Water-temperature data from 32 sites in the Cook Inlet Basin, south-central Alaska, indicate various trends that depend on watershed characteristics. Basins with 25 percent or more of their area consisting of glaciers have the coldest water temperatures during the open-water season, mid-May to mid-October. Streams and rivers that drain lowlands have the warmest water temperatures. A model that uses air temperature as input to predict water temperature as output was utilized to simulate future trends in water temperature based on increased air temperatures due to climate warming. Based on the Nash-Sutcliffe coefficient, the model produced acceptable results for 27 sites. For basins with more than 25 percent glacial coverage, the model was not as accurate. Results indicate that 15 sites had a predicted water-temperature change of 3 degrees Celsius or more, a magnitude of change that is considered significant for the incidence of disease in fish populations.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri014109","collaboration":"Prepared as part of the National Water-Quality Assessment Program","usgsCitation":"Kyle, R.E., and Brabets, T.P., 2001, Water Temperature of Streams in the Cook Inlet Basin, Alaska, and Implications of Climate Change: U.S. Geological Survey Water-Resources Investigations Report 01-4109, 24 p.","productDescription":"24 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":2887,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4109/wrir01-4109.pdf","text":"Report","size":"3.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PDF of report"},{"id":160345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4109/coverthb.jpg"}],"contact":"Director, Oregon Water Science Center
U.S. Geological Survey
2130 SW 5th Avenue
Portland, Oregon 97201
http://or.water.usgs.gov
This report presents selected low-flow and flow-duration characteristics for 386 sites throughout Ohio. These sites include 195 long-term continuous- record stations with streamflow data through water year 1997 (October 1 to September 30) and for 191 low-flow partial-record stations with measurements into water year 1999. The characteristics presented for the long-term continuous-record stations are minimum daily streamflow; average daily streamflow; harmonic mean flow; 1-, 7-, 30-, and 90-day minimum average low flow with 2-, 5-, 10-, 20-, and 50-year recurrence intervals; and 98-, 95-, 90-, 85-, 80-, 75-, 70-, 60-, 50-, 40-, 30-, 20-, and 10-percent daily duration flows. The characteristics presented for the low-flow partial-record stations are minimum observed streamflow; estimated 1-, 7-, 30-, and 90-day minimum average low flow with 2-, 10-, and 20-year recurrence intervals; and estimated 98-, 95-, 90-, 85- and 80-percent daily duration flows. The low-flow frequency and duration analyses were done for three seasonal periods (warm weather, May 1 to November 30; winter, December 1 to February 28/29; and autumn, September 1 to November 30), plus the annual period based on the climatic year (April 1 to March 31).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014140","collaboration":"Prepared in cooperation with the Ohio Department of Natural Resources, Division of Water","usgsCitation":"Straub, D.E., 2001, Low-flow characteristics of streams in Ohio through water year 1997: U.S. Geological Survey Water-Resources Investigations Report 2001–4140, iv, 415 p., https://doi.org/10.3133/wri014140.","productDescription":"iv, 415 p.","numberOfPages":"423","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":161258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4140/coverthb.jpg"},{"id":362961,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4140/wri20014140.pdf","text":"Report","size":"20.9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 2001-4140"}],"country":"United 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\"}}]}","contact":"Director, Ohio Water Science Center
U.S. Geological Survey
6460 Busch Blvd.
Columbus, OH 43229-1737
Stream-restoration projects utilizing naturalstream designs frequently are based on the bankfull- channel characteristics of a stream reach that is accommodating streamflow and sediment transport without excessive erosion or deposition. The bankfull channel is identified by the use of field indicators and confirmed with tools such as regional curves. Channel dimensions were surveyed at six streamflow-measurement stations operated by the U.S. Geological Survey in the Gettysburg-Newark Lowlands Section and Piedmont Lowlands Section of the Piedmont Physiographic Province in Pennsylvania and Maryland. Regional curves were developed from regression analyses of the relation between drainage area and cross-sectional area, mean depth, width, and streamflow of the bankfull channel. Regional curves were used to confirm the identification of the bankfull channel at a reference reach. Stream dimensions and characteristics of the reference reach were measured for extrapolation into the design of a steam-restoration project on Bermudian Creek in Adams County, Pa.
Dimensions for cross-sectional area, mean depth, width, and computed streamflow of the bankfull channel in all surveyed riffle cross sections in the reference reach were within the 95-percent confidence interval bounding the regression line representing bankfull channel geometry in the Lowland Sections of the Piedmont Physiographic Province. The average bankfull cross-sectional area, bankfull mean depth, and computed bankfull discharge for riffle cross sections in the reference reach ranged from 15.4 to 16.5 percent less than estimates determined from the lowland regional curves. Average bankfull channel width was about 2 percent greater than estimates. Cross-sectional area, mean depth, and computed streamflow corresponding to the bankfull stage at the reference reach were 31.4, 44.4, and 9.6 percent less, respectively, than estimates derived from the regional curves developed by Dunne and Leopold in 1978. Average bankfull channel width at the reference reach was 16.7 percent greater than the Dunne and Leopold estimate.
The concepts of regional curves and reference reaches can be valuable tools to support efforts in stream restoration. Practitioners of stream restoration need to recognize them as such and realize their limitations. The small number of stations available for analysis is a major limiting factor in the strength of the results of this investigation. Subjective selection criteria may have unnecessarily eliminated streamflow-measurement stations that could have been included in the regional curves. A bankfull discharge with a recurrence interval within the 1- to 2-year range was used as a criteria for confirmation of the bankfull stage at each streamflow-measurement station. Many researchers accept this range for recurrence interval of the bankfull discharge; however, literature provides contradictory evidence. The use of channel-characteristics data from a reference reach without any monitoring data to document the stability of the reference reach over time is a topic of debate.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014146","collaboration":"Prepared in cooperation with the Pennsylvania Department of Environmental Protection","usgsCitation":"White, K., 2001, Regional curve development and selection of a reference reach in the non-urban, lowland sections of the Piedmont physiographic province, Pennsylvania and Maryland: U.S. Geological Survey Water-Resources Investigations Report 2001-4146, vi, 20 p., https://doi.org/10.3133/wri014146.","productDescription":"vi, 20 p.","onlineOnly":"Y","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":351010,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4146/wri20014146.pdf","text":"Report","size":"639 KB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 2001-4146"},{"id":161291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4146/coverthb.jpg"}],"contact":"Director, Pennsylvania Water Science Center
U.S. Geological Survey
215 Limekiln Road
New Cumberland, PA 17070
A statewide study was conducted to develop regression equations for estimating flood-frequency discharges for ungaged stream sites in Iowa. Thirty-eight selected basin characteristics were quantified and flood-frequency analyses were computed for 291 streamflow-gaging stations in Iowa and adjacent States. A generalized-skew-coefficient analysis was conducted to determine whether generalized skew coefficients could be improved for Iowa. Station skew coefficients were computed for 239 gaging stations in Iowa and adjacent States, and an isoline map of generalized-skew-coefficient values was developed for Iowa using variogram modeling and kriging methods. The skew map provided the lowest mean square error for the generalized-skew- coefficient analysis and was used to revise generalized skew coefficients for flood-frequency analyses for gaging stations in Iowa.
