{"pageNumber":"7240","pageRowStart":"180975","pageSize":"25","recordCount":185258,"records":[{"id":1732,"text":"wsp800 - 1937 - The floods of March 1936, Part 3, Potomac, James, and upper Ohio Rivers","interactions":[],"lastModifiedDate":"2017-07-05T10:12:20","indexId":"wsp800","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":"800","title":"The floods of March 1936, Part 3, Potomac, James, and upper Ohio 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. 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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}]}}
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,{"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. Print. Off.,","doi":"10.3133/wsp819","usgsCitation":"Hewett, D.F., and Crickmay, G.W., 1937, The warm springs of Georgia, their geologic relations and origin, a summary report: U.S. Geological Survey Water Supply Paper 819, iv, 40 p. :illus., 8 pl. (incl. fold. maps: 1 in pocket) fold. diagrs. ;23 cm., https://doi.org/10.3133/wsp819.","productDescription":"iv, 40 p. :illus., 8 pl. (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":493,"text":"wsp782 - 1937 - Surface water supply of the United States, 1935, Part II, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp782","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":"782","title":"Surface water supply of the United States, 1935, Part II, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. 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":492,"text":"wsp781 - 1937 - Surface water supply of the United States, 1935, Part I, North Atlantic slope basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp781","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":"781","title":"Surface water supply of the United States, 1935, Part I, North Atlantic slope basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp781","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Surface water supply of the United States, 1935, Part I, North Atlantic slope basins: U.S. Geological Survey Water Supply Paper 781, 421 p. ;23 cm., https://doi.org/10.3133/wsp781.","productDescription":"421 p. ;23 cm.","costCenters":[],"links":[{"id":135990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0781/report-thumb.jpg"},{"id":25055,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0781/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6976d5","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":527464,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3153,"text":"wsp679B - 1937 - Thermal springs in the United States","interactions":[],"lastModifiedDate":"2024-02-01T22:18:55.044119","indexId":"wsp679B","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":"679","chapter":"B","title":"Thermal springs in the United States","docAbstract":"<p>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.</p><p>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.</p><p>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.</p><p>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.</p><p>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. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp679B","usgsCitation":"Stearns, N., Stearns, H.T., and Waring, G.A., 1937, Thermal springs in the United States: U.S. Geological Survey Water Supply Paper 679, Report: iv, 147 p.; 1 Plate: 29.00 x 20.00 inches, https://doi.org/10.3133/wsp679B.","productDescription":"Report: iv, 147 p.; 1 Plate: 29.00 x 20.00 inches","startPage":"59","endPage":"206","numberOfPages":"175","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science 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