Director, South Atlantic Water Science Center
U.S. Geological Survey
720 Gracern Road
Columbia, SC 29210
No abstract available.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa732","contributors":{"authors":[{"text":"White, R.K.","contributorId":96338,"corporation":false,"usgs":true,"family":"White","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":252483,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, E.D.","contributorId":83993,"corporation":false,"usgs":true,"family":"Powell","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":252482,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Francisco, P.","contributorId":101321,"corporation":false,"usgs":true,"family":"Francisco","given":"P.","email":"","affiliations":[],"preferred":false,"id":252484,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":45048,"text":"wri014073 - 2001 - An alternative regionalization scheme for defining nutrient criteria for rivers and streams","interactions":[],"lastModifiedDate":"2018-02-06T12:32:25","indexId":"wri014073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4073","title":"An alternative regionalization scheme for defining nutrient criteria for rivers and streams","docAbstract":"To protect and manage rivers and streams (hereafter, collectively referred to as streams) in the United States, the U.S. Environmental Protection Agency (USEPA) is establishing regionally based nutrient criteria that reflect the natural variability in water quality. As a basic approach to establish these criteria, the USEPA has divided the country into nutrient ecoregions (delineated on the basis of natural and anthropogenic factors) to minimize variability within regions and maximize variability among regions. The USEPA has allowed states and tribes flexibility to modify or improve on this basic approach. As part of activities of a Regional Technical Assistance Group, whose role it is to examine and refine this basic approach, an alternative regionalization scheme was developed for the Upper Midwest. In this refined approach, the relative importance of various environmental characteristics affecting nutrient concentrations are determined by use of regression-tree analysis. The area is then subdivided into relatively homogeneous areas called “environmental nutrient zones” on the basis of distributions of only the most statistically significant environmental characteristics.
\nOn the basis of data from 234 sites, the most statistically significant environmental characteristics affecting nutrient concentrations were the percentage of agriculture (or absence of forest) and factors describing the climate and geology in the watershed. Environmental nutrient zones were then delineated that incorporated distributions in land use (similar to the ecoregion approach) and also delineated with land-use information excluded so the criteria should reflect only the naturally occurring variability in water quality. With the environmental nutrient zone stratification scheme, the variability in total phosphorus concentrations among zones was reduced by approximately 50 percent compared to that among nutrient ecoregions, whereas the variability in total nitrogen concentrations was reduced only slightly. Frequency distributions of data from each zone were then used to define the potential water quality of each zone.
\nThe environmental nutrient zone approach can be applied to specific states or nutrient ecoregions and used to develop criteria as a function of stream type. This approach can also be applied on the basis of environmental characteristics of the watershed alone rather than the general environmental characteristics from the region in which the site is located. The environmental nutrient zone approach will enable states to refine the basic nutrient criteria established by the USEPA by developing attainable criteria given the environmental characteristics where the streams are located.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri014073","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency, Regions V and VII","usgsCitation":"Robertson, D.M., Saad, D.A., and Wieben, A.M., 2001, An alternative regionalization scheme for defining nutrient criteria for rivers and streams: U.S. Geological Survey Water-Resources Investigations Report 2001-4073, v, 57 p., https://doi.org/10.3133/wri014073.","productDescription":"v, 57 p.","numberOfPages":"63","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":310676,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://wi.water.usgs.gov/pubs/wrir-01-4073/wrir-01-4073.pdf"},{"id":170878,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3906,"rank":3,"type":{"id":15,"text":"Index 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The data for northeast Florida include continuous or daily discharge for 145 streams, periodic discharge for 3 streams, continuous or daily stage for 21 streams, periodic stage for 0 streams; peak stage and discharge for 0 streams; continuous or daily elevations for 12 lakes, periodic elevations for 18 lakes; continuous ground water levels for 42 wells, periodic ground water levels for 404 wells; quality-of-water data for 31 surface-water sites and 62 wells.
