Ladies and gentlemen, it is a pleasure to be invited to attend this Irrigation Institute conference and to describe the Geological Survey's program of ground-water studies in the San Joaquin Valley.
The U.S. Geological Survey has been making water-resources studies in cooperation with the State of California and other agencies in California for more than 70 years. Three of the earliest Geological Survey Water-Supply Papers--numbers 17, 18, and 19--published in 1898 and 1899, describe \"Irrigation near Bakersfield,\" \"Irrigation near Fresno,\" and \"Irrigation near Merced.\" However, the first Survey report on ground-water occurrence in the San Joaquin Valley was \"Ground Water in the San Joaquin Valley,\" by Mendenhall and others. The fieldwork was done from 1905 to 1910, and the report was published in 1916 as U.S. Geological Survey Water-Supply Paper 398.
The current series of ground-water studies in the San Joaquin Valley was begun in 1952 as part of the California Department of Water Resources-U.S. Geological Survey cooperative water-resources program. The first report of this series is Geological Survey Water-Supply Paper 1469, \"Ground-Water Conditions and Storage Capacity in the San Joaquin Valley.\" Other reports are Water-Supply Paper 1618, \"Use of Ground-Water Reservoirs for Storage of Surface Water in the San Joaquin Valley;\" Water-Supply Paper 1656, \"Geology and Ground-Water Features of the Edison-Maricopa Area;\" Water-Supply Paper 1360-G, \"Ground- Water Conditions in the Mendota-Huron Area;\" Water-Supply Paper 1457, \"Ground-Water Conditions in the Avenal-McKittrick Area;\" and an open-file report, \"Geology, Hydrology, and Quality of Water in the Terra Bella-Lost Hills Area.\"
In addition to the preceding published reports, ground-water studies currently are being made of the Kern Fan area, the Hanford- Visalia area, the Fresno area, the Merced area, and of the clays of Tulare Lake. Also, detailed studies of both shallow and deep subsidence in the southern part of the San Joaquin Valley are being made by the Subsidence Research Section at Sacramento, and research on permeability and specific yield in the San Joaquin Valley is being done by our hydrologic laboratory at Denver.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr6675","usgsCitation":"Kunkel, F., and Hofman, W., 1966, Ground water in the San Joaquin Valley, California: U.S. Geological Survey Open-File Report 66-75, 14 p., https://doi.org/10.3133/ofr6675.","productDescription":"14 p.","numberOfPages":"15","costCenters":[],"links":[{"id":174817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":329667,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0075/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d896","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":245542,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hofman, Walter","contributorId":14496,"corporation":false,"usgs":true,"family":"Hofman","given":"Walter","email":"","affiliations":[],"preferred":false,"id":245541,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":22830,"text":"ofr6621 - 1966 - Ground-Water Geology and Hydrology of the Kern River Alluvial-Fan Area, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"ofr6621","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-21","title":"Ground-Water Geology and Hydrology of the Kern River Alluvial-Fan Area, California","docAbstract":"The Kern River alluvial fan is the southernmost major alluvial fan built by the streams which drain the west side of the Sierra Nevada. The climate is semiarid with rainfall near 5 inches per year. Agricultural development within the area uses over half the 700,000 acre-feet per year flow of the Kern River, plus a considerable amount drawn from the ground-water reservoir particularly during periods of low flow. \r\n\r\nThe area overlies a deep structural trough between crystalline rocks of the Sierra Nevada and the marine rocks of Tertiary age of the Coast Ranges. The top horizon of the marine rocks that lap on the Sierra Nevada block underlies the report area at an average depth of 2,000 feet. The overlying continental deposits that form the groundwater reservoir consist of alluvial-fan and lacustrine deposits. \r\n\r\nThe continental deposits are subdivided into three lithologic units on the basis of grain size and sorting. The gravel and clay unit consists of older alluvial-fan material, of both Sierra Nevada and Coast Range provenance, that shows extremely poor sorting with some diagenetic decomposition through chemical weathering. The fine sand to clay unit consists principally of fine sand, silt, and clay deposited in a lacustrine environment, although some of the unit is of alluvial-fan origin derived from poorly consolidated marine shale of the Coast Ranges. Within the fine sand to clay unit three distinct clays, which affect ground-water conditions, can be recognized. The gravel to medium sand unit consists of unweathered alluvial-fan material that shows much better sorting than the gravel and clay unit. In the eastern part of the area the basal part of this unit is a gravel lentil that can be traced in the subsurface more than 250 square miles. The overlying deposits consist principally of medium sand. In the western part of the area the unit is a heterogeneous gravel and sand unit. Permeability in Meinzer units of the gravel and clay unit ranges between 10 and 100 with specific yield about 5 percent. For the fine sand to clay unit the permeability ranges between 0.0001 and 100 with about 10 