3. Decomposition of rock in situ resulting
from chemical change
Water (rain, fog, moisture, ocean etc) is
the key medium for chemical weathering.
Common in warm humid climate (high
temperature & high rainfall)
Weathered rocks by this process have a
dull pitted appearance
5. Oxygen dissolved in
water reacts with mineral
iron in the rock
The rock is converted to
iron oxide
Always seen as reddish-
brown crust
This conversion
weakened the mineral
bonding and
consequently the whole
6.
7.
8.
9. Involves in the expansion of minerals
resulting from the absorption of water
E.g. Clay minerals are capable of absorbing
large quantities of water into their crystal
structure
When this happen, they exerts stresses
within the rock which may eventually cause it
to break apart
10.
11. Involves a chemical reaction
between hydrogen ions in water with certain
minerals in the rock
E.g. Weakly acidic rainwater causes
feldspar to be converted into white powdery
clay (kaolin) which breaks down easily
14. Is a form of solution weathering
Common in rocks composed of calcium
carbonate such as limestone and chalk
Rainwater mixed with carbon dioxide form
carbonic acid
The acid water change the calcium
carbonate to soluble calcium bicarbonate
which is then easily washed away
15.
16.
17. Simply the
dissolving
minerals in water
E.g Halite (rock
salt) dissolve in
water
Quartz dissolves
at an extremely
slow rate
18.
19.
20.
21.
22. Spheroidical Weathering
A type of chemical
weathering
Creates rounded boulders
and domed monolith
Typically granitic in
composition
Rock forms at great
temperatures and pressures
27. Caused by the action living organisms
Can lead to physical break down of rock
(Biophysical)
Also chemical attack (Biochemical weathering)
28. 1. By plant roots
2. By animals such as rodents
and earthworms
3. By human activities
29. By plant roots:
When roots
penetrate
into
cracks, they
will usually
break rocks
apart
30.
31. By animals:
Help to widen and
loosen the joints in
rocks and expose
underlying rocks to
weathering
processes as they
burrow through the
ground
32. By human activities:
Clearing of land for
cultivation
Construction and
mining activities
This activities break
up rocks and expose
them to the
weathering
33. Organic acids from
dead plants and root
can help to decompose
rock
Chelation is the effect
of organic acid on rock
Waste and organic
acids from dead
animals help to
weather rocks
chemically
34. Human activities:
Industrialisation
can cause pollution
such emission of
sulphur dioxide
which can produce acid rain
Accelerate the chemical weathering process of
hydrolysis, carbonation and solution