This set of two posters consists of a map on one sheet and a set of seven perspective views on the other. The ocean floor image was generated from multibeam-bathymetry data acquired by Federal and local agencies as well as academic institutions including:
\n- U.S. Geological Survey mapped from the La Jolla Canyon south to the US-Mexico border using a Kongsberg Simrad multibeam echosounder system (MBES) (March - April 1998). Data and metadata available at http://pubs.usgs.gov/of/2004/1221/.
\n- Woods Hole Oceanographic Institution and SCRIPPS Institution of Oceanography mapped the majority of the La Jolla Fan Valley including the sea floor to the north and south of the valley using a Seabeam 2100 MBES. Data available at http://www.ngdc.noaa.gov/mgg/bathymetry/multibeam.html. Survey ID, AT07L09, Chief Scientists, Barrie Walden and Joseph Coburn (April 2002).
\n- California State University, Monterey Bay, mapped Scripps Canyon and the head of La Jolla Canyon using a Reson 8101 MBES (October 2001). Data and metadata available at http://seafloor.csumb.edu/SFMLwebDATA.htm. This work was funded by the California Department of Fish and Game \nCalifornia Coastal Conservancy, San Diego Association of Governments (SANDAG), California Department of Fish and Game, and Fugro Pelagos mapped the nearshore region out to about 35-40 m.
\n- The sea floor within this image that has not been mapped with MBES is filled in with interpreted bathymetry gridded from single-beam data available at http://www.ngdc.noaa.gov/mgg/bathymetry/hydro.html. Depths are in meters below sea level, which is referenced to Mean Lower Low Water.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sim2959","isbn":"1411318021","usgsCitation":"Dartnell, P., Normark, W.R., Driscoll, N.W., Babcock, J.M., Gardner, J.V., Kvitek, R.G., and Iampietro, P.J., 2007, Multibeam bathymetry and selected perspective views offshore San Diego, California (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2959, 2 Sheets: 30.0 x 36.0 inches and 30.0 x 30.0 inches, https://doi.org/10.3133/sim2959.","productDescription":"2 Sheets: 30.0 x 36.0 inches and 30.0 x 30.0 inches","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":192426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sim2959.jpg"},{"id":9876,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2007/2959/","linkFileType":{"id":5,"text":"html"}},{"id":292861,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/sim/2007/2959/SIM-2959_sheet1.pdf"},{"id":292862,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/sim/2007/2959/SIM-2959_sheet2.pdf"}],"scale":"80000","projection":"Universal Transverse Mercator projection","country":"United States","state":"California","city":"San Diego","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.5,-32.666667 ], [ -117.5,33.0 ], [ -117.166667,33.0 ], [ -117.166667,-32.666667 ], [ -117.5,-32.666667 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698bf0","contributors":{"authors":[{"text":"Dartnell, Peter 0000-0002-9554-729X pdartnell@usgs.gov","orcid":"https://orcid.org/0000-0002-9554-729X","contributorId":2688,"corporation":false,"usgs":true,"family":"Dartnell","given":"Peter","email":"pdartnell@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":291675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Normark, William R.","contributorId":69570,"corporation":false,"usgs":true,"family":"Normark","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":291677,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Driscoll, Neal W.","contributorId":63266,"corporation":false,"usgs":true,"family":"Driscoll","given":"Neal","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":291676,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Babcock, Jeffrey M.","contributorId":80576,"corporation":false,"usgs":true,"family":"Babcock","given":"Jeffrey","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":291678,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gardner, James V.","contributorId":93035,"corporation":false,"usgs":true,"family":"Gardner","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":291680,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kvitek, Rikk G.","contributorId":107804,"corporation":false,"usgs":true,"family":"Kvitek","given":"Rikk","email":"","middleInitial":"G.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":291681,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Iampietro, Pat J.","contributorId":85679,"corporation":false,"usgs":true,"family":"Iampietro","given":"Pat","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":291679,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":80086,"text":"sim2946 - 2007 - Geologic Map of the Albuquerque 30' x 60' Quadrangle, North-Central New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:39","indexId":"sim2946","displayToPublicDate":"2007-07-07T00:00:00","publicationYear":"2007","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":"2946","title":"Geologic Map of the Albuquerque 30' x 60' Quadrangle, North-Central New Mexico","docAbstract":"The Albuquerque 30' x 60' quadrangle spans the Rio Grande rift between the Colorado Plateau and Great Plains geologic provinces, and includes parts of the Basin and Range and Southern Rocky Mountain physiographic provinces. Geologic units exposed in the quadrangle range in age from Early Proterozoic schist and granite to modern river alluvium. The principal geologic features of the area, however, chiefly reflect contractional folding and thrusting of the Late Cretaceous Laramide orogeny and the Neogene extension of the Rio Grande rift. Significant parts of the history of the rift in this region are displayed and documented by the geology exposed in the Albuquerque quadrangle.\r\n\r\nPost-Laramide erosion, beginning at about 60 Ma, is recorded by the Diamond Tail and Galisteo Formations (upper Paleocene and Eocene) that are preserved in the Hagan Basin and around the uplifted margins of the younger Rio Grande rift. Intermediate volcaniclastic deposits of the Espinaso Formation (upper Eocene and Oligocene) were shed in and around the contemporaneous volcanic-intrusive complexes of the Ortiz porphyry belt in the northeastern part of the quadrangle.\r\nThe earliest fluvial sediments attributed to extension in the Rio Grande rift in this area are the Tanos and Blackshare Formations (upper Oligocene and Miocene) in the Hagan Basin, which indicate extension was underway by 25 Ma. Farther west, the oldest rift-filling sediments are eolian sand and interdune silty deposits of the Zia Formation (lower to middle Miocene). Major extension occurred during the Miocene, but subsidence and sedimentation were highly irregular from place to place. Parts of three rift sub-basins are known within the Albuquerque quadrangle, each basin locally as deep as about 14,000 ft, separated by less-extended zones (structural horsts) where the rift fill is much thinner. The geometry of these early, deep rift sub-basins suggests the primary extension direction was oriented northeast-southwest. Significant local folding and uplift within the complex rift seems to have occurred in the late Miocene, accompanied by erosion and recycling of earlier rift-fill sediments. This deformation may reflect clockwise reorientation of the primary extension direction to its Pliocene and current east-west alignment.\r\n\r\nLate Miocene and early Pliocene uplift and erosion were widespread in the region, as indicated by channeled and local angular unconformities at the bases of all Pliocene units, especially prominent along basin margins. These Pliocene fluvial and alluvial deposits (Ceja and Ancha Formations and Tuerto Gravel) and the upper part of the Cochiti Formation are all conspicuously coarser grained than the Miocene beds they cover, particularly near source areas along the margins of the rift. These observations together indicate that the regional streams flowed at much greater discharge than the Miocene streams and that the Pliocene onset of cooler, wetter climate worldwide was the most likely cause. Despite these higher discharge conditions, it appears there was no Pliocene trunk stream through the rift valley because the youngest Pliocene beds in the basin center are largely fine grained sand, pebbly sand, and sandy silt. No Pliocene cobble-gravel deposits, or thick crossbed sets indicative of major stream discharge, have been documented in the basin center.\r\n\r\nConsiderable evidence indicates significant erosion began in late Pliocene time, coincident with and following eruption of abundant basalt from several local centers at about 2.7-2.6 Ma. The onset of central valley erosion marks the initiation of the first through-flowing, high-energy trunk stream (the 'ancestral' Rio Grande), which most likely was caused by integration of drainage southward through the Socorro region. No upper Pliocene fluvial deposits have been identified in the valley center; rather, a significant unconformity separates beds with medial (or earliest late) Blancan fauna (older than about 2.2 Ma) from","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sim2946","isbn":"1411312163","usgsCitation":"Williams, P.L., and Cole, J., 2007, Geologic Map of the Albuquerque 30' x 60' Quadrangle, North-Central New Mexico (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2946, Map: 53 x 41 inches; Pamphlet: iv, 31 p.; Downloads Directory, https://doi.org/10.3133/sim2946.","productDescription":"Map: 53 x 41 inches; Pamphlet: iv, 31 p.; Downloads Directory","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":110734,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_81495.htm","linkFileType":{"id":5,"text":"html"},"description":"81495"},{"id":192425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9875,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2007/2946/","linkFileType":{"id":5,"text":"html"}}],"scale":"1","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107,35 ], [ -107,35.5 ], [ -106,35.5 ], [ -106,35 ], [ -107,35 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8258","contributors":{"authors":[{"text":"Williams, Paul L. (compiler)","contributorId":53904,"corporation":false,"usgs":true,"family":"Williams","given":"Paul","suffix":"(compiler)","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":291674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cole, J. C.","contributorId":21539,"corporation":false,"usgs":true,"family":"Cole","given":"J. C.","affiliations":[],"preferred":false,"id":291673,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":80085,"text":"ofr20071049 - 2007 - Hydrologic, Water-Quality, and Meteorological Data for the Cambridge, Massachusetts, Drinking-Water Source Area, Water Year 2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:17","indexId":"ofr20071049","displayToPublicDate":"2007-07-07T00:00:00","publicationYear":"2007","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":"2007-1049","title":"Hydrologic, Water-Quality, and Meteorological Data for the Cambridge, Massachusetts, Drinking-Water Source Area, Water Year 2005","docAbstract":"Records of water quantity, water quality, and meteorological parameters were continuously collected from three reservoirs, two primary streams, and four subbasin tributaries in the Cambridge, Massachusetts, drinking-water source area during water year 2005 (October 2004 through September 2005). Water samples were collected during base-flow conditions and storms in the subbasins of the Cambridge Reservoir and Stony Brook Reservoir drainage areas and analyzed for selected elements, organic constituents, suspended sediment, and Escherichia coli bacteria. These data were collected to assist watershed administrators in managing the drinking-water source area and to identify potential sources of contaminants and trends in contaminant loading to the water supply.\r\n\r\nMonthly reservoir capacities for the Cambridge Reservoir varied from about 59 to 98 percent during water year 2005, while monthly reservoir capacities for the Stony Brook Reservoir and the Fresh Pond Reservoir were maintained at capacities greater than 84 and 96 percent, respectively. Assuming a water demand of 15 million gallons per day by the city of Cambridge, the volume of water released from the Stony Brook Reservoir to the Charles River during the 2005 water year is equivalent to an annual water surplus of about 119 percent. Recorded precipitation in the source area for the 2005 water year was within 2 inches of the total annual precipitation for the previous 2 water years.\r\n\r\nThe monthly mean specific conductances for the outflow of the Cambridge Reservoir were similar to historical monthly mean values. However, monthly mean specific conductances for Stony Brook near Route 20, in Waltham (U.S. Geological Survey station 01104460), which is the principal tributary feeding the Stony Brook Reservoir, were generally higher than the medians of the monthly mean specific conductances for the period of record. Similarly, monthly mean specific conductances for a small tributary to Stony Brook (U.S. Geological Survey station 01104455) were generally higher than the medians of the monthly mean specific conductances for the period of record. The annual mean specific conductance for Fresh Pond Reservoir increased from 514 microsiemens per centimeter (?S/cm) in the 2004 water year to 553 ?S/cm for the 2005 water year.