{"pageNumber":"2650","pageRowStart":"66225","pageSize":"25","recordCount":68826,"records":[{"id":51568,"text":"ofr53247 - 1953 - Ground-water supply for the Battle Mountain Sanitarium, Hot Springs, South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:11:31","indexId":"ofr53247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-247","title":"Ground-water supply for the Battle Mountain Sanitarium, Hot Springs, South Dakota","language":"ENGLISH","doi":"10.3133/ofr53247","usgsCitation":"Simmons, C., and LaRocque, G., 1953, Ground-water supply for the Battle Mountain Sanitarium, Hot Springs, South Dakota: U.S. Geological Survey Open-File Report 53-247, 4 p., https://doi.org/10.3133/ofr53247.","productDescription":"4 p.","costCenters":[],"links":[{"id":178330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a50b","contributors":{"authors":[{"text":"Simmons, C.B.","contributorId":16910,"corporation":false,"usgs":true,"family":"Simmons","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":243952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaRocque, G.A. Jr.","contributorId":22837,"corporation":false,"usgs":true,"family":"LaRocque","given":"G.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":243953,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":12528,"text":"ofr538 - 1953 - Stratigraphic relationships of Cretaceous and early Tertiary rocks of a part of northwestern San Juan basin","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr538","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-8","title":"Stratigraphic relationships of Cretaceous and early Tertiary rocks of a part of northwestern San Juan basin","docAbstract":"The Bridge Timber Mountain area in south-central La Plata County, southwestern Colorado lies mostly in the northwestern part of the Central San Juan Basin but contains a segment of the bounding Hogback 'monocline' and Four-Corners platform. \r\n\r\nThe area contains rocks of late Cretaceous through early Eocene age, as well as Pliocene, Pleistocene, and Recent terrace and pediment gravels. The Pictured Cliffs sandstone of late Montana age is the latest marine formation present. Retreat of the Cretaceous seas from the area marked the beginning of Laramide orogenic activity and the earliest stages of deformation which produced the modern San Juan Basin. The Fruitland formation and Kirtland shale were deposited in brackish water and on coastal plains left by the retreating Cretaceous sea. Beds of the Farmington sandstone member and upper shale member of the Kirtland shale show evidence of a new source of sediments to the north or northeast distinct from the southwestern source area of older Cretaceous rocks. The McDermott 'formation', composed mainly of volcanic debris, is considered to be a local lower member of the Animas formation. Beds of the upper member of the Animas formation of Cretaceous and Paleocene age are considered to extend entirely across the area and into New Mexico. Overstep of higher sandstone and shale beds of the upper member across lower conglomeratic beds shows that folding on the Hogback 'monocline' began during deposition of the upper member. Beds of the upper member of the Animas formation grade laterally southward into Paleocene beds of the Nacimiento formation, but upper Nacimiento beds overstep folded beds of the Animas formation on the Hogback 'monocline' at the north end of Bridge Timber Mountain. The San Jose formation of Paleocene and Eocene age is conformable with the Nacimiento formation except at the north end of Bridge Timber Mountain where upper San Jose beds overstep all older tilted beds down to the Fruitland formation. The heavy sandstone facies of the Nacimiento and San Jose formations are correlated with similar facies of these formations on the east side of the San Juan Basin. Folding along the borders of the Central basin was completed prior to deposition of the youngest San Joss beds, and they were probably widely distributed outside of the Central Basin in Eocene time. In Pliocene time, the San Juan region was beveled by the San Juan peneplain. Rejuvenation of the San Juan Mountains in late Pliocene time caused erosion in the mountains and deposition of the Bridgetimber gravel in the San Juan Basin. Uplift in Pleistocene time caused large-scale erosion in the Bridge Timber Mountain area and gravel-covered terraces represent the various stages of uplift and erosion. \r\n\r\nThe stratigraphic relationships of uppermost Cretaceous and lower Tertiary rocks in the Bridge Timber Mountain area are similar to recently described relationships of equivalent rocks in other parts of the San Juan Basin. The southwestern lobe of the Pictured Cliffs sandstone was derived from older Cretaceous source areas to the southwest and deposited in the seaway which was retreating northeastward. The northeastern lobe consists of reworked Cretaceous sediments eroded from the flanks of the rising San Juan zone and Sangre de Cristo upwarp and deposited in an arm of the sea which was isolated by uplift of the mountain masses. This arm of the sea was forced to retreat to the southeast as sediments of the Fruitland, Kirtland, Animas, and Ojo Alamo formations were deposited in' the basin. The Animas formation which was derived from hi6hlands to the northeast spread progressively to the southwest and interfingered with lesser amounts of Fruitland and Kirtland sediments derived from the southwest. In latest Cretaceous or earliest Paleocene time folding began along the Hogback 'monocline' in northern and western San Juan Basin and sediments were eroded from the uplifted platforms around the margin of the Central Basin and rede","language":"ENGLISH","publisher":"University of New Mexico,","doi":"10.3133/ofr538","usgsCitation":"Baltz, E.H., 1953, Stratigraphic relationships of Cretaceous and early Tertiary rocks of a part of northwestern San Juan basin: U.S. Geological Survey Open-File Report 53-8, 80 p., https://doi.org/10.3133/ofr538.","productDescription":"80 p.","costCenters":[],"links":[{"id":144527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0008/report-thumb.jpg"},{"id":40780,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0008/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40781,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0008/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40782,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0008/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae2ed","contributors":{"authors":[{"text":"Baltz, Elmer Harold Jr.","contributorId":27062,"corporation":false,"usgs":true,"family":"Baltz","given":"Elmer","suffix":"Jr.","email":"","middleInitial":"Harold","affiliations":[],"preferred":false,"id":166282,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46653,"text":"ofr5329 - 1953 - Geologic map of the Smelterville and vicinity quadrangle, Idaho","interactions":[{"subject":{"id":46653,"text":"ofr5329 - 1953 - Geologic map of the Smelterville and vicinity quadrangle, Idaho","indexId":"ofr5329","publicationYear":"1953","noYear":false,"title":"Geologic map of the Smelterville and vicinity quadrangle, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":6042,"text":"pp478 - 1965 - Geology of the Coeur d'Alene district, Shoshone County, Idaho","indexId":"pp478","publicationYear":"1965","noYear":false,"title":"Geology of the Coeur d'Alene district, Shoshone County, Idaho"},"id":1}],"supersededBy":{"id":6042,"text":"pp478 - 1965 - Geology of the Coeur d'Alene district, Shoshone County, Idaho","indexId":"pp478","publicationYear":"1965","noYear":false,"title":"Geology of the Coeur d'Alene district, Shoshone County, Idaho"},"lastModifiedDate":"2019-04-30T14:56:32","indexId":"ofr5329","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-29","title":"Geologic map of the Smelterville and vicinity quadrangle, Idaho","docAbstract":"

