318233],[-173.052751,60.515252]]],[[[-160.918586,58.746935],[-160.700627,58.817368],[-160.880515,58.581325],[-161.07563,58.549916],[-160.918586,58.746935]]],[[[-151.930565,60.51632],[-151.839194,60.485862],[-152.079995,60.341191],[-151.930565,60.51632]]],[[[-131.246018,54.989555],[-131.253671,54.866779],[-131.469097,54.913153],[-131.246018,54.989555]]],[[[-131.759896,55.381845],[-131.748334,55.128588],[-131.870568,55.364553],[-131.759896,55.381845]]],[[[-158.800682,55.891025],[-158.7036,55.841532],[-158.889198,55.810123],[-158.800682,55.891025]]],[[[-131.56956,55.284114],[-131.350575,55.067042],[-131.579882,55.017576],[-131.56956,55.284114]]],[[[-133.344847,55.569327],[-133.289854,55.50187],[-133.609073,55.241486],[-133.690174,55.304409],[-133.733029,55.558757],[-133.644202,55.470815],[-133.344847,55.569327]]],[[[-133.104304,55.426907],[-133.416549,55.739647],[-133.701152,55.78516],[-133.347915,55.803943],[-133.384089,55.87677],[-133.799931,55.925349],[-133.548802,56.14284],[-133.593728,56.352192],[-133.094977,56.250583],[-132.146062,55.470346],[-132.514798,55.576767],[-132.608786,55.486348],[-132.408317,55.512522],[-132.166857,55.363039],[-132.214912,55.2457],[-131.979818,55.211787],[-132.180334,55.015557],[-131.984592,55.027978],[-131.999591,54.731975],[-132.142277,54.691674],[-132.55839,54.932612],[-132.598675,55.150482],[-132.748854,54.996007],[-133.119294,55.251405],[-132.909706,54.923594],[-132.650001,54.904387],[-132.676226,54.680865],[-132.866355,54.700386],[-133.21042,55.040269],[-133.223791,55.229317],[-133.473593,55.255547],[-133.021557,55.366336],[-133.104304,55.426907]]],[[[-147.483828,60.618636],[-147.487635,60.728092],[-147.3087,60.665274],[-147.483828,60.618636]]],[[[-147.217704,60.293504],[-146.962633,60.311911],[-147.533041,59.852401],[-147.912883,59.79224],[-147.217704,60.293504]]],[[[-147.562801,60.579821],[-147.720124,60.202002],[-147.908985,60.224359],[-147.782548,60.4833],[-147.562801,60.579821]]],[[[-132.977163,56.439673],[-132.634335,56.422174],[-132.662081,56.274795],[-133.010587,56.309492],[-132.977163,56.439673]]],[[[-135.631777,58.380673],[-135.538502,58.337842],[-135.727908,58.365444],[-135.631777,58.380673]]],[[[-134.713987,58.220748],[-134.215981,58.162128],[-133.832895,57.635733],[-134.202353,57.90633],[-133.870327,57.381298],[-134.565687,57.023737],[-134.646773,57.226327],[-134.578511,57.400291],[-134.486023,57.372492],[-134.969189,58.367542],[-134.713987,58.220748]]],[[[-155.656727,55.860872],[-155.564404,55.809476],[-155.718593,55.772356],[-155.656727,55.860872]]],[[[-152.24289,58.241192],[-152.265111,58.135732],[-152.562829,58.177979],[-152.706831,58.050577],[-153.075746,58.099571],[-152.876788,58.002307],[-152.982406,57.984697],[-153.419783,58.059638],[-153.156402,58.090087],[-153.209672,58.15035],[-152.610955,58.475775],[-152.56771,58.621304],[-152.354709,58.63828],[-152.493991,58.354684],[-152.328063,58.434372],[-151.964103,58.269049],[-152.081083,58.154275],[-152.24289,58.241192]]],[[[-153.940505,56.558317],[-154.343096,56.510171],[-154.223759,56.612955],[-153.940505,56.558317]]],[[[-152.417424,57.815464],[-152.324284,57.824444],[-152.468172,57.600996],[-152.179531,57.624809],[-152.323683,57.467861],[-152.9663,57.51217],[-152.601148,57.382165],[-153.079288,57.32196],[-152.97091,57.282624],[-153.163333,57.216713],[-152.874839,57.16095],[-153.301142,56.991192],[-153.328206,57.141993],[-153.675981,57.06983],[-153.543429,56.995245],[-153.97178,56.744861],[-154.129017,56.742168],[-153.804787,57.113158],[-154.298965,56.846479],[-154.574343,57.239919],[-154.777368,57.280008],[-154.629678,57.510197],[-154.22566,57.661366],[-153.994572,57.656905],[-153.802932,57.350896],[-153.877756,57.629529],[-153.667261,57.639008],[-153.93522,57.813047],[-153.721176,57.890615],[-153.557647,57.734741],[-153.324872,57.831048],[-153.528697,57.921717],[-153.469421,57.977282],[-153.127278,57.856748],[-153.299009,57.985626],[-152.723425,57.99172],[-152.904312,57.750825],[-152.415177,57.973081],[-152.324103,57.916604],[-152.417424,57.815464]]],[[[-134.283312,55.925175],[-134.173104,55.918519],[-134.327238,55.83644],[-134.283312,55.925175]]],[[[-134.121514,56.069847],[-134.224073,56.065223],[-134.292353,56.352644],[-134.067466,56.390