\nRegional regression analysis, using generalized least-squares regression and data from 241 gaging stations,was used to develop equations for three hydrologic regions defined for the State. The regression equations can be used to estimate flood discharges that have recurrence intervals of 2, 5, 10, 25, 50, 100, 200, and 500 years for ungaged stream sites in Iowa. One-variable equations were developed for each of the three regions and multi-variable equations were developed for two of the regions. Two sets of equations are presented for two of the regions because one-variable equations are considered easy for users to apply and the predictive accuracies of multi-variable equations are greater. Standard error of prediction for the one-variable equations ranges from about 34 to 45 percent and for the multi-variable equations ranges from about 31 to 42 percent.
\nA region-of-influence regression method was also investigated for estimating flood-frequency discharges for ungaged stream sites in Iowa. A comparison of regional and region-of influence regression methods, based on ease of application and root mean square errors, determined the regional regression method to be the better estimation method for Iowa.
\nTechniques for estimating flood-frequency discharges for streams in Iowa are presented for determining (1) regional regression estimates for ungaged sites on ungaged streams; (2) weighted estimates for gaged sites; and (3) weighted estimates for ungaged sites on gaged streams. The technique for determining regional regression estimates for ungaged sites on ungaged streams requires determining which of four possible examples applies to the location of the stream site and its basin. Illustrations for determining which example applies to an ungaged stream site and for applying both the one-variable and multi-variable regression equations are provided for the estimation techniques.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri004233","collaboration":"Prepared in cooperation with the Iowa Department of Transportation and the Iowa Highway Research Board (Project HR-395A)","usgsCitation":"Eash, D.A., 2001, Techniques for estimating flood-frequency discharges for streams in Iowa: U.S. Geological Survey Water-Resources Investigations Report 2000-4233, iv, 88 p., https://doi.org/10.3133/wri004233.","productDescription":"iv, 88 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":316664,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri004233.JPG"},{"id":2788,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ia.water.usgs.gov/pubs/reports/WRIR_00-4233.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois, Iowa, Minnesota, Missouri, Nebraska, South Dakota, Wisconsin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.923095703125,\n 43.8899753738369\n ],\n [\n -89.69238281249999,\n 40.136890695345905\n ],\n [\n -97.283935546875,\n 40.069664523297774\n ],\n [\n -97.18505859374999,\n 44.449467536006935\n ],\n [\n -95.44921875,\n 44.449467536006935\n ],\n [\n -95.44921875,\n 43.992814500489914\n ],\n [\n -89.923095703125,\n 43.8899753738369\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4886e4b07f02db519754","contributors":{"authors":[{"text":"Eash, David A. 0000-0002-2749-8959 daeash@usgs.gov","orcid":"https://orcid.org/0000-0002-2749-8959","contributorId":1887,"corporation":false,"usgs":true,"family":"Eash","given":"David","email":"daeash@usgs.gov","middleInitial":"A.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204264,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31177,"text":"ofr00413 - 2001 - Selected field and analytical methods and analytical results in the Dutch Flats area, western Nebraska, 1995-99","interactions":[],"lastModifiedDate":"2022-01-21T17:40:00.113838","indexId":"ofr00413","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2000-413","title":"Selected field and analytical methods and analytical results in the Dutch Flats area, western Nebraska, 1995-99","docAbstract":"A study of the water resources of the Dutch Flats area in the western part of the North Platte Natural Resources District, western Nebraska, was conducted from 1995 through 1999 to describe the surface water and hydrogeology, the spatial distribution of selected water-quality constituents in surface and ground water, and the surface-water/ground-water interaction in selected areas. This report describes the selected field and analytical methods used in the study and selected analytical results from the study not previously published. Specifically, dissolved gases, age-dating data, and other isotopes collected as part of an intensive sampling effort in August and November 1998 and all uranium and uranium isotope data collected through the course of this study are included in the report.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr00413","usgsCitation":"Verstraeten, I., Steele, G.V., Cannia, J.C., Bohlke, J., Kraemer, T., Hitch, D., Wilson, K., and Carnes, A., 2001, Selected field and analytical methods and analytical results in the Dutch Flats area, western Nebraska, 1995-99: U.S. Geological Survey Open-File Report 2000-413, iv, 53 p., https://doi.org/10.3133/ofr00413.","productDescription":"iv, 53 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":160340,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0413/report-thumb.jpg"},{"id":59697,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0413/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nebraska","county":"Scotts Bluff County","otherGeospatial":"Dutch Flats","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-103.3605,42.0037],[-103.361,41.7442],[-103.3684,41.744],[-103.3681,41.7004],[-103.3681,41.6986],[-104.0522,41.6975],[-104.0522,41.7004],[-104.0525,41.998],[-104.0525,42.0024],[-103.9858,42.0018],[-103.8697,42.0021],[-103.6367,42.0025],[-103.5162,42.0027],[-103.3995,42.004],[-103.3605,42.0037]]]},\"properties\":{\"name\":\"Scotts Bluff\",\"state\":\"NE\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa5b8","contributors":{"authors":[{"text":"Verstraeten, Ingrid M.","contributorId":61033,"corporation":false,"usgs":true,"family":"Verstraeten","given":"Ingrid M.","affiliations":[],"preferred":false,"id":205240,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steele, G. V.","contributorId":62543,"corporation":false,"usgs":true,"family":"Steele","given":"G.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":205241,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cannia, J. C.","contributorId":105258,"corporation":false,"usgs":true,"family":"Cannia","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":205243,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bohlke, J. K. 0000-0001-5693-6455","orcid":"https://orcid.org/0000-0001-5693-6455","contributorId":59481,"corporation":false,"usgs":true,"family":"Bohlke","given":"J. K.","affiliations":[],"preferred":false,"id":205239,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kraemer, T.E.","contributorId":6492,"corporation":false,"usgs":true,"family":"Kraemer","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":205236,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hitch, D.E.","contributorId":72425,"corporation":false,"usgs":true,"family":"Hitch","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":205242,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wilson, K.E.","contributorId":51340,"corporation":false,"usgs":true,"family":"Wilson","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":205238,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Carnes, A.E.","contributorId":25208,"corporation":false,"usgs":true,"family":"Carnes","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":205237,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":31222,"text":"ofr0153 - 2001 - Magnetotelluric and audiomagnetotelluric data collected in Alaska by the U. S. Geological Survey, 1985-1992","interactions":[],"lastModifiedDate":"2024-05-03T19:40:05.831864","indexId":"ofr0153","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-53","title":"Magnetotelluric and audiomagnetotelluric data collected in Alaska by the U. S. Geological Survey, 1985-1992","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0153","usgsCitation":"Campbell, D.L., Sampson, J.A., Wise, R.A., and Williams, J.M., 2001, Magnetotelluric and audiomagnetotelluric data collected in Alaska by the U. S. Geological Survey, 1985-1992: U.S. Geological Survey Open-File Report 2001-53, 1 DVD, https://doi.org/10.3133/ofr0153.","productDescription":"1 DVD","costCenters":[],"links":[{"id":161030,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":409008,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43229.