Deep Earth

Understanding How Gems Form

Phase 01 // Origins

Pressure & Time

Most gemstones form deep within the Earth's crust (3 to 25 miles down) or even in the mantle. Under extreme heat and pressure, minerals crystallize from magma or hydrothermal fluids.

  • Diamonds Form in the mantle (~100 miles deep)
  • Pegmatites Slow-cooling magma pockets rich in aquamarine/tourmaline
Phase 02 // Extraction

The Uprising

Gems don't stay deep forever. Tectonic plate collisions and volcanic eruptions push these deep rock layers toward the surface.

"Erosion is the miner's best friend. Wind, rain, and glaciers wear away the softer surface rock, exposing the harder gem-bearing veins."

Regeneration

You might wonder: "If people have been mining here for decades, aren't all the gems gone?" The answer is no. Nature is constantly working for you.

Freeze-Thaw

Water seeps into cracks, freezes, and expands. This hydraulic action shatters rock faces, releasing new crystals every spring.

Hydraulic Scour

Storms scour riverbanks and wash away topsoil, revealing heavy gemstones that have settled in the gravel.

Field Tactics

Go After Rain

The best time to surface collect is immediately after a storm. Water washes dust off crystals, making them sparkle against the mud.

Solar Vector

Walk with the sun at your back. Scan the ground for reflections. Glassy or metallic lusters often indicate gemstones.