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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. Both cave systems were formed by the same ...
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.
Florida Keys, Gulf Coast of the United States: Including 45 deaths from the capsizing of a boat in the Straits of Florida and 11 deaths from a helicopter crash in the Gulf of Mexico: 60 1967 1967 Chicago blizzard: Winter storm Midwestern United States: 26 deaths in Chicago 59–67 1856 Great Train Wreck of 1856: Accident – railroad
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.
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 the surrounding region. After two and a half years of improvement effort, the cave was renamed Seneca Caverns and opened to ...
The Olentangy Indian Caverns are a series of caves, natural passages and rooms occupying three different levels. The caverns were formed millions of years ago by an underground river that cut through the limestone rock.
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 ...