Crystals occur as distorted tabular triangles and are hemimorphic, polytypes exist.

It was first described in 1937 for an occurrence in the Choctaw Salt Dome of Iberville Parish, Louisiana, US.

[2] It occurs as an uncommon accessory mineral in evaporite deposits and salt domes worldwide.

In addition to the type locality it has been reported in Wayne County, Mississippi and in the Louann Salt Formation, Clarke County, Alabama in the United States and at the Penobsquis and Salt Springs evaporites, near Sussex, New Brunswick, Canada.

In Asia it is reported from the Chelkar salt dome, Uralsk district, Kazakhstan; the Ilga Basin, eastern Siberia, Russia and the Sedom Formation, Mount Sedom, Dead Sea, Israel.