{"pageNumber":"967","pageRowStart":"24150","pageSize":"25","recordCount":46896,"records":[{"id":70265,"text":"cir1276 - 2005 - Proceedings of the Federal Interagency Sediment Monitoring Instrument and Analysis Research Workshop, September 9-11, 2003, Flagstaff, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"cir1276","displayToPublicDate":"2005-03-21T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1276","title":"Proceedings of the Federal Interagency Sediment Monitoring Instrument and Analysis Research Workshop, September 9-11, 2003, Flagstaff, Arizona","docAbstract":"The Advisory Committee on Water Information's Subcommittee on Sedimentation sponsored the Federal Interagency Sediment Monitoring Instrument and Analysis Research Workshop on September 9-11, 2003, at the U.S. Geological Survey Flagstaff Field Center, Arizona. The workshop brought together a diverse group representing most Federal agencies whose mission includes fluvial-sediment issues; academia; the private sector; and others with interests and expertise in fluvial-sediment monitoring ? suspended sediment, bedload, bed material, and bed topography ? and associated data-analysis techniques. The workshop emphasized technological and theoretical advances related to measurements of suspended sediment, bedload, bed material and bed topography, and data analyses. This workshop followed and expanded upon part of the 2002 Federal Interagency Workshop on Turbidity and Other Sediment Surrogates (http://water.usgs.gov/pubs/circ/2003/circ1250/), which initiated a process to provide national standards for measurement and use of turbidity and other sediment-surrogate data. This report provides a description of the salient attributes of the workshop and related information, major deliberations and findings, and principal recommendations. This information is available for evaluation by the Subcommittee on Sedimentation, which may opt to develop an action plan based on the recommendations that it endorses for consideration by the Advisory Committee on Water Information.","language":"ENGLISH","doi":"10.3133/cir1276","isbn":"0607962321","usgsCitation":"Gray, J.R., 2005, Proceedings of the Federal Interagency Sediment Monitoring Instrument and Analysis Research Workshop, September 9-11, 2003, Flagstaff, Arizona: U.S. Geological Survey Circular 1276, 46 p., https://doi.org/10.3133/cir1276.","productDescription":"46 p.","costCenters":[],"links":[{"id":6958,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/circ1276/ ","linkFileType":{"id":5,"text":"html"}},{"id":191483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66058b","contributors":{"authors":[{"text":"Gray, John R. 0000-0002-8817-3701 jrgray@usgs.gov","orcid":"https://orcid.org/0000-0002-8817-3701","contributorId":1158,"corporation":false,"usgs":true,"family":"Gray","given":"John","email":"jrgray@usgs.gov","middleInitial":"R.","affiliations":[{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true}],"preferred":true,"id":282073,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70253,"text":"sir20045197 - 2005 - Simulation of ground-water flow in the basin-fill aquifer of the Tularosa Basin, south-central New Mexico, predevelopment through 2040","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"sir20045197","displayToPublicDate":"2005-03-20T00:00:00","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":"2004-5197","title":"Simulation of ground-water flow in the basin-fill aquifer of the Tularosa Basin, south-central New Mexico, predevelopment through 2040","docAbstract":"The hydrology of the basin-fill aquifer in the Tularosa Basin was evaluated through construction and calibration of steady-state and transient three-dimensional ground-water-flow simulations. Simulations were made using the U.S. Geological Survey finite-difference modular ground-water-flow computer software MODFLOW-96. The transient simulation covered 1948-2040. Both steady-state and transient simulations were calibrated by matching simulation output to available ground-water-level measurements. The root-mean-square error of the steady-state calibration in the well-calibrated area of the ground-water-flow simulation was 6.3 meters, and root-mean-square errors of individual transient-calibration points ranged from 0.8 to 17.0 meters. The areal distribution of water-level measurements used in the steady-state and transient calibrations restricts the well-calibrated area of the model to the eastern side of the Tularosa Basin. Water levels in the La Luz Creek subbasin area were underestimated by both the steady-state and transient models, suggesting that the hydrology of this area is not well represented in the model.\r\n\r\nAbout 143,000 cubic meters per day of recharge is estimated to enter the basin-fill aquifer from subbasins that rim the Tularosa Basin. The estimated recharge is about 4-5 percent of total precipitation in most subbasins. Approximately 88 percent of total recharge left the basin-fill aquifer as evapotranspiration under predevelopment conditions.\r\n\r\nWater levels were simulated for 1948, 1995, and 2040 under scenarios of zero and maximum return flows. Estimated return flows from municipalities were calculated on the basis of data in the Tularosa Basin Regional Water Plan for 2000-2040. Agricultural return flows were estimated primarily on the basis of ground-water-withdrawal, ground-water-depletion, surface-water-withdrawal, and surface-water-depletion data for the Tularosa Basin. The ground-water-flow simulation was sensitive to the return-flow scenario in the agricultural area near Tularosa and decreasingly sensitive to the south. Declines in simulated water levels near Tularosa between 1948 and 1995 were as large as 30 meters under the zero return-flow scenario and 15 meters under the maximum return-flow scenario. Declines in simulated water levels between 1995 and 2040 were as large as 25 meters under the zero return-flow scenario and 15 meters under the maximum return-flow scenario. Comparison of water levels measured near Tularosa in 1991 and water levels simulated under the maximum return-flow scenario for 1991 suggests that declines in simulated water levels near Tularosa may be overestimated under the zero return-flow scenario. Declines in simulated water levels near the City of Alamogordo well field between 1948 and 1995 were as large as 15 meters under the zero return-flow scenario and 10 meters under the maximum return-flow scenario. Simulated declines in water levels between 1995 and 2040 were nearly 15 meters under both return-flow scenarios assuming that all projected increases in withdrawal came from existing City of Alamogordo public-supply wells and all withdrawal from the wells came from the basin-fill aquifer. Declines in simulated water levels near the Holloman Air Force Base well fields between 1948 and 1995 and between 1995 and 2040 were less than 5 meters under both the zero and maximum return-flow scenarios. In 1995 under the zero return-flow scenario, an estimated 56,000 cubic meters of water per day was removed from aquifer storage. Of the approximately 199,000 cubic meters of water per day that left the aquifer under 1995 conditions, 40 percent left the basin-fill aquifer as ground-water withdrawal, 51 percent as evapotranspiration, 7 percent by interbasin ground-water flow into the Hueco Bolson, and 2 percent by flow into creeks and springs.\r\n\r\nGeneralized directions of ground-water flow were simulated for 1948, 1995, and 2040 for much of the eastern part of the Tularosa Basin. Localized","language":"ENGLISH","doi":"10.3133/sir20045197","usgsCitation":"Huff, G.F., 2005, Simulation of ground-water flow in the basin-fill aquifer of the Tularosa Basin, south-central New Mexico, predevelopment through 2040: U.S. Geological Survey Scientific Investigations Report 2004-5197, 108 p., https://doi.org/10.3133/sir20045197.","productDescription":"108 p.","costCenters":[],"links":[{"id":6955,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5197/","linkFileType":{"id":5,"text":"html"}},{"id":191416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db5461c7","contributors":{"authors":[{"text":"Huff, Glenn F.","contributorId":12079,"corporation":false,"usgs":true,"family":"Huff","given":"Glenn","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":282066,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70197,"text":"sir20055035 - 2005 - Hydrogeology and trichloroethene contamination in the sea-level aquifer beneath the Logistics Center, Fort Lewis, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"sir20055035","displayToPublicDate":"2005-03-11T00:00:00","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":"2005-5035","title":"Hydrogeology and trichloroethene contamination in the sea-level aquifer beneath the Logistics Center, Fort Lewis, Washington","docAbstract":"The U.S. Army disposed of waste trichloroethene (TCE) and other materials in the East Gate Disposal Yard near the Logistics Center on Fort Lewis, Washington, from the 1940s to the early 1970s. As a result, ground water contaminated with primarily TCE extends more than 3 miles downgradient from the East Gate Disposal Yard. The site is underlain by a complex and heterogeneous sequence of glacial and non-glacial deposits that have been broadly categorized into an upper and a lower aquifer (the latter referred to as the sea-level aquifer). TCE contamination was detected in both aquifers. This report describes an investigation by the U.S. Geological Survey (USGS) of the source, migration, and attenuation of TCE in the sea-level aquifer.\r\n\r\nA refined conceptual model for ground-water flow and contaminant migration into and through the sea-level aquifer was developed in large part from interpretation of environmental tracer data. The tracers used included stable isotopes of oxygen (18O), hydrogen (2H), and carbon (13C); the radioactive hydrogen isotope tritium (3H); common ions and redox-related analytes; chlorofluorocarbons; and sulfur hexafluoride. Tracer and TCE concentrations were determined for samples collected by the USGS from 37 wells and two surface-water sites in American Lake during 1999-2000. Ground-water levels were measured by the USGS in more than 40 wells during 2000-01, and were combined with measurements by the U.S. Army and others to create potentiometric-surface maps.\r\n\r\nLocalized ground-water flow features were identified that are of particular relevance to the migration of TCE in the study area. A ridge of ground water beneath American Lake diverts the flow of TCE-contaminated ground water in the sea-level aquifer to the west around the southern end of the lake. Tracer data provided clear evidence that American Lake is a significant source of recharge to the sea-level aquifer that has created that ridge of ground water. High ground-water altitudes at locations north and northeast of the Logistics Center combined with the ridge beneath American Lake prevent TCE contaminated water beneath the Logistics Center from migrating toward municipal water-supply wells northeast of the site.\r\n\r\nThe 1999-2000 TCE concentrations measured by the USGS at older wells screened in the sea-level aquifer were similar to those measured since 1995, but the known downgradient extent of the TCE contamination expanded nearly 2 miles after the Army installed and sampled new wells during 2003-04. Concentrations of TCE in the sea-level aquifer were consistently highest in the upper part of the aquifer throughout the plume, although TCE has spread throughout much of the thickness of the aquifer in the downgradient portions of the plume.\r\n\r\nEnvironmental tracer data indicated that the primary pathway for contaminant migration into the sea-level aquifer is through the previously identified confining unit window, an area where the predominately fine-grained confining unit is relatively coarse grained and more permeable. Other less substantial pathways for contaminant migration also were identified near the East Gate Disposal Yard and the I-5 pump-and-treat facilities. Those areas are near active pumping wells and ground-water reintroduction facilities, but there is no evidence that the contaminant migration was caused or enhanced by those activities.\r\n\r\nWithin the sea-level aquifer, TCE concentrations continue to migrate westward in the flow field strongly influenced by ground-water recharge from American Lake. Historical data are not available to definitively determine if the 5-?g/L leading edge of the current TCE plume is stable or if it is still moving downgradient. However, an evaluation of the available data combined with TCE traveltime estimates indicates that the peak TCE concentrations in the sea-level aquifer may have not yet reached the wells near the currently defined leading edge of the plume. Hypothetically, the 5-?g/L leading edge","language":"ENGLISH","doi":"10.3133/sir20055035","usgsCitation":"Dinicola, R., 2005, Hydrogeology and trichloroethene contamination in the sea-level aquifer beneath the Logistics Center, Fort Lewis, Washington: U.S. Geological Survey Scientific Investigations Report 2005-5035, 59 p.; 1 plate, 42 in. x 30 in., https://doi.org/10.3133/sir20055035.","productDescription":"59 p.; 1 plate, 42 in. x 30 in.","costCenters":[],"links":[{"id":193219,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6915,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5035/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db625210","contributors":{"authors":[{"text":"Dinicola, Richard S. 0000-0003-4222-294X dinicola@usgs.gov","orcid":"https://orcid.org/0000-0003-4222-294X","contributorId":352,"corporation":false,"usgs":true,"family":"Dinicola","given":"Richard S.","email":"dinicola@usgs.gov","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282007,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70198,"text":"sir20055005 - 2005 - Streamflow trends in the Spokane River and tributaries, Spokane Valley/Rathdrum Prairie, Idaho and Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"sir20055005","displayToPublicDate":"2005-03-11T00:00:00","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":"2005-5005","title":"Streamflow trends in the Spokane River and tributaries, Spokane Valley/Rathdrum Prairie, Idaho and Washington","docAbstract":"A clear understanding of the aquifer and river dynamics within the Spokane Valley/Rathdrum Prairie is essential in making proper management decisions concerning ground-water and surface-water appropriations. Management of the Spokane Valley/Rathdrum Prairie aquifer is complicated because of interstate, multi-jurisdictional responsibilities, and by the interaction between ground water and surface water.\r\n\r\nKendall?s tau trend analyses were completed on monthly mean (July through December) and annual 7-day low streamflow data for the period 1968?2002 from gaging stations located within the Spokane Valley/Rathdrum Prairie. The analyses detected trends of decreasing monthly mean streamflow at the following gaging stations: Spokane River near Post Falls, Idaho (August and September); Spokane River at Spokane, Washington (September); and Little Spokane River at Dartford, Washington (September and October); and decreasing annual 7-day low streamflows at the following gaging stations: Spokane River near Post Falls, Idaho and Spokane River at Spokane, Washington. Limited analyses of lake-level, precipitation, tributary inflow, temperature, and water-use data provided little insight as to the reason for the decreasing trends in streamflow.