{"pageNumber":"6212","pageRowStart":"155275","pageSize":"25","recordCount":184938,"records":[{"id":62332,"text":"gq1014 - 1973 - Geologic map of the Laguna Dam 7.5-minute quadrangle, Arizona and California","interactions":[],"lastModifiedDate":"2015-10-06T15:02:07","indexId":"gq1014","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1014","title":"Geologic map of the Laguna Dam 7.5-minute quadrangle, Arizona and California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq1014","usgsCitation":"Olmsted, F.H., 1973, Geologic map of the Laguna Dam 7.5-minute quadrangle, Arizona and California: U.S. Geological Survey Geologic Quadrangle 1014, Report: 1 p.; Plate: 35.31 x 27.42 inches, https://doi.org/10.3133/gq1014.","productDescription":"Report: 1 p.; Plate: 35.31 x 27.42 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309702,"rank":701,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gq/1014/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":248511,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1014/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":102027,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_420.htm","linkFileType":{"id":5,"text":"html"},"description":"420"},{"id":253572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1014/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Arizona, California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.5,32.75 ], [ -114.5,32.8675 ], [ -114.36749999999999,32.8675 ], [ -114.36749999999999,32.75 ], [ -114.5,32.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db6971e6","contributors":{"authors":[{"text":"Olmsted, F. H.","contributorId":24765,"corporation":false,"usgs":true,"family":"Olmsted","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":267239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62342,"text":"gq1063 - 1973 - Geologic map of the Felicity quadrangle, Ohio-Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq1063","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1063","title":"Geologic map of the Felicity quadrangle, Ohio-Kentucky","language":"ENGLISH","doi":"10.3133/gq1063","usgsCitation":"Osborne, R.H., Weiss, M.P., and Outerbridge, W., 1973, Geologic map of the Felicity quadrangle, Ohio-Kentucky: U.S. Geological Survey Geologic Quadrangle 1063, 1 map., https://doi.org/10.3133/gq1063.","productDescription":"1 map.","costCenters":[],"links":[{"id":107507,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10608.htm","linkFileType":{"id":5,"text":"html"},"description":"10608"},{"id":248520,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1063/report.pdf","size":"39","linkFileType":{"id":1,"text":"pdf"}},{"id":253581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1063/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.11749999999999,38.75 ], [ -84.11749999999999,38.8675 ], [ -84,38.8675 ], [ -84,38.75 ], [ -84.11749999999999,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699618","contributors":{"authors":[{"text":"Osborne, Robert H.","contributorId":83120,"corporation":false,"usgs":true,"family":"Osborne","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":267256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weiss, Malcolm P.","contributorId":98378,"corporation":false,"usgs":true,"family":"Weiss","given":"Malcolm","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":267257,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Outerbridge, William F.","contributorId":40181,"corporation":false,"usgs":true,"family":"Outerbridge","given":"William F.","affiliations":[],"preferred":false,"id":267255,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15079,"text":"ofr73197 - 1973 - Preliminary geologic map and cross-sections of the Tintic Mountain quadrangle and an adjacent part of the McIntyre quadrangle, Juab and Utah Counties, Utah","interactions":[{"subject":{"id":15079,"text":"ofr73197 - 1973 - Preliminary geologic map and cross-sections of the Tintic Mountain quadrangle and an adjacent part of the McIntyre quadrangle, Juab and Utah Counties, Utah","indexId":"ofr73197","publicationYear":"1973","noYear":false,"title":"Preliminary geologic map and cross-sections of the Tintic Mountain quadrangle and an adjacent part of the McIntyre quadrangle, Juab and Utah Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66652,"text":"i883 - 1975 - Geologic map and sections of the Tintic Mountain Quadrangle and adjacent part of the McIntyre quadrangle, Juab and Utah counties, Utah","indexId":"i883","publicationYear":"1975","noYear":false,"title":"Geologic map and sections of the Tintic Mountain Quadrangle and adjacent part of the McIntyre quadrangle, Juab and Utah counties, Utah"},"id":1}],"supersededBy":{"id":66652,"text":"i883 - 1975 - Geologic map and sections of the Tintic Mountain Quadrangle and adjacent part of the McIntyre quadrangle, Juab and Utah counties, Utah","indexId":"i883","publicationYear":"1975","noYear":false,"title":"Geologic map and sections of the Tintic Mountain Quadrangle and adjacent part of the McIntyre quadrangle, Juab and Utah counties, Utah"},"lastModifiedDate":"2012-02-02T00:07:04","indexId":"ofr73197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-197","title":"Preliminary geologic map and cross-sections of the Tintic Mountain quadrangle and an adjacent part of the McIntyre quadrangle, Juab and Utah Counties, Utah","language":"ENGLISH","publisher":"U.S Geological Survey,","doi":"10.3133/ofr73197","usgsCitation":"Morris, H.T., 1973, Preliminary geologic map and cross-sections of the Tintic Mountain quadrangle and an adjacent part of the McIntyre quadrangle, Juab and Utah Counties, Utah: U.S. Geological Survey Open-File Report 73-197, 6 p. :ill., 2 folded maps ;27 cm., https://doi.org/10.3133/ofr73197.","productDescription":"6 p. :ill., 2 folded maps ;27 cm.","costCenters":[],"links":[{"id":148727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c1e9","contributors":{"authors":[{"text":"Morris, H. T.","contributorId":15585,"corporation":false,"usgs":true,"family":"Morris","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":170531,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15249,"text":"ofr73209 - 1973 - Geologic map of the Hyannis quadrangle, Barnstable County, Massachusetts","interactions":[{"subject":{"id":15249,"text":"ofr73209 - 1973 - Geologic map of the Hyannis quadrangle, Barnstable County, Massachusetts","indexId":"ofr73209","publicationYear":"1973","noYear":false,"title":"Geologic map of the Hyannis quadrangle, Barnstable County, Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":62361,"text":"gq1158 - 1974 - Geologic map of the Hyannis quadrangle, Barnstable County, Cape Cod, Massachusetts","indexId":"gq1158","publicationYear":"1974","noYear":false,"title":"Geologic map of the Hyannis quadrangle, Barnstable County, Cape Cod, Massachusetts"},"id":1}],"supersededBy":{"id":62361,"text":"gq1158 - 1974 - Geologic map of the Hyannis quadrangle, Barnstable County, Cape Cod, Massachusetts","indexId":"gq1158","publicationYear":"1974","noYear":false,"title":"Geologic map of the Hyannis quadrangle, Barnstable County, Cape Cod, Massachusetts"},"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr73209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-209","title":"Geologic map of the Hyannis quadrangle, Barnstable County, Massachusetts","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr73209","usgsCitation":"Oldale, R.N., 1973, Geologic map of the Hyannis quadrangle, Barnstable County, Massachusetts: U.S. Geological Survey Open-File Report 73-209, 15 p. :ill. (some folded), folded map ;29 cm.; 1 sheet, scale 1:24,000, https://doi.org/10.3133/ofr73209.","productDescription":"15 p. :ill. (some folded), folded map ;29 cm.; 1 sheet, scale 1:24,000","costCenters":[],"links":[{"id":147156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f5c","contributors":{"authors":[{"text":"Oldale, Robert N.","contributorId":38953,"corporation":false,"usgs":true,"family":"Oldale","given":"Robert","email":"","middleInitial":"N.