These maps are part of a folio of maps of the Richfield 1o x 2o quadrangle, Utach, prepared under the Conterminous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.
\nLocated 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.
","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":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":"These maps are part of a folio of maps of the Richfield 1o x 2o quadrangle, Utach, prepared under the Conterminous United States Mineral Assessment Program. Other publications in this folio are listed in the selected references.
\nLocated 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.
","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":44452,"text":"wri854223 - 1985 - Maps showing altitude of the potentiometric surface and changes in water level of the Sparta sand and Memphis sand aquifers in Eastern Arkansas, spring 1984","interactions":[],"lastModifiedDate":"2023-01-11T22:12:34.260931","indexId":"wri854223","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":"85-4223","title":"Maps showing altitude of the potentiometric surface and changes in water level of the Sparta sand and Memphis sand aquifers in Eastern Arkansas, spring 1984","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854223","usgsCitation":"Edds, J., and Fitzpatrick, D.J., 1985, Maps showing altitude of the potentiometric surface and changes in water level of the Sparta sand and Memphis sand aquifers in Eastern Arkansas, spring 1984: U.S. Geological Survey Water-Resources Investigations Report 85-4223, 1 Plate: 42.34 x 36.73 inches, https://doi.org/10.3133/wri854223.","productDescription":"1 Plate: 42.34 x 36.73 inches","costCenters":[],"links":[{"id":169743,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411751,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36370.htm"},{"id":81777,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4223/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas","otherGeospatial":"Sparta Sand and Memphis Sand aquifers","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -91.19531829632703,\n 32.980389869575575\n ],\n [\n -91.14779829500537,\n 33.27064745917005\n ],\n [\n -91.233210345451,\n 33.61919543404866\n ],\n [\n -90.7751855375397,\n 34.36276687353285\n ],\n [\n -90.1315710108,\n 35.2080953870105\n ],\n [\n -89.85930607945734,\n 35.58890534894552\n ],\n [\n -89.62948021702829,\n 35.8924267847421\n ],\n [\n -89.64923488521559,\n 36.03010744154139\n ],\n [\n -90.24379748836697,\n 36.02900594885763\n ],\n [\n -89.92840007471217,\n 36.3446893320513\n ],\n [\n -90.06040729879555,\n 36.51927069670744\n ],\n [\n -92.26347695592654,\n 36.5187478937554\n ],\n [\n -92.42507489328582,\n 33.0076778799659\n ],\n [\n -91.19531829632703,\n 32.980389869575575\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60461a","contributors":{"authors":[{"text":"Edds, Joe","contributorId":48532,"corporation":false,"usgs":true,"family":"Edds","given":"Joe","email":"","affiliations":[],"preferred":false,"id":229792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fitzpatrick, Daniel J.","contributorId":31367,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Daniel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229791,"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":"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.
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.
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.
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.
","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":60393,"text":"mf1573B - 1985 - Aeromagnetic maps of the Mazatzal Wilderness and contiguous roadless areas, Gila, Maricopa, and Yavapai counties, Arizona","interactions":[],"lastModifiedDate":"2016-08-23T08:22:42","indexId":"mf1573B","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":"1573","chapter":"B","title":"Aeromagnetic maps of the Mazatzal Wilderness and contiguous roadless areas, Gila, Maricopa, and Yavapai counties, Arizona","docAbstract":"The Mazatzal Wilderness and contiguous roadless areas are located in Tonto and Coconino National Forests, west and southwest of Payson, and are almost exactly in the geographic center of Arizona. This is a region of relatively small mining districts and few mines, but occurrences of many different metals are widespread.
\nThe Mazatzal Mountains constitute the dominant physiographic feature of the wilderness. The eastern slopes of these mountains rise steeply from about 3,500 ft in altitude along the valley of Rye Creek east of the range, to 7,903 ft at Mazatzal Peak. To the west, the range slopes steeply from the crest then more gently along the lower flanks to the Werde River, one of the main drainage channels of Arizona. In the northern part of the wilderness, the East Werde River, a tributary of the Verde, occupies a deep canyon that separates the Mazatzal Mountains from mesas to the north. The lowest parts of the wilderness have altitudes of about 2,200 ft and are located near Bartlett Reservoir in the southwestern part of the area studied.
\nTwo aeromagnetic surveys were flown and interpreted to aid in the delineation of subsurface lithology and structure: one survey was flown at a low level (1,000 ft above ground) and the other at a high level (9,000 ft above sea level). In addition, the results of a small-scale electromagnetic (EM) survey are briefly discussed; the surface EM survey took place in an area of copper concentrations and past exploration activity to look for evidence of massive sulfide mineralization.
