{"pageNumber":"5867","pageRowStart":"146650","pageSize":"25","recordCount":165658,"records":[{"id":1000383,"text":"1000383 - 1968 - The alewife","interactions":[],"lastModifiedDate":"2012-02-02T00:04:13","indexId":"1000383","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2623,"text":"Limnos","active":true,"publicationSubtype":{"id":10}},"title":"The alewife","docAbstract":"When the first alewife, Alosa pseudoharengus, was discovered in Lake Michigan near South Manitou Island on May 5, 1949, few people would have guessed that it would become the best known fish of the lake in less than two decades. Now it competes only with the coho salmon in its claim to such fame. When the third specimen was officially recorded from Milwaukee, Wisconsin, in March 1952, however, a newspaper story carried a somber warning from a knowledgeable yet anonymous official of the Michigan Department of Conservation that the alewife might raise havoc with the native species. This warning was fully justified by fact in the years to follow. An upset of the entire fishery ecology of Lake Michigan was already well under way in 1949 when the sea lamprey was consuming the last vestiges of the lake trout (Salvelinus namaycush) and burbot (Lota lota)- the only abundant and widely distributed predators of the lake. Absence of large predators left the way wide open for a small and prolific species such as the alewife. Under this condition the alewife increased with almost unbelievable swiftness.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Limnos","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Smith, S.H., 1968, The alewife: Limnos, v. 1, no. 2, p. 12-20.","productDescription":"p. 12-20","startPage":"12","endPage":"20","numberOfPages":"8","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":129211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6696d9","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308487,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171724,"text":"70171724 - 1968 - A preliminary report of a recently discovered aquifer at Sioux Falls, South Dakota","interactions":[],"lastModifiedDate":"2017-10-15T12:48:04","indexId":"70171724","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5088,"text":"South Dakota Academy of Science Proceedings","active":true,"publicationSubtype":{"id":10}},"title":"A preliminary report of a recently discovered aquifer at Sioux Falls, South Dakota","docAbstract":"

A hydrologic study of the Big Sioux aquifer system was begun July 1, 1966, by the U.S. Geological Survey, in cooperation with the City of Sioux Falls and the East Dakota Conservancy Sub-District.  

\n

Test drilling being done in the search for a southern outlet to the Big Sioux aquifer has led to the discovery of the outlet and of a deeper aquifer than was previously know to exist in this area.  This aquifer, herein called the Sioux Falls aquifer, was first recognized as a very clean gravel in test hole USGS #1 between the depths of 60 to 83 feet.

\n

Subsequent test drilling and aquifer testing has shown the Sioux Falls aquifer to be capable of producing several hundred gallons of water per minute.  THe chemical quality of this water surpasses that currently being used for the city supply.

\n

Further investigation of the aquifer is planned as a part of the continuing expansion of the water-supply facilities for Sioux Falls.  

\n

This publication has been authorized by the Director of the U.S. Geological Survey and Earl McCart, Commissioner, City of Sioux Falls, South Dakota.

","language":"English","publisher":"South Dakota Academy of Science","usgsCitation":"Vaughan, K.D., and Ackroyd, E.A., 1968, A preliminary report of a recently discovered aquifer at Sioux Falls, South Dakota: South Dakota Academy of Science Proceedings, v. 47, no. 16, p. 68-74.","productDescription":"7 p.","startPage":"68","endPage":"74","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":323991,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":322193,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.sdaos.org/publications/?wpa-paged=113"}],"country":"United States","state":"South Dakota","city":"Sioux Falls","volume":"47","issue":"16","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913aee4b07657d19fef86","contributors":{"authors":[{"text":"Vaughan, Kenneth D.","contributorId":170160,"corporation":false,"usgs":false,"family":"Vaughan","given":"Kenneth","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":632207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ackroyd, Earl A.","contributorId":59425,"corporation":false,"usgs":true,"family":"Ackroyd","given":"Earl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":632208,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175658,"text":"70175658 - 1968 - Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1967","interactions":[],"lastModifiedDate":"2016-08-17T14:54:05","indexId":"70175658","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","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":"16","title":"Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1967","docAbstract":"

No abstract available.

","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Rettman, P., 1968, Chemical analyses of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas, 1967: Edwards Underground Water District Bulletin 16, 9 p.","productDescription":"9 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326756,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ac0e4b03bcb0104bb6c","contributors":{"authors":[{"text":"Rettman, Paul","contributorId":68699,"corporation":false,"usgs":true,"family":"Rettman","given":"Paul","affiliations":[],"preferred":false,"id":645938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000188,"text":"1000188 - 1968 - Annulus formation on scales of four species of coregonids reared under artificial conditions","interactions":[],"lastModifiedDate":"2019-06-11T15:23:05","indexId":"1000188","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Annulus formation on scales of four species of coregonids reared under artificial conditions","docAbstract":"

Scales from known-age coregonids reared in the laboratory were examined to determine when annuli formed and to learn possible factors of their formation. Scales were taken monthly from marked fish for periods up to 21 months. Scales were also examined from fish that died and from preserved specimens of young-of-the-year for each species. Two marks formed on almost all scales each calendar year. The stronger formed during March-April and the weaker in October-November. Both marks had all the usual characteristics of an annulus but the spring mark was considered the annulus and the fall mark an accessory check. The annulus formed during a period of constant temperatures and of little change in growth or increasing growth. The accessory check formed during a period of declining temperatures (1-5 degrees F, or 0.6-2.8 degrees C, per month) and of little change in growth or declining growth. Most fish grew throughout the winter; the only exceptions were one bloater (Coregonus hoyi) and several of the largest lake whitefish (C. clupeaformis). Fish were always given all the food they would eat to eliminate availability of food as a factor of mark formation. The temperature of the water during the winter (50 ±. 0.3 F; 10.0 ±. 0.2 C) did not arrest metabolic activity. The growth rate was related more closely to day length than to other variables examined.

