{"pageNumber":"343","pageRowStart":"8550","pageSize":"25","recordCount":11004,"records":[{"id":60340,"text":"mf1246I - 1985 - Maps showing distribution of tin in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T19:06:12.463908","indexId":"mf1246I","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"I","title":"Maps showing distribution of tin in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.</p><p>Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p><p><br></p><p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.</p><p>The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246I","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of tin in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 36.15 x 27.85 inches, https://doi.org/10.3133/mf1246I.","productDescription":"1 Plate: 36.15 x 27.85 inches","costCenters":[],"links":[{"id":182846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246i.jpg"},{"id":390901,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6853.htm"},{"id":283657,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-I/plate-1.pdf"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057ba","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263577,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60338,"text":"mf1246G - 1985 - Maps showing distribution of lead in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T19:01:20.256061","indexId":"mf1246G","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1985","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":"1246","chapter":"G","title":"Maps showing distribution of lead in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>These maps are part of a folio of maps of the Richfield 1° x 2 ° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.</p><p>Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p><p><br></p><p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.</p><p>The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of copper in two fractions of heavy-mineral concentrates of drainage sediments.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf1246G","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of lead in heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 36.38 x 27.85 inches, https://doi.org/10.3133/mf1246G.","productDescription":"1 Plate: 36.38 x 27.85 inches","costCenters":[],"links":[{"id":179800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246g.jpg"},{"id":283655,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-G/plate-1.pdf"},{"id":390898,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6851.htm"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605779","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263569,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263571,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30251,"text":"wri854064 - 1985 - Ground-water contamination in East Bay Township, Michigan","interactions":[],"lastModifiedDate":"2017-02-06T10:15:47","indexId":"wri854064","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4064","title":"Ground-water contamination in East Bay Township, Michigan","docAbstract":"<p>Glacial deposits, as much as 360 feet thick, underlie the study area. The upper 29 to 118 feet, a sand and gravel unit, is the aquifer tapped for water by all wells in the area. This unit is underlain by impermeable clay that is at least 100 feet thick. </p><p>Ground-water flow is northeastward at an estimated rate of 3 to 6 feet per day. Hydraulic conductivities in the aquifer range from 85 to 150 feet per day; 120 feet per day provided the best match of field data in a ground-water flow model. The depth to water ranged from 1 to 20 feet. </p><p>Chemical anlayses indicate that ground water is contaminated with organic chemicals from near the Hangar/Administration building at the U.S. Coast Guard Air Station to East Bay, about 4,300 feet northeast. The plume, which follows ground-water flow lines, ranges from 180 to 400 feet wide. In the upper reach of the plume, hydrocarbons less dense than water occur at the surface of the water table; they move downward in the aquifer as they move toward East Bay. Maximum concentrations of the major organic compounds include: benzene, 3,390 micrograms per liter; toluene, 55,500 micrograms per liter; xylene, 3,900 micrograms per liter; tetrachloroethylene, 3,410 micrograms per liter; and bis (2-ethyl hexyl) phthalate, 2,100 micrograms per liter. Soils are generally free of these hydrocarbons; however, in the vicinity of past drum storage, aircraft maintenance operations, and fuel storage and dispensing, as much as 1,100 micrograms per kilogram of tetrachloroethylene and 1,500 micrograms per kilogram of bis (2-ethyl hexyl) phthalate were detected. At a few locations higher molecular weight hydrocarbons, characteristic of petroleum distillates, were found.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri854064","collaboration":"Prepared in cooperation with the U.S. Coast Guard","usgsCitation":"Twenter, F.R., Cummings, T., and Grannemann, N., 1985, Ground-water contamination in East Bay Township, Michigan: U.S. Geological Survey Water-Resources Investigations Report 85-4064, Document: ix, 63 p.; 5 Plates: 23.24 x 35.59 inches or smaller, https://doi.org/10.3133/wri854064.","productDescription":"Document: ix, 63 p.; 5 Plates: 23.24 x 35.59 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":59038,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59039,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4064/report-thumb.jpg"},{"id":59040,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59041,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59042,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59043,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4064/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","otherGeospatial":"East Bay Township","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.57439804077148,\n              44.74164292754147\n            ],\n            [\n              -85.56602954864502,\n              44.75276788055599\n            ],\n            [\n              -85.5673599243164,\n              44.7531640722716\n            ],\n            [\n              -85.56911945343018,\n              44.753986923310066\n            ],\n            [\n              -85.57062149047852,\n              44.75490118850054\n            ],\n            [\n              -85.57225227355957,\n              44.75599828763615\n            ],\n            [\n              -85.57353973388672,\n              44.75706489182693\n            ],\n            [\n              -85.57529926300047,\n              44.7584971579133\n            ],\n            [\n              -85.57585716247559,\n              44.7592894600709\n            ],\n            [\n              -85.57611465454102,\n              44.760234113828844\n            ],\n            [\n              -85.58675765991211,\n              44.746885637908065\n            ],\n            [\n              -85.57439804077148,\n              44.74164292754147\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699997","contributors":{"authors":[{"text":"Twenter, F. R.","contributorId":81080,"corporation":false,"usgs":true,"family":"Twenter","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202934,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. R.","contributorId":104082,"corporation":false,"usgs":true,"family":"Cummings","given":"T. R.","affiliations":[],"preferred":false,"id":202935,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grannemann, N.G.","contributorId":11221,"corporation":false,"usgs":true,"family":"Grannemann","given":"N.G.","affiliations":[],"preferred":false,"id":202933,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2788,"text":"wsp2217 - 1985 - Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu","interactions":[{"subject":{"id":11397,"text":"ofr811119 - 1981 - Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu, with a section on flow hydraulics in dike tunnels in Hawaii","indexId":"ofr811119","publicationYear":"1981","noYear":false,"title":"Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu, with a section on flow hydraulics in dike tunnels in Hawaii"},"predicate":"SUPERSEDED_BY","object":{"id":2788,"text":"wsp2217 - 1985 - Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu","indexId":"wsp2217","publicationYear":"1985","noYear":false,"title":"Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu"},"id":1}],"lastModifiedDate":"2022-09-14T18:34:00.298716","indexId":"wsp2217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"2217","title":"Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu","docAbstract":"Ground-water reservoirs impounded by volcanic dikes receive a substantial part of the total recharge to ground water on the island of Oahu because they generally underlie the rainiest areas. These reservoirs accumulate the infiltration from rainfall, store it temporarily, and steadily leak it to abutting basal reservoirs or to streams cutting into them. The dike reservoirs have high hydraulic heads and are mostly isolated from saline water.\r\n\r\nThe most important and productive of the dike-impounded reservoirs are in an area of about 135 square miles in the main fissure zone of the Koolau volcano where the top of the dike-impounded water reaches an altitude of at least 1,000 feet. Water is impounded and stored both above and below sea level. The water stored above sea level in the 135 square mile area has been roughly estimated at 560 billion gallons. In comparison, the water stored above sea level in reservoirs underlying a dike-intruded area of about 53 square miles in the Waianae Range has been roughly estimated at 100 billion gallons. Storage below sea level is indeterminable, owing to uncertainties about the ability of the rock to store water as dike density increases and porosity decreases.