987],[-134.089604,56.472582],[-134.401407,56.725419],[-134.339168,56.90183],[-134.19095,56.861675],[-134.273113,56.933823],[-133.76778,56.780469],[-133.713331,56.598298],[-133.895746,56.511217],[-133.971228,56.083293],[-134.054411,56.224854],[-134.121514,56.069847]]],[[[-132.546463,56.606563],[-132.984751,56.51264],[-133.325392,56.791864],[-133.089388,56.535474],[-133.603669,56.435413],[-133.689996,56.839421],[-134.049218,57.029203],[-133.104611,57.005701],[-132.546463,56.606563]]],[[[-134.666587,56.169947],[-135.054049,56.527658],[-135.005249,56.602252],[-135.398678,56.779201],[-135.372021,57.228003],[-135.674687,57.336747],[-135.526036,57.509697],[-134.849477,57.40967],[-134.615955,56.637289],[-134.666587,56.169947]]],[[[-135.587961,57.89732],[-135.29156,57.737468],[-134.929726,57.759203],[-134.824891,57.500067],[-135.025148,57.454315],[-135.571606,57.674397],[-135.669416,57.389296],[-135.892131,57.408048],[-136.563223,58.035052],[-136.354836,58.192279],[-136.404805,58.267232],[-136.239246,58.171913],[-135.823562,58.282975],[-135.522646,58.185909],[-135.581753,57.997568],[-135.420107,58.144202],[-134.912854,57.979287],[-135.140674,57.926114],[-134.991819,57.835436],[-135.19896,57.775092],[-135.587961,57.89732]]],[[[-135.703464,57.32204],[-135.575722,57.104231],[-135.854131,56.995043],[-135.755997,57.121225],[-135.849974,57.265895],[-135.703464,57.32204]]],[[[-162.587754,63.275727],[-162.252411,63.541753],[-161.310181,63.471312],[-160.809089,63.731332],[-160.976038,64.235761],[-161.492926,64.407851],[-161.388621,64.532783],[-161.024185,64.499719],[-160.783398,64.71716],[-161.149655,64.911985],[-161.42986,64.759027],[-162.188146,64.672395],[-162.790167,64.325182],[-162.940776,64.542417],[-163.217757,64.632062],[-163.311983,64.58828],[-163.033231,64.519314],[-163.175336,64.399334],[-163.597834,64.563356],[-165.001961,64.433917],[-166.189546,64.575798],[-166.451788,64.691761],[-166.410198,64.827968],[-166.530518,64.937114],[-166.911922,65.125965],[-166.521506,65.149242],[-166.439404,65.319058],[-167.398458,65.400259],[-168.127044,65.626584],[-165.80503,66.33331],[-164.400727,66.58111],[-163.754171,66.551284],[-163.904813,66.230303],[-164.046937,66.209404],[-163.623921,66.058281],[-161.838018,66.022582],[-161.548429,66.239912],[-161.067871,66.235164],[-161.360743,66.375943],[-161.912946,66.344436],[-161.87488,66.511446],[-162.501415,66.742503],[-162.601052,66.898455],[-162.271769,66.904144],[-162.013623,66.779406],[-162.033156,66.631585],[-161.624334,66.450143],[-161.326349,66.478371],[-161.86618,66.704978],[-161.719587,66.916898],[-161.485121,66.945647],[-161.62216,67.008146],[-163.69887,67.114443],[-163.878781,67.416125],[-164.209816,67.639079],[-166.784578,68.340431],[-166.305962,68.46154],[-166.222496,68.860441],[-163.973678,68.985044],[-163.137614,69.352178],[-163.016456,69.538142],[-163.118176,69.589156],[-162.916958,69.692512],[-163.010545,69.728109],[-161.922949,70.291599],[-160.839536,70.344534],[-159.209082,70.870067],[-159.132483,70.828359],[-159.290577,70.811262],[-159.13779,70.758609],[-157.768452,70.875842],[-156.56865,71.352561],[-155.513987,71.096794],[-155.95205,70.964831],[-155.969194,70.827982],[-155.543031,70.847175],[-155.03174,71.146473],[-154.61605,71.026182],[-154.577386,70.835335],[-154.181863,70.768325],[-153.23848,70.922467],[-152.259966,70.84282],[-152.187197,70.801546],[-152.471531,70.68884],[-152.433781,70.616926],[-151.695162,70.549675],[-151.91921,70.472686],[-151.844375,70.434959],[-149.461755,70.518271],[-147.681722,70.199954],[-145.842689,70.164102],[-144.902304,69.96451],[-143.574986,70.154598],[-142.746807,70.042531],[-141.377718,69.634631],[-141.002672,69.645609],[-141.00184,60.306105],[-139.989142,60.18524],[-139.738924,60.31842],[-139.086669,60.357654],[-139.200346,60.090701],[-137.604277,59.243057],[-137.526424,58.906834],[-136.581521,59.164909],[-136.474326,59.464194],[-136.234229,59.524731],[-136.256889,59.623646],[-135.477436,59.799626],[-135.254125,59.701339],[-135.027456,59.563692],[-134.961972,59.280376],[-134.702383,59.247836],[-134.250526,58.858046],[-133.379908,58.427909],[-133.461475,58.385526],[-132.29792,57.269469],[-132.371312,57.095229],[-132.051044,57.051155],[-132.080262,56.850926],[-131