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,{"id":68085,"text":"ha337 - 1969 - Ground-water favorability areas and surficial geology of the lower Kennebec River basin, Maine","interactions":[],"lastModifiedDate":"2022-04-13T18:35:50.587891","indexId":"ha337","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"337","title":"Ground-water favorability areas and surficial geology of the lower Kennebec River basin, Maine","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha337","usgsCitation":"Prescott, G., 1969, Ground-water favorability areas and surficial geology of the lower Kennebec River basin, Maine: U.S. Geological Survey Hydrologic Atlas 337, 2 Plates: 37.50 × 57.00 inches and 8.00 × 10.50 inches, https://doi.org/10.3133/ha337.","productDescription":"2 Plates: 37.50 × 57.00 inches and 8.00 × 10.50 inches","costCenters":[],"links":[{"id":189800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89346,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/337/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89345,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/337/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398652,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15712.htm"}],"scale":"62500","country":"United States","state":"Maine","otherGeospatial":"lower Kennebec River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.078,\n              43.929\n            ],\n            [\n              -69.5,\n              43.929\n            ],\n            [\n              -69.5,\n              44.674\n            ],\n            [\n              -70.078,\n              44.674\n            ],\n            [\n              -70.078,\n              43.929\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649777","contributors":{"authors":[{"text":"Prescott, Glenn C.","contributorId":38126,"corporation":false,"usgs":true,"family":"Prescott","given":"Glenn C.","affiliations":[],"preferred":false,"id":277617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67091,"text":"i597 - 1969 - Geologic map of the Southwest and Southeast Pueblo quadrangles, Colorado","interactions":[],"lastModifiedDate":"2020-07-20T14:34:00.902019","indexId":"i597","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"597","title":"Geologic map of the Southwest and Southeast Pueblo quadrangles, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i597","usgsCitation":"Scott, G., 1969, Geologic map of the Southwest and Southeast Pueblo quadrangles, Colorado: U.S. Geological Survey IMAP 597, HTML Document, https://doi.org/10.3133/i597.","productDescription":"HTML Document","costCenters":[],"links":[{"id":187574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":106860,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9393.htm","linkFileType":{"id":5,"text":"html"},"description":"9393"}],"scale":"24000","country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.75,38.1175 ], [ -104.75,38.25 ], [ -104.5,38.25 ], [ -104.5,38.1175 ], [ -104.75,38.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b21c","contributors":{"authors":[{"text":"Scott, Glenn R.","contributorId":33324,"corporation":false,"usgs":true,"family":"Scott","given":"Glenn R.","affiliations":[],"preferred":false,"id":275587,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67010,"text":"i572 - 1969 - Geologic map of the Teller B-4 and southern part of the Teller C-4 quadrangles, western Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:21","indexId":"i572","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"572","subseriesTitle":"NONE","title":"Geologic map of the Teller B-4 and southern part of the Teller C-4 quadrangles, western Seward Peninsula, Alaska","language":"ENGLISH","doi":"10.3133/i572","usgsCitation":"Sainsbury, C., 1969, Geologic map of the Teller B-4 and southern part of the Teller C-4 quadrangles, western Seward Peninsula, Alaska: U.S. Geological Survey IMAP 572, 1 map :col. ;61 x 39 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i572.","productDescription":"1 map :col. ;61 x 39 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106843,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9358.htm","linkFileType":{"id":5,"text":"html"},"description":"9358"},{"id":187988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"63360","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -167,65.33333333333333 ], [ -167,65.75 ], [ -166.5,65.75 ], [ -166.5,65.33333333333333 ], [ -167,65.33333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a3fe","contributors":{"authors":[{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":275447,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35589,"text":"b1286 - 1969 - Gold Veins near Great Falls, Maryland","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"b1286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1286","title":"Gold Veins near Great Falls, Maryland","docAbstract":"Small deposits of native gold are present along an anastomosing system of quartz veins and shear zones just east of Great Falls, Montgomery County, Md. The deposits were discovered in 1861 and were worked sporadically until 1951, yielding more than 5,000 ounces of gold.\r\n\r\nThe vein system and the principal veins within it strike a few degrees west of north, at an appreciable angle to foliation and fold axial planes in enclosing rocks of the Wissahickon Formation of late Precambrian (?) age. The veins cut granitic rocks of Devonian or pre-Devonian age and may be as young as Triassic.