The type of volcano that forms where tectonic plates move apart is called a fissure volcano. These volcanoes typically occur at divergent boundaries, such as mid-ocean ridges, where magma rises to fill the gap created by the separating plates. As the magma erupts through fissures in the Earth's crust, it leads to the formation of new oceanic crust and can create extensive lava flows. An example of this is the volcanic activity along the Mid-Atlantic Ridge.
When tectonic plates move apart, it creates a divergent boundary. As the plates separate, magma from beneath the Earth's surface can rise up, creating new crust. This process can lead to the formation of volcanic activity and mid-ocean ridges.
A mid-ocean ridge forms as tectonic plates move apart, creating a gap where magma rises from the mantle to form new crust. This process is known as seafloor spreading and results in the continuous growth of the ocean floor.
The long crack that forms as two tectonic plates move apart is called a rift. It is typically seen in divergent plate boundaries, where the plates separate and magma from the mantle can rise to create new crust. Over time, as the plates continue to move apart, the rift can widen and eventually lead to the formation of a new ocean basin.
Some move away from each other and create massive trenches normally in the sea bed, for example the Mariana Trench - 10,998 m.
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.
They can move apart or in some rare cases together.
an earthquake
an earthquake
A long, linear crack that forms as two tectonic plates move apart is called a mid-ocean ridge. This type of boundary is where new oceanic crust is created as molten rock rises up from the mantle and solidifies along the spreading center. Over time, as the plates continue to move apart, the new crust forms a continuous ridge on the ocean floor.
forms when two {crustal} lithosphere plates move apart.
It forms a hole but new crust is formed.
Plates move apart on divergent plate boundaries.
When two lithospheric plates move apart, a divergent boundary is formed. This process results in the creation of new oceanic crust as magma rises to fill the gap between the plates, forming a mid-ocean ridge.
It causes what we call "sea-floor spreading." Sea-floor spreading is the process in which the ocean floor is extended when two plates move apart. As the plates move apart, the rocks break and form a crack between the plates. Earthquakes occur along the plate boundary. Magma rises through the cracks and seeps out onto the ocean floor like a long, thin, undersea volcano.
When tectonic plates move apart, it creates a divergent boundary. As the plates separate, magma from beneath the Earth's surface can rise up, creating new crust. This process can lead to the formation of volcanic activity and mid-ocean ridges.
You are a mid-ocean ridge that forms when tectonic plates move apart and new oceanic crust is created through volcanic activity. This process is known as seafloor spreading, and it results in the formation of new oceanic crust at the mid-ocean ridge.
When two plates move apart from each other, it creates a divergent boundary. Magma from the mantle rises to fill the gap, solidifies, and forms new crust. This process is called seafloor spreading and is responsible for the formation of mid-ocean ridges.