Ivanyukite-Cu is a rare titanium silicate mineral found primarily within the alkaline pegmatites of the Khibiny Massif. It typically occurs as small, sharp rhombohedral crystals that are prized by mineral collectors for their vibrant green color and crystalline clarity.

Hardness
~4
Mohs
Luster
Vitreous
Streak
Pale green
Transparency
Translucent

Is this ivanyukite-cu?

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-cu with a known reference. Ivanyukite-Cu 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: pale green.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: bright green.
  • 5
    Look at form & habit
    Crystal system: cubic. Typical habit: cubic crystals.

Often confused with

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

Often found alongside ivanyukite-cu

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

All properties

Chemical formula
CuTi₄(SiO₄)₃O₂(OH)₂·7H₂O
Mohs hardness
~4
Density
2.70 g/cm³
Streak
Pale green
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-cu

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-cu?+
Mohs hardness is ~4. Luster: vitreous. The streak is pale green. Common colors include bright green.
Where is ivanyukite-cu found?+
Notable localities include Koashva Quarry, Koashva Mountain, Khibiny Massif, Kola Peninsula, Russia.
Is ivanyukite-cu safe to handle?+
Ivanyukite-Cu contains copper. Wash your hands afterwards, never grind or breathe the dust, and store it apart from specimens you handle often.
What rocks look like ivanyukite-cu?+
Ivanyukite-Cu is most often confused with Ivanyukite-Na, Ivanyukite-K. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with ivanyukite-cu?+
Ivanyukite-Cu 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-cu 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-cu used for?+
Ivanyukite-Cu is used in collector.

Find ivanyukite-cu 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