No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr4925","usgsCitation":"Campbell, C.D., 1949, Geology of the Bechtol lead mine, Stevens County, Washington: U.S. Geological Survey Open-File Report 49-25, Report: 3 p.; 1 Plate: 32.70 x 18.81 inches, https://doi.org/10.3133/ofr4925.","productDescription":"Report: 3 p.; 1 Plate: 32.70 x 18.81 inches","costCenters":[],"links":[{"id":41301,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1949/0025/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41300,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1949/0025/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147086,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1949/0025/report-thumb.jpg"},{"id":416870,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51342.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","county":"Stevens County","otherGeospatial":"Bechtol lead mine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.6394,\n 48.8856\n ],\n [\n -117.6394,\n 48.8611\n ],\n [\n -117.5583,\n 48.8611\n ],\n [\n -117.5583,\n 48.8856\n ],\n [\n -117.6394,\n 48.8856\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68359f","contributors":{"authors":[{"text":"Campbell, Charles Duncan","contributorId":26311,"corporation":false,"usgs":true,"family":"Campbell","given":"Charles","email":"","middleInitial":"Duncan","affiliations":[],"preferred":false,"id":166894,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014102,"text":"1014102 - 1949 - Experimental fish troughs","interactions":[],"lastModifiedDate":"2025-07-31T15:19:37.778782","indexId":"1014102","displayToPublicDate":"1948-01-01T00:00:00","publicationYear":"1949","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Experimental fish troughs","docAbstract":"No abstract available.
","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8640(1949)11[79:EFT]2.0.CO;2","usgsCitation":"Snieszko, S.F., 1949, Experimental fish troughs: Progressive Fish-Culturist, v. 11, no. 1, p. 79-81, https://doi.org/10.1577/1548-8640(1949)11[79:EFT]2.0.CO;2.","productDescription":"3 p.","startPage":"79","endPage":"81","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129276,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c94","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70214512,"text":"70214512 - 1949 - Relations of bauxite and Kaolin in the Arkansas bauxite deposits","interactions":[],"lastModifiedDate":"2020-09-28T20:13:28.321387","indexId":"70214512","displayToPublicDate":"1946-09-28T15:02:03","publicationYear":"1949","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Relations of bauxite and Kaolin in the Arkansas bauxite deposits","docAbstract":"Investigation of the Arkansas bauxite deposits by the U. S. Geological Survey during the years 1942 to 1945 has brought out the fact that secondary kaolinization or silication of the bauxite is much more common than has been generally recognized. On the other hand no direct evidence was found of the development of bauxite from kaolin. These facts have led us to reconsider the genetic relations of bauxite and kaolin.
We do not mean to deny that there has been direct kaolinization of the nepheline syenite; but in view of the above observations and of the character of the kaolin derived from bauxite, we believe that the relations of bauxite and kaolin in the Arkansas deposits are more readily explained on the assumption that the bauxite is derived directly from the nepheline syenite, rather than from kaolinized nepheline syenite. The silica causing its subsequent kaolinization may be derived from overlying sediments or from remnants of unbauxitized nepheline syenite within or adjacent to it
.Our conclusions about the relations of the kaolinized and bauxitized nepheline syenite are based entirely on rock weathered in place.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.41.6.567","usgsCitation":"Goldman, M., and Tracey, J.I., 1949, Relations of bauxite and Kaolin in the Arkansas bauxite deposits: Economic Geology, v. 41, no. 6, p. 567-575, https://doi.org/10.2113/gsecongeo.41.6.567.","productDescription":"9 