Part 2: Earth's Interior & Rheology

Probing the Deep Earth

Seismic waves act as X-rays of the planet, revealing a layered interior with distinct mechanical and chemical boundaries. Understanding Earth's rheology -- how rocks deform over geological timescales -- is essential for explaining mantle convection and plate motion.

6371 km

Earth Radius

10ยฒยน Paยทs

Mantle Viscosity

5150 km

ICB Depth

Topics in This Part