{"pageNumber":"2569","pageRowStart":"64200","pageSize":"25","recordCount":184617,"records":[{"id":70113,"text":"ofr20051042 - 2005 - Construction, Geologic, and Hydrologic Data from Five Exploratory Wells on Rota, Commonwealth of the Northern Mariana Islands, 1999","interactions":[],"lastModifiedDate":"2012-03-08T17:16:18","indexId":"ofr20051042","displayToPublicDate":"2005-02-24T00:00:00","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":"2005-1042","title":"Construction, Geologic, and Hydrologic Data from Five Exploratory Wells on Rota, Commonwealth of the Northern Mariana Islands, 1999","docAbstract":"Rota is the southernmost of the 14 small islands that make up the Commonwealth of the Northern Mariana Islands. Reduced springflow at Matan Hanom and As Onan springs occurred during a drought associated with the 1997-98 El Nino. Water from the two developed springs constituted the only municipal water source for the island at that time. In April 1998, reduced water supplies forced the Commonwealth Utilities Corporation to restrict water service in the principal villages of Songsong and Sinapalu for the duration of the dry season.\r\n\r\nIn 1999, Five exploratory wells, EX-1 through EX-5 (CUC wells SP-MW1, SP-1, -2, -3, and SP-MW2), were drilled in the Sinapalu region of Rota to (1) assess the availability of fresh ground-water resources in an area where no other well information were available, and (2) to provide a new water source to help mitigate the impacts of drought associated with recurring El Nino weather events. The wells penetrated mainly light colored (dirty white to brownish), fragmental limestones containing abundant coral remains.\r\n\r\nSustained-rate, recovery, and step-drawdown aquifer tests were attempted at each of the five exploratory wells to estimate aquifer properties in the vicinity of the wells and to assess the potential for new water sources. At wells EX-1 (CUC well SPMW1) and EX-5 (CUC well SP-MW2), attempts to conduct sustained-rate aquifer tests resulted in excessive drawdown to the pump intakes in the vicinity of the wells. At well EX-2 (CUC well SP-1), the maximum drawdown measured in the pumped well was 3.93 ft during 8 days of sustained pumping at an average rate of 187 gal/min. At well EX-3 (CUC well SP-2), the maximum drawdown measured in the pumped well was 2.31 ft during 8 days of sustained pumping at an average rate of 108 gal/min, and at well EX-4 (CUC well SP-3), the maximum drawdown measured in the pumped well was 3.27 ft during 8 days of sustained pumping at an average rate of 139 gal/min. Specific conductance at the end of 8 days of pumping was 403, 358, and 445 ?S/cm at well EX-2, EX-3, and EX-4 (CUC wells SP-1, -2, and -3), respectively.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20051042","collaboration":"Prepared in cooperation with the Commonwealth Utilities Corporation, Commonwealth of the Northern Mariana Islands","usgsCitation":"Carruth, R., 2005, Construction, Geologic, and Hydrologic Data from Five Exploratory Wells on Rota, Commonwealth of the Northern Mariana Islands, 1999: U.S. Geological Survey Open-File Report 2005-1042, Report: v, 40 p.; 12 Tables; 10 Appendices, https://doi.org/10.3133/ofr20051042.","productDescription":"Report: v, 40 p.; 12 Tables; 10 Appendices","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":193284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6825,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1042/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 145.08333333333334,14.083333333333334 ], [ 145.08333333333334,14.25 ], [ 145.33333333333334,14.25 ], [ 145.33333333333334,14.083333333333334 ], [ 145.08333333333334,14.083333333333334 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698462","contributors":{"authors":[{"text":"Carruth, Rob 0000-0001-7008-2927 rlcarr@usgs.gov","orcid":"https://orcid.org/0000-0001-7008-2927","contributorId":1162,"corporation":false,"usgs":true,"family":"Carruth","given":"Rob","email":"rlcarr@usgs.gov","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":false,"id":281877,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70117,"text":"sir20045132 - 2005 - Simulation of ground-water flow to assess geohydrologic factors and their effect on source-water areas for bedrock wells in Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"sir20045132","displayToPublicDate":"2005-02-24T00:00:00","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":"2004-5132","title":"Simulation of ground-water flow to assess geohydrologic factors and their effect on source-water areas for bedrock wells in Connecticut","docAbstract":"Generic ground-water-flow simulation models show that geohydrologic factors?fracture types, fracture geometry, and surficial materials?affect the size, shape, and location of source-water areas for bedrock wells. In this study, conducted by the U.S. Geological Survey in cooperation with the Connecticut Department of Public Health, ground-water flow was simulated to bedrock wells in three settings?on hilltops and hillsides with no surficial aquifer, in a narrow valley with a surficial aquifer, and in a broad valley with a surficial aquifer?to show how different combinations of geohydrologic factors in different topographic settings affect the dimensions and locations of source-water areas in Connecticut. \r\n\r\nThree principal types of fractures are present in bedrock in Connecticut?(1) Layer-parallel fractures, which developed as partings along bedding in sedimentary rock and compositional layering or foliation in metamorphic rock (dips of these fractures can be gentle or steep); (2) unroofing joints, which developed as strain-release fractures parallel to the land surface as overlying rock was removed by erosion through geologic time; and (3) cross fractures and joints, which developed as a result of tectonically generated stresses that produced typically near-vertical or steeply dipping fractures.\r\n\r\nFracture geometry is defined primarily by the presence or absence of layering in the rock unit, and, if layered, by the angle of dip in the layering. Where layered rocks dip steeply, layer-parallel fracturing generally is dominant; unroofing joints also are typically well developed. Where layered rocks dip gently, layer-parallel fracturing also is dominant, and connections among these fractures are provided only by the cross fractures. In gently dipping rocks, unroofing joints generally do not form as a separate fracture set; instead, strain release from unroofing has occurred along gently dipping layer-parallel fractures, enhancing their aperture. In nonlayered and variably layered rocks, layer-parallel fracturing is absent or poorly developed; fracturing is dominated by well-developed subhorizontal unroofing joints and steeply dipping, tectonically generated fractures and (or) cooling joints. Cross fractures (or cooling joints) in nonlayered and variably layered rocks have more random orientations than in layered rocks. Overall, nonlayered or variably layered rocks do not have a strongly developed fracture direction.\r\n\r\nGeneric ground-water-flow simulation models showed that fracture geometry and other geohydrologic factors affect the dimensions and locations of source-water areas for bedrock wells. In general, source-water areas to wells reflect the direction of ground-water flow, which mimics the land-surface topography. Source-water areas to wells in a hilltop setting were not affected greatly by simulated fracture zones, except for an extensive vertical fracture zone. Source-water areas to wells in a hillside setting were not affected greatly by simulated fracture zones, except for the combination of a subhorizontal fracture zone and low bedrock vertical hydraulic conductivity, as might be the case where an extensive subhorizontal fracture zone is not connected or is poorly connected to the surface through vertical fractures. \r\n\r\nSource-water areas to wells in a narrow valley setting reflect complex ground-water-flow paths. The typical flow path originates in the uplands and passes through either till or bedrock into the surficial aquifer, although only a small area of the surficial aquifer actually contributes water to the well. Source-water areas in uplands can include substantial areas on both sides of a river. Source-water areas for wells in this setting are affected mainly by the rate of ground-water recharge and by the degree of anisotropy. Source-water areas to wells in a broad valley setting (bedrock with a low angle of dip) are affected greatly by fracture properties. The effect of a given fracture is to channel the ","language":"ENGLISH","doi":"10.3133/sir20045132","usgsCitation":"Starn, J.J., and Stone, J., 2005, Simulation of ground-water flow to assess geohydrologic factors and their effect on source-water areas for bedrock wells in Connecticut (Version 1.0, online only): U.S. Geological Survey Scientific Investigations Report 2004-5132, 86 p., https://doi.org/10.3133/sir20045132.","productDescription":"86 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":191538,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6829,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5132/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","edition":"Version 1.0, online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eb6e","contributors":{"authors":[{"text":"Starn, J. Jeffrey","contributorId":101617,"corporation":false,"usgs":true,"family":"Starn","given":"J.","email":"","middleInitial":"Jeffrey","affiliations":[],"preferred":false,"id":281890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stone, Janet Radway","contributorId":72793,"corporation":false,"usgs":true,"family":"Stone","given":"Janet Radway","affiliations":[],"preferred":false,"id":281889,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70122,"text":"sir20055037 - 2005 - Mercury accumulation by lower trophic-level organisms in lentic systems within the Guadalupe River watershed, California","interactions":[],"lastModifiedDate":"2020-02-03T19:52:42","indexId":"sir20055037","displayToPublicDate":"2005-02-24T00:00:00","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":"2005-5037","title":"Mercury accumulation by lower trophic-level organisms in lentic systems within the Guadalupe River watershed, California","docAbstract":"The water columns of four reservoirs (Almaden, Calero, Guadalupe and Lexington Reservoirs) and an abandoned quarry pit filled by Alamitos Creek drainage for recreational purposes (Lake Almaden) were sampled on September 14 and 15, 2004 to provide the first measurements of mercury accumulation by phytoplankton and zooplankton in lentic systems (bodies of standing water, as in lakes and reservoirs) within the Guadalupe River watershed, California. Because of widespread interest in ecosystem effects associated with historic mercury mining within and downgradient of the Guadalupe Riverwatershed, transfer of mercury to lower trophic-level organisms was examined. The propensity of mercury to bioaccumulate, particularly in phytoplankton and zooplankton at the base of the food web, motivated this attempt to provide information in support of developing trophic-transfer and solute-transport models for the watershed, and hence in support of subsequent evaluation of load-allocation strategies. Both total mercury and methylmercury were examined in these organisms. \r\n\r\nDuring a single sampling event, replicate samples from the reservoir water column were collected and processed for dissolved-total mercury, dissolved-methylmercury, phytoplankton mercury speciation, phytoplankton taxonomy and biomass, zooplankton mercury speciation, and zooplankton taxonomy and biomass. The timing of this sampling event was coordinated with sampling and analysis of fish from these five water bodies, during a period of the year when vertical stratification in the reservoirs generates a primary source of methylmercury to the watershed. Ancillary data, including dissolved organic carbon and trace-metal concentrations as well as vertical profiles of temperature, dissolved oxygen, specific conductance and pH, were gathered to provide a water-quality framework from which to compare the results for mercury. This work, in support of the Guadalupe River Mercury Total Maximum Daily Load (TMDL) Study, provides the first measurements of mercury trophic transfer through planktonic communities in this watershed. It is worth reemphasizing that this data set represents a single ?snap shot? of conditions in water bodies within the Guadalupe River watershed to: (1) fill gaps in trophic transfer information, and (2) provide a scientific basis for future process-based studies with enhanced temporal and spatial coverage. This electronic document was unconventionally formatted to enhance the accessibility of information to a wide range of interest groups.