Pekovite is an extremely rare member of the eudialyte group found primarily in the agpaitic pegmatites of the Khibiny Massif. It typically forms colorless to white equant crystals and is best identified through micro-analytical methods due to its visual similarity to other complex silicates in alkaline suites.

Hardness
6.5-7
Mohs
Luster
Vitreous, slightly greasy
Streak
White
Transparency
Transparent to translucent

Is this pekovite?

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 pekovite with a known reference. Pekovite sits at Mohs 6.5-7, 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: vitreous, slightly greasy.
  • 4
    Match the color range
    Compare against the expected color range: colorless.
  • 5
    Look at form & habit
    Crystal system: orthorhombic. Typical habit: intergrown crystals.

Often confused with

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

Often found alongside pekovite

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

All properties

Chemical formula
SrB₂Si₂O₈
Mohs hardness
6.5-7
Density
3.35 g/cm³
Colors
Streak
White
Luster
Vitreous, slightly greasy
Transparency
Transparent to translucent
Crystal system
Orthorhombic
Crystal habit
Intergrown crystals
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
Within a block of quartz in the moraine of the Dara-i-Pioz glacier, Alai mountain range, Tien Shan, northern Tajikistan

Where rockhounds find pekovite

Classic worldwide localities

  • Dara-i-Pioz glacier, Alai mountain range, Tien Shan, northern Tajikistan

Field-hunting tip

Where it forms: Within a block of quartz in the moraine of the Dara-i-Pioz glacier, Alai mountain range, Tien Shan, northern Tajikistan. If you start seeing intergrown with pectolite, highly strontian fluorite, aegirine in float, you are in the right ground. Typical habit: intergrown crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify pekovite?+
Mohs hardness is 6.5-7. Luster: vitreous, slightly greasy. The streak is white. Common colors include colorless.
Where is pekovite found?+
Notable localities include Dara-i-Pioz glacier, Alai mountain range, Tien Shan, northern Tajikistan.
What rocks look like pekovite?+
Pekovite is most often confused with Eudialyte, Kentbrooksite, Zircon. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with pekovite?+
Pekovite commonly co-occurs with Intergrown with pectolite, Highly strontian fluorite, Aegirine. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does pekovite form in?+
Where it forms: Within a block of quartz in the moraine of the Dara-i-Pioz glacier, Alai mountain range, Tien Shan, northern Tajikistan. Working float back to the host body is the standard way to chase a fresh occurrence.
What is pekovite used for?+
Pekovite is used in collector.

Find pekovite on the map

RockHoundR shows mapped rockhounding spots, access rules, and lets you log every find.

Download on the App StoreGet it on Google Play