Kobokoboite is a rare hydrous aluminum phosphate mineral first discovered in the pegmatites of the Democratic Republic of the Congo. It typically occurs as white, pearly, platy aggregates and is highly sought after by systematic mineral collectors due to its extremely limited locality distribution.

Hardness
2
Mohs
Luster
Pearly
Streak
White
Transparency
Translucent to transparent

Is this kobokoboite?

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 kobokoboite with a known reference. Kobokoboite sits at Mohs 2, 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: pearly.
  • 4
    Match the color range
    Compare against the expected color range: white.
  • 5
    Look at form & habit
    Crystal system: triclinic. Typical habit: platy aggregates, microcrystalline.

Often confused with

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

Often found alongside kobokoboite

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

All properties

Chemical formula
Al₆(PO₄)₄(OH)₆·11H₂O
Mohs hardness
2
Density
2.21 g/cm³
Colors
Streak
White
Luster
Pearly
Transparency
Translucent to transparent
Crystal system
Triclinic
Crystal habit
Platy aggregates, microcrystalline
Cleavage
None
Rarity
Rare
Uses
Collector
Host rock
A secondary mineral formed by weathering of the upper branch of a zoned albite-beryl-microcline pegmatite of the LCT family, rare-element class, Li subclass, beryl type, beryl– columbite/beryl–phosphate subtype

Where rockhounds find kobokoboite

Classic worldwide localities

  • Kobokobo pegmatite, South Kivu Province, Democratic Republic of the Congo

Field-hunting tip

Where it forms: A secondary mineral formed by weathering of the upper branch of a zoned albite-beryl-microcline pegmatite of the LCT family, rare-element class, Li subclass, beryl type, beryl– columbite/beryl–phosphate subtype. If you start seeing frondelite, keckite, planerite in float, you are in the right ground. Typical habit: platy aggregates, microcrystalline. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify kobokoboite?+
Mohs hardness is 2. Luster: pearly. The streak is white. Common colors include white.
Where is kobokoboite found?+
Notable localities include Kobokobo pegmatite, South Kivu Province, Democratic Republic of the Congo.
What rocks look like kobokoboite?+
Kobokoboite is most often confused with Wavellite, Variscite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with kobokoboite?+
Kobokoboite commonly co-occurs with Frondelite, Keckite, Planerite, Variscite, Wavellite, Evansite. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does kobokoboite form in?+
Where it forms: A secondary mineral formed by weathering of the upper branch of a zoned albite-beryl-microcline pegmatite of the LCT family, rare-element class, Li subclass, beryl type, beryl– columbite/beryl–phosphate subtype. Working float back to the host body is the standard way to chase a fresh occurrence.
What is kobokoboite used for?+
Kobokoboite is used in collector.

Find kobokoboite on the map

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