Tooele Valley is a typical basin of the Basin and Range Province located about 30 miles southwest of Salt Lake City. It is roughly 15 miles long and 10 miles wide and has a population of about 7,000. Bordered on the west by the Stansbury Range, on the east by the Oquirrh Range, and on the south by South Mountain, it opens northward to Great Salt Lake. The bordering mountain ranges are formed by Paleozoic rocks ranging in age from Lower Cambrian to Pennsylvanian but with the Ordovician and Silurian periods unrepresented. There is no sedimentary record of the interval between Pennsylvanian and Tertiary times, and the Tertiary, Quaternary, and Recent sediments are of continental origin. These continental deposits play the dominant role in the ground-water hydrology of the basin, and were mapped and studied in detail. Pleistocene sediments are of major importance because they form the surface rock over most of the area, and give rise to conditions which yield water by artesian flow in the lower part of the valley.
The development of the present land forms in this area began with the folding of Paleozoic and probably Mesozoic sediments during the Laramide revolution. The cycle of highland erosion and lowland deposition thus initiated has continued through recurrent uplift along Basin-Range faults to the present day. The principal physiographic subdivisions of the valley were developed as a result of the Basin-Range faulting, which began early in the Tertiary and has continued to Recent times.
There are about 1,100 wells in Tooele Valley, about 90 per cent of which yield or have yielded water by artesian flow. Most of them are located in the lower part of the valley below an altitude of 4,400 feet. These wells and many of the springs derive their water from the unconsolidated Quaternary sediments, which include discontinuous, lenticular and commonly elongated bodies of sand, clay, gravel, and boulders of alluvial origin alternating and inter-fingered with lacustrine beds of the same materials which are more regularly stratified and better assorted. The larger springs are intimately related to the bedding planes and faults in the bedrock and alluvial formations. The well assorted sands and gravels deposited along the shore lines of Lake Bonneville are important as recharge areas for the artesian reservoir.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Twenty-fifth biennial report of the State Engineer to the Governor of Utah: 1944-1946","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City","usgsCitation":"Thomas, H.E., 1946, Ground water in Tooele Valley, Tooele County, Utah: Technical Publication 4, 148 p.","productDescription":"148 p.","startPage":"91","endPage":"238","numberOfPages":"148","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331485,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333875,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-369","text":"Utah State Engineer's 25th Biennial Report (larger work)"},{"id":331484,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w9200083.pdf"},{"id":331483,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-100"}],"country":"United States","state":"Utah","county":"Tooele County","otherGeospatial":"Tooele Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.796630859375,\n 40.37584377696013\n ],\n [\n -112.796630859375,\n 40.94048973170136\n ],\n [\n -112.23907470703124,\n 40.94048973170136\n ],\n [\n -112.23907470703124,\n 40.37584377696013\n ],\n [\n -112.796630859375,\n 40.37584377696013\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58468aefe4b04fc80e5236df","contributors":{"authors":[{"text":"Thomas, H. 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It lies in San Diego County, about 3 miles south of Julian, and approximately 60 miles northeast of San Diego. The area was mapped, and its nickel mineralization studied, from March to June, 1944; the work was part of the U. S. Geological Survey's program of strategic mineral investigations.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"California Journal of Mines and Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"California Division of Mines","usgsCitation":"Creasey, S., 1946, Geology and nickel mineralization of the Julian-Cuyamaca area, San Diego County, California: California Journal of Mines and Geology, v. 42, no. 1, p. 15-29.","productDescription":"15 p.","startPage":"15","endPage":"29","costCenters":[],"links":[{"id":277115,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":277114,"type":{"id":15,"text":"Index Page"},"url":"https://archive.org/details/californiajourna42cali"}],"country":"United States","state":"California","county":"San Diego County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.5962,32.5342 ], [ -117.5962,33.5054 ], [ -116.081,33.5054 ], [ -116.081,32.5342 ], [ -117.5962,32.5342 ] ] ] } } ] }","volume":"42","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521f1be7e4b0f8bf2b076121","contributors":{"authors":[{"text":"Creasey, S.C.","contributorId":36109,"corporation":false,"usgs":true,"family":"Creasey","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":483200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047717,"text":"70047717 - 1946 - Mica deposits of the Petaca district, Rio Arriba County, New Mexico","interactions":[{"subject":{"id":55355,"text":"ofr4470 - 1944 - Mica deposits of the Petaca district, Rio Arriba County, New Mexico","indexId":"ofr4470","publicationYear":"1944","noYear":false,"title":"Mica deposits of the Petaca district, Rio Arriba County, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":70047717,"text":"70047717 - 1946 - Mica deposits of the Petaca district, Rio Arriba County, New