This type of volcano tends to be very wide at the base, but short. It is formed by quick-moving lava flows that cool rapdily.

These volcanoes form from alternating layers of pyroclastic materials and lava. They tend to be very steep and massive.

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.

A volcano that is awake

A volcano that is sleeping, but will wake up at some point.

A volcano that is sleeping forever.

Main path for magma to travel out of a volcano from underground.

Location underground where magma is stored

Steep indentation at the top of a volcano

Tiny, pulverized rock fragments

Hot gases, rock pieces, crystals, glass, pumice, etc., that is ejected from a volcano at immense speeds

Molten rock above Earth's surface

Volcanoes only result in destruction, and there are never any positive results of a volcanic eruption.

The largest type of volcano in height. These volcanoes have very loud, large explosions.

This type of volcano has very quiet eruptions and the lava flows quickly.

This is a hole left by the collapse of a volcanic mountain.

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