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055037","usgsCitation":"Kuwabara, J.S., Topping, B.R., Moon, G.E., Husby, P., Lincoff, A., Carter, J.L., and Croteau, M., 2005, Mercury accumulation by lower trophic-level organisms in lentic systems within the Guadalupe River watershed, California: U.S. Geological Survey Scientific Investigations Report 2005-5037, 59 p., https://doi.org/10.3133/sir20055037.","productDescription":"59 p.","onlineOnly":"Y","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":191699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6834,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5037/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","country":"United States","state":"California","otherGeospatial":"Guadalupe River watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.18170166015625,\n              37.801103690609615\n            ],\n            [\n              -121.35498046875,\n              37.801103690609615\n            ],\n            [\n              -121.35498046875,\n              38.24249456800328\n            ],\n            [\n              -122.18170166015625,\n              38.24249456800328\n            ],\n            [\n              -122.18170166015625,\n              37.801103690609615\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624622","contributors":{"authors":[{"text":"Kuwabara, James S. 0000-0003-2502-1601 kuwabara@usgs.gov","orcid":"https://orcid.org/0000-0003-2502-1601","contributorId":3374,"corporation":false,"usgs":true,"family":"Kuwabara","given":"James","email":"kuwabara@usgs.gov","middleInitial":"S.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":281910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Topping, Brent R. 0000-0002-7887-4221 btopping@usgs.gov","orcid":"https://orcid.org/0000-0002-7887-4221","contributorId":1484,"corporation":false,"usgs":true,"family":"Topping","given":"Brent","email":"btopping@usgs.gov","middleInitial":"R.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":281908,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moon, Gerald E.","contributorId":11288,"corporation":false,"usgs":true,"family":"Moon","given":"Gerald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":281911,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Husby, Peter","contributorId":35405,"corporation":false,"usgs":true,"family":"Husby","given":"Peter","email":"","affiliations":[],"preferred":false,"id":281914,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lincoff, Andrew","contributorId":29076,"corporation":false,"usgs":true,"family":"Lincoff","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":281913,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Carter, James L. 0000-0002-0104-9776 jlcarter@usgs.gov","orcid":"https://orcid.org/0000-0002-0104-9776","contributorId":3278,"corporation":false,"usgs":true,"family":"Carter","given":"James","email":"jlcarter@usgs.gov","middleInitial":"L.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":281909,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Croteau, Marie-Noële","contributorId":22863,"corporation":false,"usgs":true,"family":"Croteau","given":"Marie-Noële","affiliations":[],"preferred":false,"id":281912,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70211109,"text":"70211109 - 2005 - Reply to “Commentary: Assessment of past infiltration fluxes through Yucca Mountain on the basis of the secondary mineral record—Is it a viable methodology?” by Y.V. Dublyansky and S.Z. Smirnov","interactions":[],"lastModifiedDate":"2020-07-14T22:09:44.951946","indexId":"70211109","displayToPublicDate":"2005-02-23T16:46:42","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2233,"text":"Journal of Contaminant Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Reply to “Commentary: Assessment of past infiltration fluxes through Yucca Mountain on the basis of the secondary mineral record—Is it a viable methodology?” by Y.V. Dublyansky and S.Z. Smirnov","docAbstract":"<p>Many of the comments by Dublyansky and Smirnov (2005) on Marshall et al. (2003) reflect a longstanding debate over the origin of secondary calcite and opal deposits found in cavities and on fracture surfaces at Yucca Mountain, Nevada, site of a proposed high-level nuclear waste repository (US Department of Energy, 2001). These comments require consideration of data and interpretations beyond the scope of Marshall et al. (2003). Dublyansky et al. (2004) and Dublyansky et al. (2005) also have commented on papers published by Whelan et al. (2002) and Wilson et al. (2003), and we will refer to the replies to those comments (Whelan et al., 2004, Wilson and Cline, 2005) in addressing the comments that go beyond the scope of Marshall et al. (2003).</p>","language":"English","publisher":"Elsevier","doi":"10.1016/j.jconhyd.2005.01.002","usgsCitation":"Marshall, B.D., Neymark, L., and Peterman, Z.E., 2005, Reply to “Commentary: Assessment of past infiltration fluxes through Yucca Mountain on the basis of the secondary mineral record—Is it a viable methodology?” by Y.V. Dublyansky and S.Z. Smirnov: Journal of Contaminant Hydrology, v. 77, no. 3, p. 219-224, https://doi.org/10.1016/j.jconhyd.2005.01.002.","productDescription":"6 p.","startPage":"219","endPage":"224","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":376394,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Yucca Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.48254394531249,\n              36.91352904330221\n            ],\n            [\n              -116.43602371215822,\n              36.91352904330221\n            ],\n            [\n              -116.43602371215822,\n              36.95757376878687\n            ],\n            [\n              -116.48254394531249,\n              36.95757376878687\n            ],\n            [\n              -116.48254394531249,\n              36.91352904330221\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"77","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Marshall, Brian D. 0000-0002-8093-0093 bdmarsha@usgs.gov","orcid":"https://orcid.org/0000-0002-8093-0093","contributorId":520,"corporation":false,"usgs":true,"family":"Marshall","given":"Brian","email":"bdmarsha@usgs.gov","middleInitial":"D.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":792791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neymark, Leonid A. 0000-0003-4190-0278 lneymark@usgs.gov","orcid":"https://orcid.org/0000-0003-4190-0278","contributorId":140338,"corporation":false,"usgs":true,"family":"Neymark","given":"Leonid A.","email":"lneymark@usgs.gov","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":792792,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterman, Zell E. 0000-0002-5694-8082 peterman@usgs.gov","orcid":"https://orcid.org/0000-0002-5694-8082","contributorId":167699,"corporation":false,"usgs":true,"family":"Peterman","given":"Zell","email":"peterman@usgs.gov","middleInitial":"E.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":792793,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70105,"text":"sir20045296 - 2005 - Geological, hydrological, and biological issues related to the proposed development of a park at the confluence of the Los Angeles River and the Arroyo Seco, Los Angeles County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"sir20045296","displayToPublicDate":"2005-02-22T00:00:00","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":"2004-5296","title":"Geological, hydrological, and biological issues related to the proposed development of a park at the confluence of the Los Angeles River and the Arroyo Seco, Los Angeles County, California","docAbstract":"A new park is being considered for the confluence of the Los Angeles River and the Arroyo Seco in Los Angeles County, California. Components of the park development may include creation of a temporary lake on the Los Angeles River, removal of channel lining along part of the Arroyo Seco, restoration of native plants, creation of walking paths, and building of facilities such as a boat ramp and a visitor center. This report, prepared in cooperation with the Mountains Recreation and Conservancy Authority, delineates the geological, hydrological, and biological issues that may have an impact on the park development or result from development at the confluence, and identifies a set a tasks to help address these science issues.\r\n\r\nGeologic issues of concern relate to surface faulting, earthquake ground motions, liquefaction, landsliding, and induced seismicity. Hydrologic issues of concern relate to the hydraulics and water quality of both surface water and ground water. Biological issues of concern include colonization-extinction dynamics, wildlife corridors, wildlife reintroduction, non-native species, ecotoxicology, and restoration of local habitat and ecology. Potential tasks include (1) basic data collection and follow-up monitoring, and (2) statistical and probabilistic analyses and simulation modeling of the seismic, hydraulic, and ecological processes that may have the greatest impact on the park. The science issues and associated tasks delineated for the proposed confluence park will also have transfer value for river restoration in other urban settings.","language":"ENGLISH","doi":"10.3133/sir20045296","usgsCitation":"Land, M., Trenham, P.C., Ponti, D.J., Reichard, E.G., Tinsley, J., Warrick, J., and Meyer, R.W., 2005, Geological, hydrological, and biological issues related to the proposed development of a park at the confluence of the Los Angeles River and the Arroyo Seco, Los Angeles County, California (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5296, 56 p., https://doi.org/10.3133/sir20045296.","productDescription":"56 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":192998,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6791,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5296/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68744f","contributors":{"authors":[{"text":"Land, Michael 0000-0001-5141-0307","orcid":"https://orcid.org/0000-0001-5141-0307","contributorId":56613,"corporation":false,"usgs":true,"family":"Land","given":"Michael","affiliations":[],"preferred":false,"id":281867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trenham, Peter