\r\n\r\nTunnels, by breaching dike controls, have reduced the water stored above sea level by at least 50 billion gallons in the Koolau Range and by 5 1/2 billion gallons in the Waianae Range, only a small part of the total water stored.\r\n\r\nTotal leakage from storage in the Koolau Range has been estimated at about 280 Mgal/d (million gallons per day). This estimated leakage from the dike-impounded reservoirs makes up a significant part of the ground-water yield of the Koolau Range, which has been estimated to range from 450 to 580 Mgal/d. The largest unused surface leakage is in the Kaneohe, Kahana, and Punaluu areas, and the largest unused underflow occurs in the Waialee, Hauula-Laie, Punaluu, and Kahana areas. The unused underflow leakage is small in areas near and east of Waialae, but it is an important supply because of the great need for augmenting water supplies there.\r\n\r\nTotal leakage from storage in the Waianae Range has not been estimated because underflow is difficult to determine. Much of the surface leakage, about 4 Mgal/d in the upper parts of Waianae, Makaha, and Lualualei Valleys, has been diverted by tunnels. Hence, supplies available, other than surface leakage, cannot be estimated from the discharge end of the hydrologic cycle. Infiltration in the Waianae Range to dike-intruded reservoirs in the upper part of the valleys on the west (leeward) side has been estimated at about 20 Mgal/d, and on the east (windward) side, at about 10 Mgal/d. The available supply has been estimated at about 15 Mgal/d from the infiltration on the leeward side, of which about 4 Mgal/d is now being developed. No estimate has been made for the available supply on the windward side. Dike-intruded reservoirs at shallow depths west (lee side) of the crest are in upper Makaha, Waianae, and Lualualei Valleys. They are at moderate depths in upper Haleanu and in lower Kaukonahua Gulches on the east (windward) side.\r\n\r\nFlow hydraulics in dike tunnels is also discussed.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2217","usgsCitation":"Takasaki, K.J., and Mink, J.F., 1985, Evaluation of major dike-impounded ground-water reservoirs, Island of Oahu: U.S. Geological Survey Water Supply Paper 2217, vi, 77 p., https://doi.org/10.3133/wsp2217.","productDescription":"vi, 77 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":406706,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25463.htm","linkFileType":{"id":5,"text":"html"}},{"id":29268,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2217/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2217/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Oahu","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -158.31298828125,\n              21.21257979063059\n            ],\n            [\n              -157.60986328125,\n              21.21257979063059\n            ],\n            [\n              -157.60986328125,\n              21.70847301324597\n            ],\n            [\n              -158.31298828125,\n              21.70847301324597\n            ],\n            [\n              -158.31298828125,\n              21.21257979063059\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7274","contributors":{"authors":[{"text":"Takasaki, Kiyoshi J.","contributorId":105700,"corporation":false,"usgs":true,"family":"Takasaki","given":"Kiyoshi","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mink, John Francis","contributorId":48164,"corporation":false,"usgs":true,"family":"Mink","given":"John","email":"","middleInitial":"Francis","affiliations":[],"preferred":false,"id":145789,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44485,"text":"wri854019 - 1985 - Approximate potentiometric surface for the aquifer unit A2, Southeastern Coastal Plain aquifer system of the United States, prior to development","interactions":[],"lastModifiedDate":"2012-02-02T00:04:55","indexId":"wri854019","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4019","title":"Approximate potentiometric surface for the aquifer unit A2, Southeastern Coastal Plain aquifer system of the United States, prior to development","docAbstract":"A generalized potentiometric surface map prepared as part of the southeastern United States, Regional Sand Aquifer-System Analysis defines the altitude of water levels under conditions prior to development for aquifer unit A2, the upper group of aquifers in the sand aquifer system. Aquifer unit A2, consisting of lower Tertiary sands, is under artesian conditions except locally in the recharge areas. The regional flow direction is to the rivers in the area where the unit outcrops, west toward the Mississippi River in Mississippi, and southward to the Gulf of Mexico in Alabama and West Georgia. In eastern Georgia and South Carolina, the flow is southeast toward the Atlantic Ocean. (USGS)","language":"ENGLISH","doi":"10.3133/wri854019","usgsCitation":"Stricker, V., 1985, Approximate potentiometric surface for the aquifer unit A2, Southeastern Coastal Plain aquifer system of the United States, prior to development: U.S. Geological Survey Water-Resources Investigations Report 85-4019, 1 map : col ; 35 x 60 cm., on sheet 58 x 72 cm., https://doi.org/10.3133/wri854019.","productDescription":"1 map : col ; 35 x 60 cm., on sheet 58 x 72 cm.","costCenters":[],"links":[{"id":134665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4019/report-thumb.jpg"},{"id":81845,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a1ac","contributors":{"authors":[{"text":"Stricker, V.A.","contributorId":78703,"corporation":false,"usgs":true,"family":"Stricker","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":229860,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58669,"text":"mf1380E - 1985 - Mines and prospects map of the Glacier Peak Roadless Area, Snohomish County, Washington","interactions":[],"lastModifiedDate":"2018-10-03T12:49:26","indexId":"mf1380E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1380","chapter":"E","title":"Mines and prospects map of the Glacier Peak Roadless Area, Snohomish County, Washington","docAbstract":"<p>The Glacier Peak Roadless Area (fig. 1), covering 57,320 acres in the Cascade Range, is 50 mi northeast of Seattle, Wash.&nbsp; Over 4,000 claims have been located in or near the roadless area.&nbsp; One hundred ninety-six patented claims are in or within 1 mi of the area.&nbsp; Ore production from the roadless area is estimated to be about 280,000 tons, mainly gold-silver ore from seven mines in the Monte Cristo mining district.&nbsp; Of the 57,320 acres, about 2,100 acres are patented mining claims.&nbsp; The roadless area is bounded on the south and west by county roads and on the northeast by U.S. Forest Service roads.&nbsp; It is adjoined by the Glacier Peak Wilderness on the east.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1380E","isbn":"0607809876","usgsCitation":"Johnson, F.L., Denton, D., Iverson, S.R., McCulloch, R., Baker, S., and Stotelmeyer, R.B., 1985, Mines and prospects map of the Glacier Peak Roadless Area, Snohomish County, Washington: U.S. Geological Survey Miscellaneous Field Studies Map 1380, 2 Plates: 43.43 x 34.99 inches and 27.89 x 45.53 inches, https://doi.org/10.3133/mf1380E.","productDescription":"2 Plates: 43.43 x 34.99 inches and 27.89 x 45.53 inches","costCenters":[],"links":[{"id":183850,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1380-E/report-thumb.jpg"},{"id":358099,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1380-E/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358100,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1380-E/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Washington","county":"Snohomish County","otherGeospatial":"Glacier Peak Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.5,47.8675 ], [ -121.5,48.1175 ], [ -121.16805555555555,48.1175 ], [ -121.16805555555555,47.8675 ], [ -121.5,47.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e01","contributors":{"authors":[{"text":"Johnson, F. L.","contributorId":28236,"corporation":false,"usgs":true,"family":"Johnson","given":"F.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":260339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Denton, David K.","contributorId":108123,"corporation":false,"usgs":true,"family":"Denton","given":"David K.","affiliations":[],"preferred":false,"id":260341,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Iverson, Stephen R.","contributorId":73335,"corporation":false,"usgs":false,"family":"Iverson","given":"Stephen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":260340,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCulloch, R.B.","contributorId":67973,"corporation":false,"usgs":true,"family":"McCulloch","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":260343,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Baker, Steven 0000-0002-7250-6321","orcid":"https://orcid.org/0000-0002-7250-6321","contributorId":204985,"corporation":false,"usgs":true,"family":"Baker","given":"Steven","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":260344,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stotelmeyer, Ronald B.","contributorId":104051,"corporation":false,"usgs":true,"family":"Stotelmeyer","given":"Ronald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":260342,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":43032,"text":"ofr85167 - 1985 - Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon","interactions":[{"subject":{"id":43032,"text":"ofr85167 - 1985 - Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon","indexId":"ofr85167","publicationYear":"1985","noYear":false,"title":"Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":68212,"text":"ha696 - 1987 - Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon","indexId":"ha696","publicationYear":"1987","noYear":false,"title":"Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon"},"id":1}],"supersededBy":{"id":68212,"text":"ha696 - 1987 - Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon","indexId":"ha696","publicationYear":"1987","noYear":false,"title":"Solute distribution in ground and surface water in the Snake River Basin, Idaho and eastern Oregon"},"lastModifiedDate":"2025-02-04T15:55:07.925962","indexId":"ofr85167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-167","title":"Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85167","usgsCitation":"Low, W.H., 1985, Solute distribution in waters in the Snake River basin, Idaho and eastern Oregon: U.S. Geological Survey Open-File Report 85-167, 2 Sheets: 42.66 x 30.31 inches and 42.92 x 30.19 inches, https://doi.org/10.3133/ofr85167.","productDescription":"2 Sheets: 42.66 x 30.31 inches and 42.92 x 30.19 inches","costCenters":[],"links":[{"id":481664,"rank":2,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1985/0167/sheet-1.pdf","text":"Sheet 1","linkFileType":{"id":1,"text":"pdf"}},{"id":481665,"rank":3,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1985/0167/sheet-2.pdf","text":"Sheet 2","linkFileType":{"id":1,"text":"pdf"}},{"id":168474,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0167/report-thumb.jpg"}],"scale":"1000000","country":"United States","state":"Idaho, Oregon","otherGeospatial":"Snake River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124.44350530951343,\n              41.74876201297755\n            ],\n            [\n              -110.8748692680008,\n              41.81930230694928\n            ],\n            [\n              -110.9301365737104,\n              45.07345829172931\n            ],\n            [\n              -113.29828921312526,\n              45.01875982801852\n            ],\n            [\n              -114.23963602535332,\n              46.71316881650611\n            ],\n            [\n              -115.95601520351389,\n              49.158009080006195\n            ],\n            [\n              -117.23470852348288,\n              49.145436784766815\n            ],\n            [\n              -117.20750742851405,\n              46.17318965549089\n            ],\n            [\n              -124.31611684872718,\n              46.261807874145376\n            ],\n            [\n              -124.47999791747452,\n              41.82080483009614\n            ],\n            [\n              -124.44350530951343,\n              41.74876201297755\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5eda34","contributors":{"authors":[{"text":"Low, Walton H.","contributorId":92672,"corporation":false,"usgs":true,"family":"Low","given":"Walton","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":227605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58464,"text":"mf1737 - 1985 - Geologic section of the updip coastal plain from central Georgia to western South Carolina","interactions":[],"lastModifiedDate":"2021-10-26T16:16:33.462072","indexId":"mf1737","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1737","title":"Geologic section of the updip coastal plain from central Georgia to western South Carolina","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1737","isbn":"0607815647","usgsCitation":"Prowell, D.C., Christopher, R.A., Edwards, L.E., Bybell, L.M., and Gill, H.E., 1985, Geologic section of the updip coastal plain from central Georgia to western South Carolina: U.S. Geological Survey Miscellaneous Field Studies Map 1737, Report: 10 p.;1 Plate: 56.19 x 31.26 inches, https://doi.org/10.3133/mf1737.","productDescription":"Report: 10 p.;1 Plate: 56.19 x 31.26 inches","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":88374,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1985/1737/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185344,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1985/1737/report-thumb.jpg"},{"id":100684,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1985/1737/plate-1.pdf","size":"1489","linkFileType":{"id":1,"text":"pdf"}},{"id":106111,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7527.htm","linkFileType":{"id":5,"text":"html"},"description":"7527"}],"scale":"160000","country":"United States","state":"Georgia, South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.1884765625,\n              31.57853542647338\n            ],\n            [\n              -80.33203125,\n              31.57853542647338\n            ],\n            [\n              -80.33203125,\n              34.03445260967645\n            ],\n            [\n              -83.1884765625,\n              34.03445260967645\n            ],\n            [\n              -83.1884765625,\n              31.57853542647338\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6882e3","contributors":{"authors":[{"text":"Prowell, David C.","contributorId":46956,"corporation":false,"usgs":true,"family":"Prowell","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":259335,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christopher, Raymond A.","contributorId":29812,"corporation":false,"usgs":true,"family":"Christopher","given":"Raymond","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":259334,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":259331,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":259333,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gill, Harold E.","contributorId":91566,"corporation":false,"usgs":true,"family":"Gill","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":825752,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":15237,"text":"ofr85552 - 1985 - Sedimentation and water quality in the West Branch Shade River basin, Ohio, 1984 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:57","indexId":"ofr85552","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-552","title":"Sedimentation and water quality in the West Branch Shade River basin, Ohio, 1984 water year","docAbstract":"Sedimentation in, and flooding of, the West Branch Shade River and its tributaries have been major concerns of residents and State and local officials. The area was extensively surface mined for coal between the mid-1940 's and the early 1960's. Reclamation efforts immediately after mining were unsuccessful. The results have been elevated sediment loads and the subsequent loss of channel conveyance. Two sediment and stream gaging stations were established on West Branch Shade River in the area of past mining to provide data to evaluate the effectiveness of current reclamation activities on reducing sediment loads. A third station was established on the East Branch Shade River in an unmined area as a control. From October 1983 through September 1984, the annual suspended sediment yield/acre-ft of runoff was approximately two times as high for West Branch Shade River (0.51 ton/acre-ft of runoff) as for East Branch Shade River (0.28 ton/acre-ft). In addition, water quality of West Branch indicates that acidity is higher, pH is lower, and concentrations of dissolved sulfate and metals are higher than for East Branch. The concentration of coal in bed material increased in the downstream direction along West Branch Shade River. The concentration downstream in the West Branch was more than 20 times greater than in the East Branch. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85552","usgsCitation":"Childress, C., and Jones, R., 1985, Sedimentation and water quality in the West Branch Shade River basin, Ohio, 1984 water year: U.S. Geological Survey Open-File Report 85-552, iv, 26 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85552.","productDescription":"iv, 26 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0552/report-thumb.jpg"},{"id":44185,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0552/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5bf2","contributors":{"authors":[{"text":"Childress, C.J.","contributorId":88734,"corporation":false,"usgs":true,"family":"Childress","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":170795,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, R.L.","contributorId":39785,"corporation":false,"usgs":true,"family":"Jones","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":170794,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15236,"text":"ofr85187 - 1985 - Sediment and water-quality data for the West Branch Shade and East Branch Shade River basins, Ohio, 1983 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:57","indexId":"ofr85187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-187","title":"Sediment and water-quality data for the West Branch Shade and East Branch Shade River basins, Ohio, 1983 water year","docAbstract":"Sedimentation in and flooding of the West Branch Shade River and its tributaries have been major concerns of residents and State and local officials. The area was extensively surface mined for coal between the mid-1940's and the early 1960's. Reclamation efforts immediately after mining were unsuccessful. The results have been elevated sediment loads and the subsequent loss of channel conveyance.\r\n\r\nTwo sediment and stream-gaging stations were established on the West Branch Shade River and one station was established on the East Branch Shade River. These three stations will provide data to evalute the effectiveness of current reclamation activties on reducing sediment loads.\r\n\r\nFrom June Through September 1983, suspended-sediment yield was 18 times higher in West Branch (218 tons/mi2) than East Branch (12 tons/mi2) Shade River. In addition, acidity is higher, pH is lower, and concentrations of dissolved sulfate and metals are higher in the West Branch Shade River basin than in the East Branch Shade river basins.