The U.S. Soil Conservation Service is actively engaged in the installation of flood and soil erosion reducing measures in Texas under the authority of \"The Flood Control Act of 1936 and 1944\" and \"Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. The Soil Conservation Service has found a total of 3,438 floodwater-retarding structures to be physically and economically feasible in Texas. As of September 30, 1967, 1,196 of these structures had been built.
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\"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":152492,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":808208,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180005,"text":"70180005 - 1968 - Developing a state water plan: Ground-water conditions in Utah, spring of 1968","interactions":[],"lastModifiedDate":"2017-01-23T11:33:09","indexId":"70180005","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1968","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":"6","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1968","docAbstract":"This report is the fifth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series are prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources and are designed to provide data to enable interested parties such as legislators, administrators, and planners to keep abreast of changing ground-water conditions.
This report, like the others (see references, p. 105), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. It also contains supplementary data that are related to ground-water use in some areas. In reports of this series, the inclusion of such supplementary data as graphs showing chemical quality of water and maps showing water-table configuration is intended only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.
The report includes individual discussions of the most important areas of ground-water withdrawal in the State for the calendar year 1967. Water-level fluctuations, however, are described for the period spring 1967 to spring 1968. Included for the first time in this series of annual reports is a (1) summation of the withdrawal of water from wells in the 5 years 1963-67 (table 3) and (2) maps and discussions of water-level changes for the 5-year period 1963-68. Many of the data used in the report were collected by the Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.
","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":"Cordova, R., Bjorklund, L., Butler, R., Mower, R.W., Herbert, L.R., Bolke, E., and Sandberg, G.W., 1968, Developing a state water plan: Ground-water conditions in Utah, spring of 1968: Cooperative Investigations Report 6, 105 p.","productDescription":"105 p.","numberOfPages":"106","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333673,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-197"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58863a15e4b0cad700058b69","contributors":{"authors":[{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659701,"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":659702,"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":659703,"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":659704,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":659705,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659706,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70179726,"text":"70179726 - 1968 - Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine: Summary for water years 1960, 1961, and 1964","interactions":[],"lastModifiedDate":"2017-09-06T17:24:36","indexId":"70179726","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1968","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":"10","title":"Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine: Summary for water years 1960, 1961, and 1964","docAbstract":"The investigation of dissolved-mineral inflow to Great Salt Lake during the water years 1960, 1961, and 1964 was conducted during conditions of streamflow that were representative of the lowest and the average recorded during the water years 1934-64. The study conducted during the 1960 and 1961 water years was limited to defining surface-water inflow at sites close to the lakeshore, as well as at sites used in the 1960-6 study. From these comparative data, estimates of inflow at the lakeshore were made for the 1960 and 1961 water years. During the 1964 water year, when inflow to the lake was probably representative of the 31-year period, about 800,000 acre-feet of water containing 2,200,000 tons of dissolved solids entered the lake.
During the years of average streamflow, about 500,000 acre-feet of water which might be developed for culinary use, passes the lowest sampling sites on the Bear and Weber Rivers. Also, more than 90 percent of the flow near the mouths of the Bear, Weber, and Jordan Rivers would be suitable for irrigation.
Sources of inflow could be selected to provide a water supply for a fresh-water lake east of Antelope Island. The supply would range from 300,000 acre-feet of water containing 800 ppm (parts per million) of dissolved solids during periods of low streamflow to 1 million acre-feet containing 500 ppm during periods of average streamflow.
","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah Geological and Mineralogical Survey","usgsCitation":"Hahl, D.C., 1968, Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine: Summary for water years 1960, 1961, and 1964: Utah Geological and Mineralogical Survey Water-Resources Bulletin 10, 35 p.","productDescription":"35 p.","numberOfPages":"37","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333209,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333207,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-10.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.35693359375,\n 40.48038142908172\n ],\n [\n -113.35693359375,\n 42.01665183556825\n ],\n [\n -111.566162109375,\n 42.01665183556825\n ],\n [\n -111.566162109375,\n 40.48038142908172\n ],\n [\n -113.35693359375,\n 40.48038142908172\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44ce","contributors":{"authors":[{"text":"Hahl, D. C.","contributorId":57436,"corporation":false,"usgs":true,"family":"Hahl","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":658452,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70178831,"text":"70178831 - 1968 - An appraisal of the quality of surface water in the Sevier Lake basin, Utah, 1964","interactions":[],"lastModifiedDate":"2016-12-09T11:15:10","indexId":"70178831","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1968","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":"19","title":"An appraisal of the quality of surface water in the Sevier Lake basin, Utah, 1964","docAbstract":"The Sevier and Beaver River systems are the two major river systems in the Sevier Lake basin in Utah. This report contains an analysis of reconnaissance data collected during the 1964 water year regarding the quality of water in these rivers and their tributaries. The purpose of the reconnaissance was to obtain needed water-quality information for the basin. Corollary purposes were to (1) determine the suitability of surface water for specific
uses, (2) determine the need and criteria for a water-quality network, and (3) locate sources of organic pollution to the rivers. Data concerning item 3 are mentioned only briefly in this report and will be discussed in a report to be prepared by the Utah Water Pollution and Control Board. Data collected in connection with the reconnaissance and resulting analyses were reported by Hahl and Cabell (1965).
This report provides long-term data on streamflow at selected short-term gaging stations in Utah. The records of streamflow at the short-term or secondary gaging stations are extended on the basis of a graphical correlation with concurrent records at long-term or primary gaging stations. The data presented consist of records of runoff at the short-term stations summarized on a monthly and yearly basis; these data include the actual short-term records and the correlative estimates of runoff. Methods and information are included to enable the reader to make further extensions of runoff records.
The standard error of estimate for correlations used is 30 percent or less, and the coefficient of correlation is at least 0.8. Streamflow information is thereby obtained that is believed to be more representative of the long-term runoff than is an actual short-term record.
