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E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144939,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wenzel, L.K.","contributorId":18733,"corporation":false,"usgs":true,"family":"Wenzel","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":144940,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528007,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23321,"text":"ofr4639 - 1946 - Geology and ground-water resources of the Upper Pinal Creek area, Arizona","interactions":[],"lastModifiedDate":"2017-05-18T12:04:11","indexId":"ofr4639","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1946","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":"46-39","title":"Geology and ground-water resources of the Upper Pinal Creek area, Arizona","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr4639","issn":"0094-9140","usgsCitation":"Hazen, G., and Turner, S., 1946, Geology and ground-water resources of the Upper Pinal Creek area, Arizona: U.S. Geological Survey Open-File Report 46-39, 63 p., https://doi.org/10.3133/ofr4639.","productDescription":"63 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":154874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1946/0039/report-thumb.jpg"},{"id":52619,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1946/0039/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52620,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1946/0039/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52621,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1946/0039/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52622,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1946/0039/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52623,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1946/0039/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52624,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1946/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a54e6","contributors":{"authors":[{"text":"Hazen, G.E.","contributorId":57882,"corporation":false,"usgs":true,"family":"Hazen","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":189897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turner, S.F.","contributorId":67914,"corporation":false,"usgs":true,"family":"Turner","given":"S.F.","email":"","affiliations":[],"preferred":false,"id":189898,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3169,"text":"wsp967C - 1946 - Notable local floods of 1939, Part 3, Flood of August 21, 1939 in town of Baldwin Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"wsp967C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1946","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":"967","chapter":"C","title":"Notable local floods of 1939, Part 3, Flood of August 21, 1939 in town of Baldwin Maine","language":"ENGLISH","doi":"10.3133/wsp967C","usgsCitation":"Stackpole, M.R., 1946, Notable local floods of 1939, Part 3, Flood of August 21, 1939 in town of Baldwin Maine: U.S. Geological Survey Water Supply Paper 967, 61-68 p. I-iv., https://doi.org/10.3133/wsp967C.","productDescription":"61-68 p. I-iv.","costCenters":[],"links":[{"id":139181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0967c/report-thumb.jpg"},{"id":30127,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0967c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d93","contributors":{"authors":[{"text":"Stackpole, Miner R.","contributorId":79461,"corporation":false,"usgs":true,"family":"Stackpole","given":"Miner","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":146365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3014,"text":"wsp994 - 1946 - Cloudburst floods in Utah, 1850-1938","interactions":[],"lastModifiedDate":"2022-02-14T21:27:20.44398","indexId":"wsp994","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1946","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":"994","title":"Cloudburst floods in Utah, 1850-1938","docAbstract":"Five years after the first settlement was made in Utah, at Salt Lake City in 1847, it became manifest to the settlers both there and at Manti that \"cloudbursts\" were of common occurrence in this region. Other settlements were made and gradually expanded on the steep alluvial fans of the mountain streams, and reports of cloudburst storms and their attendant floods became increasingly numerous as farms and homes were damaged by them.
In 1890 the theory was advanced that these floods occurred because the sheep and cattle had eaten off the vegetation in the hills, leaving nothing to hold the water back. This indictment of man's flocks and herds has become so common that during the past 20 years considerable study has been given to it. Most of the study, however, has been devoted to runoff from the catchment basins and factors involved in its control and little of it to an adequate scientific analysis of the relationship between physiographic and geologic features and the meteorologic phenomena involved in the storms
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp994","usgsCitation":"Woolley, R., Marsell, R.E., and Grover, N., 1946, Cloudburst floods in Utah, 1850-1938: U.S. Geological Survey Water Supply Paper 994, Report: v, 128 p.; 12 Plates: 25.00 x 31.50 inches or smaller, https://doi.org/10.3133/wsp994.","productDescription":"Report: v, 128 p.; 12 Plates: 25.00 x 31.50 inches or smaller","numberOfPages":"154","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":247273,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0994/plate-23.pdf","text":"Plate 23","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Utah showing distribution of cloudburst floods and population"},{"id":247272,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0994/plate-22.pdf","text":"Plate 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This region is divided into two segments by the Canadian River and the name Llano Estacado has usually been assigned by geologists to the southern, or larger part, which is bounded on the east and on the west by the escarpments of the High Plains and on the north by the valley of the deeply entrenched Canadian River. The ground water occurs chiefly in the beds of sand in the Ogallala formation, which underlies the surface throughout almost the entire region and in many places is 200 to 300 feet thick. It rests on an uneven floor of older rocks, which are exposed at the base of the escarpments bounding the High Plains and in the Canadian \"River Valley. If water is found in them it is generally highly mineralized. 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