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85187","usgsCitation":"Childress, C., and Jones, R., 1985, Sediment and water-quality data for the West Branch Shade and East Branch Shade River basins, Ohio, 1983 water year: U.S. Geological Survey Open-File Report 85-187, iv, 20 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85187.","productDescription":"iv, 20 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0187/report-thumb.jpg"},{"id":44184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc108","contributors":{"authors":[{"text":"Childress, C.J.","contributorId":88734,"corporation":false,"usgs":true,"family":"Childress","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":170793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, R.L.","contributorId":39785,"corporation":false,"usgs":true,"family":"Jones","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":170792,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12402,"text":"ofr85293 - 1985 - Analytical results and sample locality map of stream-sediment and heavy-mineral-concentrate samples from the Chuckwalla Mountains Wilderness Study Area (CDCA-348), Riverside County, California","interactions":[],"lastModifiedDate":"2018-02-14T15:02:36","indexId":"ofr85293","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-293","title":"Analytical results and sample locality map of stream-sediment and heavy-mineral-concentrate samples from the Chuckwalla Mountains Wilderness Study Area (CDCA-348), Riverside County, California","docAbstract":"<p>In March 1982, we conducted a reconnaissance geochemical survey of the Chuckwalla Mountains Wilderness Study Area, Riverside County, California.</p><p>The Chuckwalla Mountains Wilderness Study Area comprises about 90 mi<sup>2</sup> (233 km) in the southeast corner of Riverside County, California, and lies just south of Interstate Highway 10 at Desert Center, California, which is approximately 180 mi east-southeast of Los Angeles (see figure 1)</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85293","usgsCitation":"Adrian, B.M., Day, G., and Watts, K.C., 1985, Analytical results and sample locality map of stream-sediment and heavy-mineral-concentrate samples from the Chuckwalla Mountains Wilderness Study Area (CDCA-348), Riverside County, California: U.S. Geological Survey Open-File Report 85-293, Report: 35 p.; 1 Plate: 31.92 x 27.48 inches, https://doi.org/10.3133/ofr85293.","productDescription":"Report: 35 p.; 1 Plate: 31.92 x 27.48 inches","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":40635,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0293/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of stream-sediment and heavy-mineral-concentrate sample sites, Chuckwalla Mountains Wilderness Study Area (CDCA-348), Riverside County, California"},{"id":40636,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0293/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0293/report-thumb.jpg"}],"country":"United States","state":"California","county":"Riverside County","otherGeospatial":"Chuckwalla Mountains Wilderness Study Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.6,\n              33.4\n            ],\n            [\n              -115,\n              33.4\n            ],\n            [\n              -115,\n             33.75\n            ],\n            [\n              -115.6,\n              33.75\n            ],\n            [\n              -115.6,\n              33.4\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67eca9","contributors":{"authors":[{"text":"Adrian, B. M.","contributorId":71535,"corporation":false,"usgs":true,"family":"Adrian","given":"B.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":166078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":166077,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Watts, K. C.","contributorId":49344,"corporation":false,"usgs":true,"family":"Watts","given":"K.","middleInitial":"C.","affiliations":[],"preferred":false,"id":166076,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60124,"text":"mf1287C - 1985 - Aeromagnetic map and selected aeroradiometric data for the Ellicott Rock Wilderness and additions, South Carolina, North Carolina, and Georgia","interactions":[],"lastModifiedDate":"2016-08-22T15:28:26","indexId":"mf1287C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1287","chapter":"C","title":"Aeromagnetic map and selected aeroradiometric data for the Ellicott Rock Wilderness and additions, South Carolina, North Carolina, and Georgia","docAbstract":"<p>The aeromagnetic and aeroradiometric data presented herin for the Ellicott Rock Wilderness and additions are taken from an airborne survey that covered a larger area in Georgia, North Carolina and South Carolina, and that was flown in December 1980 and January 1981 under contract to the U.S. Geological Survey. The flight lines were oriented northwest-southeast, approximately perpendicular to the general strike of the geology, at 0.5-mi (0.8-km) separation and at a nominal altitude of 500 ft (150 m) above mean terrain. A small amount of areomagnetic data from previous survey (Riggle and others, 1980) along the southeast edge of the study area is based on east-west flight lines spaced 1 mi (1.6 km) apart. Because of the rugged topography in the region, holding the airplane at a constant elevation abive the terrain was not possible. Actual ground clearance over short distances ranged between about 200 and 1200 ft. The International Geomagnetic Reference Field (IGRF) has been removed from the magnetic data (Barraclough and Fabiano, 1975) and 5000 gammas were added to make all values positive.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1287C","usgsCitation":"Luce, R.W., and Daniels, D.L., 1985, Aeromagnetic map and selected aeroradiometric data for the Ellicott Rock Wilderness and additions, South Carolina, North Carolina, and Georgia: U.S. Geological Survey Miscellaneous Field Studies Map 1287, 29.17 x 30.41 inches, https://doi.org/10.3133/mf1287C.","productDescription":"29.17 x 30.41 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180025,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1287C.PNG"},{"id":327326,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1287-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Georgia, North Carolina, South Carolina","otherGeospatial":"Ellicott Rock Wilderness Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.16666666666667,34.916666666666664 ], [ -83.16666666666667,35.034166666666664 ], [ -83.03416666666666,35.034166666666664 ], [ -83.03416666666666,34.916666666666664 ], [ -83.16666666666667,34.916666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6983b2","contributors":{"authors":[{"text":"Luce, Robert W.","contributorId":103685,"corporation":false,"usgs":true,"family":"Luce","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":263164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daniels, David L. 0000-0003-0599-8036 dave@usgs.gov","orcid":"https://orcid.org/0000-0003-0599-8036","contributorId":1792,"corporation":false,"usgs":true,"family":"Daniels","given":"David","email":"dave@usgs.gov","middleInitial":"L.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":263165,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3488,"text":"cir904B - 1985 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization","interactions":[{"subject":{"id":10982,"text":"ofr83699 - 1983 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization","indexId":"ofr83699","publicationYear":"1983","noYear":false,"title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization"},"predicate":"SUPERSEDED_BY","object":{"id":3488,"text":"cir904B - 1985 - Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization","indexId":"cir904B","publicationYear":"1985","noYear":false,"chapter":"B","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization"},"id":1}],"lastModifiedDate":"2019-11-07T12:09:52","indexId":"cir904B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"904","chapter":"B","title":"Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization","docAbstract":"<p>The geology and hydrology of the Basin and Range Province of the western conterminous United States are characterized in a series of data sets depicted in maps compiled for evaluation of prospective areas for further study of geohydrologic environments for isolation of high-level radioactive waste. The data sets include: (1) Average precipitation and evaporation; (2) surface distribution of selected rock types; (3) tectonic conditions; and (4) surface- and ground -water hydrology and Pleistocene lakes and marshes.</p><p>Rocks mapped for consideration as potential host media for the isolation of high-level radioactive waste are widespread and include argillaceous rocks, granitic rocks, tuffaceous rocks, mafic extrusive rocks, evaporites, and laharic breccias. The unsaturated zone, where probably as thick as 150 meters (500 feet), was mapped for consideration as an environment for isolation of high-level waste. Unsaturated rocks of various lithologic types are widespread in the Province.</p><p>Tectonic stability in the Quaternary Period is considered the key to assessing the probability of future tectonism with regard to high-level radioactive waste disposal. Tectonic conditions are characterized on the basis of the seismic record, heat-flow measurements, the occurrence of Quaternary faults, vertical crustal movement, and volcanic features. Tectonic activity, as indicated by seismicity, is greatest in areas bordering the western margin of the Province in Nevada and southern California, the eastern margin of the Province bordering the Wasatch Mountains in Utah and in parts of the Rio Grande valley. Late Cenozoic volcanic activity is widespread, being greatest bordering the Sierra Nevada in California and Oregon, and bordering the Wasatch Mountains in southern Utah and Idaho.</p><p>he arid to semiarid climate of the Province results in few perennial streams and lakes. A large part of the surface drainage is interior and the many closed basins commonly are occupied by playas or dry lake beds. The Province is divided into ground-water flow units defined on the basis of ground-water divides, ground-water flow lines, and surface streams that receive ground-water discharge.