p.","startPage":"567","endPage":"575","costCenters":[],"links":[{"id":378827,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas","county":"Saline","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-92.7396,34.8533],[-92.6527,34.8511],[-92.6518,34.8147],[-92.6533,34.7866],[-92.6542,34.7643],[-92.5501,34.7617],[-92.5506,34.748],[-92.5511,34.7403],[-92.5511,34.7367],[-92.5516,34.7294],[-92.553,34.6885],[-92.5004,34.6883],[-92.4993,34.6879],[-92.5003,34.6751],[-92.5003,34.6729],[-92.4495,34.6717],[-92.4439,34.6717],[-92.4464,34.6272],[-92.3464,34.6257],[-92.3485,34.5821],[-92.2446,34.5806],[-92.246,34.4934],[-92.3943,34.4952],[-92.3954,34.4957],[-92.4038,34.4956],[-92.4038,34.4843],[-92.4047,34.4516],[-92.5429,34.4542],[-92.5552,34.4546],[-92.568,34.455],[-92.5741,34.4549],[-92.5897,34.4553],[-92.5953,34.453],[-92.5981,34.4503],[-92.598,34.4444],[-92.6008,34.4398],[-92.6107,34.4316],[-92.6141,34.4284],[-92.6141,34.4325],[-92.6169,34.432],[-92.6235,34.4261],[-92.6246,34.4206],[-92.6201,34.417],[-92.6173,34.4166],[-92.6173,34.4134],[-92.6195,34.4134],[-92.6228,34.4138],[-92.6234,34.4129],[-92.6691,34.414],[-92.6864,34.4143],[-92.6855,34.4453],[-92.6855,34.4471],[-92.6856,34.4539],[-92.6856,34.4584],[-92.6852,34.4693],[-92.6874,34.4734],[-92.6986,34.4733],[-92.7393,34.4735],[-92.7384,34.5031],[-92.7937,34.5036],[-92.792,34.5582],[-92.7915,34.5618],[-92.8088,34.5621],[-92.8085,34.5903],[-92.8761,34.5916],[-92.876,34.6352],[-92.9604,34.6368],[-92.9816,34.6371],[-92.9809,34.6666],[-92.9805,34.6844],[-92.9699,34.6845],[-92.9697,34.7571],[-92.9693,34.7721],[-93.0219,34.7721],[-93.0751,34.7717],[-93.0757,34.8588],[-93.0388,34.8583],[-92.9687,34.8575],[-92.916,34.8561],[-92.8981,34.8558],[-92.8314,34.8545],[-92.8185,34.8482],[-92.8095,34.8469],[-92.7989,34.847],[-92.7938,34.8452],[-92.782,34.8394],[-92.7708,34.8426],[-92.7652,34.8395],[-92.7568,34.8427],[-92.7557,34.8423],[-92.7534,34.8405],[-92.7529,34.8382],[-92.7455,34.8342],[-92.7444,34.8305],[-92.741,34.8278],[-92.7396,34.8533]]]},\"properties\":{\"name\":\"Saline\",\"state\":\"AR\"}}]}","volume":"41","issue":"6","noUsgsAuthors":false,"publicationDate":"1946-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Goldman, M.I.","contributorId":6028,"corporation":false,"usgs":true,"family":"Goldman","given":"M.I.","email":"","affiliations":[],"preferred":false,"id":799764,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, Joshua Irving Jr.","contributorId":65135,"corporation":false,"usgs":true,"family":"Tracey","given":"Joshua","suffix":"Jr.","email":"","middleInitial":"Irving","affiliations":[],"preferred":false,"id":799765,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":34183,"text":"b955C - 1949 - Phosphate deposits of the Deer Creek-Wells Canyon area, Caribou County, Idaho","interactions":[{"subject":{"id":13296,"text":"ofr465 - 1946 - Summary report on the phosphate deposits in the Deer Creek-Wells Canyon area, Idaho","indexId":"ofr465","publicationYear":"1946","noYear":false,"title":"Summary report on the phosphate deposits in the Deer Creek-Wells Canyon area, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":34183,"text":"b955C - 1949 - Phosphate deposits of the Deer Creek-Wells Canyon area, Caribou County, Idaho","indexId":"b955C","publicationYear":"1949","noYear":false,"chapter":"C","title":"Phosphate deposits of the Deer Creek-Wells Canyon area, Caribou County, Idaho"},"id":1}],"lastModifiedDate":"2023-03-15T21:24:36.830306","indexId":"b955C","displayToPublicDate":"1943-01-01T00:00:00","publicationYear":"1949","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"955","chapter":"C","title":"Phosphate deposits of the Deer Creek-Wells Canyon area, Caribou County, Idaho","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b955C","usgsCitation":"Deiss, C.F., 1949, Phosphate deposits of the Deer Creek-Wells Canyon area, Caribou County, Idaho: U.S. Geological Survey Bulletin 955, Report: iv, 41 p.; 3 Plates: 12.33 x 23.84 inches or smaller, https://doi.org/10.3133/b955C.","productDescription":"Report: iv, 41 p.; 3 Plates: 12.33 x 23.84 inches or smaller","startPage":"61","endPage":"101","costCenters":[],"links":[{"id":109614,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21212.htm","linkFileType":{"id":5,"text":"html"},"description":"21212"},{"id":163507,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0955c/report-thumb.jpg"},{"id":96274,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0955c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":96277,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0955c/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":96276,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0955c/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":96275,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0955c/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Caribou County","otherGeospatial":"Deer Creek-Wells Canyon area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.25,\n 42.624\n ],\n [\n -111.25,\n 42.54\n ],\n [\n -111.175,\n 42.54\n ],\n [\n -111.175,\n 42.624\n ],\n [\n -111.25,\n 42.624\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d2d","contributors":{"authors":[{"text":"Deiss, Charles F.","contributorId":12444,"corporation":false,"usgs":true,"family":"Deiss","given":"Charles","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":212576,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70215508,"text":"70215508 - 1949 - Natural water losses in mountain drainage areas of southern California","interactions":[],"lastModifiedDate":"2020-10-21T18:04:38.12319","indexId":"70215508","displayToPublicDate":"1939-10-21T12:44:10","publicationYear":"1949","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Natural water losses in mountain drainage areas of southern California","docAbstract":"For twenty‐five small mountain drainage areas of Southern California, natural water losses are shown to vary with basin altitude, and with estimated absorptive and retentive characteristics of the drainage areas. Among other relationships demonstrated is the increase of the annual natural water loss with increased annual precipitation to an optimum, beyond which the loss is about uniform regardless of increased precipitation.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR030i005p00752","usgsCitation":"Troxell, H.C., and Stafford, H., 1949, Natural water losses in mountain drainage areas of southern California: Eos, Transactions, American Geophysical Union, v. 30, no. 5, p. 752-758, https://doi.org/10.1029/TR030i005p00752.","productDescription":"7 p.","startPage":"752","endPage":"758","costCenters":[],"links":[{"id":379601,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Southern California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.84960937499999,\n 32.175612478499325\n ],\n [\n -114.08203125,\n 32.175612478499325\n ],\n [\n -114.08203125,\n 36.38591277287651\n ],\n [\n -120.84960937499999,\n 36.38591277287651\n ],\n [\n -120.84960937499999,\n 32.175612478499325\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"30","issue":"5","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Troxell, Harold C.","contributorId":33354,"corporation":false,"usgs":true,"family":"Troxell","given":"Harold","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":802565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stafford, H.M.","contributorId":36914,"corporation":false,"usgs":true,"family":"Stafford","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":802566,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70178710,"text":"70178710 - 1948 - Ground water in the East Shore area, Utah. Part I. Bountiful District, Davis County","interactions":[],"lastModifiedDate":"2017-01-24T16:41:01","indexId":"70178710","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"5","title":"Ground water in the East Shore area, Utah. Part I. Bountiful District, Davis County","docAbstract":"The Bountiful district in Davis County, Utah, less than 10 miles from the heart of Salt Lake City, is rapidly becoming an integral part of the metropolitan area of Salt Lake City. It cannot achieve the development that its location merits unless the present water supplies are increased. The district is a fertile agricultural area favorably situated between the largest cities in the intermountain area and athwart the major routes of transportation and communication, but development of its residential, industrial, and agricultural potentialities will be restricted until existing water resources are supplemented by importation from other drainage basins that now have surplus water supplies. This conclusion is reached in the accompanying report by the Geological Survey, prepared in cooperation with the Utah State Engineer and the Davis County Water Users Association, and based on a 2-year investigation of the existing water supplies
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Twenty-sixth biennial report of the State Engineer to the Governor of Utah: 1946-1948","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Thomas, H.E., and Nelson, W., 1948, Ground water in the East Shore area, Utah. Part I. Bountiful District, Davis County: Technical Publication 5, 154 p.","productDescription":"154 p.","startPage":"53","endPage":"206","numberOfPages":"156","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331488,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333874,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-370","text":"Utah State Engineer's 26th Biennial Report (larger