Lowell Coal Member
Willman, H. B., Elwood Atherton, T. C. Buschbach, Charles Collinson, John C. Frye, M. E. Hopkins, Jerry A. Lineback, and Jack A. Simon, 1975, Handbook of Illinois Stratigraphy: Illinois State Geological Survey Bulletin 95, 261 p.
M. E. Hopkins and J. A. Simon
The Lowell Coal Member of the Carbondale Formation (Willman and Payne, 1942, p. 102-105).
Named for Lowell, La Salle County.
The type section of the Lowell Coal is an exposure on the Vermilion River (SE SW 8, 32N-2E).
Extent and thickness
The Lowell Coal is present in northern Illinois and in the southern part of western Illinois. The coal is 10 inches thick in the type section.
It is a bright-banded, rather shaly coal underlain by a silty to sandy underclay and overlain by several feet of gray shale that contains two limestone beds, which are equivalent to upper units of the Oak Grove Limestone. The underclay overlies a siltstone containing plant root impressions, which in turn is underlain by gray shale containing additional limestone units equivalent to the Oak Grove Limestone.
Well log characteristics
Age and correlation
It is equivalent to the Shawneetown Coal in southwestern, southern, and eastern Illinois.
Environments of deposition
WILLMAN, H. B., and J. N. PAYNE, 1942, Geology and mineral resources of the Marseilles, Ottawa, and Streator Quadrangles: Illinois State Geological Survey Bulletin 66, 388 p.
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