{"pageNumber":"4773","pageRowStart":"119300","pageSize":"25","recordCount":184617,"records":[{"id":28490,"text":"wri864191 - 1987 - Flooding of December 29, 1984 through January 2, 1985, in northern New York State, with flood profiles of the Black and Salmon rivers","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri864191","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4191","title":"Flooding of December 29, 1984 through January 2, 1985, in northern New York State, with flood profiles of the Black and Salmon rivers","docAbstract":"Precipitation, snowmelt, and resultant flooding throughout northern New York from December 28 through January 2, 1985, were investigated through a detailed analysis of 56 precipitation stations, 101 stage and/or discharge gaging stations, and 9 miscellaneous measurement sites. Flood damage to property and roads and bridges exceeded $5 million. Lewis and Oswego Counties were declared Federal disaster areas, primarily a result of flooding of the Black River and Salmon River. Storm-precipitation and runoff maps show the storms ' greatest intensity to have been over the Tug Hill and southwest Adirondack areas. Total rainfall from December 28 through January 2 was 6.90 inches at Stillwater Reservoir but only 0.69 inches at Lake Placid. New peak discharges of record occurred at 17 gaging stations throughout northern New York, and the maximum discharge at 17 sites had recurrence intervals equal to or greater than 100 years. Computed inflows to 11 major lakes and reservoirs in northern New York indicate that significant volumes of water (as much as 5 inches of storm runoff at Stillwater Reservoir) were stored during the storm-runoff period. Maximum 1-day flood volumes at two gaging stations on the Black River had recurrence intervals greater than 100 years. To help evaluate the extent of flooding, 67 floodmarks were obtained along a 94-mile reach of the Black River from Dexter to Forestport, and several floodmarks were surveyed within major communities along the Salmon River. The floodmarks were obtained primarily near major bridges and dams along these rivers. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864191","usgsCitation":"Lumia, R., Burke, P.M., and Johnston, W.H., 1987, Flooding of December 29, 1984 through January 2, 1985, in northern New York State, with flood profiles of the Black and Salmon rivers: U.S. Geological Survey Water-Resources Investigations Report 86-4191, v, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864191.","productDescription":"v, 53 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4191/report-thumb.jpg"},{"id":57288,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4191/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e6a","contributors":{"authors":[{"text":"Lumia, Richard rlumia@usgs.gov","contributorId":4579,"corporation":false,"usgs":true,"family":"Lumia","given":"Richard","email":"rlumia@usgs.gov","affiliations":[],"preferred":true,"id":199898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burke, P. M.","contributorId":8478,"corporation":false,"usgs":true,"family":"Burke","given":"P.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":199899,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnston, W. H.","contributorId":19960,"corporation":false,"usgs":true,"family":"Johnston","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":199900,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28457,"text":"wri824117 - 1987 - Hydrology of the White Tail Butte area, northern Campbell County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri824117","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"82-4117","title":"Hydrology of the White Tail Butte area, northern Campbell County, Wyoming","docAbstract":"Quantity of runoff and peak discharge from one small basin in the White Tail Butte area, determined from a calibrated rainfall-runoff model, is less than the quantity computed using results of a regional study. The difference is caused by the extensive beds of exposed, permeable clinker in the area. Potentiometric surfaces in the White Tail Butte area indicate that, regionally, it is a discharge area. This is consistent with the conceptual model developed elsewhere in Campbell County , Wyo. The chemical quality of water from springs and alluvium, however, is characteristic of water found in recharge areas, so movement of water in the regional system is apparently small compared to local recharge. If surface coal mining occurs in the area, the principal adverse impact to the groundwater system would be the destruction of springs and seeps in the mined area. These could be restored with special reclamation procedures. There are adequate quantities of water of suitable quality for stock or domestic use below the coal so postreclamation supplies could be obtained. Impacts of surface mining on runoff could not be evaluated, but sensitivity of runoff to infiltration indicates a 10% change in runoff for a 1% change in infiltration. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824117","usgsCitation":"Lowry, M., and Rankl, J., 1987, Hydrology of the White Tail Butte area, northern Campbell County, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 82-4117, v, 47 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824117.","productDescription":"v, 47 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4117/report-thumb.jpg"},{"id":57259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4117/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e868","contributors":{"authors":[{"text":"Lowry, M.E.","contributorId":55807,"corporation":false,"usgs":true,"family":"Lowry","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":199830,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rankl, J.G.","contributorId":107733,"corporation":false,"usgs":true,"family":"Rankl","given":"J.G.","affiliations":[],"preferred":false,"id":199831,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27680,"text":"wri874145 - 1987 - Hydrogeology, chemical quality, and availability of ground water in the Upper Floridan aquifer, Albany area, Georgia","interactions":[],"lastModifiedDate":"2017-01-24T12:56:14","indexId":"wri874145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4145","title":"Hydrogeology, chemical quality, and availability of ground water in the Upper Floridan aquifer, Albany area, Georgia","docAbstract":"Large withdrawals of groundwater in the 1500 sq mi Albany area of southwestern Georgia have lowered water levels in deep aquifers as much as 140 ft. This study was conducted to evaluate the development potential of the shallow Upper Floridan aquifer as an alternate source of groundwater, especially for public supply. The Upper Floridan stores and transmits large quantities of water, mainly in a zone of high permeability in the lower part of the aquifer. The transmissivity of the aquifer ranges from < 10,000 sq ft/day northwest of Albany, to as much as 150 ,000 sq ft/day south and southeast of Albany. Twenty-eight years of agricultural and industrial pumping has not produced a long-term decline of the water level in the Upper Floridan; the aquifer system remains at equilibrium. The Upper Floridan yields hard, calcium bicarbonate-type water but concentrations do not exceed State drinking water standards. In most of the study area , contaminants applied to or spilled on the land surface eventually can be expected to percolate through the overburden and reach the aquifer. Thus, it is important that wells be sited away from areas that have been used for the storage and disposal of potential contaminants and, probably to a lesser extent, the application of agricultural chemicals. In the area of greatest development potential east of the Flint River, wells may penetrate major groundwater conduits. By limiting drawdown during well development and during production, the likelihood of causing sinkholes to form can be minimized. Closed depressions, or sinks, throughout the Dougherty Plain probably are unsuitable as well sites, because (1) they are subject to flooding, (2) they collect water from upgradient areas and could concentrate potential contaminants, (3) water probably percolates through their bottoms and could transport contaminants into the aquifer, and (4) the depressions may overlie limestone cavities filled with sand or clay that could interfere with well yield, development, and production. