Submerged continent

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Topographic map of Zealandia Zealandia, topographic map.jpg
Topographic map of Zealandia

A submerged continent or a sunken continent is a region of continental crust, extensive in size but mainly undersea. The terminology is used by some paleogeologists and geographers in reference to some landmasses (none of which are as large as any of the seven generally-recognized continents).

The definition of this term is unclear. If continental fragments and microcontinents smaller than 2,500,000 km2 (970,000 sq mi), which is approximately one third of the area of mainland Australia, are excluded, then Zealandia (approximately 4,900,000 km2 or 1,900,000 sq mi) would be the only geological feature which is classifiable as a submerged continent.

Other notable submerged lands include Beringia, Doggerland, the Kerguelen Plateau, Mauritia, Sahul, and Sunda.

Submerged continents have been sought and speculated about in regard to a possible "lost continent" underwater in the Atlantic Ocean. [1] [2] There was also a search in the 1930s for Lemuria, thought to have been a possible submerged continent between the Indian and African coasts. [3]

See also

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<span class="mw-page-title-main">Geography of New Caledonia</span>

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<span class="mw-page-title-main">Mu (mythical lost continent)</span> Mythical lost continent

Mu is a lost continent introduced by Augustus Le Plongeon (1825–1908), who identified the "Land of Mu" with Atlantis. The name was subsequently identified with the hypothetical land of Lemuria by James Churchward (1851–1936), who asserted that it was located in the Pacific Ocean before its destruction. The place of Mu in both pseudoscience and fantasy fiction is discussed in detail in Lost Continents by L. Sprague de Camp.

Lemuria, or Limuria, was a continent proposed in 1864 by zoologist Philip Sclater, theorized to have sunk beneath the Indian Ocean, later appropriated by occultists in supposed accounts of human origins. The theory was discredited with the discovery of plate tectonics and continental drift in the 20th century.

<span class="mw-page-title-main">Continental crust</span> Layer of rock that forms the continents and continental shelves

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<span class="mw-page-title-main">Location hypotheses of Atlantis</span>

There are several hypotheses about real-world events that could have inspired Plato's fictional story of Atlantis, told in the Timaeus and Critias. While Plato's story was not part of the Greek mythic tradition and his dialogues use it solely as an allegory about hubris, researchers have speculated about real natural disasters that could have served as inspiration. Additionally, many works of pseudohistory and pseudoarchaeology treat the story as fact, offering reinterpretations which tie to national mysticism or theories of ancient aliens. While Plato's story explicitly locates Atlantis in the Atlantic Ocean beyond the Pillars of Hercules, location hypotheses include Helike, Thera, Troy, and the North Pole.

<span class="mw-page-title-main">Lord Howe Rise</span> Deep sea plateau from south west of New Caledonia to the Challenger Plateau, west of New Zealand


The Lord Howe Rise is a deep sea plateau which extends from south west of New Caledonia to the Challenger Plateau, west of New Zealand in the south west of the Pacific Ocean. To its west is the Tasman Basin and to the east is the New Caledonia Basin. Lord Howe Rise has a total area of about 1,500,000 km2 (580,000 sq mi), and generally lies about 750 to 1,200 metres under water. It is part of Zealandia, a much larger continent that is now mostly submerged, and so is composed of continental crust. Some have included the 3,500 m (11,500 ft) deep New Caledonia Basin as within the rise, given its continental crust origin, and this would give a larger total area of 1,950,000 km2 (750,000 sq mi).

<span class="mw-page-title-main">Doggerland</span> Landmass currently beneath the North Sea that connected the British Isles to mainland Europe

Doggerland was an area of land in Northern Europe, now submerged beneath the North Sea, that connected Britain to continental Europe. It was repeatedly exposed at various times during the Pleistocene epoch due to the lowering of sea levels during glacial periods. It was last flooded by rising sea levels around 6500–6200 BCE. The flooded land is known as the Dogger Littoral. Geological surveys have suggested that it stretched from what is now the east coast of Great Britain to what is now the Netherlands, the western coast of Germany and the Danish peninsula of Jutland. It was probably a rich habitat with human habitation in the Mesolithic period, although rising sea levels gradually reduced it to low-lying islands before its final submergence, possibly following a tsunami caused by the Storegga Slide. Doggerland was named after the Dogger Bank, which in turn was named after 17th-century Dutch fishing boats called doggers.

Continental crustal fragments, partly synonymous with microcontinents, are pieces of continents that have broken off from main continental masses to form distinct islands that are often several hundred kilometers from their place of origin.

<span class="mw-page-title-main">Zealandia</span> Mostly submerged continental crust area in Oceania

Zealandia, also known as Te Riu-a-Māui (Māori) or Tasmantis, is an almost entirely submerged mass of continental crust in Oceania that subsided after breaking away from Gondwana 83–79 million years ago. It has been described variously as a submerged continent, continental fragment, and microcontinent. The name and concept for Zealandia was proposed by Bruce Luyendyk in 1995, and satellite imagery shows it to be almost the size of Australia. A 2021 study suggests Zealandia is over a billion years old, about twice as old as geologists previously thought.

<span class="mw-page-title-main">Continent</span> Large geographical region identified by convention

A continent is any of several large geographical regions. Continents are generally identified by convention rather than any strict criteria. A continent could be a single landmass or a part of a very large landmass, as in the case of Asia or Europe. Due to this, the number of continents varies; up to seven or as few as four geographical regions are commonly regarded as continents. Most English-speaking countries recognize seven regions as continents. In order from largest to smallest in area, these seven regions are Asia, Africa, North America, South America, Antarctica, Europe, and Australia. Different variations with fewer continents merge some of these regions; examples of this are merging North America and South America into America, Asia and Europe into Eurasia, and Africa, Asia, and Europe into Afro-Eurasia.

<span class="mw-page-title-main">Geology of Zealandia</span> Geology of continental crust containing New Zealand and New Caledonia

Zealandia is an area of mostly submerged continental crust that contains New Zealand and New Caledonia.

References

  1. ATLANTIS SEARCH SHIFTS TO AEGEAN; Lost Continent Legend Held Based on False Statistics 1966 New York Times
  2. "A Submerged Continent". Los Angeles Times. April 4, 1882. Retrieved 2019-05-28. Ignatius Donnelly has recently published a work in defence of the story that a continent known among the ancients as Atlantis was sunk in the Atlantic Ocean by an earthquake.
  3. "Submerged continent". The Sydney Morning Herald. November 28, 1932.[ permanent dead link ]