Brevard County is an area of some 1,300 square miles located on the east coast of central Florida. The Titusville SW Quadrangle, in northern Brevard, includes part of the St. Johns River channel and valley with extensive areas of relatively low marshlands. Approximately one half of the quadrangle area lies in Orange, Seminole, and Volusia Counties.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78190","collaboration":"Prepared in cooperation with the Brevard County Board of County Commissioners","usgsCitation":"Frazee, J.M., and Laughlin, C.P., 1978, Hydrologic overlay maps of the Titusville SW Quadrangle, Brevard County, Florida: U.S. Geological Survey Open-File Report 78-190, 5 Plates: 24.17 x 36.12 inches or smaller, https://doi.org/10.3133/ofr78190.","productDescription":"5 Plates: 24.17 x 36.12 inches or smaller","costCenters":[],"links":[{"id":431636,"rank":6,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0190/sheet-5.pdf","text":"Sheet 5","linkFileType":{"id":1,"text":"pdf"}},{"id":431635,"rank":5,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0190/sheet-4.pdf","text":"Sheet 4","linkFileType":{"id":1,"text":"pdf"}},{"id":431634,"rank":4,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0190/sheet-3.pdf","text":"Sheet 3","linkFileType":{"id":1,"text":"pdf"}},{"id":431633,"rank":3,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0190/sheet-2.pdf","text":"Sheet 2","linkFileType":{"id":1,"text":"pdf"}},{"id":431632,"rank":2,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0190/sheet-1.pdf","text":"Sheet 1","linkFileType":{"id":1,"text":"pdf"}},{"id":168652,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0190/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Brevard County","otherGeospatial":"Titusville SW Quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.95578024549009,\n 28.70602324122642\n ],\n [\n -80.95578024549009,\n 27.95243335422809\n ],\n [\n -80.46378179500127,\n 27.95243335422809\n ],\n [\n -80.46378179500127,\n 28.70602324122642\n ],\n [\n -80.95578024549009,\n 28.70602324122642\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6057a3","contributors":{"authors":[{"text":"Frazee, James M. Jr.","contributorId":83887,"corporation":false,"usgs":true,"family":"Frazee","given":"James","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":228435,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laughlin, Charles P.","contributorId":6490,"corporation":false,"usgs":true,"family":"Laughlin","given":"Charles","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":228434,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":43595,"text":"ofr78192 - 1978 - Hydrologic overlay maps of the Titusville Quadrangle, Brevard County, Florida","interactions":[],"lastModifiedDate":"2024-07-30T18:50:45.021196","indexId":"ofr78192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-192","title":"Hydrologic overlay maps of the Titusville Quadrangle, Brevard County, Florida","docAbstract":"Brevard County is an area of some 1,300 square miles located on the east coast of central Florida. The Titusville quadrangle, in northern Brevard, includes part of the Atlanta Coastal Ridge, an area of relatively high sand ridges that are generally above 30 feet in altitude (sheet 1). Approximately the western one third of the quadrangle is in relatively low marshlands of the St. Johns River valley. The eastern part of the quadrangle contains estuarine waters of the Indian River and a small portion of the John F. Kennedy Space Center on Merritt Island.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78192","usgsCitation":"Frazee, J.M., and Laughlin, C.P., 1978, Hydrologic overlay maps of the Titusville Quadrangle, Brevard County, Florida: U.S. Geological Survey Open-File Report 78-192, 7 Plates: 24.12 x 36.14 inches or smaller, https://doi.org/10.3133/ofr78192.","productDescription":"7 Plates: 24.12 x 36.14 inches or smaller","costCenters":[],"links":[{"id":431645,"rank":8,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0192/sheet-7.pdf","text":"Sheet 7","linkFileType":{"id":1,"text":"pdf"}},{"id":431644,"rank":7,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0192/sheet-6.pdf","text":"Sheet 6","linkFileType":{"id":1,"text":"pdf"}},{"id":431643,"rank":6,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0192/sheet-5.pdf","text":"Sheet 5","linkFileType":{"id":1,"text":"pdf"}},{"id":431642,"rank":5,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0192/sheet-4.pdf","text":"Sheet 4","linkFileType":{"id":1,"text":"pdf"}},{"id":431641,"rank":4,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0192/sheet-3.pdf","text":"Sheet 3","linkFileType":{"id":1,"text":"pdf"}},{"id":431640,"rank":3,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0192/sheet-2.pdf","text":"Sheet 2","linkFileType":{"id":1,"text":"pdf"}},{"id":431639,"rank":2,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/of/1978/0192/sheet-1.pdf","text":"Sheet 1","linkFileType":{"id":1,"text":"pdf"}},{"id":168553,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0192/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Brevard County","otherGeospatial":"Titusville Quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.95578024549009,\n 28.70602324122642\n ],\n [\n -80.95578024549009,\n 27.95243335422809\n ],\n [\n -80.46378179500127,\n 27.95243335422809\n ],\n [\n -80.46378179500127,\n 28.70602324122642\n ],\n [\n -80.95578024549009,\n 28.70602324122642\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605750","contributors":{"authors":[{"text":"Frazee, James M. Jr.","contributorId":83887,"corporation":false,"usgs":true,"family":"Frazee","given":"James","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":228433,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laughlin, Charles P.","contributorId":6490,"corporation":false,"usgs":true,"family":"Laughlin","given":"Charles","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":228432,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":20271,"text":"ofr78959 - 1978 - Hydrologic information for land-use planning, Fairbanks vicinity, Alaska","interactions":[],"lastModifiedDate":"2021-12-17T22:40:18.314429","indexId":"ofr78959","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-959","title":"Hydrologic information for land-use planning, Fairbanks vicinity, Alaska","docAbstract":"The flood plain on the Chena and Tanana Rivers near Fairbanks, Alaska, has abundant water in rivers and in an unconfined alluvial aquifer. The principal source of ground water is the Tanana River, from which ground water flows northwesterly to the Chena River. Transmissivity of the aquifer commonly exceed 100 ,000 sq ft. The shallow water table (less than 15 ft below land surface), high hydraulic conductivity of the sediments and cold soil give the flood plain a high susceptibility to pollution by onsite sewerage systems. The Environmental Protection Agency recommended maximum concentrations for drinking water may be exceeded in surface water for manganese and bacteria and in ground water for iron, manganese, and bacteria. Residents of the uplands obtain water principally from a widely-distributed fractured schist aquifer. The aquifer is recharged by local infiltration of precipitation and is drained by springs on the lower slopes and by ground-water flow to alluvial aquifers of the valleys. The annual base flow from basins in the uplands ranged from 3,000 to 100,000 gallons per acre; the smallest base flows occur in basins nearest the city of Fairbanks. The thick silt cover and great depth to the water table give much of the uplands a low susceptibility to pollution by onsite sewage disposal. Ground water is locally high in nitrate, arsenic, iron , and manganese. