{"pageNumber":"3848","pageRowStart":"96175","pageSize":"25","recordCount":185189,"records":[{"id":6938,"text":"fs21195 - 1995 - Directions of ground-water flow in the Lost River watershed near Orleans, Indiana","interactions":[],"lastModifiedDate":"2016-05-04T13:26:13","indexId":"fs21195","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"211-95","title":"Directions of ground-water flow in the Lost River watershed near Orleans, Indiana","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs21195","usgsCitation":"Bayless, E.R., Taylor, C., Hopkins, M., and Arvin, D., 1995, Directions of ground-water flow in the Lost River watershed near Orleans, Indiana: U.S. Geological Survey Fact Sheet 211-95, 2 p. : map ; 28 cm. map ;, https://doi.org/10.3133/fs21195.","productDescription":"2 p. : map ; 28 cm. map ;","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":34222,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0211/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":125333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0211/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Lawrence, Orange","otherGeospatial":"Lost River Watershed","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-86.6853,38.994],[-86.5728,38.9941],[-86.4609,38.9942],[-86.4443,38.9942],[-86.3692,38.9941],[-86.3508,38.9941],[-86.3177,38.9936],[-86.2786,38.9935],[-86.2793,38.9636],[-86.2788,38.9341],[-86.2752,38.7642],[-86.2799,38.7628],[-86.2822,38.7601],[-86.2876,38.7533],[-86.2882,38.7474],[-86.2905,38.7447],[-86.2906,38.7356],[-86.2994,38.7343],[-86.3024,38.7357],[-86.3106,38.733],[-86.3084,38.6876],[-86.3091,38.4225],[-86.3068,38.3971],[-86.3614,38.3981],[-86.3808,38.3981],[-86.5969,38.3977],[-86.6439,38.3976],[-86.6515,38.3976],[-86.6814,38.3976],[-86.6815,38.4202],[-86.6821,38.4393],[-86.6823,38.5263],[-86.6824,38.5576],[-86.6838,38.645],[-86.6838,38.6464],[-86.6839,38.6618],[-86.6839,38.6867],[-86.6843,38.8191],[-86.6843,38.8209],[-86.6843,38.8508],[-86.6845,38.9079],[-86.6853,38.994]]]},\"properties\":{\"name\":\"Lawrence\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ab83","contributors":{"authors":[{"text":"Bayless, E. Randall 0000-0002-0357-3635","orcid":"https://orcid.org/0000-0002-0357-3635","contributorId":42586,"corporation":false,"usgs":true,"family":"Bayless","given":"E.","email":"","middleInitial":"Randall","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153608,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, C.J.","contributorId":22337,"corporation":false,"usgs":true,"family":"Taylor","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":153606,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hopkins, M.S.","contributorId":101255,"corporation":false,"usgs":true,"family":"Hopkins","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":153609,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Arvin, D.V.","contributorId":27438,"corporation":false,"usgs":true,"family":"Arvin","given":"D.V.","affiliations":[],"preferred":false,"id":153607,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":24693,"text":"ofr94480 - 1995 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, 1991-93","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"ofr94480","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-480","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, 1991-93","docAbstract":"This report contains hydrologic and climatic data that describe the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data are presented from January 1991 through December 1993. This report concentrates on data from fourth quarter 1993, and references historic data from 1991 and 1992. Total rainfall for 1993 was 95 inches which is 10 percent below the mean annual rainfall of 106 inches. In comparison, total rainfalls in 1992 and 1991 were 93 inches and 130 inches, respectively. Ground-water withdrawal has averaged 954,000 gallons per day during 1993, while with- drawals in 1992 and 1991 averaged 936,000 gallons per day and 927,000 gallons per day, respectively. In each of the five areas of ground-water produc- tion, withdrawals have remained steady since 1991. At the end of December 1993, the chloride concen- tration of the composite water supply was 36 milligrams per liter, well below the 250 milligrams per liter secondary drinking water standard established by the U.S. Environmental Protection Agency. Chloride concentrations of the composite water supply during the last quarter (October through December 1993) ranged between 35 and 75 milligrams per liter. Chloride concentrations in monitoring wells at Cantonment and Air Operations decreased during the last quarter (October through December 1993) after having risen progressively during the previous quarter (July through September 1993). There has been a general trend of increasing chloride concentrations in the deeper monitoring wells since the 1992 dry season, which began in March 1992. A fuel spill at Air Operations caused the shutdown of ten wells in May 1991. Four of the wells resumed pumping for water supply purposes in April 1992. The remaining six wells are being used to hydraulically contain and divert fuel migration.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr94480","issn":"0094-9140","usgsCitation":"Torikai, J., 1995, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, 1991-93: U.S. Geological Survey Open-File Report 94-480, v, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94480.","productDescription":"v, 41 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0480/report-thumb.jpg"},{"id":53726,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0480/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de895","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24937,"text":"ofr95800 - 1995 - Preliminary geologic map of the Newhall 7.5' quadrangle, southern California: a digital database","interactions":[{"subject":{"id":24937,"text":"ofr95800 - 1995 - Preliminary geologic map of the Newhall 7.5' quadrangle, southern California: a digital database","indexId":"ofr95800","publicationYear":"1995","noYear":false,"title":"Preliminary geologic map of the Newhall 7.5' quadrangle, southern California: a digital database"},"predicate":"SUPERSEDED_BY","object":{"id":70015,"text":"ofr20051019 - 2005 - Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California","indexId":"ofr20051019","publicationYear":"2005","noYear":false,"title":"Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California"},"id":1}],"supersededBy":{"id":70015,"text":"ofr20051019 - 2005 - Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California","indexId":"ofr20051019","publicationYear":"2005","noYear":false,"title":"Preliminary geologic map of the Los Angeles 30' x 60' quadrangle, Southern California"},"lastModifiedDate":"2012-02-02T00:08:23","indexId":"ofr95800","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-800","title":"Preliminary geologic map of the Newhall 7.5' quadrangle, southern California: a digital database","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr95800","issn":"0094-9140","usgsCitation":"Yerkes, R., and Campbell, R., 1995, Preliminary geologic map of the Newhall 7.5' quadrangle, southern California: a digital database: U.S. Geological Survey Open-File Report 95-800, 8 p.; map database, https://doi.org/10.3133/ofr95800.","productDescription":"8 p.; map database","costCenters":[],"links":[{"id":157548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7896,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/of95-800/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aed2","contributors":{"authors":[{"text":"Yerkes, R.F.","contributorId":105752,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.F.","affiliations":[],"preferred":false,"id":192833,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":192832,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24938,"text":"ofr95801 - 1995 - Preliminary geologic map of the Piru 7.5' quadrangle, southern California: A digital database","interactions":[],"lastModifiedDate":"2023-06-08T13:35:13.636878","indexId":"ofr95801","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-801","title":"Preliminary geologic map of the Piru 7.5' quadrangle, southern California: A digital database","docAbstract":"This Open-File report is a digital geologic map database. This pamphlet serves to introduce and describe the digital data. There is no paper map included in the Open-File report.\n\nThis digital map database is compiled from previously published sources combined with some new mapping and modifications in nomenclature. The geologic map database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U. S. Geological Survey. For detailed descriptions of the units, their stratigraphic relations and sources of geologic mapping consult Yerkes and Campbell (1995). More specific information about the units may be available in the original sources.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95801","usgsCitation":"Yerkes, R.F., and Campbell, R., 1995, Preliminary geologic map of the Piru 7.5' quadrangle, southern California: A digital database: U.S. Geological Survey Open-File Report 95-801, Readme; Database: .GZ files; Geology: 1 .GZ file; Structure: 1 .GZ file; Wells: 1 .GZ file; Composite base map: 1 .GZ file, https://doi.org/10.3133/ofr95801.","productDescription":"Readme; Database: .GZ files; Geology: 1 .GZ file; Structure: 1 .GZ file; Wells: 1 .GZ file; Composite base map: 1 .GZ file","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":284133,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/0801/pi-topo.e00.gz"},{"id":157549,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0801/report-thumb.jpg"},{"id":53905,"rank":8,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/1995/0801/pdf/of95-801.