Weight – 1.79 oz’s – 50.7 gm’s
Dimensions – 2.56″ x 2.17″ long/wide (6.5 x 5.5 cm’s)
Country of Origin – Colombia
Colombian Rutilated Faden Quartz Cluster
USD $26.00
SKU: Q3775
This cluster has incredible rare form with gold rutile! It is made up of Tabular Faden Crystals! Faden clusters are extremely rare! This cluster displays awesome luster with great clarity! Colombian Quartz has been tested as the most pure quartz in the world! This crystal is in excellent condition. Check out the video just above for the best look at this incredible specimen!
In stock
Use the tabs below to explore crystal origins, geological details, crystal care guidance, and metaphysical insights.
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Quartz Cluster Origins & Background
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 Cluster Geological Information
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.
Physical Properties
| 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 |
Structural Advantage of Clusters
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.
Quartz Cluster Crystal Care & Ownership Advice
⚠️ 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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Tabular Quartz Origins & Background
Tabular Quartz crystals—often affectionately called “Tabbies”—are distinguished by their flat, plate-like form, where one or more faces are significantly wider than the crystal is thick. This growth habit creates a natural bridge-like geometry that has long been associated with communication, connection, and integration.
Tabular Quartz occurs in various Quartz varieties and may be found as single plates, twins, or stacked formations. Because their formation requires very stable growth conditions, well-formed Tabular Quartz crystals are less common than standard points.
These crystals are widely regarded as cooperative and people-oriented stones, excelling in situations where clarity, understanding, and harmony are needed.
Tabular Quartz Geological Information
Tabular Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system. The tabular habit forms when crystal growth favors lateral expansion along one crystallographic plane, resulting in broad, flat faces.
This growth style reflects long-term stability in the mineralizing environment, allowing the crystal to expand evenly rather than elongate rapidly.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Tabular growth habit) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Defining Feature | Wide, flat crystal faces |
Structural Significance
The flat geometry of Tabular Quartz naturally lends itself to interaction, transfer, and balance—qualities that strongly influence how these crystals are traditionally worked with.
Tabular Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Handle by supporting the crystal evenly across its surface. Avoid pressure on thin edges.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking if fractures are present. Dry thoroughly.
☀️ Light:
Light-stable and suitable for display.
📦 Storage & Display:
Store flat or well-supported to avoid stress on thin sections. Tabular Quartz enjoys being accessible for regular use.
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Rutilated Quartz Origins & Background
Rutilated Quartz is one of the most visually striking and energetically dynamic members of the Quartz family. These crystals contain needle-like inclusions of Rutile—titanium dioxide—embedded within Quartz, creating dramatic internal patterns that range from fine hair-like threads to bold, dense lattices.
Historically, Rutilated Quartz has been regarded as a crystal of acceleration and activation. Its unique internal structure gives it a distinctly “wired” quality, often described as highly electromagnetic and immediately responsive when worked with consciously.
Rutilated Quartz is found in several regions worldwide, with notable sources including Brazil, Madagascar, Pakistan, and parts of Africa. Each locality produces distinctive rutile coloration, density, and patterning.
Rutilated Quartz Geological Information
Rutilated Quartz is composed of silicon dioxide (SiO₂) with inclusions of Rutile (TiO₂). Rutile forms before or during Quartz crystallization, becoming encapsulated as the Quartz grows.
Rutile Inclusion Characteristics
- Needle-like or hair-like crystal structures
- May appear randomly oriented or aligned
- Density varies from sparse to heavily included
Rutile Color Variations
- Gold: the most well-known and widely sought after
- Copper / Red: often associated with Hematite-rich environments
- Silver: fine, bright needle structures
- Blue: rare and highly prized
- Green: extremely rare
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz with Rutile inclusions |
| Chemical Formula | SiO₂ + TiO₂ |
| Crystal System | Trigonal (Quartz) / Tetragonal (Rutile) |
| Hardness (Mohs Scale) | 7 (Quartz), 6–6.5 (Rutile) |
| Luster | Vitreous to metallic (internal) |
| Transparency | Transparent to translucent |
| Defining Feature | Needle-like Rutile inclusions |
Rutilated Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Handle carefully to preserve clarity and internal inclusion structure. Avoid sharp impacts.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking if fractures are present.
☀️ Light:
Generally light-stable. Display lighting enhances internal Rutile brilliance.
📦 Storage & Display:
Store separately to avoid scratching polished surfaces. Display where internal structure is visible.