","language":"English","publisher":"NRC Research Press","publisherLocation":"Ottawa, Ontario","doi":"10.1139/f68-188","usgsCitation":"Hogman, W.J., 1968, Annulus formation on scales of four species of coregonids reared under artificial conditions: Journal of the Fisheries Research Board of Canada, v. 25, no. 10, p. 2111-2122, https://doi.org/10.1139/f68-188.","productDescription":"12 p.","startPage":"2111","endPage":"2122","numberOfPages":"12","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7ec1","contributors":{"authors":[{"text":"Hogman, Walter J.","contributorId":34092,"corporation":false,"usgs":true,"family":"Hogman","given":"Walter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000465,"text":"1000465 - 1968 - Distribution and abundance of the Japanese snail, Viviparus japonicus, and associated macrobenthos in Sandusky Bay, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:04:35","indexId":"1000465","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2938,"text":"Ohio Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Distribution and abundance of the Japanese snail, Viviparus japonicus, and associated macrobenthos in Sandusky Bay, Ohio","docAbstract":"A survey of the macrobenthos of Sandusky Bay, Lake Erie, in June, 1963, provided information on the abundance and distribution of the introduced Japanese snail, Viviparus japonicus, which has become a nuisance to commercial seine fishermen. The abundance and distribution varied considerably within the bay; at the time of the survey, most snails were found near the north-central shore. Environmental characteristics were nearly uniform and had no apparent effect on the distribution; concentrations in different areas at different times appeared to result from water movements induced by winds. The time of the study coincided with a period of reproduction; young-of-the-year snails were most abundant in areas where adults were most common. The frequency distributions of shell height and diameter suggested the presence of two age groups of adults in the population. Considerable natural mortality was seen, both at the time of the study and in other seasons. Only three other gastropods were observed in the bay; the most abundant was another viviparid, Campeloma decisum. Other mollusks present were four species of Sphaeriidae and 18 species of Unionidae. A summary of invertebrates found, other than the mollusks, is also presented.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ohio Journal of Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Wolfert, D.R., and Hiltunen, J.K., 1968, Distribution and abundance of the Japanese snail, Viviparus japonicus, and associated macrobenthos in Sandusky Bay, Ohio: Ohio Journal of Science, v. 68, no. 1, p. 32-40.","productDescription":"p. 32-40","startPage":"32","endPage":"40","numberOfPages":"8","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"68","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649fb3","contributors":{"authors":[{"text":"Wolfert, David R.","contributorId":49305,"corporation":false,"usgs":true,"family":"Wolfert","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hiltunen, Jarl K.","contributorId":27820,"corporation":false,"usgs":true,"family":"Hiltunen","given":"Jarl","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":308584,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000305,"text":"1000305 - 1968 - An electric beam trawl for the capture of larval lampreys","interactions":[],"lastModifiedDate":"2013-02-04T16:05:15","indexId":"1000305","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","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":"An electric beam trawl for the capture of larval lampreys","docAbstract":"The chemicals used to control the sea lamprey, Petromyzon marinus, in the Great Lakes have drastically reduced populations of larval lampreys in tributary streams. These larvicides are too costly and difficult to apply, however, in inland lakes, estuaries, and bays. Populations of sea lampreys in these areas constitute a threat to the refinement of the control. The gear available to locate, ample, and evaluate larval populations in deep water are inefficient. Electric shockers, satisfactory for collecting ammocoetes in streams, are limited to shallow water. The use of mechanical devices such as the Petersen dredge, anchor dredge, and the orange-peel dredge is time consuming, inefficient, and relatively ineffective in providing reliable quantitative evaluation of population size and composition over large areas of bottom. A device was required to sample adequately many areas in a short period of time, regardless of the depth of water. Mobility also was essential to permit operation of the unit in the various Great Lakes and in inland waters. An electrified beam trawl has been developed that most nearly meets these requirements. It has been used successfully to collect larvae of the sea lamprey, American brook lamprey (Lampetra lamottei), northern brook lamprey (Ichthyomyzon fossor), and silver lamprey (I. unicuspis). Effectiveness of the trawl did not appear to differ with species.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"London, UK","doi":"10.1577/1548-8659(1968)97[289:AEBTFT]2.0.CO;2","collaboration":"Out-of-print","usgsCitation":"McLain, A., and Dahl, F.H., 1968, An electric beam trawl for the capture of larval lampreys: Transactions of the American Fisheries Society, v. 97, no. 3, p. 289-293, https://doi.org/10.1577/1548-8659(1968)97[289:AEBTFT]2.0.CO;2.","productDescription":"5 p.","startPage":"289","endPage":"293","numberOfPages":"5","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":266966,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1968)97[289:AEBTFT]2.0.CO;2"},{"id":131663,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"97","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684b78","contributors":{"authors":[{"text":"McLain, Alberton","contributorId":81451,"corporation":false,"usgs":true,"family":"McLain","given":"Alberton","affiliations":[],"preferred":false,"id":308366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dahl, Frederick H.","contributorId":90258,"corporation":false,"usgs":true,"family":"Dahl","given":"Frederick","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308367,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000254,"text":"1000254 - 1968 - Production of sea lamprey larvae from nests in two Lake Superior streams","interactions":[],"lastModifiedDate":"2016-02-18T11:49:52","indexId":"1000254","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","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":"Production of sea lamprey larvae from nests in two Lake Superior streams","docAbstract":"

The life history of the landlocked sea lamprey, Petromyzon marinus, has been described by several authors, the two most recent of which are Applegate and Wigley. The only information on the production of larvae from nests of the sea lamprey was reported by Applegate, who counted the larvae from three nests in the Ocqueoc River, a tributary of Lake Huron. The present report presents data on the hatching success of sea lamprey larvae from 19 nests in two small tributaries of southern Lake Superior and indicates greater production per nest than that recorded by Applegate. Studies were conducted by personnel of the U.S. Bureau of Commercial Fisheries on the Little Garlic River, Marquette County, Michigan, and on the Traverse River, Keweenaw County, Michigan.

","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1968)97[484:POSLLF]2.0.CO;2","usgsCitation":"Manion, P.J., 1968, Production of sea lamprey larvae from nests in two Lake Superior streams: Transactions of the American Fisheries Society, v. 97, no. 4, p. 484-486, https://doi.org/10.1577/1548-8659(1968)97[484:POSLLF]2.0.CO;2.","productDescription":"3 p.","startPage":"484","endPage":"486","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132868,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"97","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e426","contributors":{"authors":[{"text":"Manion, Patrick J.","contributorId":99080,"corporation":false,"usgs":true,"family":"Manion","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308297,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009907,"text":"70009907 - 1968 - SrRbK and Sr isotopic relationships in ultramafic rocks, southeastern Alaska","interactions":[],"lastModifiedDate":"2020-11-29T17:15:06.635578","indexId":"70009907","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"SrRbK and Sr isotopic relationships in ultramafic rocks, southeastern Alaska","docAbstract":"

Geologic evidence suggests that a series of ultramafic complexes of the ‘Duke Island type’ located along a 560 km-long belt in southeastern Alaska crystallized from magmas of ultramafic composition. Some geologists have proposed that these magmas were derived by fractional fusion of ultramafic material in the upper mantle. The87Sr/86Sr ratios, corrected for growth of radiogenic87Sr, in total rock samples and in minerals from four ultramafic complexes range from 0.7026 to 0.7068, and the K/Rb ratios in total rock samples range from 300 to 1200. Other workers have reported that the isotopic composition of strontium in alpine peridotites is significantly different from that of oceanic volcanic rocks, but the87Sr/86Sr ratios of the Alaskan ultramafites and of oceanic volcanic rocks are similar.

