Zugshunstite-(Ce) is an extremely rare sulfate mineral found within the unique geological environment of the Zugspitze area. It typically forms small, tabular, yellow to brownish crystals in association with other rare secondary minerals in metamorphosed limestone.
Is this zugshunstite-(ce)?
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 zugshunstite-(ce) with a known reference. Zugshunstite-(Ce) sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Zugshunstite-(Ce) leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Zugshunstite-(Ce) typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellow-orange, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Zugshunstite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.

How to tell apart: Zugshunstite-(Ce) is noticeably harder (Mohs 3.5 vs. 2.5); luster reads vitreous on Zugshunstite-(Ce) and pearly on Lanthanite-(Ce).

How to tell apart: Luster reads vitreous on Zugshunstite-(Ce) and dull on Tengerite-(Y).
Often found alongside zugshunstite-(ce)
Minerals reported to co-occur with zugshunstite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaCe₂(SO₄)₂(OH)₂
- Mohs hardness
- 3.5
- Density
- 3.58 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metasomatized Limestone
- Typical price
- $200-800 per specimen
Where rockhounds find zugshunstite-(ce)
Classic worldwide localities
- ZUGspitze area, Germany
Field-hunting tip
Look in metasomatized limestone country — that is the host setting where zugshunstite-(ce) typically forms. If you start seeing anhydrite, gypsum, aphthitalite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.



