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Geography of Barbados : ウィキペディア英語版 | Geography of Barbados
Barbados is a continental island in the North Atlantic Ocean and is located at 13°10' north of the equator, and 59°32' west of the Prime Meridian. As the easternmost isle of the Lesser Antilles in the West Indies, Barbados lies 100 kilometres (62 mi) east of the Windward Islands and Caribbean Sea.〔(【引用サイトリンク】title=Windward Islands )〕 The maritime claim for Barbados is a territorial sea of , with an exclusive economic zone of , this gives Barbados a total maritime area of 183,436 km2. Of the total EEZ area 70,000 km2, is already set aside for offshore oil exploration. A pending application to UNCLOS has placed for consideration a continental shelf to the east and south (or to the edge of the continental margin). To the west, however, most of Barbados' maritime boundaries consist of median lines with neighbours. These neighbours include: Martinique, and Saint Lucia to the northwest, Saint Vincent and the Grenadines to the west, Trinidad and Tobago and Venezuela to the southwest, and Guyana to the southeast. Barbados' total land area is , and it has a coastline of length.〔()〕 Sometimes compared to a pear or leg of mutton for its physical shape. Along the north-south axis Barbados has a maximum length of , and east-west maximum breadth of . ==Physical characteristics== The physical characteristics of Barbados are its lowlands or gently sloping, terraced plains, separated by rolling hills that generally parallel the coasts. Elevations in the interior range from 180 to 240 metres above sea level. Mount Hillaby is the highest point at 340 metres above sea level. Farther south, at Christ Church Ridge, elevations range from sixty to ninety metres. Eighty-five percent of the island's surface consists of coralline limestone twenty-four to thirty metres thick; Scotland District contains outcroppings of oceanic formations at the surface, however. Sugarcane is planted on almost 80 percent of the island's limestone surface. The soils vary in fertility; erosion is a problem, with crop loss resulting from landslides, washouts, and falling rocks. Most of the small streams are in Scotland District. The rest of the island has few surface streams; nevertheless, rainwater saturates the soil to produce underground channels such as the famous Coles Cave.
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