Reliable data on Utah's water resources are essential to development of a State Water plan. While the need for such data was outlined in the report entitles \"Developing a State Water Plan - Utah's water resources, problems, and needs - A challenge\" published by the Utah Water and Power Board and Utah State University in 1963, the discussion was, of necessity, brief. Further definition and scheduling of data collection and related investigations were known to be needed.
The report which follows was prepared by the U.S. Geological Survey as part of that agency's cooperative program with the State of Utah. It outlines, in greater detail, what the Geological Survey feels is an appropriate long-range program of investigations to provide part of the basic data which will be needed during the course of the State's water planning program. Some of these investigations already are underway, and others will be undertaken in the immediate future.
In 1954 four core holes were drilled in the pre-Selma Cretaceous strata of the Alabama Coastal Plain in order to get unweathered samples within a few miles of the outcrops. During the next few years several specialists studied the cores, and their reports are published as consecutive parts of this bulletin.
\nWatson H. Monroe, who spent many years studying the Coastal Plain strata in Alabama and Mississippi, conceived and supervised the drilling and planned the later studies. His earlier published report (W. H. Monroe, 1955, Cores of pre-Selma Cretaceous rocks in the outcrop area in western Alabama: Gulf Coast Geol. Societies Trans., v. 5, p. 11-37) contains a brief description of the stratigraphy, together with logs and other information regarding the core holes, and he has provided the introductory chapter to this bulletin. Richard E. Bergenback studied the petrology of the cores, which included finding the distribution of grain sizes, determining the mineralogy of the grains and the matrix of the sediments, and having X-Ray identifications made of the clay minerals. Norman F. Sohl studied the mollusks and other large fossils obtained from the cores and compared them with other faunal suites collected in Alaban1a and Texas. Esther R. Applin studied the sparse microfauna, comparing it with faunas obtained from deep wells downdip in Georgia, Alabama, and Mississippi and with outcrop samples fron1 Texas, and has described a new species of Foraminifera. Estella B. Leopold and Helen M. Pakiser obtained a large pollen and spore assemblage by digesting carbonaceous layers of some of the cores in acid; this flora includes much new material, which is not described here.
\nThe Bergenback, Sohl, and Applin reports discuss the probable environment in which the sediments accumulated. Louis C. Conant, who spent several years studying and mapping these sediments, has written a summary chapter integrating some of the surface and subsurface information.
\nQuarter-cuts of the cores belonging to the U.S. National Museum have been deposited on indefinite loan with the Alabama Geological Survey at University, Ala., and with the Shell Oil Co. at Jackson, Miss. They are available there for inspection and study.
","language":"English","publisher":"U.S. G.P.O.","doi":"10.3133/b1160","usgsCitation":"Monroe, W.H., Bergenback, R.E., Sohl, N.F., Applin, E.R., Leopold, E.B., Pakiser, H.M., and Conant, L.C., 1964, Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama: U.S. Geological Survey Bulletin 1160, Report: ix, 108 p.; Plate: 17 x 22.25 inches, https://doi.org/10.3133/b1160.","productDescription":"Report: ix, 108 p.; Plate: 17 x 22.25 inches","numberOfPages":"162","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318661,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/b1160.jpg"},{"id":318660,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1160a/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":318659,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56deb472e4b015c306fb8a78","contributors":{"authors":[{"text":"Monroe, Watson Hiner","contributorId":93020,"corporation":false,"usgs":true,"family":"Monroe","given":"Watson","email":"","middleInitial":"Hiner","affiliations":[],"preferred":false,"id":622087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergenback, Richard E.","contributorId":65897,"corporation":false,"usgs":true,"family":"Bergenback","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":622088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sohl, Norman F.","contributorId":27906,"corporation":false,"usgs":true,"family":"Sohl","given":"Norman","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":622089,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Applin, Esther R.","contributorId":40974,"corporation":false,"usgs":true,"family":"Applin","given":"Esther","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":622090,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Leopold, Estella B.","contributorId":30979,"corporation":false,"usgs":true,"family":"Leopold","given":"Estella","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":622091,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pakiser, Helen M.","contributorId":167378,"corporation":false,"usgs":false,"family":"Pakiser","given":"Helen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":622092,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Conant, Louis C.","contributorId":83921,"corporation":false,"usgs":true,"family":"Conant","given":"Louis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":622093,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":1000486,"text":"1000486 - 1964 - Bottom sediments of Saginaw Bay, Michigan","interactions":[],"lastModifiedDate":"2013-02-12T08:07:19","indexId":"1000486","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Bottom sediments of Saginaw Bay, Michigan","docAbstract":"Saginaw Bay is a southwest extension of Lake Huron on the east shore of the Southern Peninsula of Michigan. It is a shallow-water derivative of the Pleistocene Lake Saginaw. Sixty-one bottom samples were collected on a semigrid pattern and analyzed physically. Findings were treated statistically. Sediments range in size from large pebbles to clay. Medium- to fine-grained clear quartz sand is common to all parts of the bay. Currents and wave action are primarily responsible for both median diameter and sorting distribution patterns. Only a very general correlation can be established between depth and median diameter. Heavy minerals occur in abundance locally and show an affinity to shallow-water areas subject to prevailing currents. Shape also locally determines heavy mineral concentrations. Only general conclusions can be established from roundness and sphericity and acid-soluble content. Increased organic content is correlative with quiet water environments. The shallow-water, heterogeneous nature of Saginaw Bay is not conducive to the recognition of sedimentary criteria suitable for correlations in other than a local environment.