0
Jordyn Pfeffer ∙
The Earth's core.
pole reversals seafloor spreading
asthenosphere
Where the crust is destroyed
Shearing
The weight of the rocks in the crust and upper mantle results in the pressure that allows diamonds to form.
Normal Thrust
Wondering slowly with no pattern
Mountain ranges linking in England and America
denser
compass magnets can be deflected by earths magnetic field or other permanent magnets
Continental rise is something the passive continental margin has that the active margin does not
The continental crust is up to 70 km thick.
Limestone
It can destroy homes and force people to relocate from natural disasters or even a slow erosion over time.