Geography of Seychelles

Continent	Africa
Region	Indian Ocean
Coordinates	4°35′S55°40′E / 4.583°S 55.667°E /-4.583; 55.667
Area	Ranked 180th
• Total	452 km2 (175 sq mi)
• Land	100%
• Water	0%
Coastline	491 km (305 mi)
Borders	None
Highest point	Morne Seychellois 905 metres (2,969 ft)
Lowest point	Indian Ocean 0 m
Exclusive economic zone	1,336,559 km2 (516,048 mi2)

Seychelles is a smallisland country east of theAfrican continent located in theSea of Zanj due north ofMadagascar, withAntsiranana as its nearest foreign city.^[1] Seychelles lies between approximately 4ºS and 10ºS and 46ºE and 54ºE. The nation is anarchipelago of 155tropical islands, somegranite and somecoral, the majority of which are small and uninhabited. The landmass is only 452 km² (175 mi²) but the islands are spread wide over anexclusive economic zone of 1,336,559 km² (516,048 mi²). About 90 percent of the population of 100,000 live onMahé, 9 percent onPraslin andLa Digue. Around a third of the land area is the island of Mahé and a further third the atoll ofAldabra.^[2]

There are two distinct regions, the granitic islands, the world's only oceanic islands of granitic rock and the coralline outer islands. The granite islands are the world's oldest ocean islands, while the outer islands are mainly very young, though theAldabra group and St Pierre (Farquhar Group) are unusual,raised coral islands that have emerged and submerged several times during their long history, the most recent submergence dating from about 125,000 years ago^[3]

The archipelago consists of 155 islands and thirty prominent rock formations scattered throughout a self-proclaimedexclusive economic zone of more than 1,350,000 square kilometres (520,000 sq mi) of ocean.^[4] Some forty islands aregranitic and lie in a 90-kilometre (56 mi) radius from Mahé, the main island.^[4] The remaining islands arecoralline, stretching over a 1,200-kilometre (750 mi) radius fromIle Aux Vaches in the northeast to theAldabra Atoll in the southwest.^[4] The country's Inner Islands are the granitic islands plus two nearby coralline islands,Bird Island andDenis Island.^{[citation needed]} The remaining coralline islands are theOuter Islands.^{[citation needed]} The islands are all small—the aggregate land area is only 455 square kilometres (176 sq mi).^[4][5]

Mahé is 25 kilometres (16 mi) long and no more than 8 kilometres (5.0 mi) wide,^[4] with an area of 156.7 km² (61 sq mi).^{[citation needed]} It contains the capital and only city,Victoria, an excellent port.^[4] Victoria lies approximately 1,600 kilometres (990 mi) east ofMombasa, Kenya; 2,800 kilometres (1,700 mi) southwest ofMumbai; 1,700 kilometres (1,100 mi) north of Mauritius; and 920 kilometres (570 mi) northeast of Madagascar.^[4] The only other important islands by virtue of their size and population are Praslin and La Digue, situated about thirty kilometers to the northeast of Mahé.^[4]

The granitic islands are founded on a fragment separated from the Indian continental plate during thePalaeocene about 66 million years ago during the break up of the supercontinent ofGondwana. This break-up was associated with the volcanic activity that built theMascarene Plateau.^[6] These granitic islands are characterized by boulder-covered hills and mountains as high as 940 metres (3,080 ft) rising abruptly from the sea.^[4] Elsewhere, narrow coastal plains extend to the base of the foothills.^[4] Extensively developedcoral reefs are found mainly on the east coasts because of the southwesttrade winds andequatorial current. Ninety-nine percent of the population is located on the granitic islands, and most are on Mahé.^[4]

The coralline islands differ sharply from the granitic in that they are very flat, often rising only a few feet (one meter) above sea level. They have no fresh water, and very few have a resident population.^[4] Many, like Ile aux Vaches, Ile Denis, the Amirante Isles, Platte Island, and Coetivy Island, are sand cays upon which extensive coconut plantations have been established.^[4] Some of the coralline islands consist of uplifted reefs and atolls covered with stunted vegetation.^[4] Several of these islands have been important breeding grounds for turtles and birds, as well as the sites of extensive guano deposits, which formerly constituted an important element of the Seychellois economy but now for the most part are depleted.^[4] The Aldabra Islands, the largest coralline atoll with an area greater than Mahe, are a sanctuary for rare animals and birds.^[4]