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78959","usgsCitation":"Nelson, G.L., 1978, Hydrologic information for land-use planning, Fairbanks vicinity, Alaska: U.S. Geological Survey Open-File Report 78-959, vi, 47 p., https://doi.org/10.3133/ofr78959.","productDescription":"vi, 47 p.","costCenters":[],"links":[{"id":152287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94448,"rank":800,"type":{"id":15,"text":"Index Page"},"url":"https://dggs.alaska.gov/pubs/id/11192"},{"id":393068,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14970.htm"}],"country":"United States","state":"Alaska","city":"Fairbanks","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -148.326416015625,\n 64.73429692356085\n ],\n [\n -147.3211669921875,\n 64.73429692356085\n ],\n [\n -147.3211669921875,\n 65.00026079026213\n ],\n [\n -148.326416015625,\n 65.00026079026213\n ],\n [\n -148.326416015625,\n 64.73429692356085\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606a25","contributors":{"authors":[{"text":"Nelson, Gordon L.","contributorId":55443,"corporation":false,"usgs":true,"family":"Nelson","given":"Gordon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":182362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30488,"text":"wri7781 - 1978 - Water resources of northeast North Carolina","interactions":[],"lastModifiedDate":"2019-07-22T10:15:25","indexId":"wri7781","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"77-81","title":"Water resources of northeast North Carolina","docAbstract":"Several water-related problems are associated with economic development of northeast North Carolina. The solution to these problems depends in part on adequate knowledge of the hydrology of this 8,930 square mile coastal area. Average annual precipitation on the area is about 50 inches. Of this amount, about 34 inches returns to the atmosphere by evapotranspiration, about 15 inches leaves the area as runoff, and about one inch leaves through ground-water outflow. No large stream originates within the area, but major streams entering from the north and west bring in three times as much streamflow as originates within the study area. The flat, low-lying terrane does not offer opportunities for extensive development of surface-water supplies through the use of reservoirs. Much of the surface water is contaminated by saltwater from the ocean. Ground water occurs in three major aquifers, all of which contain both freshwater and saltwater.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7781","usgsCitation":"Wilder, H.B., Robison, T.M., and Lindskov, K., 1978, Water resources of northeast North Carolina: U.S. Geological Survey Water-Resources Investigations Report 77-81, x, 113 p. , https://doi.org/10.3133/wri7781.","productDescription":"x, 113 p. 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Carolina\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3b8c","contributors":{"authors":[{"text":"Wilder, Hugh B.","contributorId":83899,"corporation":false,"usgs":true,"family":"Wilder","given":"Hugh","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":203338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robison, Tully M.","contributorId":77969,"corporation":false,"usgs":true,"family":"Robison","given":"Tully","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":203337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lindskov, K.L.","contributorId":91077,"corporation":false,"usgs":true,"family":"Lindskov","given":"K.L.","affiliations":[],"preferred":false,"id":203339,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30340,"text":"wri7830 - 1978 - Effects of land use and water management on water quality in the western South New River Canal basin: southeast Florida, 1974-75","interactions":[],"lastModifiedDate":"2019-11-13T10:27:30","indexId":"wri7830","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-30","title":"Effects of land use and water management on water quality in the western South New River Canal basin: southeast Florida, 1974-75","docAbstract":"The South New River Canal (C-11) basin between water-control structures S-9 and S-13 is an area that is primarily undeveloped and the system of waterways within the basin is highly controlled for water-management purposes. Most of the recharge to the canals is by induced ground-water inflow and seepage. The chemical character of the surface and ground waters in inundated areas is mixed calcium-bicarbonate and sodium-chloride type. Inorganic nitrogen concentrations in surface waters are slightly higher in developed areas than in undeveloped areas. Concentrations of inorganic nitrogen in ground water in drained areas are 2-4 times greater than in undeveloped inundated areas. Average orthophosphate concentrations are uniformly low (0.01 to 0.03 milligrams per liter) throughout the basin. Total residue concentrations are fairly uniform throughout the basin and fluctuate primarily in response to hydrologic conditions. Runoff and load-discharge indices indicated that the loads of inorganic nitrogen, total residue, and phosphorus, and the discharge per unit of land drained were uniform throughout most of the basin. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7830","usgsCitation":"Waller, B., 1978, Effects of land use and water management on water quality in the western South New River Canal basin: southeast Florida, 1974-75: U.S. Geological Survey Water-Resources Investigations Report 78-30, v, 56 p. , https://doi.org/10.3133/wri7830.","productDescription":"v, 56 p. ","costCenters":[],"links":[{"id":159302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"South New River Canal basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.21942138671875,\n 26.04999729224954\n ],\n [\n -80.19950866699219,\n 26.04999729224954\n ],\n [\n -80.19950866699219,\n 26.069736109561056\n ],\n [\n -80.21942138671875,\n 26.069736109561056\n ],\n [\n -80.21942138671875,\n 26.04999729224954\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611d5d","contributors":{"authors":[{"text":"Waller, B.G.","contributorId":75970,"corporation":false,"usgs":true,"family":"Waller","given":"B.G.","email":"","affiliations":[],"preferred":false,"id":203087,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29499,"text":"wri7879 - 1978 - Model evaluation of the hydrogeology of the Cypress Creek well field in west-central Florida","interactions":[],"lastModifiedDate":"2022-02-22T20:54:59.21227","indexId":"wri7879","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-79","title":"Model evaluation of the hydrogeology of the Cypress Creek well field in west-central Florida","docAbstract":"The Cypress Creek well field is being developed to help supply a rapidly growing population in west-central Florida. The ground-water system in the Cypress Creek well-field area consists of a surficial sand aquifer, a semiconfining clay layer ranging from 2 to 25 feet in thickness, and a sequence of carbonate rocks, approximately 1,000 feet thick, called the Floridan aquifer. All recharge to the Floridan aquifer in the local area is derived from the overlying surficial sand aquifer by downward percolation through the semiconfining clay bed. The major proportion of water supplied to municipal wells open to the Floridan aquifer comes from a dolomitic section of the Avon Park Limestone containing two major cavernous zones. The hydrogeology of the well-field area was evaluated by digital model simulation. Model runs were made to analyze sensitivity of the model to variations in selected hydrologic parameters. The model was tested further by attempting to simulate the potentiometric surface of the Floridan aquifer under actual pumping stresses during the January 1976 dry period.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7879","usgsCitation":"Ryder, P.D., 1978, Model evaluation of the hydrogeology of the Cypress Creek well field in west-central Florida: U.S. Geological Survey Water-Resources Investigations Report 78-79, vi, 68 p., https://doi.org/10.3133/wri7879.","productDescription":"vi, 68 p.","costCenters":[],"links":[{"id":95763,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0079/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396279,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35268.htm"},{"id":159692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0079/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Cypress Creek well field","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.45376586914062,\n 28.177349313680605\n ],\n [\n -82.26150512695312,\n 28.177349313680605\n ],\n [\n -82.26150512695312,\n 28.414352008722247\n ],\n [\n -82.45376586914062,\n 28.414352008722247\n ],\n [\n -82.45376586914062,\n 28.177349313680605\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4dae","contributors":{"authors":[{"text":"Ryder, Paul D.","contributorId":60188,"corporation":false,"usgs":true,"family":"Ryder","given":"Paul","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":201612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12239,"text":"ofr78770 - 1978 - Preparation of a geologic photo map and hydrologic study of the Yemen Arab