How to identify Prasiolite
Quartz (green variety)
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Open the appTo correctly identify Prasiolite (Quartz (green variety)), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Pale to medium green, often with a yellowish tint. Can be distinguished from other green gemstones by its specific shade and lack of strong pleochroism.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy).
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Smooth to conchoidal fracture surfaces when broken. Crystals are typically prismatic.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Hexagonal prisms terminated by rhombohedra. Often found as massive or granular aggregates, or as well-formed crystals in geodes and veins.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None (lacks cleavage).
- 6
Geological Environment
The rock formation and setting where it occurs
Naturally occurring prasiolite is found in igneous and metamorphic rocks where amethyst has been subjected to natural heating. Artificially produced prasiolite originates from amethyst or yellowish quartz found in pegmatites, hydrothermal veins, and volcanic rocks.
Key Facts
- Hardness
- 7 (Mohs scale)
- Specific Gravity
- 2.65 g/cm³
- Crystal System
- Trigonal (often described as hexagonal due to external morphology)
- Color
- Pale to medium green, yellowish-green
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Fracture
- Conchoidal
- Cleavage
- None
- Composition
- Silicon dioxide (SiO2)
Physical characteristics
- Crystal Habit: Prismatic, often terminated by rhombohedra; also massive, granular, cryptocrystalline (chalcedony form is not typically prasiolite).
- Cleavage Type: None (lacks cleavage).
- Fracture Type: Conchoidal (shell-like, curved fractures).
- Tenacity: Brittle.
- Luster Type: Vitreous (glassy).
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