.9301,56.835211],[-131.849898,56.661227],[-130.102761,56.116696],[-130.023189,55.930665],[-130.150595,55.767031],[-129.982348,55.302079],[-130.409764,54.881192],[-130.854966,54.766341],[-131.093806,55.191335],[-130.925069,55.300713],[-130.901872,55.69738],[-131.093956,55.895675],[-131.243491,55.973689],[-130.94683,55.650716],[-130.959772,55.315892],[-131.000594,55.398012],[-131.160492,55.197481],[-131.263089,55.208318],[-131.191595,55.360527],[-131.402931,55.238065],[-131.828446,55.445214],[-131.664629,55.581525],[-131.713742,55.853263],[-131.828176,55.877284],[-131.936689,55.535151],[-132.183207,55.588128],[-132.283594,55.761774],[-132.067412,55.875078],[-131.943402,56.192557],[-132.320487,55.887648],[-132.708697,56.112124],[-132.543076,56.332276],[-132.382793,56.299203],[-132.394268,56.485579],[-132.204367,56.372086],[-132.371589,56.672473],[-132.528446,56.702056],[-132.432385,56.782385],[-132.770404,56.837486],[-132.91197,56.966651],[-132.813684,57.030218],[-133.466932,57.159356],[-133.489738,57.305192],[-133.287052,57.30292],[-133.475998,57.380394],[-133.478086,57.56173],[-133.66439,57.611707],[-133.65855,57.707924],[-133.234598,57.608749],[-134.049603,58.062027],[-134.087674,58.181952],[-134.631203,58.247446],[-135.368331,59.263275],[-135.295084,59.08761],[-135.38931,58.990528],[-135.142322,58.61637],[-135.056227,58.189884],[-135.433061,58.399899],[-135.90731,58.380839],[-136.120307,58.968418],[-136.150772,58.757266],[-136.247343,58.752935],[-136.877826,58.962392],[-136.928643,58.900131],[-136.463258,58.781607],[-136.422309,58.647412],[-136.246368,58.663185],[-136.041818,58.380161],[-136.70125,58.219416],[-137.608804,58.601234],[-138.131,59.002613],[-139.855565,59.53666],[-139.51818,59.687814],[-139.625896,59.904084],[-139.486032,60.012407],[-140.272266,59.700609],[-141.423134,59.877329],[-141.299609,59.937397],[-141.384318,60.071598],[-141.73624,59.961905],[-142.698419,60.093333],[-144.035037,60.020202],[-144.59088,59.795581],[-144.052539,60.041759],[-144.892815,60.292821],[-144.964135,60.444466],[-145.113885,60.300978],[-145.9469,60.455395],[-145.712891,60.583249],[-146.689523,60.271279],[-146.637783,60.467178],[-145.795141,60.601121],[-145.841742,60.685893],[-146.253471,60.622315],[-146.101458,60.719277],[-146.191553,60.73199],[-146.668151,60.692761],[-146.183555,60.846969],[-146.262969,60.867787],[-146.801009,60.80516],[-146.653827,61.047752],[-146.262451,61.090246],[-146.613659,61.118799],[-147.378483,60.877845],[-147.525453,60.896057],[-147.514173,61.096127],[-147.66899,60.841563],[-148.134384,60.791268],[-147.715826,61.249669],[-148.426951,60.827113],[-148.384491,60.687754],[-148.148059,60.758536],[-148.091712,60.676249],[-148.30652,60.550702],[-148.115163,60.596029],[-147.942106,60.444029],[-148.025994,60.279029],[-148.171278,60.335266],[-148.362497,60.221849],[-147.913221,60.132576],[-148.016432,59.999344],[-147.848469,60.078962],[-147.917935,59.985997],[-148.225235,59.950195],[-148.148011,59.994952],[-148.274241,60.013318],[-148.293213,60.151289],[-148.401601,59.9976],[-149.133115,60.044918],[-149.287588,59.906506],[-149.341584,60.076762],[-149.584254,59.866905],[-149.526358,59.703258],[-149.666147,59.850527],[-149.746364,59.860881],[-149.74622,59.637585],[-150.028296,59.788652],[-149.928962,59.723245],[-150.392481,59.387265],[-150.316945,59.585285],[-150.478742,59.458498],[-150.547729,59.590331],[-150.942212,59.233136],[-151.915684,59.227522],[-151.991618,59.313617],[-151.826047,59.439049],[-151.272459,59.555823],[-150.927312,59.793431],[-151.503822,59.633662],[-151.829137,59.720151],[-151.71801,60.009473],[-151.30609,60.387257],[-151.40927,60.720558],[-150.353702,61.031822],[-150.217179,60.930001],[-149.111617,60.878949],[-150.039304,61.144291],[-149.429513,61.447165],[-149.542776,61.489995],[-149.919682,61.26347],[-150.646221,61.296689],[-151.783271,60.868713],[-151.702833,60.727778],[-151.860179,60.753282],[-152.309221,60.506384],[-152.234199,60.393888],[-152.715881,60.241274],[-152.596784,60.101071],[-152.745083,59.904232],[-153.225937,59.858343],[-153.021945,59.834133],[-153.214156,59.634271],[-153.366613,59.633729],[-153.439977,59.784652],[-153.577828,59.555991],[-154.087803,59.367967],[-154.260121,59.14302],[-153.254798