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Once a cave passage is abandoned by its formative stream, it can become:

- Choked with sediments deposited by the dying floods of that stream or brought in by glacial thaw (Gaping Gill, in NW England, holds vast quantities of glacial till out of erosive reach of the present stream).

- Richly decorated with stalagmites and stalactites (these won't grow under water).

- Filled with boulders falling from roof and walls as ground-water seeping through the joints in thelimestone above it, dissolves the rock enough to weaken the structure: a destructive rather than constructive act of the same process that initiated the cave.

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