{"pageNumber":"3727","pageRowStart":"93150","pageSize":"25","recordCount":185258,"records":[{"id":27407,"text":"wri964004 - 1996 - Hydrogeology in the vicinity of test holes and wells on St. Croix, St. Thomas, and St. John, U.S. Virgin Islands","interactions":[],"lastModifiedDate":"2022-01-12T21:19:52.423704","indexId":"wri964004","displayToPublicDate":"1997-04-01T00:00:00","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":"96-4004","title":"Hydrogeology in the vicinity of test holes and wells on St. Croix, St. Thomas, and St. John, U.S. Virgin Islands","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964004","usgsCitation":"Graves, R.P., 1996, Hydrogeology in the vicinity of test holes and wells on St. Croix, St. Thomas, and St. John, U.S. Virgin Islands: U.S. Geological Survey Water-Resources Investigations Report 96-4004, v, 48 p., https://doi.org/10.3133/wri964004.","productDescription":"v, 48 p.","costCenters":[],"links":[{"id":394281,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48374.htm"},{"id":56266,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4004/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4004/report-thumb.jpg"}],"country":"United States","otherGeospatial":"St. Croix, St. John, St. Thomas, , U.S. Virgin Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -65.05279541015625,\n              17.6099929086062\n            ],\n            [\n              -64.57489013671875,\n              17.6099929086062\n            ],\n            [\n              -64.57489013671875,\n              18.401442504848266\n            ],\n            [\n              -65.05279541015625,\n              18.401442504848266\n            ],\n            [\n              -65.05279541015625,\n              17.6099929086062\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db625124","contributors":{"authors":[{"text":"Graves, R. P.","contributorId":99179,"corporation":false,"usgs":true,"family":"Graves","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":198061,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44871,"text":"wri964166 - 1996 - Geohydrology of the North Park area, Jackson County, Colorado","interactions":[],"lastModifiedDate":"2022-02-01T19:39:55.887869","indexId":"wri964166","displayToPublicDate":"1997-04-01T00:00:00","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":"96-4166","title":"Geohydrology of the North Park area, Jackson County, Colorado","docAbstract":"<p>Increasing population in rural and suburban areas of Colorado is causing greater reliance on ground water as a source of domestic supply. In the primarily rural area of Jackson County, for example, the number of registered water wells increased from about 100 in 1972 to about 500 in 1995. Most of the new wells were drilled after 1988 and supply water to ranches and summer homes. In Jackson County, ground water is pumped from a series of shallow alluvial aquifers along principal stream valleys and from deeper, more extensive, bedrock aquifers. In much of the area, the alluvial aquifers are thin and can be dewatered by moderate water- level declines. Knowledge of the nature and extent of the alluvial and bedrock aquifers, the sources of recharge and discharge, and the effects of ground- water withdrawal on water levels in the aquifers is vital if management of the area's water resources is to ensure continued availability of a dependable water supply.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964166","collaboration":"Prepared in cooperation with the Colorado Department of Natural Resources, Division of Water Resources, Office of the State Engineer","usgsCitation":"Robson, S.G., and Graham, G., 1996, Geohydrology of the North Park area, Jackson County, Colorado: U.S. Geological Survey Water-Resources Investigations Report 96-4166, 1 Plate: 51.90 x 36.49 inches, https://doi.org/10.3133/wri964166.","productDescription":"1 Plate: 51.90 x 36.49 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":395233,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48511.htm"},{"id":364384,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4166/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":134675,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4166/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Jackson County","otherGeospatial":"North Park area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.1911,\n              40.3389\n            ],\n            [\n              -105.8972,\n              40.33389\n            ],\n            [\n              -105.8972,\n              40.9744\n            ],\n            [\n              -106.1911,\n              40.9744\n            ],\n            [\n              -106.1911,\n              40.3389\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8903","contributors":{"authors":[{"text":"Robson, Stanley G.","contributorId":73187,"corporation":false,"usgs":true,"family":"Robson","given":"Stanley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":230585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graham, Glenn","contributorId":95146,"corporation":false,"usgs":true,"family":"Graham","given":"Glenn","email":"","affiliations":[],"preferred":false,"id":230586,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21588,"text":"ofr96282A - 1996 - Analytical results for rock and stream-sediment samples, Coconino National Forest, Coconino, Gila, and Yavapai counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:07:49","indexId":"ofr96282A","displayToPublicDate":"1997-04-01T00:00:00","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":"96-282","chapter":"A","title":"Analytical results for rock and stream-sediment samples, Coconino National Forest, Coconino, Gila, and Yavapai counties, Arizona","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr96282A","usgsCitation":"Chaffee, M., King, H.D., Briggs, P., Fey, D., Knight, R.J., Motooka, J.M., and Roushey, B.H., 1996, Analytical results for rock and stream-sediment samples, Coconino National Forest, Coconino, Gila, and Yavapai counties, Arizona: U.S. Geological Survey Open-File Report 96-282, 160 leaves :maps ;28 cm., https://doi.org/10.3133/ofr96282A.","productDescription":"160 leaves :maps ;28 cm.","costCenters":[],"links":[{"id":154177,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0282a/report-thumb.jpg"},{"id":51168,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0282a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca78","contributors":{"authors":[{"text":"Chaffee, M.A.","contributorId":108049,"corporation":false,"usgs":true,"family":"Chaffee","given":"M.A.","affiliations":[],"preferred":false,"id":184784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":184781,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briggs, Paul H.","contributorId":107691,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul H.","affiliations":[],"preferred":false,"id":184783,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fey, D.L.","contributorId":44537,"corporation":false,"usgs":true,"family":"Fey","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":184779,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Knight, R. J.","contributorId":96255,"corporation":false,"usgs":true,"family":"Knight","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":184782,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Motooka, J. M.","contributorId":8834,"corporation":false,"usgs":true,"family":"Motooka","given":"J.","middleInitial":"M.","affiliations":[],"preferred":false,"id":184778,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Roushey, B. H.","contributorId":84387,"corporation":false,"usgs":true,"family":"Roushey","given":"B.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":184780,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":24553,"text":"ofr96201 - 1996 - Water-quality assessment of the Albemarle-Pamlico Drainage Basin, North Carolina and Virginia; organochlorine compounds in Asiatic clam (Corbicula fluminea) soft tissues and whole redbrest sunfish (Lepomis auritus) 1992-93","interactions":[],"lastModifiedDate":"2017-01-04T13:05:43","indexId":"ofr96201","displayToPublicDate":"1997-04-01T00:00:00","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":"96-201","title":"Water-quality assessment of the Albemarle-Pamlico Drainage Basin, North Carolina and Virginia; organochlorine compounds in Asiatic clam (Corbicula fluminea) soft tissues and whole redbrest sunfish (Lepomis auritus) 1992-93","docAbstract":"The analysis of potential contaminants in biological tissues is an important part of many water-quality assessment programs, including the National Water-Quality Assessment (NAWQA) Program. Tissue analyses often are used to provide information about (1) direct threats to ecosystem integrity, and (2) the occurrence and distribution of potential contaminants in the environment.