The South Florida Ecosystem Program is an intergovernmental effort to re-establish and maintain the ecosystem of South Florida. One element of the restoration effort is the development of a firm scientific basis for making management decisions. The U.S. Geologcal Survey (USGS) is one of the agencies that provides this needed scientific information through the USGS South Florida Ecosystem Program.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs18096","usgsCitation":"Bales, J.D., Fulford, J.M., and Swain, E.D., 1996, Review and evaluation of a model for simulating the natural hydrology of South Florida: U.S. Geological Survey Fact Sheet 180-96, 4 p., https://doi.org/10.3133/fs18096.","productDescription":"4 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":123042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0180/report-thumb.jpg"},{"id":31935,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0180/report.pdf","text":"Report","size":"2.34 MB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 1996-180"}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.540283203125,\n 24.337086982410497\n ],\n [\n -79.60693359375,\n 24.337086982410497\n ],\n [\n -79.60693359375,\n 26.980828590472107\n ],\n [\n -82.540283203125,\n 26.980828590472107\n ],\n [\n -82.540283203125,\n 24.337086982410497\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
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Pesticides (herbicides and insecticides) are used extensively in the White River Basin. Application of herbicides to corn and soybeans accounts for most of the use. The U.S. Geological Survey collected samples from four networks of monitoring wells in the White River Basin during 1994-95. The most frequently detected compounds in ground water were desethyl atrazine (a breakdown product of atrazine) and the commonly used herbicides, atrazine and metolachlor. Insecticides commonly used in urban and agricultural areas were not found. The highest concentration of any pesticide detected was alachlor at 0.19 micrograms per liter. Most detections of atrazine and desethyl atrazine were in agricultural areas overlying fluvial deposits, which are vulnerable to pesticide contamination, but the concentrations were small (less than 0.1 microgram per liter).
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U.S. Geological Survey
5957 Lakeside Blvd.
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During 1993-95, water samples were collected at nine sites on eight streams in the Western Lake Michigan Drainages to attempt to determine pesticide concentrations. The sampling effort was part of the U.S. Geological Survey's National Water- Quality Assessment (NAWQA) Program. Pesticides analyzed for were 58 herbicides and 30 insecticides. Pesticides are used extensively in the study area; application of herbicides to corn and soybeans accounts for most of the use. Herbicides were detected more frequently and generally at higher concentrations than insecticides. The herbicide atrazine is applied to more acreage in Wisconsin than all other pesticides and was detected in 142 of 143 samples. The herbicides simazine, metolachlor, cyanazine, prometon, and alachlor were detected in more than half of the samples. The presence of these compounds in the sampled streams, is related to agricultural use. Two streams in forested basins in the northern part of the study area were sampled and found to contain low concentrations of atrazine. Atmospheric deposition is the likely source; atrazine has been detected in rain fall in northeastern Wisconsin. Herbicide concentrations in agricultural basins were highest in samples collected during storm runoff following application. Concentrations decreased over the growing season as herbicides broke down and increased ground cover reduced runoff. The U.S. Environmental Protection Agency (USEPA) drinking-water standard for atrazine was exceeded in eight samples, and the standard for alachlor was exceeded in two samples. All exceedances occurred during brief periods of high streamflow in June and July at two streams that drain primarily agricultural basins. Herbicide data for the Western Lake Drainages and other NAWQA study units indicate that concentrations in streams are as much as two orders of magnitude higher in areas where agricultural land contains a high percentage of row crops especially corn and soybeans than in areas where grazing, hay production, and other less herbicide-intensive crops are raised.
