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Burden Falls EarthCache

Hidden : 6/5/2009
Difficulty:
1.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:


Illinois: Corn and...Waterfalls?
If you  have ever driven through Illinois, whether its from Chicago to St. Louis on I-55 or east/west on I-80 or I-70, your impression of Illinois will be that of corn, corn and more corn and all of it flat land. Millions of years ago, glaciers flatten much of the land that is now Illinois. However the glaciers did not extend to the tip of southern Illinois. The far tip of southern Illinois is considered an "unglaciated" area, or in other words, not scoured flat by pre-historic glaciers. However, even though the glaciers did not extend to the tip of Southern Illinois, the powerful force of the water from the melting glaciers did affect the area and helped carve canyons. The bedrock, consisting of sandstone and limestone is the predominant geologic feature in this area. Southern Illinois’ fascinating geological features are the products of millions of years of tectonic activity followed and accompanied by thousands of years of deluge by melted glacial  waters. (http://shawnee.fws1.com/contact.html). Today, the glacial waters have receded, but creeks fed from rain run-off or natural springs has continued to fall through these canyons, often creating waterfalls rivaled to those seen in the mountains out west.

The Anatomy of a Waterfall
Cap rock at Burden Falls

A waterfall begins as a stream or river. It does not take much water to create a waterfall, only time and soft rock. As the water continues to wear away the softer rock, valleys are formed and canyons and cliffs are created. Canyons and cliffs may be made up of different types of rock. A resistant layer, like bedrock, will remain at the top of the cliff, and is called a caprock. The caprock prevents the erosion at the top of the cliff but softer layers, like sandstone, underneath the caprock will erode as the water flows over the cliff, forming a ledge.

rocks at bottom of falls

 

 

As these layers are eroded away, the caprock is left as an overhang until finally it cannot support itself and falls as a large block. The water continues to erode more soft rock and the process continues. For more information, visit "Waterfalls 101: How are Waterfalls formed?":

http://www.world-of-waterfalls.com/featured-articles-waterfalls-101-how-are-waterfalls-formed.html

 

 

 

Not all waterfalls fit neatly into one category. Some falls may begin as a cascade and end as a plunge. The type of waterfall also depends on how much water is falling. During a drought, with little water flowing, a waterfall may be a trickle over a ledge, but after heavy rain, could be a Block/Sheet or Cataract. http://worldwaterfalls.com/waterfall_types.php

 

Burden Falls Wilderness Area
Located in the Shawnee National Forest, south of Harrisburg IL is the Burden Falls Wilderness Area, designated a Wilderness Area by the Illinois Wilderness Act of 1990. At the southern most tip of the wilderness is Burden Falls. Burden Falls is formed by the Burden Branch of the Saline River and is considered the highest waterfall in Illinois. (http://www.visitgolconda.com/node/277). The stream falls in two sections. The upper falls is visible from near the parking lot. 

There are no designated trails in the Burden Falls Wilderness Area.  There are some scramble routes up and down the side of the falls that people do use.  Use the path that leaves the west side of the parking area. The path heads a few hundred yards downstream before turning and dropping into the bottom of the canyon.  From there walk up the stream to the bottom of the Falls.  This route would be more readily accessible to people who are not avid scramblers.  This area is mildly rugged and keep in mind that you might get wet. Terrain rating is about a 2-3. Be careful if you have small kids (or adventurous teen-agers) with you. Please note that there are no handrails or other safety equipment around.  Get a good view of the falls and answer the questions below to log this earthcache.

If you are adventurous and in fairly good health, take the path to the right to descend into the canyon below the falls. The terrain difficulty here is at least a 4. Please do not try this with young children or if you you are in poor health or poor physical shape. Note that the trail runs out quickly and you will have to climb over rocks and boulders to go down to the bottom. Take extra care going in this area. I can't imagine what the cost of an emergency rescue would be for this area if you do choose to make the journey to the bottom, the view will be spectacular and worth the effort. Remember, gravity can help you get down, but it makes it more difficult to get back up.

This area is open only to foot traffic or equestrian use. No other forms of transportation is allowed beyond the parking lot such as mountain bikes nor any motorized vehicles. Please practice "Leave No Trace" when visiting this beautiful area. Also, if you do find some trash, please practice CITO. Let's leave this area as beautiful as you found it. 

To log this earthcache, email me the answers to the folllowing.

  1. The quantity of water at the falls may vary depending on the season and recent or lack of rainfall. Based on the waterfall you see, what type of waterfall would you classify this and why?
  2. What is the layer of bedrock called at the top of the falls?
  3. Take a picture of yourself with your GPS with the waterfall in the background and add it to your log entry. If you are not able to go to the bottom of the lower falls, take a picture of yourself on the path to the left or right with the falls in the background. If you are not able to get a good picture of the falls from there, stand on the caprock near where the water falls over the edge. (Please be careful, this is supposed to be fun, not scary). If you do not post of a picture of yourself with your GPS, I will delete the log entry. No hand shots either, I'd like to see your face and your reaction to this area.
Thanks to Ranger Tim Pohlman from the Shawnee National Forest for approving this earthcache.

If you have enjoyed your visit to Burden Falls, please tell your friends about it or better yet take them there. I dragged my daughter there on Mother's Day and when she saw the place, she didn't want to leave. As I stood at the bottom of the falls and again as we walked through the canyon I had to keep reminding myself that we were not in Colorodo or Wyoming, but in Southern Illinois! Enjoy.

Direction to Burden Falls Wilderness Area
From the North: Take Interstate 57 south to IL-13 in Marion IL. (exit 54). Take IL-13 east about 23 miles to Harrisburg IL. Turn Right on Commercial St. (IL-34/US45). Follow it about a mile and turn left on IL-145. Take IL-145 south about 11 miles to Delwood IL. Turn right (west) on the gravel road to Bell Smith Springs. Continue for 4.5 miles to the parking area on the right for Burden Falls Wilderness. The water flowed over the road just before the parking lot.

From the South: Take Interstate 24 north to IL-146 (exit 16). Drive east on Illinois 146 for less than mile to Illinois 147. Turn left onto Illinois 147, and drive 13 miles to Illinois 145. Turn left onto Illinois 145, and drive 12 miles. Turn left (west) on the gravel road to Bell Smith Springs. Continue for 4.5 miles to the parking area on the right for Burden Falls Wilderness. The water flowed over the road just before the parking lot.

Sources:

http://worldwaterfalls.com/waterfall_types.php
http://www.world-of-waterfalls.com/featured-articles-waterfalls-101-how-are-waterfalls-formed.html
http://www.inhs.uiuc.edu/cwe/rra/site28.html
http://www.fs.fed.us/r6/rogue-siskiyou/recreation/geology/waterfalls.shtml
http://www.shawneetourism.com/history.html
http://www.visitgolconda.com/node/277
http://michelesworld.net/dmm/waterfal/States/Illinois/burden.htm

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