{"pageNumber":"1341","pageRowStart":"33500","pageSize":"25","recordCount":46734,"records":[{"id":22139,"text":"ofr95673 - 1994 - Sediment magnetic and paleomagnetic data from Buck Lake, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr95673","displayToPublicDate":"1996-07-01T00:00:00","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":"95-673","title":"Sediment magnetic and paleomagnetic data from Buck Lake, Oregon","docAbstract":"Sediment magnetic and paleomagnetic studies were conducted on a core from Buck Lake, Klamath County, Oregon, that was collected as part of an investigation into the Quaternary climate history of the western United States. This report documents the methods used to obtain paleomagnetic directions, magnetic properties, and ancillary data, and presents these data in tabular form. Adam (1993) and Adam and others (1994) describe the site, the drilling methods, and lithology of the lacustrine sediments. Rosenbaum and others (1994) present preliminary interpretations of the sediment magnetic data and show that variations in magnetic properties closely reflect changes in climate as interpreted from the pollen record.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr95673","issn":"0094-9140","usgsCitation":"Rosenbaum, J.G., Reynolds, R.L., Fitzmaurice, P., Drexler, J., Whitney, C., and Adam, D., 1994, Sediment magnetic and paleomagnetic data from Buck Lake, Oregon (Version 1.0): U.S. Geological Survey Open-File Report 95-673, 46 p.; 28 cm., https://doi.org/10.3133/ofr95673.","productDescription":"46 p.; 28 cm.","costCenters":[],"links":[{"id":154997,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0673/report-thumb.jpg"},{"id":7864,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-673/","linkFileType":{"id":5,"text":"html"}},{"id":51587,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0673/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6864b8","contributors":{"authors":[{"text":"Rosenbaum, J. G.","contributorId":96685,"corporation":false,"usgs":true,"family":"Rosenbaum","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":187287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, R. L. 0000-0002-4572-2942","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":79885,"corporation":false,"usgs":true,"family":"Reynolds","given":"R.","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":187285,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fitzmaurice, P.L.","contributorId":50555,"corporation":false,"usgs":true,"family":"Fitzmaurice","given":"P.L.","email":"","affiliations":[],"preferred":false,"id":187284,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Drexler, J.W.","contributorId":39407,"corporation":false,"usgs":true,"family":"Drexler","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":187283,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Whitney, C.G.","contributorId":86361,"corporation":false,"usgs":true,"family":"Whitney","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":187286,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Adam, D.P.","contributorId":14815,"corporation":false,"usgs":true,"family":"Adam","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":187282,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":18594,"text":"ofr94122 - 1994 - Hydrologic, water-quality, and meteorologic data for Newberry Volcano and vicinity, Deschutes County, Oregon, 1991-93","interactions":[],"lastModifiedDate":"2017-02-07T09:53:50","indexId":"ofr94122","displayToPublicDate":"1996-04-01T00:00:00","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":"94-122","title":"Hydrologic, water-quality, and meteorologic data for Newberry Volcano and vicinity, Deschutes County, Oregon, 1991-93","docAbstract":"This report is a compilation of hydrologic, water- quality, and meteorologic data collected in the vicinity of Newberry Volcano near Bend, Oregon. These data were collected, in cooperation with the Bonneville Power Administration, the U.S. Forest Service, and the Bureau of Land Management, to provide baseline data for identifying and assessing the effects of proposed geothermal development in the vicinity of Newberry Volcano. Types of data collected include ground-water levels, lake levels, streamflow, water quality, and meteorologic measurements. Sites that were monitored include: (1) two thermal wells in the caldera, (2) several nonthermal wells in the caldera, (3) four wells outside of the caldera, (4) Paulina Creek, (5) Paulina and East Lakes, (6) hot springs that discharge into Paulina and East Lakes, and (7) meteorologic conditions near Paulina Lake. Data are presented for the period summer 1991 through fall 1993. Water-quality data collected include concentrations of common anions and cations, nutrients, trace elements, radiochemicals, and isotopes. Meteorologic data collected include wind velocity, air temperature, humidity, solar radiation, and precipitation.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94122","usgsCitation":"Crumrine, M.D., and Morgan, D.S., 1994, Hydrologic, water-quality, and meteorologic data for Newberry Volcano and vicinity, Deschutes County, Oregon, 1991-93: U.S. Geological Survey Open-File Report 94-122, 70 p, https://doi.org/10.3133/ofr94122.","productDescription":"70 p","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":150669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0122/report-thumb.jpg"},{"id":47942,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0122/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688aa1","contributors":{"authors":[{"text":"Crumrine, Milo D.","contributorId":68757,"corporation":false,"usgs":true,"family":"Crumrine","given":"Milo","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":179401,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, David S.","contributorId":73181,"corporation":false,"usgs":true,"family":"Morgan","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":179402,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44743,"text":"wri934164 - 1994 - Delineation of saltwater intrusion in the Biscayne aquifer, eastern Broward County, Florida, 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:10:55","indexId":"wri934164","displayToPublicDate":"1996-03-01T00:00:00","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":"93-4164","title":"Delineation of saltwater intrusion in the Biscayne aquifer, eastern Broward County, Florida, 1990","docAbstract":"Chloride concentrations in water samples from 63 saltwater monitoring wells in eastern Broward County were used to delineate the areal extent of 1,000 milligrams per liter of chloride concentration from the Biscayne aquifer. The 1990 landward extent of saltwater intrusion and data for 1980 and 1990 for each monitoring well are presented. The results of the study indicate that chloride concentrations in ground water east of major well fields have increased and that the saltwater-freshwater interface has moved landward from 1980 to 1990 in response to lowered regional water levels. This lowering of water levels is the result of the construction of tidal canals and the withdrawal of water from well fields. Historical data from three monitoring wells (G-1237, G-1435, and G-20555) were analyzed to determine trends in chloride concen- tration as a function of time. Samples from wells G-1435 and G-2055 indicate that the chloride concentrations have increased steadily with declines of regional water levels, whereas data from well G-1237 indicate that a decrease in pumpage can reverse saltwater intrusion.","language":"ENGLISH","doi":"10.3133/wri934164","usgsCitation":"Koszalka, E.J., 1994, Delineation of saltwater intrusion in the Biscayne aquifer, eastern Broward County, Florida, 1990: U.S. Geological Survey Water-Resources Investigations Report 93-4164, 2 maps on 1 sheet ; 44 x 21 cm., sheet 76 x 74 cm., folded to 19 x 19 cm., in envelope 31 x 23 cm., https://doi.org/10.3133/wri934164.","productDescription":"2 maps on 1 sheet ; 44 x 21 cm., sheet 76 x 74 cm., folded to 19 x 19 cm., in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":167889,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":82051,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4164/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab3e4b07f02db66f83b","contributors":{"authors":[{"text":"Koszalka, Edward J.","contributorId":47850,"corporation":false,"usgs":true,"family":"Koszalka","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":230355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23869,"text":"ofr94492 - 1994 - Documentation of hydrochemical-facies data and ranges of dissolved-solids concentrations for the northern Atlantic Coastal Plain aquifer system, New Jersey, Delaware, Maryland, Virginia and North Carolina supplement to Professional paper 1404-L","interactions":[],"lastModifiedDate":"2017-01-04T11:41:23","indexId":"ofr94492","displayToPublicDate":"1996-03-01T00:00:00","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":"94-492","title":"Documentation of hydrochemical-facies data and ranges of dissolved-solids concentrations for the northern Atlantic Coastal Plain aquifer system, New Jersey, Delaware, Maryland, Virginia and North Carolina supplement to Professional paper 1404-L","docAbstract":"Hydrochemical-facies data and ranges of dissolved- solids concentrations used to construct hydrochemical-facies maps and sections for U.S. Geological Survey Professional Paper 1404-L have not been previously published. In this report, the data are contained on a 3-1/2 high-density diskette in a file presented in American International Standard Code for Information Exchange (ASCII) format. The file requires about 0.2 megabyte of disk space on an IBM-compatible microcomputer using the MS-DOS operating system.","language":"ENGLISH","publisher":"U.S. Geological Survey ;Can be purchased from U.S. Geological Survey Earth Science Information Center, Open-file Reports Section","doi":"10.3133/ofr94492","issn":"0094-9140","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Meisler, H., and Knobel, L., 1994, Documentation of hydrochemical-facies data and ranges of dissolved-solids concentrations for the northern Atlantic Coastal Plain aquifer system, New Jersey, Delaware, Maryland, Virginia and North Carolina supplement to Professional paper 1404-L: U.S. Geological Survey Open-File Report 94-492, 9 p. 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr94492.","productDescription":"9 p. 1 computer disk ;3 1/2 in.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":29548,"text":"wri944130 - 1994 - Selected nutrients in stormwater runoff from Davenport, Iowa, 1992","interactions":[],"lastModifiedDate":"2016-03-14T12:03:59","indexId":"wri944130","displayToPublicDate":"1995-12-01T00:00:00","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":"94-4130","title":"Selected nutrients in stormwater runoff from Davenport, Iowa, 1992","docAbstract":"<p>Flow-weighted composite samples of stormwater runoff from areas of different land use in Davenport, Iowa, were collected in the summer and fall of 1992 and analyzed for selected nutrients. Annual constituent loads were estimated for the area drained by the Davenport storm-sewer network. In all cases, the regression-equation estimate of mean annual load is less than the estimate obtained by using the method of the U.S. Environmental Protection Agency. The largest mean annual loads for total nitrite nitrogen, total nitrate nitrogen, total nitrite and nitrate nitrogen, total organic nitrogen, total ammonia and organic nitrogen, total nitrogen, and total phosphorus are associated with residential land, which covers 67.2 percent of the area drained.