</p><p>Ground water contains less than 500 milligrams per liter of dissolved solids throughout most of the Province. Ground water is more mineralized in areas underlain by evaporitic rocks, overlain by playas, and near saline lakes. Ground water is of the calcium, magnesium, or sodium bicarbonate type in the areas where dissolved-solids concentrations are less than 500 milligrams per liter, and of the calcium, magnesium, or sodium sulfate or chloride type where dissolved-solids concentrations are greater than 500 milligrams per liter.</p><p>Geologic and hydrologic evidence is found for about 100 lakes and marshes that existed during the Pleistocene Epoch. The possibility of a recurrence of pluvial conditions, such as existed in the Pleistocene, is of concern in repository siting because of possible changes in hydrologic conditions. The Pleistocene lakes and marshes provide clues to the hydrology during pluvial climates.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir904B","usgsCitation":"Sargent, K., and Bedinger, M.S., 1985, Geologic and hydrologic characterization and evaluation of the Basin and Range Province relative to the disposal of high-level radioactive waste: Part II, Geologic and hydrologic characterization: U.S. Geological Survey Circular 904, iv, 30 p., https://doi.org/10.3133/cir904B.","productDescription":"iv, 30 p.","numberOfPages":"38","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":335935,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904C","text":"Circular 904-C","linkHelpText":"Part III, Geologic and hydrologic evaluation"},{"id":335934,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir904A","text":"Circular 904-A","linkHelpText":"Part I, Introduction and guidelines"},{"id":30497,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0904b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0904b/report-thumb.jpg"}],"country":"United States","state":"Arizona, California, Idaho, Nevada, New Mexico, Oregon, Texas","otherGeospatial":"Basin and Range Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.6640625,\n              32.65787573695528\n            ],\n            [\n              -114.6533203125,\n              32.80574473290688\n            ],\n            [\n    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      ],\n            [\n              -116.93847656250001,\n              36.29741818650811\n            ],\n            [\n              -118.19091796875,\n              35.02999636902566\n            ],\n            [\n              -116.08154296875001,\n              34.27083595165\n            ],\n            [\n              -115.6640625,\n              32.65787573695528\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publicComments":"This is Part II of a series of reports being prepared by the U.S. Geological Survey in consultation with States in the Basin and Range Province.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a821e","contributors":{"authors":[{"text":"Sargent, Kenneth A.","contributorId":15998,"corporation":false,"usgs":true,"family":"Sargent","given":"Kenneth A.","affiliations":[],"preferred":false,"id":147018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":147019,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44482,"text":"wri844364 - 1985 - Approximate potentiometric surface for the aquifer unit A4, southeastern coastal plain aquifer system of the United States, prior to development","interactions":[],"lastModifiedDate":"2012-02-02T00:04:55","indexId":"wri844364","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4364","title":"Approximate potentiometric surface for the aquifer unit A4, southeastern coastal plain aquifer system of the United States, prior to development","docAbstract":"A generalized potentiometric surface map prepared as part of a regional analysis of sand aquifer system defines the altitude of water levels under pre-development conditions for aquifer unit A4, the lowermost group of aquifers in the sand aquifer system. Aquifer unit A4, consisting of Upper and Lower Cretaceous sands, is under artesian conditions except locally in the recharge areas. The regional flow direction is to the rivers in the area where the unit outcrops and southward to the Gulf of Mexico in Mississippi, Alabama, and West Georgia. In coastal Georgia and South Carolina, the direction of flow is east northeast parallel to the coast and into North Carolina. (USGS)","language":"ENGLISH","doi":"10.3133/wri844364","usgsCitation":"Stricker, V., Aucott, W.R., Faye, R.E., Williams, J.S., and Mallory, M.J., 1985, Approximate potentiometric surface for the aquifer unit A4, southeastern coastal plain aquifer system of the United States, prior to development: U.S. Geological Survey Water-Resources Investigations Report 84-4364, 1 map : col. ; 35 x 60 cm., on sheet 58 x 72 cm. , https://doi.org/10.3133/wri844364.","productDescription":"1 map : col. ; 35 x 60 cm., on sheet 58 x 72 cm. ","costCenters":[],"links":[{"id":134644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81840,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4364/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a1ba","contributors":{"authors":[{"text":"Stricker, V.A.","contributorId":78703,"corporation":false,"usgs":true,"family":"Stricker","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":229854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aucott, Walter R.","contributorId":90275,"corporation":false,"usgs":true,"family":"Aucott","given":"Walter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":229855,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Faye, Robert E.","contributorId":92221,"corporation":false,"usgs":true,"family":"Faye","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229856,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, John S. johnw@usgs.gov","contributorId":329,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"johnw@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":229852,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mallory, Michael J.","contributorId":59408,"corporation":false,"usgs":true,"family":"Mallory","given":"Michael","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229853,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":60909,"text":"mf1626C - 1985 - Geochemical survey of the Devil's Den Roadless Area, Rutland and Windsor counties, Vermont","interactions":[],"lastModifiedDate":"2016-08-23T09:27:03","indexId":"mf1626C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1626","chapter":"C","title":"Geochemical survey of the Devil's Den Roadless Area, Rutland and Windsor counties, Vermont","docAbstract":"<p>The Devils Den Roadless Area comprises 8,830 acres of mountainous terrane in the Green Mountain National Forest, Rutland and Windsor Counties, Vt. (Index Map). Ludlow, the nearest large community, is approximately 7 air miles northeast of the study area. The small villages of Weston and East Wallingford are 3 to 5 mi to the south and north, respectively. Total relief is nearly 1,200 ft, ranging from a low elevation of 1,640 ft along the southwestern edge of the area, to a high point of about 2,860 ft in the northwest portion. Principal access is provided by state Route 100 and 155 on the southeast and northeast, and by Forest Service Road 10 along the western boundary. Old logging roads and foot trails allow entry to the interior of the study area. Several swamps and one small pond are located in topographically low areas. Drainage is principally to the south and southeast by tributaries of the south-flowing West River, ultimately discharging into the Connecticut River near Brattleboro.</p>\n<p>The Devils Den area is named for a large undercut cliff (Dale, 1915, p. 21) developed in Precambrian basement rocks. This undercut cliff forms a broad natural cave immediately west of and below Forest Service Road 10, at the head of Mt. Tabor Brook. Another much smaller cave is present in dolomite of probable Paleozoic (Early Cambrian) age on the east side of the same road. This smaller cave apparently is of artificial origin, having been made during early mining of the dolomite (Dale, 1915, p. 21). This man-made cave is the only evidence of previous mining activity within the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1626C","isbn":"0607814357","usgsCitation":"Slack, J.F., Atelsek, P., and Grosz, A.E., 1985, Geochemical survey of the Devil's Den Roadless Area, Rutland and Windsor counties, Vermont: U.S. Geological Survey Miscellaneous Field Studies Map 1626, Plate: 55.23 x 42.09 inches, https://doi.org/10.3133/mf1626C.","productDescription":"Plate: 55.23 x 42.09 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326357,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1626C.JPG"},{"id":327489,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1626-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Vermont","county":"Rutland County, Windsor County","otherGeospatial":"Devil's Den Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.91805555555555,43.301111111111105 ], [ -72.91805555555555,43.38472222222222 ], [ -72.80111111111111,43.38472222222222 ], [ -72.80111111111111,43.301111111111105 ], [ -72.91805555555555,43.301111111111105 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abaa3","contributors":{"authors":[{"text":"Slack, J. F.","contributorId":75917,"corporation":false,"usgs":true,"family":"Slack","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":264597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atelsek, P.J.","contributorId":104069,"corporation":false,"usgs":true,"family":"Atelsek","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":264599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grosz, A. E.","contributorId":87925,"corporation":false,"usgs":true,"family":"Grosz","given":"A.