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,{"id":2032,"text":"wsp836A - 1938 - Stages and flood discharges of the Connecticut River at Hartford, Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp836A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1938","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":"836","chapter":"A","title":"Stages and flood discharges of the Connecticut River at Hartford, Connecticut","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp836A","usgsCitation":"Kinnison, H., Conover, L., and Bigwood, B.L., 1938, Stages and flood discharges of the Connecticut River at Hartford, Connecticut: U.S. Geological Survey Water Supply Paper 836, 1-18 p. :ill. ;24 cm., https://doi.org/10.3133/wsp836A.","productDescription":"1-18 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0836a/report-thumb.jpg"},{"id":27511,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0836a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4886","contributors":{"authors":[{"text":"Kinnison, Harvey B.","contributorId":52948,"corporation":false,"usgs":true,"family":"Kinnison","given":"Harvey B.","affiliations":[],"preferred":false,"id":144556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conover, L.F.","contributorId":92649,"corporation":false,"usgs":true,"family":"Conover","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":144557,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bigwood, B. L.","contributorId":100823,"corporation":false,"usgs":true,"family":"Bigwood","given":"B.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144558,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":510,"text":"wsp822 - 1938 - Surface water supply of the United States, 1937, Part II, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1938","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":"822","title":"Surface water supply of the United States, 1937, Part II, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp822","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1938, Surface water supply of the United States, 1937, Part II, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 822, vi, 266 p. ;23 cm., https://doi.org/10.3133/wsp822.","productDescription":"vi, 266 p. ;23 cm.","costCenters":[],"links":[{"id":136113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0822/report-thumb.jpg"},{"id":25073,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0822/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6975b5","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":527482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2746,"text":"wsp774 - 1938 - Geology and ground-water resources of the Snake River Plain in southeastern Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp774","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1938","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":"774","title":"Geology and ground-water resources of the Snake River Plain in southeastern Idaho","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp774","usgsCitation":"Stearns, H.T., Crandall, L., and Steward, W.G., 1938, Geology and ground-water resources of the Snake River Plain in southeastern Idaho: U.S. Geological Survey Water Supply Paper 774, ix, 268 p. incl. illus., tables. :31 pl. (part fold., incl. maps, diagrs.) ;23 cm., https://doi.org/10.3133/wsp774.","productDescription":"ix, 268 p. incl. illus., tables. :31 pl. (part fold., incl. maps, diagrs.) ;23 cm.","costCenters":[],"links":[{"id":139052,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0774/report-thumb.jpg"},{"id":247241,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0774/plate-04.pdf","size":"9442","linkFileType":{"id":1,"text":"pdf"}},{"id":247242,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0774/plate-05.pdf","size":"4181","linkFileType":{"id":1,"text":"pdf"}},{"id":247243,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0774/plate-06.pdf","size":"3980","linkFileType":{"id":1,"text":"pdf"}},{"id":247244,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0774/plate-13.pdf","size":"3891","linkFileType":{"id":1,"text":"pdf"}},{"id":247245,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0774/plate-18.pdf","size":"7171","linkFileType":{"id":1,"text":"pdf"}},{"id":247246,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0774/plate-19.pdf","size":"14264","linkFileType":{"id":1,"text":"pdf"}},{"id":29172,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0774/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685336","contributors":{"authors":[{"text":"Stearns, Harold T.","contributorId":65831,"corporation":false,"usgs":true,"family":"Stearns","given":"Harold","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":145703,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crandall, Lynn","contributorId":7690,"corporation":false,"usgs":true,"family":"Crandall","given":"Lynn","email":"","affiliations":[],"preferred":false,"id":145702,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Steward, Willard G.","contributorId":99126,"corporation":false,"usgs":true,"family":"Steward","given":"Willard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145704,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":508,"text":"wsp834 - 1938 - Surface water supply of the United States, 1937 : Part 14, Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp834","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1938","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":"834","title":"Surface