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The Coral Sea Islands became an Australian external territory in 1969 by the Coral Sea Islands Act and extended in 1997 to include Elizabeth Reef and Middleton Reef nearly 800 km further south. The two latter reefs are much closer to Lord Howe Island , New South Wales , (about 150 km (93 mi)) than to the southernmost island of the rest of the ...
While the Great Barrier Reef with its islands and cays belong to Queensland, most reefs and islets east of it are part of the Coral Sea Islands Territory. In addition, some islands west of and belonging to New Caledonia are also part of the Coral Sea Islands in a geographical sense, such as the Chesterfield Islands and Bellona Reefs.
Willis Island is the only permanently inhabited island in the Coral Sea Islands Territory, an external territory of Australia, located beyond the Great Barrier Reef in the Coral Sea. The island is located some 450 kilometres (280 mi) east of Cairns, Queensland. It is the southernmost of the Willis Islets, a group of three islands which with ...
Middleton Reef is a coral reef in the Coral Sea. It is separated by a deep oceanic pass some 47 km wide from nearby Elizabeth Reef, forming part of the Lord Howe Rise underwater plateau. It is around 230 km from Lord Howe Island and 555 km from the coast of New South Wales.
NASA picture of the Lihou Reef. Lihou Reef National Nature Reserve is a former marine protected area covering an area of 8440 km 2 in the Australian Coral Sea Islands Territory that was incorporated into the new Coral Sea Commonwealth Marine Reserve in December 2012. [1]
The Great Barrier Reef is the world's largest coral reef system, [1] [2] composed of over 2,900 individual reefs [3] and 900 islands stretching for over 2,300 kilometres (1,400 mi) over an area of approximately 344,400 square kilometres (133,000 sq mi).
According to the Ohio Sea Grant College Program, 80% of Lake Erie's water comes from the other Great Lakes through the Detroit River, 10% from precipitation, and 10% from other tributaries. 2.
The lagoon is not the former volcanic crater. For the atoll to persist, the coral reef must be maintained at the sea surface, with coral growth matching any relative change in sea level (sinking of the island or rising oceans). [4] An alternative model for the origin of atolls is called the antecedent karst model.