No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5329","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Geologic map of the Smelterville and vicinity quadrangle, Idaho: U.S. Geological Survey Open-File Report 53-29, 1 map: 30 x 24 cm., https://doi.org/10.3133/ofr5329.","productDescription":"1 map: 30 x 24 cm.","costCenters":[],"links":[{"id":173156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0029/report-thumb.jpg"},{"id":363391,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0029/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a78c","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":531696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":72441,"text":"tei280 - 1953 - Trace elements research quarterly progress report - April 1 to June 30, 1952","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"tei280","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"280","title":"Trace elements research quarterly progress report - April 1 to June 30, 1952","language":"ENGLISH","doi":"10.3133/tei280","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Trace elements research quarterly progress report - April 1 to June 30, 1952: U.S. Geological Survey Trace Elements Investigations 280, 93 p., https://doi.org/10.3133/tei280.","productDescription":"93 p.","costCenters":[],"links":[{"id":193262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/280/report-thumb.jpg"},{"id":91154,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/280/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627cb5","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":534750,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2563,"text":"wsp1140 - 1953 - Geology and ground-water resources of the Egbert-Pine Bluffs-Carpenter area, Laramie County, Wyoming","interactions":[],"lastModifiedDate":"2023-01-11T20:13:35.023182","indexId":"wsp1140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"1140","title":"Geology and ground-water resources of the Egbert-Pine Bluffs-Carpenter area, Laramie County, Wyoming","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1140","usgsCitation":"Rapp, J.R., Warner, D.A., and Morgan, A.M., 1953, Geology and ground-water resources of the Egbert-Pine Bluffs-Carpenter area, Laramie County, Wyoming: U.S. Geological Survey Water Supply Paper 1140, Report: v, 67 p.; 3 Plates: 17.00 x 16.34 inches or smaller, https://doi.org/10.3133/wsp1140.","productDescription":"Report: v, 67 p.; 3 Plates: 17.00 x 16.34 inches or smaller","costCenters":[],"links":[{"id":411733,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24234.htm","linkFileType":{"id":5,"text":"html"}},{"id":28829,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1140/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28828,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1140/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28827,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1140/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28826,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1140/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138582,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1140/report-thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Laramie County","otherGeospatial":"Egbert-Pine Bluffs-Carpenter area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -104.475,\n 41.304\n ],\n [\n -104.475,\n 41\n ],\n [\n -104.057,\n 41\n ],\n [\n -104.057,\n 41.304\n ],\n [\n -104.475,\n 41.304\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6855fc","contributors":{"authors":[{"text":"Rapp, J. R.","contributorId":29394,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145402,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warner, D. A.","contributorId":67160,"corporation":false,"usgs":true,"family":"Warner","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145403,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morgan, Arthur Mitchell","contributorId":92104,"corporation":false,"usgs":true,"family":"Morgan","given":"Arthur","email":"","middleInitial":"Mitchell","affiliations":[],"preferred":false,"id":145404,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":51589,"text":"ofr53275 - 1953 - Geophysical and geological reconnaissance to determine ground-water resources of Chiu Chiuschu area, Papago Indian Reservation, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:11:27","indexId":"ofr53275","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-275","title":"Geophysical and geological reconnaissance to determine ground-water resources of Chiu Chiuschu area, Papago Indian Reservation, Arizona","language":"ENGLISH","doi":"10.3133/ofr53275","usgsCitation":"Yost, C., 1953, Geophysical and geological reconnaissance to determine ground-water resources of Chiu Chiuschu area, Papago Indian Reservation, Arizona: U.S. Geological Survey Open-File Report 53-275, 25 p., 3 plates, https://doi.org/10.3133/ofr53275.","productDescription":"25 p., 3 plates","costCenters":[],"links":[{"id":179364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0275/report-thumb.jpg"},{"id":86554,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0275/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86555,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0275/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86556,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0275/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86557,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0275/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86558,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0275/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c29d","contributors":{"authors":[{"text":"Yost, Coyd B. Jr.","contributorId":19631,"corporation":false,"usgs":true,"family":"Yost","given":"Coyd B.","suffix":"Jr.","affiliations":[],"preferred":false,"id":243994,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2692,"text":"wsp1220 - 1953 - Irrigation and streamflow depletion in Columbia River basin above The Dalles, Oregon","interactions":[],"lastModifiedDate":"2023-09-27T20:37:28.914126","indexId":"wsp1220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"1220","title":"Irrigation and streamflow depletion in Columbia River basin above The Dalles, Oregon","docAbstract":"The Columbia River is the largest stream in western United States. Above The Dalles, Oregon, it drains an area of 237,000 square miles, of which 39,000 square miles is in Canada. This area is largely mountainous and lies between the Rocky Mountains and the Cascade Range. The Kootenai, Pend Oreille, and Snake Rivers are the principal tributaries. Precipitation varies from 7 inches near Kennewick, Wash. to over 100 inches in some of the mountainous regions. Most of the runoff occurs in the