Another of Kubindi's three moons, Kubindi A is thought to have formed in a similar manner as Kubindi B. It is likely that some of the material from a planetary impact formed Kubindi A, while the remnants formed Kubindi B. Like Kubindi B, this moon is lacking in many of the heavier elements such as iron, which is thought to have been reabsorbed by Kubindi after the impact which ejected the material that formed the two principal moons. Kubindi A has also suffered a major impact at some point in the past, as seen by the large crater visible from space. This particular impact might have been large enough for an extinction-level event, had it struck Kubindi instead of the moon. Like Kubindi B, Kubindi A was a mining site in the early history of Kubaz space travel. Kubindi A was mined primarily for its Helium-3 isotopes which helped provide fuel for the early fusion engines used by Kubaz explorers.