The Aegirine crystals originate from Mt. Malosa in the Zomba region of Malawi, a globally recognized pegmatite locality renowned for its exceptional alkaline rock mineral diversity. Under hydrothermal conditions, the crystals formed in open cavities, yielding well-defined prismatic aggregates with sharp edges.
Aegirine is a sodium-iron silicate distinguished by its acicular to prismatic habit. This flat features Aegirine in rich paragenesis, vividly illustrating the geological complexity of the site.
Collectors value the sharp crystal habits, strong matrix attachment, and pristine surfaces, which display exceptionally well in premium showcases. With documented provenance and excellent preservation, this flat is ideal for systematic collections and themed exhibit cabinets.