Terlinguaite

A variety of Minerals

Terlinguaite specimen

What is Terlinguaite?

Terlinguaite is the naturally occurring mineral with formula Hg2ClO. It is formed by the weathering of other mercury-containing minerals. It was discovered in 1900 in the Terlingua District of Brewster County, Texas, for which it is named. Its color is yellow, greenish yellow, brown, or olive green.

Market Value Factors

Pricing varies for every rock and mineral, so use these universal factors to gauge Terlinguaite before comparing listings or appraisals.

Size & Weight

Larger, intact specimens usually command higher prices.

Rarity & Demand

Scarce material or popular varieties sell at a premium.

Condition & Finish

Chips, repairs, and heavy wear lower value; clean prep helps.

Treatment & Provenance

Untreated specimens with documented locality are prized.

Applies to all rocks & minerals.

Terlinguaite Localities Map

See where Terlinguaite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.

Map preview
North ZoneCentral RidgeSouth Basin

Interactive map layers and collecting notes are available in the app.

Quick Facts

Physical Properties

Color
Yellow-, yellow-green, brown (darkens to olive-green on exposure to light); pale olive-green in transmitted light
Hardness (Mohs)
2 - 3
Density
8.73 g/cm³
Streak
Lemon yellow

Chemical Properties

Chemical Formula
[Hg3]4+Hg2+Cl2O2
Elements
Cl, Hg, O
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Terlinguaite FAQs

How do I identify Terlinguaite?

Terlinguaite can be identified by its hardness of 2 - 3 on the Mohs scale, Yellow- color. Look for these key characteristics when examining specimens.

What color is Terlinguaite?

Terlinguaite typically appears in Yellow-, yellow-green, brown (darkens to olive-green on exposure to light); pale olive-green in transmitted light. Color can vary depending on impurities and formation conditions.

How hard is Terlinguaite?

Terlinguaite has a hardness of 2 - 3 on the Mohs scale. This makes it a soft mineral that can be scratched easily.

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