DORNOGOBI
Dornogobi Aimag covers 109,500 square kilometers and has an estimated 51,500 inhabitants. The administrative center is Sainshand town 470 kilometers from Ulaanbaatar. The aimag is in the Gobi of eastern Mongolia. It has 600km long border with on China. Lots of people visits so many our aimag energy of center, danzanrawjaa museum, khamar of monastery, burdene fountain, ergeliin zoo, suihent, ikh nart tsonjiin chuluu e.t.c
Large sand dunes of the Gobi
Burdene Bulag includes some the largest and most extensive sand dunes of the Gobi desert. The sand is used for nervous a kidney diseases with a Sanitarium.

Ergeliin zoo
The rocks of Ergeliin Zoo Natural Reserve are World famous for its palaeontological remains of Dinosaurs of the Mesozoic Era. The Natural Reserve was declared in 1996, and covers 60.900hectares of land 30 kilometers northwest of the center of Khatanbulag Soum. The northern slope is sheer. Giant dinosaurs lived here in the Mesozoic Era. New finds of ancient animals are reported here.
Hamariin hiid (monastery)
It is a monastery in which Noyon Hutagt Danzanravjaa, a Mongolian genius of the 19th century, put his famous play ‘Saran Huhuu in 1830. Tudev, who was Danzanravjaa’s disciple, saved the books and the gods of the monastery and inherited them to his offspring. His children returned the valuables to the monastery in 1990 when the monastery reopened.


Danzanravjaa Museum (In Sainshand, centre of Dorno-Gobi aimag). Objects used and created by 19th century Mongolian renowned spiritual leader and Great saint of the Gobi Danzanravjaa were preserved secretly by seven generations of curators until the period of democratic reforms in 1990, when the last of these, Z. Altangerel, unearthed the more than 1500 objects and opened a museum on the basis of this collection. Many dozens of foreign and local tourists come to visit this museum, and from their reception, funds to protect and restore the local natural area are being obtained.
2. Tsonjin Chuluu
This rock has basalt formations with an amazingly regular hexagonal columnar structure resembling six-sided symmetrical crystals. Such columnar structure is created by the systematic contraction and cracking of basalt lava under stress while it is cooling soon after solidifying. There are not many such rocks in the world, but a few others can be found in Mongolia.