C.","contributorId":11710,"corporation":false,"usgs":true,"family":"Trenham","given":"Peter","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":281866,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ponti, Daniel J. 0000-0002-2437-5144 dponti@usgs.gov","orcid":"https://orcid.org/0000-0002-2437-5144","contributorId":1020,"corporation":false,"usgs":true,"family":"Ponti","given":"Daniel","email":"dponti@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":281862,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reichard, Eric G. 0000-0002-7310-3866 egreich@usgs.gov","orcid":"https://orcid.org/0000-0002-7310-3866","contributorId":1207,"corporation":false,"usgs":true,"family":"Reichard","given":"Eric","email":"egreich@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":281863,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tinsley, John C. III jtinsley@usgs.gov","contributorId":3266,"corporation":false,"usgs":true,"family":"Tinsley","given":"John C.","suffix":"III","email":"jtinsley@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":281865,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Warrick, Jonathan A. jwarrick@usgs.gov","contributorId":1904,"corporation":false,"usgs":true,"family":"Warrick","given":"Jonathan A.","email":"jwarrick@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":281864,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Meyer, Robert W.","contributorId":69601,"corporation":false,"usgs":true,"family":"Meyer","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":281868,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70101,"text":"ofr20051067 - 2005 - Landslide hazards at La Conchita, California","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"ofr20051067","displayToPublicDate":"2005-02-22T00:00:00","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":"2005-1067","title":"Landslide hazards at La Conchita, California","language":"ENGLISH","doi":"10.3133/ofr20051067","usgsCitation":"Jibson, R.W., 2005, Landslide hazards at La Conchita, California (Version 1.0, Online only): U.S. Geological Survey Open-File Report 2005-1067, 1 p. online; 12 p. report, https://doi.org/10.3133/ofr20051067.","productDescription":"1 p. online; 12 p. report","onlineOnly":"Y","costCenters":[],"links":[{"id":193277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6789,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1067/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","edition":"Version 1.0, Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab57a","contributors":{"authors":[{"text":"Jibson, Randall W. 0000-0003-3399-0875 jibson@usgs.gov","orcid":"https://orcid.org/0000-0003-3399-0875","contributorId":2985,"corporation":false,"usgs":true,"family":"Jibson","given":"Randall","email":"jibson@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":281859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70106,"text":"ofr20041430 - 2005 - Geologic map compilation of the Upper Seco Creek Area, Medina and Uvalde Counties, south-central Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"ofr20041430","displayToPublicDate":"2005-02-22T00:00:00","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":"2004-1430","title":"Geologic map compilation of the Upper Seco Creek Area, Medina and Uvalde Counties, south-central Texas","language":"ENGLISH","doi":"10.3133/ofr20041430","usgsCitation":"Blome, C.D., Faith, J.R., Collins, E.W., Pedraza, D.E., and Murray, K., 2005, Geologic map compilation of the Upper Seco Creek Area, Medina and Uvalde Counties, south-central Texas: U.S. Geological Survey Open-File Report 2004-1430, 21 p.; 1 map, https://doi.org/10.3133/ofr20041430.","productDescription":"21 p.; 1 map","costCenters":[],"links":[{"id":110553,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70604.htm","linkFileType":{"id":5,"text":"html"},"description":"70604"},{"id":193059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6792,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1430/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3440","contributors":{"authors":[{"text":"Blome, Charles D. 0000-0002-3449-9378 cblome@usgs.gov","orcid":"https://orcid.org/0000-0002-3449-9378","contributorId":1246,"corporation":false,"usgs":true,"family":"Blome","given":"Charles","email":"cblome@usgs.gov","middleInitial":"D.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":281869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faith, Jason R.","contributorId":92758,"corporation":false,"usgs":true,"family":"Faith","given":"Jason","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":281873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collins, Edward W.","contributorId":27749,"corporation":false,"usgs":true,"family":"Collins","given":"Edward","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":281871,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pedraza, Diana E. 0000-0003-4483-8094 dpedraza@usgs.gov","orcid":"https://orcid.org/0000-0003-4483-8094","contributorId":1281,"corporation":false,"usgs":false,"family":"Pedraza","given":"Diana","email":"dpedraza@usgs.gov","middleInitial":"E.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281870,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murray, Kyle E.","contributorId":31825,"corporation":false,"usgs":true,"family":"Murray","given":"Kyle E.","affiliations":[],"preferred":false,"id":281872,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70094,"text":"sir20045282 - 2005 - Geology and preliminary hydrogeologic characterization of the cell-house site, Berlin, New Hampshire, 2003-04","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"sir20045282","displayToPublicDate":"2005-02-17T00:00:00","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":"2004-5282","title":"Geology and preliminary hydrogeologic characterization of the cell-house site, Berlin, New Hampshire, 2003-04","docAbstract":"At the cell-house site, thin, generally less than 20-foot thick overburden, consisting of till and demolition materials, overlies fractured crystalline bedrock. Bedrock at the site consists of gneiss with thin discontinuous lenses of chlorite schist and discontinuous tabular pegmatite. Two distinct fracture domains, with principal trends to the west and northwest, and to the north, overlap near the site. The cell-house site shows principal trends common to both domains. \r\n\r\nGneiss is the most abundant rock at the site. Steeply dipping fractures within the gneiss terminate on subhorizontal contacts with pegmatite and on moderately dipping contacts with chlorite schist. Steeply northwest-dipping en Echelon fracture zones, parallel joint zones, and silicified brittle faults show consistent strikes to the northeast. Gently east-dipping to subhorizontal fractures, sub-parallel to gneissosity, strike northeast. \r\n\r\nThe impermeable cap, barrier wall, and bedrock surface topography affect ground-water flow in the overburden. There is relatively little ground-water flow in the overburden in the capped area and a poor hydraulic connection between the overburden and the underlying bedrock over most of the site. The overburden beneath the cap may receive inflow through or beneath the barrier wall, or by flow through vertical fractures in the underlying bedrock beneath the barrier wall. \r\n\r\nThe bedrock aquifer near the river is well connected to the river and head difference in the bedrock across the site are large (greater than 13 ft). Horizontal hydraulic conductivities of 0.2 to 20 ft/d were estimated for the bedrock. Individual fractures or fracture zones likely have hydraulic conductivities greater than the bulk rock. Subhorizontal fractures occur at pegmatite contacts or along chlorite schist lenses and may serve as ground-water conduits to the steeply dipping fractures in gneiss. The effective hydraulic conductivity across the site is likely to be in the low range of the estimated values (0.2 ft/d). Ground water discharges to the river from the bedrock aquifer and is greatest during periods of large river stage fluctuations.","language":"ENGLISH","doi":"10.3133/sir20045282","usgsCitation":"Degnan, J.R., Clark, S.F., Harte, P.T., and Mack, T.J., 2005, Geology and preliminary hydrogeologic characterization of the cell-house site, Berlin, New Hampshire, 2003-04 (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5282, 65 p., https://doi.org/10.3133/sir20045282.","productDescription":"65 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":193223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6788,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5282/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea1a","contributors":{"authors":[{"text":"Degnan, James R. 0000-0002-5665-9010 jrdegnan@usgs.gov","orcid":"https://orcid.org/0000-0002-5665-9010","contributorId":498,"corporation":false,"usgs":true,"family":"Degnan","given":"James","email":"jrdegnan@usgs.gov","middleInitial":"R.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281855,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, Stewart F. 0000-0001-8841-2728 sclark@usgs.gov","orcid":"https://orcid.org/0000-0001-8841-2728","contributorId":3658,"corporation":false,"usgs":true,"family":"Clark","given":"Stewart","email":"sclark@usgs.gov","middleInitial":"F.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harte, Philip T. 0000-0002-7718-1204 ptharte@usgs.gov","orcid":"https://orcid.org/0000-0002-7718-1204","contributorId":1008,"corporation":false,"usgs":true,"family":"Harte","given":"Philip","email":"ptharte@usgs.gov","middleInitial":"T.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281856,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mack, Thomas J. 0000-0002-0496-3918 tjmack@usgs.gov","orcid":"https://orcid.org/0000-0002-0496-3918","contributorId":1677,"corporation":false,"usgs":true,"family":"Mack","given":"Thomas","email":"tjmack@usgs.gov","middleInitial":"J.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281857,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70085,"text":"wdrVA042 - 2005 - Water resources data, Virginia, water year 2004 volume 2.  Ground-water-level and ground-water-quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"wdrVA042","displayToPublicDate":"2005-02-16T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"VA-04-2","title":"Water resources data, Virginia, water year 2004 volume 2.  Ground-water-level and ground-water-quality records","docAbstract":"Water-resources data for the 2004 water year for Virginia consist of records of water levels and water quality of ground-water wells. This report (Volume 2. Ground-Water-Level and Ground-Water-Quality Records) contains water levels at 346 observation wells and water quality at 40 wells. Locations of these wells are shown on figures 4 through 9. The data in this report represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Virginia.","language":"ENGLISH","doi":"10.3133/wdrVA042","usgsCitation":"White, R.K., Powell, E.D., Guyer, J.R., and Owens, J.A., 2005, Water resources data, Virginia, water year 2004 volume 2.  