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,{"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":55551,"text":"ofr4636 - 1946 - Engineering report on the water problem in the Ember formation of the South Oregon Basin field, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:11:55","indexId":"ofr4636","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":"46-36","title":"Engineering report on the water problem in the Ember formation of the South Oregon Basin field, Wyoming","language":"ENGLISH","doi":"10.3133/ofr4636","usgsCitation":"Ferguson, R., and Milek, W., 1946, Engineering report on the water problem in the Ember formation of the South Oregon Basin field, Wyoming: U.S. Geological Survey Open-File Report 46-36, ill.; 2 maps; 5 cross sections; 12 tables, https://doi.org/10.3133/ofr4636.","productDescription":"ill.; 2 maps; 5 cross sections; 12 tables","costCenters":[],"links":[{"id":173933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6026fc","contributors":{"authors":[{"text":"Ferguson, R.D.","contributorId":97182,"corporation":false,"usgs":true,"family":"Ferguson","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":253683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Milek, W.A.","contributorId":6519,"corporation":false,"usgs":true,"family":"Milek","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":253682,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2287,"text":"wsp989 - 1946 - Water levels and artesian pressure in observation wells in the United States in 1943, Part 4, South-Central States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp989","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":"989","title":"Water levels and artesian pressure in observation wells in the United States in 1943, Part 4, South-Central States","language":"ENGLISH","publisher":"U.S. G.P.O. : For sale by the Supt. of Docs., U.S. G.P.O.,","doi":"10.3133/wsp989","usgsCitation":"Meinzer, O.E., Wenzel, L., and and others, 1946, Water levels and artesian pressure in observation wells in the United States in 1943, Part 4, South-Central States: U.S. Geological Survey Water Supply Paper 989, iv, 194 p. :ill. ;23 cm., https://doi.org/10.3133/wsp989.","productDescription":"iv, 194 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137638,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0989/report-thumb.jpg"},{"id":28086,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0989/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9ee1","contributors":{"authors":[{"text":"Meinzer, Oscar Edward","contributorId":12020,"corporation":false,"usgs":true,"family":"Meinzer","given":"Oscar","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":144956,"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":144957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528008,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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,{"id":15926,"text":"ofr4821C - 1946 - Water analysis as a means of prospecting for metallic ore deposits","interactions":[],"lastModifiedDate":"2012-02-02T00:07:14","indexId":"ofr4821C","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":"48-21","chapter":"C","title":"Water analysis as a means of prospecting for metallic ore deposits","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/ofr4821C","usgsCitation":"Sergeev, E., and Hawkes, H.E., 1946, Water analysis as a means of prospecting for metallic ore deposits: U.S. Geological Survey Open-File Report 48-21, 5 leaves :ill. ;28 cm., https://doi.org/10.3133/ofr4821C.","productDescription":"5 leaves :ill. ;28 cm.","costCenters":[],"links":[{"id":149397,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa394","contributors":{"authors":[{"text":"Sergeev, E.A.","contributorId":10441,"corporation":false,"usgs":true,"family":"Sergeev","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":171955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hawkes, H. E. (translator)","contributorId":68330,"corporation":false,"usgs":true,"family":"Hawkes","given":"H.","suffix":"(translator)","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":171956,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":581,"text":"wsp1008 - 1946 - Surface water supply of the United States, 1944, Part VIII, Western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1008","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":"1008","title":"Surface water supply of the United States, 1944, Part VIII, Western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1008","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1946, Surface water supply of the United States, 1944, Part VIII, Western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1008, vi, 311 p. ;23 cm., https://doi.org/10.3133/wsp1008.","productDescription":"vi, 311 p. ;23 