These channel and lobe deposits might represent fluvial (liquid) structures from the Noachian period on Mars, a time of heavy asteroid impacts and possible surface water about 4 billion years ago. The layers are also of interest to study.
ID:
ESP_060265_2170date: 5 June 2019
altitude: 297 km
https://uahirise.org/hipod/ESP_060265_2170
NASA/JPL-Caltech/University of Arizona
#Mars #science #NASA