","language":"English","publisher":"Elseiver","doi":"10.1016/0012-821X(68)90033-2","issn":"0012821X","usgsCitation":"Lanphere, M.A., 1968, SrRbK and Sr isotopic relationships in ultramafic rocks, southeastern Alaska: Earth and Planetary Science Letters, v. 4, no. 3, p. 185-190, https://doi.org/10.1016/0012-821X(68)90033-2.","productDescription":"6 p.","startPage":"185","endPage":"190","numberOfPages":"6","costCenters":[],"links":[{"id":219728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -137.4609375,\n 54.49556752187406\n ],\n [\n -129.814453125,\n 54.49556752187406\n ],\n [\n -129.814453125,\n 58.6769376725869\n ],\n [\n -137.4609375,\n 58.6769376725869\n ],\n [\n -137.4609375,\n 54.49556752187406\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"4","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9642e4b08c986b31b3d6","contributors":{"authors":[{"text":"Lanphere, M. A.","contributorId":35298,"corporation":false,"usgs":true,"family":"Lanphere","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":357417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009909,"text":"70009909 - 1968 - The relationship of geophysical measurements to engineering and construction parameters in the Straight Creek Tunnel pilot bore, Colorado","interactions":[],"lastModifiedDate":"2020-11-29T17:08:01.364611","indexId":"70009909","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2071,"text":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"The relationship of geophysical measurements to engineering and construction parameters in the Straight Creek Tunnel pilot bore, Colorado","docAbstract":"

Seismic-refraction and electrical-resistivity measurements made along the walls of the Straight Creek Tunnel pilot bore indicate that both a low-velocity and a high-resistivity layer exist in the disturbed rock surrounding the excavation. Seismic measurements were analyzed to obtain the thickness and seismic velocity of rock in the low-velocity layer, the velocity of rock behind the layer and the amplitude of seismic energy received at the detectors. Electrical-resistivity measurements were analyzed to obtain the thickness and electrical resistivity of the high-resistivity layer and the resistivity of rock behind the layer. The electrical resistivity and the seismic velocity of rock at depth, the thickness of rock in the low-velocity layer, and the relative amplitude of seismic energy were correlated against the following parameters, all of which are important in tunnel construction: height of the tension arch, stable vertical rock load, rock quality, rate of construction and cost per foot, percentage of lagging and blocking, set spacing, and type and amount of steel support required, The correlations were statistically meaningful, having correlation coefficients ranging in absolute value from about 0·7 to nearly 1·0. This finding suggests the possibility of predicting parameters of interest in tunnel construction from geophysical measurements made in feeler holes drilled ahead of a working face. Predictions might be based on correlations established either during the early stages of construction or from geophysical surveys in other tunnels of similar design in similar geologic environments.

","language":"English","publisher":"Elsevier","doi":"10.1016/0148-9062(68)90020-X","issn":"01489062","usgsCitation":"Scott, J.H., Lee, F.T., Carroll, R.D., and Robinson, C.S., 1968, The relationship of geophysical measurements to engineering and construction parameters in the Straight Creek Tunnel pilot bore, Colorado: International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, v. 5, no. 1, p. 1-30, https://doi.org/10.1016/0148-9062(68)90020-X.","productDescription":"30 p.","startPage":"1","endPage":"30","numberOfPages":"30","costCenters":[],"links":[{"id":218609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Straight Creek area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.01806640624999,\n 39.40012200014591\n ],\n [\n -105.32867431640625,\n 39.40012200014591\n ],\n [\n -105.32867431640625,\n 39.76210275375139\n ],\n [\n -106.01806640624999,\n 39.76210275375139\n ],\n [\n -106.01806640624999,\n 39.40012200014591\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baf23e4b08c986b324592","contributors":{"authors":[{"text":"Scott, J. H.","contributorId":15204,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":357419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, F. T.","contributorId":50163,"corporation":false,"usgs":true,"family":"Lee","given":"F.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":357421,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carroll, R. D.","contributorId":53373,"corporation":false,"usgs":true,"family":"Carroll","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":357422,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robinson, C. S.","contributorId":23578,"corporation":false,"usgs":true,"family":"Robinson","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":357420,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70171228,"text":"70171228 - 1968 - Some effects of mirex on two warm-water fishes","interactions":[],"lastModifiedDate":"2016-05-25T16:44:44","indexId":"70171228","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","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":"Some effects of mirex on two warm-water fishes","docAbstract":"

The effects of mirex on two species of warm-water fishes were studied in three experiments in which the fish were exposed either by feeding a mirex-treated diet, or by treating the holding ponds with a mirex formulation. Bluegills were used in the feeding experiment, where three different levels of mirex were incorporated into the diet and fed to fish held in plastic pools, and in the first pond-exposure experiment, in which the fish were held in earthen ponds treated once with a mirex-corncob grit formulation. The third experiment used goldfish held in earthen ponds which also were treated once with the mirex-corncob grit formulation. In general, higher rates of exposure produced higher whole-body residues of mirex in the fish, and, except in bluegills from the lower-treatment ponds of the first contact experiment and in control fish, whole-body residues increased throughout the terms of these experiments. Soil, water, and vegetation samples from the two contact experiments, although subject to large differences between individual samples, contained relatively unchanging mirex concentrations, illustrating that this chemical is highly resistant to degradation or removal. No mortality or tissue pathology in the bluegills could be ascribed to mirex exposure, but the gills and kidneys of mirex-exposed goldfish showed reactions beginning with the samples taken 56 days after treatment, and the numbers of these fish surviving until termination of this experiment were inversely related to treatment level. Total serum protein and hematocrit percentages had no apparent relationship to treatment levels, nor was mirex exposure a demonstrable factor in growth rates in the contact experiments. However, growth of the bluegills in the highest treatment groups of the feeding experiment was adversely affected. Invertebrate populations seemed not to be affected by the mirex treatment in either of the earthen pond experiments.

","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1968)97[185:SEOMOT]2.0.CO;2","usgsCitation":"Van Valin, C.C., Andrews, A.K., and Eller, L.L., 1968, Some effects of mirex on two warm-water fishes: Transactions of the American Fisheries Society, v. 97, no. 2, p. 185-196, https://doi.org/10.1577/1548-8659(1968)97[185:SEOMOT]2.0.CO;2.","productDescription":"12 p.","startPage":"185","endPage":"196","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":321695,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"97","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccc2e4b07e28b662dd2f","contributors":{"authors":[{"text":"Van Valin, Charles C.","contributorId":169609,"corporation":false,"usgs":false,"family":"Van Valin","given":"Charles","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":630317,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andrews, Austin K.","contributorId":85516,"corporation":false,"usgs":true,"family":"Andrews","given":"Austin","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":630318,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eller, Lafayette L.","contributorId":31259,"corporation":false,"usgs":true,"family":"Eller","given":"Lafayette","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630319,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70171224,"text":"70171224 - 1968 - Some enzymatic properties of brain Acetylcholinesterase from bluegill and channel catfish","interactions":[],"lastModifiedDate":"2016-05-25T16:30:21","indexId":"70171224","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Some enzymatic properties of brain Acetylcholinesterase from bluegill and channel catfish","docAbstract":"

Using a manometric technique an acetylcholinesterase (EC 3.1.1.7, acetylcholine acetyl-hydrolase) was demonstrated in brain tissue from the bluegill, Lepomis macrochirus Rafinesque, and the channel catfish, Ictalurus punctatus (Walbaum). The activities were 19 and 37 μmoles acetylcholine hydrolyzed/milligram protein per hour for the bluegill and channel catfish enzymes, respectively. The optimum substrate concentration for the hydrolysis of acetylcholine was 10 mMfor the enzymes from both species. Generally, the catfish acetylcholinesterase was somewhat more susceptible than the bluegill to the inhibitors tested; however, the bluegill enzyme was more susceptible to inhibition by malathion and malaoxon.

