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Hadley Crater provides deep insight into martian geology

The Mars Express images show that Hadley Crater was struck multiple times by large asteroids and/or comets after its initial formation and subsequent infilling with lava and sediments.
Hadley-Crater_1
Hadley Crater // Credit: ESA/DLR/FU Berlin (G. Neukum)
Recently engaged in providing support to the successful landing of NASA’s Mars Science Laboratory's Curiosity rover, the European Space Agency’s (ESA) Mars Express has now returned to its primary mission of studying the diverse geology and atmosphere of the Red Planet from orbit.

Earlier this year, the spacecraft observed the 75-mile-wide (120 kilometers) Hadley Crater, providing a tantalizing insight into the martian crust. The images show multiple subsequent impacts within the main crater wall, reaching depths of up to 8,500 feet (2,600 meters) below the surrounding surface.
Hadley-Crater-perspective-view_2
Hadley Crater perspective view // Credit: ESA/DLR/FU Berlin (G. Neukum)
This region imaged April 9, 2012, by the High Resolution Stereo Camera on Mars Express shows the crater that lies to the west of Al-Qahira Vallis in the transition zone between the old southern highlands and the younger northern lowlands.

Hadley is named after the British lawyer and meteorologist George Hadley (1685–1768) whose name was also given to the “Hadley cell,” a circulation system in Earth’s atmosphere that transports heat and moisture from the tropics up to higher latitudes.
Hadley-Crater-in-context_3
Hadley Crater in broader context. The smaller rectangle shows the region covered in this ESA Mars Express HRSC image release. Hadley Crater is west of the Al-Qahira Vallis in the transition zone between the old, southern highlands and the younger northern lowlands. // Credit: NASA MGS MOLA Science Team
The images show that Hadley Crater was struck multiple times by large asteroids and/or comets after its initial formation and subsequent infilling with lava and sediments.

Some of these later impacts have also been partly buried, with subtle hints of a number of crater rims to the west (top) and wrinkle ridges to the north (right side) of the main crater floor as shown in the first image at the top of the page.
Hadley-Crater-perspective-view_4
Hadley Crater perspective view // Credit: ESA/DLR/FU Berlin (G. Neukum)
Again, in the first image (top of the page), the southern (left) side, the crater appears shallower than the opposite side. This difference can be explained by an erosion process known as mass wasting. This is where surface material moves down a slope under the force of gravity.

Mass wasting can be initially started by a range of processes including earthquakes, erosion at the base of the slope, ice splitting the rocks, or water being introduced into the slope material. In this case, there is no clear indication which process caused it or over what timescales this may have occurred.
Topographical-view-of-Hadley-Crater_5
Topographical view of Hadley crater // Credit: ESA/DLR/FU Berlin (G. Neukum)
Of particular interest to scientists studying the geology of Mars are the ejecta of the smaller craters within Hadley. Two of them, one to the west (top) and the deepest one in the middle of the first image, show evidence for volatiles, possibly water ice beneath the surface. With the impact that forms the craters, this ice would mix with surrounding materials to form a kind of “mud,” which would then spread over the surface as ejecta.

Scientists believe these volatiles, which were excavated by the impacts, may indicate the presence of ice to a depth of around hundreds of feet — this being the difference in depth between the surface and the depths of the two craters.
3D-anaglyph-of-Hadley-Crater_6
3D anaglyph view of Hadley crater // Credit: ESA/DLR/FU Berlin (G. Neukum)
This deep view into the martian crust within the walls of Hadley Crater provides scientists an insight into the history of Mars — a history that rovers like those currently on the Red Planet and others that will follow will doubtlessly continue to investigate.

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