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":170816,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14999,"text":"ofr73188 - 1973 - Geologic setting and chemical characteristics of hot springs in central and western Alaska","interactions":[],"lastModifiedDate":"2016-02-03T14:33:40","indexId":"ofr73188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-188","title":"Geologic setting and chemical characteristics of hot springs in central and western Alaska","docAbstract":"<p>Numerous hot springs occur in a variety of geologic provinces in central and western Alaska. Granitic plutons are common to all the provinces and the hot springs are spatially associated with the contacts of these plutons. Of 23 hot springs whose bedrock geology is known, all occur within 3 miles of a granitic pluton. The occurrence of hot springs, however, appears to be independent of the age, composition, or magmatic history of the pluton.</p>\n<p>Preliminary chemical and isotopic analyses suggest the hot springs waters belong to two groups. Most of the analyzed hot springs appear to have chemical and Isotopic compositions indicating they were derived from deeply circulating meteoric water. About 25 percent of the analyzed hot springs show a distinct saline character with high concentrations of chloride, sodium, potassium, and calcium indicating either much more complex water rock reactions than occurred in the other hot springs or the addition of another type of water. The present chemical and isotopic data are insufficient to determine the source of the constituents of the saline hot springs.</p>\n<p>Chemical geothermometers suggest subsurface temperatures in the general range of 100&deg;C to 160&deg;C. If the hot spring waters have derived their heat solely from deep circulation, the waters must have reached depths of 9,000 to 15,000 feet, assuming geothermal gradients of 30&deg;C to 50&deg;C/km. If hot magmatic water has been added to the geothermal systems or if dilution or mixing has occurred, temperatures of 100&deg;C to 160&deg;C may be reached at shallower depths.</p>\n<p>The geologic and chemical data are too preliminary to make an estimate of the potential of the hot springs as a geothermal resource. The data suggest, however, that most of the hot springs of central and western Alaska have relatively low subsurface temperatures and limited reservoir capacities in comparison with geothermal areas presently being utilized for electrical power generation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr73188","usgsCitation":"Miller, T.P., Barnes, I., and Pattan, W.W., 1973, Geologic setting and chemical characteristics of hot springs in central and western Alaska: U.S. Geological Survey Open-File Report 73-188, Report: 19 p.; 1 Figure; 1 Table (in 2 parts), https://doi.org/10.3133/ofr73188.","productDescription":"Report: 19 p.; 1 Figure; 1 Table (in 2 parts)","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":43825,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0188/plate-1.pdf","text":"Figure 1","size":"688.14 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 1"},{"id":43826,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0188/plate-2.pdf","text":"Table 1","size":"1.21 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Table 1"},{"id":43827,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0188/plate-3.pdf","text":"Table 1, Part 2","size":"1.29 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Table 1, Part 2"},{"id":43828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0188/report.pdf","text":"Report","size":"589.73 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":148931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0188/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -165,\n              64\n            ],\n            [\n              -165,\n              66\n            ],\n            [\n              -150,\n              66\n            ],\n            [\n              -150,\n              64\n            ],\n            [\n              -165,\n              64\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881be","contributors":{"authors":[{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":170388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":170389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pattan, William Wallace Jr.","contributorId":61297,"corporation":false,"usgs":true,"family":"Pattan","given":"William","suffix":"Jr.","email":"","middleInitial":"Wallace","affiliations":[],"preferred":false,"id":170390,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14997,"text":"ofr73187 - 1973 - Distribution and chemical analyses of thermal springs in Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:06","indexId":"ofr73187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-187","title":"Distribution and chemical analyses of thermal springs in Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr73187","usgsCitation":"Miller, T.P., 1973, Distribution and chemical analyses of thermal springs in Alaska: U.S. Geological Survey Open-File Report 73-187, 5 p. :folded map ;27 cm., https://doi.org/10.3133/ofr73187.","productDescription":"5 p. :folded map ;27 cm.","costCenters":[],"links":[{"id":148800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":43822,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0187/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649fad","contributors":{"authors":[{"text":"Miller, T. P.","contributorId":49345,"corporation":false,"usgs":true,"family":"Miller","given":"T.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":170385,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13959,"text":"ofr7397 - 1973 - Geology and mineral resources of central Antioquia Department (Zone IIA), Colombia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr7397","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-97","title":"Geology and mineral resources of central Antioquia Department (Zone IIA), Colombia","docAbstract":"This report summarizes the geology of an area of some 6000 square kilometers in the northern part of the Central Cordillera of the Colombian Andes. The area, in north-central Department of Antioquia, was mapped between 1964 and 1968 as part of the Inventario Minero Nacional (IMN) project. Mineral resources are summarized within a larger area, designated as subzone ILK of IMN Zone If, which comprises almost 22,000 sq. kin, including the area mapped geologically by IMN and additional areas mapped by other agencies. \r\n\r\nThe oldest formation is a micaceous paragneiss of early Paleozoic or possibly late Precambrian age. A thick geosynclinal sedimentary series accumulated during the Paleozoic Era and became regionally metamorphosed to greenschist (locally amphibolite) facies during the Permian or early Triassic; these schists and gneisses are designated collectively as the Valdivia Group. The Permian(?) orogenic episode included intrusion of concordant syntectonic plutons, mostly of tonalitic composition. Rocks of unequivocal Triassic or Jurassic age are not recognized.