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How to identify Moss Agate

Chalcedony (silicon dioxide) with chlorite or hornblende inclusions

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To correctly identify Moss Agate (Chalcedony (silicon dioxide) with chlorite or hornblende inclusions), 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

    Colorless, white, or grayish translucent chalcedony matrix with green, black, brown, or reddish dendritic inclusions.

  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 when polished; cryptocrystalline structure.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Typically massive, botryoidal, or stalactitic; individual crystals are microscopic.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None, exhibits conchoidal fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in volcanic rocks (e.g., basalts, andesites) as amygdules or vein fillings, and in sedimentary rocks where silica-rich fluids have permeated. Also found in alluvial deposits as pebbles and cobbles.

Key Facts

Hardness
6.5 - 7 on Mohs scale
Specific Gravity
2.58 - 2.64
Crystal System
Trigonal (cryptocrystalline)
Color
Colorless, white, gray, or bluish-white matrix with green, black, brown, or red inclusions
Luster
Waxy to vitreous
Transparency
Translucent to opaque
Fracture
Conchoidal
Cleavage
None
Composition
SiO2 (silicon dioxide) with inclusions of chlorite, hornblende, manganese oxides, or iron oxides

Physical characteristics

  • Crystal Habit: Cryptocrystalline aggregates, massive, botryoidal, stalactitic
  • Cleavage Type: None
  • Fracture Type: Conchoidal
  • Tenacity: Brittle
  • Luster Type: Waxy to vitreous

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