Gemstone profile and identification guide

Apophyllite

Apophyllite is a hydrated silicate mineral group known primarily as collector crystal material and occasional faceted gem.

4.75 Mohs Colorless, Green Silicate (Phyllosilicate Group: Apophyllite Supergroup)
Apophyllite

Overview

Apophyllite is a hydrated silicate mineral group known primarily as collector crystal material and occasional faceted gem.

Did you know? Indian trap-rock geodes produce some of the world’s best-known apophyllite specimens.

Use this profile as a collector reference and educational guide for quick on-page comparison, then validate with the interactive identification system.

Identification

Name: Apophyllite

Scientific classification: Silicate (Phyllosilicate Group: Apophyllite Supergroup)

Hardness: 4.75 Mohs

Transparency: transparent

Lustre: vitreous to pearly

Crystal system: Tetragonal

Primary colour: Colorless

Secondary colour: Green

Colour family: Whites & Neutrals

Tetragonal crystal habit, perfect cleavage, and moderate hardness are key indicators.

Verification Status

Status: verified-core-fields

Reference priority: GIA, Gem-A, Mindat, International Gem Society

Core identity, locality, and physical-property fields reviewed against standard gemological references.

Values are reported as practical gemological ranges where appropriate.

Physical Properties

Hardness category: medium

Hardness value: 4.75 Mohs

Chemical composition: Potassium calcium silicate fluoride hydroxide hydrate (variable species)

Crystal system: Tetragonal

Common locations: India (Maharashtra), Brazil, Iceland, Germany, Canada

Learn more: Gem-A gemstone education resources.

Colour Variations

Typically colorless to white, with pale green crystal specimens common in collector material.

Optical effects: None specified in the current dataset.

Detailed Gemology

Mineral species: Apophyllite supergroup species

Mineral group: Phyllosilicate group

Chemical formula: Potassium calcium silicate fluoride hydroxide hydrate (variable species)

Mohs hardness: 4.75

Crystal system: Tetragonal

Lustre: vitreous to pearly

Transparency: transparent

Streak: White

Cleavage: Perfect basal cleavage

Fracture: Uneven

Specific gravity: 2.30-2.40

Refractive index: 1.535-1.551

Optical phenomena: None typically diagnostic

Colour range: Colorless, white, pale green

Common inclusions: Fluid inclusions, growth zoning, matrix contacts

Geological environment: Basalt cavities and hydrothermal veins

Principal mining regions: India (Maharashtra), Brazil, Iceland, Germany, Canada

Important commercial sources: Most gem and collector apophyllite on the market comes from basalt cavities in India

Historical significance: Widely collected in modern mineral collecting due to crystal clarity.

Common treatments: Generally untreated.

Synthetic or imitation forms: Glass may imitate transparent crystal appearance.

Common look-alikes: Calcite, quartz, prehnite (in matrix)

Jewellery uses: Used mainly as collector specimens and rarely as faceted stones.

Care recommendations: Soft with perfect cleavage; handle gently and avoid ultrasonic/steam cleaning.

Cross-check profile data with GIA Gem Encyclopedia and Mindat entry for Apophyllite.

Formation

Forms in low-temperature hydrothermal cavities, commonly in basaltic volcanic rocks.

Origin

Most gem and collector apophyllite on the market comes from basalt cavities in India

Uses

Best for: Used mainly as collector specimens and rarely as faceted stones.

Ideal uses: Display specimens and low-impact collector jewellery.

Apophyllite FAQ

How can I identify Apophyllite?

Compare hardness (4.75 Mohs), crystal system (Tetragonal), colour profile, and lustre (vitreous to pearly) with your sample. Then cross-check related gemstones listed above.

What colour range does Apophyllite appear in?

Typically colorless to white, with pale green crystal specimens common in collector material.

Where is Apophyllite commonly used?

Display specimens and low-impact collector jewellery.. For maintenance, follow the care guidance in this profile.