There are many theories about the formation of sinuous ridges on Mars. Some theories suggest these may be inverted streambeds, while others indicate they may be a glacial feature called an esker. Closer inspection of this feature may help scientists determine if this is an inverted stream bed or an esker.
ID:
ESP_082771_1735date: 23 March 2024
altitude: 268 km
https://uahirise.org/hipod/ESP_082771_1735
NASA/JPL-Caltech/UArizona
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