Ordinary chondrite meteorite fragment, likely H5 classification

Ordinary chondrites are the most common type of meteorite found on Earth, representing approximately 80% of all meteorite falls. These stony meteorites formed in the early solar system over 4.5 billion years ago and contain small spherical structures called chondrules, which are among the oldest solid materials in our solar system. H-type chondrites are characterized by their high iron content and are named for their classification within the ordinary chondrite group. Meteorite specimens like this are highly valued by collectors, researchers, and astronomy enthusiasts who appreciate holding a tangible piece of space history. The meteorite collecting community spans amateur rockhounds, serious collectors, museums, and scientific institutions, all drawn to these extraterrestrial specimens for their scientific significance, rarity, and the profound connection they provide to the cosmos beyond our planet.