{"pageNumber":"3042","pageRowStart":"76025","pageSize":"25","recordCount":184769,"records":[{"id":45002,"text":"wri20024005 - 2002 - Streamflow and Suspended-Sediment Loads Before, During, and After H-3 Highway Construction, North Halawa, Haiku, South Fork Kapunahala, and Kamooalii Drainage Basins, Oahu, Hawaii, 1983-99","interactions":[],"lastModifiedDate":"2012-03-08T17:16:16","indexId":"wri20024005","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4005","title":"Streamflow and Suspended-Sediment Loads Before, During, and After H-3 Highway Construction, North Halawa, Haiku, South Fork Kapunahala, and Kamooalii Drainage Basins, Oahu, Hawaii, 1983-99","docAbstract":"A long-term study (1983?99) was conducted to determine the effects of the H-3 Highway construction on streamflow and suspended-sediment transport on Oahu, Hawaii. Data were collected at five streamflow-gaging stations before, during, and after construction and at two stream-gaging stations during and after construction. Drainage areas at the seven streamflow-gaging stations ranged from 0.40 to 4.01 mi2 and highway construction affected from 4 to 15 percent of these areas. Analysis of covariance and regression techniques were used to assess changes in streamflow and suspended-sediment loads during and after construction, relative to before-construction conditions.\r\n\r\nStreamflow at the seven streamflow-gaging stations was compared to streamflow at an index station unaffected by highway construction. Streamflow data were divided into low- and high-flow classes, and the two flow classes were analyzed separately. Additionally, instantaneous peak flows were analyzed at three streamflow-gaging stations. During construction, observed low flows significantly increased by 108 percent at Luluku Stream, a tributary to Kamooalii Stream, and decreased by 31 percent at Kamooalii Stream. After construction, low flows increased by 47 percent at North Halawa Stream near Honolulu compared to low flows during construction. Low flows at Luluku Stream increased by 99 percent after construction compared to before construction. Increased low flows were attributed to removal of vegetation for construction and the increase of impervious areas that reduced infiltration. Decreased low flows were attributed to increased ground-water withdrawals and construction activities.\r\n\r\nHigh flows observed during highway construction compared to before construction increased significantly only at Haiku Stream (by 25 percent). Observed high flows after construction compared to during construction increased significantly only at Kamooalii Stream (by 34 percent). Observed high flows after construction compared to before construction increased by 58 percent only at Luluku Stream. All increases in observed high flows are attributed to increased runoff from land-use changes caused by the highway construction. Instantaneous peak flows increased significantly at Luluku Stream. Luluku Stream had significant increases in low and high flows both during and after construction.\r\n\r\nSuspended-sediment loads changed significantly at six out of seven sediment-gaging stations during highway construction. Construction activities increased observed suspended-sediment yields by 222, 426, 60, and 148 percent at North Halawa Stream near Kaneohe, North Halawa Stream near Honolulu, Right Branch Kamooalii Stream, and Haiku Stream, respectively. At Luluku Stream, observed suspended-sediment yields were lower during construction than before construction by 62 percent. After construction, suspended-sediment loads also changed significantly at six out of seven stream-gaging stations. Observed after-construction yields increased at North Halawa Stream near Kaneohe, North Halawa Stream near Honolulu, and Right Branch Kamooalii Stream by 49, 205, and 36 percent, respectively, and decreased at Kamooalii Stream and South Fork Kapunahala Stream by 62 and 71 percent. The observed increases in yields are smaller after construction than during construction indicating that suspended-sediment loads are likely returning to before-construction levels.\r\n\r\nThe effects of H-3 Highway construction on suspended-sediment loads were generally similar to studies of the effects of highway construction in other areas of the United States where 50 to 85 percent of the sediment loads were attributed to construction activities. The percentages of the observed yields attributable to H-3 Highway construction are similar to the above percentages, ranging from 37 to 81 percent. Decreases in suspended-sediment loads due to highway construction are unique and have not been widely reported in the literature. Where decrease in s","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri20024005","collaboration":"Prepared in cooperation with the State of Hawaii Department of Transportation and the Federal Highway Administration","usgsCitation":"Wong, M.F., and Yeatts, D.S., 2002, Streamflow and Suspended-Sediment Loads Before, During, and After H-3 Highway Construction, North Halawa, Haiku, South Fork Kapunahala, and Kamooalii Drainage Basins, Oahu, Hawaii, 1983-99: U.S. Geological Survey Water-Resources Investigations Report 2002-4005, v, 49 p., https://doi.org/10.3133/wri20024005.","productDescription":"v, 49 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1983-01-01","temporalEnd":"1999-12-31","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":122050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_2002_4005.jpg"},{"id":13774,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri02-4005/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -157.96666666666667,21.333333333333332 ], [ -157.96666666666667,21.466666666666665 ], [ -157.73333333333332,21.466666666666665 ], [ -157.73333333333332,21.333333333333332 ], [ -157.96666666666667,21.333333333333332 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4f3f","contributors":{"authors":[{"text":"Wong, Michael F.","contributorId":43815,"corporation":false,"usgs":true,"family":"Wong","given":"Michael","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":230892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yeatts, Daniel S.","contributorId":22015,"corporation":false,"usgs":true,"family":"Yeatts","given":"Daniel","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":230891,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44897,"text":"wri20014247 - 2002 - Flood of September 22, 1998, in Arecibo and Utuado, Puerto Rico","interactions":[],"lastModifiedDate":"2012-03-08T17:16:16","indexId":"wri20014247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2001-4247","title":"Flood of September 22, 1998, in Arecibo and Utuado, Puerto Rico","docAbstract":"Hurricane Georges made landfall on the southeastern part of Puerto Rico during September 21, 1998. Georges, with maximum sustained winds of 185 kilometers per hour and gusts to 240 kilometers per hour, produced 24-hour total rainfall amounts of 770 millimeters on the island's mountainous interior. Severe flooding affected almost half of the island's 78 municipios during September 21-22, 1998. The most affected municipios were Adjuntas, Aguada, Aguadilla, A?asco, Arecibo, Cayey, Ciales, Comerio, Barceloneta, Dorado, Jayuya, Manati, Mayaguez, Morovis, Orocovis, Patillas, Toa Alta, Toa Baja, and Utuado. The combination of strong winds, intense rainfall and severe flooding caused widespread property damages. More than 20,000 houses were destroyed and more than 100,000 houses sustained damage. Floodwaters and landslides destroyed or damaged many bridges and roads throughout the island.\r\n\r\nRecords indicate that Hurricane Georges induced flood discharges in the Rio Grande de Arecibo Basin that were the largest on record. Floodwaters inundated urban and rural areas, affecting urban subdivisions, businesses, vehicles, bridges, roads, and high-tension electric power lines. To define the extent and depth of inundation, more than 280 high-water marks were identified and surveyed in Arecibo and Utuado. In addition estimates of flood magnitude and frequency were made at selected gaging stations, and flood profiles were developed for certain stream reaches. Flooding was most severe in the towns of Arecibo and Utuado. In Arecibo, the most affected communities were the rural area of San Francisco, the urban subdivisions of Martell, Nolla, and Arecibo Gardens, and the low-lying areas of downtown Arecibo. In these areas, the water depths ranged from 0.6 to 1.8 meters. In Utuado, floodwaters from the Rio Vivi and the Rio Grande de Arecibo inundated the downtown area affecting homes, public facilities, and businesses. In the urban subdivision of Jesus Maria Lago, the depth of flooding exceeded 2.5 meters. Frequency analysis indicates that flood-peak discharges equaled or exceeded the 100-year recurrence interval at five streamflow-gaging stations in the Rio Grande de Arecibo Basin.