These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, State and Federal agencies in Florida.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbae2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532228,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54477,"text":"wdrFL001A - 2001 - Water resources data, Florida water year 2000. Volume 1A. Northeast Florida surface water","interactions":[],"lastModifiedDate":"2022-12-07T17:31:17.23253","indexId":"wdrFL001A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"FL-00-1A","title":"Water resources data, Florida water year 2000. Volume 1A. Northeast Florida surface water","docAbstract":"The Water Resources Division of the U.S. Geological Survey, in cooperation with State agencies, obtains a large amount of data pertaining to the water resources of Florida each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled \"Water Resources Data - Florida.\"
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL001A","collaboration":"Prepared in cooperation with the State of Florida and with other agencies or cooperators","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2001, Water resources data, Florida water year 2000. Volume 1A. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbad9","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532227,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44875,"text":"wri20014180 - 2001 - Simulated Effects of Alternative Pumping Strategies on Ground-Water-Flow Patterns and Areas Contributing Recharge to Selected Wells near Kenvil, Morris County, New Jersey","interactions":[],"lastModifiedDate":"2012-03-08T17:16:14","indexId":"wri20014180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4180","title":"Simulated Effects of Alternative Pumping Strategies on Ground-Water-Flow Patterns and Areas Contributing Recharge to Selected Wells near Kenvil, Morris County, New Jersey","docAbstract":"Ground-water-flow patterns and areas contributing recharge to supply wells change in response to new or altered pumping stresses. An understanding of these potential changes is essential for the effective evaluation of possible future water-supply alternatives, especially if the supply wells may be vulnerable to contamination from the land surface. Demand for water from a valley-fill and carbonate-rock aquifer system in the study area near Kenvil in Morris County, New Jersey, is expected to increase as the population of communities grows in and near the area. As withdrawals increase and new supplies are developed over time, ground-water-flow patterns and areas contributing recharge to supply wells in the area are expected to change. \r\n\r\nFlow patterns and areas contributing recharge to selected supply wells in the aquifer system in the study area, under a variety of hypothetical withdrawal conditions, were evaluated by use of numerical modeling techniques. Under the four alternative scenarios evaluated, withdrawals from selected wells are increased by a total of 1.3 to 2.4 million gallons per day, or 32 to 56 percent over the recent (1991-95) total withdrawals from the study area. The scenarios were incorporated in simulations of ground-water flow that were conducted by use of a previously developed three-dimensional numerical model. \r\n\r\nFlow-path comparisons indicate that ground-water-flow patterns change in response to changes in pumping rates and (or) new pumping stresses. Under the scenarios represented in the simulations, water levels (hydraulic heads) in the study area decline from 0 to as much as 63 ft. Under most of the scenarios evaluated, downward leakage of ground water increases and upward discharge to streams decreases. In some scenarios, supply wells intercept additional local flow, whereas in other scenarios additional regional flow is intercepted. Areas contributing recharge to wells also change or develop. Changes in flow patterns and in the location, size, and shape of areas contributing recharge to supply wells depend on the location and magnitude of the change in withdrawal stress and on other hydrogeologic factors, such as the configuration of aquifer boundaries and differences in aquifer properties.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri20014180","collaboration":"Prepared in cooperation with the Morris County Municipal Utilities Authority","usgsCitation":"Spitz, F.J., and Nicholson, R.S., 2001, Simulated Effects of Alternative Pumping Strategies on Ground-Water-Flow Patterns and Areas Contributing Recharge to Selected Wells near Kenvil, Morris County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 2001-4180, iii, 32 p., https://doi.org/10.3133/wri20014180.","productDescription":"iii, 32 p.","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":134765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11706,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri01-4180/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.91666666666667,40.666666666666664 ], [ -74.91666666666667,41 ], [ -74.5,41 ], [ -74.5,40.666666666666664 ], [ -74.91666666666667,40.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49b8e4b07f02db5ccd39","contributors":{"authors":[{"text":"Spitz, Frederick J. 0000-0002-1391-2127 fspitz@usgs.gov","orcid":"https://orcid.org/0000-0002-1391-2127","contributorId":2777,"corporation":false,"usgs":true,"family":"Spitz","given":"Frederick","email":"fspitz@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":230595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nicholson, Robert S. rnichol@usgs.gov","contributorId":2283,"corporation":false,"usgs":true,"family":"Nicholson","given":"Robert","email":"rnichol@usgs.gov","middleInitial":"S.","affiliations":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230594,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44906,"text":"wri014036 - 2001 - Aquifer-characteristics data for West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"wri014036","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4036","title":"Aquifer-characteristics data for West Virginia","docAbstract":"Specific-capacity, storage-coefficient, and specific-yield data for wells in West Virginia were compiled to provide a data set from which transmissivity could be estimated. This data can be used for analytical and mathematical groundwater flow modeling. Analysis of available storage-coefficient and (or) specific-yield data indicates the Ohio River alluvial aquifer has a median specific yield of 0.20, which is