It is in the centre of Costa Rica, in a mountain range known as the Cordillera Central. It is also in the Irazú Volcano National Park. Cartago is the nearest city.
No, Irazu is not a divergent boundary. Irazu is a volcano located in Costa Rica, and it is associated with the subduction boundary where the Cocos Plate is being pushed below the Caribbean Plate.
Although is known that the Pico de Orizaba had eruptions before the arrival of Spanish Conquistadores in 1521, the Aztec scrolls that detailed on specific dates have been lost. Volcanic activity on such volcano was last recorded on 1687 and ever since it has been dormant.
big eruption
It is an explosive eruption technically a strombolian eruption
Irazú Volcano was formed through a series of eruptions that deposited layers of lava, ash, and other volcanic materials over millions of years. It is a stratovolcano, characterized by its steep sides and cone shape, and it is part of the Central Volcanic Conservation Area in Costa Rica. The last major eruption occurred in the 1960s, shaping the landscape we see today.
No, Irazu is not a divergent boundary. Irazu is a volcano located in Costa Rica, and it is associated with the subduction boundary where the Cocos Plate is being pushed below the Caribbean Plate.
Although is known that the Pico de Orizaba had eruptions before the arrival of Spanish Conquistadores in 1521, the Aztec scrolls that detailed on specific dates have been lost. Volcanic activity on such volcano was last recorded on 1687 and ever since it has been dormant.
the eruption that did it was a eruption
to old
11,260 feet
YES!
The toba eruption was ultra plinian.
The type of eruption that a composite volcano has is lava flow with cinders and bombs in an explosive eruption
big eruption
Volcanic eruption can be classified mainly based on the name of the volcano. They are Surtseyan eruption, Plinian eruption, Vulcanian eruption, Strombolian eruption and Hawaiian eruption.
It had an eruption like explosive diarrhea.
it has a stombolian eruption