water supply of the United States, 1937 : Part 14, Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp834","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1938, Surface water supply of the United States, 1937 : Part 14, Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 834, v, 188 p. ;23 cm., https://doi.org/10.3133/wsp834.","productDescription":"v, 188 p. ;23 cm.","costCenters":[],"links":[{"id":136111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0834/report-thumb.jpg"},{"id":25071,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0834/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6975cb","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":527480,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2036,"text":"wsp796F - 1938 - Geology and ground-water resources of the Valley of Gila River and San Simon Creek, Graham County, Arizona","interactions":[],"lastModifiedDate":"2022-02-02T19:23:07.109187","indexId":"wsp796F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1938","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":"F","title":"Geology and ground-water resources of the Valley of Gila River and San Simon Creek, Graham County, Arizona","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1937","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp796F","usgsCitation":"Knechtel, M., and Lohr, E.W., 1938, Geology and ground-water resources of the Valley of Gila River and San Simon Creek, Graham County, Arizona: U.S. Geological Survey Water Supply Paper 796, Report: iv, 42 p.; 1 Plate: 32.50 × 35.00 inches, https://doi.org/10.3133/wsp796F.","productDescription":"Report: iv, 42 p.; 1 Plate: 32.50 × 35.00 inches","costCenters":[],"links":[{"id":395292,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24651.htm"},{"id":27527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0796f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27526,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0796f/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Graham County","otherGeospatial":"Gila River, San Simon Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.174,\n              32.405\n            ],\n            [\n              -109.417,\n              32.405\n            ],\n            [\n              -109.417,\n              33.143\n            ],\n            [\n              -110.174,\n              33.143\n            ],\n            [\n              -110.174,\n              32.405\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6853d0","contributors":{"authors":[{"text":"Knechtel, Maxwell M.","contributorId":47765,"corporation":false,"usgs":true,"family":"Knechtel","given":"Maxwell M.","affiliations":[],"preferred":false,"id":144565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lohr, E. W.","contributorId":48155,"corporation":false,"usgs":true,"family":"Lohr","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144566,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1740,"text":"wsp838 - 1938 - Floods of Ohio and Mississippi Rivers, January-February 1937, with a section on the Flood deposits of the Ohio River, January-February 1937","interactions":[],"lastModifiedDate":"2016-05-24T11:12:48","indexId":"wsp838","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1938","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":"838","title":"Floods of Ohio and Mississippi Rivers, January-February 1937, with a section on the Flood deposits of the Ohio River, January-February 1937","docAbstract":"<p>In January and February 1937 the Ohio and mid-Mississippi Rivers experienced floods which, over reaches many hundreds of miles in length, exceeded all previously recorded stages. When measured by the loss of life and property, extent of damage, and general disruption of human activities, these floods constituted a major catastrophe.</p>\n<p>The floods were caused by a succession of heavy rainstorms that began late in December 1936 and continued nearly to the end of the following January. Although the storms covered a considerable part of the lower Mississippi River Basin and almost the entire Ohio River Basin, the center of heaviest precipitation was in the middle and lower portions of the Ohio River Valley.</p>\n<p>The total storm period can be subdivided into several individual storms, which were more or less clearly demarked by short intervening periods of little or no precipitation. Although the individual storm periods were the same or nearly the same over wide areas, their subdivisions were somewhat different in the most widely separated parts of the affected areas, with intermediate gradations in the intervening areas. The heaviest rainfall--that of January 20 to 25--was centered in the lower Ohio Valley, and, falling as it did upon a region with soil saturated and waterways already running full, it had the effect of producing extreme floods.</p>\n<p>The small quantity of snow on the ground over the higher eastern parts of the area at the beginning of the storm period disappeared in a short time. Some of the precipitation occurred in the form of snow, but this snow and the associated cold weather were much less significant in their influence on the floods than in the misery and discomfort they caused to ill-sheltered flood refugees and flood-bound people.