Kerguelenplateau
The Kerguelen Plateau (Vorlage:IPAEng[1]) is an underwater volcanic large igneous province (LIP) in the Indian Ocean. It lies about 3,000 km to the southwest of Australia and is nearly three times the size of Japan. The plateau extends for more than 2,200 km in a northwest-southeast direction and lies in deep water.
The plateau was produced by the Kerguelen hotspot, starting with or following the breakup of Gondwanaland about 130 Mya. There is a small portion of the plateau that breaks sea level, forming the Kerguelen Islands, Heard Island and the McDonald Islands. Intermittent volcanism continues on Heard and McDonald islands.
Geographical extent
Symmetrically located across the Indian Ocean ridge and due west of Australia, is the Broken Ridge underwater volcanic plateau which was at one time contiguous with the Kerguelen Plateau prior to rifting by the mid-ocean ridge.
To the north of Broken ridge lies the linear Ninety East Ridge which continues almost due north into the Bay of Bengal and is considered to be a hotspot track.
Kerguelen continent
The Kerguelen Plateau was formed starting 110 million years ago from a series of large volcanic eruptions. The presence of soil layers in the basalt with included charcoal and conglomerate fragments of gneiss indicate that much of the plateau was above sea level as what is termed a microcontinent for three periods between 100 million years ago and 20 million years ago.
The so-called Kerguelen continent might have had tropical flora and fauna about 50 million years ago. The Kerguelen continent finally sank 20 million years ago and is now 1 - 2 km below sea level. It has sedimentary rocks similar to the ones found in Australia and India, suggesting they were once connected.
References
- UT Austin scientist plays major role in study of underwater "micro-continent"
- Leg 183 Summary: Kerguelen Plateau-Broken Ridge—A Large Igneous Province
- KERGUELEN PLATEAU—BROKEN RIDGE: A MAJOR LIP RELATED TO THE KERGUELEN PLUME.
See also
Related topics
Vorlage:Continents of the world
- ↑ OED