Geology of the eastern part of the Lynn Mountain syncline, Le Flore County, Oklahoma.
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Geology of the eastern part of the Lynn Mountain syncline, Le Flore County, Oklahoma.

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Published by University of Oklahoma in Norman .
Written in English

Subjects:

Places:

  • Oklahoma,
  • Le Flore Co.

Subjects:

  • Geology -- Oklahoma -- Le Flore Co.

Book details:

Edition Notes

Bibliography: p. 26-28.

SeriesOklahome Geological Survey, Circular 75, Circular (Oklahoma Geological Survey) ;, 75.
Classifications
LC ClassificationsQE153 .A3 no. 75, QE154 .A3 no. 75
The Physical Object
Paginationiv, 34 p.
Number of Pages34
ID Numbers
Open LibraryOL5027996M
LC Control Number73622840

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Details about Geology of the Eastern Part of the Lynn Mountain Syncline, Le Flore County, Okla. Geology of the Eastern Part of the Lynn Mountain Syncline, Le Flore County, Okla A book that does not look new and has been read but is in excellent condition. University of Oklahoma: Title: Geology of the Eastern Part of the Lynn Mountain S Seller Rating: % positive. the Cherokee Group (Middle Pennsylvanian), eastern Kansas and northeastern Oklahoma: Kansas Geological Survey, Geologic Series 3, 70 p. Briggs, G., , Geology of the eastern part of the Lynn Mountain syncline, Le Flore County, Oklahoma: OGS Circu 34 p. Briggs, G., , Carboniferous depositional environments in the Ouachita Mountains–File Size: KB. Le Flore County is a county located along the eastern border of the U.S. state of of the census, the population Its county seat is Poteau. The county name honors a Choctaw family named ssional district: 2nd. the Cherokee Group (Middle Pennsylvanian), eastern Kansas and northeastern Oklahoma: Kansas Geological Survey, Geologic Series 3, 70 p. Briggs, G., , Geology of the eastern part of the Lynn Mountain syncline, Le Flore County, Oklahoma: OGS Circu 34 p. Briggs, G., , Carboniferous depositional environments in the Ouachita Mountains–.

Geology of the Eastern Part of the Lynn Mountain Syncline, Le Flore County, Okla. $ Details about The Proud Heritage Of Le Flore County Oklahoma by Henry Peck, Book measures /4 inches by /4 inches pages plus 31 page memorial Rating: % positive. Briggs, Garrett, , Geology of the eastern part of the Lynn Mountain Syncline, Le Flore County, Oklahoma: Oklahoma Geological Survey Circu 31 p. Buell, G.R., , The hydrologic benchmark program-A standard to evaluate time-series trends in selected water-quality constituents for streams in Georgia: U.S. Geological Survey Water. Le Flore County, Oklahoma is home to 97 summits, ridges, ranges, trails and other mountain features. Click on the pins on the map to see the name and a link to more information about that place. Above you’ll also see links to pages with maps of all the different features in Le Flore County. Geology of the eastern part of Winding Stair Range, Le Flore County, Oklahoma, by O. D. Hart. Decem 87 pages, 15 figures, 1 plate (geologic map). Bulletin Permian salt and associated evaporites in the Anadarko basin of the western Oklahoma-Texas Panhandle region, by Louise Jordan and David L. Vosburg.

Geology of the western part of Winding Stair Range, Latimer and Le Flore Counties, Oklahoma. [Larry Dean Fellows] on *FREE* shipping on qualifying : Larry Dean Fellows. Pages in category "Geography of Le Flore County, Oklahoma" The following 4 pages are in this category, out of 4 total. This list may not reflect recent changes (). GENERAL RECONNAISSANCE WORK. The earliest report on the geology of the region is by James Blake. 1 In the early seventies he examined Pueblo Mountain, which lies directly to the south of Steens and is, in part, defined on both sides by continuations of the same faults. Here are exposed both the southern continuation of the Steens Mountain volcanic series and the underlying crystalline rocks on. Bed rock in the Rock Island area of northeastern Le Flore County in southeastern Oklahoma consists of shale, siltstone, and sandstone of the McAlester, Hartshorne, and Atoka Formations of Pennsylvanian age. The area is on the south flank of the Backbone anticline; the rocks dip to the south at 5oo. Alluvium along James Fork consists of sandy and clayey silt and may be as much as 30 feet thick.