Divergent boundaries refer to a new crust formed by molten material emerging between two divergent plates. The typical basins that get formed at divergent boundaries are rifts.
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In Divergent boundaries, new crust is created by the rising molten materials coming from the mantle when two plates separate.
A stream of hot material creates a new seabed between the separating plates, producing the sea bottom expansion.
New and young crust instantaneously gets formed.
This process occurs along with an underwater mountain range, known as the mid-oceanic ridge or divergent ridge.
An example of divergent boundary is the ridge located in the middle of the Atlantic Ocean, extending from Greenlander to the southernmost point of South America.
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