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Annobon

Annobon (lit. " good year ") - an island in the Gulf of Guinea of ​​the Atlantic Ocean . In 1973 - 1979, it was called Pagal . Belongs to Equatorial Guinea . The territory of the island forms the province of Annobon ( fr. , Spanish and port. Annobón ).

  • The administrative center of the province is the city of San Antonio de Pale .
  • Area - 17 km² , population - 5008 people ( 2001 ). The predominant language is Annobon (one of the Portuguese-Creole languages).
provinces
Annobon
fr. , Spanish and port. Annobón
A countryEquatorial Guinea
Included inIsland region
Includes1 municipality
Adm. centerSan antonio de palais
History and Geography
Area17 km² (7th place )
TimezoneUTC + 1
Population
Population5,008 people ( 2001 ) ( 7th place )
Density294.59 people / km² (2nd place)
Nationalitiesannobonts
official languagesannobon
Digital identifiers
ISO 3166-2 CodeGq-an
Official site
Annobon on the map
Notes:
провинция Ке-Нтемпровинция АннобонАтлантический океанпровинция Северный БиокоМалабопровинция Южный Биокоостров Биоко (Островной регион Экваториальной Гвинеи)Мбини (контенинтальный регион Экваториальной Гвинеи)остров Аннобон (Островной регион Экваториальной Гвинеи)Биафрский заливБиафрский заливГвинейский заливАтлантический океанпровинция Центро-Сурпровинция Литоралпровинция Литорал (остров Кориско)провинция Литорал (остров Большой Элобей)провинция Веле-НзасГабонКамерунГвинейский заливProvinces of Equatorial Guinea
Image description
Annobon Province on the map of Equatorial Guinea

Geography

 
Map of Annobon Island
 
The coast of the island is characterized by steep sea walls.
 
San Antonio de Pale, the largest settlement center in Annobon, airport runway before expansion in 2007.

The island is mountainous, of volcanic origin, with fertile soils. Annobon Island is an eroded surface of a stratovolcano with a height of about 5000 m above the ocean floor, which was laid on the oceanic crust. Its visible base is composed of palagonite breccias, which contain phenocrysts and megacrysts of clinopyroxene and olivine. They are penetrated by subvertical dikes of ancaramite basanites. With erosive disagreement, the lower complex is blocked by flows of basanite flows, the lower of which is 18.4 million years old. In turn, they are also pierced by dikes with an age of 5.35 million years. At the last stages, the formation of tristanite and trachyte domes took place, the largest of which was Pico de Fuego [1] . The climate is equatorial, constantly humid.

History

It was discovered by the Portuguese on January 1, 1473 , so it got its name, which means Happy New Year (literally “good year”). Together with the island of Fernando Po and the modern coast of Equatorial Guinea in 1778 annexed to Spain . In 1968, it became part of the independent Equatorial Guinea.

Administrative Division

The province consists of only one municipality - San Antonio de Pale.

Economics

The island is of strategic interest to Equatorial Guinea . The possession of Annobon allows the government to consider vast sea areas south of Sao Tome and Principe , potentially rich in oil fields, as their exclusive economic zone. In addition, the island is used for the storage of toxic and radioactive waste [2] .

Notes

  1. ↑ A.O. Mazarovich, S. Yu. Sokolov Faults of the Angolan Basin
  2. ↑ Alexander Smoltczyk “Volltanken in Malabo”, DER SPIEGEL 35/2006 vom 08.28.2006, Seite 82

Links

  • Annobon, or Annobom // Brockhaus and Efron Encyclopedic Dictionary : in 86 volumes (82 volumes and 4 additional). - SPb. , 1890-1907.


Source - https://ru.wikipedia.org/w/index.php?title=Annobon&oldid=99690214


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