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5.3.a The Plate Tectonic Supercyle

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