ASBOG Practice Exam 2025 – Comprehensive All-in-One Guide to Ace Your Geology Licensure!

A fault characterized by an angle of less than 90 degrees is typically referred to as a thrust fault. In the context of geology, thrust faults occur when the hanging wall is pushed up over the footwall, often due to compressive forces. This results in a shallow dip angle, usually less than 30 degrees, which is significantly less than 90 degrees.

Thrust faults are significant in the context of mountain building and can lead to the stacking of geological layers, creating complex structures in the Earth's crust. These types of faults are often found in regions where tectonic plates converge, leading to intense pressure and deformation of the rock layers involved.

Other fault types, such as normal faults and reverse faults, feature different characteristics. Normal faults typically exhibit dip angles greater than 30 degrees, while reverse faults have a steeper dip angle, generally greater than 30 degrees as well but are still categorized based on their specific movement and geologic setting. Strike-slip faults, on the other hand, primarily involve horizontal movement and do not specifically relate to the dip angle of the fault plane in the same way that thrust faults do.