{"pageNumber":"6797","pageRowStart":"169900","pageSize":"25","recordCount":184858,"records":[{"id":40608,"text":"ofr61132 - 1961 - Claim map, Anderson Mesa quadrangle, Montrose and San Miguel Counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:33","indexId":"ofr61132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-132","title":"Claim map, Anderson Mesa quadrangle, Montrose and San Miguel Counties, Colorado","language":"ENGLISH","doi":"10.3133/ofr61132","usgsCitation":"Sample, R.D., and Albee, H., 1961, Claim map, Anderson Mesa quadrangle, Montrose and San Miguel Counties, Colorado: U.S. Geological Survey Open-File Report 61-132, 1 map., https://doi.org/10.3133/ofr61132.","productDescription":"1 map.","costCenters":[],"links":[{"id":173494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0132/report-thumb.jpg"},{"id":77127,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1961/0132/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e05d5","contributors":{"authors":[{"text":"Sample, Raymond Dewey","contributorId":50587,"corporation":false,"usgs":true,"family":"Sample","given":"Raymond","email":"","middleInitial":"Dewey","affiliations":[],"preferred":false,"id":223600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Albee, Howard F.","contributorId":64252,"corporation":false,"usgs":true,"family":"Albee","given":"Howard F.","affiliations":[],"preferred":false,"id":223601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39780,"text":"pp387A - 1961 - Botanical Evidence of the Modern History of Nisqually Glacier, Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"pp387A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"387","chapter":"A","title":"Botanical Evidence of the Modern History of Nisqually Glacier, Washington","docAbstract":"A knowledge of the areas once occupied by mountain glaciers reveals at least part of the past behavior of these glaciers. From this behavior, inferences of past climate can be drawn. The maximum advance of Nisqually Glacier in the last thousand years was located, and retreat from this point is believed to have started about 1840. The maximum downvalley position of the glacier is marked by either a prominent moraine or by a line of difference between stands of trees of strikingly different size and significantly different age. The thousand-year age of the forest beyond the moraine or line between abutting stands represents the minimum time since the surface was glaciated. This age is based on the age of the oldest trees, plus an estimated interval required for the formation of humus, plus evidence of an ancient fire, plus an interval of deposition of pyroclastics. The estimate of the date when Nisqually Glacier began to retreat from its maximum advance is based upon the ages of the oldest trees plus an interval of 5 years estimated as the time required for the establishment of trees on stable moraines. This interval was derived from a study of the ages of trees growing at locations of known past positions of the glacier.\r\n\r\nReconnaissance studies were made on moraines formed by Emmons and Tahoma Glaciers. Preliminary analyses of these data suggest that Emmons Glacier started to recede from its maximum advance in about 1745. Two other upvalley moraines mark positions from which recession started about 1849 and 1896. Ages of trees near Tahoma Glacier indicate that it started to recede from its position of maximum advance in about 1635. About 1835 Tahoma Glacier started to recede again from another moraine formed by a readvance that ter minated near the 1635 position.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp387A","usgsCitation":"Sigafoos, R.S., and Hendricks, E.L., 1961, Botanical Evidence of the Modern History of Nisqually Glacier, Washington: U.S. Geological Survey Professional Paper 387, p. A1-A20, https://doi.org/10.3133/pp387A.","productDescription":"p. A1-A20","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":124576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0387a/report-thumb.jpg"},{"id":12475,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/pp/387-a/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":67649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0387a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122,46.666666666666664 ], [ -122,47 ], [ -121.25,47 ], [ -121.25,46.666666666666664 ], [ -122,46.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7276","contributors":{"authors":[{"text":"Sigafoos, Robert S.","contributorId":82379,"corporation":false,"usgs":true,"family":"Sigafoos","given":"Robert","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":222150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":222149,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40124,"text":"ofr6184 - 1961 - Copper in the United States","interactions":[{"subject":{"id":40124,"text":"ofr6184 - 1961 - Copper in the United States","indexId":"ofr6184","publicationYear":"1961","noYear":false,"title":"Copper in the United States"},"predicate":"SUPERSEDED_BY","object":{"id":62028,"text":"mr13 - 1962 - Copper in the United States, exclusive of Alaska and Hawaii","indexId":"mr13","publicationYear":"1962","noYear":false,"title":"Copper in the United States, exclusive of Alaska and Hawaii"},"id":1}],"supersededBy":{"id":62028,"text":"mr13 - 1962 - Copper in the United States, exclusive of Alaska and Hawaii","indexId":"mr13","publicationYear":"1962","noYear":false,"title":"Copper in the United States, exclusive of Alaska and Hawaii"},"lastModifiedDate":"2012-02-02T00:10:17","indexId":"ofr6184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-84","title":"Copper in the United States","language":"ENGLISH","doi":"10.3133/ofr6184","usgsCitation":"Kinkel, A.R., and Peterson, N.P., 1961, Copper in the United States: U.S. Geological Survey Open-File Report 61-84, 1 map +text (40 p. ; 28 cm.), https://doi.org/10.3133/ofr6184.","productDescription":"1 map +text (40 p. ; 28 cm.)","costCenters":[],"links":[{"id":170199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ee1","contributors":{"authors":[{"text":"Kinkel, Arthur