subduction zone <<< THIS IS WRONG #novanet user
A divergent plate boundary is where two tectonic plates move away from each other. As they separate, magma from the mantle rises to fill the gap, solidifying to form new crust. This process is known as seafloor spreading.
The main difference is the type of crust being pulled apart. At a divergent boundary on land, two tectonic plates consisting of continental crust are moving away from each other. This process can result in the formation of rift valleys or a new ocean basin. On the other hand, a divergent boundary in the sea occurs when two tectonic plates consisting of oceanic crust separate. This leads to the formation of mid-ocean ridges and new seafloor.
A divergent boundary is a tectonic plate boundary where two plates move away from each other, leading to the formation of new crust through volcanic activity. This process can result in rift valleys and mid-ocean ridges.
divergent boundary, where new crust is formed as magma rises from the mantle to fill the gap created by the moving plates. This process is known as seafloor spreading and can result in the formation of mid-ocean ridges.
Convergent (or destructive): Where two plates are moving toward each other. Collisions between oceanic plates results in subduction of the more dense plate. Collisions between an oceanic plate and a continental plate may result in the subduction of the oceanic plate because oceanic plates are more dense than continental plates. Collisions between two continental plates results in uplift and mountain formation where neither plate subducts.Divergent (or constructive): Where two plates are moving away from each other. Divergent plate boundaries are the site of new crust formation, particularly at the mid-ocean ridges, where spreading plates are infilled with basaltic magma from the asthenosphere.Transform (or conservative): Where two plates slide (actually 'grind') alongside each other and neither plate subducts. Earthquakes are common at transform faults due to the grinding and snapping movements of the plates as they move.
The antonym for divergent boundary is convergent boundary. In a divergent boundary, tectonic plates move away from each other, while in a convergent boundary, they move towards each other. This can result in subduction zones, mountain formation, or continental collision.
The Mid-Atlantic Ridge was not the result of continental convergence. Instead, it is a divergent boundary where new oceanic crust is forming as tectonic plates move apart.
No, the Alps are not a divergent boundary. The Alps are a mountain range formed from the collision of the African and Eurasian tectonic plates, a result of convergent boundary activity.
A divergent plate boundary is where two tectonic plates move away from each other. As they separate, magma from the mantle rises to fill the gap, solidifying to form new crust. This process is known as seafloor spreading.
The diverging plates move away from one another in opposite directions.
A divergent boundary results in the separation of tectonic plates, leading to the creation of new crust as magma rises up and solidifies at the boundary. This process can form features such as mid-ocean ridges or rift valleys on land.
The main difference is the type of crust being pulled apart. At a divergent boundary on land, two tectonic plates consisting of continental crust are moving away from each other. This process can result in the formation of rift valleys or a new ocean basin. On the other hand, a divergent boundary in the sea occurs when two tectonic plates consisting of oceanic crust separate. This leads to the formation of mid-ocean ridges and new seafloor.
Earthquakes can occur at any type of plate boundary, but the most powerful earthquakes tend to occur at convergent boundaries and at transform boundaries.
A divergent boundary is a tectonic plate boundary where two plates move away from each other, leading to the formation of new crust through volcanic activity. This process can result in rift valleys and mid-ocean ridges.
A divergent boundary does not occur at a convergent boundary. At convergent boundaries, tectonic plates move towards each other and usually result in the formation of mountains, ocean trenches, or volcanic activity. In contrast, divergent boundaries occur when plates move away from each other and create new oceanic crust.
A divergent boundary causes tectonic plates to move away from each other, leading to the creation of new crust through volcanic activity. This can result in the formation of mid-ocean ridges and rift valleys.
divergent boundary, where new crust is formed as magma rises from the mantle to fill the gap created by the moving plates. This process is known as seafloor spreading and can result in the formation of mid-ocean ridges.