Republic","interactions":[],"lastModifiedDate":"2018-08-21T13:24:03","indexId":"ofr78770","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-770","title":"Preparation of a geologic photo map and hydrologic study of the Yemen Arab Republic","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78770","usgsCitation":"Grolier, M.J., Ibrahim, M., Overstreet, W., Tibbitts, G., and Davidson, D., 1978, Preparation of a geologic photo map and hydrologic study of the Yemen Arab Republic: U.S. Geological Survey Open-File Report 78-770, ii, 15 p. :maps ;28 cm.; (20 p. - PGS), https://doi.org/10.3133/ofr78770.","productDescription":"ii, 15 p. :maps ;28 cm.; (20 p. - PGS)","costCenters":[],"links":[{"id":146216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0770/report-thumb.jpg"},{"id":40399,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0770/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669228","contributors":{"authors":[{"text":"Grolier, Maurice J.","contributorId":98292,"corporation":false,"usgs":true,"family":"Grolier","given":"Maurice","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":165601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ibrahim, M.","contributorId":10797,"corporation":false,"usgs":true,"family":"Ibrahim","given":"M.","email":"","affiliations":[],"preferred":false,"id":165598,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Overstreet, W.C.","contributorId":105294,"corporation":false,"usgs":true,"family":"Overstreet","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":165602,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tibbitts, G. Chase","contributorId":79453,"corporation":false,"usgs":true,"family":"Tibbitts","given":"G. Chase","affiliations":[],"preferred":false,"id":165600,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Davidson, D.F.","contributorId":68293,"corporation":false,"usgs":true,"family":"Davidson","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":165599,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":56405,"text":"wdrCA764 - 1978 - Water resources data for California, water year 1976; Volume 4: Northern Central Valley basins and the Great Basin from Honey Lake basin to Oregon State line","interactions":[],"lastModifiedDate":"2012-06-13T01:01:47","indexId":"wdrCA764","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-76-4","title":"Water resources data for California, water year 1976; Volume 4: Northern Central Valley basins and the Great Basin from Honey Lake basin to Oregon State line","docAbstract":"Water-resources data for the 1976 water year for California consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; records of water levels in selected observation wells; and selected chemical analyses of ground water. Records for a few pertinent streamflow and water-quality stations in bordering States are also included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Lee R. Peterson, district chief; Winchell Smith, assistant district chief for hydrologic data; and Leonard N. Jorgensen, chief of the basic-data section. These data, a contribution to the National Water Data System, were collected by the Geological Survey and cooperating local, State, and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA764","usgsCitation":"California District of the Water Resources Division, 1978, Water resources data for California, water year 1976; Volume 4: Northern Central Valley basins and the Great Basin from Honey Lake basin to Oregon State line: U.S. Geological Survey Water Data Report CA-76-4, 404 p., https://doi.org/10.3133/wdrCA764.","productDescription":"404 p.","costCenters":[],"links":[{"id":181330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_76_4.jpg"},{"id":257452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1976/ca-76/WDR-1976-vol4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f765d","contributors":{"authors":[{"text":"California District of the Water Resources Division","contributorId":127979,"corporation":true,"usgs":false,"organization":"California District of the Water Resources Division","id":532586,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56461,"text":"wdrCA773 - 1978 - Water resources data for California, water year 1977; Volume 3: Southern Central Valley basins and the Great Basin from Walker River to Truckee River","interactions":[],"lastModifiedDate":"2012-06-13T01:01:47","indexId":"wdrCA773","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-77-3","title":"Water resources data for California, water year 1977; Volume 3: Southern Central Valley basins and the Great Basin from Walker River to Truckee River","docAbstract":"Water-resources data for the 1977 water year for California consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; records of water levels in selected observation wells; and selected chemical analyses of ground water. Records for a few pertinent streamflow and water-quality stations in bordering States are also included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Winchell Smith, Assistant District Chief for Hydrologic Data and Leonard N. Jorgensen, Chief of the Basic-Data Section. These data, a contribution to the National Water Data System, were collected by the Geological Survey and cooperating local, State, and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA773","usgsCitation":"California District of the Water Resources Division, 1978, Water resources data for California, water year 1977; Volume 3: Southern Central Valley basins and the Great Basin from Walker River to Truckee River: U.S. Geological Survey Water Data Report CA-77-3, 396 p., https://doi.org/10.3133/wdrCA773.","productDescription":"396 p.","costCenters":[],"links":[{"id":185353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_77_3.jpg"},{"id":257455,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1977/ca-77/WDR-1977-vol3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634c31","contributors":{"authors":[{"text":"California District of the Water Resources Division","contributorId":127979,"corporation":true,"usgs":false,"organization":"California District of the Water Resources Division","id":532642,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24982,"text":"pp1100 - 1978 - Geological Survey research 1978","interactions":[],"lastModifiedDate":"2025-01-07T19:14:26.272055","indexId":"pp1100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1100","title":"Geological Survey research 1978","docAbstract":"This U.S. Geological Survey activities report includes a summary of 1978 fiscal year scientific and economic results accompanied by a list of geologic and hydrologic investigations in progress and a report on the status of topographic mapping. The summary of results includes: (1) Mineral and water resources, (2) Engineering geology and hydrology, (3) Regional geology, (4) Principles and processes, (5) Laboratory and field methods, (6) Topographic surveys and mapping, (7) Management of resources on public lands, (8) Land information and analysis, and (9) Investigations in other countries. Also included are lists of cooperating agencies and Geological Survey offices. 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Kathleen M. kjohnson@usgs.gov","contributorId":2110,"corporation":false,"usgs":true,"family":"Johnson","given":"Kathleen","email":"kjohnson@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":660852,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":4439,"text":"cir772A - 1978 - The United States Geological Survey in Alaska; organization and status of programs in 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:05:47","indexId":"cir772A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"772","chapter":"A","title":"The United States Geological Survey in Alaska; organization and status of programs in 1978","docAbstract":"United States Geological Survey projects in Alaska study a wide range of topics of economic and scientific interest. Work done in 1977 includes contributions to economic geology, regional geology, stratigraphy, engineering geology, hydrology, and marine geology. Many maps and reports covering various aspects of the geology and mineral and water resources of the State were published. In addition, the published 1:1,000,000-scale map of the State has been revised in two areas. A bibliography containing 263 reports on Alaska published in 1977 is included. (Woodard-USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, Geological Survey ;\r\ndistributed by Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir772A","usgsCitation":"Johnson, K.M., 