spring and summer months as a result of melting snow. Precipitation is generally light during the summer months, and irrigation is necessary for sustained crop production. \r\n\r\nHistorical data indicate that irrigation in the Columbia River basin began prior to 1840 at the site of missions established near Walla Walla, Wash. and Lewiston, Idaho. During the next half century the increase in irrigated area was slow and by 1890 included only 506,000 acres. The period 1890 to 1910 was marked by phenomenal increase to a total of 2,276,000 acres in 1910. Since that time there has been more gradual addition to a total of 4,004,S00 acres of irrigated land in 1946 in the Columbia River basin above The Dalles, Oreg. Of this total 918,000 acres were located in the Columbia Basin above the mouth of the Snake River; 2,830,000 acres in the Snake River basin, and the balance, 256,000 acres below the mouth of the Snake River. \r\n\r\nValues of net consumptive use were determined or estimated for various tributary basins of the Columbia River basin and compared to available experimental data. These values were then used to compute the average depletion which could be directly attributed to irrigation. The yield of a drainage basin was considered to be the rum of the ob- served runoff and the estimated depletion. For purposes of comparison, the depletion was expressed both in terms of acre-feet and as a percentage of the yield of the basin. This percentage depletion varied from less than 1 percent for many tributary basins to 53 percent for the portion of the Snake River basin between Heise and King Hill, Idaho. For the Columbia River near The Dalles, Oreg., the average depletion during the period 1921 through 1945, amounted to 4,7 percent of the yield and the depletion represented by the 1946 stage of irrigation development amounted to 5.3 percent of the long-term yield.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1220","usgsCitation":"Simons, W.D., 1953, Irrigation and streamflow depletion in Columbia River basin above The Dalles, Oregon: U.S. Geological Survey Water Supply Paper 1220, iv, 126 p., https://doi.org/10.3133/wsp1220.","productDescription":"iv, 126 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":138818,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1220/report-thumb.jpg"},{"id":421287,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24239.htm","linkFileType":{"id":5,"text":"html"}},{"id":29049,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1220/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -112,\n 49\n ],\n [\n -121.25,\n 49\n ],\n [\n -121.25,\n 42\n ],\n [\n -112,\n 42\n ],\n [\n -112,\n 49\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db6618fa","contributors":{"authors":[{"text":"Simons, Wilbur Douglas","contributorId":102469,"corporation":false,"usgs":true,"family":"Simons","given":"Wilbur","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":145619,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":167,"text":"wsp1132 - 1953 - Quality of surface waters of the United States, 1948, parts 1-6","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp1132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"1132","title":"Quality of surface waters of the United States, 1948, parts 1-6","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1132","usgsCitation":"Paulsen, C.G., 1953, Quality of surface waters of the United States, 1948, parts 1-6: U.S. Geological Survey Water Supply Paper 1132, ix, 515 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1132.","productDescription":"ix, 515 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":137272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1132/report-thumb.jpg"},{"id":24778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1132/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651c20","contributors":{"authors":[{"text":"Paulsen, C. G.","contributorId":96239,"corporation":false,"usgs":true,"family":"Paulsen","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":142038,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42837,"text":"ofr53138 - 1953 - Preliminary geologic map of Tiger Butte, Glasgow quadrangle, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr53138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-138","title":"Preliminary geologic map of Tiger Butte, Glasgow quadrangle, Montana","language":"ENGLISH","doi":"10.3133/ofr53138","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Preliminary geologic map of Tiger Butte, Glasgow quadrangle, Montana: U.S. Geological Survey Open-File Report 53-138, 1 map :photocopy ;39 x 51 cm., on sheet 68 x 81cm., https://doi.org/10.3133/ofr53138.","productDescription":"1 map :photocopy ;39 x 51 cm., on sheet 68 x 81cm.","costCenters":[],"links":[{"id":136503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80664,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0138/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf2b","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":530943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51374,"text":"ofr53218 - 1953 - Remarks on the program of the Water Resources Division, U. S. Geology Survey, and water problems in California, made before the Association of American State Geologists, Feb. 14, 1953, Los Angeles, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:33","indexId":"ofr53218","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-218","title":"Remarks on the program of the Water Resources Division, U. S. Geology Survey, and water problems in California, made before the Association of American State Geologists, Feb. 14, 1953, Los Angeles, California","language":"ENGLISH","doi":"10.3133/ofr53218","usgsCitation":"Poland, J.F., 1953, Remarks on the program of the Water Resources Division, U. S. Geology Survey, and water problems in California, made before the Association of American State Geologists, Feb. 14, 1953, Los Angeles, California: U.S. Geological Survey Open-File Report 53-218, 2 p., https://doi.org/10.3133/ofr53218.","productDescription":"2 p.","costCenters":[],"links":[{"id":177152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bfa1","contributors":{"authors":[{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":243414,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51292,"text":"ofr53121 - 1953 - Fifth progress report on the cooperative investigation of springs and streamflow in the Tecolote Tunnel area of Santa Barbara County, California","interactions":[],"lastModifiedDate":"2024-08-06T14:09:42.939311","indexId":"ofr53121","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-121","title":"Fifth progress report on the cooperative investigation of springs and streamflow in the Tecolote Tunnel area of Santa Barbara County, California","docAbstract":"

