L4-6 Chondrite Meteorite Fragment
£ 200.00
A large and well-preserved rounded chondrite meteorite fragment. This chondrite was found in Northwest Africa, and falls within the L4-6 type. L type chondrites are the second most common group of meteorites. L chondrites get their name from the low levels of iron found in the meteorite, in comparison to H chondrites, which have a high level.
Date: Circa 500 million years ago
Period: Ordovician Period, Paleozoic Era
Provenance: From a Surrey gentleman's collection (DG), purchased on the London Art Market from an ADA member, formed 1990's onward.
Condition: Excellent. The condrite displays markings and indentations on its surface.
SOLD
Chondrites are stony meteorites, formed as different types of dust and small grains combine. Chondrites are the most abundant meteorite class, constituting over 80% of meteorite falls. These chondrite falls range massively in size: from a singular stone to showers that consist of thousands of stones.
Chondrites are distinguishable by their composition – they are made up of chondrules, which are molten or partially molten droplets. Chondrites are believed to be one of the oldest solid materials in the Solar System – studying them can provide very valuable insights into the formation of our planetary system.