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874145","usgsCitation":"Hicks, D., Gill, H., and Longsworth, S., 1987, Hydrogeology, chemical quality, and availability of ground water in the Upper Floridan aquifer, Albany area, Georgia: U.S. Geological Survey Water-Resources Investigations Report 87-4145, vi, 52 p. :ill., 3 plates; maps; 28 cm., https://doi.org/10.3133/wri874145.","productDescription":"vi, 52 p. :ill., 3 plates; maps; 28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":2209,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri87-4145/","linkFileType":{"id":5,"text":"html"}},{"id":56529,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4145/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56533,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4145/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4145/report-thumb.jpg"},{"id":56530,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4145/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56531,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4145/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56532,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4145/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","city":"Albany area","otherGeospatial":"Upper Floridan aquifer","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85,31 ], [ -85,32 ], [ -83,32 ], [ -83,31 ], [ -85,31 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614889","contributors":{"authors":[{"text":"Hicks, D.W.","contributorId":61795,"corporation":false,"usgs":true,"family":"Hicks","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":198524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, H.E.","contributorId":24330,"corporation":false,"usgs":true,"family":"Gill","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":198522,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Longsworth, S.A.","contributorId":47784,"corporation":false,"usgs":true,"family":"Longsworth","given":"S.A.","affiliations":[],"preferred":false,"id":198523,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20113,"text":"ofr87404 - 1987 - Sedimentary basin models documented on computer diskettes for USGS bulletin 1810 the muPETROL expert system for classifying world sedimentary basins","interactions":[],"lastModifiedDate":"2012-02-02T00:07:37","indexId":"ofr87404","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-404","title":"Sedimentary basin models documented on computer diskettes for USGS bulletin 1810 the muPETROL expert system for classifying world sedimentary basins","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87404","usgsCitation":"Miller, B., 1987, Sedimentary basin models documented on computer diskettes for USGS bulletin 1810 the muPETROL expert system for classifying world sedimentary basins: U.S. Geological Survey Open-File Report 87-404, 5 p. ;28 cm., https://doi.org/10.3133/ofr87404.","productDescription":"5 p. ;28 cm.","costCenters":[],"links":[{"id":152269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0404/report-thumb.jpg"},{"id":49657,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0404/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd71dfe4b0b29085107f3b","contributors":{"authors":[{"text":"Miller, B.M.","contributorId":73232,"corporation":false,"usgs":true,"family":"Miller","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":182088,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11973,"text":"ofr86187 - 1987 - Chemical analysis and evaluation of 40 samples from Upper Cretaceous coal beds from the Wind River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr86187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-187","title":"Chemical analysis and evaluation of 40 samples from Upper Cretaceous coal beds from the Wind River basin, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86187","usgsCitation":"Warlow, R., Bragg, L.J., Windolph, J., Hickling, N.L., Oman, J.K., Kerry, P., and Baker, J., 1987, Chemical analysis and evaluation of 40 samples from Upper Cretaceous coal beds from the Wind River basin, Wyoming: U.S. Geological Survey Open-File Report 86-187, iv, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr86187.","productDescription":"iv, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0187/report-thumb.jpg"},{"id":39967,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4966","contributors":{"authors":[{"text":"Warlow, R. C.","contributorId":102932,"corporation":false,"usgs":true,"family":"Warlow","given":"R. C.","affiliations":[],"preferred":false,"id":164470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bragg, L. J.","contributorId":104055,"corporation":false,"usgs":true,"family":"Bragg","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":164471,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Windolph, J. F. Jr.","contributorId":96256,"corporation":false,"usgs":true,"family":"Windolph","given":"J. F.","suffix":"Jr.","affiliations":[],"preferred":false,"id":164468,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hickling, N. L.","contributorId":75935,"corporation":false,"usgs":true,"family":"Hickling","given":"N.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":164467,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Oman, J. K.","contributorId":97515,"corporation":false,"usgs":true,"family":"Oman","given":"J.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":164469,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kerry, P.T.","contributorId":11873,"corporation":false,"usgs":true,"family":"Kerry","given":"P.T.","email":"","affiliations":[],"preferred":false,"id":164465,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Baker, J.W.","contributorId":46525,"corporation":false,"usgs":true,"family":"Baker","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":164466,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":29136,"text":"wri864078 - 1987 - Hydrogeology in the area of a freshwater lens in the Floridan aquifer system, northeast Seminole County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri864078","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4078","title":"Hydrogeology in the area of a freshwater lens in the Floridan aquifer system, northeast Seminole County, Florida","docAbstract":"Northeast Seminole County, Florida, contains an isolated recharge area of the Floridan aquifer system that forms a freshwater lens completely surrounded by saline water. The freshwater lens covers an area of about 22 sq mi surrounding the town of Geneva, and generally is enclosed by the 25 ft land surface altitude contour. Thickness of the lens is about 350 ft in the center of the recharge area. The geohydrologic units in descending order consist of the post-Miocene sand and shell of the surficial aquifer; Miocene clay, sand, clay, and shell that form a leaky confining bed; and permeable Eocene limestones of the Floridan aquifer system. The freshwater lens is the result of local rainfall flushing ancient seawater from the Floridan aquifer system. Sufficient quantities of water for domestic and small public supply systems are available from the Floridan aquifer system in the Geneva area. The limiting factor for water supply in the area is the chemical quality of the water. Chloride concentrations range from < 20 mg/L in the center of the recharge area to about 5,100 mg/L near the St. Johns River southeast of Geneva. Constituents analyzed included sulfate (range 1 to 800 mg/L), hardness (range 89 to 2,076 mg/L), and iron (range 34 to 6,600 mg/L). Because the freshwater lens results entirely from local recharge, the long-term sustained freshwater yield of the aquifer in the Geneva area depends on the local recharge rate. In 1982, recharge was about 13 inches (13.8 million gal/day). Average recharge for 1941 through 1970 was estimated to be about 11 inches (11.3 million gal/day). Freshwater that recharges the aquifer in the Geneva area is either pumped out or flows north and northeast to discharge near or in the St. Johns River. Average annual outflow from the lens is about 10 in/yr. No measurable change in the size or location of the freshwater lens has occurred since studies in the early 1950's. