8 places in 7 countries · updated 13 October 2026
In short: By our ranking, the most beautiful dunes in Asia are Tottori Sand Dunes (Japan), Badain Jaran Desert (People's Republic of China) and Wahiba Sands (Oman). The list covers 8 dunes in 7 countries. The People's Republic of China has the most, with 2. Last updated 13 October 2026.
Asia holds some of the tallest and most varied sand dunes on Earth. The deserts of Inner Mongolia, the Gobi and Central Asia sit far from the sea in the rain shadow of great mountain ranges, so wind has had millions of years to pile sand into mountains of its own. Around the Arabian Peninsula, monsoon and trade winds shape long linear ridges, and even humid Japan has coastal dunes built by rivers and winter winds from the Sea of Japan. Several of these dunes sing, roaring or humming when the sand slides.
The Badain Jaran Desert in China has some of the tallest stationary dunes in the world, standing hundreds of metres high, with more than a hundred lakes fed by groundwater in the hollows between them. Khongoryn Els in Mongolia's Gobi is a belt of high dunes stretching for about a hundred kilometres along the foot of the mountains, and the Singing Sand Dunes of Dunhuang curve around the small Crescent Lake at the Silk Road oasis of Dunhuang. In Oman, the Wahiba Sands are long parallel ridges of orange sand that run north to south.
The other dunes stand apart for their setting. The Moreeb Dune in the Liwa Oasis of the United Arab Emirates is a single towering slope of red sand. The Tottori Sand Dunes run along Japan's Sea of Japan coast, its slopes rippled by wind into fine patterns. Sarykum in Dagestan is a lone dune rising from the foothills of the Caucasus, and the Singing Dune in Kazakhstan's Altyn-Emel National Park hums in dry weather between low mountains in the Ili River valley.
In this list
| # | Place | Type | Country | UNESCO |
|---|---|---|---|---|
| 1 | Tottori Sand Dunes | Dune | Japan | |
| 2 | Badain Jaran Desert | Dune | People's Republic of China | |
| 3 | Wahiba Sands | Dune | Oman | |
| 4 | Singing Sand Dunes | Dune | People's Republic of China | |
| 5 | Khongoryn Els | Dune | Mongolia | |
| 6 | Moreeb Dune | Dune | United Arab Emirates | |
| 7 | Sarykum | Dune | Russia | |
| 8 | Natural Monument «Singing barchans» | Dune | Kazakhstan |
Japan · 4.4 km from Tottori35.540° N 134.227° E

The landscape rewards close looking. The second ridge of dunes, known as Uma-no-se, "the horse's back", rises in a wall of sand some 46 metres high, and from its crest you look straight out to the sea. Wind of moderate strength draws fine ripples called fūmon across the surface; after rain, as damp sand dries, it slides away in rows of little curtains known as saren. In the hollows behind the ridge, groundwater seeps up to form the "oasis", a pool that can be over a metre deep in winter and vanishes in summer. On summer nights the lights of squid-fishing boats line the horizon.
Did you know? By 1991 about 42 percent of the dunes had turned to grassland, and regular weeding by the prefecture and city began in 1994.
People's Republic of China40.072° N 102.210° E

The combination is what makes the landscape so extraordinary: a steep golden dune falling straight into a pool of blue, green or rust-red water, . Rainfall here is only about 50–60 mm a year, and evaporation is many times greater, so the lakes are fed by groundwater whose origin scientists still debate. Their chemistry varies enormously, from almost fresh to brines of more than 330 grams of salt per litre, so that lakes a short walk apart can be entirely different in character. Some slopes also sing: in dry summer conditions the sand sliding down steep leeward faces produces a low booming rumble that can exceed 105 decibels.
Did you know? The World Heritage property alone covers about 7,260 square kilometres, surrounded by an even larger buffer zone.
Oman22.000° N 58.833° E

The desert is young in geological terms. It took shape during the Quaternary under two opposing winds — the south-west monsoon and the northern shamal — and the tall northern ridges formed after the last regional glaciation, piling up where the strongest winds lost speed and dropped their sand. Geographers divide it into a higher northern Wahiba and a lower southern one according to the shape of the dunes. Beneath the loose surface lies an older layer of cemented carbonate sand, and river-borne deposits thought to come from the ancient Wadi Batha have been found some 200 metres below the surface in the centre of the desert.
Did you know? Researchers in the 1980s described that aeolianite as the most extensive continuous deposit of its kind then identified anywhere in the world.
People's Republic of China · 6.5 km from Dunhuang40.085° N 94.675° E

The name describes a real phenomenon. When wind moves the sand, or when people slide down the slopes, the dry grains can produce a low humming or drumming sound, and these dunes are counted among the four famous singing sands of China. Their old name was the "Gods' Sand Dunes"; the historian Sima Qian, in the Records of the Grand Historian, wrote of a sound like music heard in fine weather, and the present name dates from the Ming dynasty. They are also listed among the Eight Great Landscapes of Dunhuang.
Did you know? For sand to sing, its grains generally need to be rounded, about 0.1 to 0.5 millimetres across, rich in silica and dry enough.
Mongolia43.500° N 103.167° E

The dunes are better known in Mongolia as Duut Mankhan, the "singing sands". When the wind shifts the surface, or when a climber sends a slip of sand down a steep lee slope, the grains give out a deep, sustained hum that people have compared to the drone of a distant aircraft. Explanations vary: one French study pointed to a fine coating on the grains that makes them resonate as they slide, while others stress the role of heat and dry weather. Either way, the long walk up a crest, two steps up and one slipping back, is rewarded by the noise of the descent as much as by the view.
Did you know? Published figures for its length vary widely, from about 100 kilometres to as much as 180 kilometres.
United Arab Emirates22.980° N 53.786° E

What makes the place so striking is scale rather than any single feature. The dune stands like a wall above the flat ground at its foot, and the low sun of early morning and late afternoon brings out its texture: the ripples on the flanks, the sharp edge of the crest and the shadow that fills the hollow below. From the top the view runs over ridge after ridge of the Empty Quarter.
Did you know? Around 2001 local Emiratis began racing cars and motorbikes up the dune, when the only challenge was to reach the top.
Russia · 21.5 km from Buynaksk43.007° N 47.229° E

How it came to be here is still debated. One explanation, put forward by scientists in the nineteenth and twentieth centuries, credits wind working the sands over an immense span of time; another traces the sand to the breakdown of the sandstones of the surrounding hills. Either way, the dune is very old, and wind still carves its crest into ripples and sharp ridges.
Did you know? The same study found that the dune grew most actively when the level of the Caspian Sea fell, exposing more sand to the wind.
Kazakhstan43.867° N 78.567° E

The dune owes its existence to the wind. Gusts sweeping through this part of the Ili valley lift sand from the river's shoals and carry it north until they meet the angled walls of the two Kalkan ridges, where they slacken and drop their load. Over thousands of years this trap has built a crescent-shaped barchan that, unlike most dunes, does not wander across the plain but stays in place. Its south-western face is smooth, while the north-eastern side is broken into several gentler crests. The sound comes from grains rubbing against one another as large masses of dry sand move; the more sand in motion, the louder the note, from a faint squeak to a rumble.
Did you know? The dune's voice drew scientific attention early: in 1962 the Leningrad physicist V. Arabadzhi carried out a series of observations of its sound.
Places are chosen for how they look, not for how famous they are: each one has its own description and a photograph credited to its author. The order is a single world ranking that weighs the beauty of the place in curated photography together with how widely it is documented — the number of language editions of its encyclopedia article and how often that article is read in a year. The list is rebuilt as places are added, so the order and the counts on this page are always current.