- published: 22 Apr 2013
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Kuwait City (Arabic: مدينة الكويت, transliteration: Madīnat al-Kuwayt), is the capital of Kuwait. It has a population of 2.38 million in the metropolitan area. Located at the heart of the country on the shore of the Persian Gulf, and containing Kuwait's parliament (Majlis Al-Umma), most governmental offices, the headquarters of most Kuwaiti corporations and banks, it is the political, cultural and economic center of the emirate.
Kuwait City’s trade and transportation needs are served by Kuwait International Airport, Mina Al-Shuwaik (Shuwaik Port) and Mina Al Ahmadi (Ahmadi Port) 50 kilometers to the south, on the Persian Gulf coast.
Kuwait City was first settled in the early 18th century by the Al-Sabāh clan, later the ruling family of Kuwait and a branch of the Al-Utūb tribe (that also included the Al-Khalīfah clan, the ruling family of Bahrain), and their leader, Sheikh Sabāh I. Its name may have derived from an earlier abandoned fort located there, called "Kūt" (كوت) – Arabic for a fortress by the sea.
Kuwait, officially the State of Kuwait i/kuːˈweɪt/ (Arabic: دولة الكويت, Dawlat al-Kuwayt) is a sovereign Arab state situated in the north-east of the Arabian Peninsula in Western Asia. It is bordered by Saudi Arabia to the south at Khafji, and Iraq to the north at Basra. It lies on the north-western shore of the Persian Gulf. The name Kuwait is derived from the Arabic أكوات ākwāt, the plural of كوت kūt, meaning a fortress built near water. The country covers an area of 17,820 square kilometers (6,880 sq mi) and has a population of about 3.5 million.
Historically, the region was the site of Characene, a major Parthian port for trade between Mesopotamia and India. The Bani Utbah tribe were the first permanent Arab settlers in the region, and laid the foundation of the modern emirate. By the 19th century, Kuwait came under the influence of the Ottoman Empire, and after World War I, it emerged as an independent sheikhdom under the protection of the British Empire. Kuwait's large oil fields were discovered in the late 1930s.