work)"},{"id":331486,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-130"},{"id":331487,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w9200084.pdf"}],"country":"United States","state":"Utah","county":"Davis","otherGeospatial":"Bountiful District","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.88201904296875,\n 40.98611828780413\n ],\n [\n -112.06878662109374,\n 40.950862628132775\n ],\n [\n -112.17315673828125,\n 40.84290487729676\n ],\n [\n -112.1209716796875,\n 40.73268976628568\n ],\n [\n -111.92047119140624,\n 40.670222795307346\n ],\n [\n -111.7529296875,\n 40.73893324113601\n ],\n [\n -111.741943359375,\n 40.8865244080599\n ],\n [\n -111.88201904296875,\n 40.98611828780413\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58468aefe4b04fc80e5236dd","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":654894,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, W.B.","contributorId":30282,"corporation":false,"usgs":true,"family":"Nelson","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":654895,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70160507,"text":"70160507 - 1948 - New compounds for the control of bacterial gill disease","interactions":[],"lastModifiedDate":"2016-01-04T12:05:52","indexId":"70160507","displayToPublicDate":"2015-08-11T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"New compounds for the control of bacterial gill disease","docAbstract":"BACTERIAL GILL DISEASE, a common epizootic among hatchery fish, can be controlled by copper sulphate dips, as stated by Davis (1945), or by prolonged treatments with Roccal, as noted by Fish (1947). The use of copper sulphate is not without danger because of variation in toxicity according to the hardness of the particular water supply; also, the toxicity and efficacy of Roccal have varied considerably in different lots. Neither copper sulphate nor Roccal will cure in one treatcent a well-established epizootic of bacterial gill disease. For these reasons, a series of new disinfectants has been tested in the laboratory in an attempt to find a more effective cure and preventive for bacterial Eill disease. One of these tested, pyridylmercuric acetate, was suggested by Wan Horn and Katz (1946).
\n","language":"English","publisher":" Bureau of Fisheries, U.S. Deptarment of Commerce","doi":"10.1577/1548-8640(1948)10[19:NCFTCO]2.0.CO;2","usgsCitation":"Rucker, R., 1948, New compounds for the control of bacterial gill disease: Progressive Fish-Culturist, v. 10, no. 1, p. 19-22, https://doi.org/10.1577/1548-8640(1948)10[19:NCFTCO]2.0.CO;2.","productDescription":"4 p.","startPage":"19","endPage":"22","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312596,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567930cfe4b0da412f4fb576","contributors":{"authors":[{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":584119,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70160508,"text":"70160508 - 1948 - A report upon the Grand Coulee Fish Maintenance Project 1939-1947","interactions":[],"lastModifiedDate":"2018-04-06T11:30:25","indexId":"70160508","displayToPublicDate":"2015-08-11T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"55","title":"A report upon the Grand Coulee Fish Maintenance Project 1939-1947","docAbstract":"
The construction or Grand Coulee Dam, on the upper Columbia River, involved the loss of 1,140 lineal miles of spawning and rearing stream to the production of anadromous fishes. The fact that the annual value of these fish runs to the nation was estimated at $250,000 justified reasonable expenditures to assure their perpetuation. It was found economically infeasible to safely collect and pass adult fish upstream and fingerling fish downstream at the dam because of the tremendous flow of the river and the 320 foot vertical difference in elevation between forebay and tailrace.
The Grand Coulee Fish-Maintenance Project, undertaken by the United States Fish and Wildlife Service in 1939, consisted in relocating the anadroumous runs of the upper Columbia River to four major tributaries entering below the Grand Coulee damsite. These streams were believed capable of supporting several times their existing, badly depleted, run.
The plan was predicated upon the assumption that the relocated runs, in conformity with their \"homing tendency\", would return to the lower tributaries rather than attempt to reach their ancestral spawning grounds above Grand Coulee Dam.
This interim report covers the history and accomplishments of the Grand Coulee Fish-Maintenance Project through the initial period of relocating the rune as well as the first four years of the permanent program.