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28 cm. map ;","costCenters":[],"links":[{"id":251793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0222/report-thumb.jpg"},{"id":247318,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0222/report.pdf","size":"166","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Northern Idaho","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.98242187499999,\n 46.649436163350245\n ],\n [\n -114.60937499999999,\n 46.6795944656402\n ],\n [\n -115.33447265625,\n 47.204642388766935\n ],\n [\n -115.64208984374999,\n 47.41322033016902\n ],\n [\n -115.75195312499999,\n 47.68018294648414\n ],\n [\n -116.05957031249999,\n 47.945786463687185\n ],\n [\n -116.03759765625,\n 48.472921272487824\n ],\n [\n -116.98242187499999,\n 48.472921272487824\n ],\n [\n -116.98242187499999,\n 46.649436163350245\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63595b","contributors":{"authors":[{"text":"Beckwith, Michael A.","contributorId":66670,"corporation":false,"usgs":true,"family":"Beckwith","given":"Michael","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":150621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berenbrock, Charles E. ceberenb@usgs.gov","contributorId":857,"corporation":false,"usgs":true,"family":"Berenbrock","given":"Charles","email":"ceberenb@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":150619,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Backsen, R.L.","contributorId":48550,"corporation":false,"usgs":true,"family":"Backsen","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":150620,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5480,"text":"fs24295 - 1996 - Quake Forecasting- An Emerging Capability","interactions":[],"lastModifiedDate":"2019-07-10T15:03:15","indexId":"fs24295","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"242-95","title":"Quake Forecasting- An Emerging Capability","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs24295","usgsCitation":"Michael, A., Reasenberg, P., Stauffer, P.H., and Hendley, J.W., 1996, Quake Forecasting- An Emerging Capability: U.S. Geological Survey Fact Sheet 242-95, 1 sheet ([2] p.) : col. ill., col. map ; 28 cm., https://doi.org/10.3133/fs24295.","productDescription":"1 sheet ([2] p.) : col. ill., col. map ; 28 cm.","costCenters":[{"id":235,"text":"Earthquake Hazards Program - Northern California","active":false,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":117391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0242/report-thumb.jpg"},{"id":32074,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0242/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":9105,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/1995/fs242-95/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6873ae","contributors":{"authors":[{"text":"Michael, Andrew","contributorId":97760,"corporation":false,"usgs":true,"family":"Michael","given":"Andrew","affiliations":[],"preferred":false,"id":151059,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reasenberg, Paul","contributorId":10806,"corporation":false,"usgs":true,"family":"Reasenberg","given":"Paul","affiliations":[],"preferred":false,"id":151058,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stauffer, Peter H. pstauffe@usgs.gov","contributorId":1219,"corporation":false,"usgs":true,"family":"Stauffer","given":"Peter","email":"pstauffe@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":151056,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hendley, James W. II jhendley@usgs.gov","contributorId":2547,"corporation":false,"usgs":true,"family":"Hendley","given":"James","suffix":"II","email":"jhendley@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":false,"id":151057,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":5590,"text":"fs19396 - 1996 - Study design and preliminary data analysis for a streambank fencing project in the Mill Creek Basin, Pennsylvania","interactions":[],"lastModifiedDate":"2018-02-16T15:21:10","indexId":"fs19396","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"193-96","title":"Study design and preliminary data analysis for a streambank fencing project in the Mill Creek Basin, Pennsylvania","docAbstract":"The Pequea Creek and Mill Creek Basins within Lancaster and Chester Counties in Pennsylvania have been identified as areas needing control of nonpoint-source (NFS) pollution to improve water quality. The two basins are a total of approximately 200 square miles and are primarily underlain by carbonate bedrock. Land use is predominantly agriculture. The most common agricultural NFS pollution-control practices implemented in the Pequea Creek and Mill Creek Basins are barnyard-runoff control and Streambank fencing. To provide land managers information on the effectiveness of Streambank fencing in controlling NFS pollution, a study is being conducted in two small paired watersheds within the Mill Creek Basin.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs19396","usgsCitation":"Galeone, D.G., and Koerkle, E.H., 1996, Study design and preliminary data analysis for a streambank fencing project in the Mill Creek Basin, Pennsylvania: U.S. Geological Survey Fact Sheet 193-96, 4 p., https://doi.org/10.3133/fs19396.