Mushroom rock

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Mushroom rocks in Egypt
Mushroom rocks in Timna Park, Negev, Palestine.
A mushroom rock west of Moab, Utah
The Kelchstein ("Chalice Rock") near Oybin, Lusatian Mountains, Germany
Mushroom rocks in Taiwan, Yehliu
Mushroom rocks in Kardzhali District, Bulgaria

A mushroom rock, also called rock pedestal, or a pedestal rock, is a naturally occurring rock whose shape, as its name implies, resembles a mushroom. The rocks are deformed in a number of different ways: by erosion and weathering, glacial action, or from a sudden disturbance. Mushroom rocks are related to, but different from, yardang.[1]

Definition: A rock pedestal or gour is a typical mushroom shaped landform that is formed by the action of wind. We know as we move up, the material carrying capacity of the wind decreases and speed increases. At an average height of 2 to 3 feet I from the base, both the material carrying capacity and the speed is maximum. So abrasion (erosion by wind in which transported materials hit an exposed rock surface and polish it or scratch it) is maximum there. Also in some cases hard rocks are arranged horizontally over a soft rock resulting in such erosion. Therefore we sometimes say collection of rock pedestal as Zeugen.


Usually found in desert areas, these rocks form over thousands of years when wind erosion of an isolated rocky outcrop progresses at a different rate at its bottom to that at its top. Abrasion by wind-borne grains of sand is most prevalent within the first 3 ft of the ground, causing the bases of outcrops to erode more rapidly than their tops. Running water can have the same effect. An example of this type of mushroom rock is the one in Timna Park,Palestine.

Occasionally, the chemical composition of the rocks can be an important factor; if the upper part of the rock is more resistant to erosion and weathering, it erodes more slowly than the base. Its formation has also been attributed to chemical weathering at the base of the rock due to the collection of dew near the surface.

A mushroom rock may ultimately form from an originally flat area of hard rock overlying soft rock, similar to the pattern of rocks that form a waterfall. Weathering of the exposed hard rock layer eventually exposes the lower rock to erosion from wind, water, salt intrusion, etc., depending on local conditions. The layer of softer rock is more readily eroded, leading to the formation of a depression or blowout. The overlying harder rocks are resistant to this process, and may ultimately end up as isolated mushroom rocks standing above the new, lower plain.

The nature of wind erosion is that it concentrates a few feet over the ground - wind speeds increase with height, but sediment load reduces. This means that the combination of highest sediment loads and fastest wind speed exist a few feet over the ground - leading to the characteristic narrowing of the support pedestal at this height.

Glacial action[edit]

In contrast to a mushroom rock formed by erosion of a single rock, these mushrooms are a type of balancing rock that formed from two separate rocks, one of which came to rest on top of the other. Typically, the uppermost rock was transported and deposited by the slow action of a glacier. The lower part of the rock formation might or might not have also undergone a degree of erosion to accentuate the mushroom shape. Examples of this type of rock are Mushroom Rock in Signal Point National Park, Tennessee,[2] and Le Champignon in Huelgoat, France.[3]

Rock disturbance[edit]

This type of mushroom rock forms from two rocks, one of which came to rest on the top of the other, caused by a very sudden disturbance such as a rock fall or earthquakes.


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