\nStudies of the geology, geochemistry (Marsh and others, 1983a, b, Erickson, 1984), mines and prospects (Ellis, 1982), and mineral resource potential (Wrucke and others, 1983) of the Mazatzal Wilderness and contiguous roadless areas have been published elsewhere.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1573B","isbn":"0607813288","usgsCitation":"Moss, C.K., and Abrams, G.A., 1985, Aeromagnetic maps of the Mazatzal Wilderness and contiguous roadless areas, Gila, Maricopa, and Yavapai counties, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1573, 2 Plates: 38.70 x 50.88 inches and 30.79 x 28.29 inches, https://doi.org/10.3133/mf1573B.","productDescription":"2 Plates: 38.70 x 50.88 inches and 30.79 x 28.29 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1573B.JPG"},{"id":327379,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1573-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327380,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1573-B/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Arizona","county":"Gila County, Maricopa County, Yavapai County","otherGeospatial":"Mazatzal Wilderness and contiguous roadless areas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.68333333333334,33.8675 ], [ -111.68333333333334,34.33416666666667 ], [ -111.38333333333334,34.33416666666667 ], [ -111.38333333333334,33.8675 ], [ -111.68333333333334,33.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d7e","contributors":{"authors":[{"text":"Moss, C. K.","contributorId":94661,"corporation":false,"usgs":true,"family":"Moss","given":"C.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":263672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abrams, G. A.","contributorId":27047,"corporation":false,"usgs":true,"family":"Abrams","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":263671,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":60450,"text":"mf1628B - 1985 - Stream-sediment and panned-concentrate geochemical maps of the Buffalo Peaks Wilderness Study Area, Lake, Park, and Chaffee counties, Colorado","interactions":[],"lastModifiedDate":"2016-08-23T08:29:33","indexId":"mf1628B","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":"1628","chapter":"B","title":"Stream-sediment and panned-concentrate geochemical maps of the Buffalo Peaks Wilderness Study Area, Lake, Park, and Chaffee counties, Colorado","docAbstract":"Under provisions of the Wilderness Act (Public Law 88-577, September 3, 1964), the U.S. Geological Survey and the U.S. Bureau of Mines have been conducting mineral surveys of areas selected for possible inclusion in the National Wilderness Preservation System. This report presents results of geochemical studies carried out in June and July, 1982, as part of the investigation of the Buffalo Peaks Wilderness Study Area, Colo. Stream-sediment and panned-concentrate samples were collected from about 80 sites on streams draining the study area. Analytical results and a sample locality map were published by Domenico and others (1984).
\nThe geologic and mineral resource potential maps of the study area were prepared by Hedlund and others (1983). The Buffalo Peaks Wilderness Study Area encompasses a major portion of the Mosquito Range, which is structurally part of the east flank of the north-northwest-trending Sawatch anticline. Bedrock in the west two-thirds of the study area is made up of Precambrian igneous and metamorphic rocks of the core of the anticline, whereas bedrock in the east one-third is mostly east dipping Paleozoic sedimentary rocks. In the vicinity of East and West Buffalo Peaks, the sequence of Paleozoic sedimentary rocks is covered by Tertiary extrusive rocks.
\nMajor faults generally run parallel to the north-northwest trend of the Arkansas River Valley, which is an expression of the Arkansas River segment of the Rio Grande depression, and the Sawatch anticline in the study area. Some faults are probably of late Precambrian age; major recurrent displacement is known to have occurred on most faults during Laramide time and in the Pliocene and Miocene.
\nThe study area is bounded by several areas of known mineralization (Hedl und and others, 1983). Vein and bedding replacement deposits of silver, zinc, and lead were mined from 1890 until about 1918 in the vicinity of Weston Pass (map A), on the northeastern border of the study area. Gold and silver were mined from about 1860 until about 1880 from veins in the Granite area (map A), on the northwestern border of the study area; minor prospecting activity continues today. From 1935 to 1937, veins of gold, silver, and base metals were mined in the vicinity of Fourmile Creek, on the southwestern border of the study area (map A). Recently, active uranium prospecting has been taking place in the vicinity of the Middle Fork of Salt Creek, on the southeastern border of the study area (map A).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1628B","usgsCitation":"Nowlan, G., and Gerstel, W., 1985, Stream-sediment and panned-concentrate geochemical maps of the Buffalo Peaks Wilderness Study Area, Lake, Park, and Chaffee counties, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 1628, 2 Plates: 33.46 x 58.84 inches and 40.68 x 26.65 inches, https://doi.org/10.3133/mf1628B.","productDescription":"2 Plates: 33.46 x 58.84 inches and 40.68 x 26.65 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326356,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1628B.JPG"},{"id":327389,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1628-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327390,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1628-B/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"50000","country":"United States","state":"Colorado","county":"Chaffee County, Lake County, Park County","otherGeospatial":"Buffalo Peaks Wilderness Study Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.25,39 ], [ -106.25,39.6175 ], [ -106.11749999999999,39.6175 ], [ -106.11749999999999,39 ], [ -106.25,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ffa","contributors":{"authors":[{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":263772,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gerstel, W.J.","contributorId":40988,"corporation":false,"usgs":true,"family":"Gerstel","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":263771,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61206,"text":"mf1383H - 1985 - Map showing abundance and distribution of silver in stream-sediment samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California","interactions":[],"lastModifiedDate":"2016-08-23T10:13:10","indexId":"mf1383H","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":"1383","chapter":"H","title":"Map showing abundance and distribution of silver in stream-sediment samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California","docAbstract":"The Medford quadrangle is located in mountainous southwestern Oregon adjacent to the California border and a short distance east of the Pacific coast. Various parts of this area lie in different geologic provinces. Most of the western half of the quadrangle is underlain by pre-Tertiary rocks of the Klamath Mountains province. However, the Coast Range province is represented by the Tertiary sedimentary rocks in the northwest corner. Much of the eastern half of the quadrangle lies in the Cascade Range. In Oregon, because of differences in physiographic expression and age of rocks, this province is commonly divided into the more rugged High Cascade Range on the east and the more subdued Western Cascade Range on the west. This division is approximated on the map by the contact between the Quaternary and Tertiary volcanic rocks of the High Cascade Range and the Tertiary volcanic rocks of the Western Cascade Range. The geology shown is generalized from a more detailed compilation by Smith and others (1982).