{"pageNumber":"6736","pageRowStart":"168375","pageSize":"25","recordCount":184883,"records":[{"id":947,"text":"wsp1779B - 1963 - Variations in the chemical character of the Susquehanna River at Harrisburg, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-07T09:17:39","indexId":"wsp1779B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1779","chapter":"B","title":"Variations in the chemical character of the Susquehanna River at Harrisburg, Pennsylvania","docAbstract":"The chemical quality of the Susquehanna River at Harrisburg is influenced by three major factors: streamflow, anthracite and bituminous coal-mine drainage, and geology. Water samples collected at Harrisburg near the west bank of the Susquehanna River and those of western tributaries that drain limestone terranes are similar in chemical quality. The water is alkaline and contains calcium, magnesium, and bicarbonate-ion concentrations typical of water drained from limestone. The chemical quality of water samples collected in the center of the river resembles the quality of the West Branch Susquehanna River, which has a dissolved-solids content of about 200 parts per million, and a sulfate-ion concentration that generally exceeds the bicarbonate-ion concentration. Samples collected near the east or Harrisburg bank show the effect of anthracite coalmine drainage from the river's eastern tributaries. The pH of these samples ranges from 5.7 to 7.5, and sulfate is the predominate ion. \r\n\r\nThe dissolved-solids content of the river at the Harrisburg cross-section stations is inversely proportional to the streamflow. During periods of low riverflow, the dissolved-solids content approaches a maximum; during periods of high flow, the content is low. \r\n\r\nThe chemical composition of the river at the Harrisburg cross section indicates that water from the principal tributaries above Harrisburg does not mix sufficiently to lose its chemical-quality identity before reaching Harrisburg irrespective of the long distance involved, the many islands and bridge piers, and the rough streambed. This lack of lateral mixing is probably due to the small depth-width ratio and the extreme width of the river.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1779B","usgsCitation":"Anderson, P.W., 1963, Variations in the chemical character of the Susquehanna River at Harrisburg, Pennsylvania: U.S. Geological Survey Water Supply Paper 1779, iii, 17 p. :illus., map ;24 cm., https://doi.org/10.3133/wsp1779B.","productDescription":"iii, 17 p. :illus., map ;24 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":25447,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48e3e4b07f02db54f199","contributors":{"authors":[{"text":"Anderson, Peter W.","contributorId":10400,"corporation":false,"usgs":true,"family":"Anderson","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":142902,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1009,"text":"wsp1579 - 1963 - Progress report on the ground-water resources of the Louisville area, Kentucky, 1949-55","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1579","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1579","title":"Progress report on the ground-water resources of the Louisville area, Kentucky, 1949-55","docAbstract":"In the Louisville area, the principal water-bearing formations are the glacial-outwash sand and gravel and, in places, the underlying limestone. During the period 1949 through 1955 pumpage from the two aquifers averaged about 30 mgd (million gallons per day). The pumpage was approximately in balance with the normal net recharge to the area but was only about 8 percent of the estimated potential supply of ground water, including induced infiltration from the river. In the Louisville area, ground water is used chiefly for air conditioning and for industrial cooling. In the part of the area southwest of the city, ground water is used also for public supply. \r\n\r\nHigh ground-water levels in 1937 resulted from the greatest flood of record. Subsequently, water levels generally declined in the entire Louisville area. In downtown Louisville, where ground water is used for air conditioning, the water level fluctuates seasonally in response to variations in the rate of pumping. In the heavily pumped industrial areas, where ground water is used for cooling, water-level fluctuations correlate with changes in rates of pumping caused by variations in production schedules. Levels were lowest during the years of World War II. During the period 1952-55, relatively low levels throughout the area reflected the effects of less than normal rainfall, summer drought, and sustained pumping. \r\n\r\nGround water in the Louisville area is very hard and generally of the calcium bicarbonate or calcium sulfate type. It is high in iron and sulfate content but is moderately low in chloride content. In water of the sand and gravel aquifer, the concentration of sulfate has increased gradually during the period 1949-54.