768, 1 year ago Plate tectonics and isostasy: Ocean ridges can only push so much and the denser a mountain range is, the higher the stress on the crust and mantle material. www.youtube.com/watch?v=3rk2jx3eRDE I guess this only explains the positive constraints of orogenesis.
Plate tectonics and isostasy: Ocean ridges can only push so much and the denser a mountain range is, the higher the stress on the crust and mantle material.
www.youtube.com/watch?v=3rk2jx3eRDE
I guess this only explains the positive constraints of orogenesis.