How a Waterfall Slowly Walks Upstream
A waterfall looks like a fixed part of the land, but many waterfalls are moving. Very slowly, over hundreds or thousands of years, they travel backward up the river that feeds them.
The story begins with two kinds of rock. Imagine a river that flows over a layer of hard rock that sits on top of a layer of softer rock. At the edge, the river tumbles over the hard layer and drops onto the soft layer below. That edge is the waterfall.
At the bottom, the falling water churns in a deep pool called a plunge pool. The swirling water, carrying sand and small stones, strikes the soft rock again and again and wears it away. Soon the soft rock under the hard layer is hollowed out, and the hard rock above is left hanging out like a shelf.
A shelf with nothing under it cannot stay up forever. Eventually a piece of it cracks and breaks off, and it falls into the pool. The edge of the waterfall is now a little farther upstream than before. The same thing then happens again, and again.
Each small step is tiny, but the steps add up. Over a very long time, a waterfall can carve out a deep, narrow valley called a gorge behind it. A gorge below a waterfall is the trail that the falls have left behind them.