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1579","usgsCitation":"Bell, E., Kellogg, R.W., and Kulp, W.K., 1963, Progress report on the ground-water resources of the Louisville area, Kentucky, 1949-55: U.S. Geological Survey Water Supply Paper 1579, iv, 47 p. :ill., maps ;24 cm. + separate portfolio with plates., https://doi.org/10.3133/wsp1579.","productDescription":"iv, 47 p. :ill., maps ;24 cm. + separate portfolio with plates.","costCenters":[],"links":[{"id":137977,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1579/report-thumb.jpg"},{"id":25589,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25590,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25591,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25592,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25593,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25594,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25595,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25596,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25597,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25598,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25599,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25600,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25601,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25602,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25603,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1579/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25604,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1579/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dbab","contributors":{"authors":[{"text":"Bell, Edwin A.","contributorId":96660,"corporation":false,"usgs":true,"family":"Bell","given":"Edwin A.","affiliations":[],"preferred":false,"id":143018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kellogg, Robert W.","contributorId":61793,"corporation":false,"usgs":true,"family":"Kellogg","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143017,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kulp, Willis K.","contributorId":8076,"corporation":false,"usgs":true,"family":"Kulp","given":"Willis","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":143016,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1325,"text":"wsp1619F - 1963 - Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California","interactions":[{"subject":{"id":52163,"text":"ofr6148 - 1961 - Ground-water conditions, Naval Missile Facility, Point Arguello, California","indexId":"ofr6148","publicationYear":"1961","noYear":false,"title":"Ground-water conditions, Naval Missile Facility, Point Arguello, California"},"predicate":"SUPERSEDED_BY","object":{"id":1325,"text":"wsp1619F - 1963 - Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California","indexId":"wsp1619F","publicationYear":"1963","noYear":false,"chapter":"F","title":"Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California"},"id":1},{"subject":{"id":52240,"text":"ofr6244 - 1962 - Ground-water conditions, U. S. Naval Missile Facility, Point Arguello, California, June 1961-June 1962","indexId":"ofr6244","publicationYear":"1962","noYear":false,"title":"Ground-water conditions, U. S. Naval Missile Facility, Point Arguello, California, June 1961-June 1962"},"predicate":"SUPERSEDED_BY","object":{"id":1325,"text":"wsp1619F - 1963 - Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California","indexId":"wsp1619F","publicationYear":"1963","noYear":false,"chapter":"F","title":"Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1619F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1619","chapter":"F","title":"Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1619F","usgsCitation":"Evenson, R.E., and Miller, G., 1963, Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California: U.S. Geological Survey Water Supply Paper 1619, iv, 35 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1619F.","productDescription":"iv, 35 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619f/report-thumb.jpg"},{"id":26372,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26373,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26374,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685fb1","contributors":{"authors":[{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, G.A.","contributorId":107671,"corporation":false,"usgs":true,"family":"Miller","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":143567,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52359,"text":"ofr63109 - 1963 - A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California","interactions":[{"subject":{"id":52359,"text":"ofr63109 - 1963 - A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California","indexId":"ofr63109","publicationYear":"1963","noYear":false,"title":"A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California"},"predicate":"SUPERSEDED_BY","object":{"id":2508,"text":"wsp1779Y - 1964 - A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California","indexId":"wsp1779Y","publicationYear":"1964","noYear":false,"chapter":"Y","title":"A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California"},"id":1}],"supersededBy":{"id":2508,"text":"wsp1779Y - 1964 - A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California","indexId":"wsp1779Y","publicationYear":"1964","noYear":false,"title":"A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California"},"lastModifiedDate":"2012-02-02T00:11:32","indexId":"ofr63109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-109","title":"A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California","language":"ENGLISH","doi":"10.3133/ofr63109","usgsCitation":"Pistrang, M., and