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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A.","contributorId":100365,"corporation":false,"usgs":true,"family":"Waring","given":"Gerald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146342,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4609,"text":"wsp783 - 1937 - Surface water supply of the United States, 1935, Part III, Ohio River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"wsp783","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":"783","title":"Surface water supply of the United States, 1935, Part III, Ohio River basin","language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/wsp783","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Surface water supply of the United States, 1935, Part III, Ohio River basin: U.S. Geological Survey Water Supply Paper 783, 400 p. ;23 cm., https://doi.org/10.3133/wsp783.","productDescription":"400 p. ;23 cm.","costCenters":[],"links":[{"id":139301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0783/report-thumb.jpg"},{"id":31666,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0783/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697662","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":528303,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1731,"text":"wsp799 - 1937 - The floods of March 1936, part 2, Hudson River to Susquehanna River region","interactions":[],"lastModifiedDate":"2017-07-05T10:13:12","indexId":"wsp799","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":"799","title":"The floods of March 1936, part 2, Hudson River to Susquehanna River region","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. Government Printing Office","doi":"10.3133/wsp799","usgsCitation":"Grover, N., 1937, The floods of March 1936, part 2, Hudson River to Susquehanna River region: U.S. Geological Survey Water Supply Paper 799, x, 380 p. :ill. ;23 cm., https://doi.org/10.3133/wsp799.","productDescription":"x, 380 p. :ill. ;23 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":136978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0799/report-thumb.jpg"},{"id":26837,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0799/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69756a","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":144033,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":499,"text":"wsp811 - 1937 - Surface water supply of the United States, 1936 : Part 11. 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(some folded), charts, map ;24 cm.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":138840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0796c/report-thumb.jpg"},{"id":29400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0796c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef0d3","contributors":{"authors":[{"text":"Troxell, H.C.","contributorId":69124,"corporation":false,"usgs":true,"family":"Troxell","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":145873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, John Q.","contributorId":76292,"corporation":false,"usgs":true,"family":"Peterson","given":"John Q.","affiliations":[],"preferred":false,"id":145874,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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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Print. Off.,","doi":"10.3133/wsp795","usgsCitation":"Grover, N., and Carson, M.H., 1937, Surface water supply of Hawaii : July 1, 1934 to June 30, 1935: U.S. Geological Survey Water Supply Paper 795, 138 p. ;23 cm., https://doi.org/10.3133/wsp795.","productDescription":"138 p. ;23 cm.","costCenters":[],"links":[{"id":136061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0795/report-thumb.jpg"},{"id":24868,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0795/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698299","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":142217,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carson, Max H.","contributorId":21132,"corporation":false,"usgs":true,"family":"Carson","given":"Max","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":142218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":45305,"text":"b883A - 1937 - Spirit leveling in Texas. 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. 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":2147,"text":"wsp778 - 1937 - Geology and ground-water resources of Webb County, Texas","interactions":[],"lastModifiedDate":"2016-08-22T10:17:50","indexId":"wsp778","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":"778","title":"Geology and ground-water resources of Webb County, Texas","docAbstract":"Webb County is in southwestern Texas and is a part of the Winter Garden district. The purpose of the investigation here recorded was to determine the source, quantity, and quality of the ground water used for irrigation and other purposes in the area.
","language":"English","publisher":"U. S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp778","usgsCitation":"Lonsdale, J.T., and Day, J.R., 1937, Geology and ground-water resources of Webb County, Texas: U.S. Geological Survey Water Supply Paper 778, Report: v, 104 p.; Plate: 46.35 x 35.00 inches, https://doi.org/10.3133/wsp778.","productDescription":"Report: v, 104 p.; Plate: 46.35 x 35.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0778/report-thumb.jpg"},{"id":27756,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0778/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27757,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0778/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109958,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24643.htm","linkFileType":{"id":5,"text":"html"},"description":"24643"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685816","contributors":{"authors":[{"text":"Lonsdale, John T.","contributorId":30210,"corporation":false,"usgs":true,"family":"Lonsdale","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":144738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day, James R.","contributorId":81474,"corporation":false,"usgs":true,"family":"Day","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":144739,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp796D","collaboration":"Prepared in cooperation with the City of Ogden","usgsCitation":"Leggette, R., and Taylor, G., 1937, Geology and ground-water resources of Ogden Valley, Utah: U.S. Geological Survey Water Supply Paper 796, iv, p. 63 p.; 6 Plates: 23.50 x 18.50 inches or smaller, https://doi.org/10.3133/wsp796D.","productDescription":"iv, p. 63 p.; 6 Plates: 23.50 x 18.50 inches or smaller","startPage":"99","endPage":"161","numberOfPages":"67","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":247109,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-39.pdf","text":"Plate 39","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Stream flow in Ogden valley, 1933-34"},{"id":247108,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-38.pdf","text":"Plate 38","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrographs of observation wells in Ogden valley and the flow of south fork of Ogden River"},{"id":247110,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-40.pdf","text":"Plate 40","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Well logs, Ogden Valley, Utah"},{"id":138192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0796d/report-thumb.jpg"},{"id":27674,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0796d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247105,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-35.pdf","text":"Plate 35","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Annual cumulative departure from normal precipitation at Ogden, Utah, and annual precipitation at Ogden and Huntsville, Utah"},{"id":247106,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-36.pdf","text":"Plate 36","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of a part of Ogden Valley, Weber County, Utah"},{"id":247107,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-37.pdf","text":"Plate 37","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Graphs of the flow of south fork of Ogden river, the precipitation at Ogden, the withdrawal of ground water at Artesian park, and the water levels in five observation wells in Ogden valley, 1932-35"}],"country":"United States","state":"Utah","county":"Weber County","otherGeospatial":"Ogden Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859d7","contributors":{"authors":[{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":144675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, G.H.","contributorId":85158,"corporation":false,"usgs":true,"family":"Taylor","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":144674,"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}]}} ]}