Definition: Vaughan (1917) has defined coral reef as “a ridge or mound of lime stone, the upper surface of which is near the surface of the sea and which.

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Presentation transcript:

Definition: Vaughan (1917) has defined coral reef as “a ridge or mound of lime stone, the upper surface of which is near the surface of the sea and which is formed of calcium carbonate by the actions of organisms, chiefly corals.” The coral reefs are, in fact, produced by corals belonging to Anthozoa, particularly by stony corals, the Madreporaria. Hence, these are supposed to be the principal builders of coral reefs though there are certain other contributors also. A coral reef, in fact, is a ridge of lime stone whose upper surface is just below the sea surface and it is exposed at low tides.

Types of coral reefs The various types of coral reefs are grouped into three major types: 1. Fringing Reefs: The fringing reefs also referred to as the shore reefs are built from the sea bottom and extend from the shore up to 1/4 miles having no navigable channel between the shore and reef. This zone of the sea is called edge or front. However, sometimes reef beds are broken to result into irregular channels called lagoon. Such reefs are composed largely of coral sand having living and dead corals building reefs, mud and other animals. Fringing reef is very common in East Indies.

Fringing reefs Barrier reefs

2. Barrier Reef: The barrier reefs are like fringing reefs but they are situated in the sea nearly 1 km to 15 km away from the shore. Therefore, navigable channel called lagoon separates these reefs from the shore. The lagoon may be 20 to 40 fathoms deep, hence, it becomes navigable. The Great Barrier Reef on the north-east coast of Australia is 1,200 miles long, about miles wide and situated nearly 90 miles away from the shore.

3. Atoll Reef: The atoll reef, also referred to as coral island or lagoon island, is a circular or horse-shoe-shaped reef enclosing a lagoon of water which may be small or large up to 50 miles across. Atoll reef may be broken to form channels; some suitable for navigation and other may not be suitable for it. An interesting atoll reef example is Aldabra in the Indian Ocean, about 260 miles northeast of the Malagasy Republic and 400 miles from the coast of Africa.

Atolls