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Plate Tectonics.

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Presentation on theme: "Plate Tectonics."— Presentation transcript:

1 Plate Tectonics

2 Alfred Wegener German Scientist
Ph.D in astronomy, interested in meteorology and climatology Served in German Army weather service Proposed supercontinent Pangea separated 200 mya Found paper in library that listed fossils of identical animals and plants across the Atlantic

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4 Evidence for his theory
1) Similar coastlines (jigsaw puzzle)

5 Evidence for his theory
2) Identical fossils along joining coasts Ex. South America and Africa

6 Evidence for his theory
3) Identical age and rock types along joining coasts Ex. Brazil and West Africa 4) Similar mountain chains across joining coasts Ex. Appalachians and mountains in Scotland and Northern Europe 5) Climactic changes in geologic record Pangea over south pole = glaciers in South Africa and South America Tropic or subtropic swamps in NA = coal deposits in WV and WY

7 Wegener’s Problem No mechanism to cause continental drift
Proposed continents were moving through the ocean’s crust by centrifugal and tidal forces If so, continents would be deformed There isn’t enough force from either to move continents His theory was not accepted until after his death

8 Later Support 6) Sea floor spreading
Found young rocks along Mid-Atlantic ridge in 1947 Ridge is a break in Earth’s crust Ocean floor is separating and new crust is forming Ocean floor moving = continents moving Animation:

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11 Later Support 7) Paleomagnetism Earth as a giant magnet
Arrangement of minerals along mid-ocean ridges Bands of rock oriented toward N or S pole Dating rocks supports EM reversals in the past His hypothesis was fully supported

12 Plate Tectonics Continental crusts and oceanic crust
Lithosphere – crust and upper mantle -The lithospheric plates float on the asthenosphere, carrying the continents with them There are 8 large plates and 9 small plates Some are moving towards each other, some away and some are sliding past each other This movement has made most major surface features on the earth Ex. Mountains ranges, trenches

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15 Plate Boundaries 3 Types Divergent Convergent Transform

16 Divergent Where plates move in opposite directions
Sea floor spreading (ocean ridges) Creates Rift Zones, on land they’re called rift valleys Asthenosphere rises to take up the space Ex. Mid-Atlantic ridge; Rift Valley, Africa

17 Divergent Boundary

18 Convergent Boundaries
Where two plates are colliding Located on the opposite side of plates from divergent boundaries 3 Types Oceanic – Continental Continental – Continental Oceanic – Oceanic

19 Oceanic - Continental Creates a Subduction Zone
Oceanic crust is denser and pushed beneath continental crust (subduction) Forms a trench Oceanic crust heats up, releases water, and causes the mantle to melt Magma produced then rises and forms volcanic mountains Ex. Andes Mountains, South America

20 Subduction Zone 

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22 Continental - Continental
Plates have same density, so neither is subducted Are crumpled and uplifted Forms mountains Ex. Himalayas

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25 Oceanic - Oceanic One plate is subducted Forms a trench
Subducted oceanic crust melts, releases water and causes magma to rise and make a chain of volcanic islands (Island Arc)

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27 Transform Boundaries Where plates slide past one another
Grind as they pass each other in short quick movements, causing earth quakes Ex. San Andreas Fault, CA

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30 Carrizo Plain, CA (san Andrea Fault)

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32 Causes for plate motion
Convection Seen in boiling water Movement of material due to temperature differences Act like conveyor belts that the plates ride on

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34 Microplate Terranes (Suspect Terranes)
Continents made of a variety of lithospheric chunks, each with a different geologic history

35 Theory of Continental Drift
Alfred Wegener (German Scientist) Proposed hypothesis that all the continents were once part of one large land mass called Pangaea (all lands) 200 MYA they started to separate and have led to the world we see today

36 Evidence Coastlines fit together like a jigsaw
Identical fossils found along joining coasts Ex. South American and Africa Age and rock types along joining coasts Ex. Brazil and West Africa Similar mountain chains Appalachians and mountains in Scotland and Northern Europe Climactic changes seen in the geologic record Thought that Pangaea was once positioned over the South Pole Ex. Glaciers in southern Africa and South America, Coal deposits in North America (land was once covered with tropical or subtropical swamps)

37 http://upload. wikimedia

38 Seafloor Spreading Areas along sea floor where plates are separating
Cause a underwater mountain range Actually is a rift, or break in the crust New magma rises to fill the gap Mid-Atlantic Ridge

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40 Paleomagnetism Earth is one giant magnet
As minerals rise and solidify in crust, they orient themselves toward the N pole Found rock bands along these ridges that were oriented toward the S pole Suggests that the Earth’s magnetic poles have switched throughout history

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43 Sources http://www.platetectonics.com/book/images/Pangaea.gif


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