2 edition of Structural geology of the Cat Creek anticline and related features, Central Montana found in the catalog.
Structural geology of the Cat Creek anticline and related features, Central Montana
W. John Nelson
Includes bibliographical references (p. 39-44).
|Statement||by W. John Nelson.|
|Series||Memoir ;, 64, Memoir (Montana Bureau of Mines and Geology) ;, 64.|
|LC Classifications||TN24.M9 N45 1993|
|The Physical Object|
|Pagination||viii, 44 p. :|
|Number of Pages||44|
|LC Control Number||94620928|
Cat Creek (also Frantz or Frantzville) is an unincorporated community in eastern Petroleum County, Montana, United States.. The Cat Creek community (also known as the Shay community) is located in Cat Creek Basin, in a "fertile valley land", 6 miles ( km) miles long and 4 miles ( km) wide, consisting of 16, acres. An area of about 35 square miles, situated about 30 miles southeast of Helena, Montana, was mapped during the summer of at a scale of l, The area includes a part of the eastern foothills of the Elkhorn Mountains, and is underlain by sedimentary mad volcanic rocks of Cretaceous age that were intruded during late Cretaceous or early Tertiary time by several types of igneous rocks.
Montana Geology and Geography Terms. Vocabulary and other knowledge related to geology and geography of Montana. STUDY. PLAY. geology. The scientific study of the origin, history, and structure of the earth. the Continental plates moving and mountains forming. Seas and swamps covered Montana. Paleozoic. Geologic period of time that fish. This report has had preliminary reviews for conformity with Montana Bureau of Mines and Geology’s technical and editorial standards Partial support has been provided by the STATEMAP component of the National Cooperative Geologic Mapping Program of the U.S. Geological Survey under Contract Number HQ-AG *Geology Department, University File Size: KB.
Prosser and Beede () named the Burns dome, Diamond Creek anticline, Elmdale anticline, and Cottonwood province, which now are recognized as parts of the larger structural unit. Condra and Bengston (, pp. 25, 39) used the term "Table Rock anticline" for the part of the structure in the vicinity of the Kansas-Nebraska line. The Online Books Page. Online Books by. Montana Bureau of Mines and Geology. Books from the extended shelves: Montana Bureau of Mines and Geology: Biennial report of the Montana Bureau of Mines and Geology: a department of the Montana School of Mines to the legislative assembly for the reporting period July 1, to J (Butte, Mont.: Montana School of Mines, ) (page .
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Get this from a library. Structural geology of the Cat Creek anticline and related features, Central Montana. [W John Nelson]. Nelson, W. John () Structural geology of the Cat Creek anticline and related features, central Montana: Montana Bureau of Mines and Geology Mem 44 p.
Google Scholar Nilson, Tor H. and John R. Stewart () The Antler orogeny–mid-Paleozoic tectonism in Cited by: 5. GEOLOGY AND PETROLEUM POTENTIAL CENTRAL MONTANA PROVINCE by Edwin K. Maughan] U.S. Geological Survey Open-File Report OF N This report is preliminary and has not been edited nor reviewed for conformity with U.S.
Geological Survey standards and nomenclature. 1U.S. Geological Survey, Denver, Colorado Cited by: 1. 2 Stratigraphic Framework of Lower and Upper Cretaceous Rocks in Central and Eastern Montana of low-amplitude anticlines, synclines, and domes exist along the northern border.
The central part of the study area is complexly deformed, and the group of anticlines, synclines, and domes thereCited by: 8. The Cat Creek Anticline, scene of Montana's first major oil discovery, is a Laramide foreland structure.
The anticline is a fault-propagation fold that overlies a south-dipping, slightly listric high-angle fault in crystalline basement. The Cat Creek fault has undergone several reversals of. The Cat Creek anticline, scene of central Montana's first significant oil discovery, is underlain by a south-dipping high-angle fault (Cat Creek fault) that has undergone several episodes of movement with opposite sense of displacement.
Borehole data suggest that the Cat Creek fault originated as Structural geology of the Cat Creek anticline and related features. Cat Creek (also Frantz or Frantzville) is an unincorporated community in eastern Petroleum County, Montana, United States.