\r\n","language":"ENGLISH","doi":"10.3133/wri20014247","collaboration":"In cooperation with the\r\nPUERTO RICO AQUEDUCT AND SEWER AUTHORITY","usgsCitation":"Torres-Sierra, H., 2002, Flood of September 22, 1998, in Arecibo and Utuado, Puerto Rico: U.S. Geological Survey Water-Resources Investigations Report 2001-4247, v, 23 p. : ill., maps ; 28 cm., https://doi.org/10.3133/wri20014247.","productDescription":"v, 23 p. : ill., maps ; 28 cm.","temporalStart":"1998-09-21","temporalEnd":"1998-09-22","costCenters":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"links":[{"id":170478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9216,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri01-4247/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -67.25,17.5 ], [ -67.25,18.5 ], [ -64.5,18.5 ], [ -64.5,17.5 ], [ -67.25,17.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e7049","contributors":{"authors":[{"text":"Torres-Sierra, Heriberto","contributorId":97913,"corporation":false,"usgs":true,"family":"Torres-Sierra","given":"Heriberto","email":"","affiliations":[],"preferred":false,"id":230639,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50595,"text":"ofr024 - 2002 - Chemical contaminants to Tampa Bay","interactions":[],"lastModifiedDate":"2012-02-02T00:11:17","indexId":"ofr024","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4","title":"Chemical contaminants to Tampa Bay","language":"ENGLISH","doi":"10.3133/ofr024","usgsCitation":"Fernandez, M., 2002, Chemical contaminants to Tampa Bay: U.S. Geological Survey Open-File Report 2002-4, poster, 36 by 58 inches or 11 by 17 inces, https://doi.org/10.3133/ofr024.","productDescription":"poster, 36 by 58 inches or 11 by 17 inces","costCenters":[],"links":[{"id":176161,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4395,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://gulfsci.usgs.gov/tampabay/reports/fernandz/pdf_fern.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3b9c","contributors":{"authors":[{"text":"Fernandez, Mario Jr.","contributorId":77155,"corporation":false,"usgs":true,"family":"Fernandez","given":"Mario","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":241914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53428,"text":"wri024231 - 2002 - SUTRA: A model for 2D or 3D saturated-unsaturated, variable-density ground-water flow with solute or energy transport","interactions":[],"lastModifiedDate":"2020-02-16T11:34:13","indexId":"wri024231","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4231","title":"SUTRA: A model for 2D or 3D saturated-unsaturated, variable-density ground-water flow with solute or energy transport","docAbstract":"SUTRA (Saturated-Unsaturated Transport) is a computer program that simulates fluid movement and the transport of either energy or dissolved substances in a subsurface environment. This upgraded version of SUTRA adds the capability for three-dimensional simulation to the former code (Voss, 1984), which allowed only two-dimensional simulation. The code employs a two- or three-dimensional finite-element and finite-difference method to approximate the governing equations that describe the two interdependent processes that are simulated: \r\n1) fluid density-dependent saturated or unsaturated ground-water flow; and \r\n2) either \r\n\r\n(a) transport of a solute in the ground water, in which the solute may be subject to: equilibrium adsorption on the porous matrix, and both first-order and zero-order production or decay; or \r\n(b) transport of thermal energy in the ground water and solid matrix of the aquifer. \r\nSUTRA may also be used to simulate simpler subsets of the above processes. A flow-direction-dependent dispersion process for anisotropic media is also provided by the code and is introduced in this report. As the primary calculated result, SUTRA provides fluid pressures and either solute concentrations or temperatures, as they vary with time, everywhere in the simulated subsurface system. \r\nSUTRA flow simulation may be employed for two-dimensional (2D) areal, cross sectional and three-dimensional (3D) modeling of saturated ground-water flow systems, and for cross sectional and 3D modeling of unsaturated zone flow. Solute-transport simulation using SUTRA may be employed to model natural or man-induced chemical-species transport including processes of solute sorption, production, and decay. For example, it may be applied to analyze ground-water contaminant transport problems and aquifer restoration designs. In addition, solute-transport simulation with SUTRA may be used for modeling of variable-density leachate movement, and for cross sectional modeling of saltwater intrusion in aquifers at near-well or regional scales, with either dispersed or relatively sharp transition zones between freshwater and saltwater. SUTRA energy-transport simulation may be employed to model thermal regimes in aquifers, subsurface heat conduction, aquifer thermal-energy storage systems, geothermal reservoirs, thermal pollution of aquifers, and natural hydrogeologic convection systems. \r\nMesh construction, which is quite flexible for arbitrary geometries, employs quadrilateral finite elements in 2D Cartesian or radial-cylindrical coordinate systems, and hexahedral finite elements in 3D systems. 3D meshes are currently restricted to be logically rectangular; in other words, they are similar to deformable finite-difference-style grids. Permeabilities may be anisotropic and may vary in both direction and magnitude throughout the system, as may most other aquifer and fluid properties. Boundary conditions, sources and sinks may be time dependent. A number of input data checks are made to verify the input data set. An option is available for storing intermediate results and restarting a simulation at the intermediate time. Output options include fluid velocities, fluid mass and solute mass or energy budgets, and time-varying observations at points in the system. Both the mathematical basis for SUTRA and the program structure are highly general, and are modularized to allow for straightforward addition of new methods or processes to the simulation. The FORTRAN-90 coding stresses clarity and modularity rather than efficiency, providing easy access for later modifications.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024231","usgsCitation":"Voss, C.I., and Provost, A., 2002, SUTRA: A model for 2D or 3D saturated-unsaturated, variable-density ground-water flow with solute or energy transport (Version 2D3D.1): U.S. Geological Survey Water-Resources Investigations Report 2002-4231, 250 p., https://doi.org/10.3133/wri024231.","productDescription":"250 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":182213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5211,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/nrp/gwsoftware/sutra/sutra.html","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 2D3D.1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c9f0","contributors":{"authors":[{"text":"Voss, Clifford I. 0000-0001-5923-2752 cvoss@usgs.gov","orcid":"https://orcid.org/0000-0001-5923-2752","contributorId":1559,"corporation":false,"usgs":true,"family":"Voss","given":"Clifford","email":"cvoss@usgs.gov","middleInitial":"I.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":247570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Provost, A.M.","contributorId":16098,"corporation":false,"usgs":true,"family":"Provost","given":"A.M.","affiliations":[],"preferred":false,"id":247571,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":54396,"text":"wdrAZ011 - 2002 - Water resources data, Arizona, water year 2001","interactions":[],"lastModifiedDate":"2023-02-13T17:25:21.831151","indexId":"wdrAZ011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"AZ-01-1","title":"Water resources data, Arizona, water year 2001","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey (USGS), in cooperation with State agencies, obtains a large amount of data on the water resources of Arizona each water year. These data, accumulated during many water years, constitute a valuable database for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the USGS, the data are published annually in a report series entitled \"Water Resources Data for Arizona.