This report is the fifth in a continuing series of annual progress reports giving the results of discharge measurements made at more than 120 selected sites in the \"Tecolote Tunnel Area\" of the Santa Ynez Mountains. This area derives its name from the tunnel now being built by the Bureau of Reclamation for the purpose of diverting the flood waters of the Santa Ynez River as stored in Cachuma Reservoir to the city of Santa Barbara and adjacent coastal communities. The tunnel alignment is roughly north and south through the center of this area, which extends from Refugio Pass on the west to San Marcos Pass and the Painted Cave area on the east.

The program of measuring the developed springs and headwater streams in the Tecolote Tunnel area was started on its present scale in the latter part of 1948 at the request of the Santa Barbara County Water Agency. The primary purpose of the program is to obtain sufficient factual data to determine what effect, if any, the construction and use of the Tecolote Tunnel will have on the outflow of the springs in the area. The area covered by this study was made large enough to include all springs that could possibly be affected by the tunnel, as well as springs believed to be outside the zone of influence. The program is being carried on by the Geological Survey under a cooperative agreement with the Santa Barbara County Water Agency whereby each pays one half the cost.

Prior to January 1953 the flow at each of the more than 120 locations was generally measured monthly. Since then, the number of sites at which monthly measurements are made has been reduced to about 40, with measurements made every other month or quarterly at the remaining locations. The purpose of this report is to make available the factual data obtained from May 1, 1952 to June 30, 1953.