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1383H","usgsCitation":"Whittington, C.L., Grimes, D.J., and Leinz, R.W., 1985, Map showing abundance and distribution of silver in stream-sediment samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California: U.S. Geological Survey Miscellaneous Field Studies Map 1383, 48.86 x 24.08 inches, https://doi.org/10.3133/mf1383H.","productDescription":"48.86 x 24.08 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1383H.PNG"},{"id":327563,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1383-H/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Oregon","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,42 ], [ -124,43 ], [ -122,43 ], [ -122,42 ], [ -124,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658e4e","contributors":{"authors":[{"text":"Whittington, Charles L.","contributorId":52642,"corporation":false,"usgs":true,"family":"Whittington","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265187,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grimes, David J.","contributorId":36925,"corporation":false,"usgs":true,"family":"Grimes","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":265188,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leinz, Reinhard W.","contributorId":60628,"corporation":false,"usgs":true,"family":"Leinz","given":"Reinhard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265189,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":61204,"text":"mf1383I - 1985 - Map showing abundance and distribution of chromium in stream-sediment samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California","interactions":[],"lastModifiedDate":"2016-08-23T10:14:55","indexId":"mf1383I","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":"1383","chapter":"I","title":"Map showing abundance and distribution of chromium in stream-sediment samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California","docAbstract":"The Medford quadrangle is located in mountainous southwestern Oregon adjacent to the California border and a short distance east of the Pacific coast. Various parts of this area lie in different geologic provinces. Most of the western half of the quadrangle is underlain by pre-Tertiary rocks of the Klamath Mountains province. However, the Coast Range province is represented by the Tertiary sedimentary rocks in the northwest corner. Much of the eastern half of the quadrangle lies in the Cascade Range. In Oregon, because of differences in physiographic expression and age of rocks, this province is commonly divided into the more rugged High Cascade Range on the east and the more subdued Western Cascade Range on the west. This division is approximated on the map by the contact between the Quaternary and Tertiary volcanic rocks of the High Cascade Range and the Tertiary volcanic rocks of the Western Cascade Range. The geology shown is generalized from a more detailed compilation by Smith and others (1982).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1383I","usgsCitation":"Whittington, C.L., Grimes, D.J., and Leinz, R.W., 1985, Map showing abundance and distribution of chromium in stream-sediment samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California: U.S. Geological Survey Miscellaneous Field Studies Map 1383, 42.54 x 24.18 inches, https://doi.org/10.3133/mf1383I.","productDescription":"42.54 x 24.18 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1383I.PNG"},{"id":327567,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1383-I/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Oregon","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,42 ], [ -124,43 ], [ -122,43 ], [ -122,42 ], [ -124,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658c3b","contributors":{"authors":[{"text":"Whittington, Charles L.","contributorId":52642,"corporation":false,"usgs":true,"family":"Whittington","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grimes, David J.","contributorId":36925,"corporation":false,"usgs":true,"family":"Grimes","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":265182,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leinz, Reinhard W.","contributorId":60628,"corporation":false,"usgs":true,"family":"Leinz","given":"Reinhard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265183,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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":"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.
\nThe 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.
","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":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":"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.
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.
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.
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.
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.
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.
","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 -114.6533203125,\n 32.509761735919426\n ],\n [\n -111.09374999999999,\n 31.353636941500987\n ],\n [\n -108.5009765625,\n 31.353636941500987\n ],\n [\n -108.28125,\n 31.952162238024975\n ],\n [\n -106.3916015625,\n 31.952162238024975\n ],\n [\n -104.8974609375,\n 30.751277776257812\n ],\n [\n -104.6337890625,\n 30.600093873550072\n ],\n [\n -104.5458984375,\n 30.183121842195515\n ],\n [\n -103.3154296875,\n 29.11377539511439\n ],\n [\n -102.7880859375,\n 29.99300228455108\n ],\n [\n -105.9521484375,\n 34.52466147177172\n ],\n [\n -106.8310546875,\n 34.95799531086792\n ],\n [\n -107.6220703125,\n 34.88593094075317\n ],\n [\n -108.544921875,\n 33.76088200086917\n ],\n [\n -111.57714843749999,\n 34.88593094075317\n ],\n [\n -113.0712890625,\n 35.7286770448517\n ],\n [\n -114.01611328125,\n 35.96022296929667\n ],\n [\n -111.33544921874999,\n 40.763901280945866\n ],\n [\n -111.005859375,\n 42.69858589169842\n ],\n [\n -112.67578124999999,\n 43.16512263158296\n ],\n [\n -116.76269531249999,\n 41.64007838467894\n ],\n [\n -118.30078125,\n 42.52069952914966\n ],\n [\n -119.50927734374999,\n 43.61221676817573\n ],\n [\n -120.62988281249999,\n 43.5326204268101\n ],\n [\n -121.1572265625,\n 43.26120612479979\n ],\n [\n -121.75048828124999,\n 42.53689200787315\n ],\n [\n -121.83837890625,\n 41.902277040963696\n ],\n [\n -121.728515625,\n 41.27780646738183\n ],\n [\n -120.36621093749999,\n 40.83043687764923\n ],\n [\n -120.30029296875,\n 39.30029918615029\n ],\n [\n -120.30029296875,\n 38.75408327579141\n ],\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":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":"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.
","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}]}} ,{"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":"No abstract available.
