| Specimen Details | |
|---|---|
| Weight | 8.52 oz’s – 242 g |
| Dimensions | 4.02″ x 1.7″ tall/wide (10.2 x 4.3 cm’s) |
| Country of Origin | Brazil |
Heavily Rutilated Dendritic Quartz/Agate Polished Point
SGD $50.00
SKU: P5636
This heavily Rutilated Quartz/Agate point is cut and polished featuring awesome dendritic form, rutile, color and incredible patterns! Check out the video just above!
In stock
Use the tabs below to explore crystal origins, geological details, crystal care guidance, and metaphysical insights.
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Agate Origins & Background
Agate is a banded variety of Chalcedony Quartz, valued for its wide range of colors, intricate patterns, and grounding visual presence. Unlike single-crystal Quartz, Agate forms in layered microcrystalline structures, giving rise to its distinctive banding and scenic patterns.
The name Agate is believed to originate from the Achates River (modern-day Dirillo River) in Sicily, where agates were collected in ancient times. Agate has been used for tools, seals, jewelry, and ornamental objects for thousands of years across many cultures.
Major Agate-producing regions include Brazil, Uruguay, India, Madagascar, Mexico, and the United States. Different localities produce distinct color palettes and banding styles, making provenance especially interesting for collectors.
Agates often display concentric banding, fortification patterns, or plume-like inclusions. These features are natural records of mineral-rich fluid deposition over long geological periods.
Historically, Agate has been associated with protection, balance, and stability. Many ancient cultures believed Agate offered grounding energy and physical protection during travel or battle.
Agate Geological Information
Agate is a microcrystalline variety of Quartz (Silicon Dioxide – SiO₂), belonging to the Chalcedony group. It forms when silica-rich fluids fill cavities in volcanic or sedimentary rock and slowly crystallize in layers.
Over time, successive deposits of silica create Agate’s characteristic banding. Variations in trace minerals, temperature, and fluid chemistry influence color and pattern formation.
Agate commonly forms in volcanic environments, particularly within gas bubbles in basalt. As these cavities are gradually filled, layered growth develops from the outer edges inward.
Common Geological Occurrences
- Volcanic basalt cavities
- Silica-rich sedimentary environments
- Hydrothermal Quartz deposits
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Chalcedony (Agate variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal (microcrystalline) |
| Hardness (Mohs Scale) | 6.5 – 7 |
| Luster | Waxy to vitreous |
| Transparency | Translucent to opaque |
| Fracture | Conchoidal |
Agate Crystal Care & Ownership Advice
⚠️ Sunlight & Heat:
Agate is generally stable in sunlight, but dyed Agates may fade with prolonged exposure. Natural Agate is best displayed in indirect or ambient light for long-term preservation.
✋ Handling:
Agate is durable, but sharp impacts can chip edges, especially on polished pieces. Handle with reasonable care.
🧼 Cleaning:
Agate is water-safe. Clean using lukewarm water and a soft brush or cloth. Avoid harsh chemicals that could affect surface polish or dye (if present).
📦 Storage & Display:
Store Agate away from harder or sharper stones that may scratch its surface. Polished Agates display well on padded stands or natural wood surfaces.
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Rutilated Quartz Origins & Background
Rutilated Quartz is one of the most visually striking and energetically dynamic members of the Quartz family. These crystals contain needle-like inclusions of Rutile—titanium dioxide—embedded within Quartz, creating dramatic internal patterns that range from fine hair-like threads to bold, dense lattices.
Historically, Rutilated Quartz has been regarded as a crystal of acceleration and activation. Its unique internal structure gives it a distinctly “wired” quality, often described as highly electromagnetic and immediately responsive when worked with consciously.
Rutilated Quartz is found in several regions worldwide, with notable sources including Brazil, Madagascar, Pakistan, and parts of Africa. Each locality produces distinctive rutile coloration, density, and patterning.
Rutilated Quartz Geological Information
Rutilated Quartz is composed of silicon dioxide (SiO₂) with inclusions of Rutile (TiO₂). Rutile forms before or during Quartz crystallization, becoming encapsulated as the Quartz grows.
Rutile Inclusion Characteristics
- Needle-like or hair-like crystal structures
- May appear randomly oriented or aligned
- Density varies from sparse to heavily included
Rutile Color Variations
- Gold: the most well-known and widely sought after
- Copper / Red: often associated with Hematite-rich environments
- Silver: fine, bright needle structures
- Blue: rare and highly prized
- Green: extremely rare
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz with Rutile inclusions |
| Chemical Formula | SiO₂ + TiO₂ |
| Crystal System | Trigonal (Quartz) / Tetragonal (Rutile) |
| Hardness (Mohs Scale) | 7 (Quartz), 6–6.5 (Rutile) |
| Luster | Vitreous to metallic (internal) |
| Transparency | Transparent to translucent |
| Defining Feature | Needle-like Rutile inclusions |
Rutilated Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Handle carefully to preserve clarity and internal inclusion structure. Avoid sharp impacts.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking if fractures are present.
☀️ Light:
Generally light-stable. Display lighting enhances internal Rutile brilliance.
📦 Storage & Display:
Store separately to avoid scratching polished surfaces. Display where internal structure is visible.

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