Typically continental plate convergence will result in an orogeny event, or a mountain building event. As the plates converge, the crust will deform, but there will be no plate subduction, and so continent to continent convergence is not related to volcanism. Large thrust faults are often associated with continental convergence zones as well.
The convergence of two continental plates would produce a fold fault mountain range. It would also produce Earthquakes as well as Mountain building.
Earthquakes, tsunamis, the rise of hills and mountains, change the course of rivers
when two oceanic plates collide they create a deep-ocean trench, at deep-ocean trenches subduction occurs.
A mountain range.
A mountain range
folded mountains
deep oceanic trench
Concave lens (diverging) produces an upright image that is virtual. Although to create a real upright image would require 2 convex (converging) lens with a distance of their respective focal lengths between them.
The region where the seafloor is forced beneath the continental plate is called a subduction zone. When the seafloor descends down it produces a deep-ocean trench.
Convex lens produces both real and virtual images. But concave lens produces only virtual images for real objects. If object is virtual then real image could be produced by a concave lens.
The process that produces haploid sex cells is mitosis.
The earth's outer core produces the magnetic field.
When two Continental plates come together, they both collide.This forms mountains.
Subducting crust produces volcanoes and a narrow range of mountains (like the Andes). Continental convergence does not produce volcanoes and produces a wider range of mountains (Rockies or Himalayas).
There are two basic types of convergent boundary. The first is a subduction zone, which occurs at a collision between two plates carry oceanic crust or one carrying continental and once carrying oceanic crust. In such a collision, one oceanic plate will subduct under the other and sink into the mantle. Such a collision produces volcanoes on the overriding plate and will produce mountain ranges on a continent. The other type of convergent boundary occurs when two continent collide. These collisions produce high mountains but not volcanoes. No subduction occurs as continental crust is not dense enough to sink into the mantle.
two seafloor plates and a seafloor plate and continental plate
Head-on collision produces the greatest force of impact.
Usually subduction of the denser thinner oceanic crust under the lighter thicker continental crust. This also produces a row of volcanoes in the continental crust producing lava high in water content and resulting in explosive eruptions.
Transform Boundary
convergent plate boundary
transform boundary
transform boundary
the answer to this question is a transform boundary. At a transform boundary plates slide past one another. Because tectonic plates have irregular edges, they grind and jerk as they slide, which produces earthquakes.
oceanic-continential