Page 30 - Life & Land Use on the Bahrain Islands (Curtis E Larsen)
P. 30

2. Bahrain—The Present

















                  The Bahrain Islands occupy the mouth of a shallow bay approximately midway along
                  the western shore of the Persian-Arabian Gulf and 25 km east of the Saudi Arabian
                  coast. While the political boundaries encompass many small islands and reefs, the
                  most noticeable human activity involves only six of the total (fig. 1). The largest
                  and most heavily populated Island is Bahrain itself. It is 50 km long and 20 km wide
                  and is oriented essentially north-south. Bahrain is joined by causeways to two
                 smaller but important Islands, Muharraq and Sitra. The former lies directly
                  opposite the city of Manama at the northeast shore of Bahrain. The city of
                  Muharraq, on the southwest shore of Muharraq Island, is included with Manama as
                 the urban center of the islands. Muharraq Island and Bahrain enclose a sheltered
                 harbor for coastal shipping. Sitra Island, located due south of Muharraq, is
                 separated from Bahrain by 300 to 400 m of intertidal zone. Sitra is also the site of
                 a refinery and docking facility for the Bahrain Petroleum Company. Other
                 important islands are Nabih Salih, Jidda, and Umm an-Nassan. In addition, Bahrain
                 claims a group of smaller islands 1.5 km from the west coast of Qatar. These are
                 the Hawar Islands.
                          Bahrain occupies a strategic position in the gulf. Its central location and
                 closeness to the Arabian mainland makes it a useful exchange point and service
                 center for international maritime interests. Accordingly, it has an international
                 appearance provided by a population with sizable minorities of Persians, Pakistanis,
                 Indians, and Europeans.
                          Geologically, Bahrain is an elongated dome created by folding of Tertiary
                 limestones and shales but with a central erosional depression. Barren limestone
                 slopes rise gently inland away from the coastal plains until they reach the rimrocks
                 of the central depression. Cultivatable soils are found both within the central




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