| Specimen Details | |
|---|---|
| Weight | 12.85 oz’s – 364 g |
| Dimensions | 7.68″ x 1.81″ long x wide (19.5 x 4.6 cm’s) |
| Country of Origin | Brazil |
Polished Amethyst Phantom Rainbow Double Terminated Quartz Wand
NZD $138.00
SKU: P3839
This Polished Double Terminated Wand features awesome Amethyst phantoms with great color as well as internal veils that cast epic rainbows inside!! Check out the video just above for the best look at this amazing wand!
In stock
Use the tabs below to explore crystal origins, geological details, crystal care guidance, and metaphysical insights.
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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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Phantom Quartz Origins & Background
Phantom Quartz is one of the most symbolically powerful growth forms in the Quartz family. These crystals contain visible internal “phantoms” — ghost-like images of earlier stages of the crystal’s own development preserved within the body of the crystal itself.
Each phantom represents a pause, interruption, or shift during the crystal’s growth cycle. Rather than halting development permanently, the Quartz resumes growth and carries the record of that moment forward. Because of this, Phantom Quartz has long been associated with evolution, resilience, and the ability to move forward after disruption.
Phantom Quartz occurs in many Quartz varieties, including Clear Quartz, Smoky Quartz, Amethyst, and included forms. Each variety adds its own nuance to the phantom’s expression and influence.
Phantom Quartz Geological Information
Phantom Quartz forms when a crystal’s growth is temporarily interrupted by the introduction of another substance or a change in environmental conditions. This interruption leaves a visible layer on the crystal’s termination before growth resumes, encapsulating that earlier stage within the final crystal.
Common Phantom-Causing Materials
- Chlorite: often green phantoms
- Hematite: red, brown, or metallic phantoms
- Clay or sediment: pale or earthy-toned phantoms
- Thermal changes: color-zone phantoms (often Smoky or Amethyst)
3D Phantom Formation
The most powerful and visually striking phantoms are referred to as 3D phantoms. In these specimens, the interrupting material fully coats the termination, creating a complete three-dimensional “crystal within a crystal.”
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Phantom growth) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Defining Feature | Visible internal growth stages |
Phantom Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Handle gently to protect internal clarity and phantom visibility. Lift from the base where possible.
🧼 Cleaning:
Brief water rinsing is generally safe. Avoid prolonged soaking if fractures or inclusions are present.
☀️ Light:
Protect Smoky and Amethyst Phantom Quartz from prolonged intense sunlight.
📦 Storage & Display:
Display with good lighting to reveal internal phantoms. These crystals benefit from being seen and consciously worked with.
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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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Rainbow Quartz Origins & Background
Rainbow Quartz refers to Quartz crystals that display internal spectral light effects—commonly referred to as rainbows—caused by light refracting through internal fractures, growth planes, or inclusions. These rainbows are natural optical phenomena and not surface treatments.
Rainbow effects can occur in many Quartz varieties including Clear Quartz, Smoky Quartz, Amethyst, and included forms. Each crystal expresses its rainbow uniquely, making every specimen distinct.
Rainbow Quartz has long been appreciated as a bridge between physical structure and light-based phenomena, symbolically representing the union of matter and spectrum.
Rainbow Quartz Geological Information
Rainbow effects in Quartz are produced when light passes through internal fractures or stress planes created during or after crystal growth. These micro-surfaces refract light into its component wavelengths, producing visible spectral colors.
The Quartz itself remains chemically unchanged; the rainbow effect is purely optical. These features often form under natural pressure changes, tectonic stress, or thermal fluctuations during the crystal’s geological history.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Rainbow variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Defining Feature | Internal light spectrum (rainbows) |
Rainbow Expansion Effect
When rainbows occur within different Quartz varieties, they act as energetic expanders—broadening the crystal’s default properties across a wider range of expression.
Rainbow Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Rainbow Quartz is durable but internal fractures can be sensitive to impact. Handle with care.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid sudden temperature changes that may stress internal planes.
☀️ Light:
Light-stable. Rainbows are best viewed under directional light.
📦 Storage & Display:
Display where light can interact with the crystal. Rainbows often “activate” visually when the crystal is regularly handled or moved.

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