Laptevite-(Ce) is an extremely rare silicate mineral found primarily within the alkaline massif of the Dara-i-Pioz glacier. It typically occurs as small, yellow to brown prismatic crystals embedded in pegmatite boulders and requires professional analytical identification due to its similarity to other silicate species.

Hardness
4-4.5
Mohs
Luster
Vitreous to greasy
Transparency
Translucent

Is this laptevite-(ce)?

4-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 laptevite-(ce) with a known reference. Laptevite-(Ce) sits at Mohs 4-4.5, softer than the next harder reference, harder than the previous one.
  • 2
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous to greasy.
  • 3
    Match the color range
    Compare against the expected color range: brown.
  • 4
    Look at form & habit
    Crystal system: trigonal. Typical habit: prismatic crystals.

Often confused with

Laptevite-(Ce) vs. its common look-alikes, and how to tell them apart in the field.

Often found alongside laptevite-(ce)

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

All properties

Chemical formula
NaFe((Ce,REE)₇Ca₅Y₃)(SiO₄)₄(Si₃B₂PO₁₈)(BO₃)F₁₁
Mohs hardness
4-4.5
Density
4.61 g/cm³
Colors
Luster
Vitreous to greasy
Transparency
Translucent
Crystal system
Trigonal
Crystal habit
Prismatic crystals
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
A mineral of hydrothermal origin, discovered in a glacial moraine boulder of calcite-bafertisite-aegirine-microcline rock

Where rockhounds find laptevite-(ce)

Classic worldwide localities

  • Darai-Pioz glacier, at the junction of the Turkestan, Zeravshan, and Alay Mt. Ranges, Tien-Shan, Garmskii district, Northern Tajikistan

Field-hunting tip

Where it forms: A mineral of hydrothermal origin, discovered in a glacial moraine boulder of calcite-bafertisite-aegirine-microcline rock. If you start seeing quartz, fluorite, polylithionite in float, you are in the right ground. Typical habit: prismatic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify laptevite-(ce)?+
Mohs hardness is 4-4.5. Luster: vitreous to greasy. Common colors include brown.
Where is laptevite-(ce) found?+
Notable localities include Darai-Pioz glacier, at the junction of the Turkestan, Zeravshan, and Alay Mt. Ranges, Tien-Shan, Garmskii district, Northern Tajikistan.
Is laptevite-(ce) safe to handle?+
Contains rare earth elements and potential thorium impurities; store in a contained space and wash hands after handling to avoid ingestion of dust.
What rocks look like laptevite-(ce)?+
Laptevite-(Ce) is most often confused with Aegirine, Quartz. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with laptevite-(ce)?+
Laptevite-(Ce) commonly co-occurs with Quartz, Fluorite, Polylithionite, Albite, Intergrown with bafertisite, Calcy-beborosilite-. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does laptevite-(ce) form in?+
Where it forms: A mineral of hydrothermal origin, discovered in a glacial moraine boulder of calcite-bafertisite-aegirine-microcline rock. Working float back to the host body is the standard way to chase a fresh occurrence.
What is laptevite-(ce) used for?+
Laptevite-(Ce) is used in collector.

Find laptevite-(ce) on the map

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