Mineral field guide

How to identify celestite

Celestite is a strontium sulfate mineral commonly found as pale blue, white, or colorless tabular crystals with high density, white streak, good cleavage, and hardness near 3 to 3.5.

mineralStrontium sulfate · SrSO₄

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Cluster of pale, faintly blue celestite crystals from Lampasas County, Texas
Faintly blue celestite crystals from Lampasas County, TexasPhoto: Dexter Perkins · CC0 1.0 · Wikimedia Commons
Classification

What is celestite?

Celestite is strontium sulfate and forms a solid-solution relationship with barite in some natural materials. Color may come from defects or impurities and is not a reliable measure of composition.

Appearance

What does celestite look like?

Crystals commonly form transparent to translucent tablets, blades, or prisms with vitreous to pearly luster. It also occurs fibrous, granular, or massive.

Although pale blue is memorable, many specimens are white, gray, yellowish, reddish, or colorless and can resemble barite, calcite, or gypsum.

Field tests

Identification tests

Begin with observation and use the least destructive test first. Results can change with weathering, mixtures, coatings, and grain size. Review the step-by-step field-test methods before altering an unfamiliar specimen.

Density

High; specific gravity commonly near 4

Heavier than calcite or gypsum but often slightly lighter than barite.

Hardness

About 3 to 3.5

Scratched by steel and overlaps barite and calcite.

Cleavage

Good to perfect in more than one direction

Produces flat reflective breaks but is not decisive against barite.

Streak

White

Consistent but shared by many pale minerals.

Comparison

Common lookalikes

Barite

Usually slightly denser; visual separation can be unreliable without measured density or analysis.

Calcite

Much lighter and reacts vigorously with dilute acid.

Gypsum

Much softer at Mohs 2 and lighter.

Geologic origin

How does it form?

Celestite forms in sedimentary evaporite and carbonate environments, in cavities and geodes, and through low-temperature hydrothermal processes.

It may occur with gypsum, anhydrite, calcite, sulfur, halite, fluorite, or barite.

Where it occurs

Geologic setting and occurrence

Celestite occurs in sedimentary basins, evaporite sequences, carbonate cavities, and some geodes, with important deposits in several parts of the world and scattered U.S. occurrences.

Blue color alone does not establish celestite, and a hand specimen may require specific-gravity or analytical confirmation.

Human use

Uses and significance

Celestite is the principal mineral source of strontium, used in ceramics, glass, ferrite magnets, pyrotechnics, metallurgy, and other chemical applications.

Safety and limits

Field notes

  • Do not perform flame tests outside a controlled laboratory.
  • Compare measured volume and mass rather than subjective heft when possible.
  • Avoid dust and do not ingest unknown sulfate minerals.

This guide supports preliminary field identification, not a laboratory determination, appraisal, hazard assessment, or statement of ownership or collecting permission. Verify land status and local rules before handling or collecting material.

Source basis

Authoritative sources

LithoMap wrote this guide in original language using the scientific concepts and physical-property standards supported by these sources.

Editorial review: September 17, 2026.