Ground-water-level and ground-water-quality records (Online only): U.S. Geological Survey Water Data Report VA-04-2, 418 p., https://doi.org/10.3133/wdrVA042.","productDescription":"418 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":193182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6784,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2004/WDR-VA-04-2/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688d15","contributors":{"authors":[{"text":"White, Roger K.","contributorId":19624,"corporation":false,"usgs":true,"family":"White","given":"Roger","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":281828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, Eugene D.","contributorId":80309,"corporation":false,"usgs":true,"family":"Powell","given":"Eugene","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":281831,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guyer, Joel R.","contributorId":47446,"corporation":false,"usgs":true,"family":"Guyer","given":"Joel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":281829,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Owens, Joseph A.","contributorId":73690,"corporation":false,"usgs":true,"family":"Owens","given":"Joseph","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":281830,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70083,"text":"wdrIA041 - 2005 - Water resources data, Iowa water year 2004, volume 1: surface water and precipitation","interactions":[],"lastModifiedDate":"2016-02-01T10:23:13","indexId":"wdrIA041","displayToPublicDate":"2005-02-15T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IA-04-1","title":"Water resources data, Iowa water year 2004, volume 1: surface water and precipitation","docAbstract":"<p>This volume of the annual hydrologic data report of Iowa is one of a series of annual reports that document hydrologic data gathered from the U.S. Geological Survey.s surface- and ground-water data-collection networks in each State, Puerto Rico, and the Trust Territories. These records of streamflow, ground-water levels, and quality of water provide the hydrologic information needed by local, State, and Federal agencies, and the private sector for developing and managing our Nation.s land and water resources.</p>\n<p>This report is the culmination of a concerted effort by dedicated personnel of the U.S. Geological Survey who collected, compiled, analyzed, verified, and organized the data, and who typed, edited, and assembled the report. The authors had primary responsibility for assuring that the information contained herein is accurate, complete, and adheres to Geological Survey policy and established guidelines.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrIA041","collaboration":"Prepared in cooperation with the Iowa Department of Natural Resources-Iowa Geological Survey, Iowa Department of Transportation, and Federal Agencies","usgsCitation":"Nalley, G.M., Gorman, J., Goodrich, R.D., Miller, V.E., and Housel, K.S., 2005, Water resources data, Iowa water year 2004, volume 1: surface water and precipitation: U.S. Geological Survey Water Data Report IA-04-1, xv, 506 p., https://doi.org/10.3133/wdrIA041.","productDescription":"xv, 506 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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 \"}}]}","tableOfContents":"<p>Preface<br />Surface-water stations, in downstream order, for which records&nbsp;are published in this volume<br />Discontinued surface-water discharge or stage-only stations<br />Discontinued surface-water quality stations<br />Introduction<br />Cooperation<br />Summary of hydrologic conditions<br />&nbsp; &nbsp; &nbsp;Precipitation<br />Special networks and programs<br />Explanation of Stage- and Water Discharge Records<br />&nbsp; &nbsp; &nbsp;Discontinued surface-water<br />&nbsp; &nbsp; &nbsp;Data Presentation<br />&nbsp; &nbsp; &nbsp;Identifying Estimated Daily Discharge<br />&nbsp; &nbsp; &nbsp;Accuracy of Field Data and Computed Results<br />&nbsp; &nbsp; &nbsp;Other Data Records Available<br />Explanation of Precipitation Records<br />&nbsp; &nbsp; &nbsp;Data Collection and Computation<br />&nbsp; &nbsp; &nbsp;Data Presentation<br />Explanation of Water-Quality Records<br />&nbsp; &nbsp; &nbsp;Collection and Examination of Data<br />&nbsp; &nbsp; &nbsp;Water Analysis<br />Surface-Water-Quality Records<br />&nbsp; &nbsp; &nbsp;Classification of Records<br />&nbsp; &nbsp; &nbsp;Accuracy of the Records<br />&nbsp; &nbsp; &nbsp;Arrangement of Records<br />&nbsp; &nbsp; &nbsp;On-Site Measurements and Sample Collection<br />&nbsp; &nbsp; &nbsp;Water Temperature<br />&nbsp; &nbsp; &nbsp;Sediment<br />&nbsp; &nbsp; &nbsp;Laboratory Measurements<br />&nbsp; &nbsp; &nbsp;Data Presentation<br />&nbsp; &nbsp; &nbsp;Remark Codes<br />&nbsp; &nbsp; &nbsp;Water-Quality Control Data<br />&nbsp; &nbsp; &nbsp;Blank Samples<br />&nbsp; &nbsp; &nbsp;Reference Samples<br />&nbsp; &nbsp; &nbsp;Replicate Samples<br />&nbsp; &nbsp; &nbsp;Spike Samples<br />Access to USGS Water Data<br />Definition of Terms<br />Techniques of Water-Resources Investigations of the U.S. Geological Survey.<br />Surface water records<br />Crest-stage partial-record stations<br />Index</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ee125","contributors":{"authors":[{"text":"Nalley, Greg M. 0000-0002-0151-0219","orcid":"https://orcid.org/0000-0002-0151-0219","contributorId":69650,"corporation":false,"usgs":true,"family":"Nalley","given":"Greg","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gorman, Joseph G.","contributorId":52665,"corporation":false,"usgs":true,"family":"Gorman","given":"Joseph G.","affiliations":[],"preferred":false,"id":281823,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goodrich, Robert D.","contributorId":54293,"corporation":false,"usgs":true,"family":"Goodrich","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":281824,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, Von E.","contributorId":102551,"corporation":false,"usgs":true,"family":"Miller","given":"Von","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":281827,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Housel, Kevin S.","contributorId":80754,"corporation":false,"usgs":true,"family":"Housel","given":"Kevin","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":281826,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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,{"id":70080,"text":"sir20055017 - 2005 - Evaluation of drainage-area ratio method used to estimate streamflow for the Red River of the North Basin, North Dakota and Minnesota","interactions":[],"lastModifiedDate":"2018-03-07T16:30:27","indexId":"sir20055017","displayToPublicDate":"2005-02-15T00:00:00","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":"2005-5017","title":"Evaluation of drainage-area ratio method used to estimate streamflow for the Red River of the North Basin, North Dakota and Minnesota","docAbstract":"<p>The drainage-area ratio method commonly is used to estimate streamflow for sites where no streamflow data were collected. To evaluate the validity of the drainage-area ratio method and to determine if an improved method could be developed to estimate streamflow, a multiple-regression technique was used to determine if drainage area, main channel slope, and precipitation were significant variables for estimating streamflow in the Red River of the North Basin. A separate regression analysis was performed for streamflow for each of three seasons-- winter, spring, and summer. Drainage area and summer precipitation were the most significant variables. However, the regression equations generally overestimated streamflows for North Dakota stations and underestimated streamflows for Minnesota stations. To correct the bias in the residuals for the two groups of stations, indicator variables were included to allow both the intercept and the coefficient for the logarithm of drainage area to depend on the group. Drainage area was the only significant variable in the revised regression equations. The exponents for the drainage-area ratio were 0.85 for the winter season, 0.91 for the spring season, and 1.02 for the summer season.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055017","usgsCitation":"Emerson, D.G., Vecchia, A.V., and Dahl, A.L., 2005, Evaluation of drainage-area ratio method used to estimate streamflow for the Red River of the North Basin, North Dakota and Minnesota (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5017, iv, 13 p., https://doi.org/10.3133/sir20055017.","productDescription":"iv, 13 p.","onlineOnly":"Y","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":185929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6780,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5017/","linkFileType":{"id":5,"text":"html"}},{"id":352316,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5017/pdf/sir20055017.pdf"}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 0.0025,46 ], [ 0.0025,49 ], [ 0.0025,49 ], [ 0.0025,46 ], [ 0.0025,46 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fae36","contributors":{"authors":[{"text":"Emerson, Douglas G.","contributorId":40579,"corporation":false,"usgs":true,"family":"Emerson","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":281819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vecchia, Aldo V. 0000-0002-2661-4401","orcid":"https://orcid.org/0000-0002-2661-4401","contributorId":41810,"corporation":false,"usgs":true,"family":"Vecchia","given":"Aldo","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":281820,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dahl, Ann L.","contributorId":15278,"corporation":false,"usgs":true,"family":"Dahl","given":"Ann","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":281818,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70174923,"text":"70174923 - 2005 - Heat wave brings an unprecedented red tide to San Francisco Bay","interactions":[],"lastModifiedDate":"2016-08-04T10:23:45","indexId":"70174923","displayToPublicDate":"2005-02-15T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3879,"text":"Eos, Earth and Space Science News","active":true,"publicationSubtype":{"id":10}},"title":"Heat wave brings an unprecedented red tide to San Francisco Bay","docAbstract":"<p>An exceptional red tide in San Francisco Bay was observed on 8 September 2004. The red tide had chlorophyll concentrations approaching 200 mg/m<span>3</span>&nbsp;(Figure 1) in red/purple surface streaks containing high abundances of the dinoflagellate&nbsp;<i>Akashiwo sanguinea.</i>&nbsp;Red tides and harmful algal blooms (HABs) are common features of coastal ecosystems, and their growing frequency is a suspected outcome of coastal eutrophication.</p>\n<p>However, the authors have never observed a dinoflagellate bloom of this scale during 28 years of sampling in the nutrient-rich San Francisco Bay. Phytoplankton biomass along this transect is typically &lt;5mg Chla/m<span>3</span>, and has never exceeded 21 mg Chla/m<span>3</span>&nbsp;during summer-autumn.</p>","language":"English","publisher":"AGU publications","doi":"10.1029/2005EO070003","usgsCitation":"Cloern, J.E., Schraga, T.S., and Lopez, C., 2005, Heat wave brings an unprecedented red tide to San Francisco Bay: Eos, Earth and Space Science News, v. 86, no. 7, p. 66-66, https://doi.org/10.1029/2005EO070003.","productDescription":"1 p.","startPage":"66","endPage":"66","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":325526,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": 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,{"id":70081,"text":"ofr20051052 - 2005 - Virginia aeromagnetic and gravity maps and data: A web site for distribution of data","interactions":[],"lastModifiedDate":"2023-04-05T19:47:33.251536","indexId":"ofr20051052","displayToPublicDate":"2005-02-15T00:00:00","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":"2005-1052","title":"Virginia aeromagnetic and gravity maps and data: A web site for distribution of data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051052","usgsCitation":"Snyder, S.L., 2005, Virginia aeromagnetic and gravity maps and data: A web site for distribution of data: U.S. Geological Survey Open-File Report 2005-1052, HTML 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,{"id":70066,"text":"sir20045264 - 2005 - Summary of hydraulic properties of the Floridan Aquifer system in coastal Georgia and adjacent parts of South Carolina and Florida","interactions":[],"lastModifiedDate":"2017-01-17T12:49:26","indexId":"sir20045264","displayToPublicDate":"2005-02-11T00:00:00","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":"2004-5264","title":"Summary of hydraulic properties of the Floridan Aquifer system in coastal Georgia and adjacent parts of South Carolina and Florida","docAbstract":"Hydraulic-property data for the Floridan aquifer system and equivalent clastic sediments in a 67-county area of coastal Georgia and adjacent parts of South Carolina and Florida were evaluated to provide data necessary for development of ground-water flow and solute-transport models. Data include transmissivity at 324 wells, storage coefficient at 115 wells, and vertical hydraulic conductivity of 72 core samples from 27 sites.