The Somali plate is separating from Nubia in an eastward direction at the East African Rift Valley, where rifting is occurring at approximately 6 mm/yr (McClusky et al., 2003). As the Indian plate is moving northward relative to the Eurasian plate and collides with it, a convergent boundary is created. African Plate Boundaries. What type of plate boundary is the African and Eurasian plate? The type of plate boundary that is creating Mount Vesuvius is the African Plate and the Eurasian Plate Tectonic plates float on top of the hot liquid magma of the Earth's mantle like chunks of ice on a lake. The westerly side is a divergent boundary with the North American Plate forming the northernmost part of the Mid-Atlantic Ridge , which is straddled by Iceland. The Arabian Plate consists mostly of the Arabian Peninsula; it extends westward at the Sinai Peninsula and the Red Sea and northward to the Levant. Borders.

The African plate is a large tectonic plate, one of the many that cover the surface of the Earth. These lofty mountains marked the culmination of the great uplift that occurred during the late Cenozoic when the Indian Plate drove many hundreds of kilometres into the underbelly of Asia. The plate borders are: East, with the Indian Plate, at the Owen Fracture Zone.

The Eurasian Plate is a plate tectonic boundary consisting most of Europe, Russia and China. The Arabian plate separated from Africa approximately 25 million years ago, resulting in the closure of the subducting Tethys sea in the northeast (Johnson and Stern, 2010). The Adriatic plate, also known as the Apulian plate, is situated in the deformation zone at the boundary between the Eurasian and the African plates.

Because Earth’s tectonic plate boundaries often consist of continent and ocean crust , the Eurasian Plate contains parts of the Atlantic and Arctic Ocean.

The African plate has two of these types of plate boundaries around its border. The rifting of Africa and Arabia opened the Red Sea as well as the Gulf of Aden, bordering the plate on the southwest and southern sides respectively (see figure 1). On the opposite side, the Indo-African boundary is divergent. Tectonic plates float on top of the hot liquid magma of the Earth's mantle like chunks of ice on a lake.

The Arabian plate (Figure 4) is moving away from Nubia in a northwest direction in the Red Sea at a rate varying along the strike of the rift between 14 mm/yr and 5.6 mm/yr (McClusky et al., 2003).

The Somali plate is separating from Nubia in an eastward direction at the East African Rift Valley, where rifting is occurring at approximately 6 mm/yr (McClusky et al., 2003).

The southerly side is a boundary with the African Plate to the west, the Arabian Plate in the middle and the Indo-Australian Plate to the east. Subduction zones are convergent boundaries, and where they collide, one plate dives below the other. Eurasian, Anatolian and Arabian (purple coloring) plates. The African plate has two of these types of plate boundaries around its border. The African plate is a large tectonic plate, one of the many that cover the surface of the Earth. It’s the third largest, being slightly smaller than the Pacific Plate and North American Plate. This microplate is bordered by an orogenic belt, the peri-Adriatic mountain chain that runs through Italy and Greece, in the region surrounding the Adriatic Sea (Channell and Horváth, 1976). The northern part of the plate is a convergent boundary where the African plate is subducting below the Eurasian plate. Subduction zones are convergent boundaries, and where they collide, one plate dives below the other.