characteristic of an unconfined aquifer. The Kanawha River alluvial aquifer has a median specific yield of 0.003, which is characteristic of a semi-confined aquifer. The median storage coefficient of fractured-bedrock aquifers is only 0.007, which is characteristic of confined aquifers. \r\n\r\nThe highest median transmissivity of a specific aquifer in West Virginia occurs in Ohio River alluvium (4,800 ft2/d); the second highest occurs in Kanawha River alluvium (1,600 ft2/d). The lowest median transmissivity (23 ft2/d) is for the McKenzie-Rose Hill-Tuscarora aquifer. Rocks of Cambrian age within the Waynesboro-Tomstown-Harpers-Weverton-Loudon aquifer had a low median transmissivity of only 67 ft2/d. Other aquifers with low transmissivities include the Hampshire Formation, Brallier-Harrell Formations, Mahantango Formations, Oriskany Sandstone, and the Conococheague Formation with median transmissivities of 74, 72, 92, 82, and 92 ft2/d, respectively. All other aquifers within the State had intermediate values of transmissivity (130-920 ft2/d). The highest median transmissivities among bedrock aquifers were those for aquifers within the Pennsylvanian age Pocahontas Formation (1,200 ft2/d) and Pottsville Group (1,300 ft2/d), and the Mississippian age Mauch Chunk Group (1,300 ft2/d). These rocks crop out primarily in the southern part of the State and to a lesser extent within the Valley and Ridge Physiographic Province in West Virginia's Eastern Panhandle. \r\n\r\nThe highest mean annual ground-water recharge rates within West Virginia (24.6 in.) occur within a band that extends through the central part of the State within the eastern part of the Kanawha River Basin. This area of relatively high relief has peaks higher than 4,000 ft and precipitation greater than 50 in./yr. The band of high recharge rates extends northward towards Pennsylvania and includes the Monongahela River Basin, which has a mean annual recharge of 21.4 inches. \r\n\r\nTo the west of this central band lies a region of lower relief with much lower mean annual precipitation rates. Mean annual recharge for the Tug Fork, Twelvepole Creek, and Guyandotte River Basins is only 12.6 inches. For the western part of the Kanawha River Basin, mean recharge is 11.9 inches. The lowest mean annual recharge rates (8.4 in.) within the State occur in the Little Kanawha River Basin and the tributary streams in the region that discharge directly to the Ohio River. \r\n\r\nWest Virginia's Eastern Panhandle is an area characterized by long linear northeast to southwest trending ridges and valleys. The mean annual ground-water recharge rate for this region, which is drained almost entirely by the Potomac River and its tributaries, is 9.4 inches. This area, which is located within a rain shadow resulting from orographic lifting in the higher altitude area to the west, receives less precipitation (approximately 30 in.) than the region to the west.","language":"ENGLISH","doi":"10.3133/wri014036","usgsCitation":"Kozar, M.D., and Mathes, M.V., 2001, Aquifer-characteristics data for West Virginia: U.S. Geological Survey Water-Resources Investigations Report 2001-4036, iv, 74 p. : maps (some col.) ; 28 cm., https://doi.org/10.3133/wri014036.","productDescription":"iv, 74 p. : maps (some col.) ; 28 cm.","costCenters":[],"links":[{"id":3789,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri014036/","linkFileType":{"id":5,"text":"html"}},{"id":162165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47c6e4b07f02db4aa494","contributors":{"authors":[{"text":"Kozar, Mark D. 0000-0001-7755-7657 mdkozar@usgs.gov","orcid":"https://orcid.org/0000-0001-7755-7657","contributorId":1963,"corporation":false,"usgs":true,"family":"Kozar","given":"Mark","email":"mdkozar@usgs.gov","middleInitial":"D.","affiliations":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"preferred":true,"id":230657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mathes, Melvin V.","contributorId":77571,"corporation":false,"usgs":true,"family":"Mathes","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":230658,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":54482,"text":"wdrFL003B - 2001 - Water resources data, Florida, water year 2000; Volume 3B. Southwest Florida ground water","interactions":[],"lastModifiedDate":"2023-01-23T21:17:55.48689","indexId":"wdrFL003B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"FL-00-3B","title":"Water resources data, Florida, water year 2000; Volume 3B. Southwest Florida ground water","docAbstract":"The Water Resources Division of the U.S. Geological Survey, in cooperation with local, State, and Federal agencies, obtains a large amount of data pertaining to the water resources of Florida each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled \"Water Resources Data - Florida.\"
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL003B","collaboration":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Coffin, J., and Fletcher, W., 2001, Water resources data, Florida, water year 2000; Volume 3B. Southwest Florida ground water: U.S. Geological Survey Water Data Report FL-00-3B, viii, 189 p., https://doi.org/10.3133/wdrFL003B.","productDescription":"viii, 189 p.","costCenters":[],"links":[{"id":177124,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2000/fl-00-3-b/report-thumb.jpg"},{"id":412238,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2000/fl-00-3-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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To prepare your own maps or artwork based on maps, you can order separate black-and-white film positives or negatives for any color printed on a USGS topographic map, or for one or more of the groups of related features printed in the same color on the map (such as drainage and drainage names from the blue plate.)\r\n\r\nIn this document, examples are shown with appropriate ink color to illustrate the various separates. When purchased, separates are black-and-white film negatives or positives.\r\n\r\nAfter you receive a film separate or composite from the USGS, you can crop, enlarge or reduce, and edit to add or remove details to suit your special needs.\r\n\r\nFor example, you can adapt the separates for making regional and local planning maps or for doing many kinds of studies or promotions by using the features you select and then printing them in colors of your choice.