Akimotoite is a high-pressure polymorph of enstatite that forms only under the extreme conditions of planetary collisions. It is found exclusively in shock-metamorphosed meteorites as microscopic inclusions associated with other high-pressure silicate minerals. Its identification requires advanced X-ray diffraction or microprobe analysis due to its rarity and lack of macro-scale crystal development.

Hardness
7-8
Mohs
Luster
Submetallic
Streak
Brown
Transparency
Opaque

Is this akimotoite?

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 akimotoite with a known reference. Akimotoite sits at Mohs 7-8 — softer than the next harder reference, harder than the previous one.
  • 2
    Check the streak
    Drag the specimen across an unglazed porcelain plate. Akimotoite leaves a brown streak.
  • 3
    Read the luster
    Hold the specimen under a strong light. Akimotoite typically shows a submetallic luster.
  • 4
    Match the color range
    Compare against the expected color range: dark brown, black.
  • 5
    Look at form & habit
    Crystal system: trigonal. Typical habit: microscopic grains.

Often confused with

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

Often found alongside akimotoite

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

All properties

Chemical formula
MgSiO₃
Mohs hardness
7-8
Density
4.67 g/cm³
Streak
Brown
Luster
Submetallic
Transparency
Opaque
Crystal system
Trigonal
Crystal habit
Microscopic Grains
Cleavage
None
Rarity
Rare
Uses
Collector, Scientific Research
Host rock
Shock-metamorphosed Meteorites
Typical price
very expensive, strictly restricted to research and high-end meteorite collections

Where rockhounds find akimotoite

Classic worldwide localities

  • Tenham meteorite (Australia)
  • Suizhou meteorite (China)
  • Umbala meteorite (India)

Field-hunting tip

Look in shock-metamorphosed meteorites country — that is the host setting where akimotoite typically forms. If you start seeing bridgmanite, ringwoodite, wadsleyite in float, you are in the right ground. Field specimens usually show a microscopic grains habit, so train your eye for that shape before scanning the outcrop.

Common questions

How do you identify akimotoite?+
Mohs hardness is 7-8. It typically shows a submetallic luster. The streak is brown. Common colors include dark brown, black.
Where is akimotoite found?+
Notable localities include Tenham meteorite (Australia); Suizhou meteorite (China); Umbala meteorite (India).
How much is akimotoite worth?+
Typical asking prices fall in the range of very expensive, strictly restricted to research and high-end meteorite collections. Quality, size, and provenance can move individual specimens well outside that range.
What rocks look like akimotoite?+
Akimotoite is most often confused with Enstatite, Manaccanite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with akimotoite?+
Akimotoite commonly co-occurs with Bridgmanite, Ringwoodite, Wadsleyite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does akimotoite form in?+
Akimotoite typically forms in shock-metamorphosed meteorites. Working float back to the host body is the standard way to chase a fresh occurrence.
What is akimotoite used for?+
Akimotoite is used in collector, scientific research.

Find akimotoite on the map

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