\r\n\r\nFurther development of the deposits is unlikely under present economic conditions because of their generally low gold content and because much of the vein system lies on park property, but study of the Great Falls vein system may be useful in the search for similar deposits elsewhere in the Appalachian Piedmont.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/b1286","usgsCitation":"Reed, J.C., and Reed, J., 1969, Gold Veins near Great Falls, Maryland: U.S. Geological Survey Bulletin 1286, 22 p., https://doi.org/10.3133/b1286.","productDescription":"22 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":93394,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1286/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93395,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1286/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93396,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1286/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166177,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1286/report-thumb.jpg"},{"id":12477,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/bul/1286/index.htm","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.26666666666667,38.916666666666664 ], [ -77.26666666666667,39.083333333333336 ], [ -77.05,39.083333333333336 ], [ -77.05,38.916666666666664 ], [ -77.26666666666667,38.916666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a48f7","contributors":{"authors":[{"text":"Reed, John Calvin Jr.","contributorId":8460,"corporation":false,"usgs":true,"family":"Reed","given":"John","suffix":"Jr.","email":"","middleInitial":"Calvin","affiliations":[],"preferred":false,"id":214899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, John C. jreed@usgs.gov","contributorId":1259,"corporation":false,"usgs":true,"family":"Reed","given":"John C.","email":"jreed@usgs.gov","affiliations":[],"preferred":true,"id":214898,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3780,"text":"cir612 - 1969 - Gold in minerals and the composition of native gold","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"cir612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"612","title":"Gold in minerals and the composition of native gold","docAbstract":"Gold occurs in nature mainly as the metal and as various alloys. It forms complete series of solid solutions with silver, copper, nickel, palladium, and platinum. In association with the platinum metals, gold occurs as free gold as well as in solid solution. \r\n\r\nThe native elements contain the most gold, followed by the sulfide minerals. Several gold tellurides are known, but no gold selenides have been reported, and only one sulfide, the telluride-sulfide mineral nagyagite, is known. \r\n\r\nThe nonmetallic minerals carry the least gold, and the light-colored minerals generally contain less gold than the dark minerals. \r\n\r\nSome conclusions in the literature are conflicting in regard to the relation of fineness of native gold to its position laterally and vertically within a lode, the nature of the country rocks, and the location and size of nuggets in a streambed, as well as to the variation of fineness within an individual nugget.","language":"ENGLISH","publisher":"[U.S. Dept. of the Interior, Geological Survey],","doi":"10.3133/cir612","usgsCitation":"Jones, R.S., and Fleischer, M., 1969, Gold in minerals and the composition of native gold: U.S. Geological Survey Circular 612, 17 p. ;26 cm., https://doi.org/10.3133/cir612.","productDescription":"17 p. ;26 cm.","costCenters":[],"links":[{"id":117870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0612/report-thumb.jpg"},{"id":30851,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0612/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674115","contributors":{"authors":[{"text":"Jones, Robert Sprague","contributorId":41814,"corporation":false,"usgs":true,"family":"Jones","given":"Robert","email":"","middleInitial":"Sprague","affiliations":[],"preferred":false,"id":147586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleischer, Michael","contributorId":65835,"corporation":false,"usgs":true,"family":"Fleischer","given":"Michael","email":"","affiliations":[],"preferred":false,"id":147587,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3922,"text":"cir621 - 1969 - U.S. Geological Survey heavy metals program progress report 1968 - Field studies","interactions":[],"lastModifiedDate":"2015-11-17T14:42:19","indexId":"cir621","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"621","title":"U.S. Geological Survey heavy metals program progress report 1968 - Field studies","docAbstract":"<p>The Heavy Metals program of the U.S. Geological Survey and the U.S. Bureau of Mines began in mid-1966 and thus at the end of calendar year 1968 was halfway through its third year. This progress report summarizes field studies carried out under the Geological Survey's part of the program during 1968. Topical studies for 1968 are summarized in U.S. Geological Survey Circular 622. Background of the program and results during 1966 and 1967 were reported in U.S. Geological Survey Circular 560 and will not be further discussed herein.