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":1912,"rank":7,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/0801/","linkFileType":{"id":5,"text":"html"}},{"id":284128,"rank":6,"type":{"id":9,"text":"Database"},"url":"https://pubs.usgs.gov/of/1995/0801/piru.tar.gz"},{"id":284129,"rank":5,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/0801/pi-geol.e00.gz"},{"id":284131,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/0801/pi-strc.e00.gz"},{"id":284132,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/0801/pi-wells.e00.gz"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.875,34.375 ], [ -118.875,34.500 ], [ -118.750,34.500 ], [ -118.750,34.375 ], [ -118.875,34.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67adc4","contributors":{"authors":[{"text":"Yerkes, R. F.","contributorId":24754,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":192834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":192835,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24699,"text":"ofr95473 - 1995 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1993 through March 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"ofr95473","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-473","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1993 through March 1995","docAbstract":"This report contains hydrologic and climatic data that describe the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data presented are from January 1993 through March 1995, although the report focuses on hydrologic events from January through March 1995. Cumulative rainfall for January through March 1995 was about 42 inches which is higher than the mean cumulative rainfall of about 33 inches for the same 3 months in a year. January and February are part of the annual wet season and March is the start of the annual dry season. Rainfall for each month was above average from the respective mean monthly rainfall. Ground- water withdrawal during January through March 1995 averaged 894,600 gallons per day. Withdrawal for the same 3 months in 1994 averaged 999,600 gallons per day. At the end of March 1995, the chloride concentration of the composite water supply was 26 milligrams per liter, well below the 250 milligrams per liter secondary drinking-water standard established by the U.S. Environmental Protection Agency. Chloride concentrations of the composite water supply from January through March 1995 ranged between 19 and 49 milligrams per liter. Chloride concentration of ground water in monitoring wells at Cantonment and Air Operations decreased since November 1994. The deepest monitoring wells show declines in chloride concentration by as much as 4,000 milligrams per liter. A fuel leak at Air Operations caused the shutdown of ten wells in May 1991. Four of the wells resumed pumping for water- supply purposes in April 1992. The remaining six wells are being used to hydraulically contain and divert fuel migration by recirculating about 150,000 gallons of water each day.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr95473","issn":"0094-9140","usgsCitation":"Torikai, J., 1995, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1993 through March 1995: U.S. Geological Survey Open-File Report 95-473, v, 42 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr95473.","productDescription":"v, 42 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":157921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0473/report-thumb.jpg"},{"id":53732,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0473/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e483be4b07f02db4f12d3","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192402,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24698,"text":"ofr95722 - 1995 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1993 through June 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"ofr95722","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-722","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1993 through June 1995","docAbstract":"This report contains hydrologic and climatic data that describe the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data presented are from January 1993 through June 1995, although the report focuses on hydrologic events from April through June 1995. Cumulative rainfall for April through June 1995 was about 14 inches which is 70 percent of the mean cumulative rainfall of about 20 inches for the same 3 months in a year. April through June is within the annual dry season. Rainfall for each month was below average from the respective mean monthly rainfall. All mean rainfall values are calculated for the fixed base period 1951-90. Ground-water withdrawal during April through June 1995 averaged 833,700 gallons per day. Withdrawal for the same 3 months in 1994 averaged 950,000 gallons per day.  At the end of June 1995, the chloride concentration of the composite water supply was 57 milligrams per liter, well below the 250 milligrams per liter secondary drinking-water standard established by the U.S. Environmental Protection Agency. Chloride concentrations of the composite water supply from April through June 1995 ranged between 26 and 62 milligrams per liter. Chloride concentration of ground water in monitoring wells at Cantonment and Air Operations increased since April 1995, with water from the deepest monitoring wells increasing in chloride concentra- tion by about 1000 milligrams per liter. A fuel leak at Air Operations caused the shutdown of ten wells in May 1991. Four of the wells resumed pumping for water-supply purposes in April 1992. The remaining six wells are being used to hydraulically contain and divert fuel migration away from water-supply wells by recirculating about 150,000 gallons of water each day.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr95722","issn":"0094-9140","usgsCitation":"Torikai, J., 1995, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1993 through June 1995: U.S. Geological Survey Open-File Report 95-722, v, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95722.","productDescription":"v, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0722/report-thumb.jpg"},{"id":53731,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0722/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf31","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192401,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26165,"text":"wri954234 - 1995 - Streamflow, ground-water recharge and discharge, and characteristics of surficial deposits in Buzzards Bay basin, southeastern Massachusetts","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri954234","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4234","title":"Streamflow, ground-water recharge and discharge, and characteristics of surficial deposits in Buzzards Bay basin, southeastern Massachusetts","docAbstract":"Streamflows exceeded between 50 and 99 percent of the time during water years 1967-91 were estimated for 14 low-flow partial-record stations and two discontinued streamflow-gaging stations in Buzzards Bay Basin, Massachusetts. At low flows, stream discharge per unit area for subbasins underlain primarily by stratified-drift deposits was several times greater than for subbasins underlain primarily by till and bedrock deposits. Streamflow measured three times at the Paskamanset River showed that streamflows downstream of municipal pumping wells were affected by ground-water pumpage near the river. Mean ground-water recharge rates were estimated to be 19.7 to 22.6 and 23.8 to 25.2 inches per year for basins underlain primarily by till and bedrock deposits and stratified drift deposits, respectively. Annual ground-water recharge during drought years can be less than one-half of the mean ground-water recharge rate for water years 1967-91. Ground-water discharge rates generally were estimated to be 1 to 4 inches per year less than ground-water recharge rates. Thus, ground-water discharge rates could be used as a low estimate of ground-water recharge rates. From the 50 to 99 percent flow duration, ground-water discharges averaged 85.7 percent of the total streamflow at six nearby streamflow-gaging stations. Ground-water discharges were estimated at the 16 stations in the basin by multiplying estimated streamflows at the selected flow durations from 50- to 99-percent for water years 1967-91 by 85.7 percent. Based on new well-log and seismic-refraction survey data, a few minor corrections were determined in existing saturated thickness maps for stratified-drift deposits in basin.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954234","usgsCitation":"Bent, G.C., 1995, Streamflow, ground-water recharge and discharge, and characteristics of surficial deposits in Buzzards Bay basin, southeastern Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 95-4234, v, 56 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954234.","productDescription":"v, 56 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2085,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri954234","linkFileType":{"id":5,"text":"html"}},{"id":123928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_95_4234.gif"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abac6","contributors":{"authors":[{"text":"Bent, Gardner C. 0000-0002-5085-3146 gbent@usgs.gov","orcid":"https://orcid.org/0000-0002-5085-3146","contributorId":1864,"corporation":false,"usgs":true,"family":"Bent","given":"Gardner","email":"gbent@usgs.gov","middleInitial":"C.