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.
Volcanoes are more common along convergent boundaries where two tectonic plates collide, causing subduction and the melting of rock. Divergent boundaries also have volcanoes, but they are typically less explosive and occur as a result of magma rising to fill the gap created by the moving plates.
divergent, transform and convergent
Terrane accretion typically occurs along a convergent boundary where two tectonic plates collide, rather than along a divergent boundary where they move apart. This process involves the collision and subsequent attachment of different crustal blocks or terranes to a continental margin or another terrane.
Constructive or divergent. The ridge formed is of basaltic rock type (though this is a generalisation), and is a source of volcanic activity. Iceland was formed as a result of the sea-floor spreading.
The three types of plate boundaries are divergent, convergent, and transform boundaries. At divergent boundaries, plates move away from each other, creating new crust. Convergent boundaries involve plates colliding, leading to the formation of mountain ranges or subduction zones. Transform boundaries involve plates sliding past each other horizontally.
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.
No, rift valleys form along divergent boundaries, where tectonic plates move away from each other. Convergent boundaries are where plates collide, leading to the formation of features like mountains and deep ocean trenches.
a rift valley forms along the divergent boundary
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.
The North American plate is mainly a convergent plate boundary, where it collides with other plates like the Pacific Plate and the Caribbean Plate. However, there are also small areas along its boundaries that exhibit transform fault boundaries, such as the San Andreas Fault in California.
Volcanoes are more common along convergent boundaries where two tectonic plates collide, causing subduction and the melting of rock. Divergent boundaries also have volcanoes, but they are typically less explosive and occur as a result of magma rising to fill the gap created by the moving plates.
Popocatepetl is situated along a convergent plate boundary where the Cocos Plate is subducting beneath the North American Plate.
A reverse fault is usually associated with convergent plate boundaries, where two plates are colliding and one is forced upward over the other. It is less common along divergent boundaries, where plates are moving away from each other.
divergent, transform and convergent
No, new crust is not created at a convergent boundary. Instead, at convergent boundaries, two tectonic plates come together and one plate is usually forced beneath the other in a process called subduction. This process can lead to the destruction of crust rather than the creation of new crust.
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.