percent specific yield. The gravel to medium sand unit has permeabilities between 100 and 10,000, and specific yield is about 15 percent. \r\n\r\nFor the period 1955-59 the annual gross surface-water supply was estimated at 421,000 acre-feet and pumpage was 664,000 acre-feet, giving a rounded total supply of 1,100,000 acre-feet. Annual consumptive use was estimated at 750,000 acre-feet and annual infiltration at 350,000 acre-feet. The approximate 300,000 acre-feet difference between 664,000 acre-feet pumped and 350,000 acre-feet infiltrated has caused an annual decline in water levels of up to 7 feet. \r\n\r\nGround water occurs under both unconfined and confined conditions within the report area. In general, the gravel to medium sand unit contains unconfined water, and the other two units contain confined water. \r\n\r\nPumping is less intense in the Kern River fan area than in the adjoining areas to the north or south. This fact, plus infiltration from the Kern River, results in ground-water movement being principally out of the area. There is a ground-water divide that approximately underlies the Kern River. South of the river the flow spreads out semicircularly from the river, and north of the river the flow is linear to the northwest. \r\n\r\nBased on chemical quality the ground water has been divided areally into (1) east side, (2) west side, and (3) axial water. \r\n\r\nWith the exception of two areas of comparable size northwest of Bakersfield and a much smaller area southeast of that city where ground water is somewhat saline, east-side ground water is generally of the calcium bicarbonate and calcium sodium bicarbonate type of low to medium salinity. The chemical character of east-side ground water is necessarily related to that of Kern River water, the principal source of recharge, and water of intermittent streams which drain the dissected upland","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr6621","issn":"0094-9140","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Dale, R.H., French, J.J., and Gordon, G.V., 1966, Ground-Water Geology and Hydrology of the Kern River Alluvial-Fan Area, California: U.S. Geological Survey Open-File Report 66-21, Report: iv, 92 p.; 7 Plates, https://doi.org/10.3133/ofr6621.","productDescription":"Report: iv, 92 p.; 7 Plates","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":110360,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52793.htm","linkFileType":{"id":5,"text":"html"},"description":"52793"},{"id":156947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0021/report-thumb.jpg"},{"id":52251,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0021/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52252,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0021/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52253,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0021/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52254,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0021/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52255,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0021/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52256,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0021/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52257,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0021/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52258,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d697","contributors":{"authors":[{"text":"Dale, R. H.","contributorId":98711,"corporation":false,"usgs":true,"family":"Dale","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":188955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"French, James J.","contributorId":103651,"corporation":false,"usgs":true,"family":"French","given":"James","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":188956,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gordon, G. V.","contributorId":30254,"corporation":false,"usgs":true,"family":"Gordon","given":"G.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":188954,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":22831,"text":"ofr6622 - 1966 - Hydrologic reconnaissance of Point Reyes National Seashore area, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"ofr6622","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-22","title":"Hydrologic reconnaissance of Point Reyes National Seashore area, California","docAbstract":"This report summarizes the results of a hydrologic reconnaissance of the Point Reyes National Seashore area, the primary purpose of which was to appraise potential sources of water supply at park sites where visitor accommodations are proposed. \r\n\r\nPoint Reyes National Seashore is a peninsular area on the California coast about 50miles north of San Francisco. Inverness Ridge, with peaks about 1,400 feet above sea level, forms the eastern boundary of the seashore. Marine terraces, extending from sea level to altitudes of about 400 feet, form the remainder of the area.","language":"ENGLISH","publisher":"U.S. Dept. of Interior, Geological Survey, Water Resources Division,","doi":"10.3133/ofr6622","issn":"0094-9140","usgsCitation":"Dale, R.H., and Rantz, S., 1966, Hydrologic reconnaissance of Point Reyes National Seashore area, California: U.S. Geological Survey Open-File Report 66-22, 37 p. ill., maps ;27 cm., https://doi.org/10.3133/ofr6622.","productDescription":"37 p. ill., maps ;27 