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195925,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25516,"text":"wri954200 - 1995 - Geochemical processes and the effects of natural organic solutes on the solubility of selenium in coal-mine backfill samples from the Powder River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"wri954200","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4200","title":"Geochemical processes and the effects of natural organic solutes on the solubility of selenium in coal-mine backfill samples from the Powder River basin, Wyoming","docAbstract":"Geochemical processes and the effects of natural organic solutes on the solubility of selenium in coal-mine backfill aquifers were investigated. Backfill and ground-water samples were collected at coal mines in the Powder River Basin, Wyoming. Backfill was generally dominated by aluminum (14,400 to 49,000 mg/kg (milligrams per kilogram)), iron (3,330 to 23,200 mg/kg), and potassium (7,950 to 18,000 mg/kg). Backfill saturated-paste selenium concentrations ranged from 1 to 156 mg/kg (microsiemens per kilogram). Ground-water total selenium concentrations ranged from 3 to 125 mg/L. Dissolved organic carbon in all ground-water samples was dominated by hydrophobic and hydrophilic acids (38 to 84 percent). Selenite sorption/desorption experiments were conducted using background solutions of distilled-deionized water, 0.1 molar calcium chloride, and isolated hydrophobic and hydrophilic acids. Selenite sorption was larger when 0.1 molar calcium chloride was used. The addition of hydrophilic acid decreased selenite sorption more than the addition of hydrophobic acids. Geochemical modelling was used to predict the solid phases controlling dissolved selenium concentrations and to evaluate the effects of dissolved organic carbon on selenium solubility. Results suggested that 55 to 90 percent of selenium in backfill precipitation/dissolution extracts was dominated by magnesium selenate ion pairs. Dissolved organic carbon had little effect on selenium speciation. A redox chamber was constructed to control Eh and pH in water and backfill-core sample suspensions. The response of selenite and selenate in water samples to redox conditions did not follow thermodynamic predictions. Reduction of selenate in water samples did not occur at any of the redox levels tested.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954200","usgsCitation":"See, R., Reddy, K., Vance, G., Fadlelmawla, A., and Blaylock, M., 1995, Geochemical processes and the effects of natural organic solutes on the solubility of selenium in coal-mine backfill samples from the Powder River basin, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 95-4200, v, 55 p. :ill., map ;28 cm., https://doi.org/10.3133/wri954200.","productDescription":"v, 55 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123724,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4200/report-thumb.jpg"},{"id":54233,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4200/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adef8","contributors":{"authors":[{"text":"See, R.B.","contributorId":67910,"corporation":false,"usgs":true,"family":"See","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":194012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reddy, K.J.","contributorId":74035,"corporation":false,"usgs":true,"family":"Reddy","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":194013,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vance, G.F.","contributorId":95915,"corporation":false,"usgs":true,"family":"Vance","given":"G.F.","email":"","affiliations":[],"preferred":false,"id":194014,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fadlelmawla, A.A.","contributorId":67126,"corporation":false,"usgs":true,"family":"Fadlelmawla","given":"A.A.","email":"","affiliations":[],"preferred":false,"id":194011,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Blaylock, M.J.","contributorId":13657,"corporation":false,"usgs":true,"family":"Blaylock","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":194010,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":24695,"text":"ofr94479 - 1995 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through June 1994","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"ofr94479","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-479","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through June 1994","docAbstract":"This report contains hydrologic and climatic data that describe the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data are presented from January 1992 through June 1994. This report concentrates on data from 1994, and references historic data from 1992 and 1993. Total rainfall for the first half of 1994 was 51 inches which is 48 percent of the mean annual rainfall of 106 inches. In comparison, total rainfall for the first six months of 1993 and 1992 was 56 inches and 51 inches, respectively. Annual rainfall totals in 1993 and 1992 were 95 inches and 93 inches, respectively. Ground-water withdrawal has averaged 975,000 gallons per day through June 1994, while withdrawals in 1993 and 1992 averaged 954,000 gallons per day and 936,000 gallons per day, respectively. In each of the five areas of ground- water production, withdrawals have remained steady since 1991. At the end of June 1994, the chloride concentration of the composite water supply was 68 milligrams per liter, well below the 250 milligrams per liter secondary drinking water standard established by the U.S. Environmental Protection Agency. Chloride concentrations of the composite water supply from January through June 1994 ranged between 37 and 90 milligrams per liter. Chloride concentration of ground water in monitoring wells at Cantonment and Air Operations have increased very slightly since March 1994 coinciding with the start of the dry season. There has been a general trend of increasing chloride concentrations in the deeper monitoring wells since the 1992 dry season, which began in March 1992. A fuel spill at Air Operations caused the shutdown of ten wells in May 1991. Four of the wells resumed pumping for water-supply purposes in April 1992. The remaining six wells are being used to hydraulically contain and divert fuel migration.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nFor sale by the Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr94479","issn":"0094-9140","usgsCitation":"Torikai, J., 1995, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1992 through June 1994: U.S. Geological Survey Open-File Report 94-479, v, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94479.","productDescription":"v, 41 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0479/report-thumb.jpg"},{"id":53728,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0479/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69764b","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192398,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29682,"text":"wri954114 - 1995 - Water Budget for the Kohala Area, Island of Hawaii","interactions":[],"lastModifiedDate":"2012-03-08T17:16:15","indexId":"wri954114","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4114","title":"Water Budget for the Kohala Area, Island of Hawaii","docAbstract":"Ground-water recharge is estimated as the residual component of a monthly water budget calculated using long-term average rainfall, streamflow and pan evaporation data, and soil and vegetation characteristics. The water-budget components are defined seasonally, through the use of the monthly water budget, and spatially by topographic and geologic areas, through the use of a geographic information system model.\r\n\r\nThe long-term average ground-water recharge for the Kohala area, estimated by water-budget analysis for the topographic areas used in the analysis, is 162 Mgal/d in area A (south windward Kohala), 41 percent of average rainfall; 60 Mgal/d in area B (north windward Kohala), 33 percent of average rainfall; and 24 Mgal/d in area C (leeward Kohala), 13 percent of average rainfall.