Terrain of Turkmenistan consists of a flat-to-rolling sandy
desert, the
Karakum, with its
dunes slowly rising to the south; by the time they reach the border with
Iran, they become the mountains known as the
Kopet Dag. The
Caspian Sea washes the western shores of this mostly
arid country. Turkmenistan's average elevation is above sea level, with its highest point being
Mount Aýrybaba () in the
Köýtendag Range of the
Pamir-Alay chain in the south-east, and its lowest point being the Akjagaýa Depression in
Sarygamysh Lake, close to below sea level (the actual water level in Sarygamysh Lake fluctuates widely from –110 m at its shallowest to –60 m ().
Mount Arlan rises sharply above sea level in the
Great Balkan Range in western Turkmenistan (
Balkan Province), and has a topographical prominence only slightly shorter than its height. Nearly 80% of the republic lies within the
Turan Depression, which slopes from south to north and from east to west. Turkmenistan's mountains include of the northern reaches of the Kopet Dag Range, which it shares with Iran. The Kopet Dag Range is a region characterized by foothills, dry and sandy slopes, mountain plateaus, and steep ravines;
Mount Şahşah (), also known as
Mount Rizeh, southwest of
Ashgabat, is the highest elevation of the Kopet Dag Range in Turkmenistan. The Kopet Dag is undergoing tectonic transformation, meaning that the region is threatened by
earthquakes such as the one that destroyed Ashgabat in 1948. The
Krasnovodsk and
Üstýurt plateaus are the prominent topographical features of northwestern Turkmenistan. A dominant feature of the republic's landscape is the Garagum Desert (also known as
Karakum), which occupies about . Shifting winds create desert mountains that range from in height and may be several kilometers in length. Chains of such structures are common, as are steep elevations and smooth, concrete-like clay deposits formed by the rapid evaporation of flood waters in the same area for a number of years. Large marshy salt flats, formed by capillary action in the soil, exist in many depressions, including the
Garaşor, which occupies in the northwest. The
Sandykly Desert west of the
Amu Darya river is the southernmost extremity of the
Qizilqum Desert, most of which lies in Uzbekistan to the northeast. ==Climate==