No abstract available.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1544C","usgsCitation":"Patten, E., and Bennett, G.D., 1962, Methods of flow measurement in well bores: U.S. Geological Survey Water Supply Paper 1544, 28 p., https://doi.org/10.3133/wsp1544C.","productDescription":"28 p.","costCenters":[],"links":[{"id":138322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1544c/report-thumb.jpg"},{"id":30185,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1544c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bd13","contributors":{"authors":[{"text":"Patten, Eugene P. Jr.","contributorId":34897,"corporation":false,"usgs":true,"family":"Patten","given":"Eugene P.","suffix":"Jr.","affiliations":[],"preferred":false,"id":146419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, Gordon D.","contributorId":18740,"corporation":false,"usgs":true,"family":"Bennett","given":"Gordon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":146418,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1980,"text":"wsp1529 - 1962 - Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams","interactions":[{"subject":{"id":14338,"text":"ofr5756 - 1957 - Water power possibilities of Sheep Creek, Carlson Creek, Lake Dorothy and Turner Lake near Juneau, Alaska","indexId":"ofr5756","publicationYear":"1957","noYear":false,"title":"Water power possibilities of Sheep Creek, Carlson Creek, Lake Dorothy and Turner Lake near Juneau, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":1980,"text":"wsp1529 - 1962 - Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams","indexId":"wsp1529","publicationYear":"1962","noYear":false,"title":"Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1529","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1529","title":"Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1529","usgsCitation":"Johnson, F., 1962, Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams: U.S. Geological Survey Water Supply Paper 1529, v, 102 p. :illus., maps, diagr., tables. ;24 cm., https://doi.org/10.3133/wsp1529.","productDescription":"v, 102 p. :illus., maps, diagr., tables. ;24 cm.","costCenters":[],"links":[{"id":137668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1529/report-thumb.jpg"},{"id":27362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1529/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4b62","contributors":{"authors":[{"text":"Johnson, Fred A.","contributorId":93863,"corporation":false,"usgs":true,"family":"Johnson","given":"Fred A.","affiliations":[],"preferred":false,"id":144472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1986,"text":"wsp1475H - 1962 - Availability of Additional Water for Chiricahua National Monument, Cochise County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1475H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1475","chapter":"H","title":"Availability of Additional Water for Chiricahua National Monument, Cochise County, Arizona","docAbstract":"The Chiricahua National Monument is in the eastern part of Cochise County, Ariz. The monument is about 35 miles southeast of Wilicox in the north end of the Chiricahua Mountains which border Sulphur Springs Valley on the west. The area is drained by two intermittent washes, one in Bonita and the other in Rhyolite Canyons.\r\n\r\nShake Spring is the present source of water for the monument. It ranges in rate of flow from 2 to 12 gpm (gallons per minute) and during dry periods It is not adequate to support the requirements of the monument.\r\n\r\nAmple water to meet the present and future needs of the Chiricahua National Monument is available from a combination of several sources - undeveloped springs or seeps, capture of runoff out of the canyons, and wells drilled in the alluvium.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475H","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Johnson, P.W., 1962, Availability of Additional Water for Chiricahua National Monument, Cochise County, Arizona: U.S. Geological Survey Water Supply Paper 1475, 209-216 p. & 1 map in pocket., https://doi.org/10.3133/wsp1475H.","productDescription":"209-216 p. & 1 map in pocket.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":137684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475h/report-thumb.jpg"},{"id":27370,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27371,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":12449,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/wsp/1475-H/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a98e","contributors":{"authors":[{"text":"Johnson, Phillip W.","contributorId":27422,"corporation":false,"usgs":true,"family":"Johnson","given":"Phillip","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144479,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3197,"text":"wsp1544B - 1962 - An application of thermometry to the study of ground water","interactions":[],"lastModifiedDate":"2018-04-02T10:17:13","indexId":"wsp1544B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1544","chapter":"B","title":"An application of thermometry to the study of ground water","docAbstract":"Except for studies of temperature data related to ground-water developments that induce infiltration from streams, little attention has been given to the possibility of using temperature fluctuations as a tool for studying the elements of the hydrologic cycle involving ground water.
