Formation of mountains is a direct result of plate
tectonic activity. Geologic structures such as faults,
folds, and layering found in mountains can be used to
infer the type and direction of plate tectonic stresses
in both ancient and presently active mountains.
Matthew Nyman, TERC
Martin Miller, University of Oregon
Folded metamorphic rocks in Wyoming. Note the camera lens cap for scale.
Folds and faults in the Klamath
Mountains of Oregon. Note the rock hammer for scale.
Matthew Nyman, TERC
NASA
Tilted sedimentary rocks in the Canadian Rockies. Note the person in the red circle for scale.
Large-scale folding is apparent in this satellite image of the Appalachian Mountains, Pennsylvania.