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How to identify Carnelian Agate

SiO2 (Chalcedony variety)

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To correctly identify Carnelian Agate (SiO2 (Chalcedony variety)), 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

    Ranges from pale orange to intense reddish-orange, deep red, and brownish-red. The color is generally uniform but can show subtle banding or cloudiness.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Waxy to vitreous (glassy) when polished; dull to waxy on rough surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly granular on fracture surfaces; takes a high polish.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Cryptocrystalline, meaning individual crystals are too small to be seen without high magnification. Typically occurs in botryoidal, mammillary, or stalactitic masses, or as nodular concretions and vein fillings.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None. Exhibits a conchoidal fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Primarily found in amygdaloidal cavities (vesicles) and fissures within extrusive igneous rocks (basalts, andesites, rhyolites) and in secondary alluvial or colluvial deposits derived from these rocks. Also occurs in some sedimentary formations.

Key Facts

Hardness
6.5-7 on Mohs scale
Specific Gravity
2.58-2.64
Crystal System
Trigonal (cryptocrystalline aggregates)
Color
Reddish-orange, red, brownish-red
Luster
Waxy to vitreous
Transparency
Translucent to opaque
Fracture
Conchoidal to uneven
Cleavage
None
Composition
Silicon dioxide (SiO2) with iron oxide impurities

Physical characteristics

  • Crystal Habit: Cryptocrystalline aggregates, typically massive, botryoidal, mammillary, or stalactitic. Individual crystals are microscopic.
  • Cleavage Type: None
  • Fracture Type: Conchoidal to uneven
  • Tenacity: Brittle
  • Luster Type: Waxy to vitreous

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