Weight – 1.86 oz’s – 52.8 gm’s
Dimensions – 2.36″ x 2.36″ across/wide (6 x 6 cm’s)
Country of Origin – Inner Mongolia
Calcite Coated Hematite Included Quartz Cluster
USD $26.00
SKU: Q4334
This Quartz Cluster out of Inner Mongolia is beautiful and features nice Hematite inclusions with dazzling Calcite showered over top! See the video just above for the best view of this incredible specimen! This specimen is in excellent condition.
Out of stock
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Mongolian Quartz Origins & Background
Mongolian Quartz is one of the most exciting and important Quartz discoveries of the modern era. Specimens have been emerging in increasing numbers since approximately 2013, and they represent a completely distinct and highly expressive genre of Quartz growth.
These crystals originate from regions of Mongolia that are geologically complex and mineral-rich, allowing Quartz to form alongside — and sometimes directly within — other mineral species. The result is an astonishing diversity of forms, inclusions, and structural behaviors rarely seen concentrated in a single Quartz family.
Mongolian Quartz is often referred to as a crystal for “The Now”. Its emergence coincides with a time of rapid global change, collective reassessment, and a growing need for heart-centered communication and cooperation.
Mongolian Quartz Geological Information
Mongolian Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system. What sets it apart geologically is the extraordinary range of growth environments and mineral associations involved in its formation.
Notable Geological Characteristics
- Cascading formations: stepped, flowing crystal growth.
- Dual Core (Pseudomorph) Quartz: inner clear cores later overgrown by included or differently colored Quartz.
- Extensive etching: from fine, intricate patterns to bold, chiseled surfaces.
- Complex mineral associations: including calcite, fluorite, garnet, hedenbergite, and specularite.
Common Associated Minerals
- Hedenbergite: often green, included within Quartz.
- Calcite: frequently pink or white, sometimes forming alongside or beneath Quartz.
- Specularite (Hematite):strong> reflective inclusions enhancing visual depth.
- Garnet: appearing as matrix or companion crystals.
- Fluorite: occasionally present in striking color contrast.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous to metallic (with inclusions) |
| Transparency | Transparent to opaque |
| Defining Feature | Extreme structural and mineral diversity |
Dual Core (Pseudomorph) Formation Explained
Dual Core Mongolian Quartz crystals begin life as one crystal — often clear Quartz — and later undergo overgrowth by a second Quartz phase or included material. This creates a crystal with a distinct internal core that actively radiates through the outer layer, producing a synergistic amplification effect.
Mongolian Quartz Crystal Care & Ownership Advice
⚠️ Handling:
Handle gently, especially around cascading edges and etched surfaces. Lift from the base.
🧼 Cleaning:
Avoid prolonged soaking due to associated minerals like calcite and fluorite. Use brief water rinses or dry methods.
☀️ Light:
Some inclusions may be light-sensitive. Avoid prolonged intense sunlight.
📦 Storage & Display:
Display where light can reveal internal complexity, but ensure stable placement.
Calcite
For what and How Does One Use it?
Calcite comes in many flavors and color varieties.
Calcite energizes the body’s electromagnetic systems. It helps bring the Yin and Yang aspects of us into balance. It fortifies our emotional strength, helping alleviate fear and anxiety.
Meditate with Calcite to amplify thoughts and promote astral projection.
As an elixir it has powerful detoxification properties, with a special focus on the kidneys.
Read A LOT more regarding Calcite Properties at the link below (will open in a new tab/window)….
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Hematite Origins & Background
Hematite is one of the most important and widely distributed iron minerals on Earth. Its name derives from the Greek word haima, meaning “blood,” referencing the reddish streak Hematite produces when powdered—despite often appearing metallic gray or black in solid form.
Hematite has been used by humans since prehistoric times for pigments, tools, ceremonial objects, and grounding talismans. Today, it remains prized both as a mineral specimen and as a practical stone for grounding and focus.
Major sources of Hematite include Brazil, Australia, South Africa, England, Canada, and the United States. It occurs in massive, botryoidal, tabular, and crystalline forms, as well as polished disks, pendants, and beads.
Hematite Geological Information
Hematite is an iron oxide mineral with the chemical formula Fe₂O₃. It crystallizes in the trigonal crystal system and forms in a wide range of geological environments, including sedimentary, metamorphic, and igneous settings.
Hematite is one of the primary ores of iron and plays a major role in Earth’s geologic and industrial history. It often forms alongside Quartz, Magnetite, Goethite, and other iron-rich minerals.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Hematite |
| Chemical Formula | Fe₂O₃ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 5–6 |
| Luster | Metallic to earthy |
| Color | Steel-gray, black, reddish-brown |
| Streak | Reddish-brown |
| Density | High |
Structural Notes
Hematite’s density and iron-rich composition give it a pronounced physical “weight,” which contributes to its long-standing association with grounding and stability.
Hematite Crystal Care & Ownership Advice
⚠️ Handling:
Hematite is generally durable, though polished pieces can chip if dropped.
🧼 Cleaning:
Avoid prolonged water exposure, especially for polished or coated pieces. Clean with a dry or slightly damp cloth and dry thoroughly.
☀️ Light:
Light-stable under normal conditions.
📦 Storage & Display:
Store separately from very hard minerals to avoid scratching. Hematite disks and pendants are ideal for daily wear.
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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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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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