Weight – 0.27 oz’s – 7.7 gm’s
Dimensions – 2.05″ x 1.26″ tall/long (5.2 x 3.2 cm’s)
Country of Origin – Himalayas
USD $20.00
SKU: Q4771
This Himalayan Quartz Crystal has great laser form with a nice and shiny luster as well as fantastic clarity showcasing the awesome graphite inclusions and phantom inside!! This specimen is in excellent condition.
In stock
Use the tabs below to explore crystal origins, geological details, crystal care guidance, and metaphysical insights.
Weight – 0.27 oz’s – 7.7 gm’s
Dimensions – 2.05″ x 1.26″ tall/long (5.2 x 3.2 cm’s)
Country of Origin – Himalayas
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Himalayan Quartz Crystals originate from the remote, high-altitude regions of the Himalayan mountain range, spanning parts of India, Nepal, and surrounding alpine zones. Due to extreme terrain, altitude, and weather conditions, these crystals are almost always gathered entirely by hand.
Heavy machinery and modern mining tools are impractical or impossible to use in these regions. Instead, Himalayan Quartz is carefully collected using gentle, low-impact methods and transported by pack mule on treks that can take up to seven days to reach civilization. This respectful and physically demanding process naturally limits supply and contributes to the distinct character of these crystals.
Many collectors and practitioners feel that this gentle method of recovery is reflected in the crystal’s overall presence—calm, refined, and stable rather than forceful or aggressive. Himalayan Quartz commonly forms in clusters and natural groupings, often displaying raw, untouched surfaces, subtle etching, skeletal growth, or internal clarity that reflects long, uninterrupted growth cycles.
Himalayan Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system, like all Quartz varieties. What distinguishes Himalayan Quartz is the extreme geological environment in which it forms.
These crystals grow within alpine vein systems subjected to intense tectonic pressure, dramatic temperature shifts, and long geological timeframes. Growth conditions are often stable for extended periods, allowing clusters to develop with strong structural coherence and well-formed terminations.
Repeated tectonic movement and pressure changes can interrupt and resume crystal growth, contributing to features such as skeletal forms, internal complexity, and natural etching. The relative isolation of these environments also means Himalayan Quartz forms with minimal exposure to modern industrial contamination.
| Property | Value |
|---|---|
| Mineral Species | Quartz (Himalayan variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Common Forms | Clusters, points, skeletal growth |
⚠️ Handling:
Many Himalayan Quartz specimens form in clusters with delicate terminations. Always lift from the base and avoid pressure on individual points.
🧼 Cleaning:
Water-safe for brief rinsing only. Avoid prolonged soaking, salt, or chemical cleaners. Dry thoroughly.
☀️ Light:
Light-stable under normal conditions.
📦 Storage & Display:
Store padded and separated from heavier specimens. Display securely to prevent vibration or accidental impact.
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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 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.
| 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 |
⚠️ 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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Included Quartz refers to Quartz crystals that contain other minerals trapped within them during growth. These inclusions may appear as needles, clouds, veils, phantoms, sprays, plates, threads, or granular deposits, each reflecting the geological conditions present at the time of formation.
Common inclusions include Chlorite, Rutile, Tourmaline, Titanium-bearing minerals, Iron oxides, and many others. Each specimen is inherently unique, as the timing, chemistry, and environment of growth determine the inclusion’s shape, placement, and density.
Included Quartz occurs worldwide, with notable localities in Brazil, Madagascar, Pakistan, India, the United States, and parts of Africa. Because inclusions record a snapshot of the crystal’s growth history, many collectors consider Included Quartz to be a visual and geological record of Earth’s evolving conditions.
Included Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system, consistent with all Quartz varieties. The defining feature is the presence of one or more foreign minerals incorporated during crystal growth.
Inclusions form when Quartz grows in environments where other minerals are suspended in hydrothermal fluids. As the Quartz crystal develops, these minerals may become trapped internally rather than being excluded or deposited on the surface. Growth may continue around the inclusion, fully enclosing it within the crystal body.
In some cases, inclusions outline earlier growth stages, forming phantoms. In others, needle-like or fibrous inclusions such as Rutile or Tourmaline grow simultaneously with the Quartz, creating complex internal structures.
| Property | Value |
|---|---|
| Mineral Species | Quartz with mineral inclusions |
| Chemical Formula | SiO₂ (host crystal) |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 (host crystal) |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Defining Feature | Internal mineral inclusions |
From a geological perspective, inclusions provide valuable insight into the temperature, pressure, and chemistry present during crystal formation. Each Included Quartz specimen is effectively a natural archive of its growth environment.
