The London Basin is capable of drifting east-west, contrary to assumptions that it may only move north-south. This capability is linked to its geological structure, particularly its classification as an early aulacogen, which suggests it is a weak zone for tectonic stress. The regional stress field influenced by the African plate's northward movement and rotational dynamics of Iberia and Western Europe plays a significant role in this drift. Additionally, the London Basin is not affected by Wilson Cycle subduction zones, as such processes occur over geological timescales that are too slow to impact the basin in the near future. Overall, the average behavior of Earth's crustal plates indicates that while individual regions like the London Basin can drift, the broader tectonic framework remains stable.