{"pageNumber":"2509","pageRowStart":"62700","pageSize":"25","recordCount":68760,"records":[{"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":"<p>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 (<i>Coregonus hoyi</i>) and several of the largest lake whitefish (<i>C. clupeaformis</i>). 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.</p>","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":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, <i>Petromyzon marinus</i>, 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 (<i>Lampetra lamottei</i>), northern brook lamprey (<i>Ichthyomyzon fossor</i>), and silver lamprey (<i>I. unicuspis</i>).  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":1000113,"text":"1000113 - 1968 - Rehabilitation of lake trout in the Apostle Islands region of Lake Superior","interactions":[],"lastModifiedDate":"2016-02-18T13:58:01","indexId":"1000113","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":"Rehabilitation of lake trout in the Apostle Islands region of Lake Superior","docAbstract":"<p>Marked success of rehabilitation of lake trout in Lake Superior has been due principally to the control of the sea lamprey and closure of the lake trout fishery in 1962 and large-scale plantings of yearling lake trout in 1959-66. After the sea lamprey became established in the late 1940s, spawning stocks of lake trout began to decrease and were almost nonexistent by 1960-61. After control of the sea lamprey and closure of the commercial fishery for lake trout in 1962, the abundance of spawning stocks began to rise and reached the highest levels on record in 1964-66. Successful spawning in 1964 and 1965 was demonstrated by catches of age-0 lake trout in 1965 and 1966, the first evidence of natural reproduction since 1959. Plantings of hatchery-reared lake trout in Wisconsin waters of Lake Superior began in 1952. The percentage of hatchery-reared fish in catches of juvenile lake trout increased almost steadily from 1953 to 1965 (when nearly all were of hatchery origin). The abundance of juvenile fish increased from 1959 to 1962 and remained nearly constant in 1962-66. The success of lake trout plantings was highest in 1959-61 but generally declined after 1961; the success of the plantings was inversely related to the abundance of older lake trout. Annual increments of growth of hatchery-reared lake trout varied from 1.1 to 5.0 inches after planting. The average lengths of fish of identical age-groups varied according to gear of capture, depth of water, and season. More than 65% of the season's growth of age-III lake trout took place after September. The findings indicate that the present rate of stocking lake trout may be higher than necessary to maintain optimum abundance.</p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f68-122","usgsCitation":"Dryer, W.R., and King, G.R., 1968, Rehabilitation of lake trout in the Apostle Islands region of Lake Superior: Journal of the Fisheries Research Board of Canada, v. 25, no. 7, p. 1377-1403, https://doi.org/10.1139/f68-122.","productDescription":"27 p.","startPage":"1377","endPage":"1403","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c39e","contributors":{"authors":[{"text":"Dryer, William R.","contributorId":71921,"corporation":false,"usgs":true,"family":"Dryer","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308097,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, George R.","contributorId":74721,"corporation":false,"usgs":true,"family":"King","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308098,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2013,"text":"wsp1839L - 1968 - Geology and ground-water resources of Fillmore County, Nebraska, with a section on chemical quality of the water","interactions":[],"lastModifiedDate":"2023-11-02T20:09:09.399812","indexId":"wsp1839L","displayToPublicDate":"1968-01-01T00:00:00","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":"1839","chapter":"L","title":"Geology and ground-water resources of Fillmore County, Nebraska, with a section on chemical quality of the water","docAbstract":"Fillmore County, an area 24 miles square, lies in the eastern part of the Nebraska loess plain. Although tributaries of the Big Blue River have eroded valleys into this plain, much of the original surface is intact. Broad flats and numerous shallow undrained depressions characterize the plain. \r\n\r\nThe county is underlain by unconsolidated deposits of Quaternary age to depths ranging from about 80 to 450 feet. The upper part of this depositional sequence consists largely of wind-deposited clayey silt, and the lower part of stream-deposited sand and gravel. In part of the county, deposits of glacial till also are included. The Quaternary deposits mantle an eroded surface of marine-deposited strata of Cretaceous age. \r\n\r\nThe lower deposits of Quaternary age are saturated and constitute a highly productive aquifer throughout much of the county. The saturated zone ranges from about 20 to 350 feet in thickness. Replenishment to this aquifer, derived principally from precipitation, is believed to average about 1.4 inches per year. Because the quantity of ground water pumped per year exceeds the average annual quantity of recharge, some of the water used for irrigation is from storage. Consequently, water levels in wells .are declining. This trend is likely to continue. \r\n\r\nThe ground water is of the calcium bicarbonate type and is hard, but it is chemically suitable for irrigation use on most soils in the county.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1839L","usgsCitation":"Keech, C.F., Dreeszen, V., and Petri, L.R., 1968, Geology and ground-water resources of Fillmore County, Nebraska, with a section on chemical quality of the water: U.S. Geological Survey Water Supply Paper 1839, Report: iv, 27 p.; 2 Plates: 45.81 x 36.50 inches and 37.00 x 16.49 inches, https://doi.org/10.3133/wsp1839L.","productDescription":"Report: iv, 27 p.; 2 Plates: 45.81 x 36.50 inches and 37.00 x 16.49 inches","costCenters":[],"links":[{"id":110026,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25053.htm","linkFileType":{"id":5,"text":"html"},"description":"25053"},{"id":27470,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1839l/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27471,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1839l/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137581,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1839l/report-thumb.jpg"},{"id":27469,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1839l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nebraska","county":"Fillmore