Water resources data for the 1993 water year in Florida consist of continuous or daily discharge for 312 streams, periodic discharge for 9 streams, miscellaneous discharge for 107 streams, continuous or daily stage for 91 streams, continuous daily tide stage for 9 sites, peak discharge for 30 streams, and peak stage for 30 streams; continuous or daily elevations for 41 lakes, periodic elevations for 73 lakes; continuous ground-water levels for 406 wells, periodic groundwater levels for 569 wells, and miscellaneous water-level measurements for 1,860 wells; quality-of-water data for 109 surface-water sites and 642 wells.
The data for northeast Florida include continuous or daily discharge for 117 streams, periodic discharge for 7 streams, miscellaneous discharge for 16 streams, continuous or daily stage for 37 streams, continuous or daily tide stage for 4 sites, peak discharge for 15 streams, and peak stage for 15 streams; continuous or daily elevations for 35 lakes, periodic elevations for 45 lakes; continuous ground-water levels for 61 wells, periodic ground-water levels for 150 wells, and miscellaneous water-level measurements for 888 wells; quality-of-water data for 27 surface-water sites and 61 wells.
These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, state and federal agencies in Florida.
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Volume 1A: Northeast Florida - surface water: U.S. Geological Survey Water Data Report FL-93-1A, xviii, 381 p., https://doi.org/10.3133/wdrFL931A.","productDescription":"xviii, 381 p.","costCenters":[],"links":[{"id":430226,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1993/fl-93-1-a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174455,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1993/fl-93-1-a/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"northeast Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.45415384078757,\n 30.55335715370353\n ],\n [\n -82.45415384078757,\n 28.17140876179424\n ],\n [\n -80.38661953845946,\n 28.17140876179424\n ],\n [\n -80.38661953845946,\n 30.55335715370353\n ],\n [\n -82.45415384078757,\n 30.55335715370353\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbbd7","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70017200,"text":"70017200 - 1994 - Measurement of saturated hydraulic conductivity in fine-grained glacial tills in Iowa: Comparison of in situ and laboratory methods","interactions":[],"lastModifiedDate":"2012-03-12T17:18:47","indexId":"70017200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Measurement of saturated hydraulic conductivity in fine-grained glacial tills in Iowa: Comparison of in situ and laboratory methods","docAbstract":"Nested-standpipe and vibrating-wire piezometers were installed in Pre-Illinoian Wolf Creek and Albernett formations at the Eastern Iowa Till Hydrology Site located in Linn County, Iowa. These surficial deposits are composed of fine-grained glacial diamicton (till) with occasional discontinuous lenses of sand and silt. They overlie the Silurian (dolomite) aquifer which provides private, public, and municipal drinking water supplies in the region. The saturated hydraulic conductivity of the Wolf Creek Formation was investigated in a sub-area of the Eastern Iowa Till Hydrology Site. Calculations of saturated hydraulic conductivity were based on laboratoryflexible-wall permeameter tests, bailer tests, and pumping test data. Results show that bulk hydraulic conductivity increases by several orders of magnitude as the tested volume of till increases. Increasing values of saturated hydraulic conductivity at larger spatial scales conceptually support a double-porosity flow model for this till.","largerWorkTitle":"ASTM Special Technical Publication","conferenceTitle":"Proceedings of tbe Symposium on Hydraulic Conductivity and Waste Contaminant Transport in Soil","conferenceDate":"21 January 1993 through 22 January 1993","conferenceLocation":"San Antonio, TX, USA","language":"English","publisher":"ASTM","publisherLocation":"Philadelphia, PA, United States","issn":"10403094","usgsCitation":"Bruner, D.R., and Lutenegger, A.J., 1994, Measurement of saturated hydraulic conductivity in fine-grained glacial tills in Iowa: Comparison of in situ and laboratory methods, in ASTM Special Technical Publication, no. 1142, San Antonio, TX, USA, 21 January 1993 through 22 January 1993, p. 255-265.","startPage":"255","endPage":"265","numberOfPages":"11","costCenters":[],"links":[{"id":224826,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"issue":"1142","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5313e4b0c8380cd6c869","contributors":{"authors":[{"text":"Bruner, D. Roger","contributorId":21697,"corporation":false,"usgs":true,"family":"Bruner","given":"D.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":375700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lutenegger, Alan J.","contributorId":8230,"corporation":false,"usgs":true,"family":"Lutenegger","given":"Alan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":375699,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55089,"text":"wdrWI931 - 1994 - Water resources data, Wisconsin, water year 1993. Volume 1. St. Lawrence River Basin","interactions":[],"lastModifiedDate":"2020-10-06T21:10:30.548982","indexId":"wdrWI931","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WI-93-1","title":"Water resources data, Wisconsin, water year 1993. Volume 1. St. Lawrence River Basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrWI931","usgsCitation":"Holmstrom, B.K., Kammerer, P., and Ellefson, B., 1994, Water resources data, Wisconsin, water year 1993. Volume 1. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa54e","contributors":{"authors":[{"text":"Holmstrom, B. K.","contributorId":90728,"corporation":false,"usgs":true,"family":"Holmstrom","given":"B.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":252630,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kammerer, P.A.","contributorId":21943,"corporation":false,"usgs":true,"family":"Kammerer","given":"P.A.","affiliations":[],"preferred":false,"id":252628,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellefson, B.R.","contributorId":83927,"corporation":false,"usgs":true,"family":"Ellefson","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":252629,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70017463,"text":"70017463 - 1994 - Observations on the geology and geohydrology of the Chernobyl' nuclear accident site, Ukraine","interactions":[],"lastModifiedDate":"2024-03-15T12:11:38.160115","indexId":"70017463","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2020,"text":"International Geology Review","active":true,"publicationSubtype":{"id":10}},"title":"Observations on the geology and geohydrology of the Chernobyl' nuclear accident site, Ukraine","docAbstract":"The most higly contaminated surface areas from cesium-137 fallout from the April 1986 accident at the Chernobyl' nuclear power station in Ukraine occur within the 30-km radius evacuation zone set up around the station, and an 80-km lobe extending to the west-southwest. Lower levels of contamination extend 300 km to the west of the power station. The deposition of this radioactive dust on the surface and the subsequent entombment of the damaged reactor effectively result in the de facto establishment of an above-ground nuclear waste storage site. This site is located on a thick sedimentary sequence of loose, mostly clastic deposits, with a shallow (generally 3-5 m) water table. The geology, the presence of surface water, a shallow water table, and leaky aquifers at depth make this an unfavorable environment for the long-term containment and storage of the radioactive debris. An understanding of the general geology and hydrology of the area is important to assess the environmental impact of this unintended waste storage site, and to evaluate the potential for radionuclide migration through the soil and rock and into subsurface aquifers and nearby rivers.
