{"pageNumber":"6154","pageRowStart":"153825","pageSize":"25","recordCount":184938,"records":[{"id":16524,"text":"ofr74332 - 1974 - Tungsten resources of Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:07:17","indexId":"ofr74332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-332","title":"Tungsten resources of Brazil","docAbstract":"Brazilian tungsten production, 85 percent of which is exported, comes almost entirely from scheelite-bearing tactites in northeast Brazil, and has reached an annual rate of about 2,000 metric tons (2,200 short tons) of scheelite concentrate with 70 percent WO3. Scheelite ore reserves, located principally in the State of Rio Grande do Norte, are estimated to be as high as 8,300,000 tons (9,100,000 short tons) containing 0.7 percent WO3. \r\n\r\nMinor deposits (or those about which only minimal information is available) of wolframite, with which some cassiterite is associated, are located in Sao Paulo, Santa Catarina, and Rio Grande do Sul. Both the scheelite and the wolframite deposits are considered . to be late Precambrian A (620 to 900 m.y.) or early Cambrian in age.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr74332","usgsCitation":"White, M.G., 1974, Tungsten resources of Brazil: U.S. Geological Survey Open-File Report 74-332, [1], 23 p. :maps ;27 cm., https://doi.org/10.3133/ofr74332.","productDescription":"[1], 23 p. :maps ;27 cm.","costCenters":[],"links":[{"id":150279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0332/report-thumb.jpg"},{"id":45509,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0332/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45510,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0332/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623fa6","contributors":{"authors":[{"text":"White, Max Gregg","contributorId":91841,"corporation":false,"usgs":true,"family":"White","given":"Max","email":"","middleInitial":"Gregg","affiliations":[],"preferred":false,"id":172991,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47285,"text":"ofr741 - 1974 - Generalized geologic map of the southern part of the Mantua Quadrangle, Weber County, Utah","interactions":[{"subject":{"id":47285,"text":"ofr741 - 1974 - Generalized geologic map of the southern part of the Mantua Quadrangle, Weber County, Utah","indexId":"ofr741","publicationYear":"1974","noYear":false,"title":"Generalized geologic map of the southern part of the Mantua Quadrangle, Weber County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":60937,"text":"mf720 - 1976 - Preliminary geologic map of the Mantua Quadrangle and part of the Willard Quadrangle, Box Elder, Weber, and Cache counties, Utah","indexId":"mf720","publicationYear":"1976","noYear":false,"title":"Preliminary geologic map of the Mantua Quadrangle and part of the Willard Quadrangle, Box Elder, Weber, and Cache counties, Utah"},"id":1}],"supersededBy":{"id":60937,"text":"mf720 - 1976 - Preliminary geologic map of the Mantua Quadrangle and part of the Willard Quadrangle, Box Elder, Weber, and Cache counties, Utah","indexId":"mf720","publicationYear":"1976","noYear":false,"title":"Preliminary geologic map of the Mantua Quadrangle and part of the Willard Quadrangle, Box Elder, Weber, and Cache counties, Utah"},"lastModifiedDate":"2012-02-02T00:10:42","indexId":"ofr741","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-1","title":"Generalized geologic map of the southern part of the Mantua Quadrangle, Weber County, Utah","language":"ENGLISH","doi":"10.3133/ofr741","usgsCitation":"Sorensen, M.L., and Crittenden, M.D., 1974, Generalized geologic map of the southern part of the Mantua Quadrangle, Weber County, Utah: U.S. Geological Survey Open-File Report 74-1, 1 map; scale = 1:24000, https://doi.org/10.3133/ofr741.","productDescription":"1 map; scale = 1:24000","costCenters":[],"links":[{"id":108579,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14984.htm","linkFileType":{"id":5,"text":"html"},"description":"14984"},{"id":171469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aee5a","contributors":{"authors":[{"text":"Sorensen, M. L.","contributorId":79106,"corporation":false,"usgs":true,"family":"Sorensen","given":"M.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":234979,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crittenden, M. D. Jr.","contributorId":43421,"corporation":false,"usgs":true,"family":"Crittenden","given":"M.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":234978,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13701,"text":"ofr74123 - 1974 - Land-surface subsidence in the Houston-Galveston region, Texas","interactions":[],"lastModifiedDate":"2023-09-12T21:29:59.529623","indexId":"ofr74123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-123","title":"Land-surface subsidence in the Houston-Galveston region, Texas","docAbstract":"<p>The pumping of large amounts of ground water in the Houston-Galveston region, Texas, has resulted in water-level declines of as much as 200 feet (61 metres) in wells completed in the Chicot aquifer and as much as 325 feet (99 metres) in wells completed in the Evangeline aquifer during 1943-73. The maximum annual rates of decline for 1943-73 were 6.7 feet (2.0 metres) in the Chicot aquifer and 10.8 feet (3.3 metres) in the Evangeline aquifer. During 1964-73, the maximum rates were 10 feet (3.0 metres) in the Chicot and 17.8 feet (5.4 metres) in the Evangeline. The declines in artesian pressures have resulted in pronounced regional subsidence of the land surface.</p><p>The center of subsidence is at Pasadena, where as much as 7.5 feet (2.3 metres) of subsidence occurred between 1943 and 1973. More than 1.0 foot (0.3 metre) of subsidence occurred at Pasadena between 1906 and 1943. The maximum amount of subsidence during 1964-73 was about 3.5 feet (1.1 metres).</p><p>In the southern part of Harris County, about 55 percent of the subsidence is a result of compaction in the Chicot aquifer. The area in which subsidence is 1 foot (0.3 metre) or more has increased from about 350 square miles (906 square kilometres) in 1954 to about 2,500 square miles (6,475 square kilometres) in 1973.</p><p>Estimates of subsidence are based on the amount of water-level decline, the thickness of the clay, and the compressibility of the clay. At Seabrook, it is estimated that for each 1 foot (0.3 metre) of average water-level decline, 1 foot (0.3 metre) of clay would compact 0.000031 foot (0.00094 centimetre). At Seabrook, for 1 foot (0.3 metre) of water-level decline, 0.0248 foot (0.756 centimetre) of subsidence would occur.</p><p>Planned use of surface water instead of ground water will probably result in some recovery of artesian pressures. If pressure recovery occurs the rate of subsidence should decrease substantially in the more critical areas.