Plate Tectonics And Continental Drift. Early Evidence for Continental Drift.
Warm UP 12 / 03/ 12 Give the three sources of evidence to support the theory of Continental Drift.
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Transcript of Warm UP 12 / 03/ 12 Give the three sources of evidence to support the theory of Continental Drift.
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Warm UP12 / 03/ 12•Give the three sources of evidence to support the theory of Continental Drift
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Tectonic Plates have boundaries
3 Types of Boundaries1.Divergent boundaries2.Convergent boundaries3.Transform boundaries
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DIVERGENT BOUNDARIES
Occurs where plates move apart
Most of these boundaries are found in the oceans
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CONVERGENT BOUNDARIES
Occurs where plates push together
Can be Oceanic to Oceanic, Oceanic to Continental, and Continental to Continental
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CONTINENTAL – CONTENENTAL COLLISION
• Occurs where two plates carrying continental crust push together.
• Both crusts are the same density.• This collision forms Mountain Ranges
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Oceanic-Oceanic Subduction• Subduction – when one plate sinks beneath
another• This occus where one plate with oceanic crust
sinks, under another plate with oceanic crust• Forms deep ocean trenches and island arcs
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Oceanic – Continental Subduction
• Occurs when ocean crust sinks under continental crust
• Forms deep-ocean trenches and coastal mountains
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TRANSFORM BOUNDARIES
• Occurs where plates scrape past each other• Occurs mostly on the sea
floors near mid-ocean ridges• Example of one on land is the
San Andreas Fault in California
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