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Meteorite class

Iron Meteorites

Meteorites made largely of nickel-iron metal, from the cores of differentiated asteroids.

Meteorite class

Overview

Dense meteorites of nickel-iron alloy, thought to be fragments of the metallic cores of asteroids that were shattered by collisions — the source of the largest meteorites found on Earth.

Meteorites

5 modelled meteorites.

  • An ancient field of large iron meteorites in Argentina, known to indigenous peoples for millennia, whose fragments include some of the heaviest single meteorite masses ever recovered.

    ClassIAB ironCountryArgentina
  • The iron meteorite responsible for Barringer Crater (Meteor Crater) in Arizona; fragments are scattered around the rim of the crater it formed some 50,000 years ago.

    ClassIAB ironCountryUnited States
  • Hobafind

    The largest known intact meteorite and the largest naturally-occurring piece of iron near the Earth's surface, an ~60-tonne slab still lying where it was found in Namibia.

    ClassIVB ironCountryNamibiaDate1920Mass~ 60 t (the largest single meteorite known)
  • One of the largest observed iron meteorite falls, which broke apart over the Sikhote-Alin mountains in 1947 and scattered thousands of fragments, many with dramatic regmaglypt thumbprint textures, across a strewn field.

    ClassIIAB ironCountryRussiaDate1947-02-12
  • The largest meteorite ever found in the United States, an ~15-tonne iron sacred to the Clackamas people of the Willamette Valley.

    ClassIIIAB ironCountryUnited StatesMass~ 15 t (largest found in the US)

Knowledge connections

Sources

The primary and reference sources this topic draws on.

  • NASANational Aeronautics and Space Administration

    Mission data, planetary science, space telescopes, and public-domain imagery.

    Most NASA-produced imagery is in the public domain; individual items are checked for usage terms before publication.