County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-97.3685,40.699],[-97.3678,40.4376],[-97.3686,40.3514],[-97.4827,40.3506],[-97.8206,40.351],[-97.8236,40.3505],[-97.8246,40.4367],[-97.8256,40.5243],[-97.826,40.6105],[-97.8245,40.6985],[-97.7111,40.6983],[-97.3685,40.699]]]},\"properties\":{\"name\":\"Fillmore\",\"state\":\"NE\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685b6d","contributors":{"authors":[{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":144529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dreeszen, V. H.","contributorId":8825,"corporation":false,"usgs":true,"family":"Dreeszen","given":"V. H.","affiliations":[],"preferred":false,"id":144528,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petri, L. R.","contributorId":48944,"corporation":false,"usgs":true,"family":"Petri","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":887471,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70190815,"text":"70190815 - 1968 - Hydrologic and climatologic data, 1967, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2018-03-26T15:42:53","indexId":"70190815","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":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"15","title":"Hydrologic and climatologic data, 1967, Salt Lake County, Utah","docAbstract":"<p>An investigation of the water resources of Salt Lake County, Utah, was undertaken by the Water Resources Division of the U.S. Geological Survey in July 1963. This investigation is a cooperative project financed chiefly by equal contributions of the State of Utah and the Federal Government in accordance with an agreement between the Division of Water Rights, Utah Department of Natural Resources, and the Geological Survey. The investigation was financed during the period covered by this report by the following organizations: Utah Division of Water Rights (formerly State Engineer), Utah Division of Water Resources (formerly Water and Power Board), Salt Lake County, Salt Lake County Water Conservancy District, Central Utah Water Conservancy District, Metropolitan Water District of Salt Lake City, City of Murray, Granger-Hunter Improvement District, Taylorsville-Bennion Improvement District, Holladay Water Company, Magna Water and Sewer District, U.S. Bureau of Reclamation, U.S. Geological Survey.</p><p>The investigation encompasses the collection and interpretation of a large variety of climatologic, hydrologic, and geologic data in and near Salt Lake County. Utah Basic-Data Releases 11-13 contain data collected through 1966. This release contains climatologic and surfacewater data for the 1967 water year (October 1966 to September 1967) and ground-water data collected during the 1967 calendar year. A similar annual release will contain data collected during the remainder of the investigation, and interpretive reports will be prepared as the investigation proceeds. Organizations that furnished data are acknowledged in station descriptions and footnotes to tables.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, Utah","collaboration":"Prepared in cooperation with The State of Utah and local organizations","usgsCitation":"Hely, A., Mower, R.W., and Horr, C.A., 1968, Hydrologic and climatologic data, 1967, Salt Lake County, Utah: Utah Basic-Data Release 15, iii, 74 p.","productDescription":"iii, 74 p.","numberOfPages":"81","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345790,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345789,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-290&Title=Basic+Data+Report+15"}],"country":"United States","state":"Utah","county":"Salt Lake County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-111.6432,40.7953],[-111.6438,40.7926],[-111.6396,40.7872],[-111.6439,40.7849],[-111.6403,40.7795],[-111.647,40.7749],[-111.6427,40.7731],[-111.6397,40.7704],[-111.6379,40.7695],[-111.6343,40.7677],[-111.6312,40.7658],[-111.6258,40.7626],[-111.6246,40.7604],[-111.6234,40.759],[-111.6222,40.7554],[-111.621,40.7504],[-111.6204,40.7431],[-111.6199,40.7381],[-111.6193,40.7327],[-111.6163,40.7299],[-111.612,40.7272],[-111.6078,40.724],[-111.6066,40.7204],[-111.6048,40.7172],[-111.6018,40.7145],[-111.5976,40.7122],[-111.5927,40.7072],[-111.5897,40.704],[-111.5897,40.6995],[-111.597,40.6945],[-111.5989,40.6904],[-111.5959,40.6805],[-111.5966,40.6696],[-111.5954,40.6623],[-111.593,40.6541],[-111.5798,40.6459],[-111.5755,40.6405],[-111.5738,40.6346],[-111.5689,40.6332],[-111.5653,40.6273],[-111.5593,40.6218],[-111.5557,40.6173],[-111.5503,40.6159],[-111.5497,40.6118],[-111.5533,40.61],[-111.5552,40.6087],[-111.5588,40.6064],[-111.5588,40.6032],[-111.5583,40.5969],[-111.5583,40.5937],[-111.5638,40.5855],[-111.5716,40.5842],[-111.5789,40.5833],[-111.5971,40.5784],[-111.5983,40.5789],[-111.6038,40.5657],[-111.6129,40.5667],[-111.622,40.5667],[-111.6311,40.5672],[-111.6347,40.5699],[-111.6414,40.5608],[-111.6468,40.5568],[-111.6523,40.5554],[-111.6565,40.5532],[-111.6608,40.5432],[-111.6669,40.541],[-111.6796,40.5328],[-111.6869,40.5342],[-111.6935,40.5351],[-111.7038,40.5356],[-111.7129,40.532],[-111.7202,40.5266],[-111.7335,40.5307],[-111.7371,40.5262],[-111.7474,40.5253],[-111.7619,40.5276],[-111.771,40.5235],[-111.7819,40.5149],[-111.7873,40.509],[-111.7867,40.5072],[-111.791,40.4959],[-111.7928,40.4954],[-111.8013,40.495],[-111.811,40.4905],[-111.8261,40.4846],[-111.8328,40.4814],[-111.8394,40.4742],[-111.8424,40.4755],[-111.8461,40.4765],[-111.8515,40.4692],[-111.8551,40.4669],[-111.8594,40.4688],[-111.8654,40.4715],[-111.8696,40.4765],[-111.8811,40.4715],[-111.8878,40.4683],[-111.8926,40.4656],[-111.8969,40.4638],[-111.9035,40.4588],[-111.9222,40.4525],[-111.9126,40.4416],[-111.9192,40.438],[-111.9271,40.4348],[-111.9307,40.433],[-111.9434,40.4267],[-111.9513,40.4221],[-111.9531,40.4212],[-111.9561,40.4198],[-111.9627,40.4189],[-111.9663,40.4176],[-111.97,40.4158],[-111.9748,40.4149],[-111.9772,40.4158],[-111.9923,40.4235],[-112.0038,40.4262],[-112.0141,40.4344],[-112.0213,40.4398],[-112.0261,40.4493],[-112.0286,40.4575],[-112.0322,40.4643],[-112.0425,40.4602],[-112.0443,40.4561],[-112.0527,40.4543],[-112.0582,40.4516],[-112.0636,40.4484],[-112.069,40.4457],[-112.0751,40.447],[-112.0835,40.4466],[-112.092,40.447],[-112.0998,40.4448],[-112.1034,40.442],[-112.1113,40.4389],[-112.1131,40.4429],[-112.1125,40.4457],[-112.1125,40.4515],[-112.1174,40.4534],[-112.1198,40.4543],[-112.1252,40.4606],[-112.1283,40.4633],[-112.1343,40.4665],[-112.1428,40.471],[-112.1506,40.4687],[-112.1524,40.4669],[-112.1591,40.4624],[-112.1675,40.4642],[-112.173,40.4674],[-112.17,40.4719],[-112.1754,40.4814],[-112.1724,40.4846],[-112.1864,40.4964],[-112.1797,40.5018],[-112.1864,40.514],[-112.1779,40.5204],[-112.1774,40.5299],[-112.181,40.5399],[-112.1822,40.5431],[-112.1774,40.5544],[-112.1762,40.5562],[-112.1817,40.5617],[-112.1805,40.5676],[-112.1835,40.573],[-112.1793,40.5785],[-112.1745,40.5857],[-112.1781,40.5943],[-112.1769,40.6021],[-112.1739,40.6039],[-112.18,40.6088],[-112.18,40.6129],[-112.1879,40.6152],[-112.1927,40.6233],[-112.1933,40.6242],[-112.194,40.6261],[-112.1928,40.6383],[-112.1928,40.6397],[-112.197,40.6433],[-112.1976,40.6483],[-112.2025,40.6533],[-112.2007,40.6646],[-112