{"pageNumber":"804","pageRowStart":"20075","pageSize":"25","recordCount":46714,"records":[{"id":70208460,"text":"70208460 - 2008 - Mass balance of a cirque glacier in the U.S. Rocky Mountains ","interactions":[],"lastModifiedDate":"2020-02-10T17:05:15","indexId":"70208460","displayToPublicDate":"2008-12-31T16:42:56","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Mass balance of a cirque glacier in the U.S. Rocky Mountains ","docAbstract":"<p>Glacier National Park, Montana, USA, contains 27 cirque glaciers, most less than 1 km<sup>2</sup> and together comprising about 17 km<sup>2</sup>. These glaciers lie at relatively low elevation (2000 – 3000 m a.s.l.) and latitude (48<sup>o</sup> N) and have undergone dramatic retreat since the mid-nineteenth century, when an estimated 150 glaciers existed. Continuing volume losses and the disappearance of glaciers in recent decades are used as key indicators of regional warming. Here we present initial results from a long-term study initiated in 2005 on Sperry Glacier (48.6<sup>o</sup>N, 113.75<sup>o</sup>W), a 0.8 km<sup>2</sup> cirque glacier that has undergone an 80% reduction in size since the mid 1800s. We calculated seasonal and annual balances using the direct glaciological method augmented with data from an automated weather station adjacent to the glacier and data from a nearby automated snow pillow. The net annual balance averaged -1.0 m w. eq. for the 2005 and 2006 balance years. Specific balances showed significant transverse spatial variability due to site-specific processes that augment accumulation or mute ablation. These processes have a significant effect on the mass balance of the glacier. Proxy measures showed that the 2005 and 2006 balance years likely had very low accumulation or very high ablation, respectively, relative to other years in recent decades. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the Mass Balance Measurement and Modelling Workshop","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"International Workshop on Glacier Mass Balance Measurements and Modelling","conferenceDate":"March 26-29, 2008","conferenceLocation":"Skeikampen, Norway","language":"English","publisher":"International Glaciological Society","usgsCitation":"Reardon, B.A., Harper, J.T., and Fagre, D.B., 2008, Mass balance of a cirque glacier in the U.S. Rocky Mountains , <i>in</i> Proceedings of the Mass Balance Measurement and Modelling Workshop, Skeikampen, Norway, March 26-29, 2008, 5 p.","productDescription":"5 p.","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":372200,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Glacier National Park, Sperry Glacier","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.75553131103516,\n              48.615945299728885\n            ],\n            [\n              -113.74960899353027,\n              48.62451275552683\n            ],\n            [\n              -113.74875068664551,\n              48.631547194784\n            ],\n            [\n              -113.75741958618164,\n              48.633475821350466\n            ],\n            [\n              -113.76093864440918,\n              48.629334855883336\n            ],\n            [\n              -113.76651763916016,\n              48.627859909394665\n            ],\n            [\n              -113.76866340637207,\n              48.62411562084454\n            ],\n            [\n              -113.76291275024414,\n              48.62020084032983\n            ],\n            [\n              -113.76608848571777,\n              48.61725037031813\n            ],\n            [\n              -113.7655735015869,\n              48.61583181373538\n            ],\n            [\n              -113.76205444335938,\n              48.6163424986971\n            ],\n            [\n              -113.75553131103516,\n              48.615945299728885\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Reardon, Blase A.","contributorId":178872,"corporation":false,"usgs":false,"family":"Reardon","given":"Blase","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":781980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harper, J. T.","contributorId":199751,"corporation":false,"usgs":false,"family":"Harper","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":781981,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fagre, Daniel B. 0000-0001-8552-9461 dan_fagre@usgs.gov","orcid":"https://orcid.org/0000-0001-8552-9461","contributorId":2036,"corporation":false,"usgs":true,"family":"Fagre","given":"Daniel","email":"dan_fagre@usgs.gov","middleInitial":"B.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":781982,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70217350,"text":"70217350 - 2008 - Experimental and field observations of breach dynamics accompanying erosion of Marmot Cofferdam, Sandy River, Oregon","interactions":[],"lastModifiedDate":"2021-01-19T16:05:39.909677","indexId":"70217350","displayToPublicDate":"2008-12-31T09:41:23","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Experimental and field observations of breach dynamics accompanying erosion of Marmot Cofferdam, Sandy River, Oregon","docAbstract":"<p><span>A key issue faced in dam removal is the rate and timing of remobilization and discharge of stored reservoir sediments following the removal. Different removal strategies can result in different trajectories of upstream sediment transport and knickpoint migration. We examine this issue of for the Marmot Dam removal in Sandy River, Oregon, USA using both physical experiments and field studies accompanying removal of the dam in October 2007. The physical experiment was designed to provide insights on how and if the position of a cofferdam notch will affect how reservoir sediments are remobilized, with the goal of minimizing the volume of sediment stranded in terraces. Data and observations indicate that at lower failure discharges, notch position impacts the location of cofferdam failure as well as the location of the first major knickpoint and its trajectory. In particular, notch positions that force the river to migrate laterally in order to adjust to natural valley orientation and morphology were most effective in removing larger volumes of sediment and reducing terrace heights. Actual cofferdam notching to maximize erosion produced extremely rapid and significant erosion of reservoir sediments. Comparison of model results with field observations suggests that the physical experiments provided solid predictions of rates of erosion and overall knickpoint trajectory.</span></p>","language":"English","publisher":"American Society of Civil Engineers","usgsCitation":"Grant, G.E., Marr, J.D., Hill, C., Johnson, S., Campbell, K., Mohseni, O., Wallick, J., Lewis, S., O’connor, E.A., and Major, J.J., 2008, Experimental and field observations of breach dynamics accompanying erosion of Marmot Cofferdam, Sandy River, Oregon, v. 2008, 10 p.","productDescription":"10 p.","costCenters":[],"links":[{"id":382292,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2008","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Grant, G. E.","contributorId":247843,"corporation":false,"usgs":false,"family":"Grant","given":"G.","email":"","middleInitial":"E.","affiliations":[{"id":527,"text":"Pacific Northwest Research Station","active":false,"usgs":true}],"preferred":false,"id":808465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marr, Jeffrey D. G.","contributorId":80791,"corporation":false,"usgs":false,"family":"Marr","given":"Jeffrey","email":"","middleInitial":"D. G.","affiliations":[{"id":47665,"text":"St. Anthony Falls Laboratory, University of Minnesota, Minneapolis, MN, USA","active":true,"usgs":false}],"preferred":false,"id":808466,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hill, C.","contributorId":88801,"corporation":false,"usgs":true,"family":"Hill","given":"C.","email":"","affiliations":[{"id":47665,"text":"St. Anthony Falls Laboratory, University of Minnesota, Minneapolis, MN, USA","active":true,"usgs":false}],"preferred":false,"id":808467,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, S.","contributorId":215645,"corporation":false,"usgs":false,"family":"Johnson","given":"S.","affiliations":[{"id":47665,"text":"St. Anthony Falls Laboratory, University of Minnesota, Minneapolis, MN, USA","active":true,"usgs":false}],"preferred":false,"id":808472,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Campbell, K.","contributorId":63351,"corporation":false,"usgs":false,"family":"Campbell","given":"K.","affiliations":[{"id":47665,"text":"St. Anthony Falls Laboratory, University of Minnesota, Minneapolis, MN, USA","active":true,"usgs":false}],"preferred":false,"id":808473,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mohseni, O.","contributorId":247846,"corporation":false,"usgs":false,"family":"Mohseni","given":"O.","email":"","affiliations":[{"id":47665,"text":"St. Anthony Falls Laboratory, University of Minnesota, Minneapolis, MN, USA","active":true,"usgs":false}],"preferred":false,"id":808474,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wallick, J.R.","contributorId":247847,"corporation":false,"usgs":false,"family":"Wallick","given":"J.R.","email":"","affiliations":[{"id":157,"text":"Cascades Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":808475,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lewis, S.L.","contributorId":7932,"corporation":false,"usgs":true,"family":"Lewis","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":808469,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"O’connor, E. A.","contributorId":88160,"corporation":false,"usgs":true,"family":"O’connor","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":808470,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Major, Jon J. 0000-0003-2449-4466 jjmajor@usgs.gov","orcid":"https://orcid.org/0000-0003-2449-4466","contributorId":439,"corporation":false,"usgs":true,"family":"Major","given":"Jon","email":"jjmajor@usgs.gov","middleInitial":"J.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":808471,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70206561,"text":"70206561 - 2008 - Spatial and temporal trends in nitrate concentrations in the eastern San Joaquin Valley regional aquifer and implications for fertilizer management","interactions":[],"lastModifiedDate":"2019-11-12T17:56:45","indexId":"70206561","displayToPublicDate":"2008-12-31T08:28:48","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Spatial and temporal trends in nitrate concentrations in the eastern San Joaquin Valley regional aquifer and implications for fertilizer management","docAbstract":"<p>Ground-water withdrawals in the San Joaquin Valley totaled 64 million m<sup>3</sup> /day (19 million ac-ft) in 2000, supplying about 45% of agricultural irrigation demand and about 80% of municipal supply (Hutson et al., 2004). Most of the population and ground-water use are in the eastern San Joaquin Valley, where reliance on ground water is expected to increase as a result of rapid population growth and limited surface water supplies. Protection of ground-water quality for future use requires monitoring and understanding the mechanisms controlling the long-term quality of ground water in the regional aquifer system. </p><p>Nitrate has been widely detected above background concentrations in ground water in the eastern San Joaquin Valley. Nitrate concentrations (reported as nitrogen in this paper) were above the MCL of 10 mg/L in 24% of domestic wells screened in the shallow part of the aquifer that were sampled during 1993–95 (Dubrovsky et al., 1998) and the Central Valley is one of the top three regions in the state in terms of the number of public drinking-water wells exceeding the MCL for nitrate (California State Water Resources Control Board, 2002). </p><p>To assess spatial and temporal trends in nitrate concentrations in the eastern San Joaquin Valley and to evaluate the long-term effects of nitrogen fertilizer use on ground-water quality in this region, data were evaluated at multiple spatial scales. Data from regional-scale monitoring networks were used to map the regional occurrence of nitrate and to determine whether shallow ground water containing elevated nitrate is migrating to deeper parts of the aquifer system. At the local scale, mean ground-water ages from analysis of age-dating tracers were combined with concentrations of nitrate to reconstruct nitrate inputs in recharge through time and to compare with estimated nitrogen applications. Ground-water flow and transport simulations of a typical public-supply well screened from about 100 to 400 ft below the water table were used to evaluate long-term concentrations beneath agricultural areas under different nitrogen management scenarios. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the American Society of Agronomy, California Chapter annual meeting","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","usgsCitation":"Burow, K.R., and Green, C.T., 2008, Spatial and temporal trends in nitrate concentrations in the eastern San Joaquin Valley regional aquifer and implications for fertilizer management, <i>in</i> Proceedings of the American Society of Agronomy, California Chapter annual meeting, p. 46-52.","productDescription":"7 p.","startPage":"46","endPage":"52","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"links":[{"id":369077,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":369076,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://calasa.ucdavis.edu/Conference_Proceedings/"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.81640624999999,\n              37.97884504049713\n            ],\n            [\n              -119.53125,\n              35.10193405724606\n            ],\n            [\n              -118.91601562499999,\n              34.939985151560435\n            ],\n            [\n              -118.7841796875,\n              35.29943548054545\n            ],\n            [\n              -118.861083984375,\n              35.92464453144099\n            ],\n            [\n              -118.91601562499999,\n              36.491973470593685\n            ],\n            [\n              -120.08056640625,\n              37.431250501793585\n            ],\n            [\n              -120.80566406250001,\n              38.151837403006766\n            ],\n            [\n              -121.81640624999999,\n              37.97884504049713\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Burow, Karen R. 0000-0001-6006-6667 krburow@usgs.gov","orcid":"https://orcid.org/0000-0001-6006-6667","contributorId":1504,"corporation":false,"usgs":true,"family":"Burow","given":"Karen","email":"krburow@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":774941,"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":774942,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70189929,"text":"70189929 - 2008 - Recent declines in western U.S. snowpack in the context of twentieth-century climate variability","interactions":[],"lastModifiedDate":"2017-08-01T16:06:06","indexId":"70189929","displayToPublicDate":"2008-12-31T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":736,"text":"American Meteorological Society, Journal of Hydrometeorology","active":true,"publicationSubtype":{"id":10}},"title":"Recent declines in western U.S. snowpack in the context of twentieth-century climate variability","docAbstract":"A monthly snow accumulation and melt model was used with monthly Precipitation-elevation Regressions on Independent Slopes Model (PRISM) temperature and precipitation data to generate time series of 1 April snow water equivalent (SWE) for 1900 through 2008 in the western United States. Averaged across the western United States, SWE generally was higher than long-term (1900–2008) average conditions during the periods 1900–25, 1944–55, and 1966–82; SWE was lower than long-term average conditions during the periods 1926–43, 1957–65, and 1984–2008. During the period 1900–2008, the temporal pattern in winter precipitation exhibited wetter-than-average and drier-than-average decadal-scale periods with no long-term increasing or decreasing trend. Winter temperature generally was below average from 1900 to the mid-1950s, close to average from the mid-1950s to the mid-1980s, and above average from the mid-1980s to 2008. In general, periods of higher-than-average SWE have been associated with higher precipitation and lower temperature. Since about 1980, western U.S. winter temperatures have been consistently higher than long-term average values, and the resultant lower-than-average SWE values have been only partially offset by periods of higher-than-average precipitation. The post-1980 lower-than-average SWE conditions in the western United States are unprecedented within the context of twentieth-century climate and estimated SWE.","language":"English","publisher":"American Meteorological Society","doi":"10.1175/2009EI283.1","usgsCitation":"McCabe, G., and Wolock, D.M., 2008, Recent declines in western U.S. snowpack in the context of twentieth-century climate variability: American Meteorological Society, Journal of Hydrometeorology, v. 13,  13-012; 15 p., https://doi.org/10.1175/2009EI283.1.","productDescription":" 13-012; 15 p.","ipdsId":"IP-010684","costCenters":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"links":[{"id":476565,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1175/2009ei283.1","text":"Publisher Index Page"},{"id":344521,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, Idaho, Montana, New Mexico, Nevada, Oregon, Washington, Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -126.9580078125,\n              28.34306490482549\n            ],\n            [\n              -101.8212890625,\n              28.34306490482549\n            ],\n            [\n              -101.8212890625,\n              49.83798245308484\n            ],\n            [\n              -126.9580078125,\n              49.83798245308484\n            ],\n            [\n              -126.9580078125,\n              28.34306490482549\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"13","publishingServiceCenter":{"id":2,"text":"Denver PSC"},"noUsgsAuthors":false,"publicationDate":"2009-10-16","publicationStatus":"PW","scienceBaseUri":"59819318e4b0e2f5d463b7bb","contributors":{"authors":[{"text":"McCabe, Gregory J. 0000-0002-9258-2997 gmccabe@usgs.gov","orcid":"https://orcid.org/0000-0002-9258-2997","contributorId":167116,"corporation":false,"usgs":true,"family":"McCabe","given":"Gregory J.","email":"gmccabe@usgs.gov","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":false,"id":706796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolock, David M. 0000-0002-6209-938X dwolock@usgs.gov","orcid":"https://orcid.org/0000-0002-6209-938X","contributorId":540,"corporation":false,"usgs":true,"family":"Wolock","given":"David","email":"dwolock@usgs.gov","middleInitial":"M.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":706795,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70184302,"text":"70184302 - 2008 - Slowing of coastal subsidence is good news for restoration of Louisiana's wetlands","interactions":[],"lastModifiedDate":"2017-03-07T09:19:38","indexId":"70184302","displayToPublicDate":"2008-12-31T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3431,"text":"Sound Waves: Coastal science and research news from across the USGS","active":true,"publicationSubtype":{"id":10}},"title":"Slowing of coastal subsidence is good news for restoration of Louisiana's wetlands","docAbstract":"<p><span>Every year, volunteers use thousands of discarded Christmas trees to build brush fences in the coastal waters of Louisiana. The fences slow down waves and trap sediment, allowing aquatic vegetation to take root in the still water and stimulating the growth of new marsh. This is one of many efforts to counteract wetland loss (the loss of saline, brackish, intermediate, and freshwater marshes) that has plagued coastal Louisiana since the mid-20th century. U.S. Geological Survey (USGS) scientists recently announced good news for Louisiana's coastal-restoration projects: using a combination of historical and recently released data, they discovered that subsidence of coastal land in the Mississippi River delta plain appears to have slowed considerably since the 1990s. This discovery means that new marshlands created by the Christmas tree program and other restoration projects may persist—that is, stay above sea level—longer than previously thought.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Cimitile, M., and Gibbons, H., 2008, Slowing of coastal subsidence is good news for restoration of Louisiana's wetlands: Sound Waves: Coastal science and research news from across the USGS, HTML document.","productDescription":"HTML document","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":336924,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":336923,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://soundwaves.usgs.gov/2008/10/research.html","text":"Document","linkFileType":{"id":5,"text":"html"},"description":"Document"}],"country":"United States","state":"Louisiana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.834228515625,\n              29.707139348134145\n            ],\n            [\n              -93.22998046875,\n              29.707139348134145\n            ],\n            [\n              -93.22998046875,\n              30.12612436422458\n            ],\n            [\n              -93.834228515625,\n              30.12612436422458\n            ],\n            [\n              -93.834228515625,\n              29.707139348134145\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.52734374999999,\n              29.05616970274342\n            ],\n            [\n              -89.835205078125,\n              29.05616970274342\n            ],\n            [\n              -89.835205078125,\n              29.640320395351402\n            ],\n            [\n              -90.52734374999999,\n              29.640320395351402\n            ],\n            [\n              -90.52734374999999,\n              29.05616970274342\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58bfd4f8e4b014cc3a3ba4e6","contributors":{"authors":[{"text":"Cimitile, Matthew","contributorId":50276,"corporation":false,"usgs":true,"family":"Cimitile","given":"Matthew","affiliations":[],"preferred":false,"id":680907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gibbons, Helen hgibbons@usgs.gov","contributorId":912,"corporation":false,"usgs":true,"family":"Gibbons","given":"Helen","email":"hgibbons@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":680908,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70184374,"text":"70184374 - 2008 - Estimation of water surface elevations for the Everglades, Florida","interactions":[],"lastModifiedDate":"2018-02-07T19:02:57","indexId":"70184374","displayToPublicDate":"2008-12-31T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Estimation of water surface elevations for the Everglades, Florida","docAbstract":"<p id=\"\">The Everglades Depth Estimation Network (EDEN) is an integrated network of real-time water-level monitoring gages and modeling methods that provides scientists and managers with current (2000–present) online water surface and water depth information for the freshwater domain of the Greater Everglades. This integrated system presents data on a 400-m square grid to assist in (1) large-scale field operations; (2) integration of hydrologic and ecologic responses; (3) supporting biological and ecological assessment of the implementation of the Comprehensive Everglades Restoration Plan (CERP); and (4) assessing trophic-level responses to hydrodynamic changes in the Everglades.</p><p id=\"\">This paper investigates the radial basis function multiquadric method of interpolation to obtain a continuous freshwater surface across the entire Everglades using radio-transmitted data from a network of water-level gages managed by the US Geological Survey (USGS), the South Florida Water Management District (SFWMD), and the Everglades National Park (ENP). Since the hydrological connection is interrupted by canals and levees across the study area, boundary conditions were simulated by linearly interpolating along those features and integrating the results together with the data from marsh stations to obtain a continuous water surface through multiquadric interpolation. The absolute cross-validation errors greater than 5&nbsp;cm correlate well with the local outliers and the minimum distance between the closest stations within 2000-m radius, but seem to be independent of vegetation or season.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.cageo.2007.08.004","usgsCitation":"Palaseanu, M., and Pearlstine, L., 2008, Estimation of water surface elevations for the Everglades, Florida: Computers & Geosciences, v. 34, no. 7, p. 815-826, https://doi.org/10.1016/j.cageo.2007.08.004.","productDescription":"12 p.","startPage":"815","endPage":"826","costCenters":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":337043,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    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,{"id":97177,"text":"ofr20071249 - 2008 - Temporal Geochemistry Data from Five Springs in the Cement Creek Watershed, San Juan County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:56","indexId":"ofr20071249","displayToPublicDate":"2008-12-25T00:00:00","publicationYear":"2008","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":"2007-1249","title":"Temporal Geochemistry Data from Five Springs in the Cement Creek Watershed, San Juan County, Colorado","docAbstract":"Temporal data from five springs in the Cement Creek watershed, San Juan County, Colorado provide seasonal geochemical data for further research in the formation of ferricretes. In addition, these data can be used to help understand the ground-water flow system. The resulting data demonstrate the difficulty in gathering reliable seasonal data from springs, show the unique geochemistry of each spring due to local geology, and provide seasonal trends in geochemistry for Tiger Iron Spring.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20071249","usgsCitation":"Johnson, R.H., Wirt, L., and Leib, K.J., 2008, Temporal Geochemistry Data from Five Springs in the Cement Creek Watershed, San Juan County, Colorado: U.S. Geological Survey Open-File Report 2007-1249, Report: iii, 11 p.; Downloads Directory, https://doi.org/10.3133/ofr20071249.","productDescription":"Report: iii, 11 p.; Downloads Directory","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2003-11-13","temporalEnd":"2004-10-31","costCenters":[{"id":213,"text":"Crustal Imaging and Characterization Team","active":false,"usgs":true}],"links":[{"id":196269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12161,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1249/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.83416666666666,37.75 ], [ -107.83416666666666,37.96666666666667 ], [ -107.5,37.96666666666667 ], [ -107.5,37.75 ], [ -107.83416666666666,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685699","contributors":{"authors":[{"text":"Johnson, Raymond H. rhjohnso@usgs.gov","contributorId":707,"corporation":false,"usgs":true,"family":"Johnson","given":"Raymond","email":"rhjohnso@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":301262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wirt, Laurie","contributorId":13204,"corporation":false,"usgs":true,"family":"Wirt","given":"Laurie","affiliations":[],"preferred":false,"id":301263,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leib, Kenneth J. 0000-0002-0373-0768 kjleib@usgs.gov","orcid":"https://orcid.org/0000-0002-0373-0768","contributorId":701,"corporation":false,"usgs":true,"family":"Leib","given":"Kenneth","email":"kjleib@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":301261,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97176,"text":"ofr20081368 - 2008 - Electrical Resistivity and Seismic Surveys at the Nevada Test Site, Nevada, April 2007","interactions":[],"lastModifiedDate":"2012-02-10T00:11:50","indexId":"ofr20081368","displayToPublicDate":"2008-12-25T00:00:00","publicationYear":"2008","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":"2008-1368","title":"Electrical Resistivity and Seismic Surveys at the Nevada Test Site, Nevada, April 2007","docAbstract":"In April 2007, the USGS collected direct-current (DC) electrical resistivity data and shear- (S) and compressional- (P) wave seismic data to provide new detail of previously mapped, overlapping fault splays at two administrative areas in the Nevada Test Site (NTS). In NTS Area 7, we collected two-dimensional DC resistivity data along a transect crossing the Yucca Fault parallel to, and between, two transects along which resistivity data were collected in a previous study in 2006. In addition, we collected three-dimensional DC resistivity data in a grid that overlies part of the 2007 transect. The DC resistivity data show that the fault has a footwall that is more conductive than the hanging wall and an along-strike progression of the fault in a location where overlapping splays are present. Co-located with the northernmost of the two 2006 DC resistivity transects, we acquired S- and P-wave seismic data for both reflection and refraction processing. The S-wave data are corrupted by large amounts of converted (P-wave) energy likely due to the abundance of fractured caliche in the shallow subsurface. The P-wave data show minimal reflected energy, but they show clear refracted first arrivals. We have inverted these first arrival times to determine P-wave seismic velocity models. The seismic model for the transect in Area 7 shows low velocities extending to the base of the model at the location of the Yucca Fault, as well as low velocities at the eastern end of the transect, in the vicinity of the adjacent crater. These new surveys provide further detail about the geometry of the Yucca Fault in this location where it shows two overlapping splays.