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Tishomingo Outcroppings EarthCache

Hidden : 7/17/2010
Difficulty:
1.5 out of 5
Terrain:
3.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Questions you need to answer to complete this earthcache:

1) Estimate how far out the overhang protrudes.

2)Estimate the height to the top of the overhanging structure.


To get to the coords cross the swinging bridge and follow the Outcroppings Trails. It splits off in several locations but you shouldn't have too much trouble finding the Earthcache location .It is right alongside one of the main branches. I suggest picking up a trail map at the park office.

Along the way you will encounter many large rock formations;the most famous of which is Jean's Overhang.

Once you arrive at the coords the referrenced earthcache rock outcropping will be obvious ! (The formation you are seeking is NOT Jean's Overhang)

Tishomingo State Park, named after a Chickasaw Indian Chief, is located in the foothills of the Appalachian Mountains providing the most picturesque and rugged terrain in Mississippi. The Park contains rock formations dating to the Devonian and Mississippian epochs of the Paleozoic era. This is the only location that these two formations are found in the State of Mississippi.

Archaeological surveys have revealed area occupation since Early Atchaic Period (circa 7000 B.C.) or earlier times and a long, moderately intensive use of the park area and environs from Middle Archaic Period (circa 6000 B.C.) through Early Woodland Period times (terminating circa 200 B.C.), and became intensively utilized in the Middle Woodland Period (circa 200 B.C. to 400 A.D.). Much of the aboriginal use of the park can be attributed to its unique environment as a source for materials and foodstuffs.

Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial deposits are covered by a mantle of soil and vegetation and cannot be seen or examined closely. However in places where the overlying cover is removed through erosion or tectonic uplift, the rock may be exposed, or crop out. Such exposure will happen most frequently in areas where erosion is rapid and exceeds the weathering rate such as on steep hillsides, mountin ridges and tops, river banks, and tectonically active areas. Bedrock and superficial deposits may also be exposed at the Earth's surface due to human excavations such as quarrying and building of transport routes.
Outcrops are also critically important for understanding fossil assemblages, paleo-environment, and evolution as they provide a record of relative changes within geologic strata.
The cause could be erosional, tectonic, or man-made, or any combination of them.

In order to log this cache you must e-mail me the answers to these questions.Failure to do so could result in a deleted log.Please follow this Earthcache specific guideline.Do NOT log your find unless you are sending the recquired info also. Photos of you holding a GPS at the cache site is no longer recquired but would be greatly appreciated.

1) Estimate how far out the overhang protrudes.

2) Estimate the height to the top of the overhanging structure.

Posting of photos are encouraged just be sure not to give away the answers to any questions in your photos

Additional Hints (No hints available.)