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864078","usgsCitation":"Phelps, G.G., and Rohrer, K., 1987, Hydrogeology in the area of a freshwater lens in the Floridan aquifer system, northeast Seminole County, Florida: U.S. Geological Survey Water-Resources Investigations Report 86-4078, v, 74 p. :ill., map ;28 cm., https://doi.org/10.3133/wri864078.","productDescription":"v, 74 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4078/report-thumb.jpg"},{"id":58005,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4078/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624cd9","contributors":{"authors":[{"text":"Phelps, G. G.","contributorId":82346,"corporation":false,"usgs":true,"family":"Phelps","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":201001,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rohrer, K.P.","contributorId":72421,"corporation":false,"usgs":true,"family":"Rohrer","given":"K.P.","email":"","affiliations":[],"preferred":false,"id":201000,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11991,"text":"ofr87412A - 1987 - Comprehensive bibliographies on primary and supergene Ni-Cu-PGE mineralization associated with komatiitic and mafic intrusions in Australasia, and on the Defek intrusion, Antarctica","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr87412A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-412","chapter":"A","title":"Comprehensive bibliographies on primary and supergene Ni-Cu-PGE mineralization associated with komatiitic and mafic intrusions in Australasia, and on the Defek intrusion, Antarctica","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87412A","usgsCitation":"Czamanske, G., Groves, D., Bunting, J., and Brown, A., 1987, Comprehensive bibliographies on primary and supergene Ni-Cu-PGE mineralization associated with komatiitic and mafic intrusions in Australasia, and on the Defek intrusion, Antarctica: U.S. Geological Survey Open-File Report 87-412, 51 p. ;28 cm., https://doi.org/10.3133/ofr87412A.","productDescription":"51 p. ;28 cm.","costCenters":[],"links":[{"id":145604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0412a/report-thumb.jpg"},{"id":39985,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0412a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f3c","contributors":{"authors":[{"text":"Czamanske, G.K.","contributorId":26300,"corporation":false,"usgs":true,"family":"Czamanske","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":164557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Groves, D.I.","contributorId":73616,"corporation":false,"usgs":true,"family":"Groves","given":"D.I.","email":"","affiliations":[],"preferred":false,"id":164559,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bunting, J.A.","contributorId":16836,"corporation":false,"usgs":true,"family":"Bunting","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":164556,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brown, A.V.","contributorId":63402,"corporation":false,"usgs":true,"family":"Brown","given":"A.V.","email":"","affiliations":[],"preferred":false,"id":164558,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":14139,"text":"ofr87297 - 1987 - Volcanic hazards with regard to siting nuclear-power plants in the Pacific Northwest","interactions":[],"lastModifiedDate":"2012-02-02T00:06:43","indexId":"ofr87297","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-297","title":"Volcanic hazards with regard to siting nuclear-power plants in the Pacific Northwest","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87297","usgsCitation":"Hoblitt, R., Miller, C., and Scott, W.E., 1987, Volcanic hazards with regard to siting nuclear-power plants in the Pacific Northwest: U.S. Geological Survey Open-File Report 87-297, 196 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87297.","productDescription":"196 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":987,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://vulcan.wr.usgs.gov/Hazards/NRC_Report/framework.html","linkFileType":{"id":5,"text":"html"}},{"id":145272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0297/report-thumb.jpg"},{"id":42785,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0297/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42786,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0297/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42787,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0297/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42788,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0297/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42789,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0297/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42790,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0297/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd89b","contributors":{"authors":[{"text":"Hoblitt, R.","contributorId":89536,"corporation":false,"usgs":true,"family":"Hoblitt","given":"R.","affiliations":[],"preferred":false,"id":168991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, C.D.","contributorId":34504,"corporation":false,"usgs":true,"family":"Miller","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":168990,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scott, W. E.","contributorId":22773,"corporation":false,"usgs":true,"family":"Scott","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":168989,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29132,"text":"wri874229 - 1987 - Water levels, chloride concentrations, and pumpage in the coastal aquifers of Delaware and Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:08:49","indexId":"wri874229","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4229","title":"Water levels, chloride concentrations, and pumpage in the coastal aquifers of Delaware and Maryland","docAbstract":"The Manokin, Ocean City, Pocomoke, and unconfined aquifers of coastal Delaware and Maryland are susceptible to saltwater intrusion from inland movement of offshore water, and from vertical leakage from the bays and deeper aquifer. Comparison of data for water levels, chloride, and pumpage affected during 1974-86 shows that, with the exception of the 44th Street area in Ocean City, Maryland, increased pumpage and lower water levels have not yet caused corresponding increases in chloride concentrations in the confined aquifers. Pumpage from shallow wells near the inland bays has caused localized saltwater intrusion into the unconfined aquifer. Chloride concentrations in the Ocean City aquifer at 44th Street increased from 50 to 200mg/L from 1976 to 1986. Chloride concentrations in water from wells in the Manokin aquifer ranged from 6 to 460 mg/L, whereas those in the Ocean City aquifer ranged from 6 to 260 mg/L. Chloride concentrations in water from the Pocomoke aquifer ranged from 5 to 46 mg/L, and from 11.5 to 46 mg/L in the unconfined aquifer. Seasonal high water levels are affected more by total annual rainfall than by pumpage. Seasonal low water levels generally have declined during most years in areas of heavy pumpage along the coast. Inland, water levels have remained about the same of year to year. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874229","usgsCitation":"Phelan, D.J., 1987, Water levels, chloride concentrations, and pumpage in the coastal aquifers of Delaware and Maryland: U.S. Geological Survey Water-Resources Investigations Report 87-4229, xii, 106 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874229.","productDescription":"xii, 106 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4229/report-thumb.jpg"},{"id":58000,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4229/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58001,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4229/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9cf4","contributors":{"authors":[{"text":"Phelan, D. J.","contributorId":17635,"corporation":false,"usgs":true,"family":"Phelan","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200996,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26801,"text":"wri874007 - 1987 - Ground-water quality and geochemistry of Las Vegas Valley, Clark County, Nevada, 1981-83: Implementation of a monitoring network","interactions":[],"lastModifiedDate":"2022-02-02T21:59:20.341167","indexId":"wri874007","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4007","title":"Ground-water quality and geochemistry of Las Vegas Valley, Clark County, Nevada, 