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The global occurrence of alluvial fans on the martian surface suggests that Mars was once a wetter place, perhaps even well in to the sub-optimal climate of the Amazonian Period. In several cases, geomorphic studies of martian fans estimated local paleo-hydrologic conditions, making fans important for constraining paleo-climatic and -hydrologic conditions.

However, almost all of these estimates are based on conceptual models derived from terrestrial fans in hot and arid climates, often Wyandotte MI dating personals intense precipitation from thunderstorms. This differs from the current leading hypothesis that most martian fans sourced liquid water only from their upslope catchments, likely from snowmelt, and under cold and icy climatic conditions.

Here, we present initial field and remote sensing observations of a series of alluvial fans along the eastern Aklavik Range, Northwest Territories, Canada, to explore whether they have similar sedimentologic and geomorphic characteristics to martian fans. These terrestrial fans serve as a prime analog for fans in a cold and icy Mars scenario as they are mainly sourced by snowmelt in a continuous permafrost zone.

We qualitatively describe the sedimentary and periglacial processes on the Ladies want hot sex East Woodstock and combine remote sensing datasets e.

Similar to martian fans, the Aklavik fans are large in area compared to their catchments and have surface gradients that are shallower than most other terrestrial fans mean 3. Based on comparisons to terrestrial fans, some studies have suggested that the shallow gradients of martian fans are due to a dominance of fluvial transport.

Based on observations, the Aklavik fans are likely not fluvially controlled, but rather dominated by snowmelt-derived debris flows and gelifluction processes. This suggests that slope alone cannot be used to determine process and other morphometric properties e.

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Export Citation. Abstract The global occurrence of alluvial fans on the martian surface suggests that Mars was once a wetter place, perhaps even well in to the sub-optimal climate of the Amazonian Period. No Sources Found.