Monocline

A monocline is a geological term that refers to a specific type of fold in rock layers. It is characterized by a simple, steep bend in otherwise horizontal or gently dipping strata. In a monocline, the rock layers are typically tilted in one direction, creating a stair-step-like appearance. This geological structure often forms as a result of tectonic forces, such as the movement of fault lines or the uplift of the Earth’s crust.