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":264598,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25413,"text":"wri844314 - 1985 - Chemical and isotopic characteristics of brines from three oil- and gas-producing sandstones in eastern Ohio, with applications to the geochemical tracing of brine sources","interactions":[],"lastModifiedDate":"2022-02-14T21:24:14.271237","indexId":"wri844314","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4314","title":"Chemical and isotopic characteristics of brines from three oil- and gas-producing sandstones in eastern Ohio, with applications to the geochemical tracing of brine sources","docAbstract":"Chemical and isotopic characteristics of selected inorganic constituents are reported for brines from the Berea Sandstone of Mississippian age, the Clinton sandstone, Albion Sandstone of Silurian age, and the Rose Run formation of Cambrian and Ordovician age in 24 counties in eastern Ohio. Ionic concentrations of dissolved constituents in brines from these formations generally fall in the following ranges (in millimoles per kilogram of brine): Na, Cl &gt; 1,000; 100 &lt; Ca, Mg &lt; 1,000; 1 &lt; K, Br, Sr, Li, Fe, SO4 &lt; 100; Mn, Zn, Al, I, HCO3, SiO2 &lt; 1. Mean ionic concentrations of Ca, Mg, Na, Cl, K, SO4 and Br, and mean values of density and dissolved solids are significantly different at the 95-percent confidence level in each formation. Only potassium has a unique concentration range in each formation. Selected concentration ratios are identified as potential indicators for geochemical tracing of brines having some history of dilution. The k:Na ratios work best for identifying the source formation of an unidentified brine. Isotopic characteristics of hydrogen and oxygen indicate a meteoric origin for the water matrix of the brines. Sulfur isotopes may have utility for differentiating brines from oxidizing ground water.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri844314","collaboration":"Prepared in cooperation with the Ohio Department of Natural Resources, Division of Oil and Gas","usgsCitation":"Breen, K.J., Angelo, C.G., Masters, R.W., and Sedam, A.C., 1985, Chemical and isotopic characteristics of brines from three oil- and gas-producing sandstones in eastern Ohio, with applications to the geochemical tracing of brine sources (Version 1.1): U.S. Geological Survey Water-Resources Investigations Report 84-4314, v, 58 p., https://doi.org/10.3133/wri844314.","productDescription":"v, 58 p.","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":395945,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36155.htm"},{"id":277993,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/1984/4314/"},{"id":123971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4314/report-thumb.jpg"}],"country":"United States","state":"Ohio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.083,\n              38.667\n            ],\n            [\n              -80.517,\n              38.667\n            ],\n            [\n              -80.517,\n              41.978\n            ],\n            [\n              -83.083,\n              41.978\n            ],\n            [\n              -83.083,\n              38.667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4858","contributors":{"authors":[{"text":"Breen, K. J.","contributorId":44176,"corporation":false,"usgs":true,"family":"Breen","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":193582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Angelo, Clifford G.","contributorId":48596,"corporation":false,"usgs":true,"family":"Angelo","given":"Clifford","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":193583,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Masters, Robert W.","contributorId":32195,"corporation":false,"usgs":true,"family":"Masters","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":193581,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sedam, Alan C.","contributorId":9300,"corporation":false,"usgs":true,"family":"Sedam","given":"Alan","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":193580,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26511,"text":"wri854003 - 1985 - Transit losses and traveltimes for reservoir releases during drought conditions along the Neosho River from Council Grove Lake to Iola, east-central Kansas","interactions":[],"lastModifiedDate":"2021-11-02T21:23:29.205216","indexId":"wri854003","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4003","title":"Transit losses and traveltimes for reservoir releases during drought conditions along the Neosho River from Council Grove Lake to Iola, east-central Kansas","docAbstract":"Knowledge of the transit losses and water-wave traveltimes in the Neosho River for varying reservoir-release volumes and durations is necessary for proper management of water supply. Two reaches were studied along the Neosho River in east-central Kansas. The upper reach is from Council Grove Lake to John Redmond Reservoir, a distance of 83.0 river miles. The lower reach is from John Redmond Reservoir to Iola, Kansas, a distance of 56.3 river miles. Channel and aquifer characteristics were estimated from available data and used in a streamflow routing model. These estimated characteristics were verified using the model by comparing simulated reservoir releases to observed reservoir releases. The verified model then was used to simulate transit losses (or gains) and traveltimes for selected reservoir release volumes and durations from Council Grove Lake to Iola. Transit losses and traveltimes were investigated for the selected reservoir releases while under a severe drought antecedent streamflow condition (zero base flow) and a less severe drought antecedent streamflow condition (2% drought base flows). The largest total transit loss from Council Grove Lake to Iola occurred during the severe drought antecedent streamflow condition, small reservoir release rates, and long reservoir release durations. The total transit loss included water that was temporarily lost to bank storage. For a severe drought condition, transit losses ranged from 1,100 acre-ft for a release volume of 1,840 acre-ft for a duration of 50 days to 6 ,280 acre-ft for a release volume of 6,280 acre-ft for a duration of 365 days. For a less severe drought condition, transit losses ranged from 860 acre-ft to 3,234 acre-ft for the same release volumes and durations as for the severe drought condition. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854003","usgsCitation":"Carswell, W., and Hart, R.J., 1985, Transit losses and traveltimes for reservoir releases during drought conditions along the Neosho River from Council Grove Lake to Iola, east-central Kansas: U.S. Geological Survey Water-Resources Investigations Report 85-4003, vi, 40 p., https://doi.org/10.3133/wri854003.","productDescription":"vi, 40 p.","costCenters":[],"links":[{"id":391291,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36202.htm"},{"id":55381,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4003/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157854,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4003/report-thumb.jpg"}],"country":"United States","state":"Kansas","city":"Iola","otherGeospatial":"Council Grove Lake, Neosho River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.5,\n              37.829\n            ],\n            [\n              -95.383,\n              37.829\n            ],\n            [\n              -95.383,\n              38.705\n            ],\n            [\n              -96.5,\n              38.705\n            ],\n            [\n              -96.5,\n              37.829\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0b38","contributors":{"authors":[{"text":"Carswell, W. J.","contributorId":71213,"corporation":false,"usgs":true,"family":"Carswell","given":"W. J.","affiliations":[],"preferred":false,"id":196519,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, R. J.","contributorId":62607,"corporation":false,"usgs":true,"family":"Hart","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":196518,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60342,"text":"mf1246K - 1985 - Maps showing distribution of zinc in heavy-mineral concentrates, Richfield 1° by 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2019-06-11T12:31:17","indexId":"mf1246K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1246","chapter":"K","title":"Maps showing distribution of zinc in heavy-mineral concentrates, Richfield 1° by 2° quadrangle, Utah","docAbstract":"<p>These maps are part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Coterminous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.</p><p>Located in west-central Utah, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale igneous mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p><p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related instrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in middle and late Cenozoic time.</p><p>The regional sampling program was designed to define broad geochemical patterns and trends which can be utilized along with geologic and geophysical data to assess the mineral resource potential for this quadrangle. These maps of the Richfield 1° x 2° quadrangle show the regional distributions of zinc in two fractions of heavy-mineral concentrates of drainage sediments.