.1995,40.6728],[-112.2032,40.6787],[-112.1996,40.6882],[-112.196,40.6927],[-112.1978,40.6995],[-112.2002,40.7045],[-112.2009,40.7077],[-112.2033,40.7113],[-112.2258,40.7262],[-112.2611,40.7706],[-112.2029,40.8075],[-112.2011,40.8079],[-112.1375,40.8457],[-112.0567,40.892],[-112.0069,40.9201],[-111.9558,40.9192],[-111.9558,40.897],[-111.9667,40.8843],[-111.968,40.8748],[-111.9601,40.8675],[-111.9613,40.8594],[-111.9625,40.8526],[-111.9576,40.8471],[-111.951,40.8466],[-111.9437,40.8421],[-111.9437,40.8371],[-111.9412,40.8326],[-111.9352,40.8262],[-111.9328,40.8208],[-111.9103,40.8226],[-111.8896,40.823],[-111.8811,40.8235],[-111.8684,40.8235],[-111.8526,40.8266],[-111.8374,40.8325],[-111.8259,40.8334],[-111.8186,40.8343],[-111.8082,40.8383],[-111.7985,40.8388],[-111.7851,40.8447],[-111.7778,40.8442],[-111.7645,40.8505],[-111.748,40.8546],[-111.7444,40.8609],[-111.7352,40.8627],[-111.7231,40.855],[-111.7176,40.8563],[-111.7079,40.8531],[-111.7012,40.8567],[-111.6982,40.8617],[-111.6818,40.8585],[-111.6745,40.8562],[-111.6684,40.8544],[-111.6624,40.8507],[-111.6575,40.8475],[-111.6563,40.8453],[-111.6655,40.8362],[-111.6564,40.8285],[-111.6497,40.8258],[-111.6437,40.8221],[-111.6401,40.8194],[-111.6432,40.7953]]]},\"properties\":{\"name\":\"Salt Lake\",\"state\":\"UT\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb9539e4b091459a578214","contributors":{"authors":[{"text":"Hely, A. G.","contributorId":14401,"corporation":false,"usgs":true,"family":"Hely","given":"A. G.","affiliations":[],"preferred":false,"id":710537,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mower, Reed W.","contributorId":32503,"corporation":false,"usgs":true,"family":"Mower","given":"Reed","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":710538,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horr, C. A.","contributorId":63940,"corporation":false,"usgs":true,"family":"Horr","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":710539,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70171394,"text":"70171394 - 1968 - Seattle Metro's Duwamish estuary water quality program","interactions":[],"lastModifiedDate":"2016-05-31T09:50:14","indexId":"70171394","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2573,"text":"Journal of the Water Pollution Control Federation","active":true,"publicationSubtype":{"id":10}},"title":"Seattle Metro's Duwamish estuary water quality program","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Water Environment Federation","usgsCitation":"Gibbs, C.V., and Isaac, G.W., 1968, Seattle Metro's Duwamish estuary water quality program: Journal of the Water Pollution Control Federation, v. 40, no. 3, p. 385-394.","productDescription":"10 p.","startPage":"385","endPage":"394","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321879,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":321878,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/25036045"}],"volume":"40","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574eb5dce4b0ee97d51a83fc","contributors":{"authors":[{"text":"Gibbs, Charles V.","contributorId":169725,"corporation":false,"usgs":false,"family":"Gibbs","given":"Charles","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Isaac, Gary W.","contributorId":169726,"corporation":false,"usgs":false,"family":"Isaac","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":630883,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185809,"text":"70185809 - 1968 - On the quantitative inventory of the riverscape","interactions":[],"lastModifiedDate":"2018-02-04T14:18:23","indexId":"70185809","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"On the quantitative inventory of the riverscape","docAbstract":"<p><span>In the vicinity of Berkeley, California, 24 minor valleys were described in terms of factors chosen to represent aspects of the river landscape. A total of 28 factors were evaluated at each site. Some were directly measurable, others were estimated, but each observation was assigned to one of five categories for that factor. Each factor for each site was then expressed as a uniqueness ratio, which depended on the number of sites being in the same category. The uniqueness ratio is believed to represent one way the scarcity of a given riverscape can be ranked quantitatively without bias based on notions of good or bad, and without assigning monetary value.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR004i004p00709","usgsCitation":"Leopold, L.B., and O’Brien Marchand, M., 1968, On the quantitative inventory of the riverscape: Water Resources Research, v. 4, no. 4, p. 709-717, https://doi.org/10.1029/WR004i004p00709.","productDescription":"9 p.","startPage":"709","endPage":"717","costCenters":[],"links":[{"id":338570,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Berkeley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.06884765625,\n              36.78289206199065\n            ],\n            [\n              -121.03637695312499,\n              36.78289206199065\n            ],\n            [\n              -121.03637695312499,\n              38.30718056188316\n            ],\n            [\n              -123.06884765625,\n              38.30718056188316\n            ],\n            [\n              -123.06884765625,\n              36.78289206199065\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"58dcc830e4b02ff32c685783","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Brien Marchand, Maura","contributorId":190013,"corporation":false,"usgs":false,"family":"O’Brien Marchand","given":"Maura","email":"","affiliations":[],"preferred":false,"id":686791,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":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":"<p>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).</p>","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":"<p>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.</p><p>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.</p><p>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.</p>","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":"<p>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.</p>","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":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":"<p>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.</p>","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":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":"<p>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.</p>","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":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":"<p>Study of a virus disease in&nbsp;the chinook salmon <i>(Oncorhynchus tshawytscha</i>) 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.</p>","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"}