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":32109,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0193/fs19960193.pdf","text":"Report","size":"2.23 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":117801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0193/coverthb.jpg"}],"contact":"Director, Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9632","usgsCitation":"Ratcliffe, N.M., 1996, Preliminary bedrock geologic map of the Andover quadrangle, Windsor County, Vermont: U.S. Geological Survey Open-File Report 96-32, Report: 24 p.; 3 Plates: 20.10 × 29.36 inches or smaller, https://doi.org/10.3133/ofr9632.","productDescription":"Report: 24 p.; 3 Plates: 20.10 × 29.36 inches or smaller","costCenters":[],"links":[{"id":397797,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19360.htm"},{"id":60144,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0032/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60143,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0032/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60142,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0032/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60141,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0032/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0032/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Vermont","county":"Windsor County","otherGeospatial":"Andover quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.625,\n 43.25\n ],\n [\n -72.75,\n 43.25\n ],\n [\n -72.75,\n 43.375\n ],\n [\n -72.625,\n 43.375\n ],\n [\n -72.625,\n 43.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613ce3","contributors":{"authors":[{"text":"Ratcliffe, N. M.","contributorId":80691,"corporation":false,"usgs":true,"family":"Ratcliffe","given":"N.","middleInitial":"M.","affiliations":[],"preferred":false,"id":207412,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30588,"text":"wri954243 - 1996 - Water quality of large discharges from mines in the anthracite region of eastern Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-06T14:23:27","indexId":"wri954243","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"95-4243","title":"Water quality of large discharges from mines in the anthracite region of eastern Pennsylvania","docAbstract":"In 1991, 99 of the 102 coal mines in the anthracite coal fields of Pennsylvania that discharged 1.0 cubic foot per second or more when water-quality samples were collected in 1975 were revisited. Water was not discharging from 15 of these 99 mines in 1991. Discharge, water temperature, specific conductance, pH, dissolved oxygen, sulfate, iron, manganese, alkalinity, and acidity were measured in water samples collected at 84 mines to assess changes in water quality from 1975 to 1991. The pH increased in water samples of 64 of the 81 mines. However, acidity was essentially unchanged. Concentrations of iron decreased in water discharge samples from 57 of 82 mines, manganese concentrations decreased in samples from 23 of 26 mines, and sulfate concentrations decreased in samples from 62 of 77 mines. The median change in sulfate was a decrease of 139 milligrams per liter. Alkalinity increased in water discharge samples from 43 mines, remained the same at 22 mines, and decreased at 14 mines. In 1975, the samples were collected during high base flow in the spring; in 1991, samples were collected during lower-than-normal base flow in the fall. This may have affected the comparison.\r\n Many mine discharges have elevated concentrations of aluminum, calcium, cobalt, iron, lithium, magnesium, manganese, nickel, strontium, zinc, and sulfate.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954243","usgsCitation":"Wood, C.R., 1996, Water quality of large discharges from mines in the anthracite region of eastern Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 95-4243, v, 68 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954243.","productDescription":"v, 68 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":59348,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4243/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4243/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.5802001953125,\n 40.30257076364479\n ],\n [\n -75.10528564453125,\n 40.30257076364479\n ],\n [\n -75.10528564453125,\n 41.64623592868676\n ],\n [\n -76.5802001953125,\n 41.64623592868676\n ],\n [\n -76.5802001953125,\n 40.30257076364479\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9972","contributors":{"authors":[{"text":"Wood, C. R.","contributorId":100386,"corporation":false,"usgs":true,"family":"Wood","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":203497,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5110,"text":"fs12596 - 1996 - Seawater Intrusion in a Coastal California Aquifer","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"fs12596","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"125-96","title":"Seawater Intrusion in a Coastal California Aquifer","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs12596","usgsCitation":"Izbicki, J., 1996, Seawater Intrusion in a Coastal California Aquifer: U.S. Geological Survey Fact Sheet 125-96, [4] p. : ill., maps ; 28 cm. ill., maps ;, https://doi.org/10.3133/fs12596.","productDescription":"[4] p. : ill., maps ; 28 cm. ill., maps ;","costCenters":[],"links":[{"id":478,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://ca.water.usgs.gov/archive/fact_sheets/b07/hyd.html","linkFileType":{"id":5,"text":"html"}},{"id":117451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0125/report-thumb.jpg"},{"id":31897,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0125/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc307","contributors":{"authors":[{"text":"Izbicki, John A. 0000-0003-0816-4408 jaizbick@usgs.gov","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":1375,"corporation":false,"usgs":true,"family":"Izbicki","given":"John A.","email":"jaizbick@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":150432,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27886,"text":"wri954260 - 1996 - Potential effects of climate change on streamflow, eastern and western slopes of the Sierra Nevada, California and Nevada","interactions":[],"lastModifiedDate":"2017-12-19T13:23:38","indexId":"wri954260","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"95-4260","title":"Potential effects of climate change on streamflow, eastern and western slopes of the Sierra Nevada, California and Nevada","docAbstract":"Precipitation-runoff models of the East Fork Carson and North Fork American Rivers were developed and calibrated for use in evaluating the sensitivity of streamflow in the north-central Sierra Nevada to climate change. The East Fork Carson River drains part of the rain-shadowed, eastern slope of the Sierra Nevada and is generally higher than the North Fork American River, which drains the wetter, western slope. First, a geographic information system was developed to describe the spatial variability of basin characteristics and to help estimate model parameters. The result was a partitioning of each basin into noncontiguous, but hydrologically uniform, land units. Hydrologic descriptions of these units were developed and the Precipitation- Runoff Modeling System (PRMS) was used to simulate water and energy balances for each unit in response to daily weather conditions. The models were calibrated and verified using historical streamflows over 22-year (Carson River) and 42-year (American River) periods. Simulated annual streamflow errors average plus 10 percent of the observed flow for the East Fork Carson River basin and plus 15 percent for the North Fork American River basin. Interannual variability is well simulated overall, but, at daily scales, wet periods are simulated more accurately than drier periods. The simulated water budgets for the two basins are significantly different in seasonality of streamflow, sublimation, evapotranspiration, and snowmelt. The simulations indicate that differences in snowpack and snowmelt timing can play pervasive roles in determining the sensitivity of water resources to climate change, in terms of both resource availability and amount. The calibrated models were driven by more than 25 hypothetical climate-change scenarios, each 100 years long. The scenarios were synthesized and spatially disaggregated by methods designed to preserve realistic daily, monthly, annual, and spatial statistics. Simulated streamflow timing was not very sensitive to changes in mean precipitation, but was sensitive to changes in mean temperatures. Changes in annual streamflow amounts were amplified reflections of imposed mean precipitation changes, with especially large responses to wetter climates. In contrast, streamflow amount was surprisingly insensitive to mean temperature changes as a result of temporal links between peak snowmelt and the beginning of warm-season evapotranspiration. Comparisons of simulations driven by temporally detailed climate-model changes in which mean temperature changes vary from month to month and simulations in which uniform climate changes were imposed throughout the year indicate that the snowpack accumulates the influences of short-term conditions so that season average climate changes were more important than shorter term changes.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954260","usgsCitation":"Jeton, A., Dettinger, M.D., and Smith, J.L., 1996, Potential effects of climate change on streamflow, eastern and western slopes of the Sierra Nevada, California and Nevada: U.S. Geological Survey Water-Resources Investigations Report 95-4260, v, 44 p. :ill. ;28 cm., https://doi.org/10.3133/wri954260.","productDescription":"v, 44 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4260/report-thumb.jpg"},{"id":56708,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4260/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49a2","contributors":{"authors":[{"text":"Jeton, A.E.","contributorId":61841,"corporation":false,"usgs":true,"family":"Jeton","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":198849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dettinger, M. D. 0000-0002-7509-7332","orcid":"https://orcid.org/0000-0002-7509-7332","contributorId":93069,"corporation":false,"usgs":false,"family":"Dettinger","given":"M.","middleInitial":"D.","affiliations":[{"id":16196,"text":"Scripps Institution of Oceanography, La Jolla, CA","active":true,"usgs":false}],"preferred":false,"id":198851,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, J. LaRue jlsmith@usgs.gov","contributorId":1863,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"jlsmith@usgs.gov","middleInitial":"LaRue","affiliations":[],"preferred":true,"id":198850,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":24906,"text":"ofr96103 - 1996 - Water-quality assessment of the Albemarle-Pamlico Basin, North Carolina and Virginia; chemical analyses of organic compounds and inorganic constituents in streambed sediment, 1992-93","interactions":[],"lastModifiedDate":"2017-01-04T12:54:08","indexId":"ofr96103","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"96-103","title":"Water-quality assessment of the Albemarle-Pamlico Basin, North Carolina and Virginia; chemical analyses of organic compounds and inorganic constituents in streambed sediment, 1992-93","docAbstract":"In 1991, the U.S. Geological Survey began full-scale implementation of the National Water-Quality Assessment (NAWQA) program. Long-term goals of the NAWQA program are to describe the status and trends in the quality of a large, representative part of the Nation's surface-water and ground-water resources and to describe the primary natural and human factors that affect these resources. One of the first assessment phases of the NAWQA program is to examine the occurrence and distribution of organic and inorganic constituents in streambed sediment. Streambed sediment was collected at 22 stations in the Albemarle-Pamlico drainage basin that drains into the Albemarle and Pamlico Sounds, the second largest estuarine system in the United States. Streambed-sediment samples were analyzed for 35 organochlorine and 63 semivolatile compounds; 44 major, minor, and trace elements; and forms of organic carbon.