Weight – 8.8 oz’s – 249 gm’s
Dimensions – 5.32″ x 2.24″ long/wide (13.5 x 5.7 cm’s)
Country of Origin – Colombia
USD $73.00
SKU: Q4410
This specimen is a Colombian Clear Quartz Cluster with awesome Green Clinochlore – A variety Of Chlorite! This cluster displays awesome aesthetics and sparkles with incredible luster and fantastic clarity! This crystal is in excellent condition. Check out the video just above for the best look at this wonderful specimen!
In stock
Weight – 8.8 oz’s – 249 gm’s
Dimensions – 5.32″ x 2.24″ long/wide (13.5 x 5.7 cm’s)
Country of Origin – Colombia
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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 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.
| 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 |
⚠️ 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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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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Chlorite Included Quartz is a natural Quartz crystal containing inclusions of Chlorite, a green phyllosilicate mineral group commonly associated with low-grade metamorphic environments. These inclusions may appear as wispy clouds, mossy veils, granular coatings, or distinct internal landscapes suspended within the Quartz.
In some specimens, Chlorite inclusions form phantoms—internal outlines of earlier growth stages of the Quartz crystal. This occurs when a layer of Chlorite settles on the crystal surface during growth, after which Quartz continues to crystallize over it. The result is a visible “snapshot” of the crystal at that moment in time. Multiple growth interruptions can produce multi-layered phantom formations.
Chlorite Included Quartz is found in a variety of Quartz-bearing regions, including Brazil, Pakistan, India, the Himalayas, Colombia, and parts of the United States. Each locality produces distinct inclusion styles ranging from light green dusting to deep forest-green phantoms.
This material is sometimes confused with moss agate or artificially enhanced Quartz. Genuine Chlorite Included Quartz shows inclusions fully enclosed within natural Quartz growth, not surface staining or dye.
Chlorite Included Quartz is composed of silicon dioxide (SiO₂) crystallizing in the trigonal crystal system, with Chlorite inclusions incorporated during growth. Chlorite itself is a group of hydrous magnesium, iron, and aluminum silicate minerals that typically form during metamorphism or hydrothermal alteration.
As Quartz crystals grow in mineral-rich fluids, fine Chlorite particles may settle onto crystal faces or remain suspended within the solution. Continued Quartz growth encapsulates these particles, preserving them as internal inclusions or phantom layers.
The presence of Chlorite does not significantly alter the hardness of Quartz, though heavily included specimens may have internal planes or zones that require careful handling.
| Property | Value |
|---|---|
| Mineral Species | Quartz with Chlorite inclusions |
| Chemical Formula | SiO₂ (Quartz) + Chlorite group inclusions |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Inclusion Type | Chlorite (green phyllosilicate minerals) |
| Special Features | Phantoms, internal landscapes, growth zoning |
⚠️ Handling:
Handle from the base to protect crystal terminations. Included Quartz may have internal planes that benefit from gentle treatment.
🧼 Cleaning:
Generally water-safe for brief rinsing. Avoid prolonged soaking, especially if the crystal contains fractures. Dry thoroughly.
☀️ Light:
Chlorite Included Quartz is light-stable. Normal display lighting is safe.
📦 Storage & Display:
Store separately or padded to prevent abrasion from harder minerals. Stable display helps preserve clarity and internal detail.
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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.