","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":30469,"text":"wri844294 - 1985 - Results of geohydrologic test drilling in the eastern Snake River Plain, Gooding County, Idaho","interactions":[],"lastModifiedDate":"2013-11-21T13:46:24","indexId":"wri844294","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":"84-4294","title":"Results of geohydrologic test drilling in the eastern Snake River Plain, Gooding County, Idaho","docAbstract":"A 1,123-foot test hole was core drilled near Wendell, Idaho, during 1981-82 as part of the Snake River Plain regional aquifer study. An upper basalt unit, an intermediate unconsolidated sedimentary rock unit, and a lower basalt unit were penetrated by the test hole. Drilling verified that the upper several hundred feet of high-resistivity material, as determined by surface electrical soundings, is basalt. Core examination, laboratory analysis, and correlation with other drill holes indicated that the basalt is typical of Quaternary basalt of the Snake River Group. Quaternary basalt in the test hole is 200 feet thick. Correlation with other drill holes and comparison with rock outcrops near the Snake River and in the Snake River canyon suggest that the underlying sediments and lower basalt unit are parts of the Tertiary and Quaternary Glenns Ferry Formation and Tertiary Banbury Basalt. Piezometers in the hole verify upward movement of water in a major discharge area for the regional aquifer. Hydraulic head in the bottom of the hole is about 155 feet higher than the water table. Lithologic sequence in the test hole correlates well with sequences in deep drill holes at scattered locations on the plain. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844294","collaboration":"Prepared as part of the Snake River Plain Regional Aquifer-Systems Analysis Study","usgsCitation":"Whitehead, R., and Lindholm, G.F., 1985, Results of geohydrologic test drilling in the eastern Snake River Plain, Gooding County, Idaho: U.S. Geological Survey Water-Resources Investigations Report 84-4294, Report: ii, 30 p.; 1 Plate: 25.19 x 22.52 inches, https://doi.org/10.3133/wri844294.","productDescription":"Report: ii, 30 p.; 1 Plate: 25.19 x 22.52 inches","numberOfPages":"34","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":159829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4294/report-thumb.jpg"},{"id":59251,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4294/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4294/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Gooding County","otherGeospatial":"Snake River Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.0,42.0 ], [ -115.0,44.25 ], [ -111.5,44.25 ], [ -111.5,42.0 ], [ -115.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0fe4b07f02db5feee5","contributors":{"authors":[{"text":"Whitehead, R.L.","contributorId":34891,"corporation":false,"usgs":true,"family":"Whitehead","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":203302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindholm, G. F.","contributorId":88763,"corporation":false,"usgs":true,"family":"Lindholm","given":"G.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":203303,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29905,"text":"wri854298 - 1985 - Frequency and duration of flooding of Grove Creek near Kenansville, North Carolina, for present and proposed restored channel conditions","interactions":[],"lastModifiedDate":"2017-01-24T11:41:40","indexId":"wri854298","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":"85-4298","title":"Frequency and duration of flooding of Grove Creek near Kenansville, North Carolina, for present and proposed restored channel conditions","docAbstract":"The Grove Creek basin includes an area of about 42 square miles in Duplin County, southeastern North Carolina. The North Carolina Department of Human Resources (DHR) proposes to implement a channel restoration project on about an eight-mile reach of Grove Creek. The purpose of the restoration program is to improve drainage, thereby reducing frequency and duration of overbank flooding and reducing the opportunity for mosquito breeding in frequently flooded areas adjacent to Grove Creek. This study evaluates the effects of the restoration on the frequency and duration of flooding within the study reach for present (1984) and proposed restored channel conditions.\r\n\r\nThe proposed restored channel is estimated to increase the carrying capacity of the main channel from 10 to 19 times. The greatest reduction in areas of flooded land immediately adjacent to the study reach would be west of North Carolina Highway 11 (between sites 4 and 6) and would be reduced by an average of 29 percent during floods up through the 10-year flood level and reduced by an average of 5 percent for the 25- to 100-year flood levels. An average reduction of 1 percent is indicated for areas inundated east of North Carolina Highway 11 (for sites 1 through 3) for the 2-, 5-, 10-, 25-, 50-, and 100-year floods; while reductions in inundated area of the total study reach of 13, 5, 4, and 1.5 percent are indicated for the 2-, 5-, 10-, and 100-year floods, respectively.\r\n\r\nOverbank flooding during 1983 and 1984 water years occurred 32 times and persisted from a few hours up to about 3 months. For proposed restored-channel conditions, overbank flooding would have been reduced to 5 occurrences, and areal flooding would have persisted from a few hours to about 2 days.\r\n\r\nFlooding on the Northeast Cape Fear River causes variable backwater conditions on the lower Grove Creek study reach. A 100-year flood on the Northeast Cape Fear River would create backwater for about 1.5 miles upstream on Grove Creek.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854298","usgsCitation":"Stamey, T.C., 1985, Frequency and duration of flooding of Grove Creek near Kenansville, North Carolina, for present and proposed restored channel conditions: U.S. Geological Survey Water-Resources Investigations Report 85-4298, v, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854298.","productDescription":"v, 52 p. :ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":124929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4298/report-thumb.jpg"},{"id":58722,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4298/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","city":"Kenansville","otherGeospatial":"Grove Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.11279296875,\n 34.615126683462194\n ],\n [\n -78.11279296875,\n 35.06372505419625\n ],\n [\n -77.552490234375,\n 35.06372505419625\n ],\n [\n -77.552490234375,\n 34.615126683462194\n ],\n [\n -78.11279296875,\n 34.615126683462194\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f55","contributors":{"authors":[{"text":"Stamey, T. C.","contributorId":95496,"corporation":false,"usgs":true,"family":"Stamey","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":202330,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15322,"text":"ofr85340 - 1985 - Geophysical well log data for study of water flow in fractures near Mirror Lake, West Thornton, New