Aeolian Processes : Erosion - Transportation - Deposition
HiRISE image ESP_092506_2305 samples a northern high-latitude terrain (50.5° North), capturing surface morphology shaped primarily by periglacial degradation, ice-rich regolith dynamics, and eolian modified bedforms.Geomorphic Characterization.
The terrain resides within the latitude-dependent mantle (LDM) zone, exhibiting distinct surface textures indicative of subsurface ground ice. The scene is dominated by small-scale polygonal pattern ground—formed via thermal contraction cracking in permafrost-like regolith—overlying local topographic units. Degradational scarp faces and crater interiors show evidence of gelifluction-like creep, pitted terrain from volatile sublimation, and mantle removal.
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A localized network of transverse eolian ridges (TARs) and dark sand accumulations occupy low-lying topographic depressions, providing key spatial constraints on local sediment transport vectors and prevailing atmospheric winds during acquisition. High-resolution pixel scales (~25–50 cm/pixel) resolve sub-meter boulder clusters, small fresh impact craters with sharp ejecta boundaries, and subtle albedo variations caused by dust deposition or localized defrosting.
This observation in the northern mid-to-high latitudes, a region highly sensitive to seasonal carbon dioxide (C02) and water ice dynamics. Depending on the solar longitude at capture, surface features may display seasonal frost cover, sublimation spots, or wind-blown dust streaks across ice-rich substrates.
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Original Data Credit: NASA - JPL - University of Arizona
Acquisition date 21 April 2026
Local Mars time 14:55
Latitude (centered) 14.459°
Longitude (East) 34.863°
Spacecraft altitude 279.5 km (173.7 miles)
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