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,{"id":1101,"text":"wsp1870A - 1970 - Floods of December 1966 in southwestern Utah","interactions":[],"lastModifiedDate":"2017-09-04T14:58:45","indexId":"wsp1870A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1870","chapter":"A","title":"Floods of December 1966 in southwestern Utah","docAbstract":"<p>Severe floods occurred in parts of southwestern Utah on December 5-6, 1966, as a result of precipitation of about 1 inch to more than 12 inches during December 3-6. The flood on the Virgin River was the greatest since the first settlers arrived in 1860.</p><p>The peak discharge of the Virgin River at Virgin, Utah, was 22,830 cubic feet per second on December 6; this exceeded the previous maximum discharge of 13,500 cubic feet per second on March 3, 1938, and September 17, 1961, and probably has a recurrence interval of 100 years. At eight other gage sites in the flood area, the peak discharge in December 1966 was the highest of record; the recurrence intervals of some of the peak discharges may be 100 years. The flood peaks were generally of short duration and most streams receded to near base flow within 24 hours.</p><p>The dissolved-solids content was significantly lower in the Virgin River at Virgin than at St. George, about 25 miles downstream; the water was of the calcium sulfate type at both sites. Data for the Santa Clara River above Winsor Dam and the Santa Clara River near Santa Clara show a significant increase in dissolved solids between the two sites. The water above Winsor Dam was of the calcium bicarbonate type, and the water near Santa Clara was of the calcium bicarbonate sulfate type.</p><p>The suspended-sediment discharge, during the period December 5-8, 1966, at Santa Clara River above Winsor Dam, near Santa Clara was about foyer times greater than all the suspended-sediment discharge during the preceding 3 years ; the suspended-sediment discharge of the Virgin River at Virgin was greater during the 4-day period than during any one of the preceding 3 years.</p><p>Nearly all the flood damage in the area occurred in the Virgin River basin. According to the Soil Conservation Service, total damage in the Dixie Soil Conservation District in Washington County was about $835,000; 60 percent of the damage was caused by floodwater and 40 percent by deposited sediment.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1870A","usgsCitation":"Butler, E., and Mundorff, J.C., 1970, Floods of December 1966 in southwestern Utah: U.S. Geological Survey Water Supply Paper 1870, Report: iv, 40 p.; 2 Plates: 35.50 in. x 22.11 in. and 19.50 in. x 18.05 in., https://doi.org/10.3133/wsp1870A.","productDescription":"Report: iv, 40 p.; 2 Plates: 35.50 in. x 22.11 in. and 19.50 in. x 18.05 in.","numberOfPages":"45","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":25835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1870a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137866,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1870a/report-thumb.jpg"},{"id":25834,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1870a/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing location and size of radar echoes in parts of Nevada, Arizona, and Utah during December 3-6 1966"},{"id":25833,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1870a/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of southwestern Utah showing stream-gaging and water-quality sampling sites, geology, vegetation, and precipitation at selected sites during period December 3-7, 1966"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6b001c","contributors":{"authors":[{"text":"Butler, Elmer","contributorId":33301,"corporation":false,"usgs":true,"family":"Butler","given":"Elmer","email":"","affiliations":[],"preferred":false,"id":143178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":143179,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68319,"text":"ha333 - 1970 - Reconnaissance of the Pigeon River, a cold-water river in the northcentral part of Michigan's southern peninsula","interactions":[],"lastModifiedDate":"2021-10-21T15:12:36.579623","indexId":"ha333","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"333","title":"Reconnaissance of the Pigeon River, a cold-water river in the northcentral part of Michigan's southern peninsula","docAbstract":"<p>The cold-water streams of the northern states provide unique recreational values to the American people (wilderness or semi-wilderness atmosphere, fast-water canoeing, and trout fishing), but the expanding recreational needs must be balanced against the growing demand of water for public and industrial supplies, for irrigation, and for the dilution of sewage and other wastes. In order to make intelligent decisions regarding use and management of the water resource for recreation and other demands, an analysis of the hydrologic factors related to recreational values is essential.</p><p>The Pigeon River is one of Michigan's outstanding trout streams and is the favorite of a large number of anglers who return year after year. Camping is also popular and is usually, but not always, associated with fishing. Boating is very rare on the Pigeon because of numerous portages around log jams. Cabin-living and resorting are relatively minor on this river as yet, but much of the private river front may be developed in future years.