about the formation of atolls. According to Charles Darwin's theory, when submerged volcanoes rise from the sea, a coral reef grew on its edge. When the volcanoes submerged, the coral reefs encircling a water-filled basin remained. Consequently, islands were formed on the reefs as the tides and currents brought dead coral onto sandbars. These were in turn colonised by plants.
A different view has been provided by Hans Hass. According to him, layers of coral reefs might have built up on top of the submerged mountains until they rose to the surface. The hardest and highest corals remained while the weaker corals in the center of the coral platforms broke down. The remaining corals at the outer edges formed rings that were to form the outer rims of atolls. Islands were formed as debris and sand accumulated on to the remaining reefs.
The reef is cut by deep channels, which the locals have mastered to navigate. Protective reefs safeguard the islands from the elements. However, the islands are susceptible to erosion. The islands are low-lying; emerging almost two meters above the sea level. It is frequent that one part of the island to erode while onto another part the currents and tides deposit sand expanding the island. Over the course of time, some islands may erode completely, while others may be formed gradually on a sandbank. There are still many islands and sandbanks at various stages of formation. Hence, the Maldives is a dynamic country in the making.