cm.","costCenters":[],"links":[{"id":156948,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0022/report-thumb.jpg"},{"id":52259,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0022/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52260,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0022/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52261,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0022/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52262,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6055b4","contributors":{"authors":[{"text":"Dale, R. H.","contributorId":98711,"corporation":false,"usgs":true,"family":"Dale","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":188958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rantz, S. E.","contributorId":34106,"corporation":false,"usgs":true,"family":"Rantz","given":"S. E.","affiliations":[],"preferred":false,"id":188957,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68243,"text":"ha173 - 1966 - Availability of ground water in the La Center quadrangle, Jackson Purchase region, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:11","indexId":"ha173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"173","title":"Availability of ground water in the La Center quadrangle, Jackson Purchase region, Kentucky","language":"ENGLISH","doi":"10.3133/ha173","usgsCitation":"Lambert, T.W., 1966, Availability of ground water in the La Center quadrangle, Jackson Purchase region, Kentucky: U.S. Geological Survey Hydrologic Atlas 173, 1 map., https://doi.org/10.3133/ha173.","productDescription":"1 map.","costCenters":[],"links":[{"id":189571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89623,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/173/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89,37 ], [ -89,37.1175 ], [ -88.86749999999999,37.1175 ], [ -88.86749999999999,37 ], [ -89,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d900","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277900,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68182,"text":"ha206 - 1966 - Floods in River Forest Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"ha206","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"206","title":"Floods in River Forest Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha206","usgsCitation":"May, V.J., 1966, Floods in River Forest Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 206, 1 col. map ;58 x 43 cm., on sheet 82 x 114 cm., https://doi.org/10.3133/ha206.","productDescription":"1 col. map ;58 x 43 cm., on sheet 82 x 114 cm.","costCenters":[],"links":[{"id":186466,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89492,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/206/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.86749999999999,41.8675 ], [ -87.86749999999999,42 ], [ -87.75,42 ], [ -87.75,41.8675 ], [ -87.86749999999999,41.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5178","contributors":{"authors":[{"text":"May, V. Jeff","contributorId":80358,"corporation":false,"usgs":true,"family":"May","given":"V.","email":"","middleInitial":"Jeff","affiliations":[],"preferred":false,"id":277793,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68181,"text":"ha228 - 1966 - Floods in Plainfield Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"ha228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"228","title":"Floods in Plainfield Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha228","usgsCitation":"May, V.J., and Schafish, R.J., 1966, Floods in Plainfield Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 228, 1 col. map ;58 x 44 cm., on sheet 83 x 135 cm., https://doi.org/10.3133/ha228.","productDescription":"1 col. map ;58 x 44 cm., on sheet 83 x 135 cm.","costCenters":[],"links":[{"id":186465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89491,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/228/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.25,41.5 ], [ -88.25,41.6175 ], [ -88.11749999999999,41.6175 ], [ -88.11749999999999,41.5 ], [ -88.25,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6979","contributors":{"authors":[{"text":"May, V. Jeff","contributorId":80358,"corporation":false,"usgs":true,"family":"May","given":"V.","email":"","middleInitial":"Jeff","affiliations":[],"preferred":false,"id":277792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schafish, Robert J.","contributorId":15707,"corporation":false,"usgs":true,"family":"Schafish","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":277791,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68180,"text":"ha210 - 1966 - Floods in Normantown Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"ha210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"210","title":"Floods in Normantown Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha210","usgsCitation":"May, V.J., 1966, Floods in Normantown Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 210, 1 col. map ;58 x 44 cm., on sheet 78 x 124 cm., https://doi.org/10.3133/ha210.","productDescription":"1 col. map ;58 x 44 cm., on sheet 78 x 124 cm.","costCenters":[],"links":[{"id":186379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89490,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/210/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.25,41.6175 ], [ -88.25,41.75 ], [ -88.11749999999999,41.75 ], [ -88.11749999999999,41.6175 ], [ -88.25,41.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e715b","contributors":{"authors":[{"text":"May, V. 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