</p><p>The Pigeon is located in the north-central part of the southern peninsula of Michigan (see index map). Headwaters are a few miles northeast of Gaylord, and the mouth is at Mullet Lake, a few miles northeast of Indian River. Interstate Highway 75 roughly parallels the river about 5 to 10 miles to the west. Exits from this highway at Gaylord, Vanderbilt, Wolverine, and Indian River, provide easy access to the Pigeon.</p><p>The recreational value of the river depends on the streamflow characteristics, quality of water, and character of stream channel, and bed and banks. The purpose of this atlas is to describe these characteristics, and to show how they relate to recreational uses.</p><p>Most of the information presented here was obtained from a field reconnaissance in June, 1966, and from basic records of the U.S. Geological Survey's Water Resources Division. The area of field study is limited to the channel, bed, and banks of the main stem of the Pigeon from source to mouth. The study was made in cooperation with the Michigan Geological Survey, Gerald E. Eddy, Chief. Advice and assistance were also obtained from other sections of the Michigan Conservation Department.</p><p>Sheet 1 of this atlas presents information on streamflow characteristics and water quality. Sheet 2 describes the physical characteristics of the stream channel, and bed and banks, and shows how these physical characteristics relate to streamflow, water quality, and recreational use.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha333","usgsCitation":"Hendrickson, G.E., and Doonan, C.J., 1970, Reconnaissance of the Pigeon River, a cold-water river in the northcentral part of Michigan's southern peninsula: U.S. Geological Survey Hydrologic Atlas 333, 5 Plates: 30.5 x 40.0 inches or smaller, https://doi.org/10.3133/ha333.","productDescription":"5 Plates: 30.5 x 40.0 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":185889,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha333.JPG"},{"id":89776,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/333/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390726,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15708.htm"},{"id":89775,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/333/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89774,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/333/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89773,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/333/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89772,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/333/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Michigan","otherGeospatial":"Pigeon River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.61666666666666,45.03333333333333 ], [ -84.61666666666666,45.43333333333333 ], [ -84.41666666666667,45.43333333333333 ], [ -84.41666666666667,45.03333333333333 ], [ -84.61666666666666,45.03333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63afc9","contributors":{"authors":[{"text":"Hendrickson, G. E.","contributorId":99958,"corporation":false,"usgs":true,"family":"Hendrickson","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":278021,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doonan, C. J.","contributorId":62592,"corporation":false,"usgs":true,"family":"Doonan","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278020,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47933,"text":"ofr71122 - 1970 - A proposed streamflow data program for North Carolina","interactions":[],"lastModifiedDate":"2016-12-14T09:24:07","indexId":"ofr71122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"71-122","title":"A proposed streamflow data program for North Carolina","language":"ENGLISH","doi":"10.3133/ofr71122","usgsCitation":"Goddard, G., Jackson, N., Hubbard, E., and Hinson, H., 1970, A proposed streamflow data program for North Carolina: U.S. Geological Survey Open-File Report 71-122, 113 p. ill., maps ; 28 cm., https://doi.org/10.3133/ofr71122.","productDescription":"113 p. ill., maps ; 28 cm.","costCenters":[{"id":13634,"text":"South Atlantic 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There is a distinctive difference between the assemblages in the northern and southern parts of this region. Many sublittoral cryophilic species are not present south of Cape Cod or the Northeast Channel, and several thermophilic species a.re not .found north of Cape Cod or Georges Bank. The ostracode assemblages in the southern part of the cold-temperate Nova Scotian province are a mixture of amphiatlantic cryophilic species and endemic, mainly thermophilic species; European forms make up approximately 50 percent of the species. Less than 25 percent of the species known from the mild-temperate Virginian province have been reported from European waters. More endemic species pass Cape Cod from the south than amphiatlantic cryophilic species do from the north. This is consistent with the fact that summer isotherms are more compressed than winter isotherms in the Cape Cod region, and the southern limit of distribution of most amphiatlantic species is regulated by summer high temperatures. 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