\"</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAZ011","collaboration":"Prepared in cooperation with the State of Arizona and with other agencies","usgsCitation":"McCormack, H., Fisk, G., Duet, N., Evans, D., and Castillo, N., 2002, Water resources data, Arizona, water year 2001: U.S. Geological Survey Water Data Report AZ-01-1, xxiii, 399 p., https://doi.org/10.3133/wdrAZ011.","productDescription":"xxiii, 399 p.","costCenters":[],"links":[{"id":174900,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/2001/az-01-1/report-thumb.jpg"},{"id":413004,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/2001/az-01-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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D.W.","contributorId":37807,"corporation":false,"usgs":true,"family":"Evans","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":250194,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Castillo, N.K.","contributorId":97184,"corporation":false,"usgs":true,"family":"Castillo","given":"N.K.","email":"","affiliations":[],"preferred":false,"id":250198,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":58011,"text":"ofr02226 - 2002 - Travel times and dispersion of soluble dye in thirteen New Hampshire rivers","interactions":[],"lastModifiedDate":"2022-05-05T16:16:24.193895","indexId":"ofr02226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-226","title":"Travel times and dispersion of soluble dye in thirteen New Hampshire rivers","docAbstract":"<p>Dye was injected and traced in 13 New Hampshire rivers in 2000 to determine the velocity at which a soluble substance spilled into the river would travel to drinking-water supply intakes. Travel times were studied on the Ammonoosuc, Androscoggin, Connecticut, Contoocook, East Branch Pemigewasset, Exeter, Lamprey, Mascoma, Merrimack, Oyster, Piscassic, Salmon Falls, and Sugar Rivers. Dye was injected and sampled at low and mean flows, and the measured velocities extrapolated to provide an estimate of the velocity during a mean annual flood (mean of yearly peak flows for a specific river). Rivers were sampled downstream of the dye-injection sites to measure dye concentrations and the arrival and passage times of the dye cloud. This information was used to estimate a relation between river discharge and the expected dye concentrations and velocities for each river. Results of the dye tests were used to estimate a 6-hour travel distance at mean annual flood for each of the 13 rivers, and to create graphical relations that can be used to estimate the travel times and concentrations of solutes over a range of river discharges and distances. Observed transport velocities ranged from 0.03 to 2.4 feet per second, and the estimated 6-hour travel distances ranged from 5.8 to 43 miles. Rivers in upland areas had the highest velocities, whereas rivers in the low coastal region had the slowest velocities.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02226","collaboration":"In cooperation with the New Hampshire Department of Environmental Services","usgsCitation":"Smith, T.E., 2002, Travel times and dispersion of soluble dye in thirteen New Hampshire rivers: U.S. Geological Survey Open-File Report 2002-226, v, 66 p., https://doi.org/10.3133/ofr02226.","productDescription":"v, 66 p.","costCenters":[],"links":[{"id":400218,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0226/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0226/report-thumb.jpg"}],"country":"United States","state":"New 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,{"id":69615,"text":"i2758 - 2002 - Crystal Coast North Carolina, Satellite Image Map","interactions":[],"lastModifiedDate":"2012-02-10T00:11:23","indexId":"i2758","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2758","title":"Crystal Coast North Carolina, Satellite Image Map","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/i2758","isbn":"0607985615","usgsCitation":"Thomas, J.M., and Feistner, K., 2002, Crystal Coast North Carolina, Satellite Image Map: U.S. Geological Survey IMAP 2758, 1 Sheet: 49 x 38 inches, https://doi.org/10.3133/i2758.","productDescription":"1 Sheet: 49 x 38 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":187529,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256695,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2758/plate-1.pdf","size":"14433","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.36749999999999,34.5 ], [ -77.36749999999999,35.30083333333333 ], [ -76.25,35.30083333333333 ], [ -76.25,34.5 ], [ -77.36749999999999,34.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acde4b07f02db67edc1","contributors":{"authors":[{"text":"Thomas, Jean-Claude M.","contributorId":76828,"corporation":false,"usgs":true,"family":"Thomas","given":"Jean-Claude","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":280734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feistner, Kelly","contributorId":61903,"corporation":false,"usgs":true,"family":"Feistner","given":"Kelly","email":"","affiliations":[],"preferred":false,"id":280733,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69759,"text":"i2698C - 2002 - Sea-Floor Topography of Quadrangle 2 in the Great South Channel, Western Georges Bank","interactions":[],"lastModifiedDate":"2012-02-10T00:11:33","indexId":"i2698C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2698","subseriesTitle":"GIS","chapter":"C","title":"Sea-Floor Topography of Quadrangle 2 in the Great South Channel, Western Georges Bank","docAbstract":"The Great South Channel separates the western part of Georges Bank from Nantucket Shoals and is a major conduit for the exchange of water between the Gulf of Maine to the north and the Atlantic Ocean to the south. Water depths range mostly between 65 and 80 m in the region. A minimum depth of 45 m occurs in the east-central part of the mapped area, and a maximum depth of 100 m occurs in the northwest corner. The channel region is characterized by strong tidal and storm currents that flow dominantly north and south. Major topographic features of the seabed were formed by glacial and postglacial processes. Ice containing rock debris moved from north to south, sculpting the region into a broad shallow depression and depositing sediment to form the irregular depressions and low gravelly mounds and ridges that are visible in parts of the mapped area. Many other smaller glacial featuresprobably have been eroded by waves and currents at worksince the time when the region, formerly exposed bylowered sea level or occupied by ice, was invaded by the sea. The low, irregular and somewhat lumpy fabric formed by the glacial deposits is obscured in places by drifting sand and by the linear, sharp fabric formed by modern sand features. Today, sand transported by the strong north-south-flowing tidal and storm currents has formed large, east-west-trending dunes. These bedforms (ranging between 5 and 20 m in height) contrast strongly with, and partly mask, the subdued topography of the older glacial features.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Maps Showing Sea Floor Topography, Sun-Illuminated Sea Floor Topography, and Backscatter Intensity of Quadrangles 1 and 2 in the Great South Channel Region, Western Georges Bank","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/i2698C","isbn":"0607998253 ","collaboration":"Prepared in cooperation with the U.S. National Oceanic and Atmospheric Administration","usgsCitation":"Valentine, P.C., Malczyk, J.T., and Middleton, T.J., 2002, Sea-Floor Topography of Quadrangle 2 in the Great South Channel, Western Georges Bank (Version 1.0): U.S. Geological Survey IMAP 2698, 1 Sheet: 40 x 36 inches; Also available on CD-ROM, https://doi.org/10.3133/i2698C.","productDescription":"1 Sheet: 40 x 36 inches; Also available on CD-ROM","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":191098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9790,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2698/index.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"25000","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -69.05,41.016666666666666 ], [ -69.05,41.13333333333333 ], [ -68.78333333333333,41.13333333333333 ], [ -68.78333333333333,41.016666666666666 ], [ -69.05,41.016666666666666 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc670","contributors":{"authors":[{"text":"Valentine, Page C. 0000-0002-0485-6266 pvalentine@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-6266","contributorId":1947,"corporation":false,"usgs":true,"family":"Valentine","given":"Page","email":"pvalentine@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":281212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Malczyk, Jeremy T.","contributorId":10106,"corporation":false,"usgs":true,"family":"Malczyk","given":"Jeremy","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":281213,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Middleton, Tammie J.","contributorId":27532,"corporation":false,"usgs":true,"family":"Middleton","given":"Tammie","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":281214,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":69761,"text":"i2698A - 2002 - Sea-Floor Topography of Quadrangle 1 in the Great South Channel, Western Georges Bank","interactions":[],"lastModifiedDate":"2014-08-29T15:14:56","indexId":"i2698A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2698","subseriesTitle":"GIS","chapter":"A","title":"Sea-Floor