Lecture 4: Plate tectonics Flashcards
How do Seismic waves reveal Earth’s interior?
- P waves are refracted by changes in density = p wave “shadow zone”
- S waves cannot travel through liquids = s wave “shadow zone”
Thus earth has liquid outer core
Describe continental crust:
Granite (average composition)
35-40 km thick
Density ~2.8 g/cm3
Describe Oceanic crust:
Basalt (average composition)
7-10 km thick
Density ~3 g/cm3
Describe the mantle:
Peridotite (solid rock)
Density ~3.3 g/cm3
Describe Earth’s core:
Fe-Ni alloy
Liquid outer core
Solid inner core
Describe the Lithosphere:
0 – 100 km deep
Strong, cool, rigid
- crust + upper mantle
Describe the Asthenosphere:
100 – 350 km deep
High temperature
Weak, easily deformed, solid
- mantle
Describe the Mesosphere:
350 – 2883 km deep
High temperature & pressure
Strong, solid
- mantle
Is the mantle molten?
NO
The mantle is solid rock that deforms in a ductile (plastic) way when at high pressures and temperatures (>1300°C)
How many major Lithospheric plates are there?
9 major and many minor plates
What are the three margins where plates interact?
- Divergent margins where plates pull apart - creates continental and oceanic rifts
- Convergent margins where plates are driven together - you can have Ocean to Ocean plates or Ocean to Continental plates coming together and subducting (ocean under continent) or Continent to Continent which causes a collision zone.
- Transform margins where plates move along side each other is opposite directions,