Mud flows

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Mud flow

Mud flows - dangerous phenomena consisting of rapid movement of layers of liquefied soil under the influence of gravity down the slope. They are most often found in the mountains covered with vegetation.

Often mud flows are the result of torrential rains, rapid melting of large snow masses or volcanic eruptions. Then the thick layers of loose rocks (clay, clay, sand) are strongly permeated with water and move rapidly in the form of mud and stone streams. The expelled masses of mud move with great force, capturing eg cars or big boulders at speeds up to 150 km / h.

Surface rinsing is caused by the flow of water on the slope. Usually occurs in the upper slopes. Its intensity depends on:

As a result of the precipitation of concentrated precipitation and melting water, mainly in the lower part of the slope, there is a linear rinsing process connected with erosion. There are crèches, pits, debris, ravines and steams.

Mud flows can be protected in the same way as rubbish. Bibliography

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