\nThe temperature of the water discharged from large installations that induce river infiltration through alluvial deposits depends primarily on the following factors: (a) the porosity of the aquifer, (b) the specific heat of the rocks or mineral grains making it up, (c) the temperature of the ground water in storage, (d) the temperature of the river water, and (e) the amount of mixing that occurs as a result of pumping. In six installations of this type, where the annual rivertemperature fluctuations ranged from 44° to 52°F, the average range in groundwater temperature was 22 °F. The cycles of ground-water temperature lagged behind the river-temperature cycles by 1 to 51/2 months. Under the conditions that existed, the lag of the minima of the cycles was much greater than that of the maxima, largely because of variations in pumpage and of the effect of viscosity differences on the rate of flow.
\nAn experimental study was made at Worthington in southwestern Minnesota to determine whether temperature fluctuations could be used to study rates and directions of ground-water movement or to evaluate recharge conditions. Three shallow glacial-outwash aquifers were studied by measuring temperatures at approximately monthly intervals in three municipal-supply wells whose average yields were about 60 to 150 gpm (gallons per minute). Temperatures were read with an accuracy of 0.01° to 0.02°C, and the data were analyzed graphically and correlated in detail with lake levels, lake temperatures, precipitation, and groundwater levels.
\nThermographs for 2 wells, 1 completed in a semiconfined aquifer about 200 feet from Okabena Lake and the other in a water-table aquifer about 850 feet from the lake, indicate that pumping induces water to move from the lake into the aquifers. A larger percentage of cold lake water was mixed with ground water from January to March 1958 than from January to March 1959. On the assumption that the cold or warm lake water was a distinct mass, the average time required for water to move from the lake to the well 200 feet away, under the prevailing hydraulic gradient, was 2 to 4 months; and to the well 850 feet away, 5 to 7 months.
\nThe thermograph for a well 1,800 feet from the lake, completed in an artesian aquifer that is confined by relatively impervious glacial till, indicates that the till acts as an insulating medium. However, despite the apparently low permeability of the till, the thermograph suggests that the lowering of artesian pressure, which results from pumping, induces warmer water to move downward through the till.
\nThe infiltration of relatively warm spring and summer rainfall can be detected on the thermographs of all the wells.
\nThe precise measurement of fluctuations in ground-water temperature, based on monthly readings in shallow glacial-outwash aquifers (up to about 70 feet deep), is useful in the study of ground-water movement and recharge. In addition to the study of natural phenomena in the hydrologic cycle, thermometry may be used as a tool in making detailed studies of (1) the effects of inducing the infiltration of surface water, (2) artificial recharge, (3) the effects of injecting petroleum products or radioactive or other wastes into the ground, and (4) ground-water movement in mines.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1544B","collaboration":"Prepared in cooperation with the Division of Waters, Minnesota Department of Conservation","usgsCitation":"Schneider, R., 1962, An application of thermometry to the study of ground water: U.S. Geological Survey Water Supply Paper 1544, Document: iii, 16 p.; 2 Plates: 16 x 12 inches and 16 x 17 inches, https://doi.org/10.3133/wsp1544B.","productDescription":"Document: iii, 16 p.; 2 Plates: 16 x 12 inches and 16 x 17 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":30184,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1544b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30182,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1544b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30183,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1544b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1544b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68571e","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":146417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1973,"text":"wsp1619U - 1962 - Methods of measuring soil moisture in the field","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1619U","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"U","title":"Methods of measuring soil moisture in the field","docAbstract":"For centuries, the amount of moisture in the soil has been of interest in agriculture. The subject of soil moisture is also of great importance to the hydrologist, forester, and soils engineer. \r\n\r\nMuch equipment and many methods have been developed to measure soil moisture under field conditions. This report discusses and evaluates the various methods for measurement of soil moisture and describes the equipment needed for each method. The advantages and disadvantages of each method are discussed and an extensive list of references is provided for those desiring to study the subject in more detail. \r\n\r\nThe gravimetric method is concluded to be the most satisfactory method for most problems requiring onetime moisture-content data. The radioactive method is normally best for obtaining repeated measurements of soil moisture in place. It is concluded that all methods have some limitations and that the ideal method for measurement of soil moisture under field conditions has yet to be perfected.