Hydrokenopyrochlore is a rare antimony sodium niobium oxide that forms tan to beige porous, subhedral octahedral crystals. It occurs in a Li-Cs-Ta-type pegmatite intruded into dolomitic marble. It was first described from the Antandrokomby pegmatite, Vakinankaratra region, Antananarivo Province, Madagascar.

Hardness
5-5.5
Mohs
Luster
Resinous
Streak
White
Transparency
Translucent

Is this hydrokenopyrochlore?

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 hydrokenopyrochlore with a known reference. Hydrokenopyrochlore sits at Mohs 5-5.5, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: white.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: resinous.
  • 4
    Match the color range
    Compare against the expected color range: tan, beige.
  • 5
    Look at form & habit
    Crystal system: cubic. Typical habit: porous, subhedral octahedral crystals.

Often confused with

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

Often found alongside hydrokenopyrochlore

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

All properties

Chemical formula
(☐,Sb³⁺,Na)₂Nb₂O₆·H₂O
Mohs hardness
5-5.5
Density
5.984 g/cm³
Colors
Streak
White
Luster
Resinous
Transparency
Translucent
Crystal system
Cubic
Crystal habit
Porous, subhedral octahedral crystals
Rarity
Rare
Uses
Collector, Scientific research
Host rock
From a Li-Cs-Ta-type pegmatite intruded into dolomitic marble

Where rockhounds find hydrokenopyrochlore

Classic worldwide localities

  • Antandrokomby pegmatite, near Mt. Ibity, southern Sahatany Pegmatite Field, Manandona Valley, Vakinankaratra region, Antananarivo Province, Madagascar

Field-hunting tip

Where it forms: From a Li-Cs-Ta-type pegmatite intruded into dolomitic marble. If you start seeing quartz, orthoclase, li-rich mica in float, you are in the right ground. Typical habit: porous, subhedral octahedral crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify hydrokenopyrochlore?+
Mohs hardness is 5-5.5. Luster: resinous. The streak is white. Common colors include tan, beige.
Where is hydrokenopyrochlore found?+
Notable localities include Antandrokomby pegmatite, near Mt. Ibity, southern Sahatany Pegmatite Field, Manandona Valley, Vakinankaratra region, Antananarivo Province, Madagascar.
Is hydrokenopyrochlore safe to handle?+
Hydrokenopyrochlore contains antimony. Contains antimony, which is toxic if ingested or inhaled as dust. Wash hands thoroughly after handling and avoid creating dust.
What rocks look like hydrokenopyrochlore?+
Hydrokenopyrochlore is most often confused with Pyrochlore. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with hydrokenopyrochlore?+
Hydrokenopyrochlore commonly co-occurs with Quartz, Orthoclase, Li-rich mica, Hübnerite, Stibiotantalite, Tourmaline. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does hydrokenopyrochlore form in?+
Where it forms: From a Li-Cs-Ta-type pegmatite intruded into dolomitic marble. Working float back to the host body is the standard way to chase a fresh occurrence.
What is hydrokenopyrochlore used for?+
Hydrokenopyrochlore is used in collector, scientific research.

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