No, the two plates along the coast of South America are not a divergent boundary; they are part of a convergent boundary. The Nazca Plate is subducting beneath the South American Plate, which leads to significant geological activity, including the formation of the Andes Mountains and frequent earthquakes. Divergent boundaries, in contrast, occur where tectonic plates move apart.
divergent boundary
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust. A classic example is the Mid-Atlantic Ridge where the Eurasian and African Plates are moving away from the North and South American Plates.
It is a convergent boundary The subduction of the pacific plate underneath the west coast of South America creates the uplift and volcanoes that is still producing the Andean mountain range. A divergent boundary would create a mid-ocean ridge, or somthing akin to the great rift valley in Africa.
Plates move apart along divergent boundaries where new oceanic crust is created as magma rises and solidifies between two plates. This process is known as seafloor spreading and occurs primarily along mid-ocean ridges.
It is divergent between the North American and Eurasian plates. Volcanoes and earthquakes do occur along the boundary.
The mid-ocean ridge is formed along a divergent or constructive plate boundary between two plates of oceanic crust.
Hekla volcano is located along a divergent plate boundary in Iceland, where the North American and Eurasian plates are moving apart. This movement creates rift zones where volcanic activity is common, including Hekla.
a rift valley forms along the divergent boundary
The mid-Atlantic ridge is a divergent boundary where tectonic plates are moving apart. It is an example of a constructive plate boundary where new oceanic crust is formed through volcanic activity. This process leads to the continuous separation of the North American and Eurasian plates on one side and the South American and African plates on the other side.
It is a convergent boundary The subduction of the pacific plate underneath the west coast of South America creates the uplift and volcanoes that is still producing the Andean mountain range. A divergent boundary would create a mid-ocean ridge, or somthing akin to the great rift valley in Africa.
A divergent boundary created the mid-ocean ridge. At this boundary, tectonic plates are moving away from each other, allowing magma to rise and create new oceanic crust along the ridge.
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