Water-resources data for the 1993 water year for West Virginia consist of records of stage, discharge, and water quality of streams; contents of reservoirs; and water levels of observations wells. This report contains discharge records for 78 streamflow-gaging stations; stage only records for 11 gaging stations; annual maximum discharge at 2 crest-stage partial-record stations; change in contents for 1 reservoir; water-quality records for 13 stations; and water-level records for 29 observation wells. Locations of these sites are shown on figures 4 and 5. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous sites. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in West Virginia.
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injection","interactions":[],"lastModifiedDate":"2021-03-19T12:52:00.858458","indexId":"70017448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1924,"text":"Hydrological Processes","active":true,"publicationSubtype":{"id":10}},"title":"Testing and comparison of four ionic tracers to measure stream flow loss by multiple tracer injection","docAbstract":"The ionic tracers lithium, sodium, chloride and bromide were used to measure flow loss in a small stream (≈︁ 10 ls−1). An injectate containing all four tracers was added continuously at five sites along a 507 m study reach of St Kevin Gulch, Lake County, Colorado to determine which sections of the stream were losing water to the stream bed and to ascertain how well the four tracers performed. The acidity of the stream (pH 3.6) made it possible for lithium and sodium, which are normally adsorbed by ion exchange with stream bed sediment, to be used as conservative tracers. Net flow losses as low as 0.8 ls−1, or 8% of flow, were calculated between measuring sites. By comparing the results of simultaneous injection it was determined whether subsections of the study reach were influent or effluent. Evaluation of tracer concentrations along 116 m of stream indicated that all four tracers behaved conservatively. Discharges measured by Parshall flumes were 4–18% greater than discharges measured by tracer dilution.
","language":"English","publisher":"Wiley","doi":"10.1002/hyp.3360080206","issn":"08856087","usgsCitation":"Zellweger, G.W., 1994, Testing and comparison of four ionic tracers to measure stream flow loss by multiple tracer injection: Hydrological Processes, v. 8, no. 2, p. 155-165, https://doi.org/10.1002/hyp.3360080206.","productDescription":"11 p.","startPage":"155","endPage":"165","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":384504,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","county":"Lake County","otherGeospatial":"St. Kevin Gulch","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.710205078125,\n 38.762650338334154\n ],\n [\n -105.8203125,\n 38.762650338334154\n ],\n [\n -105.8203125,\n 39.690280594818034\n ],\n [\n -106.710205078125,\n 39.690280594818034\n ],\n [\n -106.710205078125,\n 38.762650338334154\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"8","issue":"2","noUsgsAuthors":false,"publicationDate":"2006-07-31","publicationStatus":"PW","scienceBaseUri":"505ba5bee4b08c986b320c48","contributors":{"authors":[{"text":"Zellweger, G. W.","contributorId":55445,"corporation":false,"usgs":true,"family":"Zellweger","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":376500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54906,"text":"wdrOK931 - 1994 - Water resources data, Oklahoma, water year 1993: Volume 1. Arkansas River Basin","interactions":[],"lastModifiedDate":"2025-12-11T17:10:32.663106","indexId":"wdrOK931","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"OK-93-1","title":"Water resources data, Oklahoma, water year 1993: Volume 1. Arkansas River Basin","docAbstract":"Volumes 1 and 2 of the water resources data for the 1993 water year for Oklahoma consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes or reservoirs; and water levels of ground-water wells. This report contains discharge records for 135 gaging stations; stage and contents for 30 lakes or reservoirs; water quality for 58 gaging stations; 23 partial-record or miscellaneous streamflow stations and 28 ground-water sites. Also included are lists of discontinued surface-water discharge and water-quality sites. Volume 3 contains statewide miscellaneous water-quality data. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Oklahoma.