\r\n\r\nThe Cretaceous is well represented by both igneous and sedimentary assemblages. Eugeosynclinal alpine ophiolites comprising submarine basalt flows and numerous intrusions of gabbro and serpentinite are prominent in the Lower Cretaceous, together with flysch composed of marine shale and lesser sandstone and conglomerate. The Upper Cretaceous is represented along the west border of the mapped area by submarine basalt flows and pyroclastic rocks, locally Interbedded with fine-grained clastic sedimentary beds, and lenses of dark laminated chert, at least part of which is radiolarian. The Late Cretaceous was marked by an orogenic event that profoundly folded and faulted all rocks and in the Central Cordillera caused low-grade metamorphism, the overprint of which is hardly observable in pre-Cretaceous rocks elsewhere. The Late Cretaceous orogeny culminated with discordant intrusion of the epizonal tonalitic Antioquian batholith. Displacement along the great Romeral wrench fault may have begun in the Cretaceous. \r\n\r\nPlutonism continued into the Cenozoic, exemplified by the hornblende-diorite Sabanalarga pluton. Intermontane basins were filled with molasse derived from the erosion of adjacent highlands; Tertiary sedimentation in marshy areas included organic carboniferous matter subsequently converted to lignite or subbituminous coal. The Sabanalarga fault system originated in the Late Tertiary; intermittent displacement continued on the older wrench faults such as the Romeral. Epeirogenic uplift, which probably began in the Pliocene and continued through the Pleistocene and Holocene, brought on renewed erosion which has sculptured the mountains into their present form.\r\n\r\nMineral resources in subzone IIA are varied but not of outstanding importance. Gold and silver mining, significant in past centuries, is minor today. Ferruginous laterite on serpentinite once considered as a potential source of iron ore is not economically exploitable. IMN has explored nickeliferous laterite at the extreme northwest corner of subzone IIA; this is a potential resource, exploitable only after exhaustion of the larger and richer nickel laterite deposit at Cerro Matoso, farther to the north and outside the boundaries of Zone If. Known deposits of mercury, chromium, manganese, and copper are small, with limited economic potential. Nonmetallic resources include raw materials for cement, including portland cement. Saprolite clay is widely used in making common red brick and tile, still a dominant construction material in all but the most modern multistory buildings. Aggregate materials are varied and abundant. Kaolin of good quality near La Union is important as a ceramic raw mineral filler. Tertiary subbituminous coal beds are an important energy resource in western subzone IIA, and have a good potential for greater development. Deposits of sodic feldspar, talc, decorative stone, and silica a","language":"ENGLISH","publisher":"U.S. Geological Survey]","doi":"10.3133/ofr7397","usgsCitation":"Hall, R., Alvarez A., J., and Rico H., H., 1973, Geology and mineral resources of central Antioquia Department (Zone IIA), Colombia: U.S. Geological Survey Open-File Report 73-97, x, 174 p. :maps (3 folded, 1 col.) ;27 cm.; 1 map, scale 1:100,000, https://doi.org/10.3133/ofr7397.","productDescription":"x, 174 p. :maps (3 folded, 1 col.) ;27 cm.; 1 map, scale 1:100,000","costCenters":[],"links":[{"id":95182,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0097/plate-1.pdf","size":"12413","linkFileType":{"id":1,"text":"pdf"}},{"id":147401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0097/report-thumb.jpg"},{"id":42615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0097/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46fd","contributors":{"authors":[{"text":"Hall, R.B.","contributorId":17214,"corporation":false,"usgs":true,"family":"Hall","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":168699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alvarez A., Jairo","contributorId":44411,"corporation":false,"usgs":true,"family":"Alvarez A.","given":"Jairo","email":"","affiliations":[],"preferred":false,"id":168701,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rico H., Hector","contributorId":42481,"corporation":false,"usgs":true,"family":"Rico H.","given":"Hector","email":"","affiliations":[],"preferred":false,"id":168700,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24979,"text":"pp850 - 1973 - Geological Survey research 1973","interactions":[],"lastModifiedDate":"2025-01-07T17:39:30.968268","indexId":"pp850","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"850","title":"Geological Survey research 1973","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp850","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Geological Survey research 1973: U.S. Geological Survey Professional Paper 850, viii, 366 p., https://doi.org/10.3133/pp850.","productDescription":"viii, 366 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":421216,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92939.htm","text":"Biostratigraphic record extended to Early Silurian or Ordovician in western Brooks Range","linkFileType":{"id":5,"text":"html"}},{"id":53964,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0850/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118859,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0850/report-thumb.jpg"},{"id":465772,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92944.htm","text":"Upper Lower Permian rocks discovered in northeastern Alaska","linkFileType":{"id":5,"text":"html"}},{"id":465773,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92945.htm","text":"New evidence bearing on age of Wales Group","linkFileType":{"id":5,"text":"html"}},{"id":465774,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92947.htm","text":"Late Ordovician (Ashgillian) age of volcanic rocks, north-central Maine","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6876ee","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":529140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2005,"text":"wsp2024 - 1973 - Water resources of the Big Sioux River Valley near Sioux Falls, South Dakota","interactions":[],"lastModifiedDate":"2017-10-15T12:37:57","indexId":"wsp2024","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"2024","title":"Water resources of the Big Sioux River Valley near Sioux Falls, South Dakota","docAbstract":"<p>The major sources of water in the Big Sioux River valley between Sioux Falls and Dell Rapids, S.Dak., are the Big Sioux River and the glacial outwash aquifer beneath the flood plain. The river and the aquifer are hydraulically connected.</p>\n<p>The Big Sioux River has an average annual discharge of 246 cubic feet per second, on the average exceeds bankfull stage every 2.3 years, and has moderate basin storage.. Periods of low flow are common in the late summer, fall, and winter. A low flow of 0.1 cubic foot per second has been recorded.</p>\n<p>The outwash aquifer is composed of permeable sand, sand and gravel, and some boulders. The aquifer underlies an area of 33 square miles and commonly has a saturated thickness of less than 30 feet.</p>\n<p>Aquifer tests and measurements of streamflow indicate a rate of streambed infiltration of about 6 gallons per day per square foot. Analyses of streambed samples and interpretations of lithology from an electric log indicate that the streambed sediments in the diversion channel of the Big Sioux River consist largely of relatively impermeable silts and clays.</p>\n<p>Under normal climatic conditions, most of the water pumped by the city of Sioux Falls is water that entered the aquifer by streambed infiltration.