Regression analysis of chemical and physical data collected on Beech Creek resulted in two curves that relate the concentration of free hydrogen ion to the electrical specific conductance of the water. These curves provide a means of estimating, through use of data telemetered from a water-quality monitor on Beech Creek, the acid load in the stream at any time. These estimates of acid loads in Beech Creek will enable the operators of Foster Joseph Sayers Dam on Bald Eagle Creek to release sufficient alkaline water from the reservoir to prevent fish kills in lower Bald Eagle Creek that could be caused by the acid from Beech Creek.
The acid content of the West Branch Susquehanna River upstream from the city of Lock Haven usually exceeds the amount that can be neutralized by Bald Eagle Creek. However, inasmuch as the alkaline content of 13ald Eagle Creek exceeds the amount required to effectively neutralize the acidity of Beech Creek, some water may be conserved in the reservoir for the purpose of improving the quality of the West Branch when the river is unusually acid.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/ofr71108","usgsCitation":"Flippo, H.N., 1971, Acidity control in Bald Eagle Creek and West Branch Susquehanna River, Clinton County, Pennsylvania: U.S. Geological Survey Open-File Report 71-108, 28 p., https://doi.org/10.3133/ofr71108.","productDescription":"28 p.","numberOfPages":"36","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":161552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr71108.PNG"},{"id":330290,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0108/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","county":"Clinton County","otherGeospatial":"Bald Eagle Creek, Susquehanna River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.79693603515625,\n 40.947750930283476\n ],\n [\n -77.79693603515625,\n 41.366502866327224\n ],\n [\n -77.36846923828125,\n 41.366502866327224\n ],\n [\n -77.36846923828125,\n 40.947750930283476\n ],\n [\n -77.79693603515625,\n 40.947750930283476\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69e1f7","contributors":{"authors":[{"text":"Flippo, Herbert N. Jr.","contributorId":36597,"corporation":false,"usgs":true,"family":"Flippo","given":"Herbert","suffix":"Jr.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":236538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47914,"text":"ofr7112 - 1971 - Water chemistry of the Santa Clara Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"ofr7112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-12","title":"Water chemistry of the Santa Clara Valley, California","language":"ENGLISH","doi":"10.3133/ofr7112","usgsCitation":"Averett, R., Wood, P., and Muir, K.S., 1971, Water chemistry of the Santa Clara Valley, California: U.S. Geological Survey Open-File Report 71-12, 24 p. ; 27 cm. + 1 folded map in pocket, https://doi.org/10.3133/ofr7112.","productDescription":"24 p. ; 27 cm. + 1 folded map in pocket","costCenters":[],"links":[{"id":162829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa289","contributors":{"authors":[{"text":"Averett, R. C.","contributorId":35709,"corporation":false,"usgs":true,"family":"Averett","given":"R. C.","affiliations":[],"preferred":false,"id":236512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, P.R.","contributorId":102068,"corporation":false,"usgs":true,"family":"Wood","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":236514,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Muir, K. S.","contributorId":53764,"corporation":false,"usgs":true,"family":"Muir","given":"K.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":236513,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23366,"text":"ofr72166 - 1971 - Water-level changes 1964-71, northern High Plains of Colorado","interactions":[],"lastModifiedDate":"2018-01-09T16:34:55","indexId":"ofr72166","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"72-166","title":"Water-level changes 1964-71, northern High Plains of Colorado","docAbstract":"Ground-water withdrawals for irrigation increased from about 84,000 acre-feet to 430,000 acre-feet per year between 1960 and 1970 in the northern High Plains of Colorado, causing significant water-level declines in areas where high-capacity wells are concentrated. The number of wells increased from about 500 in 1960 to 2,560 in 1970. In 1968 the U.S. Geological Survey began a study in cooperation with the Colorado Water Conservation Board; the Colorado Division of Water Resources, Office of the State Engineer; and the Management Districts of the northern High Plains to provide information for administration and management of the vital ground-water reserves of the northern High Plains.
