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  2. Byrd Polar and Climate Research Center - Wikipedia

    en.wikipedia.org/wiki/Byrd_Polar_and_Climate...

    BPRC is the oldest research center at Ohio State University. [2] The name was changed to the Byrd Polar Research Center in 1987 after the polar explorer and aviator Richard E. Byrd when Ohio State purchased the Byrd papers from the Byrd family in 1985. [3] BPRC conducts interdisciplinary research at the nexus of Earth Sciences and Engineering.

  3. Geology of Ohio - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Ohio

    Ohio's State Invertebrate Fossil, is a trilobite found in the formation. The Southern Hemisphere where Ohio was located at the end of the Ordovician experienced a widespread glaciation, around 438 million years ago. Sea level dropped due to the glaciation, accompanied by a subsidence of the land.

  4. Early Lake Erie - Wikipedia

    en.wikipedia.org/wiki/Early_Lake_Erie

    St. John's (Newfoundland): Geological Association of Canada Special Paper 30. Herdendorf CE. 1990b. Great Lakes estuaries. Estuaries 13:493-503. Herdendorf CE, Braidech LL. 1972. Physical characteristics of the reef area of western Lake Erie. *Ohio Department of Natural Resources, Division of Geological Survey Report of Investigation 82. 90 *pp.

  5. Lake Monongahela - Wikipedia

    en.wikipedia.org/wiki/Lake_Monongahela

    Lake Monongahela was a proglacial lake in western Pennsylvania, West Virginia, and Ohio.It formed during the Pre-Illinoian ice epoch when the retreat of the ice sheet northwards blocked the drainage of these valleys to the north.

  6. Teays River - Wikipedia

    en.wikipedia.org/wiki/Teays_River

    The Teays River was a north- and northwest-flowing river existing before the Pleistocene Ice Ages – before 2.5 million years ago. [10] The Teays flowed through southwest West Virginia, between Kentucky and Ohio, and northwest across Ohio (see illustration). [11]

  7. Calamus Swamp - Wikipedia

    en.wikipedia.org/wiki/Calamus_Swamp

    Calamus Swamp is a 19-acre (0.077 km 2) public preserve located 1.5 miles (2.4 km) from Circleville in Pickaway County, Ohio, United States. It has a natural kettle lake/wetland and is owned by the Columbus Audubon, the local chapter of Audubon .

  8. Glacial till plains (Ohio) - Wikipedia

    en.wikipedia.org/wiki/Glacial_till_plains_(Ohio)

    The Glacial till plains are a till plain landform in Northern Ohio, located near the shore of Lake Erie and produced by the retreat of the Wisconsin glaciation.Since glacial till is highly fertile soil, agriculture on the glacial till plains is very productive.

  9. Paleontology in Ohio - Wikipedia

    en.wikipedia.org/wiki/Paleontology_in_Ohio

    The location of the state of Ohio. ... About two thirds of Ohio was covered by such glaciers. ... Division of Geological Survey. May 2005.