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri954114","usgsCitation":"Shade, P.J., 1995, Water Budget for the Kohala Area, Island of Hawaii: U.S. Geological Survey Water-Resources Investigations Report 95-4114, iv, 19 p., https://doi.org/10.3133/wri954114.","productDescription":"iv, 19 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":160144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4114/report-thumb.jpg"},{"id":58510,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4114/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd3f3","contributors":{"authors":[{"text":"Shade, Patricia J.","contributorId":30618,"corporation":false,"usgs":true,"family":"Shade","given":"Patricia","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":201946,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5534,"text":"fs20195 - 1995 - Monitoring environmental effects of irrigation projects in the West","interactions":[],"lastModifiedDate":"2017-06-30T10:23:04","indexId":"fs20195","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"201-95","title":"Monitoring environmental effects of irrigation projects in the West","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/fs20195","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1995, Monitoring environmental effects of irrigation projects in the West: U.S. Geological Survey Fact Sheet 201-95, [2] p. : ill., map ; 28 cm. ill., map ;, https://doi.org/10.3133/fs20195.","productDescription":"[2] p. : ill., map ; 28 cm. ill., map ;","costCenters":[],"links":[{"id":125327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0201/report-thumb.jpg"},{"id":32092,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0201/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.01367187499999,\n              46.01222384063236\n            ],\n            [\n              -124.45312499999999,\n              43.51668853502906\n            ],\n            [\n              -124.45312499999999,\n              41.178653972331674\n            ],\n            [\n              -124.365234375,\n              39.774769485295465\n            ],\n            [\n              -123.48632812499999,\n              37.996162679728116\n            ],\n            [\n              -120.9375,\n              34.74161249883172\n            ],\n            [\n              -118.740234375,\n              33.94335994657882\n            ],\n            [\n              -117.50976562499999,\n              33.43144133557529\n            ],\n            [\n              -117.158203125,\n              32.47269502206151\n            ],\n            [\n              -114.78515624999999,\n              32.62087018318113\n            ],\n            [\n              -110.830078125,\n              31.203404950917395\n            ],\n            [\n              -108.19335937499999,\n              31.27855085894653\n            ],\n            [\n              -108.19335937499999,\n              31.728167146023935\n            ],\n            [\n              -106.171875,\n              31.57853542647338\n            ],\n            [\n              -104.67773437499999,\n              30.14512718337613\n            ],\n            [\n              -103.974609375,\n              28.998531814051795\n            ],\n            [\n              -102.919921875,\n              28.613459424004414\n            ],\n            [\n              -102.83203125,\n              29.76437737516313\n            ],\n            [\n              -101.25,\n              29.916852233070173\n            ],\n            [\n              -100.10742187499999,\n              27.68352808378776\n            ],\n            [\n              -99.14062499999999,\n              26.194876675795218\n            ],\n            [\n              -97.29492187499999,\n              25.799891182088306\n            ],\n            [\n              -97.82226562499999,\n              27.059125784374043\n            ],\n            [\n              -96.67968749999999,\n              28.22697003891834\n            ],\n            [\n              -95.44921874999999,\n              28.844673680771766\n            ],\n            [\n              -93.33984374999999,\n              30.600093873550072\n            ],\n            [\n              -94.13085937499999,\n              33.284619968887654\n            ],\n            [\n              -94.39453125,\n              36.52729481454622\n            ],\n            [\n              -94.48242187499999,\n              38.34165619279595\n            ],\n            [\n              -94.92187499999999,\n              39.707186656826515\n            ],\n            [\n              -95.361328125,\n              40.446947059600454\n            ],\n            [\n              -95.9765625,\n              41.902277040963696\n            ],\n            [\n              -96.59179687499999,\n              42.74701217318067\n            ],\n            [\n              -96.59179687499999,\n              45.706179285330826\n            ],\n            [\n              -97.119140625,\n              48.86471476180277\n            ],\n            [\n              -111.09374999999999,\n              49.095452162534826\n            ],\n            [\n              -122.6953125,\n              48.980216985374994\n            ],\n            [\n              -122.6953125,\n              48.516604348867475\n            ],\n            [\n              -123.134765625,\n              48.04870994288686\n            ],\n            [\n              -125.15624999999999,\n              48.45835188280866\n            ],\n            [\n              -124.01367187499999,\n              46.01222384063236\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69912c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528639,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30259,"text":"wri954113 - 1995 - Ground-Water Availability from the Hawi Aquifer in the Kohala Area, Hawaii","interactions":[],"lastModifiedDate":"2012-03-08T17:16:15","indexId":"wri954113","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4113","title":"Ground-Water Availability from the Hawi Aquifer in the Kohala Area, Hawaii","docAbstract":"A ground-water study consisting of test-well drilling, aquifer tests, and numerical simulation was done to investigate ground-water availability in the basal part of the Hawi aquifer between the western drainage divide of Pololu Valley and Upolu Point in Kohala, Hawaii. The test-well drilling provided information on geology, water levels, water quality, vertical extent of the freshwater, and the thickness of the freshwater-saltwater transition zone in that aquifer. A total of 12 test wells were drilled at eight locations. Aquifer tests were done at five locations to estimate the hydraulic conductivity of the aquifer. Using information on the distribution of recharge, vertical extent of freshwater, hydraulic conductivity, and geometry of the basal aquifer, a numerical model was used to simulate the movement of water into, through, and out of the basal aquifer, and the effect of additional pumping on the water levels in the aquifer.\r\n\r\nResults of the modeling indicate that ground-water withdrawal of 20 million gallons per day above the existing withdrawal of 0.6 million gallons per day from the basal aquifer is hydrologically feasible, but that spacing, depth, and pumping rates of individual wells are important. If pumping is concentrated, the likelihood of saltwater intrusion is increased. The additional withdrawal of 20 million gallons per day would result in a reduction of ground-water discharge to the ocean by an amount equal to pumpage. Although model-calculated declines in water-level outside the area of pumping are small, pumping could cause some reduction of streamflow near the mouth of Pololu Stream.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri954113","usgsCitation":"Underwood, M.R., Meyer, W., and Souza, W.R., 1995, Ground-Water Availability from the Hawi Aquifer in the Kohala Area, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 95-4113, vi, 57 p., https://doi.org/10.3133/wri954113.","productDescription":"vi, 57 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":123867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4113/report-thumb.jpg"},{"id":59048,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4113/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db5457af","contributors":{"authors":[{"text":"Underwood, Mark R.","contributorId":45354,"corporation":false,"usgs":true,"family":"Underwood","given":"Mark","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":202950,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Souza, William R.","contributorId":90295,"corporation":false,"usgs":true,"family":"Souza","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202951,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24228,"text":"ofr95474 - 1995 - Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1994 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr95474","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-474","title":"Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1994 water year","docAbstract":"The computed annual yield and deficiency of the subbasins as defined in the Arkansas River Basin Compact, Arkansas-Oklahoma, are given in tables for the 1994 water year. Actual runoff from the subbasins and depletion caused by major reservoirs in the compact area also are given in tabular form. Monthly maximum, minimum, and mean discharges are shown for the 14 streamflow stations used in computing annual yield. Water-quality data are shown for 11 water-quality stations sampled in the Arkansas River Basin.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95474","issn":"0094-9140","usgsCitation":"Porter, J., 1995, Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1994 water year: U.S. Geological Survey Open-File Report 95-474, iii, 54 p. :map ;28 cm., https://doi.org/10.3133/ofr95474.","productDescription":"iii, 54 p. :map ;28 cm.","costCenters":[],"links":[{"id":155752,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0474/report-thumb.jpg"},{"id":53362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0474/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8228","contributors":{"authors":[{"text":"Porter, J.E.","contributorId":51779,"corporation":false,"usgs":true,"family":"Porter","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":191530,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26733,"text":"wri944253 - 1995 - Geochemistry of ground water in the Gallup, Dakota, and Morrison aquifers, San Juan Basin, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri944253","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-4253","title":"Geochemistry of ground water in the Gallup, Dakota, and Morrison aquifers, San Juan Basin, New Mexico","docAbstract":"Ground water was sampled from wells completed in the Gallup,\r\nDakota, and Morrison aquifers in the San Juan Basin, New Mexico,\r\nto examine controls on solute concentrations. Samples were \r\ncollected from 38 wells primarily from the Morrison aquifer (25 \r\nwells) in the northwestern part of the basin. A series of samples\r\nwas collected along ground-water flow paths; dissolved \r\nconstituents varied horizontally and vertically.