Duval County is situated in southern Texas, 100 to 150 miles south of San Antonio and about midway between Corpus Christi, on the Gulf of Mexico, and Laredo, on the Rio Grande. The county lies on the Coastal Plain, which for the most part is low and relatively featureless. Between the Nueces River and the Rio Grande in this part of Texas the plain is interrupted by an erosion remnant, the Reynosa Plateau, which reaches a maximum altitude of nearly 1,000 feet above sea level and stands well above the areas to the east and west. The Reynosa Plateau includes most of Duval County and parts of Webb, Zapata, Starr, Jim Hogg, Jim Wells, McMullen, and Live Oak Counties. In Duval County the plateau is bounded on the west by the westward-facing Bordas escarpment, 75 to 150 feet high, which crosses the county with a southwesterly trend from about the middle of the north boundary to about the middle of the west boundary. On the east the plateau is bounded by a low seaward-facing escarpment, which passes through San Diego, trending a little west of south.
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In 1831 Dr. John Bell issued a book entitled \"Baths and Mineral Waters\" in which he listed 21 spring localities. In the edition of his work published in 1855 the number was increased to 181. The earliest report on a geologic study of thermal springs was that of W. B, Rogers in 1840 on the thermal springs of Virginia. In 1875 G. K. Gilbert published a map and table showing thermal springs in the United States and pointed out that they are present chiefly in the mountainous areas of folded and faulted rocks. Early geologic study of them was principally inspired by the information which they afford at a few places on the deposition of minerals. The relation of hot springs to volcanic action has been studied in the Yellowstone National Park and near Lassen Peak in California. Studies in recent years have been concerned with the source of the water as well as of its heat.
All the notable thermal springs in the eastern United States are in the Appalachian Highlands, principally in the region of folded rocks. The Atlantic Coastal Plain contains no appreciably warm springs. In Florida there are large springs whose water rises from a depth of a few hundred feet and is about 5° above the mean annual temperature, but they are not usually classed as thermal.
The only warm springs in the great Interior Plains region are at and near Hot Springs, S. Dak., in the vicinity of the Black Hills uplift of crystalline rocks. In the Interior Highlands thermal springs occur only in the Ozark region, the largest group being at Hot Springs, Ark.
The Rocky Mountain System includes the Yellowstone National Park, with its world-famous hot springs and geysers (see pis. 7,12), and there are many other hot springs within this great mountainous region. In the Intermontane areas of great lava plains and faulted lava mountains in Utah, Nevada, southern Idaho, and eastern Oregon there are many hot springs, closely associated with the larger faults. In the Pacific Mountain System, including the Cascade Range and Sierra Nevada, there are many warm and hot springs, some of which issue in areas of granite, and others in areas of lava. In the Coast Ranges of California many thermal springs issue from different geologic formations.
Of the total of more than 1,000 thermal-spring localities listed in this paper more than half are situated in the three States of Idaho, California, and Nevada, each of which contains more than 150 thermal-spring localities. Wyoming, including the Yellowstone National Park, contains more than 100 hot-spring localities. Oregon, Utah, Colorado, Montana, and New Mexico contain several dozen thermal springs each, of which the principal ones are developed as resorts. The other thermal springs are scattered through 12 States, of which Massachusetts, New York, Pennsylvania, and North Carolina contain one spring or group each. More than half of the total number are developed as resorts or used for irrigation or water supply, but many have remained undeveloped because they are not easily accessible.