This study shows that the optimum period of concurrent record needed in Utah for a reliable correlation is about 15-20 years. Extensions of record for low-flow and flood-frequency studies usually cannot be obtained from correlations. Much of this information could be collected economically by converting short-term stream-gaging stations to partial-record stations after a satisfactory correlation with a long-term station has been obtained.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Reid, J., Carroon, L., and Pyper, G., 1968, Extension of streamflow records in Utah: Technical Publication 20, 110 p.","productDescription":"110 p.","numberOfPages":"114","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331738,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331736,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-440"},{"id":331737,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920008i.pdf"}],"country":"United States","state":"Utah","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-111.046551,41.251716],[-111.046723,40.997959],[-110.750727,40.996847],[-110.715026,40.996347],[-110.539819,40.996346],[-110.500718,40.994746],[-110.375714,40.994947],[-110.250709,40.996089],[-110.237848,40.995427],[-110.125709,40.99655],[-110.121639,40.997101],[-110.048476,40.997555],[-110.006495,40.997815],[-110.000708,40.997352],[-109.999838,40.99733],[-109.97553,40.997912],[-109.855299,40.997614],[-109.854302,40.997661],[-109.715409,40.998191],[-109.713877,40.998266],[-109.676421,40.998395],[-109.534926,40.998143],[-109.500694,40.999127],[-109.250735,41.001009],[-109.231985,41.002059],[-109.173682,41.000859],[-109.050076,41.000659],[-109.048455,40.826081],[-109.049088,40.714562],[-109.048373,40.662602],[-109.048249,40.653601],[-109.048044,40.619231],[-109.050074,40.540358],[-109.049955,40.539901],[-109.050698,40.499963],[-109.050314,40.495092],[-109.050946,40.444368],[-109.050969,40.222662],[-109.050973,40.180849],[-109.050944,40.180712],[-109.050813,40.059579],[-109.050873,40.058915],[-109.050615,39.87497],[-109.05104,39.660472],[-109.051363,39.497674],[-109.050765,39.366677],[-109.051512,39.126095],[-109.052436,38.999985],[-109.053292,38.942878],[-109.053233,38.942467],[-109.053797,38.905284],[-109.053943,38.904414],[-109.054189,38.874984],[-109.057388,38.795456],[-109.059541,38.719888],[-109.060253,38.599328],[-109.059962,38.499987],[-109.060062,38.275489],[-109.054648,38.244921],[-109.041762,38.16469],[-109.041837,38.153022],[-109.04282,37.999301],[-109.042819,37.997068],[-109.043121,37.97426],[-109.041058,37.907236],[-109.041653,37.88117],[-109.041844,37.872788],[-109.041723,37.842051],[-109.041754,37.835826],[-109.041461,37.800105],[-109.042098,37.74999],[-109.041636,37.74021],[-109.04176,37.713182],[-109.041732,37.711214],[-109.042269,37.666067],[-109.042089,37.623795],[-109.042131,37.617662],[-109.041806,37.604171],[-109.041865,37.530726],[-109.041915,37.530653],[-109.043137,37.499992],[-109.043464,37.484711],[-109.04581,37.374993],[-109.046039,37.249993],[-109.045584,37.249351],[-109.045487,37.210844],[-109.045978,37.201831],[-109.045995,37.177279],[-109.045156,37.112064],[-109.045203,37.111958],[-109.045173,37.109464],[-109.045189,37.096271],[-109.044995,37.086429],[-109.045058,37.074661],[-109.045166,37.072742],[-109.045223,36.999084],[-109.181196,36.999271],[-109.233848,36.999266],[-109.246917,36.999346],[-109.26339,36.999263],[-109.268213,36.999242],[-109.270097,36.999266],[-109.378039,36.999135],[-109.381226,36.999148],[-109.495338,36.999105],[-109.625668,36.998308],[-109.875673,36.998504],[-110.000677,36.997968],[-110.000876,36.998502],[-110.021778,36.998602],[-110.47019,36.997997],[-110.490908,37.003566],[-110.50069,37.00426],[-110.599512,37.003448],[-110.625605,37.003416],[-110.62569,37.003721],[-110.75069,37.003197],[-111.066496,37.002389],[-111.133718,37.000779],[-111.254853,37.001077],[-111.278286,37.000465],[-111.405517,37.001497],[-111.405869,37.001481],[-111.412784,37.001478],[-112.35769,37.001025],[-112.368946,37.001125],[-112.534545,37.000684],[-112.538593,37.000674],[-112.540368,37.000669],[-112.545094,37.000734],[-112.558974,37.000692],[-112.609787,37.000753],[-112.899366,37.000319],[-112.966471,37.000219],[-113.965907,36.999976],[-113.965907,37.000025],[-114.0506,37.000396],[-114.051749,37.088434],[-114.051822,37.090976],[-114.052827,37.103961],[-114.051867,37.134292],[-114.052179,37.14711],[-114.051673,37.172368],[-114.051405,37.233854],[-114.051974,37.283848],[-114.051974,37.284511],[-114.0518,37.293044],[-114.0518,37.293548],[-114.051927,37.370459],[-114.051927,37.370734],[-114.051765,37.418083],[-114.052448,37.43144],[-114.052701,37.492014],[-114.052685,37.502513],[-114.052718,37.517264],[-114.052689,37.517859],[-114.052962,37.592783],[-114.052472,37.604776],[-114.051728,37.745997],[-114.051785,37.746249],[-114.05167,37.746958],[-114.051109,37.756276],[-114.049919,37.765586],[-114.048473,37.809861],[-114.049677,37.823645],[-114.049928,37.852508],[-114.049658,37.881368],[-114.050423,37.999961],[-114.049903,38.148601],[-114.050138,38.24996],[-114.049417,38.2647],[-114.05012,38.404536],[-114.050091,38.404673],[-114.050485,38.499955],[-114.049834,38.543784],[-114.049862,38.547764],[-114.050154,38.57292],[-114.049883,38.677365],[-114.049749,38.72921],[-114.049168,38.749951],[-114.049465,38.874949],[-114.048521,38.876197],[-114.048054,38.878693],[-114.049104,39.005509],[-114.047079,39.499943],[-114.047728,39.542742],[-114.047273,39.759413],[-114.047783,39.79416],[-114.047214,39.821024],[-114.047134,39.906037],[-114.046555,39.996899],[-114.046835,40.030131],[-114.046386,40.097896],[-114.046741,40.104231],[-114.046683,40.116931],[-114.046153,40.231971],[-114.046178,40.398313],[-114.045826,40.424823],[-114.045218,40.430282],[-114.045518,40.494474],[-114.045577,40.495801],[-114.045281,40.506586],[-114.043505,40.726292]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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584a7f7de4b07e29c706dd3d","contributors":{"authors":[{"text":"Reid, J.K.","contributorId":54577,"corporation":false,"usgs":true,"family":"Reid","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":655285,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carroon, L.E.","contributorId":29880,"corporation":false,"usgs":true,"family":"Carroon","given":"L.E.","affiliations":[],"preferred":false,"id":655286,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pyper, G. E.","contributorId":35337,"corporation":false,"usgs":true,"family":"Pyper","given":"G. E.","affiliations":[],"preferred":false,"id":655287,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70038403,"text":"wdrCA672 - 1968 - Water Resources Data for California, 1967; Part 2: Water Quality Records","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA672","displayToPublicDate":"2012-05-13T14:53:00","publicationYear":"1968","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-67-2","title":"Water Resources Data for California, 1967; Part 2: Water Quality Records","docAbstract":"Water-resources investigations of the U.S. Geollogical 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 1967 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 R. Stanley Lord, district chief, Menlo Park, Calif.