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir621","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, U.S. Geological Survey heavy metals program progress report 1968 - Field studies: U.S. Geological Survey Circular 621, iv, 35 p., https://doi.org/10.3133/cir621.","productDescription":"iv, 35 p.","numberOfPages":"41","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311424,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir621.jpg"},{"id":311423,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0621/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691bcf","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":528167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1676,"text":"wsp1757K - 1969 - A ground-water reconnaissance of the Republic of Ghana, with a description of geohydrologic provinces","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1757K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"1757","chapter":"K","title":"A ground-water reconnaissance of the Republic of Ghana, with a description of geohydrologic provinces","docAbstract":"This report gives a general summary of the availability and use of ground water and describes the occurrence of ground water in five major geohydrologic provinces lying in the eight administrative regions of Ghana. The identification and delineation of the geohydrologic provinces are based on their distinctive characteristics with respect to the occurrence and availability of ground water. \r\n\r\nThe Precambrian province occupies the southern, western, and northern parts of Ghana and is underlain largely by intrusive crystalline and metasedimentary rocks. The Voltaian province includes that part of the Voltaian sedimentary basin in central Ghana and is underlain chiefly by consolidated sandstone, mudstone, and shale. Narrow discontinuous bands of consolidated Devonian and Jurassic sedimentary rocks near the coast constitute the Coastal Block Fault province. \r\n\r\nThe Coastal Plain province includes semiconsolidated to unconsolidated sediments of Cretaceous to Holocene age that underlie coastal plain areas in southwestern and southeastern Ghana. The Alluvial province includes the Quaternary alluvial deposits in the principal river valleys and on the delta of the Volta River. Because of the widespread distribution of crystalline and consolidated sedimentary rocks of low permeability in the Precambrian, Voltaian, and Coastal Block Fault provinces, it is difficult to develop large or event adequate groundwater supplies in much of Ghana. On the other hand, small (1 to 50 gallons per minute) supplies of water of usable quality are available from carefully sited boreholes in most parts of the country. Also, moderate (50 to 200 gpm) supplies of water are currently (1964) obtained from small-diameter screened boreholes tapping sand and limestone aquifers in the Coastal Plain province in southwestern and southeastern Ghana, but larger supplies could be obtained through properly constructed boreholes. In the Alluvial province, unconsolidated deposits in the larger stream valleys that are now largely undeveloped offer desirable locations for shallow vertical or horizontal wells, which can induce infiltration from streams and yield moderate to large water supplies. \r\n\r\nThe principal factors that limit development of ground-water supplies in Ghana are (1) prevailing low permeability and water-yielding potential of the crystalline and consolidated sedimentary rocks that underlie most of the country, (2) highly mineralized ground water which appears to be widely distributed in the northern part of the Voltaian province, and (3) potential problems of salt-water encroachment in the Coastal Plain province in the Western Region and in the Keta area. \r\n\r\nOn the other hand, weathering has increased porosity and has thus substantially increased the water-yielding potential of the crystalline and consolidated sedimentary rocks in much of central and northern Ghana. Also, with proper construction and development, much larger yields than those now (1964) prevalent could be obtained from boreholes tapping sand and limestone aquifers in the Coastal Plain province.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1757K","usgsCitation":"Gill, H., 1969, A ground-water reconnaissance of the Republic of Ghana, with a description of geohydrologic provinces: U.S. Geological Survey Water Supply Paper 1757, iii, 38 p., https://doi.org/10.3133/wsp1757K.","productDescription":"iii, 38 p.","costCenters":[],"links":[{"id":138253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1757k/report-thumb.jpg"},{"id":26751,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26752,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1757k/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26753,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1757k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b45c0","contributors":{"authors":[{"text":"Gill, H.E.","contributorId":24330,"corporation":false,"usgs":true,"family":"Gill","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":143958,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3824,"text":"cir617 - 1969 - Results of geological and geochemical investigations in an area northwest of the Chulitna River, central Alaska Range","interactions":[],"lastModifiedDate":"2017-06-25T13:03:47","indexId":"cir617","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"617","title":"Results of geological and geochemical investigations in an area northwest of the Chulitna River, central Alaska Range","docAbstract":"Sedimentary and volcanic rock units of Paleozoic and Mesozoic age, faults, and elongate bodies of intrusive rock, particularly serpentinites, have a dominant northeasterly trend in an area northwest of the Chulitna River between Eldridge