📘 How an earthquake releases energy
Trace fault loading, elastic rebound, rupture, seismic waves, and aftershocks.
What you’ll learn
- Plate motion
- Fault
- Elastic strain
- Nucleation
- Rupture
- Seismic waves
- Magnitude
- Aftershocks
- Surface effects
- Cycle
Questions this course answers
What stores energy before many earthquakes?
Tectonic loading bends rock and stores elastic energy until fault slip releases it.
What is a fault?
Faults are fractures or zones of fractures along which rock has slipped.
Which wave generally arrives first at a seismometer?
P waves travel faster through rock than S and surface waves.
How does magnitude differ from intensity?
Magnitude is a source measure, while intensity varies by location and conditions.
Why do aftershocks occur?
Stress redistribution brings nearby fault patches closer to failure.
Grounded in trusted sources
- [object Object]
- [object Object]
- [object Object]
- [object Object]
Every Wunder lesson is built from real, reputable sources — never invented.
Related Science courses
Wunder is a personalized learn-anything platform — tell it any topic and it builds a beautiful, fact-checked course in minutes, with narration, a knowledge check, and a college-style University track.
Browse more Science courses · All topics · Home
© 2026 Wunder Learning LLC · Terms & Privacy