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs04201","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2001, Map Separates: U.S. Geological Survey Fact Sheet 042-01, 3 p., https://doi.org/10.3133/fs04201.","productDescription":"3 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":175939,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0042/report-thumb.jpg"},{"id":86283,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0042/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64af76","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532041,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32689,"text":"fs04001 - 2001 - Monitoring Of Ecosystem Dynamics In The Mojave Desert: The Beatley Permanent Plots","interactions":[],"lastModifiedDate":"2012-02-02T00:09:16","indexId":"fs04001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"040-01","title":"Monitoring Of Ecosystem Dynamics In The Mojave Desert: The Beatley Permanent Plots","language":"ENGLISH","doi":"10.3133/fs04001","usgsCitation":"Webb, R., Esque, T., Medica, P.A., DeFalco, L., and Murov, M.B., 2001, Monitoring Of Ecosystem Dynamics In The Mojave Desert: The Beatley Permanent Plots: U.S. Geological Survey Fact Sheet 040-01, NA, https://doi.org/10.3133/fs04001.","productDescription":"NA","costCenters":[],"links":[{"id":121465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_040_01.jpg"},{"id":3265,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-040-01","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6991aa","contributors":{"authors":[{"text":"Webb, Robert H. rhwebb@usgs.gov","contributorId":1573,"corporation":false,"usgs":false,"family":"Webb","given":"Robert H.","email":"rhwebb@usgs.gov","affiliations":[{"id":12625,"text":"School of Natural Resources and the Environment, University of Arizona, Tucson, AZ, 85721, USA","active":true,"usgs":false}],"preferred":false,"id":208934,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Esque, Todd C. tesque@usgs.gov","contributorId":3221,"corporation":false,"usgs":true,"family":"Esque","given":"Todd C.","email":"tesque@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":208935,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Medica, Philip A.","contributorId":55780,"corporation":false,"usgs":true,"family":"Medica","given":"Philip","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":208937,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"DeFalco, Lesley A.","contributorId":42270,"corporation":false,"usgs":true,"family":"DeFalco","given":"Lesley A.","affiliations":[],"preferred":false,"id":208936,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murov, Marilyn B.","contributorId":92719,"corporation":false,"usgs":true,"family":"Murov","given":"Marilyn","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":208938,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":32688,"text":"fs01901 - 2001 - Monitoring of coarse sediment inputs to the Colorado River In Grand Canyon","interactions":[],"lastModifiedDate":"2020-12-03T13:12:31.172113","indexId":"fs01901","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"019-01","displayTitle":"Monitoring Of Coarse Sediment Inputs To The Colorado River In Grand Canyon","title":"Monitoring of coarse sediment inputs to the Colorado River In Grand Canyon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs01901","usgsCitation":"Webb, R., and Griffiths, P.G., 2001, Monitoring of coarse sediment inputs to the Colorado River In Grand Canyon: U.S. Geological Survey Fact Sheet 019-01, 4 p., https://doi.org/10.3133/fs01901.","productDescription":"4 p.","costCenters":[{"id":49157,"text":"Rocky Mountain Regional Office","active":true,"usgs":true}],"links":[{"id":120183,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_019_01.jpg"},{"id":3264,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-019-01/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona","otherGeospatial":"Colorado River, Grand Canyon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.01611328125,\n 35.68407153314097\n ],\n [\n -111.192626953125,\n 35.68407153314097\n ],\n [\n -111.192626953125,\n 36.958671131530316\n ],\n [\n -114.01611328125,\n 36.958671131530316\n ],\n [\n -114.01611328125,\n 35.68407153314097\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6991e5","contributors":{"authors":[{"text":"Webb, Robert H. rhwebb@usgs.gov","contributorId":1573,"corporation":false,"usgs":false,"family":"Webb","given":"Robert H.","email":"rhwebb@usgs.gov","affiliations":[{"id":12625,"text":"School of Natural Resources and the Environment, University of Arizona, Tucson, AZ, 85721, USA","active":true,"usgs":false}],"preferred":false,"id":208933,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griffiths, Peter G. 0000-0002-8663-8907 pggriffi@usgs.gov","orcid":"https://orcid.org/0000-0002-8663-8907","contributorId":187,"corporation":false,"usgs":true,"family":"Griffiths","given":"Peter","email":"pggriffi@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":208932,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44587,"text":"wri004234 - 2001 - Sedimentation survey of Lago Dos Bocas, Puerto Rico, October 1999","interactions":[],"lastModifiedDate":"2012-02-02T00:10:30","indexId":"wri004234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4234","title":"Sedimentation survey of Lago Dos Bocas, Puerto Rico, October 1999","language":"ENGLISH","doi":"10.3133/wri004234","usgsCitation":"Soler-Lopez, L.R., 2001, Sedimentation survey of Lago Dos Bocas, Puerto Rico, October 1999: U.S. Geological Survey Water-Resources Investigations Report 2000-4234, v, 19 p. : ill., maps ; 28 cm., https://doi.org/10.3133/wri004234.","productDescription":"v, 19 p. : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":99300,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2000/4234/report.pdf","size":"1671","linkFileType":{"id":1,"text":"pdf"}},{"id":99301,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/2000/4234/plate-1.pdf","size":"538","linkFileType":{"id":1,"text":"pdf"}},{"id":172350,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2000/4234/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbbfb","contributors":{"authors":[{"text":"Soler-Lopez, Luis R.","contributorId":27501,"corporation":false,"usgs":true,"family":"Soler-Lopez","given":"Luis","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":230046,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55083,"text":"wdrWI001 - 2001 - Water Resources Data, Wisconsin, Water Year 