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30 Cards in this Set

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  • Back
volcano
A weak spot in the crust where molten material, or magma comes to the surface
Magma
A mixture of rock-forming, gases, and water from the mantle
Ring of Fire
A belt of volcanoes that rim the Pacific Ocean
Where do volcanoes form?
1. Converging Plate Boundaries
2. Diverging Plate Boundaries
3. Hot Spots
Converging Plate Boundaries
2 Types:
1. Oceanic-Ocanic Crust
2. Oceanic-Continental Crust

Both form when one plate (denser) gets subducted or pushed down into the mantle creating a DEEP OCEAN TRENCH.
The subducted plate melts

Forms magma

Rises to the surface form a volcano.

May form an island arc

Example: Andes Mountains in S. America
Cascade Mountains in Washington USA (Mt. St. Helens)
Diverging Plate Boundaries
At MID OCEAN RIDGE

The ocean floor pulls apart

Lava pours out of the cracks and hardens forming new crust.

Example: Iceland & Azors Islands
Hot Spots
An area where magma from deep within the mantle melts through the crust like a blow torch.

The magma hardens underwater

gradually new layers harden on top of old layers creating a volcanic island

As the plate slowly moves on top of the hot spot, new volcanoes form.

Example: Hawaiian Islands
Island Arc
A chain of volcanic islands
How does magma reach the surface?
Liquid magma rises from the mantle because it is less dense than the surrounding rock

Gasses inside magma are dissolved. Pressure builds inside the volcano, and eventually it explodes
Crater
A bowl shaped area that forms the top of a volcano around a volcano's vent
Vent
an opening through which molten rock and gas leave the volcano
Magma chamber
Area where magma collects beneath a volcano
2 types of volcanic eruptions
1. Quiet Eruptions
2. Explosive Eruptions
Quiet Eruptions
When lava oozes slowly from the vent. Happens when magma is able to move slowly and freely.

Example: Composite Volcanoes
Shield Volcanoes have quiet eruptions
Quiet Eruptions produce 2 types of lava
1. Pahoehoe
2. Aa
Pahoehoe Lava
FAST moving HOT lava
Aa Lava
SLOWER moving COOLER lava
Explosive Eruptions
When magma is thick

Does not flow out of the crater easily.

Pressure builds inside the volcano because the gasses cannot escape.

Example: Cinder Cone Volcanoes & Composite Volcanoes have explosive eruptions
Pyroclastic flow
When a volcano hurls out ash, cinders, bombs, and gasses at hundreds of miles an hour.
3 Stages of a volcano
1. Active
2. Dormant
3. Extinct
Active
A volcano that IS ERUPTING or shows signs that it MAY ERUPT IN the FUTURE
Dormant
A volcano that is NOT ERUPTING currently, but MAY and erupt in the future
Extinct
A volcano that is NEVER to erupt again
3 Types of Volcanoes
1. Shield
2. Cinder Cone
3. Composite
Shield Volcano
Forms when repeated lava flows gradually during quiet eruptions

Gradually build up a broad, gently sloping volcanic mountain

Example: Hawaiian Islands
Cinder Cone Volcano
Steep, cone-shaped hill or mountain formed when volcanic ash cinders & bombs erupt explosively falling around the vent in a cone-shaped pile.

Example: Sunset Crater in Arizona
Composite Volcano
Tall, cone-shaped mountains

Layers of lava alternate with layers of ash

Has quiet & explosive eruptions
example: Mt. St. Helens in Washington, Mt. Fuji in Japan
Example: Mt. St. Helens in Washington
Mt. Fuji in Japan
Caldera
Huge hole left by the collapse of a volcanic mountain, due to an enormous eruption
How does a Caldera form?
Volcano erupts all magma from the main vent and magma chamber beneath the volcano

Leaves behind a hollow shell

With nothing to support it, the top to the magma chamber collapses inward
Lava
Magma that reaches the Earth's surface