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Published byWesley Thornton Modified over 9 years ago
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III. Plate Boundaries A. Transform B. Divergent C. Convergent
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III.Plate Boundaries A. Transform Two plates slide past each other and transform surface features Two plates slide past each other and transform surface features ex. San Andreas Fault ex. San Andreas Fault
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III.Plate Boundaries B. Divergent Two plates move away from each other Two plates move away from each other As they separate, magma rises to fill the gap As they separate, magma rises to fill the gap
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III.Plate Boundaries B. Divergent Features: Features: Midoceanic ridge Midoceanic ridge Rift valley Rift valley Seafloor spreading Seafloor spreading Surtsey Island Surtsey Island Iceland’s Hot Springs Iceland’s Hot Springs
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midoceanic ridge, sea floor spreading, rift valley
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The Great Rift Valley in Eastern Africa
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Surtsey Island, near Iceland…born in 1963
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Now it has life...
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Hot Springs in Iceland….Blue Lagoon
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III.Plate Boundaries C. Convergent Two plates approach each other Two plates approach each other 1. Continental – Continental formed Himalayas
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III.Plate Boundaries C. Convergent 2. Continental – Oceanic aka subduction zone oceanic crust dives below continental crust Trenches Trenches Mountains Mountains Volcanoes Volcanoes
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III.Plate Boundaries C. Convergent 3. Oceanic – Oceanic trenches (Marianis and Challenger Deep) trenches (Marianis and Challenger Deep) Undersea Volcanoes, aka “seamount” Undersea Volcanoes, aka “seamount” Island Arcs Island Arcs
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Undersea Volcanoes can form islands over many years of eruption Undersea Volcanoes can form islands over many years of eruption Mauna Loa and Kilauea are volcanoes on the island of Hawaii. They were once seamounts. Loihi is an undersea volcano off the southern coast of Hawaii…someday it will be an island
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Hawaii was formed as a series of volcanoes
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