Title: Earths Interior and Plate Tectonics
1Earths Interior and Plate Tectonics
2Key Terms
- crust
- mantle
- core
- lithosphere
- plate tectonics
3Key Terms
- asthenosphere
- magma
- subduction
- fault
4Objectives
- Identify Earths geologic layers
- Describe plate tectonics
- Identify plate boundaries and structures that
form - Explain how magnetic bands on ocean floor support
the theory
5What is Earths interior like?
- Crust (we live here)
- cool, hard, solid rock
- oceanic crust 4-7 km thick continental crust
20-40 km thickdeepest beneath high mountains (up
to 70 km thick) - Mantle
- denser than crust
- never been there, but can guess from earthquakes
and volcanoes
6What is Earths interior like?
- Mantle
- 2900 km thick 80 of Earths volume
- outer mantle more solid inner mantle hot and
plastic - Core
- mainly iron and nickel (we think)
- outer core liquid, inner core solid (pressure)
7Earths interior gets warmer with depth
- South African gold mines, 3 km deep, approach 50º
C (120º F) - quick whats that in Kelvins?
- (add 273)
- Mantle is hotter than crust (temps exceed 1250º
C) - Core is hotter still (6000º C )
8Radioactive elements and residual heat contribute
- core contains radioactive isotopes (ie uranium,
thorium and potassium) - huge quantity of energy
- I didnt see The Core but heard it panned...
9Did you get those terms?
- crust the othermost and thinnest layer of Earth
- mantle the layer of rock between the Earths
crust and its core - core the center of a planetary body
10Plate Tectonics
- Early 20th C Alfred Wegener (German scientist)
noticed how the continents fit together - Pangaea, one land mass maybe 200 million years
ago - Fossil evidence supports the concept
11More evidence
- In the 1960s, structures on the ocean floors
gave evidence of continental drift
12Earth has plates that move over the tar-like
mantle
- Lithosphere (100 km thick), the crust and upper
portion of mantle is made up of 7 large (and
several smaller) pieces--tectonic plates - They move.
13Theory is that they move because of convection
currents
- asthenosphere, the hot, plastic portion of the
mantle, is slowly flowing, and might circulate
like mushy oatmeal - remember when we talked about convection currents
in fluids?
14Did you get those terms?
- lithosphere the thin (100 km) outer shell of
Earth, consisting of the crust and rigid upper
mantle - plate tectonics the theory that Earths surface
is made up of large moving plates
15Did you get those terms?
- asthenosphere the zone of the mantle beneath the
lithosphere that consists of slowly flowing solid
rock
16Divergent plate boundaries
- diverge means to come apart
- two plates come apart and hot molton rock (magma)
rises from the asthenosphere and cools, forming
new lithospheric rockwhich then gets pulled away
17Mid-oceanic ridges
- underwater mountain ranges that form at divergent
rift boundaries - large central rift valley
- magma pushes up
18Convergent plate boundaries
- Con means with or together, so
- plates come together as well
- oceanic plates dive under continental plates as
they collide
19Subduction
- the denser oceanic plate dives beneath the
continental plate - ocean trenches, mountains and volcanoes
- the oceanic crust melts when it subducts
20Colliding continental plates
- colliding continental plates create mountains
- Like the Himalayas
- Everests peak is 8850 m above sea level
21Transform fault boundaries
- Plate movement causes breaks in the lithosphere,
and they pieces scrape - faults
- Earthquakes
22Strong evidence for plate tectonics
- 1960s
- bands of rock on the ocean floor with alternating
magnetic polarities - molten minerals align themselves with the Earths
magnetic field
23Magnetic field has reversed about every 200 000
years
- symmetrical bands on either side of the
mid-Atlantic ridge support the theory - The farther away, the older the rocks.
24Did you get those terms?
- magma molten rock within the Earth
- subduction the process in which a tectonic
plate dives beneath another tectonic plate and
into the asthenosphere
25Did you get those terms?
- fault a crack in the Earth created when rocks on
either side of a break move