2000","interactions":[],"lastModifiedDate":"2012-02-02T00:11:52","indexId":"wdrWI001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"WI-00-1","title":"Water Resources Data, Wisconsin, Water Year 2000","language":"ENGLISH","doi":"10.3133/wdrWI001","usgsCitation":"Garn, H., Olson, D., and Ellefson, B., 2001, Water Resources Data, Wisconsin, Water Year 2000: U.S. Geological Survey Water Data Report WI-00-1, 586 p., https://doi.org/10.3133/wdrWI001.","productDescription":"586 p.","numberOfPages":"586","costCenters":[],"links":[{"id":174188,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2000/wi-00-1/report-thumb.jpg"},{"id":87915,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2000/wi-00-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa6f4","contributors":{"authors":[{"text":"Garn, H.S.","contributorId":42601,"corporation":false,"usgs":true,"family":"Garn","given":"H.S.","affiliations":[],"preferred":false,"id":252611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, D.L.","contributorId":34943,"corporation":false,"usgs":true,"family":"Olson","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":252610,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellefson, B.R.","contributorId":83927,"corporation":false,"usgs":true,"family":"Ellefson","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":252612,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":32692,"text":"fs12201 - 2001 - Water Supply in the Mojave River Ground-Water Basin, 1931-99, and the Benefits of Artificial Recharge","interactions":[],"lastModifiedDate":"2012-02-02T00:09:16","indexId":"fs12201","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"122-01","title":"Water Supply in the Mojave River Ground-Water Basin, 1931-99, and the Benefits of Artificial Recharge","docAbstract":"The Mojave River and the associated aquifer system are important water supplies in the Mojave Desert of southern California. The river and aquifer system are in hydraulic connection in many areas, and when flow conditions change in one, the other usually is affected. The river is an unpredictable source of water; therefore, residents of the basin rely almost entirely on ground water for their water supply. This reliance on ground water has resulted in overdraft conditions that have caused water-level declines, changes in the quantity and spatial distribution of recharge from the Mojave River, and loss of riparian habitat. The U.S. Geological Survey (USGS), in cooperation with the Mojave Water Agency (MWA), has completed several studies to determine the likely effects of overdraft on the ground-water and surface-water relations along the Mojave River. This report summarizes those studies, highlighting some of the simulation results from a ground-water flow model, and describes the ground-water and surface-water conditions of the Mojave River Basin.","language":"ENGLISH","doi":"10.3133/fs12201","usgsCitation":"Stamos, C., Nishikawa, T., and Martin, P., 2001, Water Supply in the Mojave River Ground-Water Basin, 1931-99, and the Benefits of Artificial Recharge: U.S. Geological Survey Fact Sheet 122-01, NA, https://doi.org/10.3133/fs12201.","productDescription":"NA","costCenters":[],"links":[{"id":124567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_122_01.jpg"},{"id":3268,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/fs-122-01/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49a0e4b07f02db5bdba4","contributors":{"authors":[{"text":"Stamos, Christina L. 0000-0002-1007-9352","orcid":"https://orcid.org/0000-0002-1007-9352","contributorId":19593,"corporation":false,"usgs":true,"family":"Stamos","given":"Christina L.","affiliations":[],"preferred":false,"id":208945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nishikawa, Tracy 0000-0002-7348-3838 tnish@usgs.gov","orcid":"https://orcid.org/0000-0002-7348-3838","contributorId":1515,"corporation":false,"usgs":true,"family":"Nishikawa","given":"Tracy","email":"tnish@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":208944,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Martin, Peter pmmartin@usgs.gov","contributorId":799,"corporation":false,"usgs":true,"family":"Martin","given":"Peter","email":"pmmartin@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":208943,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":45054,"text":"wri004151 - 2001 - Methodology and Estimates of Scour at Selected Bridge Sites in Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:48","indexId":"wri004151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4151","title":"Methodology and Estimates of Scour at Selected Bridge Sites in Alaska","docAbstract":"The U.S. Geological Survey estimated scour depths at 325 bridges in Alaska as part of a cooperative agreement with the Alaska Department of Transportation and Public Facilities. The department selected these sites from approximately 806 State-owned bridges as potentially susceptible to scour during extreme floods. Pier scour and contraction scour were computed for the selected bridges by using methods recommended by the Federal Highway Administration. The U.S. Geological Survey used a four-step procedure to estimate scour: (1) Compute magnitudes of the 100- and 500-year floods. (2) Determine cross-section geometry and hydraulic properties for each bridge site. (3) Compute the water-surface profile for the 100- and 500-year floods. (4) Compute contraction and pier scour. This procedure is unique because the cross sections were developed from existing data on file to make a quantitative estimate of scour. This screening method has the advantage of providing scour depths and bed elevations for comparison with bridge-foundation elevations without the time and expense of a field survey. Four examples of bridge-scour analyses are summarized in the appendix.","language":"ENGLISH","doi":"10.3133/wri004151","usgsCitation":"Heinrichs, T.A., Kennedy, B., Langley, D.E., and Burrows, R.L., 2001, Methodology and Estimates of Scour at Selected Bridge Sites in Alaska: U.S. Geological Survey Water-Resources Investigations Report 2000-4151, iii, 44 p. : ill., map ; 28 cm. , https://doi.org/10.3133/wri004151.","productDescription":"iii, 44 p. : ill., map ; 28 cm. ","costCenters":[],"links":[{"id":171743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3909,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri004151","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629f86","contributors":{"authors":[{"text":"Heinrichs, Thomas