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How to identify Dendritic Agate

SiO2 (chalcedony with manganese or iron dendrites)

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To correctly identify Dendritic Agate (SiO2 (chalcedony with manganese or iron dendrites)), 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

    Base color is typically colorless, white, gray, or pale blue chalcedony. The dendritic inclusions are black, dark brown (manganese oxides), or reddish-brown to orange (iron oxides).

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to waxy.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly granular on unpolished surfaces; conchoidal fracture surfaces are 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 veins and cavities.

  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

    Typically found in volcanic rocks (e.g., basalts, rhyolites) where silica-rich fluids have filled vesicles and fractures. Also occurs in sedimentary rocks, particularly limestones and sandstones, and in hydrothermal veins.

Key Facts

Hardness
6.5-7 on the Mohs scale (due to chalcedony).
Specific Gravity
2.58-2.64.
Crystal System
Trigonal (for the constituent quartz microcrystals).
Color
Colorless, white, gray, or pale blue chalcedony with black, brown, or reddish-brown dendritic inclusions.
Luster
Vitreous to waxy.
Transparency
Translucent to opaque.
Fracture
Conchoidal.
Cleavage
None.
Composition
Silicon dioxide (SiO2) with inclusions of manganese oxides (e.g., pyrolusite, psilomelane) or iron oxides (e.g., goethite).

Physical characteristics

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

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