,{"id":70157475,"text":"70157475 - 1967 - Trends in ground-water levels in Wisconsin through 1966","interactions":[],"lastModifiedDate":"2018-01-08T19:42:04","indexId":"70157475","displayToPublicDate":"2015-09-02T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"Trends in ground-water levels in Wisconsin through 1966","docAbstract":"<p>The water supplies of Wisconsin are the State's most valuable natural resource. Although the State has abundant water supplies to maintain the perennial flow of most streams, and to sustain large increases in municipal, agricultural, and industrial use in many areas, the available supply is not distributed equally throughout the State, either areally or in time. Intelligent development of all water resources depends on knowledge of the occurrence, distribution and movement of water, the amount of discharge to and from a region, the interrelationship of ground and surface water, and the quantity and quality of the water available.</p>","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","collaboration":"Prepared by United States Geological Survey in cooperation with the Wisconsin Geological and Natural History Survey","usgsCitation":"Devaul, R.W., 1967, Trends in ground-water levels in Wisconsin through 1966: Wisconsin Geological & Natural History Survey Information Circular 9, viii, 109 p.","productDescription":"viii, 109 p.","numberOfPages":"119","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308490,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350399,"rank":2,"type":{"id":15,"text":"Index 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,{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","interactions":[{"subject":{"id":52440,"text":"ofr656 - 1965 - New Mexico State Planning Office Report - Arkansas River basin","indexId":"ofr656","publicationYear":"1965","noYear":false,"title":"New Mexico State Planning Office Report - Arkansas River basin"},"predicate":"SUPERSEDED_BY","object":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"id":1},{"subject":{"id":52441,"text":"ofr657 - 1965 - New Mexico State Planning Office Report - Southern High Plains","indexId":"ofr657","publicationYear":"1965","noYear":false,"title":"New Mexico State Planning Office Report - Southern High Plains"},"predicate":"SUPERSEDED_BY","object":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"id":2},{"subject":{"id":52450,"text":"ofr6533 - 1965 - New Mexico State Planning Office Report - Western closed basins","indexId":"ofr6533","publicationYear":"1965","noYear":false,"title":"New Mexico State Planning Office Report - Western closed basins"},"predicate":"SUPERSEDED_BY","object":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"id":3},{"subject":{"id":52451,"text":"ofr6534 - 1965 - New Mexico State Planning Office Report - San Juan basin","indexId":"ofr6534","publicationYear":"1965","noYear":false,"title":"New Mexico State Planning Office Report - San Juan basin"},"predicate":"SUPERSEDED_BY","object":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"id":4},{"subject":{"id":52455,"text":"ofr6544 - 1965 - New Mexico State Planning Office Report - Rio Grande basin","indexId":"ofr6544","publicationYear":"1965","noYear":false,"title":"New Mexico State Planning Office Report - Rio Grande basin"},"predicate":"SUPERSEDED_BY","object":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"id":5},{"subject":{"id":52456,"text":"ofr6545 - 1965 - New Mexico State Planning Office Report - Southwestern closed basins","indexId":"ofr6545","publicationYear":"1965","noYear":false,"title":"New Mexico State Planning Office Report - Southwestern closed basins"},"predicate":"SUPERSEDED_BY","object":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"id":6},{"subject":{"id":52487,"text":"ofr65114 - 1965 - New Mexico State Planning Office Report-Pecos River basin","indexId":"ofr65114","publicationYear":"1965","noYear":false,"title":"New Mexico State Planning Office Report-Pecos River basin"},"predicate":"SUPERSEDED_BY","object":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"id":7},{"subject":{"id":52511,"text":"ofr65160 - 1965 - New Mexico State Planning Office Report-Central closed basins","indexId":"ofr65160","publicationYear":"1965","noYear":false,"title":"New Mexico State Planning Office Report-Central closed basins"},"predicate":"SUPERSEDED_BY","object":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"id":8},{"subject":{"id":52512,"text":"ofr65161 - 1965 - New Mexico State Planning Office Report-Lower Colorado River basin","indexId":"ofr65161","publicationYear":"1965","noYear":false,"title":"New Mexico State Planning Office Report-Lower Colorado River basin"},"predicate":"SUPERSEDED_BY","object":{"id":70046983,"text":"70046983 - 1967 - Water resources of New Mexico: occurrence, development, and use","indexId":"70046983","publicationYear":"1967","noYear":false,"title":"Water resources of New Mexico: occurrence, development, and use"},"id":9}],"lastModifiedDate":"2013-07-17T14:30:10","indexId":"70046983","displayToPublicDate":"2013-01-01T13:55:00","publicationYear":"1967","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Water resources of New Mexico: occurrence, development, and use","language":"English","publisher":"New Mexico, State Planning Office","publisherLocation":"Santa Fe, NM","collaboration":"Compiled by New Mexico State Engineer Office in cooperation with New Mexico Interstate Stream Commission and U.S. Geological Survey [Water Resources Division]","usgsCitation":"New Mexico, O., New Mexico, P.O., New Mexico, I.S., and U.S. Geological Survey, W.R., 1967, Water resources of New Mexico: occurrence, development, and use, xx, 321 p.","productDescription":"xx, 321 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":274885,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.05,31.33 ], [ -109.05,37.0 ], [ -103.0,37.0 ], [ -103.0,31.33 ], [ -109.05,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51dfd3e7e4b0d332bf22f3c5","contributors":{"authors":[{"text":"New Mexico, Office","contributorId":105620,"corporation":false,"usgs":true,"family":"New Mexico","given":"Office","email":"","affiliations":[],"preferred":false,"id":480803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"New Mexico, Planning Office","contributorId":72687,"corporation":false,"usgs":true,"family":"New Mexico","given":"Planning","email":"","middleInitial":"Office","affiliations":[],"preferred":false,"id":480800,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"New Mexico, Interstate Stream Commission","contributorId":95362,"corporation":false,"usgs":true,"family":"New Mexico","given":"Interstate","email":"","middleInitial":"Stream Commission","affiliations":[],"preferred":false,"id":480801,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"U.S. Geological Survey, Water Resources Division","contributorId":102359,"corporation":false,"usgs":true,"family":"U.S. Geological Survey","given":"Water","email":"","middleInitial":"Resources Division","affiliations":[],"preferred":false,"id":480802,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70046926,"text":"70046926 - 1967 - Hydrologic effects of area B flood control plan on urbanization of Dade County, Florida","interactions":[{"subject":{"id":52476,"text":"ofr6587 - 1965 - The Area B flood-control plan--its influence on the future water resources of the Miami area, Florida","indexId":"ofr6587","publicationYear":"1965","noYear":false,"title":"The Area B flood-control plan--its influence on the future water resources of the Miami area, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70046926,"text":"70046926 - 1967 - Hydrologic effects of area B flood control plan on urbanization of Dade County, Florida","indexId":"70046926","publicationYear":"1967","noYear":false,"title":"Hydrologic effects of area B flood control plan on urbanization of Dade County, Florida"},"id":1}],"lastModifiedDate":"2017-09-13T17:56:12","indexId":"70046926","displayToPublicDate":"2013-01-01T13:25:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5489,"text":"Florida Geological Survey Report of Investigations","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"47","title":"Hydrologic effects of area B flood control plan on urbanization of Dade County, Florida","docAbstract":"Swampy low land (Area B) that fringes the Everglades west of Metropolitan Miami, Florida (Area A) probably will be urbanized in the future. Area B will be protected from flooding by huge pumps that will pump water westward from Area B over a levee system into Conservation Area 3B. The total capacity of the pumps will be about 13,400 cubic feet per second which is sufficient to lower water levels 2 inches per day in the 203 square miles of Area B. As this capacity is about equal to the highest gravity-flow discharge to the ocean through existing canals of the Miami area, a great potential. will exist, not only for control of floods, but also for beneficial control and management of a major segment of the water resources in southeastern Florida.","language":"English","publisher":"Florida Geological Survey","publisherLocation":"Tallahassee, FL","collaboration":"Prepared by the United States Geological Survey in cooperation with the Central and Southern Florida Flood Control District and the Division of Geology","usgsCitation":"Kohout, F.A., and Hartwell, J., 1967, Hydrologic effects of area B flood control plan on urbanization of Dade County, Florida: Florida Geological Survey Report of Investigations 47, vii, 61 p.","productDescription":"vii, 61 p.","numberOfPages":"69","costCenters":[],"links":[{"id":274775,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046926.png"},{"id":274771,"type":{"id":15,"text":"Index Page"},"url":"https://ufdc.ufl.edu/UF00001234/00001"}],"country":"United States","state":"Florida","county":"Miami-dade County","otherGeospatial":"Dade County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.8736,25.1374 ], [ -80.8736,25.9792 ], [ -80.0428,25.9792 ], [ -80.0428,25.1374 ], [ -80.8736,25.1374 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51dd30ebe4b0f72b44719c86","contributors":{"authors":[{"text":"Kohout, F. A.","contributorId":11593,"corporation":false,"usgs":true,"family":"Kohout","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":480633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hartwell, J.H.","contributorId":98356,"corporation":false,"usgs":true,"family":"Hartwell","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":480634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70038400,"text":"wdrCA662 - 1967 - Water Resources Data for California, 1966; Part 2: Water Quality Records","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA662","displayToPublicDate":"2012-05-13T13:58:00","publicationYear":"1967","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":"CA-66-2","title":"Water Resources Data for California, 1966; Part 2: Water Quality Records","docAbstract":"<p>Water-resources investigations of the U.S. Geological Survey include the collection of water-quality data on the chemical and physical characteristics of surface- and ground-water supplies of the Nation. These data for the 1966 water year for the quality of surface waters in California are presented in this report. Data for a few water-quality stations in bordering States are also included. The data were collected by the Water Resources Division of the U.S. Geological Survey under the direction of Walter Hofmann and R. Stanley Lord, successive district chiefs, Menlo Park, Calif.</p>\n<p>Water-quality information is presented for chemical quality, fluvial sediment, and water temperatures. The chemical quality includes concentrations of individual dissolved constituents and certain properties or characteristics such as hardness, sodium-adsorption ratio, specific conductance, and pH. Fluvial-sediment information is given for suspended-sediment discharges and concentrations and for particle-size distribution of suspended sediment and bed material. Water-temperature data represent once-daily observations except for stations where a continuous temperature recorder furnishes information from which daily minimums and maximums are obtained.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA662","usgsCitation":"U.S. Geological Survey, 1967, Water Resources Data for California, 1966; Part 2: Water Quality Records: U.S. Geological Survey Water Data Report CA-66-2, x, 461 p., https://doi.org/10.3133/wdrCA662.","productDescription":"x, 461 p.","costCenters":[],"links":[{"id":256926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256918,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/ca-66/WDR-1966-wq.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc493e4b08c986b32b714"}
,{"id":70038399,"text":"wdrCA6612 - 1967 - Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA6612","displayToPublicDate":"2012-05-13T13:40:00","publicationYear":"1967","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":"CA-66-1-2","title":"Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 2: Northern Great Basin and Central Valley","docAbstract":"The surface-water records for the 1966 water year for gaging stations, partial-record stations, and miscellaneous sites within California are given in this report. For convenience, also included are records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Walter Hofmann and R. Stanley Lord, successive district chiefs, Menlo Park, Calif.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA6612","usgsCitation":"U.S. Geological Survey, 1967, Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-66-1-2, xvii, 514 p., https://doi.org/10.3133/wdrCA6612.","productDescription":"xvii, 514 p.","startPage":"483","endPage":"997","temporalStart":"1965-10-01","temporalEnd":"1966-09-30","costCenters":[],"links":[{"id":256929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256917,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/ca-66/WDR-1966-vol2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Northern Great Basin;Central Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc492e4b08c986b32b70e"}
