WEATHERING AND MASS WASTING
Pressure release and expansion have caused an outer
shell of this granite outcrop to break parallel to the
main mass and then into smaller pieces (J Petersen).
INTRODUCTION
Exogenic processes:
Break down rocks
erode rock materials
Transport them from high energy locations to
low energy locations
Relocation of rock by:
Gravity
Geomorphic Agents
Flowing water, wind
moving ice, waves
NATURE OF EXOGENIC PROCESSES
Weathering
breakdown of rock materials
at and near Earth’s surface
Other exogenic processes
Erosion
Transportation
Deposition
Often occurs with assistance
from geomorphic agent (water,
ice, wind, and waves)
Why are some exposed
parts of the boulder
darker than others?
NATURE OF EXOGENIC PROCESSES
Mass wasting
Gravity-induced
downslope movement of
rock material that occurs
without a geomorphic
agent
Rock falling
High energy locations to
low energy
Endogenic processes compared with exogenic
processes
NATURE OF EXOGENIC PROCESSES
Weathering, mass wasting, and geomorphic agents
usually do not work alone
NATURE OF EXOGENIC PROCESSES
How does the cross-sectional profile of the
valley change at each phase?
Can you identify evidence of the three phases
shown in the figure below (Figure 15.3) in Idaho?
NATURE OF EXOGENIC PROCESSES
WEATHERING
Two types of
weathering
Physical weathering
Disintegrates rocks
breaking smaller
fragments from a large
block or outcrop of rock
Chemical weathering
Decomposes rock through
chemical reactions that
remove ions from the
original rock
WEATHERING
How might an animal
cause physical weathering?
Unloading
High elevation helps drive
this process
Erosional stripping of
overlying rocks, and
ultimate removal of
overlying weight
Upper granite is exposed
where it experiences lower
atmospheric pressure as
compared to the rock at
depth
WEATHERING
WEATHERING
Unloading
As outer sheet continues to
weather, segments of it may
slide off
Exfoliation
Successful removal of these
outer rock
Exfoliation sheet
Exfoliation dome
Stone Mountain, Georgia
Half Dome (Yosemite)
Sugar Loaf Mountain, Rio de
Janeiro, Brazil
Enchanted Rock, Texas
Why is granite so
susceptible to unloading
and exfoliation?
WEATHERING
Thermal expansion
and contraction
Granular
disintegration
Differential thermal
expansion and
contraction of
individual mineral
grains in coarse
crystalline rocks
What other evidence exists on
the boulder to suggest that it
has been subjected to
considerable weathering?
WEATHERING
Freeze-thaw
weathering
Also called frost
weathering or ice
wedging
Water freezes and
expands 9% causing
large pressure
differences in the
crack, widening it,
leading to rock
breaking off
How important if
freeze-thaw weathering
where you live?
WEATHERING
Freeze-thaw
weathering
Pipes bursting
Not significant at
lower latitudes
except high
elevations
Especially noticeable
in mountainous
regions near tree line Why are these rocks angular
in shape rather than
rounded?
WEATHERING
Salt crystal growth
Water with dissolved salt
accumulates in these
spaces and then
evaporates, and growing
salt crystals wedge rocks
apart
Hydration
Water molecules attach
to the crystalline
structure of a mineral
A mineral expands
when hydrated and
shrink when dehydrated
Clay minerals
Once a small hollow is formed,
how might it affect further
weathering at this site?
WEATHERING
Chemical weathering
Ions from a rock are
released into water or
combine with other
substances to form new
materials (clay minerals)
Most important catalysts
and reactive agents:
Water
Oxygen
Carbon dioxide
WEATHERING
Chemical weathering
Three types of chemical
weathering:
Oxidation
Chemical union of oxygen
atoms with another
substance to create a
new product
Solution and carbonation
Hydrolysis
What is a likely chemical
formula for the reddish-
orange substance?
WEATHERING
Chemical weathering
Solution and carbonation
Carbonation
Carbon dioxide and
water molecules
reacting with, and
decomposing rocks
Most effective on
carbonate rocks
(limestone)
Hydrolysis
Water alone reacts with
rocks
How does the fact that
lichens retain moisture also
contribute to weathering?
Why does the rock near the
bottom of the outcrop seem
to be more weathered than
that at the top?