\nWater-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.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA672","usgsCitation":"U.S. Geological Survey, 1968, Water Resources Data for California, 1967; Part 2: Water Quality Records: U.S. Geological Survey Water Data Report CA-67-2, x, 494, https://doi.org/10.3133/wdrCA672.","productDescription":"x, 494","costCenters":[],"links":[{"id":256933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256921,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1967/ca-67/WDR-1967-wq.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc495e4b08c986b32b726"} ,{"id":70038402,"text":"wdrCA6712 - 1968 - Water Resources Data for California, 1967; Part 1: Surface Water Records; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA6712","displayToPublicDate":"2012-05-13T14:35:00","publicationYear":"1968","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-67-1-2","title":"Water Resources Data for California, 1967; Part 1: Surface Water Records; Volume 2: Northern Great Basin and Central Valley","docAbstract":"The surface-water records for the 1967 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 R. Stanley Lord, district chief, Menlo Park, Calif.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA6712","usgsCitation":"U.S. Geological Survey, 1968, Water Resources Data for California, 1967; Part 1: Surface Water Records; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-67-1-2, xvii, 514 p., https://doi.org/10.3133/wdrCA6712.","productDescription":"xvii, 514 p.","startPage":"489","endPage":"1002","costCenters":[],"links":[{"id":256932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256920,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1967/ca-67/WDR-1967-vol2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Northern Great Basin;Central Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc494e4b08c986b32b720"} ,{"id":70038401,"text":"wdrCA6711 - 1968 - Water Resources Data for California, 1967; Part 1: Surface Water Records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA6711","displayToPublicDate":"2012-05-13T14:14:00","publicationYear":"1968","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-67-1-1","title":"Water Resources Data for California, 1967; Part 1: Surface Water Records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley","docAbstract":"The surface-water records for the 1967 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 R. Stanley Lord, district chief, Menlo Park, Calif.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA6711","usgsCitation":"U.S. Geological Survey, 1968, Water Resources Data for California, 1967; Part 1: Surface Water Records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Central Valley: U.S. Geological Survey Water Data Report CA-67-1-1, xviii, 488 p., https://doi.org/10.3133/wdrCA6711.","productDescription":"xviii, 488 p.","temporalStart":"1966-10-01","temporalEnd":"1967-09-30","costCenters":[],"links":[{"id":256934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256919,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1967/ca-67/WDR-1967-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Colorado River Basin;Southern Great Basin;Pacific Slope Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc493e4b08c986b32b71a"} ,{"id":70038236,"text":"70038236 - 1968 - Hydrogeologic data for the lower Thames and southeastern coastal river basins, Connecticut","interactions":[],"lastModifiedDate":"2014-05-09T07:58:11","indexId":"70038236","displayToPublicDate":"2012-04-22T11:08:00","publicationYear":"1968","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":"16","title":"Hydrogeologic data for the lower Thames and southeastern coastal river basins, Connecticut","docAbstract":"This report presents hydrologic and geologic data collected by the U.S. Geological Survey during an investigation of water resources in the lower Thames and southeastern coastal river basins in cooperation with the Connecticut Water Resources Commission. The report area occupies about 440 square miles in the southeastern part of the State; it includes about 5 square miles in southwestern Rhode Island. It includes the towns of Bozrah, Groton, Ledyard, Montville, New London, Stonington, and Waterford, and parts of Columbia, Colchester, East Lyme, Franklin, Lebanon, North Stonington, Norwich, Old Lyme, Preston, Salem, and Voluntown. A companion interpretive report, Connecticut Water Resources Bulletin No. 15, (Thomas and others, in preparation), evaluates the water resources of the area. 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 from 1963 to 1965.\nStreamflow records from continuous~record gaging stations in the report area for\nthis period have been published annually along with data from other parts of\nthe State in a series of U.S. Geological Survey reports entitled \"Surface\nWater Records of Connecticut.\" Water-level measurements in wells throughout\nthe State from 1960 through 1966~ including those made as part of this\ninvestigations are published in Connecticut Water Resources Bulletin No. 7\n(Meikle and Baker~ 1965) and Connecticut Water Resources Bulletin No. 13\n(Melklee 1967). Most other data collected during this investigation are\ntabulated on the following pages. Included are some previously unpublished\ndata collected prior to the start of this study.\nThe locations of sites at which data were collected are shown on Plate A\nin the pocket at the back of the report. Plate A includes the locations of\n42 miscellaneous sites where measurements of streamflow were made during 1963\nand 1964 and 6 other sites where continuous records are maintained. Data for\n25 of the 42 miscellaneous sites are included in this report: data for the\nremaining 17 miscellaneous sites and for 5 of the 6 continuous-record sites\nhave already been published in \"Surface Water Records of Connecticut.\"\nStreamflow records for Pawcatuck River at Westerly~ Rhode Island have been\npreviously published in \"Surface Water Records of Massachusetts, New Hampshire,\nRhode Island, and Vermont.\"\nData presented, unless otherwise noted, were collected by U.S. Geological\nSurvey 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":"Cervione, M.A., Grossman, I., and Thomas, C.E., 1968, Hydrogeologic data for the lower Thames and southeastern coastal river basins, Connecticut: Connecticut Water Resources Bulletin 16, Report: 65 p.; 1 Plate: 23.64 x 25.06 inches.","productDescription":"Report: 65 p.; 1 Plate: 23.64 x 25.06 inches","numberOfPages":"69","costCenters":[],"links":[{"id":258797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0016/report-thumb.jpg"},{"id":287013,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70038236/report.pdf"},{"id":285979,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038236/plate-a.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Coastal River Basins;Thames","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.316667,41.266667 ], [ -72.316667,41.7 ], [ -72.766667,41.7 ], [ -72.766667,41.266667 ], [ -72.316667,41.266667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a33b6e4b0c8380cd5f1e2","contributors":{"authors":[{"text":"Cervione, Michael A.","contributorId":24602,"corporation":false,"usgs":true,"family":"Cervione","given":"Michael","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grossman, I.G.","contributorId":52574,"corporation":false,"usgs":true,"family":"Grossman","given":"I.G.","email":"","affiliations":[],"preferred":false,"id":463706,"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":463705,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70038235,"text":"70038235 - 1968 - Water resources inventory of Connecticut Part 3: lower Thames and southeastern coastal river basins","interactions":[],"lastModifiedDate":"2014-06-17T11:29:43","indexId":"70038235","displayToPublicDate":"2012-04-22T10:47:00","publicationYear":"1968","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":"15","title":"Water resources inventory of Connecticut Part 3: lower Thames and southeastern coastal river basins","docAbstract":"The lower Thames and southeastern coastal river basins have a relatively abundant supply of water of generally good quality which is derived from streams entering the area and precipitation that has fallen on the area. Annual precipitation has ranged from about 32 inches to 65 inches and has averaged about 48 inches over a 30-year period. Approximately 22 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 report area through estuaries and coastal streams 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 report area, whereas in the summer most of the precipitation is lost through evaporation and transpiration, resulting in sharply reduced stream-flow and lowered ground-water levels. The mean monthly storage of water on an average is about 3.8 inches higher in November than it is in June.
\nThe amount of water that flows through and out of the report area represents the total amount of water potentially available for use by man. For the 30-year period 1931 through 1960, the annual runoff from the report area has averaged nearly 26 inches (200 billion gallons), from the entire Thames River basin above Norwich about 24 inches (530 billion gallons), and from the Pawcatuck River basin about 26 inches (130 billion gallons). A total average annual runoff of 860 billion gallons is therefore available. Although runoff indicates the total amount of water potentially available, it is usually not economically feasible for man to use all of it. On the other hand, with increased development, it is possible that some water will be reused several times.
\nThe water available may be tapped as it flows through the area or is temporarily stored in streams, lakes, and aquifers. The amounts that can be developed vary from place to place and time to time, depending on the amount of precipitation, on the size of drainage area, on the thickness, permeability, and areal extent of aquifers, and on the variations in chemical and physical quality of the water.
