This page has been simplified for faster loading and easier reading. Click the lightning bolt icon to view the original version.

Learn & Explore

From Core to Crust: Defining Earth’s Layers

The inside of our planet is made primarily out of iron and nickel and dark, dense rock.

Before learning about earthquakes, let’s look at the inside of our planet.

What happens on Earth’s surface is directly related to its interior. About 4.6 billion years ago, Earth formed from a hot cloud of dust orbiting a blazing sun. As the planet cooled, dense elements became concentrated in the core of the planet, while lighter elements formed the mantle. A thin, rigid crust formed at the surface. A constant heating and cooling cycle in the mantle drives plate movement on Earth’s surface. Heat working its way out from the core of the planet fractured the crust into irregular tectonic plates that are constantly in motion.

This post is part of Exploring Earthquakes, a rich collection of resources co-presented by the California Academy of Sciences and KQED. This material is also available as a free iBooks textbook and iTunes U course.

Don’t miss Earthquake, an interactive exhibit at the Academy exploring the seismic forces that impact us today and featuring the Shake House, an earthquake simulator.