","language":"English","publisher":"NRC Research Press","doi":"10.1139/f68-059","usgsCitation":"Hogan, J.W., and Knowles, C.O., 1968, Some enzymatic properties of brain Acetylcholinesterase from bluegill and channel catfish: Journal of the Fisheries Research Board of Canada, v. 25, no. 4, p. 615-623, https://doi.org/10.1139/f68-059.","productDescription":"9 p.","startPage":"615","endPage":"623","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":321689,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccc3e4b07e28b662dd31","contributors":{"authors":[{"text":"Hogan, James W.","contributorId":24402,"corporation":false,"usgs":true,"family":"Hogan","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":630308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knowles, Charles O.","contributorId":169621,"corporation":false,"usgs":false,"family":"Knowles","given":"Charles","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":630309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5224847,"text":"5224847 - 1968 - Reward banding to determine reporting rate of recovered mourning dove bands","interactions":[],"lastModifiedDate":"2025-02-14T16:49:41.836378","indexId":"5224847","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Reward banding to determine reporting rate of recovered mourning dove bands","docAbstract":"

Reward bands placed on the other leg of certain regularly banded immature mourning doves (Zenaidura macroura) were used to develop information on reporting rates of recovered dove bands. Reports from 15 widely separated sections of the United States showed considerable variation in recovery rate of doves both with and without reward bands. The overall percentages of banded doves that were reported as recovered were 9.69% for those with reward bands and 3.83% for controls. The bandreporting rate for states influenced by publicity was 66%; that for states not influenced was 32%.

","language":"English","publisher":"Wiley","doi":"10.2307/3798230","usgsCitation":"Tomlinson, R.E., 1968, Reward banding to determine reporting rate of recovered mourning dove bands: Journal of Wildlife Management, v. 32, no. 1, p. 6-11, https://doi.org/10.2307/3798230.","productDescription":"6 p.","startPage":"6","endPage":"11","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196029,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"geometry\": {\n \"type\": \"MultiPolygon\",\n \"coordinates\": [\n [\n [\n [\n -94.81758,\n 49.38905\n ],\n [\n -94.64,\n 48.84\n ],\n [\n -94.32914,\n 48.67074\n ],\n [\n -93.63087,\n 48.60926\n ],\n [\n -92.61,\n 48.45\n ],\n [\n -91.64,\n 48.14\n ],\n [\n -90.83,\n 48.27\n ],\n [\n -89.6,\n 48.01\n ],\n 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-95.15609,\n 49.38425\n ],\n [\n -94.81758,\n 49.38905\n ]\n ]\n ]\n ]\n },\n \"properties\": {\n \"name\": \"United States\"\n }\n }\n ]\n}","volume":"32","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6027a2","contributors":{"authors":[{"text":"Tomlinson, R. E.","contributorId":78830,"corporation":false,"usgs":true,"family":"Tomlinson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":342891,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1003254,"text":"1003254 - 1968 - Gas chromatographic separation and quantitative estimation of barbiturate mixtures in solid dosage forms","interactions":[],"lastModifiedDate":"2025-03-03T16:08:06.326502","indexId":"1003254","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2533,"text":"Journal of the Association of Official Analytical Chemists","active":true,"publicationSubtype":{"id":10}},"title":"Gas chromatographic separation and quantitative estimation of barbiturate mixtures in solid dosage forms","docAbstract":"

A gas chromatographic method has been described for the analysis of mixed barbiturates in solid dosage forms. Analysis on a 10% SE-30 column gave good separations for butabarbital, amobarbital, secobarbital, pentobarbital, and/or phenobarbital; amobarbital is not separated adequately from pentobarbital. An internal standard, mephobarbital, is used to minimize injection errors. The method gives both good quantitative and qualitative results on the barbiturates investigated. Two synthetic tablet mixtures were analyzed by this procedure and recoveries were 98—103%. It is recommended that the method be subjected to collaborative study.

","language":"English","publisher":"Oxford Academic","doi":"10.1093/jaoac/51.3.619","usgsCitation":"Allen, J.L., 1968, Gas chromatographic separation and quantitative estimation of barbiturate mixtures in solid dosage forms: Journal of the Association of Official Analytical Chemists, v. 51, no. 3, p. 619-621, https://doi.org/10.1093/jaoac/51.3.619.","productDescription":"3 p.","startPage":"619","endPage":"621","numberOfPages":"3","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":131097,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"3","noUsgsAuthors":false,"publicationDate":"2020-02-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b132b","contributors":{"authors":[{"text":"Allen, J. L.","contributorId":49295,"corporation":false,"usgs":true,"family":"Allen","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":313030,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53414,"text":"ofr6867 - 1968 - Geology, hydrology, and quality of water in the Hanford-Visalia area, San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2023-03-09T23:02:14.422878","indexId":"ofr6867","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"68-67","title":"Geology, hydrology, and quality of water in the Hanford-Visalia area, San Joaquin Valley, California","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6867","usgsCitation":"Croft, M.G., and Gordon, G.V., 1968, Geology, hydrology, and quality of water in the Hanford-Visalia area, San Joaquin Valley, California: U.S. Geological Survey Open-File Report 68-67, Report: v, 63 p.; 15 Plates: 43.83 x 23.15 inches or smaller, https://doi.org/10.3133/ofr6867.","productDescription":"Report: v, 63 p.; 15 Plates: 43.83 x 23.15 inches or smaller","costCenters":[],"links":[{"id":413936,"rank":18,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52120.htm","linkFileType":{"id":5,"text":"html"}},{"id":87299,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0067/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87298,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87297,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87296,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87295,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87294,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87293,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87292,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87291,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87290,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87289,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87288,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87287,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87286,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87285,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87284,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0067/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175000,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0067/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Hanford-Visalia area, San Joaquin Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120,\n 36.5\n ],\n [\n -120,\n 36\n ],\n [\n -118.8167,\n 36\n ],\n [\n -118.8167,\n 36.5\n ],\n [\n -120,\n 36.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8ddb","contributors":{"authors":[{"text":"Croft, Mark G.","contributorId":24426,"corporation":false,"usgs":true,"family":"Croft","given":"Mark","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":247549,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gordon, G. V.","contributorId":30254,"corporation":false,"usgs":true,"family":"Gordon","given":"G.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":247550,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18466,"text":"ofr6834 - 1968 - A distinction between bedrock and unconsolidated deposits on 3-5u infrared imagery of the Yellowstone rhyolite plateau","interactions":[],"lastModifiedDate":"2024-11-13T16:18:43.679484","indexId":"ofr6834","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"68-34","title":"A distinction between bedrock and unconsolidated deposits on 3-5u infrared imagery of the Yellowstone rhyolite plateau","docAbstract":"

Infrared imagery covering most of Yellowstone National Park was obtained in August 1966, by H. R. B. Singer Company, using the Reconofax IV system in an aircraft flying at about 20,000 feet. This imagery has been examined in order to evaluate the geologic information it contains in relation to a current study of the Yellowstone rhyolite plateau. As most of the findings contained no new information about the capabilities of the system, they will be, reviewed here only very briefly. However, one particular aspect of the interpretation, a clear local distinction between bedrock and surficial deposits, seems to be of sufficient interest to be illustrated and noted specifically.

