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A Tight Squeeze at Cantwell Cliffs EarthCache

Hidden : 5/15/2007
Difficulty:
1.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

At Cantwell Cliffs, a part of Hocking Hills State Park, you can get up close and personal with a slump block formation.

Please stay on the trail at all times when visiting Hocking Hills State Park! There are many areas off-trail that could be dangerous. Cantwell Cliffs has many sharp drop-offs. Also, the fragile ecosystem is home to rare species, and these habitats are protected by diligent park rangers. For your safety, and for the good of the environment, stay on the trail. Terrain rating was suggested by rating system at clayjar.com.

To get to Cantwell Cliffs, take US-33 to OH-374 south, near the town of Rockbridge. OH-374 will twist and wind through the hills for about 5 miles before you see the park sign. Take a look at the trail map before you leave, and find “Fat Woman’s Squeeze”. From the parking area, the walk to the listed coordinates is short but steep. GPS receivers tend to get poor readings around cliffs like this but having seen a trail map, you should have no trouble finding the Squeeze. Don’t forget to bring a tape measure. You will need it to claim your find.

Fat Woman’s Squeeze is an example of a geologic feature called a slump. A slump is the result of the force of gravity working along a sloped land surface. In this formation, a vertical crack or joint forms in the rock cliff. The crack eventually widens enough to allow a large piece of rock, called a slump block, to separate and slip down the slope. Fat Woman’s Squeeze is a narrow space between a slump block and the cliff from which it separated.

In geologic history, the stones of Cantwell Cliffs date back to the Mississippian period. Called the Cuyahoga Formation, the rocks formed around 355-350 million years ago. The Black Hand sandstone that makes up much of the park is susceptible to erosion, so Buck Run, the local stream, has carved out the cliffs and valley you will see beyond the Squeeze. While glaciers that shaped much of the rest of the state never covered the Hocking Hills State Park area, they did influence the climate and vegetation of the gorge. As you look down, you will see plant life which is generally found much farther north. Although your logging requirements can be fulfilled in a quick visit to the Squeeze, there is much more to be seen at Cantwell Cliffs, so don’t stop here! Follow the trails and see more

LOGGING REQUIREMENTS: According to Earthcache rules, in order to claim the find, you must perform an educational task. So, we ask that you measure the tightest part of the Squeeze. That is, find the narrowest step going down the stairs through the squeeze, and measure horizontally from cliff to slump block. We measured two narrow stairs at the bottom of the Squeeze (i.e. not up by the monster tree roots), and found them to be about equal width. Email us with your results. Also, please take a photo of yourself and your GPS squeezing through.

Logs not accompanied by email and photo within a reasonable amount of time will be deleted per Earthcache rules. Please don’t make us have to do that!

If you're a fan of Black Hand Sandstone formations, why not check out another one at Rockbridge? It's not far away, on the other side of US-33, and you already have the required tape measure on hand!

References:

Ohio DNR website
Camp, Mark J. 2006 Roadside Geology of Ohio. Missoula, Montana: Mountain Press Publishing Company
http://www.hockinghills.com Hocking Hills Park website (Thanks to naturalist Pat Quackenbush for allowing this Earthcache!)

Additional Hints (No hints available.)