Krinomak is a titan planet of considerable size with a thin atmosphere. Its surface is littered with basins of liquid hydrocarbons, mainly ethane and methane. The biggest of these basins, which spans a lenght of over 6000 km, can be found near the equator. Its size is rivalled by a gigantic impact crater filled with methane located on the opposite side of the planet. Four other craters are found across the surface, their diameter ranging from 700 km to 3000 km. These planetary scars are remnants of the dramatic ancient past of this celestial body. Another consequence of these cataclysmic events was the formation of Krinomak's atmosphere. It is composed mainly of nitrogen with barely measurable traces of argon and carbon monoxide. This atmosphere was created when ammonia deposits in the cru
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