The location and extent of 11 kinds of surficial deposits in Orwell quadrangle, Oswego County, N.Y., are mapped on a 7.5-minute U.S. Geological Survey topographic map. The map was compiled to indicate the lithology and potential for groundwater development at any specific location.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801116","usgsCitation":"Miller, T.S., 1980, Surficial geology of Orwell quadrangle, Oswego County, New York (WRI/OFR): U.S. Geological Survey Open-File Report 80-1116, 1 Plate: 24.14 × 26.88 inches, https://doi.org/10.3133/ofr801116.","productDescription":"1 Plate: 24.14 × 26.88 inches","costCenters":[],"links":[{"id":155548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":53125,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1116/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397644,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75346.htm"}],"country":"United States","state":"New York","county":"Oswego County","otherGeospatial":"Orwell quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76,\n 43.5\n ],\n [\n -75.875,\n 43.5\n ],\n [\n -75.875,\n 43.625\n ],\n [\n -76,\n 43.625\n ],\n [\n -76,\n 43.5\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e487fe4b07f02db515581","contributors":{"authors":[{"text":"Miller, Todd S. tsmiller@usgs.gov","contributorId":1190,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"tsmiller@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":190972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46113,"text":"ofr80748 - 1980 - Maps showing dissolved solids concentration of water in the Red River Formation and Mission Canyon Limestone in North Dakota, South Dakota, and parts of Wyoming, and Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:14","indexId":"ofr80748","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-748","title":"Maps showing dissolved solids concentration of water in the Red River Formation and Mission Canyon Limestone in North Dakota, South Dakota, and parts of Wyoming, and Montana","language":"ENGLISH","doi":"10.3133/ofr80748","usgsCitation":"Stenzil, S.R., Buss, R., and Busby, J., 1980, Maps showing dissolved solids concentration of water in the Red River Formation and Mission Canyon Limestone in North Dakota, South Dakota, and parts of Wyoming, and Montana: U.S. Geological Survey Open-File Report 80-748, 2 maps ;108 x 154 cm., https://doi.org/10.3133/ofr80748.","productDescription":"2 maps ;108 x 154 cm.","costCenters":[],"links":[{"id":169455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20019,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0748/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20020,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0748/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604b39","contributors":{"authors":[{"text":"Stenzil, Sheila R.","contributorId":98998,"corporation":false,"usgs":true,"family":"Stenzil","given":"Sheila","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":232639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buss, R.","contributorId":83796,"corporation":false,"usgs":true,"family":"Buss","given":"R.","email":"","affiliations":[],"preferred":false,"id":232638,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Busby, John F.","contributorId":42186,"corporation":false,"usgs":true,"family":"Busby","given":"John F.","affiliations":[],"preferred":false,"id":232637,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23917,"text":"ofr801115 - 1980 - Surficial geology of part of Boylston Center quadrangle, Oswego County, New York","interactions":[],"lastModifiedDate":"2022-03-25T21:15:51.070223","indexId":"ofr801115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1115","title":"Surficial geology of part of Boylston Center quadrangle, Oswego County, New York","docAbstract":"The location and extent of seven kinds of surficial deposits in part of Boylston Center quadrangle, Oswego County, N.Y., are mapped on a 7.5-minute U.S. Geological Survey topographic map. The map was compiled to indicate the lithology and potential for groundwater development at any specific location.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801115","usgsCitation":"Miller, T.S., 1980, Surficial geology of part of Boylston Center quadrangle, Oswego County, New York (WRI/OFR): U.S. Geological Survey Open-File Report 80-1115, 1 Plate: 23.86 × 27.11 inches, https://doi.org/10.3133/ofr801115.","productDescription":"1 Plate: 23.86 × 27.11 inches","costCenters":[],"links":[{"id":397646,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75345.htm"},{"id":53127,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1115/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"New York","county":"Oswego County","otherGeospatial":"Boylston Center quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76,\n 43.75\n ],\n [\n -75.875,\n 43.75\n ],\n [\n -75.875,\n 43.625\n ],\n [\n -76,\n 43.625\n ],\n [\n -76,\n 43.75\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b6e4b07f02db5342ae","contributors":{"authors":[{"text":"Miller, Todd S. tsmiller@usgs.gov","contributorId":1190,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"tsmiller@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":190974,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23919,"text":"ofr801114 - 1980 - Surficial geology of part of Sandy Creek quadrangle, Oswego County, New York","interactions":[],"lastModifiedDate":"2022-03-25T21:38:12.899738","indexId":"ofr801114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1114","title":"Surficial geology of part of Sandy Creek quadrangle, Oswego County, New York","docAbstract":"The location and extent of 11 kinds of surficial deposits in part of Sandy Creek quadrangle, Oswego County, N.Y., are mapped on a 7.5-minute U.S. Geological Survey topographic map. The map was compiled to indicate the lithology and potential for groundwater development at any specific location.