\r\n\r\nDuring 1992-93, Asiatic clam (Corbicula fluminea) soft tissues and whole redbreast sunfish (Lepomis auritus) samples were collected and analyzed to obtain information about the occurrence and distribution of organochlorine compounds in the Albemarle-Pamlico drainage Basin of North Carolina and Virginia. The investigation was conducted as part of the NAWQA Program.\r\n\r\nRelatively few organochlorine compounds were detected and of the compounds detected, all were detected in relatively low concentrations. The organochlorine compounds detected were p,p'-DDD, p,p'-DDE, p,p'-DDT, dieldrin, trans-nonachlor, PCB's, and toxaphene. Multiple compounds were detected at 16 of 19 sites sampled. Compared to Asiatic clams, redbreast sunfish appear to be better bioindicators of organochlorine contamination in aquatic systems. Except for one detection of toxaphene, pesticide concentrations are well below the National Academy of Sciences and National Academy of Engineering (NAS/NAE) guidelines for the protection of fish-eating wildlife.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr96201","issn":"0094-9140","usgsCitation":"Smith, K., and Ruhl, P.M., 1996, Water-quality assessment of the Albemarle-Pamlico Drainage Basin, North Carolina and Virginia; organochlorine compounds in Asiatic clam (Corbicula fluminea) soft tissues and whole redbrest sunfish (Lepomis auritus) 1992-93: U.S. Geological Survey Open-File Report 96-201, 6 p. :ill., maps ;65 x 28 cm. folded to 22 x 28 cm., https://doi.org/10.3133/ofr96201.","productDescription":"6 p. :ill., maps ;65 x 28 cm. folded to 22 x 28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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M.","contributorId":30251,"corporation":false,"usgs":true,"family":"Ruhl","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":192143,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29964,"text":"wri964052 - 1996 - Hydrogeology of the interstream area between Ty Ty Creek and Ty Ty Creek tributary near Plains, Georgia","interactions":[],"lastModifiedDate":"2017-01-27T13:10:06","indexId":"wri964052","displayToPublicDate":"1997-04-01T00:00:00","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":"96-4052","title":"Hydrogeology of the interstream area between Ty Ty Creek and Ty Ty Creek tributary near Plains, Georgia","docAbstract":"This report is part of an interdisciplinary effort to identify and describe processes that control movement and fate of selected fertilizers and pesticides in the surface and subsurface environments in the Fall Line Hills district of the Georgia Coastal Plain physiographic province. This report describes the hydrogeology of the interstream area between Ty Ty Creek and it's tributary near Plains, Sumter County, Georgia.  Geologic units of interest to this study are, in ascending order, (1) the Tuscahoma Formation, a bluish gray, silty clay; (2) the Tallahatta Formation, a fine-to-coarse, poorly sorted quartz sand that is divided into an upper and lower unit; and (3) the undifferentiated overburden, which consists of fine to medium poorly sorted sand, silt and clay. Continuous-core samples indicate that the unsaturated zone includes the undifferentiated overburden and the upper unit of the Tallahatta Formation, and attains a maximum thickness of about 52 feet (ft) in the southern part of the study area. The Claiborne aquifer in the study area consists of the lower unit of the Tallahatta Formation and ranges in thickness from 3 ft near Ty Ty Creek tributary to about 20 ft in the upland divide area. It is confined below by the clayey sediments of the Tuscahoma Formation.  The Claiborne aquifer in the study area generally is confined above by an extensive clay layer that is the base if the upper unit of the Tallahatta Formation. Fluctuations in the amount of vertical recharge to the aquifer result in areal and temporal changes in aquifer conditions from confined to unconfined in parts of the study area. Hydraulic conductivity of the aquifer ranges from 3.5 to 7 feet per day. The transmissivity of the aquifer is approximately 50 feet squared per day. Water-level data indicate the potentiometric surface slopes to the south, southeast, and southwest with a gradient of about 87 to 167 feet per mile. The shape of the potentiometric surface and the direction of groundwater flow remains relatively unchanged during high and low water-level periods.  Water levels in the Claiborne aquifer fluctuated by a maximum of 6 ft during the period from January to December 1991. Recharge to the Claiborne aquifer consists of a local and regional flow component. Lateral ground-water flow (regional flow) into the study area is dependent on regional hydraulic controls (pumpage, stream discharge, and rainfall). The rate of lateral movement of ground water is dependent on the hydraulic conductivity of the saturated zone, the hydraulic gradient, and other hydraulic factors, and is considered to be relatively constant. Local recharge enters the ground-water system as rainfall that percolates down to the water table. Annual water-level fluctuations in the Claiborne aquifer indicate that the majority of regional and local recharge occurs in the interstream area with recharge decreasing downslope to the streams. Ground water discharges to Ty Ty Creek and it's tributary throughout the year during low and high water-level periods.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri964052","usgsCitation":"Stewart, L.M., and Hicks, D.W., 1996, Hydrogeology of the interstream area between Ty Ty Creek and Ty Ty Creek tributary near Plains, Georgia: U.S. Geological Survey Water-Resources Investigations Report 96-4052, v, 26 p. :ill., map ;28 cm., https://doi.org/10.3133/wri964052.","productDescription":"v, 26 p. :ill., map ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":125163,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_96_4052.jpg"},{"id":2431,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri96-4052/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","city":"Plain","otherGeospatial":"Ty Ty Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85,31 ], [ -85,33 ], [ -83,33 ], [ -83,31 ], [ -85,31 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614b94","contributors":{"authors":[{"text":"Stewart, Lisa M.","contributorId":82741,"corporation":false,"usgs":true,"family":"Stewart","given":"Lisa","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":202442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hicks, David W.","contributorId":33742,"corporation":false,"usgs":true,"family":"Hicks","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":202441,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29815,"text":"wri964064 - 1996 - Hydrogeologic setting and preliminary estimates of hydrologic components for Bull Run Lake and the Bull Run Lake drainage basin, Multnomah and Clackamas counties, Oregon","interactions":[],"lastModifiedDate":"2017-02-07T08:38:17","indexId":"wri964064","displayToPublicDate":"1997-04-01T00:00:00","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":"96-4064","title":"Hydrogeologic setting and preliminary estimates of hydrologic components for Bull Run Lake and the Bull Run Lake drainage basin, Multnomah and Clackamas counties, Oregon","docAbstract":"<p>The hydrogeologic setting was described and preliminary estimates of hydrologic components prepared for the Bull Run Lake and for the Bull Run Lake drainage basin, in the Cascade Range of northwestern Oregon. The 0.73-square-mile lake and the 3.44-square-mile drainage basin lie within the Bull Run Watershed, the principal water supply for the Portland, Oregon, metropolitan area. During periods of high demand or low inflows to the watershed, the City of Portland, Bureau of Water Works, releases water from Bull Run Lake to augment the supply.</p>\n<p>Bull Run Lake is impounded by a natural dam formed by a landslide. Outflow of ground water from the lake through the landslide emerges as springflow at the toe of the landslide and forms the headwaters of the Bull Run River. The approximately 4,300-Mgal (million gallons) discharge of the Bull Run River measured below the springs during the 1993 water year is composed of (1) outflow of ground water from Bull Run Lake through the landslide (approximately 60 percent), (2) ground water originating from the contributing drainage area between the lake and the springs (approximately 34 percent), (3) streamflow from Bull Run Lake (approximately 5 percent), and (4) surface runoff (streamflow and overland flow) from the contributing drainage area between the lake and the springs (approximately 1 percent). Estimated ranges for inflows to the Bull Run Lake drainage basin during the 1993 water year were about 3,400 to 9,200 Mgal from precipitation from rain and snow, and about 0 to 3,300 Mgal from fog drip.