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Roche-A-Cri: Grotesque Towers EarthCache

This cache has been locked, but it is available for viewing.
Hidden : 3/9/2009
Difficulty:
1.5 out of 5
Terrain:
3 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:


Roche-A-Cri: Grotesque Towers

The park road is a short loop and there is parking available at several locations. Winter Parking can be found at: N43 59.777 W89 49.039. Please use due caution if planning a winter visit as your hike will be longer, ski trails must be avoided and the steps and trails may be icy. The accent to the observation deck in winter is not recommended. The foot bridge from the winter parking area may be subject to high water. Dogs are not allowed up to the observation deck.

To log this cache you will need to take and upload a photo and email me the answers to some questions.

This area of Wisconsin is dotted with tall rock formations which resemble ruined castles. The steep cliffs with their sharp angles seem out of place here resembling more closely formations found much further west on the Great Plains of the Dakotas and Montana. Here sandstone crags jut out from an unusually flat plain. How did these formations come to be?

Hundreds of millions of years ago an ancient sea left sedimentation deposits here and all but the most resistant of these layers were eventually worn away by wind, water and ice. What you see here today are the last remnants of those resistant layers.

The bluff which stands before you is one of a few isolated and rocky hills which rise from the surrounding plains. This formation is what is correctly known as a mesa (Spanish for "table") as it is a large formation. Smaller formations are known as buttes and pinnacles. Located in the "Driftless" (not glaciated) area of Wisconsin, these mesas, buttes and pinnacles escaped the land scouring activity of nearby glaciers. It's likely that hundreds or even thousands of similar formations (which were located outside the Driftless area) were worn away during the last ice age.

Because the capping material on these bluffs is cemented better than the under-laying material, erosion by wind and water wears away the soft sides of these formations until the weight of the overhanging cap causes it to fall. Frost is also major cause of erosion and tends to break the formations along joints keeping the tabletop appearance of many bluffs intact. This formation will continue to decrease in size until it eventually blends in with the plain on which it sits; this erosion accelerates once the resistant capping material has been lost.

Some of these formations stood as islands in Glacial Lake Wisconsin, while others were submerged. For several hundred years the lake's waves eroded the edges of the bluffs, giving them their distinctive steep sides. When an ice dam broke some 15,000 years ago the lake was released and the formations you see today were reveled.

Logging Requirements: In order to log this as a find you must meet the below requirements:

1. Take (and upload with your found it log) a photo of your team WITH your GPS (or your GPS alone) at a recognizable area within the park. Please do not photograph the sign at the posted coordinates.

2. Email me the answers to A, B, C and D OR A, B, E and F:
* Answers for A & B are at the posted coordinates. Answers for C, D, E & F can be found at the base of the stairs or at the top of the bluff.

From the "Outliers of Glacial Wisconsin" sign:
A. Roche a Cri and other rock outcroppings had their beginnings how many years ago?
B. The sediment here settled into extensive beds of sandstone and _________?

If you are able to climb the stairs to the top of the bluff:
C. Using your GPS, what is the altitude at the top observation deck?
D. How many informational signs are located here?

If you are not able to climb the 303 stairs to the top of the bluff:
E. Based on the sign at the base of the stairs, what kind of a climb is this?
F. What is not allowed on the stairs?


Sources & Permission:
http://www.wisconline.com/wisconsin/geoprovinces/centralplain.html
http://www.nps.gov/history/history/online_books/science/2/chap8.htm

Permission for this listing has been granted by Thomas A. Meyer, Conservation Biologist, State Natural Areas Program, Bureau of Endangered Resources, Wisconsin Department of Natural Resources. Prior to placing a geocache on state land one must submit the DNR Geocache Notification Form to the appropriate land manager: http://www.dnr.state.wi.us/org/land/parks/other/pdfs/form2500-118.pdf

Special thanks to geocache team sandlanders for their help with this listing.

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