Mineral field guide

How to identify barite

Barite is a notably heavy, relatively soft barium sulfate mineral commonly recognized by high density, white streak, tabular or bladed crystals, and hardness near 3 to 3.5.

mineralBarium sulfate · BaSO₄

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Light whitish barite crystals on iron-oxide-stained, fine-grained quartz from near Joplin, Missouri
Barite crystals on iron-stained quartz; the light crystals are baritePhoto: Twyla Baker · CC0 1.0 · Wikimedia Commons
Classification

What is barite?

Barite is barium sulfate. Strontium, lead, calcium, and other elements may substitute in limited amounts, and natural specimens commonly contain quartz, calcite, fluorite, sulfides, or iron-oxide coatings.

Appearance

What does barite look like?

Crystals may be tabular, bladed, prismatic, cockscomb-like, or arranged in rosettes. Massive barite can be white, colorless, gray, tan, yellow, blue, reddish, or brown.

Fresh surfaces are vitreous to pearly, while weathered or iron-stained material can appear dull and earthy. Density is usually more informative than color.

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 4.5

Feels conspicuously heavy compared with quartz, calcite, or gypsum of equal size.

Hardness

About 3 to 3.5

Scratched by steel and near the hardness of calcite.

Streak

White

Expected for fresh barite but not distinctive alone.

Acid response

No ordinary effervescence

Separates barite from calcite despite similar hardness.

Comparison

Common lookalikes

Calcite

Much lighter and reacts vigorously with dilute acid.

Celestite

Also a heavy sulfate with similar habit but commonly somewhat lighter; reliable separation may require density or chemical analysis.

Gypsum

Much softer and substantially lighter.

Geologic origin

How does it form?

Barite precipitates from hydrothermal fluids in veins and replacement deposits, forms in sedimentary exhalative systems, and occurs as concretions or beds in some marine sedimentary rocks.

It commonly accompanies fluorite, calcite, quartz, galena, sphalerite, and other vein minerals.

Where it occurs

Geologic setting and occurrence

Barite occurs in veins, sediment-hosted deposits, marine beds, concretions, and some hot-spring or cave settings across the United States.

A heavy white mineral is not automatically barite; lead minerals, celestite, and manufactured material require consideration.

Human use

Uses and significance

Most barite is ground as a weighting agent in drilling fluids. It is also used in barium chemicals, radiation-shielding products, fillers, and selected medical or industrial applications.

Safety and limits

Field notes

  • Compare equal-size pieces when judging heft.
  • Do not taste or ingest suspected barium minerals.
  • Mine waste may contain lead, zinc, or other sulfides; avoid dust and wash hands.

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.