Hampshire","interactions":[],"lastModifiedDate":"2022-01-24T21:58:37.315474","indexId":"ofr85340","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":"85-340","title":"Geophysical well log data for study of water flow in fractures near Mirror Lake, West Thornton, New Hampshire","docAbstract":"Four closely spaced boreholes were drilled through approximately 20 meters of till into schist bedrock near Mirror Lake, West Thornton, New Hampshire. The site was selected for borehole geophysical research because it is included in a detailed groundwater study where the effects of flow in fractures on flow in overlying drift deposits is being studied. Three of the boreholes are approximately 100 meters in depth, and the fourth is approximately 230 meters in depth. All four boreholes were logged with caliper, acoustic, gamma, single-point-resistivity, and acoustic televiewer logs. Fracture sets dipping approximately 45 degrees to the east were detected in all four boreholes. Two sets of deeper fractures were detected near the bottom of the deepest borehole. Acoustic waveform logs were obtained in all boreholes using three different source frequencies, 34, 15, and 5 kilohertz, for future comparison with surface to borehole seismic data.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85340","usgsCitation":"Paillet, F.L., 1985, Geophysical well log data for study of water flow in fractures near Mirror Lake, West Thornton, New Hampshire: U.S. Geological Survey Open-File Report 85-340, vi, 27 p., https://doi.org/10.3133/ofr85340.","productDescription":"vi, 27 p.","costCenters":[],"links":[{"id":394786,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75793.htm"},{"id":44252,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0340/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146456,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0340/report-thumb.jpg"}],"country":"United States","state":"New Hampshire","city":"West Thornton","otherGeospatial":"Mirror Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.69660568237305,\n 43.94110816034728\n ],\n [\n -71.68905258178711,\n 43.94110816034728\n ],\n [\n -71.68905258178711,\n 43.94679373516942\n ],\n [\n -71.69660568237305,\n 43.94679373516942\n ],\n [\n -71.69660568237305,\n 43.94110816034728\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b390","contributors":{"authors":[{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":170954,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27138,"text":"wri844187 - 1985 - Water-resources monitoring in the Cottonwood Creek area, Shasta and Tehama counties, California, 1982-83","interactions":[],"lastModifiedDate":"2022-12-29T22:26:03.691324","indexId":"wri844187","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":"84-4187","title":"Water-resources monitoring in the Cottonwood Creek area, Shasta and Tehama counties, California, 1982-83","docAbstract":"The Cottonwood Creek study area in the Redding basin, California , contains a network of wells established to provide baseline information on ground-water levels and quality prior to the completion of two proposed dams, one on Cottonwood Creek and one on South Fork Cottonwood Creek. Analysis of monthly ground-water levels from September 1982 through September 1983 shows lowest water levels in autumn and highest in spring. The ground-water surface slopes east and has a mound at Anderson-Cottonwood Irrigation District Canal near the town of Cottonwood. Future studies here could provide additional information needed for subsequent modeling studies. Data are insufficient upstream from the damsites, specifically in areas of future impoundment where the monitoring network could be expanded. Comparison of ground-water quality samples collected from periods of lowest and highest water levels showed little chemical variation. Ground water is good to excellent with respect to recommended drinking-water standards. Ground-water types north of Cottonwood Creek are sodium magnesium or magnesium sodium bicarbonate and south of Cottonwood Creek are calcium magnesium or magnesium calcium bicarbonate. Surface-water samples from Cottonwood and South Fork Cottonwood Creeks indicate water chemically similar to ground water south of Cottonwood Creek. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844187","usgsCitation":"Fogelman, R.P., and Evenson, K.D., 1985, Water-resources monitoring in the Cottonwood Creek area, Shasta and Tehama counties, California, 1982-83: U.S. Geological Survey Water-Resources Investigations Report 84-4187, Report: iv, 70 p.; 4 Plates: 35.97 x 26.25 inches or smaller, https://doi.org/10.3133/wri844187.","productDescription":"Report: iv, 70 p.; 4 Plates: 35.97 x 26.25 inches or smaller","costCenters":[],"links":[{"id":118704,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4187/report-thumb.jpg"},{"id":56011,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4187/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56012,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4187/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56008,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4187/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56009,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4187/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56010,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4187/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411206,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36051.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Shasta County, Tehama County","otherGeospatial":"Cottonwood Creek area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.167,\n 40.5\n ],\n [\n -122.617,\n 40.5\n ],\n [\n -122.617,\n 40.25\n ],\n [\n -122.167,\n 40.25\n ],\n [\n -122.167,\n 40.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4beb","contributors":{"authors":[{"text":"Fogelman, R. P.","contributorId":96688,"corporation":false,"usgs":true,"family":"Fogelman","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":197621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evenson, K. D.","contributorId":85978,"corporation":false,"usgs":true,"family":"Evenson","given":"K.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":197620,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3510,"text":"cir964 - 1985 - Design of the National Trends Network for monitoring the chemistry of atmospheric precipitation","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir964","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":"964","title":"Design of the National Trends Network for monitoring the chemistry of atmospheric precipitation","docAbstract":"Long-term monitoring (10 years minimum) of the chemistry of wet deposition will be conducted at National Trends Network (NTN) sites across the United States. Precipitation samples will be collected at sites that represent broad regional characteristics. Design of the NTN considered four basic elements during construction of a model to distribute 50, 75, 100, 125 or 150 sites. The modeling oriented design was supplemented with guidance developed during the course of the site selection process. Ultimately, a network of 151 sites was proposed. \r\n\r\nThe basic elements of the design are: \r\n\r\n(1) Assurance that all areas of the country are represented in the network on the basis of regional ecological properties (96 sites); \r\n\r\n(2) Placement of additional sites east of the Rocky Mountains to better define high deposition gradients (27 sites); \r\n\r\n(3) Placement of sites to assure that potentially sensitive regions are represented (15 sites); \r\n\r\n(4) Placement of sites to allow for other considerations, such as urban area effects (5 sites), intercomparison with Canada (3 sites), and apparent disparities in regional coverage (5 sites). \r\n\r\nSite selection stressed areas away from urban centers, large point sources, or ocean influences. Local factors, such as stable land ownership, nearby small emission sources (about 10 km), and close-by roads and fireplaces (about 0.5 km) were also considered. All proposed sites will be visited as part of the second phase of the study.