tectonic plates
When tectonic plates diverge on land, they often form rift valleys or rift zones. These are characterized by large fissures, volcanic activity, and minor earthquakes. Over time, the continuous separation of the plates can lead to the formation of new ocean basins.
Itis called a rift.
When oceanic plates diverge an underwater earthquake is the result. Oceanic earthquakes often result in disastrous Tsunamis.
Land plates are called continental plates. Sea plates are called oceanic plates.
A rift.
rift
When two Continental plates diverge, landforms like rift valleys and mid-ocean ridges are created. Rift valleys form on land where the plates are separating, while mid-ocean ridges are underwater mountain ranges that form in the ocean.
The feature where tectonic plates diverge on land is called a "rift valley." This occurs when tectonic forces pull the Earth's crust apart, leading to the formation of a linear trough or valley. One of the most well-known examples of a rift valley is the East African Rift.
A mid-ocean ridge is formed when plates diverge or move apart. This is where new crust is created as magma rises to fill the gap created by the separating plates.
When tectonic plates diverge, magma is allowed to well up to the Earth's surface and harden, forming new land.
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When two continental plates diverge, a rift valley forms due to the pulling apart of the Earth's crust. Magma rises to fill the gap created by the separating plates, eventually leading to the formation of new oceanic crust. Over time, this process can result in the formation of a new ocean basin.