| Specimen Details | |
|---|---|
| Weight | 1.5 oz’s – 42.5 g |
| Dimensions | 2.6″ long (6.6 cm’s) |
| Country of Origin | Brazil |
Polished Chevron Dream Amethyst Double Terminated Wand
USD $19.00
SKU: P3402
This Polished Chevron Amethyst DT Wand has rich color with awesome Chevron patterning!!
In stock
Use the tabs below to explore crystal origins, geological details, crystal care guidance, and metaphysical insights.
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Chevron / Dream Amethyst Origins & Background
Chevron Amethyst — also commonly known as Dream Amethyst — is a naturally banded variety of Amethyst characterized by distinctive V-shaped or zig-zag patterns. These patterns are created by alternating layers of purple Amethyst and white Quartz.
The term “Chevron” refers specifically to this layered, angular banding pattern, which resembles military chevrons or flowing mountain peaks. The name “Dream Amethyst” is a more modern trade name, reflecting the stone’s long-standing association with intuition, inner vision, and dreamwork.
Chevron Amethyst is most commonly sourced from Brazil, Zambia, and parts of India. Each locality produces variations in color contrast, band thickness, and overall pattern sharpness.
Unlike uniformly colored Amethyst, Chevron Amethyst visually records shifts in mineral deposition during growth. These natural transitions give the stone its dynamic, layered appearance and make each piece unique.
Chevron / Dream Amethyst Geological Information
Chevron Amethyst is a variety of Quartz (Silicon Dioxide – SiO₂) composed of alternating layers of purple Amethyst and white or milky Quartz. Both layers share the same crystal system but differ in trace element content and growth conditions.
The purple Amethyst layers form through the presence of trace iron within the Quartz lattice combined with natural irradiation. The white Quartz layers represent periods of lower iron concentration or different crystallization conditions.
These alternating conditions during crystal growth result in the distinctive chevron or zig-zag patterning. Over time, slow and stable geological conditions allow the layered structure to develop with clear definition.
Common Geological Occurrences
- Hydrothermal Quartz veins
- Amethyst-bearing geodes
- Layered Quartz growth environments
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Chevron / Amethyst variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
Chevron / Dream Amethyst Crystal Care & Ownership Advice
⚠️ Sunlight & Heat:
Prolonged exposure to strong sunlight may cause fading of the Amethyst layers over time. Display in indirect or filtered light.
✋ Handling:
Chevron Amethyst is durable, but sharp impacts may chip edges, especially on polished pieces.
🧼 Cleaning:
Clean with lukewarm water and a soft cloth or brush. Avoid harsh chemicals and ultrasonic cleaners.
📦 Storage & Display:
Store away from harder stones that may scratch the surface. Chevron patterns display best under soft, angled lighting.
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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
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Double Terminated Quartz Origins & Background
Double Terminated Quartz refers to Quartz crystals that naturally form with a termination at both ends, rather than the more common single-point growth where one end is attached to a matrix or host rock. This is a true growth habit, not a separate mineral species, and it can occur in clear quartz, smoky quartz, amethyst, and included varieties depending on locality and conditions.
Double termination typically forms when a Quartz crystal grows in an open cavity where both ends remain free, or when the crystal grows in a fluid or clay-rich environment that allows it to develop without permanently attaching to a host surface. Because this requires specific stability and space during growth, fine double terminated specimens are less common than standard points.
Some double terminated crystals are true “floaters,” meaning they grew completely free and may show overall symmetry, clear faces, and terminations at both ends. Others may have one end slightly more developed, or show subtle contact points where the crystal briefly touched surrounding material during growth.
In the marketplace, it is important to distinguish natural double termination from cut or polished pieces. Authentic double terminated Quartz shows natural growth lines, consistent termination geometry, and unpolished faces (unless the specimen has been intentionally polished as a separate treatment, which should be disclosed).
Double Terminated Quartz Geological Information
Double Terminated Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system, like all Quartz. The double terminated form is created by growth conditions rather than chemistry.
This habit most commonly develops in:
- Open vugs or cavities where the crystal can grow unobstructed
- Clay beds or sediment pockets that allow crystals to form as “floaters”
- Stable hydrothermal environments with long growth windows
Because Quartz is durable and chemically stable, double terminated crystals often preserve their terminations well—though tips can still chip if struck.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Double Terminated growth habit) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
| Defining Feature | Natural terminations on both ends |
Why Double Termination Matters (Structurally)
From a formation perspective, the key difference is that energy of growth and crystallographic development occurred in two directions. This often creates a strong sense of symmetry and “completeness,” which is one reason these crystals are treasured both aesthetically and in metaphysical practice.
Double Terminated Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Double Terminated Quartz has two vulnerable ends. Always lift from the center or base area and avoid tapping either termination against hard surfaces.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking if the crystal contains fractures or inclusions. Dry thoroughly.
☀️ Light:
Clear Double Terminated Quartz is light-stable. Colored varieties (smoky/amethyst) should be protected from prolonged intense sunlight.
📦 Storage & Display:
Store cushioned and separated from other specimens to protect both tips. For display, use stable stands that support the center without pressure on terminations.

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