The floor of Ezinu is home to a series of fractures, which are up to 200 metres deep and stretch for 22.7 km.[2] These fractures were theorised in a 2018 study to have been formed as a result of subsurface low-viscosity material flowing into the crater.[2]
References
^ ab"Ezinu". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program. Retrieved 11 February 2019.