\nDifferences in streamflow from point to point are due primarily to differences in the proportion of stratified drift in the drainage basin above each point, which affect the timing of streamflow, and to differences in precipitation, which affect the amount of streamflow.
\nGround water can be obtained from wells almost anywhere in the area, but the amount obtainable at any particular point depends upon the type and water-bearing properties of the aquifers. For practical purposes, the earth materials in the report area comprise three aquifers--stratified drift, bedrock, and till.
\nStratified drift is the only aquifer generally capable of yielding more than 100 gpm (gallons per minute) to individual wells. It covers about 20 percent of the area and occurs chiefly in lowlands where it overlies till and bedrock. The coefficient of permeability of the coarse-grained unit of stratified drift averages about 1,500 gbd (gallons per day) per sq ft. Drilled, screened wells tapping this unit are known to yield from 4 to 88o gpm and average 146 gpm. Dug wells in coarse-grained stratified drift supply about 2 gpm per foot of drawdown over a period of a few hours. Fine-grained stratified drift has an average coefficient of permeability of about 300 gpd per sq ft and can usually yield supplies sufficient for household use to dug wells.
\nBedrock and till are widespread in extent but generally provide only small water supplies. Bedrock is tapped chiefly by drilled wells, about 90 percent of which will supply at least 3 gpm. Very few, however, will supply more than 50 gpm. Till is tapped in a few places by dug wells which can yield small supplies of only a few hundred gpd throughout all or most of the year. The coefficient of permeability of till ranges from about 0.2 gpd per sq ft to 120 gpd per sq ft.
\nThe amount of ground water potentially available in the report area depends upon the amount of ground-water outflow, the amount of ground water in storage, and the quantity of water available by induced infiltration from streams and lakes. From data on permeability, saturated thickness, recharge, yield from aquifer storage, well performance, and streamflow, preliminary estimates of ground-water availability can be made for any point in the report area. Long-term yields estimated for 18 areas of stratified drift especially favorable for development of large ground-water supplies ranged from 1.3 to 66 mgd. Detailed site studies to determine optimum yields, drawdowns, and spacing of individual wells are needed before major ground-water development is undertaken in these or other areas.
\nThe chemical quality of water in the report area is generally good to excellent. Samples of naturally occurring surface water collected at 24 sites contained less than 151 ppm (parts per million) of dissolved solids and less than 63 ppm of hardness. Water from wells is more highly mineralized than naturally occurring water from streams. Even so only 12 percent of the wells sampled yielded water with more than 200 ppm of dissolved solids and only 8 percent yielded water with more than 120 ppm of hardness.
\nEven in major streams, which are used to transport industrial waste, hardness rarely exceeds 60 ppm and the dissolved mineral content is generally less than 200 ppm. At a few places in the town of Montville however, waters may contain dissolved mineral concentrations of 2,000 to 4,000 ppm.
\nIron and manganese in both ground water and surface water are the only constituents whose concentrations commonly exceed recommended limits for domestic and industrial use. Most wells in the report area yield clear water with little or no iron or manganese, but distributed among them are wells yielding ground water that contains enough of these dissolved constituents to be troublesome for most uses.
\nIron concentrations in naturally occurring stream water exceed 0.3 ppm under low-flow conditions at 33 percent of the sites sampled. Large concentrations of iron in stream water result from discharge of iron-bearing water from aquifers or from swamps where it is released largely from decaying vegetation.
\nGround water more than 30 feet below the land surface has a relatively constant temperature, usually between 48°F and 52°F. Water temperature in very shallow wells may fluctuate from about 38°F in February or March to about 55°F in late summer. Water temperature in the larger streams fluctuates much more widely, ranging from 32°F at least for brief periods in winter, to about 85°F occasionally during summer.
\nThe quality of suspended sediment transported by streams in the area is negligible. Turbidity in streams is generally not a problem although amounts large enough to be troublesome may occur locally at times.
\nThe total amount of water used in the report area for all purposes during 1964 was about 118,260 million gallons, of which 105,600 million gallons was estuarine water used for cooling by industry. The average per capita water use, excluding estuarine, temporary summer residence, and institutional water was equivalent to 186 gpd. Public water systems supplied the domestic needs of nearly tw0-thirds the population of the report area. All of the 19 systems, which were sampled, provided water of better quality than the U.S. Public Health Service suggests 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 Resources Commission","usgsCitation":"Thomas, C.E., Cervione, M.A., and Grossman, I., 1968, Water resources inventory of Connecticut Part 3: lower Thames and southeastern coastal river basins: Connecticut Water Resources Bulletin 15, Report: viii, 105 p.; 4 Plates: 23.80 x 23.86 inches and smaller.","productDescription":"Report: viii, 105 p.; 4 Plates: 23.80 x 23.86 inches and smaller","numberOfPages":"122","costCenters":[],"links":[{"id":258795,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0015/report.pdf","size":"22138","linkFileType":{"id":1,"text":"pdf"}},{"id":258796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0015/report-thumb.jpg"},{"id":285977,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038235/plate-c.pdf"},{"id":285978,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038235/plate-d.pdf"},{"id":285975,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038235/plate-a.pdf"},{"id":285976,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038235/plate-b.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Coastal River Basins;Thames","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.316667,41.283333 ], [ -72.316667,41.7 ], [ -71.766667,41.7 ], [ -71.766667,41.283333 ], [ -72.316667,41.283333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb79e4b08c986b32d687","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":463702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cervione, Michael A. Jr.","contributorId":23988,"corporation":false,"usgs":true,"family":"Cervione","given":"Michael","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463701,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grossman, I.G.","contributorId":52574,"corporation":false,"usgs":true,"family":"Grossman","given":"I.G.","email":"","affiliations":[],"preferred":false,"id":463703,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70046325,"text":"wdrNM671 - 1968 - Water resources data for New Mexico, water year 1967; Part 1. surface water records","interactions":[],"lastModifiedDate":"2013-07-08T10:52:45","indexId":"wdrNM671","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1968","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-67-1","title":"Water resources data for New Mexico, water year 1967; Part 1. surface water records","docAbstract":"The surface-water records for the 1967 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 seventh 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\nan 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 by 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/wdrNM671","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Water resources data for New Mexico, water year 1967; Part 1. surface water records: U.S. Geological Survey Water Data Report NM-67-1, 292 p., https://doi.org/10.3133/wdrNM671.","productDescription":"292 p.","costCenters":[],"links":[{"id":273454,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274523,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1967/nm-67/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":"51b300eae4b01368e589e41c","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":535535,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220440,"text":"5220440 - 1968 - Lack of association among duck broodmates during migration and wintering","interactions":[],"lastModifiedDate":"2017-06-07T12:56:03","indexId":"5220440","displayToPublicDate":"2010-06-16T12:17:39","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Lack of association among duck broodmates during migration and wintering","docAbstract":"Male (Lensink, 1964: 19) and female ducks tend to return to the area where they last bred or were raised (Sowles, 1955). Band recovery data show a similar tendency for ducks to return to wintering areas (Stewart et al., 1958; Martinson, 1966). Wintering British Columbia Mallard (Anas platyrhynchos) populations may be definite associations of birds that breed in the same general locality, migrate together, and use the same wintering area (Munro, 1943). On the other hand Gollop (1965: 36-37) showed that Mallards reared in Saskatchewan or breeding there re- turned in subsequent years, but \"neither migrated nor wintered as definite associations.\" He based his conclusions on recovery data from groups of Mallards banded on the same slough and from broodmates. His data showed, by date or area of recovery, that the birds migrated independently and sometimes to different wintering localities. This paper presents additional data suggesting that ducks banded as brood- mates may migrate independently.