A.","contributorId":93509,"corporation":false,"usgs":true,"family":"Heinrichs","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":231007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, Ben W.","contributorId":104519,"corporation":false,"usgs":true,"family":"Kennedy","given":"Ben W.","affiliations":[],"preferred":false,"id":231008,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langley, Dustin E.","contributorId":91904,"corporation":false,"usgs":true,"family":"Langley","given":"Dustin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":231006,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burrows, Robert L.","contributorId":79473,"corporation":false,"usgs":true,"family":"Burrows","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":231005,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":26484,"text":"wri004284 - 2001 - Selected data from field studies of pesticide runoff to surface waters","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri004284","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4284","title":"Selected data from field studies of pesticide runoff to surface waters","docAbstract":"Citations from the scientific literature for studies that quantified selected pesticides in field runoff or streams were obtained from two computerized bibliographic databases: Chemical Abstracts and AGRICOLA. Selected data were extracted from studies in field environments that lasted longer than a day and are summarized here. The data extracted from each article, if available, include pesticide information, environmental setting, year of study, and the mass of the pesticide in runoff as a percent of the mass applied. Data from two national studies of pesticides in surface waters done by the U.S. Geological Survey (National Water-Quality Assessment Program, 1992?1995, and National Stream-Quality Accounting Network, 1996-1998) also are summarized.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri004284","usgsCitation":"Capel, P.D., Winterstein, T.A., and Larson, S., 2001, Selected data from field studies of pesticide runoff to surface waters: U.S. Geological Survey Water-Resources Investigations Report 2000-4284, v, 70 p. ;28 cm., https://doi.org/10.3133/wri004284.","productDescription":"v, 70 p. ;28 cm.","costCenters":[],"links":[{"id":95603,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2000/4284/report.pdf","size":"4986","linkFileType":{"id":1,"text":"pdf"}},{"id":158050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2000/4284/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa601","contributors":{"authors":[{"text":"Capel, Paul D. 0000-0003-1620-5185 capel@usgs.gov","orcid":"https://orcid.org/0000-0003-1620-5185","contributorId":1002,"corporation":false,"usgs":true,"family":"Capel","given":"Paul","email":"capel@usgs.gov","middleInitial":"D.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":196467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winterstein, Thomas A.","contributorId":25971,"corporation":false,"usgs":true,"family":"Winterstein","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196468,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larson, Steven J.","contributorId":29845,"corporation":false,"usgs":true,"family":"Larson","given":"Steven J.","affiliations":[],"preferred":false,"id":196469,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":29797,"text":"wri004077 - 2001 - Ground-water flow in the shallow aquifer system at the Naval Weapons Station Yorktown, Virginia","interactions":[],"lastModifiedDate":"2014-04-10T08:21:25","indexId":"wri004077","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2000-4077","title":"Ground-water flow in the shallow aquifer system at the Naval Weapons Station Yorktown, Virginia","docAbstract":"The Environmental Directorate of the Naval Weapons Station Yorktown, Virginia, is concerned about possible contamination of ground water at the Station. Ground water at the Station flows through a shallow system of layered aquifers and leaky confining units. The units of the shallow aquifer system are the Columbia aquifer, the Cornwallis Cave confining unit, the Cornwallis Cave aquifer, the Yorktown confining unit, and the Yorktown-Eastover aquifer. The Eastover-Calvert confining unit separates the shallow aquifer system from deeper confined aquifers beneath the Station.
\n
\n
A three-dimensional, finite-difference, ground-water flow model was used to simulate steady-state ground-water flow of the shallow aquifer system in and around the Station. The model simulated ground-water flow from the peninsular drainage divide that runs across the Lackey Plain near the southern end of the Station north to King Creek and the York River and south to Skiffes Creek and the James River. The model was calibrated by minimizing the root mean square error between 4 7 measured and corresponding simulated water levels. The calibrated model was used to determine the ground-water budget and general directions of ground-water flow. A particle-tracking routine was used with the calibrated model to estimate groundwater flow paths, flow rates, and traveltimes from selected sites at the Station.
\nSimulated ground-water flow velocities of the Station-area model were small beneath the interstream areas of the Lackey Plain and Croaker Flat, but increased outward toward the streams and rivers where the hydraulic gradients are larger. If contaminants from the land surface entered the water table at or near the interstream areas of the Station, where hydraulic gradients are smaller, they would migrate more slowly than if they entered closer to the streams or the shores of the rivers where gradients commonly are larger.
\nThe ground-water flow simulations indicate that some ground water leaks downward from the water table to the Yorktown confining unit and, where the confining unit is absent, to the Yorktown-Eastover aquifer. The velocities of advective-driven contaminants would decrease considerably when entering the Yorktown confining unit because the hydraulic conductivity of the confining unit is small compared to that of the aquifers.
\nAny contaminants that moved with advective ground-water flow near the groundwater divide of the Lackey Plain would move relatively slowly because the hydraulic gradients are small there. The direction in which the contaminants would move, however, would be determined by precisely where the contaminants entered the water table. The model was not designed to accurately simulate ground-water flow paths through local karst features.
