Mary Campbell Cave
Encyclopedia
Mary Campbell Cave, also known as Old Maid's Kitchen, is a small secondary cliff cavity cave
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 water passing through the porous sandstone eroded the shale, leaving a ground-level cavity beneath the cliff. The cave is currently part of the Gorge Park, administered by Summit County Metroparks, and is accessible by Gorge Trail. It is located on the north wall of the gorge overlooking the Cuyahoga River
. GPS coordinates are N 41.124303° W 81.497349° WGS 84, Elevation of floor approximately 960 feet AMSL.
The cave is notable as the temporary home of Mary Campbell. A small plaque in the center of the cave gives visitors the story of her capture by native Americans. The approximately 40 meter wide cavity extends from a few to around fifteen meters into the cliff, and is tall enough to accommodate standing for much of the cavity's floor area. It affords good protection from precipitation in calm conditions, but the cavity would have had to be walled to provide protection from wind.
Cave
A cave or cavern is a natural underground space large enough for a human to enter. The term applies to natural cavities some part of which is in total darkness. The word cave also includes smaller spaces like rock shelters, sea caves, and grottos.Speleology is the science of exploration and study...
in Cuyahoga Falls, Ohio
Cuyahoga Falls, Ohio
As of the census of 2000, there were 49,374 people, 21,655 households, and 13,317 families residing in the city. The population density was 1,932.9 people per square mile . There were 22,727 housing units at an average density of 889.7 per square mile...
. The cliff and cave roof are sandstone
Sandstone
Sandstone is a sedimentary rock composed mainly of sand-sized minerals or rock grains.Most sandstone is composed of quartz and/or feldspar because these are the most common minerals in the Earth's crust. Like sand, sandstone may be any colour, but the most common colours are tan, brown, yellow,...
of the Sharon Formation, while the cave wall is shale of the Meadville formation. The cavity in the cliff was formed when water passing through the porous sandstone eroded the shale, leaving a ground-level cavity beneath the cliff. The cave is currently part of the Gorge Park, administered by Summit County Metroparks, and is accessible by Gorge Trail. It is located on the north wall of the gorge overlooking the Cuyahoga River
Cuyahoga River
The Cuyahoga River is located in Northeast Ohio in the United States. Outside of Ohio, the river is most famous for being "the river that caught fire", helping to spur the environmental movement in the late 1960s...
. GPS coordinates are N 41.124303° W 81.497349° WGS 84, Elevation of floor approximately 960 feet AMSL.
The cave is notable as the temporary home of Mary Campbell. A small plaque in the center of the cave gives visitors the story of her capture by native Americans. The approximately 40 meter wide cavity extends from a few to around fifteen meters into the cliff, and is tall enough to accommodate standing for much of the cavity's floor area. It affords good protection from precipitation in calm conditions, but the cavity would have had to be walled to provide protection from wind.