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir964","usgsCitation":"Robertson, J., and Wilson, J., 1985, Design of the National Trends Network for monitoring the chemistry of atmospheric precipitation: U.S. Geological Survey Circular 964, viii, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/cir964.","productDescription":"viii, 46 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0964/report-thumb.jpg"},{"id":30524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0964/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667dbc","contributors":{"authors":[{"text":"Robertson, J.K.","contributorId":43737,"corporation":false,"usgs":true,"family":"Robertson","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":147062,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, J.W.","contributorId":24331,"corporation":false,"usgs":true,"family":"Wilson","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":147061,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15443,"text":"ofr85569 - 1985 - Ground-water levels in the alluvial aquifer in eastern Arkansas, 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:07:07","indexId":"ofr85569","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":"85-569","title":"Ground-water levels in the alluvial aquifer in eastern Arkansas, 1984","docAbstract":"This report, prepared by the U.S. Geological Survey in cooperation with the Arkansas Soil and Water Conservation Commission, the U.S. Soil Conservation Service and local Conservation Districts, contains groundwater level measurements in 452 wells tapping the Mississippi River Valley alluvial aquifer of eastern Arkansas. The measurements were made by the U.S. Soil Conservation Service during 1984. The purpose of this report is to provide these data to other State and Federal agencies as well as to private landowners. On the average, a decline of 2.5 feet in water levels was observed throughout the study area after the pumping season. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85569","usgsCitation":"Plafcan, M., 1985, Ground-water levels in the alluvial aquifer in eastern Arkansas, 1984: U.S. Geological Survey Open-File Report 85-569, iv, 26 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr85569.","productDescription":"iv, 26 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":148491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0569/report-thumb.jpg"},{"id":44413,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0569/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6674ea","contributors":{"authors":[{"text":"Plafcan, Maria","contributorId":20338,"corporation":false,"usgs":true,"family":"Plafcan","given":"Maria","email":"","affiliations":[],"preferred":false,"id":171146,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30584,"text":"wri854107 - 1985 - Seismic-refraction study of suspected drift-filled bedrock valleys in Ramsey County, Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T12:17:36","indexId":"wri854107","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":"85-4107","title":"Seismic-refraction study of suspected drift-filled bedrock valleys in Ramsey County, Minnesota","docAbstract":"Seismic-refraction surveys were made across suspected buried, drift-filled bedrock valleys believed to underlie two sites of known ground-water contamination the Twin Cities Army Ammunition Plant (TCAAP) near New Brighton and the former Koppers Coke Plant in St. Paul, Ramsey County, Minnesota. Refraction data were collected along two lines at each site; each line traversed the axis of a suspected valley.
\nDrift-filled bedrock valleys were thought to incise the Prairie du Chien-Jordan aquifer to an altitude between 500 and 560 feet above sea level at the TCAAP site. The interpretation of one seismic profile indicates that a valley probably does not exist under the area surveyed; the modeled depth profile shows the bedrock surface ranging between altitudes of about 700 to 780 feet. Interpretation of a second seismic profile just south of the TCAAP indicates that a shallow valley may exist under the northern half of the line; the modeled depth profile shows that the bedrock surface declines from an altitude of about 780 feet to about 690 feet over a horizontal distance of 400 feet.
\nA drift-filled bedrock valley was thought to incise the St. Peter aquifer to an altitude between 770 and 800 feet above sea level at the Koppers site. The interpretation of a seismic profile just east of the Koppers site is not conclusive, but suggests that a bedrock valley may be present near the middle of the line. The interpretation of a second seismic profile across the westward extension of the same suspected valley also is not conclusive, but suggests that a bedrock valley may be present at the north end of the line. The optimal field layout for each line at the site (longer shot offsets) could not be obtained because of limited space available in the densely developed residential neighborhoods.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri854107","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Woodward, D.G., 1985, Seismic-refraction study of suspected drift-filled bedrock valleys in Ramsey County, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 85-4107, iv, 20 p., https://doi.org/10.3133/wri854107.","productDescription":"iv, 20 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":160279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4107/report-thumb.jpg"},{"id":59342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Ramsey County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.0207,45.1258],[-92.9838,45.1247],[-92.9875,44.8924],[-92.9978,44.8924],[-93.0191,44.8929],[-93.0229,44.8948],[-93.0294,44.8966],[-93.0357,44.904],[-93.0447,44.9122],[-93.0498,44.9168],[-93.0524,44.9204],[-93.0608,44.9209],[-93.0666,44.921],[-93.0904,44.9215],[-93.0897,44.9251],[-93.0975,44.9252],[-93.0981,44.9215],[-93.1084,44.922],[-93.1271,44.9225],[-93.1297,44.9198],[-93.1342,44.9175],[-93.1375,44.9143],[-93.1426,44.9102],[-93.1504,44.9039],[-93.1556,44.9002],[-93.164,44.8979],[-93.1704,44.8975],[-93.1775,44.8989],[-93.1833,44.8998],[-93.1897,44.9026],[-93.1955,44.904],[-93.1987,44.9085],[-93.2026,44.9122],[-93.2038,44.9145],[-93.2058,44.9172],[-93.2051,44.9209],[-93.2044,44.9263],[-93.2044,44.9305],[-93.2031,44.935],[-93.2037,44.9405],[-93.2044,44.9441],[-93.2063,44.9469],[-93.2062,44.9583],[-93.2059,45.0373],[-93.2272,45.0373],[-93.2262,45.1255],[-93.0207,45.1258]]]},\"properties\":{\"name\":\"Ramsey\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efcfc","contributors":{"authors":[{"text":"Woodward, D. G.","contributorId":106458,"corporation":false,"usgs":true,"family":"Woodward","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203492,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14862,"text":"ofr85155 - 1985 - Base-flow characteristics of segments of the Piney River, and East and West Piney Rivers, Dickson and Hickman Counties, Tennessee","interactions":[],"lastModifiedDate":"2022-01-03T20:04:46.176358","indexId":"ofr85155","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":"85-155","title":"Base-flow characteristics of segments of the Piney River, and East and West Piney Rivers, Dickson and Hickman Counties, Tennessee","docAbstract":"Base-flow profiles based on discharge measurements made during a seepage investigation on August 28, 1984, define losing and gaining reaches of segments of the Piney River, and East and West Piney Rivers, Dickson and Hickman Counties, central Tennessee. A similar profile defines losing and gaining reaches for the average 3-day minimum discharge, 20-year recurrence interval, and the variability of that discharge along the river channels. The average 3-day minimum discharge, 20-year recurrence interval, ranged from 2.4 cubic feet per second for the site on East Piney River to 45.6 cubic feet per second at the Vernon gage, farthest site downstream in the study area. On the Piney River, the lowest 3-day, 20-year discharge, occurs at river mile 23.5, 0.1 river mile downstream from the confluence of the East and West Piney Rivers. Comparison of discharge measurements to recorded August discharges at the Vernon gage shows that the measurements represent base-flow conditions in the Piney River basin. The measurements and analyses can be used to formulate water management plans for use during droughts. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85155","usgsCitation":"May, V., 1985, Base-flow characteristics of segments of the Piney River, and East and West Piney Rivers, Dickson and Hickman Counties, Tennessee: U.S. Geological Survey Open-File Report 85-155, v, 24 p., https://doi.org/10.3133/ofr85155.","productDescription":"v, 24 p.","costCenters":[],"links":[{"id":393784,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16735.htm"},{"id":43660,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0155/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0155/report-thumb.jpg"}],"country":"United States","state":"Tennessee","county":"Dickson County, Hickman County","otherGeospatial":"Piney River, and East and West Piney Rivers","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.375,\n 35.8750\n ],\n [\n -87.5,\n 35.8750\n ],\n [\n -87.5,\n 36.125\n ],\n [\n -87.375,\n 36.125\n ],\n [\n -87.375,\n 35.8750\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6488b4","contributors":{"authors":[{"text":"May, V.J.","contributorId":71539,"corporation":false,"usgs":true,"family":"May","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":170144,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15734,"text":"ofr86302 - 1985 - Permitted water use in Iowa, 1985","interactions":[],"lastModifiedDate":"2016-03-04T14:40:27","indexId":"ofr86302","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":"86-302","title":"Permitted water use in Iowa, 1985","docAbstract":"This report summarizes where, how much and for what purpose water is allocated for use in Iowa with permits issued by the Department of Water, Air and Waste Management. In Iowa, from a total permitted water use of 855,175.45 million gallons per year, about 58 percent is from surface-water sources and about 42 percent is from ground-water sources. Streams are 80.5 percent of the total surface-water use and wells make up 80.1 percent of the total ground-water use, with 65.4 percent of ground water coming from surficial aquifers. Power generation is the use category that is permitted the largest amount of total water use, 46.6 percent, with surface water being the source of 96.7 percent and 77.9 percent of the surface water is from streams. The public water suppliers' category is the next largest use type with 15.7 percent of the total permitted water. Ground water constitutes 74.4 percent of the public water supplier category with 51.7 percent from surficial aquifers. Surface water makes up 25.6 percent of this category with 83.0 percent of the surface water withdrawn from streams. Mining comprises 13.4 percent of the total water use and is the third largest water-use category. Ground water is the source of 63.3 percent of permitted mining water use with 94.3 percent of this from quarries and sand and gravel pits. Surface water is the source of 36.7 percent of the permitted mining water use with 97.6 percent from streams. Irrigation is the fourth largest permitted use type using 12.0 percent of the total water use. Eighty-eight percent of irrigation is from ground-water sources where surficial aquifers account for 94.7 percent. Streams are 81.1 percent of irrigational surface-water use. Self-supplied industrial users are permitted 10.6 percent of the total permitted water use with 85.5 percent of this from ground-water sources and 14.5 percent from surface-water sources. Of the self-supplied industrial ground-water use, 47.9 percent comes from surficial aquifers and of the self-supplied industrial surface-water use 86.1 percent is from streams. Self-supplied commercial use is allocated 1.5 percent of the total permitted water. Surface-water is the source of 37.7 percent of this and 62.3 percent is from ground-water sources. Agricultural (non-irrigation) use is 0.3 percent of the total permitted water with 73.3 percent from groundwater sources and 26.7 percent from surface-water sources. The areas that are allocated the most water permits are east-central Iowa and west-central Iowa.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr86302","collaboration":"Prepared in cooperation with Iowa Department of Water, Air and Waste Management, and the Iowa Geological Survey","usgsCitation":"Runkle, D., Newman, J., and Shields, E., 1985, Permitted water use in Iowa, 1985: U.S. Geological Survey Open-File Report 86-302, 24 p.: ill., maps; 22 x 28 cm., https://doi.org/10.3133/ofr86302.","productDescription":"24 p.: ill., maps; 22 x 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":318579,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr86302.JPG"},{"id":44752,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0302/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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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":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":29164,"text":"wri844135 - 1985 - Water-supply potential of the Floridan aquifer in Osceola, eastern Orange, and southwestern Brevard counties, Florida","interactions":[],"lastModifiedDate":"2022-09-21T19:10:10.406041","indexId":"wri844135","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":"84-4135","title":"Water-supply