This report summarizes existing knowledge on the geohydrology of the Soquel-Aptos area, near, and including the eastern part, of Santa Cruz, California, and outlines work necessary for making a complete appraisal of the water resources of the area.
The area is underlain mostly by marine and continental sedimentary deposits of Tertiary and Quaternary age. A small section in the northeastern part of the area on the eastern side of the San Andreas fault is underlain by sedimentary and metamorphic rocks of Cretaceous or older age. Quartz diorite, probably of Cretaceous age, underlies a considerable part of the area, but crops out only in small exposures along canyon bottom south of the Zayante fault.
The Soquel-Aptos area consists of two main structural blocks?one, downthrown on the northeast side of the Zayante fault; the other, upthrown on the southwest side of the fault. The main water-bearing formations in the southwestern structural block are the Santa Margarita and Purisima Formations. The Purisima, the most widespread of these units in this area, contains water under water-table and artesian conditions and furnishes water to most wells. The water-bearing character of the rocks in the northern structural block is unknown.
Presently available geohydrologic data are too limited for detailed evaluation of the ground-water potential in the Soquel-Aptos area. Work needed for a detailed evaluation includes: (1) Geophysical exploration and test drilling at selected locations, (2) pumping tests of selected existing wells and possibly of specially drilled test wells, (3) study and reconnaissance measurements of spring and streamflow, (4) chemical analysis of water samples from selected wells, and (5) establishment of a program for monitoring water quality and water levels in key wells.
","language":"English","publisher":"U.S. geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr673","collaboration":"Prepared in cooperation with the Soquel Creek County [Watershed District?], the City of Santa Cruz, and the county of Santa Cruz","usgsCitation":"Akers, J.P., and Hickey, J., 1967, Geohydrologic reconnaissance of the Soquel-Aptos area, Santa Cruz County, California: U.S. Geological Survey Open-File Report 67-3, Report: 58 p.; 1 Figure: 27.84 x 32.26 inches, https://doi.org/10.3133/ofr673.","productDescription":"Report: 58 p.; 1 Figure: 27.84 x 32.26 inches","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":77992,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0003/plate-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geologic map of the Soquel-Aptos area, California, showing location of hydrologic data stations"},{"id":77993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0003/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":110367,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_53760.htm","linkFileType":{"id":5,"text":"html"},"description":"53760"},{"id":171208,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0003/report-thumb.jpg"}],"country":"United States","state":"California","county":"Santa Cruz County","otherGeospatial":"Soquel-Aptos area","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aedf1","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":223850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hickey, J.J.","contributorId":57010,"corporation":false,"usgs":true,"family":"Hickey","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":223849,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38814,"text":"pp575A - 1967 - Geological Survey research 1967, Chapter A","interactions":[],"lastModifiedDate":"2023-10-31T19:45:13.944363","indexId":"pp575A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"575","chapter":"A","title":"Geological Survey research 1967, Chapter A","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1967 (Professional Paper 575)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp575A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Geological Survey research 1967, Chapter A: U.S. Geological Survey Professional Paper 575, viii, 377 p., https://doi.org/10.3133/pp575A.","productDescription":"viii, 377 p.","costCenters":[],"links":[{"id":65733,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0575a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120282,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0575a/report-thumb.jpg"},{"id":422301,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92908.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6877f1","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529885,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52573,"text":"ofr6771 - 1967 - Ground-water aspects of the lower Henrys Fork region, Idaho","interactions":[],"lastModifiedDate":"2013-11-19T10:29:25","indexId":"ofr6771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-71","title":"Ground-water aspects of the lower Henrys Fork region, Idaho","docAbstract":"The lower Henrys Fork region includes the plains and low benches between Ashton and the junction of Henrys Fork and Snake River in eastern Idaho. The northwestern and western parts of the area are part of the Snake River lava plain. The central part of the area is occupied by alluvial plains of the Snake, Teton, and Falls Rivers, and Henrys Fork. The southeastern part of the area is a bench (Rexburg Bench), chiefly on silicic and basaltic volcanic rocks, which rises gradually to mountain peaks southeast of the area. The basalt, and the sand and gravel under the alluvial plains are good aquifers and yield large amounts of water with small drawdowns. The silicic volcanic rocks and the interbedded ash, pyroclastics, and sedimentary deposits generally yield much less water than the basalt and alluvium. The regional water table slopes southward beneath the basalt and alluvial plains. Seepage from stream channels and irrigated tracts has resulted in an extensive body of ground water perched above the regional water table. The perched water in part moves vertically down to the regional water table and in part laterally to the streams. Ground water beneath the Rexburg Bench moves generally northwestward to join the regional ground-water body beneath the alluvial plain. The regional water table is below the level of the streams in the area and ground water in the main aquifer, therefore is not tributary to the streams. Recharge to the regional water table is estimated to average 725,000 acre-feet annually. Pumping from the regional ground-water reservoir for irrigation or other uses would have no effect on streamflow or surface-water rights within the study area. However, depletion of the underflow would eventually reduce the inflow to American Falls Reservoir unless the depletion was offset by additional recharge. Total withdrawals of ground water for irrigation in 1962 were estimated to be 25,000 acre-feet and caused no significant decline in the water table. In the Ashton area surface-water irrigation has cause water to be perched in basalt above the silicic volcanic rocks and much of this perched water contributed to streamflow. The flow of Henrys Fork would be decreased by the amount of pumped ground water consumed by crops. Ground-water prospects for irrigation in the Falls River area are not encouraging.