ⓘ Mascarene Plateau

Mascarene Plateau

ⓘ Mascarene Plateau

The Mascarene Plateau is a submarine plateau in the Indian Ocean, north and east of Madagascar. The plateau extends approximately 2.000 km, from the Seychelles in the north to Reunion in the south. The plateau covers an area of over 115.000 km 2 of shallow water, with depths ranging from 8–150 m, plunging to 4.000 m to the abyssal plain at its edges. It is the second largest undersea plateau in the Indian Ocean after the Kerguelen Plateau.


1. Geography

The northern part of the Mascarene plateau includes the Seychelles and Agalega Islands. The southern part of the Mascarene plateau includes the Mascarene Islands, Saya de Malha Bank, Nazareth Bank, Soudan Banks, and Hawkins Bank. The Mascarene Islands are the mountainous islands of Mauritius, Reunion, Rodrigues, and the Cargados Carajos Shoals.


2. Geology

The Indian subcontinent was at one time next to the east coast of the Seychelles, but seafloor spreading has moved the landmass to its current position, where it has collided and fused with the continent of Asia.

The northern part of the Mascarene plateau is formed of granite, and is a fragment of the ancient supercontinent of Gondwana. The granite is topped with deposits of limestone and basalt. The basalt deposits in the Seychelles are from the Deccan Traps eruption, which occurred in the central part of the Indian subcontinent 66 million years ago, at the end of the Cretaceous period.

The southern part of the Mascarene plateau, also known as Southern Mascarene plateau SMP, was formed by the Reunion volcanic hotspot along with the Chagos-Laccadive Ridge. The banks and shoals of the southern part of the Mascarene plateau were once volcanic islands, much like Mauritius and Reunion, which have now sunk or eroded to below sea level or, in the case of the Cargados Carajos, to low coral islands. The Saya de Malha Bank formed 35 million years ago, and the Nazareth Bank and the Cargados Carajos shoals formed later. Limestone banks found on the plateau are the remnants of coral reefs, indicating that the plateau was once a succession of islands. Some of the banks may have been islands as recently as 18.000–6.000 years ago, when sea levels were up to 130 meters lower during the most recent ice age. Mauritius formed 8–10 million years ago, and Rodrigues and Reunion formed around two million years ago. Piton de la Fournaise volcano on Reunion is one of the most active volcanoes in the world.

  • geologic origin in the volcanism of the Reunion hotspot beneath the Mascarene Plateau and form a distinct ecoregion with a unique flora and fauna. The archipelago
  • Farquhar Islands, the Amirante Islands and Amirante Plateau the Seychelles Plateau and the Mascarene Plateau To the southwest and south it is separated from
  • de Malha Bank Soudan Banks Mascarene Plateau Western Indian Ocean Geochronology of Basement Rocks from the Mascarene Plateau the Chagos Bank and the Maldives
  • Rise Pacific Manihiki Plateau Southwest Pacific Mascarene Plateau Indian Naturaliste Plateau Indian Ontong Java Plateau Southwest Pacific Shatsky
  • Hawkins Bank is a large, submerged bank off the Mascarene Plateau It is considered a dependency of Mauritius in terms of fishing banks, much like Saya
  • underwater plateaus Some microcontinents are fragments of Gondwana or other ancient cratonic continents: these include Madagascar the northern Mascarene Plateau
  • Indian Ocean. The Chagos - Laccadive Ridge and the southern part of the Mascarene Plateau are volcanic traces of the Reunion hotspot. The hotspot is believed
  • The Mascarene martin or Mascarene swallow Phedina borbonica is a passerine bird in the swallow family that breeds in Madagascar and in the Mascarene Islands
  • marine gastropod in the family Cassidae, endemic to the submarine Mascarene Plateau primarily the Saya de Malha Bank and southern Mozambique. Hardy
  • the Deccan Traps also produced the Chagos - Laccadive Ridge and the Mascarene Plateau and plays a role in the geology of Mauritius and Rodriguez Island