Continental roots stress Earth's surface
Wednesday, December 30, 2009 - 19:35
in Earth & Climate
The Earth's rigid lithosphere varies laterally in thickness and strength. Areas of thicker, older lithosphere known as continental roots penetrate deeper into the mantle in some places under continents. Because these continental roots are in contact with deeper, more viscous mantle, the shear traction at the base of the lithosphere in those areas is increased by up to a factor of 4 compared with a model lithosphere without continental roots.