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Published byCory Black Modified over 8 years ago
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“Weak sphere” Layer that is involved in mantle convection
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Asthenosphere
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Line where it is hot enough below to flow and is cool and rigid above
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Boundary between lithosphere and asthenosphere
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Thick, less dense, and older
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Continental crust
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Boundary where plates are moving toward one another
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Convergent Boundary
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Example of a transform boundary
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San Andreas Fault
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Collision zone where subduction is active, earthquakes and volcanoes are possible
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Subduction Continent-Oceanic collision
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Large forces build up within the lithosphere, forces become greater than the strength of the rock thus fracturing.
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Fault
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A place where molten rock, solid fragments and gases erupt at the Earth’s surface
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Volcanoes
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Mild Eruption
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Magma with low gas content
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Magma pockets in the mantle that do not move. Ocean plates move. Occur far from plate boundaries.
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Hot spot volcano
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Formed when 2 continental crusts collided. Still forming. No subduction.
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Himalayan mountains
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Rigid outer portion of the Earth. Composed of crust and the outer part of the mantle.
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Lithosphere
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Thin, more dense, and younger.
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Oceanic crust
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Boundary where plates are moving away from each other
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Divergent Boundary
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Boundary where plates are sliding past one another (very slow).
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Transform Boundary
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Area where plates are consumed (melted and recycled); one plate dives down underneath the other into the mantle.
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Subduction
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Collision zone where there is no subduction and mountains are formed.
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Continent-continent collision
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Fracture in the Earth’s surface
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Fault
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Explosive eruption
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Magma with high gas content
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Volcanic rock found along the Mid-Ocean Ridges
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Basalt
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Pacific Ocean rimmed with subduction zones. Earthquakes and volcanoes are common.
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Ring of fire
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A continuous mountain range extending throughout the ocean. It is seismically active and often has a rift valley. Divergent plate boundaries. Site of sea-floor spreading.
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Mid-ocean ridge
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