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -141,\n 60\n ],\n [\n -141,\n 71\n ],\n [\n -162,\n 71\n ],\n [\n -162,\n 60\n ],\n [\n -141,\n 60\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db644941","contributors":{"authors":[{"text":"Campbell, D. L.","contributorId":90726,"corporation":false,"usgs":true,"family":"Campbell","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":205365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sampson, J. A.","contributorId":57114,"corporation":false,"usgs":true,"family":"Sampson","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205363,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wise, R. A.","contributorId":79124,"corporation":false,"usgs":true,"family":"Wise","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205364,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, J. M.","contributorId":91142,"corporation":false,"usgs":true,"family":"Williams","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":205366,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":31227,"text":"ofr0165 - 2001 - Estimation of infiltration rates of saturated soils at selected sites in the Caloosahatchee River basin, southwestern Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:09:12","indexId":"ofr0165","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-65","title":"Estimation of infiltration rates of saturated soils at selected sites in the Caloosahatchee River basin, southwestern Florida","docAbstract":"Soil infiltration measurements were made at 23 sites in the Caloosahatchee River Basin in Glades, Hendry, and Lee Counties in southwestern Florida. The sandy soils of the basin are characterized by high infiltration rates limited in some areas by a high water table during the wet season. Because soil characteristics are similar within the basin, soils are classified by landscape group based on landscape cover and associated drainage. In accordance with this designation by the South Florida Water Management District, 11 sites are classified in the rock landscape group, 7 in the flatwoods landscape group, 4 in the slough landscape group, and 1 in the depression landscape group. \rData for 16 sites were fit to Horton's equation by using a regression analysis to estimate the infiltration rates of saturated soils. For some sites, an outlier value was removed prior to the regression analysis. Seven of the sites did not yield data that fit Horton's equation. The flatness of the plotted data suggests that saturated conditions may have been reached early in the test. The infiltration rate of saturated soils for these sites was estimated by averaging the data collected after the first 20 minutes of the test. \rFor all sites, the estimated infiltration rates of saturated soils ranged from 9.8 to 115 centimeters per hour in flatwoods, 3.4 to 66 centimeters per hour in rock, and 2.5 to 55 centimeters per hour in slough. The estimated soil infiltration rate at the one site in the depression was 181 centimeters per hour. Five sites were located on irrigation control berms where infiltration rates of the highly compacted and rocky soil may not represent the rates of less disturbed soils at sites within the same landscape groups. ","language":"ENGLISH","doi":"10.3133/ofr0165","usgsCitation":"Telis, P., 2001, Estimation of infiltration rates of saturated soils at selected sites in the Caloosahatchee River basin, southwestern Florida: U.S. Geological Survey Open-File Report 2001-65, iii, 16 p. : col. ill., col. map ; 28 cm. , https://doi.org/10.3133/ofr0165.","productDescription":"iii, 16 p. : col. ill., col. map ; 28 cm. ","costCenters":[],"links":[{"id":2798,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://fl.water.usgs.gov/Abstracts/ofr01_65_telis.html ","linkFileType":{"id":5,"text":"html"}},{"id":161072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0065/report-thumb.jpg"},{"id":59708,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb259","contributors":{"authors":[{"text":"Telis, P. A.","contributorId":13280,"corporation":false,"usgs":true,"family":"Telis","given":"P. A.","affiliations":[],"preferred":false,"id":205384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31230,"text":"ofr0169 - 2001 - Total recoverable selenium and other elements by HNO3 and HClO4 digestion and other soil characterization data from Wooley Valley units 3 and 4 waste rock dumps and Dairy Syncline lease area soils, Southeast Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:09:08","indexId":"ofr0169","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-69","title":"Total recoverable selenium and other elements by HNO3 and HClO4 digestion and other soil characterization data from Wooley Valley units 3 and 4 waste rock dumps and Dairy Syncline lease area soils, Southeast Idaho","language":"ENGLISH","doi":"10.3133/ofr0169","usgsCitation":"Amacher, M., Herring, J., and Stillings, L., 2001, Total recoverable selenium and other elements by HNO3 and HClO4 digestion and other soil characterization data from Wooley Valley units 3 and 4 waste rock dumps and Dairy Syncline lease area soils, Southeast Idaho: U.S. Geological Survey Open-File Report 2001-69, 65 leaves : col. ill. ; 28 cm. , https://doi.org/10.3133/ofr0169.","productDescription":"65 leaves : col. ill. ; 28 cm. ","costCenters":[],"links":[{"id":160552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0069/report-thumb.jpg"},{"id":59709,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0069/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db62820a","contributors":{"authors":[{"text":"Amacher, M.C.","contributorId":74043,"corporation":false,"usgs":true,"family":"Amacher","given":"M.C.","affiliations":[],"preferred":false,"id":205393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herring, J. R.","contributorId":43348,"corporation":false,"usgs":true,"family":"Herring","given":"J. R.","affiliations":[],"preferred":false,"id":205391,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stillings, L.L.","contributorId":52229,"corporation":false,"usgs":true,"family":"Stillings","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":205392,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31278,"text":"ofr01152 - 2001 - Preliminary compilation of data for selected oil test wells in Northern California","interactions":[],"lastModifiedDate":"2018-06-14T14:14:10","indexId":"ofr01152","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-152","title":"Preliminary compilation of data for selected oil test wells in Northern California","docAbstract":"Oil test wells can provide information on the depth, age, inclination, porosity, permeability, density, faulting, folding, and organic content of geologic formations mapped at the surface, or on units not recognized in surface outcrops. Formation density, as expressed in sonic and density logs commonly obtained when wells are drilled, has become increasingly important in making a crustal-scale 3-D seismic velocity model for the San Francisco Bay region. This model will be used for the calculation of realistic strong-ground motion synthetic seismograms (Brocher and others, 1997), and to determine the geometry of the basement surface beneath Tertiary basins (Jachens and others, 1997). The availability of this density and other information for oil test wells has, until recently, been restricted for competitive reasons, but several petroleum companies have recently made these data available. Accordingly, we began in 1992 to obtain these data to help prepare new geologic maps and geophysical models for the San Francisco Bay region, and to share the information with the public.