\r\n\r\nWe collected P- and S-wave seismic data along a transect in the southern part of NTS Area 2, corresponding with the location of a 2006 DC resistivity transect that targeted a set of small faults identified with field mapping. Again, the S-wave data are difficult to interpret. The P-wave data show clear first arrivals that we inverted, yielding a velocity model that shows lateral heterogeneity similar to the 2006 DC resistivity models. Finally, we collected P-wave data along a second transect in Area 2, located north of the first line and in an area of a very minor fault that was targeted by another 2006 DC resistivity survey. The P-wave refraction velocity model shows generally high velocities, with a zone of somewhat lower velocities in the central part of the transect. The position of the low velocity zone corresponds with the location of a minor fault, though it is unclear whether the two are related.\r\n\r\nTogether, these results demonstrate the value of geophysical data for mapping the subsurface extent of faults. The 2007 DC resistivity data complement the 2006 data and provide important new detail of the overlapping fault splays. The seismic data demonstrate the ability of P-wave refraction methods to identify the damage zones at faults, and they show the difficulties associated with S-wave methods in areas with caliche. Combining all of the geophysical data from the Area 7 studies, we are able to develop a coherent interpretation of the relation between the site geology, the fault, and the observations.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081368","collaboration":"Prepared in cooperation with the U.S. Department of Energy, National Nuclear Security Administration Nevada Site Office","usgsCitation":"Haines, S.S., Burton, B., Sweetkind, D., and Asch, T., 2008, Electrical Resistivity and Seismic Surveys at the Nevada Test Site, Nevada, April 2007: U.S. Geological Survey Open-File Report 2008-1368, iv, 33 p., https://doi.org/10.3133/ofr20081368.","productDescription":"iv, 33 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2007-04-01","temporalEnd":"2007-04-30","costCenters":[{"id":213,"text":"Crustal Imaging and Characterization Team","active":false,"usgs":true}],"links":[{"id":195348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12160,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1368/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.08333333333333,37.0675 ], [ -116.08333333333333,37.134166666666665 ], [ -116.03333333333333,37.134166666666665 ], [ -116.03333333333333,37.0675 ], [ -116.08333333333333,37.0675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605601","contributors":{"authors":[{"text":"Haines, Seth S. 0000-0003-2611-8165 shaines@usgs.gov","orcid":"https://orcid.org/0000-0003-2611-8165","contributorId":1344,"corporation":false,"usgs":true,"family":"Haines","given":"Seth","email":"shaines@usgs.gov","middleInitial":"S.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":301258,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":301257,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sweetkind, Donald S.","contributorId":18732,"corporation":false,"usgs":true,"family":"Sweetkind","given":"Donald S.","affiliations":[],"preferred":false,"id":301259,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Asch, Theodore H.","contributorId":83617,"corporation":false,"usgs":true,"family":"Asch","given":"Theodore H.","affiliations":[],"preferred":false,"id":301260,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":97178,"text":"sir20085229 - 2008 - Comparison of Atmospheric Deposition Among Three Sites In and Near the Flat Tops Wilderness Area, Colorado, 2003-2005","interactions":[],"lastModifiedDate":"2012-02-10T00:11:51","indexId":"sir20085229","displayToPublicDate":"2008-12-25T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-5229","title":"Comparison of Atmospheric Deposition Among Three Sites In and Near the Flat Tops Wilderness Area, Colorado, 2003-2005","docAbstract":"Atmospheric deposition was monitored for ammonium, nitrate, and sulfate concentrations and precipitation amounts in the Flat Tops Wilderness Area of northwestern Colorado at Ned Wilson Lake beginning in 1984 to detect changes that might result from future emissions associated with development of oil-shale resources in northwestern Colorado. Renewed monitoring, by the U.S. Geological Survey, in cooperation with Rio Blanco County, to determine the current status of atmospheric deposition has been ongoing since 2003 at Ned Wilson Lake. Two new monitoring sites were located near Ripple Creek Pass near the Flat Tops Wilderness area and about 12 kilometers north of Ned Wilson Lake because access to the area near Ripple Creek Pass is less difficult and less expensive, particularly in winter and spring. The intent of this study was to establish whether the new deposition data being collected near Ripple Creek Pass, near the northern boundary of the Flat Tops Wilderness Area, would be representative of deposition at sensitive sites within the wilderness such as Ned Wilson Lake and to compare more current (2003 through 2005) deposition data with earlier data (1984 through 1991).\r\n\r\nAt Ned Wilson Lake, bulk ammonium and nitrate concentrations collected from 1984 through 1991 were similar to those from 2003 through 2005. However, in the same comparison significant differences in sulfate concentrations were observed, indicating a decrease consistent with other regional findings for similar periods. Comparison of concentrations of constituents at two bulk-deposition sites located at Ned Wilson Lake (NWLB) and near Ripple Creek Pass (RCPB) showed only one significant difference (p = 0.05) with the winter bulk nitrate concentrations for NWLB significantly lower than winter concentrations from RCPB. Another comparison of concentrations of constituents between the bulk deposition site RCPB and a wet deposition site 100 meters away (RCPW) showed no significant differences for concentrations of ammonium, nitrate, and sulfate for both the winter and summer comparisons. While results indicate many similarities in concentrations of constituents and in seasonal variability in those concentrations, they are based on a short period of study. Precipitation amounts from RCPB were less than the amounts collected at NWLB, and precipitation amounts from RCPW were less than the amounts collected at RCPB. Although RCPB may not be a perfect replacement site for NWLB, it may be similar enough to represent atmospheric deposition in areas of the Flat Tops Wilderness of northwestern Colorado.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20085229","collaboration":"Prepared in cooperation with Rio Blanco County, Colorado","usgsCitation":"Ingersoll, G.P., Campbell, D.H., and Mast, M.A., 2008, Comparison of Atmospheric Deposition Among Three Sites In and Near the Flat Tops Wilderness Area, Colorado, 2003-2005: U.S. Geological Survey Scientific Investigations Report 2008-5229, iv, 17 p., https://doi.org/10.3133/sir20085229.","productDescription":"iv, 17 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2003-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"links":[{"id":124716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2008_5229.jpg"},{"id":12162,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5229/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.25,38.5 ], [ -109.25,40.5 ], [ -107,40.5 ], [ -107,38.5 ], [ -109.25,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae47e","contributors":{"authors":[{"text":"Ingersoll, George P. gpingers@usgs.gov","contributorId":1469,"corporation":false,"usgs":true,"family":"Ingersoll","given":"George","email":"gpingers@usgs.gov","middleInitial":"P.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Donald H. dhcampbe@usgs.gov","contributorId":1670,"corporation":false,"usgs":true,"family":"Campbell","given":"Donald","email":"dhcampbe@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":301266,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mast, M. Alisa 0000-0001-6253-8162 mamast@usgs.gov","orcid":"https://orcid.org/0000-0001-6253-8162","contributorId":827,"corporation":false,"usgs":true,"family":"Mast","given":"M.","email":"mamast@usgs.gov","middleInitial":"Alisa","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301264,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97166,"text":"sim3055 - 2008 - Hydrogeologic Framework of Onslow County, North Carolina, 2008","interactions":[],"lastModifiedDate":"2012-03-08T17:16:32","indexId":"sim3055","displayToPublicDate":"2008-12-24T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3055","title":"Hydrogeologic Framework of Onslow County, North Carolina, 2008","docAbstract":"The unconsolidated sediments that underlie the Onslow County area are composed of interlayered permeable and impermeable beds, which overlie the crystalline basement rocks. The aquifers, composed mostly of sand and limestone, are separated by confining units composed mostly of clay and silt. The aquifers from top to bottom are the surficial, Castle Hayne, Beaufort, Peedee, Black Creek, and Upper and Lower Cape Fear aquifers. For this study, the Castle Hayne aquifer is informally divided into the upper and lower Castle Hayne aquifers.\r\n\r\nThe eight aquifers and seven confining units of the Tertiary and Cretaceous strata beneath Onslow County are presented in seven hydrogeologic sections. The hydrogeologic framework was refined from existing interpretations by using geophysical logs, driller's logs, and other available data from 123 wells and boreholes.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sim3055","collaboration":"Prepared in cooperation with the City of Jacksonville, Onslow Water and Sewer Authority, and U.S. Marine Corps, Camp Lejeune","usgsCitation":"Fine, J.M., 2008, Hydrogeologic Framework of Onslow County, North Carolina, 2008: U.S. Geological Survey Scientific Investigations Map 3055, Map Sheet: 32 x 32 inches, https://doi.org/10.3133/sim3055.","productDescription":"Map Sheet: 32 x 32 inches","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2008-01-01","temporalEnd":"2008-12-31","costCenters":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"links":[{"id":196181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12152,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3055/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.91666666666667,34.333333333333336 ], [ -77.91666666666667,35.166666666666664 ], [ -77,35.166666666666664 ], [ -77,34.333333333333336 ], [ -77.91666666666667,34.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628dc2","contributors":{"authors":[{"text":"Fine, Jason M. 0000-0002-6386-256X jmfine@usgs.gov","orcid":"https://orcid.org/0000-0002-6386-256X","contributorId":2238,"corporation":false,"usgs":true,"family":"Fine","given":"Jason","email":"jmfine@usgs.gov","middleInitial":"M.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301235,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97165,"text":"ds370 - 2008 - Archive of digitized analog boomer seismic reflection data collected from Lake Pontchartrain, Louisiana, to Mobile Bay, Alabama, during cruises onboard the R/V ERDA-1, June and August 1992","interactions":[],"lastModifiedDate":"2023-12-07T17:21:11.233452","indexId":"ds370","displayToPublicDate":"2008-12-24T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"370","title":"Archive of digitized analog boomer seismic reflection data collected from Lake Pontchartrain, Louisiana, to Mobile Bay, Alabama, during cruises onboard the R/V ERDA-1, June and August 1992","docAbstract":"In June and August of 1992, the U.S. Geological Survey (USGS) conducted geophysical surveys to investigate the shallow geologic framework from Lake Pontchartrain, Louisiana, to Mobile Bay, Alabama. This work was conducted onboard the Argonne National Laboratory's R/V ERDA-1 as part of the Mississippi/Alabama Pollution Project. This report is part of a series to digitally archive the legacy analog data collected from the Mississippi-Alabama SHelf (MASH). The MASH data rescue project is a cooperative effort by the USGS and the Minerals Management Service (MMS).