</p>\n<p>To evaluate the importance of the aquifer in the hydrologic system, both an electrical analog model and a digital model were programmed for storage depletion alone. These models were used to determine the water-level declines in the aquifer that would result from 1 year of withdrawal at a rate of 9-10 million gallons per day. Both models indicated that the existing well field can yield water at that rate for more than 1 year.</p>\n<p>The analog model was also used to determine the maximum average daily yield of the aquifer-river system for a 2-year period modeled for the minimum recorded stream discharge and for streambed infiltration as the only recharge. The maximum average yield under these conditions would be less than 24 million gallons per day. Most of the water pumped during this period would be from aquifer storage.</p>\n<p>Water from the river is generally less mineralized, softer, and easier to treat than ground water. Water pumped from wells near the river is similar in quality to the river water, but does not have the objectionable odors or tastes often present in water from the river.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2024","usgsCitation":"Jorgensen, D.G., and Ackroyd, E.A., 1973, Water resources of the Big Sioux River Valley near Sioux Falls, South Dakota: U.S. Geological Survey Water Supply Paper 2024, Report: vii, 50 p.; Plate:  44.26 x 25.00 inches, https://doi.org/10.3133/wsp2024.","productDescription":"Report: vii, 50 p.; Plate:  44.26 x 25.00 inches","numberOfPages":"59","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":27449,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2024/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27450,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2024/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2024/report-thumb.jpg"}],"country":"United States","state":"South Dakota","city":"Sioux Falls","otherGeospatial":"Big Sioux River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.94335937499999,\n              43.50075243569041\n            ],\n            [\n              -96.94335937499999,\n              43.97898113341921\n            ],\n            [\n              -96.5643310546875,\n              43.97898113341921\n            ],\n            [\n              -96.5643310546875,\n              43.50075243569041\n            ],\n            [\n              -96.94335937499999,\n              43.50075243569041\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0621","contributors":{"authors":[{"text":"Jorgensen, Donald G.","contributorId":19537,"corporation":false,"usgs":true,"family":"Jorgensen","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144513,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ackroyd, Earl A.","contributorId":59425,"corporation":false,"usgs":true,"family":"Ackroyd","given":"Earl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144514,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56542,"text":"wdrND721 - 1973 - Water resources data for North Dakota, water year 1972, Part 1, Surface water records","interactions":[],"lastModifiedDate":"2020-10-27T17:56:08.714107","indexId":"wdrND721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"ND-72-1","title":"Water resources data for North Dakota, water year 1972, Part 1, Surface water records","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND721","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for North Dakota, water year 1972, Part 1, Surface water records: U.S. Geological Survey Water Data Report 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,{"id":2898,"text":"wsp2029C - 1973 - Use of finite-difference arrays of observation wells to estimate evapotranspiration from ground water in the Arkansas River Valley, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"wsp2029C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"2029","chapter":"C","title":"Use of finite-difference arrays of observation wells to estimate evapotranspiration from ground water in the Arkansas River Valley, Colorado","docAbstract":"A method to determine evapotranspiration from ground water was tested at four sites in the flood plain of the Arkansas River in Colorado. Approximate ground-water budgets were obtained by analyzing water-level data from observation wells installed in five-point arrays. The analyses were based on finite difference approximations of the differential equation describing ground-water flow. \r\n\r\nData from the sites were divided into two groups by season. It was assumed that water levels during the dormant season were unaffected by evapotranspiration of ground water or by recharge, collectively termed 'accretion.' Regression analyses of these data were made to provide an equation for separating the effects of changes in aquifer storage and of aquifer heterogeneity from those due to accretion during the growing season. The data collected during the growing season were thus analyzed to determine accretion.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2029C","usgsCitation":"Weeks, E.P., and Sorey, M., 1973, Use of finite-difference arrays of observation wells to estimate evapotranspiration from ground water in the Arkansas River Valley, Colorado: U.S. Geological Survey Water Supply Paper 2029, iii, 27 p. ;24 cm., https://doi.org/10.3133/wsp2029C.","productDescription":"iii, 27 p. ;24 cm.","costCenters":[],"links":[{"id":138379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2029c/report-thumb.jpg"},{"id":29564,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2029c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6046a9","contributors":{"authors":[{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":145976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":145977,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56522,"text":"wdrIA721 - 1973 - Water resources data for Iowa, water year 1972","interactions":[],"lastModifiedDate":"2012-02-02T00:12:05","indexId":"wdrIA721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"IA-72-1","title":"Water resources data for Iowa, water year 1972","language":"ENGLISH","doi":"10.3133/wdrIA721","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for Iowa, water year 1972: U.S. Geological Survey Water Data Report IA-72-1, 312 p., https://doi.org/10.3133/wdrIA721.","productDescription":"312 p.","costCenters":[],"links":[{"id":181564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1972/ia-72-1/report-thumb.jpg"},{"id":88141,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1972/ia-72-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5f25","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":532703,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2861,"text":"wsp1974 - 1973 - Water resources of the New Jersey part of the Ramapo River basin","interactions":[{"subject":{"id":56068,"text":"ofr70352 - 1970 - Water resources of the New Jersey part of the Ramapo River basin","indexId":"ofr70352","publicationYear":"1970","noYear":false,"title":"Water resources of the New Jersey part of the Ramapo River basin"},"predicate":"SUPERSEDED_BY","object":{"id":2861,"text":"wsp1974 - 1973 - Water resources of the New Jersey part of the Ramapo River basin","indexId":"wsp1974","publicationYear":"1973","noYear":false,"title":"Water resources of the New Jersey part of the Ramapo River basin"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1974","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1974","title":"Water resources of the New Jersey part of the Ramapo River basin","docAbstract":"The Ramapo River, a major stream in the Passaic River basin, drains an area of 161 square miles, 70 percent of which is in Orange and Rockland Counties, N.Y., and 30 percent is in Bergen and Passaic Counties, N.J. This report