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1246K","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of zinc in heavy-mineral concentrates, Richfield 1° by 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, Plate: 35.92 x 27.30 in., https://doi.org/10.3133/mf1246K.","productDescription":"Plate: 35.92 x 27.30 in.","costCenters":[],"links":[{"id":364157,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-K/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":" https://pubs.usgs.gov/mf1246K/report-thumb.jpg"}],"scale":"500000","country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057c3","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263581,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263583,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60336,"text":"mf1246E - 1985 - Maps showing distribution of bismuth in heavy-mineral concentrates, Richfield 1 degree by 2 degrees Quadrangle, Utah","interactions":[],"lastModifiedDate":"2016-08-23T08:01:45","indexId":"mf1246E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1246","chapter":"E","title":"Maps showing distribution of bismuth in heavy-mineral concentrates, Richfield 1 degree by 2 degrees Quadrangle, Utah","docAbstract":"<p><span>These maps are part of a folio of maps of the&nbsp;Richfield 1<sup>o</sup><span class=\"apple-converted-space\">&nbsp;</span>x 2<sup>o</sup><span class=\"apple-converted-space\">&nbsp;</span>quadrangle, Utach, prepared under the Conterminous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.&nbsp;</span></p>\n<p><span>Located in west-central Utach, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale ingeous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.&nbsp;</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1246E","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of bismuth in heavy-mineral concentrates, Richfield 1 degree by 2 degrees Quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 35.79 x 27.62 inches, https://doi.org/10.3133/mf1246E.","productDescription":"35.79 x 27.62 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246E.PNG"},{"id":327373,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-E/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,38 ], [ -114,39 ], [ -112,39 ], [ -112,38 ], [ -114,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6056fc","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263563,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263564,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60335,"text":"mf1246D - 1985 - Maps showing distribution of beryllium in heavy-mineral concentrates and stream sediments, Richfield 1 degree by 2 degrees Quadrangle, Utah","interactions":[],"lastModifiedDate":"2016-08-23T08:02:40","indexId":"mf1246D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1246","chapter":"D","title":"Maps showing distribution of beryllium in heavy-mineral concentrates and stream sediments, Richfield 1 degree by 2 degrees Quadrangle, Utah","docAbstract":"<p><span>These maps are part of a folio of maps of the&nbsp;Richfield 1<sup>o</sup><span class=\"apple-converted-space\">&nbsp;</span>x 2<sup>o</sup><span class=\"apple-converted-space\">&nbsp;</span>quadrangle, Utach, prepared under the Conterminous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.&nbsp;</span></p>\n<p><span>Located in west-central Utach, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale ingeous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.&nbsp;</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1246D","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of beryllium in heavy-mineral concentrates and stream sediments, Richfield 1 degree by 2 degrees Quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 41.53 x 27.85 inches, https://doi.org/10.3133/mf1246D.","productDescription":"41.53 x 27.85 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246D.PNG"},{"id":327374,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-D/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,38 ], [ -114,39 ], [ -112,39 ], [ -112,38 ], [ -114,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6056f6","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263560,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263561,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60334,"text":"mf1246C - 1985 - Maps showing distribution of barium in heavy-mineral concentrates, Richfield 1 degree by 2 degrees Quadrangle, Utah","interactions":[],"lastModifiedDate":"2016-08-24T08:11:13","indexId":"mf1246C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1246","chapter":"C","title":"Maps showing distribution of barium in heavy-mineral concentrates, Richfield 1 degree by 2 degrees Quadrangle, Utah","docAbstract":"<p><span>These maps are part of a folio of maps of the&nbsp;Richfield 1<sup>o</sup><span class=\"apple-converted-space\">&nbsp;</span>x 2<sup>o</sup><span class=\"apple-converted-space\">&nbsp;</span>quadrangle, Utach, prepared under the Conterminous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.&nbsp;</span></p>\n<p><span>Located in west-central Utach, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale ingeous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.&nbsp;</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1246C","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of barium in heavy-mineral concentrates, Richfield 1 degree by 2 degrees Quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 36.16 x 27.55 inches, https://doi.org/10.3133/mf1246C.","productDescription":"36.16 x 27.55 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246C.PNG"},{"id":327764,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,38 ], [ -114,39 ], [ -112,39 ], [ -112,38 ], [ -114,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6056d5","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263557,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263558,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60333,"text":"mf1246B - 1985 - Maps showing distribution of Arsenic in heavy-mineral concentrates, Richfield 1 degree by 2 degrees Quadrangle, Utah","interactions":[],"lastModifiedDate":"2016-08-22T15:52:15","indexId":"mf1246B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1246","chapter":"B","title":"Maps showing distribution of Arsenic in heavy-mineral concentrates, Richfield 1 degree by 2 degrees Quadrangle, Utah","docAbstract":"<p>These maps are part of a folio of maps of the&nbsp;Richfield 1<sup>o</sup> x 2<sup>o</sup> quadrangle, Utach, prepared under the Conterminous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.&nbsp;</p>\n<p>Located in west-central Utach, the Richfield quadrangle covers the eastern part of the Plioche-Marysvale ingeous and mineral belt, which extends from the vicinity of Plioche in southeastern Nevada east-northeastward for 250 km (155 mi) into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range province and the eastern third is in the High Plateaus of Utah, a subprovince of the Colorado Plateau.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1246B","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1985, Maps showing distribution of Arsenic in heavy-mineral concentrates, Richfield 1 degree by 2 degrees Quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 35.91 x 27.43 inches, https://doi.org/10.3133/mf1246B.","productDescription":"35.91 x 27.43 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246B.PNG"},{"id":327354,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,38 ], [ -114,39 ], [ -112,39 ], [ -112,38 ], [ -114,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604f20","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263554,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263555,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44480,"text":"wri844360 - 1985 - Ground-water levels in the Columbia River basalt and overlying materials, spring 1983, southeastern Washington","interactions":[],"lastModifiedDate":"2022-05-19T18:40:18.783766","indexId":"wri844360","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4360","title":"Ground-water levels in the Columbia River basalt and overlying materials, spring 1983, southeastern Washington","docAbstract":"A 2 1/2-year study of the Columbia Plateau in Washington was begun in March 1982 to define spatial and temporal variations in dissolved sodium in aquifers of the Columbia River Basalt Group and to relate these variations to the groundwater system and its geologic framework. This report is part of that study and describes groundwater level contours for four major geohydrologic units in southeastern Washington, constructed from water-level data collected from approximately 1,100 wells during the spring of 1983, data from U.S. Geological Survey studies in the area, and other indirect methods. Configuration of the groundwater level contours is controlled by: (1) extent of a geohydrologic unit and geologic structure, (2) recharge from precipitation and surface water bodies, (3) rivers, lakes, and coulees that drain the groundwater system, and (4) hydraulic conductivities of each unit. Upgradient flexures of water level contours north of Connel, Washington, show effects of prolonged irrigation while downgradient flexures in an area south of Potholes Reservoir, in the vicinity of the East Low Irrigation Canal, show the effects of increased man-induced recharge. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844360","usgsCitation":"Bauer, H.H., Vaccaro, J.J., and Lane, R.C., 1985, Ground-water levels in the Columbia River basalt and overlying materials, spring 1983, southeastern Washington: U.S. Geological Survey Water-Resources Investigations Report 84-4360, 4 Plates: 44.10 × 29.00 inches or smaller, https://doi.org/10.3133/wri844360.","productDescription":"4 Plates: 44.10 × 29.00 inches or smaller","costCenters":[],"links":[{"id":134642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":400826,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36191.htm"},{"id":81838,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81837,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81836,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81835,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4360/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Washington","otherGeospatial":"Columbia River basalt","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              45.603\n            ],\n            [\n              -116.903,\n              45.603\n            ],\n            [\n              -116.903,\n              48.2440\n            ],\n            [\n              -121,\n              48.2440\n            ],\n            [\n              -121,\n              45.603\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a384e","contributors":{"authors":[{"text":"Bauer, H. H.","contributorId":85142,"corporation":false,"usgs":true,"family":"Bauer","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":229850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vaccaro, John J. jvaccaro@usgs.gov","contributorId":5848,"corporation":false,"usgs":true,"family":"Vaccaro","given":"John","email":"jvaccaro@usgs.gov","middleInitial":"J.