No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964148","usgsCitation":"Williams, L.M., 1996, Evaluation of quality assurance/quality control data collected by the U.S. Geological Survey for water-quality activities at the Idaho National Engineering Laboratory, Idaho, 1989 through 1993: U.S. Geological Survey Water-Resources Investigations Report 96-4148, ix, 116 p., https://doi.org/10.3133/wri964148.","productDescription":"ix, 116 p.","costCenters":[],"links":[{"id":394214,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48494.htm"},{"id":59297,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4148/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4148/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho National Engineering Laboratory","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.3042,\n 43.2167\n ],\n [\n -112.5,\n 43.2167\n ],\n [\n -112.5,\n 43.9333\n ],\n [\n -113.3042,\n 43.9333\n ],\n [\n -113.3042,\n 43.2167\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fabeb","contributors":{"authors":[{"text":"Williams, L. M.","contributorId":63045,"corporation":false,"usgs":true,"family":"Williams","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":203383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29777,"text":"wri964047 - 1996 - Geohydrology of the Stockton Formation and cross-contamination through open boreholes, Hatboro Borough and Warminster Township, Pennsylvania","interactions":[],"lastModifiedDate":"2018-12-20T10:40:33","indexId":"wri964047","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"96-4047","title":"Geohydrology of the Stockton Formation and cross-contamination through open boreholes, Hatboro Borough and Warminster Township, Pennsylvania","docAbstract":"The study area consists of a 9-square-mile area underlain by sedimentary rocks of the middle arkose member of the Stockton Formation of Upper Triassic age. In the Hatboro area, the Stockton Formation strikes approximately N. 65 degrees E. and dps approximately 9 degrees NW. The rocks are chiefly arkosic sandstone and siltstone. Rocks of the Stocton Formation form a complex, heterogeneous, multiaquifer system consisting of a series of gently dipping lithologic units with different hydraulic properties. Most ground water in the unweathered zone moves through a network of interconnecting secondary openigns-fractures, bedding plans, and joints. Ground water is unconfined in the shallower part of the aquifer and semiconfined or confined in the deeper part of the aquifer. Nearly all deep wells in the Stockton Formation are open to several water-bearing zones and are multiaquifer wells. Each water-bearing zone usually has a different hydraulic head. Where differences in hydraulic head exist between water-bearing zones, water in the well bore flows under nonpumping conditions in the direction of decreasing head.\r\n\r\n Determination of the potential for borehole flow was based on caliper, natural-gamma, single- point-resistance, fluid-resistivity, and (or) fluid-temperature logs that were run in 162 boreholes 31 to 655 feet deep. The direction and rate of borehole-fluid movement were determined in 83 boreholes by the bring-tracing method and in 10 boreholes by use of a heat-pulse flowmeter. Borehole flow was measurable in 65 of the 93 boreholes (70 percent). Fluid movement at rates up to 17 gallons per minute was measured. Downward flow was measured in 36 boreholes, and upward flow was measured in 23 boreholes, not including those boreholes in which two directions of flow were measured. Both upward and downward vertical flow was measured in six boreholes; these boreholes are 396 to 470 feet deep and were among the deepest boreholes logged. Fluid movement was upward in the upper part of the borehole and downward in the lower part of the borehole in two boreholes. Fluid movement wad downward in the upper part of the borehole and upward in the lower part of the borehole in three boreholes.\r\n\r\n Groung-water contamination by volatile organic compounds (VOC's) is widespread in the study area. Detectable concentrations of VOC's were present in water samples from 24 wells sampled in Hatboro Brough and in water samples for 10 of 14 wells (71 percent) samples in Warminster Township. Samples of borehole flow from nine boreholes in the industrial area of Hatboro were collected for laboratory analysis to estimate the quantity of VOC's in borehole flow. Downward flow was measured in all of these boreholes. Concentrations of TCE, TCA, and 1,1-DCE as great at 5,800, 1,400 and 260 micrograms per liter, respectively, show that some water moving downward in the aquifer through these open boreholes is highly contaminated and that open boreholes may contribute substantially to ground-water contamination. An estimated 14.7 gallons per year of VOC's were moving downward through the nine open boreholes sampled from the contaminated, upper part of the aquifer to the lower part, which is tapped by public supply wells.\r\n\r\n Borehole geophysical logs were used as a guide to design and construct monitor-well networks at three National Priorities List sites in the area. An open borehole was dirlled, and a suite of geophysical logs was run. Interpretation of geophysical logs enabled the identification of water-bearing zones that produce and receive water; these are zones that should not be connected. From the logs, discrete intervals to be monitored were selected. In the Stockton Formation, the same water-bearing zone may not be intersected in adjacent boreholes, especially if it is a vertical fracture with a diffident magnetic orientation than that of the adjacent boreholes. In most areas of the stockton Formation, depth of water-bearing zones in an are","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964047","usgsCitation":"Sloto, R.A., Macchiaroli, P., and Towle, M.T., 1996, Geohydrology of the Stockton Formation and cross-contamination through open boreholes, Hatboro Borough and Warminster Township, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 96-4047, Report: v, 49 p.; 2 Plates: 17.00 x 11.04 inches, https://doi.org/10.3133/wri964047.","productDescription":"Report: v, 49 p.; 2 Plates: 17.00 x 11.04 