,{"id":70038398,"text":"wdrCA6611 - 1967 - Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Cenral Valley","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA6611","displayToPublicDate":"2012-05-13T13:27:00","publicationYear":"1967","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":"CA-66-1-1","title":"Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Cenral Valley","docAbstract":"The surface-water records for the 1966 water year for gaging stations, partial-record stations, and miscellaneous sites within California are given in this report. For convenience, also included are records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Walter Hofmann and R. Stanley Lord, successive district chiefs, Menlo Park, Calif.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA6611","usgsCitation":"U.S. Geological Survey, 1967, Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Cenral Valley: U.S. Geological Survey Water Data Report CA-66-1-1, xviii, 482 p., https://doi.org/10.3133/wdrCA6611.","productDescription":"xviii, 482 p.","startPage":"1","endPage":"482","temporalStart":"1965-10-01","temporalEnd":"1966-09-30","costCenters":[],"links":[{"id":256930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256916,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/ca-66/WDR-1966-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Colorado River Basin;Southern Great Basin;Pacific Slope Basins","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc491e4b08c986b32b708"}
,{"id":70038234,"text":"70038234 - 1967 - Hydrogeologic data for the Shetucket River basin, Connecticut","interactions":[],"lastModifiedDate":"2014-04-09T12:36:03","indexId":"70038234","displayToPublicDate":"2012-04-22T10:17:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"12","title":"Hydrogeologic data for the Shetucket River basin, Connecticut","docAbstract":"This report presents hydrologic and geologic data collected by the U.S. Geological Survey during an investigation of water resources in the Shetucket River basin of Connecticut in cooperation with the Connecticut Water Resources Commission. The Shetucket River basin occupies about 507 square miles in the eastern part of the State, including the towns of Andover, Ashford, Chaplin, Coventry, Mansfield, Scotland, Sprague, Windham, and Willington, and parts of Bolton, Canterbury, Columbia, Eastford, Ellington, Franklin, Lebanon, Lisbon, Hampton, Hebron, Norwich, Pomfret, Stafford, Tolland, Union, Vernon, and Woodstock. A companion interpretive report, Connecticut Water Resources Bulletin ll, (Thomas, and others, 1967), evaluates the water resources of the basin. The data on the following pages serve to document and supplement that report and should be especially useful in planning the development of water resources at specific localities.\nData were collected as part of this investigation during the period July\n1962 through December 1964. Streamflow records from continuous-record gaging\nstations in the basin for this period have been published annually along with data\nfrom other parts of the State in a series of U.S. Geological Survey reports\nentitled \"Surface Water Records of Connecticut.\" Water-level measurements in\nwells throughout the State from 1960 through 1964, including those made as part\nof this investigation, are published in Connecticut Water Resources Bulletin 7\n(Meikle and Baker, 1965). Most other data collected during this investigation\nare tabulated on the following pages. Included are some well records and chemical\nanalyses of water samples collected prior to July 1962 and not previously published.\nThe locations of sites at which data were collected are shown on\nplate A in the pocket at the back of the report. Plate A includes the\nlocations of 98 sites where 2 to 6 miscellaneous measurements of streamflow\nwere made during 1963 and 13 other sites where continuous records are\nmaintained. Data for these sites have already been published in \"Surface\nWater Records of Connecticut\" and are not repeated here.\nData presented~ unless otherwise noted, were collected by U.S.\nGeological Survey personnel.","language":"English","publisher":"Connecticut Water Resources Commission","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Water Resources Commission","usgsCitation":"Thomas, C.E., Bednar, G.A., Thomas, M.P., and Wilson, W.E., 1967, Hydrogeologic data for the Shetucket River basin, Connecticut: Connecticut Water Resources Bulletin 12, Report: 48 p.; 1 Plate: 33.28 x 56.69 inches.","productDescription":"Report: 48 p.; 1 Plate: 33.28 x 56.69 inches","numberOfPages":"54","costCenters":[],"links":[{"id":258793,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0012/report.pdf","size":"1843","linkFileType":{"id":1,"text":"pdf"}},{"id":258794,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0012/report-thumb.jpg"},{"id":285974,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70038234/plate-a.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Shetucket River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.45,41.55 ], [ -72.45,42.066667 ], [ -72.016667,42.066667 ], [ -72.016667,41.55 ], [ -72.45,41.55 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a33b2e4b0c8380cd5f1bc","contributors":{"authors":[{"text":"Thomas, Chester E. Jr.","contributorId":37182,"corporation":false,"usgs":true,"family":"Thomas","given":"Chester","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bednar, Gene A.","contributorId":81881,"corporation":false,"usgs":true,"family":"Bednar","given":"Gene","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463700,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, William E.","contributorId":46478,"corporation":false,"usgs":true,"family":"Wilson","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463698,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70038229,"text":"70038229 - 1967 - Water resources inventory of Connecticut Part 2: Shetucket River Basin","interactions":[],"lastModifiedDate":"2014-04-09T12:35:29","indexId":"70038229","displayToPublicDate":"2012-04-22T09:08:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"11","title":"Water resources inventory of Connecticut Part 2: Shetucket River Basin","docAbstract":"The Shetucket River basin has a relatively abundant supply of water of generally good quality which is derived from precipitation that has fallen on the basin. Annual precipitation has ranged from about 30 inches to 75 inches and has averaged about 45 inches over a 35-year period. Approximately 20 inches of water are returned to the atmosphere each year by evaporation and transpiration; the remainder of the annual precipitation either flows overland to streams or percolates downward to the water table and ultimately flows out of the basin in the Shetucket River or as underflow through the deposits beneath. During the autumn and winter months precipitation normally is sufficient to cause a substantial increase in the amount of water stored underground and in surface reservoirs within the basins whereas in the summer most of the precipitation is lost through evaporation and transpiration, resulting in sharply reduced streamflow and lowered groundwater levels. The mean monthly storage of water in the basin on an average is 3.5 inches higher in November than it is in June.