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Paragould

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description Paragould Overview

Paragould is an LL5 ordinary chondrite that fell near Paragould, Arkansas, in 1930. Its classification indicates a meteorite with relatively low total iron and low metallic iron whose constituent minerals were thermally equilibrated within its parent asteroid. Multiple recovered masses, including a notably large main mass, make it an important documented example of a witnessed North American chondrite fall.

help Paragould FAQ

When and where did the Paragould meteorite fall?

The Paragould meteorite fell near Paragould, Arkansas, in 1930. It was an observed fall, meaning witnesses saw the meteorite descend, and multiple fragments were subsequently recovered.

What type of meteorite is Paragould classified as?

Paragould is classified as an LL5 ordinary chondrite, indicating relatively low total iron and low metallic iron content. Its constituent minerals were thermally equilibrated within its parent asteroid before reaching Earth.

How large was the Paragould meteorite?

Multiple fragments were recovered after the 1930 fall, and the total recovered mass made it one of the more significant meteorite falls recorded in the United States. The main mass is reported to be among the largest individual meteorite specimens recovered in North America.

Where are specimens of the Paragould meteorite housed today?

Specimens from the Paragould fall are held in multiple institutional and museum collections. Major meteorite collections in the United States, including natural history museums, have portions of the recovered material.

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