describes the hydrology of the New Jersey part of the basin and evaluates the feasibility of developing large ground-water supplies from the stratified drift in the Ramapo River valley by inducing recharge to the aquifer from the river. The ground water and surface water of the basin are considered as a single resource because the development of either ground water or surface water affects the availability of the other. \r\n\r\nPrecambrian gneiss, sparsely mantled with Pleistocene glacial drift, underlies the basin west of the Ramapo River in New Jersey. To the east, bedrock consists of the Watchung Basalt and of shale, sandstone, and conglomerate of the Brunswick Formation of Triassic age. Glacial drift occurs nearly everywhere in the eastern part of the basin, and deposits of stratified drift more than 100 feet thick occur in the Ramapo valley. Average annual runoff at Pompton Lakes accounts for 25 inches of the 45 inches of annual precipitation in the New Jersey part of the basin, and the remaining 20 inches is accounted for by evapotranspiration. Streamflow is highly variable--particularly in the area underlain by gneissic rocks-because of the low storage capacity of the rocks and the rough topography. \r\n\r\nMany of the small tributaries go dry during extended periods of no precipitation. Small domestic supplies of ground water can be obtained nearly everywhere, but the Brunswick Formation is the only consolidated-rock aquifer in the basin that can be depended upon to yield 100-200 gallons per minute to wells. Supplies of more than 1,000 gallons per minute are available from wells tapping the stratified drift in the Ramapo valley. The drift supplies 75 percent of the ground water pumped for public supply in the basin. Sustained ground-water yield in upland areas, based on stream base-flow recession, is estimated to be 200,000-300,000 gallons per day per square mile for the drift-covered Brunswick Formation and about 100,000-200,000 gallons per day per square mile for the gneiss and basalt. Potential sustained yield of the stratified drift in the valley depends on the availability of the streamflow and on the induced rate of infiltration. \r\n\r\nPumping from the stratified drift results in a reduction in streamflow, which may be undesirable, mainly because of prior downstream water rights. On the basis of the storage available in the stratified drift and an analysis of daily flow during the drought period of October 1964 to September 1967 at Pompton Lakes, 20-25 million gallons per day of Ramapo River water are available for development after existing downstream water requirements are supplied. However, some low-flow augmentation will be. necessary to insure downstream rights. Rates of infiltration computed from seepage losses observed near Mahwah indicate that at least 11 million gallons per day, on an average basis, can be infiltrated from the river by the pumping of wells tapping the stratified drift. The use of recharge pits and spreading areas would increase the rate of infiltration. Losses from the Ramapo River could be minimized by returning treated sewage effluent directly to the river or, preferably, by recharging the stratified-drift aquifer with the treated effluent. \r\n\r\nGround-water quality and surface-water quality at times of low-flow vary according to the type of rock from which the water is obtained. Water from the gneiss is low in dissolved solids--less than 127 mg/l (milligrams per liter)--and soft to moderately hard--less than 94 rag/l. Water from the Brunswick Formation is more mineralized--total dissolved-solids content is as much as 278 mg/1 and hardness as much as 188 mg/1. Water from the stratified drift is generally intermediate in quality--that is, total dissolved-solids content is as ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1974","usgsCitation":"Vecchioli, J., and Miller, E., 1973, Water resources of the New Jersey part of the Ramapo River basin: U.S. Geological Survey Water Supply Paper 1974, vi, 77 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1974.","productDescription":"vi, 77 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":138982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1974/report-thumb.jpg"},{"id":29456,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29457,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29458,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29459,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29460,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1974/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef13d","contributors":{"authors":[{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":145920,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, E.G.","contributorId":44132,"corporation":false,"usgs":true,"family":"Miller","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":145921,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2858,"text":"wsp1969 - 1973 - Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan","interactions":[],"lastModifiedDate":"2017-02-06T11:55:59","indexId":"wsp1969","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1969","title":"Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan","docAbstract":"<p>The Tri-County region, consisting of Clinton, Eaton, and Ingham Counties, is an area of 1,697 square miles in Michigan's Lower Peninsula and has as its hub the Lansing metropolitan area. The land surface ranges in altitude from about 700 to about 1,000 feet. The region receives an average of about 31 inches of precipitation each year. </p><p>The population is nearing 400,000 and by 1990 will be near 600,000. Average daily water use is slightly more than 30 million gallons today; by 1980 it will be about 50 million gallons, and by 1990 it will probably be about 70 million gallons. </p><p>The Tri-County region is drained by seven river systems. The median annual 7 -day mean low flows of the principal streams in these systems were measured at the point farthest downstream within the region. These values, in cubic feet per second, are as follows: Grand River, 180; Maple River, 34; Looking Glass River, 28; Red Cedar River, 30; Portage Creek, 15; Battle Creek, 20; and Thornapple River, 24-a total of 331 cubic feet per second or about 220 million gallons per day. The areal variance in 7-day low-flow runoff ranges from 0 to 0.15 cubic foot per second per square mile. </p><p>The principal source of ground water in the Tri-County region is a complex aquifer system composed of the Saginaw and Grand River Formations and some of the overlying glacial sediments. This aquifer yields between 300 and 700 gallons per minute to individual wells in much of the western half of Ingham County, in the eastern half of Clinton County, in a small area in southeastern Clinton County, and in northeastern Eaton County. In some parts of the region, the glacial sediments are favorable for development of moderate to large supplies of water. Minor aquifers in the region are the Bayport, Michigan, and Marshall Formations. </p><p>Providing water supplies in the future requires complete and comprehensive water-management programs. Such management programs involve determining which of several alternative water-development systems is the best. Some of the chief factors and methods that must be considered when planning these systems are combined use of ground and surface water, artificial recharge, treatment of wastes, use of storage reservoirs, and importation of water from the Great Lakes.