Chapter 18: Volcanic Activity Flashcards

1
Q

explain how magma forms. 3 factors

A
  • temperature hot enough to melt the rocks (800 to 1200)
  • pressure (temperature needed to melt increases with pressure)
  • water (rocks with water will melt at higher temperatures)
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2
Q

Basaltic Magma

A

when rocks in the mantle melt

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3
Q

Andestic Magma

A

continental margins where oceanic crust is subducted into the Earth’s mantle

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4
Q

Rhyolitic Magma

A

molten material that rises and mixes with overlying silica and water rich continental crust

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5
Q

pluton

A

intrusive igneous rock bodies made from minerals mixing

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6
Q

baolith

A

the largest plutons

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7
Q

laccolith

A

mushroom shaped pluton with round top and a flat bottom

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8
Q

sill

A

pluton that forms when magma intrudes paralell layers of rock

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9
Q

Dike

A

pluton that cuts across preexisting rocks

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10
Q

stocks

A

small-irregular shaped plutons

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11
Q

calderas

A

large volcanic depressions

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12
Q

shield volcano

A

mountain with broad, gently sloping sides and a nearly circular base.
ex. Hawaii Mauna Loa

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13
Q

Cinder Cone Volcanoes

A

small with steep sides. (no more than 500m)

ex. Izalco in El Salvador

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14
Q

Composite volcanoes

A

very large, lots of explosions, dangerous

ex. Mt St Helens

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15
Q

tephra

A

rock fragments thrown into the air during a volcanic eruption

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16
Q

pyroclastic flow

A

gas, ash, and other tephra flowing down a slope at incredibly high speeds. May contain hot, poisonous gasses.

17
Q

where do volcanoes form

A

plate boundaries (80 percent at convergent boundaries)

18
Q

convergent volcanism

A

convergence of oceanic plate creates seduction zones, places where slabs of oceanic crust descend into the mantle and eventually melt. The magma generated is forced upward through the overlying plate and forms volcanoes when it reaches the surface

19
Q

divergent volcanism

A

two plates move apart, magma is forced up through the fractures and faults that form as the plates separate

20
Q

hot spots

A

unusally hot regions of Earth’s mantle where high-temperature plumes of mantle material rise to the surface