ESA has captured the cratered, fissured face of the second-highest volcano on Mars. details here

The European Space Agency (ESA) has captured the cratered, fissured flank of Escarius Mons, the second highest volcano on Mars. The report also claimed that the height of Ascraeus Mons is twice the height of Mount Everest, the tallest mountain on Earth.

Ascraeus Mons is the northernmost and highest of the three major volcanoes found in the Tharsis region of Mars. The Tharsis region of the planet is a volcanic plateau in the western hemisphere of Mars.

Ascraeus Mons measures 18 km in height and has a base diameter of 480 km, giving it a footprint on Earth the size of Romania. With this height, it shows that Ascraeus is higher than the height of Mons. mount everest Whose height is 8,848.86 meters above sea level as of March 2020.

Ascraeus Mons is only surpassed in height by Olympus Mons as the tallest volcano not only on Mars but in the entire Solar System, ESA states.

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This image shows the region around the Martian volcanoes Ascraeus Mons, Pavonis Mons and Arsia Mons. The area outlined by the large white box indicates the region imaged by ESA’s Mars Express High Resolution Stereo Camera during orbit 24045 on 15 January 2023. The small inset white box shows the special region highlighted by the new images from Mars Express. (Image: NASA/MGS/MOLA Science Team)

According to ESA, there is a dramatic difference in altitude from one side to the other, with the left (southern) part of the frame sitting about 10 km lower than the right (northern) side.

Deep, irregular cracks in the surface of Mars can be seen moving towards the camera.  (Image: NASA/MGS/MOLA Science Team)

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Deep, irregular cracks in the surface of Mars can be seen moving towards the camera. (Image: NASA/MGS/MOLA Science Team)
This annotated image from ESA's Mars Express shows the southern flanks of Escarius Mons, the second-highest volcano on Mars.

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This annotated image from ESA’s Mars Express shows the southern flanks of Escarius Mons, the second-highest volcano on Mars.

In addition, there are several wrinkly lava flows on the right side of the frame. According to the ESA, this compacted plain then encounters chains of ‘pit craters’, where strings of circular or near-circular sediments coalesce and coalesce to form troughs.

The ESA further states that ‘sinusoidal reels’, which are small, meandering channels without a rim that are often found near the edges of volcanoes, are present on the ground to the left of crater chains. Their formation is still unclear but may include lava, ash or water or a combination of all three.

Meanwhile, Mars Express has been orbiting the Red Planet since 2003, imaging the surface of Mars, mapping its minerals, identifying the composition and circulation of its tenuous atmosphere, probing beneath its crust is doing, and finding out how different phenomena interact in the Martian atmosphere.

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