Description
Snowflake Obsidian Obelisk Point – Natural Volcanic Glass Crystal
This Snowflake Obsidian Obelisk Point is a genuine natural volcanic glass specimen, carefully shaped and polished into a classic obelisk form. The photograph shows the exact piece you will receive, selected for its distinctive snowflake patterning, glossy finish, and balanced proportions. Full sizing details are available in the listing photos. Your specimen includes a Certificate of Authenticity lifetime guarantee generic card, confirming it as an authentic natural mineral example.
Mineral Type & Geological Classification
Snowflake Obsidian is a variety of obsidian, a naturally occurring volcanic glass formed from rapidly cooled silica-rich lava. Unlike crystalline minerals, obsidian does not have an ordered crystal structure because it cools too quickly for crystals to develop. It is classified as an igneous rock composed primarily of amorphous silicon dioxide (SiO₂).
The characteristic “snowflake” patterns are caused by the presence of cristobalite, a crystalline form of silica that develops within the glassy matrix during partial devitrification. These light grey to white radial clusters contrast sharply against the deep black volcanic glass, creating the distinctive snowflake appearance.
Obsidian typically measures around 5–5.5 on the Mohs hardness scale and displays a vitreous, glass-like lustre when polished.
Obelisk Shape & Craftsmanship
This specimen has been carved into a four-sided obelisk with a defined apex and flat base for stable display. The obelisk form enhances the visibility of the snowflake inclusions, allowing the radial cristobalite patterns to be viewed from multiple angles.
The polished surfaces create a smooth, reflective finish that emphasises the contrast between the dark glassy background and the lighter crystalline formations. Each face of the obelisk reveals unique pattern distribution, as the snowflake clusters form naturally and vary in size and placement.
Every snowflake obsidian piece is distinct due to the random formation of cristobalite within the volcanic glass.
Geological Formation
Snowflake Obsidian forms during volcanic eruptions when silica-rich lava cools rapidly at the Earth’s surface. As the lava solidifies into glass, small regions may begin to crystallise over time in a process known as devitrification. During this process, cristobalite crystals grow in radial patterns, creating the pale “snowflake” formations.
Obsidian deposits are commonly found in volcanic regions such as Mexico, the United States, Iceland, and parts of Central America. The stone is typically associated with rhyolitic lava flows and volcanic domes.
Historically, obsidian has been used for tools, carvings, and ornamental objects due to its sharp conchoidal fracture and glossy finish.
Physical & Visual Characteristics
Snowflake Obsidian is opaque with a high-gloss surface when polished. The contrast between black volcanic glass and light cristobalite inclusions creates a striking monochrome aesthetic.
Under direct lighting, the polished faces reflect light cleanly, enhancing the clarity of the snowflake patterns. Natural internal flow lines or minor inclusions may be visible and are characteristic of authentic volcanic glass.
Traditional & Cultural Associations
Obsidian has held cultural significance in many ancient civilisations for both practical and symbolic uses. In spiritual traditions, snowflake obsidian is sometimes symbolically associated with balance and reflection. These associations are cultural and belief-based rather than scientific.
Ideal for Collectors & Display
This Snowflake Obsidian Obelisk Point makes a bold addition to any mineral collection or decorative arrangement. Its dramatic black-and-white pattern pairs well with both modern and traditional interiors.
You will receive the exact specimen shown in the photographs, securely packaged and presented with a Certificate of Authenticity lifetime guarantee card. A genuine snowflake obsidian volcanic glass obelisk, selected for quality, pattern clarity, and craftsmanship.






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