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These volcanoes tend to be small, with relatively steep sides, but not particularly tall. They form when the shattered rock of the mountain accumulates in layers.
False
Pyroclastic Flow
Composite
Vent
Composite
Cinder Cone
Caldera
Dormant
Hot gases, rock pieces, crystals, glass, pumice, etc., that is ejected from a volcano at immense speeds
False
Pyroclastic Flow
Composite
Vent
Composite
Cinder Cone
Caldera
Dormant
The largest type of volcano in height. These volcanoes have very loud, large explosions.
False
Pyroclastic Flow
Composite
Vent
Composite
Cinder Cone
Caldera
Dormant
Main path for magma to travel out of a volcano from underground.
False
Pyroclastic Flow
Composite
Vent
Composite
Cinder Cone
Caldera
Dormant
Volcanoes only result in destruction, and there are never any positive results of a volcanic eruption.
False
Pyroclastic Flow
Composite
Vent
Composite
Cinder Cone
Caldera
Dormant
These volcanoes form from alternating layers of pyroclastic materials and lava. They tend to be very steep and massive.
False
Pyroclastic Flow
Composite
Vent
Composite
Cinder Cone
Caldera
Dormant
This is a hole left by the collapse of a volcanic mountain.
False
Pyroclastic Flow
Composite
Vent
Composite
Cinder Cone
Caldera
Dormant
A volcano that is sleeping, but will wake up at some point.
False
Pyroclastic Flow
Composite
Vent
Composite
Cinder Cone
Caldera
Dormant
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