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Krishan Gautama
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Cards (20)
Earth's layers
Inner and outer core
Mantle
Crust
Crust
Thinnest
layer
Two types:
Oceanic
(thin, dense, basaltic) and
Continental
(thicker, lighter, granite)
Core
Centre of the
Earth
Very
hot
and
dense
Outer core: Hot, made of
iron
and
nickel
Inner core: Hotter, solid ball of
iron
and
nickel
Lithosphere and Asthenosphere
Lithosphere: Crust and top layer of
mantle
, broken into
tectonic plates
Asthenosphere
: Denser, more mobile layer in upper mantle, allows
plate movement
Mantle
Thickest
layer
Temperature
ranges from 1000°C to 3,700°C
Upper mantle is mostly
solid
,
slow
moving
Lower mantle is
solid
,
hotter
and denser
What drives movement in the mantle?
Convection currents
: Rock
heated
in lower mantle rises, cools and sinks back down
Tectonic plates
Large areas of rock that make up
Earth's crust
, float on asthenosphere and are moved by
convection currents
Types of plate boundaries
Convergent
(oceanic-continental, continental-continental)
Divergent
Conservative
Convergent (oceanic-continental)
Oceanic plate
subducts
beneath
continental
plate
Melting of subducted crust creates
magma
and
volcanoes
Convergent (continental-continental)
No subduction, collision causes
folding
and faulting to form
mountains
No
volcanism
, but major
earthquakes
occur
Divergent
Plates
move apart,
asthenosphere
melts to form new crust
Shield volcanoes
and
rift valleys
form
Conservative
Plates
slide
past each other, causing
earthquakes
when they get stuck
Composite volcano
Tall,
steep-sided
, made of alternating ash and
lava
layers
Andesitic lava is viscous, eruptions are
infrequent
but
violent
Shield volcano
Gently sloping dome, made of fluid
basaltic
lava
Eruptions are
frequent
and
gentle
Hotspot volcano
Formed away from plate boundaries by a plume of
superheated
rock rising through the
mantle
Earthquake
Sudden
vibrations
in Earth's
crust
caused by rock fracturing along a fault
Energy
is released in the form of seismic waves radiating from the
focus
Earthquake impacts
Depend on magnitude,
depth
,
time
of day, population density, preparedness
Earthquake measurement
Richter
scale (logarithmic) and
Moment
Magnitude Scale (wider range, more accurate)
Tsunami
Series of giant ocean waves triggered by
seafloor
displacement from an
earthquake
Waves move fast in deep water,
slow
but
increase
in height near coasts
Earthquake/volcano preparedness methods
Seismometers
Hazard
maps
Satellite
monitoring
Tiltmeters
Earthquake-proof
building design
Public
education
Emergency services
preparation