cm.","costCenters":[],"links":[{"id":136260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1008/report-thumb.jpg"},{"id":25144,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1008/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db697058","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":527553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2274,"text":"wsp988 - 1946 - Water levels and artesian pressure in observation wells in the United States in 1943, Part 3, North-Central States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp988","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":"988","title":"Water levels and artesian pressure in observation wells in the United States in 1943, Part 3, North-Central States","language":"ENGLISH","publisher":"U.S. G.P.O. ; for sale by the Supt. of Docs.,","doi":"10.3133/wsp988","usgsCitation":"Meinzer, O.E., and Wenzel, L., 1946, Water levels and artesian pressure in observation wells in the United States in 1943, Part 3, North-Central States: U.S. Geological Survey Water Supply Paper 988, iv, 352 p. :ill., map ;23 cm., https://doi.org/10.3133/wsp988.","productDescription":"iv, 352 p. :ill., map ;23 cm.","costCenters":[],"links":[{"id":137603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0988/report-thumb.jpg"},{"id":28063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0988/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa1ca","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144936,"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":144937,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2813,"text":"wsp993 - 1946 - Geology and ground-water resources of Cedar City and Parowan Valleys, Iron County, Utah","interactions":[],"lastModifiedDate":"2017-09-07T14:10:59","indexId":"wsp993","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":"993","title":"Geology and ground-water resources of Cedar City and Parowan Valleys, Iron County, Utah","docAbstract":"<p>Cedar City Valley and Parowan Valley are situated in the eastern part of Iron County, in southwestern Utah. Both valleys are traversed by United States Highway 91, which skirts the west base of the High Plateaus of Utah. The sparse population of the valleys is chiefly dependent upon agricultural products for its livelihood. 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12","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrographs of six wells that are located along a line extending northwestward across secs. 27, 21, 17, and 8, T. 35 S., R. 11 W"},{"id":29347,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0993/plate-07.pdf","text":"Plate 13","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":" Map of Cedar City Valley showing ground-water contours about April 1, 1940, and subdivisions of the ground-water reservoir"},{"id":29348,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0993/plate-08.pdf","text":"Plate 14","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Cedar City Valley showing ground-water contours about April 1 and September 15, 1939"},{"id":29349,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0993/plate-09.pdf","text":"Plate 15","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of part of Cedar City Valley showing decline of groundwater levels between April 1 and September 15, 1939"},{"id":29361,"rank":420,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0993/plate-21.pdf","text":"Plate 27","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing ground-water districts in Parowan Valley"},{"id":29362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0993/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":29351,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0993/plate-11.pdf","text":"Plate 17","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Cedar City Valley showing lines of equal depth to water below land surface, September 1939"},{"id":29352,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0993/plate-12.pdf","text":"Plate 18","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Cedar City Valley showing location»of wells, maximum area of artesian flow, and areas of artesian flow in September 1939"},{"id":29353,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0993/plate-13.pdf","text":"Plate 19","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrographs of five wells in which the seasonal fluctuations of static level are caused chiefly by flow from artesian wells"},{"id":29354,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0993/plate-14.pdf","text":"Plate 20","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrographs of four wells located along a north-south line through the pumping district in Parowan Valley"},{"id":29355,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0993/plate-15.pdf","text":"Plate 21","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrographs of six wells in Parowan Valley that are remote from areas of intensive ground-water