5. FFrroosstt WWeeddggiinngg
Expansion of freezing
water in cracks and
crevices
Eventually breaking
rocks into pieces
• Sections of rock that are
wedged loose may
tumble into large piles
called talus
5
6. UUnnllooaaddiinngg
• Large masses of
igneous rock may
be exposed
through uplift and
erosion of
overlying rocks
• Resulting in
reduced pressure
Exfoliation—slabs
of outer rock
separate and
break loose
6
7. 7
BBiioollooggiiccaall AAccttiivviittyy
• The activity of plants- roots
breaking rock
• burrowing animals-moving
rocks to places where
weathering more rapidly occurs,
and humans
• Decaying organisms- producing
acids
• Humans- because of
deforestation, creation of roads,
and blasting mineral
9. Agents and EEvviiddeennccee ooff CChheemmiiccaall
Oxygen, water , and carbon dioxide are in
chemical weather
Water: most important agent of weathering. It
picks up CO2 and SO2 in the air which forms
acid rain.
Or dissolves these compounds into cracks of
rocks
9
WWeeaatthheerriinngg
10. RRaattee ooff WWeeaatthheerriinngg
How fast the rocks
erode
Two factors
• Rock characteristics
• Mineral composition
10
and solubility
• Climate
• Temperature and
moisture
• Favors high
temperature and
abundant moisture
11. 11
SSooiill
part of the
regolith that supports
the growth of plants.
Regolith: layer of rock
and mineral fragments
that covers Earth’s land
surface.
13. CChhaarraacctteerriissttiiccss ooff
13
SSooiill
Soil Composition
Soil has four major
components
◦ A. Mineral matter
(broken-down rock)
◦ B. Humus (decayed
remains of
organisms)
◦ C. Water
◦ D. Air
14. CChhaarraacctteerriissttiiccss ooff
SSooiill
Texture refers to
the proportions of
different particle
sizes.
A. Sand (large
size)
B. Silt – feels
like flour
C. Clay (small
size)
D. Loam (a
mixture of all three
sizes) is best suited
for plant life.
14
16. TTiimmee,, CClliimmaattee,,
OOrrggaanniissmmss aanndd SSllooppee
Time:
The longer a soil has been forming, the thicker
it becomes.
Climate
Greatest effect on soil formation
Organisms
Furnish organic matter to soil
Slope
Steep slopes often have poorly developed soils.
16
17. Soil Types Location Contents
Pedalfer under forest
17
vegetation
iron oxides and
aluminum-rich
clays in the B
horizon
Pedocal drier grasslands Calcium carbonate
Laterite Hot, wet, tropical
climates
Intense chemical
weathering to the
top layers of soil
18. HHooww ddooeess
wwaatteerr eerrooddee tthhee
ssooiill??
Rain uses gravity as
a force to move soil.
Flash flooding and
runoff of water
causes erosion
18
20. WWhhaatt iiss MMaassss
MMoovveemmeenntt??
The transfer of
rock and soil
down-slope due
to gravity
20
21. TTrriiggggeerrss ooff MMaassss MMoovveemmeenntt
Water Heavy rains and rapid melting
21
of snow
Oversteepened Slopes The steeper the slope the
greater the chance for
movement
Removal of
vegetation
Roots keep the soil intact.
Removing plants causes
erosion
Earthquakes Aftershocks dislodges rocks
22. CCllaassssiiffiiccaattiioonn ooff
MMaassss MMoovveemmeennttss
Rockfalls occurs
when rocks or rocks
fragments fall freely
through the air.
Avalanches
extremely rapid
movement of earth
material or snow
22
23. Slides
A block of material moves
suddenly along a flat,
inclined surface.Slides
that include segments of
bedrock are called
rockslides.
Slumps
The downward
movement of a block of
material along a curved
surface.
23
24. Flows
contain a large
amount of water.
Mudflows move
quickly and carry a
mixture of soil,
rock, and water
Earthflows move
relatively slowly
and carry
clay-rich sediment.
24
25. 25
Creep is the
slow, downhill
movement of
soil and
regolith.