{"pageNumber":"6401","pageRowStart":"160000","pageSize":"25","recordCount":184689,"records":[{"id":22885,"text":"ofr70110 - 1970 - Hydraulic testing of well HTH-23 in Central Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:54","indexId":"ofr70110","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":"70-110","title":"Hydraulic testing of well HTH-23 in Central Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr70110","issn":"0094-9140","usgsCitation":"Dinwiddie, G., 1970, Hydraulic testing of well HTH-23 in Central Nevada: U.S. Geological Survey Open-File Report 70-110, ii, 33 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr70110.","productDescription":"ii, 33 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":154196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a0c4","contributors":{"authors":[{"text":"Dinwiddie, G.A.","contributorId":49798,"corporation":false,"usgs":true,"family":"Dinwiddie","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":189067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56047,"text":"ofr70269 - 1970 - Preliminary geologic map of the Tybo quadrangle, Nye County, Nevada","interactions":[{"subject":{"id":56047,"text":"ofr70269 - 1970 - Preliminary geologic map of the Tybo quadrangle, Nye County, Nevada","indexId":"ofr70269","publicationYear":"1970","noYear":false,"title":"Preliminary geologic map of the Tybo quadrangle, Nye County, Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":66877,"text":"i821 - 1974 - Geologic map of the Tybo Quadrangle, Nye County, Nevada","indexId":"i821","publicationYear":"1974","noYear":false,"title":"Geologic map of the Tybo Quadrangle, Nye County, Nevada"},"id":1}],"supersededBy":{"id":66877,"text":"i821 - 1974 - Geologic map of the Tybo Quadrangle, Nye County, Nevada","indexId":"i821","publicationYear":"1974","noYear":false,"title":"Geologic map of the Tybo Quadrangle, Nye County, Nevada"},"lastModifiedDate":"2012-02-02T00:11:50","indexId":"ofr70269","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":"70-269","title":"Preliminary geologic map of the Tybo quadrangle, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/ofr70269","usgsCitation":"Quinlivan, W.D., and Rogers, C.L., 1970, Preliminary geologic map of the Tybo quadrangle, Nye County, Nevada: U.S. Geological Survey Open-File Report 70-269, 11 leaves ;27 cm.; 1 map (5 sheets), https://doi.org/10.3133/ofr70269.","productDescription":"11 leaves ;27 cm.; 1 map (5 sheets)","costCenters":[],"links":[{"id":106478,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8501.htm","linkFileType":{"id":5,"text":"html"},"description":"8501"},{"id":174951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aa45","contributors":{"authors":[{"text":"Quinlivan, W. D.","contributorId":14398,"corporation":false,"usgs":true,"family":"Quinlivan","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":254691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rogers, Cleaves Lincoln","contributorId":12858,"corporation":false,"usgs":true,"family":"Rogers","given":"Cleaves","email":"","middleInitial":"Lincoln","affiliations":[],"preferred":false,"id":254690,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1049,"text":"wsp1899C - 1970 - Sediment transport by streams in the Palouse River basin, Washington and Idaho, July 1961-June 1965","interactions":[],"lastModifiedDate":"2022-12-15T22:12:36.12682","indexId":"wsp1899C","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":"1899","chapter":"C","title":"Sediment transport by streams in the Palouse River basin, Washington and Idaho, July 1961-June 1965","docAbstract":"The Palouse River basin covers about 3,300 square miles in southeastern Washington and northwestern Idaho. The eastern part of the basin is composed of steptoes and foothills which are generally above an altitude of 2,600 feet; the central part is of moderate local relief and is mantled chiefly by thick loess deposits; and the western part is characterized by low relief and scabland topography and is underlain mostly by basalt. \r\n\r\nPrecipitation increases eastward across the study area. It ranges annually from 12 to 18 inches in the western part and from 14 to 23 inches in the central part, and it exceeds 40 inches in the eastern part. \r\n\r\nSurface runoff from the basin for the 4-year period of study (July 1961-June 1965) averaged 408,000 acre-feet per year, compared with 445,200 acre-feet per year for the 27-year period of record. The eastern part of the basin contributed about 55 percent of the total, whereas the central and western parts contributed 37 percent and 8 percent, respectively. Most sediment transport from the Palouse River basin and the highest sediment concentrations in streams occurred in the winter. Of the several storms during the study period, those of February 3-9, 1963, December 22-27, 1964, and January 27-February 4, 1965, accounted for 81 percent of the total 4-year suspended-sediment load; the storm of February 3-9, 1963, accounted for nearly one-half the total load. The discharge-weighted mean concentration of suspended sediment carried in the Palouse River past Hooper during the study period was 2,970 milligrams per liter. \r\n\r\nThe average annual sediment discharge of the Palouse River at its mouth was about 1,580,000 tons per year, and the estimated average annual sediment yield was 480 tons per square mile. The yield ranged from 5 tons per square mile from the western part of the basin to 2,100 tons per square mile from the central part. The high yield from the central part is attributed to a scarcity of vegetal cover, to the fine-grained loess soils, and to rapid runoff during winter storms. Sediment yield from the eastern part of the basin ranged from 460 to more than 1,000 tons per square mile.