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Tectonic hazards
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E15 eruption
Geography > Tectonic hazards
14 cards
Cards (38)
Atmospheric hazards are driven by processes at work in the atmosphere eg:
air
Inner core
mostly
solid
made of
iron
and
nickel
slowly growing
Continental crust
granite
rocks
known as
sial layer
as well
over
1500
million years old
subducts
the
oceanic
crust
Primoridial
is the heat left over from the Earth’s formation
Radiogenic
is the heat produced from
radioactive decay
of
isotopes
Ridge push
is when new crust is formed due to
tension forces.
mantle rock
rises
and experiences a
reduction
in
pressure
Father of plate tectonic theory is
Alfred Wegner
Harry
Hess
updated the plate tectonic theory in
1962
Constructive plate boundary
plates moving away from each other
both plates are either
oceanic
or
continental
magma rises
- filling the
void
and creating new
crust
basaltic lava
fills the gap
oceanic ridges
made
Oceanic
ridges
:
formed from the
basaltic lava
that comes up
ridges can have
breaks
in them called
transform faults
these ridges and faults
wider
at different
rates
meaning there will be
frictional
stress
causing
earthquakes
higher
than other area - it is
buoyant
Collision plate boundary
usually
continental
and
continental
crusts need to be the same
density
two plates
collide
and
crumple upwards
forms fold
mountains
eg:
Himalayas
A
magma plume
is extremely hot magma that breaks through the oceanic crust and and cools to form a small volcano
the volcano gets
bigger
over time
it later becomes
extinct
as the plates moves
the volcano moves off the plate
boundary
and the
hot
spot
Extinct
volcanoes
sink
as they become
heavy
and they also become
smaller
due to
erosion
Tephra
fragments of
volcanic
rock and
lava
thrown into the air
Crater
main opening of the volcano
Pyroclastic
flow
(speeds of
50mph
)
rock fragments,
gases
and
ash
which
destroys everything
in its
path
Andesitic
lava:
viscous
high silica content
cooler
loses gas quickly
Caldera
volcanoes: (shield)
large
circular
/
oval
depressions
some filled with
lakes
often surrounded by
steep cliffs
formed by the
inward collapse
of a volcano
Vulcanian
volcanoes: (composite)
thick
lava
,
basaltic
/
andesitic
/
rhyolitic
less
frequent
,
violent eruptions
of
gases
Vesuvian
volcanoes: (composite)
thick lava,
basaltic
/
andesitic
/
rhyolitic
long periods of inactivity
very violet has
explosions
Peléan volanoes: (composite)
andesiitic
and
rhyolitic
violent eruptions
Plinian
volcanoes: (composite)
rhyolitic
-
viscous
, tend to form
thick blocky lava flows
violent
erupt gas
,
ash
and
pumice
rainstorms
cause
lahars
Evidence for
continetal drift
:
if the
continents
were
pieced
together
, they would
fit
almost
perfectly
fossil
remains - identically evolved repitle fossils found in both
South America
and
Africa
coal found in
Antartica
- coal needs
tropical climates
and
dense vegetation
Hawaiian volcanoes: (shield)
non-explosive
eruptions
generate
red hot lava
rivers -
basaltic lava
sloping
mountains
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