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Broke Leg Falls EarthCache

Hidden : 2/19/2008
Difficulty:
1.5 out of 5
Terrain:
2 out of 5

Size: Size:   not chosen (not chosen)

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About Broke Leg Falls...

Broke Leg Falls is located on HWY 460, in Menifee County, Kentucky. The posted coordinates will take you to the parking lot for the falls. From there you will have to ascend some stairs that lead you the viewing area. The water of Broke Leg Falls flows overtop of a bed of sandstone and traces of limestone can also be seen. Sandstone is mostly made from sand sized Quartz crystals which makes it more resistant to erosion than the softer limestone. Here at the falls, the waters of Broken Leg Creek found this harder sandstone and has a more difficult time eroding this layer than the layer of limestone below the falls.

Broke Leg Falls
Broke Leg Falls in February


One very significant feature of Broke Leg Falls is you will notice that it is comprised of 3 waterfalls total. You will notice on your left as you make your way to the viewing area there are 2 other small falls making their way to the final drop.

Photobucket


Almost every waterfall will first fall into one of two main categories. They can be considered either:

1) river waterfalls: called such because they are usually found on a river. They are wider than they are tall and usually handle a high volume of water. They hardly ever go dry in summer months with little rainfall and after a large rainfall they can resemble a large rapid.

2) stream waterfalls: usually found on a mountain stream and is high than it is wide; the flow volume will be either small or medium; in dry months some stream waterfalls go dry In the case of mountain streams, the water flowing becomes wider and more shallow just aboves waterfalls due to flowing over a rock shelf. There is usually a deep pool just below the waterfall because of the kinetic energy of the water hitting the bottom.

What is a Waterfall

A waterfall is usually a geological formation resulting from water, often in the form of a stream, flowing over an erosion-resistant rock formation that forms a sudden break in elevation or nickpoint. Some waterfalls form in mountain environments where the erosive water force is high and stream courses may be subject to sudden and catastrophic change. In such cases, the waterfall may not be the end product of many years of water action over a region, but rather the result of relatively sudden geological processes such as landslides, faults or volcanic action. Typically, a river 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

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 Logging Requirements...

1) How high or tall do you estimate the waterfall to be?

2) How wide do you estimate the waterfall to be?

3) Using the waterfall classification guide above, what classification of waterfall do you believe the waterfall is?

4) Take a picture of yourself and your GPS with the waterfall in the picture

Additional Hints (No hints available.)