Evander is a large multi-ring impact basin located in Dione's southern hemisphere. Evander is estimated to be relatively young; estimates range from 2 billion years down to as recently as under 1 billion years old. Surrounding Evander is an extensive ejecta blanket, and a significant portion of Dione's small (<20 km) craters may be the result of debris blasted out from the impact event that created Evander. Evander is a significantly relaxed crater, with its topographic profile having been "muted" since its formation and resulting in a shallower impact basin than would otherwise be expected. That Evander is relaxed indicates that Dione was thermally active until recently, with a surface heat flux of over 60 mW/m2.[2][3]
References
^ ab"Evander". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program. (Center Latitude: −57.00°, Center Longitude: 145.00°; Planetographic, +West)
^White, Oliver L.; Schenk, Paul M.; Bellagamba, Anthony W.; Grimm, Ashley M.; Dombard, Andrew J.; Bray, Veronica J. (May 2017). "Impact crater relaxation on Dione and Tethys and relation to past heat flow". Icarus. 288: 37–52. Bibcode:2017Icar..288...37W. doi:10.1016/j.icarus.2017.01.025.