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How to identify Milky Quartz with Manganese Dendrites

SiO2 with MnO2 inclusions

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To correctly identify Milky Quartz with Manganese Dendrites (SiO2 with MnO2 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

    Milky white to off-white quartz matrix with black, dark brown, or dark gray dendritic (fern-like, tree-like) patterns.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) on fractured surfaces of the quartz; inclusions are typically dull to sub-metallic.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly rough, depending on the polish or natural surface. The dendrites are internal.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Quartz typically forms in hexagonal prisms with pyramidal terminations, but in milky quartz, it often occurs as massive, anhedral aggregates. The dendrites are two-dimensional or three-dimensional branching patterns within the quartz.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None (quartz). The manganese dendrites do not exhibit cleavage.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Hydrothermal veins, pegmatites, metamorphic rocks, and sedimentary environments where silica-rich fluids and manganese-rich solutions interact. Often found in areas with past or present manganese mineralization.

Key Facts

Hardness
7 on the Mohs scale (for quartz)
Specific Gravity
2.65 g/cm³ (for quartz)
Crystal System
Trigonal (for quartz)
Color
Milky white with black/dark brown dendritic inclusions
Luster
Vitreous
Transparency
Opaque to translucent (for milky quartz)
Fracture
Conchoidal (for quartz)
Cleavage
None
Composition
Silicon dioxide (SiO2) with manganese oxide (MnO2) inclusions

Physical characteristics

  • Crystal Habit: Massive, anhedral aggregates for milky quartz; dendritic (fern-like, tree-like) patterns for inclusions.
  • Cleavage Type: Absent
  • Fracture Type: Conchoidal
  • Tenacity: Brittle
  • Luster Type: Vitreous (quartz), dull to sub-metallic (manganese oxides)

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