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Sedimentary Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"SEPM Society for Sedimentary Geology","publisherLocation":"Tulsa, OK","doi":"10.1306/74D71000-2B21-11D7-8648000102C1865D","collaboration":"Out-of-print","usgsCitation":"Wood, L.E., 1964, Bottom sediments of Saginaw Bay, Michigan: Journal of Sedimentary Petrology, v. 34, no. 1, p. 173-184, https://doi.org/10.1306/74D71000-2B21-11D7-8648000102C1865D.","productDescription":"12 p.","startPage":"173","endPage":"184","numberOfPages":"12","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131764,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267262,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1306/74D71000-2B21-11D7-8648000102C1865D"}],"volume":"34","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcdf1","contributors":{"authors":[{"text":"Wood, Leonard E.","contributorId":73157,"corporation":false,"usgs":true,"family":"Wood","given":"Leonard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":308612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175637,"text":"70175637 - 1964 - Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1963","interactions":[],"lastModifiedDate":"2016-08-17T14:06:21","indexId":"70175637","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"4","title":"Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1963","docAbstract":"No abstract available.
","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Garza, S., 1964, Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1963: Edwards Underground Water District Bulletin 4, 15 p.","productDescription":"15 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326723,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58abfe4b03bcb0104bb64","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":645903,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":81377,"text":"81377 - 1964 - The true pikes","interactions":[],"lastModifiedDate":"2023-04-05T16:44:37.895882","indexId":"81377","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"569","title":"The true pikes","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Karvelis, E.G., 1964, The true pikes: Fishery Leaflet 569, 11 p.","productDescription":"11 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198084,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92142,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://spo.nmfs.noaa.gov/content/true-pikes-0","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db6349a1","contributors":{"authors":[{"text":"Karvelis, Ernest G.","contributorId":55547,"corporation":false,"usgs":true,"family":"Karvelis","given":"Ernest","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":295307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000364,"text":"1000364 - 1964 - The spottail shiner in Lower Red Lake, Minnesota","interactions":[],"lastModifiedDate":"2016-02-25T11:53:38","indexId":"1000364","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"The spottail shiner in Lower Red Lake, Minnesota","docAbstract":"On the basis of 14,564 spottail shiners (Notropis hudsonius) from Red Lakes, Minnesota, growth rates, strength of year classes, and food utilization were studied. Males and females had different body-scale relationships, and females grew faster than males. There was high correlation between water temperature and growth rate. Strength of year classes was closely related to size of spawning population. Food habits were related to food availability in both plankton and bottom fauna. Shiner eggs were significant items of food in larger shiners. Bottom organisms were selectively taken, and larger cladocerans were selected by large fish. Cladocerans were preferred to copepods.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1964)93[35:TSSILR]2.0.CO;2","usgsCitation":"Smith, L.L., and Kramer, R.H., 1964, The spottail shiner in Lower Red Lake, Minnesota: Transactions of the American Fisheries Society, v. 93, no. 1, p. 35-45, https://doi.org/10.1577/1548-8659(1964)93[35:TSSILR]2.0.CO;2.","productDescription":"11 p.","startPage":"35","endPage":"45","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"93","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63606a","contributors":{"authors":[{"text":"Smith, Lloyd L. Jr.","contributorId":103618,"corporation":false,"usgs":true,"family":"Smith","given":"Lloyd","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308460,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kramer, Robert H.","contributorId":60576,"corporation":false,"usgs":true,"family":"Kramer","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308459,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175579,"text":"70175579 - 1964 - Records of wells and springs, water levels, and chemical quality of ground water in the East Portland area, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T11:24:53","indexId":"70175579","displayToPublicDate":"1963-12-29T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Records of wells and springs, water levels, and chemical quality of ground water in the East Portland area, Oregon","docAbstract":"Data are presented on more than 300 wells, including many new ones whose records will not be a part of a forthcoming interpretative report on the occurrence of ground water in this area. A brief description of the geomorphic features is given, and the characteristics of the rock units are summarized in a table. Principal aquifers are beds of loose sand and gravel in the early Pliocene Troutdale Formation, late Pleistocene fluviolacustrine deposits, and Recent alluvium. Locally, Columbia River Basalt (Miocene) and the Boring Lava (late Pliocene to Pleistocene) yield substantial amounts of wate.. In addition to well records there are 124 driller's logs and a table of chemical analyses of the ground water.
