To the North of the Indian subcontinent are the Himalayas. These mark the Convergent plate boundary between it and the Eurasian Plate.
The boundary between the Indian-Australian Plate and the Eurasian Plate is primarily a convergent boundary. This type of boundary is characterized by the collision of the two plates, which has resulted in significant geological activity, including the uplift of the Himalayas. The intense pressure and friction at this boundary can also lead to earthquakes.
Mount Stromboli is situated on a convergent plate boundary where the African Plate is subducting beneath the Eurasian Plate. This leads to the formation of magma beneath the surface, causing volcanic activity on the island.
Oceanic crust is usually destroyed by subduction. This occurs when one tectonic plate, typically consisting of denser oceanic crust, is forced beneath another plate, often continental crust. As the oceanic plate subducts into the mantle, it melts and is recycled, leading to geological phenomena such as volcanic activity and the formation of deep ocean trenches.
Mount Vesuvius is located on a convergent plate boundary where the African plate is subducting beneath the Eurasian plate. This type of boundary is associated with intense tectonic activity and is responsible for the volcanic eruptions in the region.
The Himalayan mountains were created by the collision of the Indian and Eurasian tectonic plates. The Indian plate collided with the Eurasian plate, causing the crust to buckle and fold, resulting in the formation of the towering Himalayan mountain range.
The tectonic plate under parts of Europe and Asia is a continental crustal plate.
a subduction boundry, this is where one plate gets pushed under the other. in this case the pacific plate is being pushed under the eurasion!
When two continental plates converge, they can create large mountain ranges due to the intense pressure and folding of the Earth's crust. This process is known as continental collision and can result in the formation of features like the Himalayas where the Indian plate collided with the Eurasian plate.
The Himalayan mountains are fold mountains, formed by the collision of tectonic plates. They are the result of the Indian plate pushing against the Eurasian plate, causing the Earth's crust to fold and uplift. The Himalayas are home to some of the highest peaks in the world, including Mount Everest.
The indo-australian plate is mostly a convergent boundary with the pacific plate.
To the North of the Indian subcontinent are the Himalayas. These mark the Convergent plate boundary between it and the Eurasian Plate.
The boundary between the Indian-Australian Plate and the Eurasian Plate is primarily a convergent boundary. This type of boundary is characterized by the collision of the two plates, which has resulted in significant geological activity, including the uplift of the Himalayas. The intense pressure and friction at this boundary can also lead to earthquakes.
They are formed by the continental contienal plates
The South American plate is a major tectonic plate that covers most of the continent of South America. It is primarily composed of continental crust.
Mount Stromboli is situated on a convergent plate boundary where the African Plate is subducting beneath the Eurasian Plate. This leads to the formation of magma beneath the surface, causing volcanic activity on the island.
When one plate sinks under the other, it is callled subduction, no matter what kind of plate it is. When two oceanic plates collide, they form trenches(i.e. the mariana trench). Hope this answers your question!!!