HiPOD: Jamming with the “Spiders” from Mars

But these aren’t actual spiders. We call it “araneiform terrain,” to describe the spider-like radiating channels that form when carbon dioxide ice below the surface heats up and releases. This is an active seasonal process we don’t see on Earth. Like dry ice on Earth, the carbon dioxide ice on Mars sublimates as it warms (changes from solid to gas) and the gas becomes trapped below the surface.

https://uahirise.org/hipod/ESP_055283_0985
NASA/JPL-Caltech/UArizona