What process occurs when folded land cannot be bent any further?

When folded land cannot be bent any further, faulting occurs. This process involves the breaking and displacement of rock layers along a fault line, which can result when the stress applied to the rock exceeds its strength. This can happen after extensive folding, when the geological structures have reached their limits for deformation.

Faulting is characterized by noticeable shifts in the earth's crust, which can lead to earthquakes and the formation of new geological structures. In contrast, folding refers to the bending of rock layers due to tectonic forces, while subduction involves one tectonic plate being pushed under another, and compression is the force that causes the rocks to bend or break in the first place.

Understanding these processes is key in geology, particularly when studying how the earth's landscape evolves due to tectonic activity and stress over time.