description Sharps Overview
Sharps is an H3.4 ordinary chondrite meteorite that fell in Virginia in 1921. Its classification places it among relatively unequilibrated H-group chondrites, which contain abundant metal and preserve chondrules and other early solar system textures more clearly than strongly heated ordinary chondrites. The material is therefore useful to meteoriticists investigating primitive asteroid matter, thermal alteration, and the mineralogical conditions present during early planetary formation.
help Sharps FAQ
Where and when did the Sharps meteorite fall?
The Sharps meteorite fell in Virginia, USA, in 1921. It is named after the town of Sharps where the fall occurred. The recovery of this stone marked one of the rare observed meteorite falls in the state of Virginia.
What is the classification of the Sharps meteorite?
Sharps is classified as an H3.4 ordinary chondrite. The H stands for high iron, meaning it contains abundant metal, while the 3.4 designation indicates it is relatively unequilibrated. This means it preserves clear chondrules and early solar system textures.
Why is the Sharps meteorite significant to scientists?
Because it is an H3.4 chondrite, Sharps preserves chondrules and other early solar system textures much more clearly than strongly heat-altered meteorites. It provides researchers with a relatively unmodified look at the materials that formed the early solar nebula. Its unequilibrated nature makes it highly valuable for studying cosmochemistry.
How much of the Sharps meteorite was recovered?
A single stone weighing around 1.5 kilograms was recovered from the fall. It was acquired by the Smithsonian Institution. The main mass remains an important part of the national meteorite collection.
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