The northern High Plains of Colorado is formed from an erosional remanent of the Ogallala Formation of Pliocene Age that extends from the South Platte River on the north to the Arkansas River on the south, and from Limon, Colo. on the west across the Colorado State line on the east (fig. 1). This area includes all or part of 11 counties and contains about 9,500 square miles. General information describing the ground-water resources of the northern High Plains of Colorado is presented in table 1. Plate 1 shows the net changes in water level between 1964 and 1971. Other published water-level change maps are for the period from 1964-68 and 1964-69 (Boettcher and others, 1969). The map (pl. 1) is based on annual water-level measurements made in 1964 and 1971 in about 300 wells tapping the Ogallala aquifer. Areas with either a net decline or a net rise are shown. Large declines recorded near Yuma and Burlington correspond to relatively high concentrations (2 per sq mi) of high-capacity wells. Also included in this report are 11 hydrographs typical of the water-level changes during this period (figs. 2-4). The hydrographs show water-level changes from 1964, or as early as 1956 to 1971, and illustrate the consistency of water-level change rates. Because proper management of ground-water resources requires systematic and valid basic data, the annual water-level measurements should continue.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72166","issn":"0094-9140","usgsCitation":"Hofstra, W.E., Klein, J.M., and Major, T.J., 1971, Water-level changes 1964-71, northern High Plains of Colorado: U.S. Geological Survey Open-File Report 72-166, Report: i, 10 p.; Plate: 13.58 x 27.32 inches, https://doi.org/10.3133/ofr72166.","productDescription":"Report: i, 10 p.; Plate: 13.58 x 27.32 inches","numberOfPages":"14","costCenters":[],"links":[{"id":156735,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":52656,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0166/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.85,\n 38\n ],\n [\n -102,\n 38\n ],\n [\n -102,\n 41\n ],\n [\n -103.85,\n 41\n ],\n [\n -103.85,\n 38\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7835","contributors":{"authors":[{"text":"Hofstra, Warren E.","contributorId":75618,"corporation":false,"usgs":true,"family":"Hofstra","given":"Warren","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":189984,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klein, John M.","contributorId":27036,"corporation":false,"usgs":true,"family":"Klein","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":189985,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Major, Thomas J.","contributorId":32529,"corporation":false,"usgs":true,"family":"Major","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":189983,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23865,"text":"ofr71200 - 1971 - Water quality at the Dade-Collier Training and Transition Airport, Miami International Airport, and Cottonmouth Camp-Everglades National Park, Florida, November 1969","interactions":[],"lastModifiedDate":"2012-02-02T00:08:07","indexId":"ofr71200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-200","title":"Water quality at the Dade-Collier Training and Transition Airport, Miami International Airport, and Cottonmouth Camp-Everglades National Park, Florida, November 1969","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Water Resources Division,","doi":"10.3133/ofr71200","issn":"0094-9140","usgsCitation":"McPherson, B.F., 1971, Water quality at the Dade-Collier Training and Transition Airport, Miami International Airport, and Cottonmouth Camp-Everglades National Park, Florida, November 1969: U.S. Geological Survey Open-File Report 71-200, 29 p. :2 maps ;27 cm., https://doi.org/10.3133/ofr71200.","productDescription":"29 p. :2 maps ;27 cm.","costCenters":[],"links":[{"id":156404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9b43","contributors":{"authors":[{"text":"McPherson, B. F.","contributorId":62983,"corporation":false,"usgs":true,"family":"McPherson","given":"B.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":190880,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4321,"text":"cir665 - 1971 - Index of surface-water records to September 30, 1970; Part 15, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir665","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"665","title":"Index of surface-water records to September 30, 1970; Part 15, Alaska","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir665","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Index of surface-water records to September 30, 1970; Part 15, Alaska: U.S. Geological Survey Circular 665, 21 p. :ill. ;27 cm., https://doi.org/10.3133/cir665.","productDescription":"21 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":120770,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1971/0665/report-thumb.jpg"},{"id":31431,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1971/0665/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2be0","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":528183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4323,"text":"cir651 - 1971 - Index of surface-water records to September 30, 1970; Part 1, North Atlantic slope basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir651","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"651","title":"Index of surface-water records to September 30, 1970; Part 1, North Atlantic slope basins","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir651","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Index of surface-water records to September 30, 1970; Part 1, North Atlantic slope basins: U.S. Geological Survey Circular 651, 89 p. ;27 cm., https://doi.org/10.3133/cir651.","productDescription":"89 p. ;27 cm.","costCenters":[],"links":[{"id":117107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1971/0651/report-thumb.jpg"},{"id":31433,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1971/0651/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2cbe","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":528185,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4325,"text":"cir653 - 1971 - Index of surface-water records to September 30, 1970; Part 3, Ohio River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir653","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"653","title":"Index of surface-water records to September 30, 1970; Part 3, Ohio River basin","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir653","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Index of surface-water records to September 30, 1970; Part 3, Ohio River basin: U.S. Geological Survey Circular 653, 71 p. ;28 cm., https://doi.org/10.3133/cir653.","productDescription":"71 p. ;28 cm.","costCenters":[],"links":[{"id":120771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1971/0653/report-thumb.jpg"},{"id":31435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1971/0653/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2b57","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":528187,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4327,"text":"cir655 - 1971 - Index of surface-water records to September 30, 1970; Part 5, Hudson Bay and Upper Mississippi River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir655","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"655","title":"Index of surface-water records to September 30, 1970; Part 5, Hudson Bay and Upper Mississippi River basins","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir655","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Index of surface-water records to September 30, 1970; Part 5, Hudson Bay and Upper Mississippi River basins: U.S. Geological Survey Circular 655, 65 p. :ill ;27 cm., https://doi.org/10.3133/cir655.","productDescription":"65 p. :ill ;27 cm.","costCenters":[],"links":[{"id":117110,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1971/0655/report-thumb.jpg"},{"id":31437,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1971/0655/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2bc8","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":528189,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23396,"text":"ofr72169 - 1971 - Geology, hydrology, and water quality of the Tracy-Dos Palos area, San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2017-04-14T09:09:16","indexId":"ofr72169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"72-169","title":"Geology, hydrology, and water quality of the Tracy-Dos Palos area, San Joaquin Valley, California","docAbstract":"The Tracy-Dos Palos area includes about 1,800 square miles on the northwest side of the San Joaquin Valley. The Tulare Formation of Pliocene and Pleistocene age, terrace deposits of Pleistocene age, and alluvium and flood-basin deposits of Pleistocene and Holocene age constitute the fresh ground-water reservoir Pre-Tertiary and Tertiary sedimentary and crystalline rocks, undifferentiated, underlie the valley and yield saline water.
Hydrologically most important, the Tulare Formation is divided into a lower water-bearing zone confined by the Corcoran Clay Member and an upper zone that is confined, semiconfined, and unconfined in different parts of the area. Alluvium and flood-basin deposits are included in the upper zone. Surficial alluvium and flood-basin deposits contain a shallow water-bearing zone. Lower zone wells were flowing in 1908, but subsequent irrigation development caused head declines and land subsidence. Overdraft in both zones ended in 1951 with import of surface water.
Bicarbonate water flows into the area from the Sierra Nevada and Diablo Range. Diablo Range water is higher in sulfate, chloride, and dissolved solids. Upper zone water averages between 400 and 1,200 mg/l (milligrams per liter) dissolved solids and water hardness generally exceeds 180 mg/l as calcium carbonate. Nitrate, fluoride, iron, and boron occur in excessive concentrations in water from some wells. Dissolved constituents in lower zone water generally are sodium chloride and sodium sulfate with higher dissolved solids concentration than water from the upper zone.
