How to identify Dendritic Opal
SiO2·nH2O
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Open the appTo correctly identify Dendritic Opal (SiO2·nH2O), 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
Base color is typically white, gray, cream, pale yellow, or colorless. Dendritic inclusions are black, brown, or reddish-brown.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous to waxy, sometimes resinous.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Smooth to slightly uneven, conchoidal fracture surfaces.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Amorphous; does not form true crystals. Occurs as botryoidal, reniform, stalactitic, or massive aggregates filling cavities or veins.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None, due to its amorphous nature.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in low-temperature hydrothermal veins, as amygdule fillings in volcanic rocks, in sedimentary deposits where silica-rich waters have percolated, and as replacements of organic material or other minerals. Often associated with chalcedony, quartz, and other silica minerals.
Key Facts
- Hardness
- 5.5 - 6.5 (Mohs scale)
- Specific Gravity
- 1.98 - 2.25
- Crystal System
- Amorphous
- Color
- Colorless, white, gray, cream, pale yellow, with black, brown, or reddish-brown dendritic inclusions.
- Luster
- Vitreous to waxy, sometimes resinous.
- Transparency
- Translucent to opaque.
- Fracture
- Conchoidal to uneven.
- Cleavage
- None.
- Composition
- Hydrated silicon dioxide (SiO2·nH2O) with manganese or iron oxide inclusions.
Physical characteristics
- Crystal Habit: Massive, botryoidal, reniform, stalactitic, or as vein fillings. Never forms euhedral crystals.
- Cleavage Type: None.
- Fracture Type: Conchoidal to uneven.
- Tenacity: Brittle.
- Luster Type: Vitreous, waxy, resinous.
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