Topography of Quadrangle 1 in the Great South Channel, Western Georges Bank","docAbstract":"The Great South Channel separates the western part of Georges Bank from Nantucket Shoals and is a major conduit for the exchange of water between the Gulf of Maine to the north and the Atlantic Ocean to the south. Water depths range mostly between 65 and 80 m in the region. A minimum depth of 45 m occurs in the east-central part of the mapped area, and a maximum depth of 100 m occurs in the northwest corner. The channel region is characterized by strong tidal and storm currents that flow dominantly north and south. Major topographic features of the seabed were formed by glacial and postglacial processes. Ice containing rock debris moved from north to south, sculpting the region into a broad shallow depression and depositing sediment to form the irregular depressions and low gravelly mounds and ridges that are visible in parts of the mapped area. Many other smaller glacial featuresprobably have been eroded by waves and currents at worksince the time when the region, formerly exposed bylowered sea level or occupied by ice, was invaded by the sea. The low, irregular and somewhat lumpy fabric formed by the glacial deposits is obscured in places by drifting sand and by the linear, sharp fabric formed by modern sand features. Today, sand transported by the strong north-south-flowing tidal and storm currents has formed large, east-west-trending dunes. These bedforms (ranging between 5 and 20 m in height) contrast strongly with, and partly mask, the subdued topography of the older glacial features.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Maps Showing Sea Floor Topography, Sun-Illuminated Sea Floor Topography, and Backscatter Intensity of Quadrangles 1 and 2 in the Great South Channel Region, Western Georges Bank","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/i2698A","isbn":"0607998253","collaboration":"Prepared in cooperation with the U.S. National Oceanic and Atmospheric Administration","usgsCitation":"Valentine, P.C., Middleton, T.J., and Malczyk, J.T., 2002, Sea-Floor Topography of Quadrangle 1 in the Great South Channel, Western Georges Bank (Version 1.0): U.S. Geological Survey IMAP 2698, 1 Sheet: 40 x 36 inches; Also available on CD-ROM, https://doi.org/10.3133/i2698A.","productDescription":"1 Sheet: 40 x 36 inches; Also available on CD-ROM","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":191634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9788,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2698/index.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"25000","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -69.05,40.9 ], [ -69.05,41.01667 ], [ -68.783333,41.01667 ], [ -68.783333,40.9 ], [ -69.05,40.9 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc56a","contributors":{"authors":[{"text":"Valentine, Page C. 0000-0002-0485-6266 pvalentine@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-6266","contributorId":1947,"corporation":false,"usgs":true,"family":"Valentine","given":"Page","email":"pvalentine@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":281218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Middleton, Tammie J.","contributorId":27532,"corporation":false,"usgs":true,"family":"Middleton","given":"Tammie","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":281220,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Malczyk, Jeremy T.","contributorId":10106,"corporation":false,"usgs":true,"family":"Malczyk","given":"Jeremy","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":281219,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":50654,"text":"ofr02241 - 2002 - Preliminary data used in estimating ground-water recharge, pumpage, and evapotranspiration in part of the Republican River Basin, Nebraska, Kansas, and Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:25","indexId":"ofr02241","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-241","title":"Preliminary data used in estimating ground-water recharge, pumpage, and evapotranspiration in part of the Republican River Basin, Nebraska, Kansas, and Colorado","language":"ENGLISH","doi":"10.3133/ofr02241","usgsCitation":"Johnson, M., and Landon, M.K., 2002, Preliminary data used in estimating ground-water recharge, pumpage, and evapotranspiration in part of the Republican River Basin, Nebraska, Kansas, and Colorado: U.S. Geological Survey Open-File Report 2002-241, 42 p. plus electronic files, https://doi.org/10.3133/ofr02241.","productDescription":"42 p. plus electronic files","costCenters":[],"links":[{"id":169894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c686","contributors":{"authors":[{"text":"Johnson, Michaela R. 0000-0001-6133-0247 mrjohns@usgs.gov","orcid":"https://orcid.org/0000-0001-6133-0247","contributorId":1013,"corporation":false,"usgs":true,"family":"Johnson","given":"Michaela R.","email":"mrjohns@usgs.gov","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":242013,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landon, Matthew K. 0000-0002-5766-0494 landon@usgs.gov","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":392,"corporation":false,"usgs":true,"family":"Landon","given":"Matthew","email":"landon@usgs.gov","middleInitial":"K.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":242012,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44610,"text":"wri024274 - 2002 - Preliminary assessment of using tree-tissue analysis and passive-diffusion samplers to evaluate trichloroethene contamination of ground water at Site SS-34N, McChord Air Force Base, Washington, 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:05","indexId":"wri024274","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4274","title":"Preliminary assessment of using tree-tissue analysis and passive-diffusion samplers to evaluate trichloroethene contamination of ground water at Site SS-34N, McChord Air Force Base, Washington, 2001","docAbstract":"Two low-cost innovative sampling procedures for characterizing trichloroethene (TCE) contamination in ground water were evaluated for use at McChord Air Force Base (AFB) by the U.S. Geological Survey, in cooperation with the U.S. Air Force McChord Air Force Base Installation Restoration Program, in 2001. Previous attempts to characterize the source of ground-water contamination in the heterogeneous glacial outwash aquifer at McChord site SS-34N using soil-gas surveys, direct-push exploration, and more than a dozen ground-water monitoring wells have had limited success. The procedures assessed in this study involved analysis of tree-tissue samples to map underlying ground-water contamination and deploying passive-diffusion samplers to measure TCE concentrations in existing monitoring wells. These procedures have been used successfully at other U.S. Department of Defense sites and have resulted in cost avoidance and accelerated site characterization. Despite the presence of TCE in ground water at site SS-34N, TCE was not detected in any of the 20 trees sampled at the site during either early spring or late summer sampling. The reason the tree tissue procedure was not successful at the McChord AFB site SS-34N may have been due to an inability of tree roots to extract moisture from a water table 30 feet below the land surface, or that concentrations of TCE in ground water were not large enough to be detectable in the tree tissue at the sampling point. Passive-diffusion samplers were placed near the top, middle, and bottom of screened intervals in three monitoring wells and TCE was observed in all samplers. Concentrations of TCE from the passive-diffusion samplers were generally similar to concentrations found in samples collected in the same wells using conventional pumping methods. In contrast to conventional pumping methods, the collection of ground-water samples using the passive-diffusion samples did not generate waste purge water that would require hazardous-waste disposal. In addition, the results from the passive-diffusion samples may show that TCE concentrations are stratified across some screened intervals. The overall results of the limited test of passive-diffusion samplers at site SS-34N were similar to more detailed tests conducted at other contaminated sites across the country and indicate that further evaluation of the use of passive-diffusion samplers at McChord site SS-34N is warranted.","language":"ENGLISH","doi":"10.3133/wri024274","usgsCitation":"Cox, S., 2002, Preliminary assessment of using tree-tissue analysis and passive-diffusion samplers to evaluate trichloroethene contamination of ground water at Site SS-34N, McChord Air Force Base, Washington, 2001: U.S. Geological Survey Water-Resources Investigations Report 2002-4274, 21 p., https://doi.org/10.3133/wri024274.","productDescription":"21 