How to identify Sulfur
S
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Open the appTo correctly identify Sulfur (S), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Bright yellow, lemon yellow, brownish yellow, greenish yellow, or grayish yellow. Can be discolored by impurities.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Resinous to greasy, sometimes adamantine on crystal faces.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Typically massive, earthy, or powdery. Crystalline forms show distinct faces.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Orthorhombic dipyramidal crystals are common, often forming bipyramids, tabular crystals, or thick prisms. Also occurs as massive, reniform, stalactitic, or encrusting forms.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Poor to indistinct on {001}, {110}, and {111}. Fracture is more characteristic.
- 6
Geological Environment
The rock formation and setting where it occurs
Volcanic fumaroles and solfataras, hot springs, sedimentary evaporite deposits (especially associated with gypsum/anhydrite and hydrocarbons in salt domes), and as an alteration product of sulfide minerals.
Key Facts
- Hardness
- 1.5-2.5 (Mohs scale)
- Specific Gravity
- 2.07-2.09 g/cm³
- Crystal System
- Orthorhombic
- Color
- Bright yellow, lemon yellow, brownish yellow, greenish yellow, grayish yellow
- Luster
- Resinous to greasy, sometimes adamantine
- Transparency
- Transparent to translucent
- Fracture
- Conchoidal to uneven
- Cleavage
- Poor to indistinct on {001}, {110}, {111}
- Composition
- Elemental Sulfur (S)
Physical characteristics
- Crystal Habit: Dipyramidal, tabular, prismatic, massive, reniform, stalactitic, encrusting, powdery
- Cleavage Type: Poor/Indistinct
- Fracture Type: Conchoidal to uneven, very brittle
- Tenacity: Brittle
- Luster Type: Resinous to greasy
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