\nThe amount of water that flows out of the\nbasin in the Shetucket River represents the total\namount of water potentlally available for use by man.\nAnnual runoff from the entire basin above the\nQuinebaug River has ranged from about 13 to 42\ninches since 1929, and has averaged about 23\ninches (300 billion gallons). Although runoff\nindicates the total amount of water potentially\navailable, it is usually not economically or\nlegally feasible for man to use all of it. On\nthe other hand, with increased development, It\nis possible that some water will be reused several\ntimes.\nThe water available may be tapped as it flows\nthrough the area or is temporarily stored in\nstreams, lakes, and aquifers. The amounts that\ncan be developed vary from place to place and\ntime to time, depending on the amount of precipitation,\non the size of drainage area, on the\nthickness, permeability and areal extent of aquifers,\nand on the variations in chemical and\nphysical quality of the water.\nDifferences in streamflow from point to\npoint are due primarily to differences in the\nproportion of stratified drift in the drainage\nbasin above each point, which affect the timing\nof streamflow, and to differences in precipitation,\nwhich affect the amount of streamflow.\nInformation on streamflow from gaging stations\nmay be extended to ungaged sites by accounting\nfor both of these factors ,in calculations.\nFuture floods on the upper Willimantic\nRiver or the Shetucket River are unlikely to\ncause major damage so long as buildings are not\nconstructed below the highest flood elevations to\nbe expected with the present system of reservoirs\nfor flood control.\nGround water can be obtained from wells\nalmost anywhere in the Shetucket River basin, but\nthe amount obtainable from individual wells at\nany particular point depends upon the type and\nwater-bearing properties of the aquifers present.\nFor practical purposes, the earth materials in\nthe basin comprise three aquifers--stratified\ndrift, till, and bedrock,\nStratified drift is the only aquifer generally capable of yielding more than 100 gpm to\nindividual wells. This aquifer covers about 18\npercent of the basin and occurs chiefly In lowlands\nwhere it overlies till or bedrock. Coefficient\nof permeability of the coarse-grained unit\nof stratified drift averages about 1,900 gpd per\nsq ft. Drilled, screened wells tapping this unit,\nare known to yield from 200 to 675 gpm. Dug wells\nin coarse-grained stratified drift should supply\nat least 2 gpm per foot of drawdown over an 8-hour\nperiod. Fine-grained stratified drift has an\naverage coefficient of permeability of about 400\ngpd per sq ft and can usually yield to dug wells\nsupplies sufficient for household use.\nTill and bedrock are widespread in extent but\ncan provide only small to moderate water supplies.\nTill is tapped chiefly by dug wells; permanent\nsupplies of more than 200 gpd can be obtained from\ndug wells at a majority of sites in areas of till,\nbut there are many sites where the till is too\nimpermeable or too thin to provide this much water\nthroughout the year. The coefficient of permeability of till ranges from about 0.2 gpd per sq ft to\n55 gpd per sq it. Bedrock Is tapped chiefly by\ndrilled wells, about 90 percent of which will\nsupply at least 3 gpm. Very few, however, will\nsupply more than 50 gpm.\nThe amount of ground water potentially available\nIn an area depends upon the amount of groundwater\noutflow, the amount of ground water in storage,\nand the quantity of water available by Induced\ninfiltration from streams and lakes. From\ndata on permeability, saturated thickness, recharge,\nyield from aquifer storage, well performance, and\nstreamflow, preliminary estimates of ground-water\navailability can be made for any point in the\nbasin. Long-term yields estimated for 15 areas\nespecially favorable for development of large\nground-water supplies ranged from 1.3 to 61.8 mgd.\nDetailed site studies to determine optimum yields,\ndrawdowns, and spacing of individual wells are\nneeded before major ground-water development is\nundertaken In these or other areas.\nThe chemical quality of water in the Shetucket\nbasin Is generally good to excellent. Samples of\nnaturally occurring surface water collected from\n32 sites contained less than 61 ppm of dissolved\nsolids and less than 32 ppm of hardness. Water\nfrom wells is more highly mineralized than naturally\noccurring water from streams. Even so only\n7 percent of wells sampled yielded water with more\nthan 200 ppm of dissolved sol-ids and only 9 percent\nyielded water with more than 120 ppm of hardness.\nEven in the major rivers, which are used to\ntransport industrial waste, the dissolved mineral\ncontent is less than 100 ppm and hardness rarely\nexceeds 40 ppm. One notable exception occurs in\nthe lower reaches of Little River where an\nexceptional amount of industrial waste is discharged\ninto the river near Versailles. This\nwaste is particularly noticeable during low\nstreamflow.\nIron and manganese In both ground water and\nsurface water are the only constituents whose concentrations\ncommonly exceed recommended limits for\ndomestic and industrial use. Most wells in the\n basin yield clear water with little or no iron or\nmanganese, but distributed among them are wells\nwith ground water that contains enough of these dissolved\nconstituents to be troublesome for most uses.\niron concentrations in naturally occurring\nstream water exceeded 0.3 ppm under tow-flow conditions\nat 20 percent of the sites sampled. Large\nconcentrations of iron in stream water result\nfrom discharge of iron-bearing ground water or\nfrom the discharge of water from swamps. In\nswamps the iron is released largely from decaying\nvegetation.\nGround water more than 30 feet below the\nland surface has a relatively constant temperature,\nusually between 48°F and 50°F. Water\ntemperature in very shallow wells may fluctuate\nfrom about 38°F in February or March to about\n55°F in late summer. Water temperature in the\nlarger streams fluctuates much more widely,\nranging from 32°F at least for brief periods\nin winter, to about 85°F occasionally during\nThe quantity of suspended sediment transported\nby streams in the basin is negligible,\nthough amounts large enough to be troublesome\nmay occur locally at times.