","language":"English","publisher":"American Ornithological Society","doi":"10.2307/4083381","usgsCitation":"Martinson, R.K., and Hawkins, A., 1968, Lack of association among duck broodmates during migration and wintering: The Auk, v. 85, no. 4, p. 684-686, https://doi.org/10.2307/4083381.","productDescription":"3 p.","startPage":"684","endPage":"686","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":480327,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/4083381","text":"Publisher Index Page"},{"id":193711,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b43d1","contributors":{"authors":[{"text":"Martinson, R. K.","contributorId":106983,"corporation":false,"usgs":true,"family":"Martinson","given":"R.","middleInitial":"K.","affiliations":[],"preferred":false,"id":331817,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hawkins, A.S.","contributorId":29085,"corporation":false,"usgs":true,"family":"Hawkins","given":"A.S.","email":"","affiliations":[],"preferred":false,"id":331816,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5220597,"text":"5220597 - 1968 - Blood parasites in North American waterfowl","interactions":[],"lastModifiedDate":"2012-02-02T00:15:12","indexId":"5220597","displayToPublicDate":"2010-06-16T12:17:38","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3638,"text":"Transactions of the North American Wildlife and Natural Resources Conference","active":true,"publicationSubtype":{"id":10}},"title":"Blood parasites in North American waterfowl","docAbstract":"One thing seems to stand out in the overall knowledge we have of the blood parasites of waterfowl, as previously noted by Herman and Wehr, (1954): the greatest potential of losses is in the younger age groups, usually those birds 5-10 weeks old. In Leucocytozoon infections, death occurs as early as the first or second week of the bird's life. As a conclusion to this presentation, I wish to emphasize that there are many gaps in our knowledge of these parasites and that the answers are to be obtained by further studies in the young birds. Data obtained from studies of birds shot by hunters or from specimens taken during fall or winter banding operations can be expected to be far less rewarding and significanf than studies of goslings and ducklings. We need much more knowledge of these parasites and their vectors and other relationships before we can develop management procedures to combat or contain them. It will require many more studies in depth to achieve this goal, but the facts are there waiting to be uncovered. These parasites will have to be regulated along with breeding habitat, hunter take, and other factors that all add up to maintenance and management of waterfowl.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the North American Wildlife and Natural Resources Conference","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Herman, C.M., 1968, Blood parasites in North American waterfowl: Transactions of the North American Wildlife and Natural Resources Conference, v. 33, p. 348-359.","productDescription":"348-359","startPage":"348","endPage":"359","numberOfPages":"12","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196344,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607762","contributors":{"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":332086,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4683,"text":"twri08A1 - 1968 - Methods of measuring water levels in deep wells","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri08A1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"08-A1","title":"Methods of measuring water levels in deep wells","docAbstract":"Accurate measurement of water levels deeper than 1,000 feet in wells requires specialized equipment. Corrections for stretch and thermal expansion of measuring tapes must be considered, and other measuring devices must be calibrated periodically. Bore-hole deviation corrections also must be made. \r\nDevices for recording fluctuation of fluid level usually require mechanical modification for use at these depths. A multichannel recording device utilizing pressure transducers has been constructed. This device was originally designed to record aquifer response to nearby underground nuclear explosions but can also be used for recording data from multi-well pumping tests.\r\nBottom-hole recording devices designed for oil-field use have been utilized in a limited manner. These devices were generally found to lack the precision required, in ground-water investigations at the Nevada Test Site but may be applicable in other areas. A newly developed bottom-hole recording pressure gauge of improved accuracy has been used with satisfactory results.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/twri08A1","issn":"0565-596X","usgsCitation":"Garber, M.S., and Koopman, F.C., 1968, Methods of measuring water levels in deep wells: U.S. Geological Survey Techniques of Water-Resources Investigations 08-A1, iv, 23 p. :ill. ;26 cm. Reprinted in 1979., https://doi.org/10.3133/twri08A1.","productDescription":"iv, 23 p. :ill. ;26 cm. Reprinted in 1979.","costCenters":[],"links":[{"id":139159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":244,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri8a1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bfd8","contributors":{"authors":[{"text":"Garber, M. S.","contributorId":6433,"corporation":false,"usgs":true,"family":"Garber","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":149618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koopman, F. C.","contributorId":40586,"corporation":false,"usgs":true,"family":"Koopman","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":149619,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4713,"text":"twri04A1 - 1968 - Some statistical tools in hydrology","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"twri04A1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"04-A1","title":"Some statistical tools in hydrology","docAbstract":"This chapter of 'Techniques of Water-Resources Investigations' provides background material needed for understanding the statistical procedures most useful in hydrology; it furnishes detailed procedures, with examples, of regression analyses; it describes analysis of variance and covariance and discusses the characteristics of hydrologic data.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/twri04A1","issn":"0565-596X","usgsCitation":"Riggs, H.C., 1968, Some statistical tools in hydrology: U.S. Geological Survey Techniques of Water-Resources Investigations 04-A1, vi, 39 p. :ill. ;26 cm. Reprinted in 1977., https://doi.org/10.3133/twri04A1.","productDescription":"vi, 39 p. :ill. ;26 cm. Reprinted in 1977.","costCenters":[],"links":[{"id":139207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":342,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri4a1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a361","contributors":{"authors":[{"text":"Riggs, H. C.","contributorId":17210,"corporation":false,"usgs":true,"family":"Riggs","given":"H.","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":149662,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2494,"text":"wsp1859E - 1968 - Hydrology of Crater, East and Davis Lakes, Oregon; with section on Chemistry of the Lakes","interactions":[],"lastModifiedDate":"2017-02-03T13:43:14","indexId":"wsp1859E","displayToPublicDate":"1994-01-01T00:00:00","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":"E","title":"Hydrology of Crater, East and Davis Lakes, Oregon; with section on Chemistry of the Lakes","docAbstract":"Crater, East, and Davis Lakes are small bodies of fresh water that occupy topographically closed basins in Holocene volcanic terrane. Because the annual water supply exceeds annual evaporation, water must be lost by seepage from each lake. The seepage rates vary widely both in volume and in percentage of the total water supply. Crater Lake loses about 89 cfs (cubic feet per second), equivalent to about 72 percent of its average annual supply. East Lake loses about 2.3 cfs, or about 44 percent of its estimated supply. Davis Lake seepage varies greatly with lake level, but the average loss is about 150 cfs, more than 90 percent of its total supply. The destination of the seepage loss is not definitely known for any of the lakes. \r\n\r\nAn approximate water budget was computed for stationary level for each lake, by using estimates 'by the writer to supplement the hydrologic data available. The three lake waters are dilute. Crater Lake contains about 80 ppm, (parts per million) of dissolved solids---mostly silica, sodium, and bicarbonate, and lesser amounts of calcium, sulfate, and chloride. Much of the dissolved-solids content of Crater Lake---especially the sulfate and chloride---may be related to fumarole and thermal-spring activity that presumably followed the collapse of Mount Mazama. Although Grater Lake loses an estimated 7,000 tons of its 1.5million-ton salt content each year by leakage, the chemical character of the lake did not change appreciably between 1912 and 1964. East Lake contains 200 ppm of dissolved solids, which includes major proportions of calcium, sodium, bicarbonate, and sulfate, but almost no chloride. The lake apparently receives much of its dissolved solids from subsurface thermal springs. Annual solute loss from East Lake by leakage is about 450 tons, or 3 percent of the lake's 15,000-ton estimated solute content. Davis Lake contains only 48 ppm of dissolved solids, much of which is silica and bicarbonate; chloride is almost completely absent. Approximate physical and hydrologic data for the lakes are summarized in the following table.