","language":"English","publisher":"Prepared in cooperation with the State of Oklahoma and with other agencies","doi":"10.3133/wdrOK931","usgsCitation":"Blazs, R., Walters, D., Coffey, T., White, D., Boyle, D., and Kerestes, J., 1994, Water resources data, Oklahoma, water year 1993: Volume 1. 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D.K.","contributorId":30279,"corporation":false,"usgs":true,"family":"White","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":251953,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Boyle, D.L.","contributorId":55505,"corporation":false,"usgs":true,"family":"Boyle","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":251956,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kerestes, J.F.","contributorId":19219,"corporation":false,"usgs":true,"family":"Kerestes","given":"J.F.","affiliations":[],"preferred":false,"id":251951,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":44781,"text":"wri924142 - 1994 - Hydrogeologic Atlas of Aquifers in Indiana","interactions":[],"lastModifiedDate":"2018-11-05T15:11:39","indexId":"wri924142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"92-4142","title":"Hydrogeologic Atlas of Aquifers in Indiana","docAbstract":"Aquifers in 12 water-management basins of Indiana are identified in a series of 104 hydrogeologic sections and 12 maps that show the thickness and configuration of aquifers. The vertical distribution of water-bearing units and a generalized potentiometric profile are shown along 3,500 miles of section lines that were constructed from drillers' logs of more than 4,200 wells. The horizontal scale of the sections is 1:125,000. Maps of aquifers showing the areal distribution of each aquifer type were drawn at a scale of 1:500,000. Unconsolidated aquifers are the most widely used aquifers in Indiana and include surficial, buried, and discontinuous layers of sand and gravel. Most of the surficial sand and gravel is in large outwash plains in northern Indiana and along the major rivers. Buried sand and gravel aquifers are interbedded with till deposits in much of the northern two-thirds of Indiana. Discontinuous sand and gravel deposits are present as isolated lenses, primarily in glaciated areas. The bedrock aquifers generally have lower yields than most of the sand and gravel aquifers; however, bedrock aquifers are areally widespread and are an important source of water. Bedrock aquifer types consist of carbonates; sandstones; complexly interbedded sandstones, siltstones, shales, limestones, and coals; and an upper weathered zone in low permeability rock. Carbonate aquifers underlie about one-half of Indiana and are the most productive of the bedrock aquifers. The other principal bedrock aquifer type, sandstone, underlies large areas in the southwestern one-fifth of Indiana. No aquifer is known to be present in the southeastern corner of Indiana.","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri924142","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources, Division of Water Indiana Department of Environmental Management","usgsCitation":"Fenelon, J.M., Bobay, K., Greeman, T., Hoover, M., Cohen, D., Fowler, K.K., Woodfield, M., and and Durbin, J.M., 1994, Hydrogeologic Atlas of Aquifers in Indiana: U.S. Geological Survey Water-Resources Investigations Report 92-4142, viii, 197 p. : col. ill., col. maps ; 28 x 43 cm., https://doi.org/10.3133/wri924142.","productDescription":"viii, 197 p. : col. ill., col. maps ; 28 x 43 cm.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":82112,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4142/wri19924142.pdf ","text":"Report","size":"1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 1992-4142"},{"id":123529,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4142/coverthb.jpg"}],"contact":"Director, Indiana Water Science Center
U.S. Geological Survey
5957 Lakeside Blvd.
Indianapolis, IN 46278
Herbicide interchange between a stream and the adjacent alluvial aquifer and quantification of herbicide bank storage during high streamflow were investigated at a research site on the Cedar River flood plain, 10 km southeast of Cedar Rapids, Iowa. During high streamflow in March 1990, alachlor, atrazine, and metolachlor were detected at concentrations above background in water from wells as distant as 20, 50, and 10 m from the river's edge, respectively. During high streamflow in May 1990, alachlor, atrazine, cyanazine, and metolachlor were detected at concentrations above background as distant as 20, 50, 10, and 20 m from the river's edge, respectively. Herbicide bank storage took place during high streamflow when hydraulic gradients were from the river to the alluvial aquifer and the laterally infiltrating river water contained herbicide concentrations larger than background concentrations in the aquifer. The herbicide bank storage can be quantified by multiplying herbicide concentration by the \"effective area\" that a well represented and an assumed porosity of 0.25. During March 1990, herbicide bank storage values were calculated to be 1.7,79, and 4.0 mg/m for alachlor, atrazine, and metolachlor, respectively. During May 1990, values were 7.1, 54, 11, and 19 mg/m for alachlor, atrazine, cyanazine, and metolachlor, respectively.
","language":"English","publisher":"American Chemical Society","doi":"10.1021/es00062a018","usgsCitation":"Wang, W., and Squillace, P., 1994, Herbicide interchange between a stream and the adjacent alluvial aquifer: Environmental Science & Technology, v. 28, no. 13, p. 2336-2344, https://doi.org/10.1021/es00062a018.","productDescription":"9 p.","startPage":"2336","endPage":"2344","numberOfPages":"9","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":228465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Iowa","city":"Cedar Rapids","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.197265625,\n 41.68932225997044\n ],\n [\n -91.14257812499999,\n 41.68932225997044\n ],\n [\n -91.14257812499999,\n 42.14304156290942\n ],\n [\n -92.197265625,\n 42.14304156290942\n ],\n [\n -92.197265625,\n 41.68932225997044\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"28","issue":"13","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a3066e4b0c8380cd5d5fa","contributors":{"authors":[{"text":"Wang, Wuncheng","contributorId":189650,"corporation":false,"usgs":false,"family":"Wang","given":"Wuncheng","affiliations":[],"preferred":false,"id":376363,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Squillace, P.","contributorId":15777,"corporation":false,"usgs":true,"family":"Squillace","given":"P.","affiliations":[],"preferred":false,"id":376362,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70017365,"text":"70017365 - 1994 - Environmental geology of the Summitville mine, Colorado","interactions":[],"lastModifiedDate":"2024-01-03T17:07:29.393784","indexId":"70017365","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Environmental