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr96103","issn":"0094-9140","usgsCitation":"Woodside, M.D., and Simerl, B., 1996, Water-quality assessment of the Albemarle-Pamlico Basin, North Carolina and Virginia; chemical analyses of organic compounds and inorganic constituents in streambed sediment, 1992-93: U.S. Geological Survey Open-File Report 96-103, vi, 25 p. :map ;28 cm., https://doi.org/10.3133/ofr96103.","productDescription":"vi, 25 p. :map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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D.","contributorId":98722,"corporation":false,"usgs":true,"family":"Woodside","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":192777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simerl, B.R.","contributorId":93092,"corporation":false,"usgs":true,"family":"Simerl","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":192776,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6609,"text":"fs20396 - 1996 - Environmental behavior and fate of methyl tert-butyl ether (MTBE)","interactions":[],"lastModifiedDate":"2016-02-01T08:44:56","indexId":"fs20396","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"203-96","title":"Environmental behavior and fate of methyl tert-butyl ether (MTBE)","docAbstract":"When gasoline that has been oxygenated with methyl tert-butyl ether (MTBE) comes in contact with water, large amounts of MTBE can dissolve; at 25 degrees Celsius the water solubility of MTBE is about 5,000 milligrams per liter for a gasoline that is 10 percent MTBE by weight. In contrast, for a nonoxygenated gasoline, the total hydrocarbon solubility in water is typically about 120 milligrams per liter. MTBE sorbs only weakly to soil and aquifer materials; therefore, sorption will not significantly retard MTBE's transport by ground water. In addition, MTBE generally resists degradation in ground water. The half-life of MTBE in the atmosphere can be as short as 3 days in a regional airshed. MTBE in the air tends to partition into atmospheric water, including precipitation. However, washout of gas-phase MTBE by precipitation would not, by itself, greatly alter the gas-phase concentration of the compound in the air. The partitioning of MTBE to precipitation is nevertheless strong enough to allow for up to 3 micrograms per liter or more inputs of MTBE to surface and ground water.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20396","usgsCitation":"Squillace, P.J., Pankow, J.F., Korte, N.E., and Zogorski, J.S., 1996, Environmental behavior and fate of methyl tert-butyl ether (MTBE): U.S. Geological Survey Fact Sheet 203-96, 6 p., https://doi.org/10.3133/fs20396.","productDescription":"6 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":34056,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0203/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117836,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0203/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025a6","contributors":{"authors":[{"text":"Squillace, Paul J.","contributorId":59415,"corporation":false,"usgs":true,"family":"Squillace","given":"Paul","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":153017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pankow, James F.","contributorId":72253,"corporation":false,"usgs":true,"family":"Pankow","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":153018,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Korte, Nic E.","contributorId":100684,"corporation":false,"usgs":true,"family":"Korte","given":"Nic","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":153019,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zogorski, John S. jszogors@usgs.gov","contributorId":189,"corporation":false,"usgs":true,"family":"Zogorski","given":"John","email":"jszogors@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":153016,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":6645,"text":"fs17696 - 1996 - Quality of ground water at selected sites in the upper Mahoning Creek Basin, Pennsylvania","interactions":[],"lastModifiedDate":"2018-02-09T12:46:57","indexId":"fs17696","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"176-96","title":"Quality of ground water at selected sites in the upper Mahoning Creek Basin, Pennsylvania","docAbstract":"The ground-water quality of the upper Mahoning Creek Basin is largely unknown. Human activities in the basin have altered much of the landscape. The presence of coal mining, oil and gas exploration, agriculture, on-lot septic systems, and commercial development within the basin can introduce contaminants altering the natural chemistry of the ground water. Data collected to document current ground-water quality also can serve as a baseline for comparison of any future water-quality changes by continuing human activities. This report presents the results of a synoptic ground-water-quality sampling in the upper Mahoning Creek Basin. Present ground-water quality in the basin is characterized in relation to published standards, local land-use activities, and other areas with similar natural characteristics.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs17696","usgsCitation":"Langland, M.J., 1996, Quality of ground water at selected sites in the upper Mahoning Creek Basin, Pennsylvania: U.S. Geological Survey Fact Sheet 176-96, 4 p., https://doi.org/10.3133/fs17696.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":34071,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0176/fs19960176.pdf","text":"Report","size":"123 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 1996-0176"},{"id":117128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0176/coverthb.jpg"}],"contact":"Director, Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070