</p>\n<p>Estimated ranges for outflows from the lake basin, listed from largest to smallest, were about 1,800 to 3,400 Mgal for ground-water outflow through the landslide; about 600 to 1,800 Mgal for evapotranspiration from the land surface; about 170 to 410 Mgal for lake evaporation; and about 0 to 400 Mgal for streamflow from the lake. Ground- water outflow through the consolidated rocks could not be evaluated owing to the lack of data. The lake storage increased by a range of from about 1,700 to 1,900 Mgal. Changes in ground-water storage and soil-moisture storage could not be evaluated as a result of insufficient data.</p>\n<p>Estimated inflows to Bull Run Lake from precipitation on the lake surface during the 1993 water year ranged from about 600 to 1,600 Mgal. Inflows from ground water and surface runoff could not be evaluated owing to the lack of data. Estimated ranges for outflows from the lake were about 1,800 to 3,400 Mgal from ground-wateroutflow through the landslide, about 170 to 410 Mgal from lake evaporation, and about 0 to 400 Mgal from streamflow. Outflow of ground water through the consolidated rocks could not be evaluated owing to the lack of data. Lake storage increased by a range of from about 1,700 to 1,900 Mgal.</p>\n<p>Suggestions for further study include (1) evaluation of the surface-runoff component of inflow to the lake; (2) use of a cross-sectional ground-water flow model to estimate ground-water inflow, outflow, and storage; (3) additional data collection to reduce the uncertainties of the hydrologic components that have large relative uncertainties; and (4) determination of long-term trends for a wide range of climatic and hydrologic conditions.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/wri964064","collaboration":"Prepared in cooperation with City of Portland Bureau of Water Works","usgsCitation":"Snyder, D.T., and Brownell, D.L., 1996, Hydrogeologic setting and preliminary estimates of hydrologic components for Bull Run Lake and the Bull Run Lake drainage basin, Multnomah and Clackamas counties, Oregon: U.S. Geological Survey Water-Resources Investigations Report 96-4064, v, 47 p., https://doi.org/10.3133/wri964064.","productDescription":"v, 47 p.","numberOfPages":"56","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":123957,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4064/report-thumb.jpg"},{"id":58616,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4064/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Oregon","county":"Clackamas County, Multnomah County","otherGeospatial":"Bull Run Lake","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627933","contributors":{"authors":[{"text":"Snyder, Daniel T. dtsnyder@usgs.gov","contributorId":820,"corporation":false,"usgs":true,"family":"Snyder","given":"Daniel","email":"dtsnyder@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":true,"id":202177,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brownell, Dorie L.","contributorId":50539,"corporation":false,"usgs":true,"family":"Brownell","given":"Dorie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202178,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23194,"text":"ofr96226 - 1996 - Determination of roughness coefficients for streams in west-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:07:57","indexId":"ofr96226","displayToPublicDate":"1997-04-01T00:00:00","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":"96-226","title":"Determination of roughness coefficients for streams in west-central Florida","docAbstract":"Physical and hydraulic characteristics are presented for 10 west-central Florida stream reaches. These may be used as reference reaches for estimating Manning's roughness coefficient, n, in similar rivers and channels. Discharge in these reaches ranged from 1.8 to 3,010 cubic feet per second and water-surface slope ranged from 0.00002 to 0.00476 foot per foot. Sites were selected at or near U.S. Geological Survey streamflow gaging stations at which the stage-discharge relations were relatively stable. Crest-stage gages were installed at appropriate locations in each study reach in order to obtain water-surface elevations. Water-surface profiles were collected over a range of discharges at each of the 10 sites and the roughness coefficient was computed for each discharge. For the 104 recorded streamflow events used in this report, the computed roughness coefficients ranged from 0.021 to 0.218 and the mean was 0.072 . The median n value was 0.060; 70 percent of the time the n value was greater than 0.047 and 80 percent of the time the computed n was greater than 0.043. Bed material is so uniform at sites throughout west-central Florida that there is negligible variation in roughness as a result of variation in bed material. Streambank vegetation appears to be the major contributor to variations in roughness values for streams in west-central Florida. Channel roughness can be estimated quantitatively by evaluating the interaction of all roughness factors. Photographs of sites where n values have been computed can be used for comparison to estimate values at similar sites. Using a base n value of 0.040 and increasing n for factors of vegetation, channel obstructions, and other factors provides the best determination of n values for streams in west-central Florida.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96226","issn":"0094-9140","usgsCitation":"Gillen, D., 1996, Determination of roughness coefficients for streams in west-central Florida: U.S. Geological Survey Open-File Report 96-226, viii, 93 p. :ill. (some col.), map ;28 cm., https://doi.org/10.3133/ofr96226.","productDescription":"viii, 93 p. :ill. (some col.), map ;28 cm.","costCenters":[],"links":[{"id":155275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0226/report-thumb.jpg"},{"id":52514,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0226/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de6e","contributors":{"authors":[{"text":"Gillen, D.F.","contributorId":86805,"corporation":false,"usgs":true,"family":"Gillen","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":189615,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21869,"text":"ofr96128 - 1996 - Hydrogeologic, soil, and water-quality data for j-field, Aberdeen Proving Ground, Maryland, 1989-94","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr96128","displayToPublicDate":"1997-04-01T00:00:00","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":"96-128","title":"Hydrogeologic, soil, and water-quality data for j-field, Aberdeen Proving Ground, Maryland, 1989-94","docAbstract":"Disposal of chemical-warfare agents, munitions, and industrial chemicals in J-Field, Aberdeen Proving Ground, Maryland, has resulted in ground-water, surface-water, and soil contamination. This report presents data collected by the U.S. Geological Survey from Novembr 1989 through September 1994 as part of a remedial investigation of J-Field in response to the Comprehensive Environmental Response, Compensation, and Liability Act of 1980 (CERCLA). Hydrogeologic data, soil-gas and soil-quality data, and water-qualtiy data are included.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96128","issn":"0566-8174","usgsCitation":"Phelan, D.J., 1996, Hydrogeologic, soil, and water-quality data for j-field, Aberdeen Proving Ground, Maryland, 1989-94: U.S. Geological Survey Open-File Report 96-128, vi, 192 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96128.","productDescription":"vi, 192 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153036,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0128/report-thumb.jpg"},{"id":51360,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0128/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6278cf","contributors":{"authors":[{"text":"Phelan, D. J.","contributorId":17635,"corporation":false,"usgs":true,"family":"Phelan","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":186049,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22692,"text":"ofr95563 - 1996 - Volcanic episodes near Yucca Mountain as determined by paleomagnetic studies at Lathrop Wells, Crater Flat, and Sleeping Butte, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:51","indexId":"ofr95563","displayToPublicDate":"1997-04-01T00:00:00","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":"95-563","title":"Volcanic episodes near Yucca Mountain as determined by paleomagnetic studies at Lathrop Wells, Crater Flat, and Sleeping Butte, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95563","issn":"0094-9140","usgsCitation":"Champion, D., 1996, Volcanic episodes near Yucca Mountain as determined by paleomagnetic studies at Lathrop Wells, Crater Flat, and Sleeping Butte, Nevada: U.S. Geological Survey Open-File Report 95-563, 10 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95563.","productDescription":"10 