User:Al89762537/Iceland Plateau

The Iceland Plateau or Icelandic Plateau is an oceanic plateau in the North Atlantic Ocean consisting of Iceland and its contiguous shelf and marginal slopes. It is formed by interaction of the divergence of North American Plate and Eurasian Plate tectonic plates and the hot spot located below.

Location and Characteristics
The Iceland Plateau is bounded on the south by the Reykjanes Ridge, on the west by the Greenland-Iceland Ridge, on the north by the Kolbeinsey Ridge and on the east by the Iceland-Faeroe Ridge. It consists of a large igneous province that has been volcanically active since at least the Miocene epoch. The plateau has an average elevation of 1,700 meters above sea level.

Tectonics and Geology
The plateau is an example of ridge-hotspot interaction. The landscape is constantly experiencing deformation due to the continual addition of magma to the surface and the shifting of the ocean ridge. The plateau resides above a hot spot on an active rift zone of the Mid-Atlantic Ridge from which extensive tholeiitic plateau basalts and a number of large rhyolitic domes have been extruded.

The Icelandic Plateau began forming approximately 56 Ma, due to the opening of the North Atlantic. As the plates began to diverge from each other, piles of lava rose to the surface from the hot spot, creating the ridges present on the landscape currently. Today, there are two main parts of the island, one which is slanted towards the sea floor, and another at a level surface.

The geology of the Icelandic Plateau consists of three layers, closely mimicking the structure of oceanic crust but with one key difference, the second layer of the oceanic crust does not contain piles of Laval flow like the Icelandic Plateau does. The first layer is composed of mainly sedimentary rock, the second layer is piles of lava flows, and the third layer is a thick layer of gabbro.