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by: I-130","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683455","contributors":{"authors":[{"text":"Lindvall, Robert M.","contributorId":34523,"corporation":false,"usgs":true,"family":"Lindvall","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":189558,"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":51220,"text":"ofr5328 - 1953 - Pegmatite investigations in Maine, New Hampshire, and Connecticut, 1942-1945","interactions":[{"subject":{"id":51220,"text":"ofr5328 - 1953 - Pegmatite investigations in Maine, New Hampshire, and Connecticut, 1942-1945","indexId":"ofr5328","publicationYear":"1953","noYear":false,"title":"Pegmatite investigations in Maine, New Hampshire, and Connecticut, 1942-1945"},"predicate":"SUPERSEDED_BY","object":{"id":39189,"text":"pp255 - 1954 - Pegmatite investigations, 1942-45, New England","indexId":"pp255","publicationYear":"1954","noYear":false,"title":"Pegmatite investigations, 1942-45, New England"},"id":1}],"supersededBy":{"id":39189,"text":"pp255 - 1954 - Pegmatite investigations, 1942-45, New England","indexId":"pp255","publicationYear":"1954","noYear":false,"title":"Pegmatite investigations, 1942-45, New England"},"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr5328","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":"53-28","title":"Pegmatite investigations in Maine, New Hampshire, and Connecticut, 1942-1945","language":"ENGLISH","doi":"10.3133/ofr5328","usgsCitation":"Cameron, E., Larrabee, D.M., McNair, A., Page, J., Stewart, G.W., and Shainin, V., 1953, Pegmatite investigations in Maine, New Hampshire, and Connecticut, 1942-1945 (Superceded by: P-255): U.S. Geological Survey Open-File Report 53-28, 853 p., https://doi.org/10.3133/ofr5328.","productDescription":"853 p.","costCenters":[],"links":[{"id":176721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superceded by: P-255","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6889f4","contributors":{"authors":[{"text":"Cameron, E.E.","contributorId":34380,"corporation":false,"usgs":true,"family":"Cameron","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":243171,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larrabee, D. M.","contributorId":67571,"corporation":false,"usgs":true,"family":"Larrabee","given":"D.","middleInitial":"M.","affiliations":[],"preferred":false,"id":243175,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McNair, A.H.","contributorId":49441,"corporation":false,"usgs":true,"family":"McNair","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":243174,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Page, J.J.","contributorId":43425,"corporation":false,"usgs":true,"family":"Page","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":243173,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stewart, G. W.","contributorId":99621,"corporation":false,"usgs":true,"family":"Stewart","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":243176,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Shainin, V.E.","contributorId":34991,"corporation":false,"usgs":true,"family":"Shainin","given":"V.E.","affiliations":[],"preferred":false,"id":243172,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":37594,"text":"ssrw18 - 1953 - Investigations of woodcock, snipe, and rails in 1952","interactions":[],"lastModifiedDate":"2012-02-02T00:09:51","indexId":"ssrw18","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"18","title":"Investigations of woodcock, snipe, and rails in 1952","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"U.S. Fish and Wildlife Service, 1953, Investigations of woodcock, snipe, and rails in 1952 (Updates and revises Special Scientific Report-Wildlife 14 (1952)): Special Scientific Report  - Wildlife 18, 55 p.","productDescription":"55 p.","numberOfPages":"55","costCenters":[],"links":[{"id":101722,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486652?urlappend=%3Bseq=447"},{"id":164600,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Updates and revises Special Scientific Report-Wildlife 14 (1952)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667373","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529662,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51201,"text":"ofr534 - 1953 - A brief report on the progress of the Manatee County, Florida, ground-water investigation","interactions":[{"subject":{"id":51201,"text":"ofr534 - 1953 - A brief report on the progress of the Manatee County, Florida, ground-water investigation","indexId":"ofr534","publicationYear":"1953","noYear":false,"title":"A brief report on the progress of the Manatee County, Florida, ground-water investigation"},"predicate":"SUPERSEDED_BY","object":{"id":70046943,"text":"70046943 - 1955 - Interim report on the ground-water resources of Manatee County, Florida","indexId":"70046943","publicationYear":"1955","noYear":false,"title":"Interim report on the ground-water resources of Manatee County, Florida"},"id":1}],"supersededBy":{"id":70046943,"text":"70046943 - 1955 - Interim report on the ground-water resources of Manatee County, Florida","indexId":"70046943","publicationYear":"1955","noYear":false,"title":"Interim report on the ground-water resources of Manatee County, Florida"},"lastModifiedDate":"2013-07-09T15:52:15","indexId":"ofr534","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":"53-4","title":"A brief report on the progress of the Manatee County, Florida, ground-water investigation","language":"ENGLISH","doi":"10.3133/ofr534","usgsCitation":"Anders, R., and Heath, R., 1953, A brief report on the progress of the Manatee County, Florida, ground-water investigation (Superceded by: FL Geological Survey, Information Circular #6): U.S. Geological Survey Open-File Report 53-4, 11 p., https://doi.org/10.3133/ofr534.","productDescription":"11 p.","costCenters":[],"links":[{"id":178878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Superceded by: FL Geological Survey, Information Circular #6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd497be4b0b290850ef381","contributors":{"authors":[{"text":"Anders, R.B.","contributorId":106533,"corporation":false,"usgs":true,"family":"Anders","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":243140,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heath, R.C.","contributorId":49408,"corporation":false,"usgs":true,"family":"Heath","given":"R.C.