Mass Wasting in the environment.
Mass Wasting is the downslope movements of loose rock materials under the influence of gravity.
Water is the best factor that facilitates mass Wasting due to its lubricant nature and this easing the flow of weathered rock materials downslope.
All various forms of downward movements of weathered rock materials under the influence of gravity are collectively called mass movements.
Areas which are mainly affected by mass Wasting are;high land areas.
Types of Mass movements
There are two different types of Mass movements and the rapid movements can't easily be noticed.
Slow movements.
The slow movements can't be easily noticed and act continuously over along period of time. Such movements include;
Talus creep
It involves the movement of materials of all sizes downslope to the base of the mountain.
The process occurs highly in mountain regions where freezing and thawing take place.
Soil creep
This is the slowest type of mass movements which involves continuous movements of soil and rock particles downslope.
Solifluction
This is a process in which melting snow helps to lubricate the moving mass of rocks downslope.
The Rapid movements.
These are gradually referred to as landslides and these include;
Mudflow
It involves the movement of unconsolidated semi liquid rock materials downslope due to heavy raining.
Rockfall
This is the process that occurs when massive soils or rocks are lubricated by water.
This is where jointed rocks loosen due to weathering and fall off down asteep slope .
Rock slump
This is the process that occurs when massive soils and rocks are lubricated by heavy rains and slide downslope.
Rock side
This is where rocks a long steep slopes slide down at a high speed.
Causes of mass movements or mass Wasting
Nature of relief or slope;
Very steep slopes increases the movement of weathered rock materials downslope.
Action of plant roots;


No comments:
Post a Comment