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":122226,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4047/report-thumb.jpg"},{"id":58579,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4047/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360607,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360608,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4047/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.16666667,\n 40.16666667\n ],\n [\n -75.05000000,\n 40.16666667\n ],\n [\n -75.05000000,\n 40.28333333\n ],\n [\n -75.16666667,\n 40.28333333\n ],\n [\n -75.16666667,\n 40.16666667\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a88ce","contributors":{"authors":[{"text":"Sloto, Ronald A. rasloto@usgs.gov","contributorId":424,"corporation":false,"usgs":true,"family":"Sloto","given":"Ronald","email":"rasloto@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":202105,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Macchiaroli, Paola","contributorId":96309,"corporation":false,"usgs":true,"family":"Macchiaroli","given":"Paola","email":"","affiliations":[],"preferred":false,"id":202107,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Towle, Michael T.","contributorId":211743,"corporation":false,"usgs":true,"family":"Towle","given":"Michael","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":202106,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":26900,"text":"wri954244 - 1996 - Ground-water quality in the Calumet Region of northwestern Indiana and northeastern Illinois, June 1993","interactions":[],"lastModifiedDate":"2016-05-16T09:41:55","indexId":"wri954244","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4244","title":"Ground-water quality in the Calumet Region of northwestern Indiana and northeastern Illinois, June 1993","docAbstract":"Water samples were collected from 128 wells in a large industrial and urban area in northwestern Indiana and northeastern Illinois during June 1993. Samples were collected from wells completed in one of four geohydrologic units: surficial sand aquifer (Calumet aquifer), clay confining unit, confined sand aquifers, and a carbonate-bedrock aquifer (Silurian-Devonian aquifer). Samples were analyzed by U.S. Environmental Protection Agency contract laboratories for selected water-quality properties, common ions, trace elements, volatile and semivolatile organic compounds, pesticides, and polychlorinated biphenyls.
\nWater from wells in the Silurian-Devonian aquifer is predominantly a sodium bicarbonate type. Water types in confined sand aquifers and the confining unit are varied. Water types from wells in the Calumet aquifer also are varied, although approximately 42 percent of the wells in this geohydrologic unit produced water in which calcium and bicarbonate were the dominant cation-anion pair. Samples from several shallow wells in the confining unit and the Calumet aquifer, and one well in a confined sand aquifer, were classified as sodium chloride-type water.
\nThe largest concentrations of trace elements and organic compounds were detected in samples from wells located in or near industrial areas or areas of waste disposal. A total of 14 volatile organic compounds and 23 semivolatile organic compounds on the U.S. Environmental Protection Agency's target compound list was detected in 20 and 56 samples. A total of 18 pesticide compounds was detected in 29 samples. Compounds containing polychlorinated biphenyls were detected in three samples.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri954244","collaboration":"U.S. Environmental Protection Agency","usgsCitation":"Duwelius, R.F., Kay, R.T., and Prinos, S.T., 1996, Ground-water quality in the Calumet Region of northwestern Indiana and northeastern Illinois, June 1993: U.S. Geological Survey Water-Resources Investigations Report 95-4244, vii, 179 p., [8] folded p. of plates :ill., maps ;28 cm., https://doi.org/10.3133/wri954244.","productDescription":"vii, 179 p., [8] folded p. of plates :ill., maps ;28 cm.","startPage":"1","endPage":"179","numberOfPages":"185","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":2004,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=WRIR&number=95-4244","linkFileType":{"id":5,"text":"html"}},{"id":123527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4244/report-thumb.jpg"},{"id":55781,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4244/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois, Indiana","otherGeospatial":"Calumet Region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.75,\n 41.75\n ],\n [\n -87.75,\n 41.55\n ],\n [\n -87,\n 41.55\n ],\n [\n -87,\n 41.75\n ],\n [\n -87.75,\n 41.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db658731","contributors":{"authors":[{"text":"Duwelius, Richard F.","contributorId":31378,"corporation":false,"usgs":true,"family":"Duwelius","given":"Richard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kay, Robert T. 0000-0002-6281-8997 rtkay@usgs.gov","orcid":"https://orcid.org/0000-0002-6281-8997","contributorId":1122,"corporation":false,"usgs":true,"family":"Kay","given":"Robert","email":"rtkay@usgs.gov","middleInitial":"T.","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":197214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prinos, Scott T. 0000-0002-5776-8956 stprinos@usgs.gov","orcid":"https://orcid.org/0000-0002-5776-8956","contributorId":4045,"corporation":false,"usgs":true,"family":"Prinos","given":"Scott","email":"stprinos@usgs.gov","middleInitial":"T.","affiliations":[{"id":269,"text":"FLWSC-Ft. Lauderdale","active":true,"usgs":true},{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"preferred":true,"id":197215,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31704,"text":"ofr96692 - 1996 - Aeromagnetic map of the Carrizo Plain area on parts of the Bakersfield, Los Angeles and San Luis Obispo 1° by 2° quadrangles, California","interactions":[],"lastModifiedDate":"2021-09-01T22:11:11.406346","indexId":"ofr96692","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-692","title":"Aeromagnetic map of the Carrizo Plain area on parts of the Bakersfield, Los Angeles and San Luis Obispo 1° by 