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Glenita Fault - EarthCache EarthCache

Hidden : 12/5/2008
Difficulty:
1.5 out of 5
Terrain:
1.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

This EarthCache is located at the southern edge of Natural Tunnel State Park one-half mile from the park entrance. The fault may be seen from some distance away and is located on the site of an old quarry.

Glenita Fault”

In geology a fault is a crack in the earth along which there has been movement along either side of the crack. There may be a crack without movement but that is called a joint. Faults may vary in length from a few millimeters to thousands of kilometers. The largest faults are caused by movement of tectonic plates.

Faults are produced by stress in the earth’s crust. Stress is a force which causes a change in shape by squeezing or stretching. This change in shape may be elastic if the object returns to its original shape when the stress is removed. The change may be inelastic if the object does not return to its original shape when the stress is removed. A stressed object may also fracture or break into pieces.

Rock may deform elastically under small stress and inelastically under higher stress. Rocks which are brittle fracture with little or no inelastic deformation. Cold rocks are more brittle than rocks which are hot. Rocks are less brittle under pressure. For these reasons most faults occur in the top six miles of the earth’s surface. Below six miles rocks tend to bend and fold.

Rocks may experience stress in the following ways:

1. tension- pulls rocks apart, pushing rocks away from each other

2. compression- squeezes rocks, pushing opposites sides into each other

3. shearing- pushes opposite sides against each other in opposite parallel directions

At the listed coordinates you get a very good look at the Glenita fault. It is very evident in the exposed bluff between VA 871 and the tunnel. This fault occurs in a structural weakness between the gently folded Rye Cove syncline (a downfold) and the more tightly folded Purchase Ridge syncline. According to geologists with the Virginia Division of Mineral Resources the cause of the Glenita fault is tectonic in origin. It is the result of the collision of the African continent with North America. This collision resulted in the formation of the Appalachian Mountains during the Paleozoic Era. The Glentia fault continues on through the Natural Tunnel and was very important to its formation.

To claim a find you must post a picture (optional) of yourself with the fault in the background and answer the following:



1. Estimate the height of the bluff in front of you.



2. Estimate the width of the crack in the rock at its widest point.



When traveling into the quarry area be careful of meeting dump trucks. A very small part to the left of the dirt road is used as a spoils area by VDOT but the traffic here is very light.

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