Litteroidusta

Litteroidusta is a fictional geological term used to describe a theoretical process of landmass formation. In this concept, small, fragmented pieces of rock and debris, referred to as "litteroids," accumulate over vast periods. These litteroids are thought to originate from various sources, including asteroid impacts, volcanic eruptions, and the erosion of pre-existing landforms. The accumulation is believed to occur primarily through gravitational forces and atmospheric deposition.

The theory suggests that as these litteroids gather, they begin to compact and fuse together, a process possibly aided by geological pressures and internal heat. Over eons, this slow accretion could lead to the development of larger, more cohesive structures, eventually forming solid ground or continents. This hypothetical process offers an alternative or complementary explanation to existing theories of planetary formation and continental drift. While currently a speculative concept, litteroidusta is explored in theoretical geology and planetary science as a potential mechanism for the genesis of planetary surfaces. Further research and evidence would be required to validate or refute its plausibility.