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Geography - A Level
Hazardous Earth - A Level
Types of Volcano
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Created by
Freya Snaith
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Cards (31)
Volcanicity
All volcanic activities related to magma being forced into the crust, usually at
plate margins
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Magma at high temperatures and pressures
1. Exploits
weaknesses
in the
crust
2. May
erupt
to the surface as
lava
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Types of volcanoes
Active
Dormant
Extinct
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Active volcano
An
eruption
is currently ongoing
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Dormant
volcano
Not erupted in the last
10,000
years
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Extinct volcano
Not going to
erupt
again
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Methods of categorising volcanoes
Shape
of volcano
Nature
of the eruption
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Volcano shapes based on lava type
Basaltic
Andesitic
Rhyolitic
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Basaltic
lava
45
% silica content
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Andesitic lava
52% silica content
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Rhyolitic
lava
66-75
% silica content
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Fissure
volcano
Occur at
divergent
plate boundaries
Lava
can be ejected through fissures rather than a
central
vent
Lava
tends to
form
large plateaus, filling in hollows rather than building up
Basaltic
lava
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Fissure
volcano
Laki Fissure system
,
Iceland
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Acid
/
dome
volcano
Acid
lava solidifies on exposure to
air
Produces a
steep
sided,
convex
cone
Lava
solidifies as it comes up the vent and produces a
spine
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Acid
/
dome
volcano
Mt Pelee
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Basic/shield volcano
Often occur at
divergent
plate margins or
hot
spots
Lava flows out of a
central vent
and spreads over wide areas before
solidifying
Cone with long,
gentle
sides made up of many
layers
of lava
Runny
basaltic
lava
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Basic/shield volcano
Mauna Loa
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Composite volcano
Classically shaped volcanoes from alternating
ash
and
lava
eruptions
Found at
convergent
boundaries
May have
violent
eruptions followed by more
gentle
ones
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Composite volcano
Mt Etna
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Ash
/
Cinder cone volcano
Ash or cinder builds into a symmetrical cone
Often found at the
bottom
of
shield
volcanoes and calderas
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Ash/Cinder cone volcano
Paracutin
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Caldera
Build up of
gases
causes huge explosions that clear the
magma
chamber and allow the sides to collapse inwards
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Caldera
Krakatoa
, Yellowstone,
Flangerian Fields
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Icelandic
eruption
Persistent eruption along a fissure
Large quantities of
basaltic
lava build up vast
horizontal
plains
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Icelandic
eruption
Deccan Plateau
,
Columbian Plateau
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Hawaiian
eruption
More noticeable central activity than
Icelandic
Runny
basaltic
lava travels down the sides in flows
Low silica
content
Gases
escape easily
Can form
fire fountains
Occasional
pyroclastic
activity
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Strombolian
eruption
Frequent gas explosions blast fragments of
runny lava
into the
air
Smallest
type of
explosive
eruption
Eject short bursts of lava
15-90m
into the
air
Eruptions marked by
white steam cloud
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Vulcanian eruption
Violent gas explosions blast out
plugs
of
sticky
or cooled lava
Fragments build up into cones of
ash
and
pumice
Occurs when
viscous
lava solidifies rapidly after an explosion
Often clears a blocked
vent
and spews
ash
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Vesuvian eruption
Powerful blasts of gas push
ash clouds
high into the sky
More
violent
than Vulcanian
Lava flows and
ash
falls cover surrounding areas
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Plinian eruption
Most
explosive
and
violent
volcanic eruptions
Magma
has high
silica
content
Gas rushes up through
sticky
lava and blasts
ash
and fragments into the sky
Creates immense clouds of
gas
and
volcanic debris
Part of the volcano may be
blasted
away
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Plinian eruptions are named after
Pliny
the
Younger
who wrote about the 79AD eruption of Mt Vesuvius
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