\n\nThis report contains brief descriptions of information and materials available for 1,550 oil exploration and production wells in the following counties: Alameda (42), Butte (31), Colusa (103), Contra Costa (102), Glenn (103), Humboldt (33), Marin (6), Mendocino (2), Merced (33), Monterey (172), Napa (5), Placer (2), Sacramento (72), San Benito (51), San Joaquin (164), San Mateo (73), Santa Clara (8), Santa Cruz (23), Shasta (3), Siskiyou (1), Solano (251), Sonoma (10), Stanislaus (29), Sutter (59), Tehama (59), and Yolo (113).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01152","usgsCitation":"Brabb, E.E., Powell, C.L., and Brocher, T.M., 2001, Preliminary compilation of data for selected oil test wells in Northern California: U.S. Geological Survey Open-File Report 2001-152, 310 p., https://doi.org/10.3133/ofr01152.","productDescription":"310 p.","numberOfPages":"316","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":2902,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0152/","linkFileType":{"id":5,"text":"html"}},{"id":160187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0152/report-thumb.jpg"},{"id":59720,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0152/pdf/of01-152.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Alameda County;Butte County;Colusa County;Contra Costa County;Glenn County;Humboldt County;Marin County;Mendocino County;Merced County;Monterey County;Napa County;Placer County;Sacramento County;San Benito County;San Joaquin County;San Mateo County;Santa Clara County;Santa Cruz County;Shasta County;Siskiyou County;Solano County;Sonoma County;Stanislaus County;Sutter County;Tehama County;Yolo County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.42,35.79 ], [ -124.42,42.0 ], [ -116.7,42.0 ], [ -116.7,35.79 ], [ -124.42,35.79 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c72e","contributors":{"authors":[{"text":"Brabb, Earl E.","contributorId":48939,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":205560,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, Charles L. II 0000-0002-1913-555X cpowell@usgs.gov","orcid":"https://orcid.org/0000-0002-1913-555X","contributorId":3243,"corporation":false,"usgs":true,"family":"Powell","given":"Charles","suffix":"II","email":"cpowell@usgs.gov","middleInitial":"L.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":205559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brocher, Thomas M. 0000-0002-9740-839X brocher@usgs.gov","orcid":"https://orcid.org/0000-0002-9740-839X","contributorId":262,"corporation":false,"usgs":true,"family":"Brocher","given":"Thomas","email":"brocher@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":205558,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31279,"text":"ofr01155 - 2001 - Selected hydrologic and water-quality data for Kamas Valley and vicinity, Summit County, Utah, 1997-2000","interactions":[],"lastModifiedDate":"2017-04-11T09:49:47","indexId":"ofr01155","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-155","title":"Selected hydrologic and water-quality data for Kamas Valley and vicinity, Summit County, Utah, 1997-2000","docAbstract":"This report contains hydrologic and water-quality data collected in the Kamas Valley vicinity during a study from 1997 to 2000. The study area is in Summit County in north-central Utah and is part of the Middle Rocky Mountains Physiographic Province described by Fenneman (1931). Data were collected in Kamas Valley between the Uinta Mountains on the east and the West Hills on the west, the upper Weber River area, the Samak area along Beaver Creek, the Woodland area, and the Indian Hollow area. These areas, where population growth and water demand are concentrated, encompass about 70 square miles and include the Weber River, Beaver Creek, and Provo River drainages. Surface water is the dominant hydrologic resource. The combined average flow from these three drainages is about 345,000 acre-feet per year. Ground water is present in the unconsolidated deposits in Kamas Valley, in stream alluvium along Beaver Creek and the upper Weber River, and in the consolidated rocks surrounding Kamas Valley.
","language":"English","publisher":"U.S.Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr01155","collaboration":"Prepared in cooperation with the Utah Department Of Natural Resources, Division of Water Rights; Utah Department of Environmental Quality, Division of Water Quality; Weber Basin Water Conservancy District; Davis and Weber Counties Canal Company; and the Weber River Water Users Association","usgsCitation":"Haraden, P.L., Spangler, L., Brooks, L., and Stolp, B., 2001, Selected hydrologic and water-quality data for Kamas Valley and vicinity, Summit County, Utah, 1997-2000: U.S. Geological Survey Open-File Report 2001-155, Report: iv, 85 p.; 1 Plate: 18.92 x 26.04 inches, https://doi.org/10.3133/ofr01155.","productDescription":"Report: iv, 85 p.; 1 Plate: 18.92 x 26.04 inches","numberOfPages":"93","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":160188,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":339531,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/ofr01155/pdf/OFR01155.pdf"},{"id":2903,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr01155","linkFileType":{"id":5,"text":"html"}},{"id":258661,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2001/0155/plate-1.pdf","size":"3.70 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1","country":"United States","state":"Utah","county":"Summit County","otherGeospatial":"Kamas Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c45","contributors":{"authors":[{"text":"Haraden, Peter L.","contributorId":60276,"corporation":false,"usgs":true,"family":"Haraden","given":"Peter","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":205563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spangler, L.E.","contributorId":54230,"corporation":false,"usgs":true,"family":"Spangler","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":205562,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brooks, L.E.","contributorId":41852,"corporation":false,"usgs":true,"family":"Brooks","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":205561,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stolp, Bernard J. 0000-0003-3803-1497","orcid":"https://orcid.org/0000-0003-3803-1497","contributorId":71942,"corporation":false,"usgs":true,"family":"Stolp","given":"Bernard J.","affiliations":[],"preferred":false,"id":205564,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":31295,"text":"ofr01185 - 2001 - The Kiowa core, a continuous drill core through the Denver Basin bedrock aquifers at Kiowa, Elbert County, Colorado","interactions":[],"lastModifiedDate":"2018-12-11T12:54:41","indexId":"ofr01185","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-185","title":"The Kiowa core, a continuous drill core through the Denver Basin bedrock aquifers at Kiowa, Elbert County, Colorado","docAbstract":"The Kiowa core was obtained as a component of the Denver Basin Project, a cooperative research effort to study the evolution of the Denver Basin, Colorado. The Kiowa core provides a virtually continuous stratigraphic record of the Upper Cretaceous and lower Tertiary strata of the Denver Basin. The upper portion of the core recovered strata conventionally referred to as the Arapahoe and Denver Formations and the Dawson Arkose. A prominent unconformity marked by a mature paleosol breaks these strata into two unconformity-bounded sequences; the lower sequence is termed Dl and the upper sequence, D2. Beneath these units and also penetrated by the core occur the Laramie Formation, Fox Hills Sandstone, and Pierre Shale.
