| Specimen Details | |
|---|---|
| Weight | 1.95 oz’s – 55.4 g |
| Dimensions | 1.968″ x 2.211″ tall/wide (4.998 x 5.616 cm’s) |
| Country of Origin | Brazil |
High Grade Ametrine Phantom Heart Carving
NZD $43.00
SKU: P3908
This Amethyst has been carved and polished into a Heart. The color is incredible with wonderful clarity! With a small inclusion of Citrine, and rainbows visible when you explore the piece. 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 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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Ametrine Origins & Background
Ametrine is a naturally occurring bi-colored variety of Quartz that displays both Amethyst (purple) and Citrine (golden-yellow) within the same crystal. This striking combination forms under very specific geological conditions and is comparatively rare in nature.
The world’s most significant and well-known natural source of Ametrine is the Anahí Mine in Bolivia. This locality produces true, naturally colored Ametrine with clearly defined or softly blended color zoning.
Smaller and less consistent natural occurrences of Ametrine have also been reported in Spain and a few other locations, though material from these sources is far less common on the market.
Historically, Ametrine is linked to Spanish colonial history. According to legend, the Anahí Mine was given as a dowry to a Spanish conquistador, bringing awareness of the stone to Europe.
It is important to note that much Ametrine sold today may be cut from natural crystals to emphasize color contrast. However, genuine Ametrine should always show natural color zoning rather than uniform or artificially induced coloration.
Ametrine Geological Information
Ametrine is a variety of Quartz (Silicon Dioxide – SiO₂) that forms when both Amethyst and Citrine coloration develop within a single crystal. This occurs due to temperature variations and differential oxidation states of iron during crystal growth.
The purple Amethyst zones form in areas where iron within the Quartz lattice is exposed to natural irradiation under relatively cooler conditions. The golden Citrine zones develop where higher temperatures cause partial oxidation of the iron, altering its color expression.
In natural Ametrine, these temperature differences often occur within the same crystal during growth, creating sharp or gradual transitions between purple and gold. This is fundamentally different from heat-treated Amethyst, which produces uniform Citrine coloration.
The unique geological stability of the Bolivian deposits allows these contrasting zones to remain preserved rather than blending into a single color.
Common Geological Occurrences
- Hydrothermal Quartz veins
- Volcanic rock environments
- Geological zones with stable thermal gradients
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Ametrine variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
Ametrine Crystal Care & Ownership Advice
⚠️ Sunlight & Heat:
Prolonged exposure to intense sunlight or heat may gradually fade the Amethyst coloration. Display in indirect or filtered light.
✋ Handling:
Ametrine is durable but should be handled with care to avoid chipping polished edges or points.
🧼 Cleaning:
Clean using lukewarm water and a soft cloth or brush. Avoid harsh chemicals and ultrasonic cleaners.
📦 Storage & Display:
Store separately from harder stones to avoid scratching. Padded surfaces are ideal for display.
Bolivian Ametrine Location Photos
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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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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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