</p>\n<p>Sequence and time of the storms were such that in the upper and smaller tributary basins the associated flood rises tended to clear to a notable degree before the-next flood rises came; hence many of these tributaries were at no time in extreme flood. In the lower reaches of the largest tributaries, and especially on the middle and lower reaches of the Ohio River, there were extreme and almost continuously increasing accumulations of run-off, which culminated in the region of Louisville, Ky., in stages 10 or 11 feet higher than any previously known.</p>\n<p>The precipitation was heaviest in the Ohio River Basin, and the flood in the Mississippi River, like other notable floods of the past, was caused largely by the extraordinary contributions from the Ohio River. The river stages exceeded those previously recorded for the lower 700 miles on the Ohio River and for 250 miles .on the Mississippi River below the Ohio. At Cairo, Ill., at the mouth Of the Ohio River, the river stage was higher for a period of 19 days, from January 24 to February 11, than at any previous time on record. The height above previous flood stages diminished materially as the flood progressed down the Mississippi.</p>\n<p>The mean precipitation ever the Ohio River Basin during the storm period was. 12.85 inches. The snow on the ground at the beginning of the period is estimated to have been equivalent to a mean depth of 0.10 inch of water over the basin. Out of the total precipitation 8.9 inches appeared as flood flow. On January 26 the computed volume of water in the stream channels of the Ohio River Basin was 56,000,000 acre-feet, equivalent to a depth of 5.1 inches over the drainage basin. The maximum discharge of the Ohio River at its mouth was 1,880,000 second-feet on February 1. On February 2, the day of the crest stage at the mouth of the Ohio, the computed volume of water on the surface channel system was equivalent to a depth of 3.7 inches over the drainage basin, of which 2.4 inches was in the 337-mile reach of the Ohio River between Louisville, Ky., and the mouth.</p>\n<p>This water-supply paper presents records of stage and discharge for the period including the floods at about 250 measurement stations, records of stage and discharge for&nbsp;the period including the floods at about 250 measurement stations, records&nbsp;of storage in many reservoirs, a summary of peak discharges with comparative&nbsp;data for other floods at about 470 measurement points, and tables<br />showing crest stages along an aggregate length of stream channel for 5,000&nbsp;miles. The report also includes basic information in regard to the<br />weather associated with the floods, results of detailed studies of the&nbsp;rainfall and run-off, analyses of the volume of flood waters'in the surface<br />channel systems during the progress of the floods, and many other&nbsp;kinds of flood information.</p>\n<p>Following the main flood report is a brief report entitled \"Flood\"&nbsp;deposits of the Ohio River, January-February 1937, a study of sedimentation.\"<br />An abstract of that report is presented on page 693.</p>","language":"English","publisher":"U. S. 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,{"id":45272,"text":"b898B - 1938 - Spirit leveling in Missouri, 1896-1938. Part 2, South-central Missouri, 1896-1937","interactions":[{"subject":{"id":45272,"text":"b898B - 1938 - Spirit leveling in Missouri, 1896-1938. Part 2, South-central Missouri, 1896-1937","indexId":"b898B","publicationYear":"1938","noYear":false,"chapter":"B","title":"Spirit leveling in Missouri, 1896-1938. Part 2, South-central Missouri, 1896-1937"},"predicate":"IS_PART_OF","object":{"id":35949,"text":"b898 - 1940 - Spirit leveling in Missouri, 1896-1938","indexId":"b898","publicationYear":"1940","noYear":false,"title":"Spirit leveling in Missouri, 1896-1938"},"id":1}],"isPartOf":{"id":35949,"text":"b898 - 1940 - Spirit leveling in Missouri, 1896-1938","indexId":"b898","publicationYear":"1940","noYear":false,"title":"Spirit leveling in Missouri, 1896-1938"},"lastModifiedDate":"2017-08-08T08:36:07","indexId":"b898B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1938","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":"898","chapter":"B","title":"Spirit leveling in Missouri, 1896-1938. Part 2, South-central Missouri, 1896-1937","language":"ENGLISH","doi":"10.3133/b898B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1938, Spirit leveling in Missouri, 1896-1938. Part 2, South-central Missouri, 1896-1937: U.S. Geological Survey Bulletin 898, 133-308 p., https://doi.org/10.3133/b898B.","productDescription":"133-308 p.","costCenters":[],"links":[{"id":93903,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0898b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":134777,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0898b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a89","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":531573,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53030,"text":"ofr381 - 1938 - Water utilization in the basin of the Chewaucan River, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:11:26","indexId":"ofr381","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1938","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"38-1","title":"Water utilization in the basin of the Chewaucan River, Oregon","language":"ENGLISH","doi":"10.3133/ofr381","usgsCitation":"Helland, R., 1938, Water utilization in the basin of the Chewaucan River, Oregon: U.S. Geological Survey Open-File Report 38-1, 51 p.; 4 