Collection: Apophyllite

A hydrated potassium calcium silicate mineral,
known for its clear to pale green crystals and reflective internal structure.

Apophyllite typically forms in well-defined crystals,
often with square or pyramidal shapes,
and smooth, glass-like surfaces.

One of its distinctive features is the way it reflects light from within —
caused by natural cleavage planes that create a subtle internal shimmer.

It is commonly found growing alongside stilbite and other zeolite minerals,
forming balanced, multi-mineral compositions.

It has sometimes been associated with clarity and awareness — not as a promise,
but as a quality people have connected with it over time.

Defined by both structure and light,
it is as much about how it reflects as how it forms.