Kunkel, F., 1963, A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California: U.S. Geological Survey Open-File Report 63-109, 77 p., https://doi.org/10.3133/ofr63109.","productDescription":"77 p.","costCenters":[],"links":[{"id":178073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4979e4b0b290850ef365","contributors":{"authors":[{"text":"Pistrang, M.A.","contributorId":69603,"corporation":false,"usgs":true,"family":"Pistrang","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":245214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":245213,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38971,"text":"pp427A - 1963 - Description of physical environment and of strip-mining operations in parts of Beaver Creek basin, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp427A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"427","chapter":"A","title":"Description of physical environment and of strip-mining operations in parts of Beaver Creek basin, Kentucky","language":"ENGLISH","doi":"10.3133/pp427A","usgsCitation":"Musser, J., 1963, Description of physical environment and of strip-mining operations in parts of Beaver Creek basin, Kentucky: U.S. Geological Survey Professional Paper 427, p. A1-A25, https://doi.org/10.3133/pp427A.","productDescription":"p. A1-A25","costCenters":[],"links":[{"id":120395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0427a/report-thumb.jpg"},{"id":66037,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0427a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66038,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0427a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66039,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0427a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66040,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0427a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66041,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0427a/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66042,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0427a/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66043,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0427a/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0427a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c881","contributors":{"authors":[{"text":"Musser, J.J.","contributorId":72035,"corporation":false,"usgs":true,"family":"Musser","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":220744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1299,"text":"wsp1605 - 1963 - Geology and hydrology of Agua Caliente Spring, Palm Springs, California","interactions":[],"lastModifiedDate":"2022-01-04T22:16:29.021388","indexId":"wsp1605","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1605","title":"Geology and hydrology of Agua Caliente Spring, Palm Springs, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1605","usgsCitation":"Dutcher, L., and Bader, J., 1963, Geology and hydrology of Agua Caliente Spring, Palm Springs, California: U.S. Geological Survey Water Supply Paper 1605, Report: iv, 41 p.; 2 Plates: 18.94 × 14.81 inches and 9.82 × 14.42 inches, https://doi.org/10.3133/wsp1605.","productDescription":"Report: iv, 41 p.; 2 Plates: 18.94 × 14.81 inches and 9.82 × 14.42 inches","costCenters":[],"links":[{"id":393889,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24793.htm"},{"id":276510,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1605/plate-2.pdf"},{"id":276509,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1605/plate-1.pdf"},{"id":26312,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1605/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1605/report-thumb.jpg"}],"country":"United States","state":"California","city":"Palm Springs","otherGeospatial":"Agua Caliente Spring","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.56768798828125,\n              33.77343983379775\n            ],\n            [\n              -116.40289306640624,\n              33.77343983379775\n            ],\n            [\n              -116.40289306640624,\n              33.91259414191221\n            ],\n            [\n              -116.56768798828125,\n              33.91259414191221\n            ],\n            [\n              -116.56768798828125,\n              33.77343983379775\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4673","contributors":{"authors":[{"text":"Dutcher, L.C.","contributorId":42191,"corporation":false,"usgs":true,"family":"Dutcher","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":143523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bader, J. S.","contributorId":65830,"corporation":false,"usgs":true,"family":"Bader","given":"J. S.","affiliations":[],"preferred":false,"id":143524,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1298,"text":"wsp1419 - 1963 - Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault","interactions":[{"subject":{"id":51238,"text":"ofr5358 - 1953 - San Bernardion Area, California: Three maps showing water-level contours for the