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The formation of mosaic sand, here as exemplified from a 0.23 km2 sand field at the coast of Nordland County in Northern Norway, is thought to be related to earthquake induced shaking, re-mobilization and partial (semi-) liquefaction of water-saturated, stratified fine and medium sand. It is therefore a part of the broad class of sediments with seismically induced deformations, known as seismites.