tesselations

navigate by keyword : dry cracked earth desert naturally forming mudcracks start wet muddy sediment dries contracts strain developed top layer shrinks material size large channel cracks form dried surface relieve individual spread join polygonal interconnected network forms called tesselations

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Naturally forming mudcracks start as wet, muddy sediment dries up and contracts. A strain is developed because the top layer shrinks while the material below stays the same size. When this strain becomes large enough, channel cracks form in the dried-up surface to relieve the strain. Individual cracks spread and join up, forming a polygonal, interconnected network of forms called "tesselations."