\r\n\r\nDuring high flow, silt particles make up the largest part of the suspended-sediment load, whereas during low flow, clay particles represent the greatest part. On the average, the suspended sediment transported by the Palouse River past Hooper contained 3 percent sand, 68 percent silt, and 29 percent clay. Unmeasured sediment discharge was estimated to have been 5 percent of the total sediment discharge. \r\n\r\nData collected during the 4-year period of study show that sediment loads were higher than those recorded by V. G. Kaiser during the longer period 1939-65. Whereas Kaiser's study showed an average annual soil loss of 9.6 million tons, the average annual loss during the recent study was 14.2 million tons. \r\n\r\nThe factor that has had the greatest effect on the increase of sediment yields is land use. Lands once covered and protected by natural vegetation have been extensively, cultivated, and much of the soil has become susceptible to erosion, particularly in areas mantled by loessal soils.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1899C","usgsCitation":"Boucher, P.R., 1970, Sediment transport by streams in the Palouse River basin, Washington and Idaho, July 1961-June 1965: U.S. Geological Survey Water Supply Paper 1899, Report: iv, 37 p.; 1 Plate: 26.50 × 24.50 inches, https://doi.org/10.3133/wsp1899C.","productDescription":"Report: iv, 37 p.; 1 Plate: 26.50 × 24.50 inches","costCenters":[],"links":[{"id":110035,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25118.htm","linkFileType":{"id":5,"text":"html"},"description":"25118"},{"id":137923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1899c/report-thumb.jpg"},{"id":25713,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1899c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25714,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1899c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Washington","otherGeospatial":"Palouse River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.508,\n              47.483\n            ],\n            [\n              -118.322,\n              47.483\n            ],\n            [\n              -118.322,\n              46.517\n            ],\n            [\n              -116.508,\n              46.517\n            ],\n            [\n              -116.508,\n              47.483\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e9e4b07f02db5e94ca","contributors":{"authors":[{"text":"Boucher, P. R.","contributorId":108088,"corporation":false,"usgs":true,"family":"Boucher","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143091,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1088,"text":"wsp1899I - 1970 - Streamflow from the United States into the Atlantic Ocean during 1931-1960","interactions":[],"lastModifiedDate":"2018-02-14T16:20:07","indexId":"wsp1899I","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":"1899","chapter":"I","title":"Streamflow from the United States into the Atlantic Ocean during 1931-1960","docAbstract":"Streamflow from the United States into the Atlantic Ocean, between the international stream St. Croix River, inclusive, and Cape Sable, Fla., averaged about 355,000 cfs (cubic feet per second) during the 30-year period 1931-60, or roughly 20 percent of the water that, on the average flows out of the conterminous United States. The area drained by streams flowing into the Atlantic Ocean is about 288,000 square miles, including the Canadian part of the St. Croix and Connecticut River basins, or a little less than 10 percent of the area of the conterminous United States. Hence, the average streamflow into the Atlantic Ocean, in terms of cubic feet per second per square mile, is about twice the national average of the flow that leaves the conterminous United States. Flow from about three-fourths of the area draining into the Atlantic Ocean is gaged at streamflow measuring stations of the U.S. Geological Survey. The remaining one-fourth of the drainage area consists mostly of low-lying coastal areas from which the flow was estimated, largely on the basis of nearby gaging stations. \r\n\r\nStreamflow, in terms of cubic feet per second per square mile, decreases rather progressively from north to south. It averages nearly 2 cfs along the Maine coast, about 1 cfs along the North Carolina coast, and about 0.9 cfs along the Florida coast.