The marble's creation is owed to high level metamorphic processes in a contact zone with dome-like bulges of
migmatite. The two types of stone alternate in layers and the marble has a thickness of up to 30 metres in old fissures. The layers
strike in a northeasterly direction. Naxian marble is over 98%
calcite. Other component minerals as
dolomite,
silicate and traces of
graphite and
pyrite. Calcite crystals are randomly distributed and usually transparent. This transparence gives the stone an appearance of depth and is the cause of the blue-grey shimmer of the marble, which is more or less noticeable depending on the angle of the light source. The crystals are up to 15 millimetres in diameter and it is thus one of the largest grained marbles on Earth. In the assessment of Raymond Perrier, it has a resistance to frost and other weathering. Other parts of the deposit have a grey colour and are clearly striped, which indicates a higher level of impurities. This variant includes the unfinished
Kouros of Apollonas in a quarry near at the north end of the island. In many parts of the deposit, there are grey, black and coloured mineral grains in the calcite crystals of the stone at a microscopic scale, making the crystals appear cloudy. Minor organic impurities are the cause of the slightly
bitumen-like smell emitted while the marble is worked; it disappears after working. == Quarries ==