Geological Evolution

Geoligical differentiation Gravitational accretion on the Earth culminated in the differentiation of the planet: the creation of the core (the source of the Earth's magnetic field) and the beginning of the atmosphere. About 4.4 billion years ago, the core - which, with the mantle, drives the geothermal cycle, including volcanism - formed. Gases emerging from the interior of the planet formed the atmosphere. The surface of the Earth cooled to form a crust.

The Earth's surface is made up of gigantic rocky "plates" of crustal material, called the lithosphere, which consist of the rocky outer coating of the Earth (the crust) and the upper part of the less solid material (the mantle) that is found below the crust. The plates are moving very slowly, riding on top of more fluid layers beneath - colliding and separating.

Crustal Plate Boundaries

The crustal plates have moved over the Earth in the course of time to create the pattern of oceans and continents we know today.