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1899I","usgsCitation":"Bue, C.D., 1970, Streamflow from the United States into the Atlantic Ocean during 1931-1960: U.S. Geological Survey Water Supply Paper 1899, iv, 36p. :ill. ;23 cm., https://doi.org/10.3133/wsp1899I.","productDescription":"iv, 36p. :ill. ;23 cm.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":137126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1899i/report-thumb.jpg"},{"id":25808,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1899i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e02","contributors":{"authors":[{"text":"Bue, Conrad D.","contributorId":76716,"corporation":false,"usgs":true,"family":"Bue","given":"Conrad","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":143158,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":195,"text":"wsp1964 - 1970 - Quality of surface waters of the United States, 1965, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1964","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":"1964","title":"Quality of surface waters of the United States, 1965, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1964","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Quality of surface waters of the United States, 1965, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1964, xiii, 819 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1964.","productDescription":"xiii, 819 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1964/report-thumb.jpg"},{"id":24806,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1964/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651a39","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":527224,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":193,"text":"wsp1959 - 1970 - Quality of surface waters of the United States, 1964, Parts 12-15, Pacific slope basins in Washington and upper Columbia River basin to Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1959","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":"1959","title":"Quality of surface waters of the United States, 1964, Parts 12-15, Pacific slope basins in Washington and upper Columbia River basin to Alaska","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1959","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Quality of surface waters of the United States, 1964, Parts 12-15, Pacific slope basins in Washington and upper Columbia River basin to Alaska: U.S. Geological Survey Water Supply Paper 1959, xii, 428 p. ;28 cm., https://doi.org/10.3133/wsp1959.","productDescription":"xii, 428 p. ;28 cm.","costCenters":[],"links":[{"id":136251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1959/report-thumb.jpg"},{"id":24804,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1959/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651a13","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":527222,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68309,"text":"ha376 - 1970 - Sediment yields of Wisconsin streams","interactions":[],"lastModifiedDate":"2015-10-06T07:48:35","indexId":"ha376","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":"376","title":"Sediment yields of Wisconsin streams","docAbstract":"<p><span>Sediment in Wisconsin streams causes economic and engineering problems in water management and reduces the value of water for nearly all uses. Sediment produces problems such as reduced reservoir capacity, navigation hazards, increased cost of water treatment, property damage, temporary loss of farmland, destruction of feeding and nesting grounds of fish, and destruction of wildlife habitat. Sediment in water also reduces the aesthetic value of surface waters and is detrimental to the State's tourist and recreation industry.</span></p>\n<p><span>The yield of sediment from a drainage basin is subject to many environmental influences. Most sediment results from the weathering and erosion of soil and rock materials. Other factors such as rainfall intensity, runoff rate, topography, rock type, soil characteristics, vegetal cover, and land use also influence the rate of sediment production and movement. An understanding of the many parameters that influence sediment yield is a basic need for managing the State's water resources.</span></p>\n<p><span>The purpose of this report is to describe the magnitude and variability of sediment in Wisconsin streams, to relate sediment yields to the local environment, and to identify areas that need further study. The report is based on sediment data from 44 stream-gaging sites throughout the State. Determination of local areas of erosion and deposition are beyond the scope of the report.</span></p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha376","usgsCitation":"Hindall, S.M., and Flint, R., 1970, Sediment yields of Wisconsin streams: U.S. Geological Survey Hydrologic Atlas 376, 1 Sheet: 35.50 x 35.00 inches, https://doi.org/10.3133/ha376.","productDescription":"1 Sheet: 35.50 x 35.