Weight – 0.95 oz’s – 27 gm’s
Dimensions – 2.763″ x 1.593″ long/wide (7.019 x 4.047 cm’s)
Country of Origin – Jiang Xi Province, China
USD $36.00
SKU: M1791
This specimen is High Grade Stibnite, sometimes called Antimonite, it is a sulfide mineral. Featuring incredible lead grey metallic color with a blue hue and an incredibly shiny luster and amazing form with complete terminations on a multiple points!! White photos have been included to better gauge color. 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 – 0.95 oz’s – 27 gm’s
Dimensions – 2.763″ x 1.593″ long/wide (7.019 x 4.047 cm’s)
Country of Origin – Jiang Xi Province, China
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Bridge and Inner Child Quartz crystals are defined by a distinctive growth pattern involving a primary crystal — often referred to as the “Mother” crystal — and one or more secondary crystals that grow in direct relationship to it.
These formations are also known by alternative names such as In/Out Quartz or Penetrator Quartz, depending on how the secondary crystal interacts with the primary crystal.
In Bridge Quartz formations, the smaller crystal visibly emerges from the larger crystal, creating a clear physical connection between two distinct crystal bodies. In Inner Child Quartz formations, the smaller crystal is mostly enclosed within the larger crystal, with only a portion visible.
These formations occur naturally during crystal growth and should not be confused with Manifestation Quartz or Baby-Within Quartz, which involve different internal growth dynamics.
Bridge and Inner Child Quartz can occur in Clear Quartz, Amethyst, Smoky Quartz, and other Quartz varieties, depending on the conditions present during formation.
Bridge and Inner Child Quartz formations develop when a secondary crystal begins growing either into or out of an existing Quartz crystal during overlapping growth phases.
In Bridge Quartz, the secondary crystal grows through or outward from the primary crystal, maintaining a visible connection between two otherwise independent growth points. This indicates a shift or continuation in growth conditions during formation.
In Inner Child Quartz, the secondary crystal becomes largely enclosed within the primary crystal as growth continues around it. The larger crystal effectively grows around and protects the smaller one, leaving it partially visible.
These formations require stable conditions over time, allowing both crystals to remain intact without dissolution or separation.
| Property | Value |
|---|---|
| Mineral Species | Quartz (Bridge / Inner Child formation) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
⚠️ Structural Awareness:
While Quartz is durable, the connection point between crystals can be more vulnerable. Handle with care and avoid impacts.
☀️ Sunlight & Heat:
Generally stable, though prolonged intense sunlight may fade Amethyst varieties.
🧼 Cleaning:
Clean gently with lukewarm water and a soft brush. Avoid ultrasonic cleaners.
📦 Storage & Display:
Display where the relationship between crystals is clearly visible and protected.
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Stibnite is a striking and unmistakable mineral known for its elongated, metallic, blade-like crystal formations. It has been known and used by humankind for thousands of years and is the primary ore of antimony.
Historically, Stibnite was used in ancient civilizations for medicinal preparations, pigments, and cosmetics. In ancient Egypt, powdered stibnite was used as kohl for eye makeup, believed to protect against illness and ward off negative influences.
Major sources of fine crystal specimens include China, Japan, Romania, Italy, Mexico, and parts of South America. Modern high-quality specimens—especially large radiating sprays—are most commonly associated with China.
Because of its dramatic appearance and fragile nature, Stibnite is highly prized by collectors and advanced crystal workers alike.
Stibnite is a sulfide mineral composed of antimony trisulfide (Sb₂S₃). It crystallizes in the orthorhombic crystal system and commonly forms elongated prismatic or bladed crystals, often arranged in radiating or fan-like clusters.
Stibnite typically forms in hydrothermal veins, frequently associated with quartz, calcite, barite, and other sulfide minerals.
| Property | Value |
|---|---|
| Mineral Species | Stibnite |
| Chemical Formula | Sb₂S₃ |
| Crystal System | Orthorhombic |
| Hardness (Mohs Scale) | 2 |
| Luster | Metallic |
| Color | Lead-gray to steel-gray |
| Transparency | Opaque |
| Cleavage | Perfect in one direction |
| Defining Feature | Elongated bladed metallic crystals |
Due to its softness and perfect cleavage, Stibnite is extremely fragile and must be handled with great care.
⚠️ IMPORTANT SAFETY NOTE:
Stibnite contains antimony and should never be used internally, in elixirs, or in water-based preparations.
⚠️ Handling:
Handle minimally. Do not touch crystal edges unnecessarily, as Stibnite is soft, brittle, and can shed fine particles.
🧼 Cleaning:
Do NOT use water. Clean only with a soft dry brush or compressed air.
☀️ Light:
Light-stable. No special light precautions required.
📦 Storage & Display:
Store in a padded container or display case. Avoid vibration or movement. Best displayed where it will not be disturbed.