Nonpoint sources of pesticides are a national issue and are a major interest in the U.S. Geological Survey National Water-Quality Assessment (NAWQA) Program because of their potential toxicity to humans and aquatic life. Using the water-quality data collected by the Trinity River Basin NAWQA study-unit team, an analysis of pesticides in urban and agricultural streams was made by aggregating and grouping data from several networks. The samples were collected during March 1993 through September 1995. About 70 samples were collected from urban streams and 70 from agricultural streams. The urban dataset consists of sampling sites in the Dallas-Fort Worth metropolitan area where more than 3.5 million people lived in 1990. Land use in the sampled urban watersheds is primarily residential, but there are commercial areas, such as shopping centers and office complexes along major highways and streets. The agricultural dataset consists of sampling sites in the watershed of Richland-Chambers Reservoir, an area in the west-central part of the Trinity River Basin where fertile soils are extensively cultivated. The land use is mostly cropland and pasture with some rangeland. In the cultivated areas, the major crops are corn, cotton, and sorghum. In the rangeland areas, cattle are the dominant livestock. In the pasture areas, hay is grown along with grass for cattle feed. None of the crops are irrigated.
\nThe material in this fact sheet is condensed from a report by Land and Brown (1996) where the study is presented in greater detail.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs17896","usgsCitation":"Land, L.F., 1996, Pesticides in urban and agricultural streams, 1993-95: U.S. Geological Survey Fact Sheet 178-96, 2 p., https://doi.org/10.3133/fs17896.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":125313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0178/report-thumb.jpg"},{"id":34069,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0178/report.pdf","text":"Report","size":"1.0 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","otherGeospatial":"Richland-Chambers Reservoir, Trinity River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.3,\n 31.5\n ],\n [\n -97.3,\n 33.5\n ],\n [\n -96,\n 33.5\n ],\n [\n -96,\n 31.5\n ],\n [\n -97.3,\n 31.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881e1","contributors":{"authors":[{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":153089,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6860,"text":"fs19196 - 1996 - The Upper Colorado River; National Water-Quality Assessment Program; surface-water-monitoring network","interactions":[],"lastModifiedDate":"2017-04-20T16:53:07","indexId":"fs19196","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"191-96","title":"The Upper Colorado River; National Water-Quality Assessment Program; surface-water-monitoring network","docAbstract":"The U.S. Geological Survey began full implementation of the National Water-Quality Assessment (NAWQA) program in 1991. The long-term goals of the NAWQA program are to (1) describe current water-quality conditions for a large part of the Nation's freshwater streams, rivers, and aquifers; (2) describe how water quality is changing over time; and (3) improve understanding of the primary natural and human factors that affect water-quality conditions (Leahy and others, 1990). To meet these goals, 60 study units representing the Nation's most important river basins and aquifers are being investigated. The program design balances the unique assessment requirements of individual study units with a nationally consistent design structure that incorporates a multiscale, interdisciplinary approach for assessment of surface and ground water.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs19196","usgsCitation":"Spahr, N.E., Driver, N.E., and Stephens, V.C., 1996, The Upper Colorado River; National Water-Quality Assessment Program; surface-water-monitoring network: U.S. Geological Survey Fact Sheet 191-96, 3 p., https://doi.org/10.3133/fs19196.","productDescription":"3 p.","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"links":[{"id":34177,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0191/report.pdf","text":"Report","size":"1.8 MB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 191-96"},{"id":117956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0191/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4880e4b07f02db515e3d","contributors":{"authors":[{"text":"Spahr, Norman E. nspahr@usgs.gov","contributorId":1977,"corporation":false,"usgs":true,"family":"Spahr","given":"Norman","email":"nspahr@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":153466,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Driver, Nancy E.","contributorId":67858,"corporation":false,"usgs":true,"family":"Driver","given":"Nancy","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":153468,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stephens, Verlin