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":185690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89753,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/376/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United 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,{"id":37619,"text":"tp50 - 1970 - Food habits of five centrarchids during filling of Beaver Reservoir, 1965-66","interactions":[],"lastModifiedDate":"2012-02-02T00:10:02","indexId":"tp50","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":89,"text":"Technical Paper","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"50","title":"Food habits of five centrarchids during filling of Beaver Reservoir, 1965-66","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Mullan, J.W., and Applegate, R.L., 1970, Food habits of five centrarchids during filling of Beaver Reservoir, 1965-66: Technical Paper 50, 16 p. : ill. ; 26 cm.","productDescription":"16 p. : ill. ; 26 cm.","costCenters":[],"links":[{"id":161740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae8ec","contributors":{"authors":[{"text":"Mullan, James W.","contributorId":77197,"corporation":false,"usgs":true,"family":"Mullan","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":218348,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Applegate, Richard L.","contributorId":80722,"corporation":false,"usgs":true,"family":"Applegate","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":218349,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1116,"text":"wsp1875 - 1970 - Correlative estimates of streamflow in the upper Colorado River basin","interactions":[],"lastModifiedDate":"2017-09-04T15:05:51","indexId":"wsp1875","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":"1875","title":"Correlative estimates of streamflow in the upper Colorado River basin","docAbstract":"<p>Most hydrologic analyses, whether for appraisal of the water resource, feasibility of a particular development, design of a system of operation, assessment of gains or losses from acts of man or natural changes, or almost any other use, require the extension in time of some streamflow records. In the Upper Colorado River Basin, streamflow records have been extended by various agencies from time to time to fulfill their individual needs, resulting in different estimates of flow for the same point and time. The purpose of this report is to provide correlative estimates of monthly mean discharge at discontinued streamflow gaging stations so that all users will have access to a single set of data.</p><p>Estimates of monthly mean discharge for periods other than the period of actual record are given for certain discontinued streamflow gaging stations. The stations selected were discontinued in recent years, but they have a sufficient length of record to permit development of a meaningful correlation with the records for a nearby long-term gaging station. Where possible, estimates of monthly mean discharge are made to provide a complete record, estimated or measured, from 1930 to 1965. However, where the long-term gaging station record encompasses a shorter period, the estimates cover only that shorter period. Estimates for periods prior to 1930 were not made, although these may be computed for a few stations. Lack of a related long-term gaging-station record prevented the extension of records at many discontinued stations.</p><p>The area covered in this report (fig. 1) is that defined in the Colorado River Compact of 1922, as the Upper Basin \"those parts of the States of Arizona, Colorado, New Mexico, Utah, and Wyoming within and from which waters naturally drain into the Colorado River System above Lee Ferry,\"<sup>1</sup> but excluding \"all parts of said States located without the drainage area of the Colorado River System which are now and shall hereafter be beneficially served by waters diverted from the System above Lee Ferry\" (Wilbur and Ely, 1948, p. A18).</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1875","usgsCitation":"Carroon, L.E., 1970, Correlative estimates of streamflow in the upper Colorado River basin: U.S. Geological Survey Water Supply Paper 1875, Report: v, 145 p.; Plate: 24.50 in. x 37.42 in., https://doi.org/10.3133/wsp1875.","productDescription":"Report: v, 145 p.; Plate: 24.50 in. x 37.42 in.","numberOfPages":"152","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":137998,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1875/report-thumb.jpg"},{"id":25878,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1875/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Upper Colorado River Basin, showing location of streamflow gaging stations"},{"id":25879,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1875/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Colorado River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6844ca","contributors":{"authors":[{"text":"Carroon, Lamar E.","contributorId":34488,"corporation":false,"usgs":true,"family":"Carroon","given":"Lamar","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":196,"text":"wsp1962 - 1970 - Quality of surface waters of the United States, 1965, Parts 3 and 4, Ohio River basin and St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1962","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":"1962","title":"Quality of surface waters of the United States, 1965, Parts 3 and 4, Ohio River basin