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Melas Dorsa reveals a complex geological history on Mars

Scientists have suggested that a fluidized ejecta pattern indicates the presence of subsurface ice that melted during an impact.
Melas-Dorsa
Melas Dorsa in full color. Credit: ESA/DLR/FU Berlin (G. Neukum)
The European Space Agency’s (ESA) Mars Express has imaged an area to the south of the famed Valles Marineris canyon on the Red Planet that shows a wide range of tectonic and impact features.

On April 17, the orbiter pointed its high-resolution stereo camera at the Melas Dorsa region of Mars. This area sits in the volcanic highlands of Mars between Sinai and Thaumasia Plana, 160 miles (250 kilometers) south of Melas Chasma. Melas Chasma itself is part of the Valles Marineris rift system.

The image captures wrinkle ridges, some unusual intersecting faults, and an elliptical crater surrounded by ejecta in the shape of a butterfly and with a strange “fluid-like” appearance.
Melas-Dorsa-impact-crater
Melas Dorsa impact crater perspective view. Credit: ESA/DLR/FU Berlin (G. Neukum)
Elliptical craters like this 10-mile-wide (16km) example are formed when asteroids or comets strike the surface of the planet at a shallow angle.

Scientists have suggested that a fluidized ejecta pattern indicates the presence of subsurface ice that melted during the impact. Subsequent impacts have created a number of smaller craters in the ejecta blanket.
zoomedcrater_Melas Dorsa
Zoom view of the flooded crater seen in the upper center part of the main image. Credit: ESA/DLR/FU Berlin (G. Neukum)
The rim of another large crater is visible in the upper center part of the image, but it appears mostly to have been almost buried during some distant epoch by volcanic dust and ash.

This makes any detailed study of it almost impossible. However, its center shows concentric deposits that could provide insights into the composition of the volcanic material that buried it.
Solis_MelasDorsa
Melas Dorsa topography. Credit: ESA/DLR/FU Berlin (G. Neukum)
Several wrinkle ridges can be seen across the image. These form when horizontal compression forces in the crust pushes the crust upwards.

To the left, the ridges are bisected by crustal displacement faults. These have cut into the ridges and the surrounding surface at some later epoch. This highlights the different tectonic phases responsible for the formation of this region.
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