1978, The United States Geological Survey in Alaska; organization and status of programs in 1978: U.S. Geological Survey Circular 772, iv, p A1-A63; ill., maps ;27 cm. , https://doi.org/10.3133/cir772A.","productDescription":"iv, p A1-A63; ill., maps ;27 cm. ","costCenters":[],"links":[{"id":139535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1978/0772a/report-thumb.jpg"},{"id":31542,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0772a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6734d0","contributors":{"authors":[{"text":"Johnson, Kathleen M. kjohnson@usgs.gov","contributorId":2110,"corporation":false,"usgs":true,"family":"Johnson","given":"Kathleen","email":"kjohnson@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":149139,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1001,"text":"wsp2042 - 1978 - Mean annual runoff in the upper Ohio River basin, 1941-70, and its historical variation","interactions":[],"lastModifiedDate":"2017-07-07T08:37:22","indexId":"wsp2042","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2042","title":"Mean annual runoff in the upper Ohio River basin, 1941-70, and its historical variation","docAbstract":"A map of the Ohio River basin above the Muskingum River shows patterns of mean annual runoff for the new climatologic and hydrologic reference period, 1941-70, and provides an up-to-date, consistent basis for consideration of this streamflow characteristic. The primary data base consisted of 98 long-term gaging-station records collected within this 27,300-square-mile (70,700-square-kilometer) headwater area of the Ohio River basin. Supplemental information was derived from 83 short-term records. \r\n\r\nMean annual runoff is at a regional minimum of less than 12 inches (300 millimeters) in an area extending from the northern West Virginia panhandle to the headwaters of the Mahoning River in Ohio. Mean annual runoff of more than 32 inches {810 millimeters) occurs in parts of the upper Cheat River basin in West Virginia. The zone of high runoff trends northeastward along the western slopes of tile Allegheny Mountains; magnitudes diminish to about 25 inches (630 millimeters) at the eastern basin boundary near Ebensburg, Pa. Runoff of this magnitude occurs also in a band across tile upper Allegheny River basin in Pennsylvania. \r\n\r\nRatios of mean annual discharge to the 30-year reference-period average were computed for each year of record for all long-term gaging stations. Annual discharges have ranged from about 30 percent to 200 percent of the 30-year mean. Graphed summaries of the annual ratios document the relative duration and magnitude of wet and dry periods during the past 65 years in the upper Ohio River basin.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp2042","usgsCitation":"Beall, R.M., 1978, Mean annual runoff in the upper Ohio River basin, 1941-70, and its historical variation: U.S. Geological Survey Water Supply Paper 2042, iv, 32 p. :ill. (1 fold. in pocket), maps (1 fold. col. in pocket) ;23 cm. --, https://doi.org/10.3133/wsp2042.","productDescription":"iv, 32 p. :ill. (1 fold. in pocket), maps (1 fold. col. in pocket) ;23 cm. --","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":136144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2042/report-thumb.jpg"},{"id":94696,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2042/plate-table_3.pdf","size":"1104","linkFileType":{"id":1,"text":"pdf"}},{"id":25572,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2042/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610780","contributors":{"authors":[{"text":"Beall, Robert M.","contributorId":90695,"corporation":false,"usgs":true,"family":"Beall","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":142998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24071,"text":"ofr78684 - 1978 - Hydrologic environment of the Silurian salt deposits in parts of Michigan, Ohio, and New York","interactions":[],"lastModifiedDate":"2016-11-07T10:05:18","indexId":"ofr78684","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-684","title":"Hydrologic environment of the Silurian salt deposits in parts of Michigan, Ohio, and New York","docAbstract":"The aggregate thickness of evaporites (salt, gypsum, and anhydrite) in the Silurian Salina sequence in Michigan exceeds 1200 feet in areas near the periphery of the Michigan basin, where the salt beds are less than 3000 feet below land surface. In northeast Ohio the aggregate thickness of salt beds is as much as 200 feet in places, and in western New York it is more than 500 feet, where th beds are less than 3000 feet deep.
The salt-bearing rocks dip regionally on the order of 50 feet per mile; those in Michigan dip toward the center of the Michigan basin, and those in Ohio and New York, in the Appalachian basin, dip generally southward. The rocks in both basins thicken downdip. Minor folds and faults occur in the salt-bearing rocks in all three states. Some of this defrmation has been attenuated or absorbed bo the salt beds.
Occuring near the middle of thick sedimentary sequences, the salt beds are bounded aboe and below by beds containing water having dissolved-solids concentrations several times that seawter. The brines occur commonly in discrete zones of high permeability at specific places in the stratigraphic sequence.
In northeast Ohio two prominent brine zones are recognized by the driller, the Devonian Oriskany Sandstone, or 'first water' zone, above the Salina Formation, and the Newburg or 'second water' zone below the Salina. In each aquifer there is a vertical component of hydraulic head, but little brine probably moves through the salt beds because their permeability is extremely low. Also, ther is little evidence of dissolution of the salt in areas distant from the outcrop, suggesting that if brine does move through the salt, movement is at a slow enough rate so that, in combination with the saturated or near-saturated condition of the water, it precludes significant dissolution. Principal brine movement is probably in the permeable zones in the direction of the hydraulic gradient.
Two areas in Michigan and one area each in Ohio and New York appear suitable for additional investigation of salt beds for purposes radioactive waste disposal. One of the Michigan areas is in the northern part of the southern peninsula, in Presque Isle and Alpena Counties; the other is in the southern part of the southern peninsula, in Oakland, Macomb, and St. Clair Counties (fig. 3). In northeast Ohio the area that appears to be suitable for investigation includes most of the eastern half of Lake County and extends eastward into Ashtabula County and southward into Geauga County. In western New York conditions may warrant additional investigation in Schuyler, Tompkins, and western Cortland Counties.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Columbus, OH","doi":"10.3133/ofr78684","issn":"0094-9140","usgsCitation":"Norris, S., 1978, Hydrologic environment of the Silurian salt deposits in parts of Michigan, Ohio, and New York: U.S. Geological Survey Open-File Report 78-684, iii, 31 p., https://doi.org/10.3133/ofr78684.","productDescription":"iii, 31 p.","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":157248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":330791,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0684/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606df8","contributors":{"authors":[{"text":"Norris, Stanley E.","contributorId":63844,"corporation":false,"usgs":true,"family":"Norris","given":"Stanley E.","affiliations":[],"preferred":false,"id":191271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8223,"text":"ofr78678 - 1978 - Description of data-collection system and synopsis of selected hydrologic data for Soldier Creek Basin, Kansas","interactions":[],"lastModifiedDate":"2017-09-29T15:47:57","indexId":"ofr78678","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-678","title":"Description of data-collection system and synopsis of selected hydrologic data for Soldier Creek Basin, Kansas","docAbstract":"Soldier Creek basin is a long, narrow basin encompassing an area of about 290 square miles almost directly north of Topeka, Kansas. A wide range of hydrologic data has been collected in the basin since the spring of 1964. These data include rainfall, stream discharge, sediment concentrations, chemical quality of water, and ground-water altitudes.
