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James Darbyshire
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Cards (6)
Classification of volcanoes by shape
Shield
Composite
(Stratovolcano)
Cinder
(ash)
Acid
(dome)
Caldera
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Composite (Stratovolcano)
Made of many
layers
of solidified lava and volcanic ash from different eruptions
Lava is
slow
flowing and
solidifies
quickly
Produces
steeply
sloping sides
Ash
occurs in explosive eruptions, often after the vent has become blocked with solidified lava
Occur at
converging
plate margins
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Cinder (ash) volcano
Gas
forces lava high into the air, where it
breaks
into small fragments
Fragments cool and fall as
cinders
Produces a
short
, symmetrical cone with relatively steep sides and a
crater
at the top
Often occur on the sides of
shield
or
composite
volcanoes
Many are formed from just one
eruption
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Acid
(dome) volcano
Viscous, acid lava erupts
effusively
but cannot flow far before
solidifying
Lava
builds up to form a
steep-sided
cone
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Caldera
Gases
trapped in a magma chamber eventually cause an extremely
explosive
eruption
The
upper
part of the volcano can be destroyed
The ground above the magma chamber can subside, leaving a large
depression
, which can eventually
flood
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Shield volcanoes
Effusive
eruption where large quantities of lava pour from a
central
vent
Lava travels
long
distances before
solidifying
Produces
tall
volcanoes with
gently
sloping sides
Eruptions tend to be
frequent
but not
explosive
Occur at
diverging
plate margins and
hotspots
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