📘 How a volcano builds a cone
Follow magma, gas, viscosity, eruption styles, deposits, hazards, and cone growth.
What you’ll learn
- Magma
- Pressure
- Viscosity
- Conduit
- Effusion
- Explosivity
- Cinder cone
- Composite cone
- Shield volcano
- Domes
- Ash plume
- Pyroclastic flow
- Lahars
- Caldera
- Layers
- Monitoring
- Cone growth
Questions this course answers
What determines whether magma erupts quietly or explosively?
USGS identifies magma properties and water interaction as controls on eruption style.
What is tephra?
Tephra includes ash and larger fragments produced when magma breaks apart.
Why do shield volcanoes have gentle slopes?
Runny basaltic flows spread widely and build broad profiles.
What is a lahar?
Lahars are mudflows made when water mobilizes volcanic ash and debris.
Why can a pyroclastic flow move rapidly downhill?
Collapsed eruption columns form dense ground-hugging currents driven downslope.
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