and St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1962","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Quality of surface waters of the United States, 1965, Parts 3 and 4, Ohio River basin and St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1962, xi, 480 p. :ill. ; 23 cm., https://doi.org/10.3133/wsp1962.","productDescription":"xi, 480 p. :ill. ; 23 cm.","costCenters":[],"links":[{"id":136275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1962/report-thumb.jpg"},{"id":24807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1962/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651a2e","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":527225,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56039,"text":"ofr70241 - 1970 - Land and water for tomorrow","interactions":[],"lastModifiedDate":"2026-01-12T14:44:22.772603","indexId":"ofr70241","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":"70-241","title":"Land and water for tomorrow","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70241","usgsCitation":"Nace, R.L., 1970, Land and water for tomorrow: U.S. Geological Survey Open-File Report 70-241, 16 p., https://doi.org/10.3133/ofr70241.","productDescription":"16 p.","costCenters":[],"links":[{"id":174943,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0241/report-thumb.jpg"},{"id":498539,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0241/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae7c8","contributors":{"authors":[{"text":"Nace, Raymond L.","contributorId":93460,"corporation":false,"usgs":true,"family":"Nace","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":254680,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61918,"text":"gq809 - 1970 - Geologic map of the Fairbanks A-3 quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:10:33","indexId":"gq809","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"809","title":"Geologic map of the Fairbanks A-3 quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/gq809","usgsCitation":"Wahrhaftig, C., 1970, Geologic map of the Fairbanks A-3 quadrangle, Alaska: U.S. Geological Survey Geologic Quadrangle 809, 1 map., https://doi.org/10.3133/gq809.","productDescription":"1 map.","costCenters":[],"links":[{"id":103525,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2111.htm","linkFileType":{"id":5,"text":"html"},"description":"2111"},{"id":248206,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0809/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":253032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0809/report-thumb.jpg"}],"scale":"63360","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -148.5,64 ], [ -148.5,64.25 ], [ -148,64.25 ], [ -148,64 ], [ -148.5,64 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6998e0","contributors":{"authors":[{"text":"Wahrhaftig, Clyde","contributorId":102473,"corporation":false,"usgs":true,"family":"Wahrhaftig","given":"Clyde","email":"","affiliations":[],"preferred":false,"id":266553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":1090,"text":"wsp1939B - 1970 - Depletion of streamflow by infiltration in the main channels of the Tucson basin, southeastern Arizona","interactions":[{"subject":{"id":55970,"text":"ofr7047 - 1970 - Depletion of streamflow by infiltration in the main channels of the Tucson basin, southeastern Arizona","indexId":"ofr7047","publicationYear":"1970","noYear":false,"title":"Depletion of streamflow by infiltration in the main channels of the Tucson basin, southeastern Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":1090,"text":"wsp1939B - 1970 - Depletion of streamflow by infiltration in the main channels of the Tucson basin, southeastern Arizona","indexId":"wsp1939B","publicationYear":"1970","noYear":false,"chapter":"B","title":"Depletion of streamflow by infiltration in the main channels of the Tucson basin, southeastern Arizona"},"id":1}],"lastModifiedDate":"2022-02-14T22:11:46.011618","indexId":"wsp1939B","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":"1939","chapter":"B","title":"Depletion of streamflow by infiltration in the main channels of the Tucson basin, southeastern Arizona","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water resources of the Tucson basin","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1939B","usgsCitation":"Burkham, D., 1970, Depletion of streamflow by infiltration in the main channels of the Tucson basin, southeastern Arizona: U.S. Geological Survey Water Supply Paper 1939, Report: iv, 36 p.; 1 Plate: 17.00 × 33.00 inches, https://doi.org/10.3133/wsp1939B.","productDescription":"Report: iv, 36 p.; 1 Plate: 17.00 × 33.00 inches","costCenters":[],"links":[{"id":137931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1939b/report-thumb.jpg"},{"id":25818,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1939b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25819,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1939b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":395953,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25164.htm"}],"country":"United