maps, https://doi.org/10.3133/ofr381.","productDescription":"51 p.; 4 maps","costCenters":[],"links":[{"id":178657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eeeff","contributors":{"authors":[{"text":"Helland, R.O.","contributorId":72458,"corporation":false,"usgs":true,"family":"Helland","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":246399,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212847,"text":"70212847 - 1938 - The significance and nature of the cone of depression in ground-water bodies","interactions":[],"lastModifiedDate":"2020-08-31T14:57:33.866613","indexId":"70212847","displayToPublicDate":"1938-12-01T09:54:52","publicationYear":"1938","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"The significance and nature of the cone of depression in ground-water bodies","docAbstract":"<p><span>In nature the hydraulic system in an aquifer is in balance; the discharge is equal to the recharge and the water table or other piezometric surface is more or less fixed in position. Discharge by wells is a new discharge superimposed on the previous system. Before a new equilibrium can be established water levels must fall throughout the aquifer to an extent sufficient to reduce the natural discharge or increase the recharge by an amount equal to the amount discharged by the well. Until this new equilibrium is established water must be withdrawnfrom storage in the aquifer and conversely the new equilibrium cannot be established until an amount of water is withdrawn from storage by the well sufficient to depress the piezometric surface enough to change the recharge or natural discharge the proper amount. The depression of the piezometric surface is called the cone of depression.The characteristics of the cone of depression in an idealized aquifer of infinite areal extent are considered mathematically. Time is an essential variable in the description of this cone. The time rate of lateral growth of the cone is independent of the rate of discharge by the well and depends only on the physical characteristics of the aquifer. The cone must grow laterally much more rapidly in artesian aquifers than it does in nonartesian. The characteristics of the cone in actual aquifers are then considered. In finely porous artesian aquifers the cone appears to be much like the cone in the ideal aquifer. The cone in non-artesian aquifers must be somewhat warped. The theory out-lined implies that well discharge from extensive water-table aquifers must be a draft on storage in the aquifer for many generations.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.33.8.889","usgsCitation":"Theis, C.V., 1938, The significance and nature of the cone of depression in ground-water bodies: Economic Geology, v. 33, no. 8, p. 889-902, https://doi.org/10.2113/gsecongeo.33.8.889.","productDescription":"4 p.","startPage":"889","endPage":"902","costCenters":[],"links":[{"id":378033,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"8","noUsgsAuthors":false,"publicationDate":"1938-12-01","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":797699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207439,"text":"70207439 - 1938 - Sulphate minerals of the Comstock Lode, Nevada","interactions":[],"lastModifiedDate":"2019-12-19T11:35:37","indexId":"70207439","displayToPublicDate":"1938-11-01T11:30:27","publicationYear":"1938","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sulphate minerals of the Comstock Lode, Nevada","docAbstract":"<p><span>Seventeen representative samples of supergene sulphates from old workings on the Comstock Lode are described. They range from simple minerals such as gypsum and epsomite to complex aggregates of four or more distinct species. All are well known species except a mineral of the copper (chalcanthite) or magnesium sulphate pentahydrate group, with about half the magnesium replaced by copper, zinc, ferrous iron, and manganese. Four new analyses of Comstock Lode mine waters are given. © 1938 Society of Economic Geologists, Inc.</span></p>","language":"English","publisher":"Society of Economic Geologists ","doi":"10.2113/gsecongeo.33.7.749","issn":"03610128","usgsCitation":"Milton, C., and Johnston, W.D., 1938, Sulphate minerals of the Comstock Lode, Nevada: Economic Geology, v. 33, no. 7, p. 749-771, https://doi.org/10.2113/gsecongeo.33.7.749.","productDescription":"23 p. 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,{"id":38039,"text":"38039 - 1938 - Botulism, a recurring hazard to waterfowl: with notes on recent outbreaks in the United States and Canada, and Australia","interactions":[],"lastModifiedDate":"2014-07-21T11:45:35","indexId":"38039","displayToPublicDate":"1938-09-01T11:45:05","publicationYear":"1938","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"120","title":"Botulism, a recurring hazard to waterfowl: with notes on recent outbreaks in the United States and Canada, and Australia","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Kalmbach, E., 1938, Botulism, a recurring hazard to waterfowl: with notes on recent outbreaks in the United States and Canada, and Australia: Wildlife Leaflet 120, 8 p.","productDescription":"8 p.","numberOfPages":"8","costCenters":[],"links":[{"id":290563,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4fbee4b0b290850f2e5a","contributors":{"authors":[{"text":"Kalmbach, E.R.","contributorId":21610,"corporation":false,"usgs":true,"family":"Kalmbach","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":218766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212723,"text":"70212723 - 1938 - A recording evaporimeter","interactions":[],"lastModifiedDate":"2020-08-26T18:20:55.614369","indexId":"70212723","displayToPublicDate":"1938-08-26T13:13:11","publicationYear":"1938","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":"A recording evaporimeter","docAbstract":"<p>The instrument herein described was originally designed and built to record the evaporation‐loss from a standard Weather Bureau pan for use in a study of the variation of flow in Santa Ana River. Valuable suggestions were made by various members of the Water Resources Branch of the Geological Survey in Southern California, and financial assistance for construction was given by F. C. Ebert and H. C. Troxell of the same organization. The typing of the paper and some of the drafting were done by Works Progress Administration help.</p><p>The original instrument was damaged by flood‐waters in 1934, while in operation at Baldwin Park, California. It was then redesigned and constructed of stainless materials and installed on the campus of the San Bernardino Valley Junior College. The Weather Bureau pan was replaced by a thermally insulated pan. The damping unit was added at this time by the present writers. The evaporimeter was placed in regular operation on October 30, 1937, in a study of the relative magnitudes of the various energy‐components associated with solar and sky radiation and with evaporation from water‐surfaces, from damp soil, and from plants.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR019i002p00609","usgsCitation":"Oliver, J., and Cummings, N., 1938, A recording evaporimeter: Eos, Transactions, American Geophysical Union, v. 19, no. 2, p. 609-612, https://doi.org/10.1029/TR019i002p00609.","productDescription":"4 p.","startPage":"609","endPage":"612","costCenters":[],"links":[{"id":377902,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Oliver, J.","contributorId":167156,"corporation":false,"usgs":false,"family":"Oliver","given":"J.","affiliations":[],"preferred":false,"id":797359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, N.W.","contributorId":239604,"corporation":false,"usgs":false,"family":"Cummings","given":"N.W.","email":"","affiliations":[],"preferred":false,"id":797360,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212722,"text":"70212722 - 1938 - Ground‐water for air‐conditioning on Long Island, New York","interactions":[],"lastModifiedDate":"2020-08-26T18:02:47.291952","indexId":"70212722","displayToPublicDate":"1938-08-26T12:52:04","publicationYear":"1938","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 for air‐conditioning on Long Island, New York","docAbstract":"<p><span>During the last five years ground‐water has been more and more extensively used for air‐conditioning on Long Island, New York. The wide‐spread occurrence of highly permeable water‐bearing material and the relatively small cost of installation and operation of a ground‐water, air‐conditioning system has resulted in many such installations by theaters, restaurants, stores, and other establishments. Many companies likewise have taken advantage of these favorable factors and are utilizing low‐temperature ground‐water for cooling purposes in the manufacture of ice. This new use of ground‐water has considerably increased the draft in the western end of Long Island where there had already been so much over‐development that the watertable was below sea‐level in an area of more than 40 square miles. In 1933 the State Legislature, recognizing the seriousness of this over‐development, passed a law requiring that the approval, of the State Water Power and Control Commission be secured before constructing a well with a capacity greater than 100,000 gallons a day. Since the passage of the law the‐policy of the Commission has been to require water pumped from new‐wells for cooling purposes to be returned to the ground. This requirement has resulted in the construction of many recharge‐wells (locally called diffusion‐wells) through which the warm water is returned to the ground.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR019i001p00412","usgsCitation":"Leggette, R., and Brashears, M., 1938, Ground‐water for air‐conditioning on Long Island, New York: Eos, Transactions, American Geophysical Union, v. 19, no. 1, p. 412-418, https://doi.org/10.1029/TR019i001p00412.","productDescription":"7 p.","startPage":"412","endPage":"418","costCenters":[],"links":[{"id":377901,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.04922485351562,\n              40.564937785967224\n            ],\n            [\n              -73.80752563476562,\n              40.564937785967224\n            ],\n            [\n              -73.80752563476562,\n              40.77430186363723\n            ],\n            [\n              -74.04922485351562,\n              40.77430186363723\n            ],\n            [\n              -74.04922485351562,\n              40.564937785967224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"19","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":797357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brashears, M.L. Jr.","contributorId":23212,"corporation":false,"usgs":true,"family":"Brashears","given":"M.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":797358,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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