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Rock House of Grayson Highlands EarthCache

Hidden : 10/26/2009
Difficulty:
2 out of 5
Terrain:
1.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

The Grayson Highlands Park is on U.S. 58 midway between Independence and Damascus. The Park entrance is 8 miles west of route 16 on US 58. Just follow your GPS since this EC is easily spotted from the road!. Parking is very nearby.



The 4,935-acre Grayson Highlands State Park showcases the Natural beauty of waterfalls, red spruce-fir forests and igneous rock outcroppings such as the Buzzard's Rock , Listening Rock and the Big and Little Pinnacles as well as the Rock House Native trout streams, rugged mountains, and high alpine meadows with panoramic vistas of valleys below are features of the Park. A community of hardy wildflowers, shrubs, insects, birds, amphibians, and mammals that can withstand the harsh conditions of the open highlands have adapted to life in the alpine meadows.



The Rock House


Most people do not know that the Mount Rogers chain with the Surrounding mountain peaks are remnants of ancient volcanoes. Roughly 750 million years ago, rift-related (divergent) volcanoes erupted along part of the axis of what was to become the Appalachian Mountains. The major peaks of the Mountain Rogers Chain are: Mount Rogers, Pine Mountain, Whitetop Mountain and the Haw Orchard Mountain with it’s Twin Pinnacles. Mount Rogers is the highest peak in Virginia at an elevation of 5729 feet. The Mount Rogers chain occupies about 206 square miles. This Earthcache is but one of several wonderful outcrops of the Mount Rogers chain.

Because of the volcanic activities of the Mount Rogers Chain, its geological history is very different from most of the Appalachian Mountains. Peaks and outcroppings on most ridges of the “Appy” mountains are definitely sedimentary rock. The sedimentary rock is predominately limestone with sandstone/shale found in the more northern areas. The volcanic eruptions here have left major igneous Formations. These formations have been weathered by millions of years of wind and rain.


Beside its beauty, one of the most interesting geological facts of the Rock House is the nature of the Rock itself. While most outcrops in the Park are igneous and are composed mostly of rhyolite the Rock House is a conglomerate! As we stated earlier, the more Northern regions of the Appalachian Mountain chain are all sedimentary rock, but within the Park, most rock is igneous due to the ancient volcanic activity. Most agree that the base rock here is diamictite with many different cobbles and/or drop stones of varying composition found ‘suspended’ within the diamictite. You can easily observe large quartz, rhyolite and cranberry gneiss cobbles within the Rock House. Be sure to carefully examine the Rock because you will be required to identify and photograph one of the cobbles.




Drop Stones




More Drop Stones




And Still More Drop Stones


How was the Rock House formed? There are differing opinions but there is one thing is for sure, there had to be water and/or ice involved in the process. The drop stones or cobbles had to be transported and deposited within layer after layer of mud, which with enormous pressure and lots of time became the base rock, diamictite. All conglomerates are composed of at least two different rocks. One is the base rock such as sandstone and the other are the particular cobbles of another entirely different rock such as quartz pebbles. Instead of the more common sandstone being the base rock, this conglomerate it is diamictite and the cobbles are metamorphic (cranberry gneiss), igneous (rhyolite) and quartz rocks.



Now for the fun part of your visit. In order for you to claim a find of the Rock House you must complete the following tasks and email the answers to numbers 1. and 2. 1. Estimate to within 10 feet, the height and width of the Rock House, 2.While standing at the base of the Rock, what is the elevation?, 3. Find and photograph an example of one of the drop stones within the Rock. Point to the stone with your GPSr. You may use the above pictures as guides to finding the cobbles. Lastly, 4. as an option, post a photo of yourself holding a GPSr with the Rock House in the background. Have fun and enjoy another one of Mother Nature’s creations. There are several other EarthCaches to be discovered at the Grayson Highlands Park. Go for them!


This Earthcache was approved by the Geological Society of America


We have earned GSA's highest level:


FTF HONORS GO TO: Heironimus!

Additional Hints (Decrypt)

Gurer jvyy or n "ebpxva' tbbq gvzr va gur byq ubhfr gbavtug!"

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)