\r\n\r\n[Table]","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1859E","usgsCitation":"Phillips, K.N., and Van Denburgh, A.S., 1968, Hydrology of Crater, East and Davis Lakes, Oregon; with section on Chemistry of the Lakes: U.S. Geological Survey Water Supply Paper 1859, iv, 60 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1859E.","productDescription":"iv, 60 p. :ill. ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":138755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859e/report-thumb.jpg"},{"id":28614,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604971","contributors":{"authors":[{"text":"Phillips, Kenneth N.","contributorId":34105,"corporation":false,"usgs":true,"family":"Phillips","given":"Kenneth","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":145287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145286,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2448,"text":"wsp1859G - 1968 - Storage requirements for Arkansas streams","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1859G","displayToPublicDate":"1994-01-01T00:00:00","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":"G","title":"Storage requirements for Arkansas streams","docAbstract":"The supply of good-quality surface water in Arkansas is abundant. owing to seasonal and annual variability of streamflow, however, storage must be provided to insure dependable year-round supplies in most of the State. Storage requirements for draft rates that are as much as 60 percent of the mean annual flow at 49 continuous-record gaging stations can be obtained from tabular data in this report. \r\n\r\nThrough regional analyses of streamflow data, the State was divided into three regions. Draft-storage diagrams for each region provide a means of estimating storage requirements for sites on streams where data are scant, provided the drainage area, the mean annual flow, and the low-flow index are known. These data are tabulated for 53 gaging stations used in the analyses and for 132 partial-record sites where only base-flow measurements have been made. Mean annual flow can be determined for any stream whose drainage lies within the State by using the runoff map in this report. Low-flow indices can be estimated by correlating base flows, determined from several discharge measurements, with concurrent flows at nearby continuous-record gaging stations, whose low-flow indices have been determined.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1859G","usgsCitation":"Patterson, J.L., 1968, Storage requirements for Arkansas streams: U.S. Geological Survey Water Supply Paper 1859, 36 p. :ill. (1 col.) ;24 cm., https://doi.org/10.3133/wsp1859G.","productDescription":"36 p. :ill. (1 col.) ;24 cm.","costCenters":[],"links":[{"id":138128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859g/report-thumb.jpg"},{"id":28522,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1859g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28523,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4244","contributors":{"authors":[{"text":"Patterson, James Lee","contributorId":24329,"corporation":false,"usgs":true,"family":"Patterson","given":"James","email":"","middleInitial":"Lee","affiliations":[],"preferred":false,"id":145221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2326,"text":"wsp1859B - 1968 - Chemical quality of surface waters in Devils Lake basin North Dakota, 1952-60","interactions":[],"lastModifiedDate":"2024-07-30T19:22:21.418399","indexId":"wsp1859B","displayToPublicDate":"1994-01-01T00:00:00","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":"B","title":"Chemical quality of surface waters in Devils Lake basin North Dakota, 1952-60","docAbstract":"Above-normal precipitation in 1954, 1956, and 1957 caused the water surface of Devils Lake to rise to an altitude of 1,419.3 feet, its highest in 40 years. Nearly all the water entering the lake flowed through Big Coulee, and about three-fourths of that inflow was at rates greater than 100 cubic feet per second. At these rates, the inflow contained less than 600 ppm (parts per million) dissolved solids and was of the calcium bicarbonate type.
Because the inflow was more dilute than the lake water, the dissolved solids in the lake decreased from 8,680 ppm in 1952 to about 6,000 ppm in 1956 and 1957. Subsequently, however, they increased to slightly more than 8,000 ppm and averaged 6,800 ppm for the 1954-60 period. Sodium and sulfate were the principal dissolved constituents in the lake water. Although the concentration of dissolved solids varied significantly from time to time, the relative proportions of the chief constituents remained nearly the same.
Water flowed from Devils Lake to Mission Bay in 1956,1957, and 1958, and some flowed from Mission Bay into East Bay. However, no water moved between East Devils Lake, western Stump Lake, and eastern Stump Lake during 1952-60; these lakes received only local runoff, and the variations in their water volume caused only minor variations in dissolved solids. For the periods sampled, concentrations averaged 60,700 ppm for East Devils Lake, 23,100 ppm for western Stump Lake, and 127,000 ppm for eastern Stump Lake.
Sodium and sulfate were the chief dissolved constituents in all the lakes of the Devils Lake chain. Water in eastern Stump Lake was saturated with sodium sulfate and precipitated large quantities of granular, hydrated sodium sulfate crystals on the lakebed and shore in fall and winter. A discontinuous layer of consolidated sodium sulfate crystals formed a significant part of the bed throughout the year.
Measured concentrations! of zinc, iron, manganese, fluoride, arsenic, boron, copper, and lead were not high enough to harm fish. Data on alpha and beta particle activities in Devils Lake were insufficient to determine if present activities are less than, equal to, or more than activities before nuclear tests began.
Miscellaneous surface waters not in the Devils Lake chain contained dissolved solids that ranged from 239 to 61,200 ppm. The lakes that spill infrequently and have little or no ground-water inflow and outflow generally contain high concentrations of dissolved solids.
Salt balance computations for Devils Lake for 1952-60 indicate that a net of as much as 89,000 tons of salts was removed from the bed by the water in some years and as much as 35,000 tons was added to the bed in other years. For the 9-year period, the tons removed exceeded the tons added; the net removed averaged 2.7 tons per acre per year. Pickup of these salts from the bed increased the dissolved solids in the lake water an average of 193 ppni per year. Between 1952 and 1960, 201,000 tons of salt was added to the bed of East Devils Lake, 15,100 tons to the bed of western Stump Lake, and 421,000 tons to the bed of eastern Stump Lake.
Laboratory examination of shore and bed material indicated that the shore contained less weight of salt per unit weight of dry, inorganic material than the bed. Calcium and bicarbonate were the chief constituents dissolved from bed material of Devils Lake, whereas sodium and sulfate were the chief constituents dissolved from bed material of East Bay, East Devils Lake, and eastern and western Stump Lakes. Generally, calcium and bicarbonate were the chief constitutents dissolved from shore material of all these lakes.
