Ivanyukite-K is a rare titanium silicate mineral found primarily in the alkaline massifs of the Kola Peninsula. It typically forms small, pale bluish rhombohedral crystals or crusts within pegmatitic cavities, often requiring micro-analysis for definitive identification.

Hardness
~4
Mohs
Luster
Vitreous
Streak
White
Transparency
Translucent

Is this ivanyukite-k?

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 ivanyukite-k with a known reference. Ivanyukite-K sits at Mohs ~4, 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.
  • 4
    Match the color range
    Compare against the expected color range: pale blue.
  • 5
    Look at form & habit
    Crystal system: cubic. Typical habit: cubic crystals.

Often confused with

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

Often found alongside ivanyukite-k

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

All properties

Chemical formula
K₂Ti₄(SiO₄)₃O₂(OH)₂·9H₂O
Mohs hardness
~4
Density
2.70 g/cm³
Colors
Streak
White
Luster
Vitreous
Transparency
Translucent
Crystal system
Cubic
Crystal habit
Cubic crystals
Cleavage
Perfect on {100}
Rarity
Rare
Uses
Collector
Host rock
A late-stage, hydrothermal phase in natrolitized microcline-aegirine-sodalite lens in orthoclase-bearing urtite

Where rockhounds find ivanyukite-k

Classic worldwide localities

  • Koashva Quarry, Koashva Mountain, Khibiny Massif, Kola Peninsula, Russia

Field-hunting tip

Where it forms: A late-stage, hydrothermal phase in natrolitized microcline-aegirine-sodalite lens in orthoclase-bearing urtite. If you start seeing microcline, vinogradovite, sazykinaite- in float, you are in the right ground. Typical habit: cubic crystals. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify ivanyukite-k?+
Mohs hardness is ~4. Luster: vitreous. The streak is white. Common colors include pale blue.
Where is ivanyukite-k found?+
Notable localities include Koashva Quarry, Koashva Mountain, Khibiny Massif, Kola Peninsula, Russia.
What rocks look like ivanyukite-k?+
Ivanyukite-K is most often confused with Ivanyukite-Na, Ivanyukite-Cu. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with ivanyukite-k?+
Ivanyukite-K commonly co-occurs with Microcline, Vinogradovite, Sazykinaite-, Natrolite, Djerfisherite, Chalcopyrite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does ivanyukite-k form in?+
Where it forms: A late-stage, hydrothermal phase in natrolitized microcline-aegirine-sodalite lens in orthoclase-bearing urtite. Working float back to the host body is the standard way to chase a fresh occurrence.
What is ivanyukite-k used for?+
Ivanyukite-K is used in collector.

Find ivanyukite-k on the map

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