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801114","usgsCitation":"Miller, T.S., 1980, Surficial geology of part of Sandy Creek quadrangle, Oswego County, New York (WRI/OFR): U.S. Geological Survey Open-File Report 80-1114, 1 Plate: 23.61 × 26.58 inches, https://doi.org/10.3133/ofr801114.","productDescription":"1 Plate: 23.61 × 26.58 inches","costCenters":[],"links":[{"id":157039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":397648,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75344.htm"},{"id":53129,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1114/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New York","county":"Oswego County","otherGeospatial":"Sandy Creek quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76,\n 43.7167\n ],\n [\n -76.125,\n 43.7167\n ],\n [\n -76.125,\n 43.625\n ],\n [\n -76,\n 43.625\n ],\n [\n -76,\n 43.7167\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e481ee4b07f02db4e00ee","contributors":{"authors":[{"text":"Miller, Todd S. tsmiller@usgs.gov","contributorId":1190,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"tsmiller@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":190976,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23582,"text":"ofr80807 - 1980 - The heliothermic lake: a direct method of collecting and storing solar energy","interactions":[],"lastModifiedDate":"2018-01-31T16:08:18","indexId":"ofr80807","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-807","title":"The heliothermic lake: a direct method of collecting and storing solar energy","docAbstract":"Heliothermic lakes contain a sun-heated layer of warm, saline water beneath a surface layer of cooler, less saline water. The two layers are separated by a chemocline, a stratum in which salinity increases progressively with depth. The chemocline, the position of which varies from lake to lake, functions as a heat trap. Most sunlight that penetrates this stratum is transformed into heat, which cannot escape by radiation because water is opaque to infrared light, and which cannot escape by convection because the specific gravity of the dense water below the chemocline is not significantly decreased by the increasing temperature. Heat can escape only by conduction through the chemocline, and water or brine is a very poor conductor. As a result, the temperature within and commonly below the chemocline rises. Under ideal conditions of a clear solution, high isolation, and a suitable salinity distribution, the temperature of the chemocline will increase to the boiling point. The lower part of the chemocline in a shallow (0.8-m) manmade heliothermic lake at Sedom, Israel, for example, reached a temperature of 96°C (205°F) in spite of a brine with poor light transmissibility.
About 30 natural heliothermic lakes have been reported. The best known, Lake Ursului, occurs in Transylvania, Romania (latitude, 46°35'N). During four consecutive summers, 1899 to 1902, this lake had temperatures of 60-70°C (140-158°F) at a depth of 1-2 m. Heliothermic conditions have persisted in this lake for at least 28 and probably for more than 77 years. The most unusual, Lake Vanda, Victoria Land, Antarctica (latitude, 77°35'S), has a temperature of 26°C near the base of the chemocline at a depth of 61 despite a mean atmospheric temperature of -20°C. Sunlight penetrates into the chemocline through 5 m of remarkably clear ice.
Maintenance of the chemocline is the chief problem preventing commercial use of manmade heliothermic lakes for the collection and storage of solar energy. The most effective means of preserving this stratum from destruction by diffusion and wind mixing may be the use of salts, such as sodium sulfate and sodium borate, whose solubilities are markedly influenced by temperature. The chemoclines of ponds constructed with such salts, in theory, would persist indefinitely and could be of great size.