potential of the Floridan aquifer in Osceola, eastern Orange, and southwestern Brevard counties, Florida","docAbstract":"The city of Melbourne and adjacent areas in south Brevard County obtain their water supply from Lake Washington. As of 1982, the lake could provide a maximum of 15 million gallons per day but the projected need for the year 2000 is nearly three times that amount. As one alternative for a future water supply, this study investigated with a digital model, the potential yields of well fields completed in the Floridan aquifer. Seven pumping schemes were simulated with the digital model. Each simulation was made under steady-state conditions so that storage properties of the ground-water system were not included. The most advantageous area for ground-water development was in central Osceola County. Poor quality of water precluded locating a well field within Brevard County. If the ground-water alternative is chosen for the future supply, an observation well network is advisable to monitor head changes; chloride concentration trends east of the pumping centers; and chloride concentration trends in zones below the pumped zone.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844135","usgsCitation":"Planert, M., and Aucott, W.R., 1985, Water-supply potential of the Floridan aquifer in Osceola, eastern Orange, and southwestern Brevard counties, Florida: U.S. Geological Survey Water-Resources Investigations Report 84-4135, vi 69 p., https://doi.org/10.3133/wri844135.","productDescription":"vi 69 p.","costCenters":[],"links":[{"id":407159,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36012.htm","linkFileType":{"id":5,"text":"html"}},{"id":58039,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4135/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4135/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Brevard County, Orange County, Osceola County","otherGeospatial":"Floridan aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.662,\n 27.819\n ],\n [\n -80.537,\n 27.819\n ],\n [\n -80.537,\n 28.585\n ],\n [\n -81.662,\n 28.585\n ],\n [\n -81.662,\n 27.819\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d50","contributors":{"authors":[{"text":"Planert, Michael","contributorId":56659,"corporation":false,"usgs":true,"family":"Planert","given":"Michael","email":"","affiliations":[],"preferred":false,"id":201060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aucott, W. R.","contributorId":64288,"corporation":false,"usgs":true,"family":"Aucott","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":201061,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6295,"text":"pp1267 - 1985 - Geology of the Carlin gold deposit, Nevada","interactions":[{"subject":{"id":10769,"text":"ofr8197 - 1981 - Geology of the Carlin gold deposit, Nevada","indexId":"ofr8197","publicationYear":"1981","noYear":false,"title":"Geology of the Carlin gold deposit, Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":6295,"text":"pp1267 - 1985 - Geology of the Carlin gold deposit, Nevada","indexId":"pp1267","publicationYear":"1985","noYear":false,"title":"Geology of the Carlin gold deposit, Nevada"},"id":1}],"lastModifiedDate":"2025-09-23T16:28:15.729749","indexId":"pp1267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1267","title":"Geology of the Carlin gold deposit, Nevada","docAbstract":"This report describes the geology of the Carlin gold deposit and the Lynn mining district, including an area of about 80km2 in northern Eureka County, Nev. (fig. 1). The Carlin mine is located in secs. 13 and 14, T.35N., R.50E., at an elevation of 6,400 ft near the crest of the Tuscarora Mountains. The map area (pl. 1), centered approximately on the Carlin mine, measures about 10km east-west by 8km north-south and forms approximately the south two-thirds of the Rodeo Creek NE. 7{1/2}-minute quadrangle. Boundaries for the map area are meridians 116°15'00\" and 116°22'30\" W. and parallels 40°52'30\" and 40°57'30\"N.
The Carlin mine is accessible by an asphalt-surfaced road extending about 35km northward from the town of Carlin, Nev., which is on U.S. Highway 40. A secondary improved road extends from the Carlin mine westward into Boulder Valley and connects with both State Highway 18 to the north and U.S. Highway 40 to the south near the town of Dunphy. An unimproved road extends from the Carlin mine northward, along the west side of Little Boulder Basin, to the Blue Star mine, and continues northward and westward along Rodeo Creek to connect with a graded road extending northeastward along Boulder Valley. Numerous unimproved roads have been built to provide access to the different mining prospects.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1267","usgsCitation":"Radtke, A.S., 1985, Geology of the Carlin gold deposit, Nevada: U.S. Geological Survey Professional Paper 1267, Report: vi, 124 p.; 6 Plates: 51.75 x 48.32 inches or smaller, https://doi.org/10.3133/pp1267.","productDescription":"Report: vi, 124 p.; 6 Plates: 51.75 x 48.32 inches or smaller","costCenters":[],"links":[{"id":495910,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4778.htm","linkFileType":{"id":5,"text":"html"}},{"id":340314,"rank":8,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1267/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":268920,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1267/plate-6.pdf","text":"Plate 6","size":"24.06 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 6"},{"id":268919,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1267/plate-5.pdf","text":"Plate 5","size":"20.45 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 5"},{"id":139718,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":268915,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1267/plate-1.pdf","text":"Plate 1","size":"50.42 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":268916,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1267/plate-2.pdf","text":"Plate 2","size":"52.84 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":268917,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1267/plate-3.pdf","text":"Plate 3","size":"23.34 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":268918,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1267/plate-4.pdf","text":"Plate 4","size":"22.80 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 4"}],"country":"United States","state":"Nevada","county":"Eureka","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.2,\n 40.8\n ],\n [\n -116.4,\n 40.8\n ],\n [\n -116.4,\n 41\n ],\n [\n -116.2,\n 41\n ],\n [\n -116.2,\n 40.8\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"The report's table of contents has Plates 1 and 2 listed as 2 separate maps. They are published as combined into plate 1 and plates 3-7 are subsequently numbered 2-6.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68314a","contributors":{"authors":[{"text":"Radtke, Arthur S.","contributorId":63795,"corporation":false,"usgs":true,"family":"Radtke","given":"Arthur","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":152461,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}