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The Hopeton Earthworks are an Ohio Hopewell culture archaeological site consisting of mounds and earthwork enclosures.It is located on the eastern bank of the Scioto River just north of Chillicothe in Ross County, Ohio, about 1 mile (1.6 km) east of the Mound City Group and Shriver Circle on a terrace of the Scioto River.
The Burning Tree Mastodon was approximately 30 years old at the time of its death and is 90-95% complete, missing only the right rear leg, a few tail bones, two ribs, and all the toe bones. The lower spine and right rib cage have healed injuries which have been interpreted as the result of battles with other mastodons.
This page was last edited on 24 December 2023, at 09:00 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.
This list of fossil sites is a worldwide list of localities known well for the presence of fossils.Some entries in this list are notable for a single, unique find, while others are notable for the large number of fossils found there.
In archaeology, excavation is the exposure, processing and recording of archaeological remains. [1] An excavation site or "dig" is the area being studied. These locations range from one to several areas at a time during a project and can be conducted over a few weeks to several years.
Ohio State football enters Week 9 looking for a bounce back from a loss at Oregon.. The Buckeyes are 25 ½-point favorites against Nebraska this week, with the over/under hovering around 48.5 ...
Evidence of Early Paleoindian Bone Modification and Use at the Sheriden Cave Site (33WY252), Wyandot County, Ohio. American Antiquity 70(3):503-526. Redmond, B.G. 2005. Sheriden Cave, Wyandot County: Opening a Time Capsule. In Ohio Archaeology: An Illustrated Chronicle of Ohio's Ancient American Indian Cultures, by Bradley T. Lepper, pp. 48–49.
Southeastern Ohio was a swamp-covered coastal plain. [4] Ferns and horsetails were among the state's rich flora. [3] Ohio was only about 5 degrees north of the equator. Sand and mud deposited on local river deltas gradually filled in the swamp. Later in the Permian Ohio was subjected to geologic uplift and its sediments were eroded away ...
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