Mountains, get pushed up when two plates collide.
convergent
When two plates collide, it can form different geological features such as mountain ranges, deep-sea trenches, and volcanic arcs. The exact formations that occur depend on the type of collision, whether it's a convergent boundary where plates collide, or a transform boundary where plates slide past each other.
A mountain range forms when plates collide and one plate is pushed up over another. The collision causes intense compression, leading to the folding and uplifting of the Earth's crust to create mountainous regions. This process is known as continental collision or orogenesis.
When two continental plates collide, they can crumple and fold to form mountain ranges. This process is known as continental collision or orogenesis. The collision can also lead to seismic activity such as earthquakes and the formation of deep crustal roots.
Mountains are formed through the movement and collision of tectonic plates. When two plates collide, the land is pushed upward, forming mountain ranges. Over millions of years, erosion from forces like wind and water shape the mountains into their final forms.
earthquakes
collide into each other
A Convergence Boundary.
Mountains and grass
When tectonic plates collide they often form volcanoes or moutains. But when they slide past each other they create earthquakes...like in Haiti or Japan.
two plates collide and then their edges crumble like a paper
Usually either a mountain range, or a subduction zone.
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Yes. Tambora is located where the Indian-Australian plate and the Eurasian plate collide. When two plates collide, it forms a convergent boundary.
convergent
When two plates collide, it can form different geological features such as mountain ranges, deep-sea trenches, and volcanic arcs. The exact formations that occur depend on the type of collision, whether it's a convergent boundary where plates collide, or a transform boundary where plates slide past each other.
When two continental plates collide, they can form mountain ranges due to the intense compression and uplift of the Earth's crust. This collision can also lead to the formation of earthquakes as the plates grind against each other. Over time, the collision can result in the merging of the two continental plates into a single larger landmass.