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GEOGRPAHY
TECTONIC
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Cards (100)
Hazard
Potential threat to human
life
and
property
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Natural
Hazard
Threat caused by
climatic
or
land
processes
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Geophysical Hazard
Threat caused by land processes
near plate boundaries
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Intraplate
Earthquake
Earthquake occurring
away
from plate boundaries
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Volcanic Hotspots
Localized areas with
high
temperature due to
molten
material
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Magma
Hot
rock rising at
volcanic
hotspots
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Convergent
Boundaries
Locations where most powerful
earthquakes
occur
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OFZ
(
Oceanic Fracture Zone
)
Belt
of activity through oceans and along
mid-ocean
ridges
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CFZ
(Continental Fracture Zone)
Belt
of activity along mountain ranges from Spain to
Himalayas
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Recorded
Hazards
Total number of documented hazards
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Fatalities
Number of
deaths
resulting from
hazards
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Mega
Disasters
Events with significant
spikes
in
fatalities
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Insurance
Policies
Contracts that
mitigate
economic costs of
disasters
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Direct
Deaths
Immediate
fatalities
from a disaster
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Indirect Deaths
Fatalities
due to
post-disaster
effects
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Tectonic
Theory
Study of Earth's lithosphere movements
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Crust
Earth's
thinnest
,
least
dense outer layer
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Mantle
Layer
below
crust, semi-molten with
convection currents
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Outer
Core
Dense, semi-molten layer containing
iron
and
nickel
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Inner
Core
Solid layer below
outer
core, high pressure and
temperature
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Destructive
Plate Boundary
Plates where one
subducts
below the other
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Ocean Trench
Deep
trench formed by
subducting
oceanic plate
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Composite Volcanoes
Volcanoes formed through
explosive
eruptions
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Fold
Mountains
Mountains formed by plate
subduction
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Constructive
Plate Boundary
Plates
moving apart, forming new
land
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Sea
Floor Spreading
Formation of new
land
on ocean floor by
magma
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Fault lines
Cracks in the ground on
continental
crust caused by
movement
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Oceanic
crust
Low-density
rock, mainly
basalt
, thin, and newly created
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Continental crust
High-density rock, mainly
granite
, thick, and
old
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Density
Determines plate
subduction
or forced
uplift
, impacting landscape and hazards
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Mantle Convection
Radioactive decay in
Earth's
core produces thermal energy, creating
convection
currents
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Slab
Pull
Old, dense oceanic crust
submerges
into the mantle, pulling the
plate
with it
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Convection
currents
Previously thought primary cause of plate
movement
, now considered
weaker
than Slab Pull
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Earthquakes
Sudden release of
pressure
between
stuck plates
, causing seismic waves
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Focus
(hypocentre)
Point
underground
where
earthquake
originates
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Epicentre
Area directly above the
focus
on the ground
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Primary waves
Travels through solids,
compressional
,
vibrates
in travel direction
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Secondary
waves
Vibrates
perpendicular
to travel direction,
travels through solid rocks
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Love
waves
Near
surface, rolling motion,
vertical
ground movement
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Rayleigh
waves
Vertical
and horizontal displacement,
slower
than other waves
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See all 100 cards
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