Peridot

A variety of olivine, known for its bright green color.

Unlike many minerals,
its color comes directly from its composition,
rather than trace elements — resulting in a consistent green
that ranges from yellow-green to olive.

Peridot typically forms in volcanic environments,
brought to the surface through basaltic activity.

It has also been found in meteorites,
linking it not only to the Earth’s interior
but to material formed beyond it.

Because of this, it has often been associated with renewal and openness,
reflecting a sense of continuity rather than change.

Defined by color and origin,
it carries a green that feels inherent —
not added, but built in.