The data collection system consists of 7 recording streamflow stations, 5 recording rainfall stations, 51 non-recording rainfall stations, and 31 groundwater observation wells. Sediment and chemical quality of water samples were collected intermittently at selected sites.
A synopsis of the time and space distribution of rainfall and peak flow are provided in graphic and tabular form for selected events of rainfall and peak flow. Representative data concerning the chemical quality of water and the fluvial sediment also are included. Selected ground-water and seepage-investigation data are depicted graphically.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78678","usgsCitation":"Carswell, W., 1978, Description of data-collection system and synopsis of selected hydrologic data for Soldier Creek Basin, Kansas: U.S. Geological Survey Open-File Report 78-678, 80 p., https://doi.org/10.3133/ofr78678.","productDescription":"80 p.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":141331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0678/report-thumb.jpg"},{"id":346263,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0678/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas","otherGeospatial":"Soldier Creek Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -96.03149414062499,\n 39.09276546806873\n ],\n [\n -95.64559936523438,\n 39.09276546806873\n ],\n [\n -95.64559936523438,\n 39.659627802935226\n ],\n [\n -96.03149414062499,\n 39.659627802935226\n ],\n [\n -96.03149414062499,\n 39.09276546806873\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dcd9","contributors":{"authors":[{"text":"Carswell, William J. Jr. carswell@usgs.gov","contributorId":1787,"corporation":false,"usgs":true,"family":"Carswell","given":"William J.","suffix":"Jr.","email":"carswell@usgs.gov","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":false,"id":157369,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20940,"text":"ofr77770 - 1978 - Hydrologic data for urban studies in the Fort Worth, Texas, metropolitan area, 1976","interactions":[],"lastModifiedDate":"2017-06-14T12:57:38","indexId":"ofr77770","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"77-770","title":"Hydrologic data for urban studies in the Fort Worth, Texas, metropolitan area, 1976","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77770","usgsCitation":"Slade, R., and Taylor, J., 1978, Hydrologic data for urban studies in the Fort Worth, Texas, metropolitan area, 1976: U.S. Geological Survey Open-File Report 77-770, 84 p., https://doi.org/10.3133/ofr77770.","productDescription":"84 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":153958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607c83","contributors":{"authors":[{"text":"Slade, R.M.","contributorId":84364,"corporation":false,"usgs":true,"family":"Slade","given":"R.M.","affiliations":[],"preferred":false,"id":183546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, J.M.","contributorId":42587,"corporation":false,"usgs":true,"family":"Taylor","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":183545,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8438,"text":"ofr78556A - 1978 - Drainage areas of surface water bodies of the Royal and Presumpscot River basins in southwestern Maine","interactions":[{"subject":{"id":8438,"text":"ofr78556A - 1978 - Drainage areas of surface water bodies of the Royal and Presumpscot River basins in southwestern Maine","indexId":"ofr78556A","publicationYear":"1978","noYear":false,"chapter":"A","title":"Drainage areas of surface water bodies of the Royal and Presumpscot River basins in southwestern Maine"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":1}],"isPartOf":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"lastModifiedDate":"2026-03-06T17:23:33.427187","indexId":"ofr78556A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-556","chapter":"A","title":"Drainage areas of surface water bodies of the Royal and Presumpscot River basins in southwestern Maine","docAbstract":"The report contains drainage area values for: lakes and ponds included in the Maine Informational Display Analysis System (MIDAS) File 906-Z, streams that drain an area greater than 25 mi2, dams, and hydrologic data collection sites. Supplemental information in the report includes State and Federal location systems used to identify these lake and stream sites.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78556A","collaboration":"Prepared in cooperation with the Maine Department of Environmental Protection","usgsCitation":"Cowing, D.J., and McNelly, J., 1978, Drainage areas of surface water bodies of the Royal and Presumpscot River basins in southwestern Maine: U.S. Geological Survey Open-File Report 78-556, v, 23 p., https://doi.org/10.3133/ofr78556A.","productDescription":"v, 23 p.","costCenters":[],"links":[{"id":141367,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0556-a/report-thumb.jpg"},{"id":430535,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0556-a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maine","otherGeospatial":"southwestern Maine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -70.98686617476311,\n 44.26923875927497\n ],\n [\n -70.98686617476311,\n 43.63191537639693\n ],\n [\n -70.21252591028798,\n 43.63191537639693\n ],\n [\n -70.21252591028798,\n 44.26923875927497\n ],\n [\n -70.98686617476311,\n 44.26923875927497\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635f18","contributors":{"authors":[{"text":"Cowing, Derrill J.","contributorId":97473,"corporation":false,"usgs":true,"family":"Cowing","given":"Derrill","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157715,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNelly, J.L.","contributorId":45309,"corporation":false,"usgs":true,"family":"McNelly","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":157714,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8439,"text":"ofr78556B - 1978 - Drainage areas of surface water bodies of the Saco River basin in southwestern Maine","interactions":[{"subject":{"id":8439,"text":"ofr78556B - 1978 - Drainage areas of surface water bodies of the Saco River basin in southwestern Maine","indexId":"ofr78556B","publicationYear":"1978","noYear":false,"chapter":"B","title":"Drainage areas of surface water bodies of the Saco River basin in southwestern Maine"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":1}],"isPartOf":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"lastModifiedDate":"2026-03-06T17:26:44.40402","indexId":"ofr78556B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-556","chapter":"B","title":"Drainage areas of surface water bodies of the Saco River basin in southwestern Maine","docAbstract":"The report contains drainage area value for: lakes and ponds included in the Maine Informational Display Analysis System (MIDAS) File 906-Z, streams that drain an area greater than 25 mil2, dams, and hydrologic data collection sites. Supplemental information in the report includes State and Federal location systems used to identify these lake and stream sites.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78556B","collaboration":"Prepared in cooperation with the Maine Department of Environmental Protection","usgsCitation":"Cowing, D.J., and Caracappa, D., 1978, Drainage areas of surface water bodies of the Saco River basin in southwestern Maine: U.S. Geological Survey Open-File Report 78-556, iv, 25 p., https://doi.org/10.3133/ofr78556B.","productDescription":"iv, 25 p.","costCenters":[],"links":[{"id":141368,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0556-b/report-thumb.jpg"},{"id":430533,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0556-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maine","otherGeospatial":"southwestern Maine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -70.9760879329313,\n 43.99929831171963\n ],\n [\n -70.9760879329313,\n 43.45939825578682\n ],\n [\n -70.41732450248179,\n 43.45939825578682\n ],\n [\n -70.41732450248179,\n 43.99929831171963\n ],\n [\n -70.9760879329313,\n 43.99929831171963\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635f2f","contributors":{"authors":[{"text":"Cowing, Derrill J.","contributorId":97473,"corporation":false,"usgs":true,"family":"Cowing","given":"Derrill","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caracappa, Douglas","contributorId":7272,"corporation":false,"usgs":true,"family":"Caracappa","given":"Douglas","email":"","affiliations":[],"preferred":false,"id":157716,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9132,"text":"ofr7823 - 1978 - Selected hydrologic data, Yampa River basin and parts of the White River basin, northwestern Colorado and south-central Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr7823","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-23","title":"Selected hydrologic data, Yampa River basin and parts of the White River basin, northwestern Colorado and south-central Wyoming","docAbstract":"Selected hydrologic data are presented from four energy-related projects conducted by the U.S. Geological Survey in the Yampa River basin and parts of the White River basin in northwestern Colorado and south-central Wyoming. Water-quality data during 1974 and 1975 and parts of 1976 for 129 ground-water sites and 119 surface-water sites are tabulated. For most samples, major cations, anions, and trace metals were analyzed. For the same time period, field measurements of specific conductance, temperature, and pH were made on 252 springs and wells. These samplings sites, as well as the locations of 20 climatological stations, 18 snow-course sites, and 43 surface-water gaging stations, are shown on maps. Geologic units that contain coal deposits or supply much of the water used for stock and domestic purposes in the area also are shown on a map. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7823","usgsCitation":"Giles, T., and Brogden, R.E., 1978, Selected hydrologic data, Yampa River basin and parts of the White River basin, northwestern Colorado and south-central Wyoming: U.S. Geological Survey Open-File Report 78-23, iii, 91 p. :ill., 2 fold. maps ;31 cm.; (106 p., 2 sheets - PGS), https://doi.org/10.3133/ofr7823.","productDescription":"iii, 91 p. :ill., 2 fold. maps ;31 cm.; (106 p., 2 sheets - PGS)","costCenters":[],"links":[{"id":142040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0023/report-thumb.jpg"},{"id":36761,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0023/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36762,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0023/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36763,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0023/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f83b6","contributors":{"authors":[{"text":"Giles, T.F.","contributorId":83096,"corporation":false,"usgs":true,"family":"Giles","given":"T.F.","email":"","affiliations":[],"preferred":false,"id":159157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brogden, Robert E.","contributorId":56202,"corporation":false,"usgs":true,"family":"Brogden","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3263,"text":"cir769 - 1978 - A theoretical basis for exploration for native copper in northern Wisconsin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir769","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"769","title":"A theoretical basis for exploration for native copper in northern Wisconsin","docAbstract":"Exploration for native copper in the Keweenawan lavas of northern Wisconsin has been concentrated in areas of relatively shallow overburden that have sparse to numerous outcrops. Lack of success of this exploration suggests that if large deposits, comparable to those of northern Michigan, are present, they are more likely to be found in one or more of the large tracts that have few, if any, exposures, away from the ' copper ranges. ' A hydrologic model that may explain the mineralization of the classic native-copper district of Michigan could be helpful in suggesting that certain covered tracts are more favorable than others, and in narrowing the targets for physical exploration within these tracts. This model involves updip migration of a hydrothermal fluid of metamorphic origin, formed when ground water contained in the interstices of lava flows and conglomerate beds was carried to great depth along the axis of the Lake Superior syncline. The largest reservoirs of such buried ground water would be expected in the peripheral rather than central parts of the basins in which the lavas originally accumulated because the ratio of porous fragmental flow tops and conglomerate beds to massive basalt should increase towards the margins of a basin. Thus, the areas most promising for copper deposits should be those updip from places where the trough of the later formed Lake Superior syncline crosses the marginal parts of a lava basin. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir769","usgsCitation":"White, W., 1978, A theoretical basis for exploration for native copper in northern Wisconsin: U.S. Geological Survey Circular 769, iii, 19 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir769.","productDescription":"iii, 19 p. :ill., maps ;26 cm.","numberOfPages":"21","costCenters":[],"links":[{"id":123904,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1978/0769/report-thumb.jpg"},{"id":30257,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0769/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a56dc","contributors":{"authors":[{"text":"White, Walter S.","contributorId":34492,"corporation":false,"usgs":true,"family":"White","given":"Walter S.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":146538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9098,"text":"ofr78137 - 1978 - Water resources along the TAPS route, Alaska, 1970-74","interactions":[],"lastModifiedDate":"2021-01-11T18:32:16.46244","indexId":"ofr78137","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-137","title":"Water resources along the TAPS route, Alaska, 1970-74","docAbstract":"The U.S. Geological Survey installed 10 streamgaging and water-quality stations along the trans-Alaska pipeline route (TAPS) starting in 1970. These stations, mostly north of Fairbanks, add to the historical network of gaging stations and provide records of hydrologic conditions along the TAPS route. Selected data from 23 gaging stations along the TAPS route for the period 1970-74 (prior to construction of the pipeline) are compiled in graphic form. The data include annual hydrographs of daily mean or instantaneous values of a standard set of parameters which are indicative of physical, chemical and biological conditions of the streams. The hydrographs facilitate comparisons of data, both in time and between stream sites. Thus, they are a tool for evaluating streamflow characteristics along the TAPS route during the preconstruction period. (Woodard-USGS)
","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr78137","usgsCitation":"Childers, J.M., Nauman, J.W., Kernodle, D., and Doyle, P., 1978, Water resources along the TAPS route, Alaska, 1970-74: U.S. Geological Survey Open-File Report 78-137, vi, 269 p., https://doi.org/10.3133/ofr78137.","productDescription":"vi, 269 p.","costCenters":[],"links":[{"id":36718,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0137/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0137/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -146.95312499999997,\n 61.12201916813026\n ],\n [\n -142.646484375,\n 61.12201916813026\n ],\n [\n -142.646484375,\n 70.1403642720717\n ],\n [\n -146.95312499999997,\n 70.1403642720717\n ],\n [\n -146.95312499999997,\n 61.12201916813026\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d6e4b07f02db5491a8","contributors":{"authors":[{"text":"Childers, Joseph M.","contributorId":14379,"corporation":false,"usgs":true,"family":"Childers","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":159088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nauman, J. W.","contributorId":30630,"corporation":false,"usgs":true,"family":"Nauman","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":159090,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kernodle, D.R.","contributorId":26691,"corporation":false,"usgs":true,"family":"Kernodle","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":159089,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Doyle, P.F.","contributorId":107286,"corporation":false,"usgs":true,"family":"Doyle","given":"P.F.","email":"","affiliations":[],"preferred":false,"id":159091,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":20762,"text":"ofr78176 - 1978 - Recent and projected changes in Dead Sea level and effects on mineral production from the sea","interactions":[],"lastModifiedDate":"2022-09-23T20:25:47.485204","indexId":"ofr78176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-176","title":"Recent and projected changes in Dead Sea level and effects on mineral production from the sea","docAbstract":"Hydrologic data for the Dead Sea area were reviewed to assess the probable magnitude and rate of change of the water level of the Dead Sea. Historical average annual Dead Sea levels range from a minimum of 399.4 meters below sea level in about 1818 to a maximum of 388.6 meters below in 1896. Present levels are rapidly approaching the historical low. There is a close correlation between Dead Sea level and accumulated departure from the mean of long-term rainfall except for the most recent period since 1964. During that period rainfall has been near the long-term average but water levels have continued to decline, in part due to abstractions for irrigation in the Jordan River basin.
