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5.3 The Plate Tectonic Supercycle

Horizontales
The breakdown of rocks
Fancy name of Mountain building
Force associated with convergence
Plate Tectonic Supercycle
When two plates come together
Sediments on the continental shelve that are compressed in convergence
Structure surrounding igneous rock erupted on the the Earth's surface
Continental rock pushed up by magma at depth
Modern theory that explains the apparent movement of the continents
Rigid rock at the Earth's surface will do this under pressure
The composition of Continental rock is described as this
Hot liquid rock beneath the Earth's surface
Verticales
The plate tectonic supercycle's other name
Liquid rock erupted at MORs
The type of plate boundary when plates move away from each other
This happens when lava comes from the depth of the Earth
The mafic/extrusive igneous rock
Force at a diverging plate boundary
Weathered rock fragments
When an oceanic plate moves beneath another plate
Meaning all lands
Orogeny
The transport of weathered material
Great southern land
When a heterogeneous plate is heated
Shortened form of mid-ocean ridge
The breakup and rejoining of continents.
Another name for the breakup and movement of continents