,58.861756],[-153.445002,58.70931],[-153.851432,58.611872],[-154.291163,58.13568],[-154.990431,58.013424],[-155.37861,57.710766],[-155.617188,57.769715],[-155.731412,57.555546],[-156.044031,57.564455],[-156.036722,57.470941],[-156.481632,57.338705],[-156.551239,57.2908],[-156.336427,57.336081],[-156.355401,57.159679],[-156.5472,56.986488],[-157.201724,56.767511],[-157.45759,56.848204],[-157.536486,56.615317],[-158.042012,56.596744],[-157.859766,56.483668],[-158.402954,56.455193],[-158.498837,56.38011],[-158.112718,56.240286],[-158.475258,56.093405],[-158.417889,56.036796],[-158.575042,56.121129],[-158.737009,55.953313],[-159.472801,55.83905],[-159.696713,55.573306],[-159.627482,55.803248],[-159.81107,55.85657],[-160.410823,55.66538],[-160.481633,55.489068],[-160.909625,55.52414],[-161.231535,55.357452],[-161.445196,55.368103],[-161.376102,55.569794],[-161.587047,55.62006],[-161.878076,55.223599],[-162.041236,55.236806],[-162.053281,55.074212],[-162.489735,55.064849],[-162.4168,55.104096],[-162.584872,55.298386],[-162.692309,55.197313],[-162.569289,54.97124],[-162.881639,54.934785],[-163.165036,55.099214],[-163.226313,55.042694],[-163.067008,54.979302],[-163.373207,54.800841],[-163.057228,54.688101],[-163.344791,54.751211],[-163.572383,54.623211],[-164.179617,54.599188],[-164.41682,54.431713],[-164.844931,54.417583],[-164.949781,54.575697],[-164.48678,54.922441],[-163.568159,55.049145],[-163.318885,54.88012],[-163.268767,55.145465],[-162.86152,55.198339],[-161.816225,55.888993],[-160.898682,55.999014],[-160.814205,55.953834],[-160.940845,55.822529],[-160.806014,55.738241],[-160.668102,55.723556],[-160.769155,55.858268],[-160.293924,55.765556],[-160.273176,55.856881],[-160.534541,55.989498],[-160.357156,56.279582],[-158.957471,56.851184],[-158.660298,56.789015],[-158.659945,57.034585],[-158.376249,57.265542],[-157.786046,57.542189],[-157.573472,57.522732],[-157.703782,57.721768],[-157.596601,58.08867],[-157.39735,58.173383],[-157.524477,58.414506],[-156.980888,58.891031],[-158.190283,58.61371],[-158.512547,58.78311],[-158.487015,58.999872],[-158.179588,59.012245],[-158.522231,59.021763],[-158.789632,58.814257],[-158.827852,58.626432],[-158.704052,58.482759],[-158.880927,58.39067],[-159.657362,58.938712],[-159.908386,58.779903],[-160.322922,58.953953],[-160.31778,59.070477],[-161.751999,58.551842],[-162.171722,58.648441],[-161.769501,58.774937],[-161.828171,59.062702],[-162.048584,59.254177],[-161.738312,59.46701],[-162.453176,60.27854],[-162.1724,60.624038],[-162.571198,60.25189],[-162.453176,60.197639],[-162.503647,59.99923],[-163.349027,59.81989],[-164.079837,59.828034],[-164.1916,60.024496],[-165.129403,60.433707],[-164.961439,60.508391],[-165.362975,60.506866],[-164.97125,60.711434],[-164.945958,60.92106],[-165.132488,60.850145],[-165.194945,60.9739],[-164.87045,61.079564],[-165.2897,61.181714],[-165.403007,61.06706],[-165.578127,61.100361],[-165.662892,61.29457],[-165.921194,61.40308],[-165.767226,61.45695],[-165.807627,61.529171],[-166.165232,61.550618],[-166.158976,61.700437],[-165.82214,61.67061],[-166.092081,61.800733],[-165.640216,61.848041],[-165.706155,62.108365],[-164.837703,62.685267],[-164.783858,62.946154],[-164.493118,63.17767],[-164.066991,63.262276],[-163.316203,63.037763],[-162.587754,63.275727]]],[[[-169.267598,63.343995],[-168.692939,63.302282],[-168.818344,63.163224],[-169.396308,63.136617],[-169.638309,62.937527],[-170.512102,63.341881],[-171.067663,63.424579],[-171.433319,63.307578],[-171.849984,63.485039],[-171.699647,63.781728],[-170.950817,63.570127],[-170.281988,63.68502],[-169.974858,63.470618],[-169.267598,63.343995]]],[[[-162.614621,63.621832],[-162.341892,63.594062],[-162.676581,63.555648],[-162.614621,63.621832]]]]},\"properties\":{\"name\":\"Alaska\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b44a7","contributors":{"authors":[{"text":"Woodward, Andrea 0000-0003-0604-9115 awoodward@usgs.gov","orcid":"https://orcid.org/0000-0003-0604-9115","contributorId":3028,"corporation":false,"usgs":true,"family":"Woodward","given":"Andrea","email":"awoodward@usgs.gov","affiliations":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true},{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":572327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beever, Erik A. 0000-0002-9369-486X ebeever@usgs.gov","orcid":"https://orcid.org/0000-0002-9369-486X","contributorId":2934,"corporation":false,"usgs":true,"family":"Beever","given":"Erik","email":"ebeever@usgs.gov","middleInitial":"A.