Because of the nature of the terrain and vegetation at Yellowstone, the parameters affecting the infrared sensor are mainly ones which are themselves only poor-resolution indicators of primary geologic features. Certain geologic features not directly related to the rhyolite plateau do show up fairly well but are not discussed here as they have been described in other reports based on this imagery (Smedes, 1968; Pierce, 1963; Keefer, in preparation).

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6834","usgsCitation":"Christiansen, R.L., 1968, A distinction between bedrock and unconsolidated deposits on 3-5u infrared imagery of the Yellowstone rhyolite plateau: U.S. Geological Survey Open-File Report 68-34, 5 p., https://doi.org/10.3133/ofr6834.","productDescription":"5 p.","costCenters":[],"links":[{"id":463013,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152223,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0034/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Yellowstone rhyolite plateau","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.2083773233386,\n 44.985687153096194\n ],\n [\n -111.2083773233386,\n 44.04105318171932\n ],\n [\n -109.76565012047247,\n 44.04105318171932\n ],\n [\n -109.76565012047247,\n 44.985687153096194\n ],\n [\n -111.2083773233386,\n 44.985687153096194\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"plainLanguageSummary":"


","publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aed4a","contributors":{"authors":[{"text":"Christiansen, Robert L. 0000-0002-8017-3918 rchris@usgs.gov","orcid":"https://orcid.org/0000-0002-8017-3918","contributorId":4412,"corporation":false,"usgs":true,"family":"Christiansen","given":"Robert","email":"rchris@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":179180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2345,"text":"wsp1859A - 1968 - Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California","interactions":[{"subject":{"id":52612,"text":"ofr67164 - 1967 - Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California","indexId":"ofr67164","publicationYear":"1967","noYear":false,"title":"Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California"},"predicate":"SUPERSEDED_BY","object":{"id":2345,"text":"wsp1859A - 1968 - Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California","indexId":"wsp1859A","publicationYear":"1968","noYear":false,"chapter":"A","title":"Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California"},"id":1}],"lastModifiedDate":"2023-03-13T20:35:14.098526","indexId":"wsp1859A","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1859","chapter":"A","title":"Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California","docAbstract":"This is the third interpretive report prepared by the U.S. Geological Survey in cooperation with the Santa Barbara County Water Agency on the groundwater resources of areas along the south coast of the county. The two previous reports--one by J. E. Upson in 1951 and another by R. E. Evenson, H. D. Wilson, Jr., and K. S. Muir--were on ground-water conditions in the Goleta and Carpinteria basins. The Santa Barbara-Montecito area is between those two basins-the Goleta basin on the west and the Carpinteria basin on the east. This area of about 30 square miles extends from the Pacific Ocean on the south to the Santa Inez Mountains on the north. The city of Santa Barbara and the towns of Montecito and Summerland are within the area. \r\n\r\nThe Santa Barbara-Montecito area is a low-lying flat section of the coastal plain. Farther inland are highlands of consolidated rock and terrace deposits. The highlands are areas of uplift, folding, and faulting, and the lowlands are structural depressions. Most of the urban development in the area has been in the lowlands. The unconsolidated deposits that have partly filled the structural depressions make up the ground-water reservoir of the Santa Barbara-Montecito area. They include the Santa Barbara Formation of Pliocene and Pleistocene age, the Casitas Formation of Pleistocene age, and the alluvium of late Pleistocene and Recent age. These deposits underlie an area of about 20 square miles \r\nand have a maximum thickness of about 2,000 feet. The consolidated rocks of Tertiary age that underlie and form the boundaries of the ground-water reservoir contain ground water in fractures and in sandstone beds. However, the consolidated rocks are not an important source of ground water. \r\n\r\nIn 1959, a year the ground-water basins were full and ground water in storage was at a maximum, storage in the Santa Barbara area was 184,000 acre-feet, and storage in the Montecito area was 97,000 acre-feet. By 1964, in response to below-average recharge and continued withdrawal by pumping, the quantity of ground water in storage in the Santa Barbara area had decreased to 178,000 acre-feet. Because of a reduction in pumpage, there was little change in storage in the Montecito area between 1959 and 1964. \r\n\r\nDeep percolation of rain, seepage from streams, and subsurface inflow from consolidated rocks are the main sources of recharge to the ground-water reservoir in the Santa Barbara-Montecito area. The most important discharge is by pumping.The long-term perennial yield of the ground-water reservoir of the Santa Barbara area is estimated to be 1,700-2,000 acre-feet. Present data are insufficient to accurately determine the perennial yield of the reservoir in the Montecito area, but it is estimated to be about 2,500 acre-feet. \r\n\r\nMost ground water in the Santa Barbara-Montecito area is suitable for general use. However, ground water in some of the consolidated rocks and in the shallow unconsolidated deposits adjacent to the coast is too saline for most uses. Seawater intrusion has occurred in the Santa Barbara area and the western part of the Montecito area. The intrusion, however, is limited to the upper part of the nearshore shallow alluvial deposits and contaminates only wells which were constructed without a near-surface seal.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1859A","usgsCitation":"Muir, K.S., 1968, Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California: U.S. Geological Survey Water Supply Paper 1859, iv, 28 p., https://doi.org/10.3133/wsp1859A.","productDescription":"iv, 28 p.","costCenters":[],"links":[{"id":137740,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859a/report-thumb.jpg"},{"id":28265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414045,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25079.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Santa Barbara County","otherGeospatial":"Santa Barbara-Montecito area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.565,\n 34.483\n ],\n [\n -119.77,\n 34.483\n ],\n [\n -119.77,\n 34.397\n ],\n [\n -119.565,\n 34.397\n ],\n [\n -119.565,\n 34.483\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649dde","contributors":{"authors":[{"text":"Muir, K. S.","contributorId":53764,"corporation":false,"usgs":true,"family":"Muir","given":"K.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70210850,"text":"70210850 - 1967 - Silver-bearing black calcite in western mining districts","interactions":[],"lastModifiedDate":"2020-06-29T16:48:36.515266","indexId":"70210850","displayToPublicDate":"2020-01-01T11:45:40","publicationYear":"1967","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":"Silver-bearing black calcite in western mining districts","docAbstract":"

The name black calcite has been applied from time to time to a dark gray to black variety of calcite or aragonite in metalliferous ore deposits in the Western States. Most of the material shows curved, roughly rhombic cleavage. The color is due to dispersed minute grains of one or more oxides of manganese, so dispersed that they rarely show any relation to cleavage surfaces or outward crystal forms.Recent study shows that the black calcite from numerous metalliferous deposits in the Western States contains small amounts of several metals, especially zinc, lead, and silver; in places, the crude black calcite contains as much as one percent silver and the black residue remaining after solution of the calcite as much as 1,500 ounces of silver to the ton. Black calcite is recognized in some deposits of Late Cretaceous to early Tertiary age where the host is Paleozoic carbonate rocks; thus far, this variety contains the larger amounts of silver. It is also present in some vein deposits where the host is generally volcanic rocks of middle Tertiary age; these are known in many districts in the southwest and even though the lead and zinc content is noteworthy, the silver content rarely exceeds one ounce to the ton (8).By studying polished sections of black calcite from the Aurora mine, White Pine County, Nevada, three silver-bearing manganate minerals have been recognized; (1) an argentian chalcophanite containing 7.5 percent silver (Ag 2 O), to which, in a following paper, the name aurorite is given; (2) argentian todorokite containing 3.9 percent silver (Ag 2 O), and (3) hydrous silver-bearing lead manganese oxide, containing 1.18 percent silver (Ag 2 O).