Results obtained to date indicate conclusive success in diverting the upper Columbia fish runs into the accessible lower tributaries. The results also indicate, less conclusively, that - in spite of many existing handicaps - the upper Columbia salmon and steelhead runs may be rehabilitated through the integrated program of natural and artificial propagation incorporated in the Grand Coulee Fish-Maintenance Project.
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","language":"English","publisher":" American Association for the Advancement of Science","usgsCitation":"Fisher, F.S., 1948, The return on the blueback salmon to the Columbia River: Scientific Monthly, v. 66, no. 4, p. 283-292.","productDescription":"10 p.","startPage":"283","endPage":"292","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312631,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":312628,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/19068?seq=1#page_scan_tab_contents"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Bonnevile Dam, Columbia River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.970458984375,\n 45.89000815866184\n ],\n [\n -121.6845703125,\n 45.882360730184025\n ],\n [\n -122.794189453125,\n 46.255846818480315\n ],\n [\n -123.211669921875,\n 46.40756396630067\n ],\n [\n -123.8818359375,\n 46.42271253466717\n ],\n [\n -124.01367187499999,\n 46.15700496290803\n ],\n [\n -123.85986328124999,\n 45.897654534346884\n ],\n [\n -122.794189453125,\n 45.44471679159555\n ],\n [\n -119.410400390625,\n 45.75219336063106\n ],\n [\n -119.14672851562499,\n 45.805828539928356\n ],\n [\n -118.94897460937499,\n 45.920587344733654\n ],\n [\n -119.15771484375,\n 46.09609080214316\n ],\n [\n -119.564208984375,\n 46.14178273759234\n ],\n [\n -119.86083984375,\n 46.18743678432541\n ],\n [\n -120.970458984375,\n 45.89000815866184\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"66","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567930d7e4b0da412f4fb5b2","contributors":{"authors":[{"text":"Fisher, Frederick S.","contributorId":17979,"corporation":false,"usgs":true,"family":"Fisher","given":"Frederick","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":583038,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70160506,"text":"70160506 - 1948 - Removal of excess nitrogen in a hatchery water supply","interactions":[],"lastModifiedDate":"2016-01-04T12:06:52","indexId":"70160506","displayToPublicDate":"2015-04-06T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Removal of excess nitrogen in a hatchery water supply","docAbstract":"The water system at the U. S. Fish Cultural Station, Leavenworth, Washington, has been supplemented with two wells that were to be used to increase the temperature of the water during the winter and to cool the Water in the summer if necessary. The well water proved to be unsuitable for hatchery purposes because it was supersaturated with nitrogen, causing \"gas-bubble\" disease among fish subjected to 11. Mr. R. E. Burrows, the district biologist at the Leavenworth laboratory, devised a system by which the water from one well could be used satisfactorily in the hatchery after a circuitous routing through a mixing chamber with considerable agitation and a settling basin. The circuitous routing precluded the use of the rearing ponds, and it did not sufficiently reduce the nitrogen tension of the water from the other well.
","language":"English","publisher":"Bureau of Fisheries, U.S. Department of Commerce","doi":"10.1577/1548-8640(1948)10[88:ROENIA]2.0.CO;2","usgsCitation":"Rucker, R., 1948, Removal of excess nitrogen in a hatchery water supply: Progressive Fish-Culturist, v. 10, no. 3, p. 88-90, https://doi.org/10.1577/1548-8640(1948)10[88:ROENIA]2.0.CO;2.","productDescription":"3 p.","startPage":"88","endPage":"90","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312588,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567930d2e4b0da412f4fb58f","contributors":{"authors":[{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":584120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047889,"text":"70047889 - 1948 - Cranberry magnetite deposits Avery County, N.C., and Carter County, Tenn.","interactions":[{"subject":{"id":55399,"text":"ofr4421 - 1944 - Preliminary report on the magnetic iron ores of western North Carolina and eastern Tennessee","indexId":"ofr4421","publicationYear":"1944","noYear":false,"title":"Preliminary report on the magnetic iron ores of western North Carolina and eastern Tennessee"},"predicate":"SUPERSEDED_BY","object":{"id":70047889,"text":"70047889 - 1948 - Cranberry magnetite deposits Avery County, N.C., and Carter County, Tenn.","indexId":"70047889","publicationYear":"1948","noYear":false,"title":"Cranberry magnetite deposits Avery County, N.C., and Carter County, Tenn."