development"},{"id":29356,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0993/plate-16.pdf","text":"Plate 22","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Parowan Valley showing highest and lowest observed artesian-pressure surface in March 1940"}],"country":"United States","state":"Utah","county":"Iron County","otherGeospatial":"Cedar City valley, Parowan valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c8b","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145840,"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":145841,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1422,"text":"wsp967A - 1946 - Notable local floods of 1939: Part 1: Floods of September 1939 in Colorado River Basin below Boulder Dam","interactions":[],"lastModifiedDate":"2024-06-13T18:23:43.981771","indexId":"wsp967A","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":"A","title":"Notable local floods of 1939: Part 1: Floods of September 1939 in Colorado River Basin below Boulder Dam","docAbstract":"<p>Although the flow of Colorado River has been controlled at Boulder Dam since February 1935, flood danger still exists in the basin below the dam. This report on the first general floods to occur below Boulder lam since the dam was closed presents facts that should prove helpful in planning protection and reservoir operation to minimize the ill effects of future floods.</p><p>The floods of September 1939 were caused by a series of tropical disturbances that moved northwestward along the west coast of Mexico and culminated in unprecedently heavy rains in northwestern Mexico and southwestern United States. Three separate storms, occurring September 3-7, 8-13, and 23-26, moved across the lower Colorado River Basin. At many points in that area the mean annual precipitation was exceeded by the precipitation for September.</p><p>Because little rainfall preceded the storms, runoff from them was less than would have occurred under more unfavorable conditions. At streamflow measuring stations where past records are available no new records were set. On Gila River no flood occurred. On Colorado River the flood was not so great as those that had occurred almost every year prior to the closing of Boulder Dam. On Williams River, however, the peak discharge was of the magnitude of a major flood, and in many of the smaller drainage basins peaks occurred which probably have not been exceeded in the previous 50 to 100 years.</p><p>The relatively low flood peaks on Colorado River do not mean that there was no flood danger. The regulation of the river since Boulder Dam was closed has prevented the scouring of the channel by floods, has permitted the encroachment of vegetation in the channel, and has allowed the accumulation of sediment. As a result, flood stages today are about as high as they formerly were for discharges twice as large.</p><p>Flood peaks in Colorado River were greatly reduced by storage. Between September 5 and 20»Lake Mead stored 330,000 acre-feet of water. Between September 4 and 7 Havasu Lake stored 135,000 acre-feet, and the channel storage between Topock and Yuma, exclusive of Havasu Lake, accounted for about 110,000 acre-feet at the peak.</p><p>Storage in Havasu Lake is limited in relation to the flood flows that may enter it. When the September storms began, Havasu Lake was at normal minimum level. Had it not been low, the lake probably would have filled by the morning of September 6, and that day's peak inflow, which may have exceeded 75,000 second-feet, would necessarily have passed through with little reduction.<br></p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp967A","usgsCitation":"Gatewood, J.S., 1946, Notable local floods of 1939: Part 1: Floods of September 1939 in Colorado River Basin below Boulder Dam: U.S. Geological Survey Water Supply Paper 967, Report: iv, 39 p.; 4 Plates: 11.27 x 8.29 inches or smaller, https://doi.org/10.3133/wsp967A.","productDescription":"Report: iv, 39 p.; 4 Plates: 11.27 x 8.29 inches or smaller","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":26524,"rank":6,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0967a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393266,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0967a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393265,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0967a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393264,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0967a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393263,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0967a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138079,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0967a/report-thumb.jpg"}],"country":"United States","state":"Arizona, California, Nevada, Utah","otherGeospatial":"Colorado River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.5869140625,\n              32.0639555946604\n            ],\n            [\n              -109.8193359375,\n              32.0639555946604\n            ],\n            [\n              -109.8193359375,\n              37.77071473849609\n            ],\n            [\n              -116.5869140625,\n              37.77071473849609\n            ],\n            [\n              -116.5869140625,\n              32.0639555946604\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696b54","contributors":{"authors":[{"text":"Gatewood, Joseph Strong","contributorId":99120,"corporation":false,"usgs":true,"family":"Gatewood","given":"Joseph","email":"","middleInitial":"Strong","affiliations":[],"preferred":false,"id":143719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4629,"text":"wsp1012 - 1946 - Surface water supply of the United States, 1944, Part XII, Pacific slope basins in Washington and upper Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"wsp1012","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":"1012","title":"Surface water supply of the United States, 1944, Part XII, Pacific slope basins in Washington and upper Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1012","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1946, Surface water supply of the United States, 1944, Part XII, Pacific slope basins in Washington and upper Columbia River basin: U.S. Geological Survey Water Supply Paper 1012, vi, 261 p. ;23 cm., https://doi.org/10.3133/wsp1012.","productDescription":"vi, 261 p. ;23 cm.","costCenters":[],"links":[{"id":139256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1012/report-thumb.jpg"},{"id":31686,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1012/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db697028","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":528322,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14915,"text":"ofr466 - 1946 - Index map of important phosphate deposits of southeastern Idaho and adjoining parts of Wyoming and Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr466","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":"46-6","title":"Index map of important phosphate deposits of southeastern Idaho and adjoining parts of Wyoming and Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr466","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1946, Index map of important phosphate deposits of southeastern Idaho and adjoining parts of Wyoming and Utah: U.S. Geological Survey Open-File Report 46-6, 1 sheet ;46 x 63 cm., https://doi.org/10.3133/ofr466.","productDescription":"1 sheet ;46 x 63 cm.","costCenters":[],"links":[{"id":146359,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":43722,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1946/0006/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5309","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":528973,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215038,"text":"70215038 - 1946 - Quartz crystal in Brazil","interactions":[],"lastModifiedDate":"2020-10-06T21:15:22.849686","indexId":"70215038","displayToPublicDate":"1946-10-06T12:34:58","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Quartz crystal in Brazil","docAbstract":"<p>The peak production of Brazilian quartz crystal was reached in 1943 when 2411 metric tons were exported. Minas Gerais, Goiaz, and Bahia are the principal producing states. Minor quantities are obtained from Espirito Santo and Northeastern Brazil.</p><p>Primary veins and pegmatites yield secondary deposits of eluvial, colluvial, and alluvial origin. The veins range in form from tabular or lenticular bodies, pipes, and pockets to composite lodes and bedded masses. The mineralogy is simple; accessory minerals are few and rare. A small proportion of clear crystals, occurring in vein masses of milky quartz, furnishes the commercial product. Filling, rather than replacement, is believed to be the dominant emplacement process. Pegmatites yield a little commercial quartz. Both residual (eluvial) and water-laid (alluvial) quartz deposits are economically important.</p><p>Crystals range up to 40 metric tons in weight; those of 1 to 5 tons occur in many deposits. Quartz from every locality studied is twinned on both the Brazil and Dauphiné laws. Phantoms are abundant.</p><p>Field studies reveal little difference between the final quartz from some pegmatites and that from veins. It is inferred that the veins may grade into pegmatites at depth and that both are products of the same mineralogenic epoch. Present evidence does not justify a closer dating for the formation of the veins and pegmatites than the early Paleozoic.</p><p>There are few large quartz mines in Brazil. The impressive quartz production during the war years came from many small, scattered workings. Mining methods are primitive, and mechanization was feasible in relatively few areas. The ratio of mine-clean crystal to the total quantity of excavated material varies between 1:1000 and 1:100,000, with an over-all average for the best mines of the order of 1:10,000. Cost of mining ranges from $2 to $10 a kilogram. The average export value during 1944 was $12.50 per kilogram.