","language":"English","usgsCitation":"Foxworthy, B., Hogenson, G., and Hampton, E.R., 1964, Records of wells and springs, water levels, and chemical quality of ground water in the East Portland area, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326649,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b57e4b03bcb0104bc4d","contributors":{"authors":[{"text":"Foxworthy, B. L.","contributorId":45686,"corporation":false,"usgs":true,"family":"Foxworthy","given":"B. L.","affiliations":[],"preferred":false,"id":645748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hogenson, G.M.","contributorId":69957,"corporation":false,"usgs":true,"family":"Hogenson","given":"G.M.","affiliations":[],"preferred":false,"id":645749,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":645750,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221125,"text":"70221125 - 1964 - Origin of precambrian iron formations","interactions":[],"lastModifiedDate":"2021-06-02T17:51:31.990895","indexId":"70221125","displayToPublicDate":"1963-09-01T12:48:10","publicationYear":"1964","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":"Origin of precambrian iron formations","docAbstract":"A statistical study of the chemical composition of the Precambrian iron formations of the Canadian Shield affords a new approach to the origin of these unusual formations. The average total iron content of 2,200 samples from the literature and from unpublished mining company analyses is 26.7 percent Fe. The average Fe content for 16 iron formations in the United States and Canada ranges from 24.5 to 34.1 percent. Low contents of A1203, Ti02, P2O5, and CaO characterize the Precambrian iron formations compared to the relatively large amounts of these constituents in the post-Precambrian iron-bearing sediments. The chemical data emphasize that whereas iron, manganese, and silica were transported and deposited together in the cherty iron formations of the Precambrian, these same elements were chemically differentiated in younger geological time in large but separate deposits of iron and silica. Isotopic age determinations indicate that cherty iron formations were deposited during a long interval of geologic time from approximately 1,700 to 3,000 million years ago. A model is proposed to explain the origin of the iron formations of the Lake Superior type based on the absence or marked deficiency of free oxygen in the atmosphere prior to the Late Precambrian. Lateritic weathering under these conditions permitted the transport of iron and manganese together with silica. The weathered mantle effectively retained aluminum, titanium, phosphorus, and colloidal clay. Graphitic material of biogenic origin is closely associated with the Precambrian iron formations. Although it is uncertain whether iron was precipitated directly through biologic processes, the removal of C02 and the liberation of oxygen to the sea water through photosynthesis of primitive plants undoubtedly influenced the energy relationships among the iron minerals. As a result of the variable conditions the iron formations commonly are characterized by nonequilibrium mineral assemblages. In Late Precambrian time a critical level of free oxygen in the atmosphere was attained permitting a marked acceleration in plant growth and in accretion of oxygen. This stage in the development of an oxygenated atmosphere was reached at least 1,200 million years ago and effectively curtailed the development of cherty iron formations of the Lake Superior type.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.59.6.1025","usgsCitation":"Lepp, H., and Goldich, S., 1964, Origin of precambrian iron formations: Economic Geology, v. 59, no. 6, p. 1025-1060, https://doi.org/10.2113/gsecongeo.59.6.1025.","productDescription":"36 p.","startPage":"1025","endPage":"1060","costCenters":[],"links":[{"id":386141,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"6","noUsgsAuthors":false,"publicationDate":"1964-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Lepp, H.","contributorId":259204,"corporation":false,"usgs":false,"family":"Lepp","given":"H.","email":"","affiliations":[],"preferred":false,"id":816811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldich, S. S.","contributorId":65536,"corporation":false,"usgs":true,"family":"Goldich","given":"S. S.","affiliations":[],"preferred":false,"id":816812,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70217324,"text":"wdrMDDE63 - 1963 - Surface water records of Maryland and Delaware, water year 1963","interactions":[],"lastModifiedDate":"2021-01-22T19:13:18.810771","indexId":"wdrMDDE63","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-63","displayTitle":"Surface Water Records of Maryland and Delaware, Water Year 1963","title":"Surface water records of Maryland and Delaware, water year 1963","docAbstract":"No abstract available.