</p>\n<p>Using concentration data from this study, it is estimated that an average storm-producing runoff during the 7-day, 10-year low-flow discharge of the Mississippi River would contribute about 4 percent of the total ammonia and organic nitrogen load in the river. Precipitation-chemistry data indicate that substantial parts of the nitrate nitrogen and ammonia nitrogen contained in the stormwater runoff could be from precipitation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City, IA","doi":"10.3133/wri944130","collaboration":"Prepared in cooperation with the City of Davenport, Iowa","usgsCitation":"Schaap, B., and Lucey, K., 1994, Selected nutrients in stormwater runoff from Davenport, Iowa, 1992: U.S. Geological Survey Water-Resources Investigations Report 94-4130, iv, 29 p.: ill., maps; 28 cm., https://doi.org/10.3133/wri944130.","productDescription":"iv, 29 p.: ill., maps; 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":159941,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4130/report-thumb.jpg"},{"id":58377,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4130/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa","city":"Davenport","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.48820495605467,\n              41.51834634058004\n            ],\n            [\n              -90.516357421875,\n              41.5198886863019\n            ],\n            [\n              -90.538330078125,\n              41.52554363946853\n            ],\n            [\n              -90.56442260742188,\n              41.519374575145406\n            ],\n            [\n              -90.57952880859375,\n              41.51371908287346\n            ],\n            [\n              -90.59532165527344,\n              41.5070346821719\n            ],\n            [\n              -90.60218811035156,\n              41.494692436865364\n            ],\n            [\n              -90.62278747558594,\n              41.482862244540875\n            ],\n            [\n              -90.6427001953125,\n              41.47154438707647\n            ],\n            [\n              -90.65437316894531,\n              41.46125371076149\n            ],\n            [\n              -90.66810607910156,\n              41.46125371076149\n            ],\n            [\n              -90.67222595214844,\n              41.61236215526601\n            ],\n            [\n              -90.49095153808594,\n              41.61236215526601\n            ],\n            [\n              -90.48820495605467,\n              41.51834634058004\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b174","contributors":{"authors":[{"text":"Schaap, B.D.","contributorId":56249,"corporation":false,"usgs":true,"family":"Schaap","given":"B.D.","email":"","affiliations":[],"preferred":false,"id":201699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lucey, K.J.","contributorId":70002,"corporation":false,"usgs":true,"family":"Lucey","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":201700,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17135,"text":"ofr92657 - 1994 - Geohydrologic data collected from shallow neutron-access boreholes and resultant-preliminary geohydrologic evaluations, Yucca Mountain area, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:19","indexId":"ofr92657","displayToPublicDate":"1995-12-01T00:00:00","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":"92-657","title":"Geohydrologic data collected from shallow neutron-access boreholes and resultant-preliminary geohydrologic evaluations, Yucca Mountain area, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr92657","usgsCitation":"Blout, D.O., Hammermeister, D., Loskot, C., and Chornack, M., 1994, Geohydrologic data collected from shallow neutron-access boreholes and resultant-preliminary geohydrologic evaluations, Yucca Mountain area, Nye County, Nevada: U.S. Geological Survey Open-File Report 92-657, v, 147 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr92657.","productDescription":"v, 147 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":150409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1992/0657/report-thumb.jpg"},{"id":46258,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1992/0657/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f47","contributors":{"authors":[{"text":"Blout, Daniel O.","contributorId":55843,"corporation":false,"usgs":true,"family":"Blout","given":"Daniel","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":175100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hammermeister, D.P.","contributorId":27066,"corporation":false,"usgs":true,"family":"Hammermeister","given":"D.P.","affiliations":[],"preferred":false,"id":175099,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loskot, C. L.","contributorId":79910,"corporation":false,"usgs":true,"family":"Loskot","given":"C. L.","affiliations":[],"preferred":false,"id":175101,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chornack, Michael P.","contributorId":106902,"corporation":false,"usgs":true,"family":"Chornack","given":"Michael P.","affiliations":[],"preferred":false,"id":175102,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26045,"text":"wri934122 - 1994 - A comparison of simultaneous plasma, atomic absorption, and iron colorimetric determinations of major and trace constituents in acid mine waters","interactions":[],"lastModifiedDate":"2020-04-12T14:17:47.662418","indexId":"wri934122","displayToPublicDate":"1995-12-01T00:00:00","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":"93-4122","title":"A comparison of simultaneous plasma, atomic absorption, and iron colorimetric determinations of major and trace constituents in acid mine waters","docAbstract":"Sixty-three water samples collected during June to October 1982 from the Leviathan/Bryant Creek drainage basin were originally analyzed by simultaneous multielement direct-current plasma (DCP) atomic-emission spectrometry, flame atomic-absorption spectrometry, graphite-furnace atomic-absorption spectrometry (GFAAS) (thallium only), ultraviolet-visible spectrometry, and hydride-generation atomic-absorption spectrometry.Determinations were made for the following metallic and semi-metallic constituents: AI, As, B, Ba, Be, Bi, Cd, Ca, Cr, Co, Cu, Fe(11), Fe(total), Li, Pb, Mg, Mn, Mo, Ni, K, Sb, Se, Si, Na, Sr, TI, V, and Zn. These samples were re-analyzed later by simultaneous multielement inductively coupled plasma (ICP) atomic-emission spectrometry and Zeeman-corrected GFAAS to determine the concentrations of many of the same constituents with improved accuracy, precision, and sensitivity. The result of this analysis has been the generation of comparative concentration values for a significant subset of the solute constituents. Many of the more recently determined values replace less-than-detection values for the trace metals; others constitute duplicate analyses for the major constituents. The multiple determinations have yielded a more complete, accurate, and precise set of analytical data. They also have resulted in an opportunity to compare the performance of the plasma-emission instruments operated in their respective simultaneous multielement modes.  Flame atomic-absorption spectrometry was judged best for Na and K and hydride-generation atomic-absorption spectrometry was judged best for As because of their lower detection limit and relative freedom from interelement spectral effects. Colorimetric determination using ferrozine as the color agent was judged most accurate, precise, and sensitive for Fe. Cadmium, lead, and vanadium concentrations were too low in this set of samples to enable a determination of whether ICP or DCP is a more suitable technique. Of the remaining elements, Ba, Be, Ca, Cr, Mg, Mn, Sr, and Zn have roughly equivalent accuracy, precision, and detection limit by ICP and DCP. Cobalt and Ni were determined to be better analyzed by ICP, because of lower detection limits; B, Cu, Mo, and Si were determined to be better analyzed by DCP, because of relative freedom from interferences. The determination oral by DCP was far more sensitive, owing to the use of a more sensitive wavelength, compared with the ICP. However, there is a very serious potential interference from a strong Ca emission line near the 396.15 nanometer DCP wavelength. Thus, there is no clear choice between the plasma techniques tested, for the determination oral. The ICP and DCP detection limits are typically between 0.001 and 0.5 milligrams per liter in acid mine waters. For those metals best analyzed by ICP and/or DCP, but below these limits, GFAAS is the method of choice because of its relatively greater sensitivity and specificity. Six of the elements were not determined by DCP, ICP or Zeeman-corrected GFAAS, and are not discussed in this report. These elements are: Bi, Fe(11), Li, Sb, Se, and TI.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934122","usgsCitation":"Ball, J., and Nordstrom, D.K., 1994, A comparison of simultaneous plasma, atomic absorption, and iron colorimetric determinations of major and trace constituents in acid mine waters: U.S. Geological Survey Water-Resources Investigations Report 93-4122, viii, 151 p. , https://doi.org/10.3133/wri934122.","productDescription":"viii, 151 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":54822,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4122/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4122/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0f56","contributors":{"authors":[{"text":"Ball, J.W.","contributorId":67507,"corporation":false,"usgs":true,"family":"Ball","given":"J.W.","affiliations":[],"preferred":false,"id":195705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":195706,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31723,"text":"ofr9347 - 1994 - Physical characteristics of stream subbasins in the Pomme de Terre River Basin, west-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T09:55:56","indexId":"ofr9347","displayToPublicDate":"1995-11-01T00:00:00","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":"93-47","title":"Physical characteristics of stream subbasins in the Pomme de Terre River Basin, west-central Minnesota","docAbstract":"<p>Data describing the physical characteristics of stream subbasins upstream from selected points on streams in the Pomme de Terre River Basin, located in west-central Minnesota, are presented in this report. The physical characteristics are the drainage area of the subbasin, the percentage area of the subbasin covered only by lakes, the percentage area of the subbasin covered by both lakes and wetlands, the main-channel length, and the main-channel slope. The points on the stream include outlets of subbasins of at least 5 square miles, outfalls of sewage treatment plants, and locations of U.S. Geological Survey low-flow, high-flow, and continuous-record gaging stations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr9347","collaboration":"Prepared in cooperation with Minnesota