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Tuesday, May 12, 2020 | History

2 edition of Geothermal gradients in the Missoula and Bitterroot Valleys, west-central Montana found in the catalog.

Geothermal gradients in the Missoula and Bitterroot Valleys, west-central Montana

Robert B. Leonard

Geothermal gradients in the Missoula and Bitterroot Valleys, west-central Montana

by Robert B. Leonard

  • 213 Want to read
  • 16 Currently reading

Published by U.S. Geological Survey in [Reston, Va.?] .
Written in English

    Subjects:
  • Earth temperature -- Montana -- Bitterroot River Valley.,
  • Earth temperature -- Montana -- Missoula.,
  • Geothermal resources -- Montana.

  • Edition Notes

    Statementby Robert B. Leonard and Wayne A. Wood ; prepared in cooperation with the Montana Bureau of Mines and Geology.
    SeriesWater-resources investigations -- 80-89.
    ContributionsWood, Wayne A., Montana Bureau of Mines and Geology., Geological Survey (U.S.).
    The Physical Object
    Paginationiv, 15 p. :
    Number of Pages15
    ID Numbers
    Open LibraryOL17651883M

    ASPECTS OF LOW TEMPERATURE - University of Utah. Free essys, homework help, flashcards, research papers, book report, term papers, history, science, politics. Studylib. Documents Flashcards Grammar checker Login Upload document SMU References for the Geothermal Data base.

    The first edition of this book, Manual of Applied Field Hydrogeology, resulted from an enquiry by Bob Esposito of the McGraw-Hill Professional Book Group about Montana Tech of the University of Montana’s long running hydrogeology field camp, which was . Issuu is a digital publishing platform that makes it simple to publish magazines, catalogs, newspapers, books, and more online. Easily share your publications and get them in front of Issuu’s.

    tag:, tag:,p00ec4c4d Lily Marlene - Marlene Affeld This document should be cited as: Jones, W. M. Ecologically significant wetlands in the upper Yellowstone River watershed, including the Boulder, Clarks Fork Yellowstone, Shields, and Stillwater River drainages. Report to the Montana Department of Environmental Quality. Montana Natural Heritage Program, Helena, MT. 37pp. plus appendices.


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Geothermal gradients in the Missoula and Bitterroot Valleys, west-central Montana by Robert B. Leonard Download PDF EPUB FB2

Get this from a library. Geothermal gradients in the Missoula and Bitterroot Valleys, west-central Montana. [Robert B Leonard; Wayne A Wood; Montana Bureau of.

Temperature-depth profiles of six cased test holes in the Missoula and Bitterroot Valleys, west-central Montana, consist of linear segments, the intersections of which commonly correspond with lithologic boundaries. Geothermal gradients commonly decreased with depth, probably as a result of compaction and higher quartz content of the deeper sedimentary deposits.

Duringseven test holes were drilled by Bendix Field Engineering Service under contract to the U.S. Department of Energy for the purpose of assessing the uranium content of lower Tertiary sedimentary rock in the Missoula and Bitterroot valleys of west-central Montana. Six of the holes were. Buy Geothermal gradients in the Missoula and Bitterroot Valleys, west-central Montana (Water-resources investigations) by Robert B Leonard (ISBN:) from Amazon's Book Store.

Everyday low prices and free delivery on eligible : Robert B Leonard. Geothermal gradients in the Missoula and Bitterroot Valleys, west-central Montana / by Robert B. Leonard and Wayne A. Wood ; prepared in cooperation with. Hydrogeologic data were collected principally during to in eight hot-spring areas, in the Marysville geothermal test well, in the Butte mine and in the Bitterroot and Missoula River valleys to provide a basis for evaluating the geothermal potential of the areas.

Measurements are tabulated. Montana Bureau of Mines and Geology: Geothermal gradients in the Missoula and Bitterroot Valleys, west-central Montana / ([Reston, Va.?]: U.S.

Geological Survey, ), also by Robert B. Leonard, Wayne A. Wood, and Geological Survey (U.S.) (page images at HathiTrust). Effects of potential geothermal development in the Corwin Springs Known Geothermal Resources Area, Montana, on the thermal features of Yellowstone National Park / (Menlo Park, Calif.: U.S.

Geological Survey ; Denver, Colo.: Books and Open-File Reports Section [distributor], ), by M. Sorey and Geological Survey (U.S.) (page images at. In northwestern and west-central Montana, this ecosystem forms in openings in Douglas-fir (Pseudotsuga menziesii) and ponderosa pine (Pinus ponderosa) forests, and in intermountain and mountain valleys and big sagebrush (Artemisia tridentata) shrublands.

East of the Continental Divide, this system is found along valley bottoms and steep canyon. We use cookies to offer you a better experience, personalize content, tailor advertising, provide social media features, and better understand the use of our services.

Missoula, MT Bitterroot snowpack close to average, but could increase People can check the West Central Montana Avalanche Center website at for additional information. Upper Missoula Group: McNamara, Bonner, and Mount Shields Formations; locally includes lower Libby Formation in northwestern Montana (Middle Proterozoic) at surface, covers 26 % of this area.

McNamara Formation: Dense green and red siltite and argillite in mudcracked couplets containing diagnostic chert beds and rip-up clasts. NorthWestern Energy is still working to restore power to more than 8, customers in the Missoula and Bitterroot valleys who lost service after Monday night's severe thunderstorm.

West Central Montana (crystalline rocks) Depth: 2,m oC Marysville Water quality: TDS= mg/L Flow: ’s Lpm 0 25 50 75 Temperature, °C 0 D e p t h, m e t e r s Background Gradient Marysville MGE #1 well. Missoula Map: Google map of Missoula, Montana, USA.

access_time World Time Now - visit page. Earthquake activity: Helena Valley West Central-area historical earthquake activity is slightly above Montana state average. It is 62% greater than the overall U.S. average.

On 8/18/ ata magnitude ( UK, Class: Major, Intensity: VIII - XII) earthquake occurred miles away from Helena Valley West Central center, causing $26, total damage On 10/28/ at The geology of the north-central part of the Missoula quadrangle, Missoula County, Montana was studied and a report The Missoula quadrangle lies in the extreme west- central part of Montana, between latitude 46® 30’ and 47® 00’ ward to the Clark Fork and the Bitterroot River valleys* Cliffs are somewhat prominent about half-way up Author: William A.

Long. Low-temperature thermochronological record of exhumation of the Bitterroot metamorphic core complex, northern Cordilleran Orogen Article in Tectonophysics (1) May with 22 Reads. Full text of "Montana's comprehensive fish and wildlife conservation strategy" See other formats.

Proceedings of the International Conferences on Basement Tectonics VOLUME 2 The titles published in this series are listed at the end a/this volume.

BASEMENT TECTONICS 8 Characterization and Comparison of Ancient and Mesozoic Continental Margins Proceedings of the Eighth International Conference on Basement Tectonics. This banner text can have markup. web; books; video; audio; software; images; Toggle navigation.Ausserdeutsche regionale Geologie - Zentralantiquariat Leipzig GmbH: Dr.

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