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":572328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9000497,"text":"ofr20101203 - 2010 - Potentiometric Surface of the Magothy Aquifer in Southern Maryland, September 2009","interactions":[],"lastModifiedDate":"2012-03-08T17:16:39","indexId":"ofr20101203","displayToPublicDate":"2010-12-07T00:00:00","publicationYear":"2010","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":"2010-1203","title":"Potentiometric Surface of the Magothy Aquifer in Southern Maryland, September 2009","docAbstract":"This report presents a map showing the potentiometric surface of the Magothy aquifer in the Magothy Formation of Late Cretaceous age in Southern Maryland during September 2009. The map is based on water-level measurements in 66 wells. The highest measured water level was 85 feet above sea level near the northern boundary and outcrop area of the aquifer in the north-central part of Anne Arundel County. The potentiometric surface declined towards the south. Local hydraulic gradients were directed toward the center of a cone of depression in the Waldorf area that developed in response to pumping. Measured groundwater levels were as low as 71 feet below sea level in the Waldorf area. The map also shows well yield in gallons per day for 2008 at wells or well fields.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101203","collaboration":"Prepared in cooperation with the Maryland Gological Survey (MGS) and the Power Plant Assessment Program, Maryland Department of Natural Resources","usgsCitation":"Curtin, S.E., Andreasen, D., and Staley, A., 2010, Potentiometric Surface of the Magothy Aquifer in Southern Maryland, September 2009: U.S. Geological Survey Open-File Report 2010-1203, Map; 1 Sheet; 8.50 x 11.00 inches, https://doi.org/10.3133/ofr20101203.","productDescription":"Map; 1 Sheet; 8.50 x 11.00 inches","numberOfPages":"2","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"links":[{"id":116240,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1203.bmp"},{"id":14430,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1203/","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.5,38 ], [ -77.5,39.5 ], [ -75.75,39.5 ], [ -75.75,38 ], [ -77.5,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bfdc","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":344127,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":344129,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Staley, Andrew W.","contributorId":43319,"corporation":false,"usgs":true,"family":"Staley","given":"Andrew W.","affiliations":[],"preferred":false,"id":344128,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9000496,"text":"ofr20101207 - 2010 - Potentiometric Surface of the Lower Patapsco Aquifer in Southern Maryland, September 2009","interactions":[],"lastModifiedDate":"2012-03-08T17:16:13","indexId":"ofr20101207","displayToPublicDate":"2010-12-07T00:00:00","publicationYear":"2010","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":"2010-1207","title":"Potentiometric Surface of the Lower Patapsco Aquifer in Southern Maryland, September 2009","docAbstract":"This report presents a map showing the potentiometric surface of the lower Patapsco aquifer in the Patapsco Formation of Early Cretaceous age in Southern Maryland during September 2009. The map is based on water-level measurements in 64 wells. The highest measured water level was 110 feet above sea level near the northwestern boundary and outcrop area of the aquifer in northern Prince George's County. From this area, the potentiometric surface declined towards well fields at Severndale, Broad Creek, and Arnold. The measured groundwater levels were 99 feet below sea level at Severndale, 50 feet below sea level at Broad Creek, and 36 feet below sea level at Arnold. There was also a cone of depression in Charles County that includes Waldorf, La Plata, Indian Head, and the Morgantown power plant. The groundwater levels measured were as low as 215 feet below sea level at Waldorf, 149 feet below sea level at La Plata, 121 feet below sea level at Indian Head, and 96 feet below sea level at the Morgantown power plant. The map also shows well yield in gallons per day for 2008 at wells or well fields.