New continental crust is formed at divergent plate boundaries, where tectonic plates move away from each other. As the plates separate, magma from the mantle rises and solidifies to form new crust. This process is known as seafloor spreading and creates new oceanic crust, which can eventually be uplifted and become part of a continent.
It depends on the type of crust involved. If both plates carry oceanic crust, an ocean trench is formed along with a volcanic island are on the overriding plate. If one plate carries oceanic crust and the other continental, you will get an ocean trench, a continental volcanic arc, and a mountain range. If both plates carry continental crust, then a mountain range is formed.
Convergent boundaries are classified according to the type of tectonic plates involved. There are three main types of convergent boundaries: oceanic-continental, oceanic-oceanic, and continental-continental. The classification is based on whether the plates involved are oceanic or continental and the resulting geological features that are formed.
Mountain ranges are formed when two continental plates collide. When they converge one plate will be forced slightly under the other one.
The Eurasian Plate formed through the movement of tectonic plates around the Earth's surface, leading to the collision of several smaller plates that eventually coalesced to form the Eurasian Plate. This process primarily occurred through the subduction and convergence of oceanic plates with continental plates, resulting in the formation of the Eurasian Plate over millions of years.
Continental plates are formed through a process called plate tectonics, where molten rock rises from the Earth's mantle and solidifies to create new crust. These plates can eventually be destroyed through subduction, where one plate is forced beneath another at a convergent boundary. The subducted plate melts back into the mantle, completing the cycle of plate formation and destruction.
When two continental plates collide,fold mountains are formed.
rift valley Answer 2 Continents are formed when continental plates pull apart.
Deep-ocean trenches are formed where seafloor tectonic plates subduct under continental plates.
When two continental plates diverge, a rift valley is formed as the Earth's crust splits apart. Magma rises to the surface and creates new crust, eventually leading to the formation of a mid-ocean ridge.
fold mountains
In theory, tectonic plates. http://www.ucmp.berkeley.edu/geology/tectonics.html
New continental crust is formed at divergent plate boundaries, where tectonic plates move away from each other. As the plates separate, magma from the mantle rises and solidifies to form new crust. This process is known as seafloor spreading and creates new oceanic crust, which can eventually be uplifted and become part of a continent.
Some examples of mountain ranges created by continental-continental convergence are the Himalayas (resulting from the collision of the Indian and Eurasian plates) and the Alps (formed by the collision of African and Eurasian plates).
When it is two continental plates, new oceanic crust is formed, and when this continues, more oceanic crust is formed between the plates.
rift valley Answer 2 Continents are formed when continental plates pull apart.
They were formed on the edges of two ancient continental plates that collided with each other in the geological past.