Tvalchrelidzeite is an extremely rare mercury sulfosalt found primarily in epithermal mercury-antimony deposits. It appears as metallic, dark gray to black grains and is characterized by its high density and complex chemical composition. Collectors typically acquire this mineral as small grains within associated mercury-bearing ore matrices.

Hardness
<3
Mohs
Luster
Adamantine
Streak
Nearly black, with a dark reddish tint
Transparency
Translucent

Is this tvalchrelidzeite?

5-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Test the hardness
    Try to scratch tvalchrelidzeite with a known reference. Tvalchrelidzeite sits at Mohs <3, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: nearly black, with a dark reddish tint.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: adamantine.
  • 4
    Match the color range
    Compare against the expected color range: lead gray.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: aggregates, granular.

Often confused with

Tvalchrelidzeite vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside tvalchrelidzeite

Minerals reported to co-occur with tvalchrelidzeite. Spotting these in float or country rock is a strong cue you are in the right ground.

All properties

Chemical formula
Hg₃SbAsS₃
Mohs hardness
<3
Density
7.380 g/cm³
Colors
Streak
Nearly black, with a dark reddish tint
Luster
Adamantine
Transparency
Translucent
Crystal system
Triclinic
Crystal habit
Aggregates, granular
Cleavage
Perfect in one direction
Rarity
Rare
Uses
Collector
Host rock
In gold-bearing hydrothermal As–Sb–Hg deposits

Where rockhounds find tvalchrelidzeite

Classic worldwide localities

  • Getchell mine, Potosi district, Humboldt Co., Nevada, USA
  • Gomi deposit, Caucasus Mountains, Georgia (type locality)
  • Tyute mercury deposit, Altai Mountains, Russia
  • Chauvai Sb–Hg deposit, Fergana Valley, Alai Range, southern Kyrgyzstan
  • Hemlo gold deposit, Thunder Bay district, Ontario, Canada

Field-hunting tip

Where it forms: In gold-bearing hydrothermal As–Sb–Hg deposits. If you start seeing cinnabar, metacinnabar, realgar in float, you are in the right ground. Typical habit: aggregates, granular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify tvalchrelidzeite?+
Mohs hardness is <3. Luster: adamantine. The streak is nearly black, with a dark reddish tint. Common colors include lead gray.
Where is tvalchrelidzeite found?+
Notable localities include Getchell mine, Potosi district, Humboldt Co., Nevada, USA; Gomi deposit, Caucasus Mountains, Georgia (type locality); Tyute mercury deposit, Altai Mountains, Russia; Chauvai Sb–Hg deposit, Fergana Valley, Alai Range, southern Kyrgyzstan; Hemlo gold deposit, Thunder Bay district, Ontario, Canada.
Is tvalchrelidzeite safe to handle?+
Tvalchrelidzeite contains antimony, arsenic and mercury and calls for real care. Contains mercury, antimony, and arsenic; wash hands thoroughly after handling and avoid inhaling dust.
What rocks look like tvalchrelidzeite?+
Tvalchrelidzeite is most often confused with Cinnabar, Livingstonite, Stibnite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with tvalchrelidzeite?+
Tvalchrelidzeite commonly co-occurs with Cinnabar, Metacinnabar, Realgar, Mercurian tennantite, Mercury, Cubanite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does tvalchrelidzeite form in?+
Where it forms: In gold-bearing hydrothermal As–Sb–Hg deposits. Working float back to the host body is the standard way to chase a fresh occurrence.
What is tvalchrelidzeite used for?+
Tvalchrelidzeite is used in collector.

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