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\"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW","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":808361,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180201,"text":"70180201 - 1963 - Floods in southeastern Michigan, magnitude and frequency","interactions":[],"lastModifiedDate":"2017-01-25T14:59:42","indexId":"70180201","displayToPublicDate":"2017-01-25T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Floods in southeastern Michigan, magnitude and frequency","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/70180201","usgsCitation":"Stoimenoff, L., 1963, Floods in southeastern Michigan, magnitude and frequency: Open-File Report, 9 p., https://doi.org/10.3133/70180201.","productDescription":"9 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":333930,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Michigan","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7c7e4b0ba3b075e065c","contributors":{"authors":[{"text":"Stoimenoff, L.E.","contributorId":34157,"corporation":false,"usgs":true,"family":"Stoimenoff","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":660748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70179721,"text":"70179721 - 1963 - Hydrogeologic reconnaissance of part of the headwaters area of the Price River, Utah","interactions":[],"lastModifiedDate":"2017-09-06T17:27:11","indexId":"70179721","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"4","title":"Hydrogeologic reconnaissance of part of the headwaters area of the Price River, Utah","docAbstract":"The area investigated comprises 33 square miles in the Price River drainage basin ad is in the High Plateaus section of Utah. Precipitation on most of the area ranges from about 20 to 23 inches per year, and the average annual precipitation for the entire area was assumed to be 22 inches, of which approximately 65 percent is lost by evapotranspiration. The geologic formations underlying the area are the Blackhawk and Price River Formations of Cretaceous age, the North Horn Formation of Cretaceous and Tertiary age, the Flagstaff Limestone and Colton Formation of tertiary age, and unconsolidated deposits of probable Quaternary age.
Some ground water issues from springs and seeps and is used by stock and the cities of Price and Helper. The annual discharge from the springs and seeps in the area averages about 3,000 acre-feet. Two deep wells supply about 400 acre-feet per year for use at a steam-generating plant. The aquifers penetrated by the wells are in the Flagstaff Limestone and the North Horn formation, the deepest aquifer being about 1,500 feet below the land surface. Most of the ground water in the area is suitable for municipal and industrial use.
The surface discharge from the area is approximately 6,000 acre-feet per year. By means of a water budget, it is calculated that approximately 4,000 acre-feet per year leaves the area by subsurface flow. Further development of ground water on a large scale can be accomplished only by the use of wells. It is possible, however, that part of any newly developed supply from wells may be drawn from existing spring discharge or streamflow.
","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State Engineer of Utah and the Price River Water Improvement District","usgsCitation":"Cordova, R.M., 1963, Hydrogeologic reconnaissance of part of the headwaters area of the Price River, Utah: Utah Geological and Mineralogical Survey Water-Resources Bulletin 4, 26 p.","productDescription":"26 p.","numberOfPages":"28","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333196,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333192,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-4.pdf"}],"country":"United States","state":"Utah","county":"Carbon County, Utah County","otherGeospatial":"Price River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.13700866699219,\n 39.761047087593965\n ],\n [\n -111.13700866699219,\n 39.87127666240552\n ],\n [\n -110.98526000976562,\n 39.87127666240552\n ],\n [\n -110.98526000976562,\n 39.761047087593965\n ],\n [\n -111.13700866699219,\n 39.761047087593965\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d8","contributors":{"authors":[{"text":"Cordova, Robert M.","contributorId":178302,"corporation":false,"usgs":true,"family":"Cordova","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":658427,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70179734,"text":"70179734 - 1963 - Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data","interactions":[],"lastModifiedDate":"2017-09-06T17:19:25","indexId":"70179734","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"3-I","title":"Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data","docAbstract":"This report presents the data collected for a study of the dissolved-mineral load contributed by surficial sources to Great Salt Lake, Utah. The study was conducted by the U.S. Geological Survey in cooperation with the University of Utah during the period from July 1959 through June 1962, and is part of an overall investigation of the Great Salt Lake basin by the University. Financial support for the study was provided by the U.S. Geological Survey and by the University of Utah Research Fund and Uniform School Fund. Some of the data presented in this report were obtained as part of cooperative programs between the Geological Survey and other agencies.
","language":"English","publisher":"Utah Geological and Minerological Society","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with The College of Mines and Mineral Industries, University of Utah, Salt Lake City, Utah","usgsCitation":"Hahl, D.C., and Mitchell, C., 1963, Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data: Utah Geological and Mineralogical Survey Water-Resources Bulletin 3-I, 39 p.","productDescription":"39 p.","numberOfPages":"51","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345533,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70179736","text":"Part II: Technical report"},{"id":345532,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-3part1.pdf"},{"id":333225,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.2305908203125,\n 40.59727063442024\n ],\n [\n -113.2305908203125,\n 41.795888098191426\n ],\n [\n -111.81884765624999,\n 41.795888098191426\n ],\n [\n -111.81884765624999,\n 40.59727063442024\n ],\n [\n -113.2305908203125,\n 40.59727063442024\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d6","contributors":{"authors":[{"text":"Hahl, D. C.","contributorId":57436,"corporation":false,"usgs":true,"family":"Hahl","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":658473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mitchell, C.G.","contributorId":177183,"corporation":false,"usgs":true,"family":"Mitchell","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":658474,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70179720,"text":"70179720 - 1963 - Ground-water conditions in the southern and central parts of the East Shore area, Utah, 1953-61","interactions":[],"lastModifiedDate":"2017-09-06T17:27:46","indexId":"70179720","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Ground-water conditions in the southern and central parts of the East Shore area, Utah, 1953-61","docAbstract":"The East Shore area is in north-central Utah between the Wasatch Range and Great Salt Lake, and it has been divided into the Bountiful, Weber Delta, and Brigham ground-water districts, from south to north. The area described in this report includes the Bountiful and Weber Delta districts and the southernmost part of the Brigham district. Long-term mean annual precipitation at Ogden is 17.07 inches, and the average annual temperature over the area is about 50°F. The population of the project area increased by 54 per cent from 1950 to 1960 and should increase rapidly in the future.
