Anatomy Of An Earthquake - California Academy Of Sciences

  • Please note: Morrison Planetarium will be closed for maintenance Feb. 2–4. 0
  • Tickets
  • Join
  • Donate
California Academy of Sciences Toggle smartphone navigation
  • Home
  • Visit
    • Hours & Admission
    • Daily Calendar
    • Getting Here
    • Tours
    • Groups
    • Dining
    • Academy Store
    • Plan an Event
  • Exhibits & Events
    • Aquarium
    • Planetarium
    • Rainforest
    • Natural History Museum
    • NightLife
    • Sleepovers
    • Birthday Parties
    • Lectures & Workshops
  • Learn & Explore
    • Phenomena Blog
    • Academy @ Home
    • Meet Our Scientists
    • Scientific Expeditions
    • Creature Closeups
    • Community Science
    • Youth Programs
    • Apps & Interactives
    • Live Webcams
    • For Educators
    • For Scientists
  • About Us
    • Mission: Regeneration
    • Strategic Initiatives
    • Animal Care & Wellbeing
    • Vision & Values
    • Leadership
    • Careers & Paid Internships
    • Diversity, Equity, Inclusion, & Access
  • Support
    • Membership
    • Donor Circles
    • Gift & Estate Planning
    • Corporate Engagement
    • Foundation Partnerships
    • Annual Fundraisers
    • Volunteer
  • Back to Scientists Home
  • Back to Educators Home
Toggle Close Search calacademy.org Anatomy of an Earthquake 0

Although the ground beneath us seems solid, it’s actually in constant motion. We usually don’t see it, but we can experience it through earthquakes.

Earth's crust is broken up into irregular pieces called tectonic plates. These large pieces of crust were formed by the combination of gravity and rising heat from Earth's core. There are seven major plates and many smaller ones, all moving in relation to each other. The lithosphere refers to the crust and upper mantle that make up these plates.

As tectonic plates move past each other along fault zones, they sometimes get stuck. Pressure builds, and when the plates finally give and slip, energy is released as seismic waves, causing the ground to shake. This is an earthquake.

The focus is the place inside Earth’s crust where an earthquake originates. The point on the Earth’s surface directly above the focus is the epicenter. When energy is released at the focus, seismic waves travel outward from that point in all directions. There are different types of seismic waves, each one traveling at varying speeds and motions. It's these waves that you feel during an earthquake.

Vocabulary

Fault: A fracture in the rocks that make up the Earth’s crust

Epicenter: The point at the surface of the Earth above the focus

Plates: Massive rocks that make up the outer layer of the Earth’s surface and whose movement along faults triggers earthquakes

Seismic waves: Waves that transmit the energy released by an earthquake

Focus (Hypocenter): The point within the Earth where an earthquake rupture starts

0

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.

0

More to explore

eee Shake House Step in and hang on as our earthquake simulator recreates California's powerful 1906 and 1989 quakes. Exploring Earthquakes

Get a new perspective on earthquakes with this rich collection of multimedia resources. You'll learn why earthquakes happen, how they've shaped the Bay Area, and what you can do to prepare for the next one.

Launch the collection Earthquake Tips

Find out what you can do right now to protect yourself in the event of an earthquake. You'll be happy you did. 

Screen grab of earthquake preparedness sheetHow to Prepare for an EarthquakeDownload the tip sheet Teacher Guide: Earthquakes

Ideas for using videos, articles, and infographics about earthquakes in the classroom.

Teacher Guide

Tag » What Does An Earthquake Look Like