The earliest extensive studies of thermal springs in the United States were made by physicians. 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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Off.,","doi":"10.3133/wsp782","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Surface water supply of the United States, 1935, Part II, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 782, 233 p. ;23 cm., https://doi.org/10.3133/wsp782.","productDescription":"233 p. ;23 cm.","costCenters":[],"links":[{"id":135991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0782/report-thumb.jpg"},{"id":25056,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0782/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6976f9","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":527465,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2100,"text":"wsp796D - 1937 - Geology and ground-water resources of Ogden Valley, Utah","interactions":[],"lastModifiedDate":"2017-09-07T15:18:03","indexId":"wsp796D","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":"796","chapter":"D","title":"Geology and ground-water resources of Ogden Valley, Utah","docAbstract":"Ogden Valley is a fault trough bounded on both the east and west by faults that dip toward the middle of the valley. This fault trough contains unconsolidated deposits of clay, sand, and gravel, whose thickness is more than 600 feet. These materials are stream and lake deposits and in places are well sorted and stratified. The lake sediments were laid down in a small lake that occupied Ogden Valley and that was connected with glacial Lake Bonneville at its high stage by an arm of water that occupied Ogden Canyon. During this stage of Lake Bonneville the Ogden Valley was completely filled with lake sediments up to an altitude of about 4,900 feet. These sediments include about 70 feet of clay, sand, and gravel in alternating layers, below which is a bed of varved clay whose maximum thickness is about 70 feet. This clay is continuous under the lower parts of the valley and is the confining bed that produces the artesian conditions. Below the varved clay is a deposit of silt, sand, and gravel of unknown thickness, most of which is believed to be pre-Bonneville alluvium.
In most summers the streams entering Ogden Valley are diverted for irrigation, and the upper parts of their channels are generally dry during the irrigation season. Lower down in the valley seepage water appears in the channels, and below these points there is continuous flow. The flow of the Ogden River increases as it passes through Ogden Canyon. This gain in flow is believed to be derived chiefly from ground-water seepage from the canyon walls, although there is probably some groundwater underflow from Ogden Valley at the head of Ogden Canyon. Some of the gain is also due to leakage from pipe lines in the canyon.
Of the 146 wells whose records are given in this report, 70 are flowing wells.
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The Eska Creek coal deposits, Matanuska Valley","interactions":[{"subject":{"id":45304,"text":"b880D - 1937 - Mineral resources of Alaska, report on progress of investigations in 1935. The Eska Creek coal deposits, Matanuska Valley","indexId":"b880D","publicationYear":"1937","noYear":false,"chapter":"D","title":"Mineral resources of Alaska, report on progress of investigations in 1935. 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The Eska Creek coal deposits, Matanuska Valley: U.S. Geological Survey Bulletin 880, 185-214 p., https://doi.org/10.3133/b880D.","productDescription":"185-214 p.","costCenters":[],"links":[{"id":135155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0880d/report-thumb.jpg"},{"id":93968,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0880d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b5cb","contributors":{"authors":[{"text":"Tuck, Ralph","contributorId":107244,"corporation":false,"usgs":true,"family":"Tuck","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":231401,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":45305,"text":"b883A - 1937 - Spirit leveling in Texas. 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Part 1, Western Texas, 1896-1935: U.S. Geological Survey Bulletin 883, 1-50 p., https://doi.org/10.3133/b883A.","productDescription":"1-50 p.","costCenters":[],"links":[{"id":93969,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0883a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0883a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a47","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":531580,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35905,"text":"b881 - 1937 - Spirit leveling in Connecticut, 1922-35","interactions":[],"lastModifiedDate":"2012-02-02T00:09:44","indexId":"b881","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":"881","title":"Spirit leveling in Connecticut, 1922-35","language":"ENGLISH","publisher":"U.S. Govt. print. off.,","doi":"10.3133/b881","usgsCitation":"Staack, J.G., 1937, Spirit leveling in Connecticut, 1922-35: U.S. Geological Survey Bulletin 881, 65 p., 1 l. :incl. map, tables, pl. ;23 cm., https://doi.org/10.3133/b881.","productDescription":"65 p., 1 l. :incl. map, tables, pl. ;23 cm.","costCenters":[],"links":[{"id":93649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0881/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166378,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0881/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4b07","contributors":{"authors":[{"text":"Staack, John George","contributorId":95034,"corporation":false,"usgs":true,"family":"Staack","given":"John","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":215421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":490,"text":"wsp792 - 1937 - Surface water supply of the United States, 1935 : Part 12, North Pacific drainage basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp792","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":"792","title":"Surface water supply of the United States, 1935 : Part 12, North Pacific drainage basins","language":"ENGLISH","publisher":"U.S. Govt. 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Some of the earliest oil fields to brought into production were situated in and near this county, and new fields have been opened from time to time during the ensuing years. The production of the newer fields, however, has not kept pace with the exhaustion of the older fields, and the county now presents an excellent picture of the problems involved in adjusting a population to lands that are nearly depleted of their mineral wealth. Values of land have been greatly depressed; tax collection is far in arrears; tenancy is widespread; and in addition more people will apparently be forced to depend on the income from agriculture than the land seems capable of supporting. The county as a whole is at best indifferently suitable for general farming. The Land Use planning Section proposes to study the present and seemingly immanent maladjustments of population to the resources of the land, and make recommendations for their correction.\r\nThe writer was detailed to the Land Use Planning Section of Region VIII for the purposes of making studies of ground water problems in the region. In Creek County two investigations were made. In September, 1936, the writer spent about ten days investigating the availability of ground water for the irrigation of garden crops during drouths. If it proved feasible to do this generally throughout the county, the Land Use Planning Section might be able to encourage this practice. The second investigation made by the writer was in regard to the extent to which ground water supplies have been damaged by oil well brines. He was in county for four days late in January 1937, and again in March, 1937. During part of the second field trip he was accompanied by R.M. 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