Eurasian Plate

It also includes oceanic crust extending westward to the Mid-Atlantic Ridge and northward to the Gakkel Ridge.

Eurasian Plate
Eurasian Plate
Type	Major
Approximate area	67,800,000 km2 (26,200,000 sq mi)
Movement1	south
Speed1	7–14 mm (0.28–0.55 in)/year
Features	Europe (including part of Iceland), Asia, Atlantic Ocean, Arctic Ocean
1Relative to the African Plate

The western edge is a triple junction plate boundary with the North American Plate and Nubian Plate at the seismically active Azores Triple Junction extending northward along the Mid-Atlantic Ridge towards Iceland. Ridges like the Mid-Atlantic ridge form at a divergent plate boundary. They are located deep underwater and very difficult to study. Scientists know less about ocean ridges than the do the planets of the solar system.

There is another triple junction where the Eurasian Plate meets the Anatolian Sub-Plate and the Arabian Plate. The Anatolian Sub-Plate is currently being squeezed by the collision of the Eurasian Plate with the Arabian Plate in the East Anatolian Fault Zone.

The boundary between the North American Plate and the Eurasian Plate in the area around Japan has been described as "shifty". There are different maps for it based on recent tectonics, seismicity and earthquake focal mechanism. The simplest plate geometry draws the boundary from the Nansen ridge through a broad zone of deformation in North Asia to the Sea of Okhotsk then south through Sakhalin Island and Hokkaido to the triple junction in the Japan Trench. But this simple view has been successfully challenged by more recent research. During the 1970s, Japan was thought to be located on the Eurasian Plate at a quadruple junction with the North American Plate when the eastern boundary of the North American Plate was drawn through southern Hokkaido. New research in the 1990s supported that the Okhotsk microplate was independent from the North American Plate and a boundary with the Amurian microplate, sometimes described as "a division within the Eurasian plate"^{[additional citation(s) needed]} with an unknown western boundary.

All volcanic eruptions in Iceland, such as the 1973 eruption of Eldfell, the 1783 eruption of Laki and the 2010 eruption of Eyjafjallajökull, are caused by the North American and the Eurasian plates moving apart, which is a result of divergent plate boundary forces.

The convergent boundary between the Eurasian Plate and the Indian Plate formed the Himalayas mountain range. The geodynamics of Central Asia is dominated by the interaction between the Eurasian Plate and the Indian Plate. In this area, many sub-plates or crust blocks have been recognized, which form the Central Asian and the East Asian transit zones.

 

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