Maat Mons is a massive shield volcano on the planet Venus and the planet's second-highest mountain and highest volcano . It rises 8 kilometres (5.0 mi) above the mean planetary radius at 0°30′N 194°36′E / 0.5°N 194.6°E / 0.5; 194.6 , and nearly 5 km above the surrounding plains . It is named after the Egyptian goddess of truth and justice, Ma'at .
7-514: Maat Mons is a large shield volcano located in Atla Regio , a site of recent tectonic rifting possibly fed by an active mantle plume. Three other neighbouring major volcanic centres are situated within Atla Regio, Ozza Mons , Ongwuti Mons, and an unnamed mons. Interpretation of their respective radial dike swarm features indicates that Maat Mons is the youngest volcanic centre within Atla Regio, fed by
14-514: The Magellan probe reveals no evidence of lava flows from these craters. At least two large-scale structural collapse events seem to have occurred in the past on Maat Mons. Maat Mons is surrounded by a radial dike swarm, with grabens extending over 1,500 kilometres from the volcano's centre. Intriguingly for planetary geologists , atmospheric studies carried out by the Pioneer Venus probes in
21-470: The Latin term valles , and are named after river goddesses or after words for the planet Venus (including terms for the morning star or evening star specifically) in various languages. Undae , dune fields, are named after desert goddesses. Tesserae are areas of polygonal terrain. They are named after goddesses in world mythologies. Scarps on Venus are called rupes and are named after goddesses of
28-576: The early 1980s revealed a considerable variation in the concentrations of sulfur dioxide (SO 2 ) and methane (CH 4 ) in Venus' middle and upper atmosphere. One possible explanation for this was the injection of volcanic gases into the atmosphere by plinian eruptions at Maat Mons. More recent studies have suggested that the volcano structure, distribution of lava flows, pit craters, summit morphology, and other small-scale features are indicative of recent volcanic activity on Maat Mons. A study published by
35-414: The journal Science in 2023 concluded that there has been recent volcanic activity on Maat Mons. The study analyzed images taken between 1990 and 1992 by the Magellan spacecraft. These images, taken eight months apart, displayed changes to the volcanic vent's shape and dramatically increased in size. The image also showed features that have been interpreted as lava flows. Atla Regio Venus ,
42-484: The same mantle plume which gave rise to the previous volcanic centres. Maat Mons has a large summit caldera , 28×31 km in size. Within the large caldera, there are at least five smaller collapse craters , up to 10 km in diameter. A chain of small craters 3–5 km in diameter extends some 40 km along the southeast flank of the volcano, but rather than indicating a large fissure eruption, they seem to also be formed by collapse. Full-resolution imagery from
49-534: The second planet from the Sun , is classified as a terrestrial planet . It is sometimes called Earth's "sister planet" due to their similar size, gravity, and bulk composition (Venus is both the closest planet to Earth and the planet closest in size to Earth). The surface of Venus is covered by a dense atmosphere and presents clear evidence of former violent volcanic activity. It has shield and composite volcanoes similar to those found on Earth. Cytherean valleys are called by
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