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6771","collaboration":"Prepared in cooperation with the U.S. Bureau of Reclamation and Idaho Department of Reclamation","usgsCitation":"Crosthwaite, E., Mundorff, M., and Walker, E., 1967, Ground-water aspects of the lower Henrys Fork region, Idaho: U.S. Geological Survey Open-File Report 67-71, iii, 43 p., https://doi.org/10.3133/ofr6771.","productDescription":"iii, 43 p.","numberOfPages":"46","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":177408,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0071/report-thumb.jpg"},{"id":86960,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Henry Fork Region","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0,42.0 ], [ -117.0,49.0 ], [ -111.0,49.0 ], [ -111.0,42.0 ], [ -117.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d42a","contributors":{"authors":[{"text":"Crosthwaite, E.J.","contributorId":6525,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":245569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mundorff, M.J.","contributorId":48158,"corporation":false,"usgs":true,"family":"Mundorff","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":245570,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walker, E.H.","contributorId":104088,"corporation":false,"usgs":true,"family":"Walker","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":245571,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68350,"text":"ha176 - 1967 - Availability of ground water in parts of the Olmsted and Bandana quadrangles, in Jackson Purchase region, Kentucky","interactions":[],"lastModifiedDate":"2021-10-26T19:49:29.531192","indexId":"ha176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"176","title":"Availability of ground water in parts of the Olmsted and Bandana quadrangles, in Jackson Purchase region, Kentucky","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha176","usgsCitation":"Hansen, A., 1967, Availability of ground water in parts of the Olmsted and Bandana quadrangles, in Jackson Purchase region, Kentucky: U.S. Geological Survey Hydrologic Atlas 176, 1 Plate: 39.50 × 55.00 inches, https://doi.org/10.3133/ha176.","productDescription":"1 Plate: 39.50 × 55.00 inches","costCenters":[],"links":[{"id":188897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":390983,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15538.htm"},{"id":89826,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/176/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky","otherGeospatial":"Olmsted and Bandana quadrangles","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.1,37.125 ], [ -89.1,37.217 ], [ -88.875,37.217 ], [ -88.875,37.125 ], [ -89.1,37.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8c2","contributors":{"authors":[{"text":"Hansen, Arnold J.","contributorId":33316,"corporation":false,"usgs":true,"family":"Hansen","given":"Arnold J.","affiliations":[],"preferred":false,"id":278073,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52579,"text":"ofr6779 - 1967 - Preliminary results of the investigation of the saline-water resources in the Hueco Bolson near El Paso, Texas","interactions":[],"lastModifiedDate":"2016-08-23T16:30:26","indexId":"ofr6779","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-79","title":"Preliminary results of the investigation of the saline-water resources in the Hueco Bolson near El Paso, Texas","docAbstract":"The Hueco Bolson, as defined in this report, is in the extreme western part of Texas and includes that part of El Paso County between the Franklin and Hueco Mountains north of the Rio Grande.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6779","collaboration":"Prepared in cooperation with the Texas Water Development Board and the City of El Paso","usgsCitation":"Davis, M.E., and Leggat, E., 1967, Preliminary results of the investigation of the saline-water resources in the Hueco Bolson near El Paso, Texas: U.S. Geological Survey Open-File Report 67-79, Document: 27 p.; 4 Plates: 24.65 x 19.34 inches or smaller, https://doi.org/10.3133/ofr6779.","productDescription":"Document: 27 p.; 4 Plates: 24.65 x 19.34 inches or smaller","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":177498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0079/report-thumb.jpg"},{"id":86961,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0079/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86962,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0079/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86963,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0079/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86964,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0079/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86965,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0079/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Hueco Bolson","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673a5","contributors":{"authors":[{"text":"Davis, M. E.","contributorId":14844,"corporation":false,"usgs":true,"family":"Davis","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":245577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leggat, E. R.","contributorId":28222,"corporation":false,"usgs":true,"family":"Leggat","given":"E. R.","affiliations":[],"preferred":false,"id":245578,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":41718,"text":"ofr67258 - 1967 - Areas within which public oil shale lands are withdrawn by Executive Order 5327, (this is a current interpretation and is subject to revision with new information)","interactions":[],"lastModifiedDate":"2012-02-02T00:11:06","indexId":"ofr67258","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-258","title":"Areas within which public oil shale lands are withdrawn by Executive Order 5327, (this is a current interpretation and is subject to revision with new information)","language":"ENGLISH","doi":"10.3133/ofr67258","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Areas within which public oil shale lands are withdrawn by Executive Order 5327, (this is a current interpretation and is subject to revision with new information): U.S. Geological Survey Open-File Report 67-258, 1 map, https://doi.org/10.3133/ofr67258.","productDescription":"1 map","costCenters":[],"links":[{"id":167871,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":113803,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0258/plate-1.pdf","size":"3360","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672fe9","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530582,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":977,"text":"wsp1576H - 1967 - Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico","interactions":[{"subject":{"id":52217,"text":"ofr626 - 1962 - Geology and ground-water resources of the southern part of the Jicarilla Apache Indian Reservation and adjacent region to the