\nThe total amount of water used In the\nShetucket Rlver basin for all purposes during\n1961 was about 5,810 million gallons~ which is\nequivalent to 208 gpd per person, Public water\nsystems supplied the domestic needs of nearly\nhalf the population of the basin; 10 systems\nwere sampled, all of which provided water of\nbetter quality than the U.S. Public Health Service\nsuggests for drinking water standards.","language":"English","publisher":"Connecticut Water Resources Commission","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Water Resource Commission","usgsCitation":"Thomas, M.P., Bednar, G.A., Thomas, C.E., and Wilson, W.E., 1967, Water resources inventory of Connecticut Part 2: Shetucket River Basin: Connecticut Water Resources Bulletin 11, Report: viii, 96 p.; 4 Plates: 36.00 x 58.00 inches and smaller.","productDescription":"Report: viii, 96 p.; 4 Plates: 36.00 x 58.00 inches and smaller","numberOfPages":"112","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":258791,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0011/report.pdf","size":"22651","linkFileType":{"id":1,"text":"pdf"}},{"id":258792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0011/report-thumb.jpg"},{"id":285972,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038229/plate-c.pdf"},{"id":285973,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038229/plate-d.pdf"},{"id":285970,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038229/plate-a.pdf"},{"id":285971,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038229/plate-b.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Shetucket River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.466667,41.533333 ], [ -72.466667,42.066667 ], [ -72.0,42.066667 ], [ -72.0,41.533333 ], [ -72.466667,41.533333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb78e4b08c986b32d681","contributors":{"authors":[{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bednar, Gene A.","contributorId":81881,"corporation":false,"usgs":true,"family":"Bednar","given":"Gene","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463692,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Chester E. Jr.","contributorId":37182,"corporation":false,"usgs":true,"family":"Thomas","given":"Chester","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463690,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, William E.","contributorId":46478,"corporation":false,"usgs":true,"family":"Wilson","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463691,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70046324,"text":"wdrNM661 - 1967 - Water resources data for New Mexico, water year 1966; Part 1. Surface water records","interactions":[],"lastModifiedDate":"2013-07-08T10:52:19","indexId":"wdrNM661","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1967","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":"NM-66-1","title":"Water resources data for New Mexico, water year 1966; Part 1. Surface water records","docAbstract":"The surface-water records for the 1966 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of New Mexico are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of W. E. Hale, District Chief, Water Resources Division. This report is the sixth in a series presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951' there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in New Mexico were contained in Parts 7, 8, and 9 of that series. Beginning with the 1961 water year, streamflow records and related data have been released\nby the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports is limited and primarily for local needs. The records will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of conterminous United States will be further subdivided.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Santa Fe, NM","doi":"10.3133/wdrNM661","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Water resources data for New Mexico, water year 1966; Part 1. Surface water records: U.S. Geological Survey Water Data Report NM-66-1, 268 p., https://doi.org/10.3133/wdrNM661.","productDescription":"268 p.","costCenters":[],"links":[{"id":273453,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274522,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/nm-66/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.052,31.3322 ], [ -109.052,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.052,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b300e9e4b01368e589e418","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":535534,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006948,"text":"70006948 - 1967 - Low-temperature incubation using a water supply","interactions":[],"lastModifiedDate":"2023-09-13T01:46:58.016488","indexId":"70006948","displayToPublicDate":"2012-01-01T00:00:00","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}},"title":"Low-temperature incubation using a water supply","docAbstract":"Cell and tissue culture has been concerned primarily with homiothermic vertebrate cells which require incubation at about 37 C, and there is a great variety of incubators designed to maintain temperatures which are usually above ambient. The culture of poikilothermic vertebrate cells--and invertebrate, plant, and some microbial cells--can often be carried out at ambient temperatures, but for some work cooler conditions must be provided. Variety among the so-called low-temperature incubators is somewhat restricted; there are no small units, and all require a power source to maintain temperatures below ambient. We have used a gravity-fed water supply for 5 years to provide trouble-free, constant, low-temperature incubation of stock cultures of fish and amphibian cells. Though it is but a small part of our low-temperature incubator capacity, it has no power requirements and it provides maximal protection against temperature rises which could be lethal to some of the cell lines. Though the system has limitations, there is a considerable likelihood that the domestic water supply in other laboratories can also be used to provide low-temperature incubation.","language":"English","publisher":"American Society for Microbiology","publisherLocation":"Washington, D.C.","doi":"10.1128/am.15.6.1501-1501.1967","usgsCitation":"Wolf, K., and Quimby, M.C., 1967, Low-temperature incubation using a water supply: Applied Microbiology, v. 15, no. 6, p. 1501-1501, https://doi.org/10.1128/am.15.6.1501-1501.1967.","productDescription":"1 p.","startPage":"1501","endPage":"1501","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":480338,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/am.15.6.1501-1501.1967","text":"Publisher Index Page"},{"id":263310,"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":"50abfc17e4b0afbc75eb985a","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":355526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quimby, M. C.","contributorId":14334,"corporation":false,"usgs":true,"family":"Quimby","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":355525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}