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Science 4th quarterly
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Lexy Batak Maggizmo
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Cards (131)
Crust
Earth's
outermost
layer
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Oceanic
crust
Relatively
thin
compared to the crust below the
continents
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Continental
crust
Made up of
lighter
, less dense
granite
rocks
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Mantle
A layer of rock materials between the
crust
and the
core
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Mohorovicic
discontinuity or Moho
Marks the boundary between the
crust
and the
mantle
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Discontinuity
The interphase of
two
layers, marked by the sudden change of density of the
rock
layers
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Core
Located at the
Earth's
center
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Layers of the core
Inner core
Outer core
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Inner core
Believed to be made up of solid iron, responsible for
Earth's magnetic field
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Outer core
Thought to be composed of liquid iron-nickel alloy due to extremely high temperature
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The deepest hole drilled only went
13km
deep
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Continental Drift Theory
Theory by
Alfred Wegener
that the world's continents were once part of a single landmass called Pangaea
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Pangaea
likely began to split around 200 million years ago, and have continued to move to where they are now
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Plate Tectonic Theory
Earth's solid, brittle lithosphere is broken into several
tectonic plates
that glide over the partially molten asthenosphere
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Boundary
The place where
two plates
meet
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Types of plate boundaries
Divergent
Transform
Subduction
or
Convergent
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Divergent Boundary
Formed between
two plates
that are moving
away
from each other
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Transform Boundary
Also called
conservative plate boundaries
, formed between
two plates
that are moving horizontally past each other
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The
San Andreas
is the most popular
transform
boundary
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Convergent Boundary
Formed where
two
plates
converge
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Earthquake
The
shaking
of the ground due to the sudden movement of
Earth's lithospheric plates
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Types of earthquakes
Tectonic
earthquake
Volcanic
earthquake
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Focus
The point
underneath
the epicenter where the
displacement
of rocks originated
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Epicenter
The point on the surface of
Earth
directly above where the
displacement
of rocks originated
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Fault
Zones of
fracture
where large blocks of
rocks
move relative to each other
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Types of faults
Normal
fault
Strike-slip
fault
Reverse
fault
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Main earthquake zones
Circum-Pacific Belt
Alpide Belt
Mid-Atlantic Ridge
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Circum-Pacific Belt
Also called the
Ring of Fire
due to the large number of
active volcanoes
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Alpide Belt
Extends from Java to Sumatra, through the
Himalayas
, the Middle East, the Mediterranean, and out into the
Atlantic
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Mid-Atlantic
Ridge
Consists mostly of an
underwater mountain
range
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Intensity of an earthquake
Measure of the
damage
incurred on the
surface
and its perceived effects
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Richter
Scale
Measures the
magnitude
of earthquakes
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Instruments used to
detect earthquakes
Seismograph
Laser
rangefinder
Geiger
counter
Extensometer
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An
earthquake
can cause excessive damage to properties in towns and cities, including building and structure collapse, cracks and gaps in the ground, landslides, and tsunamis
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What to do before, during, and after an earthquake
1. Before:
Prepare emergency plans
and
supplies
2. During: Stay calm, take cover, avoid falling objects, move to
higher ground
if near
water
3. After: Check for
damage
, assist others, make
repairs
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Magma
The molten rock that collects in compartments also known as
magma chambers
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Caldera
When volcanoes deplete the magma within their chambers, the volcano may collapse on itself, creating a large, basin-shaped volcanic opening
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Parts of a volcano
Vent
Pipe
Crater
Cone
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Signs of impending volcanic eruption
Bulging
sides
Earthquakes
Gaseous
fumes
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Types of volcanic eruptions
Effusive
eruption
Explosive
eruption
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See all 131 cards
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