This type of mountain building occurs when two oceanic plates converge, and as the leading plate subducts from the other, the plate piles up, forming volcanic island arcs that consist of igneous and metamorphic rocks
Island arc
This type of mountain building is caused by the compression of the crust above the other in the collision process
Continental volcanic arc
This type of mountain building occurs along continental plate boundaries.
Andean-type
This happens when a force compresses the crust, causing the crust to bend from its sides.
Folding
Types of folds:
anticline
syncline
tight fold
overfold
recumbent fold
nappe
It is the top/highest layer of any folded rock layer
anticline
It is the lowest point of any folded rock layer
Syncline
It is a sharp-peaked anticline fold
tightfold
It is the bending or warping of folding rock layers
overfold
It is a result of too much bending that no vertical regions can be seen
recumbent fold
It is a fold that has overturned, causing rock layers to be fractured