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The Sutter's Mill meteorite is a carbonaceous chondrite which entered the Earth's atmosphere and broke up at about 07:51 Pacific Time on April 22, 2012, with fragments landing in the United States. [ 6 ] [ 7 ] The name comes from Sutter's Mill , a California Gold Rush site, near which some pieces were recovered.
The first samples of this meteorite fall were recovered close to Sutter's Mill, so it was named the Sutter's Mill meteorite. Several dozen fragments were eventually identified, with a total weight of about a kilogram. The meteorite is classified as a carbonaceous chondrite and contains some of the oldest known material in the Solar System. [17]
A search for meteorites in the Dhofar Desert in the Arabian Peninsula (Dhofar Governorate, Oman, November 2012) A meteorite find is a meteorite that was found by people, but whose fall was not observed. [1] They may have been on Earth's surface for as many as thousands of years and therefore could have been subject to varying amounts of weathering.
The exact worth of a meteorite varies depending on the specific type of meteorite in question. An 82-pound iron meteorite originating from an asteroid recently sold for $44,100 — about $540 per ...
2024 BX 1, previously known under its temporary designation Sar2736, was a 44 centimetre-sized (17 inches) [4] asteroid or meteoroid that entered Earth's atmosphere on 21 January 2024 00:33 UTC and disintegrated as a meteor over Berlin. [2] [7] The recovered fragments are known as the Ribbeck meteorite.
The space rock that slammed into Earth 66 million years ago at the end of the Cretaceous Period caused a global calamity that doomed the dinosaurs and many other life forms. Researchers assessed ...
Collection of meteorites in the National Museum of Brazil; D. Dimmitt (meteorite) E. ... Sutter's Mill meteorite; Sylacauga (meteorite) V. Vermillion meteorite; W.
The meteorite is mostly composed of iron, but also contains nickel (about 6%), as well as small amounts of chromium, cobalt, phosphorus, and sulfur. The main mass was put on display in the Smithsonian Institution from 1978 to 1980, and now resides in the Desert Discovery Center in Barstow , California. [ 2 ]