Dayton Formation

Last updated
Dayton Formation
Stratigraphic range: Silurian
Type Formation
Underlies Osgood Shale and Rochester Shale
Overlies Brassfield Formation and Cataract Group
Location
Country United States
Extent Ohio

The Dayton Formation is a geologic formation in Ohio. It dates back to the Silurian.

Ohio State of the United States of America

Ohio is a Midwestern state in the Great Lakes region of the United States. Of the fifty states, it is the 34th largest by area, the seventh most populous, and the tenth most densely populated. The state's capital and largest city is Columbus.

The Silurian is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at 443.8 million years ago (Mya), to the beginning of the Devonian Period, 419.2 Mya. The Silurian is the shortest period of the Paleozoic Era. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by several million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera were wiped out.

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