\r\n\r\nWater samples were collected from four tributaries during base-flow and stormflow conditions in December 2004, and July, August, and September 2005 and analyzed for suspended sediment, 6 major dissolved ions, total nitrogen, total phosphorus, 8 total metals, 18 polyaromatic hydrocarbons (PAHs), 61 pesticides and metabolites, and Escherichia coli bacteria. Concentrations for most dissolved constituents in samples of stormwater were generally lower than the concentrations observed in samples collected during base flow; however, concentrations of total phosphorus, PAHs, suspended sediment, and some total recoverable metals were substantially greater in stormwater samples.\r\n\r\nConcentrations of dissolved chloride and total recoverable manganese in water samples collected during base-flow conditions from three tributaries exceeded the U.S. Environmental Protection Agency (USEPA) secondary drinking water standards of 250 and 0.05 milligrams per liter (mg/L), respectively. Concentrations of total recoverable manganese exceeded the secondary drinking water standard in samples of stormwater from each tributary. Concentrations of total recoverable iron in water samples exceeded the (USEPA) secondary drinking water standard of 0.3 mg/L periodically in water samples collected at (USEPA) stations 01104415, 01104455, and 01104475, and consistently in all water samples collected at USGS station 01104433.\r\n\r\nConcentrations of Escherichia coli bacteria in water samples collected during base flow ranged from 4 to 1,400 colony-forming units per 100 milliliters (col/100mL). Concentrations of Escherichia coli bacteria in composite samples of stormwater ranged between 1,700 to 43,000 c","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20071049","collaboration":"Prepared in cooperation with the City of Cambridge, Massachusetts, Water Department","usgsCitation":"Smith, K.P., 2007, Hydrologic, Water-Quality, and Meteorological Data for the Cambridge, Massachusetts, Drinking-Water Source Area, Water Year 2005: U.S. Geological Survey Open-File Report 2007-1049, vi, 119 p., https://doi.org/10.3133/ofr20071049.","productDescription":"vi, 119 p.","additionalOnlineFiles":"Y","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":377,"text":"Massachusetts-Rhode Island Water Science Center","active":false,"usgs":true}],"links":[{"id":191447,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9874,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1049/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.33333333333333,42.333333333333336 ], [ -71.33333333333333,42.46666666666667 ], [ -71.1,42.46666666666667 ], [ -71.1,42.333333333333336 ], [ -71.33333333333333,42.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688ed9","contributors":{"authors":[{"text":"Smith, Kirk P. 0000-0003-0269-474X kpsmith@usgs.gov","orcid":"https://orcid.org/0000-0003-0269-474X","contributorId":1516,"corporation":false,"usgs":true,"family":"Smith","given":"Kirk","email":"kpsmith@usgs.gov","middleInitial":"P.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":291672,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":80084,"text":"ofr20071195 - 2007 - Comparisons of Water Quality and Biological Variables from Colorado River Shoreline Habitats in Grand Canyon, Arizona, under Steady and Fluctuating Discharges from Glen Canyon Dam","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"ofr20071195","displayToPublicDate":"2007-07-04T00:00:00","publicationYear":"2007","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":"2007-1195","title":"Comparisons of Water Quality and Biological Variables from Colorado River Shoreline Habitats in Grand Canyon, Arizona, under Steady and Fluctuating Discharges from Glen Canyon Dam","docAbstract":"Glen Canyon Dam operations are known to affect mainstem Colorado River temperature and shoreline habitats for native fish. Options for ameliorating the impacts that operations have on young native fish include changing release volumes and/or changing the daily range of releases. Long-term alterations of operations that may produce a measurable biological response can be costly, particularly if the treatment involves reduced power generation. In September and October 2005, a series of two-week releases occurred that alternated between daily fluctuations that varied by 76 m3 s-1 and steady releases. The purpose of these short-term experiments was to study the effect of daily operations on water quality parameters and biotic constituents (phytoplankton, macroinvertebrates, and fishes) of associated shoreline habitats. Our results indicate that measured biological and physical parameters were, in general, unaffected by flow treatments. However, results should be interpreted cautiously as time within and between treatments was likely insufficient to affect measured parameters. These results lead to the recommendation that studies like this may be more amenable to laboratory experiments first and then applied to a large-scale setting, preferably for longer duration.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20071195","collaboration":"Prepared in cooperation with SWCA Environmental Consultants, Inc.","usgsCitation":"Ralston, B., Lauretta, M.V., and Kennedy, T., 2007, Comparisons of Water Quality and Biological Variables from Colorado River Shoreline Habitats in Grand Canyon, Arizona, under Steady and Fluctuating Discharges from Glen Canyon Dam (Version 1.0): U.S. Geological Survey Open-File Report 2007-1195, 29 p., https://doi.org/10.3133/ofr20071195.","productDescription":"29 p.","onlineOnly":"Y","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":192760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9873,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1195/","linkFileType":{"id":5,"text":"html"}}],"scale":"1400000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,35 ], [ -114,37.5 ], [ -111,37.5 ], [ -111,35 ], [ -114,35 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa681","contributors":{"authors":[{"text":"Ralston, Barbara E.","contributorId":89848,"corporation":false,"usgs":true,"family":"Ralston","given":"Barbara E.","affiliations":[],"preferred":false,"id":291671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lauretta, Matthew V.","contributorId":60729,"corporation":false,"usgs":true,"family":"Lauretta","given":"Matthew","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":291670,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kennedy, Theodore A. 0000-0003-3477-3629","orcid":"https://orcid.org/0000-0003-3477-3629","contributorId":50227,"corporation":false,"usgs":true,"family":"Kennedy","given":"Theodore A.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":291669,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":80083,"text":"sir20065239 - 2007 - Hydrogeology and Aquifer Storage and Recovery Performance in the Upper Floridan Aquifer, Southern Florida","interactions":[],"lastModifiedDate":"2012-02-10T00:11:38","indexId":"sir20065239","displayToPublicDate":"2007-07-04T00:00:00","publicationYear":"2007","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":"2006-5239","title":"Hydrogeology and Aquifer Storage and Recovery Performance in the Upper Floridan Aquifer, Southern Florida","docAbstract":" Well construction, hydraulic well test, ambient water-quality, and cycle test data were inventoried and compiled for 30 aquifer storage and recovery facilities constructed in the Floridan aquifer system in southern Florida. Most of the facilities are operated by local municipalities or counties in coastal areas, but five sites are currently being evaluated as part of the Comprehensive Everglades Restoration Plan. The relative performance of all sites with adequate cycle test data was determined, and compared with four hydrogeologic and design factors that may affect recovery efficiency.\r\n Testing or operational cycles include recharge, storage, and recovery periods that each last days or months. Cycle test data calculations were made including the potable water (chloride concentration of less than 250 milligrams per liter) recovery efficiency per cycle, total recovery efficiency per cycle, and cumulative potable water recovery efficiencies for all of the cycles at each site. The potable water recovery efficiency is the percentage of the total amount of potable water recharged for each cycle that is recovered; potable water recovery efficiency calculations (per cycle and cumulative) were the primary measures used to evaluate site performance in this study. Total recovery efficiency, which is the percent recovery at the end of each cycle, however, can be substantially higher and is the performance measure normally used in the operation of water-treatment plants.\r\n The Upper Floridan aquifer of the Floridan aquifer system currently is being used, or planned for use, at 29 of the aquifer storage and recovery sites. The Upper Floridan aquifer is continuous throughout southern Florida, and its overlying confinement is generally good; however, the aquifer contains brackish to saline ground water that can greatly affect freshwater storage and recovery due to dispersive mixing within the aquifer. The hydrogeology of the Upper Floridan varies in southern Florida; confinement between flow zones is better in southwestern Florida than in southeastern Florida. Vertical hydraulic conductivity in the upper part of the aquifer also may be higher in southeastern Florida because of unconformities present at formation contacts within the aquifer that may be better developed in this area.\r\n Recovery efficiencies per cycle varied widely. Eight sites had recovery efficiencies of less than about 10 percent for the first cycle, and three of these sites had not yet achieved recoveries exceeding 10 percent, even after three to five cycles. The highest recovery efficiency achieved per cycle was 94 percent. Three southeastern coastal sites and two southwestern coastal sites have achieved potable water recoveries per cycle exceeding 60 percent. One of the southeastern coastal sites and both of the southwestern coastal sites achieved good recoveries, even with long storage periods (from 174 to 191 days). The high recovery efficiencies for some cycles apparently resulted from water banking?an operational approach whereby an initial cycle with a large recharge volume of water is followed by cycles with much smaller recharge volume. This practice flushes out the aquifer around the well and builds up a buffer zone that can maintain high recovery efficiency in the subsequent cycles.\r\n The relative performance of all sites with adequate cycle test data was determined. Performance was arbitrarily grouped into ?high? (greater than 40 percent), ?medium? (between 20 and 40 percent), and ?low? (less than 20 percent) categories based primarily on their cumulative recovery efficiency for the first seven cycles, or projected to seven cycles if fewer cycles were conducted. The ratings of three sites, considered to be borderline, were modified using the overall recharge rate derived from the cumulative recharge volumes. A higher overall recharge rate (greater than 300 million gallons per year) can improve recovery efficiency because of the water-bankin","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20065239","collaboration":"Prepared as part of the U.S. Geological Survey Greater Everglades Priority Ecosystems Science Initiative","usgsCitation":"Reese, R.S., and Alvarez-Zarikian, C.A., 2007, Hydrogeology and Aquifer Storage and Recovery Performance in the Upper Floridan Aquifer, Southern Florida: U.S. Geological Survey Scientific Investigations Report 2006-5239, vi, 114 p., https://doi.org/10.3133/sir20065239.","productDescription":"vi, 114 p.","additionalOnlineFiles":"Y","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":192409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9872,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5239/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83,24.5 ], [ -83,27.5 ], [ -80,27.5 ], [ -80,24.5 ], [ -83,24.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627855","contributors":{"authors":[{"text":"Reese, Ronald S. rsreese@usgs.gov","contributorId":1090,"corporation":false,"usgs":true,"family":"Reese","given":"Ronald","email":"rsreese@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":291667,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alvarez-Zarikian, Carlos A.","contributorId":83606,"corporation":false,"usgs":true,"family":"Alvarez-Zarikian","given":"Carlos","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":291668,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":80081,"text":"fs20073047 - 2007 - Hawaiian Duck's Future Threatened by Feral Mallards","interactions":[],"lastModifiedDate":"2015-03-30T10:10:07","indexId":"fs20073047","displayToPublicDate":"2007-07-04T00:00:00","publicationYear":"2007","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":"2007-3047","title":"Hawaiian Duck's Future Threatened by Feral Mallards","docAbstract":"Nearly 70 percent of Hawaii's native bird species are found nowhere else on Earth, and many of these species are declining or in danger of extinction. Although the Hawaiian Islands were once home to a remarkable diversity of waterfowl, only three species remain-the Hawaiian Goose (Nene), Laysan Duck, and Hawaiian Duck (Koloa maoli)-all Federally endangered. The Koloa maoli is the only Hawaiian bird threatened by 'genetic extinction' from hybridization with an invasive species-feral Mallard ducks. U.S. Geological Survey (USGS) biologists in Hawaii are working to find the causes of bird endangerment and ways to prevent extinction of the Koloa maoli and other threatened birds.