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74123","collaboration":"Prepared in cooperation with the Texas Water Development Board and the cities of Houston and Galveston","usgsCitation":"Gabrysch, R., and Bonnet, C., 1974, Land-surface subsidence in the Houston-Galveston region, Texas: U.S. Geological Survey Open-File Report 74-123, iii, 23 p., https://doi.org/10.3133/ofr74123.","productDescription":"iii, 23 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":146822,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0123/report-thmb.jpg"},{"id":420739,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"Galveston, Houston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -95.75589219460284,\n              30.32996230202275\n            ],\n            [\n              -95.75589219460284,\n              29.23869471186177\n            ],\n            [\n              -94.67969378429146,\n              29.23869471186177\n            ],\n            [\n              -94.67969378429146,\n              30.32996230202275\n            ],\n            [\n              -95.75589219460284,\n              30.32996230202275\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adecd","contributors":{"authors":[{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":168259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bonnet, C.W.","contributorId":44535,"corporation":false,"usgs":true,"family":"Bonnet","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":168258,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60658,"text":"mf603 - 1974 - Geologic map of the Scenic and parts of the Brennan Flat and Sheep Mountain Table quadrangles, Pennington and Shannon counties, South Dakota","interactions":[],"lastModifiedDate":"2012-02-10T00:10:38","indexId":"mf603","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"603","title":"Geologic map of the Scenic and parts of the Brennan Flat and Sheep Mountain Table quadrangles, Pennington and Shannon counties, South Dakota","language":"ENGLISH","doi":"10.3133/mf603","usgsCitation":"Raymond, W.H., and King, R., 1974, Geologic map of the Scenic and parts of the Brennan Flat and Sheep Mountain Table quadrangles, Pennington and Shannon counties, South Dakota: U.S. Geological Survey Miscellaneous Field Studies Map 603, 1 map on 2 sheets., https://doi.org/10.3133/mf603.","productDescription":"1 map on 2 sheets.","costCenters":[],"links":[{"id":104192,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3719.htm","linkFileType":{"id":5,"text":"html"},"description":"3719"},{"id":180385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102.61749999999999,40 ], [ -102.61749999999999,43.916666666666664 ], [ -102.5,43.916666666666664 ], [ -102.5,40 ], [ -102.61749999999999,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b73d","contributors":{"authors":[{"text":"Raymond, W. H.","contributorId":83919,"corporation":false,"usgs":true,"family":"Raymond","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":264150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, R.U.","contributorId":7692,"corporation":false,"usgs":true,"family":"King","given":"R.U.","email":"","affiliations":[],"preferred":false,"id":264149,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13707,"text":"ofr74227 - 1974 - Hard iron ore at the Cliffs Shaft Mines, Ishpeming, Michigan","interactions":[],"lastModifiedDate":"2023-11-20T23:54:11.088806","indexId":"ofr74227","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-227","title":"Hard iron ore at the Cliffs Shaft Mines, Ishpeming, Michigan","docAbstract":"<p>At the Cliffs Shaft Mines, for many years the premiere hard iron ore mine of Michigan, bodies of ore typically are localized in the upper part of the Negaunee iron-formation, close beneath Goodrich Quartzite in the axial part of the Marquette synclinorium. Individual ore bodies may be as much as 100 feet thick and extend laterally for many hundreds of feet. The cluster of ore bodies making up the Cliffs Shaft deposit has an overall length of about 4,500 feet from east to west parallel to the axis of the syncliorium and a width of 1,500 feet from north to south. The deposit extends beneath much of the City of Ishpeming, from a short distance west of the city limits to almost the east edge of the city.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74227","usgsCitation":"Gair, J.E., 1974, Hard iron ore at the Cliffs Shaft Mines, Ishpeming, Michigan: U.S. Geological Survey Open-File Report 74-227, 6 p., https://doi.org/10.3133/ofr74227.","productDescription":"6 p.","costCenters":[],"links":[{"id":422766,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0227/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147420,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0227/report-thumb.jpg"}],"country":"United States","state":"Michigan","city":"Ishpeming","otherGeospatial":"Cliffs Shaft Mines","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -87.72071958635472,\n              46.49679965272563\n            ],\n            [\n              -87.72071958635472,\n              46.46933892121058\n            ],\n            [\n              -87.637519822388,\n              46.46933892121058\n            ],\n            [\n              -87.637519822388,\n              46.49679965272563\n            ],\n            [\n              -87.72071958635472,\n              46.49679965272563\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644b9f","contributors":{"authors":[{"text":"Gair, Jacob Eugene","contributorId":14387,"corporation":false,"usgs":true,"family":"Gair","given":"Jacob","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":168269,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15092,"text":"ofr74257 - 1974 - Hydrologic effects of the Tampa Bypass Canal","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr74257","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-257","title":"Hydrologic effects of the Tampa Bypass Canal","language":"ENGLISH","publisher":"[s.n.],","doi":"10.3133/ofr74257","usgsCitation":"Motz, L.H., 1974, Hydrologic effects of the Tampa Bypass Canal: U.S. Geological Survey Open-File Report 74-257, 48 leaves :22 folded maps ;28 cm.; (68 p. - PGS), https://doi.org/10.3133/ofr74257.","productDescription":"48 leaves :22 folded maps ;28 cm.; (68 p. - PGS)","costCenters":[],"links":[{"id":148059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606e15","contributors":{"authors":[{"text":"Motz, Louis H.","contributorId":6934,"corporation":false,"usgs":true,"family":"Motz","given":"Louis","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":170553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16663,"text":"ofr743 - 1974 - Procedure for processing analog strip-chart records from creepmeters and strainmeters","interactions":[],"lastModifiedDate":"2025-08-01T18:46:04.375424","indexId":"ofr743","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-3","title":"Procedure for processing analog strip-chart records from creepmeters and strainmeters","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr743","usgsCitation":"Yamashita, P., Goodreau, D., and Jones, A., 1974, Procedure for processing analog strip-chart records from creepmeters and strainmeters: U.S. Geological Survey Open-File Report 74-3, iii, 78 p., https://doi.org/10.3133/ofr743.","productDescription":"iii, 78 