Myanmar
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Myanmar
II. Land and Resources

The total area of Myanmar is 676,552 sq km (261,218 sq mi). From north to south, Myanmar stretches about 2,085 km (about 1,295 mi); from east to west, the distance is about 930 km (about 575 mi). The coastal region is known as Lower Myanmar, while the interior region is known as Upper Myanmar. A horseshoe-shaped mountain complex and the valley of the Irrawaddy River system are the country’s dominant topographical features. The mountains of the northern margin rise to 5,881 m (19,295 ft) atop Hkakabo Razi, the highest peak in Southeast Asia. The two other mountain systems have northern to southern axes. The Arakan Yoma range, with peaks mostly between 915 m (3,000 ft) and 1,525 m (5,000 ft), forms a barrier between Myanmar and the subcontinent of India. The Bilauktaung Range, the southern extension of the Shan Plateau, lies along the boundary between southwestern Thailand and southeastern Lower Myanmar. The Shan Plateau, originating in China, has an average elevation of about 1,215 m (about 3,986 ft).

Generally narrow and elongated in the interior, the central lowlands attain a width of about 320 km (about 200 mi) across the Irrawaddy-Sittang delta. The deltaic plains, extremely fertile and economically the most important section of the country, cover an area of about 47,000 sq km (about 18,000 sq mi). Both the Arakan (in the northwest) and the Tenasserim (in the southwest) coasts of Myanmar are rocky and fringed with islands. The country has a number of excellent natural harbors.

A. Plant and Animal Life

Forests cover 49 percent of Myanmar. In Lower Myanmar, the dense tropical forests contain extensive stands of timber and oil-bearing trees, including commercially valuable teak forests. Other trees include rubber, cinchona, acacia, bamboo, ironwood, mangrove, coconut, betel palm, and, chiefly in the northern highlands, oak, pine, and many species of rhododendron. Tropical fruits such as citrus, bananas, mangoes, and guavas grow in the coastal regions. Vegetation in the arid regions is sparse and stunted. One consequence of Myanmar’s slow economic growth has been the preservation of much of the natural environment.

Jungle animals such as the tiger and leopard are common in Myanmar. Among the larger native animals, found mainly in the highlands of Upper Myanmar, are the elephant, rhinoceros, wild buffalo, wild boar, and several species of deer and antelope. Elephants, tamed or bred in captivity, are used as work animals, particularly in the lumber industry. Smaller animals include the gibbon, which is a small species of ape that lives in trees, several species of monkey, the wildcat, the flying fox, and the tapir. Myanmar has 867 known varieties of birds, including parrots, peafowl, pheasants, crows, herons, and paddybirds. Among typical reptiles are crocodiles, geckos, cobras, pythons, and turtles. Edible species of freshwater fish are plentiful.

B. Natural Resources

The most important resources of Myanmar are agricultural. There are approximately 250 commercially useful kinds of trees, 50 of which have been exploited. The most important forest resource is teak, of which Myanmar holds the majority of the world’s remaining supply. Important mineral resources are petroleum and natural gas, along with tin, antimony, zinc, copper, tungsten, lead, coal, and small amounts of marble and limestone. Myanmar is an outstanding source of jade and natural rubies.

Myanmar’s richest soils are found in a narrow alluvial strip along the Bay of Bengal, where mountain streams irrigate the land in the wide Irrawaddy and Sittang river valleys. These deep deposits form a vast, fertile belt especially suitable for rice cultivation because of the abundant moisture.

C. Climate

The climate of Myanmar and other countries in South and Southeast Asia follows a monsoon pattern. During the half of the year that the sun’s rays strike directly above the equator, the land mass of Asia is heated more than is the Indian Ocean. This draws moist hot air from over the ocean onto the land, bringing the rains of the southwest monsoon. When the tilt of the earth brings the direct sun rays south of the equator, the heating of the Indian Ocean draws the cooler dry air of the northeast monsoon from the highlands of Asia across the countries of South and Southeast Asia. As a result, Myanmar has three seasons: hot and wet, warm, and very hot. During the hot, wet season, from mid-May to October, rain usually falls every day and sometimes all day. Almost all of Myanmar’s annual rainfall falls during this time. In the cooler season, which runs from late October to mid-February, the temperature for January averages 25°C (77°F) in Yangon in Lower Myanmar and 20°C (68°F) in Mandalay in Upper Myanmar. The hottest season runs from late February to early May. At the end of this season, the average monthly temperature reaches the upper 30°s C (lower 100°s F) in many parts of Myanmar. By July rains have brought the average temperature down to 29°C (84°F) in Mandalay and 27°C (81°F) in Yangon. Average annual rainfall varies from about 5,000 mm (about 200 in) on the Tenasserim Coast to about 760 mm (about 30 in) at Mandalay.

D. Environmental Issues

Although rich in natural resources, Myanmar is among the most impoverished countries in Asia. Only 78 percent (2004) of Myanmar’s citizens have access to safe water, and only 77 percent (2004) of the population is serviced by adequate sanitation systems. Waterborne infectious diseases are a significant health problem throughout Myanmar. The country has a high rate of infant mortality, with 51 (2007) infants dying out of every 1,000 born.

Myanmar is being deforested at a rate of 1.19 percent (1990–2005) every year. Teak wood is in high demand worldwide, and most of the world’s remaining teak trees are in Myanmar. Forests are also being consumed for fuel.

Only 0.3 percent (2004) of Myanmar’s land is officially protected. Myanmar is inhabited by 147 (2004) threatened animal species. Myanmar has ratified international agreements pertaining to biodiversity, tropical forests, marine pollution, and the ozone layer.