\r\n\r\nA net gain in streamflow occurs between the gaging stations Spokane River near Post Falls, Idaho and Spokane River at Spokane, Washington. Significant streamflow losses occur between the gaging stations Spokane River near Post Falls, Idaho and Spokane River at Greenacres, Washington; most, if not all, of the gains occur downstream from the Greenacres gaging station. Trends of decreasing net streamflow gains in the Spokane River between the near Post Falls and at Spokane gaging stations were detected for the months of September, October, and November.","language":"ENGLISH","doi":"10.3133/sir20055005","usgsCitation":"Hortness, J., and Covert, J.J., 2005, Streamflow trends in the Spokane River and tributaries, Spokane Valley/Rathdrum Prairie, Idaho and Washington: U.S. Geological Survey Scientific Investigations Report 2005-5005, 18 p., https://doi.org/10.3133/sir20055005.","productDescription":"18 p.","costCenters":[],"links":[{"id":6916,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5005/","linkFileType":{"id":5,"text":"html"}},{"id":193220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a28b","contributors":{"authors":[{"text":"Hortness, Jon 0000-0002-9809-2876 hortness@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-2876","contributorId":3601,"corporation":false,"usgs":true,"family":"Hortness","given":"Jon","email":"hortness@usgs.gov","affiliations":[],"preferred":true,"id":282008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Covert, John J.","contributorId":72475,"corporation":false,"usgs":true,"family":"Covert","given":"John","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":282009,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70195,"text":"ds116 - 2005 - A checklist of the aquatic invertebrates of the Delaware River Basin, 1990-2000","interactions":[],"lastModifiedDate":"2017-07-10T10:46:49","indexId":"ds116","displayToPublicDate":"2005-03-11T00:00:00","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":"116","title":"A checklist of the aquatic invertebrates of the Delaware River Basin, 1990-2000","docAbstract":"This paper details a compilation of aquatic-invertebrate taxa collected at 1,080 sites as part of 13 surface-water-quality studies completed by selected Federal, state, and local environmental agencies during 1990-2000, within the 32,893-km2 area of the Delaware River Basin. This checklist is intended to be a 'working list' of aquatic invertebrates that can be applied successfully to the calculation and interpretation of various biological estimators to determine the status of water quality and can be used as a foundation to document the current state of biodiversity. It is not intended as a comprehensive historical inventory of the literature or of private and public holdings. A total of 11 phyla comprising 20 classes, 46 orders, 196 families, 685 genera, and 835 species were recorded.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds116","usgsCitation":"Bilger, M.D., Riva-Murray, K., and Wall, G.L., 2005, A checklist of the aquatic invertebrates of the Delaware River Basin, 1990-2000: U.S. Geological Survey Data Series 116, 35 p., https://doi.org/10.3133/ds116.","productDescription":"35 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":193175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6913,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ds116/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76,39 ], [ -76,43 ], [ -74,43 ], [ -74,39 ], [ -76,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4985e4b0b290850ef3ec","contributors":{"authors":[{"text":"Bilger, Michael D.","contributorId":13589,"corporation":false,"usgs":true,"family":"Bilger","given":"Michael","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":282002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riva-Murray, Karen","contributorId":85650,"corporation":false,"usgs":true,"family":"Riva-Murray","given":"Karen","affiliations":[],"preferred":false,"id":282004,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wall, Gretchen L.","contributorId":79970,"corporation":false,"usgs":true,"family":"Wall","given":"Gretchen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":282003,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70199,"text":"sir20045269 - 2005 - Simulated ground-water flow for a pond-dominated aquifer system near Great Sandy Bottom Pond, Pembroke, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"sir20045269","displayToPublicDate":"2005-03-11T00:00:00","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":"2004-5269","title":"Simulated ground-water flow for a pond-dominated aquifer system near Great Sandy Bottom Pond, Pembroke, Massachusetts","docAbstract":"A ground-water flow simulation for a 66.4-square-mile area around Great Sandy Bottom (GSB) Pond (105 acres) near Pembroke, Massachusetts, was developed for use by local and State water managers to assess the yields for public water supply of local ponds and wells for average climatic and drought conditions and the effects of water withdrawals on nearby water levels and streamflows. Wetlands and ponds cover about 30 percent of the study area and the aquifer system is dominated by interactions between ground water and the ponds. The three largest surface-water bodies in the study area are Silver Lake (640 acres), Monponsett Pond (590 acres), and Oldham Pond (236 acres). The study area is drained by tributaries of the Taunton River to the southwest, the South and North Rivers to the northeast, and the Jones River to the southeast. In 2002, 10.8 million gallons per day of water was exported from ponds and 3.5 million gallons per day from wells was used locally for public supply.\r\n\r\nA transient ground-water-flow model with 69 monthly stress periods spanning the period from January 1998 through September 2003 was calibrated to stage at GSB Pond and nearby Silver Lake and streamflow and water levels collected from September 2002 through September 2003. The calibrated model was used to assess hydrologic responses to a variety of water-use and climatic conditions. Simulation of predevelopment (no pumping or export) average monthly (1949-2002) water-level conditions caused the GSB Pond level to increase by 6.3 feet from the results of a simulation using average 2002 pumping for all wells, withdrawals, and exports. Most of this decline can be attributed to pumping, withdrawals, and exports of water from sites away from GSB Pond. The effects of increasing the export rate from GSB Pond by 1.25 and 1.5 times the 2002 rate were a lowering of pond levels by a maximum of 1.6 and 2.8 feet, respectively. Simulated results for two different drought conditions, one mild drought similar to that of 1979-82 and a more severe drought similar to that of 1963-66, but with current (2002) pumping, were compared to results for average monthly recharge conditions (1949-2002). Simulated mild drought conditions showed a reduction of GSB Pond level of about 1.3 feet and a lower streamflow of about 1.7 percent in the nearby stream. Simulated severe drought conditions reduced the pond level at GSB Pond by almost 7 feet and lowered streamflow by about 37 percent. Varying cranberry-irrigation practices had little effect on simulated GSB Pond water levels, but may be important in other ponds. The model was most sensitive to changes in areal recharge. An increase and decrease of 22 percent in recharge produced changes in the GSB Pond water level of +1.4 feet and -2.4 feet, respectively.\r\n\r\nThe accuracy of simulation results was best in the central portion of the study area in the immediate location of GSB Pond. The model was developed with the study-area boundary far enough away from the GSB Pond area that the boundary would have minimal effect on the water levels in GSB Pond, nearby ponds, and the underlying aquifer system. The model is best suited for use by local and State water managers to assess the effects of different withdrawal scenarios for wells and ponds near GSB Pond and for general delineation of areas contributing recharge to wells and ponds in the vicinity of GSB Pond. The model in its current form may not be well suited to detailed analyses of water budgets and flow patterns for parts of the study area farther from GSB Pond without further investigation, calibration, and data collection.","language":"ENGLISH","doi":"10.3133/sir20045269","usgsCitation":"Carlson, C.S., and Lyford, F.P., 2005, Simulated ground-water flow for a pond-dominated aquifer system near Great Sandy Bottom Pond, Pembroke, Massachusetts: U.S. Geological Survey Scientific Investigations Report 2004-5269, 43 p., https://doi.org/10.3133/sir20045269.","productDescription":"43 p.","costCenters":[],"links":[{"id":6917,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20045269/","linkFileType":{"id":5,"text":"html"}},{"id":124426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2004_5269.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3461","contributors":{"authors":[{"text":"Carlson, Carl S. 0000-0001-7142-3519 cscarlso@usgs.gov","orcid":"https://orcid.org/0000-0001-7142-3519","contributorId":1694,"corporation":false,"usgs":true,"family":"Carlson","given":"Carl","email":"cscarlso@usgs.gov","middleInitial":"S.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyford, Forest P.","contributorId":43334,"corporation":false,"usgs":true,"family":"Lyford","given":"Forest","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282011,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70182,"text":"sir20045115 - 2005 - Surface-water/ground-water interaction along reaches of the Snake River and Henrys Fork, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20045115","displayToPublicDate":"2005-03-09T00:00:00","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":"2004-5115","title":"Surface-water/ground-water interaction along reaches of the Snake River and Henrys Fork, Idaho","docAbstract":"Declining water levels in the eastern Snake River Plain aquifer and decreases in spring discharges from the aquifer to the Snake River have spurred studies to improve understanding of the surface-water/ground-water interaction on the plain. This study was done to estimate streamflow gains and losses along specific reaches of the Snake River and Henrys Fork and to compare changes in gain and loss estimates to changes in ground-water levels over time. Data collected during this study will be used to enhance the conceptual model of the hydrologic system and to refine computer models of ground-water flow and surface-water/ground-water interactions.\r\n\r\nEstimates of streamflow gains and losses along specific subreaches of the Snake River and Henrys Fork, based on the results of five seepage studies completed during 2001?02, varied greatly across the study area, ranging from a loss estimate of 606 ft3/s in a subreach of the upper Snake River near Heise to a gain estimate of 3,450 ft3/s in a subreach of the Snake River that includes Thousand Springs. Some variations over time also were apparent in specific subreaches. Surface spring flow accounted for much of the inflow to subreaches having large gain estimates. Several subreaches alternately gained and lost streamflow during the study.\r\n\r\nChanges in estimates of streamflow gains and losses along some of the subreaches were compared with changes in water levels, measured at three different times during 2001?02, in adjacent wells. In some instances, a strong relation between changes in estimates of gains or losses and changes in ground-water levels was apparent.","language":"ENGLISH","doi":"10.3133/sir20045115","usgsCitation":"Hortness, J., and Vidmar, P., 2005, Surface-water/ground-water interaction along reaches of the Snake River and Henrys Fork, Idaho (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5115, 27 p. with 3 appendices online, https://doi.org/10.3133/sir20045115.","productDescription":"27 p. with 3 appendices online","onlineOnly":"Y","costCenters":[],"links":[{"id":6885,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5115/","linkFileType":{"id":5,"text":"html"}},{"id":185661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db5456f9","contributors":{"authors":[{"text":"Hortness, Jon 0000-0002-9809-2876 hortness@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-2876","contributorId":3601,"corporation":false,"usgs":true,"family":"Hortness","given":"Jon","email":"hortness@usgs.gov","affiliations":[],"preferred":true,"id":281988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vidmar, Peter","contributorId":25242,"corporation":false,"usgs":true,"family":"Vidmar","given":"Peter","affiliations":[],"preferred":false,"id":281989,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70180,"text":"sir20045254 - 2005 - Chemistry of runoff and shallow ground water at the Cattlemans Detention basin site, South Lake Tahoe, California, August 2000-November 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20045254","displayToPublicDate":"2005-03-09T00:00:00","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":"2004-5254","title":"Chemistry of runoff and shallow ground water at the Cattlemans Detention basin site, South Lake Tahoe, California, August 2000-November 2001","docAbstract":"A study at the Cattlemans detention basin site began in November 2000. The site is adjacent to Cold Creek in South Lake Tahoe, California. The purpose of the study is to evaluate the effects of the detention basin on ground-water discharge and changes in nutrient loads to Cold Creek, a tributary to Trout Creek and Lake Tahoe. The study is being done in cooperation with the Tahoe Engineering Division of the El Dorado County Department of Transportation. This report summarizes data collected prior to and during construction of the detention basin and includes: (1) nutrient and total suspended solid concentrations of urban runoff; (2) distribution of unconsolidated deposits; (3) direction of ground-water flow; and (4) chemistry of shallow ground water and Cold Creek.