Mid-Ocean Trench
An enormous gap that forms as new ocean crust cools and moves apart is called a mid-ocean ridge. This is a mountain range on the ocean floor where new oceanic crust is created as tectonic plates move away from each other.
Seafloor spreading is the geologic process that forms new crust on the ocean floor. This occurs at mid-ocean ridges, where tectonic plates move apart and magma rises to the surface, solidifying to form new oceanic crust.
Some move away from each other and create massive trenches normally in the sea bed, for example the Mariana Trench - 10,998 m.
A rift is a crack or opening that forms in the Earth's crust due to tectonic forces pulling the crust apart. Rifts can lead to the formation of new ocean basins or valleys, such as the East African Rift Valley.
continental crust
a valley or a canyon
a rift hope i helped
A rift.
Mid-ocean ridges are divergent plate boundaries where new oceanic crust forms as tectonic plates move apart. At these boundaries, magma rises from the mantle, cooling and solidifying to create new crust.
where two plates pull apart from each other at oceanic ridges
the answer is rift valley
An enormous gap that forms as new ocean crust cools and moves apart is called a mid-ocean ridge. This is a mountain range on the ocean floor where new oceanic crust is created as tectonic plates move away from each other.
It forms a hole but new crust is formed.
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.
New crust forms on the ocean floor through seafloor spreading, where magma rises up from the mantle through mid-ocean ridges and solidifies into new crust as tectonic plates move apart.
Seafloor spreading is the geologic process that forms new crust on the ocean floor. This occurs at mid-ocean ridges, where tectonic plates move apart and magma rises to the surface, solidifying to form new oceanic crust.
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.