south and east, New Mexico","indexId":"ofr626","publicationYear":"1962","noYear":false,"title":"Geology and ground-water resources of the southern part of the Jicarilla Apache Indian Reservation and adjacent region to the south and east, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":977,"text":"wsp1576H - 1967 - Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico","indexId":"wsp1576H","publicationYear":"1967","noYear":false,"chapter":"H","title":"Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1576H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1576","chapter":"H","title":"Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1576H","usgsCitation":"Baltz, E.H., and West, S.W., 1967, Ground-water resources of the southern part of Jicarilla Apache Indian Reservation and adjacent areas, New Mexico: U.S. Geological Survey Water Supply Paper 1576, iv, 89 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1576H.","productDescription":"iv, 89 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1576h/report-thumb.jpg"},{"id":25543,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25544,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576h/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25545,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576h/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25546,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576h/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25547,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1576h/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25548,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1576h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a47f","contributors":{"authors":[{"text":"Baltz, Elmer Harold","contributorId":22313,"corporation":false,"usgs":true,"family":"Baltz","given":"Elmer","email":"","middleInitial":"Harold","affiliations":[],"preferred":false,"id":142955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"West, Samuel Wilson","contributorId":24763,"corporation":false,"usgs":true,"family":"West","given":"Samuel","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":142956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":985,"text":"wsp1849 - 1967 - Roughness characteristics of natural channels","interactions":[],"lastModifiedDate":"2017-06-21T09:54:47","indexId":"wsp1849","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1849","title":"Roughness characteristics of natural channels","docAbstract":"Color photographs and descriptive data are presented for 50 stream channels for which roughness coefficients have been determined. \r\n\r\nAll hydraulic computations involving flow in open channels require an evaluation of the roughness characteristics of the channel. In the absence of a satisfactory quantitative procedure this evaluation remains chiefly an art. The ability to evaluate roughness coefficients must be developed through experience. One means of gaining this experience is by examining and becoming acquainted with the appearance of some typical channels whose roughness coefficients are known. \r\n\r\nThe photographs and data contained in this report represent a wide range of channel conditions. Familiarity with the appearance, geometry, and roughness characteristics of these channels will improve the engineer's ability to select roughness coefficients for other channels .","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1849","usgsCitation":"Barnes, H.H., 1967, Roughness characteristics of natural channels: U.S. Geological Survey Water Supply Paper 1849, vi, 213 p. :illus. (part col.) ;24 cm., https://doi.org/10.3133/wsp1849.","productDescription":"vi, 213 p. :illus. (part col.) ;24 cm.","costCenters":[],"links":[{"id":136116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":342703,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/wsp_1849/pdf/wsp_1849.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":8,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wsp1849/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe1e9","contributors":{"authors":[{"text":"Barnes, Harry Hawthorne","contributorId":64630,"corporation":false,"usgs":true,"family":"Barnes","given":"Harry","email":"","middleInitial":"Hawthorne","affiliations":[],"preferred":false,"id":142968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1112,"text":"wsp1836 - 1967 - Ground-water conditions and geologic reconnaissance of the Upper Sevier River basin, Utah","interactions":[],"lastModifiedDate":"2017-09-04T17:41:05","indexId":"wsp1836","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1836","title":"Ground-water conditions and geologic reconnaissance of the Upper Sevier River basin, Utah","docAbstract":"The upper Sevier River basin is in south-central Utah and includes an area of about 2,400 .square miles of high plateaus and valleys. It comprises the entire Sevier River drainage basin above Kingston, including the East Fork Sevier River and its tributaries. The basin was investigated to determine general ground-water conditions, the interrelation of ground water and surface water, the effects of increasing the pumping of ground water, and the amount of ground water in storage.
The basin includes four main valleys - Panguitch Valley, Circle Valley, East Fork Valley, and Grass Valley - which are drained by the Sevier River, the East Fork Sevier River, and Otter Creek. The plateaus surrounding the valleys consist of sedimentary and igneous rocks that range in age from Triassic to Quaternary. The valley fill, which is predominantly alluvial gravel, sand, silt, and clay, has a maximum thickness of more than 800 feet.
The four main valleys constitute separate ground-water basins. East Fork Valley basin is divided into Emery Valley, Johns Valley, and Antimony subbasins, and Grass Valley basin is divided into Koosharem and Angle subbasins. Ground water occurs under both artesian and water-table conditions in all the basins and subbasins except Johns Valley, Emery Valley, and Angle subbasins, where water is only under water-table conditions. The water is under artesian pressure in beds of gravel and sand confined by overlying beds of silt and clay in the downstream parts of Panguitch Valley basin, Circle Valley basin, and Antimony subbasin, and in most of Koosharem subbasin. Along the sides and upstream ends of these basins, water is usually under water-table conditions.
About 1 million acre-feet of ground water that is readily available to wells is stored in the gravel and sand of the upper 200 feet of saturated valley fill. About 570,000 acre-feet is stored in Panguitch Valley basin, about 210,000 in Circle Valley basin, about 6,000 in Emery Valley subbasin, about 90,000 in Johns Valley subbasin, about 36,000 in Antimony subbasin, about 90,000 in Koosharem subbasin, and about 60,000 in Angle subbasin. Additional water, although it is not readily available to wells, is stored in beds of silt and clay. Some ground water also is available in the bedrock underlying and surrounding the basins, although the bedrock formations generally are poor aquifers.