The foothills of the Diablo Range provide favorable conditions for artificial recharge, but shallow water problems plague about 50 percent of the area and artificial recharge is undesirable at this time.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72169","issn":"0094-9140","usgsCitation":"Hotchkiss, W.R., and Balding, G., 1971, Geology, hydrology, and water quality of the Tracy-Dos Palos area, San Joaquin Valley, California: U.S. Geological Survey Open-File Report 72-169, Report: viii, 107 p.; 3 Plates: 33.24 x 31.14 inches or smaller, https://doi.org/10.3133/ofr72169.","productDescription":"Report: viii, 107 p.; 3 Plates: 33.24 x 31.14 inches or smaller","costCenters":[],"links":[{"id":156308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0169/report-thumb.jpg"},{"id":52697,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0169/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52698,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0169/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52699,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0169/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52700,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0169/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c64e","contributors":{"authors":[{"text":"Hotchkiss, W. R.","contributorId":61820,"corporation":false,"usgs":true,"family":"Hotchkiss","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":190037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Balding, G. O.","contributorId":87135,"corporation":false,"usgs":true,"family":"Balding","given":"G. 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Buckhorn area, Nevada","linkFileType":{"id":5,"text":"html"}},{"id":494595,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31127.htm","text":"Summary of mineralogic and lithologic characteristics of Tertiary sedimentary rocks in the middle Rocky Mountains and the northern Great Plains","linkFileType":{"id":5,"text":"html"}},{"id":494594,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31126.htm","text":"Clay minerals, Longfellow Mine, San Juan County, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":494593,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31125.htm","text":"Clinoptilolite-bearing tuff beds in the Creede Formation, San Juan Mountains, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":494592,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31124.htm","text":"Sequence of glaciation in the Mesabi - Vermilion Iron Range area, northeastern Minnesota","linkFileType":{"id":5,"text":"html"}},{"id":494591,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31123.htm","text":"Ordovician - Silurian boundary in the York Mountains, western Seward Peninsula, Alaska","linkFileType":{"id":5,"text":"html"}},{"id":494590,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31122.htm","text":"Eocene (Refugian) nannoplankton in the Church Creek Formation near Monterey, central California","linkFileType":{"id":5,"text":"html"}},{"id":494589,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31121.htm","text":"Potential strippable oil-shale resources of the Mahogany zone (Eocene), Cathedral Bluffs area, northwestern Colorado","linkFileType":{"id":5,"text":"html"}},{"id":494588,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31120.htm","text":"Zirconium on the continental shelf - possible indicator of ancient shoreline deposition","linkFileType":{"id":5,"text":"html"}},{"id":65504,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0750c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120101,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0750c/report-thumb.jpg"},{"id":421292,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31119.htm","text":"Grain-size distribution and the depositional history of northern Padre Island, Texas","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687735","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":529872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2851,"text":"wsp1999F - 1971 - Prospects for developing stock - Water supplies from wells in northeastern Garfield County, Montana","interactions":[],"lastModifiedDate":"2022-12-02T21:22:05.132364","indexId":"wsp1999F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1999","chapter":"F","title":"Prospects for developing stock - Water supplies from wells in northeastern Garfield County, Montana","docAbstract":"Ground-water resources in northeastern Garfield County, Mont., afford a practical and reliable source of stock water on the intermingled public and private grazing lands that together comprise an area of about 1,200 square miles. The oldest formation exposed in the area is the relatively thick and impermeable Bearpaw Shale of Cretaceous .age. Overlying the Bearpaw Shale in succession are the Fox Hills Sandstone and Hell Creek Formation of Cretaceous age, the Fort Union Formation of Tertiary age, and thin glacial deposits .and alluvium of Quaternary age. All but the Bearpaw Shale and the glacial deposits are potential aquifers. Published geologic maps were found to be satisfactory after fitting contacts to the topographic base. Mapping, therefore, was limited mainly to outlining