Department of Transportation and U.S. Army Corps of Engineers","usgsCitation":"Lorenz, D., and Payne, G.A., 1994, Physical characteristics of stream subbasins in the Pomme de Terre River Basin, west-central Minnesota: U.S. Geological Survey Open-File Report 93-47, Document: 8 p.; Plate: 24.03 x 46.44 inches, https://doi.org/10.3133/ofr9347.","productDescription":"Document: 8 p.; Plate: 24.03 x 46.44 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":59948,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1993/0047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1993/0047/report-thumb.jpg"},{"id":59949,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1993/0047/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Pomme de Terre River basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.78155517578124, 46.01460818253508 ], [ -95.76644897460936, 46.02223738582996 ], [ -95.73623657226562, 46.03177240968806 ], [ -95.71632385253906, 46.038922598236 ], [ -95.71357727050781, 46.04750160330395 ], [ -95.701904296875, 46.052743672805086 ], [ 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L.","contributorId":10776,"corporation":false,"usgs":true,"family":"Lorenz","given":"D. L.","affiliations":[],"preferred":false,"id":206813,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Payne, G. A.","contributorId":62190,"corporation":false,"usgs":true,"family":"Payne","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":206814,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29562,"text":"wri944213 - 1994 - Sources of trends in water-quality data for selected streams in Texas, 1975-89 water years","interactions":[],"lastModifiedDate":"2016-08-16T14:32:49","indexId":"wri944213","displayToPublicDate":"1995-11-01T00:00:00","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":"94-4213","title":"Sources of trends in water-quality data for selected streams in Texas, 1975-89 water years","docAbstract":"<p>Sources of trends in water-quality data for selected streams in Texas for the 1975-89 water years were investigated in this study. The investigation of sources was confined to distinct geographic patterns in the trend indicators for one constituent or for a group of related constituents.</p>\n<p>The probable source of trend patterns in nutrients and measures of oxygen in the Trinity River Basin was changes in the wastewater treatment facilities in the Dallas-Fort Worth metropolitan area. A pattern of increased concentrations of inorganic constituents in the upper Colorado River Basin resulted from emergency releases of water from the Natural Darn Lake, a salinity control structure. Trend patterns in inorganic constituents in the Rio Grande Basin were a result of increasing concentrations in the Pecos River and, to a lesser extent, the Rio Grande above the Amistad Reservoir, combined with the effects of reservoir regulation. A pattern of increasing concentrations of organic plus ammonia nitrogen and ammonia nitrogen was detected for the 1975-86 water years for stations with low concentrations (generally less than 5 milligrams per liter) of these nitrogen species. The trends were no longer evident when the period of trend analysis was extended to the 1989 water year. A positive bias in the data caused by the addition of mercuric chloride tablets to preserve nutrient samples during 1980-86 was the probable source of this trend pattern. A pattern of increasing concentrations in dissolved sulfate in the eastern part of the State was a result of a positive bias in the analytical results of a turbidimetric method of sulfate analysis. The source of a statewide pattern of increased pH in streams could not be identified.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri944213","usgsCitation":"Schertz, T., Wells, F., and Ohe, D., 1994, Sources of trends in water-quality data for selected streams in Texas, 1975-89 water years: U.S. Geological Survey Water-Resources Investigations Report 94-4213, v, 49 p., https://doi.org/10.3133/wri944213.","productDescription":"v, 49 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":160468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4213/report-thumb.jpg"},{"id":58390,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4213/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":19043,"text":"ofr94508 - 1994 - Hydrologic data from the study of acidic contamination in the Miami Wash-Pinal Creek area, Arizona, water years 1992-93","interactions":[],"lastModifiedDate":"2019-12-08T13:33:42","indexId":"ofr94508","displayToPublicDate":"1995-11-01T00:00:00","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":"94-508","title":"Hydrologic data from the study of acidic contamination in the Miami Wash-Pinal Creek area, Arizona, water years 1992-93","docAbstract":"Since 1984, hydrologic data have been collected as part of a U.S. Geological Survey study of the occurrence and movement of acidic contamination in the aquifer and streams of the Pinal Creek drainage basin near Globe, Arizona. Ground-water data from that study are presented for water years 1992 and 1993 and include location, construction information, site plans, water levels, chemical and physical field measurements, and selected chemical analyses of water samples for 10 monitoring well groups. During January 1993, a flood occurred in Pinal Creek that resulted in a record peak discharge of 5,700 cubic feet per second. During this flood, well group 450 was destroyed. Surface-water data are presented for 13 sites and include discharge measurements, chemical and physical field measure- ments, and chemical analyses of water. Data from a solute-transport study that was conducted in November 1992 are presented for shallow ground-water and surface-water sites along Pinal Creek. During this study, variations in metal chemistry with distance along Pinal Creek and depth below the streambed were determined and two filter sizes were used to quantify the partitioning of metals between dissolved and particulate phases. Monthly precipi- tation data and long-term precipitation statistics are presented for two sites.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94508","usgsCitation":"Gellenbeck, D., and Hunter, Y.R., 1994, Hydrologic data from the study of acidic contamination in the Miami Wash-Pinal Creek area, Arizona, water years 1992-93: U.S. Geological Survey Open-File Report 94-508, iv, 103 p., https://doi.org/10.3133/ofr94508.","productDescription":"iv, 103 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":151896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0508/report-thumb.jpg"},{"id":48479,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0508/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":28557,"text":"wri944247 - 1994 - Tritium, stable isotopes, and nitrogen in flow from selected springs that discharge to the Snake River, Twin Falls-Hagerman area, Idaho, 1990-93","interactions":[],"lastModifiedDate":"2022-12-16T21:24:01.05473","indexId":"wri944247","displayToPublicDate":"1995-11-01T00:00:00","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":"94-4247","title":"Tritium, stable isotopes, and nitrogen in flow from selected springs that discharge to the Snake River, Twin Falls-Hagerman area, Idaho, 1990-93","docAbstract":"In 1990-93, water from 19 springs along the north side of the Snake River near Twin Falls and Hagerman contained from 9.2+0.6 to 78.4+5.1 picocuries per liter (pCi/L) of tritium. The springs were placed into three categories based on their locations and tritium concentrations: Category I was the upstream most and contained from 52.8+3.2 to 78.4+5.1 pCi/L of tritium; Category 11 was downstream from those in Category I and contained from 9.2+0.6 to 18.6+1.2 pCi/L; and Category III was the farthest downstream and contained from 28.3+1.9 to 47.7+3.2 pCi/L. Differences in tritium concentrations in the Category I, II, and III springs are a function of the ground-water flow regime, land use, and irrigation practices in and hydraulically upgradient from each category of springs. A comparatively large part of the water from the Category I springs is derived from recharge in heavily irrigated areas in which the irrigation water largely is diverted from the Snake River. A large part of the recharge for Category II springs occurs as much as 140 miles upgradient. Tritium concentrations in Category III springs indicate an intermediate proportion of the recharge is from excess applied-irrigation water. The concept that recharge from excess applied- irrigation water from the Snake River has affected tritium in the aquifer is supported by isotopic and nitrogen data. Deuterium and oxygen-18 isotopic values, and nitrite plus nitrate as nitrogen concentrations in the flow of some springs has been impacted by irrigation.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944247","usgsCitation":"Mann, L., and Low, W.H., 1994, Tritium, stable isotopes, and nitrogen in flow from selected springs that discharge to the Snake River, Twin Falls-Hagerman area, Idaho, 1990-93: U.S. Geological Survey Water-Resources Investigations Report 94-4247, iv, 21 p., https://doi.org/10.3133/wri944247.","productDescription":"iv, 21 p.","costCenters":[],"links":[{"id":410649,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48114.htm","linkFileType":{"id":5,"text":"html"}},{"id":57389,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4247/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4247/report-thumb.jpg"}],"country":"United States","state":"Idaho","city":"Hagerman, Twin Falls","otherGeospatial":"Snake River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114.3167,\n              42.5667\n            ],\n            [\n              -114.3167,\n              42.9258\n            ],\n            [\n              -114.95,\n              42.9258\n            ],\n            [\n              -114.95,\n              42.5667\n            ],\n            [\n              -114.3167,\n              42.5667\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691e06","contributors":{"authors":[{"text":"Mann, L. J.","contributorId":39392,"corporation":false,"usgs":true,"family":"Mann","given":"L. J.","affiliations":[],"preferred":false,"id":200021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Low, W. H.","contributorId":57870,"corporation":false,"usgs":true,"family":"Low","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":200022,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31722,"text":"ofr9346 - 1994 - Physical characteristics of stream subbasins in the Lac qui Parle River basin, southwestern Minnesota and eastern South Dakota","interactions":[],"lastModifiedDate":"2018-03-19T09:57:27","indexId":"ofr9346","displayToPublicDate":"1995-11-01T00:00:00","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":"93-46","title":"Physical characteristics of stream subbasins in the Lac qui Parle River basin, southwestern Minnesota and eastern South Dakota","docAbstract":"<p>Data describing the physical characteristics of stream subbasins upstream from selected points on streams in the Lac qui Parle River basin, located in southwestern Minnesota and eastern South Dakota, are presented in this report. The physical charac- teristics are the drainage area of the subbasin, the percentage area of the subbasin covered only by lakes, the percentage area of the subbasin