R. Jr.","contributorId":27440,"corporation":false,"usgs":true,"family":"Kinkel","given":"Arthur","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":223005,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, N. P.","contributorId":29827,"corporation":false,"usgs":true,"family":"Peterson","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":223006,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66188,"text":"i339 - 1961 - Geologic map of the Goodnews quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:17","indexId":"i339","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"339","subseriesTitle":"NONE","title":"Geologic map of the Goodnews quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/i339","usgsCitation":"Hoare, J., and Coonrad, W.L., 1961, Geologic map of the Goodnews quadrangle, Alaska: U.S. Geological Survey IMAP 339, 1 map., https://doi.org/10.3133/i339.","productDescription":"1 map.","costCenters":[],"links":[{"id":102849,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1315.htm","linkFileType":{"id":5,"text":"html"},"description":"1315"},{"id":188476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -162,59 ], [ -162,60 ], [ -159,60 ], [ -159,59 ], [ -162,59 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69863c","contributors":{"authors":[{"text":"Hoare, J. M.","contributorId":52143,"corporation":false,"usgs":true,"family":"Hoare","given":"J. M.","affiliations":[],"preferred":false,"id":274128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coonrad, W. L.","contributorId":69946,"corporation":false,"usgs":true,"family":"Coonrad","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":274129,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":64306,"text":"gp244 - 1961 - Aeromagnetic map of the New Holland quadrangle, Lancaster County, Pennsylvania","interactions":[],"lastModifiedDate":"2021-12-07T19:26:37.671951","indexId":"gp244","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"244","title":"Aeromagnetic map of the New Holland quadrangle, Lancaster County, Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp244","usgsCitation":"Bromery, R.W., and Zandle, G.L., 1961, Aeromagnetic map of the New Holland quadrangle, Lancaster County, Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 244, 1 Plate: 23.28 × 27.65 inches, https://doi.org/10.3133/gp244.","productDescription":"1 Plate: 23.28 × 27.65 inches","costCenters":[],"links":[{"id":250937,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0244/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":254336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0244/report-thumb.jpg"},{"id":392586,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3167.htm"},{"id":250936,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0244/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Pennsylvania","county":"Lancaster County","otherGeospatial":"New Holland quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.125,40 ], [ -76.125,40.125 ], [ -76,40.125 ], [ -76,40 ], [ -76.125,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a7f9","contributors":{"authors":[{"text":"Bromery, Randolph Wilson","contributorId":22746,"corporation":false,"usgs":true,"family":"Bromery","given":"Randolph","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":270510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71101,"text":"wdrWI611 - 1961 - Surface water records of Wisconsin, 1961","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"wdrWI611","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WI-61-1","title":"Surface water records of Wisconsin, 1961","language":"ENGLISH","doi":"10.3133/wdrWI611","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Surface water records of Wisconsin, 1961: U.S. Geological Survey Water Data Report WI-61-1, vi, 143 p., https://doi.org/10.3133/wdrWI611.","productDescription":"vi, 143 p.","numberOfPages":"149","costCenters":[],"links":[{"id":192934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696723","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":534720,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42391,"text":"ofr6130 - 1961 - Preliminary geologic map of the Stewart Flat quadrangle, Caribou County, Idaho","interactions":[{"subject":{"id":42391,"text":"ofr6130 - 1961 - Preliminary geologic map of the Stewart Flat quadrangle, Caribou County, Idaho","indexId":"ofr6130","publicationYear":"1961","noYear":false,"title":"Preliminary geologic map of the Stewart Flat quadrangle, Caribou County, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":35284,"text":"b1217 - 1967 - Geology of the Stewart Flat quadrangle, Caribou County, Idaho","indexId":"b1217","publicationYear":"1967","noYear":false,"title":"Geology of the Stewart Flat quadrangle, Caribou County, Idaho"},"id":1}],"supersededBy":{"id":35284,"text":"b1217 - 1967 - Geology of the Stewart Flat quadrangle, Caribou County, Idaho","indexId":"b1217","publicationYear":"1967","noYear":false,"title":"Geology of the Stewart Flat quadrangle, Caribou County, Idaho"},"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr6130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-30","title":"Preliminary geologic map of the Stewart Flat quadrangle, Caribou County, Idaho","language":"ENGLISH","doi":"10.3133/ofr6130","usgsCitation":"Cheney, T.M., and Schilling, F., 1961, Preliminary geologic map of the Stewart Flat quadrangle, Caribou County, Idaho: U.S. Geological Survey Open-File Report 61-30, 1 map, https://doi.org/10.3133/ofr6130.","productDescription":"1 map","costCenters":[],"links":[{"id":136697,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67ab53","contributors":{"authors":[{"text":"Cheney, Thomas M.","contributorId":52149,"corporation":false,"usgs":true,"family":"Cheney","given":"Thomas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":226392,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schilling, F.A.","contributorId":36111,"corporation":false,"usgs":true,"family":"Schilling","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":226391,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3468,"text":"cir437 - 1961 - Progress in the application of landform analysis in studies of semiarid erosion","interactions":[],"lastModifiedDate":"2018-01-02T20:09:48","indexId":"cir437","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"437","title":"Progress in the application of landform analysis in studies of semiarid erosion","docAbstract":"The analysis of topographic and hydrologic data gathered during studies of erosion in semiarid areas of Western United States show the following relation: (a) Mean annual sediment yield from small drainage basins is related to a ratio of basin relief to length; (b) mean annual runoff from small drainage basins is related to drainage density; (c) mean annual sediment yield per unit area decreases with increase in drainage area; (d) the form of some convex hill slopes is related to surficial creep; (e) asymmetry of drainage basins, including differences in hill-slope erosion and drainage density, is related to microclimatic variations on slopes of diverse exposure; .