San Bernardino area for spring 1936, spring 1945, and spring 1951; east-west geologic section from Colton to Mill Creek Canyon; geologic section from Shandin Hills southeast to Bryn Mawr; and water level profiles along the section from Colton to Mill Creek Canyon","indexId":"ofr5358","publicationYear":"1953","noYear":false,"title":"San Bernardion Area, California: Three maps showing water-level contours for the San Bernardino area for spring 1936, spring 1945, and spring 1951; east-west geologic section from Colton to Mill Creek Canyon; geologic section from Shandin Hills southeast to Bryn Mawr; and water level profiles along the section from Colton to Mill Creek Canyon"},"predicate":"SUPERSEDED_BY","object":{"id":1298,"text":"wsp1419 - 1963 - Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault","indexId":"wsp1419","publicationYear":"1963","noYear":false,"title":"Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault"},"id":1},{"subject":{"id":51253,"text":"ofr5376 - 1953 - Maps and sections showing ground-water conditions in the San Bernardino area, California","indexId":"ofr5376","publicationYear":"1953","noYear":false,"title":"Maps and sections showing ground-water conditions in the San Bernardino area, California"},"predicate":"SUPERSEDED_BY","object":{"id":1298,"text":"wsp1419 - 1963 - Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault","indexId":"wsp1419","publicationYear":"1963","noYear":false,"title":"Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault"},"id":2}],"lastModifiedDate":"2022-02-01T20:10:25.234553","indexId":"wsp1419","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1419","title":"Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault","docAbstract":"<p>This is the second in a series of interpretive reports on subsurface outflow from the ground-water basins of San Bernardino County, Calif., prepared by the U.S. Geological Survey in cooperation with the San Bernardino County Flood Control District. One principal purpose of the study was to estimate the ground-water outflow from the Bunker Hill basin to the Rialto-Colton basin across the San Jacinto fault, which, except locally, forms a nearly impermeable boundary between the two basins. In addition, the report deals qualitatively with the geology, the fault barriers that divide the area into several ground-water basins, the physical nature and degree of imperviousness of the barriers, the occurrence and movement of ground water and fluctuations of water level in the basins, and the chemical quality of surface and ground waters in the San Bernardino area. The report includes a geologic map and sections, water-level-contour maps and profiles, and hydrographs of selected well. The Santa Ana River, the principal stream, flows generally westward across the area. Channels of the river and its tributaries overlie a large irregular structural depression filled with alluvial deposits ranging in age from late Tertiary to Recent and forming a valley bounded on the north by the San Gabriel Mountains, on the east by the San Bernardino Mountains, and on the south by an irregular group of hills. Large alluvial fans underlie most of the area, but its landforms also include alluvial benches and terraces near the mountains, stream channels, and elongate hills, ridges, and scarps along the trace of the San Jacinto fault, which strikes northwestward across the valley about in the center of the area. This fault and others divide the area into ground-water basins, which include the Bunker Hill, Rialto-Colton, upper and lower Lytle and Chino basins. The water-bearing deposits include the following units: the younger alluvium. of Recent age, which occupies principally the backfilled channels beneath the Santa Ana River and its tributaries and through which ground water moves from Bunker Hill basin to Rialto-Colton basin; the older alluvium, of Pleistocene age, which is the principal water-bearing unit of the area and yields water to more than a thousand wells; and continental deposits of Tertiary to Quaternary age, which crop out along the southern margin of the area and locally along the San Gabriel Mountains on the north. The younger alluvium attains a maximum thickness of about 125 feet beneath the Santa Ana River south of San Bernardino. Locally in the Bunker Hill basin it is composed of two members, an upper member of relatively impermeable clay and a lower member of highly permeable material in which water is confined by the upper member. The older alluvium locally has a known thickness greater than 700 feet; elsewhere in the San Bernardino Valley it may exceed 1,400 feet. Locally, where ground water is confined in Bunker Hill basin, the older alluvium is divided into three permeable water-bearing zones separated from each other and from the younger alluvium above by less permeable zones. In parts of Chino and Rialto-Colton basins the alluvium consists of a coarse-grained facies along a former course of a major stream that is interfingered with and overlain by relatively fine-grained deposits. The permeability of the younger alluvium in the area beneath the Santa Ana River downstream from the San Jacinto fault was determined from tests to be about 2,700 gallons per day per square foot. The