","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20073047","usgsCitation":"Uyehara, K.J., Engilis, A., and Reynolds, M., 2007, Hawaiian Duck's Future Threatened by Feral Mallards (Version 1.0): U.S. Geological Survey Fact Sheet 2007-3047, 4 p., https://doi.org/10.3133/fs20073047.","productDescription":"4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":124125,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2007_3047.jpg"},{"id":299120,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2007/3047/fs2007-3047.pdf","text":"Report","size":"5.6 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":9870,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2007/3047/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63f25f","contributors":{"authors":[{"text":"Uyehara, Kimberly J.","contributorId":93990,"corporation":false,"usgs":true,"family":"Uyehara","given":"Kimberly","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":291660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engilis, Andrew Jr.","contributorId":92362,"corporation":false,"usgs":true,"family":"Engilis","given":"Andrew","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":291659,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reynolds, Michelle","contributorId":49877,"corporation":false,"usgs":true,"family":"Reynolds","given":"Michelle","affiliations":[],"preferred":false,"id":291658,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":80082,"text":"ofr20071173 - 2007 - Water-Quality and Lake-Stage Data for Wisconsin Lakes, Water Year 2006","interactions":[],"lastModifiedDate":"2018-02-06T12:19:42","indexId":"ofr20071173","displayToPublicDate":"2007-07-04T00:00:00","publicationYear":"2007","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":"2007-1173","title":"Water-Quality and Lake-Stage Data for Wisconsin Lakes, Water Year 2006","docAbstract":"The U.S. Geological Survey (USGS), in cooperation with local and other agencies, collects data at selected lakes throughout Wisconsin. These data, accumulated over many years, provide a data base for developing an improved understanding of the water quality of lakes. To make these data available to interested parties outside the USGS, the data are published annually in this report series. The locations of water-quality and lake-stage stations in Wisconsin for water year 2006 are shown in figure 1. A water year is the 12-month period from October 1 through September 30. It is designated by the calendar year in which it ends. Thus, the period October 1, 2005 through September 30, 2006 is called 'water year 2006.'\r\n\r\nThe purpose of this report is to provide information about the chemical and physical characteristics of Wisconsin lakes. Data that have been collected at specific lakes, and information to aid in the interpretation of those data, are included in this report. Data collected include measurements of in-lake water quality and lake stage. Time series of Secchi depths, surface total phosphorus and chlorophyll a concentrations collected during non-frozen periods are included for all lakes. Graphs of vertical profiles of temperature, dissolved oxygen, pH, and specific conductance are included for sites where these parameters were measured. Descriptive information for each lake includes: location of the lake, area of the lake's watershed, period for which data are available, revisions to previously published records, and pertinent remarks. Additional data, such as streamflow and water quality in tributary and outlet streams of some of the lakes, are published in another volume: 'Water Resources Data-Wisconsin, 2006.'\r\n\r\nWater-resources data, including stage and discharge data at most streamflow-gaging stations, are available through the World Wide Web on the Internet. The Wisconsin Water Science Center's home page is at http://wi.water.usgs.gov/. Information on the Wisconsin Water Science Center's Lakes Program is found at http://wi.water.usgs.gov/lake/index.html and http://wi.water.usgs.gov/projects/index.html.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20071173","collaboration":"Prepared in cooperation with the State of Wisconsin and local agencies","usgsCitation":"Rose, W.J., Garn, H., Goddard, G.L., Marsh, S., Olson, D., and Robertson, D.M., 2007, Water-Quality and Lake-Stage Data for Wisconsin Lakes, Water Year 2006: U.S. Geological Survey Open-File Report 2007-1173, vi, 186 p., https://doi.org/10.3133/ofr20071173.","productDescription":"vi, 186 p.","temporalStart":"2005-10-01","temporalEnd":"2006-09-30","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":9871,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1173/","linkFileType":{"id":5,"text":"html"}},{"id":192111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -93,42 ], [ -93,48 ], [ -86,48 ], [ -86,42 ], [ -93,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fca51","contributors":{"authors":[{"text":"Rose, W. J.","contributorId":14433,"corporation":false,"usgs":true,"family":"Rose","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":291662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garn, H.S.","contributorId":42601,"corporation":false,"usgs":true,"family":"Garn","given":"H.S.","affiliations":[],"preferred":false,"id":291665,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goddard, G. L.","contributorId":10442,"corporation":false,"usgs":true,"family":"Goddard","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":291661,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marsh, S.B.","contributorId":105329,"corporation":false,"usgs":true,"family":"Marsh","given":"S.B.","email":"","affiliations":[],"preferred":false,"id":291666,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Olson, D.L.","contributorId":34943,"corporation":false,"usgs":true,"family":"Olson","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":291663,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Robertson, Dale M. 0000-0001-6799-0596 dzrobert@usgs.gov","orcid":"https://orcid.org/0000-0001-6799-0596","contributorId":150760,"corporation":false,"usgs":true,"family":"Robertson","given":"Dale","email":"dzrobert@usgs.gov","middleInitial":"M.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":291664,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70176951,"text":"70176951 - 2007 - Current and potential ant impacts in the Pacific region","interactions":[],"lastModifiedDate":"2018-01-04T13:05:23","indexId":"70176951","displayToPublicDate":"2007-07-04T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5150,"text":"Proceedings of the Hawaiian Entomological Society ","active":true,"publicationSubtype":{"id":10}},"title":"Current and potential ant impacts in the Pacific region","docAbstract":"Worldwide, ants are a powerful ecological force, and they appear to be dominant components of animal communities of many tropical and temperate ecosystems in terms of biomass and numbers of individuals (Bluthgen et al. 2000). For example, ants comprise up to 94% of arthropod individuals in fogging samples taken from diverse lowland tropical rainforest canopies, and 86% of the biomass (Davidson et al. 2003). The majority of these ant species and individuals obtain carbohydrates either from extrafloral nectaries or from sap-feeding Hemiptera that pass carbohydrate-rich “honeydew” to attending ants while concentrating nitrogen (N) from N-poor plant sap (Davidson et al. 2003). Honeydew and nectar represent key resources for arboreal ant species, although most ant species are at least partly carnivorous or scavengers (Bluthgen et al. 2004).
In contrast to most of the terrestrial world, the biotas of many Pacific islands evolved without ants. Whereas endemic ant species are found in New Zealand (ca. 10 spp.), Tonga (ca. 10 spp.), and Samoa (ca. 12 spp.), other islands of Polynesia and parts of Micronesia likely lack native ants (Wilson and Taylor 1967, Wetterer 2002, Wetterer and Vargo 2003). About 20 Indo-Australian and western Pacific ant species range to the east and north of Samoa, but it is unclear how many of these were transported there by humans at some time (Wilson and Taylor 1967). Most of the remainder of the ant species currently found on Pacific islands are widespread species that fall in the category of “tramp species,” dispersed by recent human commerce and generally closely tied to human activity and urban areas (Wilson and Taylor 1967, McGlynn 1999). In Pacific island situations, some of these tramp ant species are able to thrive beyond areas of human activity.
Relatively few ant species have been successful invaders of native communities on continents, and these include most of the species that pose the greatest problems for Pacific islands. They generally have multiple queens per colony, are unicolonial (lacking internest aggression), quickly recruit to food items, thrive in a variety of habitats including disturbed areas, and can be highly aggressive to other ant species (McGlynn 1999).