\r\n\r\n     The understanding of the flow system changed as a result of\r\nthe geochemical analyses. The conceptual model of the flow system in\r\nthe Morrison aquifer prior to the study reported here assumed the\r\nWestwater Canyon Member of the Morrison aquifer as the only \r\nsignificant regional aquifer; flow was assumed to be two \r\ndimensional; and vertical leakage was assumed to be negligible.\r\nThe geochemical results indicate that the Westwater Canyon Member\r\nis not the only major water-yielding zone and that the flow\r\nsystem is three dimensional. The data presented in this report \r\nsuggest an upward component of flow into the Morrison aquifer. The \r\nentire section above and below the Morrison aquifer appears to be \r\ncontrolled by a three-dimensional flow regime where saline brine\r\nleaks near the San Juan River discharge area.\r\n\r\n     Predominant ions in the Gallup aquifer were calcium\r\nbicarbonate in recharge areas and sodium sulfate in discharge areas.  \r\nIn the Dakota aquifer, predominant ions were sodium bicarbonate and\r\nsodium sulfate. Water in the Morrison aquifer was predominantly sodium \r\nbicarbonate in the recharge area, changing to sodium sulfate \r\ndowngradient.\r\n\r\n     Chemical and radioisotopic data indicate that water from \r\noverlying and underlying units mixes with recharge water in the \r\nMorrison aquifer. Recharge water contained a large ratio of \r\nchlorine-36 to chlorine and a small ratio of bromide to chloride.\r\nApproximately 10 miles downgradient, samples from four wells \r\ncompleted in the Morrison aquifer were considerably different in\r\ncomposition compared to recharge samples. Oxygen stable isotopes\r\ndecreased by 2.8 per mil and deuterium decreased 26 per mil, \r\nrelative to recharge. Carbon-14 radioisotope activities were not\r\ndetectable. Chloride-36 radioisotope ratios were small and\r\nbromide to chloride concentration ratios were large. These results\r\nsuggest two potentially viable processes: ion filtration or trapping of\r\nancient dilute water recharged under a humid climate. For water\r\nsamples near the San Juan River, pH decreased to about 8.0, \r\nchloride concentrations increased to more than 100 milligrams per\r\nliter, and ratios of chlorine-36 to chlorine and bromide to \r\nchloride were small. Leakage of deep basin brine into the fresher\r\nwater of the Morrison aquifer appears to control ion concentrations.","language":"ENGLISH","publisher":"U.S. Geological Survey, [Water Resources Division, New Mexico District] ;\r\nCan be purchased from U.S.G.S. Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/wri944253","usgsCitation":"Dam, W.L., 1995, Geochemistry of ground water in the Gallup, Dakota, and Morrison aquifers, San Juan Basin, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 94-4253, vii, 76 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944253.","productDescription":"vii, 76 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":125156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4253/report-thumb.jpg"},{"id":55609,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4253/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aaeb3","contributors":{"authors":[{"text":"Dam, W. L.","contributorId":100890,"corporation":false,"usgs":true,"family":"Dam","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196906,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21715,"text":"ofr95469 - 1995 - Data on selected herbicides and two triazine metabolites in precipitation of the Midwestern and Northeastern United States, 1990-91","interactions":[],"lastModifiedDate":"2019-12-07T10:40:44","indexId":"ofr95469","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-469","title":"Data on selected herbicides and two triazine metabolites in precipitation of the Midwestern and Northeastern United States, 1990-91","docAbstract":"Weekly precipitation (rain and snow) samples were collected from 81 National Atmospheric Deposition Program/National Trends Network sites in the Midwestern and Northeastern United States for the analysis of herbicides. In addition, five high- elevation background sites along the Rocky Mountains and in Alaska were sampled to provide data on herbicides in precipitation at sites far from the study area. The study began in March 1990 and continued through September 1991. The precipitation samples were shipped to the Central Analytical Laboratory operated by the Illinois State Water Survey for analyses of inorganic compounds. Subsamples of the precipitation were shipped to the U.S. Geological Survey laboratory in Lawrence, Kansas, for the analysis of 11 herbicides and 2 triazines metabolites. This report provides descriptions of the study area, sample-collection methods, laboratory methods, and quality assurance. The report also includes a compilation of herbicide concentration data from both enzyme-linked immunosorbent assay and gas chromatography/mass spectrometry methods. Laboratory analyses consisted of 6,230 samples that were analyzed by enzyme-linked immunosorbent assay using alachlor and atrazine microtiter plates and 2,341 samples that were confirmed by gas chromatography/mass spectrometry analysis. Graphical and statistical comparisons of the two analytical methods are given in this report. Data from this study have been useful in determining the spatial and temporal distribution of herbicide concentrations and deposition in precipitation of over a 26-State area of the Midwestern and Northeastern United States. The data also provide evidence of long-range atmospheric transport of herbicides and triazine metabolites.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95469","issn":"0566-8174","usgsCitation":"Goolsby, D.A., Scribner, E., Thurman, E., Pomes, M., and Meyer, M.T., 1995, Data on selected herbicides and two triazine metabolites in precipitation of the Midwestern and Northeastern United States, 1990-91: U.S. Geological Survey Open-File Report 95-469, iv, 341 p., https://doi.org/10.3133/ofr95469.","productDescription":"iv, 341 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":154557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0469/report-thumb.jpg"},{"id":51242,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0469/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.150390625,\n              48.80686346108517\n            ],\n            [\n              -101.865234375,\n              36.527294814546245\n            ],\n            [\n              -81.298828125,\n              35.02999636902566\n            ],\n            [\n              -67.587890625,\n              45.213003555993964\n            ],\n            [\n              -68.64257812499999,\n              47.39834920035926\n            ],\n            [\n              -82.353515625,\n              41.96765920367816\n            ],\n            [\n              -83.49609375,\n              46.13417004624326\n            ],\n            [\n              -88.330078125,\n              48.3416461723746\n            ],\n            [\n              -104.150390625,\n              48.80686346108517\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bdbc","contributors":{"authors":[{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":185386,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scribner, E.A.","contributorId":50925,"corporation":false,"usgs":true,"family":"Scribner","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":185387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":185390,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pomes, M.L.","contributorId":84393,"corporation":false,"usgs":true,"family":"Pomes","given":"M.L.","affiliations":[],"preferred":false,"id":185388,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meyer, M. T.","contributorId":92279,"corporation":false,"usgs":true,"family":"Meyer","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":185389,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":21671,"text":"ofr94523 - 1995 - Chemical data for water samples collected during four upriver cruises on the Mississippi River between New Orleans, Louisiana, and Minneapolis, Minnesota, May 1990-April 1992","interactions":[],"lastModifiedDate":"2018-10-22T18:45:05","indexId":"ofr94523","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-523","title":"Chemical data for water samples collected during four upriver cruises on the Mississippi River between New Orleans, Louisiana, and Minneapolis, Minnesota, May 1990-April 1992","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94523","issn":"0566-8174","usgsCitation":"1995, Chemical data for water samples collected during four upriver cruises on the Mississippi River between New Orleans, Louisiana, and Minneapolis, Minnesota, May 1990-April 1992: U.S. Geological Survey Open-File Report 94-523, xii, 297 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94523.","productDescription":"xii, 