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The Theory of Plate Tectonics The Theory of Plate Tectonics

The Theory of Plate Tectonics - PowerPoint Presentation

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The Theory of Plate Tectonics - PPT Presentation

Plate Tectonics Became a theory in the 1960s Describes plate movements AND explains why they move Plate Tectonics Two types of crust Oceanic and Continental Plates are usually made of both ID: 655098

ocean plate continental boundaries plate ocean boundaries continental crust plates rises motion sinks ridge subducted divergent convergent asthenosphere mid

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Slide1

The Theory of Plate TectonicsSlide2

Plate Tectonics

Became a theory in the 1960’s

Describes plate movements AND explains why they moveSlide3

Plate Tectonics

Two types of crust: Oceanic and Continental

Plates are usually made of both

Plates: Chunks of lithosphere “floating” around on the

asthenosphereSlide4
Slide5
Slide6

Plate Boundaries

Three Types:

Divergent Boundaries: two plates moving away from each other

Plates move apart, molten rock from

asthenosphere

fills gap

Most found on ocean floor (mid-ocean ridges)

Rift valley: valley in the center of the mid-ocean ridgeSlide7

Divergent BoundarySlide8
Slide9

Convergent Boundaries

Two plates colliding (Three types of collisions)

Ocean – Continental: ocean crust is denser, so it is

subducted

:

forced under the continental crust

Ocean trench forms

Subducting

crust melts, some rises through the continental crust to form volcanic mountainsSlide10
Slide11

Convergent Boundaries

Continental-Continental: neither is

subducted

, but both are crumpled and uplifted, forming mountain rangesSlide12

Convergent Boundaries

Oceanic-Oceanic: one plate gets

subducted

, again forming an ocean trench

Melting crust rises to form a volcanic

island arcSlide13
Slide14

Transform Fault Boundaries

Sliding and grinding past each other

Does not move smoothly – spurts of movement between periods of no motionSlide15
Slide16

Causes of Plate Motion

Convection

Hot

asthenosphere

rises, cools, sinks

 convection currents

Lithospheric

plates ride on top of these conveyer belts

Evidence: More heat near divergent plate boundaries than elsewhere along ocean floorSlide17
Slide18

Causes of Plate Motion

Ridge Push

New rock at mid-ocean ridges is hot, less dense, rises higher

As it cools, it sinks away from the ridgeSlide19

Causes of Plate Motion

Slab Pull

When a plate

subducts

and sinks, it pulls the rest of the plate with it