2. Introduction
Definition
Weathering vs. erosion
Types of weathering
Mechanical weathering
Agents of Mechanical weathering
Frost Action
Pressure Release (Exfoliation)
Insulation
Some minor Agents of Mechanical weathering
Chemical weathering
Main process of Chemical Weathering
Hydrolysis
Oxidation
Carbonation
Acidic Rain
Solution
Biological weathering
Mechanical weathering vs. chemical weathering
Factors af fecting weathering
Significance of weathering
3. “Weathering is the process of disintegration and
decomposition of rocks of the earth’s surface”.
Weathering Vs. Erosion
4. Mechanical weathering
Disintegration by physical agents
Composition of rock does not change
5. Frost Action
Weathering process by ice
Water increases in volume by about 9% when it freezes
Produces about 1890 metric tons pressure for every 1 ft2
Common in high altitude zones
6.
7. Pressure Release (Exfoliation)
Metamorphic and intrusive igneous rocks are under
pressure
Upper layer is removed by erosion
Due to pressure release the cracks are formed
8.
9. Insolation
Common in arid and desert regions
Temperature is high in day time and low in night
Disintegration due to expansion and contraction
Block Disintegration
Granular disintegration
12. Weathering process by chemical agents
Composition of rocks is changed
13. These weathered tombstones are from a burying ground in
Boston, Massachusetts. The marker on the left, carved in marble,
has been strongly weathered, weakening the lettering. The
marker on the right, made of slate, is much more resistant to
erosion.
14. Hydrolysis
Addition of water
When minerals are moistened, hydrolysis occurs.
H2O + CO2 + CaCO3 --> Ca+2 + 2HCO3-
water + carbon dioxide + calcite dissolve into calcium ion and bicarbonate ion
17. Oxidation
Iron combines with oxygen in the presence of water in a
processes called oxidation
The product of oxidation is rust
18. Carbonation
Mostly in humid areas
CO2 dissolves in rain water and creates carbonic acid
Carbonic acid easily weathers limestone and marble
CaCo3+H2CO3 Ca2+ + 2HCO3
19. Acidic Rain
Compounds from burning coal, oil and gas react chemically with
water forming acids.
Acid rain causes very rapid chemical weathering
20.
21. Solution
Rock salt and gypsum may be dissolved by water and
then removed in solution
22.
23. Can be both chemical and mechanical in
nature.
• roots split rocks apart
• roots produce acids
that dissolve rocks.
24. • Animal And
Insects
• Vegetation
• Human
Activities
25. MECHANICAL WEATHERING CHEMICAL WEATHERING
Rocks are disintegrated by Rocks are decomposed by
physical force chemical action
There is no chemical change Rocks undergo chemical change
Prominent in hot and humid
Prominent in dry and cool areas areas
Rocks are broken into great Only surface rocks are affected
depth Hard rock like quartz resist
Hard rocks are weathered too chemical weathering
26. Nature of rock
Slope of land
Joints
Vegetation cover
Climate
27. Landforms
Formation of sedimentary rocks
Mass wasting
Regolith formation