covered by both lakes and wetlands, the main-channel length. and the main-channel slope. The points on the stream include outlets of subbasins of at least 5 square miles, outfalls of sewage treatment plants, and locations of U.S. Geological Survey low-flow, high-flow, and continuous-record gaging stations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr9346","collaboration":"Prepared in cooperation with Minnesota Department of Transportation and U.S. Army Corps of Engineers","usgsCitation":"Lorenz, D., Sanocki, C., and Winterstein, T.A., 1994, Physical characteristics of stream subbasins in the Lac qui Parle River basin, southwestern Minnesota and eastern South Dakota: U.S. Geological Survey Open-File Report 93-46, Document: 12 p.; Plate: 24.58 x 27.92 inches, https://doi.org/10.3133/ofr9346.","productDescription":"Document: 12 p.; Plate: 24.58 x 27.92 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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L.","contributorId":10776,"corporation":false,"usgs":true,"family":"Lorenz","given":"D. L.","affiliations":[],"preferred":false,"id":206810,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanocki, C. A.","contributorId":92305,"corporation":false,"usgs":true,"family":"Sanocki","given":"C. A.","affiliations":[],"preferred":false,"id":206812,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winterstein, Thomas A.","contributorId":25971,"corporation":false,"usgs":true,"family":"Winterstein","given":"Thomas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":206811,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28295,"text":"wri934204 - 1994 - Data on natural organic substances in dissolved, colloidal, suspended-silt and -clay, and bed-sediment phases in the Mississippi River and some of its tributaries, 1987-90","interactions":[],"lastModifiedDate":"2019-12-08T12:50:52","indexId":"wri934204","displayToPublicDate":"1995-10-01T00:00:00","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":"93-4204","title":"Data on natural organic substances in dissolved, colloidal, suspended-silt and -clay, and bed-sediment phases in the Mississippi River and some of its tributaries, 1987-90","docAbstract":"The Mississippi River and some of its tributaries were sampled for natural organic substances dissolved in water and in suspended and bed sediments during seven sampling cruises from 1987-90. The sampling cruises were made during different seasons, in the free-flowing reaches of the river from St. Louis, Missouri, to New Orleans, Louisiana. The first three cruises were made during low-water conditions, and the last four cruises during high-water conditions. The purpose for sampling and characterizing natural organic substances in the various phases in the river was to provide an understanding of how these substances facilitate contaminant transport and transformations in the Mississippi River.  Significant conclusions of this study were: (1) Natural organic substances appear to stabilize ' certain colloids against aggregation; therefore, these colloids remain in suspension and can act as transport agents that are not affected by sedimentation. Bacteria were found to be a significant fraction of organic colloids. (2) A new class of organic contaminants (polyethylene glycols) derived from nonionic surfactant residues was discovered dissolved with natural organic substances in water. These polyethylene glycols have the potential to affect both organic and inorganic contaminant transport in water. (3) The entire dissolved organic-matter component under varying hydrologic and seasonal conditions was characterized. (4) A method was developed to characterize organic matter in sediment by solid-state, 13C-nuclear magnetic resonance spectrometry. (5) The organic matter in suspended sediments was characterized by a variety of spectral and nonspectral methods. The protein component (significant in trace-metal binding) and lipid component (significant in organic-contaminant binding) were found to be major constituents in natural organic matter in suspended sediment. (6) Pools are reservoirs acting as traps of sedimentary organic matter of allochthonous origin and export material of autochthonous nitrogen. (7) A major portion of the mass of organic colloids in transport consisted of bacterial cells.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri934204","usgsCitation":"Leenheer, J., Noyes, T., and Brown, P., 1994, Data on natural organic substances in dissolved, colloidal, suspended-silt and -clay, and bed-sediment phases in the Mississippi River and some of its tributaries, 1987-90: U.S. Geological Survey Water-Resources Investigations Report 93-4204, vii, 71 p., https://doi.org/10.3133/wri934204.","productDescription":"vii, 71 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":123958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4204/report-thumb.jpg"},{"id":57111,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4204/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Mississippi River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.2294921875,\n              45.89000815866184\n            ],\n            [\n              -96.50390625,\n              46.07323062540835\n            ],\n            [\n              -95.185546875,\n              45.02695045318546\n            ],\n            [\n              -92.7685546875,\n              43.58039085560784\n            ],\n            [\n              -90.4833984375,\n              41.73852846935917\n            ],\n            [\n              -91.4501953125,\n              39.30029918615029\n            ],\n            [\n              -91.23046875,\n              35.137879119634185\n            ],\n            [\n              -92.0654296875,\n              31.541089879585808\n            ],\n            [\n              -91.7578125,\n              29.305561325527698\n            ],\n            [\n              -88.9892578125,\n              28.34306490482549\n            ],\n            [\n              -88.505859375,\n              30.29701788337205\n            ],\n            [\n              -90.65917968749999,\n              30.486550842588485\n            ],\n            [\n              -90.791015625,\n              32.13840869677249\n            ],\n            [\n              -89.82421875,\n              34.08906131584994\n            ],\n            [\n              -88.9453125,\n              35.96022296929667\n            ],\n            [\n              -88.9453125,\n              37.579412513438385\n            ],\n            [\n              -89.912109375,\n              39.70718665682654\n            ],\n            [\n              -89.384765625,\n              41.57436130598913\n            ],\n            [\n              -90.966796875,\n              44.05601169578525\n            ],\n            [\n              -95.2294921875,\n              45.89000815866184\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696feb","contributors":{"authors":[{"text":"Leenheer, J.A.","contributorId":75123,"corporation":false,"usgs":true,"family":"Leenheer","given":"J.A.","affiliations":[],"preferred":false,"id":199545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Noyes, T.I.","contributorId":54971,"corporation":false,"usgs":true,"family":"Noyes","given":"T.I.","email":"","affiliations":[],"preferred":false,"id":199543,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, P.A.","contributorId":73245,"corporation":false,"usgs":true,"family":"Brown","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":199544,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31756,"text":"ofr94488 - 1994 - Physical characteristics of stream subbasins in the Chippewa River basin, west-central Minnesota","interactions":[],"lastModifiedDate":"2022-02-15T20:34:01.076195","indexId":"ofr94488","displayToPublicDate":"1995-10-01T00:00:00","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":"94-488","title":"Physical characteristics of stream subbasins in the Chippewa River basin, west-central Minnesota","docAbstract":"<p>Data that describe the physical characteristics of stream subbasins upstream from selected points on streams in the Chippewa River Basin, located in west-central Minnesota, are presented in this report The physical characteristics are the drainage area of the subbasin, the percentage area of the subbasin covered only by lakes, the percentage area of the subbasin covered by both lakes and wetlands, the main-channel length, and the main-channel slope. The points on the stream include outlets of subbasins of at least 5 square miles, outlets of sewage treatment plants, and locations of U.S. Geological Survey low-flow, high-flow, and continuous-record gaging stations.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/ofr94488","collaboration":"Prepared in cooperation with Minnesota Department of Transportation","usgsCitation":"Sanocki, C., and Krumrie, J.R., 1994, Physical characteristics of stream subbasins in the Chippewa River basin, west-central Minnesota: U.S. Geological Survey Open-File Report 94-488, Report: 16 p.; 1 Plate: 27.52 x 46.73 inches, https://doi.org/10.3133/ofr94488.","productDescription":"Report: 16 p.; 1 Plate: 27.52 x 46.73 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":59967,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0488/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0488/report-thumb.jpg"},{"id":395999,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0488/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Chippewa River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685be2","contributors":{"authors":[{"text":"Sanocki, Chris 0000-0001-6714-5421","orcid":"https://orcid.org/0000-0001-6714-5421","contributorId":214142,"corporation":false,"usgs":true,"family":"Sanocki","given":"Chris","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":206880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krumrie, James R.","contributorId":76368,"corporation":false,"usgs":true,"family":"Krumrie","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":206879,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28317,"text":"wri944171 - 1994 - Sources and cycling of major ions and nutrients in Devils Lake, North Dakota","interactions":[],"lastModifiedDate":"2018-03-08T13:55:40","indexId":"wri944171","displayToPublicDate":"1995-10-01T00:00:00","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":"94-4171","title":"Sources and cycling of major ions and nutrients in Devils Lake, North Dakota","docAbstract":"<p>Devils Lake is a saline lake in a large, closed drainage basin in northeastern North Dakota. Previous studies determined that major-ion and nutrient concentrations in Devils Lake are strongly affected by microbially mediated sulfate reduction and dissolution of sulfate and carbonate minerals in the bottom sediments. These studies documented substantial spatial variability in the magnitude of calculated benthic fluxes coincident with the horizontal salinity gradient in Devils Lake. The purpose of the present study is to evaluate seasonal variability in benthic-flux rates, and to understand the effect of these fluxes on the major-ion and nutrient chemistries in Devils Lake between May and October 1991. </p><p>During the study period, the water column was well mixed, and specific conductance, pH, and temperature did not vary with depth. Dissolved oxygen was enriched near the lake surface due to photosynthesis. Major-ion concentrations and nutrient concentrations did not vary with depth. Because the water-quality data were obtained during open-water periods, the vertical profiles reflect well-mixed conditions. However, the first and last profiles for the study period did document near-bottom maxima of major cations. Secchi-disk depth varied from 0.82 meter on May 7,1991, to 2.13 meters on June 5, 1991. The mean Secchi-disk depth during the study period was 1.24 meters. Seasonal variations in Secchi-disk depths were attributed to variations in primary productivity and phytoplankton communities. </p><p>Nutrient cycles in Devils Lake were evaluated using gross primary productivity rate data, sediment trap data, and major-ion and nutrient benthic-flux rate data. Gross primary productivity rate was smallest in May (0.076 gram of carbon per square meter per day) and largest in September (1.8 grams of carbon per square meter per day). Average gross primary productivity for the study period was 0.87 gram of carbon per square meter per day. Average gross primary productivity is consistent with historic data from Devils Lake and with data from other eutrophic lakes.