METEOR AND METEORITE A meteor, also known as a shooting or falling star, is the streak of light produced by the vaporization of interplanetary particles as they enter the Earth's atmosphere. While still in space the particles are called meteoroids. A large and abnormally bright meteor is referred to as a fireball, and an exploding fireball is called a bolide. Larger meteors are not completely vaporized, and the particles that reach the Earth's surface are called meteorites. They may form METEORITE CRATERS, such as those found on the Moon, the inner planets, and the satellites of Mars and Jupiter. Meteor Showers Although a few meteors can be seen on any night, especially after midnight, during certain times of the year so many are visible that they are termed meteor showers. Records of meteor showers predate the 11th century. Until the present century, when the origin of such showers began to be understood, the phenomenon was usually the cause of considerable fear. Most meteor showers are believed to be produced by the debris of comets, which leave a trail of particles behind them as they orbit the Sun. When the Earth intercepts this stream of cometary debris, the small, low-density particles strike the atmosphere at speeds between 35 and 95 km/sec (22 and 60 mi/sec), causing them to vaporize and creating the visible meteor display. The average size of a meteor, which can be estimated from its brightness, height, and distance, is about the size of a grain of sand. During a shower, meteors appear to radiate from a point in the sky, called the radiant, which can be associated with a particular constellation. These radiant points give each shower its name; thus the Perseids (July 25-August 18) appear to radiate from the constellation Perseus, and the Leonids (November 15-19) from Leo. During the height of the heaviest showers, from 30 to 70 meteors may normally be seen every hour, but on rare occasions in a spectacular display that number may be visible every second. Meteorites It has been estimated that micrometeorites, so small that they drift to the ground without vaporizing, may add 1,000 tons to the mass of the Earth each day. Micrometeorites are not associated with meteor showers, nor are the larger meteorites that form craters. Although 500 large meteorites may fall on the Earth each year, only about 1% of these are recovered. Somewhat more than 120 impact sites have been identified. Meteorites may be classified according to composition as irons (siderites), stony irons (siderolites), and stones (aerolites). Iron meteorites are extremely dense and consist of 90% iron and 10% nickel. Stone meteorites have only about 10% nickel-iron and consist chiefly of silicates. Stony iron meteorites, which are relatively rare, are composed of iron and silicates in about equal proportions. Most stone meteorites contain small, spherical particles, or chondrules, composed of the silicates olivine, pyroxene, or orthopyroxene. These are called CHONDRITES to distinguish them from the few stones without chondrules, known as achondrites. While chondrites may contain 50 different minerals along with nickel-iron, achondrites contain mainly pyroxene and plagioclase. Nickel-iron is only rarely found in achondrites. It is not known if the glassy fragments found in certain regions of the Earth, known as TEKTITES, are related to meteorites. They have never been observed to fall. Iron meteorites are the type most often found, because of their unusual appearance. Stone meteorites are actually more numerous, but since they resemble ordinary rocks, they are not often found unless a fall is actually observed. Of all observed meteorite falls, 85% are chondrites, as are 95% of all stone falls. A special class of chondrites of particular interest are the carbonaceous chondrites, which consist largely of the mineral serpentine and contain amino acids and other organic compounds believed to be of extraterrestrial origin. Most of the evidence points to the nonbiological origin of these compounds, although it is possible that primitive life might arise from them--one of the theories of the origin of life in the solar system. Very dark in color, they are extremely rare, and constitute only about 2% of all stone falls. Meteorites have never been observed to fall during a meteor shower, which indicates that they are not remnants of comets. A very few meteorites have been identified as lunar in origin, but most are believed to originate from large parent bodies that formed at the time of the formation of the solar system and later broke up. ASTEROIDS would have had a similar origin and meteorites resemble them in general range of composition. Bibliography: Burke, J. G., Cosmic Debris (1991); Dodd, R. T., Thunderstones and Shooting Stars (1986); Kerridge, J., and Matthews, M., eds., Meteorites and the Early Solar System (1988); Kronk, G. W., Meteor Showers (1988); Kronk, G. W., Meteor Showers (1988); McSween, H. Y., Jr., Meteorites and Their Parent Planets (1987); Wasson, J. T., Meteorites, 2 vols. (1974, 1985). IMPORTANT ANNUAL METEOR SHOWERS IN THE NORTHERN HEMISPHERE --------------------------------------------------------------- Name of Shower Constellation of Date of Peak Radiant Activity --------------------------------------------------------------- Quadrantids Bootes Jan. 3 Alpha Aurigids Auriga Feb. 8 Virginids Virgo Mar. 20 Lyrids Lyra Apr. 21 Eta Aquarids Aquarius May 4 Ophiuchids Ophiuchus June 20 Delta Aquarids Aquarius July 29 Perseids Perseus Aug. 12 Kappa Cygnids Cygnus Aug. 20 Alpha Aurigids Auriga Sept. 22 Draconids Draco Oct. 9 Orionids Orion Oct. 21 Taurids Taurus Nov. 1 Leonids Leo Nov. 17 Geminids Gemini Dec. 13 Ursids Ursa Major Dec. 22 Name of Shower Normal Expected Associated Duration Hourly Rates Comet --------------------------------------------------------------- Quadrantids Jan. 1-4 50 _ Alpha Aurigids Feb. 5-10 5 _ Virginids Mar. 5-Apr. 2 5 _ Lyrids Apr. 19-23 10-15 1861 I Eta Aquarids May 1-8 20 Halley Ophiuchids June 17-25 20 _ Delta Aquarids July 26-31 25 _ Perseids Aug. 10-14 60 1862 III Kappa Cygnids Aug. 18-22 5-10 _ Alpha Aurigids Sept. 20-24 5 _ METEOR AND METEORITE Draconids Oct. 7-11 Varies (low to Giacobini- high) Zinner Orionids Oct. 18-23 25 Halley Taurids Oct. 15-Dec. 1 15 Encke Leonids Nov. 14-20 Varies (low to 1866 I high) Geminids Dec. 10-15 50 - Ursids Dec. 17-24 15 Tuttle ---------------------------------------------------------------