Evidence indicates that not more than 20 percent of the salt that \"disappeared\" from the water of Devils Lake west of State Route 20 as the lake altitudes decreased years ago will redissolve if the lake altitude is restored.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1859B","usgsCitation":"Mitten, H.T., Scott, C., and Rosene, P.G., 1968, Chemical quality of surface waters in Devils Lake basin North Dakota, 1952-60: U.S. Geological Survey Water Supply Paper 1859, Report: iv, 42 p.; 1 Plate: 27.00 x 38.00 inches, https://doi.org/10.3133/wsp1859B.","productDescription":"Report: iv, 42 p.; 1 Plate: 27.00 x 38.00 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":28169,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28168,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1859b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137586,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859b/report-thumb.jpg"},{"id":431666,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25080.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Dakota","otherGeospatial":"Devils Lake basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -99.4066978557347,\n 48.373675264950265\n ],\n [\n -99.4066978557347,\n 47.70314111203487\n ],\n [\n -98.18978187218303,\n 47.70314111203487\n ],\n [\n -98.18978187218303,\n 48.373675264950265\n ],\n [\n -99.4066978557347,\n 48.373675264950265\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3305","contributors":{"authors":[{"text":"Mitten, Hugh T.","contributorId":103652,"corporation":false,"usgs":true,"family":"Mitten","given":"Hugh","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":145018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, C.H.","contributorId":101634,"corporation":false,"usgs":true,"family":"Scott","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":145017,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rosene, Philip G.","contributorId":48942,"corporation":false,"usgs":true,"family":"Rosene","given":"Philip","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145016,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4704,"text":"twri07C3_1968 - 1968 - Preparation of input data for automatic computation of stage-discharge relations at culverts","interactions":[],"lastModifiedDate":"2017-05-18T12:04:59","indexId":"twri07C3_1968","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"07-C3","title":"Preparation of input data for automatic computation of stage-discharge relations at culverts","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/twri07C3_1968","issn":"0565-596X","usgsCitation":"Matthai, H.F., Stull, H.E., and Davidian, J., 1968, Preparation of input data for automatic computation of stage-discharge relations at culverts: U.S. Geological Survey Techniques of Water-Resources Investigations 07-C3, vi, 25 p., https://doi.org/10.3133/twri07C3_1968.","productDescription":"vi, 25 p.","costCenters":[],"links":[{"id":139142,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/twri/07c03-1968/report-thumb.jpg"},{"id":94736,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/twri/07c03-1968/report.pdf","size":"2328","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6691d9","contributors":{"authors":[{"text":"Matthai, Howard Frederick","contributorId":100824,"corporation":false,"usgs":true,"family":"Matthai","given":"Howard","email":"","middleInitial":"Frederick","affiliations":[],"preferred":false,"id":149650,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stull, Harold E.","contributorId":60197,"corporation":false,"usgs":true,"family":"Stull","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":149648,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davidian, Jacob","contributorId":80245,"corporation":false,"usgs":true,"family":"Davidian","given":"Jacob","email":"","affiliations":[],"preferred":false,"id":149649,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":53419,"text":"ofr689 - 1968 - Data for springs in the northern coast ranges and Klamath Mountains of California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:39","indexId":"ofr689","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"68-9","title":"Data for springs in the northern coast ranges and Klamath Mountains of California","language":"ENGLISH","doi":"10.3133/ofr689","usgsCitation":"Berkstresser, C.F., 1968, Data for springs in the northern coast ranges and Klamath Mountains of California: U.S. Geological Survey Open-File Report 68-9, iv, 49 p. : map ; 27 cm., https://doi.org/10.3133/ofr689.","productDescription":"iv, 49 p. : map ; 27 cm.","costCenters":[],"links":[{"id":177471,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0009/report-thumb.jpg"},{"id":87387,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0009/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c904","contributors":{"authors":[{"text":"Berkstresser, Charles F. Jr.","contributorId":43390,"corporation":false,"usgs":true,"family":"Berkstresser","given":"Charles","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":247556,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32657,"text":"pp516E - 1968 - A geophysical study in Grand Teton National Park and vicinity, Teton County, Wyoming","interactions":[],"lastModifiedDate":"2025-05-21T17:47:12.819568","indexId":"pp516E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"516","chapter":"E","title":"A geophysical study in Grand Teton National Park and vicinity, Teton County, Wyoming","docAbstract":"An integrated geophysical study - comprising gravity, seismic refraction, and aeromagnetic surveys - was made of a 4,600-km2 area in Grand Teton National Park and vicinity, Wyoming, for the purpose of obtaining a better understanding of the structural relationships in the region. The Teton range is largely comprised of Precambrian crystalline rocks and layered metasedimentary gneiss, but it also includes granitic gneiss, hornblende-plagioclase gneiss, granodiorite, and pegmatite and diabase dikes. Elsewhere, the sedimentary section is thick. The presence of each system except Silurian provides a chronological history of most structures. Uplift of the Teton-Gros Ventre area began in the Late Cretaceous; most of the uplift occurred after middle Eocene time. Additional uplift of the Teton Range and downfaulting of Jackson Hole began in the late Pliocene and continues to the present.
Bouguer anomalies range from -185 mgal over Precambrian rocks of the Teton Range to -240 mgal over low-density Tertiary and Cretaceous sedimentary rocks of Jackson Hole. The Teton fault (at the west edge of Jackson Hole), as shown by steep gravity gradients and seismic-refraction data, trends north-northeast away from the front of the Teton Range in the area of Jackson Lake. The Teton fault either is shallowly inclined in the Jenny Lake area, or it consists of a series of fault steps in the fault zone; it is approximately vertical in the Arizona Creek area.
Seismic-refraction data can be fitted well by a three-layer gravity model with velocities of 2.45 km per sec for the Tertiary and Cretaceous rocks above the Cloverly Formation, 3.9 km per sec for the lower Mesozoic rocks, and 6.1 km per sec for the Paleozoic (limestone and dolomite) and Precambrian rocks. Gravity models computed along two seismic profiles are in good agreement (σ=± 2 mgal) if density contrasts with the assumed 2.67 g per cm3 Paleozoic and Precambrian rocks are assumed to be -0.35 and -0.10 g per cm3 for the 2.45 and 3.9 km per sec velocity layers, respectively. The Teton Range has a maximum vertical uplift of about 7 km, as inferred from the maximum depth to basement of about 5 km.
