weathering & erosion - weebly
TRANSCRIPT
Weathering and Erosion
Weathering - processes at or near
Earth’s surface that cause rocks and
minerals to break down
Erosion - process of removing Earth
materials from their original sites
through weathering and transport
Types of Weathering
Mechanical (Physical) -
processes that break a
rock or mineral into
smaller pieces without
altering its
composition
Chemical - processes
that change the
chemical composition
of rocks and minerals
What evidence of weathering do
you see in this picture?
Why wasn’t this mass
of land weathered
away?
Mechanical Weathering 3. Exfoliation/Unloading
– As deeply buried rock is uplifted, pressure is
reduced and the rock breaks off into leaves or
sheets along joints
Mechanical Weathering
4. Thermal Expansion/Contraction –
repeated, daily heating (expansion) and
cooling (contraction) of rock causes stress
along natural boundaries in the rock
Mechanical Weathering
6. Crystal Growth – water evaporates
leaving minerals (salt) behind; crystals grow
and fracture the rock
Chemical Weathering • Rock reacts with water,
gases and solutions
which add or remove
elements from minerals
• Most caves formed
from limestone.
Chemical Weathering
1. Oxygen
– Iron combines with oxygen in the presence of water in a processes called oxidation. The product is rust.
Chemical Weathering
2. Carbon Dioxide
– CO2 dissolves in rain water and creates
carbonic acid which easily weathers limestone
and marble
Chemical Weathering
3. Biological Activity
– Lichen that grow on rocks produce weak
acids that chemically weather rock
Mass Wasting
• Movement of large amounts of material downhill
under the influence of gravity – Creep
– Solifluction
– Mudflow
– Earthflow
– Slump
– Rockfall
– Avalanche
Triggers for rapid Mass Wasting
• Rain
• Over-steepening
– cutting at foot of slope
– piling on head of slope
• Deforestation / Devegetation
• Earthquakes