Cuyahoga Valley National Park - Virginia Kendall Area Cliffs and Ledges

The Virginia Kendall Area in Cuyahoga Valley National Park is known for its distinctive geological features, most notably the towering ledges formed by the Sharon Conglomerate Member of the Pottsville Formation. This sandstone formation dates back approximately 325 million years to the early Pennsylvanian period.
The Ledges Trail, one of the park's most popular hikes, winds along the base of these impressive ledges, offering stunning views of the surrounding valley and river. The trail also traverses several unique geological features, including:
Ice Box Cave: A natural rock shelter that provides a cool, damp environment for bats during the winter months.
Brandywine Falls: A 65-foot waterfall that plunges over the edge of the ledges, creating a scenic cascade.
In addition to the Sharon Conglomerate, the Virginia Kendall Area also features other geological formations, such as:
Ohio Shale: A thick layer of black shale that underlies the Sharon Conglomerate and contains rich fossil deposits.
Glacial Till: Deposits of rock and debris left behind by past glaciers, which can be found throughout the area.
The diverse geology of the Virginia Kendall Area has created a unique ecosystem that supports a variety of plant and animal species. The area is also home to several springs and seeps, which provide a vital water source for the local wildlife.
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