</p><p>The potential reserves of quartz crystal in Brazil are large, but actual or visual reserves in known districts are small. Future production capacity will be determined by economic factors.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1946)57[601:QCIB]2.0.CO;2","usgsCitation":"Johnston, W.D., and Butler, R., 1946, Quartz crystal in Brazil: GSA Bulletin, v. 57, no. 7, p. 601-650, https://doi.org/10.1130/0016-7606(1946)57[601:QCIB]2.0.CO;2.","productDescription":"50 p.","startPage":"601","endPage":"650","costCenters":[],"links":[{"id":379097,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-57.62513,-30.21629],[-56.2909,-28.85276],[-55.16229,-27.88192],[-54.49073,-27.47476],[-53.64874,-26.92347],[-53.62835,-26.12487],[-54.13005,-25.54764],[-54.62529,-25.73926],[-54.42895,-25.16218],[-54.29348,-24.5708],[-54.29296,-24.02101],[-54.65283,-23.83958],[-55.0279,-24.00127],[-55.40075,-23.95694],[-55.51764,-23.572],[-55.61068,-22.65562],[-55.79796,-22.35693],[-56.47332,-22.0863],[-56.88151,-22.28215],[-57.93716,-22.09018],[-57.87067,-20.73269],[-58.16639,-20.1767],[-57.8538,-19.97],[-57.95,-19.4],[-57.67601,-18.96184],[-57.49837,-18.17419],[-57.73456,-17.55247],[-58.2808,-17.27171],[-58.38806,-16.87711],[-58.24122,-16.29957],[-60.15839,-16.25828],[-60.54297,-15.09391],[-60.25115,-15.07722],[-60.26433,-14.64598],[-60.4592,-14.35401],[-60.5033,-13.77595],[-61.08412,-13.47938],[-61.7132,-13.4892],[-62.12708,-13.19878],[-62.80306,-13.00065],[-63.1965,-12.62703],[-64.31635,-12.46198],[-65.40228,-11.56627],[-65.3219,-10.89587],[-65.44484,-10.51145],[-65.33844,-9.76199],[-66.64691,-9.93133],[-67.1738,-10.30681],[-68.04819,-10.71206],[-68.27125,-11.01452],[-68.78616,-11.03638],[-69.52968,-10.95173],[-70.09375,-11.12397],[-70.54869,-11.00915],[-70.48189,-9.49012],[-71.30241,-10.07944],[-72.18489,-10.0536],[-72.56303,-9.52019],[-73.22671,-9.46221],[-73.01538,-9.03283],[-73.57106,-8.42445],[-73.98724,-7.52383],[-73.7234,-7.341],[-73.72449,-6.9186],[-73.12003,-6.62993],[-73.21971,-6.08919],[-72.96451,-5.74125],[-72.89193,-5.27456],[-71.74841,-4.59398],[-70.92884,-4.40159],[-70.79477,-4.25126],[-69.89364,-4.29819],[-69.4441,-1.55629],[-69.42049,-1.12262],[-69.57707,-0.54999],[-70.02066,-0.18516],[-70.01557,0.54141],[-69.4524,0.70616],[-69.25243,0.60265],[-69.21864,0.98568],[-69.8046,1.08908],[-69.81697,1.71481],[-67.86857,1.69246],[-67.53781,2.03716],[-67.26,1.72],[-67.06505,1.13011],[-66.87633,1.25336],[-66.32577,0.72445],[-65.54827,0.78925],[-65.35471,1.09528],[-64.61101,1.32873],[-64.19931,1.49285],[-64.08309,1.91637],[-63.36879,2.2009],[-63.42287,2.41107],[-64.27,2.49701],[-64.40883,3.12679],[-64.36849,3.79721],[-64.81606,4.05645],[-64.62866,4.14848],[-63.88834,4.02053],[-63.0932,3.77057],[-62.80453,4.00697],[-62.08543,4.16212],[-60.96689,4.53647],[-60.60118,4.9181],[-60.73357,5.20028],[-60.21368,5.24449],[-59.98096,5.01406],[-60.111,4.57497],[-59.76741,4.4235],[-59.53804,3.9588],[-59.81541,3.6065],[-59.97452,2.75523],[-59.71855,2.24963],[-59.64604,1.78689],[-59.03086,1.3177],[-58.54001,1.26809],[-58.42948,1.46394],[-58.11345,1.5072],[-57.66097,1.68258],[-57.33582,1.94854],[-56.7827,1.86371],[-56.53939,1.89952],[-55.9957,1.81767],[-55.9056,2.022],[-56.07334,2.22079],[-55.97332,2.51036],[-55.56976,2.42151],[-55.09759,2.52375],[-54.52475,2.31185],[-54.08806,2.10556],[-53.77852,2.3767],[-53.55484,2.3349],[-53.41847,2.05339],[-52.93966,2.12486],[-52.55642,2.50471],[-52.24934,3.24109],[-51.6578,4.15623],[-51.31715,4.20349],[-51.06977,3.6504],[-50.50888,1.90156],[-49.97408,1.73648],[-49.9471,1.04619],[-50.69925,0.22298],[-50.38821,-0.07844],[-48.62057,-0.23549],[-48.5845,-1.23781],[-47.82496,-0.58162],[-46.56658,-0.94103],[-44.9057,-1.55174],[-44.41762,-2.13775],[-44.58159,-2.69131],[-43.41879,-2.38311],[-41.47266,-2.91202],[-39.97867,-2.87305],[-38.50038,-3.70065],[-37.22325,-4.82095],[-36.45294,-5.1094],[-35.5978,-5.1495],[-35.23539,-5.46494],[-34.89603,-6.73819],[-34.72999,-7.34322],[-35.12821,-8.9964],[-35.63697,-9.64928],[-37.04652,-11.04072],[-37.68361,-12.17119],[-38.42388,-13.03812],[-38.67389,-13.05765],[-38.95328,-13.79337],[-38.8823,-15.66705],[-39.16109,-17.20841],[-39.26734,-17.86775],[-39.58352,-18.2623],[-39.76082,-19.59911],[-40.77474,-20.90451],[-40.94476,-21.93732],[-41.75416,-22.37068],[-41.98828,-22.97007],[-43.0747,-22.96769],[-44.64781,-23.35196],[-45.35214,-23.79684],[-46.47209,-24.08897],[-47.64897,-24.8852],[-48.49546,-25.87702],[-48.641,-26.6237],[-48.47474,-27.17591],[-48.66152,-28.18613],[-48.88846,-28.67412],[-49.58733,-29.22447],[-50.69687,-30.98447],[-51.57623,-31.7777],[-52.25608,-32.24537],[-52.7121,-33.19658],[-53.37366,-33.76838],[-53.65054,-33.202],[-53.20959,-32.72767],[-53.78795,-32.04724],[-54.57245,-31.49451],[-55.60151,-30.85388],[-55.97324,-30.88308],[-56.97603,-30.10969],[-57.62513,-30.21629]]]},\"properties\":{\"name\":\"Brazil\"}}]}","volume":"57","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Johnston, W. D. Jr.","contributorId":27193,"corporation":false,"usgs":true,"family":"Johnston","given":"W.