Glacier and Bull River. The serpentinites locally contain abnormal (as much as 0.5 percent) concentrations of nickel, have one newly identified occurrence of chromite, and are hosts to small epigenetic lodes containing copper, gold, and silver. Other epigenetic concentrations of copper or other metals occur in interlayered basalt and limestone at Partin and Canyon Creeks in the southwestern part of the area and in porphyry near Costello Creek in the northern part of the area. Tin occurs in greisen on upper Ohio Creek, and abnormal concentrations of tin also characterize mineralized rocks along Canyon Creek and at a prospect near Long Creek. Mineralized rocks characterized by silver, lead, and zinc crop out near Lookout Mountain. \r\n\r\nAnomalous concentrations of gold and other metals occur in stream sediments at isolated sites in upper Long Creek and at Coal Creek, as well as in several areas near known lode mineral occurrences. Shotgun and McCallie Creeks both contain stream sediments with anomalous concentrations of metals and both head into the basalt-limestone unit which is the host rock at Partin and Canyon Creeks; these facts suggest that other concentrations may be found.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir617","usgsCitation":"Hawley, C.C., Clark, A.L., Herdrick, M., and Clark, S.H., 1969, Results of geological and geochemical investigations in an area northwest of the Chulitna River, central Alaska Range: U.S. Geological Survey Circular 617, iii, 19 p. :maps. ;27 cm., https://doi.org/10.3133/cir617.","productDescription":"iii, 19 p. :maps. ;27 cm.","costCenters":[],"links":[{"id":30893,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1969/0617/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1969/0617/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db60635f","contributors":{"authors":[{"text":"Hawley, C. C.","contributorId":102070,"corporation":false,"usgs":true,"family":"Hawley","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":147681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, A. L.","contributorId":89502,"corporation":false,"usgs":true,"family":"Clark","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147679,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Herdrick, M.A.","contributorId":33307,"corporation":false,"usgs":true,"family":"Herdrick","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":147678,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Clark, S. H. B.","contributorId":95052,"corporation":false,"usgs":true,"family":"Clark","given":"S.","email":"","middleInitial":"H. B.","affiliations":[],"preferred":false,"id":147680,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1078,"text":"wsp1859F - 1969 - Geohydrology and water utilization in the Willcox Basin, Graham and Cochise Counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1859F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"1859","chapter":"F","title":"Geohydrology and water utilization in the Willcox Basin, Graham and Cochise Counties, Arizona","docAbstract":"The Willcox basin is an area of interior drainage in the northern part of Sulphur Springs Valley, Cochise and Graham Counties, Ariz. The basin comprises about 1,500 square miles, of which the valley floor occupies about 950 square miles. \r\n\r\nThe basin probably formed during middle and late Tertiary time, when the area was subjected to large-scale faulting accompanied by the uplift of the mountain ranges that presently border it. During and after faulting, large quantities of alluvium were deposited in the closed basin. \r\n\r\nThe rocks in the basin are divided into two broad groups--the rocks of the mountain blocks, of Precambrian through Tertiary age, and the rocks of the basin, of Tertiary and Quaternary age. The mountain blocks consist of igneous, metamorphic, and sedimentary rocks; the water-bearing characteristics of these rocks depend primarily on their degree of weathering and fracturing. Even in areas where these rocks are fractured and jointed, only small amounts of water have been developed. The rocks of the basin consist of moderately consolidated alluvium, poorly consolidated alluvium, and unconsolidated alluvium. The water-bearing characteristics of the moderately and poorly consolidated alluvium are not well known. The unconsolidated alluvium underlies most of the valley floor and consists of two facies, stream deposits and lake beds associated with the old playa. The lenticular sand and gravel layers interbedded in silt- and clay-size material of the unconsolidated alluvium constitute the principal aquifer in the basin. The other aquifers, which yield less water, consist of beds of poorly to moderately consolidated sand- and gravel-size material; these beds occur in both the poorly consolidated and moderately consolidated alluvium. \r\n\r\nIn the Stewart area the median specific capacity of wells per 100 feet of saturated unconsolidated alluvium was 20 gallons per minute, and in the Kansas Settlement area the specific capacity of wells penetrating the poorly and moderately consolidated alluvium, undifferentiated, was only 7.4 gallons per minute per 100 feet of saturated material penetrated. The aquifer in the Kansas Settlement area is much less permeable but more homogeneous than the aquifer in the Stewart area. The coefficient of transmissibility of the aquifers, which was estimated from the specific-capacity data, ranged from 58,000 to 160,000 gal. tons per day per foot. \r\n\r\nPrior