The site for coring was selected in order to obtain fine-grained strata suitable for both palynological and paleomagnetic analyses. The coring effort recovered 93 percent of the 2,256 ft of rock penetrated, resulting in a nearly continuous record of the sedimentary rocks recording the retreat of the Cretaceous Interior Seaway and the subsequent uplift of the Front Range portion of the Rocky Mountains.
Palynological data constrain the Cretaceous-Tertiary boundary to a depth between 878 and 880 ft in the core. The palynological data also serve to bracket the age of the paleosol marking the unconformity between the Dl and D2 sequences to between middle Paleocene and earliest Eocene. The paleomagnetic data are interpreted to represent polarity intervals ranging from polarity subchrons 31r to 28n and polarity subchron 24r.
Hydrologic analyses indicate variable aquifer characteristics across the State-defined bedrock aquifers. Individual aquifer units exhibit generally lower water-yield potential than was identified to the west in a core drilled by the U.S. Geological Survey (USGS) in 1987 at Castle Pines, Colorado. Downhole temperature measurements indicate a normal geothermal gradient of 30°C/ km. Perturbations of the gradient may represent active fluid flow through the aquifers penetrated by the core.
Petrographic examination of the cored sandstone and mudstone units document both the clay-rich character of the paleosol series marking the boundary between the Dl and D2 sequences, and variation in sandstone composition with depth. The lower sequence (Dl) is characterized by litharenites with a significant volcaniclastic component, while the upper sequence (D2) is more arkosic. Extensive lignite beds occur in Dl in the cored interval and these appear as strong reflectors on the seismic line that passes near the core hole. A set of electric logs, core descriptions, and derived data sets accompany this report.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01185","collaboration":"Prepared in cooperation with National Science Foundation, U.S. Geological Survey, Colorado Department of Natural Resources, Division of Water Resources, Office of the State Engineer, Colorado Geological Survey, Elbert County, Colorado, Colorado State University, University of Colorado, New Mexico Institute of Mining and Technology, University of Alaska, Scripps Institution of Oceanography","usgsCitation":"Raynolds, R.G., Johnson, K.R., Arnold, L., Farnham, T.M., Fleming, R., Hicks, J.F., Kelley, S.A., Lapey, L.A., Nichols, D.J., Obradovich, J.D., and Wilson, M., 2001, The Kiowa core, a continuous drill core through the Denver Basin bedrock aquifers at Kiowa, Elbert County, Colorado (Version 1.0): U.S. Geological Survey Open-File Report 2001-185, 127 p., https://doi.org/10.3133/ofr01185.","productDescription":"127 p.","costCenters":[],"links":[{"id":2932,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0185/","linkFileType":{"id":5,"text":"html"}},{"id":161292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0185/report-thumb.jpg"},{"id":59728,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0185/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Elbert County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.51053619384766,\n 39.319159627523035\n ],\n [\n -104.42161560058594,\n 39.319159627523035\n ],\n [\n -104.42161560058594,\n 39.37756814810105\n ],\n [\n -104.51053619384766,\n 39.37756814810105\n ],\n [\n -104.51053619384766,\n 39.319159627523035\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c03e","contributors":{"authors":[{"text":"Raynolds, Robert G.H.","contributorId":70814,"corporation":false,"usgs":true,"family":"Raynolds","given":"Robert","email":"","middleInitial":"G.H.","affiliations":[],"preferred":false,"id":205607,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Kirk R.","contributorId":16877,"corporation":false,"usgs":true,"family":"Johnson","given":"Kirk","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":205602,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Arnold, L. Rick","contributorId":101613,"corporation":false,"usgs":true,"family":"Arnold","given":"L. Rick","affiliations":[],"preferred":false,"id":205611,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Farnham, Timothy M.","contributorId":44202,"corporation":false,"usgs":true,"family":"Farnham","given":"Timothy","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":205605,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fleming, R. Farley","contributorId":83950,"corporation":false,"usgs":true,"family":"Fleming","given":"R. Farley","affiliations":[],"preferred":false,"id":205608,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hicks, Jason F.","contributorId":52235,"corporation":false,"usgs":true,"family":"Hicks","given":"Jason","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":205606,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kelley, Shari A.","contributorId":25606,"corporation":false,"usgs":true,"family":"Kelley","given":"Shari","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205604,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lapey, Laura A.","contributorId":103332,"corporation":false,"usgs":true,"family":"Lapey","given":"Laura","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":205612,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Nichols, Douglas J.","contributorId":87184,"corporation":false,"usgs":true,"family":"Nichols","given":"Douglas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":205610,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Obradovich, John D.","contributorId":84361,"corporation":false,"usgs":true,"family":"Obradovich","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":205609,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Wilson, Michael D.","contributorId":23188,"corporation":false,"usgs":true,"family":"Wilson","given":"Michael D.","affiliations":[],"preferred":false,"id":205603,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}} ,{"id":31296,"text":"ofr2001186 - 2001 - Borehole geophysical data from Eastland Woolen Mill Superfund site, Corinna, Maine, March 1999","interactions":[],"lastModifiedDate":"2022-07-22T20:05:32.728964","indexId":"ofr2001186","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-186","title":"Borehole geophysical data from Eastland Woolen Mill Superfund site, Corinna, Maine, March 1999","docAbstract":"Borehole-geophysical data were collected in\r\ncooperation with the U.S. Environmental Protection\r\nAgency in seven bedrock wells at the Eastland Woolen\r\nMill Superfund site, Penobscot County, Corinna,\r\nMaine, in March, 1999. The data were collected as part\r\nof a reconnaissance investigation to provide information\r\nneeded to address concerns about the distribution\r\nand fate of contaminants in ground-water at the site.\r\nThe borehole geophysical data were also needed to\r\nguide subsequent data collection associated with the\r\ndevelopment of a remediation workplan. The borehole\r\ngeophysical logs collected included: natural gamma,\r\ncaliper, fluid temperature, fluid conductivity, electromagnetic\r\nconductivity, electromagnetic resistivity,\r\nspontaneous potential, and single-point resistivity.