This image shows striking features. A linear trough strikes northeast, then abruptly ends (or changes into a narrow ridge). Where the trough ends, a sinuous channel has an east-southeast strike, trending at almost a right angle to the trough. What happened to form these features?
We can speculate that first there was a southwest-to-northeast trending fracture or fault, perhaps associated with a volcanic vent. Groundwater (or some other runny fluid) coursed through the fault until overflowing and forming the sinuous channel. Continued movement through the fault carved a trough up to the overflow point.
Be sure to look at the stereo anaglyph through red-blue glasses.
ID:
ESP_086934_1775date: 11 February 2025
altitude: 257 km
https://uahirise.org/hipod/ESP_086934_1775
NASA/JPL-Caltech/University of Arizona
#Mars #science #NASA