Mexico","indexId":"70047717","publicationYear":"1946","noYear":false,"title":"Mica deposits of the Petaca district, Rio Arriba County, New Mexico"},"id":1}],"lastModifiedDate":"2013-08-20T12:44:38","indexId":"70047717","displayToPublicDate":"2013-01-01T12:39:00","publicationYear":"1946","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"25","title":"Mica deposits of the Petaca district, Rio Arriba County, New Mexico","docAbstract":"Wartime increases in demand for mica of strategic quality, beryllium, tantalum, columbium, tin, lithium, and uranium have focused attention on pegmatite deposits more sharply during recent years than ever before. Not only have numerous technical developments of the past few decades involved new uses for these commodities, but during the recent period of emergency these and other uses were greatly expanded. The attendant rapid increases in demand and a heavy dependence on foreign sources of supply soon confirmed the need for a careful appraisal of domestic resources of the minor pegmatite minerals. 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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70046721","usgsCitation":"Dobbin, C.E., and Miller, J., 1946, Geologic and structure contour map of Garland and Byron anticlines, Big Horn and Park Counties, Wyoming: General Mineral Resources Map, Map: 1 Sheet, https://doi.org/10.3133/70046721.","productDescription":"Map: 1 Sheet","costCenters":[],"links":[{"id":274305,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Big Horn County, Park County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0569,43.8012 ], [ -111.0569,45.0059 ], [ -107.1436,45.0059 ], [ -107.1436,43.8012 ], [ -111.0569,43.8012 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51ceb060e4b044272b8e8921","contributors":{"authors":[{"text":"Dobbin, C. 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The main body of the manuscript and appendices A, B, and C, completed in March 1942, contain statistics through the year 1939. Since that time, records for the years 1940-1942 have become available. Because these additional data did not alter any of the conclusions of the manuscript but actually strengthened them, it was not deemed justifiable to expend the considerable amount of time and money that would be required to revise the study. The 1940-1942 records are therefore presented in appendix D. From a relatively high production in the earlier years of the period, 1879 to 1942, the yield of whitefish declined to a lower level about which the catch fluctuated until the late 1920's and early 1930's when a general increase in production occurred. This recent increase was higher and the subsequent decline more severe in the Michigan waters of Lake Huron than in other areas.","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Arlington, VA","usgsCitation":"Van Oosten, J., Hile, R., and Jobes, F.W., 1946, The whitefish fishery of Lakes Huron and Michigan with special reference to the deep-trap-net fishery: Fishery Bulletin of the U.S. Fish and Wildlife Service, v. 50, p. 297-394.","productDescription":"ii, 98 p.","startPage":"297","endPage":"394","numberOfPages":"97","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":260127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":260123,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.st.nmfs.noaa.gov/spo/FishBull/50-1/501toc.html","linkFileType":{"id":5,"text":"html"}},{"id":352108,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://www.st.nmfs.noaa.gov/spo/FishBull/50-1/vanoosten.pdf"}],"country":"United States","otherGeospatial":"Lake Huron, Lake Michigan","volume":"50","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb1dee4b08c986b32546f","contributors":{"authors":[{"text":"Van Oosten, John","contributorId":23479,"corporation":false,"usgs":true,"family":"Van Oosten","given":"John","email":"","affiliations":[],"preferred":false,"id":354744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hile, Ralph","contributorId":48510,"corporation":false,"usgs":true,"family":"Hile","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":354745,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jobes, Frank W.","contributorId":6004,"corporation":false,"usgs":true,"family":"Jobes","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":354743,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70040234,"text":"70040234 - 1946 - Record of wells in Nassau County, N.Y., Supplement 1","interactions":[],"lastModifiedDate":"2012-10-09T17:16:16","indexId":"70040234","displayToPublicDate":"2012-01-01T15:05:25","publicationYear":"1946","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-10","title":"Record of wells in Nassau County, N.Y., Supplement 1","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Roberts, C., and Brashears, M., 1946, Record of wells in Nassau County, N.Y., Supplement 1: Bulletin GW-10, 191 p.; 1 Plate.","productDescription":"191 p.; 1 Plate","numberOfPages":"191","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262496,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.7600,40.4800 ], [ -79.7600,45.0200 ], [ -71.8600,45.0200 ], [ -71.8600,40.4800 ], [ -79.7600,40.4800 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a278e4b0e8fec6cdb5fa","contributors":{"authors":[{"text":"Roberts, C.M.","contributorId":75107,"corporation":false,"usgs":true,"family":"Roberts","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":467942,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brashears, M.L. 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The listed reports embody the results of some of the work done by Survey geologists on mineral deposits in the United States, Alaska, Brazil, and Liberia. 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