The five groups of coralline islands that make up the Outer Islands areSouthern Coral Group (a collective term forÎle Platte andCoëtivy Island),Amirante Islands,Alphonse Group (Alphonse Atoll andSt. François Atoll),Aldabra Group (Aldabra Atoll,Assumption Island, and the Cosmoledo Group, consisting ofCosmoledo Atoll andAstove Island), andFarquhar Group (Farquhar Atoll,Providence Atoll and St. Pierre Island).^[7]

The Seychelles Bank is founded on a granite basement, a fragment separated from the Indian continental plate during thePalaeocene about 66 million years ago. This break-up was associated with the volcanic activity that built theMascarene Plateau. The occurrence of syenite, diorite and microgranite in the western part of the Seychelles Bank could indicate that crustal deposit across the northwestern Indian Ocean Ridge apparently drove the Seychelles block southwestwards, causing it to collide with the northeastern edge of the Mascarene Basin. This collision could have led to the development of the Amirante Trough.^[6] This rift formation is associated with theRéunion hotspot which is also responsible forRéunion Island and theDeccan Traps inIndia. Because of its long isolation, the Seychelles hosts several unique species including thecoco de mer, apalm which has the largest seeds of any plant and the world's largest population ofgiant tortoises.^{[citation needed]}

The climate of Seychelles is tropical, having little seasonal variation.^[4] Temperatures on Mahe rarely rise above 29 °C (84 °F) or drop below 24 °C (75 °F).^[4] Humidity is high, but its enervating effect is usually ameliorated by prevailing winds.^[4] The southeast monsoon from late May to September brings cooler weather, and the northwest monsoon from March to May, warmer weather.^[4]

High winds are rare inasmuch as most islands lie outside the Indian Ocean cyclone belt; Mahe suffered the only such storm in its recorded history in 1862.^[4] Mean annual rainfall in Mahe averages 2,880 millimetres (113 in) at sea level and as much as 3,550 millimetres (140 in) on the mountain slopes.^[4] Precipitation is somewhat less on the other islands, averaging as low as 500 millimetres (20 in) per year on the southernmost coral islands.^[4]

Because catchment provides most sources of water in Seychelles, yearly variations in rainfall or even brief periods of drought can produce water shortages.^[4] Small dams have been built on Mahe since 1969 in an effort to guarantee a reliable water supply, but drought can still be a problem on Mahe and particularly on La Digue.^[4]

The Seychelles contain at least 75 species of flowering plants, three mammal species, 14 bird species, 30 species of reptiles and amphibians, and several hundred species of snails, insects, spiders and other invertebrates found nowhere else.^[4] In addition, the waters contain more than 900 kinds of fish, of which more than one-third are associated with coral reefs.^[4] Specific examples of unique birds are theSeychelles paradise flycatcher, theSeychelles black parrot, theSeychelles warbler,^[20]and the flightless rail.^[4] Most famous of all the Seychelles animals are thegiant tortoises of the genusAldabrachelys.^{[citation needed]}

Vast amounts of plastic debris accumulate on beaches across Seychelles. Observational analysis suggests that most terrestrial debris originates from Indonesia, India, and Sri Lanka. Debris associated with fisheries includingfish aggregating devices also poses a major problem. Rats have reduced biodiversity on many islands.^{[citation needed]} Climate change is also a significant issue.

Seychelles began addressing the conservation problem in the late 1960s by creating the Nature Conservancy Commission, later renamed theSeychelles National Environment Commission.^[4] A system of national parks and animal preserves covering 42% of the land area and about 260 square kilometres (100 sq mi) of the surrounding water areas has been set aside.^[4] Legislation protects wildlife and bans various destructive practices.^[4]

A major project was funded by Fonds Francais pour l'environnement Mondiale (FFEM) and implemented byIsland Conservation Society.^[21] This aims to rehabilitate and enhance islands for the maintenance of native biodiversity in Seychelles through eradication of introduced predator species, rehabilitation of habitats and reintroduction of rare or threatened species.Rats have been eliminated from North Island, Cosmoledo Atoll and Conception Island.