p.","costCenters":[],"links":[{"id":167972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3712,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024274/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9c5","contributors":{"authors":[{"text":"Cox, S.E.","contributorId":66663,"corporation":false,"usgs":true,"family":"Cox","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":230099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44598,"text":"wri024070 - 2002 - Relation between geomorphic stability and the density of large shrubs on the flood plain of the Clark Fork of the Columbia River in the Deer Lodge Valley, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:27","indexId":"wri024070","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4070","title":"Relation between geomorphic stability and the density of large shrubs on the flood plain of the Clark Fork of the Columbia River in the Deer Lodge Valley, Montana","language":"ENGLISH","doi":"10.3133/wri024070","usgsCitation":"Smith, J.D., and Griffin, E.R., 2002, Relation between geomorphic stability and the density of large shrubs on the flood plain of the Clark Fork of the Columbia River in the Deer Lodge Valley, Montana: U.S. Geological Survey Water-Resources Investigations Report 2002-4070, iv, 25 p. : ill. (some col.), map ; 28 cm., https://doi.org/10.3133/wri024070.","productDescription":"iv, 25 p. : ill. (some col.), map ; 28 cm.","costCenters":[],"links":[{"id":99309,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4070/report.pdf","size":"5662","linkFileType":{"id":1,"text":"pdf"}},{"id":173440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4070/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c328","contributors":{"authors":[{"text":"Smith, James Dungan","contributorId":47008,"corporation":false,"usgs":true,"family":"Smith","given":"James","email":"","middleInitial":"Dungan","affiliations":[],"preferred":false,"id":230070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griffin, Eleanor R. 0000-0001-6724-9853 egriffin@usgs.gov","orcid":"https://orcid.org/0000-0001-6724-9853","contributorId":1775,"corporation":false,"usgs":true,"family":"Griffin","given":"Eleanor","email":"egriffin@usgs.gov","middleInitial":"R.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":230069,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44600,"text":"wri024081 - 2002 - Simulation of ground-water flow in the Silurian-Devonian aquifer, Cedar Falls, Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:10:27","indexId":"wri024081","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-4081","title":"Simulation of ground-water flow in the Silurian-Devonian aquifer, Cedar Falls, Iowa","language":"ENGLISH","doi":"10.3133/wri024081","usgsCitation":"Turco, M.J., 2002, Simulation of ground-water flow in the Silurian-Devonian aquifer, Cedar Falls, Iowa: U.S. Geological Survey Water-Resources Investigations Report 2002-4081, iv, 33 p. : ill. (some col.), maps (some col.) ; 28 cm., https://doi.org/10.3133/wri024081.","productDescription":"iv, 33 p. : ill. (some col.), maps (some col.) ; 28 cm.","costCenters":[],"links":[{"id":99310,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4081/report.pdf","size":"6718","linkFileType":{"id":1,"text":"pdf"}},{"id":173546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4081/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2628","contributors":{"authors":[{"text":"Turco, Michael J. mjturco@usgs.gov","contributorId":1011,"corporation":false,"usgs":true,"family":"Turco","given":"Michael","email":"mjturco@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":230072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47803,"text":"fs12602 - 2002 - Born of fire - restoring sagebrush steppe","interactions":[],"lastModifiedDate":"2017-03-31T11:48:22","indexId":"fs12602","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"126-02","title":"Born of fire - restoring sagebrush steppe","docAbstract":"Fire is a natural feature of sagebrush grasslands in the Great Basin. The invasion of exotic annual grasses, such as Bromus tectorum (cheatgrass), has changed the environment in these ecosystems. Invasive annual grasses provide a dense and continuous source of fuel that extends the season for fires and increases the frequency of fires in the region. Frequent fires eventually eliminate the native sagebrush. These annual grasses also change soil nutrients, especially carbon and nitrogen, such that invasive annual grasses are favored over the native plants. The Forest and Rangeland Ecosystem Science Center of the U.S. Geological Survey (USGS) is studying how to reduce the problems caused by these invasive annual grasses and restore native sagebrush grasslands. The areas of research include understanding disturbance regimes, especially fire, discerning the role of nutrients in restoring native plants, determining the potential to restore forbs important for wildlife, and ascertaining the past and present use of native and nonnative plants in revegetation projects.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs12602","usgsCitation":"Pyke, D.A., 2002, Born of fire - restoring sagebrush steppe: U.S. Geological Survey Fact Sheet 126-02, 2 p., https://doi.org/10.3133/fs12602.","productDescription":"2 p.","onlineOnly":"Y","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":125708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0126/coverthb.jpg"},{"id":4015,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0126/fs12602.pdf","text":"Report","size":"665 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 126-02"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc6ba","contributors":{"authors":[{"text":"Pyke, David A. 0000-0002-4578-8335 david_a_pyke@usgs.gov","orcid":"https://orcid.org/0000-0002-4578-8335","contributorId":3118,"corporation":false,"usgs":true,"family":"Pyke","given":"David","email":"david_a_pyke@usgs.gov","middleInitial":"A.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":236271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47802,"text":"fs12502 - 2002 - Assessing rangelands","interactions":[],"lastModifiedDate":"2017-03-31T11:49:38","indexId":"fs12502","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"125-02","title":"Assessing rangelands","docAbstract":"It is important for land managers and technical assistance specialists to be able to assess the health of rangelands in order to know where to focus management efforts. The complexity of ecological processes, and the inherent expense of directly measuring site integrity, suggests a need for an evaluation process that focuses instead on biological and physical attributes.\r\n\r\nIn a collaborative effort, the USGS, ARS, BLM, and NRCS have jointly developed a system in which 17 indicators are used to gauge three attributes of rangeland health. A qualitative, observational procedure provides an assessment of the functional status of these indicators. This quick assessment technique, by providing an understanding about each attribute, helps interpret rangeland health.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs12502","usgsCitation":"Pyke, D.A., 2002, Assessing rangelands: U.S. Geological Survey Fact Sheet 125-02, 2 p., https://doi.org/10.3133/fs12502.","productDescription":"2 p.","onlineOnly":"Y","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":4014,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0125/fs12502.pdf","text":"Report","size":"692 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 125-02"},{"id":120206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0125/coverthb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672aa7","contributors":{"authors":[{"text":"Pyke, David A. 0000-0002-4578-8335 david_a_pyke@usgs.gov","orcid":"https://orcid.org/0000-0002-4578-8335","contributorId":3118,"corporation":false,"usgs":true,"family":"Pyke","given":"David","email":"david_a_pyke@usgs.gov","middleInitial":"A.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"preferred":true,"id":236270,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61527,"text":"mf2340 - 2002 - Geologic map of the Frisco quadrangle, Summit County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf2340","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2340","title":"Geologic map of the Frisco quadrangle, Summit County, Colorado","docAbstract":"     New 1:24,000-scale geologic mapping along the Interstate-70 urban corridor in western Colorado, in support of the USGS Central Region State/USGS Cooperative Geologic Mapping Project, is contributing to a more complete understanding of the stratigraphy, structure, tectonic evolution, and hazard potential of this rapidly developing region.  