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Stilbite on basalt refers to specimens where the zeolite mineral stilbite-Ca has crystallized within the vesicles, vugs, or fractures of a basaltic host rock. Basalt is a fine-grained, dark-colored extrusive igneous rock, rich in iron and magnesium. Stilbite-Ca typically forms radiating, sheaf-like, or tabular crystal aggregates, often displaying a pearly luster, and can range in color from white, colorless, pale yellow, pink, to reddish-brown. The contrast between the delicate, often translucent stilbite crystals and the dark, opaque basalt matrix creates aesthetically pleasing mineral specimens.
How to Identify
- Color
- Stilbite: White, colorless, pale yellow, pink, salmon, reddish-brown. Basalt: Dark gray to black.
- Luster
- Stilbite: Vitreous to pearly, especially on cleavage surfaces. Basalt: Dull to sub-vitreous.
- Texture
- Stilbite: Often forms radiating, sheaf-like aggregates, sometimes tabular crystals. Basalt: Fine-grained, aphanitic, sometimes vesicular or porphyritic.
- Crystal Form
- Stilbite: Monoclinic, typically forming pseudo-orthorhombic tabular crystals, often twinned, or in characteristic 'sheaf' aggregates. Basalt: Microcrystalline to cryptocrystalline groundmass, with possible phenocrysts of olivine, pyroxene, or plagioclase.
- Cleavage
- Stilbite: Perfect on {010}. Basalt: No distinct cleavage due to its fine-grained nature.
- Geological Environment
- Found in the vesicles, amygdules, and fractures of basaltic lava flows, tuffs, and other mafic volcanic rocks. Also occurs in some metamorphic rocks and hydrothermal veins.
Key Facts
- Hardness: Stilbite: 3.5-4 on Mohs scale. Basalt: 6-7 (due to constituent minerals like plagioclase and pyroxene).
- Specific Gravity: Stilbite: 2.12-2.22. Basalt: 2.7-3.3.
- Crystal System: Stilbite: Monoclinic. Basalt: Not applicable (rock, not a single mineral crystal system).
- Color: Stilbite: White, colorless, pale yellow, pink, salmon, reddish-brown. Basalt: Dark gray to black.
- Luster: Stilbite: Vitreous to pearly. Basalt: Dull to sub-vitreous.
- Transparency: Stilbite: Transparent to translucent. Basalt: Opaque.
- Fracture: Stilbite: Uneven to subconchoidal. Basalt: Conchoidal to uneven.
- Cleavage: Stilbite: Perfect on {010}. Basalt: None.
- Composition: Stilbite: Hydrated sodium calcium aluminum silicate (NaCa2Al5Si13O36·14H2O). Basalt: Primarily plagioclase feldspar, pyroxene, and often olivine, with minor amounts of iron-titanium oxides.
Quick Check
- Color: Stilbite: White, pink, salmon. Basalt: Dark gray to black.
- Luster: Stilbite: Pearly to vitreous. Basalt: Dull.
- Streak: Stilbite: White. Basalt: Gray to black.
Physical Characteristics
- Crystal Habit: Stilbite: Tabular, often forming radiating, sheaf-like aggregates, sometimes fibrous or stellate. Basalt: Aphanitic (fine-grained) to porphyritic, vesicular.
- Cleavage Type: Stilbite: Perfect on one direction ({010}). Basalt: Not applicable.
- Fracture Type: Stilbite: Uneven to subconchoidal. Basalt: Conchoidal to uneven.
- Tenacity: Stilbite: Brittle. Basalt: Brittle.
- Luster Type: Stilbite: Vitreous to pearly. Basalt: Dull to sub-vitreous.
Formation
Stilbite-Ca forms as a secondary mineral, typically in the vesicles (gas bubbles) and fractures of basaltic and other mafic volcanic rocks. It crystallizes from low-temperature hydrothermal solutions circulating through the rock after its initial formation. The basalt provides the necessary silica, aluminum, calcium, and other elements, and its porous nature allows for fluid circulation and crystal growth within its cavities.
Usage
Stilbite on basalt is primarily a collector's specimen due to its aesthetic appeal. Stilbite itself, as a zeolite, has industrial applications in ion exchange (water softening), molecular sieves, catalysts, and as an adsorbent. However, specimens on basalt are generally not used for these industrial purposes due to their form and association with the host rock.
Age Distribution
Varies depending on the age of the basaltic host rock, ranging from ancient Precambrian to recent volcanic activity.
Where to Find
Deccan Traps, India
World-renowned for exceptional zeolite specimens, including stilbite, often found in large, aesthetic formations within basaltic cavities.
Nova Scotia, Canada
Coastal basalt cliffs yield excellent stilbite and other zeolite specimens.
Iceland
Volcanic regions with abundant basalt flows are known for various zeolite occurrences, including stilbite.
Faroe Islands
Similar to Iceland, these basaltic islands are a classic locality for zeolites.
Oregon and Washington, USA
Basalt flows in the Pacific Northwest, particularly the Columbia River Basalt Group, contain zeolite-filled vesicles.
Finding Tips
Look for Vesicular Basalt
Stilbite commonly forms in the gas bubbles (vesicles) of basalt. Search for basaltic outcrops with visible cavities or amygdules.
Examine Fractures and Veins
Hydrothermal solutions can deposit stilbite along fractures and veins within basalt, so inspect these features carefully.
Check Road Cuts and Quarries
Fresh exposures of basalt, such as those found in road cuts, construction sites, and quarries, are often good places to find mineralized cavities.
Identify Associated Minerals
Stilbite often co-occurs with other zeolites (e.g., heulandite, scolecite, analcime) and associated minerals like calcite and apophyllite. Learning to identify these can help locate stilbite.
Use Proper Tools
A rock hammer, chisels, and safety glasses are essential for carefully extracting specimens from hard basalt without damaging the delicate stilbite crystals.
Similar Rocks
Heulandite on Basalt
Heulandite-Ca ((Ca,Na)2-3Al3(Al,Si)2Si13O36·12H2O) on Basalt
Also known as: Heulandite-Ca on Basalt
Apophyllite on Basalt
Fluorapophyllite-K (KCa4(Si8O20)(F,OH)·8H2O) on Basalt
Also known as: Fluorapophyllite-K on Basalt
Scolecite on Basalt
Scolecite (CaAl2Si3O10·3H2O) on Basalt
Also known as: Scolecite on Basalt
Scientific Classification
- Mineral Class
- Silicates
- Group
- Zeolite Group
- Crystal System
- Monoclinic
- Chemical Formula
- NaCa2Al5Si13O36·14H2O (Stilbite-Ca end-member)
- Composition
- Hydrated sodium calcium aluminum silicate
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