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1619U","usgsCitation":"Johnson, A., 1962, Methods of measuring soil moisture in the field: U.S. Geological Survey Water Supply Paper 1619, iii, 25 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1619U.","productDescription":"iii, 25 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619u/report-thumb.jpg"},{"id":27349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619u/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bee4","contributors":{"authors":[{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":144460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46548,"text":"ofr6218 - 1962 - Minimum elevation of the piezometric surface of the lower water-bearing zone as of 1960, Los Banos-Kettleman City area, California","interactions":[{"subject":{"id":46548,"text":"ofr6218 - 1962 - Minimum elevation of the piezometric surface of the lower water-bearing zone as of 1960, Los Banos-Kettleman City area, California","indexId":"ofr6218","publicationYear":"1962","noYear":false,"title":"Minimum elevation of the piezometric surface of the lower water-bearing zone as of 1960, Los Banos-Kettleman City area, California"},"predicate":"SUPERSEDED_BY","object":{"id":38939,"text":"pp437E - 1975 - Land subsidence due to ground-water withdrawal in the Los Banos-Kettleman City area, California; Part 1, Changes in the hydrologic environment conducive to subsidence","indexId":"pp437E","publicationYear":"1975","noYear":false,"chapter":"E","title":"Land subsidence due to ground-water withdrawal in the Los Banos-Kettleman City area, California; Part 1, Changes in the hydrologic environment conducive to subsidence"},"id":1}],"supersededBy":{"id":38939,"text":"pp437E - 1975 - Land subsidence due to ground-water withdrawal in the Los Banos-Kettleman City area, California; Part 1, Changes in the hydrologic environment conducive to subsidence","indexId":"pp437E","publicationYear":"1975","noYear":false,"title":"Land subsidence due to ground-water withdrawal in the Los Banos-Kettleman City area, California; Part 1, Changes in the hydrologic environment conducive to subsidence"},"lastModifiedDate":"2012-02-02T00:10:45","indexId":"ofr6218","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-18","title":"Minimum elevation of the piezometric surface of the lower water-bearing zone as of 1960, Los Banos-Kettleman City area, California","language":"ENGLISH","doi":"10.3133/ofr6218","usgsCitation":"Bull, W.B., 1962, Minimum elevation of the piezometric surface of the lower water-bearing zone as of 1960, Los Banos-Kettleman City area, California: U.S. Geological Survey Open-File Report 62-18, 1 map., https://doi.org/10.3133/ofr6218.","productDescription":"1 map.","costCenters":[],"links":[{"id":170762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d25","contributors":{"authors":[{"text":"Bull, William B.","contributorId":8919,"corporation":false,"usgs":true,"family":"Bull","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":233545,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3180,"text":"wsp1369D - 1962 - Flow through openings in width constrictions","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1369D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1369","chapter":"D","title":"Flow through openings in width constrictions","docAbstract":"A highway embankment across a stream channel may have one or several bridge openings. In 1953, the pattern of flow through a single opening was quantitatively described by C. E. Kindsvater, R. W. Carter, and H. J. Tracy. The present investigation of the flow pattern at constrictions with two to seven openings is a continuation of the earlier study. Laboratory experiments and the analysis were directed toward the development of methods for (a) computing discharge through multiple-opening constrictions, (b) apportioning a given total discharge among the several openings, and (c) predicting the backwater caused by the constriction. \r\n\r\nThe division of flow among the openings was related to the relative area of each opening, and the relative velocity in the channel immediately upstream from each opening. On the basis of this relationship, the boundaries of the flow channel approaching each opening were established. The head-discharge and backwater characteristics of each opening were then analyzed separately. It is shown that the relations developed for the constriction with a single opening are applicable to each opening of a multiple-opening constriction once the boundaries of the separate flow channels have been established.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1369D","usgsCitation":"Davidian, J., Carrigan, P., and Shen, J., 1962, Flow through openings in width constrictions: U.S. Geological Survey Water Supply Paper 1369, 154 p. :illus., maps. ;24 cm. :91-122 p., https://doi.org/10.3133/wsp1369D.","productDescription":"154 p. :illus., maps. ;24 cm. :91-122 p.","costCenters":[],"links":[{"id":139023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1369d/report-thumb.jpg"},{"id":30138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1369d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cce4b07f02db544634","contributors":{"authors":[{"text":"Davidian, Jacob","contributorId":80245,"corporation":false,"usgs":true,"family":"Davidian","given":"Jacob","email":"","affiliations":[],"preferred":false,"id":146383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carrigan, P.H. Jr.","contributorId":21935,"corporation":false,"usgs":true,"family":"Carrigan","given":"P.