The objective of this observation is to examine a straight ridge that might be a dike. Sometimes magma (molten rock) below the surface may fill an existing fracture, even pushing the fracture open in the process. As the magma cools, it solidifies into a tabular rock mass, and that resulting cooled volcanic rock is called a dike.

ID: ESP_065300_2100
date: 1 July 2020
altitude: 288 km

https://uahirise.org/hipod/ESP_065300_2100
NASA/JPL-Caltech/UArizona
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