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0563/report-thumb.jpg"},{"id":52153,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0563/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd92a","contributors":{"authors":[{"text":"Champion, D.E.","contributorId":70402,"corporation":false,"usgs":true,"family":"Champion","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":188700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23088,"text":"ofr95384 - 1996 - Reconnaissance of hydrologic monitoring sites and preliminary monitoring plan for the Vale, Oregon, geothermal area","interactions":[],"lastModifiedDate":"2023-09-14T21:00:58.819722","indexId":"ofr95384","displayToPublicDate":"1997-04-01T00:00:00","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":"95-384","title":"Reconnaissance of hydrologic monitoring sites and preliminary monitoring plan for the Vale, Oregon, geothermal area","docAbstract":"<p>The Bonneville Power Administration is working with private industry to develop a geothermal demonstration project in the Known Geothermal Resources Area (KGRA) near Vale, Oregon. Hydrologic monitoring in the area is planned in order to evaluate any impacts from the proposed development. The hydrology in and around the Vale KGRA is not well known. Additionally, little is known about the targeted geothermal reservoir and the nature of its connection to the shallow ground-water system. Given this uncertainty, a variety of features were selected to ensure adequate monitoring coverage. Wells and springs in and around the geothermal area were evaluated, and 19 were selected as potential monitoring sites. In selecting wells and springs for monitoring, particular emphasis was placed on those with a known or probable connection with the geothermal system because they would most likely be the first to show any effects from development. The selected features include thermal wells in the hot-spring area near the town of Vale and a hot spring south of the KGRA. Several warm wells (70 to 90 degrees Fahrenheit) near the KGRA were also selected because it is likely that the water produced from these wells includes a component of geothermal water. In order to identify any effects of development, it is necessary to have an understanding of natural and man-caused variations and trends prior to development. A quarterly measurement schedule is proposed to help characterize these variations and trends. It is anticipated that the proposed monitoring plan will be modified as exploration and development proceed and more is learned about the geothermal system.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr95384","collaboration":"Prepared in cooperation with the Bonneville Power Administration","usgsCitation":"Gannett, M.W., and Caldwell, R.R., 1996, Reconnaissance of hydrologic monitoring sites and preliminary monitoring plan for the Vale, Oregon, geothermal area: U.S. Geological Survey Open-File Report 95-384, iv, 11 p., https://doi.org/10.3133/ofr95384.","productDescription":"iv, 11 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":52458,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0384/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":157057,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0384/report-thumb.jpg"},{"id":420807,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18469.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Oregon","otherGeospatial":"Vale Known Geothermal Resource Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.48229980468749,\n              43.61221676817573\n            ],\n            [\n              -117.48229980468749,\n              44.03133330993374\n            ],\n            [\n              -117.03186035156251,\n              44.03133330993374\n            ],\n            [\n              -117.03186035156251,\n              43.61221676817573\n            ],\n            [\n              -117.48229980468749,\n              43.61221676817573\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a63e4b07f02db637ad1","contributors":{"authors":[{"text":"Gannett, Marshall W. 0000-0003-2498-2427 mgannett@usgs.gov","orcid":"https://orcid.org/0000-0003-2498-2427","contributorId":2942,"corporation":false,"usgs":true,"family":"Gannett","given":"Marshall","email":"mgannett@usgs.gov","middleInitial":"W.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"preferred":true,"id":189411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caldwell, Rodney R. 0000-0002-2588-715X caldwell@usgs.gov","orcid":"https://orcid.org/0000-0002-2588-715X","contributorId":2577,"corporation":false,"usgs":true,"family":"Caldwell","given":"Rodney","email":"caldwell@usgs.gov","middleInitial":"R.","affiliations":[{"id":685,"text":"Wyoming-Montana Water Science Center","active":false,"usgs":true}],"preferred":true,"id":189412,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26564,"text":"wri944090 - 1996 - Hydrogeology of, and simulation of ground-water flow in, a mantled carbonate-rock system, Cumberland Valley, Pennsylvania","interactions":[],"lastModifiedDate":"2022-02-03T20:34:37.822011","indexId":"wri944090","displayToPublicDate":"1997-04-01T00:00:00","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":"94-4090","title":"Hydrogeology of, and simulation of ground-water flow in, a mantled carbonate-rock system, Cumberland Valley, Pennsylvania","docAbstract":"The U.S. Geological Survey conducted a study in a highly productive and complex regolith-mantled carbonate valley in the northeastern part of the Cumberland Valley, Pa., as part of its Appalachian Valleys and Piedmont Regional Aquifer-system Analysis program. The study was designed to quantify the hydrogeologic characteristics and understand the ground-water flow system of a highly productive and complex thickly mantled carbonate valley. The Cumberland Valley is characterized by complexly folded and faulted carbonate bedrock in the valley bottom, by shale and graywacke to the north, and by red-sedimentary and diabase rocks in the east-southeast. Near the southern valley hillslope, the carbonate rock is overlain by wedge-shaped deposit of regolith, up to 450 feet thick, that is composed of residual material, alluvium, and colluvium. Locally, saturated regolith is greater than 200 feet thick. Seepage-run data indicate that stream reaches, near valley walls, are losing water from the stream, through the regolith, to the ground-water system. Results of hydrograph-separation analyses indicate that base flow in stream basins dominated by regolith-mantled carbonate rock, carbonate rock, and carbonate rock and shale are 81.6, 93.0, and 67.7 percent of total streamflow, respectively. The relative high percentage for the regolith-mantled carbonate-rock basin indicates that the regolith stores precipitation and slowly, steadily releases this water to the carbonate-rock aquifer and to streams as base flow. Anomalies in water-table gradients and configuration are a result of topography and differences in the character and distribution of overburden material, permeability, rock type, and geologic structure. Most ground-water flow is local, and ground water discharges to nearby springs and streams. Regional flow is northeastward to the Susquehanna River. Average-annual water budgets were calculated for the period of record from two continuous streamflow-gaging stations. Average-annual precipitation range from 39.0 to 40.5 inches, and averages about 40 inches for the model area. Average-annual recharge, which was assumed equal to the average-annual base flow, ranged from 12 inches for the Conodoguinet Creek, and 15 inches for the Yellow Breeches Creek. The thickly-mantled carbonate system was modeled as a three- dimensional water-table aquifer. Recharge to, ground-water flow through, and discharge from the Cumberland Valley were simulated. The model was calibrated for steady-state conditions using average recharge and discharge data. Aquifer horizontal hydraulic conductivity was calculated from specific-capacity data for each geologic unit in the area. Particle-tracking analyses indicate that interbasin and intrabasin flows of groundwater occur within the Yellow Breeches Creek Basin and between the Yellow Breeches and Conodoguinet Creek Basins.