Rock Identifier
Green glassy mineral fragment, possibly chromium-bearing diopside (Uncertain from the photograph; green diopside is CaMgSi₂O₆, but glass or another green mineral cannot be ruled out visually.) — mineral
mineral

Green glassy mineral fragment, possibly chromium-bearing diopside

Uncertain from the photograph; green diopside is CaMgSi₂O₆, but glass or another green mineral cannot be ruled out visually.

AI-generated identification · may be incorrect

Translucent deep green with a vitreous-looking surface and irregular fracture; hardness, cleavage, and crystal structure cannot be reliably determined from the image. Diopside has Mohs hardness 5.5–6.5 and monoclinic crystals.

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Physical properties

Translucent deep green with a vitreous-looking surface and irregular fracture; hardness, cleavage, and crystal structure cannot be reliably determined from the image. Diopside has Mohs hardness 5.5–6.5 and monoclinic crystals.

Formation & geological history

If diopside, it typically forms in calcium- and magnesium-rich metamorphic rocks or mafic igneous rocks; its age depends on the host deposit. The specimen’s origin cannot be established from the image.

Uses & applications

Gem-quality diopside is cut for jewelry; rough fragments are mainly collected as mineral specimens. Identification is needed before assigning an industrial use.

Geological facts

Green appearance alone does not distinguish diopside from minerals such as olivine, fluorite, or glass; a hardness test, specific gravity, and ideally gemological testing help identify it.

Field identification & locations

The irregular shape and lack of visible crystal faces limit field identification; check for natural cleavage and test hardness only with permission. Green diopside occurs in several regions, including Russia, Pakistan, and Canada.