\r\n\r\nHydraulic properties of the Upper Floridan aquifer vary greatly in the study area due to the heterogeneity (and locally to anisotropy) of the aquifer and to variations in the degree of confinement provided by confining units. Prominent structural features in the area\u0014the Southeast Georgia Embayment, the Beaufort Arch, and the Gulf Trough\u0014influence the thickness and hydraulic properties of the sediments comprising the Floridan aquifer system. Transmissivity of the Upper Floridan aquifer and equivalent updip units was compiled for 239 wells and ranges from 530 feet squared per day (ft2/d) at Beaufort County, South Carolina, to 600,000 ft2/d in Coffee County, Georgia. In carbonate rock settings of the lower Coastal Plain, transmissivity of the Upper Floridan aquifer generally is greater than 20,000 ft2/d, with values exceeding 100,000 ft2/d in the southeastern and southwestern parts of the study area (generally coinciding with the area of greatest aquifer thickness). Transmissivity of the Upper Floridan aquifer generally is less than 10,000 ft2/d in and near the upper Coastal Plain, where the aquifer is thin and consists largely of clastic sediments, and in the vicinity of the Gulf Trough, where the aquifer consists of low permeability rocks and sediments. Large variability in the range of transmissivity in Camden and Glynn Counties, Georgia, and Nassau County, Florida, demonstrates the anisotropic distribution of hydraulic properties that may result from fractures or solution openings in the carbonate rocks. Storage coefficient of the Upper Floridan aquifer was compiled for 106 wells and ranges from about 0.00004 at Beaufort County, South Carolina, to 0.04 in Baker County, Florida. \r\n\r\nTransmissivity of the Lower Floridan aquifer and equivalent updip clastic units was compiled for 53 wells and ranges from about 170 ft2/d in Barnwell County, South Carolina, to about 43,000 ft2/d in Camden County, Georgia. Transmissivity of the Lower Floridan aquifer is greatest where the aquifer is thickest\u0014 in southeastern Georgia and northeastern Florida\u0014where estimates are greater than 10,000 ft2/d; at one well in southeastern Georgia transmissivity was estimated to be as high as 200,000 ft2/d. Storage-coefficient data for the Lower Floridan aquifer are limited to three estimates in Barnwell and Allendale Counties, South Carolina, and to estimates determined from six multi-aquifer tests in Duval County, Florida. In the South Carolina tests, storage coefficient ranges from 0.0003 to 0.0004; this range is indicative of a confined aquifer. The storage coefficient for the combined Upper and Lower Floridan wells in Duval County, Florida, ranges from 0.00002 to 0.02. \r\n\r\nVertical hydraulic conductivity was compiled from core samples collected at 27 sites. For the Upper Floridan confining unit, values from 39 core samples at 17 sites range from 0.0002 to 3 feet per day (ft/d). For the Lower Floridan confining unit, values from 10 core samples at 9 sites range from about 0.000004 to 0.16 ft/d. Vertical hydraulic conductivity of the Upper Floridan aquifer was compiled from 16 core samples at five sites, mostly in the Brunswick, Georgia, area and values range from 0.00134 to 160.4 ft/d. Vertical hydraulic conductivity for the semiconfining unit separating the upper and lower water-bearing zones of the Upper Floridan at Brunswick, Georgia, compiled from 6 core samples at three sites ranges from 0.000008 to 0.000134 ft/d. The vertical hydraulic conductivity of the Lower Floridan aquifer in a core sample from a well at Brunswick, G","language":"ENGLISH","doi":"10.3133/sir20045264","usgsCitation":"Clarke, J.S., Leeth, D.C., Taylor-Harris, D., Painter, J.A., and Labowski, J.L., 2005, Summary of hydraulic properties of the Floridan Aquifer system in coastal Georgia and adjacent parts of South Carolina and Florida (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5264, 54 p., https://doi.org/10.3133/sir20045264.","productDescription":"54 p.","onlineOnly":"Y","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":186486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6739,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5264/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","country":"United States","state":"Florida, Georgia, South Carolina","otherGeospatial":"Floridan aquifer system","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {\n        \"stroke\": \"#555555\",\n        \"stroke-width\": 2,\n        \"stroke-opacity\": 1,\n        \"fill\": \"#555555\",\n        \"fill-opacity\": 0.5\n      },\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.507568359375,\n              30.670990790779168\n            ],\n            [\n              -81.595458984375,\n              30.70878122625409\n            ],\n            [\n              -81.8701171875,\n              30.784317689718897\n            ],\n            [\n              -82.034912109375,\n              30.70878122625409\n            ],\n            [\n              -81.97998046875,\n              30.642638258763263\n            ],\n            [\n              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cleeth@usgs.gov","contributorId":1403,"corporation":false,"usgs":true,"family":"Leeth","given":"David","email":"cleeth@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":281799,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor-Harris, DaVette","contributorId":67977,"corporation":false,"usgs":true,"family":"Taylor-Harris","given":"DaVette","email":"","affiliations":[],"preferred":false,"id":281801,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Painter, Jaime A. 0000-0001-8883-9158 jpainter@usgs.gov","orcid":"https://orcid.org/0000-0001-8883-9158","contributorId":1466,"corporation":false,"usgs":true,"family":"Painter","given":"Jaime","email":"jpainter@usgs.gov","middleInitial":"A.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":316,"text":"Georgia Water Science 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,{"id":70073,"text":"wdrIA042 - 2005 - Water resources data, Iowa, water year 2004, volume 2: ground water and quality of precipitation","interactions":[],"lastModifiedDate":"2016-02-01T10:29:18","indexId":"wdrIA042","displayToPublicDate":"2005-02-11T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IA-04-2","title":"Water resources data, Iowa, water year 2004, volume 2: ground water and quality of precipitation","docAbstract":"<p>Water resources data for Iowa for the 2004 water year consists of records of ground water levels and water quality of ground-water wells. This report volume contains water-level records for 163 ground-water observation wells; water-quality data for 147 municipal wells; and precipitation-quality data for 2 precipitation sites.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrIA042","collaboration":"Prepared in cooperation with the Iowa Department of Natural Resources-Iowa Geological Survey, Iowa Department of Transportation, and Federal agencies","usgsCitation":"Nalley, G., Linhart, S.M., Littin, G.R., Miller, V., and Housel, K., 2005, Water resources data, Iowa, water year 2004, volume 2: ground water and quality of precipitation: U.S. Geological Survey Water Data Report IA-04-2, xii, 132 p., https://doi.org/10.3133/wdrIA042.","productDescription":"xii, 132 p.","onlineOnly":"Y","additionalOnlineFiles":"N","temporalStart":"2003-10-01","costCenters":[{"id":351,"text":"Iowa Water Science 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 \"}}]}","tableOfContents":"<p>Preface<br />&nbsp; &nbsp; &nbsp;Figures<br />&nbsp; &nbsp; &nbsp;Ground-Water Wells, by County, for which Records are Published in this Volume<br />Introduction<br />Cooperation<br />Summary of Hydrologic Conditions<br />&nbsp; &nbsp; &nbsp;Precipitation<br />&nbsp; &nbsp; &nbsp;Ground-Water-Level Observation Network<br />&nbsp; &nbsp; &nbsp;Ground-Water Quality<br />&nbsp; &nbsp; &nbsp;Ground-Water Monitoring Network<br />Numbering system for wells and miscellaneous sites<br />Special Networks and Programs<br />Explanation of Ground-Water-Level Records<br />&nbsp; &nbsp; &nbsp;Data Collection and Computation<br />&nbsp; &nbsp; &nbsp;Data Presentation<br />Explanation of precipitation records<br />&nbsp; &nbsp; &nbsp;Data Collection and Computation<br />&nbsp; &nbsp; &nbsp;Data Presentation<br />Explanation of Water-Quality Records<br />&nbsp; &nbsp; &nbsp;Collection and Examination of Data<br />&nbsp; &nbsp; &nbsp;Water Analysis<br />Ground-Water-Quality Data<br />&nbsp; &nbsp; &nbsp;Data Collection and Computation<br />&nbsp; &nbsp; &nbsp;Laboratory Measurements<br />&nbsp; &nbsp; &nbsp;Blank Samples<br />&nbsp; &nbsp; &nbsp;Reference Samples<br />&nbsp; &nbsp; &nbsp;Replicate Samples<br />&nbsp; &nbsp; &nbsp;Spike Samples<br />Access to USGS Water Data<br />Definition of Terms<br />Techniques of Water-Resources Investigations of the U.S. Geological Survey<br />Ground-Water Levels<br />Ground-Water-Quality Monitoring Program.<br />Quality of Precipitation<br />Index</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1424","contributors":{"authors":[{"text":"Nalley, G.M.","contributorId":23535,"corporation":false,"usgs":true,"family":"Nalley","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":281813,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linhart, S. Michael","contributorId":67932,"corporation":false,"usgs":true,"family":"Linhart","given":"S.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":281815,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Littin, G. R.","contributorId":95924,"corporation":false,"usgs":true,"family":"Littin","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":281816,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, V.E.","contributorId":43423,"corporation":false,"usgs":true,"family":"Miller","given":"V.E.","email":"","affiliations":[],"preferred":false,"id":281814,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Housel, K.S.","contributorId":22625,"corporation":false,"usgs":true,"family":"Housel","given":"K.S.","email":"","affiliations":[],"preferred":false,"id":281812,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70074,"text":"sir20055022 - 2005 - Initial-phase investigation of multi-dimensional streamflow simulations in the Colorado River, Moab Valley, Grand County, Utah, 2004","interactions":[],"lastModifiedDate":"2017-01-27T15:41:03","indexId":"sir20055022","displayToPublicDate":"2005-02-11T00:00:00","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":"2005-5022","title":"Initial-phase investigation of multi-dimensional streamflow simulations in the Colorado River, Moab Valley, Grand County, Utah, 2004","docAbstract":"<p><span>A multi-dimensional hydrodynamic model was applied to aid in the assessment of the potential hazard posed to the uranium mill tailings near Moab, Utah, by flooding in the Colorado River as it flows through Moab Valley. Discharge estimates for the 100- and 500-year recurrence interval and for the Probable Maximum Flood (PMF) were evaluated with the model for the existing channel geometry. These discharges also were modeled for three other channel-deepening configurations representing hypothetical scour of the channel at the downstream portal of Moab Valley. Water-surface elevation, velocity distribution, and shear-stress distribution were predicted for each simulation.