\r\n\r\nA standardized naming convention was established to allow for better management of scanned trackline images within the MASH data rescue project. Each cruise received a unique field activity ID based on the year the data were collected, the first two digits of the survey vessel name, and the number of cruises made (to date) by that vessel that year (i.e. 92ER2 represents the second cruise made by the R/V ERDA-1 in 1992.) The new field activity IDs 92ER2 and 92ER4 presented in this report were originally referred to as ERDA 92-2 and ERDA 92-4 at the USGS in St. Petersburg, FL, and 92010 and 92037 at the USGS in Woods Hole, MA. A table showing the naming convention lineage for cruise IDs in the MASH data rescue series is included as a PDF. This report serves as an archive of high resolution scanned Tagged Image File Format (TIFF) and Graphics Interchange Format (GIF) images of the original boomer paper records, navigation files, trackline maps, Geographic Information System (GIS) files, cruise logs, and formal Federal Geographic Data Committee (FGDC) metadata for cruises 92ER2 and 92ER4.\r\n\r\nThe boomer system uses an acoustic energy source called a plate, which consists of capacitors charged to a high voltage and discharged through a transducer in the water. The source is towed on a sled, at sea level, and when discharged emits a short acoustic pulse, or shot, which propagates through the water and sediment column. The acoustic energy is reflected at density boundaries (such as the seafloor or sediment layers beneath the seafloor), detected by the hydrophone receiver, and the amplitude of the reflected energy is recorded by an Edward P. Curley Lab (EPC) thermal plotter. This process is repeated at timed intervals (for example, 0.5 s) and recorded for specific intervals of time (for example, 100 ms). The timed intervals are also referred to as the shot interval or fire rate. On analog records, the recorded interval is referred to as the sweep, which is the amount of time the recorder stylus takes to sweep from the top of the record to the bottom of the record, thereby recording the amplitude of the reflected energy of one shot. In this way, consecutive recorded shots produce a two-dimensional (2-D) vertical image of the shallow geologic structure beneath the ship track.\r\n\r\nMany of the geophysical data collected by the USGS prior to the late 1990s were recorded in analog format and stored as paper copies. Scientists onboard made hand-written annotations onto these records to note latitude and longitude, time, line number, course heading, and geographic points of reference. Each paper roll typically contained numerous survey lines and could reach more than 90 ft in length. All rolls are stored at the USGS FISC-St. Petersburg, FL. To preserve the integrity of these records and improve accessibility, analog holdings were converted to digital files.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds370","usgsCitation":"Sanford, J.M., Harrison, A.S., Wiese, D.S., and Flocks, J.G., 2008, Archive of digitized analog boomer seismic reflection data collected from Lake Pontchartrain, Louisiana, to Mobile Bay, Alabama, during cruises onboard the R/V ERDA-1, June and August 1992: U.S. Geological Survey Data Series 370, HTML Document; DVD-ROM, https://doi.org/10.3133/ds370.","productDescription":"HTML Document; DVD-ROM","onlineOnly":"N","additionalOnlineFiles":"Y","temporalStart":"1992-06-01","temporalEnd":"1992-08-31","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":12151,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/370/","linkFileType":{"id":5,"text":"html"}},{"id":195543,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alabama, Louisiana, Mississippi","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -87.75850476330332,\n              30.630754940045918\n            ],\n            [\n              -90.9275318981158,\n              30.630754940045918\n            ],\n            [\n              -90.9275318981158,\n              29.717202798386765\n            ],\n            [\n              -87.75850476330332,\n              29.717202798386765\n            ],\n            [\n              -87.75850476330332,\n              30.630754940045918\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679d4d","contributors":{"authors":[{"text":"Sanford, Jordan M.","contributorId":17197,"corporation":false,"usgs":true,"family":"Sanford","given":"Jordan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":301233,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrison, Arnell S. 0000-0002-5581-2255","orcid":"https://orcid.org/0000-0002-5581-2255","contributorId":35021,"corporation":false,"usgs":true,"family":"Harrison","given":"Arnell","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":301234,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wiese, Dana S. dwiese@usgs.gov","contributorId":2476,"corporation":false,"usgs":true,"family":"Wiese","given":"Dana","email":"dwiese@usgs.gov","middleInitial":"S.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":301232,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flocks, James G. 0000-0002-6177-7433 jflocks@usgs.gov","orcid":"https://orcid.org/0000-0002-6177-7433","contributorId":816,"corporation":false,"usgs":true,"family":"Flocks","given":"James","email":"jflocks@usgs.gov","middleInitial":"G.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":301231,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":97164,"text":"sir20085150 - 2008 - Evaluation of four structural best management practices for highway runoff in Beaufort and Colleton Counties, South Carolina, 2005–2006","interactions":[],"lastModifiedDate":"2023-03-22T21:47:13.175524","indexId":"sir20085150","displayToPublicDate":"2008-12-24T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-5150","title":"Evaluation of four structural best management practices for highway runoff in Beaufort and Colleton Counties, South Carolina, 2005–2006","docAbstract":"<p>From 2005 to 2006, the U.S. Geological Survey worked cooperatively with the South Carolina Department of Transportation in Beaufort and Colleton Counties, South Carolina, to assess the performance of four different structural devices that served as best management practices (BMPs). These structural devices were installed to mitigate the effects of stormwater runoff on waterways near State roads. The South Carolina Department of Transportation is required to address the quality of stormwater runoff from State-maintained roadways as part of the National Pollutant Discharge Elimination System stormwater program mandated in the Clean Water Act.</p><p>The performance assessment of the four structural best management practices was based on stormflow measurements and chemical analyses of stormwater-quality samples collected during a 20-month period from March 2005 through October 2006, which represented a range of seasons and rainfall intensities. A total of 49 sample sets that included stormwater from the inlet and outlet of each of the four structural devices were collected as flow-weighted composites to provide event-mean concentrations of suspended sediment, nutrients, and trace metals. In addition, each set included grab samples that were collected to provide the first flush concentrations of oil and grease and fecal-indicator bacteria.</p><p>A tiered statistical approach was used in the data analysis. Performances of the four structural BMPs were assessed individually based on how well the BMPs were able to reduce the selected constituents. Descriptive statistics and nonparametric Wilcoxon signed rank tests were applied to event-mean concentrations and loads in the water entering the inlet and in the water leaving the outlet of each BMP for each constituent to identify if significant reductions occurred. If significant reductions occurred, the BMP was considered efficient at reducing the constituent. To quantify efficiency, a simplistic approach was applied to compute mean and geometric mean efficiency ratios for the significantly reduced constituents in each BMP. Each BMP performance was ranked based on its computed efficiency ratios, however, the computed efficiency ratios were not sufficient to determine if statistical differences occurred among the performances of the four BMPs. Consequently, a more complex approach was used to apply statistical comparison tests to reduction percentages computed for individual storms (a modified removal efficiency of individual storm-load approach) to determine if differences in event-mean concentrations, loads, and reduction percentages for significantly reduced constituents occurred among the four structural BMPs.</p><p>Overall, the four BMPs were efficient in reducing suspended-sediment event-mean concentrations and loads in the stormwater entering the inlets of the BMPs to significantly lower event-mean concentrations before discharging the stormwater from the outlets. The cumulative suspended-sediment event-mean load in stormwater entering the BMPs from the storms sampled during the data-collection period was 1,026 kilograms (1.13 tons). The BMPs removed a cumulative suspended-sediment load of 558 kilograms (0.62 ton). The BMPs tended to preferentially trap the sand-size fraction of the sediment, thereby releasing a greater percentage of fine-grained (silt and clay) sediment in the water discharging from the outlet. The preferential trapping of fine-grained sediment by the BMPs could explain, at least in part, why the BMPs were not successful at significantly reducing these constituents.</p><p>In general, the four BMPs were not successful at significantly reducing fecal bacteria, nutrients, and total organic carbon (including associated properties of biochemical oxygen demand and chemical oxygen demand). Three of the four BMPs significantly lowered oil and grease concentrations before the stormwater discharged from the outlet. Additionally, only one BMP was effective at reducing all total and particulate trace-metal event-mean concentrations and particulate trace-metal event-mean loads in stormwater entering the inlet. With respect to trace-metal event-mean concentrations, however, minimal or no improvement in outlet water quality was observed for the four BMPs, and the majority of the outlet concentrations were above the established acute and chronic aquatic-life criteria by the South Carolina Department of Health and Environmental Control.</p><p>No statistical differences among the removal-efficiency of the four BMPs were determined for suspended-sediment event-mean concentrations, total suspended solids event-mean concentrations, or oil and grease concentrations. These statistical findings indicated that differences among the mean efficiency ratios were not significant among the BMPs for these properties. Additionally, one BMP generally had statistically greater removal efficiency for total and particulate cadmium, copper, lead, and zinc than one or more of the other three BMPs.</p><p>Statistical correlation tests were unable to identify a single major factor that would explain the high variability in inlet and outlet water concentrations and in removal efficiencies estimated by reduction percentage. Highly variable inlet and outlet concentrations for each BMP that produced highly variable reduction percentages were probably the result of multiple interacting factors, particularly rainfall intensity, the amount of rainfall between sampling events, traffic density, and the period of time since the last maintenance (clean out) of the BMP.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20085150","collaboration":"Prepared in cooperation with the South Carolina Department of Transportation","usgsCitation":"Conlon, K.J., and Journey, C.A., 2008, Evaluation of four structural best management practices for highway runoff in Beaufort and Colleton Counties, South Carolina, 2005–2006: U.S. Geological Survey Scientific Investigations Report 2008-5150, xiv, 122 p., https://doi.org/10.3133/sir20085150.","productDescription":"xiv, 122 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2005-01-01","temporalEnd":"2006-12-31","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":198211,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414588,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_96516.htm","linkFileType":{"id":5,"text":"html"}},{"id":12150,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5150/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Carolina","county":"Beaufort County, Colleton County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.6417,\n              32.4167\n            ],\n            [\n              -80.6417,\n              32.7811\n            ],\n            [\n              -80.7811,\n              32.7811\n            ],\n            [\n              -80.7811,\n              32.4167\n            ],\n            [\n              -80.6417,\n              32.4167\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faff5","contributors":{"authors":[{"text":"Conlon, Kevin J. 0000-0003-0798-368X kjconlon@usgs.gov","orcid":"https://orcid.org/0000-0003-0798-368X","contributorId":2561,"corporation":false,"usgs":true,"family":"Conlon","given":"Kevin","email":"kjconlon@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":301229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Journey, Celeste A. 0000-0002-2284-5851 cjourney@usgs.gov","orcid":"https://orcid.org/0000-0002-2284-5851","contributorId":2617,"corporation":false,"usgs":true,"family":"Journey","given":"Celeste","email":"cjourney@usgs.gov","middleInitial":"A.","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":false,"id":301230,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97171,"text":"ofr20081294 - 2008 - Mapping vulnerability to disasters in Latin America and the Caribbean, 1900–2007","interactions":[],"lastModifiedDate":"2022-08-02T19:12:51.079978","indexId":"ofr20081294","displayToPublicDate":"2008-12-24T00:00:00","publicationYear":"2008","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":"2008-1294","title":"Mapping vulnerability to disasters in Latin America and the Caribbean, 1900–2007","docAbstract":"The vulnerability of a population and its infrastructure to disastrous events is a factor of both the probability of a hazardous event occurring and the community's ability to cope with the resulting impacts. Therefore, the ability to accurately identify vulnerable populations and places in order to prepare for future hazards is of critical importance for disaster mitigation programs. \r\n\r\nThis project created maps of higher spatial resolution of vulnerability to disaster in Latin America and the Caribbean from 1900 to 2007 by mapping disaster data by first-level administrative boundaries with the objective of identifying geographic trends in regional occurrences of disasters and vulnerable populations. The method of mapping by administrative level is an improvement on displaying and analyzing disasters at the country level and shows the relative intensity of vulnerability within and between countries in the region. Disaster mapping at the country level produces only a basic view of which countries experience various types of natural disasters. Through disaggregation, the data show which geographic areas of these countries, including populated areas, are historically most susceptible to different hazard types.