Plate Tectonics
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Percent composition of each boundary on Earth:
Divergent - 40% Convergent - 40% Transform - 20%
Wilson Cycle
Describes how the continents are always in a constant cycle of splitting and rejoining
Ophiolite
a slice of ancient oceanic lithosphere that has been uplifted onto Earth’s continental crust during mountain building
Seamounts
Submarine Volcanoes
Guyots
Specific types of seamounts with flat tops
Curie’s Point
the point at which a material loses its magnetic properties
Divisions of the magnetic time scale
Chrons (1 million years each)
2 models of plate-mantle convection
Whole-mantle convection model; Lower cake model
Whole-mantle convection model
the earth’s mantle convects as one continuous system
Layer-Cake model
There are two separate convection systems: a dynamic upper mantle and a sluggish lower mantle w/ limited mixing between them
Pangea began splitting during the
mesozoic era
divergent plate boundaries also known as:
spreading centers
we are in the
brunhes normal chron