</span><br><br><span>The hydrodynamic model was developed from measured channel topography and over-bank topographic data acquired from several sources. A limited calibration of the hydrodynamic model was conducted. The extensive presence of tamarisk or salt cedar in the over-bank regions of the study reach presented challenges for determining roughness coefficients.</span><br><br><span>Predicted water-surface elevations for the current channel geometry indicated that the toe of the tailings pile would be inundated by about 4 feet by the 100-year discharge and 25 feet by the PMF discharge. A small area at the toe of the tailings pile was characterized by velocities of about 1 to 2 feet per second for the 100-year discharge. Predicted velocities near the toe for the PMF discharge increased to between 2 and 4 feet per second over a somewhat larger area. The manner to which velocities progress from the 100-year discharge to the PMF discharge in the area of the tailings pile indicates that the tailings pile obstructs the over-bank flow of flood discharges. The predicted path of flow for all simulations along the existing Colorado River channel indicates that the current distribution of tamarisk in the over-bank region affects how flood-flow velocities are spatially distributed. Shear-stress distributions were predicted throughout the study reach for each discharge and channel geometry examined. Material transport was evaluated by applying these shear-stress values to empirically determined critical shear-stress values for grain sizes ranging from very fine sands to very coarse gravels.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055022","collaboration":"Prepared in cooperation with the Utah Department of Environmmental Quality, Division of Radiation Control; and the U.S. Environmental Protection Agency","usgsCitation":"Kenney, T.A., 2005, Initial-phase investigation of multi-dimensional streamflow simulations in the Colorado River, Moab Valley, Grand County, Utah, 2004: U.S. Geological Survey Scientific Investigations Report 2005-5022, viii, 69 p., https://doi.org/10.3133/sir20055022.","productDescription":"viii, 69 p.","numberOfPages":"80","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":6778,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055022/","linkFileType":{"id":5,"text":"html"}},{"id":185843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334238,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5022/pdf/SIR2005_5022.pdf"}],"scale":"5000000","country":"United States","state":"Utah","county":"Grand County","otherGeospatial":"Colorado River, Moab Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66da0a","contributors":{"authors":[{"text":"Kenney, Terry A. 0000-0003-4477-7295 tkenney@usgs.gov","orcid":"https://orcid.org/0000-0003-4477-7295","contributorId":447,"corporation":false,"usgs":true,"family":"Kenney","given":"Terry","email":"tkenney@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":281817,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70070,"text":"sir20045260 - 2005 - Pond-aquifer flow and water availability in the vicinity of two coastal area seepage ponds, Glynn and Bulloch Counties, Georgia","interactions":[],"lastModifiedDate":"2017-01-17T12:36:06","indexId":"sir20045260","displayToPublicDate":"2005-02-11T00:00:00","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":"2004-5260","title":"Pond-aquifer flow and water availability in the vicinity of two coastal area seepage ponds, Glynn and Bulloch Counties, Georgia","docAbstract":"Pond-aquifer flow and water availability at excavated seepage pond sites in Glynn County and in southern Bulloch County, Georgia, were evaluated to determine their potential as sources of water supply for irrigation. Excavated seepage ponds derive water primarily from ground water seeping into the pond, in a manner similar to a dug well completed in a surficial aquifer. The availability of water from seepage ponds is controlled by the permeability of surficial deposits, the amount of precipitation recharging the ground-water system, and the volume of water stored in the pond. The viability of seepage ponds as supplies for irrigation is limited by low seepage rates and high dependence on climatic conditions. Ponds will not refill unless there is adequate precipitation to recharge the surficial aquifer, which subsequently drains (seeps) into the pond. \r\n\r\nGround-water seepage was estimated using a water-budget approach that utilized on-site climatic and hydrologic measurements, computing pond-volume changes during pond pumping tests, and by digital simulation using steady-state and transient ground-water flow models. From August 1999 to May 2000, the Glynn County pond was mostly losing water (as indicated by negative net seepage); whereas from October 2000 to June 2001, the Bulloch County pond was mostly gaining water. At both sites, most ground-water seepage entered the pond following major rainfall events that provided recharge to the surficial aquifer. Net ground-water seepage, estimated using water-budget analysis and simulation, ranged from -11.5 to 15 gallons per minute (gal/min) at the Glynn County pond site and from -55 to 31 gal/min at the Bulloch County pond site. \r\n\r\nSimulated values during pumping tests indicate that groundwater seepage to both ponds increases with decreased pond stage. At the Glynn County pond, simulated net ground-water seepage varied between 7.8 gal/min at the beginning of the test (high pond stage and low hydraulic gradient) and 103 gal/min at the end of the test (low pond stage and high hydraulic gradient). At the Bulloch County pond site, values ranged from -17.7 gal/min at the beginning of the test to 15 gal/min at the end of the test. \r\n\r\nResults at the two pond sites indicate that the use of excavated seepage ponds as sources for irrigation supply is limited by pond-storage volume and low net ground-water seepage rates during periods of low precipitation. Pumps withdrawing 1,000 gal/min for 10 hours per day\u0014under climatic and hydrologic conditions similar to those observed during pond pumping tests at each site\u0014would drain the Glynn County pond within 30 days and the Bulloch County pond within 3.5 days. Because the two pond sites are considered to represent the extremes of likely conditions to be encountered in the coastal Georgia area, it is likely that other seepage ponds would have similar storage-depletion rates.","language":"ENGLISH","doi":"10.3133/sir20045260","usgsCitation":"Clarke, J.S., and Rumman, M.A., 2005, Pond-aquifer flow and water availability in the vicinity of two coastal area seepage ponds, Glynn and Bulloch Counties, Georgia (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5260, vi, 31 p., https://doi.org/10.3133/sir20045260.","productDescription":"vi, 31 p.","onlineOnly":"Y","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":186488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6741,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5260/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","country":"United States","state":"Georgia","county":"Bulloch County, Glynn County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.122314453125,\n              30.07860131571654\n            ],\n            [\n              -84.122314453125,\n              33.770015152780125\n            ],\n            [\n              -80.277099609375,\n              33.770015152780125\n            ],\n            [\n              -80.277099609375,\n              30.07860131571654\n            ],\n            [\n              -84.122314453125,\n              30.07860131571654\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e861","contributors":{"authors":[{"text":"Clarke, John S. jsclarke@usgs.gov","contributorId":400,"corporation":false,"usgs":true,"family":"Clarke","given":"John","email":"jsclarke@usgs.gov","middleInitial":"S.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rumman, Malek Abu","contributorId":82399,"corporation":false,"usgs":true,"family":"Rumman","given":"Malek","email":"","middleInitial":"Abu","affiliations":[],"preferred":false,"id":281807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70069,"text":"sir20045295 - 2005 - Effects of decreased ground-water withdrawal on ground-water levels and chloride concentrations in Camden County, Georgia, and ground-water levels in Nassau County, Florida, from September 2001 to May 2003","interactions":[],"lastModifiedDate":"2017-01-17T17:13:30","indexId":"sir20045295","displayToPublicDate":"2005-02-11T00:00:00","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":"2004-5295","title":"Effects of decreased ground-water withdrawal on ground-water levels and chloride concentrations in Camden County, Georgia, and ground-water levels in Nassau County, Florida, from September 2001 to May 2003","docAbstract":"During October 2002, the Durango Paper Company formerly Gillman Paper Company) in St. Marys, Georgia, shut down paper-mill operations; the shutdown resulted in decreased ground-water withdrawal in Camden County by 35.6 million gallons per day. The decrease in withdrawal resulted in water-level rise in wells completed in the Floridan aquifer system and the overlying surficial and Brunswick aquifer systems; many wells in the St. Marys area flowed for the first time since the mill began operations during 1941. \r\n\r\nPumping at the mill resulted in the development of a cone of depression that coalesced with a larger adjacent cone of depression at Fernandina Beach, Florida. Since closure of the mill, the cone at St. Marys is no longer present, although the cone still exists at Fernandina Beach, Florida. Historical water-level data from the production wells at the mill indicate that the pumping water level ranged from 68 to 235 feet (ft) below North American Vertical Datum of 1988 (NAVD 88) and averaged about 114 ft when the mill was operating. Since the shutdown, it is estimated that water levels at the mill have risen about 140 ft and are now at about 30 ft above NAVD 88. The water-level rise in wells in outlying areas in Camden County was less pronounced and ranged from about 5 to 10 ft above NAVD 88. Because of the regional upward water-level trend in the Upper Floridan aquifer that started during 1999\u00132000 in most of the coastal area, combined with a steeper upward trend beginning during October 2002, it was not possible to determine if the 5\u001310 ft rise in water levels in wells away from St. Marys was due to the mill closure. In addition to water-level rise of 22\u001326 ft in the Floridan aquifer system, water-level rises in the overlying surficial and Brunswick aquifer systems at St. Marys after the shutdown indicate upward leakage of water. Water levels had stabilized in the confined surficial and Upper and Lower Floridan aquifers by April\u0013May 2003; however, the water level in the upper Brunswick aquifer was still rising as of May 2003.