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Loading contentThe strewn fields where the fragments of a single fall are recovered.
A field of craters and large iron masses in northern Argentina, formed by an ancient fall and known to local peoples for thousands of years — the source of some of the heaviest meteorite masses on Earth.
The strewn field left by the 1947 Sikhote-Alin iron meteorite fall, where thousands of fragments and impact pits were scattered across the taiga of the Russian Far East.