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Geography of Tristan da Cunha
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Geography of Tristan da Cunha : ウィキペディア英語版
Geography of Tristan da Cunha

Tristan da Cunha is an archipelago of five islands in the southern Atlantic Ocean, the largest of which is the island of Tristan da Cunha itself and the second-largest the remote bird haven Gough Island. It forms part of a wider territory called Saint Helena, Ascension and Tristan da Cunha which includes Saint Helena and Ascension Island.
==Location and description==

This archipelago, 1500 miles (2500 km) from the continents of Africa and South America, is one of the most remote inhabited places on earth. It consists of the following islands:
* the main island Tristan da Cunha and its surrounding islands
*
* Tristan da Cunha, the main island and largest () area:
*
* Inaccessible Island area:
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* Nightingale Islands area:
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* Nightingale Island area:
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* Middle Island area:
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* Stoltenhoff Island area:
* Gough Island (''Diego Alvarez'') area: important as the largest undisturbed cool-temperate island habitat in the South Atlantic Ocean.
The main island is quite mountainous; the only flat area is the location of the capital, Edinburgh of the Seven Seas, on the northwest coast. The highest point is a volcano called Queen Mary's Peak ; it is covered by snow in winter and is listed as an ultra prominent peak. Tristan da Cunha is thought to have been formed by a long-lived centre of upwelling magma called the Tristan hotspot.
The climate is marine cool-temperate with small temperature differences between summer and winter (11.3° - 14.5°) and between day and night.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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