Earth Internal Heat Flow
Earth's internal heat flow from the core, mantle and crust to the surface through conduction, convection, and advection.
Earth's internal heat flow from the core, mantle and crust to the surface through conduction, convection, and advection.
Earth’s surface elevation and mantle density animated through space and time.
100-km depth contours outline the basic radial compositional structure of the planetary interiors of Earth, Mars, Venus, and Mercury.
The interiors of rocky planets and the Moon represented by 100-km depth contours outlining the basic compositional structure.
A schematic highlighting the travel paths of seismic waves through the Earth’s interior.