1981-83: Implementation of a monitoring network","docAbstract":"<p>As a result of rapid urban growth in Las Vegas Valley, rates of water use and wastewater disposal have grown rapidly during the last 25 years. Concern has developed over the potential water quality effects of this growth. The deep percolation of wastewater and irrigation return flow (much of which originates as imported water from Lake Mead), along with severe overdraft conditions in the principal aquifers of the valley, could combine to pose a long-term threat to groundwater quality. The quantitative investigations of groundwater quality and geochemical conditions in the valley necessary to address these concerns would include the establishment of data collection networks on a valley-wide scale that differ substantially from existing networks. The valley-wide networks would have a uniform areal distribution of sampling sites, would sample from all major depth zones, and would entail repeated sampling from each site. With these criteria in mind, 40 wells were chosen for inclusion in a demonstration monitoring network. Groundwater in the northern half of the valley generally contains 200 to 400 mg/L of dissolved solids, and is dominated by calcium, magnesium , and bicarbonate ions, reflecting a chemical equilibrium between the groundwater and the dominantly carbonate rocks in the aquifers of this area. The intermediate to deep groundwater in the southern half of the valley is of poorer quality (containing 700 to 1,500 mg/L of dissolved solids) and is dominated by calcium, magnesium, sulfate, and bicarbonate ions, reflecting the occurrence of other rock types including evaporite minerals among the still-dominant carbonate rocks in the aquifers of this part of the valley. The poorest quality groundwater in the valley is generally in the lowland parts of the valley in the first few feet beneath the water table, where dissolved solids concentrations range from 2,000 to &gt; 7,000 mg/L , and probably reflects the effects of evaporite dissolution, secondary recharge, and evapotranspiration. The most common water quality constraint on potential groundwater use is the high salinity. No evidence of large-scale contamination of deep groundwater was found in this study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874007","usgsCitation":"Dettinger, M.D., 1987, Ground-water quality and geochemistry of Las Vegas Valley, Clark County, Nevada, 1981-83: Implementation of a monitoring network: U.S. Geological Survey Water-Resources Investigations Report 87-4007, v, 69 p., https://doi.org/10.3133/wri874007.","productDescription":"v, 69 p.","costCenters":[],"links":[{"id":395317,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46696.htm"},{"id":55689,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4007/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4007/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Clark County","otherGeospatial":"Las Vegas Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.2883,\n              35.95\n            ],\n            [\n              -114.9231,\n              35.95\n            ],\n            [\n              -114.9231,\n              36.3444\n            ],\n            [\n              -115.2883,\n              36.3444\n            ],\n            [\n              -115.2883,\n              35.95\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673c0","contributors":{"authors":[{"text":"Dettinger, M. D. 0000-0002-7509-7332","orcid":"https://orcid.org/0000-0002-7509-7332","contributorId":93069,"corporation":false,"usgs":false,"family":"Dettinger","given":"M.","middleInitial":"D.","affiliations":[{"id":16196,"text":"Scripps Institution of Oceanography, La Jolla, CA","active":true,"usgs":false}],"preferred":false,"id":197027,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63114,"text":"gq1639 - 1987 - Geologic map of the Lake Eleanor quadrangle, central Sierra Nevada, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:41","indexId":"gq1639","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1639","title":"Geologic map of the Lake Eleanor quadrangle, central Sierra Nevada, California","language":"ENGLISH","doi":"10.3133/gq1639","usgsCitation":"Dodge, F., and Calk, L.C., 1987, Geologic map of the Lake Eleanor quadrangle, central Sierra Nevada, California: U.S. Geological Survey Geologic Quadrangle 1639, 1 map :col. ;45 x 35 cm., on sheet 61 x 91 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/gq1639.","productDescription":"1 map :col. ;45 x 35 cm., on sheet 61 x 91 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":101926,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_241.htm","linkFileType":{"id":5,"text":"html"},"description":"241"},{"id":249239,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1639/report.pdf","size":"73","linkFileType":{"id":1,"text":"pdf"}},{"id":252403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1639/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,37.75 ], [ -120,38 ], [ -119.75,38 ], [ -119.75,37.75 ], [ -120,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696f48","contributors":{"authors":[{"text":"Dodge, F. C.","contributorId":74012,"corporation":false,"usgs":true,"family":"Dodge","given":"F. C.","affiliations":[],"preferred":false,"id":268357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Calk, L. C.","contributorId":54261,"corporation":false,"usgs":true,"family":"Calk","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":268356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29263,"text":"wri854314 - 1987 - Analysis of sediment production from two small semiarid basins in Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri854314","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"85-4314","title":"Analysis of sediment production from two small semiarid basins in Wyoming","docAbstract":"Data were collected at two small, semiarid basins in Wyoming to determine the relation between rainfall, runoff, and sediment production. The basins were Dugout Creek tributary and Saint Marys Ditch tributary. Sufficient rainfall and runoff data were collected at Dugout Creek tributary to determine the source of sediment and the dominant sediment production processes. Because runoff from only one storm occurred in Saint Marys Ditch tributary, emphasis of the study was placed on the analysis of data collected at Dugout Creek tributary. At Dugout Creek tributary, detailed measurements were made to establish the source of sediment. To determine the quantity of material removed from headcuts during the study, two headcuts were surveyed. Aerial photographs were used to define movement of all headcuts. The total quantity of sediment removed from all headcuts between September 26, 1982, and September 26, 1983, was estimated to be 1,220 tons, or 15%-25% of the estimated total sediment load passing the streamflow-gaging station. A soil plot was used to sample upland erosion. A rainfall and runoff modeling system was used to evaluate the interaction between the physical processes which control sediment production. The greatest change in computed sediment load was caused by changing the parameter values for equations used to compute the detachment of sediment particles by rainfall and overland flow resulted in very small changes in computed sediment load. The upland areas were the primary source of sediment. A relationship was developed between the peak of storm runoff and the total sediment load for that storm runoff. The sediment concentration used to compute the total sediment load for the storm runoff was determined from sediment samples collected by two automatic pumping samplers. The coefficient of variation of the relationship is 34% with a 0.99 correlation coefficient. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854314","usgsCitation":"Rankl, J., 1987, Analysis of sediment production from two small semiarid basins in Wyoming: U.S. Geological Survey Water-Resources Investigations Report 85-4314, iv, 27 p. :ill., map ;28 cm., https://doi.org/10.3133/wri854314.","productDescription":"iv, 27 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":120075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4314/report-thumb.jpg"},{"id":58115,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4314/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db68018e","contributors":{"authors":[{"text":"Rankl, J.G.","contributorId":107733,"corporation":false,"usgs":true,"family":"Rankl","given":"J.G.","affiliations":[],"preferred":false,"id":201239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68575,"text":"ha690 - 1987 - Water withdrawn for irrigation in 1980 on the Snake River Plain, Idaho and eastern Oregon","interactions":[{"subject":{"id":44010,"text":"ofr84434 - 1984 - Water withdrawn for irrigation in 1980 on the Snake River plain, Idaho and eastern Oregon","indexId":"ofr84434","publicationYear":"1984","noYear":false,"title":"Water withdrawn for irrigation in 1980 on the Snake River plain, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":68575,"text":"ha690 - 1987 - Water withdrawn for irrigation in 1980 on the Snake River Plain, Idaho and eastern Oregon","indexId":"ha690","publicationYear":"1987","noYear":false,"title":"Water withdrawn for irrigation in 1980 on the Snake River Plain, Idaho and eastern Oregon"},"id":1}],"lastModifiedDate":"2013-11-12T14:52:30","indexId":"ha690","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"690","title":"Water withdrawn for irrigation in 1980 on the Snake River Plain, Idaho and eastern Oregon","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha690","usgsCitation":"Bigelow, B.B., Goodell, S.A., and Newton, G.D., 1987, Water withdrawn for irrigation in 1980 on the Snake River Plain, Idaho and eastern Oregon: U.S. Geological Survey Hydrologic Atlas 690, 2 Plates: 49.00 x 38.00 inches, https://doi.org/10.3133/ha690.","productDescription":"2 Plates: 49.00 x 38.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":189993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90210,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/690/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90211,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/690/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Idaho;Oregon","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.25,42.25 ], [ -117.25,44.5 ], [ -111.5,44.5 ], [ -111.5,42.25 ], [ -117.25,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eef61","contributors":{"authors":[{"text":"Bigelow, B. B.","contributorId":76317,"corporation":false,"usgs":true,"family":"Bigelow","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":278500,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodell, S. A.","contributorId":38168,"corporation":false,"usgs":true,"family":"Goodell","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":278498,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newton, G. D.","contributorId":43374,"corporation":false,"usgs":true,"family":"Newton","given":"G.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":278499,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29359,"text":"wri874198 - 1987 - Hydrogeology and geochemistry of the unsaturated zone, radioactive waste management complex, Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:49","indexId":"wri874198","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4198","title":"Hydrogeology and geochemistry of the unsaturated zone, radioactive waste management complex, Idaho National Engineering Laboratory, Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874198","usgsCitation":"Rightmire, C., and Lewis, B.D., 1987, Hydrogeology and geochemistry of the unsaturated zone, radioactive waste management complex, Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 87-4198, vii, 89 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874198.","productDescription":"vii, 89 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4198/report-thumb.jpg"},{"id":58209,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4198/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db62762e","contributors":{"authors":[{"text":"Rightmire, C.T.","contributorId":63822,"corporation":false,"usgs":true,"family":"Rightmire","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":201403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, B. D.","contributorId":85965,"corporation":false,"usgs":true,"family":"Lewis","given":"B.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":201404,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12054,"text":"ofr8754 - 1987 - Geochemical data for mineralized rocks in the Lake City area, San Juan Volcanic Field, southwest Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr8754","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-54","title":"Geochemical data for mineralized rocks in the Lake City area, San Juan Volcanic Field, southwest Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8754","usgsCitation":"Sanford, R., Korzeb, S., Seeley, J.L., and Zamudio, J., 1987, Geochemical data for mineralized rocks in the Lake City area, San Juan Volcanic Field, southwest Colorado: U.S. Geological Survey Open-File Report 87-54, iii, 213 p. :maps ;28 cm., https://doi.org/10.3133/ofr8754.","productDescription":"iii, 213 p. :maps ;28 cm.","costCenters":[],"links":[{"id":145648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0054/report-thumb.jpg"},{"id":40065,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0054/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40066,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0054/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae411","contributors":{"authors":[{"text":"Sanford, R.F.","contributorId":38562,"corporation":false,"usgs":true,"family":"Sanford","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":164853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Korzeb, S.L.","contributorId":49802,"corporation":false,"usgs":true,"family":"Korzeb","given":"S.L.","affiliations":[],"preferred":false,"id":164854,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Seeley, J. L.","contributorId":57864,"corporation":false,"usgs":true,"family":"Seeley","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":164855,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zamudio, J.A.","contributorId":29436,"corporation":false,"usgs":true,"family":"Zamudio","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":164852,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26448,"text":"wri874026 - 1987 - Sediment discharge in Rock Creek and the effect of sedimentation rate on the proposed Rock Creek Reservoir, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:27","indexId":"wri874026","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4026","title":"Sediment discharge in Rock Creek and the effect of sedimentation rate on the proposed Rock Creek Reservoir, northwestern Colorado","docAbstract":"Sediment data collected from 1976 to 1985 and stream discharge data collected from 1952 to 1980 at gaging station 09060500, Rock Creek near Toponas, Colorado, were used to determine total sediment discharge into the proposed Rock Creek Reservoir. Suspended sediment discharge and bedload discharge were related to stream discharge by using logarithmic regression relations. Mean annual suspended sediment discharge was estimated to be 309 tons/yr, and mean annual bedload discharge was estimated to be 428 tons/yr in Rock Creek at the Toponas gaging station for the 1953 through 1980 water years. The mean annual total sediment discharge into the proposed reservoir was estimated to be 768 tons/yr, which includes 10% addition to the suspended sediment discharge calculated for the Toponas gaging station to account for suspended sediment discharge from Horse Creek. This rate of mean annual total sediment discharge would decrease the long-term water storage capacity of the proposed reservoir by &lt; 1% after 100 years. Suspended sediment discharge/unit-drainage-basin area at gaging station 09060550, Rock Creek at Crater, located about 5 mi downstream for the proposed reservoir site, was equivalent to suspended-sediment discharge/unit-drainage-basin area at the Toponas gaging station during 1985. Long-term sediment data collection at the Crater gaging station could be used for detecting changes in suspended sediment discharge in Rock Creek at the proposed reservoir site. