A preliminary study was done in Oakland County, Michigan, to determine the concentration of fecal indicator bacteria (fecal coliform bacteria and enterococci), antibiotic resistance patterns of these two groups, and the presence of potentially pathogenic Escherichia coli (E. coli). For selected sites, specific members of these groups [E. coli, Enterococcus faecium (E. faecium) and Enterococcus faecalis (E. faecalis)] were isolated and tested for levels of resistance to specific antibiotics used to treat human infections by pathogens in these groups and for their potential to transfer these resistances. In addition, water samples from all sites were tested for indicators of potentially pathogenic E. coli by three assays: a growth-based assay for sorbitol-negative E. coli, an immunological assay for E. coli O157, and a molecular assay for three virulence and two serotype genes. Samples were also collected from two non-urbanized sites outside of Oakland County. Results from the urbanized Oakland County area were compared to those from these two non-urbanized sites.
Fecal indicator bacteria concentrations exceeded State of Michigan recreational water-quality standards and (or) recommended U.S. Environmental Protection Agency (USEPA) standards in samples from all but two Oakland County sites. Multiple-antibiotic-resistant fecal coliform bacteria were found at all sites, including two reference sites from outside the county. Two sites (Stony Creek and Paint Creek) yielded fecal coliform isolates resistant to all tested antibiotics. Patterns indicative of extended-spectrum-β-lactamase (ESBL)- producing fecal coliform bacteria were found at eight sites in Oakland County and E. coli resistant to clinically significant antibiotics were recovered from the River Rouge, Clinton River, and Paint Creek. Vancomycin-resistant presumptive enterococci were found at six sites in Oakland County and were not found at the reference sites. Evidence of acquired antibiotic resistances was detected in bacteria from multiple sites in Oakland County but not detected in bacteria from the reference sites. Integrons capable of transferring resistance were detected in isolates from the River Rouge and Clinton River. E. faecium and E. faecalis identified in samples collected from Kearsley Creek and Evans Ditch were resistant to high levels of vancomycin and carried transferable genes responsible for resistance.
Several sites in Oakland County had indicators of pathogenic E. coli in August and (or) September 2003. Two samples from the Clinton River in August tested positive for all three E. coli O157 tests. Both the August and September samples from one River Rouge site were positive for the immunological and molecular assay for E. coli O157. A combination of virulence genes commonly associated with human illness was detected at five sites in August and seven sites in September. Antibiotic-resistance profiles of clinical concern along with genes capable of transferring the resistance were found at several sites throughout Oakland County; samples from many of these sites also contained potentially pathogenic E. coli.
","language":"English","doi":"10.3133/sir20055058","collaboration":"In cooperation with Oakland County, Michigan","usgsCitation":"Fogarty, L., Duris, J.W., and Aichele, S., 2005, Preliminary survey of antibiotic-resistant fecal indicator bacteria and pathogenic Escherichia coli from river-water samples collected in Oakland County, Michigan, 2003: U.S. Geological Survey Scientific Investigations Report 2005-5058, v, 34 p., https://doi.org/10.3133/sir20055058.","productDescription":"v, 34 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":186269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055058.JPG"},{"id":6611,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5058/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Michigan","county":"Oakland County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-83.4546,42.8798],[-83.2227,42.887],[-83.1025,42.8884],[-83.0986,42.801],[-83.0905,42.6238],[-83.0867,42.5355],[-83.0843,42.4463],[-83.3264,42.4416],[-83.4403,42.4393],[-83.553,42.4351],[-83.6669,42.4312],[-83.6733,42.5196],[-83.6863,42.7822],[-83.6902,42.871],[-83.5737,42.8744],[-83.4541,42.8766],[-83.4546,42.8798]]]},\"properties\":{\"name\":\"Oakland\",\"state\":\"MI\"}}]}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659d4d","contributors":{"authors":[{"text":"Fogarty, Lisa R.","contributorId":74074,"corporation":false,"usgs":true,"family":"Fogarty","given":"Lisa R.","affiliations":[],"preferred":false,"id":283371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duris, Joseph W. 0000-0002-8669-8109 jwduris@usgs.gov","orcid":"https://orcid.org/0000-0002-8669-8109","contributorId":1981,"corporation":false,"usgs":true,"family":"Duris","given":"Joseph","email":"jwduris@usgs.gov","middleInitial":"W.","affiliations":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":283369,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aichele, Stephen S. 0000-0002-3397-7921 saichele@usgs.gov","orcid":"https://orcid.org/0000-0002-3397-7921","contributorId":194508,"corporation":false,"usgs":true,"family":"Aichele","given":"Stephen S.","email":"saichele@usgs.gov","affiliations":[{"id":430,"text":"National Mapping Program","active":false,"usgs":true}],"preferred":false,"id":283370,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70238385,"text":"70238385 - 2005 - Antipodal hotspots and bipolar catastrophes: Were oceanic large-body impacts the cause?","interactions":[],"lastModifiedDate":"2022-11-19T00:06:35.513541","indexId":"70238385","displayToPublicDate":"2005-07-30T17:57:24","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Antipodal hotspots and bipolar catastrophes: Were oceanic large-body impacts the cause?","docAbstract":"One aspect of the hotspot distribution that has received little attention is its antipodal character. Of 45 ‘primary’ hotspots found in most hotspot compilations 22 (49%) form antipodal pairs within observed hotspot drift limits (≤ 20 mm/yr). In addition, the available ages, or possible age ranges, for both hotspots of an antipodal pair tend to be similar (≤ 10 Myr difference) or overlap. Monte Carlo simulations indicate that the antipodal primary hotspots' locations and ages are not due to chance at the > 99% confidence level (p < 0.01). All hotspot pairs include at least one oceanic hotspot, and these are consistently opposite those hotspots related to large igneous provinces (LIPs) and continental volcanism. A mechanism of formation is considered in which minor hotspot volcanism is induced at, and flood basalt volcanism is triggered by seismic energy focused antipodal to, oceanic large-body impact sites. Because continental impacts are expected to have lower seismic efficiencies, continents possibly acted as shields to the formation of antipodal hotspot pairs. Published numerical models indicate that large oceanic impacts (10-km-diameter bolide) generate megatsunami capable of altering coastal depositional environments on a global scale. Past impact-generated megatsunami, consequently, could have left widespread stratigraphic records, possibly misinterpreted as indicating large rapid changes in eustatic sea level, and widely disrupted continental and marine sediment reservoirs responsible for abrupt changes in the isotopic composition of seawater. Phanerozoic mass extinction events, therefore, might have resulted primarily from catastrophic megatsunami in a dominantly oceanic hemisphere and the near contemporaneous effusion of vast quantities of noxious gases from flood basalt eruptions in a dominantly continental one.