","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State Engineer of Utah","usgsCitation":"Smith, R., and Gates, J., 1963, Ground-water conditions in the southern and central parts of the East Shore area, Utah, 1953-61: Utah Geological and Mineralogical Survey Water-Resources Bulletin 2, 41 p.","productDescription":"41 p.","numberOfPages":"45","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333191,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333190,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-2.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"East Shore Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.961669921875,\n 40.91351257612758\n ],\n [\n -111.807861328125,\n 40.871987756697415\n ],\n [\n -111.72546386718749,\n 40.901057866884024\n ],\n [\n -111.8243408203125,\n 41.04207384890103\n ],\n [\n -111.8792724609375,\n 41.24064190269475\n ],\n [\n -111.9232177734375,\n 41.36031866306708\n ],\n [\n -111.96716308593749,\n 41.43860847395721\n ],\n [\n -112.0660400390625,\n 41.41801503608024\n ],\n [\n -112.0440673828125,\n 41.36444153054222\n ],\n [\n -112.06192016601562,\n 41.35928790538517\n ],\n [\n -112.09762573242188,\n 41.335575973123916\n ],\n [\n -112.13882446289061,\n 41.347948493443546\n ],\n [\n -112.13470458984375,\n 41.36547220659749\n ],\n [\n -112.21435546875,\n 41.35413387210046\n ],\n [\n -112.225341796875,\n 41.3304200625732\n ],\n [\n -112.20474243164062,\n 41.31701278537454\n ],\n [\n -112.21572875976561,\n 41.30360274975627\n ],\n [\n -112.236328125,\n 41.28915808826864\n ],\n [\n -112.26104736328125,\n 41.24890252240322\n ],\n [\n -112.21710205078125,\n 41.23238023874139\n ],\n [\n -112.20199584960938,\n 41.17762034260712\n ],\n [\n -112.16903686523436,\n 41.13005574377673\n ],\n [\n -112.14019775390625,\n 41.106260503564485\n ],\n [\n -112.12646484375,\n 41.06485693206886\n ],\n [\n -112.10723876953124,\n 41.0565730874647\n ],\n [\n -112.08389282226561,\n 41.036894775104436\n ],\n [\n -112.05093383789062,\n 41.03171529379291\n ],\n [\n -112.01248168945312,\n 41.0130657870063\n ],\n [\n -111.96578979492188,\n 41.000629848685385\n ],\n [\n -111.94931030273438,\n 40.985081625514354\n ],\n [\n -111.9342041015625,\n 40.948788179193485\n ],\n [\n -111.90673828125,\n 40.944639085793064\n ],\n [\n -111.93557739257811,\n 40.91973905106219\n ],\n [\n -111.94793701171875,\n 40.91558813293605\n ],\n [\n -111.961669921875,\n 40.91351257612758\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5aee4b0847d353f44da","contributors":{"authors":[{"text":"Smith, Ralph E.","contributorId":178301,"corporation":false,"usgs":true,"family":"Smith","given":"Ralph E.","affiliations":[],"preferred":false,"id":658425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":658426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70179901,"text":"70179901 - 1963 - Effects on the shallow artesian aquifer of withdrawing water from the deep artesian aquifer near Sugarville, Millard County, Utah","interactions":[],"lastModifiedDate":"2017-01-19T17:44:45","indexId":"70179901","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5258,"text":"Utah State Engineer Water Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"10","title":"Effects on the shallow artesian aquifer of withdrawing water from the deep artesian aquifer near Sugarville, Millard County, Utah","docAbstract":"Ground water occurs in a shallow (unconfined) aquifer and in at least two artesian (confined) aquifers in the unconsolidated alluvial material composing the valley fill near Sugarville, Utah. No wells are known to withdraw water from the unconfined aquifer, and this report is limited to a discussion of the effects of pumping a well tapping one artesian aquifer on the piezometric surfaces of the water in both artesian aquifers.
