Ch.5.less.3.how do volacones shape the land?

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How do volcanoes shape the land? Chapter 5: Lesson 3:

Transcript of Ch.5.less.3.how do volacones shape the land?

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How do volcanoes shape the

land?

Chapter 5: Lesson 3:

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Openings in earth’s crust.

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Volcanoes are located on certain places on earth’s surface.

(Found where tectonic plates meet)

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A circle of volcanoes (Ring of fire) follows the boundaries of plates that meet along the

pacific ocean.

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EruptionOutpouring of ash, gases, lava or a combination of these.

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Magma chamber

Inside a volcano

Vent

Vent

Smoke and ashes

Crater

Lava

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Crater(cup shaped depression)

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Volcanoes erupt where one plate is pushed under another.

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The hole that is formed when the chamber under the volcano is emptied

and the volcano collapses.

Caldera

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1) Dike(Formed when magma hardens in vertical or nearly

vertical cracks)

Underground magma formations

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2) Sill(Formed when magma hardens in horizontal layers

of rock)

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3) Laccolith(A dome shape formed when magma is pushed into

a sill and doesn’t spread) When a laccolith is formed it may push the layers of rock above it.

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4) Batholith(Huge, irregular shape deep in the earth’s crust)

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Active volcanoes(Currently erupting or

recently erupted)

Types of volcanoes

Dormant volcanoes

(Does not erupt for some time)

Shield volcano

es

Cinder-cone

volcanoes

Composite

volcanoes

Extinct volcanoes(Stopped erupting)

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1) Shield volcanoes

Built by thinner, fluid lava that spreads over a large area.

(Broad base and gently sloping sides)

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2) Cinder-cone volcanoes

Formed by thick lava that is thrown high up in the air and fall as chunks or cinders.

(Form as cone shape with narrow base and steep sides)

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3) Composite volcanoes

Built by layers of ash and cinders sandwiched between layers of hardened

lava.(Both sides of a composite volcano look the same)

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Active volcano not on boundary

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Hot spot (A stationary pool of magma)

The Hawaiian islands are form an island chain.The origin of the Hawaiian island volcanoes is the hot spot.

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Island arc(Formed in areas where an ocean floor plate is pushed under another ocean

floor plate.)