This report contains climatologic and hydrologic data that were collected as a part of an investigation of the southeastern Uinta Basin, Utah and Colorado, by the U.S. Geological Survey. The data apply mainly to water years 1975 and 1976, which includes the period from October 1974 through September 1976. Included also are some earlier ground-water data not previously published. Similar reports will be published periodically during the data-collection phase of the project, which ends September 1979.
The investigation encompasses the collection and interpretation of a variety of climatologic, hydrologic, and geologic information in and near the southeastern Uinta Basin in order to (1) define the natural hydrologic system according to the occurrence, use, quantity, and quality of water; (2) define various hydrologic characteristics such as the seasonal and areal distribution of temperature, precipitation, evapotranspiration, and streamflow; (3) determine the water demands that might be imposed on the hydrologic system as a result of oil-shale development; and (3) develop simulation models that could be used to predict the effects of various water-use plans that would satisfy these demands .
The data collection during water years 1975 and 1976 was carried out in cooperation with the Utah Department of Natural Resources, the U.S. Bureau of Land Management, and the U. S. Environmental Protect:ion Agency.
The hydrologic settings of 150 lakes in the north central United States were investigated by principal component analysis as a first attempt to develop a general classification of the hydrologic settings of lakes. Precipitation-evaporation balance and the water quality variables have high loadings on the first principal component. Highest loadings on component 2 are for streamflow in and out of the lakes. Components 3 and 4 are characterized by geologic and groundwater flow variables. The drainage basin area/lake area ratio, the overland runoff variable, has the highest loading on component 5. The stability of the principal components was tested by randomly splitting the data and comparing a principal component analysis of each subsample. This showed the first two principal components to be the most stable. The components described by the groundwater variables are less stable, but there is justification for using them with caution. Of the variables examined in this study the distribution of dissolved solids of groundwater is most closely related to the distribution of lake types as determined by other limnological typologies in the north central United States. The study indicates that the following are the most important variables to be considered in classifying the hydrologic settings of lakes: dissolved solids concentration of groundwater, precipitation-evaporation balance, streamflow inlet and outlet, the ratio of drainage basin area to lake area, and lake depth. Of the groundwater variables, local relief and regional slope are more important than is regional position. Texture of the drift and bedrock, which is related to hydraulic conductivity of the rocks, is very important.
","language":"English","publisher":"AGU","doi":"10.1029/WR013i004p00753","usgsCitation":"Winter, T.C., 1977, Classification of the hydrologic settings of lakes in the north central United States: Water Resources Research, v. 13, no. 4, p. 753-767, https://doi.org/10.1029/WR013i004p00753.","productDescription":"15 p.","startPage":"753","endPage":"767","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":352438,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5aff5002e4b0da30c1bfdc66","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":730886,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8000,"text":"ofr77705 - 1977 - Gravity measurements on summer sea ice in the Beaufort and Chukchi seas, 1976","interactions":[],"lastModifiedDate":"2024-01-18T13:35:09.074238","indexId":"ofr77705","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","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":"77-705","title":"Gravity measurements on summer sea ice in the Beaufort and Chukchi seas, 1976","docAbstract":"During September, 1976, a series of gravity measurements was made in the western Beaufort Sea and the northern Chukchi Sea on ice floes and on a grounded ice island. The data were taken to evaluate the technique of measuring gravity on small ice floes in summer and to supplement and extend previous measurements in the area. The locations of the gravity stations are shown on the map, which also shows previously published data taken by ship-borne gravity meters in the same general area taken from Ruppel and McHendrie (1976) and Boucher et al. (1977). Seventeen gravity stations were occupied during a 26-day cruise aboard USCGC Glacier.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77705","usgsCitation":"Boucher, G., 1977, Gravity measurements on summer sea ice in the Beaufort and Chukchi seas, 1976: U.S. Geological Survey Open-File Report 77-705, 5 p., https://doi.org/10.3133/ofr77705.","productDescription":"5 p.","costCenters":[],"links":[{"id":424593,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0705/report.pdf"},{"id":140337,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0705/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Beaufort Sea, Chukchi Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -177.36551143317985,\n 71.17870556893348\n ],\n [\n -177.36551143317985,\n 69.01345914043634\n ],\n [\n -131.42579581215546,\n 69.01345914043634\n ],\n [\n -131.42579581215546,\n 71.17870556893348\n ],\n [\n -177.36551143317985,\n 71.17870556893348\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db6720f2","contributors":{"authors":[{"text":"Boucher, Gary","contributorId":48594,"corporation":false,"usgs":true,"family":"Boucher","given":"Gary","affiliations":[],"preferred":false,"id":156963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70170541,"text":"70170541 - 1977 - Preliminary determination of epicenters (PDE) and earthquake data report (EDR)","interactions":[],"lastModifiedDate":"2016-04-24T12:41:59","indexId":"70170541","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Preliminary determination of epicenters (PDE) and earthquake data report (EDR)","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Derr, J., 1977, Preliminary determination of epicenters (PDE) and earthquake data report (EDR): Earthquake Information Bulletin (USGS), v. 9, no. 4, p. 34-35.","productDescription":"2 p.","startPage":"34","endPage":"35","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320487,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571dee2ce4b071321fe56419","contributors":{"authors":[{"text":"Derr, J.S.","contributorId":37477,"corporation":false,"usgs":true,"family":"Derr","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":627547,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009904,"text":"70009904 - 1977 - The U.S. geological survey rass-statpac system for management and statistical reduction of geochemical data","interactions":[],"lastModifiedDate":"2013-01-21T16:00:05","indexId":"70009904","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"The U.S. geological survey rass-statpac system for management and statistical reduction of geochemical data","docAbstract":"RASS is an acronym for Rock Analysis Storage System and STATPAC, for Statistical Package. The RASS and STATPAC computer programs are integrated into the RASS-STATPAC system for the management and statistical reduction of geochemical data. The system, in its present form, has been in use for more than 9 yr by scores of U.S. Geological Survey geologists, geochemists, and other scientists engaged in a broad range of geologic and geochemical investigations. The principal advantage of the system is the flexibility afforded the user both in data searches and retrievals and in the manner of statistical treatment of data. The statistical programs provide for most types of statistical reduction normally used in geochemistry and petrology, but also contain bridges to other program systems for statistical processing and automatic plotting. ?? 1977.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(77)90025-5","issn":"00983004","usgsCitation":"VanTrump, G., and Miesch, A., 1977, The U.S. geological survey rass-statpac system for management and statistical reduction of geochemical data: Computers & Geosciences, v. 3, no. 3, p. 475-488, https://doi.org/10.1016/0098-3004(77)90025-5.","startPage":"475","endPage":"488","numberOfPages":"14","costCenters":[],"links":[{"id":266201,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(77)90025-5"},{"id":219725,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba948e4b08c986b322171","contributors":{"authors":[{"text":"VanTrump, G. Jr.","contributorId":68745,"corporation":false,"usgs":true,"family":"VanTrump","given":"G.","suffix":"Jr.","affiliations":[],"preferred":false,"id":357413,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miesch, A.T.","contributorId":88726,"corporation":false,"usgs":true,"family":"Miesch","given":"A.T.","affiliations":[],"preferred":false,"id":357414,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70009920,"text":"70009920 - 1977 - Radioactive springs geochemical data related to uranium exploration","interactions":[],"lastModifiedDate":"2025-03-05T18:01:19.814909","indexId":"70009920","displayToPublicDate":"1977-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Radioactive springs geochemical data related to uranium exploration","docAbstract":"Current interest in geothermal potential of thermal-spring areas in the Appalachians enhances the value of data on thermal springs and wells in these areas. This report presents maps showing locations of selected springs and wells and tables of physical and chemical data pertaining to these wells and springs. The chemical tables show compositions of gases (oxygen, nitrogen, argon, methane, carbon dioxide, and helium), isotope contents (tritium, carbon-13, and oxygen-18), trace and minor element chemical data, and concentrations of the major chemical constituents.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7725","usgsCitation":"Hobba, W., Chemerys, J., Fisher, D., and Pearson, F.J., 1977, Geochemical and hydrologic data for wells and springs in thermal-spring areas of the Appalachians: U.S. Geological Survey Water-Resources Investigations Report 77-25, v, 36 p., https://doi.org/10.3133/wri7725.","productDescription":"v, 36 p.","costCenters":[],"links":[{"id":157265,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0025/report-thumb.jpg"},{"id":406141,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0025/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6f5","contributors":{"authors":[{"text":"Hobba, W.A. Jr.","contributorId":77518,"corporation":false,"usgs":true,"family":"Hobba","given":"W.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":194005,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chemerys, J.C.","contributorId":94293,"corporation":false,"usgs":true,"family":"Chemerys","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":850709,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fisher, D.W.","contributorId":77519,"corporation":false,"usgs":true,"family":"Fisher","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":850710,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pearson, F. J. Jr.","contributorId":7696,"corporation":false,"usgs":true,"family":"Pearson","given":"F.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":850711,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70168650,"text":"70168650 - 1977 - Water resources data for Iowa, water year 1976","interactions":[],"lastModifiedDate":"2016-02-22T15:09:21","indexId":"70168650","displayToPublicDate":"1974-01-01T16:15:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data for Iowa, water year 1976","docAbstract":"No abstract available.
