This stone reminds me of a foggy winter evening. Set in sterling silver with an 18” sterling silver chain.
These stones are formed when manganese or iron oxides are deposited within microcrystalline quartz.
As water containing these oxides enters the crystal’s structure the particles of black or brown manganese or iron are left behind. Over millions of years and cooling conditions, the tiny particles that were deposited into the host material solidify, crystallizing into a branch-like imprint.
