Theory of Plate Tectonics (1960)williamsee.weebly.com/uploads/2/1/7/5/21759218/plate... · 2019....

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Theory of Plate Tectonics (1960) Earth’s lithosphere consists of rigid, but moving masses called tectonic plates

Transcript of Theory of Plate Tectonics (1960)williamsee.weebly.com/uploads/2/1/7/5/21759218/plate... · 2019....

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Theory of Plate Tectonics (1960)

Earth’s lithosphere

consists of rigid, but moving masses called

tectonic plates

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Tectonic Plates

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Lithosphere Outer shell of Earth that is

made of rigid crust and upper mantle

• Broken into moving

tectonic plates

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2 Types of Lithosphere Oceanic Crust

Made up of the ocean floor

Continental Crust

Made up of continental landmasses.

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Oceanic Crust vs. Continental Crust

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CONVECTION

How do the plates move?!

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Convection currents

• Unequal heating from the Earth’s core causes hotter magma to rise and cooler magma to sink down towards the core and heat up

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Plate Boundaries

There are 3 main ways that the plates

interact.

Points of interaction are called boundaries

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3 Types of Plate

Boundaries…

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1. Divergent Boundaries Where two plates are

moving apart,

magma rises and fills space between plates creating new

crust as it cools

CRUST IS GAINED

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Divergent boundaries

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2.Transform Boundaries

• Plates horizontally slide past one another

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3. Convergent Boundaries

When two plates collide

CRUST IS LOST

•There are 3 types….

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1. Continental + Oceanic Convergence=

SUBDUCTION ZONE

• When an oceanic plate collides with a continental plate

• One plate subducts under the other forming a trench

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SUBDUCTION ZONE

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2. Cont. + Cont. Convergence

• Two continental plates collide

• The plates crumple and uplift

• Form folded mountain ranges

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2. Cont. + Cont. Convergence

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3. Oceanic to Oceanic Convergence

• Trenches form as one plate subducts and melts

• Magma rises to the surface along the trench and slowly forms an island chain called an ISLAND ARC

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SUBDUCTION ZONE

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1. Divergent boundaries

• 1. Mid-ocean ridges: Underwater mountain range

that winds throughout the

Earth’s oceans. It is the 40,000

miles long

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New Crust Forms Here As Crust is Pulled Apart

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2. Rift Valley: When the crust is pulled or ‘rifted’ apart, valleys form with steep walls

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Transform Boundaries

Earthquakes occur when

stress is too great from plates sliding, causing fracture to form in the crust

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Example: San

Andreas Fault

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Boundary Features

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1. Volcanoes

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Volcanoes Subduction and its

resulting gas chemical reactions, causes hot lava, ash and gas to

return to the atmosphere

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2. Island Arc

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Island Arc

Magma rises to the surface along the trench and slowly forms an island

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Trench

3. Trench

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Deep depression in the ocean floor caused by

subduction

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4. (Folded) Mountains

Appalachian Mountains

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Himalaya Mountains

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Folded Mountains

Appalachian Mountains

As compressional force increases, folded mountains form

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http://www.pbs.org/wgbh/aso/tryit/tectonics/#

Let’s go to this website and review!

Click on Plate Tectonics Activity (with a yellow arrow) when you get there!

CLICK HERE>>>

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Were you right?