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How to identify Bloodstone

Heliotrope (variety of Chalcedony)

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To correctly identify Bloodstone (Heliotrope (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. 1

    Color

    Overall color and any zoning or banding

    Dark green body color with distinct red, reddish-brown, or yellow spots/streaks.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Waxy to vitreous.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly granular, cryptocrystalline.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Massive, botryoidal, or stalactitic aggregates; individual crystals are microscopic.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None (cryptocrystalline quartz).

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in amygdaloidal cavities in volcanic rocks (e.g., basalts, andesites), alluvial deposits, and as secondary deposits in some metamorphic rocks. It forms from low-temperature hydrothermal solutions.

Key Facts

Hardness
6.5-7 on Mohs scale
Specific Gravity
2.58-2.64
Crystal System
Trigonal (cryptocrystalline aggregates)
Color
Dark green with red, reddish-brown, or yellow spots/streaks
Luster
Waxy to vitreous
Transparency
Opaque to translucent
Fracture
Conchoidal to uneven
Cleavage
None
Composition
Silicon dioxide (SiO2) with inclusions of chlorite, hornblende, and hematite

Physical characteristics

  • Crystal Habit: Massive, cryptocrystalline aggregates; individual crystals are microscopic and fibrous.
  • Cleavage Type: None, due to its cryptocrystalline structure.
  • Fracture Type: Conchoidal to uneven, typical of quartz varieties.
  • Tenacity: Brittle.
  • Luster Type: Waxy to vitreous, sometimes dull on unpolished surfaces.

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