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Faden Quartz Origins & Background
The word Faden comes from the German language and translates to “thread.” This name refers to the distinctive white or milky line that runs through these crystals, often appearing as a fibrous thread connecting individual crystal segments.
Although Faden Quartz is frequently marketed as originating from Pakistan, many specimens more accurately come from Afghanistan or directly along the Afghanistan–Pakistan border region. The political complexity of this area has led to frequent oversimplification or mislabeling of origin in the mineral trade. These crystals emerge from a region with deep historical tension, and their presence carries symbolic significance that cannot be separated from that context.
Faden Quartz typically forms in groups, where multiple crystals are joined together by the central thread. This natural linking gives each crystal a sense of both individuality and connection—each point distinct, yet part of a larger whole.
Faden Quartz Geological Information
Faden Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system, like all Quartz. What distinguishes Faden Quartz is its unusual growth process.
These crystals form within fractures in rock. As the fracture opens and closes over time, Quartz repeatedly breaks and regrows, with each phase reconnecting along a fibrous central seam—the “faden.” This process creates a crystal that is structurally reinforced along its center line.
Because of this repeated breaking and healing cycle, Faden Quartz is often considered one of the strongest self-healed Quartz formations.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Faden formation) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Defining Feature | Fibrous internal “thread” linking crystal segments |
Structural Significance
Rather than representing division or weakness, the faden line is a record of repeated reconnection. It demonstrates symmetry, resilience, and the ability to reform stronger after disruption.
Faden Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Faden Quartz may appear delicate due to its segmented form. Handle gently and avoid flexing or pressure along the crystal’s length.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking. Dry thoroughly, especially around natural fracture surfaces.
☀️ Light:
Light-stable under normal conditions.
📦 Storage & Display:
Store padded and separated from heavier specimens. Display in a way that supports the crystal along its length.
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Included Quartz Origins & Background
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 Geological Information
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.
Physical Properties
| 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 |
Structural Significance
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.
Included Quartz Crystal Care & Ownership Advice
⚠️ 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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Colombian Quartz Origins & Background
Colombian Quartz is widely regarded as one of the finest and most energetically refined forms of Clear Quartz found anywhere in the world. Sourced from high-altitude regions of the Colombian Andes, these crystals are celebrated for their exceptional clarity, brightness, and highly ordered internal structure.
Many Colombian Quartz crystals display Lemurian-style striations—distinct horizontal growth lines along the crystal faces—which has made them especially sought after within the Lemurian Seed Crystal community. These striations are natural growth features and not unique to Colombia, but the combination of clarity, formation quality, and surface refinement seen in Colombian material is considered exceptional.
Nearly all Colombian Quartz is associated with what is commonly referred to as the Silver Light family of Quartz crystals. This term is used descriptively rather than mineralogically, reflecting the perceived clarity, neutrality, and high coherence traditionally attributed to this material.
In recent years, Colombian Quartz has been marketed under a wide range of alternative names, often accompanied by dramatic price increases. While branding terms may vary, experienced collectors and practitioners widely recognize that these crystals originate from the same geological sources and share the same inherent properties. As always in the mineral world, informed sourcing and discernment are essential.
Colombian Quartz Geological Information
Colombian Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system, like all Quartz varieties. What distinguishes Colombian material is not its chemistry, but the geological conditions under which it forms.
These crystals grow in high-altitude hydrothermal environments characterized by stable temperatures, low contamination, and prolonged undisturbed growth. Such conditions favor exceptional transparency, sharply defined crystal faces, and minimal internal fracturing or inclusion.
Many Colombian Quartz points grow as single, elegant terminations rather than dense clusters, further contributing to their reputation for structural purity and visual refinement. Lemurian-style striations, when present, are the result of rhythmic growth pulses during crystallization.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Colombian Clear Quartz) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Highly transparent to translucent |
| Growth Features | Lemurian-style striations, refined terminations |
| Typical Formation | High-altitude hydrothermal veins |
Colombian Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Although Quartz is durable, Colombian Quartz often features exceptionally fine terminations and surface detail. Lift from the base and avoid pressure on points or striated faces.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking if internal fractures are present. Dry thoroughly to preserve surface brilliance.
☀️ Light:
Colombian Quartz is light-stable and suitable for normal display conditions.
📦 Storage & Display:
Store separately from softer minerals to prevent abrasion. Stable display preserves both physical integrity and visual refinement.
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