\r\n\r\nUnconsolidated deposits in the area of the detention basin were categorized into three classes: fill material consisting of a red-brown loamy sand with some gravel and an occasional cobble that was placed on top of the meadow; meadow deposits consisting of gray silt and sand with stringers of coarse sand and fine gravel; and a deeper brown to yellow-brown sand and gravel with lenses of silt and sand. Prior to construction of the detention basin, ground water flowed west-northwest across the area of the detention basin toward Cold Creek. The direction of ground-water flow did not change during construction of the detention basin. \r\n\r\nMedian concentrations of dissolved iron and chloride were 500 and 30 times higher, respectively, in ground water from the meadow deposits than dissolved concentrations in Cold Creek. Median concentration of sulfate in ground water from the meadow deposits was 0.4 milligrams per liter and dissolved oxygen was below the detection level of 0.3 milligrams per liter. The relatively high concentrations of iron and the lack of sulfate in the shallow ground water likely are caused by chemical reactions and biological microbial oxidation of organic matter in the unconsolidated deposits that result in little to no dissolved oxygen in the ground water. The higher chloride concentrations in ground water compared with Cold Creek likely are caused from the application of salt on Pioneer Trail and streets in Montgomery Estates subdivision during the winter. Runoff from these roads contributes to the recharge of the shallow ground water. The range of dissolved constituents generally was greater in the meadow deposits than in the deeper sand and gravel. \r\n\r\nAmmonia plus organic nitrogen were the dominant forms of dissolved nitrogen and concentrations ranged from 0.04 to 18 milligrams per liter as nitrogen. Highest concentration was beneath the middle of the detention basin. Nitrate plus nitrite concentrations were low (<0.33 milligrams per liter as nitrogen) throughout the area and dissolved phosphorus concentrations ranged from 0.001 to 0.34 milligrams per liter. Nitrogen and dissolved organic carbon showed no consistent pattern in the direction of ground-water flow, which suggests that, similar to iron and sulfate, local variations in the chemical and biological reactions within the meadow deposits controlled the variation in nitrogen concentrations. The gradual increase in dissolved phosphorus along the direction of ground-water flow suggest that phosphorus may be slowly dissolving into ground water. Dissolved phosphorus was consistently low in July, which may be the result of greater microbial activity in the unconsolidated deposits or from uptake by roots during the summer.","language":"ENGLISH","doi":"10.3133/sir20045254","usgsCitation":"Prudic, D.E., Sager, S.J., Wood, J.L., Henkelman, K.K., and Caskey, R.M., 2005, Chemistry of runoff and shallow ground water at the Cattlemans Detention basin site, South Lake Tahoe, California, August 2000-November 2001: U.S. Geological Survey Scientific Investigations Report 2004-5254, 48 p., https://doi.org/10.3133/sir20045254.","productDescription":"48 p.","costCenters":[],"links":[{"id":6883,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5254/","linkFileType":{"id":5,"text":"html"}},{"id":185989,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e27a7","contributors":{"authors":[{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sager, Sienna J.","contributorId":55082,"corporation":false,"usgs":true,"family":"Sager","given":"Sienna","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":281983,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wood, James L.","contributorId":10059,"corporation":false,"usgs":true,"family":"Wood","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":281981,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Henkelman, Katherine K.","contributorId":26751,"corporation":false,"usgs":true,"family":"Henkelman","given":"Katherine","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":281982,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Caskey, Rachel M.","contributorId":74817,"corporation":false,"usgs":true,"family":"Caskey","given":"Rachel","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281984,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70184,"text":"sir20055029 - 2005 - Verification of 1921 peak discharge at Skagit River near Concrete, Washington, using 2003 peak-discharge data","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"sir20055029","displayToPublicDate":"2005-03-09T00:00:00","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":"2005-5029","title":"Verification of 1921 peak discharge at Skagit River near Concrete, Washington, using 2003 peak-discharge data","docAbstract":"The 1921 peak discharge at Skagit River near Concrete, Washington (U.S. Geological Survey streamflow-gaging station 12194000), was verified using peak-discharge data from the flood of October 21, 2003, the largest flood since 1921. This peak discharge is critical to determining other high discharges at the gaging station and to reliably estimating the 100-year flood, the primary design flood being used in a current flood study of the Skagit River basin.\r\n\r\nThe four largest annual peak discharges of record (1897, 1909, 1917, and 1921) were used to determine the 100-year flood discharge at Skagit River near Concrete. The peak discharge on December 13, 1921, was determined by James E. Stewart of the U.S. Geological Survey using a slope-area measurement and a contracted-opening measurement. An extended stage-discharge rating curve based on the 1921 peak discharge was used to determine the peak discharges of the three other large floods. Any inaccuracy in the 1921 peak discharge also would affect the accuracies of the three other largest peak discharges. \r\n\r\nThe peak discharge of the 1921 flood was recalculated using the cross sections and high-water marks surveyed after the 1921 flood in conjunction with a new estimate of the channel roughness coefficient (n value) based on an n-verification analysis of the peak discharge of the October 21, 2003, flood. The n value used by Stewart for his slope-area measurement of the 1921 flood was 0.033, and the corresponding calculated peak discharge was 240,000 cubic feet per second (ft3/s). Determination of a single definitive water-surface profile for use in the n-verification analysis was precluded because of considerable variation in elevations of surveyed high-water marks from the flood on October 21, 2003. Therefore, n values were determined for two separate water-surface profiles thought to bracket a plausible range of water-surface slopes defined by high-water marks. The n value determined using the flattest plausible slope was 0.024 and the corresponding recalculated discharge of the 1921 slope-area measurement was 266,000 ft3/s. The n value determined using the steepest plausible slope was 0.032 and the corresponding recalculated discharge of the 1921 slope-area measurement was 215,000 ft3/s. The two recalculated discharges were 10.8 percent greater than (flattest slope) and 10.4 percent less than (steepest slope) the 1921 peak discharge of 240,000 ft3/s. The 1921 peak discharge was not revised because the average of the two recalculated discharges (240,500 ft3/s) is only 0.2 percent greater than the 1921 peak discharge.","language":"ENGLISH","doi":"10.3133/sir20055029","usgsCitation":"Mastin, M.C., and Kresch, D., 2005, Verification of 1921 peak discharge at Skagit River near Concrete, Washington, using 2003 peak-discharge data: U.S. Geological Survey Scientific Investigations Report 2005-5029, 26 p., https://doi.org/10.3133/sir20055029.","productDescription":"26 p.","costCenters":[],"links":[{"id":6908,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5029/","linkFileType":{"id":5,"text":"html"}},{"id":186569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e482ae4b07f02db4e7635","contributors":{"authors":[{"text":"Mastin, M. C.","contributorId":90782,"corporation":false,"usgs":true,"family":"Mastin","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":281992,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kresch, D. L.","contributorId":52559,"corporation":false,"usgs":true,"family":"Kresch","given":"D. L.","affiliations":[],"preferred":false,"id":281991,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70163,"text":"sir20045233 - 2005 - Seepage investigation and selected hydrologic data for the Escalante River drainage basin, Garfield and Kane Counties, Utah, 1909-2002","interactions":[],"lastModifiedDate":"2019-12-30T16:14:37","indexId":"sir20045233","displayToPublicDate":"2005-03-04T00:00:00","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":"2004-5233","title":"Seepage investigation and selected hydrologic data for the Escalante River drainage basin, Garfield and Kane Counties, Utah, 1909-2002","docAbstract":"<p>This report contains the results of an October 2001 seepage investigation conducted along a reach of the Escalante River in Utah extending from the U.S. Geological Survey streamflow-gaging station near Escalante to the mouth of Stevens Canyon. Discharge was measured at 16 individual sites along 15 consecutive reaches. Total reach length was about 86 miles. A reconnaissance-level sampling of water for tritium and chlorofluorcarbons was also done. In addition, hydrologic and water-quality data previously collected and published by the U.S. Geological Survey for the 2,020-square-mile Escalante River drainage basin was compiled and is presented in 12 tables. These data were collected from 64 surface-water sites and 28 springs from 1909 to 2002.</p><p>None of the 15 consecutive reaches along the Escalante River had a measured loss or gain that exceeded the measurement error. All discharge measurements taken during the seepage investigation were assigned a qualitative rating of accuracy that ranged from 5 percent to greater than 8 percent of the actual flow. Summing the potential error for each measurement and dividing by the maximum of either the upstream discharge and any tributary inflow, or the downstream discharge, determined the normalized error for a reach. This was compared to the computed loss or gain that also was normalized to the maximum discharge. A loss or gain for a specified reach is considered significant when the loss or gain (normalized percentage difference) is greater than the measurement error (normalized percentage error). The percentage difference and percentage error were normalized to allow comparison between reaches with different amounts of discharge.</p><p>The plate that accompanies the report is 36\" by 40\" and can be printed in 16 tiles, 8.5 by 11 inches. An index for the tiles is located on the lower left-hand side of the plate. Using Adobe Acrobat, the plate can be viewed independent of the report; all Acrobat functions are available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20045233","collaboration":"Prepared in cooperation with the U.S. Department of the Interior, Bureau of Land Management, Grand Staircase-Escalante National Monument","usgsCitation":"Wilberg, D.E., and Stolp, B.J., 2005, Seepage investigation and selected hydrologic data for the Escalante River drainage basin, Garfield and Kane Counties, Utah, 1909-2002: U.S. Geological Survey Scientific Investigations Report 2004-5233, Report: vi, 39 p.; 1 Plate: 36.0 x 40.0 inches, https://doi.org/10.3133/sir20045233.","productDescription":"Report: vi, 39 p.; 1 Plate: 36.0 x 40.0 inches","numberOfPages":"45","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":6877,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5233/","linkFileType":{"id":5,"text":"html"}},{"id":334252,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2004/5233/PDF/SIR2004_5233.pdf","size":"3.2 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":185829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334253,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/sir/2004/5233/PDF/plate.pdf","text":"Plate 1","size":"4.6 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Utah","county":"Garfield County, Kane County","otherGeospatial":"Escalante River drainage basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-109.9271,38.1494],[-109.9267,38.1454],[-109.9291,38.1409],[-109.9297,38.14],[-109.9357,38.1364],[-109.9434,38.1339],[-109.9499,38.1321],[-109.954,38.1299],[-109.9576,38.1273],[-109.9619,38.1206],[-109.9637,38.1179],[-109.9656,38.1152],[-109.975,38.1113],[-109.9786,38.11],[-109.9815,38.1077],[-109.9876,38.1006],[-109.9905,38.1002],[-109.994,38.1007],[-109.9992,38.1039],[-110.0049,38.1081],[-110.0084,38.1095],[-110.0119,38.1087],[-110.0173,38.1056],[-110.0233,38.0989],[-110.0396,38.0801],[-110.0439,38.0738],[-110.0451,38.0716],[-110.0447,38.0652],[-110.0438,38.0562],[-110.048,38.049],[-110.061,38.0469],[-110.0651,38.0438],[-110.0719,38.0312],[-110.0756,38.0222],[-110.0769,38.0172],[-110.0753,38.0109],[-110.0749,38.0054],[-110.0755,38.0032],[-110.0792,37.9978],[-110.0851,37.9938],[-110.0898,37.9934],[-110.0939,37.9953],[-110.0962,37.9967],[-110.1002,37.9995],[-110.1053,38.0036],[-110.1122,38.0083],[-110.1174,38.0093],[-110.1286,38.009],[-110.1351,38.0059],[-110.1374,38.005],[-110.141,38.0015],[-110.1422,37.9992],[-110.1441,37.9952],[-110.1447,37.9943],[-110.1483,37.9907],[-110.1537,37.9867],[-110.1596,37.9823],[-110.1608,37.9814],[-110.1626,37.9778],[-110.1633,37.9737],[-110.1658,37.9697],[-110.1688,37.9656],[-110.1765,37.9607],[-110.1895,37.9532],[-110.1996,37.9475],[-110.2038,37.9439],[-110.2062,37.9408],[-110.2074,37.9367],[-110.2064,37.9331],[-110.2053,37.9294],[-110.2014,37.9199],[-110.1998,37.9139],[-110.2052,37.9077],[-110.2048,37.9022],[-110.206,37.8977],[-110.2078,37.8955],[-110.2126,37.8933],[-110.2184,37.8929],[-110.226,37.8948],[-110.2335,37.8958],[-110.2364,37.8954],[-110.2394,37.895],[-110.2545,37.898],[-110.262,37.8985],[-110.2685,37.8973],[-110.2738,37.8946],[-110.2756,37.8915],[-110.2781,37.8852],[-110.2788,37.8806],[-110.2767,37.8702],[-110.2803,37.8675],[-110.2855,37.8662],[-110.2896,37.8672],[-110.2907,37.8676],[-110.2913,37.869],[-110.294,37.8763],[-110.2962,37.8836],[-110.2973,37.8868],[-110.3007,37.8895],[-110.3042,37.89],[-110.3077,37.8896],[-110.3147,37.8888],[-110.3206,37.8894],[-110.3258,37.8899],[-110.3404,37.8905],[-110.3549,37.8912],[-110.3666,37.89],[-110.3812,37.8884],[-110.3971,37.8845],[-110.4036,37.8792],[-110.4026,37.8701],[-110.4004,37.8651],[-110.4,37.8578],[-110.4042,37.8501],[-110.4213,37.8408],[-110.4279,37.8355],[-110.4298,37.8269],[-110.4319,37.8097],[-110.4343,37.8075],[-110.439,37.8062],[-110.4442,37.8071],[-110.4494,37.8104],[-110.4529,37.8109],[-110.4704,37.8066],[-110.474,37.8021],[-110.4747,37.7953],[-110.4731,37.7894],[-110.4709,37.7835],[-110.4653,37.7748],[-110.463,37.7716],[-110.4584,37.7697],[-110.4531,37.7705],[-110.449,37.7718],[-110.4402,37.7758],[-110.4337,37.778],[-110.4303,37.778],[-110.4268,37.7756],[-110.4275,37.7716],[-110.4299,37.7689],[-110.4416,37.7631],[-110.4458,37.7587],[-110.4482,37.7532],[-110.449,37.7451],[-110.4492,37.7351],[-110.4662,37.7276],[-110.471,37.7213],[-110.4712,37.7146],[-110.4712,37.7105],[-110.4777,37.706],[-110.4877,37.7025],[-110.4878,37.698],[-110.4861,37.6952],[-110.4834,37.6866],[-110.4841,37.6807],[-110.4924,37.6708],[-110.4949,37.6645],[-110.4961,37.6609],[-110.4969,37.6514],[-110.4986,37.6505],[-110.5032,37.6547],[-110.5083,37.6593],[-110.5142,37.6589],[-110.5183,37.6562],[-110.5201,37.6539],[-110.5236,37.6504],[-110.5249,37.6468],[-110.5273,37.6404],[-110.5315,37.6373],[-110.5373,37.636],[-110.5431,37.6375],[-110.5506,37.6407],[-110.5552,37.6439],[-110.5592,37.6431],[-110.5616,37.6413],[-110.5634,37.6372],[-110.5629,37.6323],[-110.5636,37.6264],[-110.565,37.6182],[-110.5697,37.6142],[-110.5854,37.6117],[-110.5959,37.6086],[-110.6012,37.6055],[-110.6042,37.601],[-110.6038,37.5942],[-110.6027,37.5892