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How to identify Limonite with Quartz

FeO(OH)·nH2O (Limonite) with SiO2 (Quartz)

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To correctly identify Limonite with Quartz (FeO(OH)·nH2O (Limonite) with SiO2 (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

    Variable, ranging from yellow, orange, brown, to reddish-brown, depending on the concentration and hydration state of the limonite. The underlying quartz may be visible as colorless or white.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Earthy to dull for the limonite component; vitreous to greasy for the quartz component. The overall appearance can be dull if limonite predominates, or vitreous if quartz is dominant and merely stained.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Can be massive, botryoidal, stalactitic, or earthy for limonite, often coating or intergrown with granular or crystalline quartz. The texture will be a combination of the two minerals.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Limonite is typically amorphous or cryptocrystalline, forming botryoidal, mammillary, or stalactitic masses, or as earthy coatings. Quartz forms hexagonal prisms with pyramidal terminations, or as massive, anhedral grains.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Limonite has no true cleavage, exhibiting irregular fracture. Quartz has no cleavage, exhibiting conchoidal fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Common in the oxidized zones of iron ore deposits, gossans, weathered igneous and metamorphic rocks, and as cementing material in sedimentary rocks (e.g., ferruginous sandstones). Also found in bog iron deposits and as a product of hydrothermal alteration.

Key Facts

Hardness
Limonite: 4-5.5 (Mohs); Quartz: 7 (Mohs). The aggregate will have variable hardness depending on the dominant mineral.
Specific Gravity
Limonite: 2.7-4.3; Quartz: 2.65. The aggregate will have a specific gravity between these values.
Crystal System
Limonite: Amorphous or Orthorhombic (for goethite/lepidocrocite components); Quartz: Trigonal.
Color
Yellow, orange, brown, reddish-brown, often with colorless or white areas.
Luster
Earthy to dull (limonite); vitreous to greasy (quartz).
Transparency
Opaque (limonite); Transparent to translucent (quartz).
Fracture
Irregular to conchoidal (limonite); Conchoidal (quartz).
Cleavage
None (limonite); None (quartz).
Composition
Hydrated iron(III) oxide-hydroxide (Limonite) and Silicon Dioxide (Quartz).

Physical characteristics

  • Crystal Habit: Limonite: Massive, earthy, botryoidal, stalactitic, reniform, oolitic. Quartz: Prismatic, massive, granular.
  • Cleavage Type: None for both minerals.
  • Fracture Type: Limonite: Irregular to conchoidal. Quartz: Conchoidal.
  • Tenacity: Limonite: Brittle to earthy. Quartz: Brittle.
  • Luster Type: Limonite: Earthy, dull. Quartz: Vitreous, greasy.

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