Crystal comparisons · About 4 minutes

Selenite vs quartz

Clear crystals with very different care needs.

Selenite is a clear crystalline variety of gypsum, a hydrated calcium sulphate. Quartz is silicon dioxide. Both can look transparent or cloudy, but gypsum is much softer and needs especially gentle, dry handling.

See the differences ↓
Transparent irregular gypsum crystal on a small rock base against black
Gypsum (Selenite) reference specimen

Reference gypsum (selenite), separate from our collection. Clear areas and reflective edges provide clues to describe without splitting the crystal.

Eurico Zimbres and Tom Epaminondas / CC BY-SA 2.5 (via Wikimedia Commons). Original image; displayed at a smaller size.
Clear Quartz collection photograph
Clear Quartz

Our Clear Quartz collection specimen. Compare the visible surfaces, but do not assume every quartz crystal has this shape or clarity.

The differences at a glance

Reference properties describe the materials generally. They do not authenticate the photographed specimens.

Selenite vs quartz: reference properties
ClueSelenite (gypsum)Quartz
CompositionHydrated calcium sulphate · CaSO₄·2H₂OSilicon dioxide · SiO₂
Mohs hardness1.5–27
Cleavage and fracturePerfect cleavage in one direction; other cleavage directions also occurNo readily visible cleavage; often shell-like fracture
Possible appearanceClear, flat crystals; gypsum also has fibrous and massive formsClear or cloudy crystals, often prisms; many other forms occur
Display careKeep dry, support fragile areas and avoid soakingProtect points and avoid abrupt temperature changes

01 · Read the clues

Selenite and satin spar describe different looks.

Selenite usually refers to clear gypsum crystals. Fibrous gypsum is commonly called satin spar, while gypsum can also form rosette-like desert roses. These names describe appearances of gypsum; quartz is a different mineral.

If a shop label says selenite, record what the piece actually looks like too. Is it transparent and flat, or white and fibrous? A polished outline does not establish a naturally grown crystal shape, and a label alone is not an identification report.

02 · Read the clues

Look for surfaces, not a scratch opportunity.

Gypsum can have flat cleavage surfaces and a pearly or silky shine depending on its form. Quartz often shows a glassy surface and curved fractures. Study surfaces that already exist; neither softness nor cleavage needs to be demonstrated by damaging the piece.

In these two photographs, choose an area where light passes through and another where the surface reflects it. Describe those separately. Clear areas, cloudy patches and reflections depend on the specimen and lighting; they are not a two-question identification key.

03 · Read the clues

The practical difference is how you care for it.

Gypsum can dissolve in water. Keep a display specimen dry rather than soaking or wet-cleaning it, and do not peel layers or bend a thin crystal. A very soft dry brush may suit a sound surface; fragile edges are best left alone.

Quartz is much harder, but its points can still chip. Give both pieces their own supported space and avoid sudden heating. Where a specimen includes a matrix, repairs or coatings, ask about those too: the mineral name does not describe every part of an assembled piece.

Try it without damaging a stone

A one-minute observation

Without moving or touching either specimen, trace one clear area in each photograph and describe the surrounding edge. Write one sentence about the appearance and a separate sentence about the handling the reference properties suggest.

Should I use my fingernail to check whether a piece is selenite?

Not for this exercise. Gypsum’s low reference hardness explains why it needs care, but intentionally marking a finished or fragile specimen can spoil it. Begin with visible clues and the label; seek suitable examination if a firm identification matters.

Sources and further reading

Checked 5 October 2026. General mineral information supports these comparisons; collection labels are not laboratory identifications.

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