to extensive ground-water pumpage, the ground-water system probably was in equilibrium, with discharge equaling recharge. At that time, ground water moved toward the playa, where it was discharged by transpiration and evaporation. The estimate of the evapotranspiration in the playa area before large-scale development was about 75,000 acre-feet per year. On the basis of estimates of coefficients of transmissibility of the aquifer and on the basis of the water-table configuration, underflow toward the playa was computed to be about 54,000 acre-feet per year. \r\n\r\nBy 1963, large-scale pumping had caused marked changes in the shape of the piezometric surface; large cones of depression had developed, and ground-water movement was toward the centers of pumping. The cones of depression caused by large-scale pumping have since expanded, and water-level declines have been measured in the recharge areas along the mountain fronts. \r\n\r\nGround water has been used for irrigation since 1910. In 1928, about 4,000 acre-feet of ground water was pumped, and by 1963 180,000 acre-feet per year was being pumped. An estimated 1,860,000 acre-feet of water has been pumped for irrigation in the Willcox basin through 1963; 680,000 acre-feet from the Stewart area, 990,000 acre-feet from the Kansas Settlement area, and 190,000 acre-feet from the Pearce-Cochise area. In the Sierra Bonita Ranch area and the north playa area, ground-water withdrawal for irrigation through 1963 was small. From the spring of 1952 to the spring of 1964 water-level declines resulting from the ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1859F","usgsCitation":"Brown, S., and Schumann, H.H., 1969, Geohydrology and water utilization in the Willcox Basin, Graham and Cochise Counties, Arizona: U.S. Geological Survey Water Supply Paper 1859, 32 p. :maps (3 fold. in pocket), https://doi.org/10.3133/wsp1859F.","productDescription":"32 p. :maps (3 fold. in pocket)","costCenters":[],"links":[{"id":138054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859f/report-thumb.jpg"},{"id":25785,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1859f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25786,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1859f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25787,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1859f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25788,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b50","contributors":{"authors":[{"text":"Brown, S. 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,{"id":1155,"text":"wsp1879F - 1969 - Hydrologic effects of the 1962-66 drought on Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1879F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"1879","chapter":"F","title":"Hydrologic effects of the 1962-66 drought on Long Island, New York","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1879F","usgsCitation":"Cohen, P.M., Franke, O.L., and McClymonds, N.E., 1969, Hydrologic effects of the 1962-66 drought on Long Island, New York: U.S. Geological Survey Water Supply Paper 1879, 18 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1879F.","productDescription":"18 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1879f/report-thumb.jpg"},{"id":25958,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1879f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6497a0","contributors":{"authors":[{"text":"Cohen, Philip M.","contributorId":67860,"corporation":false,"usgs":true,"family":"Cohen","given":"Philip","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":143272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Franke, O. Lehn","contributorId":63357,"corporation":false,"usgs":true,"family":"Franke","given":"O.","email":"","middleInitial":"Lehn","affiliations":[],"preferred":false,"id":143271,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McClymonds, N. E.","contributorId":94653,"corporation":false,"usgs":true,"family":"McClymonds","given":"N.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143273,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61682,"text":"gq793 - 1969 - Geologic map of the Teton Pass quadrangle, Teton County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:32","indexId":"gq793","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"793","title":"Geologic map of the Teton Pass quadrangle, Teton County, Wyoming","language":"ENGLISH","doi":"10.3133/gq793","usgsCitation":"Schroeder, M.L., 1969, Geologic map of the Teton Pass quadrangle, Teton County, Wyoming: U.S. Geological Survey Geologic Quadrangle 793, 1 map., https://doi.org/10.3133/gq793.","productDescription":"1 map.","costCenters":[],"links":[{"id":103509,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2095.htm","linkFileType":{"id":5,"text":"html"},"description":"2095"},{"id":247984,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0793/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0793/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,43.3675 ], [ -111,43.5 ], [ -110.86749999999999,43.5 ], [ -110.86749999999999,43.3675 ], [ -111,43.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a567","contributors":{"authors":[{"text":"Schroeder, Marvin L.","contributorId":91104,"corporation":false,"usgs":true,"family":"Schroeder","given":"Marvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":266231,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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