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2001186","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency, Region 1","usgsCitation":"Hansen, B.P., Nichols, W.J., and Dudley, R.W., 2001, Borehole geophysical data from Eastland Woolen Mill Superfund site, Corinna, Maine, March 1999: U.S. Geological Survey Open-File Report 2001-186, iii, 20 p., https://doi.org/10.3133/ofr2001186.","productDescription":"iii, 20 p.","temporalStart":"1999-03-01","temporalEnd":"1999-03-31","costCenters":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"links":[{"id":59729,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0186/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0186/report-thumb.jpg"},{"id":2933,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://me.water.usgs.gov/reports/OFR01-186.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404390,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_42282.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Maine","city":"Corinna","otherGeospatial":"Eastland Woolen Mill Superfund site","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -69.267,\n 44.925\n ],\n [\n -69.258,\n 44.925\n ],\n [\n -69.258,\n 44.917\n ],\n [\n -69.267,\n 44.917\n ],\n [\n -69.267,\n 44.925\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc1c","contributors":{"authors":[{"text":"Hansen, Bruce P.","contributorId":90727,"corporation":false,"usgs":true,"family":"Hansen","given":"Bruce","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":205615,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, William J.","contributorId":20752,"corporation":false,"usgs":true,"family":"Nichols","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":205614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":205613,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31303,"text":"ofr2001220 - 2001 - Ground-water conditions in Georgia, 2000","interactions":[],"lastModifiedDate":"2016-12-07T16:06:43","indexId":"ofr2001220","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-220","title":"Ground-water conditions in Georgia, 2000","docAbstract":"Ground-water conditions in Georgia during 1999 and for the period of record were evaluated using data from U.S. Geological Survey ground-water-level and ground-water-quality monitoring networks. Data for 1999 included in this report are from continuous water-level records from 130 wells and chloride analyses from 14 wells. Data from one well is incomplete because data collection was discontinued. \r\nChloride concentration in water from the Upper Floridan aquifer in most of coastal Georgia was within drinking-water standards established by the Georgia Department of Natural Resources and the U.S. Environmental Protection Agency. In the Savannah area, chloride concentration has not changed appreciably with time. However, chloride concentration in water from some wells that tap the Floridan aquifer system in the Brunswick area exceeds the drinking-water standards.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2001220","usgsCitation":"Cressler, A.M., Blackburn, D., and McSwain, K., 2001, Ground-water conditions in Georgia, 2000: U.S. Geological Survey Open-File Report 2001-220, 182 p. , https://doi.org/10.3133/ofr2001220.","productDescription":"182 p. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d455","contributors":{"authors":[{"text":"Cressler, A. M.","contributorId":22791,"corporation":false,"usgs":true,"family":"Cressler","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":205638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blackburn, D.K.","contributorId":36602,"corporation":false,"usgs":true,"family":"Blackburn","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":205639,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McSwain, K.B.","contributorId":40643,"corporation":false,"usgs":true,"family":"McSwain","given":"K.B.","affiliations":[],"preferred":false,"id":205640,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31304,"text":"ofr01225 - 2001 - Measuring Taylor Slough boundary and internal flows, Everglades National Park, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:09:12","indexId":"ofr01225","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-225","title":"Measuring Taylor Slough boundary and internal flows, Everglades National Park, Florida","docAbstract":"Four intensive data-collection efforts, intended to represent the spectrum of precipitation events and associated flow conditions, were conducted during 1997 and 1998 in the Taylor Slough Basin, Everglades National Park. Flow velocities were measured by newly developed, portable Acoustic Doppler Velocity meters along three transects bisecting the Taylor Slough Basin from east to west, roughly perpendicular to the centerline axis of the slough as well as a fourth transect along the slough's axis. These meters provided the required levels of accuracy in flow-velocity measurements while enabling the rapid collection of multiple time series of flow data at remote sites. Concurrently, flow measurements were made along bordering road culverts and under L-31W and Taylor Slough bridges. Flows across the study area's boundaries provided net flow of water into the system and transect measurements provided flow data within the basin. Collected data are available through the World Wide Web (http://sofia.usgs.gov/projects/flow_velocity/). The high-water and low-water events corresponded with the highest and lowest flow velocities, respectively. The July 1998 data had lower than expected flow velocities and, in some cases, strong winds reversed flow direction.","language":"ENGLISH","doi":"10.3133/ofr01225","usgsCitation":"Tillis, G., 2001, Measuring Taylor Slough boundary and internal flows, Everglades National Park, Florida: U.S. Geological Survey Open-File Report 2001-225, 16 p., https://doi.org/10.3133/ofr01225.","productDescription":"16 p.","costCenters":[],"links":[{"id":2936,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr01-225 ","linkFileType":{"id":5,"text":"html"}},{"id":161421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611371","contributors":{"authors":[{"text":"Tillis, G.M.","contributorId":53840,"corporation":false,"usgs":true,"family":"Tillis","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":205641,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31305,"text":"ofr01228 - 2001 - Magnetotelluric data across the Battle Mountain-Eureka and Carlin trends, near Battle Mountain, Nevada","interactions":[],"lastModifiedDate":"2023-03-15T18:24:18.032367","indexId":"ofr01228","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-228","title":"Magnetotelluric data across the Battle Mountain-Eureka and Carlin trends, near Battle Mountain, Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01228","usgsCitation":"Williams, J.M., Rodriguez, B.D., and Klein, D.P., 2001, Magnetotelluric data across the Battle Mountain-Eureka and Carlin trends, near Battle Mountain, Nevada (Version 1.0): U.S. Geological Survey Open-File Report 2001-228, 205 p., https://doi.org/10.3133/ofr01228.","productDescription":"205 p.","costCenters":[],"links":[{"id":160005,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414242,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43385.htm","linkFileType":{"id":5,"text":"html"}},{"id":2957,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0228/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada","otherGeospatial":"Battle Mountain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.275,\n 40.833\n ],\n [\n -117.275,\n 40.375\n ],\n [\n -116.146,\n 40.375\n ],\n [\n -116.146,\n 40.833\n ],\n [\n -117.275,\n 40.833\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6493ff","contributors":{"authors":[{"text":"Williams, Jackie M.","contributorId":11217,"corporation":false,"usgs":true,"family":"Williams","given":"Jackie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":205643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodriguez, Brian D. 