Late Springtime Defrosting of Northern Dunes
This observation shows dunes in the Martian north polar sand sea (commonly referred to as the “north polar erg”) in the process of defrosting. Every winter, dunes and other surfaces at these northern latitudes are coated with several tens of centimeters of carbon dioxide frost and ice, plus a minor amount of water frost. The white material is fine grained frost.
The dark, splotchy tones on the dunes may be deposits of particulates deposited from carbon dioxide “geysers” or relatively thick deposits of carbon dioxide ice. The more brownish colors represent defrosted areas. Polygonal patterns on the surface of the dunes are probably cracks in overlying carbon dioxide ice. Landslides on the dunes’ lee slopes are apparent, with a morphology consistent with fluidization from carbon dioxide frost.