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Raven Cliff Falls EarthCache

Hidden : 6/22/2010
Difficulty:
4 out of 5
Terrain:
4 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

How to get to the trail

From Caesars Head State Park on US 276 in northern Greenville County, drive north for one mile to a large, paved parking lot on the right. Take the second right down into the lot. The trail begins across the road. It is required by law to register at the trail box.


Fee and Hours

Trail access fee: $2 adults; $1.25 SC seniors; age 15 & younger free and Days and Hours of Operation: M-Su 9am-6pm (extended to 9pm during daylight savings time). During daylight savings time the trails close one hour before sunset.

Follow the red blazes on the trees and the signs to the falls because two other, much more difficult, trails (including a spur of the Foothills Trail) intersect the Raven Cliff Falls Trail.

About the Area

Raven Cliff Falls is the king of South Carolina waterfalls at an huge drop in tons of feet. Matthews Creek plunges off Raven Cliff Mountain at the Blue Ridge Escarpment near Caesars Head. The escarpment is where the Blue Ridge Mountains (part of the Appalachian chain) drop abruptly 2,000 feet to the Piedmont below. This sudden drop is the geologic reason why there are so many falls in the area. A very popular 4.4-mile roundtrip trail leads to an overlook across the gorge from the falls. The 4.4-mile hike is moderately difficult with steep descents in the first .25 mile and last .75 mile. That means you will have to ascend on the return trip. When you reach a set of stairs on this trail, you are near the halfway point. When you reach the shelter, turn left to begin the final .75 mile descent to the overlook. Caesars Head State Park is part of the Mountain Bridge Wilderness, a 40,000-acre preserve in northwestern South Carolina

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.

How Waterfalls are Formed

Typically a stream or 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 stream will retreat upstream, creating a gorge of recession. Often the rock just below the more resistant shelf will be a softer type, meaning some undercutting will occur due to the splashback of the falling water. A shallow cave-like formation known as a rock shelter or plunge pool under and behind the waterfall will form. Eventually the outcropping of 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 boulder as they collide with each other and they also will continue to erode at the base of the waterfall by abrasion, creating a deeper plunge pool. Streams will become wider and more shallow just above waterfall due to the flowing of the water 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.The rock canyon surrounding this waterfall is a direct result of the above information. Over several thousands of years, Mother Nature has used the creek to carve out the the Falls that exist today.

Types of Waterfalls

Block: Water descends from a relatively wide stream or river.

Cascade: 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.

To get credit for this earthcache please answer the following

a)Describe what type of waterfall Raven Cliff Falls is--this may include more than one of the classifications.

b) Estimate the height these falls. (needs to be within 10 feet)

If you like include a picture of the falls that is great but its not required, please just enjoy this wonderful waterfall

Additional Hints (No hints available.)