0000-0002-2263-611X brod@usgs.gov","orcid":"https://orcid.org/0000-0002-2263-611X","contributorId":836,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Brian","email":"brod@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":205642,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klein, Douglas P.","contributorId":50896,"corporation":false,"usgs":true,"family":"Klein","given":"Douglas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":205644,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31309,"text":"ofr01236 - 2001 - Water-quality data of soil water from three watersheds, Shenandoah National Park, Virginia, 1999-2000","interactions":[],"lastModifiedDate":"2017-05-31T10:33:55","indexId":"ofr01236","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-236","title":"Water-quality data of soil water from three watersheds, Shenandoah National Park, Virginia, 1999-2000","docAbstract":"Data on the chemical composition of soil-water samples were collected quarterly from three watersheds in Shenandoah National Park, Virginia, from September 1999 through July 2000. The soil-water samples were analyzed for specific conductance and concentrations of sodium, potassium, calcium, magnesium, ammonium, chloride, nitrate, sulfate, acid-neutralizing capacity, silica, and total monomeric aluminum. The soil-water data presented in this report can be used to support water-quality modeling of the response of streams to episodic acidification. Laboratory analytical data as well as laboratory quality-assurance information also are presented.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Richmond, VA","doi":"10.3133/ofr01236","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Rice, K.C., Maben, S.W., and Webb, J., 2001, Water-quality data of soil water from three watersheds, Shenandoah National Park, Virginia, 1999-2000: U.S. Geological Survey Open-File Report 2001-236, 17 p. , https://doi.org/10.3133/ofr01236.","productDescription":"17 p. ","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"links":[{"id":341587,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0236/ofr20010236.pdf","text":"Report","size":"182 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2001-0236"},{"id":160017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0236/coverthb.jpg"}],"country":"United States","state":"Virginia","otherGeospatial":"Shenandoah National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.20068359374999,\n 38.6275996886131\n ],\n [\n -78.1512451171875,\n 38.7283759182398\n ],\n [\n -78.12103271484375,\n 38.76693348394693\n ],\n [\n -78.1182861328125,\n 38.86109762182888\n ],\n [\n -78.19244384765625,\n 38.92522904714054\n ],\n [\n -78.25286865234375,\n 38.86965182408357\n ],\n [\n -78.24188232421875,\n 38.83756825896614\n ],\n [\n -78.30230712890624,\n 38.841846903808985\n ],\n [\n -78.3929443359375,\n 38.77121637244273\n ],\n [\n -78.4259033203125,\n 38.713375686254714\n ],\n [\n -78.3984375,\n 38.638327308061875\n ],\n [\n -78.4918212890625,\n 38.55031345037904\n ],\n [\n -78.5577392578125,\n 38.567495358827344\n ],\n [\n -78.59344482421875,\n 38.51378825951165\n ],\n [\n -78.55224609374999,\n 38.436379603\n ],\n [\n -78.607177734375,\n 38.41271038284709\n ],\n [\n -78.71429443359375,\n 38.33088431959971\n ],\n [\n -78.80218505859375,\n 38.272688535980976\n ],\n [\n -78.826904296875,\n 38.21012996629426\n ],\n [\n -78.82965087890625,\n 38.13239618602294\n ],\n [\n -78.82415771484375,\n 38.07404145941957\n ],\n [\n -78.70330810546875,\n 38.1237539824224\n ],\n [\n -78.695068359375,\n 38.201496974020806\n ],\n [\n -78.56597900390625,\n 38.28131307922966\n ],\n [\n -78.45611572265625,\n 38.34381037525605\n ],\n [\n -78.37921142578125,\n 38.371808917147554\n ],\n [\n -78.3544921875,\n 38.44498466889473\n ],\n [\n -78.31054687499999,\n 38.50948995925553\n ],\n [\n -78.23638916015625,\n 38.55031345037904\n ],\n [\n -78.23638916015625,\n 38.59326051987162\n ],\n [\n -78.20068359374999,\n 38.6275996886131\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Director, Virginia Water Science Center
U.S. Geological Survey
1730 East Parham Road
Richmond, VA 23228
The overarching goal of this project is to build a spatially distributed infrastructure for information science research by forming a team of information science researchers and providing them with similar hardware and software tools to perform collaborative research. Four geographically distributed Centers of the U.S. Geological Survey (USGS) are developing their own clusters of low-cost personal computers into parallel computing environments that provide a costeffective way for the USGS to increase participation in the high-performance computing community. Referred to as Beowulf clusters, these hybrid systems provide the robust computing power required for conducting research into various areas, such as advanced computer architecture, algorithms to meet the processing needs for real-time image and data processing, the creation of custom datasets from seamless source data, rapid turn-around of products for emergency response, and support for computationally intense spatial and temporal modeling.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01244","usgsCitation":"Crane, M., Steinwand, D., Beckmann, T., Krpan, G., Haga, J., Maddox, B., and Feller, M., 2001, A parallel-processing approach to computing for the geographic sciences: U.S. Geological Survey Open-File Report 2001-244, 38 p., https://doi.org/10.3133/ofr01244.","productDescription":"38 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":159853,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0244/report-thumb.jpg"},{"id":59738,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0244/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab89e","contributors":{"authors":[{"text":"Crane, Michael","contributorId":92307,"corporation":false,"usgs":true,"family":"Crane","given":"Michael","email":"","affiliations":[],"preferred":false,"id":205664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinwand, Dan","contributorId":31438,"corporation":false,"usgs":true,"family":"Steinwand","given":"Dan","email":"","affiliations":[],"preferred":false,"id":205658,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beckmann, Tim 0000-0002-2557-0638","orcid":"https://orcid.org/0000-0002-2557-0638","contributorId":87995,"corporation":false,"usgs":true,"family":"Beckmann","given":"Tim","affiliations":[],"preferred":false,"id":205662,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Krpan, Greg","contributorId":88400,"corporation":false,"usgs":true,"family":"Krpan","given":"Greg","email":"","affiliations":[],"preferred":false,"id":205663,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haga, Jim","contributorId":31439,"corporation":false,"usgs":true,"family":"Haga","given":"Jim","email":"","affiliations":[],"preferred":false,"id":205659,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Maddox, Brian","contributorId":54637,"corporation":false,"usgs":true,"family":"Maddox","given":"Brian","affiliations":[],"preferred":false,"id":205660,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Feller, Mark","contributorId":79931,"corporation":false,"usgs":true,"family":"Feller","given":"Mark","affiliations":[],"preferred":false,"id":205661,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":31315,"text":"ofr2001256 - 2001 - Rainfall, Streamflow, and Water-Quality Data During Stormwater Monitoring, Halawa Stream Drainage Basin, Oahu, Hawaii, July 1, 2000 to June 30, 2001","interactions":[],"lastModifiedDate":"2012-03-08T17:16:15","indexId":"ofr2001256","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-256","title":"Rainfall, Streamflow, and Water-Quality Data During Stormwater Monitoring, Halawa Stream Drainage Basin, Oahu, Hawaii, July 1, 2000 to June 30, 2001","docAbstract":"The State of Hawaii Department of Transportation Stormwater Monitoring Program was implemented on January 1, 2001. The program includes the collection of rainfall, streamflow, and water-quality data at selected sites in the Halawa Stream drainage basin. Rainfall and streamflow data were collected from July 1, 2000 to June 30, 2001. Few storms during the year met criteria for antecedent dry conditions or provided enough runoff to sample. The storm of June 5, 2001 was sufficiently large to cause runoff. On June 5, 2001, grab samples were collected at five sites along North Halawa and Halawa Streams. The five samples were later analyzed for nutrients, trace metals, oil and grease, total petroleum hydrocarbons, fecal coliform, biological and chemical oxygen demands, total suspended solids, and total dissolved solids.