Lakes

The Badain Jaran Desert is well known for its numerous scattered and colorful lakes. Containing more than 140 lakes they are mainly found in the southern region in the desert. These lakes can easily be found in the larger valleys between large dunes. They are believed to provide the life sustenance in the desert supporting camels, goats and horses which are herded by nomads that travel through the desert. Most lakes also support a green ring of vegetation that populate the close vicinity around the lakes.

Throughout the desert some lakes change color due to large populations of algae, Brine shrimp and mineral formations at different times in year. Evaporation can also allow others to turn into a hypersaline lake forming a salt crust around the rim of the lake.^[4]

Although their true sources are still debated it is believed that they are being maintained by underground water streams. Most arid deserts in China are surrounded by mountains that provide water sources, and this is the case with the Badain Jaran Desert. Runoff from the mountains is then collected through gravel deposits and this allows them to run through the desert, providing water sources for the scattered oases.

Within the desert there can be two main types of lakes found regarding their morphometry. The largely elongated shallow lakes mainly appear in the megadune area in the southeastern margin of the desert. Their depth often reaches less than 2 meters (6 ft 7 in) and only measure about .2 square kilometers (0.077 sq mi; 49 acres). The oval-shaped, deep lakes can also be found in the compound transverse megadune area. Their maximum depth reaches around 15 meters (49 ft) and attain a maximum size of around 1.5 square kilometers (0.58 sq mi; 370 acres). The lake water can be extremely saline. The shallow lakes in the southeastern region of the desert tend to have low salt concentration, averaging at less than 20 grams per liter (0.67 oz/U.S. qt; 0.80 oz/imp qt). Other lakes can show higher salt concentrations going up to more than 330 grams per liter (11 oz/U.S. qt; 13 oz/imp qt).^[5]

Singing Dunes

The Badain Jaran megadunes is one of the few places where a phenomenon known as the "singing sand dunes", "whistling sands" or "booming dunes", in which the sand emits a sharp, loud noise that can be maintained for more than a minute. Although it is not fully understood, it is believed that it is caused by an electrostatic charge that is generated as wind pulls the top layers of sand down a dune slope. This will produce a low pitched rumble that can reach over 105 decibels. The "singing" starts with an avalanche of sand down the leeward face of a large dune. This phenomenon requires very specific circumstances to generate the sound. The dunes are silent throughout winter when humidity is retained in the sand. In the summer, when the sand is dry, the booming can be generated, but only on a slope of at least 30 degrees or more, on the leeward face of a dune; the same sand on the shallow, windward side cannot generate any noise. This phenomenon is only shared by around 35 other beaches and deserts around the world.

Under the same circumstances, it is also possible to generate another acoustic phenomenon. Moving a hand gently through the dry sand of a "booming sand dune" will shear the upper layer of sand off the slope and generate a burping sound emission (pulse-like, short bursts of sound).^[6]

Dunes

The Badain Jaran Desert is made up of hundreds of dunes ranging from small to large. Most of the megadunes in the desert average about 400 meters (1,300 ft) from the base while the rest average around 200 meters (660 ft). Out of all the megadunes, the Bilutu Peak ("bì lǔ tú fēng", 必鲁图峰) is the most famous. It towers at 500 meters (1,600 ft) from the base and is the tallest dune in Asia, (third tallest in the world). Unlike most of the smaller dunes the Bilutu Peak is stationary which makes it the world's tallest stationary dune.

While the larger megadunes are stationary (with only the top layer of sand shifting), the smaller dunes are constantly shifting according to wind patterns. This makes desertification a problem in surrounding areas as the desert is constantly expanding.^[3]

Badain Jaran Temple

The Badain Jaran Temple in September alongside its lake

The Badain Jaran Temple (bā dān jí lín miào 巴丹吉林庙) is a well-preserved Tibetan-Buddhist temple located in the middle of the desert. It was built in 1868 at the side of a lake. Its isolation allowed it to survive untouched and safe from the Cultural Revolution. The fine state of preservation allows visitors to explore the temples attractions including statues, wood carvings, artifacts and a small white pagoda.

The temple is only accessible by land. Visitors normally reach it by renting a sand jeep at the tourist centers located along the S317 highway. Visitors can also choose to hire a driver for a daily fee. The vehicles available for tourists are 4X4 military jeeps with reinforced frames and deflated tires. These jeeps are able to drive through the desert, ascend and descend sand dunes. They remain operational for many hours. These trips by land include several stops at lakes, scenic spots and the Bilutu Peak.^[4]

Bilutu Peak

View from Bilutu Peak

Bilutu Peak (必鲁图峰) is also a location which is commonly accessed using the sandjeeps. It is the world's highest stationary dune rising 450 meters (1,480 ft) over the surrounding area, and peaking at 1,611 meters (5,285 ft) above sea level.^[8] The surrounding dunes only reach about 200 meters (660 ft). Although the biggest, it is one of several large stationary dunes within the Badain Jaran Desert. Upon reaching the top there will be a clear view of the surrounding dunes as well as several colorful lakes.^[4]

Khara Khoto

Also known as the ancient black city, it is located in the northwestern side of the desert near the Ruo Shui River and is located fairly close to the new city of Ejin. The ancient city was a Tangut city founded in 1032 which became the center of the Tangut empire. When Genghis Khan conquered the city it flourished again under Mongol rule. However, the city fell to Chinese armies in 1372 during the Ming dynasty and was left abandoned and in ruins. It has been untouched since. Although not accessible using the same jeeps, it is possible to find transport in the city of Ejin.^[4]

Jiabiangou Labor Camp

The infamous Jiabiangou Labor Camp was located on the edge of the desert and 27 kilometers (17 mi) from Jiuquan, Gansu. Between 1957 and 1961, the camp was used for "re-education through labor" to imprison intellectuals and former government officials that were declared to be "rightist" in the Anti-Rightist Movement of the Communist Party. Out of 3,000 prisoners, 2,500 died between 1957 and 1960, during the height of the Great Chinese Famine. The remains of the camp and the unmarked graveyards were poorly maintained and are heavily guarded by the Communist Chinese government. Relatives of the dead are only permitted during the time of Qingming. In November 2013, a memorial dedicated to the dead was quickly destroyed by the local government. Many graves and human remains were also removed since then to prevent people from visiting.^[9]