Geology Field Trip Guide: an Upper Devonian-Lower Mississippian Sequence in Central Ohio, with Emphasis on the Bedford and Berea Formations
104th Annual Meeting The Ohio Academy of Science Hosted by Otterbein College and Ross Products Division of Abbott Laboratories, Columbus Held at Otterbein College, Westerville APRIL 28,29,30,1995 GEOLOGY FIELD TRIP GUIDE: AN UPPER DEVONIAN-LOWER MISSISSIPPIAN SEQUENCE IN CENTRAL OHIO, WITH EMPHASIS ON THE BEDFORD AND BEREA FORMATIONS 8:00 AM, Sunday, April 30,1995 Arranged by: LAWRENCE A. KRISSEK and KENNETH P. COATS, The Ohio State University Transportation will be in private vehicles leaving from Roush Hall at Otterbein College at 8:00 AM to visit sites in Franklin and Delaware Counties. Lunch is on your own following the field trip. The Devonian and Lower Mississippian stratigraphic sequence exposed in central and east- central Ohio consists of the Columbus Limestone, the Delaware Limestone, the Olentangy Shale, the Ohio Shale, the Bedford Shale, the Berea Sandstone, and the Sunbury Shale. On this field trip we will examine portions of the above units at three localities: Camp Lazarus, Galena, and Rocky Fork. The Camp Lazarus locality contains exposures of the uppermost Columbus Limestone (low river level permitting), Delaware Limestone, Olentangy Shale, and lower Ohio Shale. The Galena locality contains exposures of the Ohio Shale-Bedford Shale contact and the lower Bedford Shale. The Rocky Fork locality contains exposures of the "Red Bedford", upper Bedford Shale, Berea Sandstone, and Sunbury Shale. During the Late Devonian and Early Mississippian, Ohio was located at approximately 10-15 degrees south latitude, and was covered by the shallow epeiric seas of the Appalachian Basin. The composite section we will observe on this trip represents a major transgressive-regressive sequence deposited in the western part of the basin, and is capped by the subsequent transgressive deposit of the Sunbury Shale.
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