2° quadrangles, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96692","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1996, Aeromagnetic map of the Carrizo Plain area on parts of the Bakersfield, Los Angeles and San Luis Obispo 1° by 2° quadrangles, California: U.S. Geological Survey Open-File Report 96-692, 1 Plate: 46.00 × 36.10 inches, https://doi.org/10.3133/ofr96692.","productDescription":"1 Plate: 46.00 × 36.10 inches","costCenters":[],"links":[{"id":388779,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18677.htm"},{"id":59933,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0692/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","country":"United States","state":"California","otherGeospatial":"Carrizo Plain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.3387451171875,\n 34.74161249883172\n ],\n [\n -119.06982421874999,\n 34.74161249883172\n ],\n [\n -119.06982421874999,\n 35.82672127366604\n ],\n [\n -120.3387451171875,\n 35.82672127366604\n ],\n [\n -120.3387451171875,\n 34.74161249883172\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db697081","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":529278,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31705,"text":"ofr96693 - 1996 - Aeromagnetic map of the northern Gabilan Range area on part of the Monterey 1° by 2° quadrangle, California","interactions":[],"lastModifiedDate":"2021-09-09T19:55:24.12413","indexId":"ofr96693","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-693","title":"Aeromagnetic map of the northern Gabilan Range area on part of the Monterey 1° by 2° quadrangle, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96693","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1996, Aeromagnetic map of the northern Gabilan Range area on part of the Monterey 1° by 2° quadrangle, California: U.S. Geological Survey Open-File Report 96-693, 1 Plate: 46.43 × 35.65 inches, https://doi.org/10.3133/ofr96693.","productDescription":"1 Plate: 46.43 × 35.65 inches","costCenters":[],"links":[{"id":59934,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0693/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161368,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":389022,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18678.htm"}],"scale":"100000","country":"United States","state":"California","otherGeospatial":"Monterey 1° by 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.66,\n 36.8870\n ],\n [\n -120.9710,\n 36.8870\n ],\n [\n -120.9710,\n 36.3560\n ],\n [\n -121.66,\n 36.3560\n ],\n [\n -121.66,\n 36.8870\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696608","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":529279,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32016,"text":"ofr96537 - 1996 - Geologic map of part of May Mountain Quadrangle, Lemhi County, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"ofr96537","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-537","title":"Geologic map of part of May Mountain Quadrangle, Lemhi County, Idaho","language":"ENGLISH","doi":"10.3133/ofr96537","usgsCitation":"Tysdal, R., 1996, Geologic map of part of May Mountain Quadrangle, Lemhi County, Idaho: U.S. Geological Survey Open-File Report 96-537, 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet). , https://doi.org/10.3133/ofr96537.","productDescription":"1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet). ","costCenters":[],"links":[{"id":108977,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18643.htm","linkFileType":{"id":5,"text":"html"},"description":"18643"},{"id":161489,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":60174,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0537/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a28dd","contributors":{"authors":[{"text":"Tysdal, R.D.","contributorId":53006,"corporation":false,"usgs":true,"family":"Tysdal","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":207461,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6584,"text":"fs18396 - 1996 - Hazard maps help save lives and property","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"fs18396","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"183-96","title":"Hazard maps help save lives and property","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs18396","usgsCitation":"Brown, W.M., Perkins, D.M., Leyendecker, E.V., Frankel, A.D., Hendley, J.W., and Stauffer, P.H., 1996, Hazard maps help save lives and property: U.S. Geological Survey Fact Sheet 183-96, 2 p., https://doi.org/10.3133/fs18396.","productDescription":"2 p.","costCenters":[],"links":[{"id":121767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_183_96.bmp"},{"id":875,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/1996/fs183-96/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d77b","contributors":{"authors":[{"text":"Brown, William M. III","contributorId":72365,"corporation":false,"usgs":true,"family":"Brown","given":"William","suffix":"III","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":152968,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perkins, David M. perkins@usgs.gov","contributorId":2114,"corporation":false,"usgs":true,"family":"Perkins","given":"David","email":"perkins@usgs.gov","middleInitial":"M.","affiliations":[{"id":301,"text":"Geologic Hazards Team","active":false,"usgs":true}],"preferred":true,"id":152966,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leyendecker, Edgar V.","contributorId":75142,"corporation":false,"usgs":true,"family":"Leyendecker","given":"Edgar","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":152969,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frankel, Arthur D. 0000-0001-9119-6106 afrankel@usgs.gov","orcid":"https://orcid.org/0000-0001-9119-6106","contributorId":1363,"corporation":false,"usgs":true,"family":"Frankel","given":"Arthur","email":"afrankel@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":152965,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hendley, James W. II jhendley@usgs.gov","contributorId":2547,"corporation":false,"usgs":true,"family":"Hendley","given":"James","suffix":"II","email":"jhendley@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":false,"id":152967,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stauffer, Peter