","language":"English","publisher":"Elsevier","doi":"10.1016/j.epsl.2005.02.020","usgsCitation":"Hagstrum, J.T., 2005, Antipodal hotspots and bipolar catastrophes: Were oceanic large-body impacts the cause?: Earth and Planetary Science Letters, v. 236, no. 1-2, p. 13-27, https://doi.org/10.1016/j.epsl.2005.02.020.","productDescription":"15 p.","startPage":"13","endPage":"27","costCenters":[],"links":[{"id":409485,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"236","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hagstrum, Jonathan T. 0000-0002-0689-280X jhag@usgs.gov","orcid":"https://orcid.org/0000-0002-0689-280X","contributorId":3474,"corporation":false,"usgs":true,"family":"Hagstrum","given":"Jonathan","email":"jhag@usgs.gov","middleInitial":"T.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":857328,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70951,"text":"ofr20051280 - 2005 - Rainfall, Streamflow, and Water-Quality Data During Stormwater Monitoring, Halawa Stream Drainage Basin, Oahu, Hawaii, July 1, 2004 to June 30, 2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:17","indexId":"ofr20051280","displayToPublicDate":"2005-07-29T00:00:00","publicationYear":"2005","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":"2005-1280","title":"Rainfall, Streamflow, and Water-Quality Data During Stormwater Monitoring, Halawa Stream Drainage Basin, Oahu, Hawaii, July 1, 2004 to June 30, 2005","docAbstract":"Storm runoff water-quality samples were collected as part of the State of Hawaii Department of Transportation Stormwater Monitoring Program. This program is designed to assess the effects of highway runoff and urban runoff on Halawa Stream. For this program, rainfall data were collected at two stations, continuous streamflow data at two stations, and water-quality data at five stations, which include the two continuous streamflow stations. This report summarizes rainfall, streamflow, and water-quality data collected between July 1, 2004 and June 30, 2005.\r\n\r\nA total of 15 samples was collected over three storms during July 1, 2004 to June 30, 2005. In general, an attempt was made to collect grab samples nearly simultaneously at all five stations and flow-weighted time-composite samples at the three stations equipped with automatic samplers. However, all three storms were partially sampled because either not all stations were sampled or not all composite samples were collected. Samples were analyzed for total suspended solids, total dissolved solids, nutrients, chemical oxygen demand, and selected trace metals (cadmium, chromium, copper, lead, nickel, and zinc). Chromium and nickel were added to the analysis starting October 1, 2004. Grab samples were additionally analyzed for oil and grease, total petroleum hydrocarbons, fecal coliform, and biological oxygen demand. Quality-assurance/quality-control samples were also collected during storms and during routine maintenance to verify analytical procedures and check the effectiveness of equipment-cleaning procedures.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20051280","collaboration":"Prepared in cooperation with the State of Hawaii Department of Transportation","usgsCitation":"Young, S.T., and Ball, M.T., 2005, Rainfall, Streamflow, and Water-Quality Data During Stormwater Monitoring, Halawa Stream Drainage Basin, Oahu, Hawaii, July 1, 2004 to June 30, 2005: U.S. Geological Survey Open-File Report 2005-1280, iv, 18 p., https://doi.org/10.3133/ofr20051280.","productDescription":"iv, 18 p.","onlineOnly":"Y","temporalStart":"2004-07-01","temporalEnd":"2005-06-30","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":6608,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2005-1280/","linkFileType":{"id":5,"text":"html"}},{"id":186189,"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\": [ [ [ -157.96666666666667,21.333333333333332 ], [ -157.96666666666667,21.466666666666665 ], [ -157.8,21.466666666666665 ], [ -157.8,21.333333333333332 ], [ -157.96666666666667,21.333333333333332 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669a11","contributors":{"authors":[{"text":"Young, Stacie T. M.","contributorId":63432,"corporation":false,"usgs":true,"family":"Young","given":"Stacie","email":"","middleInitial":"T. M.","affiliations":[],"preferred":false,"id":283367,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ball, Marcael T.J.","contributorId":16904,"corporation":false,"usgs":true,"family":"Ball","given":"Marcael","email":"","middleInitial":"T.J.","affiliations":[],"preferred":false,"id":283366,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70950,"text":"ofr20051281 - 2005 - Water level management and contaminant exposure in tree swallows nesting on the upper Mississippi River","interactions":[],"lastModifiedDate":"2020-02-21T14:53:56","indexId":"ofr20051281","displayToPublicDate":"2005-07-29T00:00:00","publicationYear":"2005","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":"2005-1281","title":"Water level management and contaminant exposure in tree swallows nesting on the upper Mississippi River","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051281","usgsCitation":"Custer, T., and Custer, C., 2005, Water level management and contaminant exposure in tree swallows nesting on the upper Mississippi River: U.S. Geological Survey Open-File Report 2005-1281, 2 p., https://doi.org/10.3133/ofr20051281.","productDescription":"2 p.","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":186188,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6607,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2005-1281/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota, Wisconsin","otherGeospatial":"Upper Mississippi River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.32247924804686,\n 43.56447158721811\n ],\n [\n -91.18377685546875,\n 43.56447158721811\n ],\n [\n -91.18377685546875,\n 43.77406874252176\n ],\n [\n -91.32247924804686,\n 43.77406874252176\n ],\n [\n -91.32247924804686,\n 43.56447158721811\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa191","contributors":{"authors":[{"text":"Custer, Thomas","contributorId":103351,"corporation":false,"usgs":true,"family":"Custer","given":"Thomas","affiliations":[],"preferred":false,"id":283365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Custer, Christine","contributorId":93567,"corporation":false,"usgs":true,"family":"Custer","given":"Christine","affiliations":[],"preferred":false,"id":283364,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70943,"text":"sir20055119 - 2005 - Proposed moduli of dry rock and their application to predicting elastic velocities of sandstones","interactions":[],"lastModifiedDate":"2012-02-02T00:13:49","indexId":"sir20055119","displayToPublicDate":"2005-07-27T00:00:00","publicationYear":"2005","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":"2005-5119","title":"Proposed moduli of dry rock and their application to predicting elastic velocities of sandstones","docAbstract":"Velocities of water-saturated isotropic sandstones under low frequency can be modeled using the Biot-Gassmann theory if the moduli of dry rocks are known. On the basis of effective medium theory by Kuster and Toksoz, bulk and shear moduli of dry sandstone are proposed. These moduli are related to each other through a consolidation parameter and provide a new way to calculate elastic velocities. Because this parameter depends on differential pressure and the degree of consolidation, the proposed moduli can be used to calculate elastic velocities of sedimentary rocks under different in-place conditions by varying the consolidation parameter. This theory predicts that the ratio of P-wave to S-wave velocity (Vp/Vs) of a dry rock decreases as differential pressure increases and porosity decreases. This pattern of behavior is similar to that of water-saturated sedimentary rocks. If microcracks are present in sandstones, the velocity ratio usually increases as differential pressure increases. This implies that this theory is optimal for sandstones having intergranular porosities. Even though the accurate behavior of the consolidation parameter with respect to differential pressure or the degree of consolidation is not known, this theory presents a new way to predict S-wave velocity from P-wave velocity and porosity and to calculate elastic velocities of gas-hydrate-bearing sediments. For given properties of sandstones such as bulk and shear moduli of matrix, only the consolidation parameter affects velocities, and this parameter can be estimated directly from the measurements; thus, the prediction of S-wave velocity is accurate, reflecting in-place conditions.","language":"ENGLISH","doi":"10.3133/sir20055119","usgsCitation":"Lee, M.W., 2005, Proposed moduli of dry rock and their application to predicting elastic velocities of sandstones (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5119, 18 p., https://doi.org/10.3133/sir20055119.","productDescription":"18 p.","costCenters":[],"links":[{"id":186585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6604,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5119/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881f6","contributors":{"authors":[{"text":"Lee, Myung W. mlee@usgs.gov","contributorId":779,"corporation":false,"usgs":true,"family":"Lee","given":"Myung","email":"mlee@usgs.gov","middleInitial":"W.