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1969","usgsCitation":"Vanlier, K.E., Wood, W., and Brunett, J.O., 1973, Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan: U.S. Geological Survey Water Supply Paper 1969, Document: vii, 111 p.; 3 Plates: 35.70 x 31.97 inches or smaller, https://doi.org/10.3133/wsp1969.","productDescription":"Document: vii, 111 p.; 3 Plates: 35.70 x 31.97 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":139081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1969/report-thumb.jpg"},{"id":247253,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1969/plate-1.pdf","size":"5337","linkFileType":{"id":1,"text":"pdf"}},{"id":247254,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1969/plate-2.pdf","size":"10148","linkFileType":{"id":1,"text":"pdf"}},{"id":247255,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1969/plate-3.pdf","size":"13282","linkFileType":{"id":1,"text":"pdf"}},{"id":29452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1969/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","county":"Clinton County, Eaton County, Ingham County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.3681,43.1172],[-84.3675,42.9561],[-84.3679,42.9439],[-84.3666,42.861],[-84.3668,42.8561],[-84.3649,42.7746],[-84.1593,42.7779],[-84.1519,42.685],[-84.146,42.5999],[-84.1402,42.4239],[-84.2539,42.4236],[-84.2607,42.4242],[-84.3676,42.4242],[-84.3677,42.4224],[-84.4864,42.4215],[-84.6026,42.4215],[-84.7207,42.4209],[-84.83,42.421],[-84.8375,42.4215],[-84.9561,42.4221],[-85.0667,42.4215],[-85.0736,42.4211],[-85.0738,42.5956],[-85.0745,42.7707],[-84.9577,42.7712],[-84.8391,42.7706],[-84.8376,42.857],[-84.8393,42.9434],[-84.8382,43.1199],[-84.6022,43.1185],[-84.3681,43.1172]]]},\"properties\":{\"name\":\"Clinton\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99fe","contributors":{"authors":[{"text":"Vanlier, Kenneth Eugene","contributorId":6840,"corporation":false,"usgs":true,"family":"Vanlier","given":"Kenneth","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":145915,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Warren W.","contributorId":47770,"corporation":false,"usgs":false,"family":"Wood","given":"Warren W.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":145916,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brunett, Jilann O.","contributorId":92230,"corporation":false,"usgs":true,"family":"Brunett","given":"Jilann","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":145917,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1635,"text":"wsp2117 - 1973 - Surface water supply of the United States, 1966-70, Part 6, Missouri River basin, v. 2, Missouri River basin from Williston, North Dakota to Sioux City, Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp2117","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"2117","title":"Surface water supply of the United States, 1966-70, Part 6, Missouri River basin, v. 2, Missouri River basin from Williston, North Dakota to Sioux City, Iowa","language":"ENGLISH","publisher":"USGS,","doi":"10.3133/wsp2117","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Surface water supply of the United States, 1966-70, Part 6, Missouri River basin, v. 2, Missouri River basin from Williston, North Dakota to Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 2117, 612 p. ;23 cm., https://doi.org/10.3133/wsp2117.","productDescription":"612 p. ;23 cm.","costCenters":[],"links":[{"id":137221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2117/report-thumb.jpg"},{"id":26702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2117/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691bdc","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":527994,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56516,"text":"wdrIL721 - 1973 - Water resources data for Illinois, water year 1972","interactions":[],"lastModifiedDate":"2012-02-02T00:11:50","indexId":"wdrIL721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"IL-72-1","title":"Water resources data for Illinois, water year 1972","language":"ENGLISH","doi":"10.3133/wdrIL721","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for Illinois, water year 1972: U.S. Geological Survey Water Data Report IL-72-1, 295 p., https://doi.org/10.3133/wdrIL721.","productDescription":"295 p.","costCenters":[],"links":[{"id":174460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6e15","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":532697,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23312,"text":"ofr73102 - 1973 - Predicted effects of proposed navigation improvements on residence time and dissolved oxygen of the salt wedge in the Duwamish River estuary, King County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr73102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-102","title":"Predicted effects of proposed navigation improvements on residence time and dissolved oxygen of the salt wedge in the Duwamish River estuary, King County, Washington","docAbstract":"A model of the circulation and quality of water in the Duwamish River estuary has been sufficiently developed to allow prediction of the effects of a proposed widening and deepening of waterways on residence time and dissolved oxygen in the estuary's salt wedge. For a low river-discharge period in August 1970, use of the model yielded an estimated residence time of wedge water to be 6.3 days in the present waterways estuary and 8.6 days in the wider and deeper proposed-waterways estuary--a 37-percent increase. June-September 1970 and for the estuary about 4 miles upstream from its mouth, the model estimates indicate that dissolved-oxygen values in the wedge of the proposed-waterways estuary would be as much as 1.4 milligrams per liter lower and would average 0.4 milligram per liter lower than (average difference significant at 95-percent confidence level) dissolved-oxygen values in the wedge of the present-waterways estuary. \r\n\r\nExtrapolation to low dissolved-oxygen values of a regression between the predicted dissolved oxygen for both the proposed and present-waterways estuaries suggests that 4 miles upstream of the estuary mouth oxygen would be completely depleted from the proposed-waterways estuary wedge whereas there still would be 0.2 milligram of oxygen per liter of water in the wedge of the present-waterways estuary.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr73102","issn":"0094-9140","usgsCitation":"Haushild, W., and Stoner, J., 1973, Predicted effects of proposed navigation improvements on residence time and dissolved oxygen of the salt wedge in the Duwamish River estuary, King County, Washington: U.S. Geological Survey Open-File Report 73-102, 13 p. :ill., map ;27 cm., https://doi.org/10.3133/ofr73102.","productDescription":"13 p. :ill., map ;27 cm.","costCenters":[],"links":[{"id":155134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0102/report-thumb.jpg"},{"id":52612,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0102/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fde2","contributors":{"authors":[{"text":"Haushild, W.L.","contributorId":48953,"corporation":false,"usgs":true,"family":"Haushild","given":"W.L.","affiliations":[],"preferred":false,"id":189874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":189875,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2405,"text":"wsp2017 - 1973 - Improvement of trout streams in Wisconsin by augmenting low flows with ground water","interactions":[],"lastModifiedDate":"2015-10-01T13:24:03","indexId":"wsp2017","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"2017","title":"Improvement of trout streams in Wisconsin by augmenting low flows with ground water","docAbstract":"<p>Approximately 2 cubic feet per second of ground water were