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.
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.
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.
When two continental plates come together, they can form convergent boundaries where one plate is forced beneath the other in a process known as subduction. This can lead to the formation of mountain ranges, earthquakes, and volcanic activity as the plates interact and collide.
two seafloor plates and a seafloor plate and continental plate
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
A head-on collision typically produces the greatest force of impact because the kinetic energy of both vehicles is concentrated in the direction of the collision, leading to a more significant transfer of energy. This type of collision is often the most severe and can result in severe damage and injury.
A converging lens produces a virtual image that is upright and enlarged, while a diverging lens produces a virtual image that is upright and reduced in size. Additionally, the converging lens forms the virtual image on the same side as the object, while the diverging lens forms it on the opposite side.
oceanic-continential
Transform
trench