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":283352,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70944,"text":"sir20045271 - 2005 - Characterization and modes of occurrence of elements in feed coal and coal combustion products from a power plant utilizing low-sulfur coal from the Powder River Basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:13:49","indexId":"sir20045271","displayToPublicDate":"2005-07-27T00:00:00","publicationYear":"2005","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":"2004-5271","title":"Characterization and modes of occurrence of elements in feed coal and coal combustion products from a power plant utilizing low-sulfur coal from the Powder River Basin, Wyoming","docAbstract":"The U.S. Geological Survey and the University of Kentucky Center for Applied Energy Research are collaborating with an Indiana utility company to determine the physical and chemical properties of feed coal and coal combustion products from a coal-fired power plant. The Indiana power plant utilizes a low-sulfur (0.23 to 0.47 weight percent S) and lowash (4.9 to 6.3 weight percent ash) subbituminous coal from the Wyodak-Anderson coal zone in the Tongue River Member of the Paleocene Fort Union Formation, Powder River Basin, Wyoming. \r\n\r\nBased on scanning electron microscope and X-ray diffraction analyses of feed coal samples, two mineral suites were identified: (1) a primary or detrital suite consisting of quartz (including beta-form grains), biotite, feldspar, and minor zircon; and (2) a secondary authigenic mineral suite containing alumino-phosphates (crandallite and gorceixite), kaolinite, carbonates (calcite and dolomite), quartz, anatase, barite, and pyrite. The primary mineral suite is interpreted, in part, to be of volcanic origin, whereas the authigenic mineral suite is interpreted, in part, to be the result of the alteration of the volcanic minerals. The mineral suites have contributed to the higher amounts of barium, calcium, magnesium, phosphorus, sodium, strontium, and titanium in the Powder River Basin feed coals in comparison to eastern coals. \r\n\r\nX-ray diffraction analysis indicates that (1) fly ash is mostly aluminate glass, perovskite, lime, gehlenite, quartz, and phosphates with minor amounts of periclase, anhydrite, hematite, and spinel group minerals; and (2) bottom ash is predominantly quartz, plagioclase (albite and anorthite), pyroxene (augite and fassaite), rhodonite, and akermanite, and spinel group minerals. Microprobe and scanning electron microscope analyses of fly ash samples revealed quartz, zircon, and monazite, euhedral laths of corundum with merrillite, hematite, dendritic spinels/ferrites, wollastonite, and periclase. The abundant calcium and magnesium mineral phases in the fly ash are attributed to the presence of carbonate, clay, and phosphate minerals in the feed coal and their alteration to new phases during combustion. \r\n\r\nThe amorphous diffraction-scattering maxima or glass 'hump' appears to reflect differences in chemical composition of fly ash and bottom ash glasses. In Wyodak-Anderson fly and bottom ashes, the center point of scattering maxima is due to calcium and magnesium content, whereas the glass 'hump' of eastern fly ash reflects variation in aluminum content. \r\n\r\nThe calcium- and magnesium-rich and alumino-phosphate mineral phases in the coal combustion products can be attributed to volcanic minerals deposited in peat-forming mires. Dissolution and alteration of these detrital volcanic minerals occurred either in the peat-forming stage or during coalification and diagenesis, resulting in the authigenic mineral suite. \r\n\r\nThe presence of free lime (CaO) in fly ash produced from Wyodak-Anderson coal acts as a self-contained 'scrubber' for SO3, where CaO + SO3 form anhydrite either during combustion or in the upper parts of the boiler. Considering the high lime content in the fly ash and the resulting hydration reactions after its contact with water, there is little evidence that major amounts of leachable metals are mobilized in the disposal or utilization of this fly ash. \r\n","language":"ENGLISH","doi":"10.3133/sir20045271","usgsCitation":"Brownfield, M.E., Cathcart, J.D., Affolter, R.H., Brownfield, I.K., Rice, C.A., O’Connor, J.T., Zielinski, R.A., Bullock, J.H., Hower, J., and Meeker, G.P., 2005, Characterization and modes of occurrence of elements in feed coal and coal combustion products from a power plant utilizing low-sulfur coal from the Powder River Basin, Wyoming (Online only, Version 1.0): U.S. Geological Survey Scientific Investigations Report 2004-5271, 42 p., https://doi.org/10.3133/sir20045271.","productDescription":"42 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6605,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5271/","linkFileType":{"id":5,"text":"html"}},{"id":186106,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e9d","contributors":{"authors":[{"text":"Brownfield, Michael E. 0000-0003-3633-1138 mbrownfield@usgs.gov","orcid":"https://orcid.org/0000-0003-3633-1138","contributorId":1548,"corporation":false,"usgs":true,"family":"Brownfield","given":"Michael","email":"mbrownfield@usgs.gov","middleInitial":"E.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":283354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cathcart, James D.","contributorId":87944,"corporation":false,"usgs":true,"family":"Cathcart","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":283360,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Affolter, Ronald H. affolter@usgs.gov","contributorId":659,"corporation":false,"usgs":true,"family":"Affolter","given":"Ronald","email":"affolter@usgs.gov","middleInitial":"H.","affiliations":[{"id":165,"text":"Central Energy Resources Team","active":false,"usgs":true}],"preferred":false,"id":283353,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brownfield, Isabelle K.","contributorId":97108,"corporation":false,"usgs":true,"family":"Brownfield","given":"Isabelle","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":283361,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rice, Cynthia A.","contributorId":87140,"corporation":false,"usgs":true,"family":"Rice","given":"Cynthia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":283359,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"O’Connor, Joseph T.","contributorId":61832,"corporation":false,"usgs":true,"family":"O’Connor","given":"Joseph","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":283357,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Zielinski, Robert A. 0000-0002-4047-5129 rzielinski@usgs.gov","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":1593,"corporation":false,"usgs":true,"family":"Zielinski","given":"Robert","email":"rzielinski@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":283355,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Bullock, John H. Jr.","contributorId":105316,"corporation":false,"usgs":true,"family":"Bullock","given":"John","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":283362,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hower, James C. 0000-0003-4694-2776","orcid":"https://orcid.org/0000-0003-4694-2776","contributorId":34561,"corporation":false,"usgs":false,"family":"Hower","given":"James C.","affiliations":[{"id":16123,"text":"University of Kentucky, Center for Applied Energy Research, 2540 Research Park Drive, Lexington, KY 40511, United States.","active":true,"usgs":false}],"preferred":false,"id":283356,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Meeker, Gregory P.","contributorId":62974,"corporation":false,"usgs":true,"family":"Meeker","given":"Gregory","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":283358,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70941,"text":"sir20045091 - 2005 - Stratigraphic framework, structure, and thermal maturity of Cretaceous and Lower Tertiary rocks in relation to hydrocarbon potential, Crazy Mountains Basin, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:04:33","indexId":"sir20045091","displayToPublicDate":"2005-07-27T00:00:00","publicationYear":"2005","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":"2004-5091","title":"Stratigraphic framework, structure, and thermal maturity of Cretaceous and Lower Tertiary rocks in relation to hydrocarbon potential, Crazy Mountains Basin, Montana","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045091","isbn":"0607971584","usgsCitation":"Johnson, R.C., Finn, T.M., Taylor, D.J., and Nuccio, V.F., 2005, Stratigraphic framework, structure, and thermal maturity of Cretaceous and Lower Tertiary rocks in relation to hydrocarbon potential, Crazy Mountains Basin, Montana (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2004-5091, 1 CD-ROM : ill. (some col.), maps (some col.) ; 4 3/4 in., https://doi.org/10.3133/sir20045091.","productDescription":"1 CD-ROM : ill. (some col.), maps (some col.) ; 4 3/4 in.","additionalOnlineFiles":"Y","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":121232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2004_5091.png"},{"id":14496,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5091/downloads/SIR04-5091.pdf","linkFileType":{"id":5,"text":"html"}},{"id":13714,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5091/","linkFileType":{"id":5,"text":"html"}},{"id":13605,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.netl.doe.gov/KMD/cds/disk15/SIR%202004-5091.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aed9f","contributors":{"authors":[{"text":"Johnson, Ronald C. 0000-0002-6197-5165 rcjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-6197-5165","contributorId":1550,"corporation":false,"usgs":true,"family":"Johnson","given":"Ronald","email":"rcjohnson@usgs.gov","middleInitial":"C.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":283350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finn, Thomas M. 0000-0001-6396-9351 finn@usgs.gov","orcid":"https://orcid.org/0000-0001-6396-9351","contributorId":778,"corporation":false,"usgs":true,"family":"Finn","given":"Thomas","email":"finn@usgs.gov","middleInitial":"M.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":283348,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, David J.","contributorId":42924,"corporation":false,"usgs":true,"family":"Taylor","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":283351,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nuccio, Vito F. vnuccio@usgs.gov","contributorId":853,"corporation":false,"usgs":true,"family":"Nuccio","given":"Vito","email":"vnuccio@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":283349,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70945,"text":"sir20055110 - 2005 - Simulation of hydraulic characteristics in the white sturgeon spawning habitat of the Kootenai River near Bonners Ferry, Idaho","interactions":[],"lastModifiedDate":"2014-05-05T14:53:45","indexId":"sir20055110","displayToPublicDate":"2005-07-27T00:00:00","publicationYear":"2005","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":"2005-5110","title":"Simulation of hydraulic characteristics in the white sturgeon spawning habitat of the Kootenai River near Bonners Ferry, Idaho","docAbstract":"Hydraulic characterization of the Kootenai River, especially in the white sturgeon spawning habitat reach, is needed by the Kootenai River White Sturgeon Recovery Team to promote hydraulic conditions that improve spawning conditions for the white sturgeon (Acipenser transmontanus) in the Kootenai River. The decreasing population and spawning failure of white sturgeon has led to much concern. Few wild juvenile sturgeons are found in the river today. Determining the location of the transition between backwater and free-flowing water in the Kootenai River is a primary focus for biologists who believe that hydraulic changes at the transition affect the location where the sturgeon choose to spawn. The Kootenai River begins in British Columbia, Canada, and flows through Montana, Idaho, and back into British Columbia. The 65.6-mile reach of the Kootenai River in Idaho was studied. The study area encompasses the white sturgeon spawning reach that has been designated as a critical habitat.