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.62.1.1","usgsCitation":"Hewett, D.F., and Radtke, A.S., 1967, Silver-bearing black calcite in western mining districts: Economic Geology, v. 62, no. 1, p. 1-21, https://doi.org/10.2113/gsecongeo.62.1.1.","productDescription":"21 p.","startPage":"1","endPage":"21","costCenters":[],"links":[{"id":375985,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"White Pine County","otherGeospatial":"Aurora mine","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-114.0484,40.1186],[-114.0476,39.982],[-114.0474,39.9053],[-114.0469,39.7765],[-114.0468,39.747],[-114.0463,39.6464],[-114.0468,39.543],[-114.0472,39.4696],[-114.0472,39.4551],[-114.0476,39.4068],[-114.0478,39.3816],[-114.048,39.3666],[-114.0481,39.341],[-114.0483,39.2936],[-114.0484,39.2805],[-114.0488,39.2179],[-114.0488,39.2168],[-114.0502,39.1195],[-114.0506,39.0873],[-114.0515,39.0209],[-114.0517,39.0059],[-114.052,38.9994],[-114.052,38.9982],[-114.0512,38.9554],[-114.0507,38.9259],[-114.0497,38.8693],[-114.0495,38.8557],[-114.0491,38.8371],[-114.0491,38.8358],[-114.0492,38.7927],[-114.0492,38.765],[-114.0492,38.7587],[-114.0491,38.7138],[-114.0491,38.6775],[-114.5986,38.6776],[-114.6186,38.678],[-114.6375,38.6785],[-114.6776,38.6781],[-114.7554,38.6784],[-114.8168,38.678],[-114.8916,38.6782],[-114.9241,38.678],[-114.999,38.6777],[-115.0291,38.6937],[-115.0604,38.7107],[-115.0777,38.721],[-115.0969,38.7309],[-115.242,38.8093],[-115.363,38.874],[-115.3694,38.8769],[-115.4433,38.9162],[-115.4725,38.9325],[-115.5191,38.9578],[-115.9082,39.1615],[-115.9059,39.2947],[-115.9059,39.3219],[-115.9061,39.3369],[-115.9063,39.4638],[-115.8939,39.4605],[-115.8741,39.4652],[-115.8693,39.4679],[-115.8649,39.4755],[-115.8684,39.4806],[-115.8695,39.4851],[-115.8658,39.4901],[-115.8598,39.4922],[-115.8525,39.499],[-115.8518,39.5017],[-115.8524,39.5035],[-115.8523,39.5053],[-115.8444,39.5143],[-115.8414,39.5151],[-115.836,39.5182],[-115.8334,39.525],[-115.8279,39.5322],[-115.8271,39.5381],[-115.8306,39.5417],[-115.8341,39.5481],[-115.8363,39.5536],[-115.8374,39.5577],[-115.8361,39.564],[-115.8318,39.5685],[-115.83,39.5707],[-115.8263,39.5748],[-115.814,39.5891],[-115.8127,39.5945],[-115.8138,39.6],[-115.8195,39.6082],[-115.8164,39.6127],[-115.8181,39.6195],[-115.8227,39.6264],[-115.826,39.6378],[-115.8259,39.6446],[-115.8282,39.6478],[-115.8245,39.6523],[-115.8226,39.6563],[-115.823,39.6663],[-115.8234,39.6727],[-115.8233,39.6786],[-115.8237,39.6858],[-115.8248,39.6913],[-115.8312,39.6963],[-115.8314,39.7168],[-115.8305,39.7276],[-115.8315,39.7367],[-115.8266,39.7398],[-115.8236,39.7425],[-115.8223,39.7461],[-115.8193,39.747],[-115.815,39.7492],[-115.8119,39.7541],[-115.8106,39.7595],[-115.8129,39.7641],[-115.8128,39.7677],[-115.8127,39.7727],[-115.8126,39.7782],[-115.8118,39.7845],[-115.8093,39.7904],[-115.8085,39.7976],[-115.8102,39.8008],[-115.8137,39.8072],[-115.8152,39.8176],[-115.8121,39.8226],[-115.8085,39.8257],[-115.8054,39.8288],[-115.8023,39.8329],[-115.7986,39.8369],[-115.7967,39.8432],[-115.7984,39.846],[-115.7971,39.8496],[-115.7958,39.8527],[-115.7951,39.8595],[-115.8039,39.8678],[-115.8013,39.8746],[-115.8012,39.8787],[-115.8052,39.8896],[-115.8068,39.896],[-115.8061,39.9014],[-115.8036,39.905],[-115.8023,39.91],[-115.8081,39.9196],[-115.8139,39.9255],[-115.8162,39.9306],[-115.8173,39.9356],[-115.816,39.9387],[-115.8146,39.9464],[-115.8145,39.9528],[-115.8156,39.9573],[-115.8173,39.96],[-115.8241,39.9769],[-115.8276,39.981],[-115.8323,39.987],[-115.8334,39.9897],[-115.8344,39.9979],[-115.8344,40.0006],[-115.8337,40.0043],[-115.8341,40.0115],[-115.8302,40.0251],[-115.8283,40.0282],[-115.8288,40.0323],[-115.8317,40.0355],[-115.8346,40.0437],[-115.8315,40.0478],[-115.8278,40.0522],[-115.8276,40.0581],[-115.8317,40.0636],[-115.837,40.0682],[-115.8375,40.071],[-115.8344,40.0755],[-115.8349,40.0805],[-115.8384,40.085],[-115.8376,40.0946],[-115.8346,40.0959],[-115.8321,40.0995],[-115.8289,40.1076],[-115.8294,40.1121],[-115.8305,40.1167],[-115.8374,40.1286],[-115.6972,40.1289],[-115.6046,40.1284],[-115.5295,40.1264],[-115.4561,40.1266],[-115.4441,40.1264],[-115.3917,40.1264],[-115.2426,40.1257],[-115.0393,40.1241],[-114.8108,40.1222],[-114.6929,40.1214],[-114.6526,40.121],[-114.634,40.121],[-114.5312,40.1195],[-114.2256,40.1178],[-114.0484,40.1186]]]},\"properties\":{\"name\":\"White Pine\",\"state\":\"NV\"}}]}","volume":"62","issue":"1","noUsgsAuthors":false,"publicationDate":"1967-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hewett, D. F.","contributorId":19927,"corporation":false,"usgs":true,"family":"Hewett","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":791705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Radtke, A. S.","contributorId":16408,"corporation":false,"usgs":true,"family":"Radtke","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":791706,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70198465,"text":"70198465 - 1967 - Geology and mineral resources of Page County","interactions":[],"lastModifiedDate":"2018-08-03T12:53:17","indexId":"70198465","displayToPublicDate":"2018-01-01T12:53:13","publicationYear":"1967","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Geology and mineral resources of Page County","largerWorkTitle":" Bulletin (Virginia Geological Survey)","publisher":"Commonwealth of Virginia, Division of Mineral Resources","publisherLocation":"Charlottesville, VA","usgsCitation":"Allen, R.M., 1967, Geology and mineral resources of Page County, v. 81, 78 p.","productDescription":"78 p.","costCenters":[{"id":37280,"text":"Virginia and West Virginia Water Science Center ","active":true,"usgs":true}],"links":[{"id":356139,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","county":"Page County","volume":"81","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Allen, R. M.","contributorId":36170,"corporation":false,"usgs":false,"family":"Allen","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":741533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70179896,"text":"70179896 - 1967 - The effect of pumping large-discharge wells on the ground-water reservoir in southern Utah Valley, Utah County, Utah","interactions":[],"lastModifiedDate":"2017-01-19T17:08:08","indexId":"70179896","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5271,"text":"Utah State Engineer Information Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"18","title":"The effect of pumping large-discharge wells on the ground-water reservoir in southern Utah Valley, Utah County, Utah","docAbstract":"