\r\n\r\nChloride concentrations in the Upper Floridan aquifer in Camden County do not exceed the State and Federal drinking-water standard of 250 milligrams per liter (mg/L). With the exception of three wells located at St. Marys, all of the wells sampled during this study (from September 2002 to May 2003) had chloride concentrations ranging from 30 to 50 mg/L, which are considered within background levels for the Upper Floridan aquifer in this area. The three wells\u0014two at the Durango Paper Company and the other an old unused City of St. Marys well\u0014had chloride concentrations that ranged from 74 to 175 mg/L, which are above the background level, but were still below the 250-mg/L drinking-water standard. The source has not been determined for the elevated chloride concentration in these wells; the chloride concentration in one of the wells has decreased slightly since the paper-mill shutdown. Chloride concentrations throughout Camden County showed little change after the paper-mill shutdown.","language":"ENGLISH","doi":"10.3133/sir20045295","usgsCitation":"Peck, M., McFadden, K.W., and Leeth, D.C., 2005, Effects of decreased ground-water withdrawal on ground-water levels and chloride concentrations in Camden County, Georgia, and ground-water levels in Nassau County, Florida, from September 2001 to May 2003 (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5295, vi, 31 p., https://doi.org/10.3133/sir20045295.","productDescription":"vi, 31 p.","onlineOnly":"Y","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":186487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6740,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5295/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","country":"United States","state":"Florida, Georgia","county":"Camden County, Nassau County","otherGeospatial":"Brunswick aquifer system, Floridan aquifer system","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.15576171875,\n              30.56226095049944\n            ],\n            [\n              -82.15576171875,\n              31.12819929911196\n            ],\n            [\n              -81.36474609375,\n              31.12819929911196\n            ],\n            [\n              -81.36474609375,\n              30.56226095049944\n            ],\n            [\n              -82.15576171875,\n              30.56226095049944\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af2e4b07f02db6918fd","contributors":{"authors":[{"text":"Peck, Michael F. mfpeck@usgs.gov","contributorId":1467,"corporation":false,"usgs":true,"family":"Peck","given":"Michael F.","email":"mfpeck@usgs.gov","affiliations":[],"preferred":false,"id":281805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McFadden, Keith W. keithmc@usgs.gov","contributorId":1446,"corporation":false,"usgs":true,"family":"McFadden","given":"Keith","email":"keithmc@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":281804,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leeth, David C. cleeth@usgs.gov","contributorId":1403,"corporation":false,"usgs":true,"family":"Leeth","given":"David","email":"cleeth@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":281803,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70009,"text":"ofr20051038 - 2005 - Geologic shaded relief map of Venezuela","interactions":[],"lastModifiedDate":"2018-07-31T11:26:57","indexId":"ofr20051038","displayToPublicDate":"2005-02-10T00:00:00","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":"2005-1038","title":"Geologic shaded relief map of Venezuela","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051038","collaboration":"Spanish version available as OFR 2006-1109","usgsCitation":"Hackley, P.C., Urbani, F., Karlsen, A., and Garrity, C.P., 2005, Geologic shaded relief map of Venezuela (Version 1.0): U.S. Geological Survey Open-File Report 2005-1038, 2 sheets, https://doi.org/10.3133/ofr20051038.","productDescription":"2 sheets","onlineOnly":"Y","costCenters":[],"links":[{"id":188175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6242,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1038/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688258","contributors":{"authors":[{"text":"Hackley, Paul C. 0000-0002-5957-2551 phackley@usgs.gov","orcid":"https://orcid.org/0000-0002-5957-2551","contributorId":592,"corporation":false,"usgs":true,"family":"Hackley","given":"Paul","email":"phackley@usgs.gov","middleInitial":"C.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":281658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Urbani, Franco","contributorId":67163,"corporation":false,"usgs":true,"family":"Urbani","given":"Franco","email":"","affiliations":[],"preferred":false,"id":281660,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Karlsen, Alex W.","contributorId":78789,"corporation":false,"usgs":true,"family":"Karlsen","given":"Alex W.","affiliations":[],"preferred":false,"id":281661,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"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":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true}],"preferred":true,"id":281659,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":69994,"text":"ofr20051040 - 2005 - Fracture trace map and single-well aquifer test results in a carbonate aquifer in Berkeley County, West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"ofr20051040","displayToPublicDate":"2005-02-10T00:00:00","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":"2005-1040","title":"Fracture trace map and single-well aquifer test results in a carbonate aquifer in Berkeley County, West Virginia","docAbstract":"These data contain information on the results of single-well aquifer tests, lineament analysis, and a bedrock geologic map compilation for the low-lying carbonate and shale areas of eastern Berkeley County, West Virginia. Efforts have been initiated by management agencies of Berkeley County in cooperation with the U.S. Geological Survey to further the understanding of the spatial distribution of fractures in the carbonate regions and their correlation with aquifer properties. This report presents transmissivity values from about 200 single-well aquifer tests and a map of fracture-traces determined from aerial photos and field investigations.  Transmissivity values were compared to geologic factors possibly affecting its magnitude.","language":"ENGLISH","doi":"10.3133/ofr20051040","usgsCitation":"McCoy, K.J., Podwysocki, M.H., Crider, E.A., and Weary, D.J., 2005, Fracture trace map and single-well aquifer test results in a carbonate aquifer in Berkeley County, West Virginia (Online Version 1.0): U.S. Geological Survey Open-File Report 2005-1040, 1 plate, TIF and PDF map with metadata, https://doi.org/10.3133/ofr20051040.","productDescription":"1 plate, TIF and PDF map with metadata","costCenters":[],"links":[{"id":193061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6794,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1040/","linkFileType":{"id":5,"text":"html"}}],"scale":"1","edition":"Online Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a882b","contributors":{"authors":[{"text":"McCoy, Kurt J. 0000-0002-9756-8238 kjmccoy@usgs.gov","orcid":"https://orcid.org/0000-0002-9756-8238","contributorId":1391,"corporation":false,"usgs":true,"family":"McCoy","given":"Kurt","email":"kjmccoy@usgs.gov","middleInitial":"J.","affiliations":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"preferred":true,"id":281651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Podwysocki, Melvin H.","contributorId":60220,"corporation":false,"usgs":true,"family":"Podwysocki","given":"Melvin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":281652,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crider, E. Allen","contributorId":93992,"corporation":false,"usgs":true,"family":"Crider","given":"E.","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":281653,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weary, David J. 0000-0002-6115-6397 dweary@usgs.gov","orcid":"https://orcid.org/0000-0002-6115-6397","contributorId":545,"corporation":false,"usgs":true,"family":"Weary","given":"David","email":"dweary@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":281650,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006,"text":"ds110 - 2005 - Flow velocity, water temperature, and conductivity at selected locations in Shark River Slough, Everglades National Park, Florida; July 1999 - July 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:35","indexId":"ds110","displayToPublicDate":"2005-02-10T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"110","title":"Flow velocity, water temperature, and conductivity at selected locations in Shark River Slough, Everglades National Park, Florida; July 1999 - July 2003","docAbstract":"Flow-velocity, water-temperature, and conductivity data were collected at five locations in Shark River Slough, Everglades National Park (ENP), Florida, from 1999 to 2003. The data were collected as part of the U.S. Geological Survey Priority Ecosystems Science Initiative in support of the Comprehensive Everglades Restoration Plan. This report contains digital files and graphical plots of the processed, quality-checked, and edited data. Information pertinent to the locations and monitoring strategy also is presented.","language":"ENGLISH","doi":"10.3133/ds110","usgsCitation":"Schaffranek, R.W., and Riscassi, A.L., 2005, Flow velocity, water temperature, and conductivity at selected locations in Shark River Slough, Everglades National Park, Florida; July 1999 - July 2003: U.S. Geological Survey Data Series 110, data files and text, https://doi.org/10.3133/ds110.","productDescription":"data files and text","costCenters":[],"links":[{"id":6241,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ds110/","linkFileType":{"id":5,"text":"html"}},{"id":188091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de819","contributors":{"authors":[{"text":"Schaffranek, Raymond W.","contributorId":86314,"corporation":false,"usgs":true,"family":"Schaffranek","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":281657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riscassi, Ami L.","contributorId":24399,"corporation":false,"usgs":true,"family":"Riscassi","given":"Ami","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":281656,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70016,"text":"ofr20051013 - 2005 - Excavation logs of two trenches across a strand of the southern Whidbey Island fault zone near Grace, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:13:36","indexId":"ofr20051013","displayToPublicDate":"2005-02-10T00:00:00","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":"2005-1013","title":"Excavation logs of two trenches across a strand of the southern Whidbey Island fault zone near Grace, Washington","language":"ENGLISH","doi":"10.3133/ofr20051013","usgsCitation":"Sherrod, B.L., Barnett, E., and Kelsey, H.M., 2005, Excavation logs of two trenches across a strand of the southern Whidbey Island fault zone near Grace, Washington (Version 1.0): U.S. Geological Survey Open-File Report 2005-1013, 1 large sheet (36 in. by 48 in.), https://doi.org/10.3133/ofr20051013.","productDescription":"1 large sheet (36 in. by 48 in.)","costCenters":[],"links":[{"id":188788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6247,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1013/","linkFileType":{"id":5,"text":"html"}}],"scale":"1","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f944e","contributors":{"authors":[{"text":"Sherrod, Brian