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081294","collaboration":"Prepared in cooperation with the Office of U.S. Foreign Disaster Assistance","usgsCitation":"Maynard-Ford, M.C., Phillips, E.C., and Chirico, P., 2008, Mapping vulnerability to disasters in Latin America and the Caribbean, 1900–2007: U.S. Geological Survey Open-File Report 2008-1294, iv, 26 p., https://doi.org/10.3133/ofr20081294.","productDescription":"iv, 26 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1900-01-01","temporalEnd":"2007-12-31","costCenters":[{"id":229,"text":"Earth Surface Processes Team","active":false,"usgs":true}],"links":[{"id":195363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404698,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_86252.htm","linkFileType":{"id":5,"text":"html"}},{"id":12156,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1294/","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"Caribbean, Latin America","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -62.57812500000001,\n              -56.55948248376223\n            ],\n            [\n              -64.6875,\n              -49.83798245308484\n            ],\n            [\n              -30.937499999999996,\n              -6.664607562172573\n            ],\n            [\n              -47.4609375,\n              30.44867367928756\n            ],\n            [\n              -82.96875,\n              24.84656534821976\n            ],\n            [\n              -97.03125,\n              26.115985925333536\n            ],\n            [\n              -106.875,\n              31.653381399664\n            ],\n            [\n              -119.17968749999999,\n              32.84267363195431\n            ],\n            [\n              -111.09374999999999,\n              19.642587534013032\n            ],\n            [\n              -97.03125,\n              12.554563528593656\n            ],\n            [\n              -83.671875,\n              5.965753671065536\n            ],\n            [\n              -87.1875,\n              -0.7031073524364783\n            ],\n            [\n              -80.15625,\n              -12.897489183755892\n            ],\n            [\n              -73.47656249999999,\n              -19.642587534013032\n            ],\n            [\n              -78.3984375,\n              -46.8000594467873\n            ],\n            [\n              -77.34374999999999,\n              -54.36775852406839\n            ],\n            [\n              -71.015625,\n              -56.94497418085159\n            ],\n            [\n              -62.57812500000001,\n              -56.55948248376223\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699f9c","contributors":{"authors":[{"text":"Maynard-Ford, Miriam C.","contributorId":31489,"corporation":false,"usgs":true,"family":"Maynard-Ford","given":"Miriam","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":301244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, Emily C.","contributorId":65189,"corporation":false,"usgs":true,"family":"Phillips","given":"Emily","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":301245,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chirico, Peter G.","contributorId":27086,"corporation":false,"usgs":true,"family":"Chirico","given":"Peter G.","affiliations":[],"preferred":false,"id":301243,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97167,"text":"sir20085188 - 2008 - State and regional water-quality characteristics and trophic conditions of Michigan's inland lakes, 2001-2005","interactions":[],"lastModifiedDate":"2016-09-29T12:44:33","indexId":"sir20085188","displayToPublicDate":"2008-12-24T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-5188","title":"State and regional water-quality characteristics and trophic conditions of Michigan's inland lakes, 2001-2005","docAbstract":"<p>The U.S. Geological Survey and the Michigan Department of Environmental Quality are jointly monitoring selected water-quality constituents of inland lakes through 2015 as part of Michigan’s Lake Water Quality Assessment program. During 2001–2005, 433 lake basins from 364 inland lakes were monitored for baseline water-quality conditions and trophic status. This report summarizes the water-quality characteristics and trophic conditions of those monitored lake basins throughout the State. </p><p>Regional variation of water quality in lake basins was examined by grouping on the basis of the five Omernik level III ecoregions within Michigan. Concentrations of most constituents measured were significantly different between ecoregions. Less regional variation of phosphorus concentrations was noted between Northern Lakes and Forests (50) and North Central Hardwoods (51) ecoregions during summer possibly because water samples were collected when lake productivity was high; hence the utilization of the limited amount of phosphorus by algae and macrophytes may have resulted in the more uniform concentrations between these two ecoregions. </p><p>Concentrations of common ions (calcium, magnesium, potassium, sodium, chloride, and sulfate) measured in the spring typically were higher in the Michigan southern Lower Peninsula in the Eastern Corn Belt Plains (55), Southern Michigan/Northern Indiana Drift Plains (56), and Huron/Erie Lake Plains (57) ecoregions. Most ions whose concentrations were less than the minimum reporting levels or were nondetectable were from lakes in the Michigan northern Lower Peninsula and the Upper Peninsula in the Northern Lakes and Forests (50) and North Central Hardwoods (51) ecoregions. Chlorophyll a concentrations followed a similar distribution pattern. Measured properties such as pH and specific conductance (indicative of dissolved solids) also showed a regional relation. The lakes with the lowest pH and specific conductance were generally in the western Upper Peninsula (Northern Lakes and Forests (50) ecoregion). </p><p>The Michigan Department of Environmental Quality classifies Michigan lakes on the basis of their primary biological productivity or trophic characteristics using the Carlson Trophic State Index. Trophic evaluations based on data collected from 2001 through 2005 indicate 17 percent of the lakes are oligotrophic, 53 percent are mesotrophic, 22 percent are eutrophic, 4 percent are hypereutrophic, and less than 5 percent are classified into transition classes between each major class. Although the distribution of lakes throughout Michigan or between Omernik level III ecoregions is not uniform, about 85 percent of the lakes classified as oligotrophic are in the Northern Lakes and Forests (50) or North Central Hardwoods (51) ecoregions. Nearly 28 percent of all the lakes in each of these two ecoregions were classified as oligotrophic. </p><p>Historical trophic-state classes were compared to the current (2001 through 2005) trophic-state classes. Approximately 72 percent of lakes remained in the same trophic-state class, 11 percent moved up a partial or full class (indicating a decrease in water clarity) and 18 percent moved down a partial or full class (indicating an increase in water clarity). </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20085188","collaboration":"In cooperation with the Michigan Department of Environmental Quality","usgsCitation":"Fuller, L.M., and Minnerick, R., 2008, State and regional water-quality characteristics and trophic conditions of Michigan's inland lakes, 2001-2005: U.S. Geological Survey Scientific Investigations Report 2008-5188, iv, 58 p., https://doi.org/10.3133/sir20085188.","productDescription":"iv, 58 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2001-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":382,"text":"Michigan Water Science 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M.","contributorId":97987,"corporation":false,"usgs":true,"family":"Fuller","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":301237,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minnerick, R. J.","contributorId":52255,"corporation":false,"usgs":true,"family":"Minnerick","given":"R. J.","affiliations":[],"preferred":false,"id":301236,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97170,"text":"sim3035 - 2008 - Geologic map of the Fredonia 30' x 60' quadrangle, Mohave and Coconino counties, northern Arizona","interactions":[],"lastModifiedDate":"2017-03-29T12:11:43","indexId":"sim3035","displayToPublicDate":"2008-12-24T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3035","title":"Geologic map of the Fredonia 30' x 60' quadrangle, Mohave and Coconino counties, northern Arizona","docAbstract":"This geologic map is the result of a cooperative effort of the U.S. Geological Survey, the National Park Service, the U.S. Forest Service, and the Bureau of Land Management (BLM) and the Kaibab-Paiute Tribe to provide a regional geologic database for resource management officials of all government and agencies, city municipalities, private enterprises, and individuals of this part of the Arizona Strip. The Arizona Strip is part of northwestern Arizona north of the Colorado River and bounded by the States of Nevada and Utah. Field work on the Kaibab-Paiute Indian Reservation was conducted from 2002 to 2005 with permission from the Kaibab-Paiute Tribal Government of that administration and permission was granted to publish a geologic map of 4 quadrangles online (Billingsley and others, 2004). The Kaibab-Paiute Tribal government of 2006 to 2008 requested that all geologic information within the Kaibab-Paiute Indian Reservation not be published as part of the Fredonia 30' x 60' quadrangle (this publication). For further information, contact the Kaibab-Paiute Tribal government at HC 65 Box 2, Fredonia, Arizona, 86022, telephone # (928) 643-7245. Visitors to the Kaibab-Paiute Indian Reservation are required to obtain a permit and permission for access from the Tribal Offices at the junction of State Highway 389 and the paved road leading to Pipe Spring National Monument. \r\n\r\nThe Fredonia 30' x 60' quadrangle encompasses approximately 5,018 km2 (1,960 mi2) within Mohave and Coconino Counties, northern Arizona and is bounded by longitude 112 deg to 113 deg W., and latitude 36 deg 30' to 37 deg N. The map area lies within the southern Colorado Plateaus geologic province (herein Colorado Plateau). The map area is locally subdivided into seven physiographic parts: the Grand Canyon (Kanab Canyon and its tributaries), Kanab Plateau, Uinkaret Plateau, Kaibab Plateau, Paria Plateau, House Rock Valley, and Moccasin Mountains as defined by Billingsley and others, 1997, (fig. 1). Elevations range from 2,737 m (8,980 ft) just west of State Highway 67 on the Kaibab Plateau, southeast corner of the map area to about 927 m (3,040 ft) in Kanab Canyon, south-central edge of the map area. \r\n","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sim3035","collaboration":"Prepared in cooperation with the National Park Service, U.S. Forest Service, and Bureau of Land Management","usgsCitation":"Billingsley, G.H., Priest, S.S., and Felger, T.J., 2008, Geologic map of the Fredonia 30' x 60' quadrangle, Mohave and Coconino counties, northern Arizona (Version 1.0): U.S. Geological Survey Scientific Investigations Map 3035, Report: ii, 23 p.; Map Sheet: 49.5 x 36 inches; GIS files, https://doi.org/10.3133/sim3035.","productDescription":"Report: ii, 23 p.; Map Sheet: 49.5 x 36 inches; GIS files","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":110801,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_86238.htm","linkFileType":{"id":5,"text":"html"},"description":"86238"},{"id":12155,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3035/","linkFileType":{"id":5,"text":"html"}},{"id":196268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1","projection":"Universal Transverse Mercator","country":"United States","state":"Arizona","county":"Coconino County, Mohave County","city":"Fredonia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113,36.5 ], [ -113,37 ], [ -112,37 ], [ -112,36.5 ], [ -113,36.5 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8506","contributors":{"authors":[{"text":"Billingsley, George H.","contributorId":20711,"corporation":false,"usgs":true,"family":"Billingsley","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":301241,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Priest, Susan S. spriest@usgs.gov","contributorId":30204,"corporation":false,"usgs":true,"family":"Priest","given":"Susan","email":"spriest@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":false,"id":301242,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Felger, Tracey J. 0000-0003-0841-4235 tfelger@usgs.gov","orcid":"https://orcid.org/0000-0003-0841-4235","contributorId":1117,"corporation":false,"usgs":true,"family":"Felger","given":"Tracey","email":"tfelger@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":301240,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97147,"text":"ofr20081343 - 2008 - Report on the Aseismic Slip, Tremor, and Earthquakes Workshop","interactions":[],"lastModifiedDate":"2019-07-18T09:43:53","indexId":"ofr20081343","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","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":"2008-1343","title":"Report on the Aseismic Slip, Tremor, and Earthquakes Workshop","docAbstract":"This report summarizes the discussions and information presented during the workshop on Aseismic Slip, Tremor, and Earthquakes. Workshop goals included improving coordination among those involved in conducting research related to these phenomena, assessing the implications for earthquake hazard assessment, and identifying ways to capitalize on the education and outreach opportunities presented by these phenomena. Research activities of focus included making, disseminating, and analyzing relevant measurements; the relationships among tremor, aseismic or 'slow-slip', and earthquakes; and discovering the underlying causative physical processes. More than 52 participants contributed to the workshop, held February 25-28, 2008 in Sidney, British Columbia. The workshop was sponsored by the U.S. Geological Survey, the National Science Foundation?s Earthscope Program and UNAVCO Consortium, and the Geological Survey of Canada. \r\n\r\nThis report has five parts. In the first part, we integrate the information exchanged at the workshop as it relates to advancing our understanding of earthquake generation and hazard. In the second part, we summarize the ideas and concerns discussed in workshop working groups on Opportunities for Education and Outreach, Data and Instrumentation, User and Public Needs, and Research Coordination. The third part presents summaries of the oral presentations. The oral presentations are grouped as they were at the workshop in the categories of phenomenology, underlying physical processes, and implications for earthquake hazards. The fourth part contains the meeting program and the fifth part lists the workshop participants. References noted in parentheses refer to the authors of presentations made at the workshop, and published references are noted in square brackets and listed in the Reference section. Appendix A contains abstracts of all participant presentations and posters, which also have been posted online, along with presentations and author contact information at http://www.earthscope.org/science/cascadia.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20081343","collaboration":"Prepared in cooperation with Earthscope, UNAVCO, the National Science Foundation and the Geological Survey of Canada","usgsCitation":"Gomberg, J., Roeloffs, E., Trehu, A., Dragert, H., and Meertens, C., 2008, Report on the Aseismic Slip, Tremor, and Earthquakes Workshop (Version 1.0): U.S. Geological Survey Open-File Report 2008-1343, 77 p. , https://doi.org/10.3133/ofr20081343.","productDescription":"77 p. ","onlineOnly":"Y","temporalStart":"2008-02-25","temporalEnd":"2008-02-28","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":196179,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12132,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1343/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c6b7","contributors":{"authors":[{"text":"Gomberg, Joan","contributorId":77919,"corporation":false,"usgs":true,"family":"Gomberg","given":"Joan","affiliations":[],"preferred":false,"id":301184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roeloffs, Evelyn","contributorId":35417,"corporation":false,"usgs":true,"family":"Roeloffs","given":"Evelyn","affiliations":[],"preferred":false,"id":301183,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trehu, Anne","contributorId":82016,"corporation":false,"usgs":true,"family":"Trehu","given":"Anne","affiliations":[],"preferred":false,"id":301185,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dragert, Herb","contributorId":100497,"corporation":false,"usgs":true,"family":"Dragert","given":"Herb","email":"","affiliations":[],"preferred":false,"id":301186,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meertens, Charles","contributorId":28333,"corporation":false,"usgs":true,"family":"Meertens","given":"Charles","affiliations":[],"preferred":false,"id":301182,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":97145,"text":"ofr20081344 - 2008 - Comments on potential geologic and seismic hazards affecting proposed liquefied natural gas site in Santa Monica Bay, California","interactions":[],"lastModifiedDate":"2022-06-15T20:57:29.361448","indexId":"ofr20081344","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","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":"2008-1344","displayTitle":"Comments on Potential Geologic and Seismic Hazards Affecting Proposed Liquefied Natural Gas Site in Santa Monica Bay, California","title":"Comments on potential geologic and seismic hazards affecting proposed liquefied natural gas site in Santa Monica Bay, California","docAbstract":"In a letter to the U.S. Geological Survey (USGS) dated March 25, 2008, Representative Jane Harman (California 36th district) requested advice on geologic hazards that should be considered in the review of a proposed liquefied natural gas (LNG) facility off the California coast in Santa Monica Bay. In 2004, the USGS responded to a similar request from Representative Lois Capps, regarding two proposed LNG facilities offshore Ventura County, Calif., with a report summarizing potential geologic and seismic hazards (Ross and others, 2004).\r\n\r\nThe proposed LNG Deepwater Port (DWP) facility includes single point moorings (SPMs) and 35 miles of underwater pipelines. The DWP submersible buoys, manifolds, and risers would be situated on the floor of the southern Santa Monica Basin, in 3,000 feet of water, about 23 miles offshore of the Palos Verdes Peninsula. Twin 24-inch diameter pipelines would extend northeastward from the buoys across the basin floor, up the basin slope and across the continental shelf, skirting north around the Santa Monica submarine canyon. Figure 1 provides locations of the project and geologic features. Acronyms are defined in table 1.\r\n\r\nThis facility is being proposed in a region of known geologic hazards that arise from both the potential for strong earthquakes and geologic processes related to sediment transport and accumulation in the offshore environment. The probability of a damaging earthquake (considered here as magnitude 6.5 or greater) in the next 30 years within about 30 miles (50 km) of the proposed pipeline ranges from 16% at the pipeline's offshore end to 48% where it nears land (Petersen, 2008). Earthquakes of this magnitude are capable of producing strong shaking, surface fault offsets, liquefaction phenomena, landslides, underwater turbidity currents and debris flow avalanches, and tsunamis.\r\n\r\nAs part of the DWP license application for the Woodside Natural Gas proposal in Santa Monica Bay (known as the OceanWay Secure Energy Project), Fugro West, Inc., had already prepared a document discussing geologic hazards in the area, titled 'Exhibit B Topic Report 6 - Geological Resources' (Fugro West, Inc., 2007); hereafter, this will be called the 'Geological Resources document'. The USGS agreed to evaluate the information in the Geological Resources document regarding (1) proximity of active faults to the proposed project, (2) potential magnitude of seismic events from nearby faults, (3) thoroughness of the assessment of earthquake hazards in general, (4) potential hazards from ground rupture and strong shaking, (5) potential hazards from tsunamis, and (6) other geologic hazards including landslides and debris flows. Because two new earthquake probability reports were scheduled to be released in mid-April, 2008, by the USGS and the California Geological Survey (CGS), the USGS suggested a 6-month review period to enable a thorough incorporation of this new information.\r\n\r\nTwenty-seven scientists from the USGS and the CGS reviewed various sections of the Geological Resources document. This report outlines our major conclusions. The appendix is a longer list of comments by these reviewers, grouped by section of the Geological Resources document. Before discussing our reviews, we first provide a brief overview of geologic hazards in the proposed site area.\r\n\r\nThis report is a snapshot in time and any future work in the area will need to take into account ongoing research efforts. For example, USGS scientists collected seismic reflection data in the spring of 2008 to study the structure and seismic potential of several faults in the area. Their interpretations (Conrad and others, 2008a and 2008b) are too preliminary to be included in this report, but their final results, along with other researchers' studies in the project area, should be considered in any future work on the Deepwater Port project.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081344","usgsCitation":"Ross, S.L., Lee, H., Parsons, T.E., Beyer, L.A., Boore, D.M., Conrad, J.E., Edwards, B.D., Fisher, M.A., Frankel, A.D., Geist, E.L., Hudnut, K.W., Hough, S.E., Kayen, R., Lorenson, T., Luco, N., McCrory, P.A., McGann, M., Nathenson, M., Nolan, M., Petersen, M.D., Ponti, D.J., Powell, C.L., Ryan, H., Tinsley, J., Wills, C.J., Wong, F.L., and Xu, J., 2008, Comments on potential geologic and seismic hazards affecting proposed liquefied natural gas site in Santa Monica Bay, California (Version 1.0): U.S. Geological Survey Open-File Report 2008-1344, vi, 60 p., https://doi.org/10.3133/ofr20081344.","productDescription":"vi, 60 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III jtinsley@usgs.gov","contributorId":3266,"corporation":false,"usgs":true,"family":"Tinsley","given":"John C.","suffix":"III","email":"jtinsley@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":301174,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Wills, Chris J.","contributorId":97576,"corporation":false,"usgs":true,"family":"Wills","given":"Chris","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":301178,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"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":301161,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Xu, Jingping jpx@usgs.gov","contributorId":2574,"corporation":false,"usgs":true,"family":"Xu","given":"Jingping","email":"jpx@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":301166,"contributorType":{"id":1,"text":"Authors"},"rank":27}]}}
,{"id":97155,"text":"sir20085171 - 2008 - Simulation of Flood Profiles for Catoma Creek near Montgomery, Alabama, 2008","interactions":[],"lastModifiedDate":"2012-02-10T00:11:49","indexId":"sir20085171","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-5171","title":"Simulation of Flood Profiles for Catoma Creek near Montgomery, Alabama, 2008","docAbstract":"A one-dimensional step-backwater model was used to simulate flooding conditions for Catoma Creek near Montgomery, Alabama. A peak flow of 50,000 cubic feet per second was computed by the U.S. Geological Survey for the March 1990 flood at the Norman Bridge Road gaging station. Using this estimated peak flow, flood-plain surveys with associated roughness coefficients, and surveyed high-water marks for the March 1990 flood, a flow model was calibrated to closely match the known event. The calibrated model then was used to simulate flooding for the 10-, 50-, 100-, and 500-year recurrence-interval floods. The 100-year flood stage for the Alabama River also was computed in the vicinity of the Catoma Creek confluence using observed high-water profiles from the 1979 and 1990 floods and gaging-station data. \r\n\r\nThe results indicate that the 100-year flood profile for Catoma Creek within the 15-mile study reach is about 2.5 feet higher, on average, than the profile published by the Federal Emergency Management Agency. The maximum and minimum differences are 6.0 feet and 0.8 foot, respectively. All water-surface elevations computed for the 100-year flood are higher than those published by the Federal Emergency Management Agency. The 100-year flood stage computed for the Alabama River in the vicinity of the Catoma Creek confluence was about 4.5 feet lower than the elevation published by the Federal Emergency Management Agency. The results of this study provide the community with flood-profile information that can be used for flood-plain mitigation, future development, and safety plans for the city.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20085171","collaboration":"Prepared in cooperation with the City of Montgomery, Alabama","usgsCitation":"Lee, K., and Hedgecock, T., 2008, Simulation of Flood Profiles for Catoma Creek near Montgomery, Alabama, 2008: U.S. Geological Survey Scientific Investigations Report 2008-5171, iv, 33 p., https://doi.org/10.3133/sir20085171.","productDescription":"iv, 33 p.","temporalStart":"2008-01-01","temporalEnd":"2008-12-31","costCenters":[{"id":105,"text":"Alabama Water Science Center","active":true,"usgs":true}],"links":[{"id":124404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2008_5171.jpg"},{"id":12140,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5171/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.75,31.75 ], [ -86.75,32.75 ], [ -85.75,32.75 ], [ -85.75,31.75 ], [ -86.75,31.