Klendagon

Description
Klendagon is an arid terrestrial, slightly larger than Earth, but with a lower density that reflects its relative lack of heavier elements. The crust is composed of tid and aluminum, with wide deserts of dust-fine sand thar are easily stirred by the wind.

Klendagon's most striking feature is, of course, the Great Rift valley that stretches across the southern hemisphere. What is most fascinating about the Rift is that it does not appear to be natural. The geological record suggests it is the result of a "glancing blow" by a mass accelerator round of unimaginable desctructive power. This occurred some thirty-seven million years ago.