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Published byClaribel Ford Modified over 8 years ago
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ASTHENOSPHERE: An area of earth’s upper mantle that has a low density and partially melted rock material
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LITHOSPHERE: The outer portion of earth that includes the crust and upper mantle
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Continental Drift: A theory that states that the continents have drifted from one location to another over time Wegner: The scientist who came up with this hypothesis.
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Wegener’s support to his hypothesis: a. Coasts of continents fit like puzzle pieces b. Fossil remains found on two separate continents c. Rock formations found on different continents would match up d. Climate change evidence.
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Earth’s lithosphere is broken into plates that move on the asthenosphere Plate Tectonics: A theory that describes the formation, movements and interactions of these plates
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Support: Data about earthquakes, magnetism, the age of rocks on the ocean floor, some of Wegner’s findings As the plates move, the continents move.
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Most locations of earthquakes and volcanoes = Location of plate boundaries
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Magnetic minerals in magma orient themselves to face the magnetic pole as the magma solidifies Magnetic pole has reversed several times in the geologic past We have a record of age and pole switches
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Mid-Ocean Ridge: long chain of volcanic mountains on the ocean floor As new rocks rise in the middle as magma, it forces older rocks out to the side
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