geology of the Summitville mine, Colorado","docAbstract":"Although altered and mineralized rocks at Summitville mine in Colorado contain minimal amount of sulfide minerals, acid mine problems existed primarily because of the pervasive alteration of the surrounding rocks, through hydrothermal process, to highly siliceous and argillized rocks that are incapable of buffering acidic waters during weathering. The problems are compounded by the continued exposure of altered and mineralized rocks in open pit, heap leach pad and waste piles to oxygenated waters. Inadequate subsurface structural control and underground mine workings also greatly affect water quality and the location of acid mine drainage output. It is expected that with these initial results, geological studies on constrained acid-generation from ore and altered rocks will be pursued.","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.89.8.2006","issn":"03610128","usgsCitation":"Gray, J.E., Coolbaugh, M., Plumlee, G.S., and Atkinson, W., 1994, Environmental geology of the Summitville mine, Colorado: Economic Geology, v. 89, no. 8, p. 2006-2014, https://doi.org/10.2113/gsecongeo.89.8.2006.","productDescription":"9 p.","startPage":"2006","endPage":"2014","numberOfPages":"9","costCenters":[{"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}],"links":[{"id":224595,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"8","noUsgsAuthors":false,"publicationDate":"1994-12-01","publicationStatus":"PW","scienceBaseUri":"505a09cae4b0c8380cd5207e","contributors":{"authors":[{"text":"Gray, John E. jgray@usgs.gov","contributorId":1275,"corporation":false,"usgs":true,"family":"Gray","given":"John","email":"jgray@usgs.gov","middleInitial":"E.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":376247,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coolbaugh, Mark F.","contributorId":102640,"corporation":false,"usgs":true,"family":"Coolbaugh","given":"Mark F.","affiliations":[],"preferred":false,"id":376249,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plumlee, Geoffrey S. 0000-0002-9607-5626 gplumlee@usgs.gov","orcid":"https://orcid.org/0000-0002-9607-5626","contributorId":960,"corporation":false,"usgs":true,"family":"Plumlee","given":"Geoffrey","email":"gplumlee@usgs.gov","middleInitial":"S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":376246,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Atkinson, William W.","contributorId":28755,"corporation":false,"usgs":true,"family":"Atkinson","given":"William W.","affiliations":[],"preferred":false,"id":376248,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20421,"text":"ofr93486 - 1994 - Selected water-quality data for the Toppenish Creek Basin, Yakima Indian Reservation, Washington, 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:07:39","indexId":"ofr93486","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-486","title":"Selected water-quality data for the Toppenish Creek Basin, Yakima Indian Reservation, Washington, 1989","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr93486","usgsCitation":"Payne, K.L., and Sumioka, S.S., 1994, Selected water-quality data for the Toppenish Creek Basin, Yakima Indian Reservation, Washington, 1989: U.S. Geological Survey Open-File Report 93-486, iv, 27 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr93486.","productDescription":"iv, 27 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0486/report-thumb.jpg"},{"id":49963,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1993/0486/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49964,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1993/0486/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49965,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0486/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b178","contributors":{"authors":[{"text":"Payne, K. L.","contributorId":31771,"corporation":false,"usgs":true,"family":"Payne","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":182621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sumioka, S. S.","contributorId":20747,"corporation":false,"usgs":true,"family":"Sumioka","given":"S.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":182620,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44750,"text":"wri934216 - 1994 - Water-surface profile and flood boundaries for the computed 100-year flood, Lame Deer Creek, Northern Cheyenne Indian Reservation, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:57","indexId":"wri934216","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4216","title":"Water-surface profile and flood boundaries for the computed 100-year flood, Lame Deer Creek, Northern Cheyenne Indian Reservation, Montana","docAbstract":"Hydrologic and hydraulic evaluations of Lame Deer Creek were made to determine the magnitude of the 100-year flood and the extent of flooding that would occur as the result of this flood. SixtY-six cross sections were Surveyed and 25 cross sections were synthesized along a 9.5-mile reach of Lame Deer Creek. Data from the surveys were used to calculate the water-surface elevation at each cross section using a computer program (WSPRO) developed by the U.S. Geological Survey. The water-surface profile of the computed 100-year flood elevations was then drawn. The profile shows the streambed elevation and the location of the bridge, culverts, and cross sections. The computed 100-year flood elevation at each cross section was used to delineate the width of the flood plain at that section. Flood boundaries between cross sections were interpolated using contour lines on topographic maps.","language":"ENGLISH","doi":"10.3133/wri934216","usgsCitation":"Omang, R.J., 1994, Water-surface profile and flood boundaries for the computed 100-year flood, Lame Deer Creek, Northern Cheyenne Indian Reservation, Montana: U.S. Geological Survey Water-Resources Investigations Report 93-4216, 1 map ; 75 x 91 cm., on sheet 86 x 96 cm., folded in envelope 31 x 24 cm., https://doi.org/10.3133/wri934216.","productDescription":"1 map ; 75 x 91 cm., on sheet 86 x 96 cm., folded in envelope 31 x 24 cm.","costCenters":[],"links":[{"id":258704,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4216/plate-1.pdf","size":"6096","linkFileType":{"id":1,"text":"pdf"}},{"id":258705,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4216/report.pdf","size":"519","linkFileType":{"id":1,"text":"pdf"}},{"id":258706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4216/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d54","contributors":{"authors":[{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":230365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70017413,"text":"70017413 - 1994 - Assessing the fate of dredged sediments placed in open-water sites, Northern Chesapeake