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":146381,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shen, John","contributorId":34109,"corporation":false,"usgs":true,"family":"Shen","given":"John","email":"","affiliations":[],"preferred":false,"id":146382,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3172,"text":"wsp1496C - 1962 - Flame-photometric determination of strontium in natural water","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1496C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1496","chapter":"C","title":"Flame-photometric determination of strontium in natural water","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1496C","usgsCitation":"Horr, C.A., 1962, Flame-photometric determination of strontium in natural water: U.S. Geological Survey Water Supply Paper 1496, 33-53 p., https://doi.org/10.3133/wsp1496C.","productDescription":"33-53 p.","costCenters":[],"links":[{"id":138921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1496c/report-thumb.jpg"},{"id":30130,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1496c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef2e1","contributors":{"authors":[{"text":"Horr, C. Albert","contributorId":43333,"corporation":false,"usgs":true,"family":"Horr","given":"C.","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":146368,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3371,"text":"cir467 - 1962 - Floods of February 1962 in southern Idaho and northeastern Nevada","interactions":[],"lastModifiedDate":"2018-01-02T20:18:46","indexId":"cir467","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"467","title":"Floods of February 1962 in southern Idaho and northeastern Nevada","docAbstract":"The floods of February 10-15, 1969., were the highest known on many streams in southern Idaho and northeastern Nevada. Some of the peak discharges have recurrence intervals greater than a hundred years. \r\n\r\nThe floods resulted from an unusual combination of conditions, each of which contributed to the sudden severe flooding. These conditions were an extended period of above-freezing temperatures and prolonged light rainfall, an extensive area of snow at low altitudes, and deeply frozen ground, The snow at higher altitudes did not contribute to the floods. \r\n\r\nRunoff was greatest from watersheds at altitudes ranging from 4,500 to 6,500 feet. Flooding from small tributaries with large parts of their drainage within this range rank among the highest snowmelt floods ever recorded in Idaho and northeastern Nevada. The Snake River main stem had only minor flooding. \r\n\r\nThe flood damage was the greatest ever experienced in most of the flood area because of the large areas inundated and because the value and amount of improvements has increased steadily. The total damage has been estimated as more than $10 million.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir467","usgsCitation":"Thomas, C.A., and Lamke, R.D., 1962, Floods of February 1962 in southern Idaho and northeastern Nevada: U.S. Geological Survey Circular 467, iii, 30 p. :illus., maps, diagrs., tables. ;27cm., https://doi.org/10.3133/cir467.","productDescription":"iii, 30 p. :illus., maps, diagrs., tables. ;27cm.","costCenters":[],"links":[{"id":30381,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0467/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117485,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0467/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfe1e","contributors":{"authors":[{"text":"Thomas, Cecil Albert","contributorId":64228,"corporation":false,"usgs":true,"family":"Thomas","given":"Cecil","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":146736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lamke, Robert D.","contributorId":24764,"corporation":false,"usgs":true,"family":"Lamke","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":146735,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2517,"text":"wsp1619C - 1962 - Subsidence in the Santa Clara Valley, California: A progress report","interactions":[{"subject":{"id":46033,"text":"ofr5792 - 1957 - Map and graph showing land subsidence and ground-water level in Santa Clara Valley, California","indexId":"ofr5792","publicationYear":"1957","noYear":false,"title":"Map and graph showing land subsidence and ground-water level in Santa Clara Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":2517,"text":"wsp1619C - 1962 - Subsidence in the Santa Clara Valley, California: A progress report","indexId":"wsp1619C","publicationYear":"1962","noYear":false,"chapter":"C","title":"Subsidence in the Santa Clara Valley, California: A progress report"},"id":1}],"lastModifiedDate":"2022-05-11T18:44:50.672005","indexId":"wsp1619C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"C","title":"Subsidence in the Santa Clara Valley, California: A progress report","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1619C","usgsCitation":"Poland, J.F., and Green, J.H., 1962, Subsidence in the Santa Clara Valley, California: A progress report: U.S. Geological Survey Water Supply Paper 1619, iii, 16 p., https://doi.org/10.3133/wsp1619C.","productDescription":"iii, 16 p.","costCenters":[],"links":[{"id":28717,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619c/report-thumb.jpg"},{"id":400532,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24816.htm"}],"country":"United States","state":"California","otherGeospatial":"Santa Clara Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.25,\n 37.25\n ],\n [\n -121.75,\n 37.25\n ],\n [\n -121.75,\n 37.567\n ],\n [\n -122.25,\n 37.567\n ],\n [\n -122.25,\n 37.