3. Mechanical Weathering
Mechanical weathering takes place when rocks are broken
down without any change in the chemical nature of the rocks.
The rocks are essentially torn apart by physical force, rather
than by chemical breakdown.
4. The most common type of mechanical
weathering is the constant freezing, and thawing
of water.
5. Temperature changes also effect mechanical weathering. As
temperatures heat up, the rocks themselves expand somewhat.
As the temperatures cool down, rocks contract slightly. The effect
can be the weakening of the rock itself.
6.
7. Chemical reactions break down the bonds holding the
rocks together, causing them to fall apart, forming
smaller and smaller pieces. Chemical weathering is much
more common in locations where there is a lot of water.
This is because water is important to many of the
chemical reactions that can take place.
15. Biological Weathring
The word ‘bio’ means life. Thus biological
weathering is any type of weathering that is
caused by living organisms. Most often the
culprit of biological weathering are plant
roots. These roots can extend
downward, deep into rock cracks in search of
water, and nutrients. In the process they act as
a wedge, widening and extending the cracks.
16.
17.
18.
19. Other causes of biotic weathering are digging
animals, microscopic plants and animals, algae and
fungi.