New views from ESA’s Mars Express reveal fascinating ice-related features in Mars’ Utopia region – home to the largest known impact basin not only on the Red Planet, but in the Solar System.
Utopia is one of three major basins in Mars’ northern hemisphere (along with Acidalia and Arcadia) and has a diameter of roughly 3 300 km: just under twice the north-south size of Earth’s Sahara Desert.
This image shows a slice of Utopia Planitia, the plain that fills this colossal and ancient basin.
This plain is thought to have formed as the Utopia basin was filled by a mix of sediments, lavas and volatile substances (those that vaporise easily, such as nitrogen, carbon dioxide, hydrogen and water), all transported across the martian surface by water, wind or other processes.
Utopia Planitia is an intriguing and ice-rich region; ice has been spotted lying both at and just below the surface, and at greater depths (detected via observations of fresh craters and pits, and by probing Mars’ deeper layers using radar).
Visible to the left and right of this scene are large, smooth patches of surface known as ‘mantled deposits’. These are thick layers of ice- and dust-rich material that have smoothed the surface and were likely deposited as snow back when Mars’ rotational axis was much more tilted than it is today (as was last the case some 10 million years ago).
Moving back towards image centre, the two largest impact craters visible here are surrounded by double-layered mounds of material. A similarly layered appearance is also visible in the deposits that have built up within the craters themselves, and in the craters’ thick rims.
These craters are more interesting still. The second-largest crater in this image (just below-left of centre) showcases a texture known as ‘brain terrain’, where material has become deformed and warped in a concentric pattern that resembles the complex patterns and ridges found on the surface of the human brain.
Brain terrain is associated with the icy material found near the boundary between Mars’ northern plains and its southern highlands, a ‘dichotomy’ located to the south/south-west (upper left) of this scene.
Just to the right of the brain-textured crater is an especially dark-coloured region, created as the ice-rich ground contracted and cracked at low temperatures. This formed polygonal patterns and fractures that subsequently captured dark dust blown across Mars by wind, leading to the dark appearance seen here.
Additionally, scalloped depressions are omnipresent throughout this image. These have circular to elliptical shapes, depths of several tens of metres, and sizes varying from tens to thousands of metres across.
These features are the result of ground ice either melting or turning to gas, which then causes the surface to weaken and collapse. Upon closer look, layered mantled deposits can also be seen in and around these scalloped depressions.
Mars Express has been orbiting the Red Planet since 2003, imaging Mars’ surface, mapping its minerals, identifying the composition and circulation of its tenuous atmosphere, probing beneath its crust, and exploring how various phenomena interact in the martian environment.
The mission’s High Resolution Stereo Camera (HRSC), responsible for these latest images, has revealed much about Mars’ diverse surface features, with recent image releases showing everything from wind-sculpted ridges and grooves to geologically rich regions filled with volcanoes, impact craters, tectonic faults, river channels and ancient lava pools. The camera has also captured other views of Utopia Planitia, such as a snapshot of Adamas Labyrinthus.
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