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About Singapore
Singapore, city-state located at the southern tip of the Malay Peninsula, about 85 miles (137 kilometres) north of the Equator. It consists of the diamond-shaped Singapore Island and some 60 small islets; the main island occupies all but about 18 square miles of this combined area. The main island is separated from Peninsular Malaysia to the north by Johor Strait, a narrow channel crossed by a road and rail causeway that is more than half a mile long. The southern limits of the state run through Singapore Strait, where outliers of the Riau-Lingga Archipelago—which forms a part of Indonesia—extend to within 10 miles of the main island.
Singapore is the largest port in Southeast Asia and one of the busiest in the world. It owes its growth and prosperity to its focal position at the southern extremity of the Malay Peninsula, where it dominates the Strait of Malacca, which connects the Indian Ocean to the South China Sea. Once a British colony and now a member of the Commonwealth, Singapore first joined the Federation of Malaysia on its formation in 1963 but seceded to become an independent state on August 9, 1965.
Nearly two-thirds of the main island is less than 50 feet (15 metres) above sea level. Timah Hill, the highest summit, has an elevation of only 531 feet (162 metres); with other peaks, such as Panjang and Mandai hills, it forms a block of rugged terrain in the centre of the island. To the west and south are lower scarps with marked northwest-southeast trends, such as Mount Faber. The eastern part of the island is a low plateau cut by erosion into an intricate pattern of hills and valleys. These physical units reflect their geologic foundations: the central hills are formed from granite rocks, the scarp lands from highly folded and faulted sedimentary rocks, and the eastern plateau from uncompacted sands and gravels.
Drainage and soils
A dense network of short streams drains the island, but floods are locally severe because the streams have low gradients and because of excessive water runoff from cleared land. Many streams, especially those draining northward, have broad mangrove-fringed estuaries that extend far inland. None of the soils is even reasonably fertile, but those derived from the granites tend to be better than most. Soils developed from the sedimentary rocks are variable, but many contain hardpans that restrict plant roots and impede soil drainage. The soils of eastern Singapore are extremely infertile. All have suffered extensive degradation through erosion as a result of generations of careless human exploitation.
The population of Singapore is diverse, the result of considerable past immigration. Chinese predominate, making up some three-fourths of the total. Malays are the next largest ethnic group, and Indians the third. None of those three major communities is homogeneous. Among the Chinese, more than two-fifths originate from Fujian province and speak the Amoy (Xiamen) dialect, about one-fourth are Teochew from the city of Shantou in Guangdong province, and a smaller number are from other parts of Guangdong. The Chinese community as a whole, therefore, speaks mutually incomprehensible dialects. Linguistic differences are less pronounced among the Malays, but the group includes Indonesians speaking Javanese, Boyanese, and other dialects. The Indian group is most diverse, consisting of Tamils (more than half), Malayalis, and Sikhs;