Stratovolcano
Explosive and oozy.
The eruption of Mount Merapi in 2010 was primarily caused by the subduction of the Indo-Australian Plate beneath the Eurasian Plate. This tectonic interaction generates significant volcanic activity in the region, as the subducted plate melts and contributes to magma formation. The resulting pressure and accumulation of magma ultimately led to the explosive eruption of Merapi.
The last major eruption of Mount Merapi in Indonesia began on May 11, 2018, with periodic eruptions continuing for several months.
there wasnt an eruption in 2008 if i sm not wrong.the most recent eruption in 2006.
It is because the volcano has too much pressure
It is an active volcanic mountain
Mount Merapi is a convergent boundary type, specifically a subduction zone where the Indo-Australian Plate is subducting beneath the Eurasian Plate. This subduction has led to the explosive volcanic activity and frequent eruptions characteristic of Mount Merapi.
The most destructive eruption of Mount Merapi in recent history occurred in 2010. It resulted in pyroclastic flows, ash clouds, and lahars, causing widespread devastation, loss of life, and displacement of communities.
the eruption that did it was a eruption
Mount Merapi as been in the news recently a lot due to the fact that the volcano erupted. On October 26st 2010 Indonesian volcano Mount Merapi began erupting. Since that day it has erupted three times and has thrown millions of tonnes of ash and debris high into the sky. More than 100 people have been killed as a result of the eruption and many more have been injured. 70.000 People in the near viscinity of Mount Merapi have been evacuated
Mount Merapi has erupted numerous times throughout history, leading to the deaths of thousands of people. The exact number of people killed by Mount Merapi varies depending on the specific eruption being referenced. In recent years, dozens of people have been killed by eruptions and associated hazards.
Mount Merapi is near a convergent plate boundary where the Indo-Australian Plate subducts beneath the Eurasian Plate.