👉 "Coincline" is a term used in the field of geology and paleontology to describe a fault line that is tilted or inclined relative to the surface. It is often associated with faults that are part of the Earth's crust, indicating movement between different layers of rock. Coinclines can be found at the base of mountains, along fault lines, or on the edge of plate boundaries, and they play an important role in understanding the history of the Earth's tectonic plates.
