Dirty H2O

Despite the "Creative" name given to Dirty H2O (now nicknamed Snowball), it is a rather interesting due to the number of low velocity impacts detected by scans. Drity H2O originally resided in the outskirts of the system where everything during the formation was at its calmest, yet still rather chaotic if such conditions were recreated in the modern day. One example would be the Volt (named Volt not just as a tribute to Volta, but also due to the scientist being shocked by 1 volt of electricity upon scanning the 3d model and discovering this site)crater site, the celestial body that had crashed into it may have gone deep yet still remains somewhat intact. Volt isnt the only one, some of these crater types can be found littering the Equator which cements the fact that the outskirts (even during system formation) are the calmest region in the entire system. As for Dirty H2O, it has originally formed in this region with its core cooling at an early age (as subterranean oceans wouldve formed) despite it being associated with snow, it is covered in a 1km thick ice sheet which does protect a large snow layer beneath which we believe once couldve hosted an ocean during its cores short lifespan. It did suffer some impacts at a young age due to some larger ice crystals slingshoting others away or into something, it was then captured by Thatolon and temporarily had a planet spanning ocean due to it being in the habitable zone, which may open the opportunity for fossil excavations, however, it does lack most of the nessecary acids.