introduced into the Little Plover River in 1968 when natural streamflow ranged from 3 to 4 cubic feet per second. These augmentation flows were retained undiminished through the 2-mile reach of stream monitored. Maximum stream temperatures were reduced as much as 5?F (3?C) at the augmentation site during the test period, although changes became insignificant more than 1 mile downstream. Maximum temperatures might be reduced as much as 10?F (6?C) during critical periods, based on estimates using a stream temperature model developed as part of the study. During critical periods significant temperature improvement may extend 2 miles or more downstream. Changes in minimum DO (dissolved oxygen) levels were slight, primarily because of the high natural DO levels occurring during the test period. Criteria for considering other streams for flow augmentation are developed on the basis of the observed hydrologic responses in the Little Plover River. Augmentation flows of nearly 2? cubic feet per second of ground water were introduced into the headwater reach of Black Earth Creek from the end of June through mid-October 1969. Streamflow ranged from 1 to 2 cubic feet per second at the augmentation site, and the average flow at the gaging station at Black Earth, approximately 8 miles downstream, ranged from 25 to 50 cubic feet per second. Augmentation flows were retained through the 8-mile reach of stream. Temperature of the augmentation flow as it entered the stream ranged from 60? to 70?F (about 16? to 21?C) during the test period, and minimum stream temperatures were raised 5?F (3?C) or more at the augmentation site, with changes extending from 2 to 3 miles downstream. Augmentation during critical periods could maintain stream temperatures between 40? and 70?F (4? and 21?C) through most of the study reach. DO levels were increased by as much as 2 milligrams per liter or more below the augmentation site, although the improvement diminished to approximately 1 milligram per liter downstream in the problem reach. During critical periods DO improvement in the problem reach would be somewhat greater. Flow augmentation would not be necessary during normal conditions in either of the streams studied. Critical DO and temperature levels are not known to occur in the Little Plover River. Since the construction of secondary treatment facilities at the Cross Plains sewage-treatment plant, critical DO levels are no longer expected to be a problem in Black Earth Creek. However, results from this study may be used to estimate the effectiveness of flow augmentation in other streams in similar areas in which critical DO or temperature levels may occur.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2017","collaboration":"Prepared in cooperation with Wisconsin Department of Natural Resources","usgsCitation":"Novitzki, R., 1973, Improvement of trout streams in Wisconsin by augmenting low flows with ground water: U.S. Geological Survey Water Supply Paper 2017, v, 52 p., https://doi.org/10.3133/wsp2017.","productDescription":"v, 52 p.","numberOfPages":"58","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":28405,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2017/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2017/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Dane County, Portage County","otherGeospatial":"Black Earth Creek, Little Plover River","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-89.0094,43.286],[-89.0084,43.2555],[-89.0094,43.2],[-89.01,43.1131],[-89.0109,43.0849],[-89.0107,43.0271],[-89.0132,42.9353],[-89.013,42.8762],[-89.0119,42.8471],[-89.132,42.8479],[-89.2488,42.8478],[-89.3689,42.8484],[-89.3688,42.8575],[-89.4832,42.858],[-89.6026,42.8575],[-89.7196,42.8587],[-89.8377,42.8598],[-89.8375,42.9471],[-89.8386,43.0317],[-89.8384,43.1181],[-89.8394,43.205],[-89.8325,43.2123],[-89.825,43.2187],[-89.8175,43.226],[-89.8125,43.2342],[-89.8088,43.2369],[-89.8012,43.2365],[-89.7874,43.2356],[-89.771,43.237],[-89.7579,43.2379],[-89.7529,43.2443],[-89.7485,43.2507],[-89.7391,43.2548],[-89.7259,43.2644],[-89.7171,43.2739],[-89.714,43.2821],[-89.7165,43.2867],[-89.7235,43.2935],[-89.7209,43.2935],[-89.6008,43.2932],[-89.4819,43.2942],[-89.3617,43.2954],[-89.3624,43.2832],[-89.246,43.2834],[-89.1271,43.2827],[-89.0094,43.286]]],[[[-89.2234,44.6814],[-89.2231,44.5916],[-89.2235,44.504],[-89.2238,44.4174],[-89.2242,44.3308],[-89.2245,44.2433],[-89.2469,44.2438],[-89.3464,44.2439],[-89.3649,44.2439],[-89.4835,44.244],[-89.488,44.244],[-89.5977,44.2458],[-89.606,44.2458],[-89.717,44.2475],[-89.7247,44.2479],[-89.7243,44.3372],[-89.7259,44.4239],[-89.7268,44.5114],[-89.8447,44.5116],[-89.8451,44.5983],[-89.8449,44.6849],[-89.7268,44.6852],[-89.608,44.6853],[-89.4899,44.6858],[-89.346,44.6812],[-89.2234,44.6814]]]]},\"properties\":{\"name\":\"Dane\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eeb53","contributors":{"authors":[{"text":"Novitzki, R.P.","contributorId":73986,"corporation":false,"usgs":true,"family":"Novitzki","given":"R.P.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":145149,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2521,"text":"wsp1865 - 1973 - Water resources and geology of Mount Rushmore National Memorial, South Dakota","interactions":[],"lastModifiedDate":"2017-10-15T12:37:31","indexId":"wsp1865","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1865","title":"Water resources and geology of Mount Rushmore National Memorial, South Dakota","docAbstract":"<p>Ground water suitable for public supply can be obtained from fractured metamorphic and igneous rooks at Mount Rushmore National Memorial, S. Dak.</p>\n<p>The memorial comprises three main drainage basins: Starling basin, Lafferty Gulch basin, and East Boundary basin. Ground water is most prevalent in Lafferty Gulch basin but Starling basin contributes the most surface water.</p>\n<p>The total water supply was obtained from springs until 1967 when increasing numbers of visitors required development of additional sources. As a result of this investigation, wells 3 and 4 were drilled in Lafferty Gulch basin and East Boundary basin. Well 3 is 200 feet deep in mica schist and granite. It produced 7.3 million gallons of water in 1968 and 7.7 million gallons of water in 1969, the total supply for the memorial. Well 4 is 500 feet deep, also in mica schist and granite. It is not used at the present time (1970) but will be used in the future when more water is needed. Water from both wells is potable, but the quality of water from well 3 is superior to that from well 4.</p>\n<p>Mica schist is the most abundant rock in the memorial. The more prominent hills and mountains, however, are in large, northerly striking granite sills, some of which are several hundred feet thick. Pegmatite sills and dikes are also numerous. The western boundary of the memorial is at the east edge of the Harney Peak Granite batholith. The dip of schistosity and bedding in schist adjacent to the batholith is about 30 ? E. but increases across the memorial to about 65 ? E. in the northeast corner.</p>\n<p>At some locations in the memorial, granite or pegmatite sills act as ground-water dams preventing the movement of ground water down gradient. A pegmatite or granite sill is probably the cause of the accumulation of water in the vicinity of well 3. The well flows when it is not being pumped.</p>\n<p>The occurrence of ground water is dependent upon the presence of joints and fractures in the schist and granite bedrock. The rocks themselves are relatively impermeable and would yield little or no water in their unaltered state.