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80807","issn":"0094-9140","usgsCitation":"Kirkland, D.W., Bradbury, J.P., and Dean, W.E., 1980, The heliothermic lake: a direct method of collecting and storing solar energy: U.S. Geological Survey Open-File Report 80-807, vi, 126 p., https://doi.org/10.3133/ofr80807.","productDescription":"vi, 126 p.","costCenters":[],"links":[{"id":156442,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0807/report-thumb.jpg"},{"id":350863,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0807/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655576","contributors":{"authors":[{"text":"Kirkland, Douglas W.","contributorId":10067,"corporation":false,"usgs":true,"family":"Kirkland","given":"Douglas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":190355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradbury, J. Platt","contributorId":91106,"corporation":false,"usgs":true,"family":"Bradbury","given":"J.","email":"","middleInitial":"Platt","affiliations":[],"preferred":false,"id":190356,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":190354,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23933,"text":"ofr801195 - 1980 - Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978","interactions":[],"lastModifiedDate":"2013-08-02T08:00:06","indexId":"ofr801195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1195","title":"Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978","docAbstract":"This report describes the observation-well network in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough Counties, Florida. Data obtained in 1978 from the network in and adjacent to the two well fields, as well as rainfall and pumpage records, are presented. The Southwest Florida Water Management District has established regulatory water-level limits in four observation wells and water-quality limits in three observation wells. Water levels dropped below regulatory limits in the spring of 1978 in three wells. Chloride concentrations in 1978 remained above regulatory limits for the entire year in one well and exceeded the limit during the late spring in the other two deep wells, both west of Eldridge-Wilde well field. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr801195","issn":"0094-9140","usgsCitation":"Mills, L.R., 1980, Hydrologic monitoring program in Eldridge-Wilde and East Lake Road well-field areas, Pinellas and Hillsborough counties, Florida, 1978: U.S. Geological Survey Open-File Report 80-1195, iv, 27 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr801195.","productDescription":"iv, 27 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":156575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1195/report-thumb.jpg"},{"id":275925,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1195/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606973","contributors":{"authors":[{"text":"Mills, L. R.","contributorId":26281,"corporation":false,"usgs":true,"family":"Mills","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":190997,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41425,"text":"ofr80364 - 1980 - Preliminary geologic map of the eastern end of the upper zones of the Stillwater Complex, Stillwater County, Montana","interactions":[{"subject":{"id":41425,"text":"ofr80364 - 1980 - Preliminary geologic map of the eastern end of the upper zones of the Stillwater Complex, Stillwater County, Montana","indexId":"ofr80364","publicationYear":"1980","noYear":false,"title":"Preliminary geologic map of the eastern end of the upper zones of the Stillwater Complex, Stillwater County, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":67110,"text":"i1383 - 1982 - Geologic map of the banded upper zone of the Stillwater complex and adjacent rocks, Stillwater, Sweet Grass, and Park counties, Montana","indexId":"i1383","publicationYear":"1982","noYear":false,"title":"Geologic map of the banded upper zone of the Stillwater complex and adjacent rocks, Stillwater, Sweet Grass, and Park counties, Montana"},"id":1}],"supersededBy":{"id":67110,"text":"i1383 - 1982 - Geologic map of the banded upper zone of the Stillwater complex and adjacent rocks, Stillwater, Sweet Grass, and Park counties, Montana","indexId":"i1383","publicationYear":"1982","noYear":false,"title":"Geologic map of the banded upper zone of the Stillwater complex and adjacent rocks, Stillwater, Sweet Grass, and Park counties, Montana"},"lastModifiedDate":"2022-03-23T13:42:59.07662","indexId":"ofr80364","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-364","title":"Preliminary geologic map of the eastern end of the upper zones of the Stillwater Complex, Stillwater County, Montana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80364","usgsCitation":"Segerstrom, K.K., and Carlson, R.R., 1980, Preliminary geologic map of the eastern end of the upper zones of the Stillwater Complex, Stillwater County, Montana: U.S. Geological Survey Open-File Report 80-364, 1 Plate: 32.46 x 28.51 inches, https://doi.org/10.3133/ofr80364.","productDescription":"1 Plate: 32.46 x 28.51 inches","costCenters":[],"links":[{"id":397449,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11616.htm"},{"id":397399,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0364/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0364/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Montana","county":"Stillwater County","otherGeospatial":"Stillwater Complex","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.25,45.333333333333336 ], [ -110.25,45.5 ], [ -109.75,45.5 ], [ -109.75,45.333333333333336 ], [ -110.25,45.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c35b","contributors":{"authors":[{"text":"Segerstrom, Kenneth K.","contributorId":105276,"corporation":false,"usgs":true,"family":"Segerstrom","given":"Kenneth","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":834512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlson, R. 