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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.
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.
Bat Cave; Carter Caves State Park; Cascade Caverns; Colossal Cavern; Diamond Caverns; Eleven Jones Cave; Fisher Ridge Cave System; Glover's Cave; Goochland Cave; Great Onyx Cave; Great Saltpetre Cave; Horse Cave also known as "Hidden River Cave" Lost River Cave; Mammoth Cave; Martin Ridge Cave System; Oligo-Nunk Cave System
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.
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.
The core area also includes two privately owned preserves, Crane Hollow and Camp Oty-Okwa (owned by Big Brothers and Big Sisters of Central Ohio). The geological series that forms the Hocking Hills extends south and west, gradually diminishing but still forming impressive bluffs and gorges in:
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 caverns were formed millions of years ago by dissolution of limestone from an underground river. The caverns are believed to have been used by the Wyandotte Indians. The Caverns were rediscovered in 1821 by J.M. Adams, a nearby camper, who was a member of a wagon train. He carved his initials in the entrance, where they can still be seen ...