Friday 31 December 2010

Geography and climate in Socatra




ocotra is one of the most isolated landforms on Earth of continental origin (i.e. not of volcanic origin).[citation needed] The archipelago was once part of the supercontinent of Gondwana and detached during the Miocene, in the same set of rifting events that opened the Gulf of Aden to its northwest.
The archipelago consists of the main island of Socotra (3,625 km2 (1,400 sq mi)), the three smaller islands of Abd al Kuri, Samhah and Darsa and small rock outcrops like Ka'l Fir'awn and Sābūnīyah that are uninhabitable by humans but important for seabirds.[7]
The main island has three geographical terrains: the narrow coastal plains, a limestone plateau permeated with karstic caves and the Haghier Mountains.[8] The mountains rise to 5,000 feet (1,500 m). The island is a little over 80 miles (130 km) long east to west and typically 18–22 miles (29–35 km) north to south.
The climate for Socotra is classified in the Köppen climate classification as BWh and BSh, meaning a tropical desert climate and semi-desert climate with a mean annual temperature over 18°C (64°F). Yearly rainfall is light, but is fairly spread throughout the year. Generally the higher inland areas receive more rain than the coastal lowlands, due to orographic lift provided by the interior mountains.[citation needed] The monsoon season brings strong winds and high seas.

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