Geikielite is a rare magnesium titanium oxide mineral that often forms as dark, submetallic tabular crystals. It is most commonly found as water-worn pebbles in gem gravels, particularly in Sri Lanka, or as accessory minerals in contact-metamorphosed limestones.

Hardness
5-6
Mohs
Luster
Submetallic
Streak
Purplish brown
Transparency
Opaque to translucent

Is this geikielite?

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 geikielite with a known reference. Geikielite 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: purplish brown.
  • 3
    Read the luster
    Hold the specimen under a strong light. Luster: submetallic.
  • 4
    Match the color range
    Compare against the expected color range: bluish black, brownish black.
  • 5
    Look at form & habit
    Crystal system: trigonal. Typical habit: granular, prismatic, tabular.

Often confused with

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

Often found alongside geikielite

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

All properties

Chemical formula
MgTiO₃
Mohs hardness
5-6
Density
3.79-4.2 g/cm³
Streak
Purplish brown
Luster
Submetallic
Transparency
Opaque to translucent
Crystal system
Trigonal
Crystal habit
Granular, prismatic, tabular
Cleavage
{1011}
Rarity
Rare
Uses
Collector
Host rock
Forms during contact metamorphism of impure magnesian limestones

Where rockhounds find geikielite

Classic worldwide localities

  • Crestmore quarry, Riverside Co. and in the Santa Lucia Mountains, Monterey Co., California, USA
  • Skeleton Canyon, Cochise Co., Arizona, USA
  • Rakwana and Balangoda districts, Sri Lanka
  • Baltistan, Kashmir, Pakistan
  • Maxwell quarry, near Wakefield, Quebec, Canada
  • Fiskenæsset complex, western Greenland

Field-hunting tip

Where it forms: Forms during contact metamorphism of impure magnesian limestones. If you start seeing rutile, spinel, clinohumite in float, you are in the right ground. Typical habit: granular, prismatic, tabular. Train your eye for that shape before scanning the outcrop.

Common questions

How do you identify geikielite?+
Mohs hardness is 5-6. Luster: submetallic. The streak is purplish brown. Common colors include bluish black, brownish black.
Where is geikielite found?+
Notable localities include Crestmore quarry, Riverside Co. and in the Santa Lucia Mountains, Monterey Co., California, USA; Skeleton Canyon, Cochise Co., Arizona, USA; Rakwana and Balangoda districts, Sri Lanka; Baltistan, Kashmir, Pakistan; Maxwell quarry, near Wakefield, Quebec, Canada.
What rocks look like geikielite?+
Geikielite is most often confused with Ilmenite, Hematite, Pyrophanite. A quick hardness test and a streak check separate the look-alikes faster than color alone.
What minerals are found with geikielite?+
Geikielite commonly co-occurs with Rutile, Spinel, Clinohumite, Perovskite, Diopside, Serpentine. Spotting any of these in float or country rock is a useful trip signal.
What kind of rock does geikielite form in?+
Where it forms: Forms during contact metamorphism of impure magnesian limestones. Working float back to the host body is the standard way to chase a fresh occurrence.
What is geikielite used for?+
Geikielite is used in collector.

Find geikielite on the map

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