p.","costCenters":[],"links":[{"id":150351,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0003/report-thumb.jpg"},{"id":493365,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6609e9","contributors":{"authors":[{"text":"Yamashita, P.A.","contributorId":50536,"corporation":false,"usgs":true,"family":"Yamashita","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":173244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodreau, D.D.","contributorId":46547,"corporation":false,"usgs":true,"family":"Goodreau","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":173243,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, A.C.","contributorId":26302,"corporation":false,"usgs":true,"family":"Jones","given":"A.C.","email":"","affiliations":[],"preferred":false,"id":173242,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15108,"text":"ofr74239 - 1974 - Volcanic hazards on the Island of Hawaii","interactions":[],"lastModifiedDate":"2020-09-27T17:29:19.888457","indexId":"ofr74239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-239","title":"Volcanic hazards on the Island of Hawaii","docAbstract":"Volcanic hazards on the Island of Hawaii have been determined to be chiefly products of eruptions: lava flows, falling fragments, gases, and particle-and-gas clouds. Falling fragments and particle-and-gas clouds can be substantial hazards to life, but they are relatively rare. Lava flows are the chief hazard to property; they are frequent and cover broad areas. Rupture, subsidence, earthquakes, and sea waves (tsunamis) caused by eruptions are minor hazards; those same events caused by large-scale crustal movements, however, are major hazards to both life and property. \r\n\r\nVolcanic hazards are greatest on Mauna Loa and Kilauea, and the risk is highest along the rift zones of those volcanoes. The hazards are progressively less severe on Hualalai, Mauna Kea, and Kohala volcanoes. Some risk from earthquakes extends across the entire island, and the risk from tsunamis is high all along the coast. \r\n\r\nThe island has been divided into geographic zones of different relative risk for each volcanic hazard, and for all those hazards combined. Each zone is assigned a relative risk for that area as a whole; the degree of risk varies within the zones, however, and in some of them the risk decreases gradationally across the entire zone. Moreover, the risk in one zone may be locally as great or greater than that at some points in the zone of next higher overall risk. Nevertheless, the zones can be highly useful for land-use planning. \r\n\r\nPlanning decisions to which the report is particularly applicable include the selection of kinds of structures and kinds of land use that are appropriate for the severity and types of hazards present. For example, construction of buildings that can resist a lava flow is generally not feasible, but it is both feasible and desirable to build structures that can resist falling rock fragments, earthquakes, and tsunamis in areas where risk from those hazards is relatively high. The report can also be used to select sites where overall risk is relatively low, to identify sites where either overall risk or risk from some specific hazard is relatively high, and to identify areas in which there is a threat to lives as well as to property. The report further can serve as a basis for warning persons about hazards in areas most likely to be affected by volcanic eruptions. Perhaps most important, however, the report provides basic information needed for zoning to control future land use.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74239","usgsCitation":"Mullineaux, D.R., and Peterson, D.W., 1974, Volcanic hazards on the Island of Hawaii: U.S. Geological Survey Open-File Report 74-239, Report: ii, 61 p.; 2 Plates: 45.44 x 27.41 inches and 45.52 x 36.01 inches, https://doi.org/10.3133/ofr74239.","productDescription":"Report: ii, 61 p.; 2 Plates: 45.44 x 27.41 inches and 45.52 x 36.01 inches","costCenters":[],"links":[{"id":44034,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0239/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44033,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0239/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44032,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0239/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0239/report-thumb.jpg"}],"country":"United States","state":"Hawaii","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.4453125,\n              18.8335153964335\n            ],\n            [\n              -154.66552734375,\n              18.8335153964335\n            ],\n            [\n              -154.66552734375,\n              20.46818922264095\n            ],\n            [\n              -156.4453125,\n              20.46818922264095\n            ],\n            [\n              -156.4453125,\n              18.8335153964335\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e482ae4b07f02db4e762b","contributors":{"authors":[{"text":"Mullineaux, Donal Ray","contributorId":31759,"corporation":false,"usgs":true,"family":"Mullineaux","given":"Donal","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":170584,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, Donald W.","contributorId":11209,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":170583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29200,"text":"wri7422 - 1974 - Special techniques for determining chemical properties of geothermal water","interactions":[],"lastModifiedDate":"2018-11-14T09:51:46","indexId":"wri7422","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-22","title":"Special techniques for determining chemical properties of geothermal water","docAbstract":"<p>A reliable determination of the chemical composition of geothermal fluids may require special sampling and preservation techniques. A sample collected without pretreatment is usually adequate for the analysis of sodium, potassium, and chloride. Other constituents may require further treatment or even analysis in the field, depending on the data requirements. The collection and preservation methods described permit accurate results for 31 chemical variables, including major and minor chemical constituents.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7422","usgsCitation":"Presser, T.S., and Barnes, I., 1974, Special techniques for determining chemical properties of geothermal water: U.S. Geological Survey Water-Resources Investigations Report 74-22, iv, 11 p., https://doi.org/10.3133/wri7422.","productDescription":"iv, 11 p.","costCenters":[],"links":[{"id":159433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0022/report-thumb.jpg"},{"id":359408,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e6343","contributors":{"authors":[{"text":"Presser, T. S.","contributorId":93875,"corporation":false,"usgs":true,"family":"Presser","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":201134,"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":201133,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60094,"text":"mf621A - 1974 - Contour map of the bedrock surface, Mount Toby Quadrangle, Massachusetts","interactions":[],"lastModifiedDate":"2013-08-12T11:39:30","indexId":"mf621A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"621","chapter":"A","title":"Contour map of the bedrock surface, Mount Toby Quadrangle, Massachusetts","language":"ENGLISH","doi":"10.3133/mf621A","usgsCitation":"Londquist, C., 1974, Contour map of the bedrock surface, Mount Toby Quadrangle, Massachusetts: U.S. Geological Survey Miscellaneous Field Studies Map 621, 1 map., https://doi.org/10.3133/mf621A.","productDescription":"1 map.","costCenters":[],"links":[{"id":183684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":276379,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0621a/plate-1.pdf"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.61749999999999,42.3675 ], [ -72.61749999999999,42.5 ], [ -72.5,42.5 ], [ -72.5,42.3675 ], [ -72.61749999999999,42.