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  2. Olympus Mons - Wikipedia

    en.wikipedia.org/wiki/Olympus_Mons

    Olympus Mons is partially surrounded by a region of distinctive grooved or corrugated terrain known as the Olympus Mons aureole. The aureole consists of several large lobes. Northwest of the volcano, the aureole extends a distance of up to 750 km (470 mi) and is known as Lycus Sulci ( 24°36′N 219°00′E  /  24.600°N 219.000°E ...

  3. Tharsis - Wikipedia

    en.wikipedia.org/wiki/Tharsis

    Tharsis (/ ˈ θ ɑːr s ɪ s /) is a vast volcanic plateau centered near the equator in the western hemisphere of Mars. [note 1] The region is home to the largest volcanoes in the Solar System, including the three enormous shield volcanoes Arsia Mons, Pavonis Mons, and Ascraeus Mons, which are collectively known as the Tharsis Montes.

  4. Tharsis Montes - Wikipedia

    en.wikipedia.org/wiki/Tharsis_Montes

    Mons (plural montes) is the Latin word for mountain; it is a descriptor term used in astrogeology for mountainous features in the Solar System. The three Tharsis Montes volcanoes are enormous by terrestrial standards, ranging in diameter from 375 km (233 mi) (Pavonis Mons) to 475 km (295 mi) (Arsia Mons). [1]

  5. Amazonis quadrangle - Wikipedia

    en.wikipedia.org/wiki/Amazonis_quadrangle

    The central part contains Amazonis Planitia and the eastern part includes the western flank of the largest known volcano in the Solar System, Olympus Mons. The Amazonis quadrangle is one of a series of 30 quadrangle maps of Mars used by the United States Geological Survey (USGS) Astrogeology Research Program .

  6. Marsquake - Wikipedia

    en.wikipedia.org/wiki/Marsquake

    Illustration of the shadow zone of a P-wave for Earth. S-waves don't penetrate the outer core. A marsquake is a quake which, much like an earthquake, is a shaking of the surface or interior of the planet Mars.

  7. Noctis Labyrinthus - Wikipedia

    en.wikipedia.org/wiki/Noctis_Labyrinthus

    The shield volcano Pavonis Mons is at upper left. Mariner 9 view of the Noctis Labyrinthus "labyrinth" at the western end of Valles Marineris on Mars. Linear graben, grooves, and crater chains dominate this region, along with a number of flat-topped mesas. The image is roughly 400 km across, centered at 6 S, 105 W, at the edge of the Tharsis bulge.

  8. Volcanism on Mars - Wikipedia

    en.wikipedia.org/wiki/Volcanism_on_Mars

    However, the largest volcano on the planet, Olympus Mons, is thought to have formed when the plates were not moving. Olympus Mons may have formed just after the plate motion stopped. The mare-like plains on Mars are roughly 3 to 3.5 billion years old. [72] The giant shield volcanoes are younger, formed between 1 and 2 billion years ago.

  9. Ulysses Fossae - Wikipedia

    en.wikipedia.org/wiki/Ulysses_Fossae

    Tharsis contains many volcanoes, including Olympus Mons, the tallest known volcano in the Solar System. Notice Ceraunius Tholus , although it looks small, it is about as high as Earth's Mount Everest .