The 1:24,000-scale Frisco quadrangle is near the headwaters of the Blue River and straddles features of the Blue River graben (Kellogg, K.S., 1999, Neogene basins of the northern Rio Grande rift?partitioning and asymmetry inherited from Laramide and older uplifts: Tectonophysics, v. 305, p. 141-152.), part of the northernmost reaches of the Rio Grande rift, a major late Oligocene to recent zone of extension that extends from Colorado to Mexico.  The Williams Range thrust fault, the western structural margin of the Colorado Front Range, cuts the northeastern corner of the quadrangle.\r\n\r\n      The oldest rocks in the quadrangle underlie the Tenmile Range and include biotite-sillimanite schist and gneiss, amphibolite, and migmatite that are intruded by granite inferred to be part of the 1,667-1,750 Ma Routt Plutonic Suite (Tweto, Ogden, 1987, Rock units of the Precambrian- basement in Colorado: U.S. Geological Survey Professional Paper 1321-A, 54 p.).  The oldest sedimentary unit is the Pennsylvanian Maroon Formation, a sequence of red sandstone, conglomerate, and interbedded shale.  The thickest sequence of sedimentary rocks is Cretaceous in age and includes at least 500 m of the Upper Cretaceous Pierre Shale.  The sedimentary rocks are intruded by sills and dikes of dacite porphyry sills of Swan Mountain, dated at 44 Ma (Marvin, R.F., Mehnert, H.H., Naeser, C.W., and Zartman, R.E., 1989, U.S. Geological Survey radiometric ages, compilation ?C??Part five?Colorado, Montana, Utah, and Wyoming:  Isochron/West, no. 53, p. 14-19. Simmons, E.C., and Hedge, C.E., 1978, Minor-element and Sr-isotope geochemistry of Tertiary stocks, Colorado mineral belt:  Contributions to Mineralogy and Petrology, v. 67, p. 379-396.).  Surficial deposits include (1) an old, deeply dissected landslide deposit, possibly as old as Tertiary, on the south flank of Tenderfoot Mountain, (2) deeply weathered, very coarse gravel deposits, mostly along Gold Run and underlying Mesa Cortina; the gravels are gold bearing and were mined by hydraulic methods in the 1800's, (3) glacial deposits of both Bull Lake (middle Pleistocene) and Pinedale (late Pleistocene) that were derived from large valley glaciers that flowed down Tenmile and North Tenmile Creeks; the town of Frisco is underlain mostly by Pinedale-age glacial outwash, (4) recent landslide deposits, including one large (about 1 square kilometer) area just downslope from Lilly Pad Lake, west of I-70, and (5)extensive colluvial and alluvial deposits.\r\n\r\n      The latest seismic events appear to be middle Pliestocene in age and are associated with small scarps that cut Bull Lake till but do not cut Pinedale till.","language":"ENGLISH","doi":"10.3133/mf2340","usgsCitation":"Kellogg, K., Bartos, P.J., and Williams, C.L., 2002, Geologic map of the Frisco quadrangle, Summit County, Colorado (Version 1.0): U.S. Geological Survey Miscellaneous Field Studies Map 2340, 1 map : col. ; 58 x 45 cm., on sheet 85 x 88 cm. + 1 pamphlet (15 p. ; 28 cm.). , https://doi.org/10.3133/mf2340.","productDescription":"1 map : col. ; 58 x 45 cm., on sheet 85 x 88 cm. + 1 pamphlet (15 p. ; 28 cm.). ","costCenters":[],"links":[{"id":110389,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54462.htm","linkFileType":{"id":5,"text":"html"},"description":"54462"},{"id":182586,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6056,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2002/mf-2340/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.11749999999999,39.5 ], [ -106.11749999999999,39.6175 ], [ -106,39.6175 ], [ -106,39.5 ], [ -106.11749999999999,39.5 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697933","contributors":{"authors":[{"text":"Kellogg, Karl S.","contributorId":89896,"corporation":false,"usgs":true,"family":"Kellogg","given":"Karl S.","affiliations":[],"preferred":false,"id":265882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bartos, Paul J.","contributorId":49661,"corporation":false,"usgs":true,"family":"Bartos","given":"Paul","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":265880,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, Cindy L.","contributorId":75382,"corporation":false,"usgs":true,"family":"Williams","given":"Cindy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265881,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":54074,"text":"wdrCA024 - 2002 - Water Resources Data--California, Water Year 2002, Volume 4. Northern Central Valley Basins and The Great Basin from Honey Lake Basin to Oregon State Line","interactions":[],"lastModifiedDate":"2012-02-02T00:11:37","indexId":"wdrCA024","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"CA-02-4","title":"Water Resources Data--California, Water Year 2002, Volume 4. Northern Central Valley Basins and The Great Basin from Honey Lake Basin to Oregon State Line","docAbstract":"Water-resources data for the 2002 water year for California consist of records of stage, discharge, and water quality of streams, stage and contents in lakes and reservoirs, and water levels and water quality in wells. Volume 4 contains discharge records for 191 gaging stations, stage and contents for 60 lakes and reservoirs, gage-height records for 2 stations, and water quality for 21 stations. Also included are 4 miscellaneous partial-record sites. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"ENGLISH","doi":"10.3133/wdrCA024","usgsCitation":"Smithson, J., Friebel, M., Webster, M., and Rockwell, G., 2002, Water Resources Data--California, Water Year 2002, Volume 4. Northern Central Valley Basins and The Great Basin from Honey Lake Basin to Oregon State Line: U.S. Geological Survey Water Data Report CA-02-4, 494 p., https://doi.org/10.3133/wdrCA024.","productDescription":"494 p.","costCenters":[],"links":[{"id":177968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5515,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrca024/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9f1d","contributors":{"authors":[{"text":"Smithson, J.R.","contributorId":41073,"corporation":false,"usgs":true,"family":"Smithson","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":249132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friebel, M.F.","contributorId":23207,"corporation":false,"usgs":true,"family":"Friebel","given":"M.F.","email":"","affiliations":[],"preferred":false,"id":249131,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Webster, M.D.","contributorId":68385,"corporation":false,"usgs":true,"family":"Webster","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":249134,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rockwell, G.L.","contributorId":47408,"corporation":false,"usgs":true,"family":"Rockwell","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":249133,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50697,"text":"ofr02380 - 2002 - EMINERS -- An Economic Mineral Resource Simulator","interactions":[{"subject":{"id":50697,"text":"ofr02380 - 2002 - EMINERS -- An Economic Mineral Resource Simulator","indexId":"ofr02380","publicationYear":"2002","noYear":false,"title":"EMINERS -- An Economic Mineral Resource Simulator"},"predicate":"SUPERSEDED_BY","object":{"id":58155,"text":"ofr20041344 - 2012 - Version 3.0 of EMINERS - Economic Mineral Resource Simulator","indexId":"ofr20041344","publicationYear":"2012","noYear":false,"title":"Version 3.0 of EMINERS - Economic Mineral Resource Simulator"},"id":1}],"supersededBy":{"id":58155,"text":"ofr20041344 - 2012 - Version 3.0 of EMINERS - Economic Mineral Resource Simulator","indexId":"ofr20041344","publicationYear":"2012","noYear":false,"title":"Version 3.0 of EMINERS - Economic Mineral Resource Simulator"},"lastModifiedDate":"2012-02-02T00:11:22","indexId":"ofr02380","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"2002-380","title":"EMINERS -- An Economic Mineral Resource Simulator","language":"ENGLISH","doi":"10.3133/ofr02380","usgsCitation":"Duval, J.S., 2002, EMINERS -- An Economic Mineral Resource Simulator: U.S. Geological Survey Open-File Report 2002-380, program and documentation, https://doi.org/10.3133/ofr02380.","productDescription":"program and documentation","costCenters":[],"links":[{"id":178511,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4170,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-380/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c37f","contributors":{"authors":[{"text":"Duval, Joseph S.","contributorId":22314,"corporation":false,"usgs":true,"family":"Duval","given":"Joseph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":242098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53342,"text":"wdrFL013A - 2002 - Water Resources Data, Florida, Water Year 2001, Volume 3A. Southwest Florida Surface Water","interactions":[],"lastModifiedDate":"2012-02-02T00:11:39","indexId":"wdrFL013A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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-01-3A","title":"Water Resources Data, Florida, Water Year 2001, Volume 3A. Southwest Florida Surface Water","docAbstract":"Water resources data