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699626","contributors":{"authors":[{"text":"Londquist, C.J.","contributorId":86796,"corporation":false,"usgs":true,"family":"Londquist","given":"C.J.","affiliations":[],"preferred":false,"id":263123,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14841,"text":"ofr74213 - 1974 - Long term flow of the Truckee River in California and Nevada","interactions":[],"lastModifiedDate":"2024-02-22T22:43:06.260352","indexId":"ofr74213","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-213","title":"Long term flow of the Truckee River in California and Nevada","docAbstract":"<p>The Office of the Solicitor, Department of the Interior, requested the Geological Survey to evaluate the reliability of streamflow records in the Truckee River basin and to determine the long-term average annual runoff.</p><p>The reliability of streamflow records was evaluated by comparisons between pairs of records at six locations along the Truckee River between Lake Tahoe and Pyramid Lake.</p><p>The observed or estimated annual runoff near Nixon, Nevada was adjusted for changes in storage, evaporation losses, diversions, and depletions to approximate the inflow into Pyramid Lake under natural conditions.</p><p>The long-term average annual runoff near Nixon was computed on the basis of streamflow records since 1899. The long-term (124-year) record of precipitation at Sacramento and tree ring information were used to substantiate the conclusion that the average runoff during the 74 years of streamflow record is a reliable measure of the average runoff for a longer period.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74213","usgsCitation":"Matthai, H.F., 1974, Long term flow of the Truckee River in California and Nevada: U.S. Geological Survey Open-File Report 74-213, 24 p., https://doi.org/10.3133/ofr74213.","productDescription":"24 p.","costCenters":[],"links":[{"id":147594,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0213/report-thumb.jpg"},{"id":425895,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0213/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California, Nevada","otherGeospatial":"Truckee River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.32360558817447,\n              40.51053025647829\n            ],\n            [\n              -120.32360558817447,\n              38.82780030300307\n            ],\n            [\n              -118.92834191629952,\n              38.82780030300307\n            ],\n            [\n              -118.92834191629952,\n              40.51053025647829\n            ],\n            [\n              -120.32360558817447,\n              40.51053025647829\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63bf11","contributors":{"authors":[{"text":"Matthai, Howard Frederick","contributorId":100824,"corporation":false,"usgs":true,"family":"Matthai","given":"Howard","email":"","middleInitial":"Frederick","affiliations":[],"preferred":false,"id":170103,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16523,"text":"ofr74333 - 1974 - Tin resources of Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:07:17","indexId":"ofr74333","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-333","title":"Tin resources of Brazil","docAbstract":"Annual tin production in Brazil, most of it from cassiterite placer deposits in Rondonia Territory, amounts to about 4,000 metric tons (4,400 short tons) of concentrate containing 66 percent tin, much of which is consumed by Brazilian industry.\r\n\r\nReserves of cassiterite concentrate in the placers of Rondonia district are estimated at about 160,000 (176,000 short tons) containing 66 percent tin. Extensive undiscovered resources of cassiterite possibly exist in southern Rondonia Territory and to the east of the Territory in northern Mato Grosso, southern Amazonas, and southern Para. Numerous occurrences have been reported in these regions and as far to the east as the headwaters of the Tapajos and the Xingo Rivers.\r\n\r\nMinor deposits or occurrences of cassiterite (or lode deposits about which there is only minimal information available) are located in Para, Amapa, Paraiba, Rio Grande do Norte, Ceara, Bahia, Minas Gerais, Goias, Sao Paulo, and Rio Grande do Sul.\r\n\r\nAll the lode tin deposits are dated or enclosed in rocks that date as Precambrian B (900 to 1,300 m.y.).","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr74333","usgsCitation":"White, M.G., 1974, Tin resources of Brazil: U.S. Geological Survey Open-File Report 74-333, ii, 32 p. :maps ;27 cm.; (44 p. - PGS), https://doi.org/10.3133/ofr74333.","productDescription":"ii, 32 p. :maps ;27 cm.; (44 p. - PGS)","costCenters":[],"links":[{"id":150278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0333/report-thumb.jpg"},{"id":45508,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0333/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8e2b","contributors":{"authors":[{"text":"White, Max Gregg","contributorId":91841,"corporation":false,"usgs":true,"family":"White","given":"Max","email":"","middleInitial":"Gregg","affiliations":[],"preferred":false,"id":172990,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26835,"text":"wri7419 - 1974 - Limnological study of Lake Shastina, Siskiyou County, California","interactions":[],"lastModifiedDate":"2018-10-29T14:34:49","indexId":"wri7419","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-19","title":"Limnological study of Lake Shastina, Siskiyou County, California","docAbstract":"<p>Lake Shastina provides water for irrigation in Shasta Valley, as well as recreation. Presently, its shoreline is being developed for summer homes. Surface water constituted more than 90 percent of the approximately 50,000 acre-foot (62-cubic hectometre) inflow to Lake Shastina in the 1972 water year. Controlled outflow is via the Montague Main Canal; however, leakage from the lake through volcanic rocks to the northwest was estimated to be greater than the measured outflow. Appreciable annual changes in the quantity of water in storage in the lake are related mainly to variations in annual inflow.</p><p>From June through August the lake was thermally stratified. In the spring and summer the epilimnion was often supersaturated with oxygen, while at the same time the hypolimnion was undersaturated and 'often devoid of dissolved oxygen. Vertical stratification of carbon dioxide, carbonate, bicarbonate, hydrogen ion, nitrogen, and phosphorus was also recorded during the spring and summer. Orthophosphate, total phosphorus, and total nitrogen concentrations (organic, ammonium, and nitrate) were highest in the hypolimnion during the period of thermal stratification.</p><p>Ten-inch (25-centimetre) core samples from the reservoir bottom were chemically analyzed at 0.8-inch (2-centimetre) intervals. The concentrations ranged from 6.3 to 28.9 milligrams per gram of iron, 0.07 to 0.43 milligrams per gram of manganese, 0.4 to 2.7 milligrams per gram of organic nitrogen plus ammonium, and 0.06 to 1.3 milligrams per gram of total phosphorus. Organic matter in the cores ranged from 4 to 14 percent.