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101207","collaboration":"Prepared in cooperation with the Maryland Geological Survey and the\r\nMaryland Department of Natural Resources","usgsCitation":"Curtin, S.E., Andreasin, D.C., and Staley, A., 2010, Potentiometric Surface of the Lower Patapsco Aquifer in Southern Maryland, September 2009: U.S. Geological Survey Open-File Report 2010-1207, Map; 1 Sheet 8.50 x 11.00 inches, https://doi.org/10.3133/ofr20101207.","productDescription":"Map; 1 Sheet 8.50 x 11.00 inches","numberOfPages":"2","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2009-09-01","temporalEnd":"2009-09-30","costCenters":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"links":[{"id":126168,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1207.gif"},{"id":14386,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1207/","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.41666666666667,38.1175 ], [ -77.41666666666667,39.5 ], [ -75.83333333333333,39.5 ], [ -75.83333333333333,38.1175 ], [ -77.41666666666667,38.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db6832c6","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":344124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasin, David C.","contributorId":89498,"corporation":false,"usgs":true,"family":"Andreasin","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":344126,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Staley, Andrew W.","contributorId":43319,"corporation":false,"usgs":true,"family":"Staley","given":"Andrew W.","affiliations":[],"preferred":false,"id":344125,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9000501,"text":"ofr20101209 - 2010 - Potentiometric Surface of the Patuxent Aquifer in Southern Maryland, September 2009","interactions":[],"lastModifiedDate":"2012-03-08T17:16:14","indexId":"ofr20101209","displayToPublicDate":"2010-12-07T00:00:00","publicationYear":"2010","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":"2010-1209","title":"Potentiometric Surface of the Patuxent Aquifer in Southern Maryland, September 2009","docAbstract":"This report presents a map showing the potentiometric surface of the Patuxent aquifer in the Patuxent Formation of Early Cretaceous age in Southern Maryland during September 2009. The map is based on water-level measurements in 42 wells. The highest measured water level was 169 feet above sea level in the outcrop area of the aquifer in northern Prince George's County. From this area, the potentiometric surface declined south towards well fields at Glen Burnie, Bryans Road, the Morgantown power plant, and the Chalk Point power plant. The measured groundwater levels were 78 feet below sea level at Glen Burnie, 56 feet below sea level at Bryans Road, 29 feet below sea level at the Morgantown power plant, and 28 feet below sea level at the Chalk Point power plant. The map also shows well yield in gallons per day for 2008 at wells or well fields.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101209","collaboration":"Prepared in cooperation with the Maryland Geological Survey and the\r\nMaryland Department of Natural Resources","usgsCitation":"Curtin, S.E., Andreasen, D., and Staley, A., 2010, Potentiometric Surface of the Patuxent Aquifer in Southern Maryland, September 2009: U.S. Geological Survey Open-File Report 2010-1209, Map; 1 Sheet , https://doi.org/10.3133/ofr20101209.","productDescription":"Map; 1 Sheet ","numberOfPages":"2","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2009-09-01","temporalEnd":"2009-09-30","costCenters":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"links":[{"id":126170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1209.gif"},{"id":14387,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1209/","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.41666666666667,38.1175 ], [ -77.41666666666667,39.5 ], [ -75.83333333333333,39.5 ], [ -75.83333333333333,38.1175 ], [ -77.41666666666667,38.