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,{"id":1594,"text":"wsp756 - 1936 - Surface water supply of the United States, 1934, Part 1, North Atlantic slope basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp756","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"756","title":"Surface water supply of the United States, 1934, Part 1, North Atlantic slope basins","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp756","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1936, Surface water supply of the United States, 1934, Part 1, North Atlantic slope basins: U.S. Geological Survey Water Supply Paper 756, x, 383 p. :ill. ;23 cm., https://doi.org/10.3133/wsp756.","productDescription":"x, 383 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0756/report-thumb.jpg"},{"id":26659,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0756/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6977cc","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":527957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":305,"text":"wsp770 - 1936 - Surface water supply of Hawaii : July 1, 1933 to June 30, 1934","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp770","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"770","title":"Surface water supply of Hawaii : July 1, 1933 to June 30, 1934","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp770","usgsCitation":"Grover, N., and Carson, M.H., 1936, Surface water supply of Hawaii : July 1, 1933 to June 30, 1934: U.S. Geological Survey Water Supply Paper 770, 120 p. ;23 cm., https://doi.org/10.3133/wsp770.","productDescription":"120 p. ;23 cm.","costCenters":[],"links":[{"id":136060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0770/report-thumb.jpg"},{"id":24867,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0770/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697ee5","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":142215,"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":142216,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2650,"text":"wsp678 - 1936 - Geology and ground-water resources of Uvalde and Medina Counties, Texas","interactions":[],"lastModifiedDate":"2016-08-22T10:14:22","indexId":"wsp678","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"678","title":"Geology and ground-water resources of Uvalde and Medina Counties, Texas","docAbstract":"<p>This report is based on an investigation by the United States Geological Survey, the Texas State Board of Water Engineers, and the Texas State Board of Health to determine the ground-water resources of Uvalde and Medina Counties, especially in relation to irrigation, both in these counties and in the counties to the south where water is obtained for irrigation from the Carrizo sand and younger formations. This investigation was carried on between September 12, 1928, and May 25, 1930. Observations of the water levels in selected wells were made at intervals up to August 1935.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp678","usgsCitation":"Sayre, A.N., 1936, Geology and ground-water resources of Uvalde and Medina Counties, Texas: U.S. Geological Survey Water Supply Paper 678, v, 146 p., https://doi.org/10.3133/wsp678.","productDescription":"v, 146 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":28970,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0678/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0678/report-thumb.jpg"},{"id":109955,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24626.htm","linkFileType":{"id":5,"text":"html"},"description":"24626"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685821","contributors":{"authors":[{"text":"Sayre, Albert Nelson","contributorId":83102,"corporation":false,"usgs":true,"family":"Sayre","given":"Albert","email":"","middleInitial":"Nelson","affiliations":[],"preferred":false,"id":145555,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3168,"text":"wsp773E - 1936 - The New York State flood of July 1935","interactions":[],"lastModifiedDate":"2022-02-09T20:49:02.246137","indexId":"wsp773E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"773","chapter":"E","title":"The New York State flood of July 1935","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1936","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Print Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp773E","usgsCitation":"Johnson, H., 1936, The New York State flood of July 1935: U.S. Geological Survey Water 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,{"id":70213007,"text":"70213007 - 1936 - The diurnal fluctuation in the ground‐water and flow of the Santa Ana River and its meaning","interactions":[],"lastModifiedDate":"2020-09-08T15:27:29.575745","indexId":"70213007","displayToPublicDate":"1936-09-03T13:34:33","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The diurnal fluctuation in the ground‐water and flow of the Santa Ana River and its meaning","docAbstract":"<p>In the time alloted for this subject it will be impossible to discuss, in its entirety, all phases of the methods used in computing the loss of water by transpiration from native plant‐life along the Santa Ana River. The results of this work are published in Bulletin 44 of the Division of Water Resources, State of California. The present paper is confined to a discussion of the diurnal fluctuations that occur in the flow of the Santa Ana River and the adjacent ground‐water.</p><p>On Figure 1 have, been plotted the gage‐height records for a short period (July 5–8, 1935) for eight southern California streams. These records have been selected at random from the large number of records filed in the local office of the United States Geological Survey. Some of these streams have a large drainage‐area, others are small; some are short and steep, others flat and long. The points of measurement range from 15 to 2950 feet above sea‐level. One of the streams (Mojave River) is in the desert‐region; the others drain into the Pacific Ocean. The object of Figure 1 is to demonstrate, that the diurnal fluctuation exists and is, to a large degree, similar at most points of measurement. As a rule, the maximum discharge occurs about 10 o'clock in the morning, and the minimum late in the afternoon. It is readily recognized that these fluctuations are in the main caused by the evaporation and transpiration‐loss in or adjacent to the stream‐channel.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00496","usgsCitation":"Troxell, H.C., 1936, The diurnal fluctuation in the ground‐water and flow of the Santa Ana River and its meaning: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 496-504, https://doi.org/10.1029/TR017i002p00496.","productDescription":"9 p.","startPage":"496","endPage":"504","costCenters":[],"links":[{"id":378149,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Santa Ana River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.7679443359375,\n              33.858442151927896\n            ],\n            [\n              -117.71026611328125,\n              33.89093747081252\n            ],\n            [\n              -117.77000427246094,\n              33.91202429999497\n            ],\n            [\n              -117.84278869628908,\n              33.86699475113557\n            ],\n            [\n              -117.9045867919922,\n              33.81110228864701\n            ],\n            [\n              -117.93754577636719,\n              33.713488158266806\n            ],\n            [\n              -117.96501159667967,\n              33.646063909385845\n            ],\n            [\n              -117.97050476074219,\n              33.62719851659249\n            ],\n            [\n              -117.94784545898436,\n              33.61919376817004\n            ],\n            [\n              -117.88330078125,\n              33.751176960544875\n            ],\n            [\n              -117.83729553222655,\n              33.830497692052425\n            ],\n            [\n              -117.7679443359375,\n              33.858442151927896\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Troxell, Harold C.","contributorId":33354,"corporation":false,"usgs":true,"family":"Troxell","given":"Harold","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":797963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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