Cason Shale

Last updated
Cason Shale
Stratigraphic range: Ordovician-Silurian
Type Formation
Unit ofnone
Underlies Brassfield Limestone
Overlies Fernvale Limestone
Thicknessup to appx. 23 feet [1]
Lithology
Primary Shale
Location
Region Arkansas
Country United States
Type section
Named forCason tract and mine, near Batesville, Independence County, Arkansas
Named by Henry Shaler Williams [2]

The Cason Shale is a Late Ordovician to Middle Silurian geologic formation in the Ozark Plateaus of Arkansas. [1] The name was introduced in 1894 by Henry Shaler Williams in his study of Arkansas. [2] Williams designated a type locality at what was known as the Cason tract and mine, near Batesville, Independence County, Arkansas, however, he did not assign a stratotype. As of 2017, a reference section has not been designated for this unit.

Contents

Paleofauna

Conodonts

See also

References

  1. 1 2 McFarland, John David (2004) [1998]. "Stratigraphic summary of Arkansas" (PDF). Arkansas Geological Commission Information Circular. 36: 7. Archived from the original (PDF) on 2016-12-21. Retrieved 2018-01-11.
  2. 1 2 Williams, Henry S. (1894). "On the age of the manganese beds of the Batesville region of Arkansas". The American Journal of Science. 3rd Series. 48: 325–331.
  3. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 Craig, William (1968). The stratigraphy and conodont paleontology of Ordovician and Silurian strata, Batesville district, Independence and Izard counties, Arkansas (PhD). The University of Texas.