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Its formation takes place in pegmatite rocks during the cooling of magma (if this is sufficiently rich in beryllium), in the form of mineral deposit in river sediments and in metamorphic rocks.
Aquamarine is not a rare stone, so much so that it is possible to find even large specimens, mainly in Braziland Africa(Nigeria, Mozambique, Zambia and Madagascar). The color of Aquamarine is due to the presence of iron: the different concentrations of this element give life to its range of shades: from pastel colors to darker and more precious shades, deep blue, with sometimes flashes of green.