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":243139,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12778,"text":"ofr5326 - 1953 - Geology of the Plumtree area, Spruce Pine district, North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr5326","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":"53-26","title":"Geology of the Plumtree area, Spruce Pine district, North Carolina","docAbstract":"This report describes the results of study and geologic mapping (1:12,000) in the 70-square-mile Plumtree area in the northeastern part of the Spruce Pine pegmatite district, on the Blue Ridge upland in western North Carolina. The district has been the chief domestic source of feldspar and sheet mica. The mining belt just west of the Blue Ridge Front trends northeast and is 25 miles long and 10 miles wide. The center of the Plumtree area lies 10 miles northeast of Spruce Pine pegmatite district, on the Blue Ridge upland in western North Carolina. The district has been the chief domestic source of feldspar and sheet mica. The mining belt just west of the Blue Ridge Front trends northeast and is 25 miles long and 10 miles wide. The center of the Plumtree area lies 10 miles northeast of Spruce Pine and includes parts of Mitchell and Avery Counties shown on the portions of the 7.5-minute Spruce Pine, Linville Falls, Newland, North Carolina, and Carvers Gap, North Carolina and Tennessee quadrangle.\r\n\r\nThe topography varies from rugged mountains to rounded or flat topped hills near the entrenched, meandering master streams. Old erosion surfaces are approximately 600,1,100, 1,500, and 2,500 feet above the present master stream level. The area is in late youth or early maturity after rejuvenation..\r\n\r\nThe regionally metamorphosed rocks of the amophibolite facies form three mappable units: mica gneiss, mica schist, and hornblende rock. These rocks, perhaps of Precambrian age, are intimately interlayered with thicknesses of the individual layers ranging from less than one inch to several tons of feet. Field relationships and chemical data suggest that the mica (Carolina-type) rocks were derived from sandstones, graywackes, and shales and that the hornblende-rich (Roan-type) layers were derived from impure carbonate rocks.\r\n\r\nThe igneous rocks include alaskite and associated pegmatite of early Paleozoic age (?), dunite and associated soapstone of a prepegmatite age, and a few diabasic dikes of post-pegmatite age (Triassic?).\r\n\r\nThe alaskite and pegmatite have similar bulk compositions, notably low in iron (0.3 percent). The major constituents in order of decreasing abundance are plagioclase, perthitic microcline, quartz, and muncovite. All of these minerals, as well as clay deposits derived from the weathering of alaskite under old terraces, have economic value. The zoned pegmatites contain fewer zones which are less complex mineralogically than those in the pegmatites of many other areas. These essentially unmetamorphosed bodies were intruded approximately at the peak of the regional metamorphism. Their emplacement was controlled by local structure and rock type. The source of this igneous material may have been the mobilized portions of the Cranberry gneiss which underlies the area.\r\n\r\nThe dunite bodies were intruded early in the metamorphic cycle. The bodies are commonly zoned: from the wall rock inwards (1) talc-antrophyllite-serpentine fringe, (3) serpentinized dunite, (3) granular olivine core. Dunite, chromite, vermiculite, and anthophyllite are the major economic commodities. Extensive hydrothermal alteration of dunite bodies produced soapstone.\r\n\r\nThe area is the northeast end of a southwest plunging synclinorium about 20 miles wide with the steeper limb on the northwest side. There are three structural zones: zone I on the northwest is characterized by the northeast-trending isoclinal folds with steep southeast dips; zone II on the southwest includes an area of rocks with low and variable dip; zone III is the complex central core. In the extreme northeast zones I and II have an indistinct boundary where they coalesce along the rim of the synclinorium. Six stratigraphic units are exposed totaling approximately 10,500 feet of metamorphic rocks.\r\n\r\nSmall scale structural features include a foliation, and a lineation in the planes of the foliation. Minor folding reflects the trends of the major structures. There are randomly orient","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr5326","usgsCitation":"Brobst, D.A., 1953, Geology of the Plumtree area, Spruce Pine district, North Carolina: U.S. Geological Survey Open-File Report 53-26, 115 p, https://doi.org/10.3133/ofr5326.","productDescription":"115 p","costCenters":[],"links":[{"id":145017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0026/report-thumb.jpg"},{"id":41175,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1953/0026/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41176,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e853","contributors":{"authors":[{"text":"Brobst, Donald Albert","contributorId":36117,"corporation":false,"usgs":true,"family":"Brobst","given":"Donald","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":166691,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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