</p><p>Green algae and diatoms were the dominant algal types, reaching maximum concentrations of about 7 and 30 million cells per litre, respectively. These phytoplankton occurred near the surface during thermally stratified periods, but were distributed at greater depths during nonthermally stratified periods. Blue-green algae were present only in the spring samples, and reached a maximum concentration of about 5 million cells per litre.</p><p>Zooplankton numbers were greatest in March, July, and September, with lesser concentrations in June. Three major zooplankton groups, Cladocera, Copepoda, and Rotifera, were present. The major groups of benthic organisms were Oligochaeta, Chironomidae, and Chaoborus, with numbers ranging from 3350, 890, and 8450 per square metre, respectively.</p><p>A discussion on algal control is included.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7419","usgsCitation":"Dong, A.E., Beatty, K.W., and Averett, R.C., 1974, Limnological study of Lake Shastina, Siskiyou County, California: U.S. Geological Survey Water-Resources Investigations Report 74-19, vi, 52 p., https://doi.org/10.3133/wri7419.","productDescription":"vi, 52 p.","costCenters":[],"links":[{"id":158213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0019/report-thumb.jpg"},{"id":358911,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Siskiyou County","otherGeospatial":"Lake Shastina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.4539566040039,\n              41.48929196487705\n            ],\n            [\n              -122.35919952392578,\n              41.48929196487705\n            ],\n            [\n              -122.35919952392578,\n              41.55021401530996\n            ],\n            [\n              -122.4539566040039,\n              41.55021401530996\n            ],\n            [\n              -122.4539566040039,\n              41.48929196487705\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a522c","contributors":{"authors":[{"text":"Dong, Alex E.","contributorId":27476,"corporation":false,"usgs":true,"family":"Dong","given":"Alex","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":197089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beatty, Kenneth W.","contributorId":35362,"corporation":false,"usgs":true,"family":"Beatty","given":"Kenneth","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":197090,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Averett, Robert C.","contributorId":27500,"corporation":false,"usgs":true,"family":"Averett","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":197091,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68173,"text":"ha517 - 1974 - Ground water in Gray County, southwestern Kansas","interactions":[],"lastModifiedDate":"2017-02-13T16:27:34","indexId":"ha517","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"517","title":"Ground water in Gray County, southwestern Kansas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha517","usgsCitation":"McGovern, H.E., and Long, W., 1974, Ground water in Gray County, southwestern Kansas: U.S. Geological Survey Hydrologic Atlas 517, 2 Sheets: 31.5 x 29.0 in., https://doi.org/10.3133/ha517.","productDescription":"2 Sheets: 31.5 x 29.0 in.","costCenters":[],"links":[{"id":186051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89481,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/517/plate-1.pdf","text":"Sheet 1 of 2","linkFileType":{"id":1,"text":"pdf"}},{"id":89482,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/517/plate-2.pdf","text":"Sheet 2 of 2","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Kansas","county":"Gray County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-100.2272,37.915],[-100.2275,37.8284],[-100.2164,37.8281],[-100.217,37.4758],[-100.652,37.4757],[-100.6526,37.7364],[-100.6507,37.8285],[-100.6641,37.8296],[-100.6638,38.0005],[-100.2269,38.0007],[-100.2272,37.915]]]},\"properties\":{\"name\":\"Gray\",\"state\":\"KS\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db60","contributors":{"authors":[{"text":"McGovern, Harold E.","contributorId":9634,"corporation":false,"usgs":true,"family":"McGovern","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":277774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, W.A.","contributorId":46619,"corporation":false,"usgs":true,"family":"Long","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":277775,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12722,"text":"ofr74247 - 1974 - Saline ground-water resources of Lee County, Florida","interactions":[],"lastModifiedDate":"2024-06-26T19:06:36.76483","indexId":"ofr74247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-247","title":"Saline ground-water resources of Lee County, Florida","docAbstract":"<p>Lee County, an area of 786 square miles (1260 square kilometres) on the southwest coast of Florida, is underlain at depths greater than 400 feet (120 metres) by formations containing saline water. Two saline water-bearing zones occur within the depth interval 400 to 1,200 feet (120 to 370 metres); the upper zone is termed the lower Hawthorn aquifer and the lower zone is termed the Suwannee aquifer. Fresh water infiltrates into the aquifers in the central highlands region of Florida where water levels are as much as 130 feet (40 metres) above sea level. The water subsequently moves southwestward into the report area becoming progressively more saline toward the coast.</p><p>Both aquifers are under sufficient artesian pressure to cause wells tapping them to flow at land surface. Water levels range from more than 50 feet (15 metres) above sea level in the northeastern part of the county to about 30 feet (9 metres) or less along the coast. Artesian pressure in the aquifers has been reduced along the Caloosahatchee River by heavy withdrawal and this reduction in pressure is a major factor in deterioration of water quality in the McGregor Isles area, south of Fort Myers.</p><p>The average depth of wells tapping the lower Hawthorn aquifer is 572 feet (174 metres); the average depth of wells tapping both the lower Hawthorn and Suwannee aquifers is 858 feet (262 metres). Few wells tap only the Suwannee aquifer. The average length of casing in wells tapping the lower Hawthorn aquifer is 170 feet (52 metres), whereas the average length in wells tapping both aquifers is only 179 feet (55 metres). Flow rates range from 20 to 750 gallons per minute (1 to 47 litres per second) and average 233 gallons per minute (15 litres per second).</p><p>The saline water from the lower Hawthorn and Suwannee aquifers is hard and sulfurous. The dissolved solids, as determined from analyses of 31 samples,ranged from 700 to 3,300 mg/1 (milligrams per litre) and averaged 1,936 mg/1. The chloride concentrations ranged from 160 to 1,600 mg/1 and averaged 869 mg/l. The calcium magnesium hardness ranged from 110 to 1,000 mg/1 and averaged 625 mg/l. Sulfate concentrations ranged from 92 to 800 mg/1 and averaged 289 mg/l.</p><p>Although the mineral content is high, water from the lower Hawthorn and Suwannee aquifers has been used in the past for many purposes, particularly for irrigation. Currently, water from these aquifers may be used to supplement the dwindling supplies of better quality from aquifers at shallow depths.