Originally, a large waterfall flowed over the Cove at Malham as a glacier melted above it. The remnant of a stream which once fell over the cliff flows out of the small lake of Malham Tarn, on the moors above the cove. The stream now disappears underground at the aptly-named 'Water Sinks', one and a half kilometres before its valley reaches the top of the cove.

A stream of a similar size emerges from a cave at the bottom of the cove. It used to be assumed that the two streams were one and the same. However, experiments with dyes have now shown that two separate streams go underground at different locations, cross paths without mixing behind the cliff, and re-emerge a couple of kilometres apart. This is a testimony to the complexity of the system of caves behind the cliff, which are thought to be around 50,000 years old.

Creation of Malham Cove.