An avalanche or rockfall is mainly air. The mixture of lumps and air constitutes a fluid denser than the air around it, so it slides downhill, accelerating until the drag of the fluid against the hillside matches its excess weight. This limiting speed is akin to the "terminal velocity" of the skydiver, 120 mph or 200 km/h, which it may exceed, depending on the slope and density.
A rockfall at the Elm in Switzerland in 1881, composed of fragments a few centimetres in diameter, reached in excess of 300 km/h with an average 155 km/h. It sloshed up the opposite hillside then flowed down along the valley floor, "destroying houses and everything in its path, killing 115 people". (Principles of Geology, Gilluly, Waters, and Woodford).Earthflows underwater give rise to a particular type of sedimentary rock called "turbidites", evidence of even greater energies.