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How to identify Tree Agate

Chalcedony (variety of Quartz)

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To correctly identify Tree Agate (Chalcedony (variety of Quartz)), 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

    White, colorless, or milky translucent base with green, brown, or black dendritic (tree-like or fern-like) patterns.

  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, conchoidal fracture surfaces are smooth.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Cryptocrystalline, meaning individual crystals are microscopic and not visible to the naked eye. Forms botryoidal, mammillary, or stalactitic masses, or as vein fillings and nodules.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None, due to its cryptocrystalline nature.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in amygdaloidal cavities in volcanic rocks (e.g., basalt, andesite), hydrothermal veins, and as nodules in sedimentary deposits. Often associated with areas of past volcanic activity or silica-rich groundwater flow.

Key Facts

Hardness
6.5-7 on the Mohs scale.
Specific Gravity
2.58-2.64 g/cm³.
Crystal System
Trigonal (as a variety of Quartz, though cryptocrystalline).
Color
White, colorless, or milky translucent with green, brown, or black dendritic inclusions.
Luster
Waxy to vitreous.
Transparency
Translucent to opaque.
Fracture
Conchoidal to uneven.
Cleavage
None.
Composition
Silicon dioxide (SiO2) with inclusions of manganese oxides (e.g., MnO2) or iron oxides (e.g., Fe2O3).

Physical characteristics

  • Crystal Habit: Cryptocrystalline aggregates, typically massive, botryoidal, mammillary, or stalactitic. Individual crystals are microscopic.
  • Cleavage Type: Absent.
  • Fracture Type: Conchoidal to uneven, splintery.
  • Tenacity: Brittle.
  • Luster Type: Waxy to vitreous (glassy).

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