| Specimen Details | |
|---|---|
| Weight | 5.66 lb’s – 2.57 kg’s |
| Dimensions | 9.84″ x 5.12″ long/wide (25 x 13 cm’s) |
| Country of Origin | Madagascar |
Madagascan Elestial Amethyst Cluster
USD $411.00
SKU: A1121
This Amethyst Cluster from Madagascar features great form with nice large points and lovely lavender color! There is superb elestial etching on the sides. This cluster is just packed with information! This specimen is in excellent condition.
In stock
Use the tabs below to explore crystal origins, geological details, crystal care guidance, and metaphysical insights.
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Amethyst Clusters Origins & Background
Amethyst Clusters are among the most recognized and widely collected forms of Amethyst. Rather than growing as single points, clusters consist of multiple crystal points sharing a common base, creating a radiating crystalline surface.
The appearance of Amethyst clusters varies significantly depending on geological conditions, growth environment, and locality. Factors such as available space, mineral concentration, temperature stability, and fluid movement all influence point size, density, color zoning, and overall structure.
Some clusters form as dense carpets of small points, while others develop fewer but larger, well-terminated crystals. Color can range from pale lavender to deep violet, sometimes with zoning, phantoms, or smoky undertones.
Major sources of Amethyst clusters include Brazil, Uruguay, Zambia, Madagascar, and Russia. Each region is known for distinct characteristics — for example, Uruguay is often associated with deeper color saturation, while Brazil commonly produces larger clusters with lighter hues.
Because clusters form in open cavities, their growth is influenced by the shape and size of the host rock, resulting in highly individual specimens with natural variation and character.
Amethyst Clusters Geological Information
Amethyst clusters form when silica-rich fluids enter open cavities within volcanic or metamorphic rock and crystallize over long periods. Multiple crystal points nucleate simultaneously on the cavity walls, growing inward toward the center.
The trigonal crystal structure of Quartz causes crystals to grow as six-sided prisms with pointed terminations. When conditions allow many growth sites to remain active at once, clusters develop rather than isolated points.
Variations in fluid chemistry, temperature, and mineral availability can cause differences in point size, clarity, and coloration within a single cluster. Growth interruptions may result in features such as phantoms, growth lines, or uneven point heights.
The characteristic purple color of Amethyst results from trace iron within the Quartz lattice combined with natural irradiation and subsequent geological heating.
Common Geological Occurrences
- Volcanic basalt cavities and geodes
- Hydrothermal Quartz veins
- Metamorphic rock environments
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Amethyst variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
Amethyst Clusters Crystal Care & Ownership Advice
⚠️ Sunlight & Heat:
Prolonged exposure to strong sunlight or heat may cause some Amethyst clusters to fade over time. Indirect or filtered light is recommended for display.
✋ Handling:
While Quartz is relatively hard, cluster points can chip if struck. Lift clusters from the base rather than by individual points.
🧼 Cleaning:
Clean using lukewarm water and a soft brush to remove dust between points. Avoid harsh chemicals or ultrasonic cleaners.
📦 Storage & Display:
Place clusters on stable surfaces where they are unlikely to be bumped. Padding beneath the base can help prevent accidental movement.
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Elestial Quartz Origins & Background
Elestial Quartz—sometimes referred to as Elestial Crystals—are among the most complex and information-rich Quartz formations known. While Elestials have been found in several countries including India, Australia, Africa, and the United States, the most significant and consistent source is Brazil, specifically the state of Minas Gerais.
Minas Gerais is an immense and intricate mining region, consisting of thousands of small, often hand-worked mines spread across a wide area. Within this region, true Elestial Quartz originates from a remarkably localized source—essentially a single large hill. Elestials occur in small to medium-sized pockets, and each pocket produces crystals with unmistakable family traits.
One of the most fascinating aspects of Elestial Quartz is that even when two pockets are found only feet apart, the crystals from each pocket will often display distinctly different growth signatures, surface features, and internal character. This phenomenon highlights the extraordinary adaptability of Elestial Quartz as it responds to subtle variations in geological and energetic conditions during formation.
This extreme variability is a defining hallmark of Elestials and contributes greatly to their reputation as crystals of adaptability, integration, and multidimensional awareness.
Elestial Quartz Geological Information
Elestial Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system, like all Quartz. What distinguishes Elestials is not chemistry, but an exceptionally complex growth process involving repeated phases of expansion, contraction, dissolution, and regrowth.
