Evidence suggests that the landslide created its own lubrication, which allowed it to travel further than it would have otherwise: the limestone at the bottom of the slide melted from the heat caused by friction.
The limestone at the bottom of the slide melted from the heat caused by friction. Evidence suggests that the landslide created its own lubrication which allowed it to travel further than it would have otherwise.
Evidence suggests that the landslide created its own lubrication which allowed it to travel further than it would have otherwise. The limestone at the bottom of the slide melted from the heat caused by friction.
Evidence suggests that the landslide created its own lubrication which allowed it to travel further than it would have otherwise. The limestone at the bottom of the slide melted from the heat caused by friction.