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6977fb","contributors":{"authors":[{"text":"Lee, K.G.","contributorId":28319,"corporation":false,"usgs":true,"family":"Lee","given":"K.G.","email":"","affiliations":[],"preferred":false,"id":301206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedgecock, T.S.","contributorId":16107,"corporation":false,"usgs":true,"family":"Hedgecock","given":"T.S.","email":"","affiliations":[],"preferred":false,"id":301205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97149,"text":"ofr20081289 - 2008 - Floods of December 2004 and January 2005 in Ohio: FEMA Disaster Declaration 1580","interactions":[],"lastModifiedDate":"2022-08-04T21:15:16.232185","indexId":"ofr20081289","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","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":"2008-1289","title":"Floods of December 2004 and January 2005 in Ohio: FEMA Disaster Declaration 1580","docAbstract":"A large snowstorm at the end of December 2004 that left more than 20 inches of snow in some areas of Ohio, followed by unseasonably warm temperatures in early January 2005, caused snowmelt to begin filling river channels. Widespread rain showers during January 2005 combined with this snowmelt to cause flooding throughout Ohio and mudslides in some areas. Record peak streamflows occurred at nine U.S. Geological Survey (USGS) streamgages. Damages caused by the snowstorms, flooding, and mudslides were severe enough for 62 counties in Ohio to be declared Federal disaster areas. In all, approximately 3,664 private structures were damaged or destroyed, and an estimated $238 million in damages occurred.\r\n\r\nThis report describes the meteorological factors that resulted in severe flooding throughout Ohio between December 22, 2004, and February 1, 2005, and examines the damages caused by the storms and flooding. Peak-stage, peak-streamflow, and recurrence-interval data are reported for selected USGS streamgages. Flood profiles determined by the USGS are presented for selected streams.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20081289","collaboration":"Prepared in cooperation with the Ohio Emergency Management Agency","usgsCitation":"Ebner, A.D., Straub, D.E., and Lageman, J.D., 2008, Floods of December 2004 and January 2005 in Ohio: FEMA Disaster Declaration 1580: U.S. Geological Survey Open-File Report 2008-1289, viii, 98 p., https://doi.org/10.3133/ofr20081289.","productDescription":"viii, 98 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2004-12-22","temporalEnd":"2005-02-01","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":195739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404853,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_85397.htm","linkFileType":{"id":5,"text":"html"}},{"id":12134,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1289/","linkFileType":{"id":5,"text":"html"}}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfe1c","contributors":{"authors":[{"text":"Ebner, Andrew D. aebner@usgs.gov","contributorId":1849,"corporation":false,"usgs":true,"family":"Ebner","given":"Andrew","email":"aebner@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":301191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Straub, David E. destraub@usgs.gov","contributorId":1908,"corporation":false,"usgs":true,"family":"Straub","given":"David","email":"destraub@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":301192,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lageman, Jonathan D. jlageman@usgs.gov","contributorId":1910,"corporation":false,"usgs":true,"family":"Lageman","given":"Jonathan","email":"jlageman@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":301193,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97141,"text":"ds386 - 2008 - Hydraulic and substrate maps of reaches used by sturgeon (<i>Genus Scaphirhynchus</i>) in the Lower Missouri River, 2005-07","interactions":[],"lastModifiedDate":"2017-05-24T15:22:41","indexId":"ds386","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"386","title":"Hydraulic and substrate maps of reaches used by sturgeon (<i>Genus Scaphirhynchus</i>) in the Lower Missouri River, 2005-07","docAbstract":"<p><span>This report is a repository of reach-scale maps of hydraulic and substrate characteristics generated for the habitat-use portion of an interdisciplinary sturgeon research project on the Lower Missouri River (from Gavins Point Dam to the junction with the Mississippi River). The maps were derived from hydroacoustic data sets that were collected for the purpose of assessing physical aquatic habitat in the vicinity of locations of adult shovelnose sturgeon (</span><i>Scaphirhynchus platorynchus</i><span>) and pallid sturgeon (</span><i>S. albus</i><span>). Hydroacoustic data sets were collected at the reach scale (mean reach length, 2.4 kilometers) in order to include the immediate vicinity of a targeted sturgeon location as well as the full range of habitat available at the bend and crossover scale. Reaches typically were surveyed on the day following the relocation of a telemetered sturgeon and at a discharge within 10 percent of the discharge on the sturgeon relocation date in order to characterize as closely as possible the channel morphology and flow-field conditions at the time that the sturgeon was present. One hundred fifty-three reaches were mapped during April–September in the years 2005 through 2007, with the majority of data collection occurring in the months of May and June (coinciding with the period of sturgeon migration and spawning in the Lower Missouri River). Interpolated maps (grid cell size, 5 meters) depict depth, generalized substrate, and depth-averaged velocity. Side-scan sonar imagery is also available for a subset of reaches. Collectively, the maps represent more than 20 percent of the length of the Lower Missouri River.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds386","collaboration":"Prepared for the Missouri River Recovery-Integrated Science Program, U.S. Army Corps of Engineers, Yankton, South Dakota","usgsCitation":"Reuter, J.M., Jacobson, R.B., Elliott, C.M., Johnson, H.E., and DeLonay, A.J., 2008, Hydraulic and substrate maps of reaches used by sturgeon (<i>Genus Scaphirhynchus</i>) in the Lower Missouri River, 2005-07 (Version 1.0): U.S. Geological Survey Data Series 386, vi, 442 p., https://doi.org/10.3133/ds386.","productDescription":"vi, 442 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2005-04-01","temporalEnd":"2007-09-30","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":195439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":341688,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ds/386/pdf/DS386_508.pdf","text":"Report","size":"166.7 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":12125,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/386/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100,38 ], [ -100,44 ], [ -88,44 ], [ -88,38 ], [ -100,38 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a353","contributors":{"authors":[{"text":"Reuter, Joanna M.","contributorId":50179,"corporation":false,"usgs":true,"family":"Reuter","given":"Joanna","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":301141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacobson, Robert B. 0000-0002-8368-2064 rjacobson@usgs.gov","orcid":"https://orcid.org/0000-0002-8368-2064","contributorId":1289,"corporation":false,"usgs":true,"family":"Jacobson","given":"Robert","email":"rjacobson@usgs.gov","middleInitial":"B.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":301138,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Elliott, Caroline M. 0000-0002-9190-7462 celliott@usgs.gov","orcid":"https://orcid.org/0000-0002-9190-7462","contributorId":2380,"corporation":false,"usgs":true,"family":"Elliott","given":"Caroline","email":"celliott@usgs.gov","middleInitial":"M.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":301139,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, Harold E. III","contributorId":47470,"corporation":false,"usgs":true,"family":"Johnson","given":"Harold","suffix":"III","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":301140,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"DeLonay, Aaron J.","contributorId":53360,"corporation":false,"usgs":true,"family":"DeLonay","given":"Aaron","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":301142,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":97162,"text":"tm2A7 - 2008 - Protocol for Monitoring Fish Assemblages in Pacific Northwest National Parks","interactions":[],"lastModifiedDate":"2012-02-10T00:11:46","indexId":"tm2A7","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2-A7","title":"Protocol for Monitoring Fish Assemblages in Pacific Northwest National Parks","docAbstract":"Rivers and streams that drain from Olympic, Mount Rainier, and North Cascades National Parks are among the most protected corridors in the lower 48 States, and represent some of the largest tracts of contiguous, undisturbed habitat throughout the range of several key fish species of the Pacific Northwest. These watersheds are of high regional importance as freshwater habitat sanctuaries for native fish, where habitat conditions are characterized as having little to no disturbance from development, channelization, impervious surfaces, roads, diversions, or hydroelectric projects. Fishery resources are of high ecological and cultural importance in Pacific Northwest National Parks, and significantly contribute to economically important recreational, commercial, and tribal fisheries.\r\n\r\nThis protocol describes procedures to monitor trends in fish assemblages, fish abundance, and water temperature in eight rivers and five wadeable streams in Olympic National Park during summer months, and is based on 4 years of field testing. Fish assemblages link freshwater, marine, and terrestrial ecosystems. They also serve as focal resources of national parks and are excellent indicators of ecological conditions of rivers and streams. Despite the vital importance of native anadromous and resident fish populations, there is no existing monitoring program for fish assemblages in the North Coast and Cascades Network.\r\n\r\nSpecific monitoring objectives of this protocol are to determine seasonal and annual trends in: (1) fish species composition, (2) timing of migration of adult fish, (3) relative abundance, (4) age and size structure, (5) extent of non-native and hatchery fish, and (6) water temperature. To detect seasonal and annual trends in fish assemblages in reference sites, we rely on repeated and consistent annual sampling at each monitoring site. The general rationale for the repeated sampling of reference sites is to ensure that we account for the high interannual variability in fish movements and abundances in rivers. One underlying assumption is that the monitoring program is designed in perpetuity, and consequently our capability to detect trends substantially increases with time.\r\n\r\nThe protocol describes sampling designs, methods, training procedures, safety considerations, data management, data analysis, and reporting. The allocation of sampling effort represents a balance between ecological considerations, a sound monitoring approach, and practical limitations caused by logistical constraints and a limited annual budget of $55,000. The widespread declines of native fish species in western North America highlights the importance and urgency of understanding trends in fish assemblages from undisturbed habitats. Seasonal and annual trends in fish assemblages will provide insights at the individual, population, and assemblage level.\r\n\r\nThis protocol will allow managers to detect increases and decreases in abundance of priority management species, and occurrence of non-native, hatchery, and federally listed fish. The detection of trends in fish assemblages will allow for specific management actions that may include: implementation of more appropriate fishing regulations, evaluation of existing hatchery releases, control of non-native fish species, and prioritization of habitat restoration projects. Dissemination and communication of scientific findings on North Coast and Cascades Network fish assemblages will be a core product of this protocol, which will have much relevance to decision makers, park visitors, researchers, and educators.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Chapter 7 of Section A, Biological Science, Book 2, Collection of Environmental Data","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/tm2A7","collaboration":"Prepared in cooperation with the North Coast and Cascades Network, National Park Service","usgsCitation":"Brenkman, S.J., and Connolly, P., 2008, Protocol for Monitoring Fish Assemblages in Pacific Northwest National Parks: U.S. Geological Survey Techniques and Methods 2-A7, vi, 131 p., https://doi.org/10.3133/tm2A7.","productDescription":"vi, 131 p.","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":124593,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tm_2_a7.png"},{"id":12147,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/tm2a7/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125,47.25 ], [ -125,48.5 ], [ -122,48.5 ], [ -122,47.25 ], [ -125,47.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687ec3","contributors":{"authors":[{"text":"Brenkman, Samuel J.","contributorId":50864,"corporation":false,"usgs":true,"family":"Brenkman","given":"Samuel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":301225,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Connolly, Patrick J. 0000-0001-7365-7618 pconnolly@usgs.gov","orcid":"https://orcid.org/0000-0001-7365-7618","contributorId":2920,"corporation":false,"usgs":true,"family":"Connolly","given":"Patrick J.","email":"pconnolly@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":301224,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97160,"text":"fs20083095 - 2008 - Management and research applications of long-range surveillance radar data for birds, bats, and flying insects","interactions":[],"lastModifiedDate":"2019-09-20T10:07:27","indexId":"fs20083095","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-3095","displayTitle":"Management and Research Applications of Long-range Surveillance Radar Data for Birds, Bats, and Flying Insects","title":"Management and research applications of long-range surveillance radar data for birds, bats, and flying insects","docAbstract":"There is renewed interest in using long-range surveillance radar as a biological research tool due to substantial improvements in the network of radars within the United States. Technical improvements, the digital nature of the radar data, and the availability of computing power and geographic information systems, enable a broad range of biological applications. This publication provides a summary of long-range surveillance radar technology and applications of these data to questions about movement patterns of birds and other flying wildlife. The intended audience is potential radar-data end users, including natural-resource management and regulatory agencies, conservation organizations, and industry. This summary includes a definition of long-range surveillance radar, descriptions of its strengths and weaknesses, information on applications of the data, cost, methods of calibration, and what end users need to do, and some key references and resources.