The principal source of recharge to the valley fill in the upper Sevier River basin is infiltration from streams, canals, and irrigated fields. Some ground water also miles into the valley till from the bedrock surrounding the basins.
The basin contains about 300 wells, most of which are less than 4 inches in diameter, are less than 250 feet deep, and are used for domestic purposes and stock watering. More than half the wells are flowing wells in Koosharem subbasin.
Approximately 82,000 acre-feet of ground water was discharged in 1962 from the valley till. Springs discharged about 33,000 acre-feet, wells about 3,000, and drains about 3,000; and evapotranspiration from phreatophyte areas about 43,000 acre-feet. Springs in bedrock discharged an additional 75,000 acre-feet. Most of the water discharged by springs, wells, and drains was used for irrigation.
The ground water in the basin generally is of good chemical quality. The water is excellent for irrigation and stock but is not as desirable for most domestic and industrial uses because of its hardness. The dissolved-solids content of the ground water generally increases slightly from the upstream end of the individual ground-water basins to. the downstream end owing mostly to repeated use of the water for irrigation.
Surface water and ground water in the upper Sevier River basin are inter- connected, and the base flows of streams are affected by changes in ground- water levels. Increased pumping of ground water would result in (1) an increase in the recharge to the aquifers from surface-water sources or (2) a decrease in the discharge from streams, springs, flowing wells, and areas of phreatophytes or (3) a combination of these.
About 43,000 acre-feet of ground water is now discharged annually by evapotranspiration from phreatophyte areas, and perhaps one-third of this loss, or about 14,000 acre-feet, could be salvaged by eliminating wet areas and phreatophytes. The areas where water could be salvaged are at the downstream ends of Panguitch Valley basin, Circle Valley basin, and Antimony subbasin. Most of the 14,000 acre-feet 'of water could be pumped from large-diameter wells or developed by properly designed drains without greatly affecting stream- flow and with only moderate effect on 'spring discharge. If the wells were properly located, the pumping would lower water levels and dry up wet areas where phreatophytes grow. Conjunctive use of ground water and surface water would facilitate the more efficient use of all water resources in the basin
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1836","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Carpenter, C.H., Robinson, G., and Bjorklund, L.J., 1967, Ground-water conditions and geologic reconnaissance of the Upper Sevier River basin, Utah: U.S. Geological Survey Water Supply Paper 1836, Report: vi, 91 p.; 3 Plates: 35.00 in. x 49.87 in. or smaller, https://doi.org/10.3133/wsp1836.","productDescription":"Report: vi, 91 p.; 3 Plates: 35.00 in. x 49.87 in. or smaller","numberOfPages":"98","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":138011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1836/report-thumb.jpg"},{"id":25869,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1836/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Reconnaissance geologic map and sections of the Upper Sevier River Basin, Utah"},{"id":25870,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1836/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing hydrologic data and phreatophyte areas in the Upper Sevier River Basin, Utah"},{"id":25871,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1836/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Graphs of water levels in selected wells and selected analyses of ground and surface water in the Upper Sevier River Basin, Utah"},{"id":25872,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1836/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Upper Sevier River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d2be","contributors":{"authors":[{"text":"Carpenter, Carl H.","contributorId":46074,"corporation":false,"usgs":true,"family":"Carpenter","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143197,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Gerald B.","contributorId":46497,"corporation":false,"usgs":true,"family":"Robinson","given":"Gerald B.","affiliations":[],"preferred":false,"id":143198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bjorklund, Louis Jay","contributorId":21138,"corporation":false,"usgs":true,"family":"Bjorklund","given":"Louis","email":"","middleInitial":"Jay","affiliations":[],"preferred":false,"id":143196,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":40721,"text":"ofr678 - 1967 - Measured stratigraphic sections, Salt Croton and Croton Creek valleys, Kent and Stonewall Counties, Texas","interactions":[],"lastModifiedDate":"2016-08-24T11:24:30","indexId":"ofr678","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-8","title":"Measured stratigraphic sections, Salt Croton and Croton Creek valleys, Kent and Stonewall Counties, Texas","language":"ENGLISH","doi":"10.3133/ofr678","usgsCitation":"Baker, R.C., 1967, Measured stratigraphic sections, Salt Croton and Croton Creek valleys, Kent and Stonewall Counties, Texas: U.S. Geological Survey Open-File Report 67-8, 24 p., https://doi.org/10.3133/ofr678.","productDescription":"24 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":77995,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0008/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77996,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0008/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0008/report-thumb.jpg"},{"id":77994,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0008/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610f85","contributors":{"authors":[{"text":"Baker, R. 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Rocks other than alluvium, in all but the northern fourth of the monument, are dense igneous or metamorphic types that, unless fractured, have little potential for development of ground water. However, in some areas near faults these rocks probably will yield small supplies of water. The alluvium along Chalone Creek contains water of good chemical quality in quantities sufficient to supply the monument's needs. The Temblor Formation, a fanglomerate in the northeastern part of the monument, seems to be capable of absorbing and transmitting water but has not been drilled. A test well to determine the potential of the Temblor is suggested.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr672","collaboration":"Prepared in cooperation with the National Park Service U.S. Department of the Interior","usgsCitation":"Akers, J.P., 1967, The geohydrology of Pinnacles National Monument, California: U.S. Geological Survey Open-File Report 67-2, Report: iii, 14 p; 1 Plate: 17.28 x 22.78 inches, https://doi.org/10.3133/ofr672.","productDescription":"Report: iii, 14 p; 1 Plate: 17.28 x 22.78 inches","numberOfPages":"17","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":77990,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0002/plate-1.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geologic map of Pinnacles national Monument, California, showing location of wells, favorable areas for ground-water development, and proposed well sites"},{"id":77991,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0002/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0002/report-thumb.jpg"}],"country":"United States","state":"California","county":"Monterey County, San Benito County","otherGeospatial":"Pinnacles National Monument","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.21198654174803,\n 36.448903794892864\n ],\n [\n -121.13285064697266,\n 36.448903794892864\n ],\n [\n -121.13285064697266,\n 36.53681226263767\n ],\n [\n -121.21198654174803,\n 36.53681226263767\n ],\n [\n -121.21198654174803,\n 36.448903794892864\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf08","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":223844,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24493,"text":"ofr67195 - 1967 - Floods on Otter Creek in Linn County, Iowa","interactions":[],"lastModifiedDate":"2016-02-22T10:50:23","indexId":"ofr67195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-195","title":"Floods on Otter Creek in Linn County, Iowa","docAbstract":"No abstract available.