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr2001256","collaboration":"Prepared in cooperation with the State of Hawaii Department of Transportation","usgsCitation":"Presley, T.K., 2001, Rainfall, Streamflow, and Water-Quality Data During Stormwater Monitoring, Halawa Stream Drainage Basin, Oahu, Hawaii, July 1, 2000 to June 30, 2001: U.S. Geological Survey Open-File Report 2001-256, iii, 11 p., https://doi.org/10.3133/ofr2001256.","productDescription":"iii, 11 p.","temporalStart":"2000-07-01","temporalEnd":"2001-06-30","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":121871,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_2001_256.jpg"},{"id":2961,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://hi.water.usgs.gov/publications/pubs/ofr/ofr01-256.pdf","size":"703","linkFileType":{"id":1,"text":"pdf"}},{"id":13725,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/256/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -157.96666666666667,21.333333333333332 ], [ -157.96666666666667,21.466666666666665 ], [ -157.8,21.466666666666665 ], [ -157.8,21.333333333333332 ], [ -157.96666666666667,21.333333333333332 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660511","contributors":{"authors":[{"text":"Presley, Todd K. 0000-0001-5851-0634 tkpresle@usgs.gov","orcid":"https://orcid.org/0000-0001-5851-0634","contributorId":2671,"corporation":false,"usgs":true,"family":"Presley","given":"Todd","email":"tkpresle@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":205666,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24451,"text":"ofr012 - 2001 - PTCOUNT - a Fortran-77 computer program to calculate the areal distribution of mapped data points using count-circle methodology","interactions":[],"lastModifiedDate":"2012-02-02T00:08:19","indexId":"ofr012","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-2","title":"PTCOUNT - a Fortran-77 computer program to calculate the areal distribution of mapped data points using count-circle methodology","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr012","issn":"0094-9140","usgsCitation":"Savage, W.Z., Coe, J.A., and Sweeney, R.E., 2001, PTCOUNT - a Fortran-77 computer program to calculate the areal distribution of mapped data points using count-circle methodology (Version 1.0): U.S. Geological Survey Open-File Report 2001-2, 10 p., https://doi.org/10.3133/ofr012.","productDescription":"10 p.","costCenters":[],"links":[{"id":157196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1785,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0002/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689dd1","contributors":{"authors":[{"text":"Savage, William Z.","contributorId":107686,"corporation":false,"usgs":true,"family":"Savage","given":"William","email":"","middleInitial":"Z.","affiliations":[],"preferred":false,"id":191951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coe, Jeffrey A. 0000-0002-0842-9608 jcoe@usgs.gov","orcid":"https://orcid.org/0000-0002-0842-9608","contributorId":1333,"corporation":false,"usgs":true,"family":"Coe","given":"Jeffrey","email":"jcoe@usgs.gov","middleInitial":"A.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":191949,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sweeney, Ronald E.","contributorId":89564,"corporation":false,"usgs":true,"family":"Sweeney","given":"Ronald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":191950,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23329,"text":"ofr0177 - 2001 - Clay mineral content of continental shelf and river sediments, southern California","interactions":[],"lastModifiedDate":"2014-02-05T11:33:59","indexId":"ofr0177","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-77","title":"Clay mineral content of continental shelf and river sediments, southern California","docAbstract":"This report contains data on the clay mineral content of 250 shelf surface-sediment samples from the California Continental Borderland (Tables 1, 2; Figures 1-7), 79 samples with depth in cores from Santa Monica Bay (Table 3; see Table 1 for surface sediment data for those same cores and for core locations), 24 suspended and 13 bottom sediment samples from rivers draining Southern California (Table 4), and six rock samples or composite rock samples from the Palos Verdes Headland (Table 4). This report is designed as the data repository and these data are discussed in a paper by Hein et al. 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Long-term water-level data are required to address the effects of aquifer development and to compile a hydrologic record of water-level monitoring, uses of long-term water-level data, and improvements in the collection and accessibility of water-level data.","language":"ENGLISH","doi":"10.3133/cir1217","usgsCitation":"Taylor, C.J., and Alley, W., 2001, Ground-water-level monitoring and the importance of long-term water-level data: U.S. Geological Survey Circular 1217, 68 p., https://doi.org/10.3133/cir1217.","productDescription":"68 p.","costCenters":[],"links":[{"id":123410,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1217.bmp"},{"id":2634,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/circ1217/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697d7e","contributors":{"authors":[{"text":"Taylor, Charles J.","contributorId":93100,"corporation":false,"usgs":true,"family":"Taylor","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":203932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alley, William M.","contributorId":93030,"corporation":false,"usgs":true,"family":"Alley","given":"William M.","affiliations":[],"preferred":false,"id":203931,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70178302,"text":"70178302 - 2001 - Development of marine toxicity data for ordnance compounds","interactions":[],"lastModifiedDate":"2016-11-10T15:41:27","indexId":"70178302","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Development of marine toxicity data for ordnance compounds","docAbstract":"A toxicity database for ordnance compounds was generated using eight compounds of concern and marine toxicity tests with five species from different phyla. 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These were also the most degradable compounds, often being reduced to very low or below-detection levels at the end of the test exposure. Among the dinitro- and trinitrotoluenes and benzenes, toxicity tended to increase with the level of nitrogenation. Picric acid and RDX were the least toxic chemicals tested overall.
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