The dissolved-solids concentration of Dead Sea water presently is approximately 322,000 milligrams per liter and is generally well mixed throughout. This concentration is at the saturation level, resulting in continuous precipitation of some salts. The increase in dissolved solids to the present high concentration has resulted in an evaporation rate less than that estimated in previous reports. Evaporation rate from the North Basin is estimated at 1,310 millimeters per year at present. The evaporation rate from the South Basin was not estimated due to extensive existing or planned modifications for mineral production facilities.
Water budget computations were performed at various inflow rates in order to project water-level changes for 50 years. Computations assumed closure of the South Basin by existing and proposed mineral extraction facilities. The projected 50-year changes ranged from a decline of 51 meters with no inflow from any sources to a rise of 10.2 meters when average annual inflow from the Jordan River was 750 cubic hectometers. An average annual inflow to the Sea of 900 cubic hectometers from all sources is required to stabilize the Sea at the present level. Principal impact of declining water levels on proposed potash production facilities in Jordan would be an increase in power requirements.
A cursory review of a proposed plan to divert water from the Mediterranean Sea into the Dead Sea to generate electric power and stabilize water levels indicates a very limited impact on chemical, physical, and ecological characteristics of the Dead Sea in the near future. Water-budget computations indicate that if all but 200 cubic hectometers of tributaries' waters were utilized for irrigation and other purposes, a maximum diversion of 700 cubic hectometers per year into the Dead Sea would be possible without significantly raising long-term average water levels.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78176","collaboration":"Prepared in cooperation with the U.S. Agency for International Development","usgsCitation":"Sauer, S.P., 1978, Recent and projected changes in Dead Sea level and effects on mineral production from the sea: U.S. Geological Survey Open-File Report 78-176, iv, 43 p., https://doi.org/10.3133/ofr78176.","productDescription":"iv, 43 p.","costCenters":[],"links":[{"id":407296,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0176/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0176/report-thumb.jpg"}],"country":"Israel, Jordan, West Bank","otherGeospatial":"Dead Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 35.36773681640625,\n 30.954057859276126\n ],\n [\n 35.6011962890625,\n 30.954057859276126\n ],\n [\n 35.6011962890625,\n 31.826231907142883\n ],\n [\n 35.36773681640625,\n 31.826231907142883\n ],\n [\n 35.36773681640625,\n 30.954057859276126\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485a7","contributors":{"authors":[{"text":"Sauer, Stanley P.","contributorId":38966,"corporation":false,"usgs":true,"family":"Sauer","given":"Stanley","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":183201,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6431,"text":"pp1044A - 1978 - The hydrothermal system of Long Valley Caldera, California","interactions":[{"subject":{"id":11262,"text":"ofr77347 - 1977 - The hydrothermal system of Long Valley Caldera, California","indexId":"ofr77347","publicationYear":"1977","noYear":false,"title":"The hydrothermal system of Long Valley Caldera, California"},"predicate":"SUPERSEDED_BY","object":{"id":6431,"text":"pp1044A - 1978 - The hydrothermal system of Long Valley Caldera, California","indexId":"pp1044A","publicationYear":"1978","noYear":false,"chapter":"A","title":"The hydrothermal system of Long Valley Caldera, California"},"id":1}],"lastModifiedDate":"2025-04-17T16:29:27.483672","indexId":"pp1044A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1044","chapter":"A","title":"The hydrothermal system of Long Valley Caldera, California","docAbstract":"Long Valley caldera, an elliptical depression covering 450 km 2 on the eastern front of the Sierra Nevada in east-central California, contains a hot-water convection system with numerous hot springs and measured and estimated aquifer temperatures at depths of 180?C to 280?C. In this study we have synthesized the results of previous geologic, geophysical, geochemical, and hydrologic investigations of the Long Valley area to develop a generalized conceptual and mathematical model which describes the gross features of heat and fluid flow in the hydrothermal system. \r\n\r\nCenozoic volcanism in the Long Valley region began about 3.2 m.y. (million years) ago and has continued intermittently until the present time. The major event that resulted in the formation of the Long Valley caldera took place about 0.7 m.y. ago with the eruption of 600 km 3 or more of Bishop Tuff of Pleistocene age, a rhyolitic ash flow, and subsequent collapse of the roof of the magma chamber along one or more steeply inclined ring fractures. Subsequent intracaldera volcanism and uplift of the west-central part of the caldera floor formed a subcircular resurgent dome about 10 km in diameter surrounded by a moat containing rhyolitic, rhyodacitic, and basaltic rocks ranging in age from 0.5 to 0.05 m.y. \r\n\r\nOn the basis of gravity and seismic studies, we estimate an aver- age thickness of fill of 2.4 km above the precaldera granitic and metamorphic basement rocks. A continuous layer of densely welded Bishop Tuff overlies the basement rocks, with an average thickness of 1.4 km; the fill above the welded Bishop Tuff consists of intercalated volcanic flows and tuffs and fluvial and lacustrine deposits. Assuming the average grain density of the fill is between 2.45 and 2.65 g/cm 3 , we calculate the average bulk porosity of the total fill as from 0.11 to 0.21. Comparison of published values of porosity of the welded Bishop Tuff exposed southeast of the caldera with calculated values indicates average bulk porosity for the welded tuff (including fracture porosity) from 0.05 to 0.10. Because of its continuity and depth and the likelihood of significant fracture permeability in the more competent rocks such as the welded tuff, our model of the hydrothermal system assumes that the Bishop Tuff provides the principal hot-water reservoir. However, because very little direct information exists from drill holes below 300 m, this assumption must be considered tentative. \r\n\r\nLong Valley caldera is drained by the Owens River and several tributaries which flow into Lake Crowley in the southeast end of the caldera. Streamflow and springflow measurements for water years 1964-74 indicate a total inflow to Lake Crowley of about 10,900 L/s. In contrast, the total discharge of hot water from the hydrothermal reservoir is about 300 L/s. For modeling purposes, the ground-water system is considered as comprising a shallow subsystem in the fill above the densely welded Bishop Tuff containing relatively cold ground water, and a deep subsystem or hydrothermal reservoir in the welded tuff containing relatively hot ground water. Hydrologic, isotopic, and thermal data indicate that recharge to the hydrothermal reservoir occurs in the upper Owens River drainage basin along the western periphery of the caldera. Temperature profiles in a 2.11- km-deep test well drilled by private industry in the southeastern part of the caldera suggest that an additional flux of relatively cool ground water recharges the deep subsystem around the northeast rim. Flow in the shallow ground-water subsystem is neglected in the model except in recharge areas and along Hot Creek gorge, where approximately 80 percent of the hot-water discharge from the hydrothermal reservoir moves upward along faults toward springs in the gorge. \r\n\r\nHeat-flow data from the Long Valley region indicate that the resurgent dome overlies a residual magma chamber more circular in plan than the original magma chamber that supplied the Bishop Tuff","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1044A","usgsCitation":"Sorey, M., Lewis, R.E., and Olmsted, F.H., 1978, The hydrothermal system of Long Valley Caldera, California: U.S. Geological Survey Professional Paper 1044, Report: 60 p.; 1 Plate: 34.00 x 25.00 inches, https://doi.org/10.3133/pp1044A.","productDescription":"Report: 60 p.; 1 Plate: 34.00 x 25.00 