States","state":"Arizona","otherGeospatial":"Tucson basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.167,\n              31.329\n            ],\n            [\n              -110.5,\n              31.329\n            ],\n            [\n              -110.5,\n              32.633\n            ],\n            [\n              -111.167,\n              32.633\n            ],\n            [\n              -111.167,\n              31.329\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab1e4b07f02db66ea8f","contributors":{"authors":[{"text":"Burkham, D. E.","contributorId":97073,"corporation":false,"usgs":true,"family":"Burkham","given":"D. E.","affiliations":[],"preferred":false,"id":143160,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":127,"text":"wsp1971 - 1970 - Methods and applications of electrical simulation in ground-water studies in the lower Arkansas and Verdigris River Valleys, Arkansas and Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1971","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":"1971","title":"Methods and applications of electrical simulation in ground-water studies in the lower Arkansas and Verdigris River Valleys, Arkansas and Oklahoma","docAbstract":"The Arkansas River Multiple-Purpose Plan will provide year-round navigation on the Arkansas River from near its mouth to Muskogee, Okla., and on the Verdigris River from Muskogee to Catoosa, Okla. The altered regimen in the Arkansas and Verdigris Rivers will affect ground-water conditions in the adjacent alluvial aquifers. In 1957 the U.S. Geological Survey \r\n\r\nand U.S. Army Corps of Engineers entered into a cooperative agreement for a comprehensive ground-water study of the lower Arkansas and Verdigris River valleys. At the request of the Corps of Engineers, the Geological Survey agreed to provide (1) basic ground-water data before, during, and after construction of the Multiple-Purpose Plan and (2) interpretation and projections of postconstruction ground-water conditions. The data collected were used by the Corps of Engineers in preliminary foundation and excavation estimates and by the Geological Survey as the basis for defining the hydrologic properties of, and the ground-water conditions in, the aquifer. The projections of postconstruction ground-water conditions were used by the Corps of Engineers in the planning, design, construction, and operation of the Multiple-Purpose Plan. \r\n\r\nAnalysis and projections of ground-water conditions were made by use of electrical analog models. These models use the analogy between the flow of electricity in a resistance-capacitance circuit and the flow of a liquid in a porous and permeable medium.\r\n\r\nVerification provides a test of the validity of the analog to perform as the aquifer would, within the range of historic forces. The verification process consists of simulating the action of historic forces which have acted upon the aquifer and of duplicating the aquifer response with the analog. The areal distribution of accretion can be treated as an unknown and can be determined by analog simulation of the piezometric surface in an aquifer. Comparison of accretion with depth to piezometric surface below land surface shows that accretion decreases with decreasing depth to water level. The decrease in accretion is attributed mostly to the increase in evapotranspiration from the aquifer, and where water levels are very near the land surface, to the rejection of recharge. The maximum accretion and the decrease in accretion with the decrease in depth to water are dependent upon the climate and the thickness and lithology of the fine-grained material overlying the aquifer. \r\n\r\nDams on the Arkansas and Verdigris Rivers will impose a direct change in water levels in the aquifers adjacent to the rivers. This change will be attenuated by the resultant change in accretion to the aquifer. The analogs of aquifers in the valleys were used to determine the change in ground-water level from preconstruction to postconstruction conditions.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1971","usgsCitation":"Bedinger, M.S., Reed, J., Wells, C., and Swafford, B., 1970, Methods and applications of electrical simulation in ground-water studies in the lower Arkansas and Verdigris River Valleys, Arkansas and Oklahoma: U.S. Geological Survey Water Supply Paper 1971, vi, 71 p. :illus., maps (4 fold. in pocket) ;23 cm., https://doi.org/10.3133/wsp1971.","productDescription":"vi, 71 p. :illus., maps (4 fold. in pocket) ;23 