https://ilstratwiki.web.illinois.edu/index.php?title=Inglefield_Sandstone_Member&feed=atom&action=historyInglefield Sandstone Member - Revision history2024-03-28T17:31:11ZRevision history for this page on the wikiMediaWiki 1.38.4https://ilstratwiki.web.illinois.edu/index.php?title=Inglefield_Sandstone_Member&diff=16099&oldid=prevJennifer.Obrad at 18:01, 24 January 20172017-01-24T18:01:03Z<p></p>
<p><b>New page</b></p><div>{{Editwithform}}<br />
{{Tree<br />
|category1=Paleozoic Erathem<br />
|category2=Pennsylvanian Subsystem<br />
|category3=Absaroka Sequence<br />
|category4=McLeansboro Group<br />
|category5=Missourian Series<br />
|category6=Modesto Formation<br />
|category7=Sandstone<br />
|tree1=McLeansboro Group<br />
|tree2=Modesto Formation<br />
|tree3=Inglefield Sandstone Member<br />
|tree21=Paleozoic Erathem<br />
|tree22=Pennsylvanian Subsystem<br />
|tree23=Missourian Series<br />
|tree31=Absaroka Sequence<br />
}}<br />
==Primary source==<br />
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.<br />
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==Contributing author&#40;s&#41;==<br />
M. E. Hopkins and J. A. Simon<br />
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==Name==<br />
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===Original description===<br />
The Inglefield Sandstone Member of the Modesto Formation (Fuller and Ashley, 1902, p. 3).<br />
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===Derivation===<br />
Named for Inglefield, Vanderburgh County, Indiana.<br />
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===Other names===<br />
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===History&#47;background===<br />
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==Type section==<br />
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===Type location===<br />
The type locality consists of exposures in a railroad cut south of the town of Inglefield.<br />
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===Type author&#40;s&#41;===<br />
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===Type status===<br />
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==Reference section==<br />
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===Reference location===<br />
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===Reference status===<br />
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==Stratigraphic relationships==<br />
The sandstone occurs above the Chapel (No. 8) Coal and below the Womac Coal (Andresen, 1961).<br />
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==Extent and thickness==<br />
It is known primarily in eastern Illinois, but it was reported by Andresen to split into two distinct sandstones in southwestern Illinois, the lower unit occurring below the Carlinville Limestone. The Inglefield Sandstone locally exceeds 80 feet in channels oriented south-southwest, but it is relatively widespread as a much thinner sheet sandstone in most of the Illinois Basin.<br />
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==Lithology==<br />
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==Core&#40;s&#41;==<br />
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==Photograph&#40;s&#41;==<br />
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==Contacts==<br />
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==Well log characteristics==<br />
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==Fossils==<br />
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==Age and correlation==<br />
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==Environments of deposition==<br />
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==Economic importance==<br />
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==Remarks==<br />
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==References==<br />
ANDRESEN, M. J., 1961 , Geology and petrology of the Trivoli Sandstone in the Illinois Basin: Illinois State Geological Survey Circular 316, 31 p.<br><br />
FULLER, M. L., and G. H. ASHLEY, 1902, Ditney Quadrangle: USGS Geologic Atlas Folio 84, 8 p.<br />
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{{Codes<br />
|membercode=2210<br />
|geo_unit=--<br />
}}</div>Jennifer.Obrad