permeability of the coarse water-yielding materials of the older alluvium several miles downstream was estimated from tests to be about the same magnitude. Rocks that yield practically no water include continental rocks of Tertiary age, which are not exposed in the area but are tapped by wells in Rialto-Colton basin, and crystalline and metamorphic rocks of pre-Tertiary age that form the bedrock of the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1419","usgsCitation":"Dutcher, L., and Garrett, A., 1963, Geologic and hydrologic features of the San Bernardino area, California; with special reference to underflow across the San Jacinto fault: U.S. Geological Survey Water Supply Paper 1419, Report: vi, 114 p.; 19 Plates: \t37.00 × 52.19 inches or smaller, https://doi.org/10.3133/wsp1419.","productDescription":"Report: vi, 114 p.; 19 Plates: \t37.00 × 52.19 inches or 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,{"id":1275,"text":"wsp1691 - 1963 - Ground-water contamination and legal controls in Michigan","interactions":[{"subject":{"id":52078,"text":"ofr6036 - 1960 - Ground-water contamination and legal controls in Michigan","indexId":"ofr6036","publicationYear":"1960","noYear":false,"title":"Ground-water contamination and legal controls in Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":1275,"text":"wsp1691 - 1963 - Ground-water contamination and legal controls in Michigan","indexId":"wsp1691","publicationYear":"1963","noYear":false,"title":"Ground-water contamination and legal controls in Michigan"},"id":1}],"lastModifiedDate":"2016-09-22T13:46:38","indexId":"wsp1691","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1691","title":"Ground-water contamination and legal controls in Michigan","docAbstract":"<p>The great importance of the fresh ground-water resources of Michigan is evident because 90 percent of the rural and about 70 percent of the total population of the State exclusive of the Detroit metropolitan area are supplied from underground sources. The water-supply and public-health problems that have been caused by some cases of ground-water contamination in the State illustrate the necessity of protecting this vital resource.</p><p>Manmade and natural contaminants, including many types of chemical and organic matter, have entered many of the numerous aquifers of the State. Aquifers have been contaminated by waste-laden liquids percolating from the surface or from the zone of aeration and by direct injection to the aquifer itself. Industrial and domestic wastes, septic tanks, leaking sewers, flood waters or other poor quality surface waters, mine waters, solids stored or spread at the surface, and even airborne wastes all have been sources of ground-water contamination in Michigan. In addition, naturally occurring saline waters have been induced into other aquifers by overpumping or unrestricted flow from artesian wells, possibly by dewatering operations, and by the deepening of surface stream channels. Vertical migration of saline waters through open holes from formations underlying various important aquifers also has spoiled some of the fresh ground waters in the State. In spite of the contamination that has occurred, however, the total amount of ground water that has been spoiled is only a small part of the total resource. Neither is the contamination so widespread as that of the surface streams of Michigan.</p><p>Overall legal authority to control most types of ground-water contamination in the State has been assigned by the Michigan Legislature to the Water Resources Commission, although the Department of Conservation and the Health Department also exercise important water-pollution control functions. The Michigan Supreme Court, in an important case upholding the power of the Water Resources Commission to control pollution of ground water, in effect has introduced the doctrine of reasonable use into the law of the State. Excluding controls administered by the Department of Conservation on activities of the oil and gas industry, however, legal controls have not been used abate intrusion of natural saline waters into fresh-water aquifers in response to pumping and other manmade changes in the hydrologic regimen.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1691","usgsCitation":"Deutsch, M., 1963, Ground-water contamination and legal controls in Michigan: U.S. Geological Survey Water Supply Paper 1691, v, 79 p., https://doi.org/10.3133/wsp1691.","productDescription":"v, 79 p.","costCenters":[{"id":382,"text":"Michigan Water Science 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,{"id":52366,"text":"ofr63122 - 1963 - Geology and availability of ground water in the vicinity of Gila Cliff Dwellings National Monument, Catron County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:11:32","indexId":"ofr63122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-122","title":"Geology and availability of ground water in the vicinity of Gila Cliff Dwellings National Monument, Catron County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr63122","usgsCitation":"Trauger, F., 1963, Geology and availability of ground water in the vicinity of Gila Cliff Dwellings National Monument, Catron County, New Mexico: U.S. Geological Survey