Book contents
- Frontmatter
- Contents
- Colophon
- Preface
- Acknowledgements
- Maps
- Units of measurement and abbreviations
- 1 Geology: An Australian perspective
- 2 The Earth: A geology primer
- 3 Telling geological time: The great canvas
- 4 The cratons: Building the core of Precambrian rocks
- 5 Mountain building: Paleozoic orogenic rock systems
- 6 Warm times: Tropical corals and arid lands
- 7 Icehouse: Carboniferous and Permian glaciation
- 8 Mesozoic warming: The great inland plains and seas
- 9 The birth of modern Australia: Flowering plants, mammals and deserts
- 10 Fossils: The Australian record of past life in context
- 11 The land stirs: Volcanoes and the eastern highlands
- 12 The outline and submerged terrace: Building the continental shelf and coastlines
- 13 The coral reefs: Unique parts of the continental shelf
- 14 Patterns of change: Cycles in Australia's journey
- Epilogue
- Sources and references
- Index
- References
13 - The coral reefs: Unique parts of the continental shelf
- Frontmatter
- Contents
- Colophon
- Preface
- Acknowledgements
- Maps
- Units of measurement and abbreviations
- 1 Geology: An Australian perspective
- 2 The Earth: A geology primer
- 3 Telling geological time: The great canvas
- 4 The cratons: Building the core of Precambrian rocks
- 5 Mountain building: Paleozoic orogenic rock systems
- 6 Warm times: Tropical corals and arid lands
- 7 Icehouse: Carboniferous and Permian glaciation
- 8 Mesozoic warming: The great inland plains and seas
- 9 The birth of modern Australia: Flowering plants, mammals and deserts
- 10 Fossils: The Australian record of past life in context
- 11 The land stirs: Volcanoes and the eastern highlands
- 12 The outline and submerged terrace: Building the continental shelf and coastlines
- 13 The coral reefs: Unique parts of the continental shelf
- 14 Patterns of change: Cycles in Australia's journey
- Epilogue
- Sources and references
- Index
- References
Summary
Although restricted to northern Australia and of limited distribution, coral reefs are a striking feature of Australia's continental shelves. The Great Barrier Reef, on the northeastern shelf, is a reef complex of great international significance and one of Australia's prime assets. It is famous for the diversity and colour of its inhabitants, especially fish and corals. The history of the reef reflects its geological context, including Australia's journey into the tropics and the consequences of changing sea levels. The long-term future of the Great Barrier Reef will be influenced by processes that apply on the adjoining coastal fringe and on the continental shelf where it is developed.
The Australian coral reefs were great hazards to early seafarers. Even today, with highly accurate navigation equipment and powerful engines, boats and even ships still run aground within the Great Barrier Reef. For example, in 2010 the bulk coal carrier Shen Neng became grounded on Douglas Shoal of the Great Barrier Reef, east of Rockhampton. Navigating the waters must have been far more difficult for explorers like James Cook and Matthew Flinders, who had to command sailing vessels that were at the mercies of the winds and tidal currents. This was particularly the case when navigating the intricacies of the Great Barrier Reef. On 1 June 1770 Cook's vessel, HM Bark Endeavour, became firmly fixed on a reef, yet he was able to refloat it, make hasty repairs, sail to the mainland and there careen it on a river bank at present-day Cooktown. With the repairs complete he sailed the short distance to Lizard Island and climbed its granitic hill, 300 m high, to search for a way out of the reefs, taking a bearing on a channel to the safety of the open sea. Matthew Flinders, following Cook in early European exploration along the northeastern coastline, directed steerage of the Investigator from the masthead. Both men and their vessels survived their encounters with the reef.
Not so fortunate were those on the Pandora, which was carrying mutineers from the Bounty home to England for trial. In 1791 she struck Pandora Reef, at the entrance to Torres Strait, and was dragged across it through the night before being tipped into 34 m depth of water the next morning.
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- The Geology of Australia , pp. 305 - 326Publisher: Cambridge University PressPrint publication year: 2016