297 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":154405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0523/report-thumb.jpg"},{"id":51215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0523/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3c50","contributors":{"editors":[{"text":"Moody, J. A.","contributorId":32930,"corporation":false,"usgs":true,"family":"Moody","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":749279,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":25523,"text":"wri944237 - 1995 - Geohydrology and water quality of the Durham Center Area, Durham, Connecticut","interactions":[],"lastModifiedDate":"2019-10-15T06:53:59","indexId":"wri944237","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-4237","title":"Geohydrology and water quality of the Durham Center Area, Durham, Connecticut","docAbstract":"Contaminated ground water is widespread and persistent beneath the Durham Center area in the town of Durham, Conn. Most of the contaminants are organic halides, usually trichloroethene, 1,1,1-trichloroethane, and tetrachloroethene. Less extensive chemical contamination of surface water, soil, and glacial sediments also has been detected. Two manufacturing companies, located at the northern and southern ends of this largely residential area, are believed to be the principal sources of the organic compounds detected in ground water. The contamination of water in the bedrock, the primary source of drinking water throughout the area, is the major environmental concern. Maximum concentrations of trichloroethene in three bed- rock wells range from 4,500 to about 5,500 mg/L (micrograms per liter). Concentrations of trichloroethene greater than 5 mg/L, the maximum contaminant level established for drinking water by the U.S Environmental Protection Agency, have regularly been detected in water samples from many other bedrock wells for at least 9 years. The geohydrology of the area is highly complex. Compact lodgment till that is up to 30 feet thick and probably fractured, overlies the bedrock. The bedrock is lithologically heterogeneous, and con- sists mostly of red fluvial sandstone, siltstone, and conglomerate; it is locally interbedded with black lacustrine shales and gray sandstones. Lithology and stratigraphy interpreted from borehole-geophysical logs at Durham Center are consistent with the Portland Formation subfacies described in earlier geologic studies. Beds strike nearly north-south and dip gently eastward. At least one high-angle normal fault transects the bedrock; it strikes northeast and dips northwest. Acoustic televiewer logs, measurements at out-crops, and azimuthal, square-array, resistivity data indicate a dominance of northeast-striking fractures that dip steeply northwest and southeast. Less prevalent strike directions are north to east-north-east. The till and sedimentary bedrock are dual-porosity, dual-permeability media. The hydraulic conductivity of the bulk mass of till is believed to be on the order of tenths of a foot per day to about 2.5 feet per day, with a total porosity of about 25 percent and an estimated average fracture porosity of less than 1 percent. The reported transmissivities of the bedrock range from less than 1 to about 17,000 feet squared per day and storativity is generally about 10-4, but the accuracy of these values is uncertain. The intergranular porosity of the sandstone units is estimated to average 5 percent, and estimates of fracture porosity from square-array, resistivity soundings at two sites were 1.1 and 2.7 percent. The bedrock has characteristics of both a single aquifer and a multi-unit, artesian or leaky aquifer system. A local ground-water-flow system that includes the upper part of the bedrock is unconfined. A large- scale flow system in deeper parts of the bedrock has transported organic compounds across topographic drainage divides. Borehole-geophysical logs and head measurements indicate that the natural ground- water-flow system in the bedrock has been altered by drilled wells that connect fractures and by with- drawals from wells. A conceptual model of the movement and fate of organic contaminants suggests that (1) nonaqueous phase organic halides are retained near their source; (2) flow is primarily through fractures in the till and through fractures and bedding-plane openings in the sedimentary rocks; (3) retardation of contaminants occurs primarily by diffusion from fractures into the aquifer matrix; and (4) transport directions of dissolved organic halides are controlled by a combination of natural hydraulic gradients, hydraulic gradients produced by the cyclical pumping of wells, and by the strike directions of bedrock faults, fractures, and bedding planes.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri944237","usgsCitation":"Melvin, R., Stone, J.R., Craft, P.A., Lane, J., and Davies, B., 1995, Geohydrology and water quality of the Durham Center Area, Durham, Connecticut: U.S. Geological Survey Water-Resources Investigations Report 94-4237, v, 97 p., https://doi.org/10.3133/wri944237.","productDescription":"v, 97 p.","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":124048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4237/report-thumb.jpg"},{"id":54239,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4237/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Connecticut","county":"Middlesex 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R.","contributorId":87964,"corporation":false,"usgs":true,"family":"Stone","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":194037,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Craft, P. A.","contributorId":102105,"corporation":false,"usgs":true,"family":"Craft","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194038,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lane, J.W. Jr.","contributorId":66723,"corporation":false,"usgs":true,"family":"Lane","given":"J.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":194035,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Davies, B.S. III","contributorId":72413,"corporation":false,"usgs":true,"family":"Davies","given":"B.S.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":194036,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":23762,"text":"ofr95423 - 1995 - Water-resources activities in Arkansas, 1992-94","interactions":[],"lastModifiedDate":"2012-02-02T00:08:11","indexId":"ofr95423","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-423","title":"Water-resources activities in Arkansas, 1992-94","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Report Section [distributor],","doi":"10.3133/ofr95423","issn":"0094-9140","usgsCitation":"Louthian, B.L., 1995, Water-resources activities in Arkansas, 1992-94: U.S. Geological Survey Open-File Report 95-423, iv, 44 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95423.","productDescription":"iv, 44 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0423/report-thumb.jpg"},{"id":52992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0423/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa147","contributors":{"authors":[{"text":"Louthian, Bobbie L. louthian@usgs.gov","contributorId":737,"corporation":false,"usgs":true,"family":"Louthian","given":"Bobbie","email":"louthian@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":190673,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23700,"text":"ofr95435 - 1995 - Bibliography for Hayes, Spurr, Crater Peak, Redoubt, Iliamna, Augustine, Douglas, and Aniakchak volcanoes, Alaska","interactions":[],"lastModifiedDate":"2019-06-05T12:34:31","indexId":"ofr95435","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-435","title":"Bibliography for Hayes, Spurr, Crater Peak, Redoubt, Iliamna, Augustine, Douglas, and Aniakchak volcanoes, Alaska","docAbstract":"Alaska has more than 40 active volcanoes, many of which are close to the major population centers of south-central Alaska. This bibliography was compiled to assist in the preparation of volcano hazard evaluations at Cook Inlet volcanoes. It lists articles, reports, and maps about the geology and hydrology of Hayes, Spurr, Redoubt, Iliamna, Augustine, and Douglas volcanoes in the Cook Inlet region as well as Aniakchak Volcano on the Alaska Peninsula. References on the biology and archaeology of areas surrounding each volcano also are included because they may provide useful background information.","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/ofr95435","issn":"0094-9140","usgsCitation":"Lemke, K., May, B., and Vanderpool, A., 1995, Bibliography for Hayes, Spurr, Crater Peak, Redoubt, Iliamna, Augustine, Douglas, and Aniakchak volcanoes, Alaska: U.S. Geological Survey Open-File Report 95-435, iii, 32 p. , https://doi.org/10.3133/ofr95435.","productDescription":"iii, 32 p. ","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":52948,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0435/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0435/report-thumb.jpg"}],"country":"United States","state":"Alaska","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629ac5","contributors":{"authors":[{"text":"Lemke, K.J.","contributorId":12519,"corporation":false,"usgs":true,"family":"Lemke","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":190566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, B.A.","contributorId":8872,"corporation":false,"usgs":true,"family":"May","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":190565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vanderpool, A.M.","contributorId":14451,"corporation":false,"usgs":true,"family":"Vanderpool","given":"A.M.","affiliations":[],"preferred":false,"id":190567,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23617,"text":"ofr95816 - 1995 - Re-examination of rock geochemistry in the Copper Canyon area, Lander County, Nevada","interactions":[],"lastModifiedDate":"2022-08-31T18:25:11.201831","indexId":"ofr95816","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-816","title":"Re-examination of rock geochemistry in the Copper Canyon area, Lander County, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95816","usgsCitation":"Kotlyar, B.B., Theodore, T.G., and Jachens, R., 1995, Re-examination of rock geochemistry in the Copper Canyon area, Lander County, Nevada: U.S. Geological Survey Open-File Report 95-816, 47 p., https://doi.org/10.3133/ofr95816.","productDescription":"47 p.","costCenters":[],"links":[{"id":406010,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18553.htm","linkFileType":{"id":5,"text":"html"}},{"id":52894,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0816/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154871,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0816/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Lander County","otherGeospatial":"Copper Canyon area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.15,\n              40.517\n            ],\n            [\n              -117.1179,\n              40.517\n            ],\n            [\n              -117.117,\n              40.567\n            ],\n            [\n              -117.15,\n              40.567\n            ],\n            [\n              -117.15,\n              40.517\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6486c3","contributors":{"authors":[{"text":"Kotlyar, B. B.","contributorId":74408,"corporation":false,"usgs":true,"family":"Kotlyar","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Theodore, T. G.","contributorId":38122,"corporation":false,"usgs":true,"family":"Theodore","given":"T.","middleInitial":"G.","affiliations":[],"preferred":false,"id":190421,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jachens, R.C.","contributorId":55433,"corporation":false,"usgs":true,"family":"Jachens","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":190422,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27410,"text":"wri944110 - 1995 - Water levels in the Calumet aquifer and their relation to surface-water levels in northern Lake County, Indiana, 1985-92","interactions":[],"lastModifiedDate":"2016-05-24T10:55:16","indexId":"wri944110","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-4110","title":"Water levels in the Calumet aquifer and their relation to surface-water levels in northern Lake County, Indiana, 1985-92","docAbstract":"<p>The U.S. Geological Survey made 2,328 water-level measurements at a total of 96 ground-water and surface-water sites in northern Lake County, Indiana, from August 1985 through September 1992. This report lists and summarizes the significance of the measurements. Northern Lake County is on the southern shore of Lake Michigan and includes the cities of East Chicago, Gary, Hammond, and Whiting. The study area is underlain by the unconfined Calumet aquifer and receives about 36 inches of precipitation per year.</p>\n<p>The U.S. Geological Survey investigated ground-water levels and flow in the Calumet aquifer and the effect of Lake Michigan levels on ground-water and surface-water levels throughout the study area. Summary statistics of the water-level data were computed for each site.</p>\n<p>Ground-water levels annually reach a maximum in June or July and a minimum in September or October. Measured groundwater fluctuations in the Calumet aquifer during the study period ranged from 0.40 to 5.01 feet, and the mean ground-water fluctuation was about 2.3 feet The largest surface-water fluctuations were affected by record setting Lake Michigan levels. Midmonth daily averages for the data-collection period show that Lake Michigan fluctuated 4.14 feet Water-level fluctuations on the Grand Calumet River were from 1.06 to 2.45 feet.</p>\n<p>Analysis of water-level data indicates that the 1988 drought did not substantially affect water levels in the Calumet aquifer, but the deficit in precipitation reversed vertical flow gradients in ground water at three paired deep and shallow wells. High water levels in Lake Michigan during 1985-87 created long-term backwater effects on the Grand Calumet River as far as 11.0 miles upstream from Lake Michigan.</p>\n<p>Analysis of water-level data from the data-collection network indicates that the water table normally slopes toward streams, ditches, sewers, the Indiana Harbor Canal, and Lake Michigan. The slope of the water table toward the Grand Calumet River is greatest in the winter and can decrease to being almost horizontal in the summer. Wells near streams respond quickly to nearby surface-water-level changes. Water-table maps indicate that sewers and dewatering systems are lowering ground-water levels in large areas. Ditches, the Grand Calumet River, and the Indiana Harbor Canal connect the Lake Michigan water level to large parts of the study area. The surface-water stage in the Indiana Harbor Canal, which functions as a ditch, can equal Lake Michigan's stage up to 3.75 miles inland from the lakeshore. Human activity, the stage of Lake Michigan, and the storage capacity of the Calumet aquifer combine to reduce vertical changes in the water table in the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri944110","collaboration":"Indiana Department of Environmental Management","usgsCitation":"Greeman, T.K., 1995, Water levels in the Calumet aquifer and their relation to surface-water levels in northern Lake County, Indiana, 1985-92: U.S. Geological Survey Water-Resources Investigations Report 94-4110, v, 61 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944110.","productDescription":"v, 61 p. :ill., maps ;28 cm.","startPage":"1","endPage":"61","numberOfPages":"67","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":158683,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4110/report-thumb.jpg"},{"id":56269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Lake","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-87.2223,41.6248],[-87.2222,41.6152],[-87.2221,41.6039],[-87.2218,41.5698],[-87.22,41.4632],[-87.2198,41.3747],[-87.2196,41.3601],[-87.22,41.3388],[-87.2198,41.3188],[-87.2197,41.3043],[-87.2189,41.2893],[-87.2187,41.2744],[-87.2193,41.2671],[-87.219,41.2426],[-87.2184,41.2417],[-87.2263,41.2353],[-87.2762,41.2187],[-87.2859,41.2154],[-87.3241,41.1862],[-87.3313,41.1829],[-87.3405,41.1824],[-87.3448,41.1824],[-87.38,41.1726],[-87.394,41.1625],[-87.4,41.1625],[-87.4055,41.1625],[-87.4147,41.1619],[-87.4411,41.1731],[-87.4466,41.174],[-87.4484,41.1744],[-87.4587,41.1702],[-87.4801,41.1701],[-87.5263,41.1661],[-87.5261,41.267],[-87.5265,41.2983],[-87.527,41.4086],[-87.5265,41.4712],[-87.5255,41.5516],[-87.5239,41.6941],[-87.524,41.7135],[-87.5234,41.7131],[-87.5134,41.7054],[-87.5158,41.7027],[-87.5133,41.7004],[-87.4997,41.6914],[-87.4922,41.6865],[-87.4848,41.6843],[-87.4829,41.6811],[-87.4768,41.6789],[-87.4712,41.6753],[-87.4613,41.6718],[-87.4503,41.6741],[-87.4397,41.6647],[-87.436,41.6656],[-87.4355,41.6729],[-87.4245,41.6802],[-87.4177,41.6753],[-87.4396,41.6565],[-87.4228,41.6439],[-87.4167,41.6439],[-87.4099,41.644],[-87.4087,41.644],[-87.4044,41.6413],[-87.392,41.6382],[-87.3748,41.6329],[-87.3711,41.6315],[-87.3538,41.6285],[-87.3384,41.6259],[-87.3274,41.6259],[-87.3218,41.6219],[-87.315,41.6201],[-87.3101,41.6201],[-87.3058,41.6202],[-87.3003,41.6202],[-87.296,41.6198],[-87.2831,41.6203],[-87.2702,41.6208],[-87.2223,41.6248]]]},\"properties\":{\"name\":\"Lake\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9d21","contributors":{"authors":[{"text":"Greeman, Theodore K.","contributorId":30655,"corporation":false,"usgs":true,"family":"Greeman","given":"Theodore","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":198064,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28047,"text":"wri954055 - 1995 - Methods to estimate annual mean spring discharge to the Snake River between Milner Dam and King Hill, Idaho","interactions":[],"lastModifiedDate":"2013-11-22T13:14:41","indexId":"wri954055","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4055","title":"Methods to estimate annual mean spring discharge to the Snake River between Milner Dam and King Hill, Idaho","docAbstract":"Many individual springs and groups of springs discharge water from volcanic rocks that form the north canyon wall of the Snake River between Milner Dam and King Hill. Previous estimates of annual mean discharge from these springs have been used to understand the hydrology of the eastern part of the Snake River Plain. Four methods that were used in previous studies or developed to estimate annual mean discharge since 1902 were (1) water-budget analysis of the Snake River; (2) correlation of water-budget estimates with discharge from 10 index springs; (3) determination of the combined discharge from individual springs or groups of springs by using annual discharge measurements of 8 springs, gaging-station records of 4 springs and 3 sites on the Malad River, and regression equations developed from 5 of the measured springs; and (4) a single regression equation that correlates gaging-station records of 2 springs with historical water-budget estimates. Comparisons made among the four methods of estimating annual mean spring discharges from 1951 to 1959 and 1963 to 1980 indicated that differences were about equivalent to a measurement error of 2 to 3 percent. The method that best demonstrates the response of annual mean spring discharge to changes in ground-water recharge and discharge is method 3, which combines the measurements and regression estimates of discharge from individual springs.