The Moving Continents An Introduction to Plate Tectonics.

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Presentation transcript:

The Moving Continents An Introduction to Plate Tectonics

The Theory of Plate Tectonics l Suggests that the crust is broken into sections called plates l Plates move about the earth l Boundaries of plates are considered faults

Alfred Wegener l First person to suggest the Theory of Continental Drift in 1910 l His hypothesis was that all the continents had once been joined together in a single landmass and have drifted apart. l Science community rejected his theory because of lack of support l Published a book giving support for his theory in 1915

Evidence for Continental Drift: l Same type of fossils found on four different continents l Folded mountains on Africa and South America l Glacial deposits on different continents that should not have l Coal beds in areas that normally would not form, Michigan for example

Why do the plates move? l Convection in the mantle –The heating and cooling of the fluid, –changes in the fluid’s density, and –the force of gravity combine to set convection currents in motion

Words to define l Faults l Mantle l Convection l Core l Crust l Molten l Folded mountains l Hot spots l Earthquakes l Volcanoes

Technology and the Earth’s Changing Surface l Surface mining l Urban development l Farming l Dams l Landfills l Restoring marshlands l Reclaiming spoiled lands

Geological Time l Sedimentary Rocks and Fossils are used to determine the age and geological history of the earth l Rock layers fossils l Relative dating l Petoskey stones

Evolution l Geological time l Fossil l Bone l Embryo l limb