],[-110.6005,37.5833],[-110.6,37.5769],[-110.603,37.5711],[-110.6071,37.5684],[-110.6182,37.5658],[-110.6288,37.5596],[-110.6376,37.552],[-110.6424,37.5475],[-110.6471,37.5403],[-110.6542,37.534],[-110.6596,37.5277],[-110.6633,37.5146],[-110.6664,37.5033],[-110.6682,37.5006],[-110.6683,37.4952],[-110.6584,37.4937],[-110.648,37.4927],[-110.6422,37.4913],[-110.6406,37.4881],[-110.6412,37.4849],[-110.6441,37.4831],[-110.6628,37.4784],[-110.6726,37.4789],[-110.686,37.48],[-110.7004,37.481],[-110.7092,37.4798],[-110.7197,37.4767],[-110.725,37.4695],[-110.7245,37.4654],[-110.7257,37.46],[-110.7298,37.4573],[-110.7339,37.4569],[-110.7408,37.4606],[-110.746,37.4602],[-110.7478,37.4561],[-110.7433,37.4488],[-110.7376,37.4438],[-110.7302,37.4378],[-110.7227,37.4341],[-110.7181,37.4345],[-110.7088,37.4349],[-110.7047,37.4344],[-110.7013,37.4316],[-110.7014,37.4226],[-110.7033,37.418],[-110.7086,37.4104],[-110.7163,37.4023],[-110.7227,37.4001],[-110.7348,37.4057],[-110.744,37.4067],[-110.7511,37.4031],[-110.7528,37.4],[-110.7512,37.3927],[-110.7461,37.3872],[-110.7392,37.3835],[-110.7318,37.3793],[-110.7261,37.3729],[-110.725,37.3689],[-110.7321,37.3612],[-110.7364,37.3463],[-110.7387,37.3445],[-110.7416,37.3432],[-110.7457,37.345],[-110.7467,37.3487],[-110.749,37.3519],[-110.7537,37.3506],[-110.7585,37.3384],[-110.762,37.3339],[-110.7708,37.3285],[-110.7755,37.3245],[-110.7819,37.3223],[-110.7993,37.3211],[-110.8367,37.3369],[-110.8493,37.3447],[-110.8568,37.3489],[-110.8625,37.3494],[-110.8701,37.3463],[-110.8731,37.3413],[-110.8726,37.334],[-110.8681,37.3281],[-110.8514,37.323],[-110.8439,37.3211],[-110.8404,37.3174],[-110.8371,37.307],[-110.8396,37.2979],[-110.8443,37.2943],[-110.8524,37.2917],[-110.8663,37.29],[-110.8733,37.2855],[-110.8729,37.2783],[-110.869,37.2692],[-110.8598,37.2641],[-110.8593,37.2591],[-110.8622,37.2555],[-110.8738,37.2534],[-110.8813,37.2539],[-110.8877,37.2517],[-110.889,37.2453],[-110.8827,37.2398],[-110.8805,37.2344],[-110.8799,37.2312],[-110.8783,37.2267],[-110.8835,37.2222],[-110.8899,37.2204],[-110.8946,37.2186],[-110.8975,37.215],[-110.8976,37.2114],[-110.8919,37.2041],[-110.8902,37.2005],[-110.8927,37.1923],[-110.9032,37.1852],[-110.8987,37.1729],[-110.9086,37.1712],[-110.9229,37.1781],[-110.9287,37.1754],[-110.9272,37.1627],[-110.9267,37.1555],[-110.9291,37.1514],[-110.9372,37.1478],[-110.9435,37.1497],[-110.9504,37.1502],[-110.9539,37.1498],[-110.9574,37.1467],[-110.9569,37.1412],[-110.9501,37.1307],[-110.9543,37.1253],[-110.9612,37.1222],[-110.9745,37.1255],[-110.9802,37.1251],[-110.9843,37.122],[-110.9861,37.117],[-110.9879,37.1125],[-110.9908,37.1111],[-110.9949,37.1112],[-110.9989,37.1112],[-111.0046,37.1122],[-111.0173,37.1123],[-111.0306,37.111],[-111.0393,37.1097],[-111.0505,37.0966],[-111.055,37.0976],[-111.0585,37.0994],[-111.0619,37.1013],[-111.0711,37.1041],[-111.0769,37.1032],[-111.0838,37.1028],[-111.0867,37.1028],[-111.0896,37.1024],[-111.0965,37.1024],[-111.1058,37.1034],[-111.1161,37.1053],[-111.123,37.1054],[-111.1365,37.0891],[-111.1469,37.0883],[-111.1498,37.0897],[-111.1549,37.0929],[-111.1652,37.1061],[-111.1732,37.1062],[-111.1837,37.0976],[-111.1884,37.0886],[-111.1978,37.0773],[-111.206,37.0642],[-111.2113,37.0574],[-111.2177,37.0534],[-111.2223,37.0539],[-111.2251,37.0562],[-111.2274,37.063],[-111.2331,37.0667],[-111.24,37.0662],[-111.2429,37.0613],[-111.2465,37.0545],[-111.2459,37.05],[-111.2442,37.0459],[-111.2351,37.0422],[-111.2287,37.0403],[-111.2288,37.034],[-111.2323,37.0286],[-111.2416,37.0227],[-111.2468,37.0219],[-111.2485,37.0264],[-111.253,37.0364],[-111.261,37.0473],[-111.2684,37.0533],[-111.2787,37.0565],[-111.2845,37.0588],[-111.2954,37.0666],[-111.3,37.0653],[-111.3046,37.0626],[-111.307,37.0598],[-111.3053,37.0512],[-111.3013,37.0453],[-111.2921,37.0443],[-111.2858,37.0439],[-111.2835,37.0411],[-111.2847,37.0366],[-111.2905,37.033],[-111.3003,37.0294],[-111.305,37.0272],[-111.3056,37.0218],[-111.3033,37.0177],[-111.3028,37.0131],[-111.3063,37.01],[-111.3103,37.0109],[-111.3177,37.0173],[-111.3241,37.0187],[-111.331,37.0169],[-111.3351,37.0138],[-111.342,37.0093],[-111.349,37.0079],[-111.357,37.0066],[-111.3703,37.0058],[-111.3789,37.0058],[-111.3864,37.0059],[-111.3951,37.0059],[-111.3991,37.0055],[-111.4043,37.0037],[-111.4233,37.0038],[-111.4418,37.0034],[-111.5253,37.0035],[-111.6002,37.0033],[-111.6221,37.0031],[-111.64,37.003],[-111.6613,37.0029],[-111.678,37.0031],[-111.689,37.0032],[-111.7057,37.003],[-111.708,37.003],[-111.7501,37.0033],[-111.7656,37.0032],[-111.8388,37.0028],[-111.8466,37.0028],[-111.8567,37.0028],[-111.8964,37.0027],[-111.961,37.0025],[-112.0013,37.0024],[-112.0284,37.0024],[-112.033,37.0024],[-112.0784,37.0026],[-112.082,37.0026],[-112.0998,37.0026],[-112.1206,37.0027],[-112.1339,37.0027],[-112.1892,37.0028],[-112.207,37.0029],[-112.2284,37.0029],[-112.2433,37.003],[-112.3621,37.0033],[-112.445,37.0032],[-112.4964,37.0032],[-112.5424,37.0032],[-112.6231,37.0031],[-112.7055,37.0031],[-112.7447,37.0033],[-112.8231,37.003],[-112.8697,37.0028],[-112.9037,37.0027],[-112.9029,37.0304],[-112.9035,37.034],[-112.9031,37.0485],[-112.9033,37.0607],[-112.9027,37.0639],[-112.9028,37.0675],[-112.9024,37.0852],[-112.9027,37.1106],[-112.903,37.1315],[-112.9025,37.1387],[-112.9031,37.1451],[-112.9032,37.1532],[-112.9029,37.175],[-112.9038,37.1954],[-112.9023,37.2158],[-112.9029,37.2235],[-112.9029,37.2666],[-112.9031,37.2824],[-112.9054,37.2824],[-112.9056,37.2992],[-112.9057,37.3559],[-112.9058,37.364],[-112.9059,37.3717],[-112.9055,37.3858],[-112.9051,37.4003],[-112.9053,37.4152],[-112.9043,37.4279],[-112.9045,37.4429],[-112.9041,37.4579],[-112.9046,37.5005],[-112.9047,37.5154],[-112.9051,37.5449],[-112.8534,37.5448],[-112.8331,37.5449],[-112.7948,37.5448],[-112.7641,37.5445],[-112.6874,37.545],[-112.6877,37.574],[-112.6902,37.7186],[-112.6931,37.7185],[-112.6934,37.7525],[-112.6931,37.7752],[-112.6928,37.8065],[-112.6567,37.8076],[-112.6491,37.8085],[-112.6275,37.8082],[-112.5949,37.8065],[-112.5815,37.8057],[-112.5812,37.8383],[-112.5815,37.8832],[-112.5909,37.8832],[-112.5909,37.8909],[-112.5623,37.8905],[-112.5256,37.8912],[-112.5245,37.8912],[-112.5075,37.8912],[-112.4895,37.8913],[-112.489,37.9063],[-112.4715,37.9059],[-112.4711,37.9349],[-112.4706,37.9462],[-112.4707,37.9635],[-112.4696,37.9789],[-112.483,37.9788],[-112.4825,37.9847],[-112.4822,38.0273],[-112.4817,38.0418],[-112.4818,38.0572],[-112.4813,38.0658],[-112.4808,38.0862],[-112.481,38.1098],[-112.481,38.1148],[-112.4805,38.1293],[-112.4806,38.1379],[-112.4806,38.1474],[-112.4754,38.1474],[-112.4754,38.1497],[-112.4543,38.1498],[-112.4362,38.1494],[-112.3893,38.1505],[-112.3583,38.1501],[-112.3226,38.1498],[-112.3068,38.1498],[-112.2869,38.1503],[-112.2629,38.1504],[-112.2477,38.1499],[-112.2149,38.15],[-112.1734,38.1496],[-112.1605,38.1496],[-112.1412,38.1501],[-112.0622,38.1497],[-112.0622,38.1465],[-112.0429,38.1466],[-112.0207,38.1466],[-112.0078,38.147],[-112.0019,38.1466],[-111.9855,38.147],[-111.968,38.147],[-111.951,38.147],[-111.9516,38.152],[-111.9352,38.152],[-111.9317,38.152],[-111.8574,38.1528],[-111.8427,38.1528],[-111.8211,38.1523],[-111.7912,38.1527],[-111.7666,38.1527],[-111.7479,38.1522],[-111.7456,38.1522],[-111.7315,38.1526],[-111.7075,38.1526],[-111.6941,38.1525],[-111.6601,38.1524],[-111.6543,38.1524],[-111.6397,38.1524],[-111.5998,38.1527],[-111.5636,38.1521],[-111.5372,38.152],[-111.5074,38.1524],[-111.4594,38.1522],[-111.4284,38.1516],[-111.4173,38.1515],[-111.4172,38.1551],[-111.3897,38.155],[-111.2698,38.1539],[-111.2335,38.1537],[-111.2147,38.154],[-111.189,38.1534],[-111.1785,38.1533],[-111.1229,38.1529],[-111.1176,38.1529],[-111.1024,38.1528],[-111.0936,38.1523],[-111.0842,38.1527],[-111.0661,38.1525],[-111.0608,38.1525],[-111.0152,38.1526],[-111.0105,38.1521],[-111.0023,38.1525],[-110.9918,38.1524],[-110.9847,38.1523],[-110.9742,38.1522],[-110.9689,38.1522],[-110.9561,38.1521],[-110.9011,38.1516],[-110.897,38.1516],[-110.8812,38.1514],[-110.8782,38.1514],[-110.863,38.1517],[-110.8443,38.1515],[-110.7899,38.151],[-110.7863,38.151],[-110.7682,38.1508],[-110.7495,38.1506],[-110.7489,38.1506],[-110.7313,38.1504],[-110.6769,38.1507],[-110.6582,38.151],[-110.6394,38.1512],[-110.6213,38.1511],[-110.5669,38.1509],[-110.547,38.1511],[-110.5282,38.1513],[-110.5101,38.1516],[-110.4703,38.1511],[-110.4557,38.1509],[-110.4375,38.1511],[-110.4205,38.1509],[-110.4024,38.1511],[-110.3468,38.1508],[-110.3269,38.1506],[-110.3087,38.1508],[-110.2906,38.151],[-110.2561,38.1509],[-110.2373,38.1507],[-110.2169,38.1504],[-110.2016,38.1502],[-110.1981,38.1501],[-110.18,38.1503],[-110.1618,38.1505],[-110.0992,38.1495],[-110.0664,38.1499],[-110.0518,38.1497],[-109.9962,38.1492],[-109.9271,38.1494]]]},\"properties\":{\"name\":\"Garfield\",\"state\":\"UT\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb9fa","contributors":{"authors":[{"text":"Wilberg, Dale E.","contributorId":101275,"corporation":false,"usgs":true,"family":"Wilberg","given":"Dale","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":281966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stolp, Bernard J. 0000-0003-3803-1497 bjstolp@usgs.gov","orcid":"https://orcid.org/0000-0003-3803-1497","contributorId":963,"corporation":false,"usgs":true,"family":"Stolp","given":"Bernard","email":"bjstolp@usgs.gov","middleInitial":"J.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281965,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70161,"text":"sir20055045 - 2005 - Calibrating a tensor magnetic gradiometer using spin data","interactions":[],"lastModifiedDate":"2025-05-14T18:56:24.226938","indexId":"sir20055045","displayToPublicDate":"2005-03-04T00:00:00","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":"2005-5045","title":"Calibrating a tensor magnetic gradiometer using spin data","docAbstract":"Scalar magnetic data are often acquired to discern characteristics of geologic source materials and buried objects. It is evident that a great deal can be done with scalar data, but there are significant advantages to direct measurement of the magnetic gradient tensor in applications with nearby sources, such as unexploded ordnance (UXO). To explore these advantages, we adapted a prototype tensor magnetic gradiometer system (TMGS) and successfully implemented a data-reduction procedure. One of several critical reduction issues is the precise determination of a large group of calibration coefficients for the sensors and sensor array. To resolve these coefficients, we devised a spin calibration method, after similar methods of calibrating space-based magnetometers (Snare, 2001). The spin calibration procedure consists of three parts: (1) collecting data by slowly revolving the sensor array in the Earth?s magnetic field, (2) deriving a comprehensive set of coefficients from the spin data, and (3) applying the coefficients to the survey data. To show that the TMGS functions as a tensor gradiometer, we conducted an experimental survey that verified that the reduction procedure was effective (Bracken and Brown, in press). Therefore, because it was an integral part of the reduction, it can be concluded that the spin calibration was correctly formulated with acceptably small errors.","language":"ENGLISH","doi":"10.3133/sir20055045","usgsCitation":"Bracken, R.E., Smith, D.V., and Brown, P., 2005, Calibrating a tensor magnetic gradiometer using spin data (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5045, 1 p. online; 9 p. report, https://doi.org/10.3133/sir20055045.","productDescription":"1 p. online; 9 p. report","costCenters":[],"links":[{"id":6875,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5045/","linkFileType":{"id":5,"text":"html"}},{"id":185741,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f93e0","contributors":{"authors":[{"text":"Bracken, Robert E. 0000-0001-7759-2743 rbracken@usgs.gov","orcid":"https://orcid.org/0000-0001-7759-2743","contributorId":2640,"corporation":false,"usgs":true,"family":"Bracken","given":"Robert","email":"rbracken@usgs.gov","middleInitial":"E.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":281961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, David V. 0000-0003-0426-4401 dvsmith@usgs.gov","orcid":"https://orcid.org/0000-0003-0426-4401","contributorId":1306,"corporation":false,"usgs":true,"family":"Smith","given":"David","email":"dvsmith@usgs.gov","middleInitial":"V.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":281960,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Philip J.","contributorId":70483,"corporation":false,"usgs":true,"family":"Brown","given":"Philip J.","affiliations":[],"preferred":false,"id":281962,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70162,"text":"sir20055046 - 2005 - Reducing tensor magnetic gradiometer data for unexploded ordnance detection","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20055046","displayToPublicDate":"2005-03-04T00:00:00","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":"2005-5046","title":"Reducing tensor magnetic gradiometer data for unexploded ordnance detection","docAbstract":"We performed a survey to demonstrate the effectiveness of a prototype tensor magnetic gradiometer system (TMGS) for detection of buried unexploded ordnance (UXO). In order to achieve a useful result, we designed a data-reduction procedure that resulted in a realistic magnetic gradient tensor and devised a simple way of viewing complicated tensor data, not only to assess the validity of the final resulting tensor, but also to preview the data at interim stages of processing. The final processed map of the surveyed area clearly shows a sharp anomaly that peaks almost directly over the target UXO. This map agrees well with a modeled map derived from dipolar sources near the known target locations. From this agreement, it can be deduced that the reduction process is valid, making the prototype TMGS a foundation for development of future systems and processes.","language":"ENGLISH","doi":"10.3133/sir20055046","usgsCitation":"Bracken, R.E., and Brown, P., 2005, Reducing tensor magnetic gradiometer data for unexploded ordnance detection (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5046, 1 p. online; 10 p. report, https://doi.org/10.3133/sir20055046.","productDescription":"1 p. online; 10 p. report","costCenters":[],"links":[{"id":185828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6876,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5046/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689f40","contributors":{"authors":[{"text":"Bracken, Robert E. 0000-0001-7759-2743 rbracken@usgs.gov","orcid":"https://orcid.org/0000-0001-7759-2743","contributorId":2640,"corporation":false,"usgs":true,"family":"Bracken","given":"Robert","email":"rbracken@usgs.gov","middleInitial":"E.