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683205","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":344136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":344138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Staley, Andrew W.","contributorId":43319,"corporation":false,"usgs":true,"family":"Staley","given":"Andrew W.","affiliations":[],"preferred":false,"id":344137,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9000505,"text":"ofr20101202 - 2010 - The Difference Between the Potentiometric Surfaces of the Aquia Aquifer in Southern Maryland, September 1982 and September 2009","interactions":[],"lastModifiedDate":"2012-03-08T17:16:39","indexId":"ofr20101202","displayToPublicDate":"2010-12-07T00:00:00","publicationYear":"2010","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":"2010-1202","title":"The Difference Between the Potentiometric Surfaces of the Aquia Aquifer in Southern Maryland, September 1982 and September 2009","docAbstract":"This report presents a map showing the change in the potentiometric surface of the Aquia aquifer in the Aquia Formation of Paleocene age in Southern Maryland between September 1982 and September 2009. The map, based on water level differences obtained from 49 wells, shows that the potentiometric surface during the 27-year period declined from zero in the northernmost part of the study area, which is the outcrop of the aquifer, to 111 feet at Lexington Park. Lexington Park is near the southeasternmost part of the study area and approaches the downdip boundary of the aquifer. The map also shows well yield in gallons per day for 2008 at wells or well fields.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101202","collaboration":"Prepared in cooperation with the Maryland Geological Survey (MGS) and the Power Plant Assessment Program, Maryland Department of Natural Resources","usgsCitation":"Curtin, S.E., Andreasen, D., and Staley, A., 2010, The Difference Between the Potentiometric Surfaces of the Aquia Aquifer in Southern Maryland, September 1982 and September 2009: U.S. Geological Survey Open-File Report 2010-1202, Map; 1 Sheet; 8.50 x 11.00 inches, https://doi.org/10.3133/ofr20101202.","productDescription":"Map; 1 Sheet; 8.50 x 11.00 inches","numberOfPages":"2","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"links":[{"id":116239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1202.bmp"},{"id":14431,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1202/","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.5,38 ], [ -77.5,39.5 ], [ -75.75,39.5 ], [ -75.75,38 ], [ -77.5,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e665","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":344151,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":344153,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Staley, Andrew W.","contributorId":43319,"corporation":false,"usgs":true,"family":"Staley","given":"Andrew W.","affiliations":[],"preferred":false,"id":344152,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9000502,"text":"ofr20101206 - 2010 - The difference between the potentiometric surfaces of the Upper Patapsco aquifer in southern Maryland, September 1990 and September 2009","interactions":[],"lastModifiedDate":"2012-03-08T17:16:39","indexId":"ofr20101206","displayToPublicDate":"2010-12-07T00:00:00","publicationYear":"2010","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":"2010-1206","title":"The difference between the potentiometric surfaces of the Upper Patapsco aquifer in southern Maryland, September 1990 and September 2009","docAbstract":"This report presents a map showing the change in the potentiometric surface of the upper Patapsco aquifer in the Patapsco Formation of Early Cretaceous age in Southern Maryland between September 1990 and September 2009. The map, based on water level differences obtained from 33 wells, shows that during the 19-year period, the change in the potentiometric surface ranged from zero at the edge of the outcrop area in northern Anne Arundel County to a decline of 20 feet at Broad Creek, 16 feet near Arnold, 32 feet at Waldorf, 37 feet at the Chalk Point power plant, and 43 feet at Lexington Park. The map also shows well yield in gallons per day for 2008 at wells or well fields.