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water year for Washington, consist of records, of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels in wells and springs. This report, in two volumes, contains discharge records for 248 gaging stations; stage only records for 3 gaging stations; stage and contents for 44 lakes and reservoirs; water quality for 124 stations, and 8 lakes; and water levels for 108 observation wells. Also included are 172 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Washington.
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\"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcdc9","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":533119,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180025,"text":"70180025 - 1976 - Developing a state water plan: Ground-water conditions in Utah, spring of 1976","interactions":[],"lastModifiedDate":"2017-01-23T12:58:20","indexId":"70180025","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1976","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":"15","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1976","docAbstract":"This report is the thirteenth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.
This report, like the others (see references, p. 16), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing water-table configuration are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.
This report includes individual discussions of selected major areas of ground-water withdrawal in the State for the calendar year 1975. Water-level fluctuations, however, are described for the period spring 1975 to spring 1976. Much of the data used in this report were collected by the U.S. 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":"Sumison, C., Jibson, W., Bolke, E., Mower, R.W., Herbert, L.R., Cordova, R., Jensen, V., ReMillard, M.D., Sandberg, G.W., and Bjorklund, L., 1976, Developing a state water plan: Ground-water conditions in Utah, spring of 1976: Cooperative Investigations Report 15, viii, 69 p.","productDescription":"viii, 69 p.","numberOfPages":"79","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333715,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333714,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-189"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5887248fe4b08aa8f945abfc","contributors":{"authors":[{"text":"Sumison, C.T.","contributorId":39057,"corporation":false,"usgs":true,"family":"Sumison","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":659859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jibson, W.N.","contributorId":27928,"corporation":false,"usgs":true,"family":"Jibson","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":659860,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":659861,"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":659862,"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":659863,"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":659864,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jensen, V.L.","contributorId":99034,"corporation":false,"usgs":true,"family":"Jensen","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":659865,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"ReMillard, M. D.","contributorId":38645,"corporation":false,"usgs":true,"family":"ReMillard","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":659866,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659867,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659868,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70043109,"text":"70043109 - 1976 - Electronic thermal sensor and Data Collection Platform technology: Part 5 in Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System","interactions":[{"subject":{"id":10744,"text":"ofr7787 - 1977 - Electronic thermal sensor and Landsat data collection platform technology","indexId":"ofr7787","publicationYear":"1977","noYear":false,"title":"Electronic thermal sensor and Landsat data collection platform technology"},"predicate":"SUPERSEDED_BY","object":{"id":70043109,"text":"70043109 - 1976 - Electronic thermal sensor and Data Collection Platform technology: Part 5 in Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System","indexId":"70043109","publicationYear":"1976","noYear":false,"title":"Electronic thermal sensor and Data Collection Platform technology: Part 5 in Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System"},"id":1}],"lastModifiedDate":"2013-02-05T12:00:58","indexId":"70043109","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":360,"text":"Final Report","active":false,"publicationSubtype":{"id":6}},"title":"Electronic thermal sensor and Data Collection Platform technology: Part 5 in Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System","docAbstract":"Five Data Collection Platforms (DCP) were integrated electronically with thermall sensing systems, emplaced and operated in an analog mode at selected thermally significant volcanic and geothermal sites. The DCP's transmitted 3260 messages comprising 26,080 ambient, surface, and near-surface temperature records at an accuracy of ±1.15 °C for 1121 instrument days between November 14, 1972 and April 17, 1974. In harsh, windy, high-altitude volcanic environments the DCP functioned best with a small dipole antenna. Sixteen kg of alkaline batteries provided a viable power supply for the DCP systems, operated at a low-duty cycle, for 5 to 8 months. A proposed solar power supply system would lengthen the period of unattended operation of the system considerably. Special methods of data handling such as data storage via a proposed memory system would increase the significance of the twice-daily data reception enabling the DCP's to record full diurnal-temperature cycles at volcanic or geothermal sites. Refinements in the temperature-monitoring system designed and operated in experiment SR 251 included a backup system consisting of a multipoint temperature scanner, a servo mechanism and an analog-to-digital recorder. Improvements were made in temperature-probe design and in construction of corrosion-resistant seals by use of a hydrofluoric-acid-etching technique.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043109","usgsCitation":"Preble, D.M., Friedman, J.D., and Frank, D., 1976, Electronic thermal sensor and Data Collection Platform technology: Part 5 in Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System: Final Report, 64 p., https://doi.org/10.3133/70043109.","productDescription":"64 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":266996,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5112382ce4b0ebe69d7eb6ce","contributors":{"authors":[{"text":"Preble, Duane M.","contributorId":36560,"corporation":false,"usgs":true,"family":"Preble","given":"Duane","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":472977,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Jules D.","contributorId":79464,"corporation":false,"usgs":true,"family":"Friedman","given":"Jules","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":472978,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frank, David","contributorId":13969,"corporation":false,"usgs":true,"family":"Frank","given":"David","affiliations":[],"preferred":false,"id":472976,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70042814,"text":"70042814 - 1976 - Exploration for porphyry copper deposits in Pakistan using digital processing of Landsat-1 data","interactions":[{"subject":{"id":15841,"text":"ofr7518 - 1975 - Exploration for porphyry copper deposits in Pakistan using digital processing of ERTS-1 data","indexId":"ofr7518","publicationYear":"1975","noYear":false,"title":"Exploration for porphyry copper deposits in Pakistan using digital processing of ERTS-1 data"},"predicate":"SUPERSEDED_BY","object":{"id":70042814,"text":"70042814 - 1976 - Exploration for porphyry copper deposits in Pakistan using digital processing of Landsat-1 data","indexId":"70042814","publicationYear":"1976","noYear":false,"title":"Exploration for porphyry copper deposits in Pakistan using digital processing of Landsat-1 data"},"id":1}],"lastModifiedDate":"2023-08-17T20:03:26.50537","indexId":"70042814","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Exploration for porphyry copper deposits in Pakistan using digital processing of Landsat-1 data","docAbstract":"Rock-type classification by digital-computer processing of Landsat-1 (formerly ERTS-1) multispectral scanner data has been used to select 23 prospecting targets in the Chagai District, Pakistan, 5 of which have proved to be large areas of hydrothermally altered porphyry containing pyrite. The known porphyry copper deposit at Saindak was used as a control area. Empirical maximum and minimum apparent reflectance limits were selected for each multispectral scanner band in each rock type classified, and a relatively unrefined classification table was prepared. Where the values for all four bands fitted within the limits designated for a particular class, a symbol for the presumed rock type was printed by the computer at the appropriate location; these symbols formed a classification map. Drainage channels, areas of mineralized quartz diorite, areas of pyrite-rich rock, and the approximate limit of propylitic alteration were very well delineated on the computer-generated map of the test area. The classification method was then used to evaluate 2,100 km2 in the Mashki Chah region, east of the test area, and a partial check of the results was made in the field. The results of the experiment show that outcrops of hydrothermally altered and mineralized rock can be identified from Landsat-1 data under favorable conditions. The empirical method of digital computer classification of the multispectral scanner data was relatively unrefined and rapid. The five mineralized prospecting sites identified are in locations that I would not have selected as favorable on the basis of geologic knowledge or photogeologic interpretation at the time of the investigation.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Schmidt, R.G., 1976, Exploration for porphyry copper deposits in Pakistan using digital processing of Landsat-1 data: Journal of Research of the U.S. Geological Survey, v. 4, no. 1, p. 27-34.","productDescription":"8 p.","startPage":"27","endPage":"34","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":266418,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue1/report.pdf","text":"report","size":"16.