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":281963,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Philip J.","contributorId":70483,"corporation":false,"usgs":true,"family":"Brown","given":"Philip J.","affiliations":[],"preferred":false,"id":281964,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70156,"text":"sim2868 - 2005 - Water-surface elevation data and flood and floodway boundaries for the upper Yellowstone River, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sim2868","displayToPublicDate":"2005-03-03T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2868","title":"Water-surface elevation data and flood and floodway boundaries for the upper Yellowstone River, Montana","language":"ENGLISH","doi":"10.3133/sim2868","usgsCitation":"Parrett, C., Holnbeck, S.R., and Chase, K.J., 2005, Water-surface elevation data and flood and floodway boundaries for the upper Yellowstone River, Montana (Online only): U.S. Geological Survey Scientific Investigations Map 2868, 5 sheets, 48 in. x 42 in., https://doi.org/10.3133/sim2868.","productDescription":"5 sheets, 48 in. x 42 in.","onlineOnly":"Y","costCenters":[],"links":[{"id":6873,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sim20042868/","linkFileType":{"id":5,"text":"html"}},{"id":185657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d70","contributors":{"authors":[{"text":"Parrett, Charles","contributorId":9635,"corporation":false,"usgs":true,"family":"Parrett","given":"Charles","email":"","affiliations":[],"preferred":false,"id":281958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holnbeck, Stephen R. 0000-0001-7313-9298 holnbeck@usgs.gov","orcid":"https://orcid.org/0000-0001-7313-9298","contributorId":1724,"corporation":false,"usgs":true,"family":"Holnbeck","given":"Stephen","email":"holnbeck@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":281957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chase, Katherine J. 0000-0002-5796-4148 kchase@usgs.gov","orcid":"https://orcid.org/0000-0002-5796-4148","contributorId":454,"corporation":false,"usgs":true,"family":"Chase","given":"Katherine","email":"kchase@usgs.gov","middleInitial":"J.","affiliations":[{"id":685,"text":"Wyoming-Montana Water Science Center","active":false,"usgs":true}],"preferred":true,"id":281956,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70209603,"text":"70209603 - 2005 - Evaluation of groundwater movement in the Frenchman Flat CAU using geochemical and isotopic analysis","interactions":[],"lastModifiedDate":"2020-04-15T13:40:05.420066","indexId":"70209603","displayToPublicDate":"2005-03-01T08:18:22","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":295,"text":"Technical Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"DOE/NV/13609-36","title":"Evaluation of groundwater movement in the Frenchman Flat CAU using geochemical and isotopic analysis","docAbstract":"<div class=\"biblio-detail\"><p id=\"citation-abstract\" class=\"description\">The principal pathway for radionuclide migration from underground tests in Frenchman Flat, on the Nevada Test Site, to the accessible environment is groundwater flow. Two potential pathways for radionuclide transport via groundwater have been identified from hydrologic data: (1) radionuclide transport downward from the alluvial and volcanic aquifers into the underlying carbonate aquifer; and (2) radionuclide transport laterally to the carbonate aquifer surrounding Frenchman Flat. This report presents an evaluation of geochemical and environmental isotopic data to test these potential pathways and to identify other groundwater flowpaths in, and out of, Frenchman Flat.</p></div><div class=\"biblio-detail\"><br data-mce-bogus=\"1\"></div>","language":"English","publisher":"Desert Research Institute","doi":"10.2172/839138","usgsCitation":"Hershey, R., Thomas, J., Rose, T., Paces, J.B., Farnham, I.M., and Benedict, F.C., 2005, Evaluation of groundwater movement in the Frenchman Flat CAU using geochemical and isotopic analysis: Technical Report DOE/NV/13609-36, viii, 65 p., https://doi.org/10.2172/839138.","productDescription":"viii, 65 p.","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":477679,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://www.osti.gov/biblio/839138","text":"External Repository"},{"id":374008,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Frenchman Flat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.09939575195312,\n              36.72017310567465\n            ],\n            [\n              -115.89889526367188,\n              36.72017310567465\n            ],\n            [\n              -115.89889526367188,\n              36.89499795802219\n            ],\n            [\n              -116.09939575195312,\n              36.89499795802219\n            ],\n            [\n              -116.09939575195312,\n              36.72017310567465\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationDate":"2005-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hershey, R.","contributorId":224122,"corporation":false,"usgs":false,"family":"Hershey","given":"R.","affiliations":[],"preferred":false,"id":787103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, J.","contributorId":224124,"corporation":false,"usgs":false,"family":"Thomas","given":"J.","affiliations":[],"preferred":false,"id":787104,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rose, T.","contributorId":224125,"corporation":false,"usgs":false,"family":"Rose","given":"T.","affiliations":[],"preferred":false,"id":787105,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Paces, James B. 0000-0002-9809-8493 jbpaces@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-8493","contributorId":2514,"corporation":false,"usgs":true,"family":"Paces","given":"James","email":"jbpaces@usgs.gov","middleInitial":"B.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787106,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Farnham, I. M.","contributorId":224126,"corporation":false,"usgs":false,"family":"Farnham","given":"I.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":787107,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Benedict, F. C.","contributorId":97068,"corporation":false,"usgs":true,"family":"Benedict","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":787108,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70184390,"text":"70184390 - 2005 - Geochemistry and the understanding of ground-water systems","interactions":[],"lastModifiedDate":"2018-03-21T15:05:45","indexId":"70184390","displayToPublicDate":"2005-02-25T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1923,"text":"Hydrogeology Journal","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry and the understanding of ground-water systems","docAbstract":"<p><span>Geochemistry has contributed significantly to the understanding of ground-water systems over the last 50 years. Historic advances include development of the hydrochemical facies concept, application of equilibrium theory, investigation of redox processes, and radiocarbon dating. Other hydrochemical concepts, tools, and techniques have helped elucidate mechanisms of flow and transport in ground-water systems, and have helped unlock an archive of paleoenvironmental information. Hydrochemical and isotopic information can be used to interpret the origin and mode of ground-water recharge, refine estimates of time scales of recharge and ground-water flow, decipher reactive processes, provide paleohydrological information, and calibrate ground-water flow models. Progress needs to be made in obtaining representative samples. Improvements are needed in the interpretation of the information obtained, and in the construction and interpretation of numerical models utilizing hydrochemical data. The best approach will ensure an optimized iterative process between field data collection and analysis, interpretation, and the application of forward, inverse, and statistical modeling tools. Advances are anticipated from microbiological investigations, the characterization of natural organics, isotopic fingerprinting, applications of dissolved gas measurements, and the fields of reaction kinetics and coupled processes. A thermodynamic perspective is offered that could facilitate the comparison and understanding of the multiple physical, chemical, and biological processes affecting ground-water systems.</span></p>","language":"English","publisher":"Springer-Verlag","doi":"10.1007/s10040-004-0429-y","usgsCitation":"Glynn, P.D., and Plummer, N., 2005, Geochemistry and the understanding of ground-water systems: Hydrogeology Journal, v. 13, no. 1, p. 263-287, https://doi.org/10.1007/s10040-004-0429-y.","productDescription":"26 p. ","startPage":"263","endPage":"287","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":337065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"1","noUsgsAuthors":false,"publicationDate":"2005-02-25","publicationStatus":"PW","scienceBaseUri":"58c12640e4b014cc3a3d34ca","contributors":{"authors":[{"text":"Glynn, Pierre D. 0000-0001-8804-7003 pglynn@usgs.gov","orcid":"https://orcid.org/0000-0001-8804-7003","contributorId":2141,"corporation":false,"usgs":true,"family":"Glynn","given":"Pierre","email":"pglynn@usgs.gov","middleInitial":"D.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":681277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":681278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":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":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":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 Document, https://doi.org/10.3133/ofr20051052.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":185930,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6781,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1052/","linkFileType":{"id":5,"text":"html"}},{"id":415288,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70517.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","country":"United States","state":"Virginia","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-75.973607,37.835817],[-75.971705,37.830928],[-75.977301,37.825821],[-75.982158,37.806226],[-75.987301,37.804917],[-75.9983,37.812626],[-75.999658,37.848198],[-75.992556,37.848889],[-75.988018,37.841085],[-75.973607,37.835817]]],[[[-76.029405,37.953776],[-75.994739,37.953501],[-76.017592,37.935161],[-76.032491,37.915008],[-76.04653,37.953586],[-76.029405,37.953776]]],[[[-75.242266,38.027209],[-75.296871,37.959043],[-75.334296,37.893477],[-75.359036,37.864143],[-75.374642,37.859454],[-75.40054,37.874865],[-75.437868,37.872324],[-75.467951,37.851328],[-75.514921,37.799149],[-75.581333,37.683593],[-75.586136,37.660653],[-75.610808,37.605909],[-75.612237,37.585602],[-75.608123,37.578018],[-75.595716,37.576657],[-75.594044,37.569698],[-75.63337,37.52214],[-75.666178,37.472124],[-75.66179,37.455028],[-75.665957,37.439209],[-75.697914,37.405301],[-75.720739,37.373129],[-75.727335,37.360346],[-75.726691,37.350127],[-75.735829,37.335426],[-75.765401,37.305596],[-75.778817,37.297176],[-75.784634,37.300976],[-75.798448,37.296285],[-75.79083,37.276207],[-75.799343,37.251779],[-75.789929,37.228134],[-75.804446,37.208011],[-75.800755,37.197297],[-75.897298,37.118037],[-75.912308,37.115154],[-75.92552,37.133601],[-75.945872,37.120514],[-75.97043,37.118608],[-75.978083,37.157338],[-76.013071,37.205366],[-76.010535,37.231579],[-76.025753,37.257407],[-76.023664,37.268971],[-76.015507,37.280874],[-76.023475,37.289067],[-76.018645,37.31782],[-76.014251,37.331943],[-75.987122,37.368548],[-75.97997,37.404608],[-75.983105,37.415802],[-75.981624,37.434116],[-75.960877,37.467562],[-75.963326,37.481785],[-75.958966,37.500133],[-75.940318,37.534582],[-75.937665,37.549652],[-75.941182,37.563839],[-75.924756,37.600215],[-75.909586,37.622671],[-75.868481,37.668224],[-75.868355,37.687609],[-75.859262,37.703111],[-75.837685,37.712985],[-75.827922,37.737986],[-75.812155,37.749502],[-75.803041,37.762464],[-75.818125,37.791698],[-75.784599,37.806826],[-75.743097,37.806656],[-75.73588,37.816561],[-75.723224,37.820124],[-75.71659,37.826696],[-75.709114,37.8477],[-75.689837,37.861817],[-75.685293,37.873341],[-75.687584,37.88634],[-75.709626,37.900622],[-75.753048,37.896605],[-75.758796,37.897615],[-75.757694,37.903912],[-75.712065,37.936082],[-75.704318,37.92901],[-75.693942,37.930362],[-75.669711,37.950796],[-75.655681,37.945435],[-75.647606,37.947027],[-75.648229,37.966775],[-75.638221,37.979397],[-75.629532,37.975966],[-75.633712,37.983057],[-75.624342,37.994208],[-75.242266,38.027209]]],[[[-77.041898,38.741514],[-77.041398,38.724515],[-77.045498,38.714315],[-77.053199,38.709915],[-77.079499,38.709515],[-77.1059,38.696815],[-77.132501,38.673816],[-77.135901,38.649817],[-77.1302,38.635017],[-77.157501,38.636417],[-77.174902,38.624217],[-77.202002,38.617217],[-77.216303,38.637817],[-77.240604,38.638917],[-77.246704,38.635217],[-77.247003,38.590618],[-77.26443,38.582845],[-77.26083,38.56533],[-77.276603,38.54712],[-77.276303,38.53962],[-77.283503,38.525221],[-77.310334,38.493926],[-77.322622,38.467131],[-77.32544,38.44885],[-77.310719,38.397669],[-77.317288,38.383576],[-77.296077,38.369797],[-77.279633,38.339444],[-77.265295,38.333165],[-77.240072,38.331598],[-77.162692,38.345994],[-77.138224,38.367917],[-77.08481,38.368297],[-77.069956,38.377895],[-77.056032,38.3962],[-77.043526,38.400548],[-77.011827,38.374554],[-77.016932,38.341697],[-77.030683,38.311623],[-77.026304,38.302685],[-76.99767,38.278047],[-76.981372,38.274214],[-76.96215,38.256486],[-76.957417,38.236341],[-76.967335,38.227185],[-76.962311,38.214075],[-76.937134,38.202384],[-76.910832,38.197073],[-76.875272,38.172207],[-76.838795,38.163476],[-76.788445,38.169199],[-76.760241,38.166581],[-76.743064,38.156988],[-76.738938,38.14651],[-76.721722,38.137635],[-76.704048,38.149264],[-76.701297,38.155718],[-76.684892,38.156497],[-76.665127,38.147638],[-76.643448,38.14825],[-76.629476,38.15305],[-76.613939,38.148587],[-76.604131,38.128771],[-76.600937,38.110084],[-76.579497,38.09487],[-76.543155,38.076971],[-76.535919,38.069532],[-76.516547,38.026566],[-76.469343,38.013544],[-76.462542,37.998572],[-76.416299,37.966828],[-76.343848,37.947345],[-76.265998,37.91138],[-76.236725,37.889174],[-76.251358,37.833072],[-76.275178,37.812664],[-76.282592,37.814109],[-76.284904,37.822308],[-76.293525,37.822717],[-76.307482,37.81235],[-76.310307,37.794849],[-76.306489,37.788646],[-76.312108,37.750522],[-76.304917,37.729913],[-76.312858,37.720338],[-76.300067,37.695364],[-76.302545,37.689],[-76.324808,37.676983],[-76.339892,37.655966],[-76.332562,37.645817],[-76.292534,37.636098],[-76.279447,37.618225],[-76.28037,37.613715],[-76.309174,37.621892],[-76.36232,37.610368],[-76.381106,37.627003],[-76.390054,37.630326],[-76.399236,37.628636],[-76.472392,37.665772],[-76.489576,37.666201],[-76.497564,37.647056],[-76.510187,37.642324],[-76.536548,37.663574],[-76.537228,37.698892],[-76.560476,37.727827],[-76.584289,37.76889],[-76.602024,37.772731],[-76.651413,37.796239],[-76.680197,37.825654],[-76.701606,37.822677],[-76.72718,37.842263],[-76.747552,37.875864],[-76.765711,37.879274],[-76.784618,37.869569],[-76.766328,37.840437],[-76.723863,37.788503],[-76.689773,37.78519],[-76.683775,37.781391],[-76.683372,37.765507],[-76.677002,37.7561],[-76.61971,37.744795],[-76.61997,37.731271],[-76.597213,37.717269],[-76.597868,37.702918],[-76.579591,37.671508],[-76.583143,37.661986],[-76.574049,37.646781],[-76.542666,37.616857],[-76.527188,37.611315],[-76.435474,37.612807],[-76.420252,37.598686],[-76.410781,37.581815],[-76.383