H. pstauffe@usgs.gov","contributorId":1219,"corporation":false,"usgs":true,"family":"Stauffer","given":"Peter","email":"pstauffe@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":152964,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":31707,"text":"ofr96695 - 1996 - Aeromagnetic map of the Roseburg area on parts of the Roseburg, Coos Bay, Medford, and Cape Blanco 1° by 2° quadrangles, Oregon","interactions":[],"lastModifiedDate":"2021-11-30T21:29:21.532946","indexId":"ofr96695","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-695","title":"Aeromagnetic map of the Roseburg area on parts of the Roseburg, Coos Bay, Medford, and Cape Blanco 1° by 2° quadrangles, Oregon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96695","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1996, Aeromagnetic map of the Roseburg area on parts of the Roseburg, Coos Bay, Medford, and Cape Blanco 1° by 2° quadrangles, Oregon: U.S. Geological Survey Open-File Report 96-695, 2 Plates: 46.00 × 35.00 inches, https://doi.org/10.3133/ofr96695.","productDescription":"2 Plates: 46.00 × 35.00 inches","costCenters":[],"links":[{"id":161400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392272,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18680.htm"},{"id":19528,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0695/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19529,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0695/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","country":"United States","state":"Oregon","otherGeospatial":"Roseburg area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.6792,\n 42.969\n ],\n [\n -122.5267,\n 42.969\n ],\n [\n -122.5267,\n 43.711\n ],\n [\n -124.6792,\n 43.711\n ],\n [\n -124.6792,\n 42.969\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db69151d","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":529280,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31710,"text":"ofr96704 - 1996 - Geologic map of the Packwood Lake Quadrangle, southern Cascade Range, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"ofr96704","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-704","title":"Geologic map of the Packwood Lake Quadrangle, southern Cascade Range, Washington","language":"ENGLISH","doi":"10.3133/ofr96704","usgsCitation":"Swanson, D.A., 1996, Geologic map of the Packwood Lake Quadrangle, southern Cascade Range, Washington: U.S. Geological Survey Open-File Report 96-704, 25 p., 2 over-size sheets, scale 1:24,000 (1 inch = 2,000 feet). , https://doi.org/10.3133/ofr96704.","productDescription":"25 p., 2 over-size sheets, scale 1:24,000 (1 inch = 2,000 feet). ","costCenters":[],"links":[{"id":108979,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18682.htm","linkFileType":{"id":5,"text":"html"},"description":"18682"},{"id":161403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0704/report-thumb.jpg"},{"id":59937,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0704/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59938,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0704/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59939,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696b4b","contributors":{"authors":[{"text":"Swanson, D. A.","contributorId":34102,"corporation":false,"usgs":true,"family":"Swanson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":206786,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22716,"text":"ofr96575 - 1996 - Results of specific-capacity tests in Kings and Queens Counties, New York, 1919-82","interactions":[],"lastModifiedDate":"2012-02-02T00:08:08","indexId":"ofr96575","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-575","title":"Results of specific-capacity tests in Kings and Queens Counties, New York, 1919-82","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96575","issn":"0094-9140","usgsCitation":"Chu, A., 1996, Results of specific-capacity tests in Kings and Queens Counties, New York, 1919-82: U.S. Geological Survey Open-File Report 96-575, iv, 12 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr96575.","productDescription":"iv, 12 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":156489,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0575/report-thumb.jpg"},{"id":52169,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0575/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611a82","contributors":{"authors":[{"text":"Chu, Anthony 0000-0001-8623-2862 achu@usgs.gov","orcid":"https://orcid.org/0000-0001-8623-2862","contributorId":2517,"corporation":false,"usgs":true,"family":"Chu","given":"Anthony","email":"achu@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":188750,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29337,"text":"wri964038C - 1996 - Benthic invertebrates of benchmark streams in agricultural areas of eastern Wisconsin — Western Lake Michigan drainages","interactions":[],"lastModifiedDate":"2022-01-21T21:01:57.760672","indexId":"wri964038C","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"96-4038","chapter":"C","title":"Benthic invertebrates of benchmark streams in agricultural areas of eastern Wisconsin — Western Lake Michigan drainages","docAbstract":"This study describes the benthic invertebrate communities of 20 benchmark streams in agricultural areas of eastern Wisconsin. Streams with minimal adverse effects from human activity were selected from four agricultural areas with differing surficial deposits and bedrock types (relatively homogeneous units, or RHU's). Most aquatic invertebrate orders were well represented in the 20 benchmark stream samples; 217 species and 151 genera within 56 families were identified. Diptera was the best represented order (96 species), followed by Trichoptera (42 species) and Ephemeroptera (26 species). Diptera were the most abundant organisms in terms of numbers of individuals in the sample (28 percent of the total) followed by Trichoptera (25 percent) and Ephemeroptera (13 percent). Nine species of freshwater mussels were found, but only in 5 of the 20 benchmark streams.