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874026","usgsCitation":"Butler, D.L., 1987, Sediment discharge in Rock Creek and the effect of sedimentation rate on the proposed Rock Creek Reservoir, northwestern Colorado: U.S. Geological Survey Water-Resources Investigations Report 87-4026, iv, 23 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874026.","productDescription":"iv, 23 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":157897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4026/report-thumb.jpg"},{"id":55271,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc037","contributors":{"authors":[{"text":"Butler, D. L.","contributorId":36967,"corporation":false,"usgs":true,"family":"Butler","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196408,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26741,"text":"wri864132 - 1987 - Statistical analysis relating well yield to construction practices and siting of wells in the Piedmont and Blue Ridge provinces of North Carolina","interactions":[],"lastModifiedDate":"2017-01-24T12:12:48","indexId":"wri864132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-4132","title":"Statistical analysis relating well yield to construction practices and siting of wells in the Piedmont and Blue Ridge provinces of North Carolina","docAbstract":"A statistical analysis was made of data from more than 6,200 water wells drilled in the fractured crystalline rocks of the Blue Ridge, Piedmont, and western edge of the Coastal Plain where crystalline rocks underlie sediments at shallow depths. The study area encompassed 65 countries in western North Carolina, an area of 30,544 square mi, comprising nearly two-thirds of the State. Additional water supplies will be needed in western North Carolina as population and industrial development continue to increase. Ground water is an attractive alternative to surface water sources for moderate to large supplies. The statistical analysis was made to identify the geologic, topographic, and construction factors associated with high-yield wells. It is generally held that the crystalline rocks of Blue Ridge and Piedmont provinces yield only small amounts of water to wells, that water is obtained from vertical fractures that pinch out at a depth of about 300 feet because of lithostatic pressure, and that the function of a larger diameter well is primarily for storage. These concepts are reasonable when based upon the average well drilled in these rocks: a domestic well, 125 feet deep, 6 inches or less in diameter, and located on a hill or ridge. However, statistical analysis shows that wells in draws or valleys have average yields three times those of wells on hills and ridges. Wells in the most productive hydrogeologic units have average yields twice those of wells in the least productive units. Wells in draws and valleys in the most productive units average five times more yield than wells on hills and ridges in the least productive units. Well diameter can have significant influence on yield; for a given depth, yield is directly proportional to well diameter. Maximum well yields are obtained from much greater depths than previously believed. For example, the average yield of 6-inch diameter wells located in draws and valleys can be expected to reach a maximum of about 45 gallons per minute at depths of 500 to 525 feet; for similarly located 12-inch diameter wells, the average yield can be expected to reach a maximum of about 150 gallons per min at depths of 700 to 800 ft. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864132","usgsCitation":"Daniel, C., 1987, Statistical analysis relating well yield to construction practices and siting of wells in the Piedmont and Blue Ridge provinces of North Carolina: U.S. Geological Survey Water-Resources Investigations Report 86-4132, v, 54 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864132.","productDescription":"v, 54 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158536,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4132/report-thumb.jpg"},{"id":55619,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4132/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Blue Ridge Province, Piedmont 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,{"id":41969,"text":"ofr87333 - 1987 - Aeromagnetic map of the Woolsey Peak-Dendora Valley area, southwestern Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr87333","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-333","title":"Aeromagnetic map of the Woolsey Peak-Dendora Valley area, southwestern Arizona","language":"ENGLISH","doi":"10.3133/ofr87333","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1987, Aeromagnetic map of the Woolsey Peak-Dendora Valley area, southwestern Arizona: U.S. Geological Survey Open-File Report 87-333, 1 map :photocopy ;80 x 132 cm., on sheet 92 x 146 cm., https://doi.org/10.3133/ofr87333.","productDescription":"1 map :photocopy ;80 x 132 cm., on sheet 92 x 146 cm.","costCenters":[],"links":[{"id":136694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21240,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0333/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68bc7b","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":530739,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68888,"text":"om220 - 1987 - Map showing wells drilled for oil and gas deeper than 20,000 feet in the conterminous United States and offshore","interactions":[{"subject":{"id":44013,"text":"ofr83922 - 1983 - Wells drilled for oil and gas deeper than 20,000 feet in the conterminous United States and offshore","indexId":"ofr83922","publicationYear":"1983","noYear":false,"title":"Wells drilled for oil and gas deeper than 20,000 feet in the conterminous United States and offshore"},"predicate":"SUPERSEDED_BY","object":{"id":68888,"text":"om220 - 1987 - Map showing wells drilled for oil and gas deeper than 20,000 feet in the conterminous United States and offshore","indexId":"om220","publicationYear":"1987","noYear":false,"title":"Map showing wells drilled for oil and gas deeper than 20,000 feet in the conterminous United States and offshore"},"id":1}],"lastModifiedDate":"2019-12-31T11:23:51","indexId":"om220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":329,"text":"Oil and Gas Investigation Map","code":"OM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"220","title":"Map showing wells drilled for oil and gas deeper than 20,000 feet in the conterminous United States and offshore","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/om220","usgsCitation":"comiled by Takahashi, K.I., and Cunningham, K.I., 1987, Map showing wells drilled for oil and gas deeper than 20,000 feet in the conterminous United States and offshore (Supersedes OFR 83-922): U.S. Geological Survey Oil and Gas Investigation Map 220, HTML, https://doi.org/10.3133/om220.","productDescription":"HTML","costCenters":[],"links":[{"id":188283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":105001,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5376.htm","linkFileType":{"id":5,"text":"html"},"description":"5376"}],"scale":"5000000","country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -129.7265625,\n              23.885837699862005\n            ],\n            [\n              -65.390625,\n              23.885837699862005\n            ],\n            [\n              -65.390625,\n              49.15296965617042\n            ],\n            [\n              -129.7265625,\n              49.15296965617042\n            ],\n            [\n              -129.7265625,\n              23.885837699862005\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Supersedes OFR 83-922","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64959d","contributors":{"editors":[{"text":"Varnes, Katharine L.","contributorId":65927,"corporation":false,"usgs":true,"family":"Varnes","given":"Katharine","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":745413,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"comiled by Takahashi, K. I.","contributorId":86633,"corporation":false,"usgs":true,"family":"comiled by Takahashi","given":"K.