188,37.573056],[-76.357835,37.573699],[-76.300144,37.561734],[-76.29796,37.557636],[-76.302762,37.551295],[-76.330598,37.536391],[-76.348992,37.536548],[-76.360474,37.51924],[-76.352678,37.504913],[-76.32947,37.49492],[-76.306952,37.497488],[-76.297739,37.506863],[-76.297651,37.515424],[-76.293599,37.516499],[-76.281043,37.507821],[-76.265056,37.481365],[-76.252415,37.447274],[-76.245283,37.386839],[-76.24846,37.375135],[-76.264847,37.357399],[-76.272888,37.335174],[-76.275552,37.309964],[-76.282555,37.319107],[-76.308581,37.329366],[-76.31205,37.338088],[-76.337476,37.364014],[-76.387112,37.385061],[-76.393958,37.39594],[-76.415167,37.402133],[-76.418719,37.3978],[-76.418176,37.385064],[-76.437525,37.37975],[-76.445333,37.36646],[-76.406388,37.332924],[-76.38777,37.30767],[-76.381075,37.28534],[-76.369029,37.279311],[-76.352556,37.278334],[-76.349489,37.273963],[-76.392788,37.264973],[-76.417173,37.26395],[-76.421765,37.255198],[-76.429141,37.25331],[-76.475927,37.250543],[-76.48284,37.254831],[-76.493302,37.24947],[-76.50364,37.233856],[-76.494008,37.225408],[-76.471799,37.216016],[-76.394132,37.22515],[-76.389793,37.222981],[-76.396052,37.201087],[-76.389284,37.193503],[-76.391252,37.179887],[-76.399659,37.160272],[-76.381379,37.155711],[-76.35969,37.16858],[-76.348658,37.170655],[-76.343234,37.166207],[-76.34405,37.160367],[-76.334017,37.144223],[-76.311088,37.138495],[-76.292344,37.126615],[-76.271262,37.084544],[-76.304272,37.001378],[-76.315008,37.001683],[-76.318065,37.013846],[-76.34011,37.015212],[-76.348066,37.006747],[-76.383367,36.993347],[-76.411768,36.962847],[-76.428869,36.969947],[-76.452118,36.998163],[-76.452461,37.004603],[-76.448231,37.007705],[-76.464471,37.027547],[-76.518242,37.055351],[-76.526273,37.062947],[-76.526203,37.077773],[-76.536875,37.083942],[-76.555066,37.075859],[-76.564219,37.077507],[-76.579499,37.096627],[-76.618252,37.119347],[-76.62478,37.127091],[-76.622252,37.142146],[-76.604476,37.160034],[-76.606684,37.166674],[-76.610972,37.166994],[-76.623292,37.198738],[-76.649869,37.220914],[-76.689166,37.222866],[-76.730951,37.213813],[-76.74,37.195379],[-76.75047,37.190098],[-76.757765,37.191658],[-76.780532,37.209336],[-76.801023,37.206043],[-76.802511,37.198308],[-76.796905,37.189404],[-76.756899,37.161582],[-76.747632,37.150548],[-76.73032,37.145395],[-76.715295,37.148035],[-76.696735,37.174403],[-76.691918,37.195731],[-76.685614,37.198851],[-76.663774,37.173875],[-76.67147,37.158739],[-76.671588,37.14206],[-76.666542,37.138179],[-76.656894,37.109843],[-76.669822,37.06426],[-76.662558,37.045748],[-76.646013,37.036228],[-76.612124,37.035604],[-76.586491,37.02874],[-76.562923,37.003796],[-76.524853,36.983833],[-76.521006,36.973187],[-76.513363,36.968057],[-76.500355,36.965212],[-76.487559,36.952372],[-76.482407,36.917364],[-76.483369,36.896239],[-76.469914,36.882898],[-76.454692,36.884077],[-76.453941,36.89274],[-76.441605,36.906116],[-76.407507,36.897444],[-76.387567,36.899547],[-76.385867,36.923247],[-76.345569,36.924531],[-76.344663,36.919313],[-76.328864,36.918447],[-76.330765,36.938647],[-76.327365,36.959447],[-76.315867,36.955351],[-76.297663,36.968147],[-76.267962,36.964547],[-76.22166,36.939547],[-76.139557,36.923047],[-76.095508,36.908817],[-76.058154,36.916947],[-76.033454,36.931946],[-76.013753,36.930746],[-75.996252,36.922047],[-75.94955,36.76115],[-75.921748,36.692051],[-75.890946,36.630753],[-75.874145,36.583853],[-75.867044,36.550754],[-76.915897,36.552093],[-76.916048,36.543815],[-77.152691,36.544078],[-77.16966,36.547315],[-77.205156,36.544581],[-78.245462,36.544411],[-78.529722,36.540981],[-80.122183,36.542646],[-80.295243,36.543973],[-80.704831,36.562319],[-80.837089,36.559154],[-81.003802,36.563629],[-81.176712,36.571926],[-81.442228,36.576822],[-81.600934,36.587019],[-81.677535,36.588117],[-81.6469,36.611918],[-81.922644,36.616213],[-81.934144,36.594213],[-83.248933,36.593827],[-83.2763,36.598187],[-83.55681,36.597384],[-83.675413,36.600814],[-83.649513,36.616683],[-83.645213,36.624183],[-83.628913,36.624083],[-83.607913,36.637083],[-83.577312,36.641784],[-83.562612,36.651284],[-83.541812,36.656584],[-83.529612,36.666184],[-83.498011,36.670485],[-83.466483,36.6647],[-83.423707,36.667385],[-83.395806,36.676786],[-83.386099,36.686589],[-83.307103,36.711387],[-83.194597,36.739487],[-83.136395,36.743088],[-83.127833,36.750828],[-83.126719,36.761],[-83.132477,36.764398],[-83.128494,36.775588],[-83.131694,36.781488],[-83.103092,36.806689],[-83.098492,36.814289],[-83.101792,36.829089],[-83.07519,36.840889],[-83.07259,36.854589],[-83.047589,36.851789],[-83.026887,36.855489],[-83.021887,36.849989],[-83.009222,36.847295],[-82.998376,36.85663],[-82.970253,36.857686],[-82.951685,36.866152],[-82.907774,36.874706],[-82.906325,36.87974],[-82.879492,36.889085],[-82.870068,36.901735],[-82.877473,36.90796],[-82.858635,36.927785],[-82.861282,36.944848],[-82.856099,36.952471],[-82.87023,36.965498],[-82.868455,36.976481],[-82.862926,36.979975],[-82.857936,36.978276],[-82.853729,36.985178],[-82.845002,36.983812],[-82.836008,36.988837],[-82.830802,36.993445],[-82.828592,37.005707],[-82.782144,37.008242],[-82.759175,37.027333],[-82.747981,37.025214],[-82.743684,37.041397],[-82.722472,37.045101],[-82.727022,37.073019],[-82.718353,37.075706],[-82.717204,37.079544],[-82.724954,37.091905],[-82.721617,37.101276],[-82.726449,37.114985],[-82.722097,37.120168],[-82.684601,37.135835],[-82.676765,37.134965],[-82.651646,37.151908],[-82.633493,37.154264],[-82.592451,37.182847],[-82.550372,37.204458],[-82.531576,37.209163],[-82.528746,37.213742],[-82.520117,37.212906],[-82.498858,37.227044],[-82.491486,37.225086],[-82.487317,37.230578],[-82.457016,37.238288],[-82.449164,37.243908],[-82.350948,37.267077],[-82.342068,37.274109],[-82.341849,37.280886],[-82.324619,37.28318],[-82.309415,37.300066],[-81.968297,37.537798],[-81.969279,37.534325],[-81.959362,37.53522],[-81.953524,37.528056],[-81.943981,37.5303],[-81.94766,37.52508],[-81.943693,37.521212],[-81.944756,37.513657],[-81.938749,37.512902],[-81.933088,37.518968],[-81.926391,37.514207],[-81.941151,37.509483],[-81.943912,37.502929],[-81.951831,37.50205],[-81.953264,37.491763],[-81.964986,37.493488],[-81.977593,37.484603],[-81.992916,37.482969],[-81.995649,37.469833],[-81.987006,37.454878],[-81.976176,37.457186],[-81.965582,37.446918],[-81.949367,37.445687],[-81.945765,37.440214],[-81.935621,37.438397],[-81.940553,37.429058],[-81.93695,37.41992],[-81.923481,37.411379],[-81.930042,37.405291],[-81.928778,37.393845],[-81.936744,37.38073],[-81.926697,37.364618],[-81.928497,37.360645],[-81.916678,37.349346],[-81.899495,37.341102],[-81.893773,37.330105],[-81.880886,37.331146],[-81.860267,37.315715],[-81.865429,37.31012],[-81.859624,37.304765],[-81.856032,37.306742],[-81.853551,37.287701],[-81.849949,37.285227],[-81.838762,37.286343],[-81.834432,37.285416],[-81.83447,37.281763],[-81.819625,37.279411],[-81.805382,37.285622],[-81.793595,37.284838],[-81.793639,37.282188],[-81.789294,37.284416],[-81.774747,37.274847],[-81.76022,37.275254],[-81.745505,37.26133],[-81.744291,37.244178],[-81.739277,37.238837],[-81.723061,37.240493],[-81.716248,37.234321],[-81.71573,37.228771],[-81.695113,37.21357],[-81.683544,37.211452],[-81.683268,37.205649],[-81.678603,37.202467],[-81.5536,37.208443],[-81.545211,37.220165],[-81.508786,37.232564],[-81.498874,37.258025],[-81.492287,37.25096],[-81.480144,37.251121],[-81.449068,37.269583],[-81.416663,37.273214],[-81.40506,37.298794],[-81.398185,37.302965],[-81.394287,37.316411],[-81.388132,37.319903],[-81.374455,37.318614],[-81.362156,37.337687],[-81.320105,37.299323],[-81.225104,37.234874],[-81.167029,37.262881],[-81.112596,37.278497],[-80.979589,37.302279],[-80.981322,37.293465],[-80.966556,37.292158],[-80.947896,37.295872],[-80.900535,37.315],[-80.868986,37.338573],[-80.849451,37.346909],[-80.883248,37.383933],[-80.862761,37.411829],[-80.865148,37.419927],[-80.859563,37.429558],[-80.846324,37.423394],[-80.837678,37.425658],[-80.808769,37.406271],[-80.806129,37.398074],[-80.784188,37.394587],[-80.770082,37.372363],[-80.705203,37.394618],[-80.645893,37.422147],[-80.63439,37.431227],[-80.622664,37.433307],[-80.552036,37.473563],[-80.511391,37.481672],[-80.492981,37.457749],[-80.49728,37.444779],[-80.494867,37.43507],[-80.475601,37.422949],[-80.371952,37.474069],[-80.36317,37.480001],[-80.366838,37.484879],[-80.309331,37.50288],[-80.299789,37.508271],[-80.282385,37.533517],[-80.291644,37.536505],[-80.309346,37.527381],[-80.330306,37.536244],[-80.312393,37.546239],[-80.328504,37.564315],[-80.258919,37.595499],[-80.240272,37.606961],[-80.220984,37.627767],[-80.267228,37.646011],[-80.279372,37.657077],[-80.296138,37.691783],[-80.253077,37.725899],[-80.252024,37.729825],[-80.262765,37.738336],[-80.257411,37.756084],[-80.251622,37.755866],[-80.246902,37.768309],[-80.230458,37.778305],[-80.217634,37.776775],[-80.215892,37.781989],[-80.227965,37.791714],[-80.227092,37.798886],[-80.218611,37.809783],[-80.206482,37.81597],[-80.199633,37.827507],[-80.179391,37.839751],[-80.183062,37.850646],[-80.176712,37.854029],[-80.162202,37.875122],[-80.148951,37.886892],[-80.141947,37.882616],[-80.12362,37.897943],[-80.117747,37.89772],[-80.118967,37.903614],[-80.102931,37.918911],[-80.096563,37.918112],[-80.074514,37.942221],[-80.04841,37.957481],[-79.999384,37.995842],[-79.995901,38.005791],[-79.973701,38.032556],[-79.954369,38.080397],[-79.92633,38.107151],[-79.938051,38.110759],[-79.944843,38.131585],[-79.933751,38.135508],[-79.925512,38.150237],[-79.918662,38.15479],[-79.914884,38.167524],[-79.917924,38.168399],[-79.916622,38.177994],[-79.921026,38.179954],[-79.91441,38.188418],[-79.898426,38.193045],[-79.888045,38.20736],[-79.850324,38.233329],[-79.846445,38.240003],[-79.835124,38.241892],[-79.830882,38.249687],[-79.817149,38.249511],[-79.811987,38.260401],[-79.806333,38.259193],[-79.790134,38.267654],[-79.789791,38.281167],[-79.795448,38.290228],[-79.802778,38.292073],[-79.810115,38.305037],[-79.808711,38.309429],[-79.79655,38.32348],[-79.77309,38.335529],[-79.764432,38.356514],[-79.740615,38.354101],[-79.725973,38.363229],[-79.72679,38.370832],[-79.730494,38.372217],[-79.72635,38.38707],[-79.706634,38.41573],[-79.689675,38.431439],[-79.691478,38.446282],[-79.688365,38.45687],[-79.698929,38.469869],[-79.693424,38.481011],[-79.697572,38.487223],[-79.692273,38.496474],[-79.682974,38.501317],[-79.680374,38.510617],[-79.670474,38.507717],[-79.663474,38.514117],[-79.662974,38.518717],[-79.672974,38.528717],[-79.666874,38.538317],[-79.669275,38.549516],[-79.665075,38.560916],[-79.659275,38.562416],[-79.659375,38.572616],[-79.649075,38.591515],[-79.53827,38.551817],[-79.521469,38.533918],[-79.476638,38.457228],[-79.312276,38.411876],[-79.288432,38.42096],[-79.282971,38.418095],[-79.279678,38.424173],[-79.282762,38.431647],[-79.267414,38.438322],[-79.254435,38.455949],[-79.242641,38.454168],[-79.240059,38.469841],[-79.225669,38.476471],[-79.219067,38.487441],[-79.210591,38.492913],[-79.206959,38.503522],[-79.210959,38.507422],[-79.205859,38.524521],[-79.176658,38.56552],[-79.170958,38.56812],[-79.170858,38.574119],[-79.158657,38.592319],[-79.159158,38.601219],[-79.151257,38.620618],[-79.131057,38.653217],[-79.122256,38.659817],[-79.106356,38.656217],[-79.092955,38.659517],[-79.084355,38.686516],[-79.090755,38.692515],[-79.092755,38.702315],[-79.072555,38.747513],[-79.057554,38.760213],[-79.055654,38.770913],[-79.051554,38.772613],[-79.054954,38.785713],[-79.046554,38.792113],[-79.029253,38.791013],[-79.023053,38.798613],[-79.024053,38.809212],[-79.019553,38.817912],[-79.006152,38.824512],[-78.998171,38.847353],[-78.993997,38.850102],[-78.869276,38.762991],[-78.786025,38.887187],[-78.759085,38.900529],[-78.738921,38.927283],[-78.718482,38.934267],[-78.71981,38.905907],[-78.717178,38.904296],[-78.704323,38.915231],[-78.69738,38.915602],[-78.670679,38.9338],[-78.646589,38.968138],[-78.638423,38.966819],[-78.625672,38.982575],[-78.620453,38.982601],[-78.618676,38.974082],[-78.611184,38.976134],[-78.601655,38.964603],[-78.570462,39.001552],[-78.550467,39.018065],[-78.571901,39.031995],[-78.540216,39.060631],[-78.522714,39.071062],[-78.495984,39.09898],[-78.478426,39.109843],[-78.475376,39.107469],[-78.459869,39.113351],[-78.439429,39.132146],[-78.427294,39.152726],[-78.403697,39.167451],[-78.426315,39.182762],[-78.428697,39.187217],[-78.424292,39.192156],[-78.438651,39.198049],[-78.405585,39.231176],[-78.404214,39.241214],[-78.399669,39.243874],[-78.418584,39.256065],[-78.414204,39.26391],[-78.367242,39.310148],[-78.364686,39.317312],[-78.35894,39.319484],[-78.346301,39.339108],[-78.347634,39.34272],[-78.339284,39.348605],[-78.34048,39.353492],[-78.366867,39.35929],[-78.343214,39.388807],[-78.350014,39.392861],[-78.349436,39.397252],[-78.359918,39.409028],[-78.346718,39.427618],[-78.353227,39.436792],[-78.346061,39.445613],[-78.345143,39.459484],[-78.349476,39.462205],[-78.347087,39.466012],[-77.828157,39.132329],[-77.822182,39.139985],[-77.821413,39.15241],[-77.805991,39.172421],[-77.793631,39.210125],[-77.771415,39.236776],[-77.767277,39.24938],[-77.770589,39.249393],[-77.770669,39.255262],[-77.762844,39.258445],[-77.747287,39.295001],[-77.730047,39.315666],[-77.719029,39.321125],[-77.692984,39.31845],[-77.677123,39.324077],[-77.650997,39.310784],[-77.615939,39.302722],[-77.592739,39.30129],[-77.566596,39.306121],[-77.561826,39.301913],[-77.560854,39.286152],[-77.540581,39.264947],[-77.486813,39.247586],[-77.45812,39.22614],[-77.459883,39.218682],[-77.47361,39.208407],[-77.477362,39.190495],[-77.505162,39.18205],[-77.516426,39.170891],[-77.527282,39.146236],[-77.524559,39.127821],[-77.519929,39.120925],[-77.4858,39.109303],[-77.458202,39.073723],[-77.38568,39.061987],[-77.340287,39.062991],[-77.293105,39.046508],[-77.274706,39.034091],[-77.248403,39.026909],[-77.244603,39.020109],[-77.255703,39.002409],[-77.249203,38.993709],[-77.249803,38.985909],[-77.234803,38.97631],[-77.232268,38.979502],[-77.221502,38.97131],[-77.197502,38.96681],[-77.183002,38.96881],[-77.148179,38.965002],[-77.1034,38.912911],[-77.0902,38.904211],[-77.067299,38.899211],[-77.058254,38.880069],[-77.049099,38.870712],[-77.046599,38.874912],[-77.039099,38.868112],[-77.031698,38.850512],[-77.032798,38.841712],[-77.044199,38.840212],[-77.044899,38.834712],[-77.039199,38.832212],[-77.035798,38.814913],[-77.041898,38.741514]]]]},\"properties\":{\"name\":\"Virginia\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdf09","contributors":{"authors":[{"text":"Snyder, Stephen L. ssnyder@usgs.gov","contributorId":4753,"corporation":false,"usgs":true,"family":"Snyder","given":"Stephen","email":"ssnyder@usgs.gov","middleInitial":"L.","affiliations":[{"id":5068,"text":"Midwest Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":281821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70082,"text":"ofr20051022 - 2005 - South Carolina aeromagnetic and gravity maps and data: A web site for distribution of data","interactions":[],"lastModifiedDate":"2023-04-04T21:03:32.663158","indexId":"ofr20051022","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":"2005-1022","title":"South Carolina 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/ofr20051022","usgsCitation":"Daniels, D.L., 2005, South Carolina aeromagnetic and gravity maps and data: A web site for distribution of data: U.S. Geological Survey Open-File Report 2005-1022, HTML Document, https://doi.org/10.3133/ofr20051022.