Mountain building like the Himalayas. Or one plate slides under another.
Converging plates come together. They converge together. Diverging plates come apart.
When tectonic plates push together, they converge, forming a convergent boundary.
When tectonic plates converge, they can form various geological features such as mountain ranges, deep ocean trenches, and volcanoes. This convergent boundary can result in one plate being pushed beneath the other in a process known as subduction.
It is called the concept of Biologically it is Plate tectonic. Scientifically it is Converge Belt By Terny Winblock Woods
When tectonic plates converge, they can form features such as mountain ranges, deep-sea trenches, volcanic arcs, and earthquakes. The collision and subduction of plates at convergent boundaries can also lead to the formation of island arcs and continental crust deformation.
When plates converge, a fold mountain is formed. This happens when the edges of two tectonic plates push against each other, causing the land to buckle and fold, creating mountain ranges like the Himalayas or the Andes.
The 1755 Lisbon earthquake was primarily caused by the movement of the Eurasian and African tectonic plates. These plates converge along the southwestern coast of Portugal, resulting in frequent seismic activity in the region.
because the tectonic plates converge and form mountains then the lava forms underground and erupts with burnin hot maga and lava
Im pretty sure its ridge push, slab pull, and mantle convection
No, when two continental plates converge, they typically do not form a rift valley. Instead, this convergence often leads to the formation of mountain ranges due to the collision and uplift of the plates. Rift valleys are more commonly associated with divergent boundaries, where tectonic plates move apart.
They are pieces of land that either are divergent which means that they spread apart from each other, they can also be transform plates which slide on each other and the last kind that mostly shapes the earth are tectonic plates that collide or converge which causes earthquakes, volcanoes, and tsunamis.
When two tectonic plates converge, a subduction zone can form where one plate is pushed beneath the other, creating deep oceanic trenches and volcanic arcs. Another possibility is a collision boundary, where the two plates collide and form mountain ranges due to intense pressure and folding of the Earth's crust.