Weathering and Erosion
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Transcript Weathering and Erosion
Changing Earth’s Surface
Weathering and Erosion
Changes to Earth’s Surface
Earth’s crust is constantly in a process of change
Weathering
Erosion
Deposition
Weathering
The process by which
rocks are broken down
into small pieces called
sediment
Caused by
Wind
Water
Glaciers
Meteorites
Erosion
Occurs when
weathered material is
carried away by wind or
water
Responsible for some
of our most impressive
natural monuments
Example—The Grand
Canyon
Deposition
Occurs when sediment
is dropped off at a new
location
Wind or water slows
down or comes to a
stop
Example—River Delta
Changing Earth’s Surface
Volcanoes
Plate Tectonics
Theory that the lithosphere is divided into
plates that are always moving
Pangaea
Supercontinent that once existed over 350
million years ago
Evidence: Puzzle piece fit of the continents, fossil
and soil matches on different continents
Responsible for the formation of volcanoes
and earthquakes
Volcanoes
Form when magma
rises to Earth’s
surface
Pyroclastic Flow
Ashes, Gases, and
Magma that ooze or
explode from
volcanoes
Can form at divergent
boundaries or
subduction zones
Divergent Volcanoes
Plates above the asthenosphere separate
Magma rises up
As lava cools, new crust is formed
May be oozing or explosive
Divergent Volcano
Subduction Volcanoes
Formed when a denser
ocean plate sinks under
a lighter plate (either
ocean or land)
Magma comes to the
surface
Shield Volcano
Broad and flat volcano
Resemble a shield
laying on its side
Built up slowly over
thousands of years,
most often in layers of
hardened lava
Mostly ooze lava from
vents
Example—Mauna Loa,
Hawaii
Composite Volcano
Formed of alternating
layers of ashes and
hardened lava
May be dormant for
many years before
exploding rapidly or
may ooze for thousands
of years
Example—Crater
Lake, OR
Cinder Cone
Formed from blobs of
congealed lava in a
simple cone shape
Capable of violent
explosions
Bowl-shaped crater at
the summit
Example—Paricutin,
Mexico
Changing Earth’s Surface
Earthquakes
World Earthquake Map
Earthquakes
Energy released from the snap and slide of
Earth’s crust at a fault line
Fault
Focus
2 or more plates slide past one another
Point inside Earth where an Earthquake begins
Epicenter
Point on Earth’s surface where Earthquake
waves begin
3 Types of Seismic Waves
Primary (P) Waves
Fastest and Smallest
Waves
Secondary (S) Waves
Medium Waves
Surface (R) Waves
Slowest and Most
Dangerous Waves
Earthquake Waves
Measured with a
seismograph
Scaled using the
Richter Scale
Scale of 1-10
1 = least amount of
damage
10 = greatest
amount of damage