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":800614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butler, R.D.","contributorId":242663,"corporation":false,"usgs":false,"family":"Butler","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":800615,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215037,"text":"70215037 - 1946 - Notes on determining the effective distance to a line of recharge","interactions":[],"lastModifiedDate":"2020-10-06T17:31:34.027294","indexId":"70215037","displayToPublicDate":"1946-10-06T12:13:09","publicationYear":"1946","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":"Notes on determining the effective distance to a line of recharge","docAbstract":"<p><span>Increasing emphasis has been given in recent years to the installation of wells in sand and gravel deposits along perennial streams. Under favorable conditions water enters the aquifer from the adjacent stream so that the safe yield is not limited by recharge from local precipitation [see “References” at end of paper, Jeffords, 1946]. Some of the installations tested, however, have not been successful. At times the preliminary investigations have been inadequate, and often quantitative hydrologic techniques have been applied without adequate consideration of the existing local conditions.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i006p00854","usgsCitation":"Kazmann, R., 1946, Notes on determining the effective distance to a line of recharge: Eos, Transactions, American Geophysical Union, v. 27, no. 6, p. 854-859, https://doi.org/10.1029/TR027i006p00854.","productDescription":"6 p.","startPage":"854","endPage":"859","costCenters":[],"links":[{"id":379096,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Kazmann, R.G.","contributorId":242662,"corporation":false,"usgs":false,"family":"Kazmann","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":800613,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214998,"text":"70214998 - 1946 - Appendix A—Report of the subcommittee on permeability","interactions":[],"lastModifiedDate":"2020-10-05T19:16:32.873158","indexId":"70214998","displayToPublicDate":"1946-10-05T13:58:53","publicationYear":"1946","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":"Appendix A—Report of the subcommittee on permeability","docAbstract":"<p><span>The Subcommittee on Permeability of the Permanent Research Committee on Ground Water of the Section of Hydrology, was organized in 1943 to provide for the open discussion of the terminology relating to permeability with a view toward the elimination of conflicting usages and the clarification and standardization of acceptable terms. Confusion had arisen not only in the units of measurement but also in the notation and nomenclature of permeability. It seemed desirable to have general agreement particularly in regard to the names of the different physical parameters in common use and their symbols.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00245","usgsCitation":"Jacob, C.E., 1946, Appendix A—Report of the subcommittee on permeability: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 245-256, https://doi.org/10.1029/TR027i002p00245.","productDescription":"12  p.","startPage":"245","endPage":"256","costCenters":[],"links":[{"id":379066,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":800516,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214997,"text":"70214997 - 1946 - Appendix B—Notes on the permeability coefficient and its units","interactions":[],"lastModifiedDate":"2020-10-05T18:58:32.033392","indexId":"70214997","displayToPublicDate":"1946-10-05T13:51:45","publicationYear":"1946","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":"Appendix B—Notes on the permeability coefficient and its units","docAbstract":"<p><span>In the development of terms and units for a new science such as ground‐water hydrology, which is based on physics, it would seem fitting to adopt the terminology that has become standard in other branches of physics such as heat and electricity. Darcy's law has its counterpart in similar laws in the other branches of physics.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00256","usgsCitation":"Fishel, V., 1946, Appendix B—Notes on the permeability coefficient and its units: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 256-269, https://doi.org/10.1029/TR027i002p00256.","productDescription":"4 p.","startPage":"256","endPage":"269","costCenters":[],"links":[{"id":379065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":800515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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