Weathering - Paradise Valley
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Transcript Weathering - Paradise Valley
Weathering
GPH 111
Weathering Game Plan:
What is WEATHERING and how
does it fit within gemorphology?
Major TYPES of weathering
How does climate affect weathering?
What is Weathering?
The collective processes that lead to the
surface and sub-surface disintegration and
dissolution of rock. The major types include
physical, chemical, and biological weathering.
Weathering within Geomorphology
Sierra Estrella Mountains
and the Gila River
Weathering Processes
Salt Weathering
Sheeting
Solution
Frost Action
Oxidation
Hydration
Hydrolysis
Thermal Expansion
Chemical
_________
_________
_________
_________
Weathering Processes
-
Minerals chemically combine with water
Mineral breakdown through contact with Oxygen (Rust)
Mineral absorption of water causes swelling and stress
Mineral dissolution by water
Examples: Spheroidal Weathering, Karst Topography, Gnamma Pits
Physical
_________ - Water freezing induced expansion
_________ - Mineral crystal growth induced expansion
_________ - Pressure released expansion through unloading
_________ - Rapid heating from lightning and fires
Examples - Exfoliation Domes and talus slopes
Extra
Weathering Processes
Chemical
Hydrolysis - Minerals chemically combine with water
Oxidation - Mineral breakdown through contact with Oxygen (Rust)
Hydration - Mineral absorption of water causes swelling and stress
Solution - Mineral dissolution by water into their ionic form
Examples: Spheroidal Weathering, Karst Topography, Gnamma Pits
Physical
Frost Action - Water freezing induced expansion
Crystallization - Mineral crystal growth induced expansion
Sheeting - Pressure released expansion through unloading
Thermal Expansion - Rapid heating from lightning and fires
Examples - Exfoliation Domes and talus slopes
Extra
Chemical Weathering
Processes
Weathering Processes
Hydrolysis
Oxidation
Hydration
Solution
Associated Weathering Landforms
Spheriodal Weathering
Karst Topography
Gnama Pits
Chemical Weathering
Hydrolysis
Minerals chemically
combine with water,
substituting silica
for hydrogen and
weathering
individual mineral
grains
This process
removes CO2
from the
atmosphere,
counteracting
global warming
Feldspar (K, Al, Si, O) + carbonic acid and water
residual clays (Kaolinite) + dissolved minerals + Si
Chemical Weathering
Oxidation
Iron bearing minerals
(like biotite) combine
with Oxygen to
generate oxides and
softer clay minerals.
Rusted railway car; that
has undergone oxidation
Chemical Weathering
Oxidation
The Wave, Southern Utah
Wupatki, Northern Arizona
Chemical Weathering
Hydration - Clay minerals
absorb moisture along
their cleavage planes,
dramatically increasing in
volume.
Chemical Weathering
Solution
Minerals can
dissolve into ions
with water, like
dissolving sugar in
coffee
Water is the
universal solvent,
capable of
dissolving at least
57 of the natural
elements
Weathering Landform
Karst Topography - generated through
solution mostly into limestone bedrock
Weathering Landform
Caves and Caverns
Sinkholes
Karst Topography
Can Be Associated
with Extensive
Damage (Sink Holes)
Weathering Landform
Spheroidal Weathering - Chemical weathering
attacks all surface areas, rounding sharp edges into
spheroid shapes.
Weathering Landform
Weathering Landform
Gnamma Pits - How do you think these guys form,
what chemical weathering processes could affect
their growth?
Physical Weathering
Processes
Weathering Processes
Frost Action
Salt Weathering
Sheeting
Thermal Expansion
Associated Weathering Landforms
Talus Slopes
Exfoliation Domes
Physical Weathering
Frost Action - Where water seeps into rock
weaknesses during day, then freezes and
expands at night--breaking the rock apart.
Physical Weathering
Weathering Landform
Chemical weathering rounds rocks--physical weathering
generates angular rocks.
Talus Slope - A pile of angular rock fragments
Physical Weathering
Crystallization Where mineral rich
water seeps into rock,
evaporates, and allows
the dissolved solids to
crystallize, breaking the
rock apart.
Physical Weathering
Only non-water
related process
Sheeting - Buried rocks are under tremendous
pressure and once uncovered, pressure drop
sharply and the rocks rebound.
Sandstone
Granite
Weathering Landform
Exfoliation Dome Develop after extensive
unloading and sheeting.
Enchanted Rock, Texas
Half Dome, CA
Physical Weathering
Thermal Expansion Rocks dramatically heated
by forest fires can explode
when water absorbed in
the rock flashes to steam.
Physical Weathering
Thermal Expansion - Rocks dramatically heated by
lightning can explode when water absorbed in the rock
flashes to steam.
Physical Weathering
Thermal Expansion - Different rates of mineral
expansion and water absorption throughout numerous day
and night cycles.
Extra Weathering
Root Growth - Root growth extends into rock fractures,
expand and bust the rock apart
Where do you think the different
weathering processes dominate
on the planet?
In the Amazon (Tropical Rainforest)
Serengeti of Africa (Savanna)
Death Valley (Arid)
Minnesota (Humid Continental)
The Sierras (High Alpine)
Alabama (Humid subtropical)
Make a list for each one!!!
Importance of Surface Area
What will weather quicker, one huge
boulder or a huge boulder broken down
into a bunch of smaller boulders? Why?
What does Weathering DO?
The in situ disintegration of rock
supplied by tectonic (and isostatic)
rock input!
Things to Know:
What is weathering
Chemical processes round edges, physical
processes generate angles
Types of chemical weathering and
associated landforms
Types of physical weathering and
associated landforms
Importance of SURFACE AREA
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