C.","contributorId":34479,"corporation":false,"usgs":true,"family":"Stephens","given":"Verlin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":153467,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5034,"text":"fs19096 - 1996 - Real-time streamflow conditions","interactions":[],"lastModifiedDate":"2015-09-29T09:29:47","indexId":"fs19096","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"190-96","title":"Real-time streamflow conditions","docAbstract":"Would you like to know streamflow conditions before you go fishing in Wisconsin or in more distant locations? Real-time streamflow data throughout Wisconsin and the United States are available on the Internet from the U.S. Geological Survey. You can see if the stream you are interested in fishing is high due to recent rain or low because of an extended dry spell. Flow conditions at more than 100 stream-gaging stations located throughout Wisconsin can be viewed by accessing the Wisconsin District Home Page at: http://wwwdwimdn.er.usgs.gov
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Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:38","indexId":"wri954239","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","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":"95-4239","title":"Geohydrology of Pahute Mesa-3 test well, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri954239","usgsCitation":"Kilroy, K., and Savard, C., 1996, Geohydrology of Pahute Mesa-3 test well, Nye County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 95-4239, v, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954239.","productDescription":"v, 37 p. :ill., maps ;28 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The estimated total ground-water pumpage in 1990 was about 340,000 acre-feet. Ground water in the study area is pumped mainly from Quaternary sediment; lesser amounts are withdrawn from Tertiary volcanic materials. Large parts of the area are used for agriculture, and about two and one-half times as much ground water was pumped for irrigation as for either public- supply or industrial needs. Estimates of ground- water pumpage for irrigation in the central part of the Willamette Valley were generated by using image-processing techniques and Landsat Thematic Mapper data. Field data and published reports were used to estimate pumpage for irrigation in other parts of the study area. Information on public- supply and industrial pumpage was collected from Federal, State, and private organizations and individuals.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/wri964111","usgsCitation":"Collins, C., and Broad, T.M., 1996, Ground-water pumpage in the Willamette lowland regional aquifer system, Oregon and Washington, 1990: U.S. Geological Survey Water-Resources Investigations Report 96-4111, iii, 27 p., https://doi.org/10.3133/wri964111.","productDescription":"iii, 27 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":125024,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4111/report-thumb.jpg"},{"id":55498,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4111/report.pdf","text":"Report","size":"549.91 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Willamette Regional Aquifer System","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.16748046874999,\n 43.78695837311561\n ],\n [\n -124.16748046874999,\n 49.76707407366792\n ],\n [\n -119.00390625,\n 49.76707407366792\n ],\n [\n -119.00390625,\n 43.78695837311561\n ],\n [\n -124.16748046874999,\n 43.78695837311561\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673ed","contributors":{"authors":[{"text":"Collins, Charles A.","contributorId":79510,"corporation":false,"usgs":true,"family":"Collins","given":"Charles A.","affiliations":[],"preferred":false,"id":196733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broad, Tyson M.","contributorId":76786,"corporation":false,"usgs":true,"family":"Broad","given":"Tyson","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":196732,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4893,"text":"ds41 - 1996 - Great Basin geoscience data base","interactions":[],"lastModifiedDate":"2014-02-28T13:28:18","indexId":"ds41","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"41","title":"Great Basin geoscience data base","docAbstract":"This CD-ROM serves as the archive for 73 digital GIS data set for the Great Basin. The data sets cover Nevada, eastern California, southeastern Oregon, southern Idaho, and western Utah. Some of the data sets are incomplete for the total area. On the CD-ROM, the data are provided in three formats, a prototype Federal Data Exchange standard format, the ESRI PC ARCVIEW1 format for viewing the data, and the ESRI ARC/INFO export format. Extensive documentation is provided to describe the data, the sources, and data enhancements. The following data are provided. One group of coverages comes primarily from 1:2,000,000-scale National Atlas data and can be assembled for use as base maps. These various forms of topographic information. In addition, public land system data sets are provided from the 1:2,500,000-scale Geologic Map of the United States and 1:500,000-scale geologic maps of Nevada, Oregon, and Utah. Geochemical data from the National Uranium Resource Evaluation (NURE) program are provided for most of the Great Basin. Geophysical data are provided for most of the Great Basin, typically gridded data with a spacing of 1 km. The geophysical data sets include aeromagnetics, gravity, radiometric data, and several derivative products. 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