Pg. 219, 229. Chardon sandstone. Thin-bedded shaly sandstone, 7 feet 8 inches to 9 feet 8 inches thick, in middle of Orangeville formation in Lake and Geauga Counties, northeastern Ohio. Underlies Brecksville shale and separated from underlying Berea sandstone by 29 feet of shale forming lower part of Orangeville formation. [This shale is now (ca. 1936) called Sunbury shale.] Latter shale interval is twice or three times as thick as shale between Berea sandstone and Aurora sandstone of Cleveland region, hence correlation with Aurora is doubtful. [Age is Mississippian.]
Named from Chardon Twp., Geauga Co., northeastern OH.
Source: US geologic names lexicon (USGS Bull. 896, p. 401).
Pg. 1363-1364; J.F. Pepper, Wallace de Witt, Jr., and D.F. Demarest, 1954, USGS Prof. Paper 259, p. 42. Chardon siltstone member of Orangeville shale. Renamed [and adopted by the USGS]. Consists of thin- to thick-bedded gray siltstones and intercalated silty shale. Thickness about 8 feet. Occurs in Orangeville about 30 feet above Berea sandstone. Lithologically similar to Aurora member; names Chardon and Aurora may have been applied to different parts of a single unit. Age is Mississippian.
Source: US geologic names lexicon (USGS Bull. 1200, p. 724).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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