on aerial photographs the alluvial deposits in the stream valleys. \r\n\r\nThe major structural feature is the Blood Creek syncline, the axis of which plunges eastward 10-15 feet per mile across the southern part of the area. Beds generally dip 15-25 feet per mile toward the synclinal axis. Water in bedrock aquifers is under artesian pressure, .and most wells in Big and Little Dry Creek valleys flow at the land surface. \r\n\r\nThe only bedrock aquifer having appreciable areal extent is a sandstone 30-70 feet thick that has been mapped by previous investigators as the upper part of the Fox Hills Sandstone. This aquifer crops out in the northern and northwestern parts of the area and dips about 20 feet per mile southeastward beneath younger beds. Most wells in the northern half of the area obtain water from this sandstone at drilling depths of less than 200 feet. \r\n\r\nThe depth to the Fox Hills Sandstone increases progressively southward, and most wells south of Woody Creek obtain water from irregularly distributed sandstone beds and lenses in the overlying Hell Creek and Fort Union Formations. The depth at which water may be obtained from these beds is not accurately predictable, but the depth seldom exceeds 300 feet. \r\n\r\nThe results of the investigation indicate that the prospects for obtaining ample water for livestock from wells drilled into the bedrock formations are very favorable in most of the area. The average depth of bedrock wells in the area is 195 feet. \r\n\r\nUnderflow in the alluvial deposits along all the larger stream valleys also affords a practical source of stock water. \r\n\r\nChemical analyses of samples collected at 43 wells and three springs show the water quality to be generally poor. Water from bedrock aquifer contains 530-5,340 milligrams per liter total dissolved solids, whereas water from alluvium contains less than 1,500 milligrams per liter total dissolved solids. The predominant constituents are sodium, bicarbonate, and sulfate. So far as could be determined, all water supplies in the area are suitable for livestock.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1999F","usgsCitation":"Van Lewen, M.C., and King, N.J., 1971, Prospects for developing stock - Water supplies from wells in northeastern Garfield County, Montana: U.S. Geological Survey Water Supply Paper 1999, Report; iv, 38 p.; 1 Plate: 22.00 × 33.60 inches, https://doi.org/10.3133/wsp1999F.","productDescription":"Report; iv, 38 p.; 1 Plate: 22.00 × 33.60 inches","costCenters":[],"links":[{"id":410017,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25490.htm","linkFileType":{"id":5,"text":"html"}},{"id":29440,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1999f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29439,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139068,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1999f/report-thumb.jpg"}],"country":"United States","state":"Montana","county":"Garfield County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -106.17,\n 47.941\n ],\n [\n -107.012,\n 47.941\n ],\n [\n -107.012,\n 47.151\n ],\n [\n -106.17,\n 47.151\n ],\n [\n -106.17,\n 47.941\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a92e4b07f02db657bdb","contributors":{"authors":[{"text":"Van Lewen, M. 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The reach consists principally of lake surface, which results in large amounts of flood-storage volume. The regional-flood profile ranges from 1.7 feet to 3.1 feet above normal low-water elevation.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72168","usgsCitation":"Holmstrom, B.K., and Lawrence, C.L., 1971, Floods on Yahara River, Lake Mendota to Lake Kegonsa, Dane County, Wisconsin, 1971: U.S. Geological Survey Open-File Report 72-168, Report: 6p.; 6 Plates: 22.91 x 30.24 inches or smaller, https://doi.org/10.3133/ofr72168.","productDescription":"Report: 6p.; 6 Plates: 22.91 x 30.24 inches or smaller","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":99866,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0168/report.pdf","size":"1033","linkFileType":{"id":1,"text":"pdf"}},{"id":99867,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0168/plate-1.pdf","size":"11272","linkFileType":{"id":1,"text":"pdf"}},{"id":99868,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0168/plate-2.pdf","size":"2712","linkFileType":{"id":1,"text":"pdf"}},{"id":99869,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0168/plate-3.pdf","size":"5707","linkFileType":{"id":1,"text":"pdf"}},{"id":99870,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0168/plate-4.pdf","size":"6185","linkFileType":{"id":1,"text":"pdf"}},{"id":99871,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0168/plate-5.pdf","size":"5814","linkFileType":{"id":1,"text":"pdf"}},{"id":99872,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0168/plate-6.pdf","size":"2946","linkFileType":{"id":1,"text":"pdf"}},{"id":135233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0168/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Dane County","otherGeospatial":"Lake Kegonsa, Lake Mendota, Yahara River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.3792724609375,\n 