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Published byBryan Melton Modified over 9 years ago
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Alfred Wegener 1880-1930
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How Wegener Proved His theory Continental Fit Matching Fossils Matching Mountains Sea Floor Age
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Mesosaurus
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Describe what is happening in this photograph. Time Two countries Plate movements Everest
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What causes plates to move Caused by thermal convection currents 1. Hot rock moves like tar 2. Hot interior of the earth
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Types of plate margins Divergent – constructive Plates pull apart Hot magma released to the surface New oceans can form – mid atlantic ridge Continents pull apart at 2.5 cm per year.
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Types of plate margins Convergent - Destruction of Crust When two plates collide, one plate travels beneath another. This is known as subduction
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Types of Convergent Plates Oceanic – Cceanic Convergence Oceanic - Continental Convergence Continental – Continental Convergence
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Oceanic – Oceanic Plates The smaller plate slips below the thicker plate A Trench forms where the plate subducts Example – The Mariana Trench where the Pacific and Phillipines plates collide
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Oceanic – Continental Plates The oceanic crust is heavier and sinks beneath the continental crust The continental plate deforms forming a mountain range Exampe Nazca Plate and South American Plate converge to form the Andes
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Andes Mountains Oceanic – Continental Plate Convergence
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Continental - Continental The two plates are very light Neither plate subducts They fold upwards to form a mountain range Example the Indian Plate and the Eurasian Plate began to form the Himalayas 50 million years ago
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Red Sea
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Africa Pulling Apart. Separating Plates form the Agen and the Red Seas
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