cm.","costCenters":[],"links":[{"id":136437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1971/report-thumb.jpg"},{"id":24734,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1971/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24735,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1971/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24736,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1971/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24737,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1971/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24738,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1971/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a01b","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":141978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":141977,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wells, C.J.","contributorId":80242,"corporation":false,"usgs":true,"family":"Wells","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":141979,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swafford, B.F.","contributorId":38528,"corporation":false,"usgs":true,"family":"Swafford","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":141976,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":68341,"text":"ha379 - 1970 - Reconnaissance bathymetry of Pyramid Lake, Washoe County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:11:12","indexId":"ha379","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":"379","title":"Reconnaissance bathymetry of Pyramid Lake, Washoe County, Nevada","language":"ENGLISH","doi":"10.3133/ha379","usgsCitation":"Harris, E., 1970, Reconnaissance bathymetry of Pyramid Lake, Washoe County, Nevada: U.S. Geological Survey Hydrologic Atlas 379, 1 map., https://doi.org/10.3133/ha379.","productDescription":"1 map.","costCenters":[],"links":[{"id":190415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89817,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/379/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.75,39.75 ], [ -119.75,40.25 ], [ -119.25,40.25 ], [ -119.25,39.75 ], [ -119.75,39.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db64475e","contributors":{"authors":[{"text":"Harris, E. E.","contributorId":24328,"corporation":false,"usgs":true,"family":"Harris","given":"E. E.","affiliations":[],"preferred":false,"id":278064,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38714,"text":"pp644B - 1970 - Hydrocarbons in thermal areas, northwestern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"pp644B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"644","chapter":"B","title":"Hydrocarbons in thermal areas, northwestern Wyoming","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter Contributions to General Geology, 1969","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp644B","usgsCitation":"Love, J.D., 1970, Hydrocarbons in thermal areas, northwestern Wyoming: U.S. Geological Survey Professional Paper 644, p. B1-B23, https://doi.org/10.3133/pp644B.","productDescription":"p. B1-B23","costCenters":[],"links":[{"id":119991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0644b/report-thumb.jpg"},{"id":65572,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0644b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628f31","contributors":{"authors":[{"text":"Love, J. D.","contributorId":64620,"corporation":false,"usgs":true,"family":"Love","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":220332,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46493,"text":"ofr70270 - 1970 - Map showing relative amounts of landslides in California","interactions":[{"subject":{"id":46493,"text":"ofr70270 - 1970 - Map showing relative amounts of landslides in California","indexId":"ofr70270","publicationYear":"1970","noYear":false,"title":"Map showing relative amounts of landslides in California"},"predicate":"SUPERSEDED_BY","object":{"id":66882,"text":"i747 - 1973 - Map showing areas of estimated relative amounts of landslides in California","indexId":"i747","publicationYear":"1973","noYear":false,"title":"Map showing areas of estimated relative amounts of landslides in California"},"id":1}],"supersededBy":{"id":66882,"text":"i747 - 1973 - Map showing areas of estimated relative amounts of landslides in California","indexId":"i747","publicationYear":"1973","noYear":false,"title":"Map showing areas of estimated relative amounts of landslides in California"},"lastModifiedDate":"2012-02-02T00:10:41","indexId":"ofr70270","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":"70-270","title":"Map showing relative amounts of landslides in California","language":"ENGLISH","doi":"10.3133/ofr70270","usgsCitation":"Radbruch, D.H., and Crowther, K.C., 1970, Map showing relative amounts of landslides in California: U.S. Geological Survey Open-File Report 70-270, 1 map on 2 sheets :photocopy ;sheets 123 x 160 cm. + 1 pamphlet (36 p. ; 28 cm.), https://doi.org/10.3133/ofr70270.","productDescription":"1 map on 2 sheets :photocopy ;sheets 123 x 160 cm. + 1 pamphlet (36 p. ; 28 cm.)","costCenters":[],"links":[{"id":171246,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a340d","contributors":{"authors":[{"text":"Radbruch, Dorothy H.","contributorId":65874,"corporation":false,"usgs":true,"family":"Radbruch","given":"Dorothy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":233441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crowther, Kenneth C.","contributorId":61494,"corporation":false,"usgs":true,"family":"Crowther","given":"Kenneth","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":233440,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39677,"text":"pp641B - 1970 - Gneissic and igneous rocks of the