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BIRITE ROCK

Naturally Occurring Mineral Sample: Authentic birite specimen with intact surface characteristics for accurate geological study.

Education-Grade Preparation: Cleaned and size-standardized for safe handling, display, and repeated instructional use.

220.00

Quick Answer: This specimen belongs to the barite (barium sulphate) mineral group, prized in teaching collections for one surprising property: it feels noticeably heavier than its pale, non-metallic appearance suggests, making it a classic demonstration of specific gravity.

Product Description

Barite (barium sulphate, BaSO₄) is best known in mineralogy classrooms for its unusually high specific gravity relative to its appearance. Most students expect a pale, non-metallic mineral to feel light, similar to quartz or calcite — barite defies that expectation, weighing noticeably more than same-sized specimens of common silicate minerals. This makes it a memorable, hands-on counter-example when teaching that colour and lustre alone are unreliable indicators of a mineral’s density.

Barite typically forms tabular or bladed crystals and commonly occurs in hydrothermal veins and as a cement in sedimentary rocks, often associated with sulphide ore deposits. Its high density comes from barium, a relatively heavy element, being tightly bound within its crystal lattice. Beyond the classroom, barite’s density is put to industrial use as a weighting agent in drilling fluids — a real-world link that helps students see how a single physical property can matter well outside a geology lab.

Specimen Details

Detail Description
Mineral group Barite (barium sulphate, BaSO₄)
Key teaching property Unusually high specific gravity for a non-metallic mineral
Typical crystal habit Tabular or bladed crystals
Typical occurrence Hydrothermal veins, sedimentary cement near sulphide deposits
Typical use Specific gravity and density-comparison teaching demonstrations

Applications

  • Demonstrating that appearance alone doesn’t predict a mineral’s density
  • Specific gravity comparison exercises alongside lighter silicate minerals
  • Introducing barium-bearing minerals in a chemistry-linked earth science unit
  • Discussing real-world mineral uses, such as drilling-fluid weighting agents

Care & Handling

Handle the specimen carefully, as tabular or bladed crystal edges can chip if dropped. Store separated from harder specimens in a compartmented tray, and keep it with the rest of the collection’s density-comparison set so students can weigh it against lighter reference minerals.

Why Choose LabEquip

This specimen is part of LabEquip’s wider Educational Rock and Minerals range. Pair it with our Specific Gravity Collection for a broader density-comparison lesson, or browse our Chemistry Lab Equipment range for related classroom apparatus.

Frequently Asked Questions

Why does this specimen feel heavier than expected?

It belongs to the barite (barium sulphate) group, which has an unusually high specific gravity for a non-metallic-looking mineral, due to the relatively heavy barium atoms in its crystal structure.

What is barite chemically?

Barite is barium sulphate (BaSO₄), typically forming tabular or bladed crystals in hydrothermal veins or as a cement in sedimentary rocks.

What is barite used for outside the classroom?

Its high density makes it a common weighting agent in drilling fluids used in the oil and gas industry, a practical real-world application of a mineral property taught in geology class.

How should I use this specimen for a specific gravity lesson?

Compare its weight against a similarly sized lighter mineral, such as quartz or calcite, by hand or using a balance, to illustrate that appearance doesn’t reliably predict density.

Is this specimen fragile?

The tabular or bladed crystal edges can chip if dropped, so it should be handled carefully and stored separated from harder specimens.

What level is this specimen suited to?

It works well for secondary school earth science and as a supporting specimen in introductory college mineralogy coursework.

Last Updated: September 2026

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