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":229848,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, R. C.","contributorId":6421,"corporation":false,"usgs":true,"family":"Lane","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":229849,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28232,"text":"wri854155 - 1985 - A preliminary assessment of land-surface subsidence in the El Paso area, Texas","interactions":[],"lastModifiedDate":"2018-10-30T12:49:42","indexId":"wri854155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4155","title":"A preliminary assessment of land-surface subsidence in the El Paso area, Texas","docAbstract":"<p>The northeast and southeast parts of the El Paso area are underlain by Hueco bolson deposits as much as 9,000 feet thick. The deposits consist of lenses of gravel, sand, silt, and clay. In the Rio Grande Valley, about 400 to 450 feet of these deposits have been eroded and replaced with as much as 200 feet of alluvium. Ground water in the shallow alluvial aquifer in the Rio Grande Valley and in the Hueco bolson aquifer outside the valley is under water-table conditions, whereas ground water in the bolson aquifer in the valley is under leaky artesian conditions. Maximum water-level declines in the Hueco bolson aquifer are 110 feet east of the Franklin Mountains and 150 feet in the downtown El Paso area. For the shallow aquifer, the maximum declines have been 125 feet in the downtown area. Compressable materials in the freshwater zone of the aquifer range from 50 to 450 feet.</p>\n<p>Recharge from the Rio Grande to the shallow alluvial aquifer has increased from an estimated 15,000 acre-feet during 1968 to 30,000 acre-feet during 1983, an increase of about 1,000 acre-feet per year. Leakage from the Rio Grande is expected to continually increase in the near future because of a continued decline in ground-water levels. The amount of leakages from the canals is much less than from the river.</p>\n<p>Releveling of bench marks along lines to the northeast and the southeast of the Rio Grande, and along its channel commonly show land subsidence of about 0.2 foot. The maximum measured subsidence is 0.41 foot along the river in the Chamizal zone. No subsidence was detected at the Riverside Diversion Dam. A comparison of subsidence, water-level declines, and clay thickness along the three survey lines shows the expected correlation of greater subsidence with thicker accumulated clay material for a given decline in water levels. The preconsolidation stress was expected to range from 85 to 115 feet of water-level decline on the basis of subsidence studies in Arizona and California. A study of specific-unit compaction along the three survey lines shows that the values usually range between 1.0 to 2.5 x 10-5 feet per feet squared. These values are comparable to the ones computed in the Tulare-Wasco, California, and Houston-Galveston, Texas, areas following the exceedance of the local preconsolidation stress. Because of this comparability, the specific-unit compaction for future periods in the El Paso area probably will not increase dramatically when the preconsolidation stress is exceeded, if it has not already been exceeded.</p>\n<p>In addition to regional subsidence, local subsidence is indicated by observable surface fractures but has not been verified by precise leveling. These local areas coincide with areas that historically were swamps along the Rio Grande.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri854155","collaboration":"Prepared in cooperation with the Bureau of Reclamation","usgsCitation":"Land, L.F., and Armstrong, C.A., 1985, A preliminary assessment of land-surface subsidence in the El Paso area, Texas: U.S. Geological Survey Water-Resources Investigations Report 85-4155, vi, 96 p., https://doi.org/10.3133/wri854155.","productDescription":"vi, 96 p.","numberOfPages":"108","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":57062,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4155/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4155/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"El Paso","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.32293701171874,\n              31.647536225797772\n            ],\n            [\n              -106.35314941406249,\n              31.701882151861714\n            ],\n            [\n              -106.37443542480469,\n              31.71122878128754\n            ],\n            [\n              -106.38198852539062,\n              31.73400724374667\n            ],\n            [\n              -106.45271301269531,\n              31.764369817056387\n            ],\n            [\n              -106.468505859375,\n              31.76145077153307\n            ],\n            [\n              -106.47468566894531,\n              31.750941445321764\n            ],\n            [\n              -106.48773193359375,\n              31.74918977495709\n            ],\n            [\n              -106.50421142578125,\n              31.756780107186728\n            ],\n            [\n              -106.51588439941406,\n              31.770791393089315\n            ],\n            [\n              -106.52961730957031,\n              31.783633207994736\n            ],\n            [\n              -106.53648376464844,\n              31.94633593313394\n            ],\n            [\n              -106.32980346679686,\n              31.94808386339691\n            ],\n            [\n              -106.32293701171874,\n              31.647536225797772\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aaf25","contributors":{"authors":[{"text":"Land, L. F.","contributorId":17253,"corporation":false,"usgs":true,"family":"Land","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199434,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27260,"text":"wri844315 - 1985 - Estimated water and nutrient inflows and outflows Lake Cochituate, eastern Massachusetts, 1977-79","interactions":[],"lastModifiedDate":"2022-02-16T20:37:17.448552","indexId":"wri844315","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4315","title":"Estimated water and nutrient inflows and outflows Lake Cochituate, eastern Massachusetts, 1977-79","docAbstract":"<p>Streamflow was the major source of water and nutrients (nitrogen and phosphorus) to Lake Cochituate, followed by ground water, and then precipitation during April 1978 through March 1979. Compared to all sources during that period, streams contributed 7,217 million gallons (a little over 82 percent) of water, 63 ,000 pounds (between 50 and 60 percent) of nitrogen, and 3,000 pounds (94 percent) of phosphorus. A little over 60 percent of all the water that entered Lake Cochituate flowed from Fisk Pond. This single source transported about 38,000 pounds of nitrogen and 2,000 pounds of phosphorus. Ground-water inflow to Lake Cochituate occurs along its shoreline except at the north end of Lake Cochituate 's North Pond where natural seepage from the lake is occurring and at locations on the lake 's Middle and South Ponds where municipal wells induce infiltration of lake water amounting to 1,228 million gallons for that period. Discharge of ground water to the lake was estimated to range from 462 to 816 million gallons and transported from 31,000 to 55,000 pounds of nitrogen and from 46 to 82 pounds of phosphorus. Bulk precipitation was estimated to contribute about the same volume of water to the lake as ground water but double its phosphorus load. However, the load of nitrogen, 8000 pounds, from bulk precipitation was the smallest of any source.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri844315","usgsCitation":"Gay, F.B., 1985, Estimated water and nutrient inflows and outflows Lake Cochituate, eastern Massachusetts, 1977-79: U.S. Geological Survey Water-Resources Investigations Report 84-4315, Report: vi, 59 p.; 2 Plates: 21.50 × 29.50 inches and 17.00 × 18.00 inches, https://doi.org/10.3133/wri844315.","productDescription":"Report: vi, 59 p.; 2 Plates: 21.50 × 29.50 inches and 17.00 × 18.00 inches","costCenters":[],"links":[{"id":123985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4315/report-thumb.jpg"},{"id":56133,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4315/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56134,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4315/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56135,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4315/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396033,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36156.htm"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Lake Cochituate","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.458,\n              42.233\n            ],\n            [\n              -71.328,\n              42.233\n            ],\n            [\n              -71.328,\n              42.35\n            ],\n            [\n              -71.458,\n              42.35\n            ],\n            [\n              -71.458,\n              42.233\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcca3","contributors":{"authors":[{"text":"Gay, F. B.","contributorId":55002,"corporation":false,"usgs":true,"family":"Gay","given":"F.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":197815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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