12 plates
Move relative to one another and relative to interior.
- Account for earthquakes, volcanos, ridges, "excitement". 

Plate Tectonics

Alfred Wegener
Father of plate tectonics "badass of plate tectonics". 
- Saw a fit of South America and Africa (fit = geographic distribution of similar rock types, fossils, and ancient climates).
Observed:
1) Geographic mapping/fit "puzzle piece fit"
2) Matching geologic units; sediment, patterns of rocks, etc.
3) Distribution of fossils and modern day organisms 
4) Distribution of climate belts. Evidence of ancient glaciers and rocks underneath. 
Pangea
Supercontinent
Continent drift caused the continents we see today. 
Wegener's Problem
1) Unrealistic mechanism for driving plate motion
2) Passive role of oceanic crust 
Evidence for Plate Tectonics
Variations in magnetism of seafloor rocks.
Symmetric patterns of age of seafloor crust across plate tectonic ridges. 
Formation of magnetic lava crystals 
Magnetic minerals crystalize in lavas and align themselves parallel to Earth's magnetic field. 
Fun fact: Oldest oceanic crust is ~200 million years old 
Reversals in Earth's magnetic field 
Preserved in lava flows! They reveal age of seafloor crust. 
Hot Spots
Reveal plate motion in relation to relatively fixed mantle plumes. 
Operations of Plate Tectonics
Lithosphere
Consists of continental crust / oceanic crust and lithospheric mantle. 
Asthenosphere
Weak, partially molten, capable of allowing plates to flow on it.
Divergent
Important for life on earth! Separating plates. 
Convergent 
Important for life on earth! Coming together of plates.
Transform
Ex. San Andreas fault. 
Slab Pull
Cauases actual movement of plate tectonics 
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