Siudaite is an extremely rare member of the eudialyte group typically found in agpaitic pegmatites on the Kola Peninsula. It most commonly occurs as small, tabular, yellow-tinted crystals in association with other rare alkaline minerals. Identification usually requires professional analysis due to its striking similarity to other eudialyte-group members.
Is this siudaite?
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 siudaite with a known reference. Siudaite sits at Mohs 4.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow, brownish yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: tabular crystals.
Often confused with
Siudaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside siudaite
Minerals reported to co-occur with siudaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₈(Mn₂Na)Ca₆Fe₃Zr₃NbSi₂₅O₇₄(OH)₂Cl(H₂O)₅
- Mohs hardness
- 4.5
- Density
- 2.96 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Tabular crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A product of the hydrothermal alteration of a primary eudialyte-group mineral presumably related to georgbarsanovite, in a peralkaline pegmatite
Where rockhounds find siudaite
Classic worldwide localities
- Astrophyllitovyi Stream valley, Mt. Eveslogchorr, Khibiny alkaline massif, Kola Peninsula, Russia
Field-hunting tip
Where it forms: A product of the hydrothermal alteration of a primary eudialyte-group mineral presumably related to georgbarsanovite, in a peralkaline pegmatite. If you start seeing aegirine, albite, microcline in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.







