The sands were formed from the decomposition of volcanic rock (basalt) gullies into clay, further transformed into ferralitic soil by total hydrolysis (chemical break- down of minerals by water). The two main elements of the resulting soil, iron and aluminium, are responsible for red/anthracite and blue/purplish colours respectively. The different shades of colour are believed to be a consequence of the molten volcanic rock cooling down at different external temperatures.
An unusual property of the sands is that they settle in different layers even if mixed together that gives the dunes a surrealistic, striped colouring. This strange phenomenon can be observed even on a smaller scale, if one takes a handful of sands of different colours and mixes them together, they'll eventually separate into a layered spectrum. The cause of their consistent spontaneous separation is yet to be explained. Another interesting feature of Chamarel's Coloured Earths is that the dunes seemingly never erode, in spite of Mauritius' torrential, tropical rains.
