Yes, when two continental plates converge, they can create a subduction zone where one plate is forced under the other, leading to the melting of rock and the formation of magma. This magma can rise to the surface, leading to the formation of a volcanic arc and volcanoes.
When two continental plates collide, the crust is thickened, buckled and deformed--gaining elevation. Mountain chains are the result; their creation occurring over periods of millions of years.
A volcano is formed at a continental rift when the Earth's tectonic plates move apart, creating a gap in the Earth's crust. Magma from the mantle rises to the surface through this gap, leading to the formation of a volcano.
At a convergent boundary, two lithospheric plates are colliding. This collision can involve oceanic lithosphere converging with either oceanic or continental lithosphere, or continental lithosphere converging with continental lithosphere. The type of lithosphere involved in the collision influences the resulting geological features, such as subduction zones or mountain ranges.
Mountains formed by continental plates colliding are known as fold mountains. These mountains are created when the intense pressure from the converging plates causes rocks to buckle and fold, resulting in uplifted and folded mountain ranges. Examples of fold mountains include the Himalayas and the Alps.
When oceanic and continental plates collide, the denser oceanic plate subducts beneath the continental plate. This subduction causes melting of the mantle, creating magma that rises to the surface, forming volcanoes on the continental plate. The magma eventually erupts through the volcano, leading to the formation of volcanic islands or mountain ranges.
The energy spews out Lava
The type of tectonic forces that create mountains are called converging plates. As two continental plates push together, the stress forces them both upwards. Because of this the Himalayas are still growing.
Converging continental plates create mountain ranges through a process called continental collision. When two continental plates collide, neither is subducted due to their similar density. Instead, the plates crumple and fold, leading to the uplift of the Earth's crust and the formation of mountain ranges.
When two continental plates collide, the crust is thickened, buckled and deformed--gaining elevation. Mountain chains are the result; their creation occurring over periods of millions of years.
the nazca(oceanic) and caribbean (continental) plates
It is natural! They were formed by two continental plates converging, coming together.
two seafloor plates and a seafloor plate and continental plate
A volcano is formed at a continental rift when the Earth's tectonic plates move apart, creating a gap in the Earth's crust. Magma from the mantle rises to the surface through this gap, leading to the formation of a volcano.
Volcanoes cannot be formed at a continental rift, due to the fact that a volcano cannot form between two continental plates: it normally forms when one continental plate and an oceanic plate collide. Normally, a volcano forms when one continental and one oceanic plate collides. The denser oceanic plate
At a convergent boundary, two lithospheric plates are colliding. This collision can involve oceanic lithosphere converging with either oceanic or continental lithosphere, or continental lithosphere converging with continental lithosphere. The type of lithosphere involved in the collision influences the resulting geological features, such as subduction zones or mountain ranges.
Converging (destructive) plate boundary: where two plates collide. Diverging (constructive) plate boundary: where two plates move away from each other. Transform plate boundary: where two plates move, or grind, past each other. Like the boundary in California.
The action of earth's crust buckling in wave-like patterns is due to two plates coming together or converging. These plates can be either oceanic or continental plates. Examples of these types of plates are the Eurasian, Pacific, Australian, Caribbean plates.