VARIABILITY IN WEATHERING
Effectiveness of
Weathering
Climate
Type of rock
Nature and amount
of fractures
VARIABILITY IN WEATHERING
Climate
Chemical weathering
dominates humid
regions
Slopes in wetter
climates have a
rounded appearance
What kind of chemical
weathering has impacted
the iron fence?
VARIABILITY IN WEATHERING
Rock type
Differential weathering
and erosion
Strong rock may be
easily eroded in a
different environment
Structural weakness
Joints and fractures
Exposed rock, collect
salts, accumulation of
water, and plants
VARIABILITY IN WEATHERING
Structural weakness
Joint set
Two joint sets will cross
each other at an angle
Spheroidal weathering
With north at the top of
this photo (top right),
what directions do the
two most apparent joint
sets trend?
VARIABILITY IN WEATHERING
Differential weathering and erosion
Grand Canyon
VARIABILITY IN WEATHERING
Differential weathering
and erosion
Appalachian ridge and
valley region
Resistant rocks form
ridges and weaker
rocks form valleys
MASS WASTING
Mass movement
Downslope transport of
material due to gravity
What other kinds of
problems on roads are
related to mass
wasting?
MASS WASTING
Mass movement
Slope angle
Gravity is the principal
force
Water is also a
contributing factor
How might vegetative cover or
moisture content affect the
potential for downslope
movement of soil?
MASS WASTING
Materials and motion
Types of Earth material
Involves almost all kinds of
surface materials
Rock, snow, ice, soil, earth,
debris, and mud
Soil – thin, and
unconsolidated
Earth – thicker soil
Debris – wide range of
grain sizes
Mud – saturated sediment
Speed of motion
Slow mass wasting
Fast mass wasting
MASS WASTING
Slow mass wasting
Creep
slow migration, but most
persistent
Heaving process
Are there places near
where you live that
show evidence of soil
creep?
MASS WASTING
Slow mass wasting
Creep
What other
constructed features
might be changed by
creep?
MASS WASTING
Slow mass wasting
Solifluction
Most common in high
latitudes or high
elevation tundra regions
Permafrost
Active layer
Summer thaw
Tundra landscapes
How does solifluction differ
from soil creep?
MASS WASTING
Fast mass wasting
Four major types:
Falls
Avalanches
Slides
Flows
Effects more dramatic than slow mass wasting
MASS WASTING
Falls
Rockfalls
Due to:
Weathering weakens the
bonds between clasts
and cliff
Large rock masses that
fall from a cliff face or an
overhanging ledge
What weathering
processes might be acting
on the sandstone cliff at
the base of the ledge
when it becomes wet?
MASS WASTING
Falls
Talus slope
Talus cone
Angle of repose
How would the angle of
repose of rounded
particles differ from that
of angular particles of the
same size?
MASS WASTING
Falls
Yosemite Valley, California
Serious hazard
MASS WASTING
Avalanches
Material is pulverized
(broken down into
small powdery
fragments) and then
flows rapidly
Snow
Rock
debris
MASS WASTING
Slides
Water plays biggest role
Rockslides
Threaten lives and property
MASS WASTING
Slides
Rockslides
Debris slide
Mudslide
Slumps
Landslide
Earthquake lake
rockslide
Southwestern Montana
(1959)
killed 28 people
Why can earthquakes
trigger landslides?
MASS WASTING
Slides
Mudslide (California)
Landslides
May contain more than
category of motion or
material
MASS WASTING
Slides
Slumps – common when it is wet
How does the earthflow component differ from the
slump component?
MASS WASTING
Flows
Earthflow
Slump-earthflow
Debris flows
Mudflows
Flow levees
What evidence is there
to indicate this is a sit
of repeated debris
flows?
MASS WASTING
Flows
Debris flow in La
Conchita, CA.
Lahars
Why might a specific site
experience repeated slope
failures over time?
MASS WASTING
Flows
Lahars
Why might a specific
site experience
repeated slope
failures over time?
WEATHERING, MASS WASTING, AND THE
LANDSCAPE
Weathering and mass wasting typically determined by the
properties of the rocks and the local climate factors
Slow weathering of resistant rocks leaves steeps slopes
Rapid weathering of weak rocks produces gentle slopes
Weathering proceeds rapidly in warm, humid climates
Rocks in arid and cold climates weather slower