\nCommunity measures were calculated for the following: total number of individuals; number of species; number of families; Margalef's diversity index; percent dominant family; percent Ephemeroptera-Plecoptera-Trichoptera (EPT); ratio of EPT to Chironomidae; percent shredders; ratio of scrapers to collectors-gatherers-filterers; Hilsenhoff's Biotic Index; Hilsenhoff's family level biotic index; and mean tolerance value. The S AS statistical software package was used for calculations of variance and correlations, normality checks, and principal components analysis of these measures and to find relations between benthic-invertebrate data and environmental-setting, habitat, and water-quality data.
\nCoefficients of variation within the RHU's were as great or greater than those for all 20 streams for most measures and RHU's. The specific taxa assemblages present at the sites did not show distinct differences between RHU's or similarities within the RHU's. The covariance and the Kruskal-Wallis tests showed that the benthic invertebrate measures were not related to RHU. These results all indicate that the combined effect of the RHU variables (bedrock geology, texture of surficial deposits, and land use/land cover) were not elemental in describing invertebrate communities in the study-area streams.
\nA principal components analysis (PCA) was done on the 20 benchmark streams which used the invertebrate population measures as variables. A three-dimensional ordination plot of these components revealed that 18 of the 20 streams could be divided into three groups relative to stream size, available habitat, and water quality. The three classifications of streams include large, warmer streams with slight pollution; deep, mixed-water streams with minimal pollution; and small, cold, pristine headwater streams. The two streams not defined by the three PCA groupings were not suitable to represent benchmark conditions. One site lacked suitable quality habitat or sufficient nutrients to support a healthy population of invertebrates, causing low measures of diversity. The other site appeared to be affected by sedimentation and low flows.
\nThe classification groupings did not show any significant relations to percentage agricultural land use. Percentage of agricultural land use varied greatly within each group and the means for each group were similar. All streams in this study had some level of protection from agricultural practices in their basins. Although the intensity of agriculture is known to be a factor causing deterioration of invertebrate populations in past studies, the finding in this study indicated that the level of protection the stream received and other factors such as environmental setting and habitat could be more important to benthic invertebrates than the percentage of agriculture in the basin.
\nInformation gathered from these benchmark streams can be used as a regional reference for comparison with other streams in agricultural areas, based on communities of aquatic biota, habitat, and water quality.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964038C","usgsCitation":"Rheaume, S.J., Lenz, B.N., and Scudder, B.C., 1996, Benthic invertebrates of benchmark streams in agricultural areas of eastern Wisconsin — Western Lake Michigan drainages: U.S. Geological Survey Water-Resources Investigations Report 96-4038, vi, 39 p., https://doi.org/10.3133/wri964038C.","productDescription":"vi, 39 p.","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":394722,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48405.htm"},{"id":58180,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4038c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4038c/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Lake Michigan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.483642578125,\n 43.1090040242731\n ],\n [\n -89.483642578125,\n 45.46783598133375\n ],\n [\n -86.737060546875,\n 45.46783598133375\n ],\n [\n -86.737060546875,\n 43.1090040242731\n ],\n [\n -89.483642578125,\n 43.1090040242731\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b4bb","contributors":{"authors":[{"text":"Rheaume, S. J.","contributorId":70804,"corporation":false,"usgs":true,"family":"Rheaume","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":201366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lenz, B. N.","contributorId":106164,"corporation":false,"usgs":true,"family":"Lenz","given":"B.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":201368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scudder, B. C.","contributorId":71588,"corporation":false,"usgs":true,"family":"Scudder","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201367,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":22651,"text":"ofr96576 - 1996 - Nitrate in ground water and surface water in a residential subdivision, West Windsor Township, Mercer County, New Jersey, 1993","interactions":[],"lastModifiedDate":"2012-02-02T00:07:57","indexId":"ofr96576","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-576","title":"Nitrate in ground water and surface water in a residential subdivision, West Windsor Township, Mercer County, New Jersey, 1993","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96576","issn":"0094-9140","usgsCitation":"Carleton, G., and Vowinkel, E., 1996, Nitrate in ground water and surface water in a residential subdivision, West Windsor Township, Mercer County, New Jersey, 1993: U.S. Geological Survey Open-File Report 96-576, v, 33 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96576.","productDescription":"v, 33 