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74247","collaboration":"Prepared in cooperation with the Florida Department of Natural Resources and the County Commissioners of Lee County","usgsCitation":"Boggess, D.H., 1974, Saline ground-water resources of Lee County, Florida: U.S. Geological Survey Open-File Report 74-247, 62 p., https://doi.org/10.3133/ofr74247.","productDescription":"62 p.","costCenters":[],"links":[{"id":430531,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0247/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145742,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0247/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Lee County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.21444741315855,\n              26.78093390007551\n            ],\n            [\n              -82.21444741315855,\n              26.407624298567683\n            ],\n            [\n              -81.714569483471,\n              26.407624298567683\n            ],\n            [\n              -81.714569483471,\n              26.78093390007551\n            ],\n            [\n              -82.21444741315855,\n              26.78093390007551\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdfda","contributors":{"authors":[{"text":"Boggess, Durward Hoye","contributorId":13243,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"Hoye","affiliations":[],"preferred":false,"id":166601,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6506,"text":"pp772 - 1974 - Gold-bearing gravel of the ancestral Yuba River, Sierra Nevada, California","interactions":[],"lastModifiedDate":"2013-03-08T11:13:37","indexId":"pp772","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"772","title":"Gold-bearing gravel of the ancestral Yuba River, Sierra Nevada, California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp772","usgsCitation":"Yeend, W.E., 1974, Gold-bearing gravel of the ancestral Yuba River, Sierra Nevada, California: U.S. Geological Survey Professional Paper 772, 44 p., https://doi.org/10.3133/pp772.","productDescription":"44 p.","costCenters":[],"links":[{"id":140360,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0772/report-thumb.jpg"},{"id":268921,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0772/plate-2.pdf"},{"id":268351,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0772/report.pdf"},{"id":268352,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0772/plate-1.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49dc","contributors":{"authors":[{"text":"Yeend, Warren E.","contributorId":65053,"corporation":false,"usgs":true,"family":"Yeend","given":"Warren","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":152838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14458,"text":"ofr74129 - 1974 - Summary of activities, U.S. Geological Survey Saudi Arabian project, 1950 to 1974","interactions":[],"lastModifiedDate":"2024-02-16T22:10:36.002347","indexId":"ofr74129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-129","title":"Summary of activities, U.S. Geological Survey Saudi Arabian project, 1950 to 1974","docAbstract":"<p>The U. S. Geological Survey (USGS) first began work in the Kingdom of Saudi Arabia in 1950 under the sponsorship of the Ministry of Finance and National Economy. The basic objective of the work was to investigate the mineral and water resource potential in western Saudi Arabia, but little was known of the region and it therefore was necessary to prepare geographic and geologic maps. Aerial photographs were taken and controlled mosaics produced, some paid for by the USGS but most paid for by the Saudi Arabian government, and reconnaissance geologic mapping was undertaken until the USGS team left Saudi Arabia in 1955. This mapping, in cooperation with mapping of the Arabian American Oil Company, was compiled as a series of scale 1:500,000 geographic and geologic maps in Arabic and English covering all of Saudi Arabia. A total of 42 of these maps were prepared. Three scale 1:2,000,000 geographic and geologic maps in Arabic and English, covering the Arabian Peninsula, also were prepared from this work. All of the maps were printed in the United States and published by the USGS, the last in 1963.</p><p>Other work done by the USGS between 1950 and 1955 included locating and examining ancient mines, indentifying the Wadi Fatima oolitic iron deposit and other iron deposits in northwest Saudi Arabia, and advising on many water supply problems including those for Riyadh, Qizan, Qunfudhah, Rabigh, Yenbo, Umm Lejh, and Al Wajh. The mapping work and the geologic investigations laid the groundwork for the more detailed studies that followed.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74129","usgsCitation":"Kiilsgaard, T.H., 1974, Summary of activities, U.S. Geological Survey Saudi Arabian project, 1950 to 1974: U.S. Geological Survey Open-File Report 74-129, ii, 53 p., https://doi.org/10.3133/ofr74129.","productDescription":"ii, 53 p.","costCenters":[],"links":[{"id":425771,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149007,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0129/report-thumb.jpg"}],"country":"Kingdom of Saudi Arabia","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[42.77933,16.34789],[42.64957,16.77464],[42.34799,17.07581],[42.27089,17.47472],[41.75438,17.83305],[41.22139,18.6716],[40.93934,19.48649],[40.24765,20.17463],[39.80168,20.33886],[39.1394,21.2919],[39.0237,21.98688],[39.06633,22.57966],[38.49277,23.68845],[38.02386,24.07869],[37.48363,24.28549],[37.15482,24.85848],[37.20949,25.08454],[36.93163,25.60296],[36.6396,25.82623],[36.24914,26.57014],[35.64018,27.37652],[35.13019,28.06335],[34.63234,28.05855],[34.78778,28.60743],[34.83222,28.95748],[34.95604,29.35655],[36.06894,29.19749],[36.50121,29.50525],[36.74053,29.86528],[37.50358,30.00378],[37.66812,30.33867],[37.99885,30.5085],[37.00217,31.50841],[39.00489,32.01022],[39.19547,32.16101],[40.39999,31.88999],[41.88998,31.19001],[44.7095,29.17889],[46.56871,29.09903],[47.45982,29.00252],[47.70885,28.52606],[48.41609,28.552],[48.80759,27.68963],[49.29955,27.46122],[49.47091,27.11],[50.15242,26.68966],[50.21294,26.27703],[50.1133,25.94397],[50.23986,25.60805],[50.52739,25.32781],[50.66056,24.9999],[50.81011,24.75474],[51.11242,24.55633],[51.38961,24.62739],[51.57952,24.2455],[51.61771,24.01422],[52.00073,23.00115],[55.0068,22.49695],[55.20834,22.70833],[55.66666,22],[54.99998,19.99999],[52.00001,19],[49.11667,18.61667],[48.18334,18.16667],[47.46669,17.11668],[47,16.95],[46.74999,17.28334],[46.36666,17.23332],[45.4,17.33334],[45.21665,17.43333],[44.06261,17.41036],[43.79152,17.31998],[43.38079,17.57999],[43.1158,17.08844],[43.21838,16.66689],[42.77933,16.34789]]]},\"properties\":{\"name\":\"Saudi Arabia\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699503","contributors":{"authors":[{"text":"Kiilsgaard, Thor H.","contributorId":68738,"corporation":false,"usgs":true,"family":"Kiilsgaard","given":"Thor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":169491,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69507,"text":"hu16 - 1974 - Hydrologic Unit Map -- 