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How to identify Chlorite-Included Quartz with Iron Staining

SiO2 (Quartz) with (Mg,Fe)3(Si,Al)4O10(OH)2 (Chlorite) and Fe-oxides

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To correctly identify Chlorite-Included Quartz with Iron Staining (SiO2 (Quartz) with (Mg,Fe)3(Si,Al)4O10(OH)2 (Chlorite) and Fe-oxides), 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

    Quartz matrix is typically colorless, white, or smoky. Chlorite inclusions are green, dark green, or black. Iron staining is reddish-brown, orange, or yellowish-brown.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) for quartz; dull to pearly for chlorite inclusions; earthy to dull for iron staining.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Crystalline, often with visible quartz crystal faces. Chlorite inclusions can be flaky or fibrous. Iron staining may be powdery or a thin coating.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Quartz typically forms hexagonal prisms terminated by rhombohedra. Chlorite inclusions may be disseminated flakes, radiating aggregates, or phantom layers within the quartz. Iron oxides are typically amorphous coatings or microcrystalline aggregates.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Quartz: None (conchoidal fracture). Chlorite: Perfect basal cleavage (one direction). Iron oxides: None.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Hydrothermal veins, metamorphic rocks (e.g., greenschist facies), pegmatites, and sedimentary environments where iron-rich fluids interact with quartz-bearing rocks. Often found in areas of active faulting or alteration.

Key Facts

Hardness
Quartz: 7 on Mohs scale. Chlorite: 2-2.5. Iron oxides (e.g., goethite, hematite): 5-6.5.
Specific Gravity
Quartz: 2.65 g/cm³. Chlorite: 2.6-3.3 g/cm³. Iron oxides: 3.3-5.3 g/cm³.
Crystal System
Quartz: Trigonal. Chlorite: Monoclinic. Iron oxides: Orthorhombic (goethite), Trigonal (hematite).
Color
As described above: colorless/white/smoky quartz, green/dark green/black chlorite, reddish-brown/orange/yellowish-brown iron oxides.
Luster
Vitreous (quartz), dull to pearly (chlorite), earthy to dull (iron oxides).
Transparency
Quartz: Transparent to translucent. Chlorite: Opaque to translucent. Iron oxides: Opaque.
Fracture
Quartz: Conchoidal. Chlorite: Uneven. Iron oxides: Uneven to splintery.
Cleavage
Quartz: None. Chlorite: Perfect basal (one direction). Iron oxides: None.
Composition
Silicon dioxide (SiO2) for quartz. Hydrous magnesium iron aluminum silicate for chlorite ((Mg,Fe)3(Si,Al)4O10(OH)2). Iron oxides (e.g., FeO(OH) for goethite, Fe2O3 for hematite).

Physical characteristics

  • Crystal Habit: Quartz: Prismatic, massive, granular. Chlorite: Flaky, platy, massive, radiating. Iron oxides: Earthy, botryoidal, massive.
  • Cleavage Type: Quartz: Absent. Chlorite: Perfect in one direction {001}. Iron oxides: Absent.
  • Fracture Type: Quartz: Conchoidal. Chlorite: Uneven. Iron oxides: Uneven to splintery.
  • Tenacity: Quartz: Brittle. Chlorite: Flexible, inelastic. Iron oxides: Brittle.
  • Luster Type: Quartz: Vitreous. Chlorite: Dull to pearly. Iron oxides: Earthy to dull.

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