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Quebec City speaks French
Answer:
i south American plate(Note that the south american plate has both oceanic and continental plates) convergence with the Caribbean plate
ii Pacific plate converging with the North American plate
iii Pacific and the Mariana plates
Explanation:
Convergent boundaries are boundaries where tectonic plates collides. The plate collision might be between oceanic plate and continental plate, continental and continental plate and oceanic and oceanic plates. Usually, when the continental plate collides with the oceanic plates the more denser plate which is the oceanic plate subduct.
Ocean-ocean convergent boundaries is the collision between oceanic plates.Three different occurrence of ocean-ocean convergence are
i south American plate(Note that the south american plate has both oceanic and continental plates) convergence with the Caribbean plate. The more denser plate subduct after the collision which is the south American plate. The south American plate is more cooler and denser than the Caribbean plate so it will descend beneath the Caribbean plate.
ii Pacific plate converging with the North American plate(oceanic plate section). The pacific plate will descend beneath North American plate because of it denser nature.
iii Pacific and the Mariana plates. The pacific will also be subducted here because Mariana plate is less dense than it and even more buoyant .
The general geologic features/phenomenon found in this kind of boundaries are trenches , Island arc, volcanoes, earthquakes etc
The Earth's surface is covered by a series of crustal plates.The ocean floors are continually moving, spreading from the center, sinking at the edges, and being regenerated.Convection currents beneath the plates move the crustal plates in different directions.The source of heat driving the convection currents is radioactivity deep in the Earths mantle.
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<span>Oxbow lakes are generally formed by d</span></span>eposition along the outside banks of the
curve in a meandering stream. The river finds a shorter course cutting off its
curved parts hence forming the oxbow lake. This phenomenon normally occurs on
flat plains close to the river’s outlets to seas or lakes.