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circular, bowl-shaped depression on the earth's surface. (For a discussion of lunar craters, see moonmoon,
natural satellite of a planet (see satellite, natural) or dwarf planet, in particular, the single natural satellite of the earth. The Earth-Moon System

The moon is the earth's nearest neighbor in space.
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.) Simple craters are bowl-shaped with a raised outer rim. Complex craters have a raised central peak surrounded by a trough and a fractured rim.

Many of the largest craters are formed by the impact of meteoritesmeteorite,
meteor that survives the intense heat of atmospheric friction and reaches the earth's surface. Because of the destructive effects of this friction, only the very largest meteors become meteorites.
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. Impacting at speeds in excess of 10 mi/sec (16 km/sec), a meteorite creates pressures on the order of millions of atmospheres, producing shock waves that blast out a circular hole and often destroy the meteorite. Meteor, or Barringer, Crater, near Winslow, Arizona, c. 3-4 mi (1 1-5 km) in diameter and 600 ft (180 m) deep, is probably the best-known crater of this type. Of the 190 impact locations identified on earth, the largest craters by diameter (80 mi/130 km or greater) are at Vredefort, South Africa; and Chicxulub (off the coast of the Yucatán peninsula), Mexico. Others include Acraman Crater, South Australia; Brent Crater, Ontario; the Chesapeake Bay impact crater, Virginia; Chubb Crater, Quebec; Lake Bosumtwi, Ghana; and Manicouagan, Quebec; and Popigai Crater, Siberia. Two sizable impact events occurred in the 20th cent., both in Siberia. In 1908 in the Tunguska BasinTunguska Basin,
c.400,000 sq mi (1,036,000 sq km), Krasnoyarsk Territory and Sakha Republic, E central Siberian Russia, between the Yenisei and Lena rivers. It has a huge untapped coal reserve.
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 near Lake Baykal one occurred that caused vast destruction of timber from its blast, and the other in 1947 at Sikhote-Alin also caused great damage. Craters that have been obliterated by erosion over thousands of years, leaving only a circular scar on the earth's surface, are called astroblemesastrobleme
, large, circular structure ranging from c. 1-2 mi to 40 mi (.8–64 km) in diameter. Astroblemes are found at numerous places on the earth's surface, e.g., Meteor, or Barringer, Crater in Arizona, Brent Crater in Ontario, and Vredefort Ring in South Africa.
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. The fractured rock of buried impact craters (e.g., Chicxulub) may become a trap for oil and natural gas.

Craters are also commonly formed at the surface opening, or vent, of erupting volcanoesvolcano,
vents or fissures in the earth's crust through which gases, molten rock, or lava, and solid fragments are discharged. Their study is called volcanology. The term volcano
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, particularly of the type called cinder cones, where the lava is extruded rather explosively. Virtually all volcanoes display a crater, called a sink, around the vent; this is believed to be a collapse feature caused by molten lava subsiding as an eruption phase diminishes. Volcanic craters formed in these ways are relatively small, usually less than 1 mi (1.6 km) in diameter, and represent only a small fraction of the cone's diameter at the base. A caldera is a much larger crater, typically ranging from 3 to 18 mi (5–30 km) in diameter, and represents a considerable fraction of the volcano's basal diameter. In a few instances, however, tremendous volcanic eruptions have left calderas 50 mi (80 km) or so, such as that that forms much of Yellowstone National Park or the basin of Lake Toba, Sumatra, Indonesia. Most calderas are formed by the collapse of the central part of a cone during great eruptions; the pressure that a caldera collapse produces on a magma chamber helps drive such eruptions. A few small calderas have been formed by explosive eruptions in which the top of a volcano was blown out. Some volcanic craters are created by a combination of these events. Formed thousands of years ago, the caldera that contains Crater Lake, Oreg., is 6 mi (9.7 km) in diameter. In recent times, caldera-producing eruptions occurred at Krakatoa, Indonesia, in 1883 and Katmai, Alaska, in 1912.

See also tektitetektite
, naturally occurring, silica-rich (65%–80% SiO2) glass resembling obsidian and sometimes shale, and is normally jet black to olive green. They appear as small rounded or elongated objects that often have aerodynamic shapes and range from a fraction of
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See P. Hodge, Meteorite Craters and Impact Structures of the Earth (1994).

The Columbia Electronic Encyclopedia™ Copyright © 2013, Columbia University Press. Licensed from Columbia University Press. All rights reserved.