43.21068107507132\n ],\n [\n -89.54750061035156,\n 43.08543891099317\n ],\n [\n -89.34013366699219,\n 42.93179328323594\n ],\n [\n -89.20898437499999,\n 42.867912483915305\n ],\n [\n -89.17053222656249,\n 42.90866300062528\n ],\n [\n -89.15199279785156,\n 42.979032509768984\n ],\n [\n -89.1375732421875,\n 43.025733503088\n ],\n [\n -89.3792724609375,\n 43.21068107507132\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df7a8","contributors":{"authors":[{"text":"Holmstrom, Barry K.","contributorId":80644,"corporation":false,"usgs":true,"family":"Holmstrom","given":"Barry","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":234794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lawrence, Carl L.","contributorId":57435,"corporation":false,"usgs":true,"family":"Lawrence","given":"Carl","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":234793,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38669,"text":"pp750A - 1971 - Geological Survey research 1971, Chapter A","interactions":[],"lastModifiedDate":"2012-02-02T00:10:00","indexId":"pp750A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"750","chapter":"A","title":"Geological Survey research 1971, Chapter A","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1971","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp750A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Geological Survey research 1971, Chapter A: U.S. Geological Survey Professional Paper 750, 417 p., https://doi.org/10.3133/pp750A.","productDescription":"417 p.","costCenters":[],"links":[{"id":120099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0750a/report-thumb.jpg"},{"id":65502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0750a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db68772a","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":529870,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46577,"text":"ofr71321 - 1971 - Map showing the altitude and configuration of the water level in the \"shallow aquifer,\" January 1969, Roswell basin, Chaves and Eddy Counties, New Mexico","interactions":[],"lastModifiedDate":"2022-12-12T20:58:22.339853","indexId":"ofr71321","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-321","title":"Map showing the altitude and configuration of the water level in the \"shallow aquifer,\" January 1969, Roswell basin, Chaves and Eddy Counties, New Mexico","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71321","usgsCitation":"Welder, G.E., 1971, Map showing the altitude and configuration of the water level in the \"shallow aquifer,\" January 1969, Roswell basin, Chaves and Eddy Counties, New Mexico: U.S. Geological Survey Open-File Report 71-321, Report: 1 p.; 1 Plate: 26.14 × 52.93 inches, https://doi.org/10.3133/ofr71321.","productDescription":"Report: 1 p.; 1 Plate: 26.14 × 52.93 inches","costCenters":[],"links":[{"id":410313,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8644.htm","linkFileType":{"id":5,"text":"html"}},{"id":172782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0321/report-thumb.jpg"},{"id":99750,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0321/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":99751,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0321/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","county":"Chaves County, Eddy County","otherGeospatial":"Roswell basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -104.518,\n 33.5\n ],\n [\n -104.518,\n 32.547\n ],\n [\n -104.248,\n 32.547\n ],\n [\n -104.248,\n 33.5\n ],\n [\n -104.518,\n 33.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db6447ea","contributors":{"authors":[{"text":"Welder, G. E.","contributorId":100814,"corporation":false,"usgs":true,"family":"Welder","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":233595,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":58071,"text":"wdrCO692 - 1971 - Water Resources Data for Colorado, 1969; Part 2. Water Quality Records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:14","indexId":"wdrCO692","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CO-69-2","title":"Water Resources Data for Colorado, 1969; Part 2. Water Quality Records","language":"ENGLISH","doi":"10.3133/wdrCO692","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Water Resources Data for Colorado, 1969; Part 2. Water Quality Records: U.S. Geological Survey Water Data Report CO-69-2, 89 p., https://doi.org/10.3133/wdrCO692.","productDescription":"89 p.","costCenters":[],"links":[{"id":185419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1969/co-69-2/report-thumb.jpg"},{"id":88311,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1969/co-69-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd108","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":533195,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68423,"text":"ha364 - 1971 - Water-resources reconnaissance of a part of the Matanuska-Susitna Borough, Alaska","interactions":[],"lastModifiedDate":"2023-03-20T19:23:51.15645","indexId":"ha364","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"364","title":"Water-resources reconnaissance of a part of the Matanuska-Susitna Borough, Alaska","docAbstract":"No abstract available.
