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Carolina\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6696e0","contributors":{"authors":[{"text":"White, Amos McNairy","contributorId":27465,"corporation":false,"usgs":true,"family":"White","given":"Amos","email":"","middleInitial":"McNairy","affiliations":[],"preferred":false,"id":172980,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64423,"text":"gp339 - 1962 - Aeromagnetic map of parts of the Monroe and Maybrook quadrangles, Orange County, New York","interactions":[],"lastModifiedDate":"2012-02-10T00:10:53","indexId":"gp339","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"339","title":"Aeromagnetic map of parts of the Monroe and Maybrook quadrangles, Orange County, New York","language":"ENGLISH","doi":"10.3133/gp339","usgsCitation":"Henderson, J.R., and Smith, F.C., 1962, Aeromagnetic map of parts of the Monroe and Maybrook quadrangles, Orange County, New York: U.S. Geological Survey Geophysical Investigations Map 339, 1 map., https://doi.org/10.3133/gp339.","productDescription":"1 map.","costCenters":[],"links":[{"id":251147,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0339/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":251148,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0339/plate-1.pdf","size":"2771","linkFileType":{"id":1,"text":"pdf"}},{"id":251969,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0339/report-thumb.jpg"}],"scale":"680","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.25,41.25 ], [ -74.25,41.416666666666664 ], [ -74.11749999999999,41.416666666666664 ], [ -74.11749999999999,41.25 ], [ -74.25,41.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6975dc","contributors":{"authors":[{"text":"Henderson, J. R.","contributorId":78705,"corporation":false,"usgs":true,"family":"Henderson","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, F. C.","contributorId":45783,"corporation":false,"usgs":true,"family":"Smith","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":270872,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63597,"text":"gp408 - 1962 - Airborne-radioactivity survey of the northern part of the Shelby quadrangle, Cleveland and Rutherford Counties, North Carolina","interactions":[],"lastModifiedDate":"2012-02-10T00:10:58","indexId":"gp408","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"408","title":"Airborne-radioactivity survey of the northern part of the Shelby quadrangle, Cleveland and Rutherford Counties, North Carolina","language":"ENGLISH","doi":"10.3133/gp408","isbn":"0607734248","usgsCitation":"Overstreet, W., Meuschke, J.L., and Moxham, R., 1962, Airborne-radioactivity survey of the northern part of the Shelby quadrangle, Cleveland and Rutherford Counties, North Carolina: U.S. Geological Survey Geophysical Investigations Map 408, 1 map., https://doi.org/10.3133/gp408.","productDescription":"1 map.","costCenters":[],"links":[{"id":104151,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3348.htm","linkFileType":{"id":5,"text":"html"},"description":"3348"},{"id":186969,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.75,35.3675 ], [ -81.75,35.5 ], [ -81.5,35.5 ], [ -81.5,35.3675 ], [ -81.75,35.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688f71","contributors":{"authors":[{"text":"Overstreet, W.C.","contributorId":105294,"corporation":false,"usgs":true,"family":"Overstreet","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":269201,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meuschke, J. L.","contributorId":53349,"corporation":false,"usgs":true,"family":"Meuschke","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":269200,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moxham, R.M.","contributorId":42234,"corporation":false,"usgs":true,"family":"Moxham","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":269199,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1987,"text":"wsp1539S - 1962 - Water in the Coconino sandstone for the Snowflake-Hay Hollow area, Navajo County, Arizona","interactions":[],"lastModifiedDate":"2022-12-19T19:46:02.249571","indexId":"wsp1539S","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":"1539","chapter":"S","title":"Water in the Coconino sandstone for the Snowflake-Hay Hollow area, Navajo County, Arizona","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539S","usgsCitation":"Johnson, P.W., 1962, Water in the Coconino sandstone for the Snowflake-Hay Hollow area, Navajo County, Arizona: U.S. Geological Survey Water Supply Paper 1539, Report: iv, 46 p.; 4 Plates: 18.00 × 19.15 inches or smaller, https://doi.org/10.3133/wsp1539S.","productDescription":"Report: iv, 46 p.; 4 Plates: 18.00 × 19.15 inches or smaller","costCenters":[],"links":[{"id":27375,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539s/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27374,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539s/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27373,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539s/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109985,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24740.htm","linkFileType":{"id":5,"text":"html"},"description":"24740"},{"id":27376,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539s/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27372,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539s/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539s/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Navajo County","otherGeospatial":"Snowflake-Hay Hollow area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.846,\n 34.732\n ],\n [\n -109.846,\n 34.307\n ],\n [\n -110.272,\n 34.307\n ],\n [\n -110.272,\n 34.732\n ],\n [\n -109.846,\n 34.732\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa0d7","contributors":{"authors":[{"text":"Johnson, Phillip W.","contributorId":27422,"corporation":false,"usgs":true,"family":"Johnson","given":"Phillip","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144480,"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":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":3054,"text":"wsp1702 - 1962 - Surface water supply of the United States, 1960, Part 1-B, North Atlantic slope basins, New York to York River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp1702","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":"1702","title":"Surface water supply of the United States, 1960, Part 1-B, North Atlantic slope basins, New York to York River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1702","usgsCitation":"Hendricks, E.L., 1962, Surface water supply of the United States, 1960, Part 1-B, North Atlantic slope basins, New York to York River: U.S. Geological Survey Water Supply Paper 1702, xi, 567 p. ;23 cm., https://doi.org/10.3133/wsp1702.","productDescription":"xi, 567 p. ;23 cm.","costCenters":[],"links":[{"id":139335,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1702/report-thumb.jpg"},{"id":29908,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1702/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6943b2","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146212,"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":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.

\n

The 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.

\n

An 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.

\n

Thermographs 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.

\n

The 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.

\n

The infiltration of relatively warm spring and summer rainfall can be detected on the thermographs of all the wells.

\n

The 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":3198,"text":"wsp1544C - 1962 - Methods of flow measurement in well bores","interactions":[],"lastModifiedDate":"2022-07-19T11:31:11.072932","indexId":"wsp1544C","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":"C","title":"Methods of flow measurement in well bores","docAbstract":"

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":3259,"text":"cir464 - 1962 - Floods in New Mexico, magnitude and frequency","interactions":[],"lastModifiedDate":"2018-01-02T20:01:15","indexId":"cir464","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":"464","title":"Floods in New Mexico, magnitude and frequency","docAbstract":"This report presents a method of determining the magnitude and frequency of floods that can be expected in New Mexico The discharge of the mean annual flood for various regions in the State is defined. Curves relate mean annual flood and drainage area. Drainage area was the only basin characteristic found to have an appreciable effect on discharge of the mean annual flood except in two regions where a relation with altitude also is defined. Composite frequency curves relate discharge of the mean annual flood to the discharge of floods having recurrence intervals from 1.1 to 50 years. These relationships are based on records 5 or more years in length from gaging stations that had flow essentially unregulated.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir464","usgsCitation":"Wiard, L.A., 1962, Floods in New Mexico, magnitude and frequency: U.S. Geological Survey Circular 464, 13 p. :col. map, diagrs. ;27 cm., https://doi.org/10.3133/cir464.","productDescription":"13 p. :col. map, diagrs. ;27 cm.","costCenters":[],"links":[{"id":122608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1962/0464/report-thumb.jpg"},{"id":30254,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1962/0464/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e700b","contributors":{"authors":[{"text":"Wiard, Leon A.","contributorId":99538,"corporation":false,"usgs":true,"family":"Wiard","given":"Leon","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":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":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":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. 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