","language":"English","publisher":"Utah State Engineer's Office","publisherLocation":"Salt Lake City, UT","usgsCitation":"Mower, R.W., 1963, Effects on the shallow artesian aquifer of withdrawing water from the deep artesian aquifer near Sugarville, Millard County, Utah: Utah State Engineer Water Circular 10, 9 p.","productDescription":"9 p.","numberOfPages":"12","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333519,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333518,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-4-190"}],"country":"United States","state":"Utah","city":"Sugarville","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5881def9e4b01192927d9ffd","contributors":{"authors":[{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659147,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70179902,"text":"70179902 - 1963 - Test drilling in the upper Sevier River drainage basin, Garfield and Piute Counties, Utah","interactions":[],"lastModifiedDate":"2017-01-19T17:51:02","indexId":"70179902","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5258,"text":"Utah State Engineer Water Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"12","title":"Test drilling in the upper Sevier River drainage basin, Garfield and Piute Counties, Utah","docAbstract":"A test-drilling program was conducted by the U.S. Geological Survey in the upper Sevier River drainage basin (fig. 1) in the summer of 1962. The program was part of a ground-water investigation made in cooperation with the Utah State Engineer. The drilling was financed cooperatively through the State Engineer by the U.S. Geological Survey, Garfield, Piute, Sevier, Sanpete, and Millard Counties, and various water users within those counties. Drilling began in May and continued through September 1962, and 21 test holes were drilled.
","language":"English","publisher":"Utah State Engineer's Office","publisherLocation":"Salt Lake City, UT","usgsCitation":"Feltis, R., and Robinson, G., 1963, Test drilling in the upper Sevier River drainage basin, Garfield and Piute Counties, Utah: Utah State Engineer Water Circular 12, 32 p.","productDescription":"32 p.","numberOfPages":"36","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333521,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333520,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-4-230"}],"country":"United States","state":"Utah","otherGeospatial":"Sevier Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5881def9e4b01192927d9ffb","contributors":{"authors":[{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":659148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, G.B.","contributorId":178487,"corporation":false,"usgs":true,"family":"Robinson","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":659149,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70161788,"text":"70161788 - 1963 - Hermaphroditism in rainbow trout","interactions":[],"lastModifiedDate":"2016-08-15T21:28:03","indexId":"70161788","displayToPublicDate":"2015-10-13T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Hermaphroditism in rainbow trout","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1963)92[313:HIRT]2.0.CO;2","usgsCitation":"Ross, A.J., Yasutake, W.T., and White, G., 1963, Hermaphroditism in rainbow trout: Transactions of the American Fisheries Society, v. 92, no. 3, p. 313-315, https://doi.org/10.1577/1548-8659(1963)92[313:HIRT]2.0.CO;2.","productDescription":"3 p.","startPage":"313","endPage":"315","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":313906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"92","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e490fe4b0e7a44bc419d0","contributors":{"authors":[{"text":"Ross, A. J.","contributorId":105267,"corporation":false,"usgs":true,"family":"Ross","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":587769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, W. T.","contributorId":103222,"corporation":false,"usgs":true,"family":"Yasutake","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":587770,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, G.R.","contributorId":152066,"corporation":false,"usgs":false,"family":"White","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":587771,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70161191,"text":"70161191 - 1963 - In vitro culture of the flagellate protozoan Hexamita salmonis","interactions":[],"lastModifiedDate":"2017-01-12T11:34:26","indexId":"70161191","displayToPublicDate":"2015-10-06T05:15:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"In vitro culture of the flagellate protozoan Hexamita salmonis","docAbstract":"Trophozoites of Hexamita salmonis, asserted pathogen of juvenile salmonid fishes, were isolated from two species of Pacific salmon hosts and cultured repeatedly in an organic medium saturated with nitrogen. Primary isolates and serial subcultures usually exhibited five- to tenfold population increases per passage.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.140.3564.290","usgsCitation":"Uzmann, J., and Hayduk, S., 1963, In vitro culture of the flagellate protozoan Hexamita salmonis: Science, v. 140, no. 3564, p. 290-292, https://doi.org/10.1126/science.140.3564.290.","productDescription":"3 p.","startPage":"290","endPage":"292","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313397,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"140","issue":"3564","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568cf744e4b0e7a44bc0f16d","contributors":{"authors":[{"text":"Uzmann, J. R.","contributorId":38647,"corporation":false,"usgs":true,"family":"Uzmann","given":"J. R.","affiliations":[],"preferred":false,"id":585141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayduk, S.H.","contributorId":151275,"corporation":false,"usgs":false,"family":"Hayduk","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":585142,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70161779,"text":"70161779 - 1963 - Sacramento River chinook disease","interactions":[],"lastModifiedDate":"2016-01-06T09:15:15","indexId":"70161779","displayToPublicDate":"2015-10-05T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":42,"text":"Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"497","title":"Sacramento River chinook disease","docAbstract":"Epizootics among chinook salmon fingerlings at the Coleman National Fish Hatchery have occurred periodically since 1941. A virus or virus-like filterable agent has been demonstrated to be the causative agent of this disease.