1974, Kansas","interactions":[],"lastModifiedDate":"2014-07-16T12:49:12","indexId":"hu16","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"16","subseriesTitle":"Kansas 1974","title":"Hydrologic Unit Map -- 1974, Kansas","language":"ENGLISH","doi":"10.3133/hu16","isbn":"060776774X","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Hydrologic Unit Map -- 1974, Kansas: U.S. Geological Survey Hydrologic Unit 16, col. map 72 x 149 cm. fold. in envelope 30 x 24 cm.; An overprint of the 1:500,000-scale state base map. Shows counties, location, and names of all cities and towns and most of the smaller settlements, railroads, and township and range lines in black; water features in blue; hydrologic boundaries and codes in red; county codes in green. No contours. Sheet 31 by 60 inches., https://doi.org/10.3133/hu16.","productDescription":"col. map 72 x 149 cm. fold. in envelope 30 x 24 cm.; An overprint of the 1:500,000-scale state base map. Shows counties, location, and names of all cities and towns and most of the smaller settlements, railroads, and township and range lines in black; water features in blue; hydrologic boundaries and codes in red; county codes in green. No contours. Sheet 31 by 60 inches.","costCenters":[],"links":[{"id":191405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/hu/16/report-thumb.jpg"},{"id":290286,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/hu/16/plate-1.pdf"}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6143ff","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":534602,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6410,"text":"pp833 - 1974 - Computer model for determining bank storage at Hungry Horse Reservoir, northwestern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"pp833","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"833","title":"Computer model for determining bank storage at Hungry Horse Reservoir, northwestern Montana","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp833","usgsCitation":"Thompson, T.H., 1974, Computer model for determining bank storage at Hungry Horse Reservoir, northwestern Montana: U.S. Geological Survey Professional Paper 833, 16 p., https://doi.org/10.3133/pp833.","productDescription":"16 p.","costCenters":[],"links":[{"id":117803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0833/report-thumb.jpg"},{"id":33802,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0833/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a79c7","contributors":{"authors":[{"text":"Thompson, T. H.","contributorId":23927,"corporation":false,"usgs":true,"family":"Thompson","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":152672,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14476,"text":"ofr74187 - 1974 - Straight line fitting of an observation path by least normal squares","interactions":[],"lastModifiedDate":"2023-11-20T23:20:25.501826","indexId":"ofr74187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-187","title":"Straight line fitting of an observation path by least normal squares","docAbstract":"<p>In curtain hydro graphic problems, and perhaps in other geophysical problems, information must be collected as profiles along straight-line courses. When the inevitable deviations from perfect linearity occur, one must then find the straight line course that best approximates the actual observation path. Classical least squares (regression) does not solve this problem, because the line thus fitted depends upon which coordinate is taken as the dependent variable.</p><p>A coordinate-free solution is obtained by minimizing the sum of squares of normal distances between the line and the observation points. As in classical least squares, the line of best fit passes through the geometrical centroid of the observation points. The slope of this line, however, is closer to 1.0 than the slope of the classical regression line. The least normal squares and classical least squares solutions coincide when the observation path is nearly perfectly straight or when it runs generally parallel to one of the coordinate axes.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74187","usgsCitation":"Kirby, W.H., 1974, Straight line fitting of an observation path by least normal squares: U.S. Geological Survey Open-File Report 74-187, v, 11 p., https://doi.org/10.3133/ofr74187.","productDescription":"v, 11 p.","costCenters":[],"links":[{"id":422760,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0187/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147807,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0187/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b165e","contributors":{"authors":[{"text":"Kirby, William H.","contributorId":7294,"corporation":false,"usgs":true,"family":"Kirby","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":169520,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38998,"text":"pp352J - 1974 - Chemical weathering, soil development, and geochemical fractionation in a part of the White Mountains, Mono and Inyo counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:15","indexId":"pp352J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"352","chapter":"J","title":"Chemical weathering, soil development, and geochemical fractionation in a part of the White Mountains, Mono and Inyo counties, California","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Erosion and sedimentation in a semiarid environment","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp352J","usgsCitation":"Marchand, D.E., 1974, Chemical weathering, soil development, and geochemical fractionation in a part of the White Mountains, Mono and Inyo counties, California: U.S. Geological Survey Professional Paper 352, 45 p., https://doi.org/10.3133/pp352J.","productDescription":"45 p.","costCenters":[],"links":[{"id":120469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0352j/report-thumb.jpg"},{"id":66111,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0352j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e31e6","contributors":{"authors":[{"text":"Marchand, D. E.","contributorId":86004,"corporation":false,"usgs":true,"family":"Marchand","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":220786,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62375,"text":"gq1176 - 1974 - Surficial geologic map of the Framingham quadrangle, Middlesex and Worcester Counties, Massachusetts","interactions":[],"lastModifiedDate":"2015-10-01T11:52:35","indexId":"gq1176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"1176","title":"Surficial geologic map of the Framingham quadrangle, Middlesex and Worcester Counties, Massachusetts","docAbstract":"<p>The Framingham quadrangle covers about 55 square miles and is centered approximately 18 miles west of Boston. &nbsp;Even though the major topographic features are controlled by the lithology and structure of the bedrock, glacial features, such as drumlins, kames and kettles, kame terraces, eskers, gently sloping deltas, and flat-lying lake-bottom deposits, have modified the preglacial topography. &nbsp;Some bedrock plucking occurred, especially on the south or southeast sides of some hills, and some valleys probably were deepened. &nbsp;A thin veneer of till overlies much of the bedrock and is most extensive in the hills in the western half of the map area. &nbsp;These deposits, which are mostly gently sloping kame deltas or flat-lying lake-bottom deposits, were laid down in or graded to glacial Lakes Charles (Clapp, 1904, p. 198) and Sudbury (Goldthwait, 1905, p. 274), which formed during deglaciation when melt waters were temporarily impounded. &nbsp;Some glacial-lake deposits were laid down in three smaller higher level lakes in the western part of the quadrangle.