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Part 1, Western Texas, 1896-1935","interactions":[],"lastModifiedDate":"2012-02-02T00:04:53","indexId":"b883A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1937","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"883","chapter":"A","title":"Spirit leveling in Texas. Part 1, Western Texas, 1896-1935","language":"ENGLISH","doi":"10.3133/b883A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Spirit leveling in Texas. 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The depths of rainfall mark this period as one of the greatest concentrations of precipitation, in respect to time and magnitude of the area covered, of which there is record in this country. \r\n\r\nAt the time of the rain there were also accumulations of snow on the ground over much of the storm-affected region that were large for the season. The comparatively warm temperatures associated with the storms thawed the snow and added materially to the quantities of water to be disposed of by drainage into the waterways, by surface storage in lakes, ponds, and reservoirs, by absorption in the ground, and, probably in comparatively negligible degree, by evaporation. \r\n\r\nThe total quantity of water that had to be disposed of in these ways ranged between 10 and 30 inches in depth over much of the region. The water disposed of by natural storage, absorption, and evaporation amounted to average depths over the many river basins generally within the range of 1 to 3 inches, with a significant degree of uniformity and systematic areal distribution. The remainder of the rain and snow water, generally much larger or even several times larger in amount than surface storage, absorption, and evaporation, required accommodation by the channels of the brooks, creeks, and rivers. \r\n\r\nThere were generally two distinct flood peaks, and in many of the basins the destruction was seriously aggravated, especially during the first flood, by the break-up of thick ice cover accumulated through a winter of exceptionally continuous and severe cold weather. The resulting floods were extraordinarily severe, and records of river stages, extending on some streams back to or nearly to the time of settlement by white men, were broken many of them by wide margins. The peak of the Connecticut River at Hartford, Conn., was 8.6 feet higher than had been experienced since the settlement by white men, 300 years ago. The Susquehanna River at Harrisburg, Pa., was 3.5 feet higher than had been known in a period of record covering about 200 years. The Ohio River at Pittsburgh, Pa., was 6.1 feet higher than had been known in the period beginning 1762. \r\n\r\nThis volume presents many of the facts of these notable floods with respect to the New England rivers, for permanent record and for study and reference by engineers concerned with the building of highways, bridges, and industrial plants, planners of river development, and others. Similar volumes for the region from the Hudson River to the Susquehanna River and for the Potomac, James, and upper Ohio River Basins are presented in companion Water-Supply Papers 799 and 800 respectively. In this volume records of stage and discharge for the period Including the floods are presented for about 150 measurement stations; peak discharges with comparative data for other floods at more than 400 measurement points are summarized; crest stages along an aggregate length of stream channel of 2,820 miles are tabulated; and results of detailed studies of the rainfall and run-off and many other kinds of flood information are presented.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp800","usgsCitation":"Grover, N., and Lichtblau, S., 1937, The floods of March 1936, Part 3, Potomac, James, and upper Ohio Rivers: U.S. Geological Survey Water Supply Paper 800, ix, 351 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp800.","productDescription":"ix, 351 p. :ill., maps ;24 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":26838,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0800/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0800/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65db64","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":144034,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lichtblau, Stephen","contributorId":18340,"corporation":false,"usgs":true,"family":"Lichtblau","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":144035,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1739,"text":"wsp798 - 1937 - The floods of March 1936, part 1, New England rivers","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp798","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1937","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":"798","title":"The floods of March 1936, part 1, New England rivers","docAbstract":"During the period March 9-22, 1936, there occurred in close succession over the northeastern United States, from the James and upper Ohio River Basins in Virginia and Pennsylvania to the river basins of Maine, two extraordinarily heavy storms, in which the precipitation was almost entirely in the form of rain. The depths of rainfall mark this period as one of the greatest concentrations of precipitation, in respect to time and magnitude of the area covered, of which there is record in this country. \r\n\r\nAt the time of the rain there were also accumulations of snow on the ground over much of the storm-affected region that were large for the season. The comparatively warm temperatures associated with the storms thawed the snow and added materially to the quantities of water to be disposed of by drainage into the waterways, by surface storage in lakes, ponds, and reservoirs, by absorption in the ground, and, probably in comparatively negligible