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":266419,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Pakistan","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 60.87,23.54 ], [ 60.87,37.06 ], [ 77.82,37.06 ], [ 77.82,23.54 ], [ 60.87,23.54 ] ] ] } } ] }","volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51026611e4b0d4f5ea817bd9","contributors":{"authors":[{"text":"Schmidt, Robert G.","contributorId":19243,"corporation":false,"usgs":true,"family":"Schmidt","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":472320,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70043031,"text":"70043031 - 1976 - Gravity and magnetic studies of the Geysers-Clear Lake geothermal region, California, USA","interactions":[{"subject":{"id":14265,"text":"ofr75368 - 1975 - Gravity and magnetic studies of The Geysers-Clear Lake geothermal region, California","indexId":"ofr75368","publicationYear":"1975","noYear":false,"title":"Gravity and magnetic studies of The Geysers-Clear Lake geothermal region, California"},"predicate":"SUPERSEDED_BY","object":{"id":70043031,"text":"70043031 - 1976 - Gravity and magnetic studies of the Geysers-Clear Lake geothermal region, California, USA","indexId":"70043031","publicationYear":"1976","noYear":false,"title":"Gravity and magnetic studies of the Geysers-Clear Lake geothermal region, California, USA"},"id":1}],"lastModifiedDate":"2013-01-31T11:10:00","indexId":"70043031","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Gravity and magnetic studies of the Geysers-Clear Lake geothermal region, California, USA","docAbstract":"Gravity and magnetic fields in The Geysers-Clear Lake region are interpreted in relation to the known geology and other available geophysical data. New gravity data provide additional detail with the area of geothermal steam production. Computer techniques were used for removal of the regional gravity field, anomaly enhancement, and modeling subsurface structures. The gravity field was separated into three components: (1) a regional field presumed to be due to deep crustal structure related to the continental margin; (2) a residual gravity low of approximately 30 mgal centered over Mount Hannah and having an approximate diameter of 20 km, which is caused, according to our model, by a magma chamber whose top lies within 10 km of the surface; and (3) a closed residual low over the original steam production field. This low is probably related to effects within 1.5 km of the surface and was modeled as a steam-saturated reservoir structure. Local magnetic highs correlate with surface outcrops of serpentinite and relief on the volcanic rocks. Upward continuation of the aeromagnetic data suggests that the serpentinite body along the Collayomi fault may extend to a depth of more than 3 km near Boggs Mountain, but that other serpentinite bodies are probably more shallow. A long-wavelength magnetic high (centered at ~39°03'N 122°33'W) and a magnetic low (centered at ~38°:43'N 122°47'W) give half-width depth estimates of about 10 km. The center of the Mount Hannah gravity low lies in an area between these features and appears devoid of deep magnetic expression.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"U.S. Energy Research and Development Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Isherwood, W., 1976, Gravity and magnetic studies of the Geysers-Clear Lake geothermal region, California, USA, in Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975, v. 2, p. 1065-1073.","productDescription":"9 p.","startPage":"1065","endPage":"1073","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":266800,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.41,32.53 ], [ -124.41,42.0 ], [ -114.13,42.0 ], [ -114.13,32.53 ], [ -124.41,32.53 ] ] ] } } ] }","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"510ba08ae4b0947afa3c85ac","contributors":{"authors":[{"text":"Isherwood, William F.","contributorId":71547,"corporation":false,"usgs":true,"family":"Isherwood","given":"William F.","affiliations":[],"preferred":false,"id":472806,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70039591,"text":"70039591 - 1976 - National Cartographic Information Center Newsletter No. 4","interactions":[],"lastModifiedDate":"2012-08-14T01:01:44","indexId":"70039591","displayToPublicDate":"2012-01-01T13:05:24","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":373,"text":"Newsletter","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"4","title":"National Cartographic Information Center Newsletter No. 4","docAbstract":"Last week, the editor of this publication was told to start signing the introduction. Something to do with credit given for work done. We look at it in the unfortunate light of accountability; our days under the bushel of anonymity are over. Speaking of accountability, it's about time we gave some recognition to the Newsletter's unknowing progenitor, John Wright, of the British