Site Formation
Fell's Cave is located in the Río Chico canyon, Chile, near the Straits of Magellan and the Argentine border. This area is known as the southeastern Patagonian basalt plateaus. Situated on the southeast side of what was once a river bank, it is more accurately described as a shelter. It was formed by river water wearing away at the sandstone bank, leaving behind a canopy of lava conglomerate and thus creating a shelter 28 feet deep and 38 feet wide. The erosion formed a smooth floor of hard clay. Remnants of sandstone still clinging to the conglomerate roof eventually fell to the floor, forming a sterile layer that later separated human occupation periods.
Read more about this topic: Cueva Fell
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