Skip to content

On Top of Comers Rock EarthCache

Hidden : 4/9/2009
Difficulty:
2 out of 5
Terrain:
3.5 out of 5

Size: Size:   not chosen (not chosen)

Join now to view geocache location details. It's free!

Watch

How Geocaching Works

Please note Use of geocaching.com services is subject to the terms and conditions in our disclaimer.

Geocache Description:

From Wytheville, take US 21 south. Turn right on FR 57 and continue west for 3.7 miles to Comers Rock Campground. (CAUTION: FR 57 is a winding dirt road that should not be driven in low clearance vehicles especially after wet or snowy weather).



The Rock


While to the south and southeast of the Comers Rock summit you will find the ancient volcanoes of Mount Rogers and Whitetop Mountain here is a totally different geological formation. No igneous rock and no metamorphic rock. Here is the more common sedimentary rock.


Among the different types of sedimentary rocks:


1. Sandstone- made up of sand grains cemented together. 2. Shale- made up of clay particles smaller than sand which makes it smoother 3. Conglomerate- made up of usually quartz pebbles cemented together 4. Limestone- made of calcium carbonate often deposited by sea life 5. Dolomite- like limestone but with more magnesium in it 6. Coal- composed by the remains of plants and animals


Comers Rock is a beautiful sandstone outcrop that dominates one of the summits of the Iron Mountain range. Sandstone is the most commonly found rock of the Iron Mountain as well as Applacichian Mountains. Just what is sandstone and how is it formed?


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. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions


.
The formation of sandstone involves two principal stages. First, a layer or layers of sand accumulates as the result of sedimentation, either from water (as in a river, lake, or sea) or from air (as in a desert). Typically, sedimentation occurs by the sand settling out from suspension, i.e., ceasing to be rolled or bounced along the bottom of a body of water (e.g., seas or rivers) or ground surface (e.g., in a desert or sand dune region). Finally, once it has accumulated, the sand becomes sandstone when it is compacted by pressure of overlying deposits and cemented by the precipitation of minerals within the pore spaces between sand grains.


For thousands, even millions of years, little pieces of our earth have been eroded--broken down and worn away by wind and water. Layer after layer of eroded earth is deposited on top of each. These layers are pressed down more and more through time, until the bottom layers slowly turn into rock.


While the sandstone of Comers Rock is more common than the dramatically formed volcanic peaks of the nearby Mount Rogers chain, it is just as beautiful. The colors are vibrant and the views of the valleys below are breath taking. The climb to the summit is fairly steep but it is a very short distance from the parking spot (use the steps, not the elevator!) Take a picnic lunch and take lots of pictures. Enjoy another creation of Mother Nature. After all, she took about 600 million years to complete the picture!


Note: In order to claim a find you must post a photo of your group at the given coordinates with your GPSr in hand. Also, please email us with the answers to the following questions: 1. What is the elevation of the Rock? 2. Did you find the benchmark (its not listed)? If so, what does it say? (Caution, this is a little tricky) 3. What are the predominant colors of the rocks found at the peak?


Be sure to go for Papafuz's very near traditional cache - GC1NYDZ.


We hope you enjoy your trip and always remember, Earthcaches rock or at least some are made of rock!


This Earthcache was approved by the Geological Society of America


We have earned GSA's highest level:

Additional Hints (Decrypt)

Arj pbzzref ner jrypbzr ng Pbzref!

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)