# - 302 Tranca geode (un-broken)
On the outside, geodes appear like common, generally spherical, rocks but when split open they reveal stunning crystal caves. Discovered in 1971, Trancas geodes are sourced from Chihuahua in Mexico. A distinctive feature of trancas geodes is the long, curved, tentacle shaped quartz/chalcedony crystals which resemble stalagmites/stalactites. These geodes also often contain clear quartz, chalcedony, calcite, and quartz scepter crystals; as well as druzy quartz centers. Under short and medium wave UV lights, trancas geodes fluoresce neon green.
On the outside, geodes appear like common, generally spherical, rocks but when split open they reveal stunning crystal caves. Discovered in 1971, Trancas geodes are sourced from Chihuahua in Mexico. A distinctive feature of trancas geodes is the long, curved, tentacle shaped quartz/chalcedony crystals which resemble stalagmites/stalactites. These geodes also often contain clear quartz, chalcedony, calcite, and quartz scepter crystals; as well as druzy quartz centers. Under short and medium wave UV lights, trancas geodes fluoresce neon green.
On the outside, geodes appear like common, generally spherical, rocks but when split open they reveal stunning crystal caves. Discovered in 1971, Trancas geodes are sourced from Chihuahua in Mexico. A distinctive feature of trancas geodes is the long, curved, tentacle shaped quartz/chalcedony crystals which resemble stalagmites/stalactites. These geodes also often contain clear quartz, chalcedony, calcite, and quartz scepter crystals; as well as druzy quartz centers. Under short and medium wave UV lights, trancas geodes fluoresce neon green.