Because the Earth's crust is composed of not one solid layer like a shell, but many pieces, like in a puzzle. These plates are floating on layer of magma. So at these fault lines it is easier for lava to get through the crust and cause volcanoes and such.... yeah
This forms on the plate tectonic boundaries.... particularly the convergent plate boundries.
Subduction zones form along some tectonic plate boundaries. Of the three general types of tectonic plate boundaries, we will see them form at some (but not all) of what are called convergent plate boundaries.
Convergent plate boundariesDestructive plate boundaries
hot spots, divergent plate boundaries, and convergent plate boundaries.
Volcanoes are formed by tetonic plates pushing together. Therefore they often form in lines. Such as the Himalyers and the alpes.
This forms on the plate tectonic boundaries.... particularly the convergent plate boundries.
Convergent plate boundaries, usually oceanic plate to continental plate.
Subduction zones form along some tectonic plate boundaries. Of the three general types of tectonic plate boundaries, we will see them form at some (but not all) of what are called convergent plate boundaries.
Convergent plate boundariesDestructive plate boundaries
hot spots, divergent plate boundaries, and convergent plate boundaries.
Subduction zones have the deepest earthquakes.
They are concentrated in zones - specifically at or near tectonic plate boundaries.
Volcanoes are formed by tetonic plates pushing together. Therefore they often form in lines. Such as the Himalyers and the alpes.
At subduction zones along convergent plate boundaries.
most earthquakes occur at the plate boundaries because the plate boundaries are the weakest zones and earthquakes are likely to occur there . you can also take help from science ncert of 8 class.
Ocean trenches are associated with subduction zones, which are convergent plate boundaries.
In plate tectonics, when two tectonic plates move toward each other, it results in the formation of what is called a convergent plate boundary. The two plates are said to converge. One plate may be more dense than the other, and with the two plates pushing against each other, the plate that is more dense will "slide under" the other plate. The plate sliding under is said to subduct the other plate, and this creates what is called a subduction zone. Not all convergent plate boundaries have subduction zones, but all subduction zones are formed at convergent plate boundaries.