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
|Statement||by Robert B. Leonard and Wayne A. Wood ; prepared in cooperation with the Montana Bureau of Mines and Geology.|
|Series||Water-resources investigations -- 80-89.|
|Contributions||Wood, Wayne A., Montana Bureau of Mines and Geology., Geological Survey (U.S.).|
|The Physical Object|
|Pagination||iv, 15 p. :|
|Number of Pages||15|
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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.
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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