inches","costCenters":[],"links":[{"id":33842,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1044a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104540,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4695.htm","linkFileType":{"id":5,"text":"html"},"description":"4695"},{"id":33841,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117933,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1044a/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Long Valley Caldera","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.0969,\n 37.7778\n ],\n [\n -119.0969,\n 37.5\n ],\n [\n -118.635,\n 37.5\n ],\n [\n -118.635,\n 37.7778\n ],\n [\n -119.0969,\n 37.7778\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a86e4b07f02db64da25","contributors":{"authors":[{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":152712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, Robert Edward","contributorId":73595,"corporation":false,"usgs":true,"family":"Lewis","given":"Robert","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":152713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Olmsted, F. H.","contributorId":24765,"corporation":false,"usgs":true,"family":"Olmsted","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":152711,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":6512,"text":"pp993 - 1978 - Historic ground failures in Northern California triggered by earthquakes","interactions":[],"lastModifiedDate":"2021-02-26T16:11:31.116168","indexId":"pp993","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"993","title":"Historic ground failures in Northern California triggered by earthquakes","docAbstract":"A major source of earthquake-related damage and casualties in northern California has been ground failures generated by the seismic shaking, including landslides, lateral spreads, ground settlement, and surface cracks. The historical record shows that, except for offshore shocks, the geographic area affected and the quantity and general severity of ground failures increase markedly with Richter magnitude. Hence, the largest historical event, the 1906 San Francisco earthquake, has been the most important generator of ground failures. Because of recent population growth and land development in northern California, the potential for damage in future events is enormous compared with that existing in 1906.\r\n\r\nReports of the 1906 San Francisco earthquake and other northern California earthquakes and descriptions of ground failures therein are used to (1) identify and clarify the types of ground failures associated with earthquakes, (2) provide a guide for engineers, planners, and others responsible for minimizing seismic hazards, and (3) form a data base for other geotechnical studies of earthquake-triggered pound failures.\r\n\r\nGeologic, hydrologic, and topographic setting have an important influence on ground failure development as well as distance from the causative fault. Areas especially vulnerable to ground failure in northern California have been oversteepened slopes, such as mountain cliffs, streambanks, and coastal bluffs, and lowland deposits, principally Holocene fluvial deposits, deltaic deposits, and poorly compacted fills. Liquefaction has been the direct cause of most lowland failures. The historical record suggests that ground failures during future large earthquakes are most likely to occur at the same or geologically similar locations as failures during previous earhquakes.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp993","usgsCitation":"Youd, T.L., and Hoose, S.N., 1978, Historic ground failures in Northern California triggered by earthquakes: U.S. Geological Survey Professional Paper 993, Report: iv, 177 p.; 5 Plates: 34.00 x 21.00 inches and smaller; 2 Photographs folders, https://doi.org/10.3133/pp993.","productDescription":"Report: iv, 177 p.; 5 Plates: 34.00 x 21.00 inches and smaller; 2 Photographs folders","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":650,"text":"Western Earthquake Hazards Team","active":false,"usgs":true}],"links":[{"id":123718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_993.jpg"},{"id":9879,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/","linkFileType":{"id":5,"text":"html"}},{"id":383646,"rank":10,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/photographs/web-resolution","text":"Web-resolution Photographs folder","linkFileType":{"id":5,"text":"html"}},{"id":383645,"rank":9,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/photographs/print-resolution","text":"Print-resolution Photographs folder","linkFileType":{"id":5,"text":"html"}},{"id":383644,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_plate5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383639,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383640,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383641,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_plate3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383642,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_plate2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383643,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_plate4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,35 ], [ -124,41 ], [ -119,41 ], [ -119,35 ], [ -124,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68864d","contributors":{"authors":[{"text":"Youd, T. Leslie","contributorId":107678,"corporation":false,"usgs":true,"family":"Youd","given":"T.","email":"","middleInitial":"Leslie","affiliations":[],"preferred":false,"id":152848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoose, Seena N.","contributorId":95870,"corporation":false,"usgs":true,"family":"Hoose","given":"Seena","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":152847,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30195,"text":"wri7796 - 1978 - Preliminary hydrologic budget of the sand-and-gravel aquifer under unstressed conditions: with a section on water-quality monitoring, Pensacola, Florida","interactions":[],"lastModifiedDate":"2019-07-23T11:24:56","indexId":"wri7796","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"77-96","title":"Preliminary hydrologic budget of the sand-and-gravel aquifer under unstressed conditions: with a section on water-quality monitoring, Pensacola, Florida","docAbstract":"The sand-and-gravel aquifer is the only freshwater aquifer in southern Escambia County, Fla. Problems related to the development of the aquifer include sustained yield, contamination, and saltwater intrusion. A digital model was applied to the sand-and-gravel aquifer in central and southern Escambia County treating the aquifer 's 'main producing zone ' as a discrete, leaky, confined aquifer. Under conditions of no pumping, most values for the final-head matrix agreed with assumed values within 4 feet in the area of principal interest. Discharge per unit land area was 1.04 cubic feet per second per square mile, in close agreement with the base runoff streams maintained by the aquifer. Total natural aquifer discharge within the area of principal interest determined by the model was 159 million gallons per day. The applicability of the present non-unique calibration for predicting the effects of pumping is questionable; a multilayered model may be required. Effluent infiltrating from holding lagoons for spray irrigation at the Scenic Hills Sewage Plant may have affected the quality of local perched ground water in the sand-and-gravel aquifer. Observation wells drilled near areas of heavy pumping around Bayou Chico indicated no saltwater intrusion. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7796","usgsCitation":"Trapp, H., 1978, Preliminary hydrologic budget of the sand-and-gravel aquifer under unstressed conditions: with a section on water-quality monitoring, Pensacola, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-96, iv, 57 p. , https://doi.org/10.3133/wri7796.","productDescription":"iv, 57 p. ","costCenters":[],"links":[{"id":365848,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0096/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0096/report-thumb.jpg"}],"country":"United States","state":"Florida","city":"Pensacola","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.4072265625,\n 30.306503259848835\n ],\n [\n -87.08862304687499,\n 30.306503259848835\n ],\n [\n -87.08862304687499,\n 30.56226095049944\n ],\n [\n -87.4072265625,\n 30.56226095049944\n ],\n [\n -87.4072265625,\n 30.306503259848835\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673397","contributors":{"authors":[{"text":"Trapp, Henry Jr.","contributorId":6034,"corporation":false,"usgs":true,"family":"Trapp","given":"Henry","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":202842,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}