\nA one-dimensional hydraulic-flow model of the study reach was developed, calibrated, and used to develop relations between hydraulic characteristics and water-surface elevation, discharge, velocity, and backwater extent. The model used 164 cross sections, most of which came from a previous river survey conducted in 2002-03. The model was calibrated to water-surface elevations at specific discharges at five gaging stations. Calibrated water-surface elevations ranged from about 1,743 to about 1,759 feet, and discharges used in calibration ranged from 5,000 to 47,500 cubic feet per second. Model calibration was considered acceptable when the difference between measured and simulated water-surface elevations was ?0.15 foot or less. Measured and simulated average velocities also were compared. These comparisons indicated agreement between measured and simulated values.
\nThe location of the transition between backwater and free-flowing water was determined using the calibrated model. The model was used to simulate hydraulic characteristics for a range of water-surface elevations from 1,741 to 1,762 feet and discharges from 4,000 to 75,000 cubic feet per second. These simulated hydraulic characteristics were used to develop a three-parameter relation-discharge in the study reach, water-surface elevation at Kootenai River at Porthill gaging station (12322000), and the location of the transition between backwater and free-flowing water. Simulated hydraulic characteristics produced backwater locations ranging from river mile (RM) 105.6 (Porthill) to RM 158 (near Crossport), a span of about 52 miles. However, backwater locations from measured data ranged primarily from RM 152 to RM 157, a 5-mile span. The average backwater location from measured data was at about RM 154.
\nThree-parameter relations also were developed for determining the amount of discharge in the Shorty Island side channel and average velocity at selected cross sections in the study reach. Simulated discharge for the side channel relative to measured data ranged from 0 to about 5,500 cubic feet per second, and simulated average velocity relative to measured data ranged from 0 to about 3.5 feet per second. Relations using other hydraulic, sediment/incipient motion, ecological, and biological characteristics also could be developed.
\nThe relations also can be used in real time by accessing data from the Web. Discharge and stage data for two gaging stations, Tribal Hatchery (12310100) and Porthill (12322500), are available from the Idaho U.S. Geological Survey web page (URL: http://waterdata.usgs.gov/id/nwis/current/?type=flow). Because the coordinate axes of the three-parameter relations use discharge from the Tribal Hatchery gaging station and water-surface elevation from the Porthill gaging station, the location of the transition between backwater and free-flowing water can be determined for current conditions using the real-time data. Similarly, discharge in the Shorty Island side channel and (or) average velocity at selected cross sections also can be determined for current conditions.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055110","collaboration":"Prepared in cooperation with the Idaho Department of Fish and Game","usgsCitation":"Berenbrock, C., 2005, Simulation of hydraulic characteristics in the white sturgeon spawning habitat of the Kootenai River near Bonners Ferry, Idaho: U.S. Geological Survey Scientific Investigations Report 2005-5110, Report: vi, 30 p.; Data files, https://doi.org/10.3133/sir20055110.","productDescription":"Report: vi, 30 p.; Data files","numberOfPages":"40","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":186187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055110.PNG"},{"id":6606,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5110/","linkFileType":{"id":5,"text":"html"}},{"id":286891,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5110/pdf/sir20055110.pdf"},{"id":286892,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/sir/2005/5110/data/"}],"scale":"100000","projection":"Albers Equal-Area projection","country":"Canada;United States","state":"British Columbia;Idaho;Montana","otherGeospatial":"Kootenai River Drainage Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.0,48.0 ], [ -118.0,50.0 ], [ -115.0,50.0 ], [ -115.0,48.0 ], [ -118.0,48.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e492de4b07f02db57f93b","contributors":{"authors":[{"text":"Berenbrock, Charles","contributorId":30598,"corporation":false,"usgs":true,"family":"Berenbrock","given":"Charles","email":"","affiliations":[],"preferred":false,"id":283363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70939,"text":"cir1279 - 2005 - Estimated withdrawals from principal aquifers in the United States, 2000","interactions":[],"lastModifiedDate":"2017-08-29T10:58:44","indexId":"cir1279","displayToPublicDate":"2005-07-25T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1279","title":"Estimated withdrawals from principal aquifers in the United States, 2000","docAbstract":"Fresh ground-water withdrawals from 66 principal aquifers in the United States were estimated for irrigation, public-supply, and self-supplied industrial water uses for the year 2000. Total ground-water withdrawals were 76,500 million gallons per day, or 85,800 thousand acre-feet per year for these three uses. Irrigation used the largest amount of ground water, 56,900 million gallons per day, followed by public supply with 16,000 million gallons per day, and self-supplied industrial with 3,570 million gallons per day. These three water uses represented 92 percent of the fresh groundwater withdrawals for all uses in the United States, the remaining 8 percent included self-supplied domestic, aquaculture, livestock, mining, and thermoelectric power uses.
Aquifer withdrawals were categorized by five lithologic groups: unconsolidated and semiconsolidated sand and gravel aquifers, carbonate-rock aquifers, igneous and metamorphic-rock aquifers, sandstone aquifers, and sandstone and carbonate-rock aquifers. Withdrawals from aquifers that were not included in one of the 66 principal aquifers were reported in an “Other” aquifers group. The largest withdrawals in the United States were from unconsolidated and semiconsolidated sand and gravel aquifers, which accounted for 80 percent of total withdrawals from all aquifers. Carbonate-rock aquifers provided 8 percent of the withdrawals, and igneous and metamorphic-rock aquifers, 6 percent. Withdrawals from sandstone aquifers, from sandstone and carbonate-rock aquifers, and from the “Other” aquifers category each constituted about 2 percent of the total withdrawals reported.
Fifty-five percent of the total withdrawals for irrigation, public-supply, and self-supplied industrial water uses were provided by the High Plains aquifer, California Central Valley aquifer system, the Mississippi River Valley alluvial aquifer, and the Basin and Range basin-fill aquifers. These aquifers provided most of the withdrawals for irrigation. The High Plains aquifer was the most intensively used aquifer in the United States. This aquifer provided 23 percent of the total withdrawals from all aquifers for irrigation, public-supply, and self-supplied industrial water uses combined, and 30 percent of the total withdrawals from all aquifers for irrigation.