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b5b","contributors":{"authors":[{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, J. H.","contributorId":43312,"corporation":false,"usgs":true,"family":"Green","given":"J.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":145329,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3723,"text":"cir460B - 1962 - A national network of hydrological benchmarks","interactions":[],"lastModifiedDate":"2017-03-24T15:54:22","indexId":"cir460B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"460","chapter":"B","title":"A national network of hydrological benchmarks","docAbstract":"We are engaged in great national programs of water control and development. An expanding population demands ever-increasing supplies of the natural resources which are to be found in or upon the landscape soil, water, minerals, food, timber, and fiber. By his works, by his extractions, man's mark upon his environment becomes ever deeper, his effects more indelible.
We often read that water tables are falling, that floods are increasing, that springs go dry more often now than in grandfather's time, or that rivers are muddier than before. Such changes, if true, are troublesome but water is a fluctuating resource, responding over time to changes in the environment. A recurring question of our times, and one that we anticipate will be increasingly vexing to posterity, is to know how much of the change in our environment is caused by man and how much is natural. In trying to answer this question we immediately face the insurmountable fact that changes must be measured relative to some standard base or datum. What can we compare against?
The most pervasive and probably the most important of the slow and subtle changes result directly or indirectly from variations in climate. Over a shorter or longer period of time, pulsations in precipitation and temperature change the amounts of water that are evaporated or transpired by the soil and vegetation, the amount of water that replenishes soil water, the quantity of water for recharge to ground water and for riverflow. Climatic variations also cause changes in the pattern of erosion, of which some spectacular consequences can be observed in the arid zones. Changes in climatic pattern, through their effects on the hydrologic cycle, on soil, and on vegetation, can produce results remarkably similar to those effected by the works of man.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir460B","usgsCitation":"Leopold, L.B., 1962, A national network of hydrological benchmarks: U.S. Geological Survey Circular 460, 4 p., https://doi.org/10.3133/cir460B.","productDescription":"4 p.","startPage":"1","endPage":"4","numberOfPages":"7","costCenters":[],"links":[{"id":139231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0460b/report-thumb.jpg"},{"id":30783,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0460b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade1d","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":147484,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3506,"text":"cir468 - 1962 - Ground-water studies and analog models","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir468","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"468","title":"Ground-water studies and analog models","docAbstract":"Hydrologists make ground-water studies to aid managers and users of water resources in solving their problems in the development and management of ground water. Geologic and hydrologic information provides the basic knowledge for construction of electric analog models that portray the ground-water system in miniature. Analog models can be analyzed electrically, and the results of the analysis are presented in terms of the ground-water system so that the effects of alternative methods of water development can be assessed.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir468","usgsCitation":"Robinove, C.J., 1962, Ground-water studies and analog models: U.S. Geological Survey Circular 468, 12 p. :ill. ;27 cm., https://doi.org/10.3133/cir468.","productDescription":"12 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":123185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0468/report-thumb.jpg"},{"id":30520,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0468/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696865","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":147055,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2808,"text":"wsp1619I - 1962 - Pumping tests in the Los Alamos Canyon well field near Los Alamos, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1619I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"I","title":"Pumping tests in the Los Alamos Canyon well field near Los Alamos, New Mexico","language":"ENGLISH","publisher":"United States Government Printing Office,","doi":"10.3133/wsp1619I","usgsCitation":"Theis, C., and Conover, C., 1962, Pumping tests in the Los Alamos Canyon well field near Los Alamos, New Mexico: U.S. Geological Survey Water Supply Paper 1619, iii, 24 p. :ill., maps ;24 cm. & 2 maps in pocket., https://doi.org/10.3133/wsp1619I.","productDescription":"iii, 24 p. :ill., maps ;24 cm. & 2 maps in