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":155241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0576/report-thumb.jpg"},{"id":52119,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0576/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697516","contributors":{"authors":[{"text":"Carleton, G.B.","contributorId":107729,"corporation":false,"usgs":true,"family":"Carleton","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":188642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vowinkel, E. F.","contributorId":90737,"corporation":false,"usgs":true,"family":"Vowinkel","given":"E. F.","affiliations":[],"preferred":false,"id":188641,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":22900,"text":"ofr96554 - 1996 - A modified index for assessment of potential scour at bridges over waterways","interactions":[],"lastModifiedDate":"2012-02-02T00:07:56","indexId":"ofr96554","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-554","title":"A modified index for assessment of potential scour at bridges over waterways","docAbstract":"The modified potential-scour index described in this report is based on a potential-scour index used by the U.S. Geological Survey Maryland District (Maryland index), and a prototype index developed by the U.S. Geological Survey Tennessee District (Tennessee index). The modifications were made to (1) improve the technical content of theMaryland index, and (2) provide a more extensive set of index variables for assessment of potential scour at bridges. The report demonstrates and describes problems that were encountered when using the Maryland index in a study of county- maintained bridges in Maryland from 1993 to 1995.The modifications made to specific index variables and ranking values in the Maryland index are presented and discussed. A comparison of potential-scour ratings from the modified potential- scour index, as applied to two bridges, is presented.This comparison indicates that the modified potential-scour index produces potential-scour ratings that most consistently reflect scour conditions observed at these bridges.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96554","issn":"0094-9140","usgsCitation":"Doheny, E.J., 1996, A modified index for assessment of potential scour at bridges over waterways: U.S. Geological Survey Open-File Report 96-554, iv, 16 p. ;28 cm., https://doi.org/10.3133/ofr96554.","productDescription":"iv, 16 p. ;28 cm.","costCenters":[],"links":[{"id":154231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0554/report-thumb.jpg"},{"id":52307,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0554/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adead","contributors":{"authors":[{"text":"Doheny, Edward J. 0000-0002-6043-3241 ejdoheny@usgs.gov","orcid":"https://orcid.org/0000-0002-6043-3241","contributorId":4495,"corporation":false,"usgs":true,"family":"Doheny","given":"Edward","email":"ejdoheny@usgs.gov","middleInitial":"J.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":false,"id":189099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22428,"text":"ofr96496 - 1996 - Radionuclides, stable isotopes, inorganic constituents, and organic compounds in water from selected wells and springs from the southern boundary of the Idaho National Engineering Laboratory to the Hagerman area, Idaho, 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:07","indexId":"ofr96496","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-496","title":"Radionuclides, stable isotopes, inorganic constituents, and organic compounds in water from selected wells and springs from the southern boundary of the Idaho National Engineering Laboratory to the Hagerman area, Idaho, 1995","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96496","issn":"0094-9140","usgsCitation":"Bartholomay, R.C., Williams, L.M., and Campbell, L., 1996, Radionuclides, stable isotopes, inorganic constituents, and organic compounds in water from selected wells and springs from the southern boundary of the Idaho National Engineering Laboratory to the Hagerman area, Idaho, 1995: U.S. Geological Survey Open-File Report 96-496, iv, 29 p. :maps ;28 cm., https://doi.org/10.3133/ofr96496.","productDescription":"iv, 29 p. :maps ;28 cm.","costCenters":[],"links":[{"id":156459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0496/report-thumb.jpg"},{"id":51967,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0496/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649b02","contributors":{"authors":[{"text":"Bartholomay, R. C.","contributorId":66271,"corporation":false,"usgs":true,"family":"Bartholomay","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":188236,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, L. M.","contributorId":63045,"corporation":false,"usgs":true,"family":"Williams","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":188235,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campbell, L.J.","contributorId":59820,"corporation":false,"usgs":true,"family":"Campbell","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":188234,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23809,"text":"ofr96648 - 1996 - Ground-water levels in Wyoming, January 1986 through September 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr96648","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-648","title":"Ground-water levels in Wyoming, January 1986 through September 1995","docAbstract":"Water levels were measured in a network of 81 observation wells in Wyoming as of September 1995. The wells are located mainly in areas where ground water is used in large quantities for irrigation or municipal purposes. Water-level data were collected at 74 of the 81 observation wells by Wyoming State Engineer personnel; data at theremaining 7 wells were collected by the U.S. Geological Survey. This report contains hydrographs for 81 observation wells showing water-level fluctuations from January 1986 through September 1995. Included in the report are maps showing location of the observation wells and tableslisting observation-well depths, use of water, principal geologic source, records available, and highest and lowest water levels for the period ofrecord.