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Meteorite fall statistics

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Meteorite fall statistics are frequently used by planetary scientists to approximate the true flux of meteorites on Earth. Meteorite falls are those meteorites that are collected soon after being witnessed to fall, whereas meteorite finds are discovered at a later time. Although there are 30 times as much finds than falls, their raw distribution of types does not accurately reflect what falls to Earth.

ChondriteChondriteA chondrite (, ) is a stony (non-metallic) meteorite that has not been modified by either melting or differentiation of the parent body. They are formed when various types of dust and small grains in the early Solar System accreted to form primitive asteroids. Some such bodies that are captured in the planet's gravity well become the most common type of meteorite by arriving on a trajectory toward the planet's surface.Lunar meteoriteLunar meteoriteA lunar meteorite is a meteorite that is known to have originated on the Moon. A meteorite hitting the Moon is normally classified as a transient lunar phenomenon. DiscoveryIn January 1982, John Schutt, leading an expedition in Antarctica for the ANSMET program, found a meteorite that he recognized to be unusual.Meteorite fallMeteorite fallCollected meteorite whose fall was observedWitnessed bolideA meteorite fall, also called an observed fall, is a meteorite collected after its fall from outer space, that was observed by people or automated devices. Any other meteorite is called a "find". The Meteoritical Bulletin Database maintained by the Meteoritical Society is the authoritative reference for the recognition, naming and classification of meteorites.AchondriteAchondriteAn achondrite is a stony meteorite that does not contain chondrules. It consists of material similar to terrestrial basalts or plutonic rocks and has been differentiated and reprocessed to a lesser or greater degree due to melting and recrystallization on or within meteorite parent bodies. As a result, achondrites have distinct textures and mineralogies indicative of igneous processes.Meteorite classificationMeteorite classificationIn meteoritics, a meteorite classification system attempts to group similar meteorites and allows scientists to communicate with a standardized terminology when discussing them. Meteorites are classified according to a variety of characteristics, especially mineralogical, petrological, chemical, and isotopic properties.Meteorite findMeteorite findA meteorite find is a meteorite that was found by people, but whose fall was not observed. They may have been on Earth's surface for thousands of years and therefore could have been subject to varying amounts of weathering. Finds are distinguished from "meteorite falls", which were observed during their descent and collected shortly afterwards.MeteoriteMeteoriteA 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".Glossary of meteoriticsGlossary of meteoriticsThis is a glossary of terms used in meteoritics, the science of meteorites.Allende meteoriteAllende meteoriteThe Allende meteorite is the largest carbonaceous chondrite ever found on Earth. The fireball was witnessed at 01:05 on February 8, 1969, falling over the Mexican state of Chihuahua. After it broke up in the atmosphere, an extensive search for pieces was conducted and over 2 tonnes (2.2 tons) were recovered.Enstatite chondriteEnstatite chondriteEnstatite chondrites (E-type chondrites) are a rare form of meteorite, rich in the mineral enstatite. Only about 200 E-Type chondrites are currently known, comprising about 2% of the chondrites that fall on Earth. There are two main subtypes: EH and EL, classified based on their iron content. OriginE-type chondrites are among the most chemically reduced rocks known, with most of their iron taking the form of metal or sulfide rather than an oxide.

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