You can see that green chlorite coating and inclusions running through the quartz crystals. These pieces form when hot, mineral-rich fluids move through cracks in the rock. As things cool down, the quartz starts to crystallize, and minerals like Chlorite get trapped inside or grow alongside it.
Mineral Breakdown:
Quartz (SiO₂): The clear to milky crystals — hard, resistant, and forms in hexagonal shapes.
Chlorite (iron/magnesium aluminum silicate): That green color — usually forms in low to medium-grade metamorphic environments and hydrothermal systems.
This combo usually tells you there was some pressure, heat, and fluid movement involved — classic conditions for veins and pockets where crystals grow over time.
Not the flashiest piece, but it’s raw, natural, and tells a solid geological story — and that’s what matters.
Now I want to see yours 👇
What did you find this week? Drop your photos and tell us where it came from.
Let’s see what everyone’s pulling out of the ground 🌎🔥