\nBeneath Croaker Flat, ground water flows downward through the Columbia aquifer and the Yorktown confining unit into the Yorktown-Eastover aquifer. Analyses of the movement of simulated particles from two adjacent sites at Croaker Flat indicated that ground-water flow paths were similar at first but diverged and discharged to different tributaries of Indian Field Creek or to the York River. These simulations indicate that complex and possibly divergent flow paths and traveltimes are possible at the Station. Although the Station-area model is not detailed enough to simulate ground-water flow at the scales commonly used to track and remediate contaminants at specific sites, general concepts about possible contaminant migration at the Station can be inferred from the simulations.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Richmond, VA","doi":"10.3133/wri004077","collaboration":"Prepared in cooperation with the Environmental Directorate, Naval Weapons Station Yorktown","usgsCitation":"Smith, B.S., 2001, Ground-water flow in the shallow aquifer system at the Naval Weapons Station Yorktown, Virginia: U.S. Geological Survey Water-Resources Investigations Report 2000-4077, iv, 33 p., https://doi.org/10.3133/wri004077.","productDescription":"iv, 33 p.","numberOfPages":"38","costCenters":[],"links":[{"id":286097,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2000/4077/report-thumb.jpg"},{"id":286096,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2000/4077/report.pdf"}],"country":"United States","state":"Virginia","city":"Yorktown","otherGeospatial":"Columbia Aquifer;Cornwallis Cave;Croaker Flat;Lackey Plain;Yorktown-eastover Aquifer","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.799712,37.083759 ], [ -76.799712,37.322371 ], [ -76.447786,37.322371 ], [ -76.447786,37.083759 ], [ -76.799712,37.083759 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669173","contributors":{"authors":[{"text":"Smith, Barry S.","contributorId":21532,"corporation":false,"usgs":true,"family":"Smith","given":"Barry","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":202142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32694,"text":"fs12401 - 2001 - Pesticides in Ground Water - Big Horn County, Wyoming, 1999-2000","interactions":[],"lastModifiedDate":"2012-02-02T00:09:16","indexId":"fs12401","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"124-01","title":"Pesticides in Ground Water - Big Horn County, Wyoming, 1999-2000","language":"ENGLISH","doi":"10.3133/fs12401","usgsCitation":"Eddy-Miller, C.A., and Norris, J.R., 2001, Pesticides in Ground Water - Big Horn County, Wyoming, 1999-2000: U.S. Geological Survey Fact Sheet 124-01, NA, https://doi.org/10.3133/fs12401.","productDescription":"NA","costCenters":[],"links":[{"id":120186,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_124_01.jpg"},{"id":3270,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/fs12401/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6882f2","contributors":{"authors":[{"text":"Eddy-Miller, Cheryl A. (Prepared by)","contributorId":79524,"corporation":false,"usgs":true,"family":"Eddy-Miller","given":"Cheryl","suffix":"(Prepared by)","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":208949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norris, Jodi R.","contributorId":43746,"corporation":false,"usgs":true,"family":"Norris","given":"Jodi","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":208948,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42407,"text":"ofr01226 - 2001 - Reconnaissance geologic map of the Dixonville 7.5' quadrangle, Oregon","interactions":[],"lastModifiedDate":"2023-06-27T13:52:57.216332","indexId":"ofr01226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2001","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":"2001-226","title":"Reconnaissance geologic map of the Dixonville 7.5' quadrangle, Oregon","docAbstract":"The Dixonville 7.5 minute quadrangle is situated near the edge of two major geologic and tectonic provinces the northernmost Klamath Mountains and the southeastern part of the Oregon Coast Ranges (Figure 1). Rocks of the Klamath Mountains province that lie within the study area include ultramafic, mafic, intermediate and siliceous igneous types (Diller, 1898, Ramp, 1972, Ryberg, 1984). Similar rock associations that lie to the southwest yield Late Jurassic and earliest Cretaceous radiometric ages (Dott, 1965, Saleeby, et al., 1982, Hotz, 1971, Harper and Wright, 1984). These rocks, which are part of the Western Klamath terrane (Western Jurassic belt of (Irwin, 1964), are considered to have formed within an extensive volcanic arc and rifted arc complex (Harper and Wright, 1984) that lay along western North America during the Late Jurassic (Garcia, 1979, Garcia, 1982, Saleeby, et al., 1982, Ryberg, 1984). Imbricate thrust faulting and collapse of the arc during the Nevadan orogeny, which ranged in age between about 150 to 145 Ma in the Klamath region (Coleman, 1972, Saleeby, et al., 1982, Harper and Wright, 1984) was syntectonic with, or closely followed by deposition of the volcano-lithic clastic rocks of the Myrtle Group. The Myrtle Group consists of Upper Jurassic and Lower to middle Cretaceous turbidity and mass flow deposits considered to be either arc basin and/or post-orogenic flysh basins that were syntectonic with the waning phases of arc collapse (Imlay et al., 1959, Ryberg, 1984, Garcia, 1982, Roure.and Blanchet, 1983). The intermediate and mafic igneous rocks of the Rogue arc and the pre-Nevadan sedimentary cover (the Galice Formation, (Garcia, 1979) are intruded by siliceous and intermediate plutonic rocks principally of quartz diorite and granodiorite composition (Dott, 1965, Saleeby, et al., 1982, Garcia, 1982, Harper and Wright, 1984). The plutonic rocks are locally tectonized into amphibolite, gneiss, banded gneiss and augen gneiss. Similar metamorphic rocks have yielded metamorphic ages of 165 to 150 Ma (Coleman, 1972, Hotz, 1971, Saleeby, et al., 1982, Coleman and Lanphere, 1991).
\nThe Jurassic arc rocks and sedimentary cover occur as a tectonic outlier in this region (Figure 2) as they are bound to the northwest and southeast by melange, broken formation and semi-schists of the Dothan Formation and Dothan Formation(?) that are considered part of a late Mesozoic accretion complex (Ramp, 1972, Blake, et al., 1985). The plutonism that accompanied arc formation and tectonic collapse of the arc does not intrude the structurally underlying Dothan Formation, indicating major fault displacements since the Early Cretaceous. Semischistose and schistose rocks of the accretion complex have yielded metamorphic ages of around 125-140 Ma where they have been studied to the southwest (Coleman and Lanphere, 1971, Dott, 1965, Coleman, 1972). These rocks were unroofed and unconformably overlain by marine deposits by late early Eocene time (Baldwin, 1974).
\nThe early Tertiary history of this region is controversial. The most recent interpretation is that during the Paleocene and early Eocene the convergent margin was undergoing transtension or forearc extension as suggested by the voluminous extrusion of pillow basalt and related dike complexes (Wells, et al., 1984, Snavely, 1987). This episode was followed shortly by thrust and strike-slip faulting in the late early Eocene (Ryberg, 1984).