degree, by evaporation. \r\n\r\nThe total quantity of water that had to be disposed of in these ways ranged between 10 and 30 inches in depth over much of the region. The water disposed of by natural storage, absorption, and evaporation amounted to average depths over the many river basins generally within the range of 1 to 3 inches, with a significant degree of uniformity and systematic areal distribution. The remainder of the rain and snow water, generally much larger or even several times larger in amount than surface storage, absorption, and evaporation, required accommodation by the channels of the brooks, creeks, and rivers. \r\n\r\nThere were generally two distinct flood peaks, and in many of the basins the destruction was seriously aggravated, especially during the first flood, by the break-up of thick ice cover accumulated through a winter of exceptionally continuous and severe cold weather. The resulting floods were extraordinarily severe, and records of river stages, extending on some streams back to or nearly to the time of settlement by white men, were broken many of them by wide margins. The peak of the Connecticut River at Hartford, Conn., was 8.6 feet higher than had been experienced since the settlement by white men, 300 years ago. The Susquehanna River at Harrisburg, Pa., was 3.5 feet higher than had been known in a period of record covering about 200 years. The Ohio River at Pittsburgh, Pa., was 6.1 feet higher than had been known in the period beginning 1762. \r\n\r\nThis volume presents many of the facts of these notable floods with respect to the New England rivers, for permanent record and for study and reference by engineers concerned with the building of highways, bridges, and industrial plants, planners of river development, and others. Similar volumes for the region from the Hudson River to the Susquehanna River and for the Potomac, James, and upper Ohio River Basins are presented in companion Water-Supply Papers 799 and 800 respectively. In this volume records of stage and discharge for the period Including the floods are presented for about 150 measurement stations; peak discharges with comparative data for other floods at more than 400 measurement points are summarized; crest stages along an aggregate length of stream channel of 2,820 miles are tabulated; and results of detailed studies of the rainfall and run-off and many other kinds of flood information are presented.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp798","usgsCitation":"Grover, N.C., 1937, The floods of March 1936, part 1, New England rivers: U.S. Geological Survey Water Supply Paper 798, x, 466 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp798.","productDescription":"x, 466 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136962,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0798/report-thumb.jpg"},{"id":26844,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0798/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65db1b","contributors":{"authors":[{"text":"Grover, Nathan Clifford","contributorId":66660,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan","email":"","middleInitial":"Clifford","affiliations":[],"preferred":false,"id":144050,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1875,"text":"wsp819 - 1937 - The warm springs of Georgia, their geologic relations and origin, a summary report","interactions":[],"lastModifiedDate":"2017-02-03T12:39:19","indexId":"wsp819","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1937","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":"819","title":"The warm springs of Georgia, their geologic relations and origin, a summary report","language":"ENGLISH","publisher":"U.S. Govt. 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(incl. fold. maps: 1 in pocket) fold. diagrs. ;23 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":27162,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0819/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27163,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0819/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0819/report-thumb.jpg"}],"country":"United States","state":"Alabama, Georgia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.71307373046874,\n 35.67068501330236\n ],\n [\n -83.71307373046874,\n 35.67068501330236\n ],\n [\n -83.7103271484375,\n 35.67068501330236\n ],\n [\n -83.7103271484375,\n 35.67068501330236\n ],\n [\n -83.71307373046874,\n 35.67068501330236\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.4072265625,\n 32.0639555946604\n ],\n [\n -87.4072265625,\n 33.48185394054361\n ],\n [\n -83.38623046875,\n 33.48185394054361\n ],\n [\n -83.38623046875,\n 32.0639555946604\n ],\n [\n -87.4072265625,\n 32.0639555946604\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62eef8","contributors":{"authors":[{"text":"Hewett, D. F.","contributorId":19927,"corporation":false,"usgs":true,"family":"Hewett","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crickmay, Geoffrey William","contributorId":105696,"corporation":false,"usgs":true,"family":"Crickmay","given":"Geoffrey","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":144291,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70195886,"text":"70195886 - 1937 - The fluoride content of North Dakota ground waters as related to the occurrence and distribution of mottled enamel","interactions":[],"lastModifiedDate":"2018-03-07T13:07:45","indexId":"70195886","displayToPublicDate":"1959-01-01T00:00:00","publicationYear":"1937","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5645,"text":"North Dakota Geological Survey Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"The fluoride content of North Dakota ground waters as related to the occurrence and distribution of mottled enamel","docAbstract":"No abstract available.