Open-File Report 63-122, 24 p., https://doi.org/10.3133/ofr63122.","productDescription":"24 p.","costCenters":[],"links":[{"id":100166,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0122/report.pdf","size":"13077","linkFileType":{"id":1,"text":"pdf"}},{"id":178148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0122/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68650d","contributors":{"authors":[{"text":"Trauger, F.D.","contributorId":102520,"corporation":false,"usgs":true,"family":"Trauger","given":"F.D.","email":"","affiliations":[],"preferred":false,"id":245226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6425,"text":"pp363 - 1963 - Geology of the Capitol Reef area, Wayne and Garfield Counties, Utah","interactions":[],"lastModifiedDate":"2025-09-22T17:57:42.361737","indexId":"pp363","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"363","title":"Geology of the Capitol Reef area, Wayne and Garfield Counties, Utah","docAbstract":"<p>The Capitol Reef area includes about 900 square miles in western Wayne and north-central Garfield Counties, Utah. It is along the border between the High Plateaus of Utah and the Canyon Lands sections of the Colorado' Plateaus province. Capitol Reef National Monument is in the eastern part of the mapped area. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp363","usgsCitation":"Smith, J.F., Huff, L.C., Hinrichs, E.N., and Luedke, R.G., 1963, Geology of the Capitol Reef area, Wayne and Garfield Counties, Utah: U.S. Geological Survey Professional Paper 363, Report: iv, 102 p.; 2 Plates: 38.88 x 44.60 inches and 18.44 x 18.72 inches, https://doi.org/10.3133/pp363.","productDescription":"Report: iv, 102 p.; 2 Plates: 38.88 x 44.60 inches and 18.44 x 18.72 inches","numberOfPages":"107","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":495847,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4361.htm","linkFileType":{"id":5,"text":"html"}},{"id":140281,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0363/report-thumb.jpg"},{"id":112832,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0363/plate-2.pdf","text":"Plate 2","size":"1.16 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Structure contour map and wall sections of the Oyler Mine, Capitol Reef area"},{"id":112830,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0363/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":112831,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0363/plate-1.pdf","text":"Plate 1","size":"14.6 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geologic map and sections of the Capitol Reef area"}],"country":"United States","state":"Utah","county":"Garfield County, Wayne County","otherGeospatial":"Capitol Reef area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.625,\n              38.5\n            ],\n            [\n              -111.25,\n              38.5\n            ],\n            [\n              -111.25,\n              38.37317\n            ],\n            [\n              -111.1296,\n              38.37317\n            ],\n            [\n              -111.1296,\n              38.25\n            ],\n            [\n              -111,\n              38.25\n            ],\n            [\n              -111,\n              38\n            ],\n            [\n              -111.5,\n              38\n            ],\n            [\n              -111.5,\n              38.1167\n            ],\n            [\n              -111.625,\n              38.1167\n            ],\n            [\n              -111.625,\n              38.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publicComments":"Prepared on behalf of the U.S. Atomic Energy Commission.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683207","contributors":{"authors":[{"text":"Smith, J. Fred Jr.","contributorId":106482,"corporation":false,"usgs":true,"family":"Smith","given":"J.","suffix":"Jr.","email":"","middleInitial":"Fred","affiliations":[],"preferred":false,"id":152702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huff, Lyman C.","contributorId":47440,"corporation":false,"usgs":true,"family":"Huff","given":"Lyman","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":152699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hinrichs, E. Neal","contributorId":46488,"corporation":false,"usgs":true,"family":"Hinrichs","given":"E.","email":"","middleInitial":"Neal","affiliations":[],"preferred":false,"id":152701,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Luedke, Robert G.","contributorId":18339,"corporation":false,"usgs":true,"family":"Luedke","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":152700,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":6460,"text":"pp414E - 1963 - Algebraic and graphic methods for evaluating discordant lead-isotope ages","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"pp414E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"414","chapter":"E","title":"Algebraic and graphic methods for evaluating discordant lead-isotope ages","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp414E","usgsCitation":"Stieff, L.R., Stern, T.W., and Eicher, R.N., 1963, Algebraic and graphic methods for evaluating discordant lead-isotope ages: U.S. Geological Survey Professional