Rift valley of Iceland

 Rift valley of Iceland

This image is of a valley in Iceland that is part of the Thingvellir National Park - this valley is not formed by the erosion of a river but by the moving of tectonic plates away from each other - at this point two tectonic plates are separated from each other - on the right is the Eurasian plate which consists of Asia and Europe while on the left The North American plate is composed of the continent of North America - most of the boundary of these plates is at the bottom of the sea so usually not visible - but in Iceland this boundary passes right in the middle of the country

The Eurasian Plate is sliding to the right due to the movement of underground magma while the North American Plate is sliding to the left, which is also expanding the valley and increasing its depth - this type of valley is Rift valley. is done because such valleys are due to the rift of tectonic plates ie moving away from each other are formed. These plates are moving away from each other at the rate of about two centimeters per year. In Thingvellir National Park you can easily walk from one plate to another  

Where tectonic plates are moving towards each other, their collision begins to form mountain ranges and where they are moving away from each other, rift valleys begin to form - in Iceland, since tectonic plates are moving away from each other. Therefore, this valley is forming here - the union and the European plates in the northern regions of the subcontinent They are moving towards the other, so there is a plate sliding over the other, from which the Himalayan mountain ranges are getting higher and higher.

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