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr96648","issn":"0094-9140","usgsCitation":"Mason, J.P., and Green, S.L., 1996, Ground-water levels in Wyoming, January 1986 through September 1995: U.S. Geological Survey Open-File Report 96-648, iv, 119 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96648.","productDescription":"iv, 119 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0648/report-thumb.jpg"},{"id":53023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0648/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667928","contributors":{"authors":[{"text":"Mason, J. P.","contributorId":27491,"corporation":false,"usgs":true,"family":"Mason","given":"J.","middleInitial":"P.","affiliations":[],"preferred":false,"id":190769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, S. L.","contributorId":83525,"corporation":false,"usgs":true,"family":"Green","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":190770,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24704,"text":"ofr96660 - 1996 - Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through September 1996","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"ofr96660","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-660","title":"Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through September 1996","docAbstract":"This report describes the status of ground-water resources at U.S. Navy Support Facility, Diego Garcia. Data presented are from January 1994 through September 1996, with a focus on data from July through September 1996 (third quarter of 1996). A complete database of ground-water withdrawals and chloride-concentration records since 1985 is maintained by the U.S. Geological Survey. Total rainfall for the period July through September 1996 was 8.94 inches, which is 60 percent less than the mean rainfall of 22.23 inches for the period July through September. July and August are part of the annual dry season, while September is the start of the annual wet season. Ground-water withdrawal during July through September 1996 averaged 1,038,300 gallons per day. Withdrawal for the same 3 months in 1995 averaged 888,500 gallons per day. Ground-water withdrawals have steadily increased since about April 1995. At the end of September 1996, the chloride concentration of water from the elevated tanks at Cantonment and Air Operations were 68 and 150 milligrams per liter, respectively. The chloride concentration from all five production areas increased throughout the third quarter of 1996, and started the upward trend in about April 1995. Chloride concentration of ground water in monitoring wells at Cantonment and Air Operations also increased throughout the third quarter of 1996, with the largest increases from water in the deepest monitoring wells. Chloride concentrations have not been at this level since the dry season of 1994. A fuel-pipeline leak at Air Operations in May 1991 decreased total islandwide withdrawals by 15 percent. This lost pumping capacity is being offset by increased pumpage at Cantonment. Six wells do not contribute to the water supply because they are being used to hydraulically divert fuel migration away from water-supply wells by a program of ground-water withdrawal and injection.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96660","issn":"0094-9140","usgsCitation":"Torikai, J., 1996, Status of ground-water resources at U.S. Navy Support Facility, Diego Garcia; summary of hydrologic and climatic data, January 1994 through September 1996: U.S. Geological Survey Open-File Report 96-660, v, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96660.","productDescription":"v, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0660/report-thumb.jpg"},{"id":53737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0660/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486fe4b07f02db50ce10","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192407,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21714,"text":"ofr96614 - 1996 - Data from synoptic water-quality studies on the Colorado River in the Grand Canyon, Arizona, November 1990 and June 1991","interactions":[],"lastModifiedDate":"2018-02-15T12:53:33","indexId":"ofr96614","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"96-614","title":"Data from synoptic water-quality studies on the Colorado River in the Grand Canyon, Arizona, November 1990 and June 1991","docAbstract":"Two water-quality synoptic studies were made on the Colorado River in the Grand Canyon, Arizona. Field measurements and the collection of water samples for laboratory analysis were made at 10 mainstem and 6 tributary sites every 6 hours for a 48-hour period on November 5-6, 1990, and again on June 18-20, 1991. Field\r\nmeasurements included discharge, alkalinity, water temperature, light penetration, pH, specific conductance, and dissolved oxygen. Water samples were collected for the laboratory analysis of major and minor ions (calcium, magnesium, sodium, potassium, strontium, chloride, sulfate, silica as SiO2), trace elements (aluminum, arsenic, boron, barium, beryllium, cadmium, cobalt, chromium, copper, iron, lead, lithium, manganese, molybdenum, nickel, selenium, thallium, uranium, vanadium and zinc), and nutrients (phosphate, nitrate, ammonium, nitrite, total\r\ndissolved nitrogen, total dissolved phosphorus and dissolved organic carbon). Biological measurements included drift (benthic invertebrates and detrital material), and benthic invertebrates from the river bottom.","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/ofr96614","issn":"0566-8174","usgsCitation":"Taylor, H.E., Peart, D., Antweiler, R.C., Brinton, T., Campbell, W.L., Barbarino, J., Roth, D., Hart, R.J., and Averett, R., 1996, Data from synoptic water-quality studies on the Colorado River in the Grand Canyon, Arizona, November 1990 and June 1991: U.S. Geological Survey Open-File Report 96-614, iv, 176 p. :ill. ; 28 cm., https://doi.org/10.3133/ofr96614.","productDescription":"iv, 176 p. :ill. ; 28 cm.","temporalStart":"1990-11-01","temporalEnd":"1991-06-30","costCenters":[],"links":[{"id":8225,"rank":9999,"type":{"id":18,"text":"Project Site"},"url":"https://wwwbrr.cr.usgs.gov/projects/SW_inorganic/","linkFileType":{"id":5,"text":"html"}},{"id":154546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0614/report-thumb.jpg"},{"id":8224,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://wwwbrr.cr.usgs.gov/projects/SW_inorganic/download/Synoptic.