the magma cool and then it becomes a solid and that solid will then become a plate tectonic
Mid-ocean ridges form at divergent plate boundaries, where tectonic plates are moving away from each other. This movement allows magma to rise from beneath the Earth's crust and create new oceanic crust at the ridge.
A divergent boundary is a boundary between two tectonic plates that are moving away from each other. This movement creates new crust as magma rises from the mantle and solidifies, forming mid-ocean ridges on the seafloor.
This type of plate boundary is called a divergent boundary. At divergent boundaries, tectonic plates move away from each other, allowing magma to rise from the mantle and create new crust at mid-ocean ridges. This process is known as seafloor spreading.
earthquakes occur where there are transformed boundaries.
divergent
Divergent plate boundaries create ridges like the Mid-Atlantic Oceanic Ridge. At these boundaries, tectonic plates move away from each other, allowing magma to rise and solidify, forming new oceanic crust. This process leads to the formation of mid-ocean ridges.
Mid-ocean ridges form at divergent plate boundaries, where tectonic plates are moving away from each other. This movement allows magma to rise from beneath the Earth's crust and create new oceanic crust at the ridge.
A transform boundary is typically marked by a fault line, which is a crack in the Earth's crust where two tectonic plates slide past each other horizontally. This movement can create features such as earthquake activity and linear valleys or ridges along the boundary.
In a divergent boundary, arrows typically point away from each other, indicating the movement of tectonic plates that are separating. This movement allows magma to rise from below the Earth's surface, creating new crust as the plates pull apart. Such boundaries are commonly found at mid-ocean ridges, where the ocean floor is formed.
Constructive or divergent. The ridge formed is of basaltic rock type (though this is a generalisation), and is a source of volcanic activity. Iceland was formed as a result of the sea-floor spreading.
A divergent boundary can create mid-ocean ridges and rift valleys. Mid-ocean ridges form when tectonic plates move apart, allowing magma to rise and create new oceanic crust. Rift valleys occur on land, where tectonic plates diverge and create a low-lying area between them, often leading to volcanic activity.
A divergent boundary forms when tectonic plates pull apart. As the plates move away from each other, magma rises up to create new crust, resulting in features like mid-ocean ridges or rift valleys on land.
Mid-ocean ridges are caused by divergent plate boundaries, where tectonic plates move away from each other. This movement allows magma to rise to the surface, creating new crust and forming underwater mountain ranges.
Divergent plate boundary movement causes mid-ocean ridges and sea-floor spreading. This occurs when two tectonic plates move away from each other, creating new oceanic crust at the boundary. Magma rises to the surface, solidifies, and forms undersea mountain ranges known as mid-ocean ridges.
A divergent boundary is a tectonic boundary where two plates move away from each other. This movement results in the formation of new oceanic crust through seafloor spreading. It is associated with features like rift valleys and mid-ocean ridges.
A divergent boundary is where two tectonic plates move away from each other. This movement results in the formation of new crust as magma rises to fill the gap created by the separating plates. In oceanic settings, this process leads to the formation of mid-ocean ridges, while on land it can create rift valleys.
A divergent boundary is a boundary between two tectonic plates that are moving away from each other. This movement creates new crust as magma rises from the mantle and solidifies, forming mid-ocean ridges on the seafloor.