How to identify Bloodstone
Heliotrope (a variety of Chalcedony)
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Open the appTo correctly identify Bloodstone (Heliotrope (a variety of Chalcedony)), 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
Dark green to greenish-blue body color with characteristic red, reddish-brown, or yellow spots/patches.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Waxy to vitreous (glassy) when polished, dull to waxy on rough surfaces.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Smooth, microcrystalline texture. Fracture surfaces are typically conchoidal.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Cryptocrystalline, meaning individual crystals are too small to be seen without high magnification. Forms in massive, botryoidal, or stalactitic habits.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None, due to its cryptocrystalline nature.
- 6
Geological Environment
The rock formation and setting where it occurs
Typically found in association with volcanic rocks (e.g., basalts, andesites) where silica-rich fluids have circulated, or in alluvial deposits (riverbeds, gravels) where it has been eroded from its primary source.
Key Facts
- Hardness
- 6.5-7 on Mohs scale
- Specific Gravity
- 2.58-2.64
- Crystal System
- Trigonal (cryptocrystalline)
- Color
- Dark green with red, reddish-brown, or yellow spots
- Luster
- Waxy to dull (unpolished), vitreous (polished)
- Transparency
- Translucent to opaque
- Fracture
- Conchoidal to uneven
- Cleavage
- None
- Composition
- Silicon dioxide (SiO2) with iron oxide (hematite) and chlorite/hornblende inclusions
Physical characteristics
- Crystal Habit: Massive, botryoidal, stalactitic; cryptocrystalline aggregates
- Cleavage Type: None
- Fracture Type: Conchoidal to uneven
- Tenacity: Tough
- Luster Type: Waxy to dull (unpolished), vitreous (polished)
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