\nDuring the Eocene, the Mesozoic convergent margin association of arc, clastic basin, and accretion complex was partly unroofed and faulted against early Cenozoic rocks of the Oregon Coast Ranges (Ramp, 1972, Baldwin, 1974, Champ, 1969, Ryberg, 1984). Faults that are typical of this period of deformation include high-angle reverse faults with a very strong component of strike-slip displacement characterized by a low-angle rake of striae. Thrust and oblique-slip faults are ubiquitous in early Tertiary rocks to the northwest (Ryberg, 1984, Niem and Niem, 1990).
\nThe late Mesozoic and early Cenozoic arc and forearc rocks are unconformably overlain to the east by the late Eocene and younger, mainly continental fluvial deposits and pyroclastic flows of the Cascade arc (Peck, et al., 1964, Baldwin, 1974, Walker and MacLeod, 1991). Minor fossiliferous shallow marine sandstone is locally present. The volcanic sequence consists of a homoclinal section of about 1 to 2 kilometers of andesitic to rhyolitic flows and ash flow tuff. The section is gently east-tilted and is slightly disrupted by NE trending faults with apparent normal separation.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01226","usgsCitation":"Jayko, A.S., Wells, R., Givler, R.W., Fenton, J., and Sinor, M., 2001, Reconnaissance geologic map of the Dixonville 7.5' quadrangle, Oregon: U.S. Geological Survey Open-File Report 2001-226, Map: 48.0 x 36.0 inches; Readme; Metadata: PDF; Metadata: TXT; Pamphlet: PDF, 10 p.; Pamphlet: TXT; Dataset; Map for plotting, https://doi.org/10.3133/ofr01226.","productDescription":"Map: 48.0 x 36.0 inches; Readme; Metadata: PDF; Metadata: TXT; Pamphlet: PDF, 10 p.; Pamphlet: TXT; Dataset; Map for plotting","numberOfPages":"10","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":135308,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110198,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_42120.htm","linkFileType":{"id":5,"text":"html"},"description":"42120"},{"id":3685,"rank":8,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0226/","linkFileType":{"id":5,"text":"html"}},{"id":282593,"rank":7,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2001/0226/pdf/readme.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":282592,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2001/0226/pdf/01-226m.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":282595,"rank":5,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2001/0226/pdf/metadata.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":282594,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0226/pdf/geol.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":282596,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0226/ofr01226md.tar.gz","linkFileType":{"id":6,"text":"zip"}},{"id":282597,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0226/ofr01226ps.tar.gz","linkFileType":{"id":6,"text":"zip"}}],"scale":"24000","projection":"Universal Transverse Mercator projection","datum":"National Geodetic Datum of 1929","country":"United States","state":"Oregon","otherGeospatial":"Klamath Mountains,Oregon Coast Ranges","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.25,43.125 ], [ -123.25,43.25 ], [ -123.125,43.25 ], [ -123.125,43.125 ], [ -123.25,43.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a72e4b07f02db642aeb","contributors":{"authors":[{"text":"Jayko, Angela S. 0000-0002-7378-0330 ajayko@usgs.gov","orcid":"https://orcid.org/0000-0002-7378-0330","contributorId":2531,"corporation":false,"usgs":true,"family":"Jayko","given":"Angela","email":"ajayko@usgs.gov","middleInitial":"S.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":226423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, Ray E. 0000-0002-7796-0160 rwells@usgs.gov","orcid":"https://orcid.org/0000-0002-7796-0160","contributorId":2692,"corporation":false,"usgs":true,"family":"Wells","given":"Ray E.","email":"rwells@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":226424,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Givler, R. 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Emergency management and defense operations rely on this information. Private industry, nongovernmental organizations, and individual citizens use the same geographic data. Geographic information underpins an increasingly large part of the Nation's economy.\r\n\r\nAvailable geographic data often have the following problems:\r\n* They do not align with each other because layers are frequently created or revised separately,\r\n* They do not match across administrative boundaries because each producing organization uses different methods and standards, and\r\n* They are not up to date because of the complexity and cost of revision.\r\n\r\n\r\nThe U.S. Geological Survey (USGS) is developing The National Map to be a seamless, continuously maintained, and nationally consistent set of online, public domain, geographic base information to address these issues. The National Map will serve as a foundation for integrating, sharing, and using other data easily and consistently.\r\n\r\n\r\nIn collaboration with other government agencies, the private sector, academia, and volunteer groups, the USGS will coordinate, integrate, and, where needed, produce and maintain base geographic data.\r\n\r\n\r\nThe National Map will include digital orthorectified imagery; elevation data; vector data for hydrography, transportation, boundary, and structure features; geographic names; and land cover information. The data will be the source of revised paper topographic maps.\r\n\r\n\r\nMany technical and institutional issues must be resolved as The National Map is implemented. To begin the refinement of this new paradigm, pilot projects are being designed to identify and investigate these issues. The pilots are the foundation upon which future partnerships for data sharing and maintenance will be built.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","publisherLocation":"Reston, VA","doi":"10.3133/fs11601","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2001, The National Map - Delaware Pilot Project: U.S. Geological Survey Fact Sheet 116-01, 2 p., https://doi.org/10.3133/fs11601.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":160526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2001/0116/report-thumb.jpg"},{"id":59489,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2001/0116/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b0a8","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}