","language":"English","publisher":"North Dakota Geological Survey","usgsCitation":"Abbott, G.A., 1937, The fluoride content of North Dakota ground waters as related to the occurrence and distribution of mottled enamel: North Dakota Geological Survey Bulletin 9, 16 p.","productDescription":"16 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352280,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6f71e4b0da30c1bfe573","contributors":{"authors":[{"text":"Abbott, G. A.","contributorId":203049,"corporation":false,"usgs":false,"family":"Abbott","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":730397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70260101,"text":"70260101 - 1937 - The importance of lead poisoning in waterfowl","interactions":[],"lastModifiedDate":"2024-10-28T14:39:16.366474","indexId":"70260101","displayToPublicDate":"1937-12-01T09:29:01","publicationYear":"1937","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The importance of lead poisoning in waterfowl","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Transactions of the second North American Wildlife Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Second North American Wildlife Conference","conferenceDate":"March 1-4, 1937","conferenceLocation":"St. Louis, MO","language":"English","publisher":"American Wildlife Institute","usgsCitation":"Shillinger, J., and Cottam, C., 1937, The importance of lead poisoning in waterfowl, in Transactions of the second North American Wildlife Conference, St. Louis, MO, March 1-4, 1937, p. 398-403.","productDescription":"6 p.","startPage":"398","endPage":"403","costCenters":[],"links":[{"id":463247,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Shillinger, J.E.","contributorId":47879,"corporation":false,"usgs":true,"family":"Shillinger","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":916995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cottam, Clarence","contributorId":41490,"corporation":false,"usgs":true,"family":"Cottam","given":"Clarence","email":"","affiliations":[],"preferred":false,"id":916996,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70212784,"text":"70212784 - 1937 - Resistivity‐studies of some salt‐water boundaries in the Hawaiian Islands","interactions":[],"lastModifiedDate":"2020-08-27T19:28:29.255956","indexId":"70212784","displayToPublicDate":"1937-08-27T14:15:45","publicationYear":"1937","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Resistivity‐studies of some salt‐water boundaries in the Hawaiian Islands","docAbstract":"In the course of a systematic survey of the ground‐water resources of the Hawaiian Islands which is being made under the direction of H. T. Stearns of the United States Geological Survey in cooperation with the Territorial Government of Hawaii, it was found desirable to test the utility of geophysical methods in the solution of certain Hawaiian water‐supply problems. A cooperative geophysical survey for this purpose was undertaken by the Geophysical Section, then with the Bureau of Mines but later transferred to the Geological Survey, during the course of which a series of resistivity‐studies of certain salt‐water boundaries was begun. Since the location of such boundaries is of considerable importance in many areas it has been thought worth while to present the results which have thus far been obtained.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00387","usgsCitation":"Swartz, J., 1937, Resistivity‐studies of some salt‐water boundaries in the Hawaiian Islands: Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 387-393, https://doi.org/10.1029/TR018i002p00387.","productDescription":"7 p.","startPage":"387","endPage":"393","costCenters":[],"links":[{"id":377960,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Swartz, J.H.","contributorId":101721,"corporation":false,"usgs":true,"family":"Swartz","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":797459,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212782,"text":"70212782 - 1937 - The use of resistivity‐methods in the location of salt‐water bodies in the El Paso, Texas, Area","interactions":[],"lastModifiedDate":"2021-10-22T19:39:20.628529","indexId":"70212782","displayToPublicDate":"1937-08-27T13:57:10","publicationYear":"1937","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The use of resistivity‐methods in the location of salt‐water bodies in the El Paso, Texas, Area","docAbstract":"During 1935 and 1936 the Ground‐Water Division of the United States Geological Survey made an investigation of the ground‐water resources of the El Paso, Texas, Area. Geological and hydrological studies comprised the principal part of the investigation, and these studies were supplemented by measurements of earth‐resistivity made largely by the Geophysical Section of the Geological Survey along traverses aggregating 51 miles. The extent to which resistivity‐methods may be useful in ground‐water work has been the subject of much discussion. A full evaluation of the method can not be made at this time. However, the work in the El Paso Area indicates that the presence of faults and of underground bodies of salt water may be definitely determined by resistivity‐measurements.