Louis","contributorId":33400,"corporation":false,"usgs":true,"family":"Sherrod","given":"Brian","email":"","middleInitial":"Louis","affiliations":[],"preferred":false,"id":281671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnett, Elizabeth eli@usgs.gov","contributorId":2156,"corporation":false,"usgs":true,"family":"Barnett","given":"Elizabeth","email":"eli@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":281670,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kelsey, Harvey M.","contributorId":101713,"corporation":false,"usgs":true,"family":"Kelsey","given":"Harvey","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281672,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70017,"text":"ofr20051012 - 2005 - Simulation of ground-water flow and areas contributing ground water to production wells, Cadillac, Michigan","interactions":[],"lastModifiedDate":"2025-06-05T18:06:11.897936","indexId":"ofr20051012","displayToPublicDate":"2005-02-10T00:00:00","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":"2005-1012","title":"Simulation of ground-water flow and areas contributing ground water to production wells, Cadillac, Michigan","docAbstract":"<p>Ground water is the primary source of water for domestic, municipal, and industrial use within the northwest section of Michigan's Lower Peninsula. Because of the importance of this resource, numerous communities including the city of Cadillac in Wexford County, Michigan, have begun local well-head protection programs. In these programs, communities protect their ground-water resources by identifying the areas that contribute water to production wells, identifying potential sources of contamination, and developing methods to cooperatively manage and minimize threats to the water supply.</p><p>The U.S. Geological Survey, in cooperation with the city of Cadillac, simulated regional ground-water flow and estimated areas contributing recharge and zones of transport to the production well field. Ground-water flow models for the Clam River watershed, in Wexford and Missaukee Counties, were developed using the U.S. Geological Survey modular three-dimensional finite-difference ground-water flow model (MODFLOW 2000). Ground-water flow models were calibrated using the observation, sensitivity, and parameter estimation packages of MODFLOW 2000. Ground-water-head solutions from calibrated flow models were used in conjunction with MODPATH, a particle-tracking program, to simulate regional ground-water flow and estimate areas contributing recharge and zones of transport to the Cadillac production-well field for a 10-year period.</p><p>Model simulations match the conceptual model in that regional ground-water flow in the deep ground-water system is from southeast to northwest across the watershed. Areas contributing water were determined for the optimized parameter set and an alternate parameter set that included increased recharge and hydraulic conductivity values. Although substantially different hydrologic parameters (assumed to represent end-member ranges of realistic hydrologic parameters) were used in alternate numerical simulations, simulation results differ little in predictions of the size of the contributing area to the city well field. However, increasing recharge and hydraulic conductivity values appreciably affected the shape of the contributing area and zone of contribution of reacharge. Simulation results indicate that the region immediately to the south and southeast of the well field is contributing water to the production wells. Detailed aquifer characterization would be needed to describe and simulate</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051012","collaboration":"Prepared in cooperation with the city of Cadillac, Michigan","usgsCitation":"Hoard, C.J., and Westjohn, D., 2005, Simulation of ground-water flow and areas contributing ground water to production wells, Cadillac, Michigan: U.S. Geological Survey Open-File Report 2005-1012, iv, 18 p., https://doi.org/10.3133/ofr20051012.","productDescription":"iv, 18 p.","costCenters":[],"links":[{"id":489704,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1012/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188789,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2005/1012/report-thumb.jpg"}],"country":"United States","state":"Michigan","city":"Cadillac","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -85.53972619961374,\n              44.307248039247895\n            ],\n            [\n              -85.53972619961374,\n              44.18815560084593\n            ],\n            [\n              -85.29494633065546,\n              44.18815560084593\n            ],\n            [\n              -85.29494633065546,\n              44.307248039247895\n            ],\n            [\n              -85.53972619961374,\n              44.307248039247895\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2d28","contributors":{"authors":[{"text":"Hoard, Christopher J. 0000-0003-2337-506X cjhoard@usgs.gov","orcid":"https://orcid.org/0000-0003-2337-506X","contributorId":191767,"corporation":false,"usgs":true,"family":"Hoard","given":"Christopher","email":"cjhoard@usgs.gov","middleInitial":"J.","affiliations":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":false,"id":281674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Westjohn, D.B.","contributorId":68411,"corporation":false,"usgs":true,"family":"Westjohn","given":"D.B.","affiliations":[],"preferred":false,"id":281673,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70015,"text":"ofr20051019 - 2005 - Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California","interactions":[{"subject":{"id":24937,"text":"ofr95800 - 1995 - Preliminary geologic map of the Newhall 7.5' quadrangle, southern California: a digital database","indexId":"ofr95800","publicationYear":"1995","noYear":false,"title":"Preliminary geologic map of the Newhall 7.5' quadrangle, southern California: a digital database"},"predicate":"SUPERSEDED_BY","object":{"id":70015,"text":"ofr20051019 - 2005 - Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California","indexId":"ofr20051019","publicationYear":"2005","noYear":false,"title":"Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California"},"id":1}],"lastModifiedDate":"2019-11-19T06:56:09","indexId":"ofr20051019","displayToPublicDate":"2005-02-10T00:00:00","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":"2005-1019","title":"Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California","docAbstract":"<p>This data set maps and describes the geology of the Los Angeles 30? x 60? quadrangle, southern California. Compilation of the Los Angeles quadrangle is based upon published mapping at scales of 1:12,000 and smaller, unpublished mapping at scales of 1:12,000 and smaller, with reconnaissance mapping by the compilers to resolve some edge-matching problems. The Los Angeles 30' x 60' quadrangle covers approximately 5,000 km2 including some of the most densely populated urban and suburban areas of the southern California megalopolis. It extends about 90 km E-W and about 55 km N-S, from Fillmore and Thousand Oaks in the west to Vincent in the northeast and Montebello in the southeast, and includes urban San Gabriel Valley and San Gabriel Mountain foothill communities from Monrovia to Pasadena, as well as Glendale, downtown Los Angeles, Hollywood, Santa Monica, Malibu, in addition to all the communities in the San Fernando Valley, Simi Valley, and the upper Santa Clara River Valley. From the 2000 Census, the population of these urban and suburban areas totals approximately 5.6 million, and estimates of property value total hundreds of billions of dollars. Residents and transient visitors are subject to potential hazards from earthquakes, debris flows and other landslides, floods, wildfires, subsidence from ground water and petroleum withdrawal, and swelling soils; and coastal areas are exposed to flooding and erosion by storm and tsunami waves. Topographic relief ranges from about one hundred meters sub sea (in Santa Monica Bay) to more than 2,000 meters above sea level at Pacifico Mountain in the high San Gabriel Mountains. In addition to the populated area, the quadrangle includes significant areas of wilderness in the Angeles and Los Padres National Forests, in the Santa Monica Mountains National Recreation Area, and the Sespe Condor Sanctuary. The geologic map illustrates the general distribution of the rocks and surficial deposits in the area and their structural and stratigraphic relations to one another. The principal characteristics of the map units are described and are part of the database. The map provides a regional geologic framework as an aid to better evaluations of the potential for hazard from active earth processes. It synthesizes and combines studies by many earth scientists. Most of the source maps are at more detailed scales than 1:100,000, and we utilized the most detailed source materials available. We have not attempted to resolve all problems of stratigraphic correlation and nomenclature. In most areas we have retained the unit designations of source-map authors, but in some areas, particularly in the igneous-metamorphic complex of the San Gabriel Mountains, some unit designations have been changed. Hopefully, this map will stimulate further work to describe and correlate the many units within the scope of a more coherent, more accurate geologic history.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20051019","usgsCitation":"complied by Yerkes, R.F., Campbell, R., Alvarez, R.M., and Bovard, K.R., 2005, Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California (Version 1.0): U.S. Geological Survey Open-File Report 2005-1019, HTML, https://doi.org/10.3133/ofr20051019.","productDescription":"HTML","costCenters":[],"links":[{"id":188709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6246,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1019/","linkFileType":{"id":5,"text":"html"}},{"id":110546,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70332.htm","linkFileType":{"id":5,"text":"html"},"description":"70332"}],"scale":"1","country":"United States","state":"California","city":"Los Angeles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.00,\n              34.30\n            ],\n            [\n              -118.00,\n              34.30\n            ],\n            [\n              -118.00,\n              34.00\n            ],\n            [\n              -119.00,\n              34.00\n            ],\n            [\n              -119.00,\n              34.30\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b117","contributors":{"authors":[{"text":"complied by Yerkes, Robert F.","contributorId":93136,"corporation":false,"usgs":true,"family":"complied by Yerkes","given":"Robert","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":281669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":281667,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alvarez, Rachel M.","contributorId":66354,"corporation":false,"usgs":true,"family":"Alvarez","given":"Rachel","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281666,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bovard, Kelly R.","contributorId":91577,"corporation":false,"usgs":true,"family":"Bovard","given":"Kelly","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":281668,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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