Plate Tectonics. Outline  Pangaea  Continental Drift  Mid-ocean ridges and seafloor spreading  Magnetic patterns on the seafloor  Plate tectonics:

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Presentation transcript:

Plate Tectonics

Outline  Pangaea  Continental Drift  Mid-ocean ridges and seafloor spreading  Magnetic patterns on the seafloor  Plate tectonics: map of plates and theory  Plate boundaries

Pangaea  Means “all lands”  Name given to the single landmass composed of all the continents  Idea developed by Wegener  Pangaea broke apart into 7 continents (200 MYA): Continental drift

Continental Drift: Evidence  Fossils  Rock type  Paleoclimates  Fit of coastlines  Structural similarities

Rock Type

Paleoclimate

Rejection of the theory  Continental drift was not accepted initially  Wegener believed that continents moved through the ocean: FALSE  Continents and oceans actually move together!  Wegener could not explain WHY the plates move

Mid-ocean ridges  Mid-ocean ridges discovered in early 1960s  Mountain ranges on the ocean floor  Discovered using echo sounders

Mid-Atlantic Ridge

Seafloor spreading  Seafloor spreading occurs at MORs  Sea floor on either side of the ridge pushed away by rising magma from the mantle

Magnetic patterns on the seafloor  Earth’s magnetic polarity reverses  The magnetism is trapped in the rocks at the spreading center when rocks cool  Creates a pattern on the seafloor

Plates are pieces of the lithosphere

Putting it all together  Magnetic patterns  Seafloor spreading  Continental drift  Lithosphere divided into plates

How does it happen?

Types of boundaries

Why is this important?  Most geologic activity occurs at plate boundaries  Volcanoes, earthquakes, tsunamis