</p><p>The average flux of organic carbon for the study period was 12 grams per square meter per day. The calculated carbon to nitrogen to phosphorus ratio (317:25:1) is similar to the Redfield ratio (106:16:1); therefore, most organic matter probably is derived from lacustrine phytoplankton.</p><p>Calculated benthic-flux rates indicated that bottom sediments are important sources of majorions and nutrients to Devils Lake. Only one of the cores collected during this study indicated a net sulfate flux from the lake into the sediments. Seasonal variations in major-ion and nutrient benthic fluxes generally were small. However, there were important differences between the calculated benthic fluxes for this study and the calculated benthic fluxes for 1990. Calculated benthic fluxes of bicarbonate, ammonia, and phosphorus for this study were smaller than&nbsp;calculated benthic fluxes for 1990. The large differences between fluxes for 1990 and 1991 were attributed to calm, stratified water-column conditions in 1990 and well-mixed water-column conditions in 1991.</p><p>The role of benthic fluxes in the chemical mass balances in Devils Lake was evaluated by calculating response times for major ions and nutrients in Devils Lake. The calculated response times for major ions in Devils Lake ranged from 6.7 years for bicarbonate to 34 years for sulfur (as 804). The response times for major ions are significantly shorter than previous estimates that did not include benthic fluxes. In addition, the relatively short response times for nitrogen (4.2 years) and phosphorus (0.95 year) indicate that nutrients are recycled rapidly between bottom sediments and the lake. During the study period, benthic fluxes were the dominant source of major ions and nutrients to Devils Lake and greatly reduced the response times of all major ions and nutrients for Devils Lake. As a result, bottom-sediment processes appear to buffer major-ion and nutrient concentrations in the lake. Any future attempt to evaluate water quality in Devils Lake should include the effects of bottom-sediment processes. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944171","usgsCitation":"Lent, R., 1994, Sources and cycling of major ions and nutrients in Devils Lake, North Dakota: U.S. Geological Survey Water-Resources Investigations Report 94-4171, vi, 63 p., https://doi.org/10.3133/wri944171.","productDescription":"vi, 63 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":57132,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4171/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4171/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686422","contributors":{"authors":[{"text":"Lent, R.M.","contributorId":80317,"corporation":false,"usgs":true,"family":"Lent","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":199582,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20600,"text":"ofr94388 - 1994 - Global energy and water cycle experiment (GEWEX) continental-scale international project (GCIP); reference data sets CD-ROM","interactions":[],"lastModifiedDate":"2012-02-02T00:07:40","indexId":"ofr94388","displayToPublicDate":"1995-10-01T00:00:00","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":"94-388","title":"Global energy and water cycle experiment (GEWEX) continental-scale international project (GCIP); reference data sets CD-ROM","docAbstract":"The data sets on this compact disc are a compilation of several geographic reference data sets of interest to the global-change research community. The data sets were chosen with input from the Global Energy and Water Cycle Experiment (GEWEX) Continental-Scale International Project (GCIP) Data Committee and the GCIP Hydrometeorology and Atmospheric Subpanels. The data sets include: locations and periods of record for stream gages, reservoir gages, and meteorological stations; a 500-meter-resolution digital elevation model; grid-node locations for the Eta numerical weather-prediction model; and digital map data sets of geology, land use, streams, large reservoirs, average annual runoff, average annual precipitation, average annual temperature, average annual heating and cooling degree days, hydrologic units, and state and county boundaries. Also included are digital index maps for LANDSAT scenes, and for the U.S. Geological Survey 1:250,000, 1:100,000, and 1:24,000-scale map series. Most of the data sets cover the conterminous United States; the digital elevation model also includes part of southern Canada. The stream and reservoir gage and meteorological station files cover all states having area within the Mississippi River Basin plus that part of the Mississippi River Basin lying within Canada. Several data-base retrievals were processed by state, therefore many sites outside the Mississippi River Basin are included.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr94388","usgsCitation":"Rea, A., and Cederstrand, J.R., 1994, Global energy and water cycle experiment (GEWEX) continental-scale international project (GCIP); reference data sets CD-ROM: U.S. Geological Survey Open-File Report 94-388, 1 computer laser optical disc ;4 3/4 in. +1 booklet ([4] p. ; 12 cm.), both in plastic box (13 x 15 x 1 cm.), https://doi.org/10.3133/ofr94388.","productDescription":"1 computer laser optical disc ;4 3/4 in. +1 booklet ([4] p. ; 12 cm.), both in plastic box (13 x 15 x 1 cm.)","costCenters":[],"links":[{"id":153261,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abee4b07f02db674ae9","contributors":{"authors":[{"text":"Rea, Alan","contributorId":41018,"corporation":false,"usgs":true,"family":"Rea","given":"Alan","affiliations":[],"preferred":false,"id":182916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cederstrand, Joel R.","contributorId":15223,"corporation":false,"usgs":true,"family":"Cederstrand","given":"Joel","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":182915,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":20942,"text":"ofr94536 - 1994 - Records of water levels in monitoring wells in the Gallatin Valley, southwestern Montana, 1947-93","interactions":[],"lastModifiedDate":"2012-02-02T00:07:47","indexId":"ofr94536","displayToPublicDate":"1995-10-01T00:00:00","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":"94-536","title":"Records of water levels in monitoring wells in the Gallatin Valley, southwestern Montana, 1947-93","docAbstract":"Water-level data were collected in the Gallatin Valley to provide a basis for evaluation of the configuration of the ground-water surface and water-level change. Water-level records collected during a 2-year study of the area and historical water-level data for 121 wells in the Gallatin Valley are summarized in the report. Well-depth and primary-aquifer data are included. The locations of the wells are shown on a map at a scale of 1:275,500.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94536","usgsCitation":"Slagle, S.E., 1994, Records of water levels in monitoring wells in the Gallatin Valley, southwestern Montana, 1947-93: U.S. Geological Survey Open-File Report 94-536, iii, 41 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94536.","productDescription":"iii, 41 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":153960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0536/report-thumb.jpg"},{"id":50529,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0536/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626cd3","contributors":{"authors":[{"text":"Slagle, Steven E.","contributorId":35284,"corporation":false,"usgs":true,"family":"Slagle","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":183550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26076,"text":"wri904095 - 1994 - Interactions of metallic substances and acidic ground water in the New Jersey Coastal Plan","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"wri904095","displayToPublicDate":"1995-09-01T00:00:00","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":"90-4095","title":"Interactions of metallic substances and acidic ground water in the New Jersey Coastal Plan","docAbstract":"Four ancillary studies were undertaken in support of an investigation into the extent and distribution of corrosive ground water in the Kirkwood- Cohansey aquifer system of southern New Jersey.The ancillary studies were (1) analysis of tap-water samples for metals and the acquisition of metal data from a county study, (2) leaching experiments in which copper pipe with various types of solder were exposed to a variety of ground-water types, (3) analysis of pipe-scale deposits on plumbing from houses with wells that tap the Kirkwood-Cohansey aquifer system, and (4) measurement of corrosion rates for carbon steel and copper exposed to shallow ground water from the Kirkwood-Cohansey aquifer system.  The results studies indicate that substantial concentrations of lead, copper, and zinc can leach from plumbing materials exposed to corrosive water from the Kirkwood-Cohansey aquifer system, and that leaching appears more pronounced during the summer than during the winter. The leaching experiments indicate that the corrosiveness of water, as estimated by the calculation of a corrosion index (the Aggressive Index), is related to the concentration of trace metals in the leachate.Further, although the leaching of lead-bearing solders produced lead concentrations in leachate above the Primary Drinking Water Criterion in effect at the time of the study (50 micrograms per liter), no potentially toxic levels of metals were leached from lead-free solders, although copper concentrations in some leachate samples were in excess of the Secondary Drinking Water Criterion of 1,000 micrograms per liter.   Analyses of pipe-scale deposits indicate the formation of iron oxide coatings on some copper-pipe interiors exposed to untreated well water.   Treated water from a public-supply system precipitated copper carbonate and copper chloride minerals. Corrosion rates measured for copper exposed to corrosive water from the Kirkwood-Cohansey aquifer system were slow (less than 0.0254 millimeters per year). Carbon-steel corrosion rates were faster; the fastest rate (0.229 millimeters per year) was measured in oxygen-saturated water.