Chapter 11 - Mountain Building Flashcards
dip-slip faults
occur when one block of crust is displaced up or down relative to another
normal faults
tensional fault in which the two crust blocks pull apart from each other and the hanging wall falls relative to the footwall
reverse faults
compressional fault in which the hanging wall is displaced upwards relative to the footwall
thrust fault
a special case of reverse faults when the inclined fault plane is less than 45 degrees, usually about 30
strike-slip faults
when two blocks of crust move laterally relative to the fault line
orogenic belts
tectonic belts which involve mountain building by folding and thrusting
orogeny
mountains built by folding and thrusting
isotasy
the principle that as mountains get eroded, the crust gets lighter and “floats” up resulting in the mountains staying at relatively the same level
grabens
blocks of crust displaced vertically downward
horsts
blocks of crust displaced vertically upward