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Two different properties aid mechanical weathering. First, simple dissolution and subsequent precipitation of salts will help destroy rock's surface structure.

And the expansion of water below -4oC causes a 'freeze-thaw' weathering as it breaks up the rock.

[note, in both Roman times, and more recently in Scotland, a method of breaking large boulders was to drill a series of holes across the stone, and on a frosty night allow water in the holes to break the stone apart. A minor variant of this is to hammer dry hardwood pegs into the holes as above, and wet the surface. As the wood swells, it breaks the stone. ]

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