The Cat Creek community (also known as the Shay community) is located in Cat Creek Basin, in a "fertile valley land", 6 miles ( km) long and 4 miles ( km) wide, consisting of 16, acres. It lies along local roads east of the town of Winnett, the county seat of County: Petroleum.
Montana College of Mineral Science and Technology Publisher - 43 works / 4 ebooks. Cenozoic tectonic evolution of southwest Montana and east-central Idah Not In Library.
Structural geology of the Cat Creek Anticline and related features, ce Not In Library. The geology of Montana includes thick sequences of Paleozoic, Mesozoic and Cenozoic sedimentary rocks overlying ancient Archean and Proterozoic crystalline basement rock.
Eastern Montana has considerable oil and gas resources, while the uplifted Rocky Mountains in the west, which resulted from the Laramide orogeny and other tectonic events have locations with metal ore.
Structural geology of the Cat Creek anticline and related features, central Montana  Nelson, W. John. Butte, Mont.: Montana Bureau of Mines and Geology, Montana College of Mineral Science and Technology, Economic geology of eastern Montana and adjacent areas.
[Billings, Montana Geological Society, ?] (OCoLC) Material Type: Conference publication: Document Type: Book: All Authors / Contributors: Montana Geological Society. OCLC Number: Notes: Papers presented at the 20th annual conference, Montana Geological Society. #F GEOLOGY AND PHOSPHATE DEPOSITS OF THE PERMIAN ROCKS IN CENTRAL WESTERN MONTANA By Swanson, R.
4to, wrps with label else light wear, very good, 58 pp., 5 pls, 34 figs. Good reference on Park City and Phosphoria and related units. Price: $ (stock#PPF). Geology and mineral deposits of Lincoln and Flathead counties, Montana, (Montana.
Bureau of Mines and Geology. Bulletin 79) [Johns, Willis M] on *FREE* shipping on qualifying offers. Geology and mineral deposits of Lincoln and Flathead counties, Montana, (Montana. Bureau of Mines and Geology. Bulletin 79)3/5(1). STRUCTURAL GEOLOGY. Cincinnati Arch.—The Cincinnati arch is one of several structural highs which determine the distribution of outcrop in the central interior of the United axis passes through central Tennessee and Kentucky in a north by east direction and splits in northern Kentucky with one limb passing on each side of the Michigan Basin.
This book is a good overview of Montana's geologic story, but the maps are lacking detail and it lacks a milepost listing of features. It is suitable for reading in preparation for a trip, but without milepost listings, it is not a good field by: A GIS database of geologic units and structural features in Montana, with lithology, age, data structure, and format written and arranged just like the other states.
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The geology theme is a constantly evolving data set. It is not a theme that is static. Although the rocks themselves might not change, what geologists think of them will definitely change.
Melrose, Montana (Fig. 2), where south-to-north thermal and strain gradients can be studied. SETTING The McCarthy Mountain salient is an east-projecting 1 Geology Department, University of Montana, Missoula MT 2 6th Avenue North, Great Falls, MT 3 Wallingford Avenue North, Seattle, WA File Size: 3MB.
The geologic setting of the Crow Reservation includes the west flank of the Powder River basin, a northwest-trending synclinal feature at least miles long and as much as miles wide in eastern Wyoming and southeastern Montana; the south flank of the Bull Creek syncline, a large east-trending fold in central Montana; and the northern parts of the Bighorn and Pryor uplifts which extend.
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View. The Top 10 Geological Field Trip Locations in Montana and Yellowstone The MSU web development team has put their heads together to name the top ten geology field trips in Montana and Yellowstone, based on superb geology, scenery, access, and educational value.
For each location, we list our favorite road logs or field guides. They are listed below in no particular order.Geology of the Cripple Creek gold-telluride deposit, Colorado: Descriptions and locations of field trip stops Eric P. Jensen Bronco Creek Exploration, Inc., E. Winsett, Tucson, ArizonaUSA ([email protected]) All coordinates in UTM projection, NAD27 datum for the conterminous US.