Kaersutite is a titanium-rich amphibole typically found as short, prismatic, dark-colored crystals in alkaline volcanic or plutonic rocks. It is most easily identified by its distinctive dark brown color and classic amphibole cleavage, though it is often difficult to distinguish from other dark members of the amphibole group without chemical analysis.

Hardness
5-6
Mohs
Luster
Vitreous
Streak
Brownish gray
Transparency
Semitransparent

Is this kaersutite?

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 kaersutite with a known reference. Kaersutite sits at Mohs 5-6, softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Streak: brownish gray.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: vitreous.
  • 4
    Match the color range
    Compare against the expected color range: dark brown, black.
  • 5
    Look at form & habit
    Crystal system: monoclinic. Typical habit: prismatic crystals.

Often confused with

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

Often found alongside kaersutite

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

All properties

Chemical formula
NaCa₂(Mg₃AlTi)(Si₆Al₂)O₂₂O₂
Mohs hardness
5-6
Density
3.2-3.28 g/cm³
Streak
Brownish gray
Luster
Vitreous
Transparency
Semitransparent
Crystal system
Monoclinic
Crystal habit
Prismatic crystals
Cleavage
Perfect on {110}, intersecting at 56° and 124°; partings on {100}, {001}
Rarity
Uncommon
Uses
Collector
Host rock
Common as phenocrysts in alkalic volcanic rocks; in gabbroic and peridotitic nodules in alkalic basalts; in syenites, monzonites, carbonatite tuffs, and alkalic gabbros

Where rockhounds find kaersutite

Classic worldwide localities

  • Boulder Dam, Mohave Co., and near San Carlos, Gila Co., Arizona, USA
  • Linosa, Pelagian Islands, south of Sicily, Italy
  • Mont Saint-Hilaire, Quebec, Canada
  • Chikaishi, Oki Island, Shimane Prefecture, and at Mushozu and Numazu, Iki Island, Nagasaki Prefecture, Japan
  • Kakanui, New Zealand

Field-hunting tip

Where it forms: Common as phenocrysts in alkalic volcanic rocks; in gabbroic and peridotitic nodules in alkalic basalts; in syenites, monzonites, carbonatite tuffs, and alkalic gabbros. If you start seeing titanian augite, rhönite, olivine 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 kaersutite?+
Mohs hardness is 5-6. Luster: vitreous. The streak is brownish gray. Common colors include dark brown, black.
Where is kaersutite found?+
Notable localities include Boulder Dam, Mohave Co., and near San Carlos, Gila Co., Arizona, USA; Linosa, Pelagian Islands, south of Sicily, Italy; Mont Saint-Hilaire, Quebec, Canada; Chikaishi, Oki Island, Shimane Prefecture, and at Mushozu and Numazu, Iki Island, Nagasaki Prefecture, Japan; Kakanui, New Zealand.
What rocks look like kaersutite?+
Kaersutite is most often confused with Hornblende, Hastingsite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with kaersutite?+
Kaersutite commonly co-occurs with Titanian augite, Rhönite, Olivine, Ilmenite, Spinel, Plagioclase. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does kaersutite form in?+
Where it forms: Common as phenocrysts in alkalic volcanic rocks; in gabbroic and peridotitic nodules in alkalic basalts; in syenites, monzonites, carbonatite tuffs, and alkalic gabbros. Working float back to the host body is the standard way to chase a fresh occurrence.
What is kaersutite used for?+
Kaersutite is used in collector.

Find kaersutite on the map

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