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944090","usgsCitation":"Chichester, D., 1996, Hydrogeology of, and simulation of ground-water flow in, a mantled carbonate-rock system, Cumberland Valley, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 94-4090, v, 39 p., https://doi.org/10.3133/wri944090.","productDescription":"v, 39 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":395404,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47983.htm"},{"id":55429,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4090/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4090/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Cumberland Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.6167,\n              39.95\n            ],\n            [\n              -76.8528,\n              39.95\n            ],\n            [\n              -76.8528,\n              40.333\n            ],\n            [\n              -77.6167,\n              40.333\n            ],\n            [\n              -77.6167,\n              39.95\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6148e9","contributors":{"authors":[{"text":"Chichester, D. C.","contributorId":61856,"corporation":false,"usgs":true,"family":"Chichester","given":"D. C.","affiliations":[],"preferred":false,"id":196626,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28839,"text":"wri954065 - 1996 - Geochemistry of selected aquifers in Tertiary rocks of the Upper Colorado River basin in Wyoming, Colorado, and Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri954065","displayToPublicDate":"1997-04-01T00:00:00","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":"95-4065","title":"Geochemistry of selected aquifers in Tertiary rocks of the Upper Colorado River basin in Wyoming, Colorado, and Utah","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri954065","usgsCitation":"Naftz, D.L., 1996, Geochemistry of selected aquifers in Tertiary rocks of the Upper Colorado River basin in Wyoming, Colorado, and Utah: U.S. Geological Survey Water-Resources Investigations Report 95-4065, v, 45 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri954065.","productDescription":"v, 45 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":121652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4065/report-thumb.jpg"},{"id":57714,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b1e4b07f02db530755","contributors":{"authors":[{"text":"Naftz, D. L.","contributorId":40624,"corporation":false,"usgs":true,"family":"Naftz","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200488,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6749,"text":"fs14396 - 1996 - Radon in ground water in Idaho, 1989-95","interactions":[],"lastModifiedDate":"2012-02-02T00:06:01","indexId":"fs14396","displayToPublicDate":"1997-04-01T00:00:00","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":"143-96","title":"Radon in ground water in Idaho, 1989-95","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs14396","usgsCitation":"Parliman, D., 1996, Radon in ground water in Idaho, 1989-95: U.S. Geological Survey Fact Sheet 143-96, 1 sheet : ill., map ; 28 cm. ill., map ;, https://doi.org/10.3133/fs14396.","productDescription":"1 sheet : ill., map ; 28 cm. ill., map ;","costCenters":[],"links":[{"id":125294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0143/report-thumb.jpg"},{"id":34119,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649b6b","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":153271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30588,"text":"wri954243 - 1996 - Water quality of large discharges from mines in the anthracite region of eastern Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-06T14:23:27","indexId":"wri954243","displayToPublicDate":"1997-04-01T00:00:00","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":"95-4243","title":"Water quality of large discharges from mines in the anthracite region of eastern Pennsylvania","docAbstract":"In 1991, 99 of the 102 coal mines in the anthracite coal fields of Pennsylvania that discharged 1.0 cubic foot per second or more when water-quality samples were collected in 1975 were revisited. Water was not discharging from 15 of these 99 mines in 1991. Discharge, water temperature, specific conductance, pH, dissolved oxygen, sulfate, iron, manganese, alkalinity, and acidity were measured in water samples collected at 84 mines to assess changes in water quality from 1975 to 1991. The pH increased in water samples of 64 of the 81 mines. However, acidity was essentially unchanged. Concentrations of iron decreased in water discharge samples from 57 of 82 mines, manganese concentrations decreased in samples from 23 of 26 mines, and sulfate concentrations decreased in samples from 62 of 77 mines. The median change in sulfate was a decrease of 139 milligrams per liter. Alkalinity increased in water discharge samples from 43 mines, remained the same at 22 mines, and decreased at 14 mines. In 1975, the samples were collected during high base flow in the spring; in 1991, samples were collected during lower-than-normal base flow in the fall. This may have affected the comparison.\r\n      Many mine discharges have elevated concentrations of aluminum, calcium, cobalt, iron, lithium, magnesium, manganese, nickel, strontium, zinc, and sulfate.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954243","usgsCitation":"Wood, C.R., 1996, Water quality of large discharges from mines in the anthracite region of eastern Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 95-4243, v, 68 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954243.","productDescription":"v, 68 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":59348,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4243/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4243/report-thumb.jpg"}],"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              -76.5802001953125,\n              40.30257076364479\n            ],\n            [\n              -75.10528564453125,\n              40.30257076364479\n            ],\n            [\n              -75.10528564453125,\n              41.64623592868676\n            ],\n            [\n              -76.5802001953125,\n              41.64623592868676\n            ],\n            [\n              -76.5802001953125,\n              40.30257076364479\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9972","contributors":{"authors":[{"text":"Wood, C. R.","contributorId":100386,"corporation":false,"usgs":true,"family":"Wood","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":203497,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29788,"text":"wri964306 - 1996 - Geologic framework and hydrogeologic characteristics of the Edwards aquifer outcrop (Barton Springs segment), northeastern Hays and southwestern Travis Counties, Texas","interactions":[],"lastModifiedDate":"2016-08-22T09:09:36","indexId":"wri964306","displayToPublicDate":"1997-04-01T00:00:00","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":"96-4306","title":"Geologic framework and hydrogeologic characteristics of the Edwards aquifer outcrop (Barton Springs segment), northeastern Hays and southwestern Travis Counties, Texas","docAbstract":"<p>The hydrogeologic subdivisions within the Barton Springs segment of the Edwards aquifer outcrop in northeastern Hays and southwestern Travis Counties generally are porous and permeable. The most porous and permeable appear to be hydrogeologic subdivision VI, the Kirschberg evaporite member of the Kainer Formation; and hydrogeologic subdivision III, the leached and collapsed members, undivided, of the Person Formation. Hydrogeologic subdivision II, the cyclic and marine members, undivided, of the Person Formation, also is quite porous and permeable in Hays County. The porosity of the rocks in the Edwards aquifer outcrop is related to depositional or diagenetic elements along specific stratigraphic horizons (fabric selective) and to dissolution and structural elements that can occur in any lithostratigraphic horizon (not fabric selective). Permeability depends on the physical properties of the rock such as pore size, shape, distribution, fissuring, dissolution, and interconnection of pores and vugs.</p>\n<p>The Edwards aquifer rocks that crop out in the Barton Springs segment of the Edwards aquifer generally have the same lithologic characteristics as the Edwards aquifer rocks that crop out in Comal and southwestern Hays Counties. However, in the northeastern part of the segment in Travis County, the rock unit that is apparently equivalent to the basal nodular member of the Kainer Formation is called the Walnut Formation. Because the units appear to be stratigraphically and lithologically equivalent, the basal nodular member is used instead of the Walnut Formation for this report. Essentially all of hydrogeologic subdivision II, which is about 70 feet thick in Hays County, is missing in Travis County.</p>\n<p>In the Barton Springs segment of the Edwards aquifer, the aquifer probably is most vulnerable to surface contamination in the rapidly urbanizing areas on the Edwards aquifer outcrop. Contamination can result from spills or leakage of hazardous materials; or runoff on the intensely faulted and fractured, karstic limestone outcrops characteristic of the recharge zone.