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How to identify Carnelian Agate

Chalcedony (variety Carnelian Agate)

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To correctly identify Carnelian Agate (Chalcedony (variety Carnelian Agate)), 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 deep reddish-orange, brownish-red, and sometimes almost blackish-red. The color is typically uniform or exhibits subtle banding.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Waxy to vitreous (glassy) on fractured surfaces, dull to waxy on unpolished surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly granular, often conchoidal fracture surfaces. Polished surfaces are very smooth.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Cryptocrystalline, meaning individual crystals are too small to be seen without high magnification. Forms botryoidal, mammillary, or stalactitic masses, or fills amygdules and veins.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None. Carnelian Agate, like all chalcedony, lacks cleavage.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Typically found in the cavities (geodes, amygdules) of volcanic rocks (basalts, andesites, rhyolites) and in sedimentary rocks (limestones, sandstones) where silica-rich solutions have permeated and deposited the material. Also found in alluvial deposits as pebbles and nodules.

Key Facts

Hardness
7 (Mohs scale)
Specific Gravity
2.58 - 2.64
Crystal System
Trigonal (cryptocrystalline aggregates)
Color
Reddish-orange, 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, stalactitic, or forming amygdules and nodules.
  • Cleavage Type: None
  • Fracture Type: Conchoidal to uneven
  • Tenacity: Brittle
  • Luster Type: Waxy to vitreous

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