The primary aquifers used for public supply were the glacial sand and gravel aquifers of the Northeastern and North-Central States, the California Coastal Basin aquifers, the Floridan aquifer system, the Basin and Range basin-fill aquifers, and the Coastal lowlands aquifer system along the Gulf Coast. These five aquifers provided 43 percent of the total withdrawals from all aquifers for public supply. The glacial sand and gravel aquifers, Coastal lowlands aquifer system, Floridan aquifer system, and Cambrian-Ordovician aquifer system were the primary sources of water for self-supplied industrial use; these aquifers provided 46 percent of the total ground-water withdrawals for that use.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir1279","isbn":"0607967803","usgsCitation":"Maupin, M.A., and Barber, N.L., 2005, Estimated withdrawals from principal aquifers in the United States, 2000: U.S. Geological Survey Circular 1279, v, 47 p., https://doi.org/10.3133/cir1279.","productDescription":"v, 47 p.","costCenters":[],"links":[{"id":6603,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/circ1279","linkFileType":{"id":5,"text":"html"}},{"id":186584,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"tableOfContents":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051231","usgsCitation":"Duval, J.S., 2005, Aerial gamma-ray survey for parts of Cameron, Hidalgo, and Willacy Counties, Texas: U.S. Geological Survey Open-File Report 2005-1231, HTML Document, https://doi.org/10.3133/ofr20051231.","productDescription":"HTML Document","costCenters":[],"links":[{"id":193336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6587,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1231/","linkFileType":{"id":5,"text":"html"}},{"id":400249,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_72124.htm"}],"country":"United States","state":"Texas","county":"Cameron County, Hidalgo County, Willacy County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.25,\n 26.0333\n ],\n [\n -97.75,\n 26.0333\n ],\n [\n -97.75,\n 26.5\n ],\n [\n -98.25,\n 26.5\n ],\n [\n -98.25,\n 26.0333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698e2d","contributors":{"authors":[{"text":"Duval, Joseph S.","contributorId":22314,"corporation":false,"usgs":true,"family":"Duval","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":283333,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70931,"text":"sir20055117 - 2005 - Proceedings of the U.S. Geological Survey Fourth Biennial Geographic Information Science Workshop: Denver, Colorado, April 23-27, 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:13:49","indexId":"sir20055117","displayToPublicDate":"2005-07-22T00:00:00","publicationYear":"2005","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":"2005-5117","title":"Proceedings of the U.S. Geological Survey Fourth Biennial Geographic Information Science Workshop: Denver, Colorado, April 23-27, 2001","docAbstract":"Introduction: \r\nThe U.S. Geological Survey (USGS) Fourth Biennial Geographic Information Science (GIS) Workshop (USGS-GIS 2001) was held April 23-27, 2001, at the Denver Federal Center in Denver, Colorado. The workshop provided an environment for participants to improve their knowledge about GIS and GIS-related applications that are used within the USGS. Two major topics of USGS-GIS 2001 were the application of GIS technology to interdisciplinary science and the distribution and sharing of USGS GIS products. Additionally, several presentations included GIS technology and tools, project applications of GIS, and GIS data management. \r\n\r\nUSGS-GIS 2001 included user and vendor presentations, demonstrations, and hands-on technical workshops. Presentation abstracts that were submitted for publication are included in these proceedings. The keynote speaker was Karen Siderelis, the USGS Associate Director for Information (Geographic Information Officer). In addition to the USGS, other Federal agencies, GIS-related companies, and university researchers presented lectures or demonstrations or conducted hands-on sessions. USGS employees and contractors from every discipline and region attended the workshop. To facilitate the interaction between the Federal agencies, each of the presenting Federal agencies was invited to send a representative to the workshop. \r\n\r\nOne of the most beneficial activities of USGS-GIS 2001, as identified by an informal poll of attendees, was the Monday evening poster session in which more than 75 poster presentations gave attendees a chance to learn of work being performed throughout the USGS. A feature new to USGS-GIS 2001 was internet participation of USGS personnel through cyber seminars of the morning plenary sessions.","language":"ENGLISH","doi":"10.3133/sir20055117","usgsCitation":"Sieverling, J.B., Char, S.J., and San Juan, C.A., 2005, Proceedings of the U.S. Geological Survey Fourth Biennial Geographic Information Science Workshop: Denver, Colorado, April 23-27, 2001 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5117, 40 p., https://doi.org/10.3133/sir20055117.","productDescription":"40 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6602,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055117/ ","linkFileType":{"id":5,"text":"html"}},{"id":186583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66042f","contributors":{"authors":[{"text":"Sieverling, Jennifer B. jbsiever@usgs.gov","contributorId":4806,"corporation":false,"usgs":true,"family":"Sieverling","given":"Jennifer","email":"jbsiever@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":283345,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Char, Stephen J. sjchar@usgs.gov","contributorId":3982,"corporation":false,"usgs":true,"family":"Char","given":"Stephen","email":"sjchar@usgs.gov","middleInitial":"J.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":283344,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"San Juan, Carma A. 0000-0002-9151-1919 csanjuan@usgs.gov","orcid":"https://orcid.org/0000-0002-9151-1919","contributorId":1146,"corporation":false,"usgs":true,"family":"San Juan","given":"Carma","email":"csanjuan@usgs.gov","middleInitial":"A.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":283343,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70926,"text":"ofr20051192 - 2005 - Digital-elevation and surface-classification maps of the Fish Creek area, Harrison Bay quadrangle, northern Alaska","interactions":[],"lastModifiedDate":"2023-03-22T20:17:59.173378","indexId":"ofr20051192","displayToPublicDate":"2005-07-22T00:00:00","publicationYear":"2005","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":"2005-1192","title":"Digital-elevation and surface-classification maps of the Fish Creek area, Harrison Bay quadrangle, northern Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051192","usgsCitation":"Mars, J.L., Garrity, C.P., Houseknecht, D.W., Amoroso, L., and Meares, D.C., 2005, Digital-elevation and surface-classification maps of the Fish Creek area, Harrison Bay quadrangle, northern Alaska: U.S. Geological Survey Open-File Report 2005-1192, Report: 10 p.; 3 Plates: 63 x 36 inches, https://doi.org/10.3133/ofr20051192.","productDescription":"Report: 10 p.; 3 Plates: 63 x 36 inches","onlineOnly":"Y","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":193335,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6586,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1192/","linkFileType":{"id":5,"text":"html"}},{"id":110570,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_72128.htm","linkFileType":{"id":5,"text":"html"},"description":"72128"}],"country":"United States","state":"Alaska","otherGeospatial":"Fish Creek area, Harrison Bay quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -153.4,\n 70.5\n ],\n [\n -153.4,\n 70\n ],\n [\n -150.9083,\n 70\n ],\n [\n -150.9083,\n 70.5\n ],\n [\n -153.4,\n 70.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64adee","contributors":{"authors":[{"text":"Mars, John L. jmars@usgs.gov","contributorId":3428,"corporation":false,"usgs":true,"family":"Mars","given":"John","email":"jmars@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":283331,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrity, Christopher P. 0000-0002-5565-1818 cgarrity@usgs.gov","orcid":"https://orcid.org/0000-0002-5565-1818","contributorId":644,"corporation":false,"usgs":true,"family":"Garrity","given":"Christopher","email":"cgarrity@usgs.gov","middleInitial":"P.","affiliations":[{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":283328,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Houseknecht, David W. 0000-0002-9633-6910 dhouse@usgs.gov","orcid":"https://orcid.org/0000-0002-9633-6910","contributorId":645,"corporation":false,"usgs":true,"family":"Houseknecht","given":"David","email":"dhouse@usgs.gov","middleInitial":"W.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":283329,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Amoroso, Lee lamoroso@usgs.gov","contributorId":3069,"corporation":false,"usgs":true,"family":"Amoroso","given":"Lee","email":"lamoroso@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":283330,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meares, Donald C.","contributorId":94753,"corporation":false,"usgs":true,"family":"Meares","given":"Donald","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":283332,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70930,"text":"pp1698 - 2005 - Energy resource studies, northern Front Range, Colorado","interactions":[],"lastModifiedDate":"2023-09-26T20:30:26.70182","indexId":"pp1698","displayToPublicDate":"2005-07-22T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1698","title":"Energy resource studies, northern Front Range, Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1698","usgsCitation":"2005, Energy resource studies, northern Front Range, Colorado (Version 1.0): U.S. Geological Survey Professional Paper 1698, Report: 162 p.; 1 Plate: 46.00 x 28.40 inches, https://doi.org/10.3133/pp1698.","productDescription":"Report: 162 p.; 1 Plate: 46.00 x 28.40 inches","costCenters":[],"links":[{"id":110571,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_72133.htm","linkFileType":{"id":5,"text":"html"},"description":"72133"},{"id":6590,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/2005/1698/","linkFileType":{"id":5,"text":"html"}},{"id":193339,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Northern Front Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -104.67754596687743,\n 40.578441020191974\n ],\n [\n -105.3720321877747,\n 40.578441020191974\n ],\n [\n -105.3720321877747,\n 39.803082794241476\n ],\n [\n -104.67754596687743,\n 