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri904095","usgsCitation":"Barringer, J.L., 1994, Interactions of metallic substances and acidic ground water in the New Jersey Coastal Plan: U.S. Geological Survey Water-Resources Investigations Report 90-4095, vi, 68 p. :ill., map ;28 cm., https://doi.org/10.3133/wri904095.","productDescription":"vi, 68 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4095/report-thumb.jpg"},{"id":54848,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4095/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4930e4b07f02db581757","contributors":{"authors":[{"text":"Barringer, J. L.","contributorId":13994,"corporation":false,"usgs":true,"family":"Barringer","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195760,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16977,"text":"ofr94714 - 1994 - Circum-North Pacific tectonostratigraphic terrane map","interactions":[],"lastModifiedDate":"2022-07-22T19:13:20.313093","indexId":"ofr94714","displayToPublicDate":"1995-09-01T00:00:00","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":"94-714","title":"Circum-North Pacific tectonostratigraphic terrane map","docAbstract":"<p>The companion tectonostratigraphic terrane and overlap assemblage of map the Circum-North Pacific presents a modern description of the major geologic and tectonic units of the region. The map illustrates both the onshore terranes and overlap volcanic assemblages of the region, and the major offshore geologic features. The map is the first collaborative compilation of the geology of the region at a scale of 1:5,000,000 by geologists of the Russian Far East, Japanese, Alaskan, Canadian, and U.S.A. Pacific Northwest. The map is designed to be a source of geologic information for all scientists interested in the region, and is designed to be used for several purposes, including regional tectonic analyses, mineral resource and metallogenic analyses (Nokleberg and others, 1993, 1994a), petroleum analyses, neotectonic analyses, and analyses of seismic hazards and volcanic hazards. This text contains an introduction, tectonic definitions, acknowledgments, descriptions of postaccretion stratified rock units, descriptions and stratigraphic columns for tectonostratigraphic terranes in onshore areas, and references for the companion map (Sheets 1 to 5).</p>\n<br>\n<p>This map is the result of extensive geologic mapping and \nassociated tectonic studies in the Russian Far East, Hokkaido \nIsland of Japan, Alaska, the Canadian Cordillera, and the \nU.S.A. Pacific Northwest in the last few decades. Geologic \nmapping suggests that most of this region can be interpreted as \na collage of fault-bounded tectonostratigraphic terranes that \nwere accreted onto continental margins around the Circum-\n. orth Pacific mainly during the Mesozoic and Cenozoic (Fujita \nand ewberry, 1983; 1987; Parfenov, 1984, 1991; Howell, \n1985; Watson and Fujita, 1985; Parfenov and Natal'in, 1984; \nJones and others. 1987; Monger and Berg, 1987, Fujita and \nCook. 1990; Zonenshain and others. 1990; Natal'in, 1991, \n1993; Moore and others, 1992; Silberling and others, 1992; \nNokleberg and others. 1992, 1993, 1994a; Parfenov and \nothers. 1993; Plaflcer and Berg, 1994; Tabor, 1994).</p>\n<br>\n<p>This map is the result of extensive geologic mapping and \nassociated tectonic studies in the Russian Far East, Hokkaido \nIsland of Japan, Alaska, the Canadian Cordillera, and the \nU.S.A. Pacific Northwest in the last few decades. Geologic \nmapping suggests that most of this region can be interpreted as \na collage of fault-bounded tectonostratigraphic terranes that \nwere accreted onto continental margins around the Circum-\n. orth Pacific mainly during the Mesozoic and Cenozoic (Fujita \nand ewberry, 1983; 1987; Parfenov, 1984, 1991; Howell, \n1985; Watson and Fujita, 1985; Parfenov and Natal'in, 1984; \nJones and others. 1987; Monger and Berg, 1987, Fujita and \nCook. 1990; Zonenshain and others. 1990; Natal'in, 1991, \n1993; Moore and others, 1992; Silberling and others, 1992; \nNokleberg and others. 1992, 1993, 1994a; Parfenov and \nothers. 1993; Plaflcer and Berg, 1994; Tabor, 1994).</p> \n<br>\n<p>On the companion map and in the descriptions bel?w· \nterranes are interpreted according to inferred tectonic \nenvironments. These environments are (I) cratonai; (2) \npassive continental margin; (3) metamorphosed continental \nmargin; (4) continental-margin arc; (5) island arc; (6) oceanic \ncrust, seamount, and ophiolite; (7) accretionary wedge and \nsubduction zone: (8) turbidite basin; and (9) metamorphic for \nterranes that are too highly-deformed and metamorphosed to \nde~ermine the original tectonic environment. For terranes with \ncomplex geologic histories, the chosen color indicates the \ntectonic environment most prevalent during this history of the \nterrane. The tectonic environments inf~rred for igneous rocks \nare both temporal and genetic. The temporal environments are \npreaccretion and postaccretion. The genetic environments are \nsubduction-related, rift-related, and collisional (anatectic)-\nrelated.</p> \n<br>\n<p>In addition to terranes, the map also depicts postaccretion \nunits that include: (I) Cenozoic and Mesozoic overlap \nassemblages of sedimentary and volcanic rocks that are \ndeposited across two or more terranes that formed generally\nafter accretion of most terranes in the region; (2) Cenozoic and \nMesozoic basinal deposits that occur within a terrane or on the \ncraton; (3) plutonic rocks. The postaccretion igneous units are \nidentified by age-lithologic abbreviations and by name. These \noverlap assemblages and basinal deposits formed mainly \nduring sedimentation and magmatism that occurred after \naccretion of terranes to each other or to a continental margin. \nOverlap assemblages provide minimum ages on the timing of \naccretion of terranes. Some Cenozoic and Mesozoic overlap \nassemblages and basinal deposits, as well as fragments of \nterranes, are extensively offset by movement along \npostaccretion faults. In addition, in onshore areas, the map \ndepicts major preaccretion plutonic rocks that are limited to \nindividual terranes. and in offshore areas. the map depicts \nmajor oceanic plates,-ocean floor magnetic lineations. oceanic \nspreading ridges, and seamounts.</p> \n<br>\n<p>The map consists of five sheets. Sheets I and 2 depict, at a \nscale of I :5.000.000. the tectonostratigraphic terranes. \npreaccretion plutonic rocks, and postaccretion Cenozoic and \nMesozoic overlap sedimentary, volcanic. and plutonic \nassemblages, and basinal deposits for the Circum- orth Pacific \nincluding the Russian Far East, northern Hokkaido Island of \nJapan, Alaska. the Canadian Cordillera, part of the U.S.A. \nPacific Northwest. and adjacent offshore areas. Sheet 3 \nprovides the list of map units for Sheets I and 2. Sheet 4 is a \nindex map showing generalized onshore terranes and overlap \nassemblages for onshore parts of the Circum-North Pacific at a \nscale of I: I 0,000,000. Sheet 4 is a guide to the more \ncomplicated onshore features depicted on Sheets I and 2. Sheet \n5 is an index map showing the major geographic regions for \nthe Circum-North Pacific. </p>\n<br>\n<p>Significant differences exist between the representation of \nonshore and offshore geology on Sheets I and 2. These are: (I) \ncompared to the onshore part of the map, the offshore part is \ndepicted in a more schematic fashion because of more limited \ndata and because the offshore terranes and early Cenozoic and \nolder overlap assemblages generally are obscured by extensive \nlate Cenozoic sedimentary cover that is not shown unless \nthicker than two kilometers; (2) marginal contacts of offshore \nCenozoic and Cretaceous sedimentary basins do not match \ncontacts of onshore Cenozoic and Cretaceous sedimentary units \nbecause offshore basins are limited to those regions with \nsediment thicknesses greater than two kilometers; (3) \nstratigraphic columns, included at the end of this explanation. \nare provided only for onshore terranes because the geology of \noffshore terranes is generally less well-known; and (4) for \nsimplicity, the major onshore Cenozoic sedimentary basins are \ngenerally not defined and described separately because the \nonshore part of the map is designed to emphasize terranes and \noverlap volcanic assemblages that are crucial for both for \ntectonic and metallogenic analyses published elsewhere \n(Nokleberg and others, 1993, 1994a).</p>\n<br>\n<p>Several key geologic sources were used in the compilation \nof the map. For Alaska. the basic outcrop pattern for the map is \nfrom Beikman (1980), Gehrels and Berg (1992, 1994). Barker \nand others ( 1994). Brew (1994), and Moli-Stalcup and others \n( 1994b). The distribution of terranes is from Jones and others \n(1987) and Monger and Berg (1987), with modification by \nGrantz and other (1991 ). Worall (199 1 ), okleberg and others \n(1993, 1994a), the cited references, and the Alaskan co-authors \nof this report. For the Canadian Cordillera. the basic outcrop \npattern is from Monger and Berg ( 1987), Wheeler and other \n(1988). and Wheeler and McFeeley ( 1991) with modifications \nby the Canadian authors. For the northern part of the Russian \nFar East. the basic outcrop pattern is from So unov (1985) with \nmodifications by the Russian authors. For the outhern part of \nthe Russian Far East, the basic outcrop pattern is from Krasny \n(1991) and Bazhanov and Oleinik ( 1986) with modification \nby the Russian authors. The Russian Far East part of the map is \nthe first attempt to define and delineate terranes in that region. \nIn their compilation. the Russian authors utilized the \nmethodology of U.S.A. and Canadian geologists. Because this \nmap is the first attempt to display the terranes. Cenozoic and \nMesozoic overlap assemblages. basinal deposit , and plutonic \nbelts of the Russian Far East. the Russian author will \nappreciate constructive sugge tions for improving the map.