pocket.","costCenters":[],"links":[{"id":138247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619i/report-thumb.jpg"},{"id":29310,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29311,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29312,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619i/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29313,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649504","contributors":{"authors":[{"text":"Theis, C.V.","contributorId":101641,"corporation":false,"usgs":true,"family":"Theis","given":"C.V.","email":"","affiliations":[],"preferred":false,"id":145828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conover, C.S.","contributorId":79862,"corporation":false,"usgs":true,"family":"Conover","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":145827,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3140,"text":"wsp1708 - 1962 - Surface water supply of the United States, 1960, Part 5, Hudson Bay, Upper Mississippi River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"wsp1708","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1708","title":"Surface water supply of the United States, 1960, Part 5, Hudson Bay, Upper Mississippi River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1708","usgsCitation":"Hendricks, E.L., 1962, Surface water supply of the United States, 1960, Part 5, Hudson Bay, Upper Mississippi River: U.S. Geological Survey Water Supply Paper 1708, xii, 588 p. ;23 cm., https://doi.org/10.3133/wsp1708.","productDescription":"xii, 588 p. ;23 cm.","costCenters":[],"links":[{"id":138867,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1708/report-thumb.jpg"},{"id":30051,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1708/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6942c0","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146323,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68185,"text":"ha26 - 1962 - Availability of ground water in Butler and Ohio Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:13:42","indexId":"ha26","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"26","title":"Availability of ground water in Butler and Ohio Counties, Kentucky","language":"ENGLISH","doi":"10.3133/ha26","usgsCitation":"Maxwell, B.W., and Devaul, R.W., 1962, Availability of ground water in Butler and Ohio Counties, Kentucky: U.S. Geological Survey Hydrologic Atlas 26, 3 col. maps ;56 x 68 cm. (Two maps scale 1:125,000 and generalized columnar section. Sheet 1, 22 1/2 by 30 1/2 inches; sheet 2, 23 by 30 inches; and sheet 3, 20 by 21 inches.), https://doi.org/10.3133/ha26.","productDescription":"3 col. maps ;56 x 68 cm. (Two maps scale 1:125,000 and generalized columnar section. Sheet 1, 22 1/2 by 30 1/2 inches; sheet 2, 23 by 30 inches; and sheet 3, 20 by 21 inches.)","costCenters":[],"links":[{"id":186469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89495,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/026/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89496,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/026/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89497,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/026/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6672c5","contributors":{"authors":[{"text":"Maxwell, Bruce William","contributorId":67489,"corporation":false,"usgs":true,"family":"Maxwell","given":"Bruce","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Devaul, Robert Washburn","contributorId":84338,"corporation":false,"usgs":true,"family":"Devaul","given":"Robert","email":"","middleInitial":"Washburn","affiliations":[],"preferred":false,"id":277799,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":224,"text":"wsp1720 - 1962 - Quantity and quality of surface waters of Alaska, 1960","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1720","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1720","title":"Quantity and quality of surface waters of Alaska, 1960","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1720","usgsCitation":"Hendricks, E.L., and Love, S.K., 1962, Quantity and quality of surface waters of Alaska, 1960: U.S. Geological Survey Water Supply Paper 1720, vi, 122 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1720.","productDescription":"vi, 122 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1720/report-thumb.jpg"},{"id":24835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1720/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64af4f","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142095,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3367,"text":"cir469 - 1962 - Water and the Southwest -- What is the future?","interactions":[],"lastModifiedDate":"2018-01-02T20:01:13","indexId":"cir469","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"469","title":"Water and the Southwest -- What is the future?","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir469","usgsCitation":"Thomas, H.E., 1962, Water and the Southwest -- What is the future?: U.S. Geological Survey Circular 469, iii, 15 p. :maps, diagrs., https://doi.org/10.3133/cir469.","productDescription":"iii, 15 p. :maps, diagrs.","costCenters":[],"links":[{"id":122954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0469/report-thumb.jpg"},{"id":30377,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0469/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa33b","contributors":{"authors":[{"text":"Thomas, H. 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