Atascosa County, Tex., is underlain by water-bearing sands of Tertiary age that furnish water for domestic and stock supplies throughout the county, for the public supply of all except one of the towns and cities in the county, for irrigation in several localities, for drilling oil wells in the central and southern parts of the county, for washing glass sand in the northern part of the county, and for maintaining several lakes that are used for hunting and fishing. By far the most productive formation is the Carrizo sand, but supplies of considerable magnitude are also obtained from sands in the Mount Selman and Cook Mountain. formations. The rate of withdrawal from the Carrizo sand amounted to about 15,500 acre-feet a year in 1944-45 or an average of about 13.8 million gallons a day. This was about 6,000 acre-feet a year greater in 1944-45 than it was in 1929-30. Of the total amount of water withdrawn in 1944-45 about 6,500 acre-feet a year is largely wasted from uncontrolled flowing wells. If the waste of water from wells in the Carrizo sand were stopped, the consumption of water for useful purposes could be increased about 70 percent without increasing the draft on the underground reservoir. The increase in total withdrawals from the Carrizo sand has been accompanied by a general decline in the artesian head between 1929-30 and 1944 ranging from 3 to 25 feet. On the whole, the evidence shows that the artesian reservoir is not being overdrawn and that it will sustain a somewhat greater draft.
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A.","contributorId":99819,"corporation":false,"usgs":true,"family":"La Rocque","given":"G. A.","affiliations":[],"preferred":false,"id":144616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Upson, J. E.","contributorId":49342,"corporation":false,"usgs":true,"family":"Upson","given":"J. E.","affiliations":[],"preferred":false,"id":144614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Worts, G. 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The geologic formations discussed in this report in upward sequence consist of the Oakville sandstone of Miocene age and the Lagarto clay of Miocene (?) age, the Willis sand of Pliocene (?) age, and the Lissie formation and Beaumont clay of Pleistocene age. The rocks of these formations crop out in belts roughly parallel to the Gulf shore and dip southeastward. As one travels across San Jacinto and Liberty Counties from northwest to southeast the belts of outcrop are traversed in the above order, beginning with the 0akville sandstone and Lagarto clay. The land surface slopes southeastward toward the Gulf at a rate less than the dip of the rocks; consequently artesian conditions exist in all parts of the county. The valley of the Trinity River is well known for its flowing weds, which range from 100 to 808 feet in depth. Most of the ground water used in the county is obtained from wells ranging in depth from 350 to about 1,000 feet and is drawn from the Lissie formation. Wells yielding 1,000 to 3,500 gallons a minute and ranging from 740 to 1,030 feet in depth have been developed for rice irrigation in the North Dayton area, in the southwestern part of the county. These wells draw water mostly from sands in the Lissie formation, but most of them are also screened in overlying thinner sands in the Beaumont clay. The municipal water supplies of Liberty, Cleveland, Dayton, and Diasetta are obtained from wells ranging from 350 to 833 feet in depth with reported yields of 300 to 350 gallons a minute. Most of the wells in the rural areas are less than 50 feet in depth and furnish small supplies of water for domestic use and for stock. Such supplies can be obtained almost anywhere in the county from shallow wells in the Lissie and Beaumont formations or in alluvial deposits. The average daily withdrawal of ground water for irrigation, public supply, and industrial use is estimated to have been about 7,500,000 gallons in 1944, distributed as follows: irrigation, 6,780,000 gallons; public supply, 325,000 gallons; and industrial use, 395,000 gallons.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1079A","usgsCitation":"Alexander, W.H., and Breeding, S.D., 1950, Ground-water resources of Liberty County, Texas, with a section on Stream runoff: U.S. Geological Survey Water Supply Paper 1079, iv, 61 p., https://doi.org/10.3133/wsp1079A.","productDescription":"iv, 61 p.","numberOfPages":"65","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137201,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1079a/report-thumb.jpg"},{"id":25411,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1079a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649cc0","contributors":{"authors":[{"text":"Alexander, Walter H. 