A thrust fault is a type of geological fault where one block of the Earth's crust is pushed up over another. This occurs due to compressional forces, which can happen during tectonic plate movements. Thrust faults are typically found in regions where the Earth's crust is being squeezed, such as at convergent plate boundaries. These faults can create significant geological features, including mountain ranges and folded rock layers. An example of a thrust fault is the Himalayas, where the Indian Plate is colliding with the Eurasian Plate, causing the land to uplift and form some of the highest peaks in the world.