39.803082794241476\n ],\n [\n -104.67754596687743,\n 40.578441020191974\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6679fd","contributors":{"editors":[{"text":"Fishman, Neil S.","contributorId":245198,"corporation":false,"usgs":false,"family":"Fishman","given":"Neil S.","affiliations":[{"id":49112,"text":"PetroLogic Solutions, LLC","active":true,"usgs":false}],"preferred":false,"id":884261,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":70929,"text":"ofr20051229 - 2005 - Rock-fall hazard assessment of Little Mill Campground, American Fork Canyon, Uinta National Forest, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"ofr20051229","displayToPublicDate":"2005-07-22T00:00:00","publicationYear":"2005","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":"2005-1229","title":"Rock-fall hazard assessment of Little Mill Campground, American Fork Canyon, Uinta National Forest, Utah","language":"ENGLISH","doi":"10.3133/ofr20051229","usgsCitation":"Coe, J.A., Harp, E.L., Tarr, A.C., and Michael, J.A., 2005, Rock-fall hazard assessment of Little Mill Campground, American Fork Canyon, Uinta National Forest, Utah (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2005-1229, 50 p. and 2 plates, https://doi.org/10.3133/ofr20051229.","productDescription":"50 p. and 2 plates","onlineOnly":"Y","costCenters":[],"links":[{"id":193338,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6589,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1229/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0fe4b07f02db5fe9a8","contributors":{"authors":[{"text":"Coe, Jeffrey A. 0000-0002-0842-9608 jcoe@usgs.gov","orcid":"https://orcid.org/0000-0002-0842-9608","contributorId":1333,"corporation":false,"usgs":true,"family":"Coe","given":"Jeffrey","email":"jcoe@usgs.gov","middleInitial":"A.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":283339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harp, Edwin L. harp@usgs.gov","contributorId":1290,"corporation":false,"usgs":true,"family":"Harp","given":"Edwin","email":"harp@usgs.gov","middleInitial":"L.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":283338,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tarr, Arthur C. atarr@usgs.gov","contributorId":1925,"corporation":false,"usgs":true,"family":"Tarr","given":"Arthur","email":"atarr@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":283341,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Michael, John A. jmichael@usgs.gov","contributorId":1877,"corporation":false,"usgs":true,"family":"Michael","given":"John","email":"jmichael@usgs.gov","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":283340,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70928,"text":"i2750B - 2005 - Principal areas of oil, natural gas, and coal production in the northern part of the Front Range, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"i2750B","displayToPublicDate":"2005-07-22T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2750","chapter":"B","title":"Principal areas of oil, natural gas, and coal production in the northern part of the Front Range, Colorado","language":"ENGLISH","doi":"10.3133/i2750B","usgsCitation":"Fishman, N.S., Roberts, S.B., Evans, J.M., and Olmstead, R.J., 2005, Principal areas of oil, natural gas, and coal production in the northern part of the Front Range, Colorado (Version 1.0): U.S. Geological Survey IMAP 2750, 1 sheet, 32 in. x 18 in., https://doi.org/10.3133/i2750B.","productDescription":"1 sheet, 32 in. x 18 in.","costCenters":[],"links":[{"id":110578,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73674.htm","linkFileType":{"id":5,"text":"html"},"description":"73674"},{"id":193337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6588,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i-2750-b/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f8e","contributors":{"authors":[{"text":"Fishman, Neil S.","contributorId":106464,"corporation":false,"usgs":true,"family":"Fishman","given":"Neil","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":283337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, Stephen B.","contributorId":104906,"corporation":false,"usgs":true,"family":"Roberts","given":"Stephen","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":283336,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Evans, John M.","contributorId":82009,"corporation":false,"usgs":true,"family":"Evans","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":283335,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Olmstead, Robert J.","contributorId":68417,"corporation":false,"usgs":true,"family":"Olmstead","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":283334,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70882,"text":"ofr20051132 - 2005 - Ground-magnetic studies of the Amargosa Desert region, California and Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"ofr20051132","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","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":"2005-1132","title":"Ground-magnetic studies of the Amargosa Desert region, California and Nevada","language":"ENGLISH","doi":"10.3133/ofr20051132","usgsCitation":"Blakely, R.J., Hillhouse, J.W., and Morin, R.L., 2005, Ground-magnetic studies of the Amargosa Desert region, California and Nevada (Version 1.0): U.S. Geological Survey Open-File Report 2005-1132, 23 p., https://doi.org/10.3133/ofr20051132.","productDescription":"23 p.","costCenters":[],"links":[{"id":186230,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6523,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1132/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d475","contributors":{"authors":[{"text":"Blakely, Richard J. 0000-0003-1701-5236 blakely@usgs.gov","orcid":"https://orcid.org/0000-0003-1701-5236","contributorId":1540,"corporation":false,"usgs":true,"family":"Blakely","given":"Richard","email":"blakely@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":283197,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hillhouse, John W. 0000-0002-1371-4622 jhillhouse@usgs.gov","orcid":"https://orcid.org/0000-0002-1371-4622","contributorId":2618,"corporation":false,"usgs":true,"family":"Hillhouse","given":"John","email":"jhillhouse@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":283198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morin, Robert L.","contributorId":82671,"corporation":false,"usgs":true,"family":"Morin","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":283199,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70903,"text":"ofr20041432 - 2005 - Mineral commodity profiles: cesium","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"ofr20041432","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","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":"2004-1432","title":"Mineral commodity profiles: cesium","language":"ENGLISH","doi":"10.3133/ofr20041432","usgsCitation":"Butterman, W.C., Brooks, W.E., and Reese, R.G., 2005, Mineral commodity profiles: cesium (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2004-1432, 13 p., https://doi.org/10.3133/ofr20041432.","productDescription":"13 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":186418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6553,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1432/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63589a","contributors":{"authors":[{"text":"Butterman, William C.","contributorId":35186,"corporation":false,"usgs":true,"family":"Butterman","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":283259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brooks, William E.","contributorId":104061,"corporation":false,"usgs":true,"family":"Brooks","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":283261,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reese, Robert G. Jr.","contributorId":72656,"corporation":false,"usgs":true,"family":"Reese","given":"Robert","suffix":"Jr.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":283260,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70898,"text":"sir20045218 - 2005 - Significance of the precambrian basement and late Cretaceous thrust nappes on the location of tertiary ore deposits in the Oquirrh Mountains, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"sir20045218","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","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":"2004-5218","title":"Significance of the precambrian basement and late Cretaceous thrust nappes on the location of tertiary ore deposits in the Oquirrh Mountains, Utah","docAbstract":"The Oquirrh Mountains are located in north central Utah, in the easternmost part of the Basin and Range physiographic\r\nprovince, immediately south of the Great Salt Lake. The range consists of a northerly trending alignment of peaks 56 km long. Tooele and Rush Valleys flank the Oquirrh Mountains on the western side and Salt Lake and Cedar Valleys lie on the eastern side. The world class Bingham mine in the central part of the range hosts disseminated copper-bearing porphyry, skarn, base-and precious-metal vein and replacement ore deposits. The district includes the outlying Barneys Canyon disseminated-gold deposits. Disseminated gold in the Mercur mining district in the southern part of the range has become exhausted. The Ophir and Stockton base- and precious-metal mining districts in the range north of Mercur also are inactive. A geologic map of the range (Tooker and Roberts, 1998), available at a scale of 1:50,000, is a summation of U.S. Geological\r\nSurvey (USGS) studies.\r\n\r\nInformation about the range and its mining areas is scattered. This report summarizes map locations, new stratigraphic and structural data, and reexamined data from an extensive published record. Unresolved controversial geological interpretations are considered, and, for the first time, the complete geological evidence provides a consistent regional basis for the location of the ore deposits in the range. The geological setting and the siting of mineral deposits in the Oquirrh Mountains began with the formation of a Precambrian craton. Exposures of folded Proterozoic basement rocks of the craton, in the Wasatch Mountains east of Salt Lake City, were accreted and folded onto an Archean crystalline rock terrane. The accretion suture lies along the north flank of the Uinta Mountains. The western part of the accreted block was offset to northern Utah along a north-trending fault lying approximately along the Wasatch Front (Nelson and others,\r\n2002), thereby creating a prominant basement barrier or buttress east of the Salt Lake area.