مرجانی جل پتھر
Darwin’s theory starts with a volcanic island which becomes extinct
As the island and ocean floor subside, coral growth builds a fringing reef, often including a shallow lagoon between the land and the main reef.
As the subsidence continues, the fringing reef becomes a larger barrier reef further from the shore with a bigger and deeper ساحلی جھیل inside.
Ultimately, the island sinks below the sea, and the barrier reef becomes an جزیرہ مرجانی enclosing an open lagoon.