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How to identify Stilbite on Chalcedony with Mordenite

Stilbite-Ca, Chalcedony, Mordenite

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To correctly identify Stilbite on Chalcedony with Mordenite (Stilbite-Ca, Chalcedony, Mordenite), 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

    Stilbite-Ca: White, pink, orange, salmon-red, brown. Chalcedony: White, gray, blue, brown, often translucent. Mordenite: White, pale pink, yellowish, colorless.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Stilbite-Ca: Vitreous to pearly on cleavage surfaces. Chalcedony: Waxy to dull. Mordenite: Silky to vitreous.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Stilbite-Ca: Sheaf-like, tabular, radiating aggregates. Chalcedony: Botryoidal, mammillary, stalactitic, microcrystalline. Mordenite: Fibrous, acicular, cotton-like aggregates.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Stilbite-Ca: Monoclinic, typically tabular crystals often twinned into 'bow-tie' or 'sheaf' aggregates. Chalcedony: Cryptocrystalline quartz, no macroscopic crystal form, but forms botryoidal or mammillary masses. Mordenite: Orthorhombic, typically as fine acicular or fibrous crystals, often radiating or in felted masses.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Stilbite-Ca: Perfect on {010}. Chalcedony: None (conchoidal fracture). Mordenite: Good on {100} and {010}.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Typically found in the amygdaloidal cavities and veins of basaltic and other mafic volcanic rocks, as well as in some granitic pegmatites and hydrothermal alteration zones. It forms under low-temperature, low-pressure hydrothermal conditions.

Key Facts

Hardness
Stilbite-Ca: 3.5-4. Chalcedony: 6.5-7. Mordenite: 3-5.
Specific Gravity
Stilbite-Ca: 2.1-2.2. Chalcedony: 2.55-2.65. Mordenite: 2.1-2.12.
Crystal System
Stilbite-Ca: Monoclinic. Chalcedony: Trigonal (cryptocrystalline). Mordenite: Orthorhombic.
Color
Variable, as described above, depending on the dominant mineral and impurities.
Luster
Variable, as described above.
Transparency
Stilbite-Ca: Transparent to translucent. Chalcedony: Translucent to opaque. Mordenite: Transparent to translucent.
Fracture
Stilbite-Ca: Uneven. Chalcedony: Conchoidal. Mordenite: Uneven to splintery.
Cleavage
Stilbite-Ca: Perfect on {010}. Chalcedony: None. Mordenite: Good on {100} and {010}.
Composition
Stilbite-Ca: Hydrated calcium sodium aluminum silicate. Chalcedony: Silicon dioxide (SiO2). Mordenite: Hydrated sodium calcium potassium aluminum silicate.

Physical characteristics

  • Crystal Habit: Stilbite-Ca: Sheaf-like, tabular, radiating. Chalcedony: Botryoidal, mammillary, stalactitic. Mordenite: Fibrous, acicular, cotton-like.
  • Cleavage Type: Stilbite-Ca: Perfect. Chalcedony: None. Mordenite: Good.
  • Fracture Type: Stilbite-Ca: Uneven. Chalcedony: Conchoidal. Mordenite: Uneven to splintery.
  • Tenacity: Stilbite-Ca: Brittle. Chalcedony: Brittle. Mordenite: Brittle.
  • Luster Type: Stilbite-Ca: Vitreous to pearly. Chalcedony: Waxy to dull. Mordenite: Silky to vitreous.

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