</p>\n<p>With the exception of a small part of the southeast corner, which is drained by the Charles River, the quadrangle is drained by the Sudbury River, whose waters eventually flow into the Merrimack River in the northeast part of the state.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/gq1176","collaboration":"Prepared in coopartion with the Commonwealth of Massachusetts Department of Public Works","usgsCitation":"Nelson, A.E., 1974, Surficial geologic map of the Framingham quadrangle, Middlesex and Worcester Counties, Massachusetts: U.S. Geological Survey Geologic Quadrangle 1176, 1 Plate: 37.10 x 32.01 inches, https://doi.org/10.3133/gq1176.","productDescription":"1 Plate: 37.10 x 32.01 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309396,"rank":701,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gq/1176/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":248550,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1176/report.pdf","text":"Document","linkFileType":{"id":1,"text":"pdf"}},{"id":107609,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10715.htm","linkFileType":{"id":5,"text":"html"},"description":"10715"},{"id":253694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1176/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Middlesex County, Worcester County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.5,42.25 ], [ -71.5,42.3675 ], [ -71.36749999999999,42.3675 ], [ -71.36749999999999,42.25 ], [ -71.5,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688fcb","contributors":{"authors":[{"text":"Nelson, Arthur E.","contributorId":6035,"corporation":false,"usgs":true,"family":"Nelson","given":"Arthur","email":"","middleInitial":"E.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":267298,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46783,"text":"ofr7418 - 1974 - Geologic map of parts of the Louisville West and Lanesville quadrangles, Jefferson County, Kentucky","interactions":[{"subject":{"id":46783,"text":"ofr7418 - 1974 - Geologic map of parts of the Louisville West and Lanesville quadrangles, Jefferson County, Kentucky","indexId":"ofr7418","publicationYear":"1974","noYear":false,"title":"Geologic map of parts of the Louisville West and Lanesville quadrangles, Jefferson County, Kentucky"},"predicate":"SUPERSEDED_BY","object":{"id":62732,"text":"gq1202 - 1974 - Geologic map of parts of the Louisville West and Lanesville quadrangles, Jefferson County, Kentucky","indexId":"gq1202","publicationYear":"1974","noYear":false,"title":"Geologic map of parts of the Louisville West and Lanesville quadrangles, Jefferson County, Kentucky"},"id":1}],"supersededBy":{"id":62732,"text":"gq1202 - 1974 - Geologic map of parts of the Louisville West and Lanesville quadrangles, Jefferson County, Kentucky","indexId":"gq1202","publicationYear":"1974","noYear":false,"title":"Geologic map of parts of the Louisville West and Lanesville quadrangles, Jefferson County, Kentucky"},"lastModifiedDate":"2012-02-02T00:05:00","indexId":"ofr7418","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-18","title":"Geologic map of parts of the Louisville West and Lanesville quadrangles, Jefferson County, Kentucky","language":"ENGLISH","doi":"10.3133/ofr7418","usgsCitation":"Kepferle, R., 1974, Geologic map of parts of the Louisville West and Lanesville quadrangles, Jefferson County, Kentucky: U.S. Geological Survey Open-File Report 74-18, 1 map; scale = 1:24000, https://doi.org/10.3133/ofr7418.","productDescription":"1 map; scale = 1:24000","costCenters":[],"links":[{"id":135267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2714","contributors":{"authors":[{"text":"Kepferle, R.C.","contributorId":17588,"corporation":false,"usgs":true,"family":"Kepferle","given":"R.C.","affiliations":[],"preferred":false,"id":234053,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62153,"text":"gq1207 - 1974 - Geologic map of the Artemus quadrangle, Bell and Knox Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:28","indexId":"gq1207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"1207","title":"Geologic map of the Artemus quadrangle, Bell and Knox Counties, Kentucky","language":"ENGLISH","doi":"10.3133/gq1207","usgsCitation":"Rice, D.D., 1974, Geologic map of the Artemus quadrangle, Bell and Knox Counties, Kentucky: U.S. Geological Survey Geologic Quadrangle 1207, 1 map :col. ;58 x 19 cm., on sheet 79 x 92 cm., folded to 29 x 19 cm., https://doi.org/10.3133/gq1207.","productDescription":"1 map :col. ;58 x 19 cm., on sheet 79 x 92 cm., folded to 29 x 19 cm.","costCenters":[],"links":[{"id":107637,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10745.htm","linkFileType":{"id":5,"text":"html"},"description":"10745"},{"id":248344,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1207/report.pdf","size":"38","linkFileType":{"id":1,"text":"pdf"}},{"id":253239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1207/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.86749999999999,36.75 ], [ -83.86749999999999,36.8675 ], [ -83.75,36.8675 ], [ -83.75,36.75 ], [ -83.86749999999999,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b11e4b07f02db6a23d7","contributors":{"authors":[{"text":"Rice, Dudley D.","contributorId":11601,"corporation":false,"usgs":true,"family":"Rice","given":"Dudley","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":266995,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45964,"text":"ofr74232 - 1974 - Landslide susceptibility map of Oakdale 7 1/2-minute Quadrangle, Allegheny County and vicinity, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr74232","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-232","title":"Landslide susceptibility map of Oakdale 7 1/2-minute Quadrangle, Allegheny County and vicinity, Pennsylvania","language":"ENGLISH","doi":"10.3133/ofr74232","usgsCitation":"Pomeroy, J.S., 1974, Landslide susceptibility map of Oakdale 7 1/2-minute Quadrangle, Allegheny County and vicinity, Pennsylvania: U.S. Geological Survey Open-File Report 74-232, 1 map +1 booklet (16 leaves : 7 ill. ; 28 cm.) pasted on 1 sheet., https://doi.org/10.3133/ofr74232.","productDescription":"1 map +1 booklet (16 leaves : 7 ill. ; 28 cm.) pasted on 1 sheet.","costCenters":[],"links":[{"id":162071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0232/report-thumb.jpg"},{"id":82946,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0232/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82947,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0232/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab460","contributors":{"authors":[{"text":"Pomeroy, J. S.","contributorId":16807,"corporation":false,"usgs":true,"family":"Pomeroy","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":232380,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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