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[],"links":[{"id":185931,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":415191,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70518.htm"},{"id":6782,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1022/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Carolina","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-79.290754,33.110051],[-79.329909,33.089986],[-79.337169,33.072302],[-79.335346,33.065362],[-79.339313,33.050336],[-79.359961,33.006672],[-79.403712,33.003903],[-79.416515,33.006815],[-79.423447,33.015085],[-79.483499,33.001265],[-79.488727,33.015832],[-79.506923,33.032813],[-79.522449,33.03535],[-79.55756,33.021269],[-79.580725,33.006447],[-79.58659,32.991334],[-79.606615,32.972248],[-79.617611,32.952726],[-79.617715,32.94487],[-79.606194,32.925953],[-79.585897,32.926461],[-79.581687,32.931341],[-79.572614,32.933885],[-79.569762,32.926692],[-79.576006,32.906235],[-79.631149,32.888606],[-79.695141,32.850398],[-79.702956,32.835781],[-79.719879,32.825796],[-79.716761,32.813627],[-79.726389,32.805996],[-79.811021,32.77696],[-79.818237,32.766352],[-79.84035,32.756816],[-79.848527,32.755248],[-79.866742,32.757422],[-79.872232,32.752128],[-79.873605,32.745657],[-79.868352,32.734849],[-79.870336,32.727777],[-79.888028,32.695177],[-79.884961,32.684402],[-79.915682,32.664915],[-79.968468,32.639732],[-79.975248,32.639537],[-79.986917,32.626388],[-79.99175,32.616389],[-79.999374,32.611851],[-80.010505,32.608852],[-80.037276,32.610236],[-80.077039,32.603319],[-80.121368,32.590523],[-80.148406,32.578479],[-80.167286,32.559885],[-80.171764,32.546118],[-80.188401,32.553604],[-80.20523,32.555547],[-80.246361,32.531114],[-80.277681,32.516161],[-80.332438,32.478104],[-80.338354,32.47873],[-80.343883,32.490795],[-80.363956,32.496098],[-80.380716,32.486359],[-80.386827,32.47881],[-80.392561,32.475332],[-80.413487,32.470672],[-80.417896,32.476076],[-80.418502,32.490894],[-80.423454,32.497989],[-80.439407,32.503472],[-80.452078,32.497286],[-80.46571,32.4953],[-80.472068,32.496964],[-80.48025,32.477407],[-80.484617,32.460976],[-80.480156,32.447048],[-80.467588,32.425259],[-80.446075,32.423721],[-80.43296,32.410659],[-80.429941,32.401782],[-80.429291,32.389667],[-80.434303,32.375193],[-80.445451,32.350335],[-80.456814,32.336884],[-80.455192,32.326458],[-80.466342,32.31917],[-80.517871,32.298796],[-80.545688,32.282076],[-80.571096,32.273278],[-80.596394,32.273549],[-80.618286,32.260183],[-80.638857,32.255618],[-80.658634,32.248638],[-80.669166,32.216783],[-80.688857,32.200971],[-80.721463,32.160427],[-80.749091,32.140137],[-80.789996,32.122494],[-80.812503,32.109746],[-80.82153,32.108589],[-80.828394,32.113222],[-80.831531,32.112709],[-80.844431,32.109709],[-80.858735,32.099581],[-80.905378,32.051943],[-80.892344,32.043764],[-80.885517,32.0346],[-80.922794,32.039151],[-80.954482,32.068622],[-80.983133,32.079609],[-80.994333,32.094608],[-81.002297,32.100048],[-81.011961,32.100176],[-81.021622,32.090897],[-81.032674,32.08545],[-81.050234,32.085308],[-81.060442,32.087503],[-81.088234,32.10395],[-81.091498,32.110782],[-81.111134,32.112005],[-81.117234,32.117605],[-81.119994,32.134268],[-81.118334,32.144403],[-81.122034,32.161803],[-81.129634,32.165602],[-81.128134,32.169102],[-81.119434,32.175402],[-81.120434,32.178702],[-81.118234,32.189201],[-81.12315,32.201329],[-81.128283,32.208634],[-81.136012,32.212858],[-81.143139,32.221731],[-81.156587,32.24391],[-81.148334,32.255098],[-81.145834,32.263397],[-81.136534,32.272697],[-81.128034,32.276297],[-81.119633,32.287596],[-81.122333,32.305395],[-81.137633,32.328194],[-81.133032,32.334794],[-81.133632,32.341293],[-81.142532,32.350893],[-81.147632,32.349393],[-81.150589,32.34587],[-81.154,32.345924],[-81.155032,32.350093],[-81.170126,32.361318],[-81.169332,32.369436],[-81.181072,32.380398],[-81.178131,32.38459],[-81.177231,32.39169],[-81.20513,32.423788],[-81.20843,32.435987],[-81.201595,32.44136],[-81.202359,32.450448],[-81.192629,32.456286],[-81.186829,32.464086],[-81.194829,32.465086],[-81.200029,32.467985],[-81.233585,32.498488],[-81.238728,32.508896],[-81.234834,32.512271],[-81.23466,32.51627],[-81.252882,32.51833],[-81.277131,32.535417],[-81.274927,32.544158],[-81.281298,32.55644],[-81.297955,32.563026],[-81.320588,32.559534],[-81.328753,32.561228],[-81.366964,32.577059],[-81.369757,32.591231],[-81.373178,32.592115],[-81.379216,32.589022],[-81.389261,32.595383],[-81.393865,32.60234],[-81.411906,32.61841],[-81.41866,32.629392],[-81.418431,32.634704],[-81.414761,32.63744],[-81.41026,32.631392],[-81.407271,32.631737],[-81.402846,32.63621],[-81.405109,32.64269],[-81.393033,32.651543],[-81.398314,32.656307],[-81.405273,32.656517],[-81.407193,32.660519],[-81.401029,32.677494],[-81.40831,32.694908],[-81.4131,32.692648],[-81.427517,32.701896],[-81.421194,32.711978],[-81.418542,32.732586],[-81.411549,32.740145],[-81.410281,32.744653],[-81.416198,32.750428],[-81.415212,32.757753],[-81.417606,32.762684],[-81.426481,32.769023],[-81.425636,32.77184],[-81.421269,32.774658],[-81.421128,32.778039],[-81.428313,32.78311],[-81.429017,32.785505],[-81.424999,32.790334],[-81.423772,32.810514],[-81.419752,32.813731],[-81.417984,32.818196],[-81.421614,32.835178],[-81.426475,32.840773],[-81.444866,32.850967],[-81.451199,32.847925],[-81.453949,32.849761],[-81.455978,32.854107],[-81.451351,32.868583],[-81.45392,32.874074],[-81.475918,32.877641],[-81.479445,32.881082],[-81.4771,32.887469],[-81.464069,32.897814],[-81.479184,32.905638],[-81.483198,32.921802],[-81.502427,32.935353],[-81.502716,32.938688],[-81.499446,32.944988],[-81.507045,32.951194],[-81.508536,32.957156],[-81.506449,32.962423],[-81.49983,32.963816],[-81.494736,32.978998],[-81.491197,32.997824],[-81.492253,33.009342],[-81.50203,33.015113],[-81.511245,33.027786],[-81.519632,33.029181],[-81.538789,33.039185],[-81.544258,33.046905],[-81.553643,33.044137],[-81.557013,33.0451],[-81.559179,33.047386],[-81.560502,33.055207],[-81.57288,33.05418],[-81.588539,33.07085],[-81.594555,33.069887],[-81.599248,33.071813],[-81.600211,33.075182],[-81.598165,33.081078],[-81.601655,33.084688],[-81.608995,33.0818],[-81.609476,33.089862],[-81.612725,33.093953],[-81.617779,33.095277],[-81.637232,33.092952],[-81.646433,33.094552],[-81.658433,33.103152],[-81.683533,33.112651],[-81.696934,33.116551],[-81.704634,33.116451],[-81.743835,33.14145],[-81.763135,33.159449],[-81.766735,33.170749],[-81.772435,33.180449],[-81.765735,33.187948],[-81.760635,33.189248],[-81.756935,33.197848],[-81.763535,33.203648],[-81.768935,33.217447],[-81.774035,33.221147],[-81.780135,33.221147],[-81.777535,33.211347],[-81.784535,33.208147],[-81.805236,33.211447],[-81.807936,33.213747],[-81.809636,33.222647],[-81.827936,33.228746],[-81.837016,33.237652],[-81.846536,33.241746],[-81.851979,33.247382],[-81.853137,33.250745],[-81.847336,33.266345],[-81.840078,33.26704],[-81.838257,33.272975],[-81.844036,33.278644],[-81.851836,33.283544],[-81.861336,33.286244],[-81.863236,33.288844],[-81.861536,33.297944],[-81.849636,33.299544],[-81.846136,33.303843],[-81.847296,33.306783],[-81.867936,33.314043],[-81.875836,33.307443],[-81.884137,33.310443],[-81.886637,33.316943],[-81.897329,33.322331],[-81.896937,33.327642],[-81.900301,33.331117],[-81.906444,33.324181],[-81.909285,33.324181],[-81.919137,33.334442],[-81.917973,33.34159],[-81.924737,33.345341],[-81.932737,33.343541],[-81.939737,33.344941],[-81.934837,33.356041],[-81.944737,33.364041],[-81.946337,33.37064],[-81.939637,33.37254],[-81.930634,33.368165],[-81.925737,33.37114],[-81.924837,33.37414],[-81.930861,33.380076],[-81.936961,33.404197],[-81.92306,33.408266],[-81.920121,33.410753],[-81.91933,33.415613],[-81.924893,33.419307],[-81.927241,33.422846],[-81.926789,33.426576],[-81.924981,33.429288],[-81.916236,33.433114],[-81.913356,33.437418],[-81.913532,33.441274],[-81.926336,33.462937],[-81.934136,33.468337],[-81.985938,33.486536],[-81.990938,33.494235],[-81.991938,33.504435],[-82.001338,33.520135],[-82.007138,33.522835],[-82.011538,33.531735],[-82.019838,33.535035],[-82.028238,33.544934],[-82.033023,33.546454],[-82.037375,33.554662],[-82.046335,33.56383],[-82.057727,33.566774],[-82.073104,33.57751],[-82.094128,33.582742],[-82.10624,33.595637],[-82.115328,33.596501],[-82.12908,33.589925],[-82.142872,33.594278],[-82.148816,33.598092],[-82.156288,33.60863],[-82.174351,33.613117],[-82.186154,33.62088],[-82.196583,33.630582],[-82.201186,33.646898],[-82.200718,33.66464],[-82.208411,33.669872],[-82.216868,33.6844],[-82.234576,33.700216],[-82.237192,33.70788],[-82.235753,33.71439],[-82.239098,33.730872],[-82.247472,33.752591],[-82.255267,33.75969],[-82.263206,33.761962],[-82.266127,33.766745],[-82.277681,33.772032],[-82.285804,33.780058],[-82.298286,33.783518],[-82.300213,33.800627],[-82.313339,33.809205],[-82.32448,33.820033],[-82.346933,33.834298],[-82.371775,33.843813],[-82.37975,33.851086],[-82.395736,33.859089],[-82.403881,33.865477],[-82.422803,33.863754],[-82.43115,33.867051],[-82.440503,33.875123],[-82.455105,33.88165],[-82.480111,33.901897],[-82.492929,33.909754],[-82.50764,33.931456],[-82.51295,33.936969],[-82.524515,33.94336],[-82.534111,33.943651],[-82.543128,33.940949],[-82.556835,33.945353],[-82.564531,33.955741],[-82.568288,33.968772],[-82.579576,33.979761],[-82.580571,33.98514],[-82.575351,33.990904],[-82.576222,33.993106],[-82.583394,33.995286],[-82.589245,34.000118],[-82.595655,34.016118],[-82.594555,34.028717],[-82.609655,34.039917],[-82.626963,34.063457],[-82.630972,34.065528],[-82.635991,34.064941],[-82.64398,34.072237],[-82.645661,34.076046],[-82.640345,34.086304],[-82.641553,34.092212],[-82.648184,34.098649],[-82.658561,34.103118],[-82.666879,34.113591],[-82.668113,34.12016],[-82.67732,34.131657],[-82.68629,34.134454],[-82.692152,34.138986],[-82.70414,34.141007],[-82.717507,34.150504],[-82.723312,34.165895],[-82.731881,34.178363],[-82.732761,34.195338],[-82.74192,34.210063],[-82.740447,34.219679],[-82.744415,34.224913],[-82.74198,34.230196],[-82.744834,34.242957],[-82.744056,34.252407],[-82.748756,34.263407],[-82.746656,34.266407],[-82.755028,34.276067],[-82.770928,34.285402],[-82.780308,34.296701],[-82.781752,34.302901],[-82.78684,34.310381],[-82.794054,34.339772],[-82.835004,34.366069],[-82.836611,34.382676],[-82.841524,34.39013],[-82.841326,34.397332],[-82.847446,34.412049],[-82.848651,34.423844],[-82.854434,34.432275],[-82.855762,34.443977],[-82.860874,34.451469],[-82.860707,34.457428],[-82.875463,34.463503],[-82.876464,34.465803],[-82.873831,34.471508],[-82.876864,34.475303],[-82.902665,34.485902],[-82.922866,34.481402],[-82.928466,34.484202],[-82.940867,34.486102],[-82.947367,34.479602],[-82.954667,34.477302],[-82.960668,34.482002],[-82.979568,34.482702],[-82.992215,34.479198],[-82.995279,34.475648],[-82.99509,34.472483],[-83.002924,34.472132],[-83.029315,34.484147],[-83.034712,34.483495],[-83.043771,34.488816],[-83.054463,34.50289],[-83.069451,34.502131],[-83.087189,34.515939],[-83.077995,34.523746],[-83.087789,34.532078],[-83.102179,34.532179],[-83.103987,34.540166],[-83.122901,34.560129],[-83.129676,34.561699],[-83.152577,34.578299],[-83.154577,34.588198],[-83.170278,34.592398],[-83.169994,34.605444],[-83.179439,34.60802],[-83.196979,34.605998],[-83.199779,34.608398],[-83.211598,34.610905],[-83.23178,34.611297],[-83.243381,34.617997],[-83.240676,34.624307],[-83.255281,34.637696],[-83.271982,34.641896],[-83.292883,34.654196],[-83.300848,34.66247],[-83.301477,34.666582],[-83.304641,34.669561],[-83.316401,34.669316],[-83.321463,34.677543],[-83.330284,34.681342],[-83.336207,34.680534],[-83.33869,34.682002],[-83.340383,34.688998],[-83.349975,34.699155],[-83.347718,34.705474],[-83.352485,34.715993],[-83.353238,34.728648],[-83.348829,34.737194],[-83.338666,34.742295],[-83.320062,34.759616],[-83.319945,34.773725],[-83.323866,34.789712],[-83.313782,34.799911],[-83.301182,34.804008],[-83.302395,34.813241],[-83.294292,34.814725],[-83.289914,34.824477],[-83.275656,34.816862],[-83.268159,34.821393],[-83.267293,34.832748],[-83.269982,34.837196],[-83.267656,34.845289],[-83.254605,34.846402],[-83.252582,34.853483],[-83.24722,34.85844],[-83.245602,34.865522],[-83.240847,34.866736],[-83.238419,34.869771],[-83.239081,34.875661],[-83.22924,34.879907],[-83.220099,34.878124],[-83.213323,34.882796],[-83.205627,34.880142],[-83.201183,34.884653],[-83.204572,34.890284],[-83.203351,34.893717],[-83.186541,34.899534],[-83.168524,34.91788],[-83.160937,34.918269],[-83.153253,34.926342],[-83.140621,34.924915],[-83.130554,34.930932],[-83.129493,34.937402],[-83.121112,34.939129],[-83.121214,34.942684],[-83.126761,34.948742],[-83.127035,34.953778],[-83.12114,34.958966],[-83.120387,34.968406],[-83.106991,34.98272],[-83.1046,34.992783],[-83.108535,35.000771],[-82.787867,35.085024],[-82.783283,35.0856],[-82.776357,35.081349],[-82.781973,35.066817],[-82.777376,35.064143],[-82.764464,35.068177],[-82.757704,35.068019],[-82.754162,35.069629],[-82.749491,35.078487],[-82.738379,35.079453],[-82.729683,35.087827],[-82.72701,35.094142],[-82.715297,35.092943],[-82.703916,35.097651],[-82.694898,35.098456],[-82.688456,35.106347],[-82.691194,35.114721],[-82.68604,35.124545],[-82.683625,35.125833],[-82.676861,35.12535],[-82.669614,35.118103],[-82.662381,35.118123],[-82.642237,35.129215],[-82.629031,35.126155],[-82.621185,35.134635],[-82.609706,35.139039],[-82.59814,35.137729],[-82.59243,35.139002],[-82.588158,35.142928],[-82.578316,35.142104],[-82.569912,35.145268],[-82.563767,35.151575],[-82.556168,35.151736],[-82.554227,35.156911],[-82.550508,35.159498],[-82.540483,35.160306],[-82.529973,35.155617],[-82.521403,35.158851],[-82.516044,35.163442],[-82.495506,35.164312],[-82.483937,35.173798],[-82.476136,35.175486],[-82.467991,35.174633],[-82.460092,35.178143],[-82.455609,35.177425],[-82.452987,35.17469],[-82.451201,35.16526],[-82.439595,35.165863],[-82.435689,35.167715],[-82.424461,35.193092],[-82.419744,35.198613],[-82.403348,35.204473],[-82.39293,35.215402],[-82.384029,35.210542],[-82.378744,35.198053],[-82.380903,35.189565],[-82.376808,35.184427],[-82.371298,35.181449],[-82.364299,35.184725],[-82.361469,35.190831],[-82.344554,35.193115],[-82.340133,35.189188],[-82.333934,35.190661],[-82.330779,35.189032],[-82.330549,35.186767],[-82.32335,35.184789],[-82.315871,35.190678],[-82.295354,35.194965],[-82.288453,35.198605],[-82.27492,35.200071],[-82.176874,35.19379],[-81.716259,35.178852],[-81.241686,35.160081],[-81.043625,35.149877],[-81.047826,35.143743],[-81.051037,35.131654],[-81.038968,35.126299],[-81.033005,35.113747],[-81.032806,35.108049],[-81.037369,35.102541],[-81.046524,35.100617],[-81.052078,35.096276],[-81.057236,35.086129],[-81.058029,35.07319],[-81.057648,35.062433],[-81.041489,35.044703],[-80.93495,35.107409],[-80.884887,35.05351],[-80.782042,34.935782],[-80.797543,34.819786],[-80.499788,34.817261],[-79.870693,34.805378],[-79.675299,34.804744],[-79.358317,34.545358],[-79.249763,34.449774],[-78.541087,33.851112],[-78.553944,33.847831],[-78.584841,33.844282],[-78.67226,33.817587],[-78.714116,33.800138],[-78.772737,33.768511],[-78.812931,33.743472],[-78.862931,33.705654],[-78.938076,33.639826],[-79.007356,33.566565],[-79.028516,33.533365],[-79.084588,33.483669],[-79.10136,33.461016],[-79.135441,33.403867],[-79.147496,33.378243],[-79.152035,33.350925],[-79.158429,33.332811],[-79.162332,33.327246],[-79.180318,33.254141],[-79.180563,33.237955],[-79.172394,33.206577],[-79.18787,33.173712],[-79.195631,33.166016],[-79.215453,33.155569],[-79.238262,33.137055],[-79.24609,33.124865],[-79.290754,33.110051]]]},\"properties\":{\"name\":\"South Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7555","contributors":{"authors":[{"text":"Daniels, David L. 0000-0003-0599-8036 dave@usgs.gov","orcid":"https://orcid.org/0000-0003-0599-8036","contributorId":1792,"corporation":false,"usgs":true,"family":"Daniels","given":"David","email":"dave@usgs.gov","middleInitial":"L.