","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ha364","usgsCitation":"Feulner, A.J., 1971, Water-resources reconnaissance of a part of the Matanuska-Susitna Borough, Alaska: U.S. Geological Survey Hydrologic Atlas 364, 1 Plate: 44.50 x 31.00 inches, https://doi.org/10.3133/ha364.","productDescription":"1 Plate: 44.50 x 31.00 inches","costCenters":[],"links":[{"id":186610,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414373,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15742.htm","linkFileType":{"id":5,"text":"html"}},{"id":89949,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/364/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Matanuska-Susitna Borough","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -150.75,\n 61.167\n ],\n [\n -150.75,\n 62.417\n ],\n [\n -148.875,\n 62.417\n ],\n [\n -148.875,\n 61.167\n ],\n [\n -150.75,\n 61.167\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4dc5","contributors":{"authors":[{"text":"Feulner, Alvin J.","contributorId":49775,"corporation":false,"usgs":true,"family":"Feulner","given":"Alvin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278190,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68444,"text":"ha357 - 1971 - Hydrogeology of the Pine Ridge Indian Reservation, South Dakota","interactions":[],"lastModifiedDate":"2017-10-15T12:38:32","indexId":"ha357","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"357","title":"Hydrogeology of the Pine Ridge Indian Reservation, South Dakota","docAbstract":"An investigation of the geology and ground-water resources of the Pine Ridge Indian Reservation, South Dakota, was made at the request of the Bureau of Indian Affairs as part of the U.S. Department of the Interior's program for the development of the Missouri River basin. The area of investigation (about 3,930 square miles) includes all the land within the original boundaries of the Reservation, except for that part of Bennett County south of the U.S. Highway 18, where there are only small tracts of Indian land.
\nEmphasis in the study was placed on mapping major rock units and on determining their potential as sources of water for domestic and stock use. The geologic map on sheet 1 shows the areal extent of the major rock units, and a summary of the stratigraphy and physical characteristics of the exposed geologic formations is given in the table on this sheet.
\nThe writers appreciate the cooperation of the personnel of the South Dakota State Geological Survey, who provided most of the well data for Bennett County, information about the stratigraphy and geology of selected areas, and copies of published and unpublished geologic maps. (See map showing areas mapped prior to this investigation.) Also, they appreciate the cooperation of ranch owners and tenants, who permitted access to their lands, and the personnel of the Bureau of Indian affairs, who supplied soils mps and other data.
\nData on which this report is based, including logs of wells and test holes, chemical analyses of water and records of wells and springs, have been summarized by the authors in a basic-data report published jointly by the South Dakota Geological Survey and South Dakota Water Resources Commission (Water Resources Report 4, Basic hydrogeologic data - Pine Ridge Indian Reservation, South Dakota). A selected bibliography of reports pertaining to the geology of the area has been included in the basic-data report. This atlas will be more useful if studied in conjunction with a copy of the basic-data report.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha357","usgsCitation":"Ellis, M.J., and Adolphson, D.G., 1971, Hydrogeology of the Pine Ridge Indian Reservation, South Dakota: U.S. Geological Survey Hydrologic Atlas 357, 2 Plates: 54.25 x 33.00 inches and 35.50 x 32.00 inches, https://doi.org/10.3133/ha357.","productDescription":"2 Plates: 54.25 x 33.00 inches and 35.50 x 32.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":186220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha357.PNG"},{"id":89975,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/357/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89974,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/357/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","country":"United States","state":"South Dakota","otherGeospatial":"Pine Ridge Indian Reservation","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103,43 ], [ -103,43.75 ], [ -101.25,43.75 ], [ -101.25,43 ], [ -103,43 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db615063","contributors":{"authors":[{"text":"Ellis, M. J.","contributorId":27840,"corporation":false,"usgs":true,"family":"Ellis","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278230,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}