Pseudomarkeyite is a rare pseudomorph where calcium carbonate (calcite) has replaced the unstable mineral ikaite, which typically forms in cold marine sediments. Collectors prize these for their unique, often elongated or 'fleur-de-lis' crystal shapes that retain the structural history of the original ikaite phase. They are typically found in glacial-marine sediments and require careful handling due to the fragile nature of these pseudomorphs.
Is this pseudomarkeyite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch pseudomarkeyite with a known reference. Pseudomarkeyite sits at Mohs 3, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pseudomarkeyite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pseudomarkeyite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, gray.
- 5Look at form & habitCrystal system: trigonal. Typical habit: pseudomorphs after ikaite.
Often confused with
Pseudomarkeyite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside pseudomarkeyite
Minerals reported to co-occur with pseudomarkeyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaCO₃
- Mohs hardness
- 3
- Density
- 2.71 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Trigonal
- Crystal habit
- Pseudomorphs After Ikaite
- Cleavage
- Perfect Rhombohedral
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Sedimentary Marine Deposits
- Typical price
- $20-150 per specimen
Where rockhounds find pseudomarkeyite
Classic worldwide localities
- Greenland
- Canada
- Norway
Field-hunting tip
Look in sedimentary marine deposits country, the host setting where pseudomarkeyite typically forms. If you start seeing calcite, aragonite in float, you are in the right ground. Field specimens usually show a pseudomorphs after ikaite habit, so train your eye for that shape before scanning the outcrop.