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00393","usgsCitation":"Sayre, A., and Stephenson, E., 1937, The use of resistivity‐methods in the location of salt‐water bodies in the El Paso, Texas, Area: Eos, Transactions, American Geophysical Union, no. 18, p. 393-398, https://doi.org/10.1029/TR018i002p00393.","productDescription":"6 p.","startPage":"393","endPage":"398","costCenters":[],"links":[{"id":377956,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"El Paso","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.41048431396484,\n 31.74977366876081\n ],\n [\n -106.32362365722656,\n 31.74977366876081\n ],\n [\n -106.32362365722656,\n 31.803476141595862\n ],\n [\n -106.41048431396484,\n 31.803476141595862\n ],\n [\n -106.41048431396484,\n 31.74977366876081\n ]\n ]\n ]\n }\n }\n ]\n}","issue":"18","edition":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Sayre, A.N.","contributorId":84339,"corporation":false,"usgs":true,"family":"Sayre","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":825605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephenson, E.L.","contributorId":98382,"corporation":false,"usgs":true,"family":"Stephenson","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":797458,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70212780,"text":"70212780 - 1937 - Ground‐water in Utah","interactions":[],"lastModifiedDate":"2020-08-27T18:28:31.097458","indexId":"70212780","displayToPublicDate":"1937-08-27T13:18:40","publicationYear":"1937","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Ground‐water in Utah","docAbstract":"In common with many of the arid and semiarid States, the prosperity of Utah probably is more dependent upon the amount of water available than upon any other natural resource. Although only about four per cent of the State is irrigated, a shortage of water for irrigation becomes a major calamity. A large part of the water‐supply for the State is derived from surface‐streams, but a most valuable supplement to this supply is the water available from underground sources. Ground‐water is used extensively for domestic, stock‐watering, and industrial purposes as well as for irrigation. The primary source of the municipal water‐supply for Salt Lake City is from streams entering the Jordan River Valley from the western slope of the Wasatch Mountains. However, since the drought‐year of 1931, a supplementary municipal supply has been obtained from ground‐water, and, among the 17 wells developed by the City during the extreme drought of 1934, one—yielding about ten cubic feet per second, or 4500 gallons a minute—is probably the largest in the State. Ogden, the second largest city in Utah, with a population of about 40,000, obtains the major part of its municipal water‐supply from a group of artesian wells in Ogden Valley about 12 miles east of the City. A considerable part of the water‐supply for the City of Brigham is obtained from wells. Springs constitute the source of most of the water‐supply for Logan, Provo, and many smaller towns and localities in the State. In nearly every developed area of the State ground‐water is used for some purpose, and in some areas the water‐supply is obtained almost entirely from wells.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00536","usgsCitation":"Taylor, G.H., 1937, Ground‐water in Utah: Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 536-541, https://doi.org/10.1029/TR018i002p00536.","productDescription":"6 p.","startPage":"536","endPage":"541","costCenters":[],"links":[{"id":377954,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Ground Water Provinces","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.84033203125,\n 38.272688535980976\n ],\n [\n -113.51074218749999,\n 37.3002752813443\n ],\n [\n -112.3681640625,\n 37.64903402157866\n ],\n [\n -111.29150390625,\n 39.977120098439634\n ],\n [\n -109.423828125,\n 40.12849105685408\n ],\n [\n -110.74218749999999,\n 40.64730356252251\n ],\n [\n -111.4453125,\n 40.863679665481676\n ],\n [\n -111.15966796875,\n 41.95131994679697\n ],\n [\n -113.99414062499999,\n 41.78769700539063\n ],\n [\n -113.84033203125,\n 40.730608477796636\n ],\n [\n -112.8076171875,\n 40.16208338164617\n ],\n [\n -113.13720703125,\n 39.13006024213511\n ],\n [\n -113.84033203125,\n 38.272688535980976\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"18","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Taylor, George H.","contributorId":24386,"corporation":false,"usgs":true,"family":"Taylor","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":797455,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212777,"text":"70212777 - 1937 - Extraordinary topaz‐replacement body in the Brewer Mine, South Carolina","interactions":[],"lastModifiedDate":"2020-08-28T12:46:30.919473","indexId":"70212777","displayToPublicDate":"1937-08-27T13:00:29","publicationYear":"1937","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Extraordinary topaz‐replacement body in the Brewer Mine, South Carolina","docAbstract":"A large body of massive topaz forms a part of the gold‐bearing lode at the Brewer Mine, South Carolina. This gold‐mine was opened 100 years ago and merits the distinction of being one of the early gold‐discoveries of the Southern Appalachian Region. The Brewer Mine is located near Jefferson, in Chesterfield County, near the northern boundary of South Carolina, and on the eastern edge of the Piedmont Province.
