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Draba aizoides has a wide distribution in the mountains of southern and central Europe, from the Pyrenees in the west, through the Alps to the Carpathians.
For much of its history the Weald had been slowly subsiding basin, but the growth of the Alpine Chain to the south during the Cenozoic caused a reactivation of the Variscan basement basin-bounding faults, the rocks were arched into a broad anticline which stretched across the English Channel to Northern France, the Weald–Artois anticline.
The southern limits of its range are essentially marked by the Pyrenees and the Alpide belt.