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Off.,","doi":"10.3133/wsp1119","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1950, Surface water supply of the United States, 1948, Part IX, Colorado River basin: U.S. Geological Survey Water Supply Paper 1119, ix, 421 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1119.","productDescription":"ix, 421 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1119/report-thumb.jpg"},{"id":25184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1119/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696825","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":527593,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1063,"text":"wsp1079B - 1950 - Ground-water resources of Gregg County, Texas, with a section on Stream runoff","interactions":[],"lastModifiedDate":"2016-08-19T15:27:11","indexId":"wsp1079B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"1079","chapter":"B","title":"Ground-water resources of Gregg County, Texas, with a section on Stream runoff","docAbstract":"Field work in the island of St. Croix, V. I., was carried on from December 1938 to April 1939 in connection with a test-drilling program for water sup- plies. The island is 21 miles long and has a maximum width of 6 miles. Its western part consists of a range of mountains flanked on the south by a rolling plain; its narrower eastern part is entirely mountainous. There are only a few small streams. The rolling and fiat lands are cultivated or are in grass, and the mountainous areas are either wooded or in grass. The average rain- fall of the island is 46.34 inches, but severe droughts and periods of excess precipitation are not uncommon. The island is made up of rocks of Upper Cretaceous age, mostly volcanic tufts and limestones known as the Mount Eagle volcanics; diorite intruded into the cretaceous rocks; and Oligocene to Miocene blue clays and yellow marls (the Jealousy formation and Kingshill marl, respectively). Alluvium is widely distributed. The Mount Eagle rocks were strongly folded in early Tertiary time and the Kingshill strata gently folded in post Lower-Miocene time along an east-northeast axis. Three early Tertiary cycles of erosion are recognized. After the folding of the Kingshill marl, streams followed the strike of the folded rocks in a westerly direction, but they gradually assumed southward courses across the marl plain and as a result a western area of old-age topography, a central area of late-mature topography, and an eastern area of early-mature topography have been created. Submerged reefs and emergent reefs and beaches indicate several fairly recent stands of the sea. Water for human consumption is obtained by collecting rain water in cis- terns, but water for other purposes is almost entirely supplied by wells which are generally less than 100 feet deep. Many dug wells are used, but in recent years drilled wells have been constructed. Most of them are discharged by wind-powered pumps of small capacity. Wells are developed in all the rocks mentioned (except coral reef), but the best yields are obtained from the alluvium. A maximum yield of 80 gallons a minute was obtained from a gravel-packed well in the alluvial valley at Fair Plain. Further exploration of the alluvium is recommended. The weathered diorite also appears to be a fairly good water-bearing formation. Test drilling showed that deep water- bearing formations should probably not be expected beneath the Tertiary rocks. Most of the ground waters of St. Croix contain a moderately high mineral content owing to the solution of rock-forming minerals and the deposition of alkali and salt spray in the soil. Only a few wells are contaminated by sea water. The low hardness of some highly mineralized waters is believe due to base exchange. The most highly mineralized waters are found in the alluvium in areas with alkali soil and in some places in the Tertiary limestones where presumably soluble salts were deposited in those strata. The least mineralized waters are found in shallow wells in the alluvial near the foot of the mountains and in the areas of dioritic rock. Many well waters in Croix, if properly protected from contamination might be entirely suited to human consumption. Although many waters are hard, they are used for domestic purposes. Most waters, even those high in chloride, are reported to be excellent for cattle consumption. Most ground waters in St. Croix cannot be used for boiler feed without treatment but are used for o*her purposes in the manufacture of sugar and rum. A brief discussion of the results of test drilling by the National Park Service in 1940-41 is also given.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1079B","usgsCitation":"Broadhurst, W., and Breeding, S., 1950, Ground-water resources of Gregg County, Texas, with a section on Stream runoff: U.S. Geological Survey Water Supply Paper 1079, 48 p., https://doi.org/10.3133/wsp1079B.","productDescription":"48 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":138101,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1079b/report-thumb.jpg"},{"id":25742,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1079b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d7c8","contributors":{"authors":[{"text":"Broadhurst, W. 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L.","affiliations":[],"preferred":false,"id":143113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breeding, S.D.","contributorId":73983,"corporation":false,"usgs":true,"family":"Breeding","given":"S.D.","email":"","affiliations":[],"preferred":false,"id":143114,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":608,"text":"wsp1083 - 1950 - Surface water supply of the United States, 1947, Part III, Ohio River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1083","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"1083","title":"Surface water supply of the United States, 1947, Part III, Ohio River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. 