","language":"English","publisher":"U.S. Department of the Interior, Bureau Sport Fisheries and Wildlife","usgsCitation":"Ross, A.J., and Rucker, R., 1963, Sacramento River chinook disease: Leaflet 497, 3 p.","productDescription":"3 p.","numberOfPages":"3","costCenters":[],"links":[{"id":313893,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":313891,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://spo.nmfs.noaa.gov/Fishery%20Leaflets/leaflet497.pdf","text":"pdf"},{"id":313892,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://spo.nwr.noaa.gov/fisheryleaflets.htm"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e4928e4b0e7a44bc41a56","contributors":{"authors":[{"text":"Ross, A. J.","contributorId":105267,"corporation":false,"usgs":true,"family":"Ross","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":587733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":587734,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70161190,"text":"70161190 - 1963 - The Hexamita(= Octomitus) problem: A preliminary report","interactions":[],"lastModifiedDate":"2017-01-11T16:01:49","indexId":"70161190","displayToPublicDate":"2015-09-15T09:15:00","publicationYear":"1963","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":"The Hexamita(= Octomitus) problem: A preliminary report","docAbstract":"THE INTESTINAL FLAGELLATE, Hexamita salmonis (Moore), was described in 1922 from trout in hatcheries throughout New York State. At first associated with the so-called whirling disease of brook trout (Salvelinus fontinalis), now believed to be a virus disease, Hexamita was subsequently held responsible for practically any otherwise unexplainable mortality in underyearling salmonids. Over the years, Hexamita, ostensibly H. salmonis, has been the most readily recognized parasite of juvenile salmonids.
\n","language":"English","publisher":"The Progressive Fish-Culturist","doi":"10.1577/1548-8659(1963)25[141:THOP]2.0.CO;2","usgsCitation":"Uzmann, J., and Jesse, J., 1963, The Hexamita(= Octomitus) problem: A preliminary report: Progressive Fish-Culturist, v. 25, no. 3, p. 141-143, https://doi.org/10.1577/1548-8659(1963)25[141:THOP]2.0.CO;2.","productDescription":"3 p.","startPage":"141","endPage":"143","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313396,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568cf74ae4b0e7a44bc0f190","contributors":{"authors":[{"text":"Uzmann, J. R.","contributorId":38647,"corporation":false,"usgs":true,"family":"Uzmann","given":"J. R.","affiliations":[],"preferred":false,"id":585139,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jesse, J.W.","contributorId":151274,"corporation":false,"usgs":false,"family":"Jesse","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":585140,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70161146,"text":"70161146 - 1963 - Formalin in the Hatchery","interactions":[],"lastModifiedDate":"2016-01-05T10:35:51","indexId":"70161146","displayToPublicDate":"2015-09-14T09:30:00","publicationYear":"1963","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":"Formalin in the Hatchery","docAbstract":"
FORMALIN is used extensively in hatcheries to control external parasites of fish. There are reports that formalin is toxic at some hatcheries, especially when used on rainbow trout (Salmo gairdneri). This is a discussion of the development of the use of formalin to control fish parasite-in the hatchery, its properties, and some experimental work.
\n","language":"English","publisher":"Bureau of Fisheries, U.S. Department of Commerce","doi":"10.1577/1548-8659(1963)25[203:FITH]2.0.CO;2","usgsCitation":"Rucker, R., Taylor, W., and Toney, D., 1963, Formalin in the Hatchery: Progressive Fish-Culturist, v. 25, no. 4, p. 203-207, https://doi.org/10.1577/1548-8659(1963)25[203:FITH]2.0.CO;2.","productDescription":"5 p.","startPage":"203","endPage":"207","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313366,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568cf741e4b0e7a44bc0f15b","contributors":{"authors":[{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":584929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, W.G.","contributorId":76264,"corporation":false,"usgs":true,"family":"Taylor","given":"W.G.","email":"","affiliations":[],"preferred":false,"id":584930,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Toney, D.P.","contributorId":151243,"corporation":false,"usgs":false,"family":"Toney","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":584931,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70161780,"text":"70161780 - 1963 - A new geographic and host record for infectious pancreatic necrosis","interactions":[],"lastModifiedDate":"2016-01-06T09:21:33","indexId":"70161780","displayToPublicDate":"2015-09-14T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":" A new geographic and host record for infectious pancreatic necrosis","docAbstract":"
The occurrence of infectious pancreatic necrosis in rainbow trout (Salmo gairdneri), brook trout (Salvelinus fontinalis), and cutthroat trout (Salmo clarki) has been experimentally authenticated for the first time in the western United States. The cutthroat trout represents a new host. Brook trout fin tissue culture inoculated with bacteria-free filtrate from the diseased fish tissue showed marked degenerative changes after 24 hours. Chinook salmon (Oncorhynchus tshawytscha), kokanee (O. nerka), and silver salmon (O. kisutch) were not susceptible to the virus when inoculated. Histologically, extensive pancreatic necrosis was observed in the original and experimental materials, but striated muscle hyalinization was detected only in the original material.