Group Weight – 2.52 oz’s – 71.3 gm’s
Length – 1.796″ – 2.079″ Shortest/Longest (4.563 – 5.282 cm’s)
Country of Origin – Colombia
5 Piece Blue Smoke Phantom Bridging Key Quartz Crystal Gridding Set
USD $29.00
SKU: Q4317
This Majestic Quartz Gridding set includes 5 Natural Blue Smoke Phantom Quartz Points! This beautiful Bundle of quartz typically sports Stunning clarity, Flawless luster, and Delicate Phantoms throughout multiple pieces. The condition of these points are Pristine and Excellent Condition.
Out of stock
Use the tabs below to explore crystal origins, geological details, crystal care guidance, and metaphysical insights.
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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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Bridge / Inner Child Quartz Origins & Background
Bridge and Inner Child Quartz crystals are defined by a distinctive growth pattern involving a primary crystal — often referred to as the “Mother” crystal — and one or more secondary crystals that grow in direct relationship to it.
These formations are also known by alternative names such as In/Out Quartz or Penetrator Quartz, depending on how the secondary crystal interacts with the primary crystal.
In Bridge Quartz formations, the smaller crystal visibly emerges from the larger crystal, creating a clear physical connection between two distinct crystal bodies. In Inner Child Quartz formations, the smaller crystal is mostly enclosed within the larger crystal, with only a portion visible.
These formations occur naturally during crystal growth and should not be confused with Manifestation Quartz or Baby-Within Quartz, which involve different internal growth dynamics.
Bridge and Inner Child Quartz can occur in Clear Quartz, Amethyst, Smoky Quartz, and other Quartz varieties, depending on the conditions present during formation.
Bridge / Inner Child Quartz Geological Information
Bridge and Inner Child Quartz formations develop when a secondary crystal begins growing either into or out of an existing Quartz crystal during overlapping growth phases.
In Bridge Quartz, the secondary crystal grows through or outward from the primary crystal, maintaining a visible connection between two otherwise independent growth points. This indicates a shift or continuation in growth conditions during formation.
In Inner Child Quartz, the secondary crystal becomes largely enclosed within the primary crystal as growth continues around it. The larger crystal effectively grows around and protects the smaller one, leaving it partially visible.
These formations require stable conditions over time, allowing both crystals to remain intact without dissolution or separation.
Common Geological Occurrences
- Hydrothermal Quartz veins
- Volcanic and metamorphic rock environments
- Quartz growth zones with overlapping nucleation phases
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Bridge / Inner Child formation) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
Bridge / Inner Child Quartz Crystal Care & Ownership Advice
⚠️ Structural Awareness:
While Quartz is durable, the connection point between crystals can be more vulnerable. Handle with care and avoid impacts.
☀️ Sunlight & Heat:
Generally stable, though prolonged intense sunlight may fade Amethyst varieties.
🧼 Cleaning:
Clean gently with lukewarm water and a soft brush. Avoid ultrasonic cleaners.
📦 Storage & Display:
Display where the relationship between crystals is clearly visible and protected.
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Teacher / Babies on the Side Quartz Origins & Formation
Teacher Quartz and Babies-on-the-Side Quartz are growth formations in which a dominant “Mother” crystal is accompanied by one or more smaller secondary crystals attached along its sides. These formations naturally occur during periods of active crystal growth when environmental conditions allow multiple points of crystallization to develop simultaneously.
In Babies-on-the-Side Quartz, the secondary crystals are generally well-formed and distinct, often mirroring the structure of the main crystal at a smaller scale. This differentiates them from Barnacle Quartz, where the side crystals are much smaller, less structured, and sometimes appear as clustered growths rather than clearly terminated individuals.
Both formations are often grouped together due to their shared symbolic and metaphysical themes, particularly those involving teaching, learning, mentorship, and the transmission of knowledge.
These crystals are found in many Quartz-producing regions worldwide, including Brazil, Arkansas (USA), Colombia, Madagascar, and the Himalayas, and may occur in Clear Quartz, Amethyst, Smoky Quartz, and other Quartz varieties.
Teacher / Babies on the Side Quartz Geological Information
These formations develop when a primary Quartz crystal establishes itself early in the growth cycle, followed by later nucleation events that allow smaller crystals to form along its sides. Variations in temperature, pressure, and silica saturation influence how many secondary crystals form and how well-defined they become.
In Teacher Quartz formations, the main crystal typically dominates in size and clarity, acting as the primary growth axis. Babies-on-the-Side formations may feature fewer or more prominent secondary crystals, while Barnacle Quartz forms reflect rapid or fluctuating growth conditions that produce many tiny side attachments.
Despite their visual differences, all of these formations arise from the same fundamental Quartz growth processes, with their final appearance shaped by environmental timing rather than mineral composition.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
Teacher / Babies on the Side Quartz Care & Ownership Advice
✋ Handling:
These crystals often have delicate secondary growths. Handle gently to avoid knocking or chipping smaller attached crystals.
🧼 Cleaning:
Quartz is water-safe. Clean using lukewarm water and a soft brush. Avoid ultrasonic cleaners if the crystal has fine side attachments.
📦 Storage & Display:
Display on stable surfaces where side crystals are protected. Avoid placing weight or pressure against the secondary growths.
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Clear Quartz Origins & Background
Clear Quartz is the most widespread and versatile form of Quartz, valued for its transparency, structural clarity, and wide range of natural growth habits. Composed of silicon dioxide, it forms in diverse geological environments and is found on every continent.
Throughout history, Clear Quartz has been used by cultures worldwide for tools, ornamentation, ceremonial objects, and symbolic practices. Its clarity and durability made it a natural focal point for observation, reflection, and intention-based work long before modern terminology existed.
While Clear Quartz occurs globally, certain localities are especially prized for exceptional quality. Colombian Clear Quartz, particularly from high-altitude Andean regions, is widely regarded among collectors and practitioners as some of the highest-quality Clear Quartz in the world. These crystals are known for their exceptional clarity, brightness, and refined growth, often displaying high-frequency visual purity with minimal internal disruption.
Other notable sources include Brazil, Arkansas (USA), Madagascar, Himalayan regions, and Alpine environments, each producing distinctive variations in form and internal character.
Clear Quartz Geological Information
Clear Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system. It commonly forms in hydrothermal veins, pegmatites, and igneous, metamorphic, and sedimentary environments.
Quartz crystals grow when silica-rich fluids cool and crystallize over extended periods. The clarity of Clear Quartz depends on growth stability, temperature consistency, and the absence of inclusions during formation.
Clear Quartz may occur as single points, clusters, twin crystals, or specialized growth formations. Its hardness and chemical stability make it one of the most durable naturally occurring minerals.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Clear / Rock Crystal) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
| Typical Formation | Hydrothermal veins, pegmatites, igneous & metamorphic rocks |
Clear Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Clear Quartz is durable but crystal points and terminations can chip if knocked. Lift from the base when possible.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking if fractures or inclusions are present. Dry thoroughly.
☀️ Light:
Clear Quartz is light-stable and safe for normal display conditions.
📦 Storage & Display:
Store separately from softer minerals to prevent scratching. Stable display helps preserve terminations and clarity.
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