beryllos

Beryllos is a mineral term used in some mineralogical and gemological texts to denote a hypothetical species within the beryl group. It would be a transparent hexagonal silicate containing beryllium, aluminum, and silicon, with color variations produced by trace elements.

Ideal formula Be3Al2Si6O18 is often cited, with substitutions by iron, manganese, and chromium accounting for color diversity.

The crystal system is hexagonal, with a vitreous luster and a Mohs hardness of about 7.5 to 8; typical specific gravity ranges from 2.7 to 2.9.

Beryllos is said to form in late-stage pegmatites and hydrothermal veins rich in beryllium and aluminum, commonly associated with muscovite, spodumene, and tourmaline.

Color varieties are described as colorless to pale green, blue, or yellow, depending on trace elements such as iron, chromium, manganese, or titanium.

In jewelry, a gem labeled beryllos would be cut similarly to other beryls, though confirmed natural occurrences are rare and the term remains largely scholarly.

Major mineral databases do not recognize beryllos as an officially distinct species, and discussions of its status are primarily within teaching or speculative literature.

Handling beryllium-bearing minerals requires safety precautions due to health risks associated with beryllium exposure.