Eyjafjallajokull volcano is located on the divergent boundary between the North American Plate and the Eurasian Plate in Iceland.
Yes. It is believed to have erupted in 2010 twice because of the constructive margin. The plates were pulled apart by convection currents then because of this basalt lava seeps in to form a new crust beneath the sea and existing volcano. Much of the magma was intruded as dolerite dykes (thin sheets of igneous rock.) New lava and dykes then added extra crust at each side of the spreading ridge.
Yes. It is believed to have erupted in 2010 twice because of the constructive margin. The plates were pulled apart by convection currents then because of this basalt lava seeps in to form a new crust beneath the sea and existing volcano. Much of the magma was intruded as dolerite dykes (thin sheets of igneous rock.) New lava and dykes then added extra crust at each side of the spreading ridge.
Yes. Eyjafjallajokull is located in Iceland and is situated on or very near the Mid-Atlantic-Ridge which is a divergent plate boundary.
Eyjafjallajokull is located in Iceland on the Mid-Atlantic-Ridge which separates the North American and Eurasian plates.
Krakatoa is located on a destructive plate margin where the Indo-Australian plate subducts beneath the Eurasian plate. This subduction zone has led to the formation of volcanic islands in the region, including Krakatoa.
A constructive plate margin or spreading centre known as the Mid-Atlantic-Ridge.
Niether. Kilauea is in the middle of the Pacific plate, thousands of miles from the nearest plate boundary. The volcanic activty is due to a hot spot.
Eyjafjallajokull volcano is located on the divergent boundary between the North American Plate and the Eurasian Plate in Iceland.
Yes. It is believed to have erupted in 2010 twice because of the constructive margin. The plates were pulled apart by convection currents then because of this basalt lava seeps in to form a new crust beneath the sea and existing volcano. Much of the magma was intruded as dolerite dykes (thin sheets of igneous rock.) New lava and dykes then added extra crust at each side of the spreading ridge.
Yes. It is believed to have erupted in 2010 twice because of the constructive margin. The plates were pulled apart by convection currents then because of this basalt lava seeps in to form a new crust beneath the sea and existing volcano. Much of the magma was intruded as dolerite dykes (thin sheets of igneous rock.) New lava and dykes then added extra crust at each side of the spreading ridge.
Yes. Eyjafjallajokull is located in Iceland and is situated on or very near the Mid-Atlantic-Ridge which is a divergent plate boundary.
Japan sits on top of a destructive plate margin.
Eyjafjallajokull is located in Iceland on the Mid-Atlantic-Ridge which separates the North American and Eurasian plates.
Mount Etna is located on a destructive plate boundary, where the African Plate is being subducted beneath the Eurasian Plate. The melting of the subducted plate generates magma that rises to the surface, leading to volcanic activity at Mount Etna.
No,plate margin&plate boundary are not same.plate boundaries are definite regions where tectonic occurs,while margins are surface lines.
The Himalayas were formed at a convergent plate margin where the Indian Plate collided with the Eurasian Plate. This collision resulted in the uplift of the Himalayan mountain range.