| Turkmenistan | Article View | ||||
| On the File menu, click Print to print the information. | |||||
| II. | Land and Resources |
Turkmenistan covers an area of 488,100 sq km (188,500 sq mi), making it the second largest country in Central Asia, after Kazakhstan. The entire central part of the country is occupied by one of the largest sand deserts in the world, the Garagum. About four-fifths of the country is steppe (semiarid grassy plain) that is part of the southern portion of the vast Turan lowland.
Most of Turkmenistan lies at an elevation of 500 m (1,640 ft) or less. The Akdzhakaya Depression, located in the north central part of the country, is the lowest point in the republic at 110 m (360 ft) below sea level. The Köpetdag mountains, which are prone to violent earthquakes, fringe the Garagum desert along the country’s southern border with Iran. Along the mountain foothills is a belt of oases, which are fed by mountain streams.
| A. | Rivers and Lakes |
Freshwater resources are scant in Turkmenistan, and extensive canal systems are crucial conduits for irrigation and drinking water. The mountain streams of Turkmenistan dissipate upon reaching the arid sands and parched clay of the Garagum, so Turkmenistan’s only significant water sources are rivers that originate in other countries. The Amu Darya, which originates in the mountainous Pamirs region of Tajikistan east of Turkmenistan and forms part of the country’s border with Uzbekistan, and the Murgap, which originates in Afghanistan, are the two largest permanent rivers. Water from the Amu Darya and the Murgap is diverted into the Garagum Canal (built during the Soviet period) to supply water to the arid southern portions of Turkmenistan. Other canals divert water from the Amu Darya in the northern part of the country. The Caspian Sea, a landlocked saltwater lake, forms Turkmenistan’s entire western border. The most prominent feature along the Caspian shoreline is the Garabogazköl Gulf, which occupies a sizable portion of northwestern Turkmenistan.
| B. | Plant and Animal Life |
Plant life is sparse in the vast, arid desert, where only drought-resistant grasses and desert scrub grow. The mountain valleys in the south support wild grapevines, fig plants, and ancient forests of wild walnut trees. The mountain slopes are covered with forests of juniper and pistachio trees. Dense thickets called tugai grow along riverbanks. The wildlife in the mountains of Turkmenistan includes the caracal (or Persian lynx), goats, cheetahs, and snow leopards. In the desert, gazelles, foxes, and wildcats thrive. In the tugai live jackals, wild boar, and the rare pink deer. Reptiles are abundant and include the Central Asian cobra, the desert monitor (a large lizard), several species of gecko (a small lizard), and the tortoise. Migratory birds, such as ducks, geese, and swans, inhabit the Caspian shore during winter.
| C. | Natural Resources |
Turkmenistan has substantial reserves of oil and natural gas in the Caspian Sea area and in the Garagum desert. Other natural resources include deposits of coal, sulfur, magnesium, and salt. Only 5 percent of the country’s total land area is cultivated, nearly all of which (18,500 sq km; 7,143 sq mi) is irrigated.
| D. | Climate |
The climate of Turkmenistan is desert continental, with cold winters and very hot summers. For most of the country, the average daily temperature in January ranges from -6° to 5°C (21° to 41°F), while in July it is 27° to 32°C (81° to 90°F). Average annual precipitation ranges from 80 to 400 mm (3 to 16 in), although two-thirds of the country receives 150 mm (6 in) or less.
| E. | Environmental Issues |
Turkmenistan suffers from a number of serious environmental problems, many of which stem from decades of economic mismanagement under Soviet planning. Excessive irrigation has severely degraded soil and water quality in Turkmenistan. Irrigation of the naturally saline soil has brought underground salts to the surface, making the soil even more saline while also making irrigation more necessary. Thus, excessive irrigation has contributed to desertification (a process whereby arable land becomes desert, or arid salt flats). In addition, Turkmenistan’s soil has become heavily contaminated with agricultural chemicals, such as pesticides and herbicides, that are applied in large doses to cotton crops. These agricultural chemicals also contaminate the water supply, mainly through irrigation runoff. Untreated wastewater also pollutes groundwater, although there has been some improvement in northern Turkmenistan since the 1995 opening of a new water-treatment plant near Dashhowuz, constructed with aid from the United States. Since the late 1980s environmental awareness has been growing in Turkmenistan. The government has a ministry in charge of environmental protection, but only a small portion of the national budget is allocated for this purpose.
Turkmenistan is also involved in a regional effort to address the problem of the Aral Sea. This saltwater lake in Uzbekistan and Kazakhstan has shrunk to less than half of its former size since the early 1960s. The greatest single contributor to the drying of the Aral is Turkmenistan’s Garagum Canal, which receives more water from the Amu Darya (one of two inflow sources for the Aral) than any other irrigation structure in the Aral Sea basin. The drying of the Aral Sea is considered one of the worst ecological disasters in the world.