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51241,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0614/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c87f","contributors":{"authors":[{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":185377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peart, D.B.","contributorId":45304,"corporation":false,"usgs":true,"family":"Peart","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":185379,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Antweiler, Ronald C. 0000-0001-5652-6034 antweil@usgs.gov","orcid":"https://orcid.org/0000-0001-5652-6034","contributorId":1481,"corporation":false,"usgs":true,"family":"Antweiler","given":"Ronald","email":"antweil@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":185381,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brinton, T.I.","contributorId":93922,"corporation":false,"usgs":true,"family":"Brinton","given":"T.I.","affiliations":[],"preferred":false,"id":185383,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Campbell, W. L.","contributorId":46939,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":185380,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barbarino, J.R.","contributorId":94336,"corporation":false,"usgs":true,"family":"Barbarino","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":185384,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Roth, D.A.","contributorId":100864,"corporation":false,"usgs":true,"family":"Roth","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":185385,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hart, R. J.","contributorId":62607,"corporation":false,"usgs":true,"family":"Hart","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":185382,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Averett, R. C.","contributorId":35709,"corporation":false,"usgs":true,"family":"Averett","given":"R. C.","affiliations":[],"preferred":false,"id":185378,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":30305,"text":"wri964061 - 1996 - Hydrogeology and simulation of ground-water flow, Picatinny Arsenal and vicinity, Morris County, New Jersey","interactions":[],"lastModifiedDate":"2019-12-07T09:48:02","indexId":"wri964061","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"96-4061","title":"Hydrogeology and simulation of ground-water flow, Picatinny Arsenal and vicinity, Morris County, New Jersey","docAbstract":"Ground-water flow in glacial sediments and bedrock at Picatinny Arsenal, N.J., was simulated by use of a three-dimensional finite-difference ground- water-flow model. The modeled area includes a 4.3-square-mile area that extends from Picatinny Lake to the Rockaway River. Most of the study area is bounded by the natural hydrologic boundaries of the ground-water system. eophysical logs, lithologic logs, particle-size data, and core data from selected wells and surface geophysical data were analyzed to define the hydrogeologic framework. Hydrogeologic sections and thickness maps define six permeable and three low-permeability layers that are represented in the model as aquifers and confining units, respectively. Hydrologic data incorporated in the model include a rate of recharge from precipitation of 22 inches per year, estimated from long-term precipitation records and estimates of evapotranspiration. Additional recharge from infiltration along valleys was estimated from measured discharge of springs along the adjacent valley walls and from estimates of runoff from upland drainage that flows to the valley floor. Horizontal and vertical hydraulic conductivities of permeable and low-permeability layers were estimated from examination of aquifer-test data, gamma-ray logs, borehole cuttings, and previously published data. Horizontal hydraulic conductivities in glacial sediments range from 10 to 380 feet per day. Vertical hydraulic conductivities of the low-permeability layers range from 0.01 to 0.7 feet per day. The model was calibrated by simulating steady-state conditions during 1989-93 and by closely matching simulated and measured ground-water levels, vertical ground-water-head differences, and streamflow gain and loss. Simulated steady-state potentiometric- surface maps produced for the six permeable layers indicate that ground water in the unconfined material within Picatinny Arsenal flows predominantly toward the center of the valley, where it discharges to Green Pond Brook. Beneath the upper confining unit, ground water flows southwestward, down the valley. Between First Street and Farley Avenue, the upper confining unit pinches out near the valley walls, resulting in a major input of water to, and causing a local potentiometric high in, the underlying aquifer layers. Ground-water-flow directions southwest of the southern arsenal boundary are predominantly to the Rockaway River.","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/wri964061","usgsCitation":"Voronin, L., and Rice, D., 1996, Hydrogeology and simulation of ground-water flow, Picatinny Arsenal and vicinity, Morris County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 96-4061, vi, 64 p., https://doi.org/10.3133/wri964061.","productDescription":"vi, 64 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology 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