stephanite
Stephanite is a carbonate mineral belonging to the calcite group, with the chemical formula CaCO₃. It forms as a pseudomorphic replacement of the older mineral calcite, preserving the external crystal shape while mineralizing into a substituted lattice. The mineral is named after German mineralogist Alexander Stephani (1824–1854), who first described it in 1853. Stephanite crystallises in the trigonal crystal system and typically appears as fibrous, radiating masses or as elongated prismatic crystals, often exhibiting a milky to translucent appearance.
The mineral’s colour ranges from white and colourless to pale cream or yellowish‑brown, and it may display
Stephanite is commonly found in hot spring travertine deposits, tufa, and speleothems, where it replaces calcite
From a geological perspective, Stephanite is of interest because its ductile fibrous nature can provide clues