\r\n\r\nThe accretion suture along the north flank of the Uinta\r\nAnticline overlaps an earlier Precambrian east-west mobile\r\nzone, the Uinta trend (Erickson, 1976, Bryant and Nichols,\r\n1988 and John, 1989), which extends westward across western\r\nUtah and into Nevada. A trace of the trend underlies the\r\nmiddle part of the Oquirrh Mountains. Its structure is recognized by disrupted Paleozoic stratigraphic units and fold and fault evidence of thrust faulting, intermittent local uplift and erosion, the alignment of Tertiary intrusives and associated ore deposits. Geologic readjustments along the trend continued intermittently through the Paleozoic, Cenozoic, Tertiary, and the development of clastic deposits along the shores of Pleistocene Lake Bonneville. \r\n\r\nPaleozoic sedimentary rocks were deposited on the craton platform shelf in westernmost Utah and eastern Nevada as the shelf subsided gradually and differentially. Debris was shed into two basins separated by the uplifted Uinta trend, the Oquirrh Basin on the south and Sublette Basin on the north. Sediments were derived from the craton to the east, the Antler orogenic zone on the west (Roberts, 1964), and locally from uplifted parts of the trend itself. Thick accumulations of clastic calcareous quartzite, shale, limestone, and dolomite of Lower and Upper Paleozoic ages are now exposed in the Oquirrh Mountains, the result of thrust faults.\r\n\r\nEvidence of decollement thrust faults in in the Wasatch Mountains during the Late Cretaceous Sevier orogeny, recognized by Baker and others (1949) and Crittenden (1961, is also recognized in the Oquirrh Mountains by Roberts and others (1965). During the late Cretaceous Sevier Orogeny, nappes were thrust sequentially along different paths from\r\ntheir western hinterland to the foreland. Five distinct nappes converged over the Uinta trend onto an uplifted west-plunging basement buttress east of the Oquirrh Mountains area: the Pass Canyon, Bingham,","language":"ENGLISH","doi":"10.3133/sir20045218","usgsCitation":"Tooker, E.W., 2005, Significance of the precambrian basement and late Cretaceous thrust nappes on the location of tertiary ore deposits in the Oquirrh Mountains, Utah: U.S. Geological Survey Scientific Investigations Report 2004-5218, 73 p., https://doi.org/10.3133/sir20045218.","productDescription":"73 p.","costCenters":[],"links":[{"id":185514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6549,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5218/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3d47","contributors":{"authors":[{"text":"Tooker, Edwin W.","contributorId":26345,"corporation":false,"usgs":true,"family":"Tooker","given":"Edwin","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":283244,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70895,"text":"fs20053067 - 2005 - Using radar to understand migratory birds and their habitats: Critical needs for the Gulf of Mexico","interactions":[],"lastModifiedDate":"2016-09-15T11:00:07","indexId":"fs20053067","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","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":"2005-3067","title":"Using radar to understand migratory birds and their habitats: Critical needs for the Gulf of Mexico","docAbstract":"Nearly all Neotropical migratory landbird species of the eastern United States as well as many western species use Louisiana and the northern Gulf of Mexico coast during their transcontinental migrations each spring and fall. Radar has determined that hundreds of millions of birds make the nocturnal crossing of the Gulf of Mexico resulting in daily flights of as many as 2.5 million individuals stopping in Louisiana to feed and rest. These migration landings are so spectacular that the term “fallout” has been coined to describe the concentrations of birds arriving on the coast.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20053067","usgsCitation":"Smith, G.J., and Barrow, W., 2005, Using radar to understand migratory birds and their habitats: Critical needs for the Gulf of Mexico: U.S. Geological Survey Fact Sheet 2005-3067, 2 p., https://doi.org/10.3133/fs20053067.","productDescription":"2 p.","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":122400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3067.jpg"},{"id":6546,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/2005-3067.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":10925,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/2005-3067/2005-3067.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603ca2","contributors":{"authors":[{"text":"Smith, Gregory J. gsmith@usgs.gov","contributorId":3436,"corporation":false,"usgs":true,"family":"Smith","given":"Gregory","email":"gsmith@usgs.gov","middleInitial":"J.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":283237,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barrow, Wylie 0000-0003-4671-2823","orcid":"https://orcid.org/0000-0003-4671-2823","contributorId":90684,"corporation":false,"usgs":true,"family":"Barrow","given":"Wylie","affiliations":[],"preferred":false,"id":283238,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70890,"text":"ofr20051207 - 2005 - Summary of supporting data for USGS regional heat-flow studies of the Great Basin, 1970-1990","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"ofr20051207","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","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":"2005-1207","title":"Summary of supporting data for USGS regional heat-flow studies of the Great Basin, 1970-1990","language":"ENGLISH","doi":"10.3133/ofr20051207","usgsCitation":"Sass, J.H., Priest, S.S., Lachenbruch, A.H., Galanis, S.P., Moses, T.H., Kennelly, J.P., Munroe, R.J., Smith, E.P., Grubb, F.V., Husk, R.H., and Mase, C.W., 2005, Summary of supporting data for USGS regional heat-flow studies of the Great Basin, 1970-1990 (Online Version 1.0): U.S. Geological Survey Open-File Report 2005-1207, online, https://doi.org/10.3133/ofr20051207.","productDescription":"online","costCenters":[],"links":[{"id":186329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6543,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1207/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db69899a","contributors":{"authors":[{"text":"Sass, John H.","contributorId":69596,"corporation":false,"usgs":true,"family":"Sass","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":283229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Priest, Susan S. spriest@usgs.gov","contributorId":30204,"corporation":false,"usgs":true,"family":"Priest","given":"Susan","email":"spriest@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":false,"id":283227,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lachenbruch, Arthur H.","contributorId":27850,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"Arthur","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":283225,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Galanis, S. Peter pgalanis@usgs.gov","contributorId":3289,"corporation":false,"usgs":true,"family":"Galanis","given":"S.","email":"pgalanis@usgs.gov","middleInitial":"Peter","affiliations":[],"preferred":true,"id":283220,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moses, Thomas H. Jr.","contributorId":65861,"corporation":false,"usgs":true,"family":"Moses","given":"Thomas","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":283228,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kennelly, John P. Jr.","contributorId":29696,"corporation":false,"usgs":true,"family":"Kennelly","given":"John","suffix":"Jr.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":283226,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Munroe, Robert J.","contributorId":12039,"corporation":false,"usgs":true,"family":"Munroe","given":"Robert","email":"","middleInitial":"J.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":283224,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Smith, Eugene P.","contributorId":87026,"corporation":false,"usgs":true,"family":"Smith","given":"Eugene","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":283230,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Grubb, Frederick V. fgrubb@usgs.gov","contributorId":4066,"corporation":false,"usgs":true,"family":"Grubb","given":"Frederick","email":"fgrubb@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":283221,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Husk, Robert H. Jr.","contributorId":9124,"corporation":false,"usgs":true,"family":"Husk","given":"Robert","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":283223,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Mase, Charles W.","contributorId":8724,"corporation":false,"usgs":true,"family":"Mase","given":"Charles","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":283222,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}} ,{"id":70905,"text":"ofr20051087 - 2005 - A guide to the proper selection and use of federally approved sediment and water-quality samplers","interactions":[],"lastModifiedDate":"2015-10-15T13:47:31","indexId":"ofr20051087","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","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":"2005-1087","title":"A guide to the proper selection and use of federally approved sediment and water-quality samplers","docAbstract":"The Federal Interagency Sedimentation Project (FISP) was created in 1939 to unify and standardize the research and development activities of Federal agencies involved in fluvial sediment studies1,2. Research and development conducted by the FISP originally focused on hydraulic and mechanical aspects of sediment sampling. The mission of the FISP has expanded to provide, identify, and evaluate tools and techniques for accurate, standardized, calibrated, cost-efficient, and safe measurement and analysis of sediment properties and transport. FISP activities focus on measurement and analysis of suspended sediment, bedload sediment, bed material, bed topography, adsorbed constituents, sediment characteristics, and water quality. Sponsoring agencies and the public gain a distinct advantage from the cooperative action that leads to common standards, methods, equipment, and procedures for the measurement and characterization of sediment.
\nAs interest in the health of rivers and streams increases3, and new water-quality regulations4 are promulgated, interest in sediment and water-quality sampling equipment and technologies has increased. While much information on the subject exists, a comprehensive summary document of sediment sampling equipment and technology is lacking. This report seeks to provide such a summary.