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954055","usgsCitation":"Kjelstrom, L., 1995, Methods to estimate annual mean spring discharge to the Snake River between Milner Dam and King Hill, Idaho: U.S. Geological Survey Water-Resources Investigations Report 95-4055, iv, 9 p., https://doi.org/10.3133/wri954055.","productDescription":"iv, 9 p.","numberOfPages":"13","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":123596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4055/report-thumb.jpg"},{"id":56885,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Snake River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.25,42.0 ], [ -115.25,43.0 ], [ -114.0,43.0 ], [ -114.0,42.0 ], [ -115.25,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62d060","contributors":{"authors":[{"text":"Kjelstrom, L.C.","contributorId":89104,"corporation":false,"usgs":true,"family":"Kjelstrom","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":199124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21863,"text":"ofr9575G - 1995 - Hydrocarbon source rock characterization and maturity based on rock-eval pyrolysis and vitrinite reflectance of Eocene strata, southern Oregon Coast Range, Douglas and Coos Counties, southwest Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr9575G","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-75","chapter":"G","title":"Hydrocarbon source rock characterization and maturity based on rock-eval pyrolysis and vitrinite reflectance of Eocene strata, southern Oregon Coast Range, Douglas and Coos Counties, southwest Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr9575G","issn":"0566-8174","usgsCitation":"Lillis, P.G., Daws, T., Pawlewicz, M., Niem, A.R., and Ryu, I., 1995, Hydrocarbon source rock characterization and maturity based on rock-eval pyrolysis and vitrinite reflectance of Eocene strata, southern Oregon Coast Range, Douglas and Coos Counties, southwest Oregon: U.S. Geological Survey Open-File Report 95-75, 27 p.; 30 leaves :ill., map ;28 cm., https://doi.org/10.3133/ofr9575G.","productDescription":"27 p.; 30 leaves :ill., map ;28 cm.","costCenters":[],"links":[{"id":153025,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0075g/report-thumb.jpg"},{"id":51349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0075g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db6296a1","contributors":{"authors":[{"text":"Lillis, Paul G. 0000-0002-7508-1699 plillis@usgs.gov","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":1817,"corporation":false,"usgs":true,"family":"Lillis","given":"Paul","email":"plillis@usgs.gov","middleInitial":"G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":186025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daws, T.A.","contributorId":56651,"corporation":false,"usgs":true,"family":"Daws","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":186027,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pawlewicz, M. J.","contributorId":75111,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"M. J.","affiliations":[],"preferred":false,"id":186029,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Niem, A. R.","contributorId":54984,"corporation":false,"usgs":true,"family":"Niem","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":186026,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ryu, In-Chang","contributorId":69584,"corporation":false,"usgs":true,"family":"Ryu","given":"In-Chang","email":"","affiliations":[],"preferred":false,"id":186028,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":22276,"text":"ofr95315 - 1995 - Water-quality data for the Santa Clara-Calleguas hydrologic unit, Ventura County, California, October 1989 through December 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:08:02","indexId":"ofr95315","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-315","title":"Water-quality data for the Santa Clara-Calleguas hydrologic unit, Ventura County, California, October 1989 through December 1993","docAbstract":"More than 700 water samples were collected from 232 wells and 34 surface-water sites in the Santa Clara-Calleguas Hydrologic Unit, Ventura County, California, from October 1989 through December 1993 as part of the U.S. Geological Survey's Southern California Regional Aquifer-System Analysis study. Most samples were analyzed for major ions, nutrients, selected trace elements, oxygen-18, and deuterium. Selected samples were analyzed for one or more of the following isotopes: carbon-13/12, carbon-14, strontium-87/86, sulfur-34/32, and tritium. Other samples were analyzed for one or more of the following dissolved gases: hydrogen, methane, oxygen, and freon-11. Location of sampling sites is shown on maps and the results are presented in tables.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95315","issn":"0094-9140","usgsCitation":"Izbicki, J., Martin, P.M., Densmore, J., and Clark, D.A., 1995, Water-quality data for the Santa Clara-Calleguas hydrologic unit, Ventura County, California, October 1989 through December 1993: U.S. Geological Survey Open-File Report 95-315, iv, 124 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95315.","productDescription":"iv, 124 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":155776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0315/report-thumb.jpg"},{"id":51698,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0315/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64858c","contributors":{"authors":[{"text":"Izbicki, J. A. 0000-0003-0816-4408","orcid":"https://orcid.org/0000-0003-0816-4408","contributorId":28244,"corporation":false,"usgs":true,"family":"Izbicki","given":"J. A.","affiliations":[],"preferred":false,"id":187904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, P. M.","contributorId":39003,"corporation":false,"usgs":true,"family":"Martin","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":187905,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Densmore, J.N. 0000-0002-5345-6613","orcid":"https://orcid.org/0000-0002-5345-6613","contributorId":100882,"corporation":false,"usgs":true,"family":"Densmore","given":"J.N.","affiliations":[],"preferred":false,"id":187907,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, D. A.","contributorId":57488,"corporation":false,"usgs":false,"family":"Clark","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":187906,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":21879,"text":"ofr95813 - 1995 - Hydrologic effects associated with the January 17, 1994 Northridge, California, earthquake","interactions":[],"lastModifiedDate":"2019-09-06T15:49:42","indexId":"ofr95813","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-813","title":"Hydrologic effects associated with the January 17, 1994 Northridge, California, earthquake","docAbstract":"<p>This report compiles hydrologic observations in southern California associated with the 1994 Mw = 6.7 Northridge, California earthquake. In southern California, the largest ground water level change was a drop of 52 cm at Crystalaire. Most of the steplike water-level changes recorded following the Northridge earthquake agreed in direction with the sign of the calculated coseismic volume strain field. A spring discharge increase at Southern Pacific Springs was reported to have preceded the earthquake by several days. Outside of southern California, water-level changes were also observed, but are not consistent in sign or size with the static strain field of the earthquake sequence.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95813","issn":"0566-8174","usgsCitation":"Quilty, E., Farrar, C.D., Galloway, D., Hamlin, S.N., Laczniak, R.J., Roeloffs, E., Sorey, M., and Woodcock, D., 1995, Hydrologic effects associated with the January 17, 1994 Northridge, California, earthquake: U.S. Geological Survey Open-File Report 95-813, ii, 47 p., https://doi.org/10.3133/ofr95813.","productDescription":"ii, 47 p.","numberOfPages":"49","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":51367,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0813/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0813/report-thumb.jpg"}],"country":"United States","state":"California, Nevada, Oregon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125.41992187499999,\n              31.615965936476076\n            ],\n            [\n              -113.99414062499999,\n              31.615965936476076\n            ],\n            [\n              -113.99414062499999,\n              43.100982876188546\n            ],\n            [\n              -125.41992187499999,\n              43.100982876188546\n            ],\n            [\n              -125.41992187499999,\n              31.615965936476076\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607120","contributors":{"authors":[{"text":"Quilty, E.G.","contributorId":87160,"corporation":false,"usgs":true,"family":"Quilty","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":186096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrar, C. 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