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20083095","usgsCitation":"Ruth, J.M., Buler, J., Diehl, R.H., and Sojda, R.S., 2008, Management and research applications of long-range surveillance radar data for birds, bats, and flying insects (Version 1.0): U.S. Geological Survey Fact Sheet 2008-3095, 4 p., https://doi.org/10.3133/fs20083095.","productDescription":"4 p.","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":121084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2008_3095.jpg"},{"id":367582,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2008/3095/pdf/FS08-3095_508.pdf"},{"id":12145,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2008/3095/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.8277587890625,\n              27.22044113007616\n            ],\n            [\n              -96.74011230468749,\n              27.22044113007616\n            ],\n            [\n              -96.74011230468749,\n              28.001676807403094\n            ],\n            [\n              -97.8277587890625,\n              28.001676807403094\n            ],\n            [\n              -97.8277587890625,\n              27.22044113007616\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1e4","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":301219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buler, Jeffrey J.","contributorId":78431,"corporation":false,"usgs":true,"family":"Buler","given":"Jeffrey J.","affiliations":[],"preferred":false,"id":301222,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diehl, Robert H. 0000-0001-9141-1734 rhdiehl@usgs.gov","orcid":"https://orcid.org/0000-0001-9141-1734","contributorId":3396,"corporation":false,"usgs":true,"family":"Diehl","given":"Robert","email":"rhdiehl@usgs.gov","middleInitial":"H.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":301221,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sojda, Richard S. sojda@usgs.gov","contributorId":1663,"corporation":false,"usgs":true,"family":"Sojda","given":"Richard","email":"sojda@usgs.gov","middleInitial":"S.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"preferred":true,"id":301220,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":97157,"text":"sir20065171 - 2008 - Potential Chemical Effects of Changes in the Source of Water Supply for the Albuquerque Bernalillo County Water Utility Authority","interactions":[],"lastModifiedDate":"2012-03-08T17:16:26","indexId":"sir20065171","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5171","title":"Potential Chemical Effects of Changes in the Source of Water Supply for the Albuquerque Bernalillo County Water Utility Authority","docAbstract":"Chemical modeling was used by the U.S. Geological Survey, in cooperation with the Albuquerque Bernalillo County Water Utility Authority (henceforth, Authority), to gain insight into the potential chemical effects that could occur in the Authority's water distribution system as a result of changing the source of water used for municipal and industrial supply from ground water to surface water, or to some mixture of the two sources. From historical data, representative samples of ground-water and surface-water chemistry were selected for modeling under a range of environmental conditions anticipated to be present in the distribution system. Mineral phases calculated to have the potential to precipitate from ground water were compared with the compositions of precipitate samples collected from the current water distribution system and with mineral phases calculated to have the potential to precipitate from surface water and ground-water/surface-water mixtures.\r\n\r\nSeveral minerals that were calculated to have the potential to precipitate from ground water in the current distribution system were identified in precipitate samples from pipes, reservoirs, and water heaters. These minerals were the calcium carbonates aragonite and calcite, and the iron oxides/hydroxides goethite, hematite, and lepidocrocite. Several other minerals that were indicated by modeling to have the potential to precipitate were not found in precipitate samples. For most of these minerals, either the kinetics of formation were known to be unfavorable under conditions present in the distribution system or the minerals typically are not formed through direct precipitation from aqueous solutions.\r\n\r\nThe minerals with potential to precipitate as simulated for surface-water samples and ground-water/surface-water mixtures were quite similar to the minerals with potential to precipitate from ground-water samples. Based on the modeling results along with kinetic considerations, minerals that appear most likely to either dissolve or newly precipitate when surface water or ground-water/surface-water mixtures are delivered through the Authority's current distribution system are carbonates (particularly aragonite and calcite). Other types of minerals having the potential to dissolve or newly precipitate under conditions present throughout most of the distribution system include a form of silica, an aluminum hyroxide (gibbsite or diaspore), or the Fe-containing mineral Fe3(OH)8. Dissolution of most of these minerals (except perhaps the Fe-containing minerals) is not likely to substantially affect trace-element concentrations or aesthetic characteristics of delivered water, except perhaps hardness. Precipitation of these minerals would probably be of concern only if the quantities of material involved were large enough to clog pipes or fixtures. The mineral Fe3(OH)8 was not found in the current distribution system. Some Fe-containing minerals that were identified in the distribution system were associated with relatively high contents of selected elements, including As, Cr, Cu, Mn, Pb, and Zn. However, these Fe-containing minerals were not identified as minerals likely to dissolve when the source of water was changed from ground water to surface water or a ground-water/surface-water mixture.\r\n\r\nBased on the modeled potential for calcite precipitation and additional calculations of corrosion indices ground water, surface water, and ground-water/surface-water mixtures are not likely to differ greatly in corrosion potential. In particular, surface water and ground-water/surface-water mixtures do not appear likely to dissolve large quantities of existing calcite and expose metal surfaces in the distribution system to substantially increased corrosion. Instead, modeling calculations indicate that somewhat larger masses of material would tend to precipitate from surface water or ground-water/surface-water mixtures compared to ground water alone.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065171","isbn":"9781411311367","collaboration":"Prepared in cooperation with the Albuquerque Bernalillo County Water Utility Authority","usgsCitation":"Bexfield, L.M., and Anderholm, S.K., 2008, Potential Chemical Effects of Changes in the Source of Water Supply for the Albuquerque Bernalillo County Water Utility Authority (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2006-5171, iv, 49 p., https://doi.org/10.3133/sir20065171.","productDescription":"iv, 49 p.","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":195578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12142,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5171/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.83333333333333,35 ], [ -106.83333333333333,35.25 ], [ -106.41666666666667,35.25 ], [ -106.41666666666667,35 ], [ -106.83333333333333,35 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c163","contributors":{"authors":[{"text":"Bexfield, Laura M. 0000-0002-1789-654X bexfield@usgs.gov","orcid":"https://orcid.org/0000-0002-1789-654X","contributorId":1273,"corporation":false,"usgs":true,"family":"Bexfield","given":"Laura","email":"bexfield@usgs.gov","middleInitial":"M.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":301210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderholm, Scott K.","contributorId":94270,"corporation":false,"usgs":true,"family":"Anderholm","given":"Scott","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":301211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":97156,"text":"sim3058 - 2008 - Well Inventory and Geophysical Logging of Selected Wells in Troup County, Georgia, 2007-2008","interactions":[],"lastModifiedDate":"2017-01-11T12:22:21","indexId":"sim3058","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"3058","title":"Well Inventory and Geophysical Logging of Selected Wells in Troup County, Georgia, 2007-2008","docAbstract":"The U.S. Geological Survey (USGS) - in cooperation with the Troup County Board of Commissioners - conducted a well inventory to provide information to help evaluate ground-water resources for Troup County, Georgia. In addition, borehole geophysical logs were collected in selected wells to provide a better understanding of the subsurface geologic and water-bearing characteristics in specific areas of interest. This investigation provides information to help guide future ground-water development and water-management decisions for Troup County while enhancing understanding of the hydrogeology of fractured rocks in the Piedmont physiographic province. This report presents well data compiled from USGS files and from site visits to wells during November and December 2007. Data were entered into the USGS National Water Information System (NWIS) and made available on the Web at http://waterdata.usgs.gov/ga/nwis/inventory.\r\n\r\nPrevious studies of ground-water resources have been conducted in the vicinity, but did not include Troup County. The ground-water resources of Heard and Coweta Counties, located north and northeast, respectively, of Troup County were part of a larger study by Cressler and others (1983) that encompassed the Greater Atlanta Region. That study evaluated the quantity and quality of ground water in the Atlanta region and described the methods that could be used for locating high-yielding wells in the Piedmont Province. The geology underlying the Atlanta area is similar to that underlying Troup County. Clarke and Peck (1990) conducted a similar investigation that included Meriwether and Coweta Counties, located to the east and northeast of Troup County.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sim3058","collaboration":"Prepared in cooperation with the Troup County Board of Commissioners","usgsCitation":"Peck, M., Leeth, D.C., and Hamrick, M.D., 2008, Well Inventory and Geophysical Logging of Selected Wells in Troup County, Georgia, 2007-2008: U.S. Geological Survey Scientific Investigations Map 3058, Map Sheet: 42 x 32 inches, https://doi.org/10.3133/sim3058.","productDescription":"Map Sheet: 42 x 32 inches","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2007-01-01","temporalEnd":"2008-12-31","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":195700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12141,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3058/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","county":"Troup County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.33333333333333,32.833333333333336 ], [ -85.33333333333333,33.25 ], [ -84.83333333333333,33.25 ], [ -84.83333333333333,32.833333333333336 ], [ -85.33333333333333,32.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0c51","contributors":{"authors":[{"text":"Peck, Michael F. mfpeck@usgs.gov","contributorId":1467,"corporation":false,"usgs":true,"family":"Peck","given":"Michael F.","email":"mfpeck@usgs.gov","affiliations":[],"preferred":false,"id":301208,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leeth, David C. cleeth@usgs.gov","contributorId":1403,"corporation":false,"usgs":true,"family":"Leeth","given":"David","email":"cleeth@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":301207,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hamrick, Michael D. hamrick@usgs.gov","contributorId":3237,"corporation":false,"usgs":true,"family":"Hamrick","given":"Michael","email":"hamrick@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":301209,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":97153,"text":"fs20083099 - 2008 - Hydrologic Streamflow Conditions for Georgia, 2007","interactions":[],"lastModifiedDate":"2016-12-07T09:56:59","indexId":"fs20083099","displayToPublicDate":"2008-12-23T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-3099","title":"Hydrologic Streamflow Conditions for Georgia, 2007","docAbstract":"The U.S. Geologic Survey (USGS) Georgia Water Science Center (GaWSC) maintains a long-term hydrologic monitoring network of more than 260 real-time streamflow stations and more than 100 noncontinuous streamflow stations throughout Georgia. This network is operated by the USGS GaWSC in cooperation with more than 50 different partners at Federal, State, and local government levels. One of the many benefits of data collected from this monitoring network is that it allows for the analysis of the overall hydrologic condition of streams and lakes of Georgia.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs20083099","usgsCitation":"Knaak, A.E., and Joiner, J.K., 2008, Hydrologic Streamflow Conditions for Georgia, 2007: U.S. Geological Survey Fact Sheet 2008-3099, 4 p. (available as 11 x 17 or 8.5 x 11), https://doi.org/10.3133/fs20083099.","productDescription":"4 p. 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