","language":"English","doi":"10.3133/ofr53121","collaboration":"Prepared in cooperation with the Santa Barbara County Water Agency","usgsCitation":"Hofmann, W., 1953, Fifth progress report on the cooperative investigation of springs and streamflow in the Tecolote Tunnel area of Santa Barbara County, California: U.S. Geological Survey Open-File Report 53-121, Report: 156 p.; 1 Plate: 25.52 x 19.41 inches, https://doi.org/10.3133/ofr53121.","productDescription":"Report: 156 p.; 1 Plate: 25.52 x 19.41 inches","costCenters":[],"links":[{"id":432279,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0121/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179365,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0121/report-thumb.jpg"},{"id":432278,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0121/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"50000","country":"United States","state":"California","county":"Santa Barbara County","otherGeospatial":"Tecolote Tunnel","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.61474653419313,\n 35.107477322182945\n ],\n [\n -120.61474653419313,\n 33.603227658961316\n ],\n [\n -119.21258359397822,\n 33.603227658961316\n ],\n [\n -119.21258359397822,\n 35.107477322182945\n ],\n [\n -120.61474653419313,\n 35.107477322182945\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f497c","contributors":{"authors":[{"text":"Hofmann, Walter","contributorId":30604,"corporation":false,"usgs":true,"family":"Hofmann","given":"Walter","email":"","affiliations":[],"preferred":false,"id":243277,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23331,"text":"ofr53109 - 1953 - Water power of the coast streams of Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:08:11","indexId":"ofr53109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-109","title":"Water power of the coast streams of Oregon","language":"ENGLISH","publisher":"United States Department of the Interior, Geological Survey,","doi":"10.3133/ofr53109","issn":"0094-9140","usgsCitation":"Helland, R., 1953, Water power of the coast streams of Oregon: U.S. Geological Survey Open-File Report 53-109, 46 p, https://doi.org/10.3133/ofr53109.","productDescription":"46 p","costCenters":[],"links":[{"id":156203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9cee","contributors":{"authors":[{"text":"Helland, Randolph O.","contributorId":55473,"corporation":false,"usgs":true,"family":"Helland","given":"Randolph O.","affiliations":[],"preferred":false,"id":189919,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51583,"text":"ofr53267 - 1953 - Modification of the electric tape for measuring water levels in wells","interactions":[],"lastModifiedDate":"2012-02-02T00:11:28","indexId":"ofr53267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-267","title":"Modification of the electric tape for measuring water levels in wells","language":"ENGLISH","doi":"10.3133/ofr53267","usgsCitation":"Waterman, W., 1953, Modification of the electric tape for measuring water levels in wells: U.S. Geological Survey Open-File Report 53-267, 2 p., https://doi.org/10.3133/ofr53267.","productDescription":"2 p.","costCenters":[],"links":[{"id":178393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69956a","contributors":{"authors":[{"text":"Waterman, W.D.","contributorId":103353,"corporation":false,"usgs":true,"family":"Waterman","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":243972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51582,"text":"ofr53266 - 1953 - Water levels in observation wells in Santa Barbara County, California, in 1952","interactions":[{"subject":{"id":51582,"text":"ofr53266 - 1953 - Water levels in observation wells in Santa Barbara County, California, in 1952","indexId":"ofr53266","publicationYear":"1953","noYear":false,"title":"Water levels in observation wells in Santa Barbara County, California, in 1952"},"predicate":"SUPERSEDED_BY","object":{"id":810,"text":"wsp1226 - 1955 - Water levels and artesian pressures in observation wells in the United States in 1952: Part 6, southwestern states and territory of