Constructive Plate Boundaries make Volcanoes. The Oceanic Plate (Sea) is in between two Continental Plates (Land). Both Constructive Plates are being pulled in their respective directions and the Oceanic Plate is stuck in the middle. It forms a crack in the centre and this then allows the magma from under the Earths Crust to rise up through the crust to form a cone shaped structure of magma. The magma cools and is left as rock, therefore having a volcano.
Yes, earthquakes can occur at constructive margins where tectonic plates are moving apart. As the plates separate, tension builds up in the crust which can lead to faults slipping and causing earthquakes. However, earthquakes at constructive margins tend to be less frequent and less intense compared to those at other types of plate boundaries.
constuctive
Brasstown Bald was formed by tectonic plates crashing together. This is the same thing as earthquakes which causes it to be constructive.
The Cohutta Mountains were formed by the collision of tectonic plates, which is a constructive process. Over time, the pressure and movement of these plates caused the land to uplift and form the mountain range.
When plates move apart from each other in opposite directions, it is called divergent boundary or a constructive boundary. This process typically happens at mid-ocean ridges where new oceanic crust is formed as magma rises up and solidifies.
Constructive because two tectonic plates pushed together and pushed it up.
when the land is pushed farther apart to form more land
Constructive because new land is 'constructed'
Plates pushed together makes mountains therefore plates pulled apart makes volcanos
Divergent plates.
They are called constructive boundaries. New crust is constructed as the plates move apart and magma erupts.
The plates which are constantly moving move apart at divergent boundaries. These are also called constructive boundaries because of the fact that new magma rises here and heals the diverging plates.
A boundary where the plates are moving apart is called a divergent boundary. It is also called a constructive boundary because new crust is made there.
The spreading apart of plates is considered constructive because it results in the creation of new crust along divergent boundaries. As the plates move apart, magma from below the Earth's surface rises to fill the gap, solidifies, and forms new crust. This process leads to the growth of the Earth's surface and contributes to the renewal of oceanic basins.
Both continental and oceanic plates float on the top surface of the mantle, which is divided into convection cells. The movement of these convection cells drag the plates along: where convection causes the mantle material to fall the plates are pushed together and where convection causes the mantle material to rise the plates are pulled apart.
Constructive plate margins are when two plates move away from each other, creating more ocean floor.
The magma is in the mantle, the layer under the crust. There is a convection current caused by radioactivity in the inner core which causes the plates to move. Therefore the constructive plates move apart which means magma can rise up. It'll then solidify and this is what makes volcanoes. Hence CONSTRUCTive.