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":279162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cunningham, K. I. (compiler)","contributorId":104341,"corporation":false,"usgs":true,"family":"Cunningham","given":"K.","suffix":"(compiler)","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":279163,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26757,"text":"wri874084 - 1987 - Movement of ground water in coal-bearing rocks near Fishtrap Lake in Pike County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri874084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4084","title":"Movement of ground water in coal-bearing rocks near Fishtrap Lake in Pike County, Kentucky","docAbstract":"Eight test holes were core-drilled from various altitudes in a typical coal-bearing sequence rocks of Pennsylvania age in Pike County, eastern Kentucky. Vertical fractures were common in cores from shallow depths, but became less common or absent toward the bottom of two test holes drilled 400 and 291 ft deep. Most fractures readily injected water, and near the bottoms of the two deep holes, coal beds accepted water in the non-fractured rocks. Rhodamin-WT dye was injected in a 61-ft deep ridge-top well on October 24, 1985 and was detected in varying concentrations in water samples taken from all down-gradient piezometers at the study site on November 7, 1985. The presence of dye in down-gradient piezometers indicated that groundwater in the Eastern Kentucky coal field can move from areas of higher head to areas of lower head. The movement probably occurs in a stair-step fashion through a complex system of near-vertical fractures, and laterally through permeable rocks, which probably are the coal beds. This suggests that land uses on ridges could affect the quality of water from wells or springs at lower altitudes on hillsides or in the valley bottoms even though separated by a thick interval of rocks that include beds of low primary permeability. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874084","usgsCitation":"Davis, R.W., 1987, Movement of ground water in coal-bearing rocks near Fishtrap Lake in Pike County, Kentucky: U.S. Geological Survey Water-Resources Investigations Report 87-4084, iv, 24 p. :ill. ;28 cm., https://doi.org/10.3133/wri874084.","productDescription":"iv, 24 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":126418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4084/report-thumb.jpg"},{"id":55647,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641027","contributors":{"authors":[{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196949,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29378,"text":"wri854291 - 1987 - Possible changes in ground-water flow to the Pecos River caused by Santa Rosa Lake, Guadalupe County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri854291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"85-4291","title":"Possible changes in ground-water flow to the Pecos River caused by Santa Rosa Lake, Guadalupe County, New Mexico","docAbstract":"In 1980 Santa Rosa Dam began impounding water on the Pecos River about 7 miles north of Santa Rosa, New Mexico, to provide flood control, sediment control, and storage for irrigation. Santa Rosa Lake has caused changes in the groundwater flow system, which may cause changes in the streamflow of the Pecos River that cannot be detected at the present streamflow gaging stations. Data collected at these stations are used to measure the amount of water available for downstream users. A three-dimensional groundwater flow model for a 950 sq mi area between Anton Chico and Puerto de Luna was used to simulate the effects of Santa Rosa Lake on groundwater flow to a gaining reach of the Pecos River for lake levels of 4,675, 4,715, 4,725, 4,750, 4,776, and 4,797 feet above sea level and durations of impoundment of 30, 90, 182, and 365 days for all levels except 4 ,797 feet. These simulations indicated that streamflow in the Pecos River could increase by as much as 2 cu ft/sec between the dam and Puerto de Luna if the lake level were maintained at 4 ,797 feet for 90 days or 4,776 feet for 1 year. About 90% of this increased streamflow would occur &lt; 0.5 mi downstream from the dam, some of which would be measured at the streamflow gaging station located 0.2 mile downstream from the dam. Simulations also indicated that the lake will affect groundwater flow such that inflow to the study area may be decreased by as much as 1.9 cu ft/sec. This water may leave the Pecos River drainage basin or be diverted back to the Pecos River downstream from the gaging station near Puerto de Luna. In either case, this quantity represents a net loss of water upstream from Puerto de Luna. Most simulations indicated that the decrease in groundwater flow into the study area would be of about the same quantity as the simulated increase in streamflow downstream from the dam. Therefore, the net effect of the lake on the flow of the Pecos River in the study area appears to be negligible. Model simulations indicated that effect of lake levels below 4 ,750 feet on water levels in observation wells completed in the San Andres Limestone could not be distinguished from the effects of other hydrologic stresses. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854291","usgsCitation":"Risser, D.W., 1987, Possible changes in ground-water flow to the Pecos River caused by Santa Rosa Lake, Guadalupe County, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 85-4291, viii, 79 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854291.","productDescription":"viii, 79 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4291/report-thumb.jpg"},{"id":58223,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4291/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0fe4b07f02db6a0372","contributors":{"authors":[{"text":"Risser, D. W.","contributorId":48211,"corporation":false,"usgs":true,"family":"Risser","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":201433,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14151,"text":"ofr86560H - 1987 - Dive report: Alvin dive #1461; September 28, 1984 (JD 272); Plume site, southern Juan de Fuca Rift","interactions":[],"lastModifiedDate":"2017-09-13T16:40:59","indexId":"ofr86560H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"86-560","chapter":"H","title":"Dive report: Alvin dive #1461; September 28, 1984 (JD 272); Plume site, southern Juan de Fuca Rift","docAbstract":"<p>Dive 1461 was the seventh of nine dives during a sea-going field program to investigate hydrothermal activity along the crest of the southern Juan de Fuca Ridge. During this dive on the Plume site, ALVIN crossed the western floor of the axial valley and traversed about 300 ra of the rim and floor of the narrow inner cleft. Hydrotherraal vents were observed only along the east wall of the inner cleft, and venting was concentrated in a single area less than 50 ra long near the base of that wall. The principal vents extended up the wall from the floor of the cleft to a height of about 10 m. Deposits of hydrothermal minerals occur as incrustations and chimneys on the floor and wall of the cleft. Associated with the hydrothermal vents is a community of vent organisms dominated by vestimentiferan worms and fluffy materials of uncertain nature. </p><p>The inner cleft at the Plume Site is about 60 ra wide and 15-30 m deep. It has a simple U-shaped profile north of the active vent area, but to the south it contains at least one high, narrow ridge which converges with the east wall of the cleft at the site of hydrothermal venting. This area was also the site of a volcanic eruption, which occurred sometime earlier. Like many similar but subaerial examples, this eruption was episodic, but the cause of its interruptions is not yet known. The present hydrotherraal activity appears to be a residual effect of that last eruption, and the rate of hydrothermal deposition will probably decline in this area until another eruption occurs. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86560H","usgsCitation":"Holcomb, R.T., Kappel, E.S., and Ross, S.L., 1987, Dive report: Alvin dive #1461; September 28, 1984 (JD 272); Plume site, southern Juan de Fuca Rift: U.S. Geological Survey Open-File Report 86-560, 101 p., https://doi.org/10.3133/ofr86560H.","productDescription":"101 p.","numberOfPages":"101","costCenters":[],"links":[{"id":42799,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0560h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0560h/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d8a4","contributors":{"authors":[{"text":"Holcomb, R. T.","contributorId":99146,"corporation":false,"usgs":true,"family":"Holcomb","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":169007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kappel, Ellen S.","contributorId":71181,"corporation":false,"usgs":true,"family":"Kappel","given":"Ellen","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":169006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ross, Stephanie L. 0000-0003-1389-4405 sross@usgs.gov","orcid":"https://orcid.org/0000-0003-1389-4405","contributorId":1024,"corporation":false,"usgs":true,"family":"Ross","given":"Stephanie","email":"sross@usgs.gov","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":169005,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14118,"text":"ofr87247 - 1987 - National and regional trends in water-well drilling in the United States, 1964-84","interactions":[],"lastModifiedDate":"2019-11-27T10:19:05","indexId":"ofr87247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-247","title":"National and regional trends in water-well drilling in the United States, 1964-84","docAbstract":"<p>Information on national and regional water well drilling activity is important for water resource planning and management and for water related equipment marketing. A study was conducted to analyze drilling trends on the basis of data for selected years from 1964 through 1984. The study focused primarily on the years 1964 and 1980-84, but also included data from 1960. Approximately 397,000 water wells were drilled in the United States in 1984. Seven states--Florida, Texas, New York, Michigan, North Carolina, Virginia, and Ohio--accounted for 39% of all the wells drilled in the United States in 1984. Florida led the nation in drilling activity with 45,600 new wells. The 1984 national drilling total was 2.6% &gt; the total for 1980 (387,000) and 8.5% &lt; the total for 1964 (434,000). However, these moderate differences do not reflect substantial year-to-year fluctuations that may have occurred during that 20-yr period. Qualitative comparisons suggest that drilling activity for a given year is closely related to the number of housing starts for that year. If so, there may have been peaks in drilling activity in 1972 and 1977-78 (corresponding to peaks in housing starts) that are not identified in this study because of a lack of available well drilling data for those years. Well drilling data for 1964 and the 1980-84 period probably represent a low to moderate level of drilling activity, and, if compared to earlier data, suggest that there has been no substantial growth or decline in the water well industry as a whole since the 1940's. (Author's abstract)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr87247","usgsCitation":"Hindall, S.M., and Eberle, M., 1987, National and regional trends in water-well drilling in the United States, 1964-84: U.S. Geological Survey Open-File Report 87-247, iv, 25 p. , https://doi.org/10.3133/ofr87247.","productDescription":"iv, 25 p. ","costCenters":[],"links":[{"id":145932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0247/report-thumb.jpg"},{"id":369715,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0247/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"geometry\": {\n        \"type\": \"MultiPolygon\",\n        \"coordinates\": [\n          [\n            [\n              [\n                -94.81758,\n                49.38905\n              ],\n              [\n                -94.64,\n                48.84\n              ],\n              [\n                -94.32914,\n                48.67074\n              ],\n              [\n                -93.63087,\n                48.60926\n              ],\n              [\n                -92.61,\n                48.45\n              ],\n             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M.","contributorId":59414,"corporation":false,"usgs":true,"family":"Hindall","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":168951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eberle, Michael","contributorId":39770,"corporation":false,"usgs":true,"family":"Eberle","given":"Michael","email":"","affiliations":[],"preferred":false,"id":168950,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29178,"text":"wri874140 - 1987 - Hydrogeology of McMullen Valley, west-central Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri874140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4140","title":"Hydrogeology of McMullen Valley, west-central Arizona","docAbstract":"The geohydrology of McMullen Valley, west-central Arizona, was investigated using geologic, geophysical, and hydrologic data and a numerical model of the groundwater system. Interpretation of geologic and geophysical information indicates that the main structure of McMullen Valley is a syncline that has been normal faulted on the southeast side. Basin fill that accumulated in the structural depression during late Miocene to Pleistocene time is the main aquifer and is divided into upper and lower units on the basis of lithologic information. The upper unit is a thin layer of coarse-grained sediments and generally is not saturated. The lower unit is 3,000 to 4,000 ft thick, includes a fine-grained facies in the upper 1,000 ft, and is the main source of water. The fine-grained facies is found in the southwest half of the basin and is further divided into upper and lower parts. The lower part of the fine-grained facies has: a higher percentage of silt and clay than the upper part, contains evaporites, does not yield water to wells, and separates the aquifer into shallow and deep systems. A numerical model was used to analyze the groundwater system for both steady-state and transient conditions. The transient model was used to analyze system response to pumping stress. The transient system is one of storage depletion, and water level declines are controlled by pumping and specific yield distributions. Water level declines are also influenced by hydraulic properties and areal extent of the fine-grained facies. Significant water level declines may extend to aquifer boundaries in most of the basin; in one area, impermeable boundary greatly influences declines. The location of the nearby boundary was estimated through gravity data modeling. Several hydrologic components, including hydraulic properties and areal extent of the fine-grained facies , storage properties, and aquifer boundaries, need better definition in order to develop a more accurate model of the groundwater system. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874140","usgsCitation":"Pool, D.R., 1987, Hydrogeology of McMullen Valley, west-central Arizona: U.S. Geological Survey Water-Resources Investigations Report 87-4140, v, 51 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874140.","productDescription":"v, 51 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4140/report-thumb.jpg"},{"id":58049,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4140/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db54595a","contributors":{"authors":[{"text":"Pool, D. R.","contributorId":75581,"corporation":false,"usgs":true,"family":"Pool","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":201091,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15722,"text":"ofr87276 - 1987 - Generalized geologic map of the basement rocks of the southern Sierra Nevada, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr87276","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-276","title":"Generalized geologic map of the basement rocks of the southern Sierra Nevada, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87276","usgsCitation":"Ross, D.C., 1987, Generalized geologic map of the basement rocks of the southern Sierra Nevada, California: U.S. Geological Survey Open-File Report 87-276, 30 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87276.","productDescription":"30 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":148605,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0276/report-thumb.jpg"},{"id":44742,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0276/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44743,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0276/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0276/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aee7b","contributors":{"authors":[{"text":"Ross, D. C.","contributorId":103681,"corporation":false,"usgs":true,"family":"Ross","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":171600,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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