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S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":223852,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42325,"text":"ofr67248 - 1967 - Aeromagnetic map of the Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles, Nevada-California","interactions":[],"lastModifiedDate":"2022-11-22T21:58:09.747382","indexId":"ofr67248","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-248","title":"Aeromagnetic map of the Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles, Nevada-California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67248","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles, Nevada-California: U.S. Geological Survey Open-File Report 67-248, 1 Plate: 30.88 × 40.85 inches, https://doi.org/10.3133/ofr67248.","productDescription":"1 Plate: 30.88 × 40.85 inches","costCenters":[],"links":[{"id":409554,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8203.htm","linkFileType":{"id":5,"text":"html"}},{"id":80088,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0248/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -118,\n 38\n ],\n [\n -118,\n 37.5\n ],\n [\n -117.5,\n 37.5\n ],\n [\n -117.5,\n 38\n ],\n [\n -118,\n 38\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691a38","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530904,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32630,"text":"pp579 - 1967 - The Parkfield-Cholame, California, earthquakes of June–August 1966— Surface geologic effects water-resources aspects, and preliminary seismic data","interactions":[],"lastModifiedDate":"2021-10-27T18:21:00.771926","indexId":"pp579","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"579","title":"The Parkfield-Cholame, California, earthquakes of June–August 1966— Surface geologic effects water-resources aspects, and preliminary seismic data","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp579","usgsCitation":"Brown, R.D., Vedder, J.G., Wallace, R.E., Roth, E.F., Yerkes, R.F., Castle, R.O., Waananen, A., Page, R.W., and Eaton, J.P., 1967, The Parkfield-Cholame, California, earthquakes of June–August 1966— Surface geologic effects water-resources aspects, and preliminary seismic data: U.S. Geological Survey Professional Paper 579, 66 p., https://doi.org/10.3133/pp579.","productDescription":"66 p.","costCenters":[],"links":[{"id":391020,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4623.htm"},{"id":119203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0579/report-thumb.jpg"},{"id":60504,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0579/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.5,\n 35.6667\n ],\n [\n -120.25,\n 35.6667\n ],\n [\n -120.25,\n 36\n ],\n [\n -120.5,\n 36\n ],\n [\n -120.5,\n 35.6667\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aeb3","contributors":{"authors":[{"text":"Brown, Robert David Jr.","contributorId":18382,"corporation":false,"usgs":true,"family":"Brown","given":"Robert","suffix":"Jr.","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":208823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":208827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wallace, R. E.","contributorId":6823,"corporation":false,"usgs":true,"family":"Wallace","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":208821,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roth, E. F.","contributorId":6056,"corporation":false,"usgs":true,"family":"Roth","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":208820,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Yerkes, R. F.","contributorId":24754,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":208824,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Castle, R. O.","contributorId":79880,"corporation":false,"usgs":true,"family":"Castle","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":208825,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Waananen, A. O.","contributorId":87121,"corporation":false,"usgs":true,"family":"Waananen","given":"A. O.","affiliations":[],"preferred":false,"id":208826,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":208822,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Eaton, J. P.","contributorId":105313,"corporation":false,"usgs":true,"family":"Eaton","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":208828,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":2380,"text":"wsp1839K - 1967 - Ground-water resources of the Pascagoula River basin, Mississippi and Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1839K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1839","chapter":"K","title":"Ground-water resources of the Pascagoula River basin, Mississippi and Alabama","docAbstract":"Abundant ground-water resources underlie the Pascagoula River basin. These resources have been developed intensively in only a few places--namely, Hattiesburg, Laurel, Meridian, and Pascagoula. Seepage from the ground water reservoirs sustains the base flows of the Leaf, Chickasawhay, Pascagoula, and Escatawpa Rivers and their tributaries. \r\n\r\nThe fresh-water-bearing section is 300 to 3,500 feet thick and is composed chiefly of sand and clay of Eocene to Recent age. Major rock units represented are the Wilcox, Claiborne, Jackson, and Vicksburg Groups and formations of Miocene and Pliocene ages. \r\n\r\nAquifers in the Claiborne Group provide water for all purposes in the northern third of the basin. The Claiborne is underlain by the potentially important but virtually untapped Wilcox Group. Miocene aquifers are the main source of water supplies in the southern half of the basin, but Pliocene aquifers furnish most supplies in the Jackson County area at the basin's southern extremity. Much of the fresh-water section has undergone no water-supply development because of the great depth of many aquifers and the availability, at shallow depths, of supplies adequate for present needs. However, a large part of any substantial increase in ground-water withdrawal will probably come from wells deeper than those commonly drilled in the region. \r\n\r\nGround-water levels are within 50 feet