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Bruno Balestrini/ Mineralogy/ Gypsum Rose
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Sulphates

Gypsum Rose

Gypsum is a typical sedimentary mineral of chemical origin: it forms in evaporitic environments by direct precipitation from water or by hydration of anhydrite. The tabular, elongated crystals can reach up to a metre in length, and are often twinned in “swallowtail” or “spearhead” forms. Gypsum is a soft mineral (2 on the Mohs scale), light and easily cleaved into sheets and flakes. It is sometimes luminescent under ultraviolet rays. Soluble in hydrochloric acid and also in hot water.

It is used in building and, often, thanks to its low hardness, to make sculptures and ornamental objects.

This English text was translated with the help of artificial intelligence (Claude) from the Italian original, except where an English version already existed in the original archive. Read the Italian version.