Hawaii’s arthropod fauna evolved in the absence of ants and has been observed by many biologists to be highly vulnerable to displacement by non-native ants. Pacific island biotas have also very likely suffered greatly from displacement by ants. However, in contrast to Hawaii, virtually nothing has been published on effects of non-native ants on native arthropod fauna elsewhere on Pacific islands, with the exception of the Galapagos archipelago, which may have at least four species of endemic ants (Lubin 1984, Nishida and Evenhuis 2000) and New Caledonia (Jourdan et al. 2001, Le Breton et al. 2005). In addition, many ant species in the Pacific have long been a nuisance for humans, and significant agricultural impacts have occurred from ants tending hemipteran insects of crop plants.
","language":"English","publisher":"Hawaiian Entomological Society","publisherLocation":"Honolulu, HI","usgsCitation":"Loope, L.L., and Krushelnycky, P.D., 2007, Current and potential ant impacts in the Pacific region: Proceedings of the Hawaiian Entomological Society , v. 36, p. 69-73.","startPage":"69","endPage":"73","numberOfPages":"5","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":329541,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Pacific region","volume":"36","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdf00e4b0824b2d179d08","contributors":{"authors":[{"text":"Loope, Lloyd L.","contributorId":107848,"corporation":false,"usgs":true,"family":"Loope","given":"Lloyd","email":"","middleInitial":"L.","affiliations":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"preferred":false,"id":650841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krushelnycky, Paul D.","contributorId":24252,"corporation":false,"usgs":true,"family":"Krushelnycky","given":"Paul","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":650842,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":80078,"text":"ofr20071190 - 2007 - Geophysical Data from Spring Valley to Delamar Valley, East-Central Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:11:40","indexId":"ofr20071190","displayToPublicDate":"2007-07-03T00:00:00","publicationYear":"2007","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":"2007-1190","title":"Geophysical Data from Spring Valley to Delamar Valley, East-Central Nevada","docAbstract":"Cenozoic basins in eastern Nevada and western Utah constitute major ground-water recharge areas in the eastern part of the Great Basin and these were investigated to characterize the geologic framework of the region. Prior to these investigations, regional gravity coverage was variable over the region, adequate in some areas and very sparse in others. Cooperative studies described herein have established 1,447 new gravity stations in the region, providing a detailed description of density variations in the middle to upper crust. All previously available gravity data for the study area were evaluated to determine their reliability, prior to combining with our recent results and calculating an up-to-date isostatic residual gravity map of the area. A gravity inversion method was used to calculate depths to pre-Cenozoic basement rock and estimates of maximum alluvial/volcanic fill in the major valleys of the study area. The enhanced gravity coverage and the incorporation of lithologic information from several deep oil and gas wells yields a much improved view of subsurface shapes of these basins and provides insights useful for the development of hydrogeologic models for the region.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20071190","collaboration":"In Cooperation with the Southern Nevada Water Authority (SNWA)","usgsCitation":"Mankinen, E.A., Roberts, C.W., McKee, E.H., Chuchel, B.A., and Morin, R.L., 2007, Geophysical Data from Spring Valley to Delamar Valley, East-Central Nevada (Version 1.0): U.S. Geological Survey Open-File Report 2007-1190, Report: 42 p.; Data, https://doi.org/10.3133/ofr20071190.","productDescription":"Report: 42 p.; Data","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":314,"text":"Geophysics Unit of Menlo Park, CA (GUMP)","active":false,"usgs":true}],"links":[{"id":192059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9867,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1190/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115,37 ], [ -115,40 ], [ -113.5,40 ], [ -113.5,37 ], [ -115,37 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c470","contributors":{"authors":[{"text":"Mankinen, Edward A. 0000-0001-7496-2681 emank@usgs.gov","orcid":"https://orcid.org/0000-0001-7496-2681","contributorId":1054,"corporation":false,"usgs":true,"family":"Mankinen","given":"Edward","email":"emank@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":291648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, Carter W.","contributorId":45282,"corporation":false,"usgs":true,"family":"Roberts","given":"Carter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":291651,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":291650,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chuchel, Bruce A. chuchel@usgs.gov","contributorId":2415,"corporation":false,"usgs":true,"family":"Chuchel","given":"Bruce","email":"chuchel@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":291649,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Morin, Robert L.","contributorId":82671,"corporation":false,"usgs":true,"family":"Morin","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":291652,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":80077,"text":"sir20075094 - 2007 - Preliminary volcano-hazard assessment for the Tanaga volcanic cluster, Tanaga Island, Alaska","interactions":[],"lastModifiedDate":"2019-02-25T09:53:37","indexId":"sir20075094","displayToPublicDate":"2007-07-03T00:00:00","publicationYear":"2007","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":"2007-5094","title":"Preliminary volcano-hazard assessment for the Tanaga volcanic cluster, Tanaga Island, Alaska","docAbstract":"Summary of Volcano Hazards at Tanaga Volcanic Cluster The Tanaga volcanic cluster lies on the northwest part of Tanaga Island, about 100 kilometers west of Adak, Alaska, and 2,025 kilometers southwest of Anchorage, Alaska. The cluster consists of three volcanoes-from west to east, they are Sajaka, Tanaga, and Takawangha. All three volcanoes have erupted in the last 1,000 years, producing lava flows and tephra (ash) deposits. A much less frequent, but potentially more hazardous phenomenon, is volcanic edifice collapse into the sea, which likely happens only on a timescale of every few thousands of years, at most. Parts of the volcanic bedrock near Takawangha have been altered by hydrothermal activity and are prone to slope failure, but such events only present a local hazard. Given the volcanic cluster's remote location, the primary hazard from the Tanaga volcanoes is airborne ash that could affect aircraft. In this report, we summarize the major volcanic hazards associated with the Tanaga volcanic cluster.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20075094","usgsCitation":"Coombs, M.L., McGimsey, R.G., and Browne, B., 2007, Preliminary volcano-hazard assessment for the Tanaga volcanic cluster, Tanaga Island, Alaska: U.S. Geological Survey Scientific Investigations Report 2007-5094, Report: vi, 37 p.; Plate: 30 x 20 inches, https://doi.org/10.3133/sir20075094.","productDescription":"Report: vi, 37 p.; Plate: 30 x 20 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":190844,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9866,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2007/5094/","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","projection":"Albers Equal Area Conic","country":"United States","state":"Alaska","otherGeospatial":"Tanaga Volcanic Cluster","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614253","contributors":{"authors":[{"text":"Coombs, Michelle L. 0000-0002-6002-6806 mcoombs@usgs.gov","orcid":"https://orcid.org/0000-0002-6002-6806","contributorId":2809,"corporation":false,"usgs":true,"family":"Coombs","given":"Michelle","email":"mcoombs@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":291646,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGimsey, Robert G. 0000-0001-5379-7779 mcgimsey@usgs.gov","orcid":"https://orcid.org/0000-0001-5379-7779","contributorId":2352,"corporation":false,"usgs":true,"family":"McGimsey","given":"Robert","email":"mcgimsey@usgs.gov","middleInitial":"G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":291645,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Browne, Brandon L.","contributorId":21646,"corporation":false,"usgs":true,"family":"Browne","given":"Brandon L.","affiliations":[],"preferred":false,"id":291647,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":80080,"text":"sir20075005 - 2007 - PONDCALC: A tool to estimate discharge from the Alviso Salt Ponds, California","interactions":[],"lastModifiedDate":"2024-07-01T18:34:33.026978","indexId":"sir20075005","displayToPublicDate":"2007-07-03T00:00:00","publicationYear":"2007","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":"2007-5005","title":"PONDCALC: A tool to estimate discharge from the Alviso Salt Ponds, California","docAbstract":"Former commercial salt ponds in Alviso, California, now are operated by the U.S. Fish and Wildlife Service (USFWS) to provide habitat for birds. The USFWS has modified the operation of the ponds to prevent exceedingly high salinity. Ponds that were formerly hydraulically isolated from South San Francisco Bay and adjacent sloughs now are managed as flow-through ponds, and some are allowed to discharge to the Bay and sloughs. This discharge is allowed under a permit issued by the Regional Water Quality Control Board. As a requirement of the permit, the USFWS must estimate the amount of discharge from each discharge pond for the period May through November of each year. To facilitate the accurate estimation of pond discharge, a calculation methodology (hereafter referred to as 'calculator' or PONDCALC) for the discharging Alviso ponds has been developed as a Microsoft Excel file and is presented in this report. The presence of flap gates on one end of the discharge culverts, which allow only outflow from a pond, complicates the hydraulic analysis of flow through the culverts. The equation typically used for culvert flow contains an energy loss coefficient that had to be determined empirically using measured water discharge and head at the discharge structure of one of the ponds. A standard weir-flow equation is included in PONDCALC for discharge calculation in the ponds having weir box structures in addition to culverts. The resulting methodology is applicable only to the five Alviso ponds (A2W, A3W, A7, A14, and A16) that discharge to South San Francisco Bay or adjacent sloughs under the management practices for 2005.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20075005","collaboration":"Prepared in cooperation with the U.S. Fish and Wildlife Service","usgsCitation":"Shellenbarger, G., Schoellhamer, D., and Lionberger, M., 2007, PONDCALC: A tool to estimate discharge from the Alviso Salt Ponds, California: U.S. Geological Survey Scientific Investigations Report 2007-5005, vi, 12 p., https://doi.org/10.3133/sir20075005.","productDescription":"vi, 12 p.","additionalOnlineFiles":"Y","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":430678,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_81491.htm","linkFileType":{"id":5,"text":"html"}},{"id":9869,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2007/5005/","linkFileType":{"id":5,"text":"html"}},{"id":194842,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Alviso Salt Ponds","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.09883923989116,\n 37.42784265679187\n ],\n [\n -121.98409404393976,\n 37.38513390208625\n ],\n [\n -121.89377068730562,\n 37.449934689562426\n ],\n [\n -121.93488835367184,\n 37.48357412131861\n ],\n [\n -122.04068118573318,\n 37.51395325611291\n ],\n [\n -122.06647625298967,\n 37.576468030102944\n ],\n [\n -122.07843717685319,\n 37.57752130183435\n ],\n [\n -122.19274180694762,\n 37.49004794282594\n ],\n [\n -122.09883923989116,\n 37.42784265679187\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ec6","contributors":{"authors":[{"text":"Shellenbarger, Gregory gshellen@usgs.gov","contributorId":1133,"corporation":false,"usgs":true,"family":"Shellenbarger","given":"Gregory","email":"gshellen@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":291656,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoellhamer, David H. 0000-0001-9488-7340 dschoell@usgs.gov","orcid":"https://orcid.org/0000-0001-9488-7340","contributorId":631,"corporation":false,"usgs":true,"family":"Schoellhamer","given":"David H.","email":"dschoell@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":291655,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lionberger, Megan A.","contributorId":29904,"corporation":false,"usgs":true,"family":"Lionberger","given":"Megan A.","affiliations":[],"preferred":false,"id":291657,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":80079,"text":"ds258 - 2007 - Ground-water quality data in the Monterey Bay and Salinas Valley Basins, California, 2005— Results from the California GAMA program","interactions":[],"lastModifiedDate":"2021-09-15T19:13:32.416447","indexId":"ds258","displayToPublicDate":"2007-07-03T00:00:00","publicationYear":"2007","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":"258","title":"Ground-water quality data in the Monterey Bay and Salinas Valley Basins, California, 2005— Results from the California GAMA program","docAbstract":"Ground-water quality in the approximately 1,000-square-mile Monterey Bay and Salinas Valley study unit was investigated from July through October 2005 as part of the California Ground-Water Ambient Monitoring and Assessment (GAMA) program. The study was designed to provide a spatially unbiased assessment of raw ground-water quality, as well as a statistically consistent basis for comparing water quality throughout California. Samples were collected from 94 public-supply wells and 3 monitoring wells in Monterey, Santa Cruz, and San Luis Obispo Counties. Ninety-one of the public-supply wells sampled were selected to provide a spatially distributed, randomized monitoring network for statistical representation of the study area. Six wells were sampled to evaluate changes in water chemistry: three wells along a ground-water flow path were sampled to evaluate lateral changes, and three wells at discrete depths from land surface were sampled to evaluate changes in water chemistry with depth from land surface.