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":281822,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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 Center","active":true,"usgs":true}],"links":[{"id":185932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6783,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ia-04-1/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","country":"United States","state":"Iowa","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.217706,43.50055],[-91.216035,43.481142],[-91.233367,43.455168],[-91.200359,43.412701],[-91.198953,43.389835],[-91.21477,43.365874],[-91.20662,43.352524],[-91.132813,43.32803],[-91.107237,43.313645],[-91.07371,43.274746],[-91.071698,43.261014],[-91.058644,43.257679],[-91.066398,43.239293],[-91.12217,43.197255],[-91.1462,43.152405],[-91.1562,43.142945],[-91.175253,43.134665],[-91.179457,43.067427],[-91.156562,42.978226],[-91.14543,42.958211],[-91.14988,42.941955],[-91.1438,42.922877],[-91.146177,42.90985],[-91.100565,42.883078],[-91.097656,42.859871],[-91.091837,42.851225],[-91.09406,42.830813],[-91.078665,42.827678],[-91.069549,42.769628],[-91.060261,42.761847],[-91.065783,42.753387],[-91.056297,42.747341],[-91.051275,42.737001],[-91.035418,42.73734],[-91.026786,42.724228],[-91.000128,42.716189],[-90.977735,42.696816],[-90.949213,42.685573],[-90.923634,42.6855],[-90.88743,42.67247],[-90.731132,42.643437],[-90.706303,42.634169],[-90.692031,42.610366],[-90.686975,42.591774],[-90.661527,42.567999],[-90.654127,42.5499],[-90.643927,42.540401],[-90.636927,42.513202],[-90.655927,42.491703],[-90.654027,42.478503],[-90.624328,42.458904],[-90.567968,42.440389],[-90.560439,42.432897],[-90.555018,42.416138],[-90.477279,42.383794],[-90.462619,42.367253],[-90.443874,42.355218],[-90.416535,42.325109],[-90.430884,42.27823],[-90.419326,42.254467],[-90.400653,42.239293],[-90.391108,42.225473],[-90.356964,42.205445],[-90.328273,42.201047],[-90.282173,42.178846],[-90.234919,42.165431],[-90.209479,42.15268],[-90.197342,42.128163],[-90.167533,42.122475],[-90.161159,42.106372],[-90.168358,42.075779],[-90.164485,42.042105],[-90.151579,42.030633],[-90.140061,42.003252],[-90.146225,41.981329],[-90.164135,41.956178],[-90.163847,41.944934],[-90.152659,41.933058],[-90.153584,41.906614],[-90.181401,41.844647],[-90.181973,41.80707],[-90.278633,41.767358],[-90.310708,41.742214],[-90.317668,41.72269],[-90.313435,41.698082],[-90.334525,41.679559],[-90.343452,41.646959],[-90.339528,41.598633],[-90.343228,41.587833],[-90.41283,41.565333],[-90.461432,41.523533],[-90.500633,41.518033],[-90.540935,41.526133],[-90.591037,41.512832],[-90.602137,41.506032],[-90.605937,41.494232],[-90.655839,41.462132],[-90.750142,41.449632],[-90.846558,41.455141],[-90.930016,41.421404],[-90.979815,41.434321],[-91.027787,41.423603],[-91.043988,41.415897],[-91.05101,41.387556],[-91.06652,41.365246],[-91.074841,41.305578],[-91.092034,41.286911],[-91.114186,41.250029],[-91.113648,41.241401],[-91.07298,41.207151],[-91.041536,41.166138],[-91.027214,41.163373],[-91.007586,41.166183],[-90.99496,41.160624],[-90.946627,41.096632],[-90.949383,41.072711],[-90.942253,41.034702],[-90.945949,41.006495],[-90.958142,40.979767],[-90.952233,40.954047],[-90.965344,40.921633],[-91.009536,40.900565],[-91.021562,40.884021],[-91.044653,40.868356],[-91.05643,40.848387],[-91.092993,40.821079],[-91.097649,40.805575],[-91.091703,40.779708],[-91.110424,40.745528],[-91.115735,40.725168],[-91.11194,40.697018],[-91.123928,40.669152],[-91.185428,40.638071],[-91.253074,40.637962],[-91.306524,40.626231],[-91.339719,40.613488],[-91.359873,40.601805],[-91.379752,40.57445],[-91.401482,40.559458],[-91.406373,40.551831],[-91.404125,40.539127],[-91.384531,40.530948],[-91.369059,40.512532],[-91.364211,40.500043],[-91.364915,40.484168],[-91.381769,40.442555],[-91.372554,40.4012],[-91.381958,40.387632],[-91.419422,40.378264],[-91.441243,40.386255],[-91.452458,40.375501],[-91.463895,40.375659],[-91.465116,40.385257],[-91.484507,40.3839],[-91.490977,40.393484],[-91.487829,40.403866],[-91.498093,40.401926],[-91.522333,40.409648],[-91.527057,40.416689],[-91.519012,40.431298],[-91.529132,40.434272],[-91.533548,40.440804],[-91.523271,40.450061],[-91.526155,40.458625],[-91.552691,40.458769],[-91.574746,40.465664],[-91.590817,40.492292],[-91.621353,40.510072],[-91.618028,40.53403],[-91.6219,40.542292],[-91.6887,40.55739],[-91.691557,40.564867],[-91.686357,40.580875],[-91.716769,40.59853],[-91.729115,40.61364],[-92.686693,40.589809],[-94.294813,40.571341],[-94.632032,40.571186],[-95.765645,40.585208],[-95.753148,40.59284],[-95.748626,40.603355],[-95.768926,40.621264],[-95.776251,40.647463],[-95.795489,40.662384],[-95.822913,40.66724],[-95.842801,40.677496],[-95.852615,40.702262],[-95.883178,40.717579],[-95.888907,40.731855],[-95.879027,40.753081],[-95.84662,40.768619],[-95.835232,40.779151],[-95.834523,40.787778],[-95.845342,40.811324],[-95.837186,40.835347],[-95.847084,40.854174],[-95.847785,40.864328],[-95.838735,40.872191],[-95.815933,40.879846],[-95.809474,40.891228],[-95.813458,40.901693],[-95.836438,40.921642],[-95.839743,40.93278],[-95.829074,40.975688],[-95.838908,40.986484],[-95.867286,41.001599],[-95.869486,41.009399],[-95.859918,41.025403],[-95.859654,41.035695],[-95.882415,41.060411],[-95.862587,41.088399],[-95.865888,41.117898],[-95.882088,41.143998],[-95.883489,41.154898],[-95.871912,41.168122],[-95.846188,41.166698],[-95.841288,41.174998],[-95.856788,41.187098],[-95.90969,41.184398],[-95.91829,41.186698],[-95.92599,41.195698],[-95.924891,41.211198],[-95.910891,41.231798],[-95.921891,41.264598],[-95.913991,41.271398],[-95.928691,41.281398],[-95.927491,41.298397],[-95.90589,41.300897],[-95.90429,41.293497],[-95.912491,41.279498],[-95.90249,41.273398],[-95.87689,41.285097],[-95.871489,41.295797],[-95.883089,41.316697],[-95.92569,41.322197],[-95.946891,41.334096],[-95.956691,41.345496],[-95.954891,41.351796],[-95.93549,41.360596],[-95.92879,41.370096],[-95.93689,41.396387],[-95.929721,41.411331],[-95.933169,41.42943],[-95.919865,41.447922],[-95.922529,41.455766],[-95.936801,41.46519],[-95.962329,41.46281],[-96.011757,41.476212],[-96.019542,41.486617],[-95.997903,41.504789],[-95.992599,41.514174],[-95.999529,41.538679],[-96.005079,41.544004],[-96.019686,41.545743],[-96.027289,41.541081],[-96.034305,41.512853],[-96.040701,41.507076],[-96.05369,41.508859],[-96.07307,41.525052],[-96.08822,41.530595],[-96.09409,41.539265],[-96.093613,41.558271],[-96.081152,41.577289],[-96.085771,41.585746],[-96.109387,41.596871],[-96.117558,41.609999],[-96.116233,41.621574],[-96.100701,41.635507],[-96.095046,41.647365],[-96.099837,41.66103],[-96.120983,41.677861],[-96.121401,41.688522],[-96.111968,41.697773],[-96.082429,41.698159],[-96.073063,41.705004],[-96.079682,41.717962],[-96.10261,41.728016],[-96.106425,41.73789],[-96.102772,41.746339],[-96.079915,41.757895],[-96.077543,41.777824],[-96.064537,41.793002],[-96.075548,41.807811],[-96.107592,41.820685],[-96.110246,41.84885],[-96.142045,41.868865],[-96.148826,41.888132],[-96.161756,41.90182],[-96.160767,41.908044],[-96.136743,41.920826],[-96.144583,41.941544],[-96.133318,41.955732],[-96.1289,41.969727],[-96.141228,41.978063],[-96.156538,41.980137],[-96.184243,41.976696],[-96.192141,41.984461],[-96.183568,41.999987],[-96.194556,42.008662],[-96.215225,42.006701],[-96.223896,41.995456],[-96.236487,41.996428],[-96.241932,42.006965],[-96.223611,42.022652],[-96.223822,42.033346],[-96.238392,42.041088],[-96.261132,42.038974],[-96.271427,42.044988],[-96.279342,42.07028],[-96.267636,42.096177],[-96.2689,42.11359],[-96.279203,42.12348],[-96.310085,42.132523],[-96.319528,42.146647],[-96.342395,42.160491],[-96.349688,42.172043],[-96.348066,42.194747],[-96.35987,42.210545],[-96.358141,42.214088],[-96.336323,42.218922],[-96.323723,42.229887],[-96.330004,42.240224],[-96.328905,42.254734],[-96.336003,42.264806],[-96.365792,42.285875],[-96.369212,42.308344],[-96.375307,42.318339],[-96.407998,42.337408],[-96.417786,42.351449],[-96.417093,42.361443],[-96.408436,42.376092],[-96.41498,42.393442],[-96.413609,42.407894],[-96.387608,42.432494],[-96.380707,42.446394],[-96.385407,42.473094],[-96.396107,42.484095],[-96.409408,42.487595],[-96.474409,42.491895],[-96.476909,42.497795],[-96.473339,42.503537],[-96.477454,42.509589],[-96.490089,42.512441],[-96.49297,42.517282],[-96.479909,42.524195],[-96.476952,42.556079],[-96.498041,42.558153],[-96.498709,42.57087],[-96.489328,42.5708],[-96.485796,42.575001],[-96.49545,42.579474],[-96.494777,42.585741],[-96.499885,42.588539],[-96.509468,42.61273],[-96.517048,42.615343],[-96.525671,42.609312],[-96.531604,42.615148],[-96.518542,42.62035],[-96.516338,42.630435],[-96.537881,42.646446],[-96.542366,42.660736],[-96.559281,42.657903],[-96.556461,42.663939],[-96.566684,42.675942],[-96.576381,42.671302],[-96.575299,42.682665],[-96.596405,42.688514],[-96.59908,42.697296],[-96.61017,42.694568],[-96.629625,42.705102],[-96.624446,42.714294],[-96.624704,42.725497],[-96.631931,42.725086],[-96.638621,42.734921],[-96.630485,42.750378],[-96.620548,42.753534],[-96.620272,42.757124],[-96.632212,42.761512],[-96.633168,42.768325],[-96.61949,42.784034],[-96.604559,42.783034],[-96.595283,42.792982],[-96.590757,42.808255],[-96.596008,42.815044],[-96.585699,42.818041],[-96.577937,42.827645],[-96.581604,42.837521],[-96.571353,42.837155],[-96.565605,42.830434],[-96.560572,42.839373],[-96.552092,42.836057],[-96.549513,42.839143],[-96.554709,42.846142],[-96.545502,42.849956],[-96.54146,42.857682],[-96.550439,42.863171],[-96.549659,42.870281],[-96.537851,42.878475],[-96.540396,42.888877],[-96.526563,42.893755],[-96.542847,42.903737],[-96.537354,42.908791],[-96.541689,42.922576],[-96.525536,42.935511],[-96.516203,42.933769],[-96.52012,42.938183],[-96.500308,42.959391],[-96.505028,42.970844],[-96.515922,42.972886],[-96.520773,42.980385],[-96.512237,42.985937],[-96.509986,42.995126],[-96.49782,42.998143],[-96.49167,43.009707],[-96.499187,43.019213],[-96.510995,43.024701],[-96.509146,43.03668],[-96.518431,43.042068],[-96.510256,43.049917],[-96.490365,43.050789],[-96.476905,43.062383],[-96.463094,43.062981],[-96.458201,43.067554],[-96.454188,43.083379],[-96.462636,43.089614],[-96.460516,43.09494],[-96.436589,43.120842],[-96.450361,43.142237],[-96.458854,43.143356],[-96.466537,43.150281],[-96.464896,43.182034],[-96.473834,43.189804],[-96.470781,43.205099],[-96.475571,43.221054],[-96.496454,43.223652],[-96.519273,43.21769],[-96.535741,43.22764],[-96.56044,43.224219],[-96.568505,43.231554],[-96.571194,43.238961],[-96.552963,43.247281],[-96.552591,43.257769],[-96.582904,43.26769],[-96.586317,43.274319],[-96.577588,43.2788],[-96.580346,43.298204],[-96.553087,43.29286],[-96.530392,43.300034],[-96.526004,43.309999],[-96.534913,43.336473],[-96.524289,43.347214],[-96.527345,43.368109],[-96.521323,43.374607],[-96.521572,43.38564],[-96.524044,43.394762],[-96.529152,43.397735],[-96.537116,43.395063],[-96.573579,43.419228],[-96.569628,43.427527],[-96.575181,43.431756],[-96.592905,43.43317],[-96.602608,43.449649],[-96.600039,43.45708],[-96.584603,43.46961],[-96.586364,43.478251],[-96.580997,43.481384],[-96.590452,43.494298],[-96.598396,43.495074],[-96.598929,43.500441],[-91.217706,43.50055]]]},\"properties\":{\"name\":\"Iowa\",\"nation\":\"USA  \"}}]}","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}]}}
,{"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":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              -81.990966796875,\n              30.510216587229984\n            ],\n            [\n              -82.012939453125,\n              30.396568538569365\n            ],\n            [\n              -82.166748046875,\n              30.36813582872057\n            ],\n            [\n              -82.2216796875,\n              30.462879341709886\n            ],\n            [\n              -82.265625,\n              30.54806979910353\n            ],\n            [\n              -84.18823242187499,\n              30.68988785772121\n            ],\n            [\n              -84.67163085937499,\n              32.838058359277056\n            ],\n            [\n              -83.73779296875,\n              34.175453097578526\n            ],\n            [\n              -81.01318359375,\n              34.266296360583546\n            ],\n            [\n              -80.386962890625,\n              33.81110228864701\n            ],\n            [\n              -79.815673828125,\n              32.676372772089834\n            ],\n            [\n              -80.33203125,\n              32.43097672054704\n            ],\n            [\n              -80.44189453125,\n              32.324275588876525\n            ],\n            [\n              -80.518798828125,\n              32.2778445149827\n            ],\n            [\n              -80.6781005859375,\n              32.15236189465577\n            ],\n            [\n              -80.88134765625001,\n              31.91953017247695\n            ],\n            [\n              -81.14501953125,\n              31.62064369245056\n            ],\n            [\n              -81.23291015625,\n              31.367708915120826\n            ],\n            [\n              -81.309814453125,\n              31.208103321325254\n            ],\n            [\n              -81.39770507812499,\n              31.08586989620833\n            ],\n            [\n              -81.419677734375,\n              30.850363469502337\n            ],\n            [\n              -81.39770507812499,\n              30.68988785772121\n            ],\n            [\n              -81.507568359375,\n              30.670990790779168\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a3e4b07f02db49641a","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":281798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leeth, David C. cleeth@usgs.gov","contributorId":1403,"corporation":false,"usgs":true,"family":"Leeth","given":"David","email":"cleeth@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":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 Center","active":true,"usgs":true}],"preferred":true,"id":281800,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Labowski, James L.","contributorId":87631,"corporation":false,"usgs":true,"family":"Labowski","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":281802,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
]}