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr94714","collaboration":"Prepared in collaboration with Russian Academy of Sciences, Geological Survey of Canada, Alaska Division of Geological and Geophysical Surveys, Russian Committee on Geology, Michigan State University, Exxon Production Research Company, University of Alaska, Geological Survey of Japan","usgsCitation":"Nokleberg, W.J., Parfenov, L.M., Monger, J.W., Baranov, B., Byalobzhesky, S.G., Bundtzen, T., Feeney, T.D., Fujita, K., Gordey, S.P., Grantz, A., Khanchuk, A.I., Natal’in, B.A., Natapov, L.M., Norton, I.O., Patton, W.W., Plafker, G., Scholl, D.W., Sokolov, S.D., Sosunov, G.M., Stone, D., Tabor, R.W., Tsukanov, N.V., Vallier, T.L., and Wakita, K., 1994, Circum-North Pacific tectonostratigraphic terrane map: U.S. Geological Survey Open-File Report 94-714, Report: 221 p.; 5 Plates: 49.97 x 36.00 inches and smaller, https://doi.org/10.3133/ofr94714.","productDescription":"Report: 221 p.; 5 Plates: 49.97 x 36.00 inches and smaller","numberOfPages":"222","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":286641,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404382,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13179.htm","linkFileType":{"id":5,"text":"html"}},{"id":286636,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0714/sheet-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286634,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0714/sheet-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286637,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0714/sheet-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286638,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0714/sheet-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286639,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0714/sheet-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286633,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0714/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","projection":"Lambert Azimuthal Equal Area projection","otherGeospatial":"Circum-north Pacific","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e479de4b07f02db49224d","contributors":{"authors":[{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":174404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parfenov, Leonid M.","contributorId":59112,"corporation":false,"usgs":true,"family":"Parfenov","given":"Leonid","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":174418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Monger, James W.H.","contributorId":53900,"corporation":false,"usgs":true,"family":"Monger","given":"James","email":"","middleInitial":"W.H.","affiliations":[],"preferred":false,"id":174417,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baranov, Boris B.","contributorId":107145,"corporation":false,"usgs":true,"family":"Baranov","given":"Boris B.","affiliations":[],"preferred":false,"id":174426,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Byalobzhesky, Stanislav G.","contributorId":73684,"corporation":false,"usgs":true,"family":"Byalobzhesky","given":"Stanislav","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":174421,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bundtzen, Thomas K.","contributorId":83560,"corporation":false,"usgs":true,"family":"Bundtzen","given":"Thomas K.","affiliations":[],"preferred":false,"id":174423,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Feeney, Tracey D.","contributorId":7136,"corporation":false,"usgs":true,"family":"Feeney","given":"Tracey","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":174409,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Fujita, Kazuya","contributorId":15654,"corporation":false,"usgs":true,"family":"Fujita","given":"Kazuya","email":"","affiliations":[],"preferred":false,"id":174411,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Gordey, Steven P.","contributorId":50042,"corporation":false,"usgs":true,"family":"Gordey","given":"Steven","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":174415,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":174405,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Khanchuk, Alexander I.","contributorId":19585,"corporation":false,"usgs":true,"family":"Khanchuk","given":"Alexander","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":174412,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Natal’in, Boris A.","contributorId":91357,"corporation":false,"usgs":true,"family":"Natal’in","given":"Boris","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":174424,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Natapov, Lev M.","contributorId":94154,"corporation":false,"usgs":true,"family":"Natapov","given":"Lev","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":174425,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Norton, Ian O.","contributorId":82575,"corporation":false,"usgs":true,"family":"Norton","given":"Ian","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":174422,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Patton, William W. Jr.","contributorId":107355,"corporation":false,"usgs":true,"family":"Patton","given":"William","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":174427,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":174408,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Scholl, David W. 0000-0001-6500-6962 dscholl@usgs.gov","orcid":"https://orcid.org/0000-0001-6500-6962","contributorId":3738,"corporation":false,"usgs":true,"family":"Scholl","given":"David","email":"dscholl@usgs.gov","middleInitial":"W.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":174406,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Sokolov, Sergei D.","contributorId":68590,"corporation":false,"usgs":true,"family":"Sokolov","given":"Sergei","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":174420,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Sosunov, Gleb M.","contributorId":7560,"corporation":false,"usgs":true,"family":"Sosunov","given":"Gleb","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":174410,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Stone, David B.","contributorId":65324,"corporation":false,"usgs":true,"family":"Stone","given":"David B.","affiliations":[],"preferred":false,"id":174419,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Tabor, Rowland W. rtabor@usgs.gov","contributorId":3816,"corporation":false,"usgs":true,"family":"Tabor","given":"Rowland","email":"rtabor@usgs.gov","middleInitial":"W.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":174407,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Tsukanov, Nickolai V.","contributorId":44035,"corporation":false,"usgs":true,"family":"Tsukanov","given":"Nickolai","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":174414,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"Vallier, Tracy L.","contributorId":28857,"corporation":false,"usgs":true,"family":"Vallier","given":"Tracy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":174413,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Wakita, Koji","contributorId":52672,"corporation":false,"usgs":true,"family":"Wakita","given":"Koji","email":"","affiliations":[],"preferred":false,"id":174416,"contributorType":{"id":1,"text":"Authors"},"rank":24}]}}
,{"id":19091,"text":"ofr94385 - 1994 - Hydrologic data collection at Crowders Creek and Steele Creek, York County, South Carolina, 1991-92","interactions":[],"lastModifiedDate":"2017-01-04T11:17:30","indexId":"ofr94385","displayToPublicDate":"1995-09-01T00:00:00","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":"94-385","title":"Hydrologic data collection at Crowders Creek and Steele Creek, York County, South Carolina, 1991-92","docAbstract":"Rapid industrial and urban growth is anticipated in the vicinity of Crowders Creek near Clover, S.C., and Steele Creek near Fort Mill, S.C. These subbasins are in the Catawba River Basin in York County, S.C. To obtain baseline information on these basins prior to urbanization, gaging stations 02145642 (Crowders Creek near Clover, S.C.) and 021467801 (Steele Creek near Fort Mill, S.C.) were established to collect streamflow and water-quality data. Continuous stream-stage and streamflow data were collected during the periods of March 23, 1991 to September 30, 1992, and May 29, 1991 to September 30, 1992, for stations 02145642 and 021467801, respectively. Average streamflows for stations 02145642 and 021467801 for the study period were 80.5 cubic feet per second and 28.6 cubic feet per second, respectively. Water-quality data were collected on four separate occasions at each gage site; two samplings during low-flow events and two samplings during high-flow events. Fecal coliform concentrations exceeded minimum standards for freshwater with other physical and chemical constituents meeting South Carolina Department of Health and Environmental Control standards.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94385","usgsCitation":"Gissendanner, J.W., 1994, Hydrologic data collection at Crowders Creek and Steele Creek, York County, South Carolina, 1991-92: U.S. Geological Survey Open-File Report 94-385, iv, 18 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94385.","productDescription":"iv, 18 p. :ill., map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":151053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0385/report-thumb.jpg"},{"id":48529,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0385/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Carolina","county":"York County","city":"Fort Mill","otherGeospatial":"Crowders Creek, Steele Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.6448974609375,\n              34.6060845921693\n            ],\n            [\n              -81.6448974609375,\n              35.4382955473967\n            ],\n            [\n              -80.321044921875,\n              35.4382955473967\n            ],\n            [\n              -80.321044921875,\n              34.6060845921693\n            ],\n            [\n              -81.6448974609375,\n              34.6060845921693\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f832","contributors":{"authors":[{"text":"Gissendanner, John W.","contributorId":26710,"corporation":false,"usgs":true,"family":"Gissendanner","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":180296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27705,"text":"wri944250 - 1994 - Refining 1970's Land-Use Data With 1990 Population Data to Indicate New Residential Development","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri944250","displayToPublicDate":"1995-09-01T00:00:00","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":"94-4250","title":"Refining 1970's Land-Use Data With 1990 Population Data to Indicate New Residential Development","docAbstract":"A procedure using a geographic information system was developed to define urban land use representative of the 1990's by overlaying U.S. Bureau of the Census 1990 population density at the block group level on 1970's digital land-use data from 1:250,000-and 1: 100,000scale maps. Any area having a population density of 1,000 or more people per square mile is re-classified as &quot;urban&quot; land use in the derivative product. The procedure was applied to 20 study units of the National Water-Quality Assessment program to provide what are considered reasonable indications of urbanization that has occurred since the 1970's.