The 2004 Northern Sumatra earthquake occurred at a convergent plate boundary, where the Indo-Australian Plate is subducting beneath the Eurasian Plate. This tectonic interaction is responsible for significant seismic activity in the region, contributing to the generation of large earthquakes and tsunamis. The earthquake, registering a magnitude of 9.1-9.3, was one of the largest ever recorded, triggering a devastating tsunami that affected multiple countries around the Indian ocean.
The 2004 Sumatra earthquake occurred on the interface between the Indian Plate and the Burma Plate along a subduction zone. This subduction zone is known as the Sunda Megathrust and is located off the west coast of Sumatra, Indonesia.
The 2004 tsunami was on a convergent boundary where the Indian Plate was subducted beneath the Burma Plate, displacing a massive amount of water and triggering the devastating tsunami in the Indian Ocean.
The 2004 Boxing Day tsunami was caused by a megathrust earthquake, which occurred along a convergent plate boundary. Specifically, it happened where the Indian Plate subducted beneath the Burma Plate, releasing large amounts of energy that triggered the devastating tsunami.
The 2004 earthquake in northern Sumatra, Indonesia was caused by a megathrust subduction zone fault between the Indian Plate and the Burma Plate. This type of fault is known as a subduction zone fault, where one tectonic plate is forced beneath another.
The tsunami of Sumatra happened on December 14, 2004.
It occured in the Indian Ocean (the epicentre was just off the northern tip of the island of Sumatra) on the plate boundary where the Indo-Australian Plate is subducted under the Eurasian plate.
The 2004 Sumatra earthquake occurred on the interface between the Indian Plate and the Burma Plate along a subduction zone. This subduction zone is known as the Sunda Megathrust and is located off the west coast of Sumatra, Indonesia.
The December 26, 2004 tsunami occurred at a plate boundary, a few miles off the coast of Sumatra, Indonesia. A natural sensation called 'subduction' occurred. That is when a plate slides over or under another plate. There was an earthquake and also a displaced water mass trying to regain it's equilibrium position. Shockwaves were sent in all directions.
The 2004 tsunami was on a convergent boundary where the Indian Plate was subducted beneath the Burma Plate, displacing a massive amount of water and triggering the devastating tsunami in the Indian Ocean.
The 2004 Boxing Day tsunami was caused by a megathrust earthquake, which occurred along a convergent plate boundary. Specifically, it happened where the Indian Plate subducted beneath the Burma Plate, releasing large amounts of energy that triggered the devastating tsunami.
Subduction zone plate boundaries are responsible for the most powerful earthquakes because of the immense pressure and stress that builds up as one tectonic plate is forced beneath another. These earthquakes can reach very high magnitudes, such as the 2004 Sumatra-Andaman earthquake which had a magnitude of 9.1-9.3.
The 2004 earthquake in northern Sumatra, Indonesia was caused by a megathrust subduction zone fault between the Indian Plate and the Burma Plate. This type of fault is known as a subduction zone fault, where one tectonic plate is forced beneath another.
Operation Sumatra Assist happened in 2004.
The tsunami of Sumatra happened on December 14, 2004.
The earthquake in 2004 started on the west coast of Sumatra, Indonesia.
tsunami
Sumatra.