Bytownite is a calcium-rich member of the plagioclase feldspar group, representing the compositional range between labradorite and anorthite. Collectors identify it by its specific gravity and optical properties often associated with mafic intrusive rocks like gabbros.
Is this bytownite?
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 bytownite with a known reference. Bytownite sits at Mohs 6-6.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Bytownite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Bytownite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, gray, yellowish, colorless.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, massive, granular.
Often confused with
Bytownite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside bytownite
Minerals reported to co-occur with bytownite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)(Al,Si)₄O₈
- Mohs hardness
- 6-6.5
- Density
- 2.72-2.75 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Perfect in Two Directions At Nearly 90 Degrees
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Mafic Igneous Rocks Such as Gabbro and Anorthosite
- Typical price
- $10-50 for small specimens
Where rockhounds find bytownite
Classic worldwide localities
- Ontario, Canada
- Norway
- Scotland
- Japan
- South Africa
Field-hunting tip
Look in mafic igneous rocks such as gabbro and anorthosite country — that is the host setting where bytownite typically forms. If you start seeing pyroxene, amphibole, olivine in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.