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri944250","usgsCitation":"Hitt, K.J., 1994, Refining 1970's Land-Use Data With 1990 Population Data to Indicate New Residential Development: U.S. Geological Survey Water-Resources Investigations Report 94-4250, vi, 15 p., https://doi.org/10.3133/wri944250.","productDescription":"vi, 15 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":158517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11621,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri944250/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635169","contributors":{"authors":[{"text":"Hitt, Kerie J.","contributorId":54565,"corporation":false,"usgs":true,"family":"Hitt","given":"Kerie","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26168,"text":"wri934003 - 1994 - Ground-water flow and quality, and geochemical processes, in Indian Wells Valley, Kern, Inyo, and San Bernardino counties, California, 1987-88","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri934003","displayToPublicDate":"1995-09-01T00:00:00","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":"93-4003","title":"Ground-water flow and quality, and geochemical processes, in Indian Wells Valley, Kern, Inyo, and San Bernardino counties, California, 1987-88","docAbstract":"An existing water-quality data base for the 300- square-mile Indian Wells Valley was updated by means of chemical and isotopic analysis of ground water. The wide range in measured concentrations of major ions and of minor constituents such as fluoride, borate, nitrate, manganese, and iron is attributed to geochemical reactions within lacustrine deposits of the valley floor. These reactions include sulfate reduction accompanied by generation of alkalinity, precipitation of carbonates, exchange of aqueous alkaline-earth ions for sodium on clays, and dissolution of evaporite minerals. Differences in timing and location of recharge, which originates primarily in the Sierra Nevada to the west, and evapotranspiration from a shallow water table on the valley floor result in a wide range in ratios of stable hydrogen and oxygen isotopes. As ground water moves from alluvium into lustrine deposits of the ancestral China Lake, dissolved-solids concen- trations increase from about 200 to more than 1,000 milligrams per liter; further large increases to several thousand milligrams per liter occur beneath the China Lake playa. Historical data show an increase during the past 20 years in dissolved- solids concentration in several wells in the principal pumping areas at Ridgecrest and between Ridgecrest and Inyokern. The increase apparently is caused by induced flow of saline ground water from nearby China, Mirror, and Satellite Lakes. A simplified advective-transport model calculates ground-water travel times between parts of the valley of at least several thousand years, indi- cating the presence of old ground water. A local ground-water line and an evaporation line estimated using isotopic data from the China Lake area inter- sect at a delta-deuterium value of about -125 permil. This indicates that late Pleistocene recharge was 15 to 35 permil more negative than current recharge.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-File Reports Section [distributor],","doi":"10.3133/wri934003","usgsCitation":"Berenbrock, C., and Schroeder, R.A., 1994, Ground-water flow and quality, and geochemical processes, in Indian Wells Valley, Kern, Inyo, and San Bernardino counties, California, 1987-88: U.S. Geological Survey Water-Resources Investigations Report 93-4003, vi, 59 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934003.","productDescription":"vi, 59 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4003/report-thumb.jpg"},{"id":54956,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4003/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce7c","contributors":{"authors":[{"text":"Berenbrock, Charles","contributorId":30598,"corporation":false,"usgs":true,"family":"Berenbrock","given":"Charles","email":"","affiliations":[],"preferred":false,"id":195929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schroeder, R. A.","contributorId":15554,"corporation":false,"usgs":true,"family":"Schroeder","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195928,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18766,"text":"ofr94500 - 1994 - Flood magnitude and frequency of Chandlers Run at two sites, at Pennsauken Township, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr94500","displayToPublicDate":"1995-09-01T00:00:00","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":"94-500","title":"Flood magnitude and frequency of Chandlers Run at two sites, at Pennsauken Township, New Jersey","docAbstract":"Six methods were used to estimate the magnitude and frequency of floods at Chandlers Run at the culvert on New Jersey Route 612, and at a second site about 2,100 feet upstream, at New Jersey Route 70 at Pennsauken Township, New Jersey. Flood magnitude and frequency calculated by the six methods, as well as drainage-basin characteristics, are included in this report. The 100-year-flood estimates for the culvert site on Route 612 range from 268 cubic feet per second to 2,050 cubic feet per second. The 100-year-flood estimates for the upstream site at Route 70 range from 246 cubic feet per second to 2,320 cubic feet per second. Flood magnitude and frequency estimates obtained by using the New Jersey Department of Environmental Protection Special Report 38 method and other pre- viously published estimates fall within the range of values estimated by using the U.S. Geological Survey transfer method with data collected from three nearby crest-stage gages.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94500","usgsCitation":"Dunne, P., 1994, Flood magnitude and frequency of Chandlers Run at two sites, at Pennsauken Township, New Jersey: U.S. Geological Survey Open-File Report 94-500, iv, 12 leaves :map ;28 cm., https://doi.org/10.3133/ofr94500.","productDescription":"iv, 12 leaves :map ;28 cm.","costCenters":[],"links":[{"id":150935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0500/report-thumb.jpg"},{"id":48125,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0500/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef022","contributors":{"authors":[{"text":"Dunne, Paul","contributorId":86794,"corporation":false,"usgs":true,"family":"Dunne","given":"Paul","email":"","affiliations":[],"preferred":false,"id":179705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18768,"text":"ofr94499 - 1994 - Flood magnitude and frequency of Pochack Creek at two sites, at Pennsauken Township, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr94499","displayToPublicDate":"1995-09-01T00:00:00","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":"94-499","title":"Flood magnitude and frequency of Pochack Creek at two sites, at Pennsauken Township, New Jersey","docAbstract":"Six methods were used to estimate the magnitude and frequency of floods at Pochack Creek at the down- stream end of the culvert on United States Route 130 and at a second site about 1,600 feet upstream at Pennsauken Township, New Jersey. Flood magnitude and frequency calculated by the six methods, as well as drainage-basin characteristics, are included in this report. The 100-year-flood estimates for the culvert site range from 280 cubic feet per second to 2,600 cubic feet per second. The 100-year-flood estimates for the upstream site range from 216 cubic feet per second to 1,800 cubic feet per second. Flood magni- tude and frequency estimates obtained by using the New Jersey Department of Environmental Protection Special Report 38 method fall within the range of values estimated by using the U.S. Geological Survey transfer method with data collected from three nearby crest-stage gages.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94499","usgsCitation":"Dunne, P., 1994, Flood magnitude and frequency of Pochack Creek at two sites, at Pennsauken Township, New Jersey: U.S. Geological Survey Open-File Report 94-499, iv, 11 leaves :map ;28 cm., https://doi.org/10.3133/ofr94499.","productDescription":"iv, 11 leaves :map ;28 cm.","costCenters":[],"links":[{"id":150937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0499/report-thumb.jpg"},{"id":48127,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0499/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef019","contributors":{"authors":[{"text":"Dunne, Paul","contributorId":86794,"corporation":false,"usgs":true,"family":"Dunne","given":"Paul","email":"","affiliations":[],"preferred":false,"id":179708,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32782,"text":"ofr94504 - 1994 - Hydrologic data for the alluvium and terrace deposits of the Cimarron River from Freedom to Guthrie, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"ofr94504","displayToPublicDate":"1995-09-01T00:00:00","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":"94-504","title":"Hydrologic data for the alluvium and terrace deposits of the Cimarron River from Freedom to Guthrie, Oklahoma","docAbstract":"Ground water in the Quaternary alluvium and terrace deposits associated with the Cimarron River in northwestern Oklahoma is used extensively for irrigation, municipal, stock, and domestic supplies. The data in this report were collected as part of an investigation to provide State water managers with the quantitative knowledge necessary to manage the ground-water resource effectively. The investigation was conducted by the U.S. Geological Survey in cooperation with the Oklahoma Geological Survey. The information presented in this report include data collected in the field from 1985 through 1989, and unpublished data compiled from files of the U.S. Geological Survey and the Oklahoma Water Resources Board. Data include well and test-bole records, consisting of ground-water levels, depth of wells, principal aquifer, and primary use of water. Water levels include continuous, daily, monthly, and periodic measure- ments for selected wells. Concentrations of common chemical constituents, selected trace elements, organic analyses, and tritium analyses of water samples from wells completed in the Cimarron River alluvium and terrace deposits and Permian geologic units are reported. Winter and summer base-flow discharge measurements of the Cimarron River and its Tributaries are presented together with water-quality data from the measuring sites. Continuous water-level and precipitation-gage data are presented graphically. Locations of data- collection sites are shown on plates.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94504","usgsCitation":"Adams, G.P., Bergman, D.L., Pruitt, D., May, J., and Kurklin, J., 1994, Hydrologic data for the alluvium and terrace deposits of the Cimarron River from Freedom to Guthrie, Oklahoma: U.S. Geological Survey Open-File Report 94-504, vi, 231 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94504.","productDescription":"vi, 231 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":161327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0504/report-thumb.jpg"},{"id":60725,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0504/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db6080ce","contributors":{"authors":[{"text":"Adams, Gregory P.","contributorId":13095,"corporation":false,"usgs":true,"family":"Adams","given":"Gregory","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":209154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergman, D. L.","contributorId":93038,"corporation":false,"usgs":true,"family":"Bergman","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":209157,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pruitt, D.J.","contributorId":79756,"corporation":false,"usgs":true,"family":"Pruitt","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":209156,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"May, J.E.","contributorId":7741,"corporation":false,"usgs":true,"family":"May","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":209153,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kurklin, J. K.","contributorId":59032,"corporation":false,"usgs":true,"family":"Kurklin","given":"J. K.","affiliations":[],"preferred":false,"id":209155,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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