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An Amethyst Geode with Stilbite is a hollow, roughly spherical to ovoid rock formation lined with amethyst crystals and often adorned with stilbite crystals. The outer shell of the geode is typically basalt or other volcanic rock, or sometimes sedimentary rock. Inside, the cavity is lined with a layer of chalcedony, followed by inward-growing, terminated amethyst crystals. The amethyst crystals range in color from pale lilac to deep purple. Stilbite-Ca typically forms delicate, often sheaf-like or radiating aggregates of tabular crystals, commonly white, cream, salmon-pink, or orange, growing on or among the amethyst crystals. The combination creates a visually striking mineral specimen.
How to Identify
- Color
- Amethyst: Purple (ranging from pale lilac to deep violet). Stilbite: White, cream, salmon-pink, orange, or brownish-red. Geode exterior: Typically dull, often dark gray to black basalt or brownish sedimentary rock.
- Luster
- Amethyst: Vitreous (glassy). Stilbite: Vitreous to pearly on cleavage surfaces.
- Texture
- Amethyst: Smooth, glassy crystal faces. Stilbite: Often delicate, radiating, or sheaf-like aggregates, sometimes with a slightly rough or granular feel due to crystal habit. Geode exterior: Rough, often vesicular.
- Crystal Form
- Amethyst: Hexagonal prisms terminated by rhombohedral faces, often forming drusy linings. Stilbite: Tabular crystals, often aggregated into characteristic sheaf-like, bow-tie, or radiating forms. Individual crystals are monoclinic.
- Cleavage
- Amethyst (Quartz): None (conchoidal fracture). Stilbite: Perfect on {010}, good on {100}.
- Geological Environment
- Volcanic environments, particularly in vesicles within basaltic lava flows, or less commonly in hydrothermal veins within sedimentary or metamorphic rocks. The presence of both amethyst and stilbite indicates a multi-stage hydrothermal deposition process.
Key Facts
- Hardness: Amethyst (Quartz): 7 on Mohs scale. Stilbite: 3.5-4 on Mohs scale.
- Specific Gravity: Amethyst (Quartz): 2.65 g/cm³. Stilbite: 2.12-2.22 g/cm³.
- Crystal System: Amethyst (Quartz): Trigonal. Stilbite: Monoclinic.
- Color: Amethyst: Purple. Stilbite: White, cream, salmon-pink, orange, brownish-red.
- Luster: Amethyst: Vitreous. Stilbite: Vitreous to pearly.
- Transparency: Amethyst: Transparent to translucent. Stilbite: Transparent to translucent.
- Fracture: Amethyst (Quartz): Conchoidal. Stilbite: Uneven to subconchoidal.
- Cleavage: Amethyst (Quartz): None. Stilbite: Perfect on {010}, good on {100}.
- Composition: Amethyst (Quartz): Silicon dioxide (SiO2). Stilbite-Ca: Hydrated sodium calcium aluminum silicate ((Na,Ca)9[Al9Si27O72]·nH2O).
Quick Check
- Color: Purple (Amethyst) and White/Pink/Orange (Stilbite)
- Luster: Vitreous (Amethyst), Vitreous to Pearly (Stilbite)
- Streak: White (both Amethyst and Stilbite)
Physical Characteristics
- Crystal Habit: Amethyst: Prismatic, often terminated, forming drusy linings. Stilbite: Tabular, often aggregated into sheaf-like, bow-tie, or radiating forms.
- Cleavage Type: Amethyst (Quartz): Absent. Stilbite: Perfect basal cleavage {010}, good {100}.
- Fracture Type: Amethyst (Quartz): Conchoidal. Stilbite: Uneven to subconchoidal.
- Tenacity: Amethyst (Quartz): Brittle. Stilbite: Brittle.
- Luster Type: Amethyst (Quartz): Vitreous. Stilbite: Vitreous to pearly.
Formation
Amethyst geodes form in volcanic environments, specifically in basaltic lava flows or sometimes in sedimentary rocks. Gas bubbles (vesicles) in cooling lava provide cavities. Over time, silica-rich hydrothermal solutions percolate through these cavities, depositing layers of chalcedony (microcrystalline quartz) on the interior walls, followed by macrocrystalline quartz (amethyst). The purple color of amethyst is due to irradiation of trace iron impurities within the quartz crystal lattice. Stilbite-Ca, a zeolite mineral, forms later from lower-temperature hydrothermal fluids, often lining or growing on the amethyst crystals within the geode.
Usage
Primarily ornamental and collector's specimens. Amethyst is widely used in jewelry and decorative items. Stilbite, while less common in jewelry, is prized by collectors for its aesthetic appeal in mineral specimens, especially when associated with other minerals like amethyst. Zeolites, in general, have industrial uses as molecular sieves, catalysts, and ion-exchange agents, but stilbite from geodes is rarely extracted for these purposes.
Age Distribution
Typically Cenozoic to Mesozoic, but can vary depending on the host rock formation.
Where to Find
Rio Grande do Sul, Brazil
World-renowned for large, high-quality amethyst geodes, often found in basalt flows. Stilbite associations are common here.
Artigas, Uruguay
Another major source of amethyst geodes, similar to Brazil, with frequent occurrences of associated zeolite minerals including stilbite.
Deccan Traps, India
Known for a wide variety of zeolite minerals, including stilbite, often found in basaltic cavities. Amethyst can also occur, sometimes in association.
Nova Scotia, Canada
Coastal basalt flows yield amethyst and various zeolites, including stilbite, though geodes are typically smaller than South American examples.
Finding Tips
Look for Volcanic Rocks
Geodes are most commonly found in areas with ancient volcanic activity, particularly basalt flows. Look for rounded or irregular bumps on weathered rock surfaces.
Examine Road Cuts and Quarries
These exposures often reveal cross-sections of rock formations where geodes might be visible. Freshly broken rock can expose geode interiors.
Check for Associated Minerals
The presence of other zeolite minerals (e.g., heulandite, analcime) or chalcedony can indicate a favorable environment for stilbite and amethyst formation.
Safety Precautions
When collecting, always wear appropriate safety gear (gloves, eye protection, sturdy footwear). Be aware of unstable rock formations and potential hazards in quarries or cliffs. Respect private property and local regulations.
Similar Rocks
Amethyst Geode
Quartz (SiO2)
Also known as: Quartz Geode
Citrine Geode
Quartz (SiO2)
Also known as: Heated Amethyst Geode
Celestite Geode
Celestite (SrSO4)
Also known as: Celestine Geode
Scientific Classification
- Mineral Class
- Amethyst (Quartz): Tectosilicate. Stilbite: Zeolite Group (Tectosilicate).
- Group
- Amethyst (Quartz): Quartz Group. Stilbite: Heulandite-Stilbite Group.
- Crystal System
- Amethyst (Quartz): Trigonal. Stilbite: Monoclinic.
- Chemical Formula
- Amethyst (Quartz): SiO2. Stilbite-Ca: (Na,Ca)9[Al9Si27O72]·nH2O
- Composition
- Amethyst (Quartz): Silicon dioxide. Stilbite-Ca: Hydrated sodium calcium aluminum silicate.
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