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri964306","collaboration":"Prepared in cooperation with the Barton Springs/Edwards Aquifer Conservation District and the Texas Water Development Board","usgsCitation":"Small, T.A., Hanson, J., and Hauwert, N.M., 1996, Geologic framework and hydrogeologic characteristics of the Edwards aquifer outcrop (Barton Springs segment), northeastern Hays and southwestern Travis Counties, Texas: U.S. Geological Survey Water-Resources Investigations Report 96-4306, Document: iii, 15 p.; Plate: 25 x 30 inches, https://doi.org/10.3133/wri964306.","productDescription":"Document: iii, 15 p.; Plate: 25 x 30 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":123723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_96_4306.jpg"},{"id":8716,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri96-4306/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","county":"Hays County, Travis County","otherGeospatial":"Edwards Aquifer Outcrop","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a28bf","contributors":{"authors":[{"text":"Small, Ted A.","contributorId":77533,"corporation":false,"usgs":true,"family":"Small","given":"Ted","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanson, John A.","contributorId":73649,"corporation":false,"usgs":true,"family":"Hanson","given":"John A.","affiliations":[],"preferred":false,"id":202127,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hauwert, Nico M.","contributorId":40248,"corporation":false,"usgs":true,"family":"Hauwert","given":"Nico","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":202126,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29143,"text":"wri964065 - 1996 - Water-quality assessment of the Hudson River basin in New York and adjacent states: Analysis of available nutrient, pesticide volatile organic compound, and suspended-sediment data, 1970-90","interactions":[],"lastModifiedDate":"2022-12-14T20:34:52.175408","indexId":"wri964065","displayToPublicDate":"1997-04-01T00:00:00","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":"96-4065","title":"Water-quality assessment of the Hudson River basin in New York and adjacent states: Analysis of available nutrient, pesticide volatile organic compound, and suspended-sediment data, 1970-90","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964065","usgsCitation":"Phillips, P.J., and Hanchar, D., 1996, Water-quality assessment of the Hudson River basin in New York and adjacent states: Analysis of available nutrient, pesticide volatile organic compound, and suspended-sediment data, 1970-90: U.S. Geological Survey Water-Resources Investigations Report 96-4065, ix, 76 p., https://doi.org/10.3133/wri964065.","productDescription":"ix, 76 p.","costCenters":[],"links":[{"id":410491,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48430.htm","linkFileType":{"id":5,"text":"html"}},{"id":58013,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4065/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4065/report-thumb.jpg"}],"country":"United States","state":"Connecticut, Massachusetts, New Jersey, New York, Pennsylvania, Vermont","otherGeospatial":"Hudson River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.65,\n              40.75\n            ],\n            [\n              -73,\n              40.75\n            ],\n            [\n              -73,\n              44.1\n            ],\n            [\n              -75.65,\n              44.1\n            ],\n            [\n              -75.65,\n              40.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6e97","contributors":{"authors":[{"text":"Phillips, P. J.","contributorId":31728,"corporation":false,"usgs":true,"family":"Phillips","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":201012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanchar, D. W.","contributorId":87986,"corporation":false,"usgs":true,"family":"Hanchar","given":"D. W.","affiliations":[],"preferred":false,"id":201013,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6715,"text":"fs07796 - 1996 - Using geochemical and statistical tools to identify irrigated areas that might contain high selenium concentrations in surface water","interactions":[],"lastModifiedDate":"2019-12-05T13:12:37","indexId":"fs07796","displayToPublicDate":"1997-04-01T00:00:00","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":"077-96","title":"Using geochemical and statistical tools to identify irrigated areas that might contain high selenium concentrations in surface water","docAbstract":"<p>Ir<span>rigated agriculture has a long history in the Western United States, beginning with Native American Indians. After passage of the Reclamation Act of 1902, the United States Government began building and subsidizing irrigation projects to foster settlement and development of the arid and semi-arid areas of the Western United States (National Research Council, 1989). Precipitation in the mountainous areas of the West (fig. 1) is stored in reservoirs and used for irrigation of farmland. With the development of irrigated agriculture, unforeseen environmental problems have occurred.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs07796","usgsCitation":"Naftz, D.L., 1996, Using geochemical and statistical tools to identify irrigated areas that might contain high selenium concentrations in surface water: U.S. Geological Survey Fact Sheet 077-96, 4 p., https://doi.org/10.3133/fs07796.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":121614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_077_96.bmp"},{"id":334642,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/FS-077-96/images/FS-077-96.pdf","size":"231 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":758,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/FS/FS-077-96","linkFileType":{"id":5,"text":"html"}}],"publicComments":"National Irrigation Water Quality Program","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603d2b","contributors":{"authors":[{"text":"Naftz, David L. 0000-0003-1130-6892 dlnaftz@usgs.gov","orcid":"https://orcid.org/0000-0003-1130-6892","contributorId":1041,"corporation":false,"usgs":true,"family":"Naftz","given":"David","email":"dlnaftz@usgs.gov","middleInitial":"L.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5270,"text":"fs08496 - 1996 - Occurrence of pesticides in ground water in the White River Basin, Indiana, 1994–95","interactions":[],"lastModifiedDate":"2019-05-02T10:30:59","indexId":"fs08496","displayToPublicDate":"1997-04-01T00:00:00","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":"1996–0084","title":"Occurrence of pesticides in ground water in the White River Basin, Indiana, 1994–95","docAbstract":"<p>Pesticides (herbicides and insecticides) are used extensively in the White River Basin. Application of herbicides to corn and soybeans accounts for most of the use. The U.S. Geological Survey collected samples from four networks of monitoring wells in the White River Basin during 1994-95. The most frequently detected compounds in ground water were desethyl atrazine (a breakdown product of atrazine) and the commonly used herbicides, atrazine and metolachlor. Insecticides commonly used in urban and agricultural areas were not found. The highest concentration of any pesticide detected was alachlor at 0.19 micrograms per liter. Most detections of atrazine and desethyl atrazine were in agricultural areas overlying fluvial deposits, which are vulnerable to pesticide contamination, but the concentrations were small (less than 0.1 microgram per liter).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs08496","usgsCitation":"Fenelon, J.M., and Moore, R.C., 1996, Occurrence of pesticides in ground water in the White River Basin, Indiana, 1994–95: U.S. Geological Survey Fact Sheet 1996–0084, Document: 4 p., https://doi.org/10.3133/fs08496.","productDescription":"Document: 4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":31976,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0084/fs19960084.pdf","text":"Report","size":"617 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 1996-0084"},{"id":118375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0084/coverthb.jpg"}],"country":"United States","state":"Indiana","otherGeospatial":"White River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.8309326171875,\n              40.24808787647333\n            ],\n            [\n              -85.2264404296875,\n              40.250184183819854\n            ],\n            [\n              -85.27313232421875,\n              40.29000168607602\n            ],\n            [\n              -85.3143310546875,\n              40.32141999593439\n            ],\n            [\n              -85.37200927734375,\n              40.34235741658332\n            ],\n            [\n              -85.462646484375,\n           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Center","active":true,"usgs":true}],"preferred":true,"id":150749,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, Rhett