of the surface in most places, and flowing wells are common in the valleys and near the coast. Water-level declines due to pumping have become serious problems only in a few localities of heavy withdrawal. In most of these places redistribution of pumpage would alleviate the problem of excessive drawdown. \r\n\r\nAlthough few wells in the basin yield more than 500 gallons per minute, yields of 2,000 gallons per minute or more could be reasonably expected from efficiently constructed wells almost anywhere in the region. \r\n\r\nTotal ground-water pumpage is estimated to be about 60 million gallons per day. Potential pumpage is many times that figure. Well fields capable of yielding several million gallons of water per day would be feasible in most places. The ground water is of good to excellent quality. Most of it is a sodium bicarbonate type of water. It usually is soft and has a low to moderate dissolved-solids content. Excessive iron is a problem in places, particularly where water supplies are obtained from shallow aquifers, but at least a part of the excess iron comes from corrosion of well and distribution-line fittings by slightly acidic water. \r\n\r\nSalt-water encroachment is a potential problem in the coastal area, but little increase in salinity has been observed in monitor wells in the period 1960-65. Saline-water resources are available for development at considerable depth in most of the region.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1839K","usgsCitation":"Newcome, R., 1967, Ground-water resources of the Pascagoula River basin, Mississippi and Alabama: U.S. Geological Survey Water Supply Paper 1839, iv, 36 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1839K.","productDescription":"iv, 36 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1839k/report-thumb.jpg"},{"id":28339,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1839k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a70d","contributors":{"authors":[{"text":"Newcome, Roy","contributorId":14796,"corporation":false,"usgs":true,"family":"Newcome","given":"Roy","affiliations":[],"preferred":false,"id":145109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":933,"text":"wsp1839G - 1967 - Water resources of Jackson and Independence Counties, Arkansas","interactions":[],"lastModifiedDate":"2022-04-29T21:49:44.290206","indexId":"wsp1839G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1839","chapter":"G","title":"Water resources of Jackson and Independence Counties, Arkansas","docAbstract":"The present (1965) water use in Jackson and Independence Counties is about 55.6 million gallons per day, and quantities sufficient for any foreseeable use are available. Supplies for the large-scale uses--municipal, industrial, and irrigation--can best be obtained from wells in the Coastal Plain and from streams in the highlands. \r\n\r\nWells in the Coastal Plain will yield 1,000-2,000 gallons of water per minute when screened at depths from 100 to 150 feet in alluvial sand and gravel of Quaternary age. The water will require treatment for the removal of iron and the reduction of hardness to be suitable for municipal and industrial uses. Wells in the highlands generally yield less than 50 gallons per minute of water that is of good quality, though hard. \r\n\r\nThe dependable flow of .the White River at Newport is about 4.2 billion gallons per day. The dependable 'base flows of the small streams tributary to the White River in the Salem Plateau and Springfield Plateau sections range from 0.25 to 5 million gallons per day, and the dependable flow of Polk Bayou at Batesville is about 21 million gallons per day. These streams can be utilized for water supply with little or no artificial storage required. Streams in the Boston Mountains section and in the Arkansas Valley section recede to very low flow or to no flow during extended dry periods, but dependable, supplies can be obtained from these streams 'by construction of storage facilities Water from all the highland streams is af excellent chemical quality except that it generally is hard.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1839G","usgsCitation":"Albin, D.R., Hines, M.S., and Stephens, J.W., 1967, Water resources of Jackson and Independence Counties, Arkansas: U.S. Geological Survey Water Supply Paper 1839, iv, 29 p., https://doi.org/10.3133/wsp1839G.","productDescription":"iv, 29 p.","costCenters":[],"links":[{"id":399957,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25048.htm"},{"id":25406,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1839g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1839g/report-thumb.jpg"}],"country":"United States","state":"Arkansas","county":"Independence County, Jackson County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-91.7126,35.9418],[-91.6882,35.9413],[-91.5479,35.9381],[-91.5434,35.9381],[-91.4627,35.936],[-91.4647,35.8951],[-91.4641,35.8911],[-91.3602,35.8919],[-91.2507,35.8895],[-91.2444,35.8894],[-91.199,35.89],[-91.1371,35.8896],[-91.0951,35.8875],[-91.0894,35.8874],[-91.0321,35.8847],[-91.0333,35.8366],[-91.0334,35.8271],[-91.0347,35.8185],[-91.0344,35.7967],[-91.0355,35.7082],[-91.0374,35.6883],[-91.0382,35.6715],[-91.039,35.6048],[-91.0382,35.495],[-91.0378,35.4791],[-91.0366,35.4423],[-91.0374,35.4246],[-91.0399,35.3543],[-91.0614,35.3554],[-91.0805,35.3555],[-91.1414,35.3569],[-91.1425,35.3564],[-91.1623,35.3566],[-91.1679,35.3566],[-91.1814,35.3567],[-91.1989,35.3568],[-91.2514,35.3567],[-91.2522,35.4457],[-91.3482,35.4453],[-91.3476,35.439],[-91.3482,35.439],[-91.478,35.4401],[-91.5853,35.4423],[-91.5834,35.4823],[-91.5827,35.5036],[-91.5815,35.5163],[-91.5808,35.5308],[-91.6006,35.5313],[-91.6289,35.5319],[-91.6543,35.5324],[-91.6628,35.5329],[-91.6933,35.533],[-91.7068,35.533],[-91.7922,35.5341],[-91.7902,35.6217],[-91.7889,35.7047],[-91.7883,35.7156],[-91.7951,35.712],[-91.8064,35.7052],[-91.837,35.7048],[-91.8364,35.7488],[-91.8477,35.7592],[-91.8545,35.7629],[-91.8652,35.7706],[-91.8646,35.7792],[-91.8669,35.7856],[-91.8697,35.7929],[-91.8697,35.8051],[-91.8714,35.8105],[-91.8674,35.821],[-91.856,35.8391],[-91.8509,35.8573],[-91.8497,35.8672],[-91.7536,35.9428],[-91.7484,35.9428],[-91.7126,35.9418]]]},\"properties\":{\"name\":\"Independence\",\"state\":\"AR\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faff9","contributors":{"authors":[{"text":"Albin, Donald