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  2. Meteorite - Wikipedia

    en.wikipedia.org/wiki/Meteorite

    Few meteorites are large enough to create large impact craters. Instead, they typically arrive at the surface at their terminal velocity and, at most, create a small pit. 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.

  3. Glossary of meteoritics - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_meteoritics

    Fossil meteorite – a meteorite that was buried under layers of sediment before the start of the Quaternary period. Some or all of the original cosmic material has been replaced by diagenetic minerals. [3]: 320 (It is, however, not a fossil). Fusion crust – a coating on meteorites that forms during their passage through the atmosphere.

  4. Meteoroid - Wikipedia

    en.wikipedia.org/wiki/Meteoroid

    A meteor, known colloquially as a shooting star or falling star, is the visible passage of a glowing meteoroid, micrometeoroid, comet or asteroid through Earth's atmosphere, after being heated to incandescence by collisions with air molecules in the upper atmosphere, [11] [23] [24] creating a streak of light via its rapid motion and sometimes ...

  5. Chondrite - Wikipedia

    en.wikipedia.org/wiki/Chondrite

    A chondrite / ˈ k ɒ n d r aɪ t / is a stony (non-metallic) meteorite that has not been modified, by either melting or differentiation of the parent body. [a] [1] They are formed when various types of dust and small grains in the early Solar System accreted to form primitive asteroids.

  6. Widmanstätten pattern - Wikipedia

    en.wikipedia.org/wiki/Widmanstätten_pattern

    Widmanstätten patterns, also known as Thomson structures, are figures of long phases of nickel–iron, found in the octahedrite shapes of iron meteorite crystals and some pallasites. Iron meteorites are very often formed from a single crystal of iron-nickel alloy, or sometimes a number of large crystals that may be many meters in size, and ...

  7. Meteoric iron - Wikipedia

    en.wikipedia.org/wiki/Meteoric_iron

    Meteoric iron also has an effect on the Earth's atmosphere. When meteorites descend through the atmosphere, outer parts are ablated. Meteoric ablation is the source of many elements in the upper atmosphere. When meteoric iron is ablated, it forms a free iron atom that can react with ozone (O 3) to form FeO. This FeO may be the source of the ...

  8. Meteorite classification - Wikipedia

    en.wikipedia.org/wiki/Meteorite_classification

    Meteorite classification may indicate that a "genetic" relationship exists between similar meteorite specimens. Similarly classified meteorites may share a common origin, and therefore may come from the same astronomical object (such as a planet, asteroid, or moon) known as a parent body. However, with current scientific knowledge, these types ...

  9. Kamacite - Wikipedia

    en.wikipedia.org/wiki/Kamacite

    Kamacite primarily forms on meteorites but has been found on extraterrestrial bodies such as Mars. This was discovered by The Mars Exploration Rover (MER) Opportunity. The kamacite did not originate on Mars but was put there by a meteorite. This was particularly of interest because the meteorite fell under the lesser known class of ...