Weight – 38.6 oz’s – 1095 gm’s
Dimensions – 4.536″ x 5.542″ tall/wide (11.521 x 14.077 cm’s)
Country of Origin – Jiangxi Province, China
Red Hematite Included Quartz Flower Cluster with Tetrahedrite and Pyrite
USD $317.00
SKU: M1437
This is a Red Hematite Included Quartz Flower Cluster with Tetrahedrite and Pyrite! Underneath the Hematite, the crystals are clear! All throughout the Flower Cluster you can find chunks of Tetrahedrite with Pyrite partially coating some of them and sprinkled around. Found in the Jiangxi Province, China. Spectacular color from the Rich Hematite really helps the Tetrahedrite and Pyrite pop! This specimen is in Excellent Condition!
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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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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Pyrite Origins & Interesting Facts
Pyrite has been known and worked with since ancient times and was used by many early civilizations for both decorative and practical purposes. Its metallic luster and golden color earned it the nickname “Fool’s Gold,” though Pyrite has always been far more than a simple look-alike.
The name Pyrite comes from the Greek word pyr, meaning fire, as sparks are produced when it is struck against steel or stone. This property made Pyrite an important early fire-starting material long before modern ignition tools existed.
Pyrite commonly forms in cubes, pyritohedrons, clusters, and massive aggregates. Perfect cubic crystals with sharp edges are among the most visually striking mineral forms found in nature.
Pyrite is frequently found growing alongside other minerals such as Quartz, Fluorite, Calcite, Lapis Lazuli, and various sulfides. In many cases, Pyrite enhances the visual and energetic appeal of the host crystal it forms with.
From a metaphysical perspective, Pyrite has long been associated with vitality, strength, and resilience, reflecting its robust and enduring physical structure.
Pyrite Geological Information
Pyrite is an iron sulfide mineral with the chemical formula FeS₂. It crystallizes in the isometric (cubic) crystal system and is one of the most abundant sulfide minerals on Earth.
It forms in a wide range of geological environments including hydrothermal veins, sedimentary deposits, metamorphic rocks, and coal seams. Pyrite can grow slowly over long periods, producing exceptionally well-formed crystals.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Pyrite |
| Chemical Formula | FeS₂ |
| Crystal System | Isometric (Cubic) |
| Hardness (Mohs) | 6 – 6.5 |
| Luster | Metallic |
| Color | Brassy yellow |
| Common Forms | Cubes, clusters, massive |
Although visually similar to gold, Pyrite is much harder and more brittle, breaking rather than bending under stress.
Pyrite Crystal Care & Ownership Advice
🧼 Cleaning:
Do not soak Pyrite in water. Moisture can cause oxidation over time. Clean gently with a dry or slightly damp cloth and dry immediately.
📦 Storage:
Store Pyrite in a dry environment, ideally with airflow. Avoid sealed damp containers.
☀️ Light & Handling:
Pyrite is light-stable but should be handled with care to avoid chipping sharp edges.
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