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This is how Weiss and Head think the DLEs formed: the impact into the Martian surface tears through the ice layer, breaking apart rock and other ejecta out onto the encircling ice. However, the ejected material is positioned on slippery ice and, thus, not all of the material stays in the same place. According to the researchers, the layering takes place when material near the top of an elevated crater rim moves down the slick ice and floods over material on the lower slopes. That earthfall forms the the DLEs’ two-layered appearance.
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