\r\n\r\nThe ground-water samples were analyzed for volatile organic compounds (VOCs), pesticides, pesticide degradates, nutrients, major and minor ions, trace elements, radioactivity, microbial indicators, and dissolved noble gases (the last in collaboration with Lawrence Livermore National Laboratory). Naturally occurring isotopes (tritium, carbon-14, helium-4, and the isotopic composition of oxygen and hydrogen) also were measured to help identify the source and age of the sampled ground water. In total, 270 constituents and water-quality indicators were investigated for this study. This study did not attempt to evaluate the quality of water delivered to consumers; after withdrawal from the ground, water typically is treated, disinfected, and (or) blended with other waters to maintain water quality. In addition, regulatory thresholds apply to treated water that is served to the consumer, not to raw ground water.\r\n\r\nIn this study, only six constituents, alpha radioactivity, N-nitrosodimethylamine, 1,2,3-trichloropropane, nitrate, radon-222, and coliform bacteria were detected at concentrations higher than health-based regulatory thresholds. Six constituents, including total dissolved solids, hexavalent chromium, iron, manganese, molybdenum, and sulfate were detected at concentrations above levels set for aesthetic concerns.\r\n\r\nOne-third of the randomized wells sampled for the Monterey Bay and Salinas Valley GAMA study had at least a single detection of a VOC or gasoline additive. Twenty-eight of the 88 VOCs and gasoline additives investigated were found in ground-water samples; however, detected concentrations were one-third to one-sixty-thousandth of their respective regulatory thresholds. Compounds detected in 10 percent or more of the wells sampled include chloroform, a compound resulting from the chlorination of water, and tetrachloroethylene (PCE), a common solvent.\r\n\r\nPesticides and pesticide degradates also were detected in one-third of the ground-water samples collected; however, detected concentrations were one-thirtieth to one-fourteen-thousandth of their respective regulatory thresholds. Ten of the 122 pesticides and pesticide degradates investigated were found in ground-water samples. Compounds detected in 10 percent or more of the wells sampled include the herbicide simazine, and the pesticide degradate deethylatrazine.\r\n\r\nGround-water samples had a median total dissolved solids (TDS) concentration of 467 milligrams per liter (mg/L), and 16 of the 34 samples had TDS concentrations above the recommended secondary maximum contaminant level (SMCL-a threshold established for aesthetic qualities: taste, odor, and color) of 500 mg/L, while four samples had concentrations above the upper SMCL of 1,000 mg/L. Concentrations of nitrate plus nitrite ranged from 0.04 to 37.8 mg/L (as nitrogen), and two samples had concentrations above the health-based threshold for nitrate of 10 mg/L (as nitrogen). The median sulfate concentration","language":"English","publisher":"Geological Survey (U.S.)","doi":"10.3133/ds258","usgsCitation":"Kulongoski, J., and Belitz, K., 2007, Ground-water quality data in the Monterey Bay and Salinas Valley Basins, California, 2005— Results from the California GAMA program: U.S. Geological Survey Data Series 258, x, 84 p., https://doi.org/10.3133/ds258.","productDescription":"x, 84 p.","additionalOnlineFiles":"Y","temporalStart":"2005-07-01","temporalEnd":"2005-10-31","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":194915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9868,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2007/258/","linkFileType":{"id":5,"text":"html"}},{"id":389287,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_81494.htm"}],"projection":"Albers Equal Area Conic","country":"United States","state":"California","otherGeospatial":"Monterey Bay and Salinas Valley Basins","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.14599609375001,\n 34.994003757575776\n ],\n [\n -120.43212890625,\n 34.994003757575776\n ],\n [\n -120.43212890625,\n 37.37015718405753\n ],\n [\n -122.14599609375001,\n 37.37015718405753\n ],\n [\n -122.14599609375001,\n 34.994003757575776\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a85fb","contributors":{"authors":[{"text":"Kulongoski, Justin T. 0000-0002-3498-4154","orcid":"https://orcid.org/0000-0002-3498-4154","contributorId":94750,"corporation":false,"usgs":true,"family":"Kulongoski","given":"Justin T.","affiliations":[],"preferred":false,"id":291654,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":291653,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70179396,"text":"70179396 - 2007 - Fish rhabdovirus models for understanding the host response to DNA vaccines","interactions":[],"lastModifiedDate":"2016-12-30T11:35:33","indexId":"70179396","displayToPublicDate":"2007-07-02T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5249,"text":"CAB Review","active":true,"publicationSubtype":{"id":10}},"title":"Fish rhabdovirus models for understanding the host response to DNA vaccines","docAbstract":"n/a
","language":"English","publisher":"CABI Publishing","doi":"10.1079/PAVSNNR20072048","usgsCitation":"Kurath, G., Purcell, M., and Garver, K.A., 2007, Fish rhabdovirus models for understanding the host response to DNA vaccines: CAB Review, v. 2, no. 48, https://doi.org/10.1079/PAVSNNR20072048.","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":332686,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"48","noUsgsAuthors":false,"publicationDate":"2007-09-05","publicationStatus":"PW","scienceBaseUri":"586781fae4b0cd2dabe7c727","contributors":{"authors":[{"text":"Kurath, Gael 0000-0003-3294-560X gkurath@usgs.gov","orcid":"https://orcid.org/0000-0003-3294-560X","contributorId":2629,"corporation":false,"usgs":true,"family":"Kurath","given":"Gael","email":"gkurath@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":true,"id":657081,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Purcell, Maureen K. mpurcell@usgs.gov","contributorId":138685,"corporation":false,"usgs":true,"family":"Purcell","given":"Maureen K.","email":"mpurcell@usgs.gov","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":657082,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Garver, Kyle A.","contributorId":77816,"corporation":false,"usgs":true,"family":"Garver","given":"Kyle","email":"","middleInitial":"A.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":657083,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70228812,"text":"70228812 - 2007 - High-resolution climate records of the past 2,400 years from the offshore of northernmost California and central Oregon","interactions":[],"lastModifiedDate":"2022-02-22T16:19:23.290952","indexId":"70228812","displayToPublicDate":"2007-07-01T10:08:55","publicationYear":"2007","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"High-resolution climate records of the past 2,400 years from the offshore of northernmost California and central Oregon","docAbstract":"High resolution diatom and pollen data from piston core TN062 0550 off northernmost California, and Kasten core WW7710A-26 off coastal Oregon, are compiled for the past 2,400 years. Diatom proxy data for Fall SST from both cores record warm SST's in the intervals from ca. AD 400 to 600, and from ca. AD 1050 to 1300 (later part of the Medieval Warm Period). The intervening AD 650 to 1000 interval, and the post-AD 1350 interval at both sites appear to be relatively cool. Whereas the pollen assemblage from TN062 0550 is dominated by coastal redwood, the pollen assemblage from WW7710A-26 displays alternating moist-dry cycles of alder vs. pine, as well as cycles of western hemlock (typical of the coastal forests of Oregon) vs. coastal redwood (typical of the coastal forests of northern California). Coincidence of intervals characterized by warmer diatom SST with drier pollen assemblages, and those of cooler diatom SST with moister pollen assemblages in the coastal Oregon core, recall the modern-day association of cool PDO with increased precipitation, and warm PDO with decreased precipitation, in the Pacific Northwest.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the twenty-first annual Pacific climate workshop","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Twenty-first Annual Pacific Climate Workshop","conferenceDate":"March 28-31, 2004","conferenceLocation":"Pacific Grove, CA","language":"English","publisher":"Interagency Ecological Program for the San Francisco Estuary","usgsCitation":"Barron, J.A., and Heusser, L., 2007, High-resolution climate records of the past 2,400 years from the offshore of northernmost California and central Oregon, in Proceedings of the twenty-first annual Pacific climate workshop, Pacific Grove, CA, March 28-31, 2004, 20 p.","productDescription":"20 p.","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":396248,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Oregon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -130.341796875,\n 37.31775185163688\n ],\n [\n -122.78320312499999,\n 37.31775185163688\n ],\n [\n -122.78320312499999,\n 45.66012730272194\n ],\n [\n -130.341796875,\n 45.66012730272194\n ],\n [\n -130.341796875,\n 37.31775185163688\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Starratt, Scott W. 0000-0001-9405-1746 sstarrat@usgs.gov","orcid":"https://orcid.org/0000-0001-9405-1746","contributorId":2891,"corporation":false,"usgs":true,"family":"Starratt","given":"Scott","email":"sstarrat@usgs.gov","middleInitial":"W.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":835615,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Cornelius, Patrica","contributorId":279868,"corporation":false,"usgs":false,"family":"Cornelius","given":"Patrica","email":"","affiliations":[],"preferred":false,"id":835616,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Joelson, James G. Jr.","contributorId":279869,"corporation":false,"usgs":false,"family":"Joelson","given":"James","suffix":"Jr.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":835617,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Barron, John A. 0000-0002-9309-1145 jbarron@usgs.gov","orcid":"https://orcid.org/0000-0002-9309-1145","contributorId":2222,"corporation":false,"usgs":true,"family":"Barron","given":"John","email":"jbarron@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":835622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heusser, Linda E.","contributorId":54203,"corporation":false,"usgs":true,"family":"Heusser","given":"Linda E.","affiliations":[],"preferred":false,"id":835623,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70161246,"text":"70161246 - 2007 - Assessment and control of an invasive aquaculture species: An update on Nile tilapia (Oreochromis niloticus) in coastal Mississippi after Hurricane Katrina","interactions":[],"lastModifiedDate":"2016-06-17T11:37:20","indexId":"70161246","displayToPublicDate":"2007-07-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5031,"text":"Southeastern Fishes Council Proceedings","active":true,"publicationSubtype":{"id":10}},"title":"Assessment and control of an invasive aquaculture species: An update on Nile tilapia (Oreochromis niloticus) in coastal Mississippi after Hurricane Katrina","docAbstract":"We provide information about the effects of Hurricane Katrina on populations of an invasive fish, the Nile tilapia (Oreochromis niloticus) in southern Mississippi. By resampling areas surveyed before the storm, we attempted to determine whether the species expanded its range by moving with storm-related floods. Additionally, we used rotenone to eradicate individuals of this species at a hurricane-damaged aquaculture facility on the Mississippi coast. Although our survey was limited geographically, we did not find the species to occur beyond the aquaculture facility, other than in an adjacent bayou. Our rotenone treatment of the facility appeared effective with only a single O. niloticus being collected six weeks after the treatment. To reduce the spread of O. niloticus in the southeastern U.S., it is important to continue to control feral populations, work to eliminate vectors for dispersal, and continue monitoring their distribution.
