1
Q
areas of cratons laid bare by erosion
A
Shields
2
Q
belts that indicate crustal shortening produced by compression
A
Fold/thrust belts
3
Q
intense deformation, compressionary forces result in deformation of the rock (metamorphism)
A
Orogeny
4
Q
vertical movement of mountain belts, both during and after orogeny
A
Isostacy
5
Q
rate of weathering and erosion varies with climate, type of rock, and landmass height above sea level
A
Weathering and Erosion
6
Q
the four stages of mountain building
A
accumulation, orogeny, uplift, and block faulting
