Keriya 001 is an Ordinary Chondrite (L6) discovered near Yutian in Xinjiang, China and officially named in 2021. As an L‑group stony meteorite, it contains silicate minerals with moderate iron content and exhibits the high‑grade metamorphism characteristic of L6 material, where original chondrules have been partially to fully integrated into the matrix. This type of meteorite offers a window into the deep thermal history of its parent asteroid, preserving evidence of ancient heating, impact processes, and the structural evolution of early solar‑system rock. Energetically, L‑type chondrites are often associated with grounding, coherence, and anchoring awareness into long‑scale cosmic time. Each specimen is presented in a clear acrylic display box (3.5 cm × 5.5 cm) with an identification label.
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1X KERIYA 001 ORDINARY CHONDRITE METEORITE | APPROX 2CM
Keriya 001 Ordinary Chondrite - China 2021
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KERIYA 001 ORDINARY CHONDRITE METEORITE
MKeriya 001 is an Ordinary Chondrite (L6) recovered near Yutian in Xinjiang, China and formally recognised in 2021. As an L‑group specimen, it contains moderate metal content and shows the advanced metamorphic features typical of the L6 classification, where early chondrules have been largely recrystallised into a compact, fine‑grained matrix. These characteristics make L6 chondrites valuable for understanding how parent asteroids underwent prolonged heating, internal reorganisation, and structural consolidation over geological time. The mineralogy records a mature stage in asteroidal evolution, offering insight into the processes that transformed primitive solar‑system material into more integrated stony bodies. Metaphysically, L‑type chondrites are associated with stability, long‑range focus, and the steady organisation of energy, supporting work that involves clarity, endurance, and alignment with broader cosmic patterns.