R.","contributorId":67486,"corporation":false,"usgs":true,"family":"Albin","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":142878,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hines, Marion S.","contributorId":29388,"corporation":false,"usgs":true,"family":"Hines","given":"Marion","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":142877,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stephens, John W.","contributorId":76286,"corporation":false,"usgs":true,"family":"Stephens","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":142879,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2329,"text":"wsp1819K - 1967 - Correlation and analysis of water-temperature data for Oregon streams","interactions":[{"subject":{"id":52485,"text":"ofr65112 - 1965 - Correlation and analysis of water-temperature data for Oregon streams","indexId":"ofr65112","publicationYear":"1965","noYear":false,"title":"Correlation and analysis of water-temperature data for Oregon streams"},"predicate":"SUPERSEDED_BY","object":{"id":2329,"text":"wsp1819K - 1967 - Correlation and analysis of water-temperature data for Oregon streams","indexId":"wsp1819K","publicationYear":"1967","noYear":false,"chapter":"K","title":"Correlation and analysis of water-temperature data for Oregon streams"},"id":1}],"lastModifiedDate":"2017-02-03T13:42:02","indexId":"wsp1819K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1819","chapter":"K","title":"Correlation and analysis of water-temperature data for Oregon streams","language":"ENGLISH","publisher":"U.S. Govt. Print. Office,","doi":"10.3133/wsp1819K","usgsCitation":"Moore, A., 1967, Correlation and analysis of water-temperature data for Oregon streams: U.S. Geological Survey Water Supply Paper 1819, iv, 53 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1819K.","productDescription":"iv, 53 p. :ill. ;23 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":137616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819k/report-thumb.jpg"},{"id":28172,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28173,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684749","contributors":{"authors":[{"text":"Moore, A.M.","contributorId":87909,"corporation":false,"usgs":true,"family":"Moore","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":145021,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42348,"text":"ofr67224 - 1967 - Aeromagnetic map of the Aurora, Powell Mountain, and Huntoon Valley quadrangles and part of the Trench Canyon quadrangle, Nevada-California","interactions":[],"lastModifiedDate":"2025-07-24T19:44:54.186569","indexId":"ofr67224","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-224","title":"Aeromagnetic map of the Aurora, Powell Mountain, and Huntoon Valley quadrangles and part of the Trench Canyon quadrangle, Nevada-California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67224","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Aurora, Powell Mountain, and Huntoon Valley quadrangles and part of the Trench Canyon quadrangle, Nevada-California: U.S. Geological Survey Open-File Report 67-224, 1 Plate: 29.67 x 42.79 inches, https://doi.org/10.3133/ofr67224.","productDescription":"1 Plate: 29.67 x 42.79 inches","costCenters":[],"links":[{"id":414489,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8179.htm","linkFileType":{"id":5,"text":"html"}},{"id":80114,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0224/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173477,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Aurora, Powell Mountain, Huntoon Valley, and Trench Canyon quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119,\n 38.5\n ],\n [\n -119,\n 38\n ],\n [\n -118.5,\n 38\n ],\n [\n -118.5,\n 38.5\n ],\n [\n -119,\n 38.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697271","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68206,"text":"ha242 - 1967 - Ground water of Baker Valley, Baker County, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:24:56","indexId":"ha242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"242","title":"Ground water of Baker Valley, Baker County, Oregon","language":"ENGLISH","doi":"10.3133/ha242","usgsCitation":"Lystrom, D.J., Nees, W., and Hampton, E.R., 1967, Ground water of Baker Valley, Baker County, Oregon: U.S. Geological Survey Hydrologic Atlas 242, 1 map., https://doi.org/10.3133/ha242.","productDescription":"1 map.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":185550,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89551,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/242/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89552,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/242/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"96000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -12.25,45 ], [ -12.25,45 ], [ -12.25,45 ], [ -12.25,45 ], [ -12.25,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d777","contributors":{"authors":[{"text":"Lystrom, David J.","contributorId":101283,"corporation":false,"usgs":true,"family":"Lystrom","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":277840,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nees, W.L.","contributorId":93571,"corporation":false,"usgs":true,"family":"Nees","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":277839,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":277838,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68482,"text":"ha174 - 1967 - Availability of ground water in the Melber quadrangle, Jackson Purchase region, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:25","indexId":"ha174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"174","title":"Availability of ground water in the Melber quadrangle, Jackson Purchase region, Kentucky","language":"ENGLISH","doi":"10.3133/ha174","usgsCitation":"Davis, R.W., 