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Tectonic Plates, Faults, and Volcanoes
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Types of Volcanoes
Active Volcano
Potentially active
Inactive Volcano
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Types of Volcanoes
Cinder
or
scoria
cone
Composite
volcanoes or
stratovolcanoes
Shield
volcanoes
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Cinder Volcano
Taal Volcano
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Composite volcanoes
Mt.
Fuji Volcano
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Shield
volcanoes
Fernandina Volcano
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Parts of a Volcano
1.
Volcanic Edifice
2.
Vent
3.
Chamber
4.
Conduit
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When magma overflows in the chamber & rises to the conduit and goes out of the vent
Erupted
magma is called
lava
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Thick
Magma
Gasses
build up pressure until violently released along with lava, ashes, &
gasses
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Lava
Flows out of the
vent
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Explosive Eruptions
Lava splits up & solidifies into pieces called
tephra
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Effusive Eruptions
Magma
is very runny and can easily release
gas
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300
volcanoes in the Philippines but only
24
are active
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Taal Volcano
is known as the
smallest active
volcano in the world
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Taal
erupted for the first time in
1572
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Mount Mayon is known for its
steep-sloped
cone
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7 Major Tectonic Plates
Pacific
Plate
North American
Plate
Eurasian
Plate
Antarctic
Plate
Indo-Australian
Plate
South American
Plate
African
Plate
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Sections or parts of the earth’s crust
Constantly in
motion
&
collide
with other plates
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Tectonic Plates
The plates make up Earth's
outer
shell, called the
lithosphere
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Convergent Plate Boundaries
1. Plates go
towards
each other and
collide
2. Usually forms
mountain ranges
and
sea trenches
3. Occur when an
oceanic
plate dives beneath a
landmass
or subduction
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Divergent Plate Boundaries
1. Plates move
away
from each other
2. Causes
magma
to rise & solidify to form
oceanic
crust
3.
Earthquakes
are common in nearby areas
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Transform Plate Boundaries
1. Plates slide horizontally past each other
2.
Earthquakes
caused by rock breaking
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Himalayan
mountains are a product of a
convergent
boundary
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Alfred Wegener
discovered the
tectonic plates
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Types of Faults
Hanging
wall
Foot
wall
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Types of Faults
Strike-slip
Reverse
Normal
Oblique
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Plate
Boundaries
Related to types of
faults
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Types of Faults
Strike-slip
: sides horizontally slide past each other
Reverse
: hanging wall moves upwards
Normal
: hanging wall moves downwards
Oblique
: normal or reverse with horizontal motion
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Types of Faults
Reverse
Fault
Normal
Fault
Strike Slip
Fault
Oblique
Fault
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Plate Boundaries vs. Faults
Plate boundaries ARE
faults
There can be faults within
tectonic plates
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More than
10,000
earthquakes are recorded in the Philippines every
year
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There are
175
active faults in the
Philippines
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The biggest
fault
system in the
Philippines
is the Philippine fault zone (PFZ)
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Plate boundaries
are always
faults
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Faults
can exist within the
interiors
of plates
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There are more than
10,000
earthquakes recorded in the Philippines every
year
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The Philippines has
175
active faults
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