Hypersthene specimens for sale

3 for sale ยท $80โ€“$300 USD

1 in the gallery

Hypersthene is a magnesium-iron silicate that crystallizes in the orthorhombic system. It typically forms short to elongated prisms or grains with a vitreous to metallic sheen and a color range from dark gray to brownish black, sometimes showing a subtle greenish tint in polished surfaces. The mineral often occurs in pyroxene-rich rocks such as basalt and gabbro, and can appear isolated or as part of larger mineral assemblies, including augite-bearing assemblages.

Formula
(Mg,Fe)SiO3
Rarity
Common
Stability
Stable
Collector interest
Moderate Interest
Classification notes
Inosilicate; Pyroxene group (orthorhombic)

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Where Hypersthene is found

Top localities

  1. Kansas1 specimen

About Hypersthene

Classic specimen sources include basaltic provinces where high-temperature crystallization of pyroxenes dominates, with notable specimens from regions that yield well-formed crystals or large crystal faces. Collectors value Hypersthene for its chatoyant, sometimes bronze-tinted luster and its role in understanding cooling histories of magmatic rocks, as well as for integration into balanced display mineral suites. While not as flashy as some gemstones, well-formed crystals and sizeable, clean faces can be highly desirable for in-depth mineral study and aesthetic cabinet collections.