The Eurasian Plate is primarily moving eastward. Its motion is influenced by the dynamics of plate tectonics, as it interacts with several neighboring plates, including the North American Plate to the north, the Arabian Plate to the south, and the Indian Plate to the southeast.
This eastward movement is a result of the divergent boundaries it shares with the North American Plate, where new crust is formed as magma rises. Additionally, the interaction with the surrounding plates leads to various geological activities, such as earthquakes and mountain building, particularly along the edges of the Eurasian Plate.
In summary, the ongoing eastward movement of the Eurasian Plate plays a crucial role in shaping the geological landscape of not just Eurasia, but also contributes to the tectonic activity in adjacent regions.