</p>\n<p>Mica schist that has been intruded by granite and (or) pegmatite is more fractured and yields more ground water in the memorial than mica schist alone. This condition may be due to jointing and to the greater fracturability of the intruded rocks in the vicinity of granitic intrusions.</p>\n<p>Ground water is also available from alluvium in major valleys such as Starling basin and the valleys of Grizzly Bear Creek and Battle Creek.</p>\n<p>Evapotranspiration is the greatest use-item in the water budget. An approximation of evapotranspiration based upon an average annual precipitation of 19 inches is 1,600 acre-feet, or 80 percent of the annual precipitation.</p>\n<p>Several locations in the memorial have potential as future, sources of ground-water supplies. The most promising areas are near spring 6 in the southeast corner and alluvium in the valleys of Battle and Grizzly Bear Creeks.</p>\n<p>Developed and potential water resources in the memorial probably are sufficient to meet demands beyond the year 2000.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1865","usgsCitation":"Powell, J., Norton, J.J., and Adolphson, D.G., 1973, Water resources and geology of Mount Rushmore National Memorial, South Dakota: U.S. Geological Survey Water Supply Paper 1865, Report: vi, 49 p.; Plate: 34.00 x 22.00 inches, https://doi.org/10.3133/wsp1865.","productDescription":"Report: vi, 49 p.; Plate: 34.00 x 22.00 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":28723,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1865/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1865/report-thumb.jpg"},{"id":28724,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1865/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Dakota","otherGeospatial":"Mount Rushmore National Memorial","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.46400260925293,\n              43.873705074113886\n            ],\n            [\n              -103.46400260925293,\n              43.88391319597796\n            ],\n            [\n              -103.45061302185059,\n              43.88391319597796\n            ],\n            [\n              -103.45061302185059,\n              43.873705074113886\n            ],\n            [\n              -103.46400260925293,\n              43.873705074113886\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687e04","contributors":{"authors":[{"text":"Powell, J.E.","contributorId":27030,"corporation":false,"usgs":true,"family":"Powell","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":145336,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norton, James Jennings","contributorId":59412,"corporation":false,"usgs":true,"family":"Norton","given":"James","email":"","middleInitial":"Jennings","affiliations":[],"preferred":false,"id":145337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145338,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":6199,"text":"pp716E - 1973 - Distribution, thickness, and lithology of Paleocene rocks in Pakistan","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"pp716E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"716","chapter":"E","title":"Distribution, thickness, and lithology of Paleocene rocks in Pakistan","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp716E","usgsCitation":"Meissner, C.R., and Rahman, H., 1973, Distribution, thickness, and lithology of Paleocene rocks in Pakistan: U.S. Geological Survey Professional Paper 716, 6 p., https://doi.org/10.3133/pp716E.","productDescription":"6 p.","costCenters":[],"links":[{"id":117306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0716e/report-thumb.jpg"},{"id":33365,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0716e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33366,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0716e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33367,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0716e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33368,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0716e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33369,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0716e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db636048","contributors":{"authors":[{"text":"Meissner, Charles R. Jr.","contributorId":28970,"corporation":false,"usgs":true,"family":"Meissner","given":"Charles","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rahman, Habib-ur.","contributorId":18764,"corporation":false,"usgs":true,"family":"Rahman","given":"Habib-ur.","email":"","affiliations":[],"preferred":false,"id":152283,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62701,"text":"gq1118 - 1973 - Surficial geologic map of the Pepperell quadrangle, Middlesex County, Massachusetts, and Hillsborough County, New Hampshire","interactions":[{"subject":{"id":42654,"text":"ofr72213 - 1972 - Preliminary surficial geologic and materials maps of the Pepperell quadrangle, Massachusetts-New Hampshire","indexId":"ofr72213","publicationYear":"1972","noYear":false,"title":"Preliminary surficial geologic and materials maps of the Pepperell quadrangle, Massachusetts-New Hampshire"},"predicate":"SUPERSEDED_BY","object":{"id":62701,"text":"gq1118 - 1973 - Surficial geologic map of the Pepperell quadrangle, Middlesex County, Massachusetts, and Hillsborough County, New Hampshire","indexId":"gq1118","publicationYear":"1973","noYear":false,"title":"Surficial geologic map of the Pepperell quadrangle, Middlesex County, Massachusetts, and Hillsborough County, New Hampshire"},"id":1}],"lastModifiedDate":"2022-12-28T22:52:03.47442","indexId":"gq1118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1118","title":"Surficial geologic map of the Pepperell quadrangle, Middlesex County, Massachusetts, and Hillsborough County, New Hampshire","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq1118","usgsCitation":"Koteff, C., and Volckmann, R.P., 1973, Surficial geologic map of the Pepperell quadrangle, Middlesex County, Massachusetts, and Hillsborough County, New Hampshire: U.S. Geological Survey Geologic Quadrangle 1118, Report: 1 p.; 1 Plate: 43.04 x 30.40 iniches, https://doi.org/10.3133/gq1118.","productDescription":"Report: 1 p.; 1 Plate: 43.04 x 30.40 iniches","costCenters":[],"links":[{"id":107554,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10659.htm","linkFileType":{"id":5,"text":"html"},"description":"10659"},{"id":254250,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1118/report-thumb.jpg"},{"id":248857,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1118/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Massachusetts. New Hampshire","county":"Hillsborough County, Middlesex County","otherGeospatial":"Pepperell quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.625,\n              42.625\n            ],\n            [\n              -71.625,\n              42.75\n            ],\n            [\n              -71.5,\n              42.75\n            ],\n            [\n              -71.5,\n              42.625\n            ],\n            [\n              -71.625,\n              42.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688e33","contributors":{"authors":[{"text":"Koteff, Carl","contributorId":73172,"corporation":false,"usgs":true,"family":"Koteff","given":"Carl","email":"","affiliations":[],"preferred":false,"id":267751,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Volckmann, Richard P.","contributorId":35791,"corporation":false,"usgs":true,"family":"Volckmann","given":"Richard","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":267750,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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