","language":"English","publisher":"Southeastern Fishes Council","publisherLocation":"Milledgeville, GA","usgsCitation":"Schofield, P., Slack, W.T., Peterson, M.S., and Gregoire, D.R., 2007, Assessment and control of an invasive aquaculture species: An update on Nile tilapia (Oreochromis niloticus) in coastal Mississippi after Hurricane Katrina: Southeastern Fishes Council Proceedings, v. 49, p. 9-15.","productDescription":"7 p.","startPage":"9","endPage":"15","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"links":[{"id":323880,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":313439,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://trace.tennessee.edu/sfcproceedings/vol1/iss49/"}],"volume":"49","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57651f31e4b07657d19c7883","contributors":{"authors":[{"text":"Schofield, Pamela J. 0000-0002-8752-2797 pschofield@usgs.gov","orcid":"https://orcid.org/0000-0002-8752-2797","contributorId":138883,"corporation":false,"usgs":true,"family":"Schofield","given":"Pamela J.","email":"pschofield@usgs.gov","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":585393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slack, W. Todd","contributorId":151319,"corporation":false,"usgs":false,"family":"Slack","given":"W.","email":"","middleInitial":"Todd","affiliations":[],"preferred":false,"id":585394,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterson, Mark S.","contributorId":8979,"corporation":false,"usgs":true,"family":"Peterson","given":"Mark","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":585395,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gregoire, Denise R.","contributorId":107028,"corporation":false,"usgs":true,"family":"Gregoire","given":"Denise","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":585396,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70174096,"text":"70174096 - 2007 - Viability criteria for steelhead of the south-central and southern California coast","interactions":[],"lastModifiedDate":"2016-08-24T11:02:45","indexId":"70174096","displayToPublicDate":"2007-07-01T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesNumber":"NOAA-TM-NMFS-SWFSC-407","title":"Viability criteria for steelhead of the south-central and southern California coast","docAbstract":"Recovery planning for threatened and endangered steelhead requires measurable, objective criteria for determining an acceptably low risk of extinction. Here we propose viability criteria for two levels of biological organization: individual populations, and groups of populations within the SouthCentral/Southern California Coast Steelhead Recovery Planning Domain. For populations, we adapt criteria commonly used by the IUCN (The World Conservation Union) for identifying at-risk species. For groups of populations we implement a diversity-based “representation and redundancy rule,” in which diversity includes both life-history diversity and biogeographic groupings of populations. The resulting criteria have the potential for straightforward assessment of the risks posed by evolutionary, demographic, environmental, and catastrophic factors; and are designed to use data that are readily collected. However, our prescriptive approach led to one criterion whose threshold could not yet be specified due to inadequate data, and others in which the simplicity of the criteria may render them inefficient for populations with stable run sizes or stable life-history polymorphisms. Both of these problems could likely be solved by directed programs of research and monitoring aimed at developing more efficient (but equally risk-averse) “performance-based criteria.” Of particular utility would be data on the natural fluctuations of populations, research into the stabilizing influence of life-history polymorphisms, and research on the implications of drought, wildfires, and fluvial sediment regimes. Research on estuarine habitat could also yield useful information on the generality and reliability of its role as nursery habitat. Currently, risk assessment at the population level is not possible due to data deficiency, highlighting the need to implement a comprehensive effort to monitor run sizes, anadromous fractions, spawner densities and perhaps marine survival. Assessment at the group level indicates a priority for securing inland populations in the southern Coast Ranges and Transverse Ranges, and a need to maintain not just the fluvial-anadromous life-history form, but also lagoon-anadromous and freshwater-resident forms in each population.
","largerWorkTitle":"NOAA Technical Memorandum NMFS","language":"English","publisher":"National Marine Fisheries Service, NOAA","usgsCitation":"Boughton, D.A., Adams, P.B., Anderson, E., Fusaro, C., Keller, E.A., Kelley, E., Lentsch, L., Nielsen, J.L., Perry, K., Regan, H., Smith, J., Swift, C.C., Thompson, L., and Watson, F., 2007, Viability criteria for steelhead of the south-central and southern California coast (July 2007), 34 p.","productDescription":"34 p.","startPage":"1","endPage":"33","numberOfPages":"41","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":324473,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"July 2007","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57724e36e4b07657d1a819e2","contributors":{"authors":[{"text":"Boughton, David A.","contributorId":172477,"corporation":false,"usgs":false,"family":"Boughton","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":640878,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, Peter B.","contributorId":172478,"corporation":false,"usgs":false,"family":"Adams","given":"Peter","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":640879,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, Eric","contributorId":168940,"corporation":false,"usgs":false,"family":"Anderson","given":"Eric","affiliations":[],"preferred":false,"id":640880,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fusaro, Craig","contributorId":172479,"corporation":false,"usgs":false,"family":"Fusaro","given":"Craig","email":"","affiliations":[],"preferred":false,"id":640881,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Keller, Edward A.","contributorId":106598,"corporation":false,"usgs":true,"family":"Keller","given":"Edward","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":640882,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kelley, Elsie","contributorId":172480,"corporation":false,"usgs":false,"family":"Kelley","given":"Elsie","email":"","affiliations":[],"preferred":false,"id":640883,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lentsch, Leo","contributorId":172481,"corporation":false,"usgs":false,"family":"Lentsch","given":"Leo","email":"","affiliations":[],"preferred":false,"id":640884,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Nielsen, Jennifer L.","contributorId":43722,"corporation":false,"usgs":true,"family":"Nielsen","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":640885,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Perry, Katie","contributorId":172482,"corporation":false,"usgs":false,"family":"Perry","given":"Katie","email":"","affiliations":[],"preferred":false,"id":640886,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Regan, Helen","contributorId":172483,"corporation":false,"usgs":false,"family":"Regan","given":"Helen","affiliations":[],"preferred":false,"id":640887,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Smith, Jerry","contributorId":172484,"corporation":false,"usgs":false,"family":"Smith","given":"Jerry","email":"","affiliations":[],"preferred":false,"id":640888,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Swift, Camm C.","contributorId":139395,"corporation":false,"usgs":false,"family":"Swift","given":"Camm","email":"","middleInitial":"C.","affiliations":[{"id":12725,"text":"Natural History Museum of Los Angeles County","active":true,"usgs":false}],"preferred":false,"id":640889,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Thompson, Lisa","contributorId":172485,"corporation":false,"usgs":false,"family":"Thompson","given":"Lisa","affiliations":[],"preferred":false,"id":640890,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Watson, Fred","contributorId":172486,"corporation":false,"usgs":false,"family":"Watson","given":"Fred","email":"","affiliations":[],"preferred":false,"id":640891,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}} ,{"id":70246280,"text":"70246280 - 2007 - Structure and properties of the San Andreas fault in central California: Recent results from the SAFOD experiment","interactions":[],"lastModifiedDate":"2023-06-30T11:20:12.126178","indexId":"70246280","displayToPublicDate":"2007-06-30T06:17:01","publicationYear":"2007","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3356,"text":"Scientific Drilling","active":true,"publicationSubtype":{"id":10}},"title":"Structure and properties of the San Andreas fault in central California: Recent results from the SAFOD experiment","docAbstract":"No abstract available.