(kray -ter) (Cup) A small inconspicuous constellation in the southern hemisphere near Leo, the brightest stars being of 3rd and 4th magnitude. Abbrev.: Crt; genitive form: Crateris; approx. position: RA 11.5h, dec –l5°; area: 282 sq deg.
Collins Dictionary of Astronomy © Market House Books Ltd, 2006
The following article is from The Great Soviet Encyclopedia (1979). It might be outdated or ideologically biased.



a bowl- or funnel-shaped depression with a diameter measuring between dozens of meters and several kilometers and a depth from a few meters to hundreds of meters. Craters form during volcanic eruptions, as a result of the impact of meteorites, and as a result of large man-made explosions. Volcanic craters are usually located on the peaks or slopes of volcanoes. At the bottom of the crater are one or several vents through which lava and other volcanic products rising along an outlet channel from the magmatic center reach the surface. Sometimes the bottom of the crater is covered with a lake of lava or a small, newly formed volcanic cone.

The craters on the moon and Mars are round depressions surrounded by circular ridges; their diameters are up to 100–200 km and they are up to several kilometers deep. A distinction is made among them between craters formed during the impact of meteorites and asteroids and craters of volcanic origin (similar to the earth's volcanic craters and calderas).



(the Cup), a constellation of the southern hemisphere; its brightest star has a visual stellar magnitude of 3.6. The constellation is most easily viewed in March; it is visible from the central and southern regions of the USSR. (SeeSTELLAR SKY.)

The Great Soviet Encyclopedia, 3rd Edition (1970-1979). © 2010 The Gale Group, Inc. All rights reserved.


A large, bowl-shaped topographic depression with steep sides.
A rimmed structure at the summit of a volcanic cone; the floor is equal to the vent diameter.
(mechanical engineering)
A depression in the face of a cutting tool worn down by chip contact.
A depression at the end of the weld head or under the electrode during welding.


A constellation, right ascension 11 hours, declination 15°S. Abbreviated Crt. Also known as Cup.
McGraw-Hill Dictionary of Scientific & Technical Terms, 6E, Copyright © 2003 by The McGraw-Hill Companies, Inc.


1. the bowl-shaped opening at the top or side of a volcano or top of a geyser through which lava and gases are emitted
2. a similarly shaped depression formed by the impact of a meteorite or exploding bomb
3. any of the circular or polygonal walled formations covering the surface of the moon and some other planets, formed probably either by volcanic action or by the impact of meteorites. They can have a diameter of up to 240 kilometres (150 miles) and a depth of 8900 metres (29 000 feet)
4. a large open bowl with two handles, used for mixing wines, esp in ancient Greece
Collins Discovery Encyclopedia, 1st edition © HarperCollins Publishers 2005
References in periodicals archive ?
Since Mars is littered with craters, the researchers had to analyze each of them in order to find the one that showed traces of an impact as well as a ( tsunami .
The body was discovered by residents after a foul smell started emanating from the crater.The body was trapped in a tree and it took the team three days to retrieve it due to the steepness of the crater.
According to the scientists, younger craters tend to be covered by more boulders and rocks than older craters.
The small size of the Meteor Crater and the frequent occurrence of DWFs in the crater during clear-sky, undisturbed nights make it an ideal site for the study of downslope windstorms, as it can be extensively instrumented.
The bottom of the crater is covered with white sodium phosphate crystals.
The crater, named after the Antarctic explorer Ernest Shackleton, is two miles deep and more than 12 miles wide.
The craters form as noted above: flow from low surface tension to high surface tension.
The scientists took this to be evidence of a series of smaller explosions, culminating in the big one that created the main crater Older dates, going back 3,000-5,000 years were taken to mark the creation of nearby maars.
Where is the crater that is twice the diameter of Glover Bluff located?
The target studied was the Cabeus crater, which lies in a permanently shaded region of the Moon where temperatures fall as low as 35 Kelvin (minus 238C).
The crater rises above its desert surroundings, and during visits to the site over the past two years researchers have collected around 5,000 iron meteorites (the dark rocks pictured at right).
BEIRUT: The International Astronomical Union (IAU) recently approved a proposal from the MESSENGER Science Team to confer the name of Lebanese writer and painter Gibran Khalil Gibran on an impact crater on Mercury, Lebanese media reported on Monday.