Pigeonite - (Mg,Fe,Ca)SiO3

Single-Chain Inosilicates

Habit: Brown or greenish brown to black. Prismatic crystals, granular or massive. Vitreous luster; semitransparent. Grayish white streak.


Environment: Commonly occurs in rapidly cooled siliceous volcanic rocks. Inverted varieties with exsolved augite found in layered mafic intrusives; also in metamorphosed iron formations.


Etymology: From its occurrence at Pigeon Point, Minnesota, in the United States.