| Specimen Details | |
|---|---|
| Weight | 1.83 oz’s – 51.2 g |
| Dimensions | 1.97″ x 1.26″ wide/tall (5 x 3.2 cm’s) |
| Country of Origin | Meig Mine, Sichuan province, China |
Natural Lepidocrocite Included Skeletal Elestial Amethyst Quartz Point
USD $23.00
SKU: Q3258
This Included Quartz Point from Meig Mine, Sichuan province China features exceptional Skeletal-Elestial form with deep color and awesome inclusions of Lepidocrocite inside!! 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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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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Skeletal Quartz Origins & Interesting Facts
Skeletal Quartz refers to Quartz crystals that have grown in a layered, framework-like structure rather than forming solid, fully infilled faces. This growth habit is the result of fluctuating environmental conditions during crystal formation, particularly changes in temperature, pressure, and mineral saturation.
These crystals are found in many Quartz-producing regions around the world, including Brazil, the Himalayas, the Alps, Arkansas, Madagascar, and parts of Africa. Skeletal growth can occur in Clear Quartz, Smoky Quartz, Amethyst, Citrine, and other Quartz varieties.
A key point of distinction is that while many Elestial Quartz crystals are skeletal in nature, not all Skeletal Quartz qualifies as Elestial. Elestial Quartz refers to a specific evolutionary growth pattern often associated with advanced, multi-terminated or etched forms, whereas skeletal growth can occur in many unrelated Quartz habits.
Skeletal Quartz crystals often display visible internal architecture, stepped growth layers, hollow sections, or partially formed faces. These features make each specimen visually unique and highly sought after by collectors who appreciate complex crystal growth habits.
From a metaphysical perspective, Skeletal Quartz is associated with understanding processes, layers of awareness, and incremental revelation rather than instant insight.
Skeletal Quartz Geological Information
Skeletal Quartz forms when crystal growth occurs faster at the edges and corners than in the central portions of the crystal faces. This results in hollowed sections, stepped layers, and a framework-like appearance.
These conditions typically arise when:
- Silica-rich fluids fluctuate rapidly in concentration
- Crystal growth is interrupted and resumes repeatedly
- Environmental chemistry changes during formation
Because of this interrupted growth, Skeletal Quartz often traps other materials between its layers. These may include:
- Other minerals such as Chlorite, Hematite, or Calcite
- Gas or liquid inclusions
- Water inclusions, forming Enhydro Quartz
These trapped layers provide valuable geological records of the crystal’s growth environment over time.
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Skeletal Growth Habit) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Common Associations | Elestial Quartz, Enhydro Quartz, Included Quartz |
Skeletal Quartz Crystal Care & Handling
⚠️ Handling:
Due to hollow sections and delicate skeletal structures, handle with care. Avoid pressure on thin edges or protruding layers.
🧼 Cleaning:
Water-safe for brief rinsing, but avoid prolonged soaking—especially for Enhydro specimens or crystals with inclusions.
☀️ Light:
Safe for normal display lighting. Avoid extreme heat or prolonged direct sunlight for included varieties.
📦 Storage:
Store separately from heavier or harder crystals to prevent chipping or abrasion.
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Elestial Quartz Origins & Background
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 Geological Information
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:
- Skeletal or layered growth (onion-like structure)
- Deep etching and terracing
- Multiple terminations and recessed faces
- Internal veils, windows, and cavities
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.
Physical Properties
| 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 |
Elestial Quartz Crystal Care & Ownership Advice
⚠️ 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.
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Amethyst Origins & Background
Amethyst has been valued across cultures for thousands of years for its rich violet coloration and its association with clarity, balance, and composure. The name Amethyst originates from the Greek word amethystos, meaning “not intoxicated,” reflecting an ancient belief that the stone helped maintain clear thinking and moderation.
Historically, Amethyst was considered a stone of royalty and spiritual authority. It adorned crowns, rings, and ceremonial objects in Ancient Greece and Rome and later throughout medieval Europe. Its purple color was rare and strongly associated with wisdom, restraint, and elevated status.
Significant Amethyst deposits are found in Brazil, Uruguay, Zambia, Madagascar, and Russia. Each locality produces crystals with distinctive growth habits, color zoning, and internal features, making provenance an important consideration for collectors and natural crystal enthusiasts.
Amethyst’s coloration develops through trace amounts of iron within the Quartz lattice combined with natural irradiation and geological heating over extended time periods. This process often creates layered growth zones that contribute to the depth and visual complexity seen in higher-quality specimens.
Some Amethyst crystals display structural growth features such as internal windows, phantoms, record keepers, and time-link faces. These are physical indicators of crystal formation traits and are valued for both the insight they provide into natural growth processes and to possible Metaphysical propoties.
Amethyst Geological Information
Amethyst is a violet variety of Quartz (Silicon Dioxide – SiO₂) that typically forms within cavities, veins, and geodes in igneous and metamorphic rock environments. Crystals usually grow as hexagonal prisms with pointed terminations.
The purple coloration results from trace iron incorporated into the Quartz structure combined with natural irradiation from surrounding rock. Subsequent geological heating stabilizes these color centers, producing hues that range from pale lavender to deep royal purple.
Amethyst commonly forms in volcanic environments, particularly within gas cavities of cooling basalt flows. Over millions of years, silica-rich fluids crystallize slowly, allowing layered growth and the development of internal zoning and structural features.
Common Geological Occurrences
- Volcanic basalt cavities and geodes
- Hydrothermal Quartz veins
- Metamorphic rock environments
Physical Properties
| Property | Value |
|---|---|
| Mineral Species | Quartz (Amethyst variety) |
| Chemical Formula | SiO₂ |
| Crystal System | Trigonal |
| Hardness (Mohs Scale) | 7 |
| Luster | Vitreous |
| Transparency | Transparent to translucent |
| Fracture | Conchoidal |
Amethyst Crystal Care & Ownership Advice
⚠️ Sunlight & Heat:
Prolonged exposure to intense sunlight or heat may cause some Amethyst specimens to fade over time. For long-term preservation, extended placement in direct sunlight is best avoided.
✋ Handling:
Amethyst is relatively durable, but sharp impacts can chip crystal points or edges. Handle specimens gently, especially clusters and terminated points.
🧼 Cleaning:
Clean Amethyst using lukewarm water and a soft brush. Avoid harsh chemicals, ultrasonic cleaners, or abrasive tools, which may damage crystal surfaces.
📦 Storage & Display:
Prolonged exposure to intense sunlight or high heat may cause some Amethyst specimens to fade over time.
For long-term preservation, extended placement in direct sunlight is best avoided. Indirect light or filtered natural light is ideal for display. This preserves color while still allowing the crystal’s natural beauty to be appreciated.
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