Bay","interactions":[],"lastModifiedDate":"2012-03-12T17:19:58","indexId":"70017413","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Assessing the fate of dredged sediments placed in open-water sites, Northern Chesapeake Bay","docAbstract":"An integrated series of field studies and experiments have been carried out on dredged sediments placed in open water sites in Northern Chesapeake Bay. The studies include: (1) examination of the potential for fluidized sediment flow, (2) quantifying the volumetric changes that the sediments undergo during dredging process and subsequent to deposition, (3) estimating parameters for cohesive sediment erosion models from field data on currents and suspended sediment concentrations, and (4) incorporating the erosion model parameters and sediment transport equation into a 3-D hydrodynamic model for the upper Chesapeake Bay to predict transport directions and setting sites of eroded sediments under a variety of seasonal weather and river flow conditions.","largerWorkTitle":"International Conference on Dredging and Dredged Material Placement","conferenceTitle":"Proceedings of the 2nd International Conference on Dredging and Dredged Material Placement. Part 2 (of 2)","conferenceDate":"13 November 1994 through 16 November 1994","conferenceLocation":"Lake Buena Vista, FL, USA","language":"English","publisher":"ASCE","publisherLocation":"New York, NY, United States","usgsCitation":"Halka, J., Panageotou, W., Sanford, L., and Yu-Chou, S., 1994, Assessing the fate of dredged sediments placed in open-water sites, Northern Chesapeake Bay, in International Conference on Dredging and Dredged Material Placement, v. 2, Lake Buena Vista, FL, USA, 13 November 1994 through 16 November 1994, p. 1162-1171.","startPage":"1162","endPage":"1171","numberOfPages":"10","costCenters":[],"links":[{"id":228506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ede9e4b0c8380cd49ad2","contributors":{"editors":[{"text":"McNair Clark E.","contributorId":128385,"corporation":true,"usgs":false,"organization":"McNair Clark E.","id":536363,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Halka, Jeffrey","contributorId":96033,"corporation":false,"usgs":true,"family":"Halka","given":"Jeffrey","email":"","affiliations":[],"preferred":false,"id":376368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Panageotou, William","contributorId":14966,"corporation":false,"usgs":true,"family":"Panageotou","given":"William","email":"","affiliations":[],"preferred":false,"id":376365,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sanford, Lawrence","contributorId":59195,"corporation":false,"usgs":true,"family":"Sanford","given":"Lawrence","email":"","affiliations":[],"preferred":false,"id":376367,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yu-Chou, Shenn","contributorId":15359,"corporation":false,"usgs":true,"family":"Yu-Chou","given":"Shenn","email":"","affiliations":[],"preferred":false,"id":376366,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":54947,"text":"wdrPA933 - 1994 - Water Resources Data, Pennsylvania, Water Year 1993. Volume 3. Ohio and St. Lawrence River Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:11:38","indexId":"wdrPA933","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"PA-93-3","title":"Water Resources Data, Pennsylvania, Water Year 1993. Volume 3. Ohio and St. Lawrence River Basins","language":"ENGLISH","doi":"10.3133/wdrPA933","usgsCitation":"Lescinsky, J., Coll, M., and Siwicki, R., 1994, Water Resources Data, Pennsylvania, Water Year 1993. Volume 3. Ohio and St. Lawrence River Basins: U.S. Geological Survey Water Data Report PA-93-3, 166 p., https://doi.org/10.3133/wdrPA933.","productDescription":"166 p.","costCenters":[],"links":[{"id":177276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67acbf","contributors":{"authors":[{"text":"Lescinsky, J.B.","contributorId":83197,"corporation":false,"usgs":true,"family":"Lescinsky","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":252111,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coll, M.B.","contributorId":19629,"corporation":false,"usgs":true,"family":"Coll","given":"M.B.","affiliations":[],"preferred":false,"id":252110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Siwicki, R.W.","contributorId":100060,"corporation":false,"usgs":true,"family":"Siwicki","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":252112,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44749,"text":"wri934215 - 1994 - Water-surface profile and flood boundaries for the computed 100-year flood, Muddy Creek, Northern Cheyenne Indian Reservation, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:57","indexId":"wri934215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"93-4215","title":"Water-surface profile and flood boundaries for the computed 100-year flood, Muddy Creek, Northern Cheyenne Indian Reservation, Montana","docAbstract":"Hydrologic and hydraulic evaluations of Muddy Creek were made to determine the magnitude of the 100-year flood and the extent of flooding that would occur as the result of this flood. Forty-three cross sections were surveyed and 14 cross sections were synthesized along a 6.7-mile reach of Muddy Creek. Data from the surveys were used to calculate the water-surface flood elevation at each cross section using a computer program (WSPRO) developed by the U.S. Geological Survey. The water-surface profile of the computed 100-year flood elevations was then drawn. The profile shows the streambed elevation and the location of one bridge, one culvert, and cross sections. The computed 100-year flood elevation at each cross section was used to delineate the width of the flood plain at that section. Flood boundaries between cross sections were interpolated using contour lines on topographic maps.","language":"ENGLISH","doi":"10.3133/wri934215","usgsCitation":"Omang, R.J., 1994, Water-surface profile and flood boundaries for the computed 100-year flood, Muddy Creek, Northern Cheyenne Indian Reservation, Montana: U.S. Geological Survey Water-Resources Investigations Report 93-4215, 1 map ; 60 x 18 cm., on sheet 76 x 95 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/wri934215.","productDescription":"1 map ; 60 x 18 cm., on sheet 76 x 95 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":168801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82055,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4215/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d60","contributors":{"authors":[{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":230364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21514,"text":"ofr94115 - 1994 - Activities, programs, and cooperating agencies of the U.S. Geological Survey, Water Resources Division, Massachusetts and Rhode Island, 