|Email Page||Printer Friendly Version||Submit a Report|
Much of the bedrock in the Wildcat valley has been eroded by pre-glacial drainage, and the valley has been covered by glacial drift as a result of glaciation. Several large glacial kames (mounds) are visible from the South Fork of Wildcat Creek. The North Fork of Wildcat cuts through bedrock in a few areas, creating scenic overlooks up to 130 feet above the stream.
Classic Freestanding Rack
Kayak & Canoe Covers