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1963)92[63:ANGAHR]2.0.CO;2","usgsCitation":"Parisot, T., Yasutake, W.T., and Bressler, V., 1963, A new geographic and host record for infectious pancreatic necrosis: Transactions of the American Fisheries Society, v. 92, no. 1, p. 63-66, https://doi.org/10.1577/1548-8659(1963)92[63:ANGAHR]2.0.CO;2.","productDescription":"4 p.","startPage":"63","endPage":"66","numberOfPages":"4","costCenters":[],"links":[{"id":313895,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"92","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e48c6e4b0e7a44bc417f8","contributors":{"authors":[{"text":"Parisot, T. J.","contributorId":43014,"corporation":false,"usgs":true,"family":"Parisot","given":"T. J.","affiliations":[],"preferred":false,"id":587738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yasutake, W. T.","contributorId":103222,"corporation":false,"usgs":true,"family":"Yasutake","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":587739,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bressler, V.","contributorId":152056,"corporation":false,"usgs":false,"family":"Bressler","given":"V.","email":"","affiliations":[],"preferred":false,"id":587740,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70161192,"text":"70161192 - 1963 - Co-oxidation of the sulfur-containing amino acids in an autoxidizing lipid system","interactions":[],"lastModifiedDate":"2016-01-05T10:57:40","indexId":"70161192","displayToPublicDate":"2015-09-08T05:15:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2293,"text":"Journal of Food Science","active":true,"publicationSubtype":{"id":10}},"title":"Co-oxidation of the sulfur-containing amino acids in an autoxidizing lipid system","docAbstract":"Oxidation of the sulfur amino acids by autoxidizing lipids was studied in a model system consisting of an amino acid dispersed in cold-pressed, molecularly distilled menhaden oil (20–80% w/w). Under all conditions investigated, cysteine was oxidized completely to cystine. Preliminary results suggest that at 110°C the oxidation follows first-order kinetics for at least the first 8 hr. A specific reaction rate constant of 0.25 per hour was calculated. When fatty acids were added to the system, cystine was oxidized to its thiosulfinate ester. When the fatty acid-cystine ratio was 1:2, oxidation of cystine was a maximum. No oxidation of cystine occurred unless either a fatty acid, volatile organic acid, or ethanol was added. Under the conditions investigated, methionine was not oxidized to either its sulfoxide or its sulfone.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2621.1963.tb00239.x","usgsCitation":"Wedemeyer, G., and Dollar, A., 1963, Co-oxidation of the sulfur-containing amino acids in an autoxidizing lipid system: Journal of Food Science, v. 28, no. 5, p. 537-540, https://doi.org/10.1111/j.1365-2621.1963.tb00239.x.","productDescription":"4 p.","startPage":"537","endPage":"540","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313399,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"5","noUsgsAuthors":false,"publicationDate":"2006-08-25","publicationStatus":"PW","scienceBaseUri":"568cf73ee4b0e7a44bc0f13f","contributors":{"authors":[{"text":"Wedemeyer, Gary","contributorId":94244,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","affiliations":[],"preferred":false,"id":585143,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dollar, A.M.","contributorId":150882,"corporation":false,"usgs":false,"family":"Dollar","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":585144,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70161787,"text":"70161787 - 1963 - Mycobacteria in adult salmonid fishes returning to national fish hatcheries in Washington, Oregon and California in 1958-59","interactions":[],"lastModifiedDate":"2016-01-06T09:53:08","indexId":"70161787","displayToPublicDate":"2015-09-07T00:00:00","publicationYear":"1963","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":"462","title":"Mycobacteria in adult salmonid fishes returning to national fish hatcheries in Washington, Oregon and California in 1958-59","docAbstract":"Incidence of acid-fast bacillus infections in salmonid fishes at West Coast hatcheries was determined for 1957-59. No evidence was obtained which would indicate a definite trend towards either increased or decreased rates of infection. It is apparent that the incidence of infection is higher in hatchery-marked fish than in unmarked fish. Only one hatchery was found free of infection during the 3 years covered by the investigation. This installation had never used raw salmon products in diet.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei830","usgsCitation":"Robie, R.A., Bethke, P., Toulmin, M., and Edwards, J.L., 1963, X-ray crystallographic data for minerals: U.S. Geological Survey Trace Elements Investigations 830, 38 p., https://doi.org/10.3133/tei830.","productDescription":"38 p.","numberOfPages":"42","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310434,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/830/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":309848,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei830.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"561e2b3ee4b0cdb063e59d01","contributors":{"authors":[{"text":"Robie, Richard A.","contributorId":92235,"corporation":false,"usgs":true,"family":"Robie","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":577267,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bethke, Philip M.","contributorId":52829,"corporation":false,"usgs":true,"family":"Bethke","given":"Philip M.","affiliations":[],"preferred":false,"id":577268,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Toulmin, M.S.","contributorId":62677,"corporation":false,"usgs":true,"family":"Toulmin","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":577269,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, Jerry L.","contributorId":149197,"corporation":false,"usgs":false,"family":"Edwards","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":577270,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}