Geographic coordinates:4°35′S55°40′E / 4.583°S 55.667°E /-4.583; 55.667

Area:
total:459 km²
land:459 km²
water:0 km²

Land boundaries:0 km

Coastline:491 km

Maritime claims:
continental shelf:200 nmi (370.4 km; 230.2 mi) or to the edge of the continental margin
exclusive economic zone:1,336,559 km² (516,048 mi²) with 200 nmi (370.4 km; 230.2 mi)
territorial sea:12 nmi (22.2 km; 13.8 mi)

Elevation extremes:
lowest point:Indian Ocean 0 m
highest point:Morne Seychellois 905 m

Natural resources:fish,copra,cinnamon trees

Land use:
arable land:2%
permanent crops:13%
permanent pastures:0%
forests and woodland:11%
other:74% (1993 est.)

Irrigated land:0 km²

Environment - international agreements:
party to:Biodiversity, Climate Change,Desertification, Endangered Species, Hazardous Wastes, Law of the Sea, Marine Dumping, Nuclear Test Ban, Ozone Layer Protection, Ship Pollution, Whaling
signed, but not ratified:Climate Change-Kyoto Protocol

This is a list of the extreme points ofSeychelles, the points that are farther north, south, east or west than any other location.

• Northernmost point –Bird Island,Outer Islands district
• Easternmost point –Coëtivy Island,Outer Islands district
• Southernmost point -Goelette Island,Farquhar Group,Outer Islands district
• Westernmost point -West Island,Aldabra Islands,Outer Islands district

• Seychelles Plate
• Mascarene Plateau

• Hardy, Dennis (2023)."Sovereignty and Seychelles: Borders and boundaries in a small island state"(PDF).Seychelles Research Journal.5 (1):52–64. Retrieved2025-06-20.
• Swanborn, D. J. B.; Fassbender, N.; Huvenne, V. A. I. (2022)."Geomorphological drivers of deeper reef habitats around Seychelles".Coral Reefs.41:1001–1016.doi:10.1007/s00338-022-02281-4. Retrieved2025-06-20.
• Malcolm, James A.; Murday, Linganaden (2018). "Small islands' understanding of maritime security: the cases of Mauritius and Seychelles".Indian Ocean Islands (1st ed.). Routledge. p. 23.ISBN 9781351019989. Retrieved2025-06-20.
• Persaud, I. (2017).Unpacking paradise: geography education narratives from the Seychelles (PhD thesis).University College London. Retrieved2025-06-20.
• Hammond, J. O. S.; Kendall, J.-M.; Collier, J. S.; Rümpker, G. (2013)."The extent of continental crust beneath the Seychelles".Earth and Planetary Science Letters.381:166–176.doi:10.1016/j.epsl.2013.08.023. Retrieved2025-06-20.
• Johnson, Markes E.; Baarli, B. Gudveig (2005)."Erosion and Burial of Granite Rocky Shores in the Recent and Late Pleistocene of the Seychelles Islands: Physical and Biological Perspectives".Journal of Coastal Research.21 (5 (215)):867–879.doi:10.2112/05-0019.1. Retrieved2025-06-20.
• Plummer, Ph. S.; Belle, E. R. (1995)."Mesozoic tectono-stratigraphic evolution of the Seychelles microcontinent".Sedimentary Geology.96 (1–2):73–91.doi:10.1016/0037-0738(94)00127-G. Retrieved2025-06-20.
• Fauvel, A. A. (1909).Unpublished Documents on the History of the Seychelles Islands Anterior to 1810: Together with a Cartography and a Bibliography (in English and French). Government Printer, South Africa. p. 441. Retrieved2025-06-20.

• Geography of Seychelles
• Geography of the Indian Ocean

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