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A Cut In The Wall EarthCache

Hidden : 4/8/2008
Difficulty:
1 out of 5
Terrain:
1 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

This earthcache is beside the highway. You can park across the road from it. Parking coords are provided below. There appears to be an old mine at the bottom, that has been there for a long time. You are looking at whats around the small opening.

This earthcache may look like a rockslide or a mudslide that happened at one time. Although some sliding may have occurred over the years, this is no ordinary slide. Some type of mining appears to have happened here.



Upon talking with some people around the nearby area, this opening could have been here since the early 1900s. It could have been a small pony mine that the locals used to retrieve the mineral at the bottom. The structure around the small opening is made up of mostly slate rock, with a small patch of sandstone near the top. Slate rock and sandstone are very common in this area, and are very common in mining. Over time, erosion has chipped away at this site. Still not a slide, as time has went on, alot of pieces has fallen down from around the opening. The combination of Rain, heat, cold, wind, and time have helped the erosion process of chipping away around the opening. Also, overtime, it has created this wide cut in the mountain. It almost looks like a perfect square or rectangle, sitting inside this cliff line..

Slate is a fine-grained, foliated, homogeneous, metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low grade regional metamorphism. The result is a foliated rock in which the foliation may not correspond to the original sedimentary layering. Slate is frequently grey in colour especially when seen en masse covering roofs. However, slate occurs in a variety of colours even from a single locality.

Sandstone is a sedimentary rock composed mainly of sand-size mineral 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 color, but the most common colors are tan, brown, yellow, red, gray and white.

If you live and play in eastern part of the state here, you've probably seen these numerous times. Usually they are not near the highway though, as this one is. It does look pretty neat. Looks as if someone cut this hillside just perfect. Looks like a near perfect square around the opening at the bottom.

You do not have to go near the hillside to be able to log this earthcache. You can do all you need to from the parking coordinates. If you do go near the hillside PLEASE USE EXTREME CAUTION as for rocks may fall off the hillside. Again you can gather all info from the parking coords.(Parking coords:N=37 15.262, W=82 55.928).

To be able to log this earthcache, please do the following:
1) post a picture of yourself and GPSr with cut in the wall in the background,
2)Estimate how wide the cut is,
3)Estimate how high the cut is,
4)What kind of mineral appears to be at the bottom.

Additional Hints (No hints available.)