Quadrilatero Ferrifero, Minas Gerais, Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:10:19","indexId":"pp641B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"641","chapter":"B","title":"Gneissic and igneous rocks of the Quadrilatero Ferrifero, Minas Gerais, Brazil","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Regional geology of the Quadrilatero Ferrifero, Minas Gerais, Brazil","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp641B","usgsCitation":"Herz, N., 1970, Gneissic and igneous rocks of the Quadrilatero Ferrifero, Minas Gerais, Brazil: U.S. Geological Survey Professional Paper 641, p. B1-B58, https://doi.org/10.3133/pp641B.","productDescription":"p. B1-B58","costCenters":[],"links":[{"id":121423,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0641b/report-thumb.jpg"},{"id":67400,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0641b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":67401,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0641b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674288","contributors":{"authors":[{"text":"Herz, Norman","contributorId":49806,"corporation":false,"usgs":true,"family":"Herz","given":"Norman","email":"","affiliations":[],"preferred":false,"id":221963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39685,"text":"pp660 - 1970 - Geology and mineral resources of Libya - a reconnaissance","interactions":[{"subject":{"id":13862,"text":"ofr5944 - 1959 - A summary of the geologic history of Libya","indexId":"ofr5944","publicationYear":"1959","noYear":false,"title":"A summary of the geologic history of Libya"},"predicate":"SUPERSEDED_BY","object":{"id":39685,"text":"pp660 - 1970 - Geology and mineral resources of Libya - a reconnaissance","indexId":"pp660","publicationYear":"1970","noYear":false,"title":"Geology and mineral resources of Libya - a reconnaissance"},"id":1},{"subject":{"id":13864,"text":"ofr6798 - 1967 - Geology and mineral resources of Libya, a reconnaissance","indexId":"ofr6798","publicationYear":"1967","noYear":false,"title":"Geology and mineral resources of Libya, a reconnaissance"},"predicate":"SUPERSEDED_BY","object":{"id":39685,"text":"pp660 - 1970 - Geology and mineral resources of Libya - a reconnaissance","indexId":"pp660","publicationYear":"1970","noYear":false,"title":"Geology and mineral resources of Libya - a reconnaissance"},"id":2},{"subject":{"id":13865,"text":"ofr6253 - 1962 - Idri salt deposits, Fezzan Province, Libya","indexId":"ofr6253","publicationYear":"1962","noYear":false,"title":"Idri salt deposits, Fezzan Province, Libya"},"predicate":"SUPERSEDED_BY","object":{"id":39685,"text":"pp660 - 1970 - Geology and mineral resources of Libya - a reconnaissance","indexId":"pp660","publicationYear":"1970","noYear":false,"title":"Geology and mineral resources of Libya - a reconnaissance"},"id":3},{"subject":{"id":13866,"text":"ofr6252 - 1958 - Iron deposit of the Shatti Valley area of the Fezzan Province, Libya","indexId":"ofr6252","publicationYear":"1958","noYear":false,"title":"Iron deposit of the Shatti Valley area of the Fezzan Province, Libya"},"predicate":"SUPERSEDED_BY","object":{"id":39685,"text":"pp660 - 1970 - Geology and mineral resources of Libya - a reconnaissance","indexId":"pp660","publicationYear":"1970","noYear":false,"title":"Geology and mineral resources of Libya - a reconnaissance"},"id":4},{"subject":{"id":13867,"text":"ofr6254 - 1962 - Pisida salt deposit, Libya","indexId":"ofr6254","publicationYear":"1962","noYear":false,"title":"Pisida salt deposit, Libya"},"predicate":"SUPERSEDED_BY","object":{"id":39685,"text":"pp660 - 1970 - Geology and mineral resources of Libya - a reconnaissance","indexId":"pp660","publicationYear":"1970","noYear":false,"title":"Geology and mineral resources of Libya - a reconnaissance"},"id":5},{"subject":{"id":13868,"text":"ofr6255 - 1962 - Report on Marada, Pisida, Idri and Taurga salt deposits in Libya","indexId":"ofr6255","publicationYear":"1962","noYear":false,"title":"Report on Marada, Pisida, Idri and Taurga salt deposits in Libya"},"predicate":"SUPERSEDED_BY","object":{"id":39685,"text":"pp660 - 1970 - Geology and mineral resources of Libya - a reconnaissance","indexId":"pp660","publicationYear":"1970","noYear":false,"title":"Geology and mineral resources of Libya - a reconnaissance"},"id":6},{"subject":{"id":13928,"text":"ofr6257 - 1962 - Exploration of the Jefren gypsum-anhydrite deposit, Tripolitania, Libya","indexId":"ofr6257","publicationYear":"1962","noYear":false,"title":"Exploration of the Jefren gypsum-anhydrite deposit, Tripolitania, Libya"},"predicate":"SUPERSEDED_BY","object":{"id":39685,"text":"pp660 - 1970 - Geology and mineral resources of Libya - a reconnaissance","indexId":"pp660","publicationYear":"1970","noYear":false,"title":"Geology and mineral resources of Libya - a reconnaissance"},"id":7}],"lastModifiedDate":"2012-02-02T00:10:18","indexId":"pp660","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"660","title":"Geology and mineral resources of Libya - a reconnaissance","language":"ENGLISH","publisher":"U.S. Govt. 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