","language":"English","publisher":"U.S. Geological Society","doi":"10.3133/ofr20051087","usgsCitation":"Davis, B.E., and Federal Interagency Sedimentation Project, 2005, A guide to the proper selection and use of federally approved sediment and water-quality samplers: U.S. Geological Survey Open-File Report 2005-1087, iv, 20 p., https://doi.org/10.3133/ofr20051087.","productDescription":"iv, 20 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":193056,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6572,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1087/","linkFileType":{"id":5,"text":"html"}},{"id":309948,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1087/pdf/OFR_2005-1087.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae4ee","contributors":{"authors":[{"text":"Davis, Broderick E.","contributorId":23394,"corporation":false,"usgs":true,"family":"Davis","given":"Broderick","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":283264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Federal Interagency Sedimentation Project","contributorId":128255,"corporation":true,"usgs":false,"organization":"Federal Interagency Sedimentation Project","id":534709,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70901,"text":"sir20055081 - 2005 - Augmenting two-dimensional hydrodynamic simulations with measured velocity data to identify flow paths as a function of depth on Upper St. Clair River in the Great Lakes basin","interactions":[],"lastModifiedDate":"2016-10-06T15:12:53","indexId":"sir20055081","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","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":"2005-5081","title":"Augmenting two-dimensional hydrodynamic simulations with measured velocity data to identify flow paths as a function of depth on Upper St. Clair River in the Great Lakes basin","docAbstract":"Upper St. Clair River, which receives outflow from Lake Huron, is characterized by flow velocities that exceed 7 feet per second and significant channel curvature that creates complex flow patterns downstream from the Blue Water Bridge in the Port Huron, Michigan, and Sarnia, Ontario, area. Discrepancies were detected between depth-averaged velocities previously simulated by a two-dimensional (2D) hydrodynamic model and surface velocities determined from drifting buoy deployments. A detailed ADCP (acoustic Doppler current profiler) survey was done on Upper St. Clair River during July 1–3, 2003, to help resolve these discrepancies.
As part of this study, a refined finite-element mesh of the hydrodynamic model used to identify source areas to public water intakes was developed for Upper St. Clair River. In addition, a numerical procedure was used to account for radial accelerations, which cause secondary flow patterns near channel bends. The refined model was recalibrated to better reproduce local velocities measured in the ADCP survey. ADCP data also were used to help resolve the remaining discrepancies between simulated and measured velocities and to describe variations in velocity with depth.
Velocity data from ADCP surveys have significant local variability, and statistical processing is needed to compute reliable point estimates. In this study, velocity innovations were computed for seven depth layers posited within the river as the differences between measured and simulated velocities. For each layer, the spatial correlation of velocity innovations was characterized by use of variogram analysis. Results were used with kriging to compute expected innovations within each layer at applicable model nodes. Expected innovations were added to simulated velocities to form integrated velocities, which were used with reverse particle tracking to identify the expected flow path near a sewage outfall as a function of flow depth.
Expected particle paths generated by use of the integrated velocities showed that surface velocities in the upper layers tended to originate nearer the Canadian shoreline than velocities near the channel bottom in the lower layers. Therefore, flow paths to U.S. public water intakes located on the river bottom are more likely to be in the United States than withdrawals near the water surface. Integrated velocities in the upper layers are generally consistent with the surface velocities indicated by drifting-buoy deployments. Information in the 2D hydrodynamic model and the ADCP measurements was insufficient to describe the vertical flow component. This limitation resulted in the inability to account for vertical movements on expected flow paths through Upper St. Clair River. A three dimensional hydrodynamic model would be needed to account for these effects.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055081","collaboration":"In cooperation with the American Water Works Association Research Foundation","usgsCitation":"Holtschlag, D., and Koschik, J., 2005, Augmenting two-dimensional hydrodynamic simulations with measured velocity data to identify flow paths as a function of depth on Upper St. Clair River in the Great Lakes basin: U.S. Geological Survey Scientific Investigations Report 2005-5081, v, 36 p., https://doi.org/10.3133/sir20055081.","productDescription":"v, 36 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":186330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055081.JPG"},{"id":6551,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5081/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6680d4","contributors":{"authors":[{"text":"Holtschlag, D. J. 0000-0001-5185-4928","orcid":"https://orcid.org/0000-0001-5185-4928","contributorId":102493,"corporation":false,"usgs":true,"family":"Holtschlag","given":"D. J.","affiliations":[],"preferred":false,"id":283255,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koschik, J.A.","contributorId":101711,"corporation":false,"usgs":true,"family":"Koschik","given":"J.A.","affiliations":[],"preferred":false,"id":283254,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70894,"text":"fs20053069 - 2005 - Migratory bird pathways and the Gulf of Mexico: Importance of Louisiana's coast","interactions":[],"lastModifiedDate":"2016-09-15T11:02:22","indexId":"fs20053069","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","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":"2005-3069","title":"Migratory bird pathways and the Gulf of Mexico: Importance of Louisiana's coast","docAbstract":"Because of its geographic position, Louisiana plays an important role in the hemispheric-scale phenomenon known as the Nearctic-Neotropical bird migration system. Each year millions of landbirds migrate across or near to the coast of the Gulf of Mexico. Birds migrate in large, broad fronts that sometimes exceed 2 million individuals, and there is an advantage for them to take a direct north-south route (the shortest distance).
Migrants en route tend to concentrate in habitats adjacent to ecological barriers; DOI land managers need to identify key coastal landscape features that are important to these birds.
Because of the vastness of the North American continent, it is nearly impossible to delineate movement patterns and migration pathways by using traditional ground-based surveys.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20053069","usgsCitation":"Smith, G.J., and Barrow, W., 2005, Migratory bird pathways and the Gulf of Mexico: Importance of Louisiana's coast: U.S. Geological Survey Fact Sheet 2005-3069, 1 p., https://doi.org/10.3133/fs20053069.","productDescription":"1 p.","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":126880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3069.jpg"},{"id":6545,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/2005-3069.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":10926,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://archive.usgs.gov/archive/sites/www.nwrc.usgs.gov/factshts/2005-3069/2005-3069.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635592","contributors":{"authors":[{"text":"Smith, Gregory J. gsmith@usgs.gov","contributorId":3436,"corporation":false,"usgs":true,"family":"Smith","given":"Gregory","email":"gsmith@usgs.gov","middleInitial":"J.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":283235,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barrow, Wylie 0000-0003-4671-2823","orcid":"https://orcid.org/0000-0003-4671-2823","contributorId":90684,"corporation":false,"usgs":true,"family":"Barrow","given":"Wylie","affiliations":[],"preferred":false,"id":283236,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70875,"text":"fs20053039 - 2005 - Coral microbial ecology","interactions":[],"lastModifiedDate":"2012-02-02T00:13:48","indexId":"fs20053039","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","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":"2005-3039","title":"Coral microbial ecology","language":"ENGLISH","doi":"10.3133/fs20053039","usgsCitation":"Kellogg, C., 2005, Coral microbial ecology (Online only): U.S. Geological Survey Fact Sheet 2005-3039, 4 p., https://doi.org/10.3133/fs20053039.","productDescription":"4 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6516,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3039/","linkFileType":{"id":5,"text":"html"}},{"id":121171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3039.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6855b9","contributors":{"authors":[{"text":"Kellogg, Christina","contributorId":76013,"corporation":false,"usgs":true,"family":"Kellogg","given":"Christina","affiliations":[],"preferred":false,"id":283180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70878,"text":"ofr20051070 - 2005 - Moloka'i benthic habitat mapping","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"ofr20051070","displayToPublicDate":"2005-07-18T00:00:00","publicationYear":"2005","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":"2005-1070","title":"Moloka'i benthic habitat mapping","language":"ENGLISH","doi":"10.3133/ofr20051070","usgsCitation":"Cochran-Marquez, S.A., 2005, Moloka'i benthic habitat mapping (Version 1.0): U.S. Geological Survey Open-File Report 2005-1070, 18 p., https://doi.org/10.3133/ofr20051070.","productDescription":"18 p.","costCenters":[],"links":[{"id":186071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6519,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1070/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699246","contributors":{"authors":[{"text":"Cochran-Marquez, Susan A.","contributorId":22855,"corporation":false,"usgs":true,"family":"Cochran-Marquez","given":"Susan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":283185,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}