Elestial crystals commonly exhibit:
- Skeletal or layered growth (onion-like structure)
- Deep etching and terracing
- Multiple terminations and recessed faces
- Internal veils, windows, and cavities
Many Elestials grow in skeletal form, meaning the crystal develops in layers rather than completing each growth phase uniformly. In some specimens, outer layers fully enclose earlier stages, allowing the observer to gaze through successive layers from the outside inward. In others, the layers remain incomplete, creating stepped surfaces that can be both seen and felt.
Some Elestial Quartz crystals also contain moving water bubbles, known as Enhydro Crystals. These trapped ancient fluids are geological records of the environment at the time of formation.
Etching is common, though not universal, in Elestial Quartz. These etched patterns often resemble complex symbols or glyph-like markings created by selective dissolution during growth pauses.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Elestial formation) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous to matte (etched areas) |
| Transparency | Transparent to translucent |
| Common Features | Skeletal growth, etching, internal chambers |
Elestial Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Elestial Quartz often features deep etching, layered growth, and delicate recesses. Handle gently and avoid impacts, especially on stepped or skeletal areas.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking, ultrasonic cleaners, or chemical agents, which may lodge in etched surfaces. Dry thoroughly.
☀️ Light:
Light-stable under normal conditions. Specimens with enhydros should be protected from extreme temperature changes.
📦 Storage & Display:
Display securely where airflow and vibration are minimal. Store padded and separate from other crystals to protect intricate surfaces.
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Amethyst Origins & Background
Amethyst has been valued across cultures for thousands of years for its rich violet coloration and its association with clarity, balance, and composure. The name Amethyst originates from the Greek word amethystos, meaning “not intoxicated,” reflecting an ancient belief that the stone helped maintain clear thinking and moderation.
Historically, Amethyst was considered a stone of royalty and spiritual authority. It adorned crowns, rings, and ceremonial objects in Ancient Greece and Rome and later throughout medieval Europe. Its purple color was rare and strongly associated with wisdom, restraint, and elevated status.
Significant Amethyst deposits are found in Brazil, Uruguay, Zambia, Madagascar, and Russia. Each locality produces crystals with distinctive growth habits, color zoning, and internal features, making provenance an important consideration for collectors and natural crystal enthusiasts.
Amethyst’s coloration develops through trace amounts of iron within the Quartz lattice combined with natural irradiation and geological heating over extended time periods. This process often creates layered growth zones that contribute to the depth and visual complexity seen in higher-quality specimens.
Some Amethyst crystals display structural growth features such as internal windows, phantoms, record keepers, and time-link faces. These are physical indicators of crystal formation traits and are valued for both the insight they provide into natural growth processes and to possible Metaphysical propoties.
Amethyst Geological Information
Amethyst is a violet variety of Quartz (Silicon Dioxide – SiO₂) that typically forms within cavities, veins, and geodes in igneous and metamorphic rock environments. Crystals usually grow as hexagonal prisms with pointed terminations.
The purple coloration results from trace iron incorporated into the Quartz structure combined with natural irradiation from surrounding rock. Subsequent geological heating stabilizes these color centers, producing hues that range from pale lavender to deep royal purple.
Amethyst commonly forms in volcanic environments, particularly within gas cavities of cooling basalt flows. Over millions of years, silica-rich fluids crystallize slowly, allowing layered growth and the development of internal zoning and structural features.
Common Geological Occurrences
- Volcanic basalt cavities and geodes
- Hydrothermal Quartz veins
- Metamorphic rock environments
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Amethyst variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
Amethyst Crystal Care & Ownership Advice
⚠️ Sunlight & Heat:
Prolonged exposure to intense sunlight or heat may cause some Amethyst specimens to fade over time. For long-term preservation, extended placement in direct sunlight is best avoided.
✋ Handling:
Amethyst is relatively durable, but sharp impacts can chip crystal points or edges. Handle specimens gently, especially clusters and terminated points.
🧼 Cleaning:
Clean Amethyst using lukewarm water and a soft brush. Avoid harsh chemicals, ultrasonic cleaners, or abrasive tools, which may damage crystal surfaces.
📦 Storage & Display:
Prolonged exposure to intense sunlight or high heat may cause some Amethyst specimens to fade over time.
For long-term preservation, extended placement in direct sunlight is best avoided. Indirect light or filtered natural light is ideal for display. This preserves color while still allowing the crystal’s natural beauty to be appreciated.

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