An extensive aquifer test in southern Utah Valley, Utah County, Utah, was made during January-March 1967 by the U.S. Geological Survey in cooperation with the Utah State Engineer. The purpose of the test was to obtain data about the hydraulic characteristics of the aquifer in the valley and to determine whether pumping large-diameter wells decreased artesian pressures and resulting flow from the numerous small-diameter flowing wells in the valley (fig. 1).

","language":"English","publisher":"Utah State Engineer's Office","publisherLocation":"Salt Lake City, UT","usgsCitation":"Cordova, R., and Mower, R.W., 1967, The effect of pumping large-discharge wells on the ground-water reservoir in southern Utah Valley, Utah County, Utah: Utah State Engineer Information Bulletin 18, 35 p.","productDescription":"35 p.","numberOfPages":"34","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333505,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333504,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-4-350"}],"country":"United States","state":"Utah","county":"Utah","otherGeospatial":"Utah Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5881def9e4b01192927d9ff7","contributors":{"authors":[{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659137,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659138,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70180004,"text":"70180004 - 1967 - Developing a state water plan: Ground-water conditions in Utah, spring of 1967","interactions":[],"lastModifiedDate":"2017-01-23T11:32:48","indexId":"70180004","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"5","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1967","docAbstract":"

This report is the fourth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series are prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources and are designed to provide data to enable interested parties such as legislators, administrators, and planners to keep abreast of changing ground-water conditions.

This report, like the others (see references, p. 89), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. It also contains supplementary data that are related to ground-water use in some areas. In reports of this series, the inclusion of such supplementary data as graphs showing chemical quality of water and maps showing water-table configuration is intended only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.

The report includes individual discussions of the most important areas of ground-water withdrawal in the State for the calendar year 1966. Water-level fluctuations, however, are described for the period spring 1966 to spring 1967. Many of the data used in the report were collected by the Geological Survey in cooperation with the Utah State Engineer.

","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Baker, C., Price, D., Butler, R., Mower, R.W., Herbert, L.R., Cordova, R., Bolke, E., Bjorklund, L., Robinson, G., and Sandberg, G.W., 1967, Developing a state water plan: Ground-water conditions in Utah, spring of 1967: Cooperative Investigations Report 5, 89 p.","productDescription":"89 p.","numberOfPages":"92","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333672,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333671,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-198"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58863a15e4b0cad700058b6b","contributors":{"authors":[{"text":"Baker, C.H. Jr.","contributorId":67526,"corporation":false,"usgs":true,"family":"Baker","given":"C.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":659690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":659691,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Butler, R.G.","contributorId":60706,"corporation":false,"usgs":true,"family":"Butler","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":659692,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659693,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659694,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659695,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":659696,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659697,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Robinson, G.B.","contributorId":178487,"corporation":false,"usgs":true,"family":"Robinson","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":659698,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659699,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70179724,"text":"70179724 - 1967 - Reconnaissance of the chemical quality of water in western Utah, Part I: Sink Valley area, drainage basins of Skull, Rush, and Government Creek Valleys, and the Dugway Valley-Old River Bed area","interactions":[],"lastModifiedDate":"2017-09-06T17:26:00","indexId":"70179724","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1967","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":"9-I","title":"Reconnaissance of the chemical quality of water in western Utah, Part I: Sink Valley area, drainage basins of Skull, Rush, and Government Creek Valleys, and the Dugway Valley-Old River Bed area","docAbstract":"

This report presents data collected during the first part of an investigation that was started in 1963 by the U.S. Geological Survey in cooperation with the Utah Geological and Mineralogical Survey. The investigation has the purpose of providing information about the chemical quality of water in western Utah that will help interested parties to evaluate the suitability of the water for various uses in a broad area of Utah where little information of this type previously has been available. The area studied includes the Sink Valley area, the drainage basins of Skull, Rush, and Government Creek Valleys, and the Dugway Valley-Old River Bed area (fig. 1). Osamu Hattori and G. L. Hewitt started the investigation, and the author completed it and prepared the report.

","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, Utah","collaboration":"Prepared in cooperation with the Utah Geological and Mineralogical Survey","usgsCitation":"Waddell, K., 1967, Reconnaissance of the chemical quality of water in western Utah, Part I: Sink Valley area, drainage basins of Skull, Rush, and Government Creek Valleys, and the Dugway Valley-Old River Bed area: Utah Geological and Mineralogical Survey Water-Resources Bulletin 9-I, 15 p.","productDescription":"15 p.","numberOfPages":"23","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333203,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-9.pdf"},{"id":333206,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Dugway Valley-Old River Bed area, Government Creek Valley, Rush Valley, Sink Valley, Skull Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.49426269531249,\n 39.6268459848669\n ],\n [\n -113.49426269531249,\n 41.04207384890103\n ],\n [\n -112.401123046875,\n 41.04207384890103\n ],\n [\n -112.401123046875,\n 39.6268459848669\n ],\n [\n -113.49426269531249,\n 39.6268459848669\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d0","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":658438,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70178829,"text":"70178829 - 1967 - Ground-water resources of northern Juab Valley, Utah","interactions":[],"lastModifiedDate":"2016-12-09T11:16:40","indexId":"70178829","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1967","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":"17","title":"Ground-water resources of northern Juab Valley, Utah","docAbstract":"

This report gives the results of an investigation of the ground-water resources of northern Juab Valley, Utah, that was carried out between June 1964 and July 1966, by the U. S. Geological Survey in cooperation with the Utah State Engineer. The study was made in order to provide water users, administrators, and other interested parties with information on the character and extent of the water-bearing formations and the origin, quantity, movement, availability, chemical quality, and use of ground water in the valley.