for the 2001 water year in Florida consist of continuous or daily discharges for 406 streams, periodic discharge for 12 streams, continuous daily stage for 142 streams, periodic stage for 12 streams, peak stage and discharge for 37 streams, continuous or daily elevations for 11 lakes, periodic elevations for 30 lakes; continuous ground-water levels for 424 wells, periodic ground-water levels for 1,426 wells, and quality-of-water data for 80 surface-water sites and 245 wells. \r\n\r\nThe data for Southwest Florida include records of stage, discharge, and water quality of streams; stage, contents, water quality of lakes and reservoirs, and water levels and water quality of ground-water wells. Volume 3A contains continuous or daily discharge for 83 streams, periodic discharge for 10 streams, continuous or daily stage for 43 streams, peak stage and discharge for 8 streams, continuous or daily elevations for 2 lakes, periodic elevations for 26 lakes, and quality-of-water data for 37 surface-water sites. \r\n\r\nThese data represent the national Water Data System records collected by the U.S. Geological Survey and cooperating local, state, and federal agencies in Florida.","language":"ENGLISH","doi":"10.3133/wdrFL013A","usgsCitation":"Stoker, Y., Kane, R., and Fletcher, W., 2002, Water Resources Data, Florida, Water Year 2001, Volume 3A. Southwest Florida Surface Water: U.S. Geological Survey Water Data Report FL-01-3A, 416 p., https://doi.org/10.3133/wdrFL013A.","productDescription":"416 p.","costCenters":[],"links":[{"id":5045,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrfl013A/","linkFileType":{"id":5,"text":"html"}},{"id":177566,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbc4a","contributors":{"authors":[{"text":"Stoker, Y.E.","contributorId":13253,"corporation":false,"usgs":true,"family":"Stoker","given":"Y.E.","email":"","affiliations":[],"preferred":false,"id":247314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kane, R.L.","contributorId":29873,"corporation":false,"usgs":true,"family":"Kane","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":247315,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fletcher, W.L.","contributorId":97977,"corporation":false,"usgs":true,"family":"Fletcher","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":247316,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53345,"text":"wdrFL013B - 2002 - Water Resources Data, Florida, Water Year 2001, Volume 3B. Southwest Florida Ground Water","interactions":[],"lastModifiedDate":"2012-02-02T00:11:25","indexId":"wdrFL013B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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-01-3B","title":"Water Resources Data, Florida, Water Year 2001, Volume 3B. Southwest Florida Ground Water","docAbstract":"Water resources data for the 2001 water year in Florida consist of continuous or daily discharges for 406 streams, periodic discharge for 12 streams, continuous daily stage for 142 streams, periodic stage for 12 streams, peak stage and discharge for 37 streams, continuous or daily elevations for 11 lakes, periodic elevations for 30 lakes; continuous ground-water levels for 424 wells, periodic ground-water levels for 1,426 wells, and quality-of-water data for 80 surface-water sites and 245 wells. \r\n\r\nThe data for Southwest Florida include records of stage, discharge, and water quality of streams; stage, contents, water quality of lakes and reservoirs, and water levels and water quality of ground-water wells. Volume 3B contains records for continuous ground-water elevations for 128 wells; periodic ground-water elevations at 33 wells; miscellaneous ground-water elevations at 347 wells; and water quality at 25 ground-water sites. \r\n\r\nThese data represent the national Water Data System records collected by the U.S. Geological Survey and cooperating local, state, and federal agencies in Florida.","language":"ENGLISH","doi":"10.3133/wdrFL013B","usgsCitation":"Stoker, Y., Kane, R., and Fletcher, W., 2002, Water Resources Data, Florida, Water Year 2001, Volume 3B. Southwest Florida Ground Water: U.S. Geological Survey Water Data Report FL-01-3B, 240 p., https://doi.org/10.3133/wdrFL013B.","productDescription":"240 p.","costCenters":[],"links":[{"id":5068,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrfl013B/","linkFileType":{"id":5,"text":"html"}},{"id":178951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbabd","contributors":{"authors":[{"text":"Stoker, Y.E.","contributorId":13253,"corporation":false,"usgs":true,"family":"Stoker","given":"Y.E.","email":"","affiliations":[],"preferred":false,"id":247319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kane, R.L.","contributorId":29873,"corporation":false,"usgs":true,"family":"Kane","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":247320,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fletcher, W.L.","contributorId":97977,"corporation":false,"usgs":true,"family":"Fletcher","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":247321,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53338,"text":"wdrFL011A - 2002 - Water Resources Data, Florida, Water Year 2001, Volume 1A. Northeast Florida Surface Water","interactions":[],"lastModifiedDate":"2012-02-02T00:11:44","indexId":"wdrFL011A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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-01-1A","title":"Water Resources Data, Florida, Water Year 2001, Volume 1A. Northeast Florida Surface Water","docAbstract":"Water resources data for the 2001 water year in Florida consist of continuous or daily discharge for 404 streams, periodic discharge for 17 streams, continuous or daily stage for 105 streams, periodic stage for 1 stream, peak stage and discharge for 41 streams; continuous or daily elevations for 11 lakes, periodic elevations for 28 lakes; continuous ground-water levels for 424 wells, periodic ground-water levels for 1,326 wells; quality-of-water data for 79 surface-water sites and 114 wells. \r\n\r\nThe data for northeast Florida include continuous or daily discharge for 150 streams, periodic discharge for 3 streams, continuous or daily stage for 22 streams, periodic stage for 0 streams; peak stage and discharge for 0 streams; continuous or daily elevations for 10 lakes, periodic elevations for 20 lakes; continuous ground water levels for 55 wells, periodic groundwater levels for 619 wells; quality-of-water data for 40 surface-water sites and 57 wells. \r\n\r\nThese data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, State and Federal agencies in Florida.","language":"ENGLISH","doi":"10.3133/wdrFL011A","usgsCitation":"prepared by Dickerson, S.M., 2002, Water Resources Data, Florida, Water Year 2001, Volume 1A. Northeast Florida Surface Water: U.S. Geological Survey Water Data Report FL-01-1A, 398 p., https://doi.org/10.3133/wdrFL011A.","productDescription":"398 p.","costCenters":[],"links":[{"id":5041,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdrfl011A/","linkFileType":{"id":5,"text":"html"}},{"id":174603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f79b1","contributors":{"authors":[{"text":"prepared by Dickerson, S. M.","contributorId":21212,"corporation":false,"usgs":true,"family":"prepared by Dickerson","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":247306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53361,"text":"wdrAK011 - 2002 - Water Resources Data, Alaska, Water Year 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:25","indexId":"wdrAK011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"AK-01-1","title":"Water Resources Data, Alaska, Water Year 2001","docAbstract":"Water-resources data for the 2001 water year for Alaska consists of records of stage, discharge, and water quality of streams; stages of lakes; and water levels and water quality of ground-water wells. This volume contains records for water discharge at 112 gaging stations; stage or contents only at 4 gaging stations; water quality at 37 gaging stations; and water levels for 30 observation wells. Also included are data for 51 crest-stage partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Alaska.","language":"ENGLISH","doi":"10.3133/wdrAK011","usgsCitation":"Meyer, D.F., Solin, G., Apgar, M., Hess, D., and Swenson, W., 2002, Water Resources Data, Alaska, Water Year 2001: U.S. Geological Survey Water Data Report AK-01-1, 468 p., https://doi.org/10.3133/wdrAK011.","productDescription":"468 