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The Break
up…
Today, I should be able
to:
a. define weathering and
distinguish between the two
main types of weathering
b. identify the factors that affect
the rate of weathering
Before After
Terms to encounter…
a. Weathering
b. Mechanical weathering
c. Abrasion
 d. Chemical weathering
e. Hydrolysis
f. Carbonation
 g. Oxidation
h. Frost wedging
2 types of
weathering
Physical weathering (or mechanical
weathering) disintegrates rocks,
breaking them into smaller pieces.
Chemical weathering decomposes
rocks through chemical reactions that
change the original rock-forming
Physical or
mechanical
weathering
a. Frost wedging- when water gets inside
the joints, alternate freezing and thawing
episodes pry the rock apart.
b. Salt crystal growth- force exerted by salt
crystal that formed as water evaporates from pore
spaces or cracks in rocks can cause the rock to fall
apart
c. Abrasion – wearing away of rocks by constant
collision of loose particles
d. Biological activity – plants and animals as agents of
mechanical weathering
Chemica
l
a. Dissolution – dissociation of molecules into ions;
common example includes dissolution of calcite
and salt
b. Oxidation- reaction between minerals and oxygen
dissolved in water
c. Hydrolysis- change in the composition of minerals
when they react with water
Factors that
affect the type
weathering
a.
b.Rock
c. Rock
structu
d.
Topograph
e. Time
Break me
down…
 Identify the type of weathering and its
subtype…
Picture no. Type of weathering subtype factor
1 Chemical hydrolysis time
1.
2.
3.
4.
5.
6.
7.
8.

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Break me up.pptx

Editor's Notes

  1. Weathering occurs as a response to the low pressure, low temperature, and water and oxygen-rich nature of the Earth’s surface. Point out that physical weathering and chemical weathering almost always occur together in nature and reinforce each other
  2. – areas that are cold and dry tend to have slow rates of chemical weathering and weathering is mostly physical; chemical weathering is most active in areas with high temperature and rainfal
  3. – the minerals that constitute rocks have different susceptibilities to weathering. Those that are most stable to surface conditions will be the most resistant to weathering. Thus, olivine for example which crystallizes at high temperature conditions will weather first than quartz which crystallizes at lower temperature conditions.
  4. rate of weathering is affected by the presence of joints, folds, faults, bedding planes through which agents of weathering enter a rock mass. Highly-jointed/fractured rocks disintegrate faster than a solid mass of rock of the same dimension
  5. weathering occurs more quickly on a steep slope than on a gentle one
  6. length of exposure to agents of weather determines the degree of weathering of a rock