","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Bjorklund, L., 1967, Ground-water resources of northern Juab Valley, Utah: Technical Publication 17, 69 p.","productDescription":"69 p.","numberOfPages":"77","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331726,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331724,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-390"},{"id":331725,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920008f.pdf"}],"country":"United States","state":"Utah","county":"Juab County","otherGeospatial":"Northern Juab Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.91497802734375,\n 39.89498716884207\n ],\n [\n -111.91497802734375,\n 40.07386810509482\n ],\n [\n -111.73370361328125,\n 40.07386810509482\n ],\n [\n -111.73370361328125,\n 39.89498716884207\n ],\n [\n -111.91497802734375,\n 39.89498716884207\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584a7f7ee4b07e29c706dd43","contributors":{"authors":[{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":655280,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70178828,"text":"70178828 - 1967 - Ground-water conditions in Cedar Valley, Utah County, Utah","interactions":[],"lastModifiedDate":"2016-12-09T11:17:39","indexId":"70178828","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1967","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":"16","title":"Ground-water conditions in Cedar Valley, Utah County, Utah","docAbstract":"

This study of the ground-water conditions in Cedar Valley, Utah, was made by the U.S. Geological Survey in cooperation with the Utah State Engineer during the period July 1965-July 1966. The purposes of the study were to estimate the recharge to and the yield of the ground-water reservoir and to determine the direction of ground-water movement through Cedar Valley.

","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Feltis, R., 1967, Ground-water conditions in Cedar Valley, Utah County, Utah: Technical Publication 16, 34 p.","productDescription":"34 p.","numberOfPages":"39","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331719,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331717,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-370"},{"id":331718,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920008e.pdf"}],"country":"United States","state":"Utah","county":"Utah County","otherGeospatial":"Cedar Valley Drainage Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.862548828125,\n 39.80009595634838\n ],\n [\n -112.862548828125,\n 40.39676430557203\n ],\n [\n -112.027587890625,\n 40.39676430557203\n ],\n [\n -112.027587890625,\n 39.80009595634838\n ],\n [\n -112.862548828125,\n 39.80009595634838\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584a7f7fe4b07e29c706dd45","contributors":{"authors":[{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":655279,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70161814,"text":"70161814 - 1967 - Biodegradation of dichlorodiphenyltrichloroethane: Intermediates in dichlorodiphenylacetic acid metabolism by Aerobacter aerogenes","interactions":[],"lastModifiedDate":"2023-09-13T01:54:44.474108","indexId":"70161814","displayToPublicDate":"2015-10-16T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":843,"text":"Applied Microbiology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Biodegradation of dichlorodiphenyltrichloroethane: Intermediates in dichlorodiphenylacetic acid metabolism by Aerobacter aerogenes","title":"Biodegradation of dichlorodiphenyltrichloroethane: Intermediates in dichlorodiphenylacetic acid metabolism by Aerobacter aerogenes","docAbstract":"

The final product of dichlorodiphenyltrichloroethane (DDT) degradation by vertebrates is commonly considered to be dichlorodiphenylacetic acid, DDA (J. E. Peterson and W. H. Robison, Toxicol. Appl. Pharmacol. 6:321, 1964). Recently, certain organisms (A. S. Perry, S. Miller, and A. J. Buckner. J. Agr. Food Chem. 11:457, 1963; J. D. Pinto, M. N. Comien, and M. S. Dunn. J. Biol. Chem. 240:2148, 1965) have been found to degrade further DDA to dichlorobenzophenone (DBP), but the possibility that such degradation was due to microbial action could not be excluded. Significantly, dichlorobenzhydrol (DBH), dichlorophenylmethane (DPM), and dichlorodiphenylethylene (DDE) have been tentatively identified in rats fed DDA (Pinto et al., J. Biol. Chem. 240:2148, 1965). Since DDA as well as DDT is degraded by the ubiquitous microorganism Aerobacter aerogenes (G. Wedemeyer, Appl. Microbiol. 15:569, 1967; J. L. Mendel, and M. S. Walton, Science 151:1527, 1966), it seemed reasonable that the intestinal microflora might be involved in DBP formation, DPM and DBH being intermediates in its pathway from DDA. Since DDA is a (3,y-unsaturated acid, ketone formation via an alkene and an alcohol would be expected (S. G. Waley, Mechanisms of Organic and Enzymatic Reactions, Oxford University Press, London, England 1962).

","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/am.15.6.1494-1495.1967","usgsCitation":"Wedemeyer, G., 1967, Biodegradation of dichlorodiphenyltrichloroethane: Intermediates in dichlorodiphenylacetic acid metabolism by Aerobacter aerogenes: Applied Microbiology, v. 15, no. 6, p. 1494-1495, https://doi.org/10.1128/am.15.6.1494-1495.1967.","productDescription":"2 p.","startPage":"1494","endPage":"1495","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":480336,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/am.15.6.1494-1495.1967","text":"Publisher Index Page"},{"id":313960,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e48e8e4b0e7a44bc418b1","contributors":{"authors":[{"text":"Wedemeyer, Gary gwedemeyer@usgs.gov","contributorId":5504,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"gwedemeyer@usgs.gov","affiliations":[],"preferred":true,"id":882893,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70161813,"text":"70161813 - 1967 - A closed recirculated sea-water system","interactions":[],"lastModifiedDate":"2016-01-06T13:37:15","indexId":"70161813","displayToPublicDate":"2015-10-12T00:00:00","publicationYear":"1967","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":"A closed recirculated sea-water system","docAbstract":"

Study of a virus disease in the chinook salmon (Oncorhynchus tshawytscha) necessitated the use of a marine environment to study the long range effects of the disease and to complete the life cycle of its etiologic agent. A closed recirculated sea-water system was designed for use under experimental laboratory conditions so that controlled studies of the disease could be made. As others may wish to do marine environment studies in the laboratory, the design and operation of our system are presented. Other systems currently in use have been described by Chin (1959), DeWitt and Salo (1960), McCrimmon and Berst (1966), and the authors of collected papers edited by Clark and Clark (1964). Preparatory to the design and construction of the system in use in this laboratory, visits were made to marine systems in use at the University of Washington's College of Fisheries, Seattle, -washington, and Friday Harbor Laboratory, San Juan Island, Washington; the Washington State Department of Fisheries' Point whitney Shellfish Laboratory, Brinnon, Washington; Humboldt State College, Arcata, California; and the Steinhart Aquarium of the California Academy of Science, San Francisco, California.

","language":"English","publisher":" Bureau of Fisheries, U.S. Department of Commerce","doi":"10.1577/1548-8640(1967)29[133:ACRSS]2.0.CO;2","usgsCitation":" Bureau of Fisheries, U.S. Department of Commerce, 1967, A closed recirculated sea-water system: Progressive Fish-Culturist, v. 29, no. 3, p. 133-139, https://doi.org/10.1577/1548-8640(1967)29[133:ACRSS]2.0.CO;2.","productDescription":"7 p.","startPage":"133","endPage":"139","numberOfPages":"7","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":313955,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e48cee4b0e7a44bc41831"} ]}