Aeromagnetic data show a 400γ positive anomaly in the Gros Ventre Range, which trends out of the surveyed area at the east edge. Exposed Precambrian rocks contain concentrations of magnetite and hematite. A prominent anomaly of about 100γ is associated with the Gros Ventre Range, and 100γ anomalies are associated with the layered gneiss of the Teton Range. On this basis the unmapped Precambrian rocks of the Gross Ventre Range are interpreted as layered gneiss. The sources of the magnetic anomalies, as indicated by depth determination, are at the surface of the Precambrian rocks. A model fitted to a profile across the Gros Ventre Range gives a depth to the Precambrian surface and a susceptibility of 0.0004 emu (electromagnetic units) for the source, which is consistent with modal analyses of the layered gneisses. A residual magnetic map shows that the granitic rocks and layered gneiss probably continue beneath the floor of Jackson Hole east of the Teton fault. The location of aeromagnetic anomalies is consistent with the interpretation that the Teton fault diverges from the front of the Teton Range.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geophysical field investigations, 1964-67 (Professional Paper 516)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp516E","usgsCitation":"Behrendt, J.C., Tibbetts, B.L., Bonini, W.E., Lavin, P.M., Love, J.D., and Reed, J., 1968, A geophysical study in Grand Teton National Park and vicinity, Teton County, Wyoming: U.S. Geological Survey Professional Paper 516, Report: v, 23 p.; 3 Plates: 14.00 × 20.00 inches or smaller, https://doi.org/10.3133/pp516E.","productDescription":"Report: v, 23 p.; 3 Plates: 14.00 × 20.00 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":125352,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0516e/report-thumb.jpg"},{"id":60549,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0516e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394917,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4545.htm"},{"id":60546,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0516e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60547,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0516e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60548,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0516e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","county":"Teton County","otherGeospatial":"Grand Teton National Park and vicinity","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.0223388671875,\n 43.09697190802465\n ],\n [\n -110.2313232421875,\n 43.09697190802465\n ],\n [\n -110.2313232421875,\n 44.15068115978094\n ],\n [\n -111.0223388671875,\n 44.15068115978094\n ],\n [\n -111.0223388671875,\n 43.09697190802465\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4957e4b0b290850ef129","contributors":{"authors":[{"text":"Behrendt, John Charles jbehrendt@usgs.gov","contributorId":74747,"corporation":false,"usgs":true,"family":"Behrendt","given":"John","email":"jbehrendt@usgs.gov","middleInitial":"Charles","affiliations":[],"preferred":false,"id":208873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tibbetts, Benton L.","contributorId":105169,"corporation":false,"usgs":true,"family":"Tibbetts","given":"Benton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":208875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bonini, William E.","contributorId":87417,"corporation":false,"usgs":true,"family":"Bonini","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":208874,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lavin, Peter M.","contributorId":42087,"corporation":false,"usgs":true,"family":"Lavin","given":"Peter","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":208871,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Love, J. D.","contributorId":64620,"corporation":false,"usgs":true,"family":"Love","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":208872,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Reed, John C. jreed@usgs.gov","contributorId":1259,"corporation":false,"usgs":true,"family":"Reed","given":"John C.","email":"jreed@usgs.gov","affiliations":[],"preferred":true,"id":208870,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":13737,"text":"ofr69104 - 1968 - Infrared survey of the Pisgah Crater area, San Bernardino County, California - a geologic interpretation","interactions":[],"lastModifiedDate":"2012-02-02T00:06:51","indexId":"ofr69104","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"69-104","title":"Infrared survey of the Pisgah Crater area, San Bernardino County, California - a geologic interpretation","docAbstract":"The infrared survey of the Pisgah Crater Area, San Bernardino County, California was primarily undertaken to establish parameters by which rock types, structures, and textures peculiar to this locale could be recognized or differentiated. A secondary purpose was to provide an adequate evaluation and calibration of airborne and ground-based instruments used in the survey.\r\n \r\nPisgah Crater and its vicinity was chosen as one of the fundamental test sites for the NASA remote sensing program because of its relatively fresh basaltic flows and pyroclastics. Its typical exposure of basalt also made it a possible lunar analogue. A fundamental test site for the purpose of the program is defined as a readily accessible area for which the topography, geology, hydrology, soils, vegetation and other features are relatively well known. All remote sensor instrument teams, i.e. infrared, radar, microwave, and photography, were obligated to use the fundamental test sites for instrument evaluation and to establish terrain identification procedures. \r\n\r\nPisgah Crater, nearby Sunshine Cone, and their associated lava flows are in the southern Mojave Desert about 40 miles east-southeast of Barstow, California. (See fig. 1.) U. S. Highway 66 skirts .the northern part of the area and provides access via asphalt-paved and dirt roads to the Crater and to the perimeters of the flows. Pisgah Crater, which is a pumiceous cone, is owned and occasionally quarried by the Atchison, Topeka and Santa Fe Railroad. The remaining part of the area to the south is within the boundary of the Marine Corps Base, Twentynine Palms, California and is currently being used as a gunnery, and bombing range. The proximate area to east, west, and north of Pisgah Crater is public domain. \r\n\r\nOriginally, an area totaling 10 square miles was outlined for detailed study. (See plate 1.) This included an 8 mile long strip extending south- east from and including Pisgah Crater to Lavic Dry Lake, and a 2 mile strip aligned to include a portion of the Sunshine lava flow and the dry lake. Additional aerial infrared imagery of the Sunshine and Pisgah flows along the Pisgah fault proved so interesting and informative that this area is included in the discussion. \r\n\r\nInfrared surveys were flown February ii through 13, 1965 and August 5 and 9, 1966. The initial survey was flown by the NASA personnel aboard the NASA 926 Convair 240 aircraft. Because of technical problems with the infrared scanners (4.5-5.5 and 8-14 micron bands) and with certain ground instruments, most of the imagery and ground temperature data obtained during the initial survey period was of little value. However, excellent infrared imagery in the 8-14 micron (?) region of the spectrum was acquired by the Geological Survey during the August 1966 survey. The scanner was mounted in a Beech D-18 aircraft provided by the Survey's Water Resources Division. Likewise, more reliable ground data was obtained at this time owing to improved instrumentation and technique. Ground data were taken by Geological Survey personnel including W. A. Fischer, J. D. Friedman, W. R. Hemphill, D. L. Daniels, G. R. Boynton, Po W. Philbin and the author. C. R. Fross operated the infrared scanner during the August, 1966 survey and R. M. Turner was-responsible for photo processing of the infrared imagery. Their assistance is gratefully acknowledged.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr69104","usgsCitation":"Gawarecki, S.J., 1968, Infrared survey of the Pisgah Crater area, San Bernardino County, California - a geologic interpretation: U.S. Geological Survey Open-File Report 69-104, 49 p. :maps ;29 cm., https://doi.org/10.3133/ofr69104.","productDescription":"49 p. :maps ;29 cm.","costCenters":[],"links":[{"id":147296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0104/report-thumb.jpg"},{"id":42312,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0104/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42313,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0104/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42314,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0104/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66daf1","contributors":{"authors":[{"text":"Gawarecki, Stephen J.","contributorId":52189,"corporation":false,"usgs":true,"family":"Gawarecki","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":168313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":58093,"text":"wdrWI6712 - 1968 - Water resources data for Wisconsin, 1967; Part 1. Surface water records and Part 2. Water quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:32","indexId":"wdrWI6712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"WI-67-1-2","title":"Water resources data for Wisconsin, 1967; Part 1. Surface water records and Part 2. Water quality records","language":"ENGLISH","doi":"10.3133/wdrWI6712","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1968, Water resources data for Wisconsin, 1967; Part 1. Surface water records and Part 2. Water quality records: U.S. Geological Survey Water Data Report WI-67-1-2, 228 p., https://doi.org/10.3133/wdrWI6712.","productDescription":"228 p.","numberOfPages":"228","costCenters":[],"links":[{"id":182569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1967/wi-67-1-2/report-thumb.jpg"},{"id":88322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1967/wi-67-1-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1694","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":533206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}