Hawaii","indexId":"wsp1226","publicationYear":"1955","noYear":false,"title":"Water levels and artesian pressures in observation wells in the United States in 1952: Part 6, southwestern states and territory of Hawaii"},"id":1}],"supersededBy":{"id":810,"text":"wsp1226 - 1955 - Water levels and artesian pressures in observation wells in the United States in 1952: Part 6, southwestern states and territory of Hawaii","indexId":"wsp1226","publicationYear":"1955","noYear":false,"title":"Water levels and artesian pressures in observation wells in the United States in 1952: Part 6, southwestern states and territory of Hawaii"},"lastModifiedDate":"2012-02-02T00:11:28","indexId":"ofr53266","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-266","title":"Water levels in observation wells in Santa Barbara County, California, in 1952","language":"ENGLISH","doi":"10.3133/ofr53266","usgsCitation":"Waller, R., and Wilson, H., 1953, Water levels in observation wells in Santa Barbara County, California, in 1952 (Superceded by: W-1226): U.S. Geological Survey Open-File Report 53-266, 20 p., 9 plates, https://doi.org/10.3133/ofr53266.","productDescription":"20 p., 9 plates","costCenters":[],"links":[{"id":178392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superceded by: W-1226","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9da1","contributors":{"authors":[{"text":"Waller, R.M.","contributorId":13659,"corporation":false,"usgs":true,"family":"Waller","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":243970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, H.D. Jr.","contributorId":51370,"corporation":false,"usgs":true,"family":"Wilson","given":"H.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":243971,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":51579,"text":"ofr53259 - 1953 - Memorandum on ground water for public supply at the Canoncito Reservation Day School, Bernalillo County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:11:28","indexId":"ofr53259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-259","title":"Memorandum on ground water for public supply at the Canoncito Reservation Day School, Bernalillo County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr53259","usgsCitation":"Trauger, F., 1953, Memorandum on ground water for public supply at the Canoncito Reservation Day School, Bernalillo County, New Mexico: U.S. Geological Survey Open-File Report 53-259, 11 p., https://doi.org/10.3133/ofr53259.","productDescription":"11 p.","costCenters":[],"links":[{"id":178389,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613d7e","contributors":{"authors":[{"text":"Trauger, F.D.","contributorId":102520,"corporation":false,"usgs":true,"family":"Trauger","given":"F.D.","email":"","affiliations":[],"preferred":false,"id":243966,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3494,"text":"cir201 - 1953 - Ground-water resources of the Rapid Valley unit, Cheyenne Division, South Dakota, with a section on the surface waters of Rapid Valley","interactions":[],"lastModifiedDate":"2019-11-07T11:52:05","indexId":"cir201","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"201","title":"Ground-water resources of the Rapid Valley unit, Cheyenne Division, South Dakota, with a section on the surface waters of Rapid Valley","docAbstract":"

The Rapid Valley unit is in Pennington County, S. Dak., and extends from the east city limits of Rapid City southeastward for 21 miles along Rapid Creek.

\n

The bedrock formations that underlie the region are chiefly marine in origin, and they generally dip eastward from the center of the Black Hills uplift. The exposed formations are of Cretaceous age and consist of the Greenhorn limestone, the Carlile shale, the Niobrara formation, and the Pierre shale. The Pierre shale, which underlies the unconsolidated flood plain and terrace deposits in much Of the region is exposed in the erosional slopes along the south side of the valley and in the deeper draws on the north side. The areas in which the other formations are exposed are relatively small and are restricted to the western part of-the region.

