Weight – 4.07 oz’s – 115 gm’s
Dimensions – 2.09″ x 2.28″ long/wide (5.3 x 5.8 cm’s)
Country of Origin – Brazil
USD $42.00
SKU: E454
This Brazilian Smoky Quartz Crystal has wonderful Elestial Scepter form, shiny luster and great light Smoky color as well as small amounts of red clay inclusions!! This crystal is in excellent condition.
In stock
Use the tabs below to explore crystal origins, geological details, crystal care guidance, and metaphysical insights.
Weight – 4.07 oz’s – 115 gm’s
Dimensions – 2.09″ x 2.28″ long/wide (5.3 x 5.8 cm’s)
Country of Origin – Brazil
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Smoky Quartz is one of the most practical, grounding, and widely used Quartz varieties and is often considered a default crystal in healing layouts. Its naturally smoky coloration ranges from light translucent brown through to deep smoky grey and near-black tones.
Smoky Quartz forms when Clear Quartz is exposed to natural radiation within the Earth over long periods, causing aluminum impurities in the crystal lattice to change the way light is absorbed. This process is entirely natural and produces a grounding, stabilizing crystal with remarkable resilience.
Morion Crystals are a very dark to opaque, nearly black variety of smoky quartz, a brownish-to-black form of quartz crystal colored by natural radiation – it must still be translucent to be termed a “Morion”.
Smoky Quartz may occur as single points, clusters (rare), Elestial formations, Phantoms, and on very rare occasions Cathedral formations. It can also combine naturally with other Quartz varieties such as Amethyst and Citrine, creating powerful hybrid crystals.
Smoky Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system, like all Quartz. Its coloration is caused by natural ionizing radiation acting on trace aluminum within the crystal structure.
True Smoky Quartz remains at least partially translucent. Completely opaque specimens are extremely rare and should be treated with caution, as much material on the market is artificially heat-treated Clear Quartz.
| Property | Value |
|---|---|
| Mineral Species | Quartz (Smoky variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Translucent to transparent |
| Defining Feature | Natural radiation-induced coloration |
A significant amount of Smoky Quartz on the market is artificially heated Clear Quartz. Majestic Quartz goes to great lengths to only natural Smoky Quartz.
⚠️ Handling:
Smoky Quartz is durable and well suited for frequent handling and healing work.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking if inclusions or fractures are present. Dry thoroughly.
☀️ Light:
Prolonged intense sunlight may gradually fade color in some specimens.
📦 Storage & Display:
Smoky Quartz performs best when actively used rather than stored away. Ideal for daily grounding and protection.
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Scepter Quartz is one of the most visually dramatic and symbolically potent growth forms in the Quartz world. These crystals form when a Quartz point grows, pauses or changes conditions, and then later continues growth with a larger “crown” crystal that develops on top of the earlier stem. The result is a crystal that resembles a scepter — a stem with a commanding head.
Because of this crown-over-stem structure, Scepter Quartz has long been regarded as a crystal of power, authority, and directed purpose. It carries the feeling of energy flowing toward the heart (center) of things — the essential truth beneath surface complexity.
Scepter Quartz occurs in many Quartz varieties including Clear Quartz, Smoky Quartz, and Amethyst. Some scepters are subtle and elegant; others are bold and unmistakable, with thick crowns and strong structural contrast.
Scepter Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal system like all Quartz. What defines a scepter is its two-stage growth history.
A scepter forms when a crystal grows normally as a point (the stem), then experiences a change in conditions — such as shifts in temperature, chemistry, or available growth space. Later, growth resumes, but the new growth develops wider than the earlier stem, producing a larger termination (the crown).
| Property | Value |
|---|---|
| Mineral Species | Quartz (Scepter growth habit) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Defining Feature | Widened crown from a second growth phase |
⚠️ Handling:
Scepters often have a structural “neck” where stem meets crown. Always lift from the base or thickest portion and avoid twisting pressure.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking if fractures, internal veils, or delicate surface etching are present.
☀️ Light:
Clear scepters are generally light-stable. Smoky and Amethyst scepters should be protected from prolonged intense sunlight.
📦 Storage & Display:
Store cushioned and separated from other specimens. Display securely to avoid falls — crowns chip easily if dropped.
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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.
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Elestial Quartz—sometimes referred to as Elestial Crystals—are among the most complex and information-rich Quartz formations known. While Elestials have been found in several countries including India, Australia, Africa, and the United States, the most significant and consistent source is Brazil, specifically the state of Minas Gerais.
Minas Gerais is an immense and intricate mining region, consisting of thousands of small, often hand-worked mines spread across a wide area. Within this region, true Elestial Quartz originates from a remarkably localized source—essentially a single large hill. Elestials occur in small to medium-sized pockets, and each pocket produces crystals with unmistakable family traits.
One of the most fascinating aspects of Elestial Quartz is that even when two pockets are found only feet apart, the crystals from each pocket will often display distinctly different growth signatures, surface features, and internal character. This phenomenon highlights the extraordinary adaptability of Elestial Quartz as it responds to subtle variations in geological and energetic conditions during formation.
This extreme variability is a defining hallmark of Elestials and contributes greatly to their reputation as crystals of adaptability, integration, and multidimensional awareness.
Elestial Quartz is composed of silicon dioxide (SiO₂) and crystallizes in the trigonal crystal system, like all Quartz. What distinguishes Elestials is not chemistry, but an exceptionally complex growth process involving repeated phases of expansion, contraction, dissolution, and regrowth.
Elestial crystals commonly exhibit:
Many Elestials grow in skeletal form, meaning the crystal develops in layers rather than completing each growth phase uniformly. In some specimens, outer layers fully enclose earlier stages, allowing the observer to gaze through successive layers from the outside inward. In others, the layers remain incomplete, creating stepped surfaces that can be both seen and felt.
Some Elestial Quartz crystals also contain moving water bubbles, known as Enhydro Crystals. These trapped ancient fluids are geological records of the environment at the time of formation.
Etching is common, though not universal, in Elestial Quartz. These etched patterns often resemble complex symbols or glyph-like markings created by selective dissolution during growth pauses.
| Property | Value |
|---|---|
| Mineral Species | Quartz (Elestial formation) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous to matte (etched areas) |
| Transparency | Transparent to translucent |
| Common Features | Skeletal growth, etching, internal chambers |
⚠️ Handling:
Elestial Quartz often features deep etching, layered growth, and delicate recesses. Handle gently and avoid impacts, especially on stepped or skeletal areas.
🧼 Cleaning:
Water-safe for brief rinsing. Avoid prolonged soaking, ultrasonic cleaners, or chemical agents, which may lodge in etched surfaces. Dry thoroughly.
☀️ Light:
Light-stable under normal conditions. Specimens with enhydros should be protected from extreme temperature changes.
📦 Storage & Display:
Display securely where airflow and vibration are minimal. Store padded and separate from other crystals to protect intricate surfaces.