C.","contributorId":82687,"corporation":false,"usgs":true,"family":"Moore","given":"Rhett","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":150750,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31969,"text":"ofr9518 - 1996 - Reconnaissance geologic map of the White Rock 7.5 minute quadrangle, Oregon","interactions":[],"lastModifiedDate":"2023-01-06T20:21:49.006285","indexId":"ofr9518","displayToPublicDate":"1997-04-01T00:00:00","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":"95-18","title":"Reconnaissance geologic map of the White Rock 7.5 minute quadrangle, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9518","usgsCitation":"Jayko, A.S., 1996, Reconnaissance geologic map of the White Rock 7.5 minute quadrangle, Oregon: U.S. Geological Survey Open-File Report 95-18, Report: 13 p.; 1 Plate: 48.24 x 32.00 inches, https://doi.org/10.3133/ofr9518.","productDescription":"Report: 13 p.; 1 Plate: 48.24 x 32.00 inches","costCenters":[],"links":[{"id":60126,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0018/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":108931,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18376.htm","linkFileType":{"id":5,"text":"html"},"description":"18376"},{"id":60125,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0018/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164321,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0018/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Oregon","otherGeospatial":"White Rock 7.5 minute quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.125,\n              43\n            ],\n            [\n              -123.125,\n              43.125\n            ],\n            [\n              -123,\n              43.125\n            ],\n            [\n              -123,\n              43\n            ],\n            [\n              -123.125,\n              43\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db6411c3","contributors":{"authors":[{"text":"Jayko, A. S. 0000-0002-7378-0330","orcid":"https://orcid.org/0000-0002-7378-0330","contributorId":18011,"corporation":false,"usgs":true,"family":"Jayko","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":207380,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31974,"text":"ofr95377 - 1996 - Assessment of severity and distribution of corrosive ground water in Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-22T10:48:39","indexId":"ofr95377","displayToPublicDate":"1997-04-01T00:00:00","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":"95-377","title":"Assessment of severity and distribution of corrosive ground water in Pennsylvania","docAbstract":"Relations between corrosive ground water, water chemistry, and geology in Pennsylvania were evaluated by use of a modified version of the Langelier Saturation Index (LSIsn) and a geologic contact dataset in a Geographic Information System. Water-chemistry information for water samples collected from 4,839 combined private and public-supply wells from 1900 to 1993 was used to calculate the LSIsn. Thirty-eight lithologic subgroups within four major rock types-carbonate, siliciclastic, crystalline, and unconsolidated-in Pennsylvania were grouped together if the mean of ranked LSIsn values were not significantly different. A water is considered corrosive if the LSIsn value is negative, preventing the precipitation of calcium carbonate, therefore, allowing corrosive reactions with the interior of piping systems. Statistical tests of the LSIsn values show the least corrosive waters are in the carbonate lithologic subgroup, and the most corrosive waters are in the quartzite lithologic subgroup. Approximately 58 percent of the 4,839 LSIsn values were considered moderately to extremely corrosive. A map showing the location of 4,839 wells and associated corrosivity range within 11 lithologic subgroups will aid in identifying potential areas of corrosive ground water in Pennsylvania.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95377","usgsCitation":"Langland, M., and Dugas, D., 1996, Assessment of severity and distribution of corrosive ground water in Pennsylvania: U.S. Geological Survey Open-File Report 95-377, 2 over-size sheets. , https://doi.org/10.3133/ofr95377.","productDescription":"2 over-size sheets. ","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":163116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":19590,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0377/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":19591,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0377/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671e6e","contributors":{"authors":[{"text":"Langland, M. J.","contributorId":36173,"corporation":false,"usgs":true,"family":"Langland","given":"M. J.","affiliations":[],"preferred":false,"id":207388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dugas, D.L.","contributorId":25820,"corporation":false,"usgs":true,"family":"Dugas","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":207387,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6642,"text":"fs17896 - 1996 - Pesticides in urban and agricultural streams, 1993-95","interactions":[],"lastModifiedDate":"2016-08-17T17:59:37","indexId":"fs17896","displayToPublicDate":"1997-04-01T00:00:00","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":"178-96","title":"Pesticides in urban and agricultural streams, 1993-95","docAbstract":"<p>Nonpoint sources of pesticides are a national issue and are a major interest in the U.S. Geological Survey National Water-Quality Assessment (NAWQA) Program because of their potential toxicity to humans and aquatic life. Using the water-quality data collected by the Trinity River Basin NAWQA study-unit team, an analysis of pesticides in urban and agricultural streams was made by aggregating and grouping data from several networks. The samples were collected during March 1993 through September 1995. About 70 samples were collected from urban streams and 70 from agricultural streams. The urban dataset consists of sampling sites in the Dallas-Fort Worth metropolitan area where more than 3.5 million people lived in 1990. Land use in the sampled urban watersheds is primarily residential, but there are commercial areas, such as shopping centers and office complexes along major highways and streets. The agricultural dataset consists of sampling sites in the watershed of Richland-Chambers Reservoir, an area in the west-central part of the Trinity River Basin where fertile soils are extensively cultivated. The land use is mostly cropland and pasture with some rangeland. In the cultivated areas, the major crops are corn, cotton, and sorghum. In the rangeland areas, cattle are the dominant livestock. In the pasture areas, hay is grown along with grass for cattle feed. None of the crops are irrigated.</p>\n<p>The material in this fact sheet is condensed from a report by Land and Brown (1996) where the study is presented in greater detail.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs17896","usgsCitation":"Land, L.F., 1996, Pesticides in urban and agricultural streams, 1993-95: U.S. Geological Survey Fact Sheet 178-96, 2 p., https://doi.org/10.3133/fs17896.","productDescription":"2 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":125313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0178/report-thumb.jpg"},{"id":34069,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0178/report.pdf","text":"Report","size":"1.0 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","otherGeospatial":"Richland-Chambers Reservoir, Trinity River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.3,\n              31.5\n            ],\n            [\n              -97.3,\n              33.5\n            ],\n            [\n              -96,\n              33.5\n            ],\n            [\n              -96,\n              31.5\n            ],\n            [\n              -97.3,\n              31.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881e1","contributors":{"authors":[{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":153089,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6645,"text":"fs17696 - 1996 - Quality of ground water at selected sites in the upper Mahoning Creek Basin, Pennsylvania","interactions":[],"lastModifiedDate":"2018-02-09T12:46:57","indexId":"fs17696","displayToPublicDate":"1997-04-01T00:00:00","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":"176-96","title":"Quality of ground water at selected sites in the upper Mahoning Creek Basin, Pennsylvania","docAbstract":"<p>The ground-water quality of the upper Mahoning Creek Basin is largely unknown. Human activities in the basin have altered much of the landscape. The presence of coal mining, oil and gas exploration, agriculture, on-lot septic systems, and commercial development within the basin can introduce contaminants altering the natural chemistry of the ground water. Data collected to document current ground-water quality also can serve as a baseline for comparison of any future water-quality changes by continuing human activities. This report presents the results of a synoptic ground-water-quality sampling in the upper Mahoning Creek Basin. Present ground-water quality in the basin is characterized in relation to published standards, local land-use activities, and other areas with similar natural characteristics. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs17696","usgsCitation":"Langland, M.J., 1996, Quality of ground water at selected sites in the upper Mahoning Creek Basin, Pennsylvania: U.S. Geological Survey Fact Sheet 176-96, 4 p., https://doi.org/10.3133/fs17696.","productDescription":"4 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":34071,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0176/fs19960176.pdf","text":"Report","size":"123 KB","linkFileType":{"id":1,"text":"pdf"},"description":"FS 1996-0176"},{"id":117128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0176/coverthb.jpg"}],"contact":"<p><a href=\"mailto:dc_pa@usgs.gov\" data-mce-href=\"mailto:dc_pa@usgs.gov\">Director</a>, <a href=\"https://pa.water.usgs.gov/\" data-mce-href=\"https://pa.water.usgs.gov/\">Pennsylvania Water Science Center</a><br> U.S. Geological Survey <br> 215 Limekiln Road <br> New Cumberland, PA 17070</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db65515a","contributors":{"authors":[{"text":"Langland, Michael J. 0000-0002-8350-8779 langland@usgs.gov","orcid":"https://orcid.org/0000-0002-8350-8779","contributorId":2347,"corporation":false,"usgs":true,"family":"Langland","given":"Michael","email":"langland@usgs.gov","middleInitial":"J.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":153092,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31970,"text":"ofr9520 - 1996 - Reconnaissance geologic map of the Lane Mountain 7.5 minute quadrangle, Oregon","interactions":[],"lastModifiedDate":"2023-01-06T20:16:36.954274","indexId":"ofr9520","displayToPublicDate":"1997-04-01T00:00:00","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":"95-20","title":"Reconnaissance geologic map of the Lane Mountain 7.5 minute quadrangle, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9520","usgsCitation":"Jayko, A.S., 1996, Reconnaissance geologic map of the Lane Mountain 7.5 minute quadrangle, Oregon: U.S. Geological Survey Open-File Report 95-20, Report: 14 p.; 1 Plate: 48.66 x 32.00 inches, https://doi.org/10.3133/ofr9520.","productDescription":"Report: 14 p.; 1 Plate: 48.66 x 32.00 inches","costCenters":[],"links":[{"id":60128,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0020/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60127,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0020/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164322,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0020/report-thumb.jpg"},{"id":108932,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18377.htm","linkFileType":{"id":5,"text":"html"},"description":"18377"}],"scale":"24000","country":"United States","state":"Oregon","otherGeospatial":"Lane Mountain 7.5 minute quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.125,\n              43.25\n            ],\n            [\n              -123.125,\n              43.125\n            ],\n            [\n              -123,\n              43.125\n            ],\n            [\n              -123,\n              43.25\n            ],\n            [\n              -123.125,\n              43.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a71e4b07f02db64205d","contributors":{"authors":[{"text":"Jayko, Angela S. 0000-0002-7378-0330 ajayko@usgs.gov","orcid":"https://orcid.org/0000-0002-7378-0330","contributorId":2531,"corporation":false,"usgs":true,"family":"Jayko","given":"Angela","email":"ajayko@usgs.gov","middleInitial":"S.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":207381,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26625,"text":"wri964111 - 1996 - Ground-water pumpage in the Willamette lowland regional aquifer system, Oregon and Washington, 1990","interactions":[],"lastModifiedDate":"2017-02-07T08:40:00","indexId":"wri964111","displayToPublicDate":"1997-04-01T00:00:00","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":"96-4111","title":"Ground-water pumpage in the Willamette lowland regional aquifer system, Oregon and Washington, 1990","docAbstract":"<p>Ground-water pumpage for 1990 was estimated for an area of about 5,700 square miles in northwestern Oregon and southwestern Washington as part of the Puget-Willamette Lowland Regional Aquifer System Analysis study. The estimated total ground-water pumpage in 1990 was about 340,000 acre-feet. Ground water in the study area is pumped mainly from Quaternary sediment; lesser amounts are withdrawn from Tertiary volcanic materials. Large parts of the area are used for agriculture, and about two and one-half times as much ground water was pumped for irrigation as for either public- supply or industrial needs. Estimates of ground- water pumpage for irrigation in the central part of the Willamette Valley were generated by using image-processing techniques and Landsat Thematic Mapper data. Field data and published reports were used to estimate pumpage for irrigation in other parts of the study area. Information on public- supply and industrial pumpage was collected from Federal, State, and private organizations and individuals.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/wri964111","usgsCitation":"Collins, C., and Broad, T.M., 1996, Ground-water pumpage in the Willamette lowland regional aquifer system, Oregon and Washington, 1990: U.S. Geological Survey Water-Resources Investigations Report 96-4111, iii, 27 p., https://doi.org/10.3133/wri964111.","productDescription":"iii, 27 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":125024,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4111/report-thumb.jpg"},{"id":55498,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4111/report.pdf","text":"Report","size":"549.91 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Willamette Regional Aquifer System","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.16748046874999,\n              43.78695837311561\n            ],\n            [\n              -124.16748046874999,\n              49.76707407366792\n            ],\n            [\n              -119.00390625,\n              49.76707407366792\n            ],\n            [\n              -119.00390625,\n              43.78695837311561\n            ],\n            [\n              -124.16748046874999,\n              43.78695837311561\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673ed","contributors":{"authors":[{"text":"Collins, Charles A.","contributorId":79510,"corporation":false,"usgs":true,"family":"Collins","given":"Charles A.","affiliations":[],"preferred":false,"id":196733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broad, Tyson M.","contributorId":76786,"corporation":false,"usgs":true,"family":"Broad","given":"Tyson","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":196732,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4982,"text":"fs18596 - 1996 - Monitoring ground water at Jefferson Patterson Park and Museum; the effects of agricultural practices on ground-water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"fs18596","displayToPublicDate":"1997-04-01T00:00:00","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":"185-96","title":"Monitoring ground water at Jefferson Patterson Park and Museum; the effects of agricultural practices on ground-water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs18596","usgsCitation":"Hayes, M.A., and Bachman, L.J., 1996, Monitoring ground water at Jefferson Patterson Park and Museum; the effects of agricultural practices on ground-water quality: U.S. Geological Survey Fact Sheet 185-96, 1 sheet : ill., maps ; 43 x 28 cm. folded to 22 x 28 cm. ill., maps ;, https://doi.org/10.3133/fs18596.","productDescription":"1 sheet : ill., maps ; 43 x 28 cm. folded to 22 x 28 cm. ill., maps ;","costCenters":[],"links":[{"id":125316,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0185/report-thumb.jpg"},{"id":31824,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0185/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db62744e","contributors":{"authors":[{"text":"Hayes, Martha A.","contributorId":31749,"corporation":false,"usgs":true,"family":"Hayes","given":"Martha","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":150236,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bachman, L. Joseph","contributorId":33304,"corporation":false,"usgs":true,"family":"Bachman","given":"L.","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":150237,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}