The country rock is described by J. T. Pardee and C. F. Park, Jr., (Gold‐deposits of the Southern Appalachians, U. S. Geol. Surv. Prof. Paper, in preparation) as a quartz‐sericite schist that locally preserves the structure of a fine‐grained, waterlaid tuff, probably a rhyolite,from which it was derived. Exposures of granite that intrude the schist appear on the north and west at distances of a mile to a mile and a half.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i001p00243","usgsCitation":"Glass, J.J., 1937, Extraordinary topaz‐replacement body in the Brewer Mine, South Carolina: Eos, Transactions, American Geophysical Union, v. 18, no. 1, p. 243-246, https://doi.org/10.1029/TR018i001p00243.","productDescription":"4 p.","startPage":"243","endPage":"246","costCenters":[],"links":[{"id":377976,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Jefferson","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.42953491210938,\n 34.616256875628956\n ],\n [\n -80.34576416015625,\n 34.616256875628956\n ],\n [\n -80.34576416015625,\n 34.6704879985043\n ],\n [\n -80.42953491210938,\n 34.6704879985043\n ],\n [\n -80.42953491210938,\n 34.616256875628956\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"18","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Glass, Jewell J.","contributorId":106948,"corporation":false,"usgs":true,"family":"Glass","given":"Jewell","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":797453,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212775,"text":"70212775 - 1937 - Appendix A—A selected list of papers relating to ground‐water hydrology","interactions":[],"lastModifiedDate":"2020-08-27T17:31:16.707426","indexId":"70212775","displayToPublicDate":"1937-08-27T12:24:01","publicationYear":"1937","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Appendix A—A selected list of papers relating to ground‐water hydrology","docAbstract":"In the following list, brief‐statements have been added to certain references to call attention to special phases of ground‐water problems which are not apparent from the titles. Abstracts of most of the papers have been or will be published in the Annotated Bibliography of Economic Geology.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00325","usgsCitation":"Sayre, A.N., 1937, Appendix A—A selected list of papers relating to ground‐water hydrology: Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 325-328, https://doi.org/10.1029/TR018i002p00325.","productDescription":"4 p.","startPage":"325","endPage":"328","costCenters":[],"links":[{"id":377946,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Sayre, Albert Nelson","contributorId":83102,"corporation":false,"usgs":true,"family":"Sayre","given":"Albert","email":"","middleInitial":"Nelson","affiliations":[],"preferred":false,"id":797449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212774,"text":"70212774 - 1937 - Amount of ground‐water recharge in the southern High Plains","interactions":[],"lastModifiedDate":"2020-08-27T17:11:47.399447","indexId":"70212774","displayToPublicDate":"1937-08-27T12:02:29","publicationYear":"1937","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Amount of ground‐water recharge in the southern High Plains","docAbstract":"For the last six years the United States Geological Survey, in cooperation with the State Engineer of New Mexico, has been making somewhat intensive studies of ground‐water in the part of the High Plains that lies in New Mexico, and in 1933 and 1934 the Geological Survey, with funas allocated by the Public Works Administration, made an extensive reconnaissance‐survey of the ground‐water conditions in the southern High Plains. These studies have resulted in considerable data that throw much light on the quantity of recharge to the ground‐water in this area. An estimate of the quantity of recharge is of immediate value for this area, because the use of ground‐water is constantly being increased. In addition, it has a general value in serving as a criterion for estimating recharge in other areas in the Southwest for which fewer data are available. Estimates of the recharge in the High Plains as previously made without the advantage of quantitative data have ranged from less than three or four inches a year [see 1 of “References” at end of paper] to less than six inches [2]. The work of the last few years indicates they should be greatly reduced.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00564","usgsCitation":"Theis, C.V., 1937, Amount of ground‐water recharge in the southern High Plains: Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 564-568, https://doi.org/10.1029/TR018i002p00564.","productDescription":"5 p.","startPage":"564","endPage":"568","costCenters":[],"links":[{"id":377945,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas, Oklahoma, Texas","otherGeospatial":"Southern High Plains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.623046875,\n 30.826780904779774\n ],\n [\n -97.119140625,\n 30.826780904779774\n ],\n [\n -97.119140625,\n 39.90973623453719\n ],\n [\n -103.623046875,\n 39.90973623453719\n ],\n [\n -103.623046875,\n 30.826780904779774\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"18","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Theis, Charles V.","contributorId":48080,"corporation":false,"usgs":true,"family":"Theis","given":"Charles","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":797448,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}