Iron meteorite
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Iron meteorites, also called siderites or ferrous meteorites, are a type of meteorite that consist overwhelmingly of an iron–nickel alloy known as meteoric iron that usually consists of two mineral phases: kamacite and taenite. Most iron meteorites originate from cores of planetesimals, with the exception of the IIE iron meteorite group
Tamentit Iron Meteorite, found in 1864 in the Sahara, weighing about 500 kg (1,100 lb). On display at Vulcania park in France.
Widmanstätten pattern as seen on an etched and polished slice of the Seymchan meteorite. Scale unknown.
The Hoba meteorite, the biggest known iron meteorite. It lies in Namibia and weighs about 60 tons.
The Willamette Meteorite on display at the American Museum of Natural History. It weighs about 14,500 kilograms (32,000 pounds). This is the largest meteorite ever found in the United States.
Meteorite
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A meteorite is a rock that originated in outer space and has fallen to the surface of a planet or moon. When the original object enters the atmosphere, various factors such as friction, pressure, and chemical interactions with the atmospheric gases cause it to heat up and radiate energy. It then becomes a meteor and forms a fireball, also known as a shooting star; astronomers call the brightest examples "bolides". Once it settles on the larger body's surface, the meteor becomes a meteorite. Meteorites vary greatly in size. For geologists, a bolide is a meteorite large enough to create an impact crater.
The 60-tonne, 2.7 m-long (8.9 ft) Hoba meteorite in Namibia is the largest known intact meteorite.
NWA 859 iron meteorite showing effects of atmospheric ablation
The impact pit made by a 61.9-gram Novato meteorite when it hit the roof of a house on 17 October 2012.
Meteorite fallen near Flensburg in 2019.