A large volcanic depression, usually several kilometres in diameter, formed primarily by the collapse of a magma chamber roof or, less frequently, by a volcanic explosion. A caldera often contains smaller craters, cones, and other types of volcanic vent. Small collapse craters less than 1 km in diameter are known as collapse pits. Calderas are often non-circular in shape. Many of the small number of volcanic craters on the Moon appear to be calderas, some of them at the heads of sinuous rilles. There are also huge calderas at the summits of many of the giant volcanoes of Mars. Olympus Mons has a complex of summit calderas more than 60 km in diameter, apparently the result of several collapse events. Similar features are found on the volcanoes of Venus.
http://www.esa.int/spaceinimages/Images/2004/02/Detail_of_the_complex_caldera_of_Olympus_Mons