Great Chagos Bank
The Great Chagos Bank, in the Chagos Archipelago, about 500 km (310 mi) south of Maldives, is the largest atoll structure in the world, with a total area of 12,642 km2 (4,881 sq mi). The atoll is administered by the United Kingdom through the British Indian Ocean Territory (BIOT).
Islands [ edit ]
Despite its enormous size, the Great Chagos Bank is largely a submarine structure. There are only four emerging reefs, mostly located on the western rim of the atoll, except for lonely Nelson Island, which lies wholly isolated in the middle of the northern fringe. These reefs have seven or eight individual low and sandy islands, with a total land area of about 5.6 km2 (2.2 sq mi). All islands and their surrounding waters are a Strict Nature Reserve since 1998. The total length of the eastern and southern expanses of the bank, as well as the reefs in its central area are wholly submerged.
The islands of the Great Chagos Bank, starting clockwise from the south, are:
- Danger Island (slightly more than 2 km (1.2 mi) long from North to South, by 1 km (0.62 mi) wide, land area 0.66 km2 (0.25 sq mi), vegetated with palm trees up to 12 m (39 ft) high.
- Eagle Islands
- Three Brothers (Trois Frères) and Resurgent Islands, vegetated with high coconut trees, land area 0.4 km2 (0.15 sq mi).
- Île du Sud (South Island, largest of the group), 23 ha (57 acres)
- Île du Milieu (Middle Island), 8 ha (20 acres)
- unnamed rocky islet
- Île du Nord (North Island), 6 ha (15 acres)
- Nelson Island (2 km (1.2 mi) long from East to West, up to 0.41 km (0.25 mi) wide, land area 0.4 km2 (0.15 sq mi), with 3 m (9.8 ft) high, bushy vegetation.
Cartography of the submerged reefs [ edit ]
The Great Chagos Bank was surveyed for the first time by Commander Robert Moresby of the Indian Navy in 1837; all other maps that would be drawn for over a century and a half were based on his chart. Although the charts of atolls made up of mostly emerged reefs, like Peros Banhos and Diego Garcia, were relatively accurate, the cartography of the vast sunken reefs forming the Great Chagos Bank proved quite a challenge. The real shape of these sunken reefs was known only when satellite imagery became available in the latter part of the 20th century.
Moresby's original hydrographic drawings were somewhat at variance with the true shape of the submerged reef, especially in areas where there were no emerging islands close by, like in the South east of the bank. The outlines of the first hydrographic surveys were marked in the 1980s navigational maps of the Chagos with a dotted line and the legend "existence doubtful" until the 1998 edition.
See also [ edit ]
References [ edit ]
- Purdy, Edward G., ed. (2001). "Origin of atoll lagoons" (PDF). GSA Bulletin. 113: 837. doi:10.1130/0016-7606(2001)113<0837:ooal>2.0.co;2. Retrieved 14 July 2018. CS1 maint: ref=harv (link)
- "[Nature Conservation of the] British Indian Ocean Territory"(PDF). Department for Environment, Food & Rural Affairs. 22 December 2004. Retrieved 14 July 2018.
- University of Washington Library - Great Chagos Bank 1890Archived 2012-11-05 at the Wayback Machine
- British Admiraltynautical chart 11000030 - 3 Chagos Archipelago, Scale 1:360 000
[ edit ]
- Oceandots - Great Chagos Bank at the Wayback Machine (archived December 23, 2010)
- Geochronology of Basement Rocks from the Mascarene Plateau, the Chagos Bank and the Maldives Ridge