Paper 414, p. E1-E27, https://doi.org/10.3133/pp414E.","productDescription":"p. E1-E27","costCenters":[],"links":[{"id":121978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0414e/report-thumb.jpg"},{"id":33878,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0414e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6880bf","contributors":{"authors":[{"text":"Stieff, Lorin Rollins","contributorId":46509,"corporation":false,"usgs":true,"family":"Stieff","given":"Lorin","email":"","middleInitial":"Rollins","affiliations":[],"preferred":false,"id":152762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stern, T. W.","contributorId":36122,"corporation":false,"usgs":true,"family":"Stern","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":152761,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eicher, Ralph Newton","contributorId":9648,"corporation":false,"usgs":true,"family":"Eicher","given":"Ralph","email":"","middleInitial":"Newton","affiliations":[],"preferred":false,"id":152760,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":52340,"text":"ofr6373 - 1963 - A brief summary of ground water in the Furnace Creek Wash area, Death Valley National Monument, California","interactions":[{"subject":{"id":52340,"text":"ofr6373 - 1963 - A brief summary of ground water in the Furnace Creek Wash area, Death Valley National Monument, California","indexId":"ofr6373","publicationYear":"1963","noYear":false,"title":"A brief summary of ground water in the Furnace Creek Wash area, Death Valley National Monument, California"},"predicate":"SUPERSEDED_BY","object":{"id":2508,"text":"wsp1779Y - 1964 - A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California","indexId":"wsp1779Y","publicationYear":"1964","noYear":false,"chapter":"Y","title":"A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California"},"id":1}],"supersededBy":{"id":2508,"text":"wsp1779Y - 1964 - A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California","indexId":"wsp1779Y","publicationYear":"1964","noYear":false,"title":"A brief geologic and hydrologic reconnaissance of the Furnace Creek Wash area, Death Valley National Monument, California"},"lastModifiedDate":"2012-02-02T00:11:32","indexId":"ofr6373","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-73","title":"A brief summary of ground water in the Furnace Creek Wash area, Death Valley National Monument, California","language":"ENGLISH","doi":"10.3133/ofr6373","usgsCitation":"Kunkel, F., 1963, A brief summary of ground water in the Furnace Creek Wash area, Death Valley National Monument, California: U.S. Geological Survey Open-File Report 63-73, 7 p., https://doi.org/10.3133/ofr6373.","productDescription":"7 p.","costCenters":[],"links":[{"id":178909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd497be4b0b290850ef389","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":245185,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6477,"text":"pp378A - 1963 - Geology and ore deposits of the South Silverton mining area, San Juan County, Colorado","interactions":[],"lastModifiedDate":"2025-09-22T18:08:00.677768","indexId":"pp378A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"378","chapter":"A","title":"Geology and ore deposits of the South Silverton mining area, San Juan County, Colorado","docAbstract":"<p>The South Silverton mining area is immediately southeast of the town of Silverton, San Juan County, in southwestern Colorado (fig. 1). The town of&nbsp;Silverton itself lies in a relatively flat and open reach of the Animas Valley, called Bakers Park, in the western part of the San Juan Mountains. (See figs. 2 and 8.) The roughly circular area of the geologic map map (pl. 1) includes about 18½ square miles of the mountainous country southeast of Silverton. It is bounded on the west and north by the Animas River, on the east by Cunningham Creek, and on the south by Mountaineer Creek and Deer Park Creek. Altitudes range from 9,125 feet above sea level in the canyon of the Animas, at the southwest corner of the area, to 13,451 feet on Kendall Peak, 2¾ miles to the northeast.</p><p>Within this area nearly a dozen horn-like peaks and sharp ridges separated by deep glacial cirques rise to altitudes of 13,000 feet or more. (See figs. 3, 7, 10, and 24.) Exposures are excellent along the crests and upper flanks of the ridges, but the bedrock along the lower parts of the valley walls and floors of the cirques is largely concealed by accumulations of talus. The timbered slopes along the south side of the Animas Valley are extensively covered with glacial moraine. Several of the high basins within the cirques hold ponds or small lakes; the largest is Silver Lake (fig. 23).