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1985 - Geologic map of the Arlington West 7.5 minute Quadrangle, Snohomish County, Washington","indexId":"mf1740","publicationYear":"1985","noYear":false,"title":"Geologic map of the Arlington West 7.5 minute Quadrangle, Snohomish County, Washington"},"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr80461","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-461","title":"Distribution and description of the geologic units in the Arlington West Quadrangle, Washington","language":"ENGLISH","publisher":"United States Dept. of Interior, Geological Survey,","doi":"10.3133/ofr80461","issn":"0094-9140","usgsCitation":"Minard, J.P., 1980, Distribution and description of the geologic units in the Arlington West Quadrangle, Washington: U.S. Geological Survey Open-File Report 80-461, 1 map ;58 x 38 cm. +1 text (8 p. ; 28 cm.), https://doi.org/10.3133/ofr80461.","productDescription":"1 map ;58 x 38 cm. +1 text (8 p. ; 28 cm.)","costCenters":[],"links":[{"id":108038,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11643.htm","linkFileType":{"id":5,"text":"html"},"description":"11643"},{"id":154908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649cce","contributors":{"authors":[{"text":"Minard, James P.","contributorId":84761,"corporation":false,"usgs":true,"family":"Minard","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":191007,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23939,"text":"ofr80462 - 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These models have been used to provide information and predictions for water managers. Too frequently, groundwater was neglected in water-resource planning because managers believed that it could not be adequately evaluated in terms of availability, quality, and effect of development on surface water supplies. Now, however, with newly developed digital groundwater models, effects of development can be predicted. Such models have been used to predict hydrologic and quality changes under different stresses. These models have grown in complexity over the last 10 years from simple one-layer flow models to three-dimensional simulations of groundwater flow which may include solute transport, heat transport, effects of land subsidence, and encroachment of salt water. This paper illustrates, through case histories, how predictive groundwater models have provided the information needed for the sound planning and management of water resources in the United States. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80880","usgsCitation":"Mosier, E.L., Ludington, S.D., and Yeoman, R.A., 1980, Analyses of rocks and stream sediments from the Hunter-Fryingpan Wilderness Area and the Porphyry Mountain Wilderness Study Area, Pitkin County, Colorado: U.S. Geological Survey Open-File Report 80-880, i, 118 p., https://doi.org/10.3133/ofr80880.","productDescription":"i, 118 p.","costCenters":[],"links":[{"id":404089,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75306.htm","linkFileType":{"id":5,"text":"html"}},{"id":53167,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0880/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0880/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Pitkin County","otherGeospatial":"Hunter-Fryingpan Wilderness Area and the Porphyry Mountain Wilderness Study Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.5,\n 39.0917\n ],\n [\n -106.75,\n 39.0917\n ],\n [\n -106.75,\n 39.3319\n ],\n [\n -106.5,\n 39.3319\n ],\n [\n -106.5,\n 39.0917\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680e42","contributors":{"authors":[{"text":"Mosier, Elwin L.","contributorId":70374,"corporation":false,"usgs":true,"family":"Mosier","given":"Elwin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191072,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ludington, Steve D.","contributorId":10807,"corporation":false,"usgs":true,"family":"Ludington","given":"Steve","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":191071,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yeoman, R. 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The cost effectiveness of 19 stream gages in terms of minimizing the sum of the variances of the errors of estimation of annual mean discharge is explored by means of a sequential-search optimization scheme. The search is conducted over a set of decision variables that describes the number of times that each gaging route is traveled in a year. A gage route is defined as the most expeditious circuit that is made from a field office to visit one or more stream gages and return to the office. The error variance is defined as a function of the frequency of visits to a gage by using optimal estimation theory. Currently a minimum of 12 visits per year is made to any gage. By changing to a six-visit minimum, the same total error variance can be attained for the 19 stations with a budget of 10% less than the current one. Other strategies are also explored. 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