It was first described in 1850 for an occurrence in Cervantes, Galicia, Spain, and named for the locality.[4] The mineral was questioned and disapproved, but re-approved and verified in 1962 based on material from the Zajaca-Stolice district, Brasina, Serbia.[3] It occurs as a secondary alteration product of antimony bearing minerals, mainly stibnite.[3]
^James Dwight Dana A. M., Brush G. J. A system of mineralogy : Descriptive mineralogy, comprising the most recent discoveries. — New York : J. Wiley & Sons, 1884.