1994","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr94115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-115","title":"Activities, programs, and cooperating agencies of the U.S. Geological Survey, Water Resources Division, Massachusetts and Rhode Island, 1994","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr94115","usgsCitation":"Yurewicz, M., 1994, Activities, programs, and cooperating agencies of the U.S. Geological Survey, Water Resources Division, Massachusetts and Rhode Island, 1994: U.S. Geological Survey Open-File Report 94-115, 2 p. ;28 cm., https://doi.org/10.3133/ofr94115.","productDescription":"2 p. ;28 cm.","costCenters":[],"links":[{"id":153088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0115/report-thumb.jpg"},{"id":51091,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0115/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c52","contributors":{"authors":[{"text":"Yurewicz, M.C.","contributorId":40237,"corporation":false,"usgs":true,"family":"Yurewicz","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":184575,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70017078,"text":"70017078 - 1994 - The use of slug tests to describe vertical variations in hydraulic conductivity","interactions":[],"lastModifiedDate":"2024-10-23T11:09:46.881574","indexId":"70017078","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"The use of slug tests to describe vertical variations in hydraulic conductivity","docAbstract":"The Porco Ag-Zn-Pb-Sn deposit, a major Ag producer in the 16th century and currently the major Zn producer in Bolivia, consists of a swarm of fissure-filling veins in the newly recognized Porco caldera. The caldera measures 5 km north-south by 3 km east-west and formed in response to the eruption of the 12 Ma crystal-rich dacitic Porco Tuff. Well-defined topographic walls of the caldera are cut in Ordovician and Cretaceous sedimentary rocks. The mineralization is associated with, and is probably genetically related to, the 8.6 Ma Huayna Porco stock (elev 4,528 m); the deposit is part of a system of radial dikes, metal zonation, and alteration mineral patterns centered on the stock. The outflow Porco Tuff to the north underlies the 6 to 9 Ma ash-flow tuffs of the Los Frailes volcanic field.The Porco deposit consists of steeply dipping irregular and curvilinear veins that cut the intracaldera Porco Tuff about 1 km east of the Huayna Porco stock. Major veins are generally less than a meter wide and as much as 2 km long. Most of the veins, especially the most productive ones, together with a small stock, dike, and breccia pipe, are aligned along the structural margin (ring fracture) of the caldera. The ore deposit is zoned around the Huayna Porco stock--cassiterite is generally close to the stock, and base metals, mostly as sphalerite and galena, are farther away, along the ring fracture veins. The primary Ag minerals, chiefly pyragyrite, acanthite, and stephanite, are most abundant in the upper parts of the veins.Fluid inclusions in sphalerite stalactites have homogenization temperatures of about 225 degrees C and salinities of about 8 wt percent NaCl equiv. The stalactites and the presence of sparse vapor-rich inclusions suggest deposition of sphalerite under boiling conditions. Modeling the depth of formation below the water table indicates that the present ground surface is close to the surface that existed at the time of mineralization.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.89.8.1833","issn":"03610128","usgsCitation":"Cunningham, C.G., Aparicio N., H., Murillo S., F., Jimenez, N.C., Lizeca B., J.L., McKee, E.H., Ericksen, G., and Tavera V., F., 1994, Relationship between the Porco, Bolivia, Ag-Zn-Pb-Sn deposit and the Porco Caldera: Economic Geology, v. 89, no. 8, p. 1833-1841, https://doi.org/10.2113/gsecongeo.89.8.1833.","productDescription":"9 p.","startPage":"1833","endPage":"1841","numberOfPages":"9","costCenters":[],"links":[{"id":228700,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"8","noUsgsAuthors":false,"publicationDate":"1994-12-01","publicationStatus":"PW","scienceBaseUri":"50e4a762e4b0e8fec6cdc42f","contributors":{"authors":[{"text":"Cunningham, Charles G.","contributorId":85940,"corporation":false,"usgs":true,"family":"Cunningham","given":"Charles","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":376290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aparicio N., Hugo","contributorId":69410,"corporation":false,"usgs":true,"family":"Aparicio N.","given":"Hugo","email":"","affiliations":[],"preferred":false,"id":891347,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murillo S., Fernando","contributorId":32398,"corporation":false,"usgs":true,"family":"Murillo S.","given":"Fernando","email":"","affiliations":[],"preferred":false,"id":891348,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jimenez, Nestor C.","contributorId":86221,"corporation":false,"usgs":true,"family":"Jimenez","given":"Nestor","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":891349,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lizeca B., J. L.","contributorId":107560,"corporation":false,"usgs":true,"family":"Lizeca B.","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":891350,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":891351,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ericksen, George E.","contributorId":54651,"corporation":false,"usgs":true,"family":"Ericksen","given":"George E.","affiliations":[],"preferred":false,"id":891352,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Tavera V., Franz","contributorId":61293,"corporation":false,"usgs":true,"family":"Tavera V.","given":"Franz","email":"","affiliations":[],"preferred":false,"id":891353,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":19737,"text":"ofr9454 - 1994 - Selected ground-water data for Yucca Mountain region, southern Nevada and eastern California, through December 1992","interactions":[],"lastModifiedDate":"2022-06-30T20:35:32.577105","indexId":"ofr9454","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-54","title":"Selected ground-water data for Yucca Mountain region, southern Nevada and eastern California, through December 1992","docAbstract":"Tne U.S. Geological Survey. in support of the U.S. Department of Energy, Yucca Mountain Site- Characterization Project, collects, compiles, and summarizes water-resource data in the Yucca Mountain region. The data are collected to document the historical and current condition of ground-water resources, to detect and document changes in those resources through time, and to allow assessments of ground-water resources during investigations to determine the potential suitability of Yucca Mountain for storing high-level nuclear waste. Data on ground-water levels at 36 sites, ground- water discharge at 6 sites, ground-water quality at 19 sites, and ground-water withdrawals within Crater Fiat, Jackass Flats, Mercury Valley, and the Amargosa Desert are presented. Data on ground-water levels, discharges, and withdrawals collected by other agencies or as part of other programs are included to further indicate variations through time. A statistical summary of ground-water levels and median annual ground-water withdrawals in Jackass Flats is presented. The statistical summary includes the number of measurements, the maximum, minimum, and median water-level altitudes, and the average deviation of a11 water-level altitudes for selected baseline periods and for calendar year 1992. Data on ground-water quality are compared to established, proposed, or tentative primary and secondary drinking-water standards, and measures which exceeded those standards are listed for 18 sites. Detected organic compounds for which established, proposed, or tentative drinking-water standards exist also are listed.