Murchison is one of the most famous and scientifically important Carbonaceous Chondrite falls, landing near Murchison, Victoria, Australia, on 28 September 1969. It is classified as a CM2 Carbonaceous Chondrite and is known for preserving primitive, volatile-rich material from the early solar system. More than 100 kg of material was recovered after the fall, and its relatively rapid collection helped preserve material suitable for detailed scientific study.

Murchison specimens are typically dark, fine-grained, and fragile, reflecting their Carbonaceous composition and history of aqueous alteration on the parent body. As a CM2 meteorite, it contains hydrated minerals, fine matrix material, and organic-rich components. Murchison is especially famous for its complex organic chemistry, including amino acids and other carbon-bearing compounds, making it one of the key meteorites for studying prebiotic chemistry.

Studying Murchison provides valuable insight into early solar system chemistry, water alteration, and the delivery of organic compounds to young planetary bodies. Its scientific importance, Australian provenance, witnessed fall status, and long research history make it one of the most desirable Carbonaceous Chondrites for collectors. Each specimen represents ancient asteroid material connected to one of the most influential meteorite falls in modern science.