\n

Four terraces are present on the north side of Rapid Creek. The lowest terrace and the flood plain in the western half of the region are irrigated at the present time, and the two lower terraces and the flood plain in the eastern half have been proposed for irrigation.

\n

Abundant supplies of ground water occur in the flood plain and terrace deposits where they are now irrigated. Because the waterbearing materials consist of interfingering layers of differing permeability, the ground water is under water-table conditions in some places whereas it is confined in others.

\n

Locally, where there is a confining layer below other water-bearing materials or where a confined layer is itself saturated, the ground water may occur under both water-table and artesian conditions. Seepage from irrigation canals, which is the principal source of recharge, causes high ground-water levels from June to November; as a result, parts of the areas have become waterlogged. In the parts of the region that are not now affected by irrigation, the surface of the ground water is only a few feet above the bedrock surface and 6 ft to 42 ft below land surface; its position is relatively constant throughout the year.

\n

Harmful concentrations of salt in the soil are in part due to evaporation of ground water. These are found only locally in the Rapid Valley region and do not present a serious problem at this time. It is thought, however, that the fine-grained materials underlying the Rapid terrace may contain sufficient salt to cause detrimental salt accumulations in the soil if the proposed irrigation causes ground-water levels to rise close to the surface.

\n

Lining of the irrigation canals would reduce the amount of seepage and would effect a lowering of ground-water levels, if irrigation practices are extended to other areas, drainage facilities will be necessary both to avoid aggravating the existing conditions of waterlogging and to prevent the waterlogging of other low-lying lands.

\n

The flow of Rapid Creek is affected by a variety of conditions. A few miles west of Rapid City, where Rapid Creek flows over the Englewood and Pahasapa limestones and the Minnelusa sandstone, there is a loss of about 8 cfs of water in a distance of a few miles. In the 3-mile reach of Rapid Creek between the Canyon Lake stream-gaging station and the Rapid City stream-gaging station there is a gain of about 20 cfs; much of this gain in flow may be attributed to the inflow from Cleghorn and Jackson springs and to the addition of water from the State-owned cement plant. In the Rapid Valley unit, the flow of the creek during the irrigation season is affected largely by the amount of water diverted for irrigation. The irrigation canals act as bypass channels, much of the water being returned to Rapid Creek by way of spillage into normally dry tributary creek channels and by movement through ground-water bodies that discharge into Rapid Creek.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","doi":"10.3133/cir201","usgsCitation":"Rosier, A.J., and Snell, L., 1953, Ground-water resources of the Rapid Valley unit, Cheyenne Division, South Dakota, with a section on the surface waters of Rapid Valley: U.S. Geological Survey Circular 201, iii, 32 p., https://doi.org/10.3133/cir201.","productDescription":"iii, 32 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":30502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1953/0201/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124632,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1953/0201/report-thumb.jpg"}],"country":"United States","state":"South Dakota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.8922119140625,\n 43.361132106881726\n ],\n [\n -102.073974609375,\n 43.361132106881726\n ],\n [\n -102.073974609375,\n 44.55133484083592\n ],\n [\n -103.8922119140625,\n 44.55133484083592\n ],\n [\n -103.8922119140625,\n 43.361132106881726\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a685","contributors":{"authors":[{"text":"Rosier, Arthur J.","contributorId":69537,"corporation":false,"usgs":true,"family":"Rosier","given":"Arthur","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":147032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snell, L.J.","contributorId":25555,"corporation":false,"usgs":true,"family":"Snell","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":147031,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2456,"text":"wsp1176 - 1953 - Surface water supply of the United States, 1950, Part VI, Missouri River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"wsp1176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"1176","title":"Surface water supply of the United States, 1950, Part VI, Missouri River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1176","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Surface water supply of the United States, 1950, Part VI, Missouri River basin: U.S. Geological Survey Water Supply Paper 1176, xv, 826 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1176.","productDescription":"xv, 826 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":138692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1176/report-thumb.jpg"},{"id":28532,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1176/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696579","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":528014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2464,"text":"wsp1162 - 1953 - Quality of surface waters of the United States, 1949 : Parts 1 -6","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"1162","title":"Quality of surface waters of the United States, 1949 : Parts 1 -6","language":"ENGLISH","publisher":"U.S. Govt. 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