(f) the cutting of discontinuous gullies is closely related to steepening by deposition of the semiarid valley floor; (g) aggradation in ephemeral streams seems to be most prevalent in reaches where the ratio of contributing drainage area to channel length is relatively small; and (h) streamchannel shape, expressed as a width-depth ratio, is related to the percentage of silt-clay in bed and bank alluvium. The above relations cannot be detected without measurement of terrain characteristics. They further indicate the importance of quantitative terrain analysis in studies of erosion.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir437","usgsCitation":"Schumm, S.A., and Hadley, R.F., 1961, Progress in the application of landform analysis in studies of semiarid erosion: U.S. Geological Survey Circular 437, iii, 14 p. :diagrs., profile. ;27cm., https://doi.org/10.3133/cir437.","productDescription":"iii, 14 p. :diagrs., profile. ;27cm.","costCenters":[],"links":[{"id":30480,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0437/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118117,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0437/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649cc5","contributors":{"authors":[{"text":"Schumm, Stanley Alfred","contributorId":101652,"corporation":false,"usgs":true,"family":"Schumm","given":"Stanley","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":146984,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":146983,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4057,"text":"cir442 - 1961 - Ground-water resources--Development and management","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"cir442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"442","title":"Ground-water resources--Development and management","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir442","usgsCitation":"Conover, C.S., 1961, Ground-water resources--Development and management: U.S. Geological Survey Circular 442, 7 p. ;27 cm., https://doi.org/10.3133/cir442.","productDescription":"7 p. ;27 cm.","costCenters":[],"links":[{"id":117098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0442/report-thumb.jpg"},{"id":31151,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0442/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a3ab","contributors":{"authors":[{"text":"Conover, Clyde Stuart","contributorId":42197,"corporation":false,"usgs":true,"family":"Conover","given":"Clyde","email":"","middleInitial":"Stuart","affiliations":[],"preferred":false,"id":148086,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23879,"text":"ofr6196 - 1961 - Water levels in observation wells in Santa Barbara County, California, in 1960","interactions":[{"subject":{"id":23879,"text":"ofr6196 - 1961 - Water levels in observation wells in Santa Barbara County, California, in 1960","indexId":"ofr6196","publicationYear":"1961","noYear":false,"title":"Water levels in observation wells in Santa Barbara County, California, in 1960"},"predicate":"SUPERSEDED_BY","object":{"id":95,"text":"wsp1770 - 1963 - Ground-water levels in the United States, 1956-60, southwestern states","indexId":"wsp1770","publicationYear":"1963","noYear":false,"title":"Ground-water levels in the United States, 1956-60, southwestern states"},"id":1}],"supersededBy":{"id":95,"text":"wsp1770 - 1963 - Ground-water levels in the United States, 1956-60, southwestern states","indexId":"wsp1770","publicationYear":"1963","noYear":false,"title":"Ground-water levels in the United States, 1956-60, southwestern states"},"lastModifiedDate":"2024-07-30T13:51:40.155402","indexId":"ofr6196","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-96","title":"Water levels in observation wells in Santa Barbara County, California, in 1960","docAbstract":"<p>Investigation of the ground-water resources of Santa Barbara County was continued during 1960 by the U. S. Geological Survey in cooperation with the Santa Barbara County Water Agency. Monthly water-level measurements were made in 193 wells, in 9 of which automatic water-level recorders were operated. Earlier measurements, covering the period 1941 through 1955, have been published in Geological Survey Water-Supply Papers; those for 1956, 1957, 1958, and 1959 have been released locally in duplicated form. Water-Supply Paper 1068 contains tabulated descriptions of 2,246 wells in existence in 1942 in the several ground-water basins of the county. The same publication also contains many water-level measurements made prior to 1942 by the city of Santa Barbara, Santa Maria Valley Voter Conservation District, San Joaquin Power Division of the Pacific Gas and Electric Co., Union Sugar Co., Union Oil Co., and other organizations and individuals.</p><p>Comprehensive reports on the geology and ground-water resources of the Santa Ynez River basin (Upson and Thomasson, 1951, and Wilson, 1959), the south-coast basins (Upson, 1951), the Santa Maria Valley area (Worts, 1951), and the Cuyama Valley (Upson and Worts, 1951) have been published as Water-Supply Papers 1107, 1467, 1108, 1000, and 1110-B, respectively. A similar report on the San Antonio Creek Valley is in preparation. 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