Directorate of Overseas Surveys. Editorially and stylistically, the NCIC Newsletter owes him a large debt. Last month we received a suggestion from a reader that the Newsletter begin consistently listing prices for new products. In the publishing business, however, there is an infallible law of inflation prices increase as soon as they appear in print. We do try to quote exact prices where possible, and as our reader suggested, ballpark figures when we have to. In nearly all cases, additional information is available either by contacting the addresses listed in the article or indexed in the back or by calling NCIC's User Services Section. Numerous bits and pieces of information make up the bulk of this issue. Among them are the possibility of the Geological Survey issuing readable indexes to available topographic maps, the development of an NCIC classification system for U.S. cartographic data, and information on the publication of prototype topographic-bathymetric maps. Lastly, here is our quarterly solicitation for suggestions, comments, criticism, notes, and information for publication. Call it your bicentennial contribution to participatory democracy.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039591","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, National Cartographic Information Center Newsletter No. 4: Newsletter 4, 12 p., https://doi.org/10.3133/70039591.","productDescription":"12 p.","numberOfPages":"14","costCenters":[{"id":409,"text":"National Cartographic Information Center","active":false,"usgs":true}],"links":[{"id":261115,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039591/report.pdf"},{"id":261116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039591/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a619ce4b0c8380cd71a77","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":535383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70001132,"text":"70001132 - 1976 - Measurements of exclusive photoproduction processes at large values of t and u from 4 to 7.5 GeV","interactions":[],"lastModifiedDate":"2021-04-26T12:52:01.035502","indexId":"70001132","displayToPublicDate":"2010-09-28T23:09:32","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3062,"text":"Physical Review D","active":true,"publicationSubtype":{"id":10}},"title":"Measurements of exclusive photoproduction processes at large values of t and u from 4 to 7.5 GeV","docAbstract":"Exclusive photoproduction cross sections have been measured for the processes γp→π+n, γp→π0p, γp→π−Δ++, γp→ρ0p, γp→K+Λ, and γp→K+Σ0 at large t and u values at several energies for each process between 4 and 7.5 GeV. These measurements taken together with past data taken at small values of t and u provide complete angular distributions. The data show the usual small t and u peaks and a central region in which the cross section decreases approximately as s−7. The results are discussed within the context of parton or constituent models.
","language":"English","publisher":"APS Physics","doi":"10.1103/PhysRevD.14.679","issn":"05562821","usgsCitation":"Anderson, R., Gustavson, D., Ritson, D., Weitsch, G., Halpern, H., Prepost, R., Tompkins, D.H., and Wiser, D., 1976, Measurements of exclusive photoproduction processes at large values of t and u from 4 to 7.5 GeV: Physical Review D, v. 14, no. 3, p. 679-697, https://doi.org/10.1103/PhysRevD.14.679.","productDescription":"19 p.","startPage":"679","endPage":"697","costCenters":[],"links":[{"id":203725,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"3","noUsgsAuthors":false,"publicationDate":"1976-08-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611291","contributors":{"authors":[{"text":"Anderson, R.L.","contributorId":45045,"corporation":false,"usgs":true,"family":"Anderson","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":346636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gustavson, D.B.","contributorId":47068,"corporation":false,"usgs":true,"family":"Gustavson","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":346637,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ritson, D.M.","contributorId":83245,"corporation":false,"usgs":true,"family":"Ritson","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":346640,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weitsch, G.A.","contributorId":34638,"corporation":false,"usgs":true,"family":"Weitsch","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":346635,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Halpern, H.J.","contributorId":53508,"corporation":false,"usgs":true,"family":"Halpern","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":346638,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Prepost, R.","contributorId":100512,"corporation":false,"usgs":true,"family":"Prepost","given":"R.","email":"","affiliations":[],"preferred":false,"id":346641,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Tompkins, Donald H.","contributorId":13231,"corporation":false,"usgs":true,"family":"Tompkins","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":346634,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Wiser, D.E.","contributorId":54331,"corporation":false,"usgs":true,"family":"Wiser","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":346639,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":70001187,"text":"70001187 - 1976 - Relative influence upon microwave emissivity of fine-scale stratigraphy, internal scattering, and dielectric properties","interactions":[],"lastModifiedDate":"2021-03-10T14:28:11.203058","indexId":"70001187","displayToPublicDate":"2010-09-28T23:09:32","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3209,"text":"Pure and Applied Geophysics PAGEOPH","active":true,"publicationSubtype":{"id":10}},"title":"Relative influence upon microwave emissivity of fine-scale stratigraphy, internal scattering, and dielectric properties","docAbstract":"The microwave emissivity of relatively low-loss media such as snow, ice, frozen ground, and lunar soil is strongly influenced by fine-scale layering and by internal scattering. Radiometric data, however, are commonly interpreted using a model of emission from a homogeneous, dielectric halfspace whose emissivity derives exclusively from dielectric properties. Conclusions based upon these simple interpretations can be erroneous. Examples are presented showing that the emission from fresh or hardpacked snow over either frozen or moist soil is governed dominantly by the size distribution of ice grains in the snowpack. Similarly, the thickness of seasonally frozen soil and the concentration of rock clasts in lunar soil noticeably affect, respectively, the emissivities of northern latitude soils in winter and of the lunar regolith. Petrophysical data accumulated in support of the geophysical interpretation of microwave data must include measurements of not only dielectric properties, but also of geometric factors such as finescale layering and size distributions of grains, inclusions, and voids.
Progress in understanding the behavior of trace elements during the processes that produce igneous rocks has been made possible by the parallel development of theoretical models to describe that behavior and analytical techniques that permit precise measurement of trace-element concentrations in igneous rocks and minerals. The result of this progress is that trace-element studies may now be used to place strong limits on both the degree of partial melting or fractional crystallization involved in the production of a given magma and the identity and quantity of the residual phases. A summary of quantitative trace-element theory and partition coefficient data for igneous rocks is presented.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Arth, J.G., 1976, Behavior of trace elements during magmatic processes - A summary of theoretical models and their applications: Journal of Research of the U.S. Geological Survey, v. 4, no. 1, p. 41-47.","productDescription":"7 p.","startPage":"41","endPage":"47","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314837,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":314836,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue1/report.pdf","text":"Report","size":"16.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56a75543e4b0b28f1184d7cc","contributors":{"authors":[{"text":"Arth, Joseph G.","contributorId":104546,"corporation":false,"usgs":true,"family":"Arth","given":"Joseph","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":589710,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011175,"text":"70011175 - 1976 - Revised Miocene and Pliocene diatom biostratigraphy of Upper Newport Bay, Newport Beach, California","interactions":[],"lastModifiedDate":"2025-05-12T16:14:14.401738","indexId":"70011175","displayToPublicDate":"2003-03-26T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2673,"text":"Marine Micropaleontology","active":true,"publicationSubtype":{"id":10}},"title":"Revised Miocene and Pliocene diatom biostratigraphy of Upper Newport Bay, Newport Beach, California","docAbstract":"North Pacific diatom zones XXIII through IX of Schrader are recognizable in the middle Miocene to lower Pliocene stratigraphic section exposed around Upper Newport Bay in Newport Beach, California. Correlation with DSDP Site 173 and other stratigraphic sections in California allows the selection of diatom datums that are the most reliable for long-distance correlation. Individual diatom datums are proposed as markers for North Pacific diatom zones XXIII through IX.
Correlations with DSDP Site 173 reveal a hiatus in the lower part of Core 15 that corresponds with a distinct lithologic and floral change in the core.
Preliminary silicoflagellate data for the Upper Newport Bay stratigraphic section supports the diatom correlations. Correlation with calcareous nannofossil, radiolarian, and silicoflagellate zones at Upper Newport Bay and at DSDP Site 173 suggests that the boundary between North Pacific diatom zones XVII and XVI approximates the middle Miocene/upper Miocene boundary. The Miocene/Pliocene boundary is estimated to be in North Pacific diatom zone X.
One new stratigraphically useful diatom species is described, Lithodesmium reynoldsii.
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