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Ohio Caverns is a show cave located 30 miles (48 km) from Dayton, Ohio near West Liberty, in Salem Township, Champaign County, Ohio in the United States.A popular tourist destination and member of the National Caving Association, it is the largest of all the cave systems in Ohio and contains many crystal formations.
Entrance to Blue Hole. The Blue Hole is a fresh water pond and cenote located in Castalia, Erie County, Ohio, in the United States.From the 1920s to 1990 the Blue Hole was a tourist site, attracting 165,000 visitors annually at the height of its popularity, partly because of its location on State Route 269, about 7 miles (11 km) southwest of the Cedar Point amusement park in Sandusky, Ohio.
The Zane Shawnee Caverns is a cave system in Jefferson Township, Logan County, Ohio, United States. The caverns are show caves owned by the nonprofit United Remnant Band of the Shawnee Nation as of 1995. [1] These caverns are located between Zanesfield and Bellefontaine, Ohio, near the Ohio Caverns.
Sheriden Cave is a Paleo-Indian archaeological site from the late Ice age in Wyandot County, Ohio. [1] Glacial deposits sealed off the cave more than 10,000 years ago. Sheriden Cave is a karst sinkhole on a dolomite ridge that crosses Hancock and Wyandot Counties. It is associated with the Indian Trail Caverns that opened in 1927.
Hocking Hills State Park is a state park in the Hocking Hills region of Hocking County, Ohio, United States.In some areas the park adjoins the Hocking State Forest.Within the park are over 25 miles (40 km) of hiking trails, rock formations, waterfalls, and recess caves.
Pages in category "Caves of Ohio" The following 6 pages are in this category, out of 6 total. This list may not reflect recent changes. C. Crystal Cave (Ohio) M.
Mary Campbell Cave. Note the woman at the far end of the cave, for scale. Mary Campbell Cave, also known as Old Maid's Kitchen, is a small secondary rock shelter in Cuyahoga Falls, Ohio. The cliff and cave roof are sandstone of the Sharon Formation, while the cave wall is shale of the Meadville formation. The cavity in the cliff was formed when ...
The cave became known as Good's Cave, named for Emmanuel Good, the owner of the farm on which the cave was located. [ 1 ] In 1931, Don Bell, a lawyer from Bellevue , discovered a series of passageways and rooms in the cave which led to an underground river, called Ole' Mist'ry River, which is part of the vast groundwater system that underlies ...