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Off.,","doi":"10.3133/wsp1081","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1950, Surface water supply of the United States, 1947, Part I, North Atlantic slope basins: U.S. Geological Survey Water Supply Paper 1081, xiii, 682 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1081.","productDescription":"xiii, 682 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1081/report-thumb.jpg"},{"id":25169,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1081/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69687b","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":527578,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":620,"text":"wsp1118 - 1950 - Surface water supply of the United States, 1948: Part VIII, Western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2022-02-16T16:33:13.655817","indexId":"wsp1118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"1118","title":"Surface water supply of the United States, 1948: Part VIII, Western Gulf of Mexico basins","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1118","collaboration":"Prepared in cooperation with the States of Colorado, Louisiana, New Mexico, and Texas and other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1950, Surface water supply of the United States, 1948: Part VIII, Western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1118, ix, 371 p., https://doi.org/10.3133/wsp1118.","productDescription":"ix, 371 p.","costCenters":[],"links":[{"id":25183,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1118/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1118/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Gulf of Mexico","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6967ba","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":527592,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1121,"text":"wsp1067 - 1950 - Geology and ground-water resources of St. Croix, Virgin Islands","interactions":[],"lastModifiedDate":"2022-03-22T18:16:25.496326","indexId":"wsp1067","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"1067","title":"Geology and ground-water resources of St. Croix, Virgin Islands","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1067","usgsCitation":"Cederstrom, D.J., 1950, Geology and ground-water resources of St. Croix, Virgin Islands: U.S. Geological Survey Water Supply Paper 1067, Report: vi, 117 p.; 1 Plate: 42.15 × 17.39 inches, https://doi.org/10.3133/wsp1067.","productDescription":"Report: vi, 117 p.; 1 Plate: 42.15 × 17.39 inches","costCenters":[],"links":[{"id":25886,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1067/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397408,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24200.htm"},{"id":276518,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1067/plate-1.pdf"},{"id":138013,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1067/report-thumb.jpg"}],"scale":"40000","otherGeospatial":"St. Croix, Virgin Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -64.90104675292969,\n 17.67281087850531\n ],\n [\n -64.82414245605469,\n 17.680007371394908\n ],\n [\n -64.67033386230469,\n 17.704865765761966\n ],\n [\n -64.56733703613281,\n 17.746724751690945\n ],\n [\n -64.5611572265625,\n 17.757187970064102\n ],\n [\n -64.67857360839844,\n 17.765034982321307\n ],\n [\n -64.68818664550781,\n 17.757187970064102\n ],\n [\n -64.70329284667969,\n 17.75195643734173\n ],\n [\n -64.75273132324219,\n 17.787920134296662\n ],\n [\n -64.82070922851562,\n 17.781381818516973\n ],\n [\n -64.83718872070312,\n 17.76765057656712\n ],\n [\n -64.88800048828125,\n 17.773535523719293\n ],\n [\n -64.89692687988281,\n 17.74149291315094\n ],\n [\n -64.88731384277344,\n 17.711406876502377\n ],\n [\n -64.90997314453125,\n 17.675427818339383\n ],\n [\n -64.90104675292969,\n 17.67281087850531\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6858fd","contributors":{"authors":[{"text":"Cederstrom, Dagfin John","contributorId":90287,"corporation":false,"usgs":true,"family":"Cederstrom","given":"Dagfin","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":143210,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":50902,"text":"ofr5013 - 1950 - The upper Mississippi Valley zinc-lead district; In two parts: I General structural relations of the upper Mississippi Valley zinc-lead district. II. The ore deposits of the upper Mississippi Valley zinc-lead district","interactions":[],"lastModifiedDate":"2025-08-25T16:06:40.667255","indexId":"ofr5013","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"50-13","title":"The upper Mississippi Valley zinc-lead district; In two parts: I General structural relations of the upper Mississippi Valley zinc-lead district. II. The ore deposits of the upper Mississippi Valley zinc-lead district","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5013","usgsCitation":"Heyl, A.V., 1950, The upper Mississippi Valley zinc-lead district; In two parts: I General structural relations of the upper Mississippi Valley zinc-lead district. II. 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