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Tectonic Plates

Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

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Page 1: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Tectonic Plates

Page 2: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Lithosphere – outer part of the Earth’s crust. Composed of solid rock.Asthenosphere - the zone below the lithosphere which is more ‘plastic’ so it is easier to bend and moveRadioactivity is the sourc of heat in the mantle

Layers of Earth

Page 3: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

2 Kinds of CrustContinental – less dense, thickerOceanic – more dense, thinner

Page 4: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

2 Kinds of MantleUpper – solid, floats on…Lower – plastic (somewhat fluid)–Why?•Earth’s crust and upper mantle “float” on the plastic portion of the mantle. (asthenosphere)

Page 5: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Convection Currents

Movement of hot liquid or gas –Heated – rises–Cools – dropsEarth’s Crust Cracks…–Convection currents in mantle cause

cracking in crust–Thermal Convection cause seafloor

to spread and continents to drift

Page 6: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Divergent

Boundary

Convergent Boundary

Page 7: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Divergent – Ocean to Ocean

New crust formed and pushed up - Mid Oceanic Ridges–Ex. Mid-Atlantic Ridge

Ocean Ridges

Page 8: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Divergent-Continent to Continent Continent spreads, ocean basin may

formPaleontologist noticed that fossils were on different continentsArthur Holmes – First proposed that thermal convection in the mantle causes continental driftEx. Red Sea

Page 9: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Convergent –Ocean to Ocean

Older slips below newerSubducted plate melts–Volcanic islands formedEx. Aleutian islands, Japan

Page 10: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Convergent –Ocean to Continent

Ocean plate goes below continent– SubductionSubducted plate partially meltsTrenches – the deepest parts of the ocean.Volcanic mountains– Ex. Western South America

Page 11: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Aleutian Islands

Islands of Japan

Page 12: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Convergent – Continent to

ContinentSame densities, no subductionCompression, folding, upliftingEx. Himalayas, Alps

Page 13: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Transform faulting:Plates move past each other

Another type of plate movement…

San Andreas FaultSan Andreas Fault

Page 14: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

How do you think scientists identified the plate boundaries?What is the “Ring of

Fire?”

Page 15: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Crustal Plates

“Connect the dots” – volcanoes and earthquakes8 major plates

Page 16: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Pangea Theory1912 – Alfred WegenerIdea that continents were once part of one large land mass – theory of continental driftHow did he know?–Continents’ shapes fit together like a

puzzle–Rocks and fossils found on different

continents matched

Page 17: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Early 1960sScientific evidence proves continental drift, plate tectonics, and Pangea theory

Page 18: Tectonic Plates. Lithosphere – outer part of the Earth’s crust. Composed of solid rock. Asthenosphere - the zone below the lithosphere which is more ‘plastic’

Ocean Features Picture 2