p.","costCenters":[],"links":[{"id":179199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5083,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/WDRAK011/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc61d","contributors":{"authors":[{"text":"Meyer, D. F.","contributorId":21167,"corporation":false,"usgs":true,"family":"Meyer","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":247381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Solin, G. L.","contributorId":106132,"corporation":false,"usgs":true,"family":"Solin","given":"G. L.","affiliations":[],"preferred":false,"id":247385,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Apgar, M.L.","contributorId":50218,"corporation":false,"usgs":true,"family":"Apgar","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":247384,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hess, D.L.","contributorId":23209,"corporation":false,"usgs":true,"family":"Hess","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":247382,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Swenson, W.A.","contributorId":26363,"corporation":false,"usgs":true,"family":"Swenson","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":247383,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":53363,"text":"wdrCA011 - 2002 - Water Resources Data--California, Water Year 2001, Volume 1, Southern Great Basin from Mexican Border to Mono Lake Basin, and Pacific Slope Basins from Tijuana River to Santa Maria River","interactions":[],"lastModifiedDate":"2012-02-02T00:11:25","indexId":"wdrCA011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"CA-01-1","title":"Water Resources Data--California, Water Year 2001, Volume 1, Southern Great Basin from Mexican Border to Mono Lake Basin, and Pacific Slope Basins from Tijuana River to Santa Maria River","docAbstract":"Water-resources data for the 2001 water year for California consist of records of stage, discharge, and water quality of streams, stage and contents in lakes and reservoirs, and water levels and water quality in wells. Volume 1 contains discharge records for 180 gaging stations and 13 crest-stage partial-record stations, stage and contents for 20 lakes and reservoirs, gage-height records for 2 stations, water quality for 37 streamflow-gaging stations and 2 partial-record stations, and precipitation data for 3 stations. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"ENGLISH","doi":"10.3133/wdrCA011","usgsCitation":"Agajanian, J., Rockwell, G., Anderson, S., and Pope, G., 2002, Water Resources Data--California, Water Year 2001, Volume 1, Southern Great Basin from Mexican Border to Mono Lake Basin, and Pacific Slope Basins from Tijuana River to Santa Maria River: U.S. Geological Survey Water Data Report CA-01-1, 511 p., https://doi.org/10.3133/wdrCA011.","productDescription":"511 p.","costCenters":[],"links":[{"id":5085,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/WDRCA011","linkFileType":{"id":5,"text":"html"}},{"id":179278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa491","contributors":{"authors":[{"text":"Agajanian, J.","contributorId":78394,"corporation":false,"usgs":true,"family":"Agajanian","given":"J.","affiliations":[],"preferred":false,"id":247395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rockwell, G.L.","contributorId":47408,"corporation":false,"usgs":true,"family":"Rockwell","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":247393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Anderson, S.W.","contributorId":25628,"corporation":false,"usgs":true,"family":"Anderson","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":247392,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pope, G.L.","contributorId":58692,"corporation":false,"usgs":true,"family":"Pope","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":247394,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":53346,"text":"wdrND011 - 2002 - Water Resources Data North Dakota Water Year 2001, Volume 1. Surface Water","interactions":[],"lastModifiedDate":"2018-06-01T12:17:28","indexId":"wdrND011","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"ND-01-1","title":"Water Resources Data North Dakota Water Year 2001, Volume 1. Surface Water","docAbstract":"Water-resources data for the 2001 water year for North Dakota consists of records of discharge, stage, and water quality for streams; contents, stage, and water quality for lakes and reservoirs; and water levels and water quality for ground-water wells. Volume 1 contains records of water discharge for 103 streamflow-gaging stations; stage only for 20 river-stage stations; contents and/or stage for 13 lake or reservoir stations; annual maximum discharge for 35 crest-stage stations; and water-quality for 94 streamflow-gaging stations, 2 river-stage stations, 9 lake or reservoir stations, 7 miscellaneous sample sites on rivers, and 58 miscellaneous sample sites on lakes and wetlands. Data are included for 9 water-quality monitor sites on streams and 2 precipitation-chemistry stations. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal, State, and local agencies in North Dakota.","language":"ENGLISH","doi":"10.3133/wdrND011","usgsCitation":"Harkness, R., Berkas, W., Norbeck, S., and Robinson, S., 2002, Water Resources Data North Dakota Water Year 2001, Volume 1. Surface Water: U.S. Geological Survey Water Data Report ND-01-1, 467 p., https://doi.org/10.3133/wdrND011.","productDescription":"467 p.","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":5069,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-nd-01-1/","linkFileType":{"id":5,"text":"html"}},{"id":178952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd20f","contributors":{"authors":[{"text":"Harkness, R.E.","contributorId":24412,"corporation":false,"usgs":true,"family":"Harkness","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":247323,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berkas, W.R.","contributorId":59808,"corporation":false,"usgs":true,"family":"Berkas","given":"W.R.","affiliations":[],"preferred":false,"id":247324,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Norbeck, S.W.","contributorId":23158,"corporation":false,"usgs":true,"family":"Norbeck","given":"S.W.","affiliations":[],"preferred":false,"id":247322,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robinson, S.M.","contributorId":79162,"corporation":false,"usgs":true,"family":"Robinson","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":247325,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":53355,"text":"wdrWA021 - 2002 - Water resources rata - Washington water year 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:25","indexId":"wdrWA021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"2002","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":"WA-02-1","title":"Water resources rata - Washington water year 2002","docAbstract":"The Washington Water-Data Report includes records for both surface and ground water in the State. The report contains discharge records for 244 stream-gaging stations, stage only records for 9 gaging stations, discharge measurements for 211 miscellaneous streamflow stations, and annual maximum discharge for 3 crest-stage partial-record streamflow stations; stage and(or) content records for 36 lakes and reservoirs; water-quality records for 40 surface-water sites; water-level records for 25 observation wells; and water quality records for 11 observation wells.","language":"ENGLISH","doi":"10.3133/wdrWA021","usgsCitation":"Kimbrough, R.A., Wiggins, W., Smith, R.R., Ruppert, G., Knowles, S., and Renslow, V., 2002, Water resources rata - Washington water year 2002: U.S. Geological Survey Water Data Report WA-02-1, 578 p., https://doi.org/10.3133/wdrWA021.","productDescription":"578 p.","costCenters":[],"links":[{"id":179125,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5077,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/WDR-WA-02-1/adr.2002.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69934f","contributors":{"authors":[{"text":"Kimbrough, R. A.","contributorId":21150,"corporation":false,"usgs":true,"family":"Kimbrough","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":247356,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wiggins, W.D.","contributorId":41882,"corporation":false,"usgs":true,"family":"Wiggins","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":247359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, R. R.","contributorId":31699,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":247357,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ruppert, G.P.","contributorId":67111,"corporation":false,"usgs":true,"family":"Ruppert","given":"G.P.","email":"","affiliations":[],"preferred":false,"id":247360,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Knowles, S.M.","contributorId":32596,"corporation":false,"usgs":true,"family":"Knowles","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":247358,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Renslow, V.F.","contributorId":8160,"corporation":false,"usgs":true,"family":"Renslow","given":"V.F.","email":"","affiliations":[],"preferred":false,"id":247355,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
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