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9454","usgsCitation":"La Camera, R.J., and Westenburg, C.L., 1994, Selected ground-water data for Yucca Mountain region, southern Nevada and eastern California, through December 1992: U.S. Geological Survey Open-File Report 94-54, Report: 161 p.; 1 Plate: 16.92 × 11.82 inches, https://doi.org/10.3133/ofr9454.","productDescription":"Report: 161 p.; 1 Plate: 16.92 × 11.82 inches","costCenters":[],"links":[{"id":402788,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12448.htm"},{"id":264551,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0054/report-thumb.jpg"},{"id":264550,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0054/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49211,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0054/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Nevada","otherGeospatial":"Yucca Mountain region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117,\n 36.267\n ],\n [\n -116,\n 36.267\n ],\n [\n -116,\n 37\n ],\n [\n -117,\n 37\n ],\n [\n -117,\n 36.267\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68647a","contributors":{"authors":[{"text":"La Camera, Richard J.","contributorId":52212,"corporation":false,"usgs":true,"family":"La Camera","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":181420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Westenburg, Craig L.","contributorId":63831,"corporation":false,"usgs":true,"family":"Westenburg","given":"Craig","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":181421,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6027,"text":"pp1044L - 1994 - Hydrothermal systems of the Cascade Range, north-central Oregon","interactions":[{"subject":{"id":19504,"text":"ofr9169 - 1991 - Hydrothermal systems of the Cascade Range, north-central Oregon","indexId":"ofr9169","publicationYear":"1991","noYear":false,"title":"Hydrothermal systems of the Cascade Range, north-central Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":6027,"text":"pp1044L - 1994 - Hydrothermal systems of the Cascade Range, north-central Oregon","indexId":"pp1044L","publicationYear":"1994","noYear":false,"chapter":"L","title":"Hydrothermal systems of the Cascade Range, north-central Oregon"},"id":1}],"lastModifiedDate":"2025-04-18T13:38:36.82201","indexId":"pp1044L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1044","chapter":"L","title":"Hydrothermal systems of the Cascade Range, north-central Oregon","docAbstract":"Quaternary volcanoes of the Cascade Range form a 1,200- kilometer-long arc that extends from southern British Columbia to northern California. The section of the Cascade Range volcanic arc in central Oregon is characterized by relatively high Quaternary volcanic extrusion rates and hot-spring discharge rates. Stableisotope data and measurements of hot-spring heat discharge indicate that gravity-driven thermal fluid circulation transports about 1 MW (megawatt) of heat per kilometer of arc length from the Quaternary arc into Western Cascade rocks older than about 7 Ma (millions of years before present). Inferred flow-path lengths for the Na-Ca-Cl thermal waters of the Western Cascades are 10 to 40 kilometers (km), and an average topographic gradient as large as 0.1 separates the inferred recharge areas from the hot-spring groups. Thermal-fluid residence times are probably 102 to 104 years: sulfate-water isotopic equilibrium indicates residence times of more than 102 years, and our interpretation of stable-isotope data implies residence times of less than 104 years.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1044L","usgsCitation":"Ingebritsen, S.E., Mariner, R.H., and Sherrod, D.R., 1994, Hydrothermal systems of the Cascade Range, north-central Oregon: U.S. Geological Survey Professional Paper 1044, Document: iv, 86 p.; 2 Plates: 15.0 x 23.0 inches, https://doi.org/10.3133/pp1044L.","productDescription":"Document: iv, 86 p.; 2 Plates: 15.0 x 23.0 inches","numberOfPages":"91","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":484688,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4700.htm","linkFileType":{"id":5,"text":"html"}},{"id":32975,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044l/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32976,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1044l/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118179,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1044l/report-thumb.jpg"},{"id":32974,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Cascade Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.9,\n 45.4197\n ],\n [\n -122.9,\n 43.6167\n ],\n [\n -120.8078,\n 43.6167\n ],\n [\n -120.8078,\n 45.4197\n ],\n [\n -122.9,\n 45.4197\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc2de","contributors":{"authors":[{"text":"Ingebritsen, S. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr93648","usgsCitation":"Kleeschulte, M., and Imes, J., 1994, Geohydrology, water quality, and simulation of ground-water flow at the Weldon Spring chemical plant and vicinity, St. Charles County, Missouri, 1987-90: U.S. Geological Survey Open-File Report 93-648, vi, 106 p., https://doi.org/10.3133/ofr93648.","productDescription":"vi, 106 p.","costCenters":[],"links":[{"id":411079,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12787.htm","linkFileType":{"id":5,"text":"html"}},{"id":49129,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0648/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152159,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0648/report-thumb.jpg"}],"country":"United States","state":"Missouri","otherGeospatial":"Weldon Spring chemical plant","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -90.51429779606438,\n 38.803136761049814\n ],\n [\n -90.78968096118078,\n 38.803136761049814\n ],\n [\n -90.78968096118078,\n 38.594377092401174\n ],\n [\n -90.51429779606438,\n 38.594377092401174\n ],\n [\n -90.51429779606438,\n 38.803136761049814\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8760","contributors":{"authors":[{"text":"Kleeschulte, M. 