This document discusses weathering processes that break down rocks at Earth's surface. It defines weathering and distinguishes it from erosion. The main types of weathering are mechanical, chemical and biological. Mechanical weathering breaks rocks through frost cracking, heat expansion and other physical processes without changing the chemical composition. Chemical weathering alters the minerals through hydrolysis, oxidation and other reactions. Factors like climate, topography and vegetation influence weathering rates and produce landforms over time.
2. ο Introduction
ο Definition
ο Weathering vs. erosion
ο Types of weathering
ο Mechanical weathering
ο Agents of Mechanical weathering
ο Frost Action
ο Pressure Release (Exfoliation)
ο Insulation
ο Some minor Agents of Mechanical weathering
ο Chemical weathering
ο Main process of Chemical Weathering
ο Hydrolysis
ο Oxidation
ο Carbonation
ο Acidic Rain
ο Solution
ο Biological weathering
ο Mechanical weathering vs. chemical weathering
ο Factors af fecting weathering
ο Significance of weathering
3. ο βWeathering is the process of disintegration and
decomposition of rocks of the earthβs surfaceβ.
ο Weathering Vs. Erosion
4. ο Mechanical weathering
ο Disintegration by physical agents
ο Composition of rock does not change
5. ο Frost Action
ο Weathering process by ice
ο Water increases in volume by about 9% when it freezes
ο Produces about 1890 metric tons pressure for every 1 ft2
ο Common in high altitude zones
6.
7. ο Pressure Release (Exfoliation)
ο Metamorphic and intrusive igneous rocks are under
pressure
ο Upper layer is removed by erosion
ο Due to pressure release the cracks are formed
8.
9. ο Insolation
ο Common in arid and desert regions
ο Temperature is high in day time and low in night
ο Disintegration due to expansion and contraction
ο Block Disintegration
ο Granular disintegration
12. ο Weathering process by chemical agents
ο 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. ο Hydrolysis
ο Addition of water
ο When minerals are moistened, hydrolysis occurs.
H2O + CO2 + CaCO3 --> Ca+2 + 2HCO3-
ο water + carbon dioxide + calcite dissolve into calcium ion and bicarbonate ion
17. ο Oxidation
ο Iron combines with oxygen in the presence of water in a
processes called oxidation
ο The product of oxidation is rust
18. ο Carbonation
ο Mostly in humid areas
ο CO2 dissolves in rain water and creates carbonic acid
ο Carbonic acid easily weathers limestone and marble
CaCo3+H2CO3 Ca2+ + 2HCO3
19. ο Acidic Rain
ο Compounds from burning coal, oil and gas react chemically with
water forming acids.
ο Acid rain causes very rapid chemical weathering
20.
21. ο Solution
ο Rock salt and gypsum may be dissolved by water and
then removed in solution
22.
23. ο Can be both chemical and mechanical in
nature.
β’ roots split rocks apart
β’ roots produce acids
that dissolve rocks.
24. β’ Animal And
Insects
β’ Vegetation
β’ Human
Activities
25. MECHANICAL WEATHERING CHEMICAL WEATHERING
ο Rocks are disintegrated by ο Rocks are decomposed by
physical force chemical action
ο There is no chemical change ο Rocks undergo chemical change
ο Prominent in hot and humid
ο Prominent in dry and cool areas areas
ο Rocks are broken into great ο Only surface rocks are affected
depth ο Hard rock like quartz resist
ο Hard rocks are weathered too chemical weathering
26. ο Nature of rock
ο Slope of land
ο Joints
ο Vegetation cover
ο Climate
27. ο Landforms
ο Formation of sedimentary rocks
ο Mass wasting
ο Regolith formation