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“Recent discoveries by planetary geoscientists at Brown and elsewhere have shown that the climate of Mars has varied in the past,” Head noted. “During these times, ice from the polar caps is redistributed into the mid-latitudes of Mars as a layer about 50 meters thick, in the same place that we see that the DLEs have formed. This made us think that this ice layer could be part of the explanation for the formation of the unusual DLE second layer.”