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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Open the appTo 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
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
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
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
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
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Quartz: None (conchoidal fracture). Chlorite: Perfect basal cleavage (one direction). Iron oxides: None.
- 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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