Back to Plate Tectonics
Table of Contents
Postulates
- Plate Postulate
- A mosaic of rigid geologic plates covers the Earth’s surface, forming the Lithosphere.
- Movement Postulate
- The plates move horizontally relative to each other on top of a thick layer of molten rock, the Asthenosphere.
- Boundary Postulate
- Contiguous plates converge, diverge, or slide past one another.
Plate Postulate
A mosaic of rigid geologic plates covers the Earth’s surface, forming the Lithosphere.

Countries in Gray, Plate in Color, Source
View Interactive NASA Animation of Plate Boundaries on a Rotating Globe
Movement Postulate
The plates move horizontally relative to each other on top of a thick layer of molten rock, the Asthenosphere.

- Lithosphere
- Where the plates live
- Rigid rocky outer layer of Earth
- Consists of the crust and the solid outermost layer of the upper mantle.
- 30-60 miles deep
- Asthenosphere
- What makes the plates move
- Layer of molten rock lying beneath the lithosphere
- Convection currents within the asthenosphere affect the lithosphere
- Extends from 60 miles below the Earth’s surface to about 450 miles.

Boundary Postulate
Contiguous plates converge, diverge, or slide past one another.
Where the Plates Meet
- Convergent Boundaries
- A. Oceanic subducts under Continental
- B. Oceanic subducts under Oceanic
- Continental subducts under Continental
- Divergent Boundary
- Transform Boundary
Convergent Boundaries

Divergent Boundary

Transform Boundary