},"id":1}],"lastModifiedDate":"2017-09-13T18:17:40","indexId":"70047889","displayToPublicDate":"2013-01-01T08:28:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":67,"text":"U.S. Bureau of Mines Report of Investigations","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"4274","title":"Cranberry magnetite deposits Avery County, N.C., and Carter County, Tenn.","docAbstract":"The Cranberry magnetite deposits occur in pre-Cambrian granite-gneiss in a belt extending from 3 miles southeast of Cranberry, N.C., to about 6 miles southwest of Magnetic City, Tenn. The belt forms a curve, elongated to the north, approximately 26 miles in length.","language":"English","publisher":"U.S. Bureau of Mines","usgsCitation":"Kline, M., and Ballard, T., 1948, Cranberry magnetite deposits Avery County, N.C., and Carter County, Tenn.: U.S. Bureau of Mines Report of Investigations 4274, 85 p.","productDescription":"85 p.","costCenters":[],"links":[{"id":277140,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047889.JPG"},{"id":277139,"type":{"id":11,"text":"Document"},"url":"https://babel.hathitrust.org/cgi/pt?id=mdp.39015078468728;view=1up;seq=1"}],"country":"United States","state":"North Carolina;Tennessee","county":"Avery County;Carter County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.342606,35.910275 ], [ -82.342606,36.510864 ], [ -81.737953,36.510864 ], [ -81.737953,35.910275 ], [ -82.342606,35.910275 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52206d61e4b0645fc25e8c22","contributors":{"authors":[{"text":"Kline, M.H.","contributorId":25067,"corporation":false,"usgs":true,"family":"Kline","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":483224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ballard, T.J.","contributorId":94196,"corporation":false,"usgs":true,"family":"Ballard","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":483225,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70046715,"text":"70046715 - 1948 - Geologic map of part of eastern San Juan Basin, Rio Arriba County, New Mexico","interactions":[{"subject":{"id":53033,"text":"ofr384 - 1938 - Preliminary map showing geologic structure of part of the Rio Arriba County, New Mexico","indexId":"ofr384","publicationYear":"1938","noYear":false,"title":"Preliminary map showing geologic structure of part of the Rio Arriba County, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":70046715,"text":"70046715 - 1948 - Geologic map of part of eastern San Juan Basin, Rio Arriba County, New Mexico","indexId":"70046715","publicationYear":"1948","noYear":false,"title":"Geologic map of part of eastern San Juan Basin, Rio Arriba County, New Mexico"},"id":1}],"lastModifiedDate":"2013-06-27T13:23:50","indexId":"70046715","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":374,"text":"Oil and Gas Preliminary Investigations Map","active":false,"publicationSubtype":{"id":6}},"title":"Geologic map of part of eastern San Juan Basin, Rio Arriba County, New Mexico","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70046715","usgsCitation":"Dane, C.H., 1948, Geologic map of part of eastern San Juan Basin, Rio Arriba County, New Mexico: Oil and Gas Preliminary Investigations Map, Map: 1 Sheet, https://doi.org/10.3133/70046715.","productDescription":"Map: 1 Sheet","costCenters":[],"links":[{"id":274276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51cd5ee0e4b0e7a904971bc4","contributors":{"authors":[{"text":"Dane, C. 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S. Geological Survey and the University of Wisconsin. Pumping tests on wells that yield water from the Ordovician and Cambrian sandstones underlying the Milwaukee-Waukesha area have been made as a part a larger regional investigation. The purpose of the tests has been to determine the water-bearing characteristics of the aquifer. These characteristics, the coefficients of transmissibility and storage, are used to determine the effect on water levels caused by changes in the rate of withdrawal from the aquifer. Average coefficients of transmissibility and storage determined from the results of 47 pumping tests at five different locations are 23,800 gallons a day per foot, and 0.00039, respectively. The amount of drawdown in the water level at any point caused by pumping a well for a given length of time may be computed by the nonequilibrium formula, using the coefficients and correcting for the effects of boundaries and of any changes in the character of the aquifer. Further study of the geology is needed to determine the location of the recharge area, the location of possible boundaries, and changes in the character of the aquifer. 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