</p><p>Roads skirt the northern and eastern edges of the area but none give good access into the interior. Silverton is adjacent to U.S. Highway 550, which passes over the mountains by way of Red Mountain Pass from Ouray, 24 miles to the north, to Durango, 53 miles to the south. The community is also served by the narrow-gage line of the Denver and Rio Grande Western Railroad that follows the Animas River upstream from Durango. A gravel road, State Highway 110, follows the Animas River upstream, eastward from Silverton. From this highway a side road branches off to Cunningham Gulch as far as the Highland Mary mill, and another goes up Arrastra Gulch for about 2 miles. The higher ridges east of Arrastra Basin are most easily reached by way of the Shenandoah-Dives aerial tram and mine workings. A few trails suitable for horses lead from the main valleys into the larger basins and across the intervening ridges, but much of the area is accessible only on foot. Most of the cirque heads and many of the high cliffs along Cunningham Gulch could not be examined at close range. Timberline is at about 11,500 feet.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp378A","collaboration":"Prepared in cooperation with the Colorado Metal Mining Fund and the Colorado Geological Survey Board","usgsCitation":"Varnes, D., 1963, Geology and ore deposits of the South Silverton mining area, San Juan County, Colorado: U.S. Geological Survey Professional Paper 378, Report: iv, 56 p.; 6 Plates: 40.18 x 45.27 inches or smaller, https://doi.org/10.3133/pp378A.","productDescription":"Report: iv, 56 p.; 6 Plates: 40.18 x 45.27 inches or smaller","costCenters":[],"links":[{"id":272571,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0378a/plate-4.pdf","text":"Plate 4","size":"1.10 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 4"},{"id":271118,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0378a/plate-7.pdf","text":"Plate 7","size":"3.32 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 7"},{"id":271117,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0378a/plate-2.pdf","text":"Plate 2","size":"1.13 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":271116,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0378a/plate-1.pdf","text":"Plate 1","size":"4.42 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":272572,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0378a/plate-5.pdf","text":"Plate 5","size":"3.35 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 5"},{"id":276480,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0378a/plate-3.pdf","text":"Plate 3","size":"2.35 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":140316,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":495855,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4376.htm","linkFileType":{"id":5,"text":"html"}},{"id":340316,"rank":9,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0378a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":272573,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0378a/plate-6.pdf","text":"Plate 6","size":"2.02 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 6"}],"country":"United States","state":"Colorado","county":"San Juan County","otherGeospatial":"South Silverton Mining Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.97,37.64 ], [ -107.97,37.96 ], [ -107.46,37.96 ], [ -107.46,37.64 ], [ -107.97,37.64 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b2fe4b07f02db6b406c","contributors":{"authors":[{"text":"Varnes, David J.","contributorId":86322,"corporation":false,"usgs":true,"family":"Varnes","given":"David J.","affiliations":[],"preferred":false,"id":152790,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52364,"text":"ofr63118 - 1963 - Transport and dispersion of labeled bed material, North Loup River, Nebraska","interactions":[{"subject":{"id":52364,"text":"ofr63118 - 1963 - Transport and dispersion of labeled bed material, North Loup River, Nebraska","indexId":"ofr63118","publicationYear":"1963","noYear":false,"title":"Transport and dispersion of labeled bed material, North Loup River, Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":38976,"text":"pp433C - 1965 - Transport and dispersion of labeled bed material, North Loup River, Nebraska","indexId":"pp433C","publicationYear":"1965","noYear":false,"chapter":"C","title":"Transport and dispersion of labeled bed material, North Loup River, Nebraska"},"id":1}],"supersededBy":{"id":38976,"text":"pp433C - 1965 - Transport and dispersion of labeled bed material, North Loup River, Nebraska","indexId":"pp433C","publicationYear":"1965","noYear":false,"title":"Transport and dispersion of labeled bed material, North Loup River, Nebraska"},"lastModifiedDate":"2012-02-02T00:11:32","indexId":"ofr63118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-118","title":"Transport and dispersion of labeled bed material, North Loup River, Nebraska","language":"ENGLISH","doi":"10.3133/ofr63118","usgsCitation":"Sayre, W., and Hubbell, D.W., 1963, Transport and dispersion of labeled bed material, North Loup River, Nebraska: U.S. Geological Survey Open-File Report 63-118, 69 p., https://doi.org/10.3133/ofr63118.","productDescription":"69 p.","costCenters":[],"links":[{"id":178146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626c68","contributors":{"authors":[{"text":"Sayre, W.W.","contributorId":12899,"corporation":false,"usgs":true,"family":"Sayre","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":245223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubbell, D. W.","contributorId":15997,"corporation":false,"usgs":true,"family":"Hubbell","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":245224,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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