","language":"English","publisher":"Copernicus","doi":"10.2204/iodp.sd.s01.39.2007","usgsCitation":"Hickman, S., Zoback, M., Ellsworth, W., Boness, N., Malin, P., Roecker, S., and Thurber, C., 2007, Structure and properties of the San Andreas fault in central California: Recent results from the SAFOD experiment: Scientific Drilling, p. 29-32, https://doi.org/10.2204/iodp.sd.s01.39.2007.","productDescription":"4 p.","startPage":"29","endPage":"32","costCenters":[],"links":[{"id":476892,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2204/iodp.sd.s01.39.2007","text":"Publisher Index Page"},{"id":418634,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Special Issue","noUsgsAuthors":false,"publicationDate":"2007-11-30","publicationStatus":"PW","contributors":{"authors":[{"text":"Hickman, S.","contributorId":79995,"corporation":false,"usgs":true,"family":"Hickman","given":"S.","email":"","affiliations":[],"preferred":false,"id":876631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zoback, M.","contributorId":17797,"corporation":false,"usgs":true,"family":"Zoback","given":"M.","email":"","affiliations":[],"preferred":false,"id":876632,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellsworth, W.","contributorId":59967,"corporation":false,"usgs":true,"family":"Ellsworth","given":"W.","email":"","affiliations":[],"preferred":false,"id":876633,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boness, N.","contributorId":31218,"corporation":false,"usgs":true,"family":"Boness","given":"N.","affiliations":[],"preferred":false,"id":876634,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Malin, P.","contributorId":19719,"corporation":false,"usgs":true,"family":"Malin","given":"P.","affiliations":[],"preferred":false,"id":876635,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Roecker, S.","contributorId":10173,"corporation":false,"usgs":true,"family":"Roecker","given":"S.","email":"","affiliations":[],"preferred":false,"id":876636,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Thurber, C.","contributorId":107046,"corporation":false,"usgs":true,"family":"Thurber","given":"C.","email":"","affiliations":[],"preferred":false,"id":876637,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":80076,"text":"sir20075117 - 2007 - Relation Between Selected Water-Quality Variables, Climatic Factors, and Lake Levels in Upper Klamath and Agency Lakes, Oregon, 1990-2006","interactions":[],"lastModifiedDate":"2012-03-08T17:16:19","indexId":"sir20075117","displayToPublicDate":"2007-06-30T00:00:00","publicationYear":"2007","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":"2007-5117","title":"Relation Between Selected Water-Quality Variables, Climatic Factors, and Lake Levels in Upper Klamath and Agency Lakes, Oregon, 1990-2006","docAbstract":"Growth and decomposition of dense blooms of Aphanizomenon flos-aquae in Upper Klamath Lake frequently cause extreme water-quality conditions that have led to critical fishery concerns for the region, including the listing of two species of endemic suckers as endangered. The Bureau of Reclamation has asked the U.S. Geological Survey (USGS) to examine water-quality data collected by the Klamath Tribes for relations with lake level. This analysis evaluates a 17-year dataset (1990-2006) and updates a previous USGS analysis of a 5-year dataset (1990-94).\r\n\r\nBoth univariate hypothesis testing and multivariable analyses evaluated using an information-theoretic approach revealed the same results-no one overarching factor emerged from the data. No single factor could be relegated from consideration either. The lack of statistically significant, strong correlations between water-quality conditions, lake level, and climatic factors does not necessarily show that these factors do not influence water-quality conditions; it is more likely that these conditions work in conjunction with each other to affect water quality. A few different conclusions could be drawn from the larger dataset than from the smaller dataset examined in 1996, but for the most part, the outcome was the same. Using an observational dataset that may not capture all variation in water-quality conditions (samples were collected on a two-week interval) and that has a limited range of conditions for evaluation (confined to the operation of lake) may have confounded the exploration of explanatory factors. In the end, all years experienced some variation in poor water-quality conditions, either in timing of occurrence of the poor conditions or in their duration. The dataset of 17 years simply provided 17 different patterns of lake level, cumulative degree-days, timing of the bloom onset, and poor water-quality conditions, with no overriding causal factor emerging from the variations.\r\n\r\nWater-quality conditions were evaluated for their potential to be harmful to the endangered sucker species on the basis of high-stress thresholds-water temperature values greater than 28 degrees Celsius, dissolved-oxygen concentrations less than 4 milligrams per liter, and pH values greater than 9.7. Few water temperatures were greater than 28 degrees Celsius, and dissolved-oxygen concentrations less than 4 milligrams per liter generally were recorded in mid to late summer. In contrast, high pH values were more frequent, occurring earlier in the season and parallel with growth in the algal bloom.\r\n\r\nThe 10 hypotheses relating water-quality variables, lake level, and climatic factors from the earlier USGS study were tested in this analysis for the larger 1990-2006 dataset. These hypotheses proposed relations between lake level and chlorophyll-a, pH, dissolved oxygen, total phosphorus, and water temperature. As in the previous study, no evidence was found in the larger dataset for any of these relations based on a seasonal (May-October) distribution. When analyzing only the June data, the previous 5-year study did find evidence for three hypotheses relating lake level to the onset of the bloom, chlorophyll-a concentrations, and the frequency of high pH values in June. These hypotheses were not supported by the 1990-2006 dataset, but the two hypotheses related to cumulative degree-days from the previous study were: chlorophyll-a concentrations were lower and onset of the algal bloom was delayed when spring air temperatures were cooler. Other relations between water-quality variables and cumulative degree-days were not significant.\r\n\r\nIn an attempt to identify interrelations among variables not detected by univariate analysis, multiple regressions were performed between lakewide measures of low dissolved-oxygen concentrations or high pH values in July and August and six physical and biological variables (peak chlorophyll-a concentrations, degree-days, water temperature, median October-May discharg","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20075117","collaboration":"Prepared in cooperation with the Bureau of Reclamation","usgsCitation":"Morace, J.L., 2007, Relation Between Selected Water-Quality Variables, Climatic Factors, and Lake Levels in Upper Klamath and Agency Lakes, Oregon, 1990-2006: U.S. Geological Survey Scientific Investigations Report 2007-5117, vi, 55 p., https://doi.org/10.3133/sir20075117.","productDescription":"vi, 55 p.","temporalStart":"1990-01-01","temporalEnd":"2006-12-31","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":192245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9865,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2007/5117/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.16666666666667,42.166666666666664 ], [ -122.16666666666667,42.833333333333336 ], [ -121.66666666666667,42.833333333333336 ], [ -121.66666666666667,42.166666666666664 ], [ -122.16666666666667,42.166666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c339","contributors":{"authors":[{"text":"Morace, Jennifer L. 0000-0002-8132-4044 jlmorace@usgs.gov","orcid":"https://orcid.org/0000-0002-8132-4044","contributorId":945,"corporation":false,"usgs":true,"family":"Morace","given":"Jennifer","email":"jlmorace@usgs.gov","middleInitial":"L.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":291644,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":80075,"text":"sir20065228 - 2007 - Ground-Water Flow Model of the Sierra Vista Subwatershed and Sonoran Portions of the Upper San Pedro Basin, Southeastern Arizona, United States, and Northern Sonora, Mexico","interactions":[],"lastModifiedDate":"2018-04-02T15:22:18","indexId":"sir20065228","displayToPublicDate":"2007-06-30T00:00:00","publicationYear":"2007","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":"2006-5228","title":"Ground-Water Flow Model of the Sierra Vista Subwatershed and Sonoran Portions of the Upper San Pedro Basin, Southeastern Arizona, United States, and Northern Sonora, Mexico","docAbstract":"A numerical ground-water model was developed to simulate seasonal and long-term variations in ground-water flow in the Sierra Vista subwatershed, Arizona, United States, and Sonora, Mexico, portions of the Upper San Pedro Basin. This model includes the simulation of details of the groundwater flow system that were not simulated by previous models, such as ground-water flow in the sedimentary rocks that surround and underlie the alluvial basin deposits, withdrawals for dewatering purposes at the Tombstone mine, discharge to springs in the Huachuca Mountains, thick low-permeability intervals of silt and clay that separate the ground-water flow system into deep-confined and shallow-unconfined systems, ephemeral-channel recharge, and seasonal variations in ground-water discharge by wells and evapotranspiration.\r\n\r\nSteady-state and transient conditions during 1902-2003 were simulated by using a five-layer numerical ground- water flow model representing multiple hydrogeologic units. Hydraulic properties of model layers, streamflow, and evapotranspiration rates were estimated as part of the calibration process by using observed water levels, vertical hydraulic gradients, streamflow, and estimated evapotranspiration rates as constraints. Simulations approximate observed water-level trends throughout most of the model area and streamflow trends at the Charleston streamflow-gaging station on the San Pedro River. Differences in observed and simulated water levels, streamflow, and evapotranspiration could be reduced through simulation of climate-related variations in recharge rates and recharge from flood-flow infiltration.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20065228","collaboration":"Prepared in cooperation with the Upper San Pedro Partnership and Bureau of Land Management","usgsCitation":"Pool, D.R., and Dickinson, J.E., 2007, Ground-Water Flow Model of the Sierra Vista Subwatershed and Sonoran Portions of the Upper San Pedro Basin, Southeastern Arizona, United States, and Northern Sonora, Mexico (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2006-5228, vi, 49 p., https://doi.org/10.3133/sir20065228.","productDescription":"vi, 49 p.","onlineOnly":"Y","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":192894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9864,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5228/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.75,30.75 ], [ -110.75,32 ], [ -109.75,32 ], [ -109.75,30.75 ], [ -110.75,30.75 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d616","contributors":{"authors":[{"text":"Pool, D. R.","contributorId":75581,"corporation":false,"usgs":true,"family":"Pool","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":291643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickinson, Jesse E. 0000-0002-0048-0839 jdickins@usgs.gov","orcid":"https://orcid.org/0000-0002-0048-0839","contributorId":152545,"corporation":false,"usgs":true,"family":"Dickinson","given":"Jesse","email":"jdickins@usgs.gov","middleInitial":"E.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":291642,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":80074,"text":"ofr20071122 - 2007 - Flood of May 2006 in New Hampshire","interactions":[],"lastModifiedDate":"2012-03-08T17:16:20","indexId":"ofr20071122","displayToPublicDate":"2007-06-29T00:00:00","publicationYear":"2007","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":"2007-1122","title":"Flood of May 2006 in New Hampshire","docAbstract":"From May 13-17, 2006, central and southern New Hampshire experienced severe flooding caused by as much as 14 inches of rainfall in the region. As a result of the flood damage, a presidential disaster declaration was made on May 25, 2006, for seven counties-Rockingham, Hillsborough, Strafford, Merrimack, Belknap, Carroll, and Grafton. Following the flooding, the U.S. Geological Survey, in a cooperative investigation with the Federal Emergency Management Agency, determined the peak stages, peak discharges, and recurrence-interval estimates of the May 2006 flood at 65 streamgages in the counties where the disaster declaration was made. Data from flood-insurance studies published by the Federal Emergency Management Agency also were compiled for each streamgage location for comparison purposes.\r\n\r\nThe peak discharges during the May 2006 flood were the largest ever recorded at 14 long-term (more than 10 years of record) streamgages in New Hampshire. In addition, peak discharges equaled or exceeded a 100-year recurrence interval at 14 streamgages and equaled or exceeded a 50-year recurrence interval at 22 streamgages. The most severe flooding occurred in Rockingham, Strafford, Merrimack, and eastern and northern Hillsborough Counties.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20071122","collaboration":"Prepared in cooperation with the Federal Emergency Management Agency ","usgsCitation":"Olson, S.A., 2007, Flood of May 2006 in New Hampshire: U.S. Geological Survey Open-File Report 2007-1122, iv, 33 p., https://doi.org/10.3133/ofr20071122.","productDescription":"iv, 33 p.","onlineOnly":"Y","costCenters":[{"id":468,"text":"New Hampshire-Vermont Water Science Center","active":false,"usgs":true}],"links":[{"id":192301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9863,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2007/1122/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73,42.5 ], [ -73,45.5 ], [ -70,45.5 ], [ -70,42.5 ], [ -73,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c14c","contributors":{"authors":[{"text":"Olson, Scott A. 0000-0002-1064-2125 solson@usgs.gov","orcid":"https://orcid.org/0000-0002-1064-2125","contributorId":2059,"corporation":false,"usgs":true,"family":"Olson","given":"Scott","email":"solson@usgs.gov","middleInitial":"A.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":291641,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":80069,"text":"ofr20061353 - 2007 - Occurrences of calcareous nannofossil, dinoflagellate cyst, and pollen taxa in Paleocene strate in South Carolina","interactions":[],"lastModifiedDate":"2021-08-23T11:41:09.376649","indexId":"ofr20061353","displayToPublicDate":"2007-06-29T00:00:00","publicationYear":"2007","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-1353","title":"Occurrences of calcareous nannofossil, dinoflagellate cyst, and pollen taxa in Paleocene strate in South Carolina","docAbstract":"This report presents 26 diagrams showing the occurrences of fossil dinocyst, calcareous nannofossil, and pollen assemblages in Paleocene samples from 15 boreholes in South Carolina.
