Sulfhydrylbystrite is a rare member of the sodalite group often found in association with skarn-type metamorphic deposits. It is best distinguished by its vibrant yellow color and strong fluorescence, which makes it a highly sought-after specimen for advanced mineral collectors.
Is this sulfhydrylbystrite?
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 sulfhydrylbystrite with a known reference. Sulfhydrylbystrite sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Sulfhydrylbystrite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Sulfhydrylbystrite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, golden-yellow.
- 5Look at form & habitCrystal system: trigonal. Typical habit: prismatic crystals.
Often confused with
Sulfhydrylbystrite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sulfhydrylbystrite
Minerals reported to co-occur with sulfhydrylbystrite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)₈(Al₆Si₆O₂₄)(S,SO₄)₂
- Mohs hardness
- 5.5-6
- Density
- 2.3-2.4 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Prismatic Crystals
- Cleavage
- Poor
- Fluorescence
- Bright Yellow Under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Limestone
- Typical price
- $50-500 depending on crystal size and clarity
Where rockhounds find sulfhydrylbystrite
Classic worldwide localities
- Lake Baikal, Russia
- Lazurite deposits, Slyudyanka
Field-hunting tip
Look in metamorphic limestone country, the host setting where sulfhydrylbystrite typically forms. If you start seeing calcite, diopside, phlogopite in float, you are in the right ground. Field specimens usually show a prismatic crystals habit, so train your eye for that shape before scanning the outcrop.