⚠️ Handling:
Included Quartz is generally durable, but internal fractures or delicate inclusions may be present. Handle gently and avoid sudden impacts.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking, especially for crystals with visible fractures or porous inclusions. Dry thoroughly.
☀️ Light:
Most Included Quartz is light-stable. Some iron-rich inclusions may darken slightly with prolonged intense sunlight.
📦 Storage & Display:
Store separated from harder specimens to prevent chipping. Display securely to protect terminations.
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Quartz Clusters are natural groupings of multiple Quartz crystal points growing together on a shared base. Each point retains its own termination while remaining energetically and structurally connected to the whole. This formation allows Quartz Clusters to function as collective radiators of energy rather than single directional tools.
Clusters form in open cavities where many crystals nucleate simultaneously under stable conditions. Because of this cooperative growth, clusters are often viewed as symbols of unity, cooperation, and shared purpose.
Quartz Clusters can occur in Clear Quartz, Smoky Quartz, Amethyst, Citrine, and many other Quartz varieties, with each type adding its own character to the cluster’s overall influence.
Quartz Clusters are composed of silicon dioxide (SiO₂) and crystallize in the trigonal crystal system. The clustered habit forms when multiple crystal points grow together from a shared substrate, typically within vugs or cavities in host rock.
Each point within a cluster follows the same crystallographic rules as individual Quartz crystals, but the collective arrangement allows for multidirectional growth and energy dispersion.
| Property | Value |
|---|---|
| Mineral Species | Quartz (Cluster formation) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Defining Feature | Multiple naturally terminated points |
Because each point radiates outward, clusters naturally disperse energy in all directions rather than focusing it in a single beam. This makes them ideal for environmental work, group settings, and energetic stabilization of larger spaces.
⚠️ Handling:
Lift Quartz Clusters from the base rather than individual points. Terminations can chip if knocked together.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking if fractures or inclusions are present. Dry thoroughly.
☀️ Light:
Clear Quartz Clusters are light-stable. Amethyst or Smoky varieties should be protected from prolonged intense sunlight.
📦 Storage & Display:
Display where the cluster can radiate freely. Avoid stacking heavy objects on top of points.
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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 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.
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.”
| 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 |
⚠️ 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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The term Laser Wand Quartz is the most widely used and accepted naming convention in both the collector and practitioner communities, and is therefore used throughout this listing.
Laser Wand Quartz crystals are naturally occurring Quartz points that are long, slender, and very sharply tapered. They are often extremely clear, with minimal side faces, giving them a needle-like or beam-focused appearance. These formations are not cut or shaped — true Laser Wands are born this way through natural growth conditions.
Because of their precision form, Laser Wand Quartz crystals have long been regarded as advanced light tools, capable of condensing, focusing, and directing energy with exceptional accuracy.
Laser Wand Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system, like all Quartz. What distinguishes Laser Wands is not chemistry, but highly specialized growth behavior.
These crystals form under conditions that strongly favor elongation along a single axis, with minimal lateral face development. The result is a crystal that is extremely narrow relative to its length, often terminating in a very sharp point.
The most highly regarded Laser Wand Quartz crystals come from the Diamantina region of Brazil. Diamantina Laser Wands are widely acknowledged as some of the highest-quality Laser Wands in the world.
Notably, Diamantina Laser Wands are often measured at approximately 7.5 on the Mohs hardness scale, compared to the standard 7.0 hardness of most Quartz crystals. This increased hardness contributes to their durability, clarity, and in some cases, their distinctive acoustic “singing” properties.
| Property | Value |
|---|---|
| Mineral Species | Quartz (Laser Wand formation) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7.0 (up to ~7.5 for Diamantina material) |
| Luster | Vitreous |
| Transparency | Often highly transparent |
| Defining Feature | Extreme elongation and sharp termination |
⚠️ Handling:
Laser Wand Quartz crystals are often thin and sharply terminated. Handle gently and avoid pressure on the tip.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking, especially for very slender specimens. Dry thoroughly.
☀️ Light:
Light-stable under normal conditions.
📦 Storage & Display:
Store padded and separated from other crystals to protect delicate terminations. Display securely to prevent rolling or tipping.