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L.","affiliations":[],"preferred":false,"id":181297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19873,"text":"ofr9442 - 1994 - Report on the U.S. Geological Survey's evaluation program for standard reference samples distributed in October 1993 : T-127 (trace constituents), M-128 (major constituents), N-40 (nutrients), N-41 (nutrients), P-21 (low ionic strength), Hg-17 (mercury), AMW-3 (acid mine water), and WW-1 (whole water)","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr9442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-42","title":"Report on the U.S. Geological Survey's evaluation program for standard reference samples distributed in October 1993 : T-127 (trace constituents), M-128 (major constituents), N-40 (nutrients), N-41 (nutrients), P-21 (low ionic strength), Hg-17 (mercury), AMW-3 (acid mine water), and WW-1 (whole water)","docAbstract":"This report presents the results of the U.S. Geological Survey's analytical evaluation program for eight standard reference samples--T-127 (trace constituents), M-128 (major constituents), N-40 (nutrients), N-41 (nutrients), P-21 (low ionic strength), Hg-17 (mercury), AMW-3 (acid mine water), and WW-1 (whole water)--that were distributed in October 1993 to 158 laboratories registered in the U.S. Geological Survey sponsored interlaboratory testing program. Analytical data that were received from 145 of the laboratories were evaluated with respect to: overall laboratory performance and relative laboratory performance for each analyte in the eight reference samples. Results of these evaluations are presented in tabular form. Also presented are tables and graphs summarizing the analytical data provided by each laboratory for each analyte in the eight standard reference samples. The most probable value for each analyte was determined using nonparametric statistics.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr9442","usgsCitation":"Long, H., and Farrar, J., 1994, Report on the U.S. Geological Survey's evaluation program for standard reference samples distributed in October 1993 : T-127 (trace constituents), M-128 (major constituents), N-40 (nutrients), N-41 (nutrients), P-21 (low ionic strength), Hg-17 (mercury), AMW-3 (acid mine water), and WW-1 (whole water): U.S. Geological Survey Open-File Report 94-42, iii, 177 p. :ill. ;28 cm., https://doi.org/10.3133/ofr9442.","productDescription":"iii, 177 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153414,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0042/report-thumb.jpg"},{"id":49383,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0042/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610ef6","contributors":{"authors":[{"text":"Long, H.K.","contributorId":50547,"corporation":false,"usgs":true,"family":"Long","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":181671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrar, J.W.","contributorId":26715,"corporation":false,"usgs":true,"family":"Farrar","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":181670,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19842,"text":"ofr9462 - 1994 - Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory-Extraction of nitroaromatic compounds from water by polystyrene divinylbenzene cartridge and determination by high-performance liquid chromatography","interactions":[],"lastModifiedDate":"2021-05-28T18:05:08.775834","indexId":"ofr9462","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","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":"94-62","title":"Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory-Extraction of nitroaromatic compounds from water by polystyrene divinylbenzene cartridge and determination by high-performance liquid chromatography","docAbstract":"Organic explosives are determined in samples of ground water and surface water with emphasis on identifying and quantifying trinitrotoluene (TNT) metabolites. Water samples are filtered to remove suspended particulate material and passed through a polystyrene divinylbenzene-packed cartridge by a vacuum-extraction system. The target analytes subsequently are eluted with acetonitrile. A high-performance liquid chromatograph (HPLC) equipped with a photodiode-array detector is used for sample analysis. Analytes are separated on an octadecylsilane column using a methanol, water, and acetonitrile gradient elution. The compounds 2,4- and 2,6-dinitrotoluene are separated through an independent, isocratic elution. Method detection limits, on the basis of a 1-liter sample size, range from 0.11 to 0.32 microgram per liter. Recoveries averaged from 71 to 101 percent for 13 analytes in one set of HPLC-grade water fortified at about 1 microgram per liter. The method is limited to use by analysts experienced in handling explosive materials. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9462","usgsCitation":"Lindley, C., Burkhardt, M., and DeRusseau, S., 1994, Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory-Extraction of nitroaromatic compounds from water by polystyrene divinylbenzene cartridge and determination by high-performance liquid chromatography: U.S. Geological Survey Open-File Report 94-62, iv, 15 p., https://doi.org/10.3133/ofr9462.","productDescription":"iv, 15 p.","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":152401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0062/report-thumb.jpg"},{"id":49323,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0062/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bc1f","contributors":{"authors":[{"text":"Lindley, C.E.","contributorId":55031,"corporation":false,"usgs":true,"family":"Lindley","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":181614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burkhardt, M.R.","contributorId":70410,"corporation":false,"usgs":true,"family":"Burkhardt","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":181615,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeRusseau, S.N.","contributorId":31784,"corporation":false,"usgs":true,"family":"DeRusseau","given":"S.N.","affiliations":[],"preferred":false,"id":181613,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70195437,"text":"70195437 - 1994 - Secondary minerals and acid mine-water chemistry","interactions":[],"lastModifiedDate":"2018-09-12T08:18:26","indexId":"70195437","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesTitle":{"id":5629,"text":"Mineralogical Association of Canada Short Course Volumes","active":true,"publicationSubtype":{"id":24}},"seriesNumber":"22","title":"Secondary minerals and acid mine-water chemistry","docAbstract":"No abstract available.
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