Badain Jaran, Gobi, Lop, and Taklamakan are major Chinese what?
Badain Jaran Desert the dunes also contribute to maintain their fixed state. This rigid structure also allows peaks, cliffs, gullies and even caves to form as a result of water erosion and desertification. The Badain Jaran Desert, like the Tengger Desert which lies to the east (and with which the Badain Jaran Desert is currently merging due to extensive desertification) is about one-half barren, sandy desert and one-half a mixture of solid bedrock and loose gravel. Several small lakes and oases scatter the desert around which limited vegetation is able to grow. The Badain Jaran Desert is well known for its numerous scattered
Badain Jaran Desert Badain Jaran megadunes is one of the few places where a phenomenon known as the "singing sand dunes", "whistling sands" or "booming dunes". This rare occasion emits a sharp, loud noise that can be maintained for more than a minute. Although it is not widely 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 dunes will manifest itself by initiating an avalanche of sand down the leeward