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Upper Falls of the Stony EarthCache

Hidden : 8/13/2007
Difficulty:
1 out of 5
Terrain:
2 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

Take VA SR 72 from either Dungannon or Coeburn to the Little Stony Trail. Here you will find the parking spot and the short walk to cross the foot bridge and down to the falls. It took her millions of years so give Mother Nature full credit for her work.

The Geological Formation of the Upper Falls

Typically, a river or a stream in this case, flows over a large step in the rocks which may have been formed by a fault line. Over a period of years, the edges of this shelf will gradually break away and the waterfall will steadily retreat upstream, creating a gorge of recession. Often, the rock stratum just below the more resistant shelf will be of a softer type, meaning undercutting, due to splashback, will occur here to form a shallow cave-like formation known as a rock shelter or plunge pool under and behind the waterfall. Eventually, the outcropping, more resistant cap rock will collapse under pressure to add blocks of rock to the base of the waterfall. These blocks of rock are then broken down into smaller boulders by attrition as they collide with each other, and they also erode the base of the waterfall by abrasion, creating a deep plunge pool.

The Little Stony Creek, as with other waterfalls, becomes wider and more shallow just above waterfalls due to flowing over the rock shelf, and there is usually a deep pool just below the waterfall because of the kinetic energy of the water hitting the bottom. At the Upper Stony, you will see the results of this geological change. Remember, it took thousands of years for all of this to happen!

This is a classification of waterfalls including the most common types :

Block: Water descends from a relatively wide stream or river. Water descends a series of rock steps.
Cataract: A large waterfall.
Fan: Water spreads horizontally as it descends while remaining in contact with bedrock.
Horsetail: Descending water maintains some contact with bedrock.
Plunge: Water descends vertically, losing contact with the bedrock surface.
Punchbowl: Water descends in a constricted form, then spreads out in a wider pool.
Segmented: Distinctly separate flows of water form as it descends.
Tiered: Water drops in a series of distinct steps or falls.
Multi-Step: A series of waterfalls one after another of roughly the same size each with its own sunken plunge pool.

Some Of The Types




The Little Stony Creek flows for about 2.8 miles through a gorge that is 400 feet deep and 1700 feet wide. Of the two magnificent falls, this is the Upper and is narrow but fairly high. Be sure to walk on down the trail a bit and see the Middle falls.

In order to receive credit for this Earthcache you must do ALL the following:
1. Email us with answers to the following questions:
A. Estimate to within 10+/- feet the height and width of the falls,
B. From the above classification, what type is this waterfall?
2. Take and upload a photo your GPSr pointing to the defining characteristic (see definitions) of the the waterfall. While it would be nice, you do not have to have to show your face(s) in the photo.

Thanks and we sincerely hope you enjoy.

Please note: There is no need to leave the trails and above all, do not disturb the surroundings. Leave the area cleaner (CITO) than you found it.


This Earthcache was approved by the Geological Society of America


We have earned GSA's highest level:

Additional Hints (Decrypt)

Jr jbhyq tvir lbh bar ohg ba na Rnegupnpur gung jbhyq or purngvat.

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)