1967, Availability of ground water in the Melber quadrangle, Jackson Purchase region, Kentucky: U.S. Geological Survey Hydrologic Atlas 174, 1 map., https://doi.org/10.3133/ha174.","productDescription":"1 map.","costCenters":[],"links":[{"id":188023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90035,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/174/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.75,36.8675 ], [ -88.75,37 ], [ -88.61749999999999,37 ], [ -88.61749999999999,36.8675 ], [ -88.75,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d853","contributors":{"authors":[{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":278303,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63992,"text":"gp610 - 1967 - Aeromagnetic map of parts of the Ralph and Norway quadrangles, Dickinson County, Michigan","interactions":[],"lastModifiedDate":"2012-02-10T00:10:51","indexId":"gp610","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"610","title":"Aeromagnetic map of parts of the Ralph and Norway quadrangles, Dickinson County, Michigan","language":"ENGLISH","doi":"10.3133/gp610","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of parts of the Ralph and Norway quadrangles, Dickinson County, Michigan: U.S. Geological Survey Geophysical Investigations Map 610, 1 map., https://doi.org/10.3133/gp610.","productDescription":"1 map.","costCenters":[],"links":[{"id":250384,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0610/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":250385,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0610/plate-1.pdf","size":"6582","linkFileType":{"id":1,"text":"pdf"}},{"id":253840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0610/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88,45.75 ], [ -88,46.1175 ], [ -87.75,46.1175 ], [ -87.75,45.75 ], [ -88,45.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6974f9","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533461,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5868,"text":"pp522 - 1967 - Areal geology of the western Mojave Desert, California","interactions":[{"subject":{"id":43027,"text":"ofr5739 - 1957 - Simplified geologic map of the western Mojave Desert, California","indexId":"ofr5739","publicationYear":"1957","noYear":false,"title":"Simplified geologic map of the western Mojave Desert, California"},"predicate":"SUPERSEDED_BY","object":{"id":5868,"text":"pp522 - 1967 - Areal geology of the western Mojave Desert, California","indexId":"pp522","publicationYear":"1967","noYear":false,"title":"Areal geology of the western Mojave Desert, California"},"id":1}],"lastModifiedDate":"2017-04-25T14:08:32","indexId":"pp522","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"522","title":"Areal geology of the western Mojave Desert, California","docAbstract":"This report and map represent part of a geologic investigation by the U.S. Geological Survey of the known and potential deposits of borate minerals in the southern California desert regions. The primary purpose of this report and the geologic map (pl. 1) is to provide a geologic background for the exploration for possible concealed borate deposits in the western Mojave Desert, based upon (1) the geology of the known deposits of these minerals within the region, (2) the areal geology of the region, and (3) the subsurface geology as determined insofar as possible from logs of exploratory test holes, mine workings, and geophysical data. Available logs of test holes so used, including those drilled for petroleum and some for water, and of borate mine shafts are summarized in tabulated form (tables 2-4); the gravity geophysical data are published separately (Mabey, 1960).
The resulting geologic data are of use for many secondary purposes, such as exploration for other commodities, including petroleum and gas, and in evaluation of ground-water conditions.
The base for the geologic map was prepared by joining parts of the Bakersfield, Trona, Los Angeles, and San Bernardino quadrangles, as published by the U.S. Geological Survey at a scale of 1:250,000, and then enlarging the mosaicked map to a scale of 1:125,000. Although lacking in detail and accuracy, the base is the best that is available. Numerous maps at a scale of an inch to a mile or larger show the geology of most of the complex areas in greater detail.
","language":"English","publisher":"U.S.Government Printing Office","doi":"10.3133/pp522","usgsCitation":"Dibblee, T.W., 1967, Areal geology of the western Mojave Desert, California: U.S. Geological Survey Professional Paper 522, Report: vii, 153 p.; 5 Plates: 40.26 x 48.24 inches or smaller, https://doi.org/10.3133/pp522.","productDescription":"Report: vii, 153 p.; 5 Plates: 40.26 x 48.24 inches or smaller","costCenters":[],"links":[{"id":340296,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0522/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":112641,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0522/report.pdf","text":"Report","size":"22.06 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":340297,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0522/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":139825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0522/report-thumb.jpg"},{"id":340293,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0522/plate-1_east.pdf","text":"Plate 1 (East Half)","linkFileType":{"id":1,"text":"pdf"}},{"id":340294,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0522/plate-1_west.pdf","text":"Plate 1 (West Half)","linkFileType":{"id":1,"text":"pdf"}},{"id":340295,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0522/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119,\n 34\n ],\n [\n -117,\n 34\n ],\n [\n -117,\n 36\n ],\n [\n -119,\n 36\n ],\n [\n -119,\n 34\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673222","contributors":{"authors":[{"text":"Dibblee, Thomas W. Jr.","contributorId":189713,"corporation":false,"usgs":false,"family":"Dibblee","given":"Thomas","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":151710,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}