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101206","collaboration":"Prepared in cooperation with the Maryland Geological Survey and the Maryland Department of Natural Resources","usgsCitation":"Curtin, S.E., Andreasen, D., and Staley, A., 2010, The difference between the potentiometric surfaces of the Upper Patapsco aquifer in southern Maryland, September 1990 and September 2009: U.S. Geological Survey Open-File Report 2010-1206, 1 p., https://doi.org/10.3133/ofr20101206.","productDescription":"1 p.","numberOfPages":"2","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1990-09-01","temporalEnd":"2009-09-30","costCenters":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"links":[{"id":126779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1206.gif"},{"id":14421,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1206/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.5,38 ], [ -77.5,39.5 ], [ -75.83333333333333,39.5 ], [ -75.83333333333333,38 ], [ -77.5,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6684e4","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":344139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":344141,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Staley, Andrew W.","contributorId":43319,"corporation":false,"usgs":true,"family":"Staley","given":"Andrew W.","affiliations":[],"preferred":false,"id":344140,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9000506,"text":"ofr20101204 - 2010 - The Difference Between the Potentiometric Surfaces of the Magothy Aquifer in Southern Maryland, September 1975 and September 2009","interactions":[],"lastModifiedDate":"2012-03-08T17:16:39","indexId":"ofr20101204","displayToPublicDate":"2010-12-07T00:00:00","publicationYear":"2010","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":"2010-1204","title":"The Difference Between the Potentiometric Surfaces of the Magothy Aquifer in Southern Maryland, September 1975 and September 2009","docAbstract":"This report presents a map showing the change in the potentiometric surface of the Magothy aquifer in the Magothy Formation of Late Cretaceous age in Southern Maryland between September 1975 and September 2009. The map, based on water level differences obtained from 48 wells, shows that during the 34-year period, the potentiometric surface had little change at the outcrop area, which is in the northernmost part of the study area, but declined 75 feet at Waldorf. Waldorf is located near the southwesternmost part of the study area, and approaches the downdip boundary of the aquifer. The map also shows well yield in gallons per day for 2008 at wells or well fields.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20101204","collaboration":"Prepared in cooperation with the Maryland Geological Survey (MGS) and the Power Plant Assessment Program, Maryland Department of Natural Resources","usgsCitation":"Curtin, S.E., Andreasen, D., and Staley, A., 2010, The Difference Between the Potentiometric Surfaces of the Magothy Aquifer in Southern Maryland, September 1975 and September 2009: U.S. Geological Survey Open-File Report 2010-1204, Map; 1 Sheet; 8.50 x 11.00 inches, https://doi.org/10.3133/ofr20101204.","productDescription":"Map; 1 Sheet; 8.50 x 11.00 inches","numberOfPages":"2","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"links":[{"id":116263,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2010_1204.bmp"},{"id":14432,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2010/1204/","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.5,38 ], [ -77.5,39.5 ], [ -75.75,39.5 ], [ -75.75,38 ], [ -77.5,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e64a","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":344154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":344156,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Staley, Andrew W.","contributorId":43319,"corporation":false,"usgs":true,"family":"Staley","given":"Andrew W.","affiliations":[],"preferred":false,"id":344155,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}