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Earth","interactions":[],"lastModifiedDate":"2012-02-02T00:14:11","indexId":"fs20073004","displayToPublicDate":"2007-06-29T00:00:00","publicationYear":"2007","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":"2007-3004","title":"Precambrian Time - The Story of the Early Earth","docAbstract":"The Precambrian is the least-understood part of Earth history, yet it is arguably the most important. Precambrian time spans almost nine-tenths of Earth history, from the formation of the Earth to the dawn of the Cambrian Period. It represents time so vast and long ago that it challenges all comprehension.\r\n\r\nThe Precambrian is the time of big questions. How old is the Earth? How old are the oldest rocks and continents? What was the early Earth like? What was the early atmosphere like? When did life appear, and what did it look like? And, how do we know this?\r\n\r\nIn recent years, remarkable progress has been made in understanding the early evolution of the Earth and life itself. Yet, the scientific story of the early Earth is still a work in progress, humankind's latest attempt to understand the planet. Like previous attempts, it too will change as we learn more about the Earth. Read on to discover what we know now, in the early 21st century.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20073004","usgsCitation":"Lindsey, D.A., 2007, Precambrian Time - The Story of the Early Earth (Version 1.0): U.S. Geological Survey Fact Sheet 2007-3004, 4 p., https://doi.org/10.3133/fs20073004.","productDescription":"4 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":125740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2007_3004.jpg"},{"id":9861,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2007/3004/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acbe4b07f02db67e36e","contributors":{"authors":[{"text":"Lindsey, D. A.","contributorId":49814,"corporation":false,"usgs":true,"family":"Lindsey","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":291640,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":80072,"text":"fs20063145 - 2007 - Geohydrologic Framework of the Edwards and Trinity Aquifers, South-Central Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:14:20","indexId":"fs20063145","displayToPublicDate":"2007-06-29T00:00:00","publicationYear":"2007","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":"2006-3145","title":"Geohydrologic Framework of the Edwards and Trinity Aquifers, South-Central Texas","docAbstract":"This five-year USGS project, funded by the National Cooperative Geologic Mapping Program, is using multidisciplinary approaches to reveal the surface and subsurface geologic architecture of two important Texas aquifers: (1) the Edwards aquifer that extends from south of Austin to west of San Antonio and (2) the southern part of the Trinity aquifer in the Texas Hill Country west and south of Austin. The project's principal areas of research include: Geologic Mapping, Geophysical Surveys, Geochronology, Three-dimensional Modeling, and Noble Gas Geochemistry.\r\n\r\nThe Edwards aquifer is one of the most productive carbonate aquifers in the United States. It also has been designated a sole source aquifer by the U.S. Environmental Protection Agency and is the primary source of water for San Antonio, America's eighth largest city. The Trinity aquifer forms the catchment area for the Edwards aquifer and it intercepts some surface flow above the Edwards recharge zone. The Trinity may also contribute to the Edwards water budget by subsurface flow across formation boundaries at considerable depths. Dissolution, karst development, and faulting and fracturing in both aquifers directly control aquifer geometry by compartmentalizing the aquifer and creating unique ground-water flow paths.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20063145","usgsCitation":"Blome, C.D., Faith, J.R., and Ozuna, G.B., 2007, Geohydrologic Framework of the Edwards and Trinity Aquifers, South-Central Texas (Version 1.0): U.S. Geological Survey Fact Sheet 2006-3145, 4 p., https://doi.org/10.3133/fs20063145.","productDescription":"4 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":120782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3145.jpg"},{"id":9860,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3145/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688907","contributors":{"authors":[{"text":"Blome, Charles D. 0000-0002-3449-9378 cblome@usgs.gov","orcid":"https://orcid.org/0000-0002-3449-9378","contributorId":1246,"corporation":false,"usgs":true,"family":"Blome","given":"Charles","email":"cblome@usgs.gov","middleInitial":"D.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":291637,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faith, Jason R.","contributorId":92758,"corporation":false,"usgs":true,"family":"Faith","given":"Jason","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":291639,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ozuna, George B. gbozuna@usgs.gov","contributorId":1247,"corporation":false,"usgs":true,"family":"Ozuna","given":"George","email":"gbozuna@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":291638,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":80071,"text":"sir20075046 - 2007 - Mineral Resources of the Hells Canyon Study Area, Wallowa County, Oregon, and Idaho and Adams Counties, Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:11:38","indexId":"sir20075046","displayToPublicDate":"2007-06-29T00:00:00","publicationYear":"2007","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":"2007-5046","title":"Mineral Resources of the Hells Canyon Study Area, Wallowa County, Oregon, and Idaho and Adams Counties, Idaho","docAbstract":"Field studies supporting the evaluation of the mineral potential of the Hells Canyon study area were carried out by the U.S. Geological Survey and the U.S. Bureau of Mines in 1974-76 and 1979. The study area includes (1) the Hells Canyon Wilderness; (2) parts of the Snake River, Rapid River, and West Fork Rapid River Wild and Scenic Rivers; (3) lands included in the second Roadless Area Review and Evaluation (RARE II); and (4) part of the Hells Canyon National Recreation Area. The survey is one of a series of studies to appraise the suitability of the area for inclusion in the National Wilderness Preservation System as required by the Wilderness Act of 1964. The spectacular and mineralized area covers nearly 950 mi2 (2,460 km2) in northeast Oregon and west-central Idaho at the junction of the Northern Rocky Mountains and the Columbia Plateau.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20075046","usgsCitation":"Simmons, G., Gualtieri, J., Close, T.J., Federspiel, F.E., and Leszcykowski, A.M., 2007, Mineral Resources of the Hells Canyon Study Area, Wallowa County, Oregon, and Idaho and Adams Counties, Idaho (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2007-5046, Pamphlet: vii, 62 p.; 4 Plates - Plate 1: 58 x 45 inches, Plate 2: 55 x 45 inches, Plate 3: 43 x 45 inches, and Plate 4: 55 x 45 inches, https://doi.org/10.3133/sir20075046.","productDescription":"Pamphlet: vii, 62 p.; 4 Plates - Plate 1: 58 x 45 inches, Plate 2: 55 x 45 inches, Plate 3: 43 x 45 inches, and Plate 4: 55 x 45 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9859,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2007/5046/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.5,45 ], [ -117.5,46 ], [ -116,46 ], [ -116,45 ], [ -117.5,45 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6357ad","contributors":{"authors":[{"text":"Simmons, George C.","contributorId":68836,"corporation":false,"usgs":true,"family":"Simmons","given":"George C.","affiliations":[],"preferred":false,"id":291635,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gualtieri, James L.","contributorId":64349,"corporation":false,"usgs":true,"family":"Gualtieri","given":"James L.","affiliations":[],"preferred":false,"id":291634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Close, Terry J.","contributorId":36159,"corporation":false,"usgs":true,"family":"Close","given":"Terry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":291633,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Federspiel, Francis E.","contributorId":28290,"corporation":false,"usgs":true,"family":"Federspiel","given":"Francis","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":291632,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Leszcykowski, Andrew M.","contributorId":78387,"corporation":false,"usgs":true,"family":"Leszcykowski","given":"Andrew","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":291636,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ]}