Mongolia - Cretaceous Dinosaur Fossil Sites in the Mongolian Gobi

Bayanshiree N44-16-1320; E109-54-4864; A-730m Khongil Tsav N44-26-1904; E109-51-2928; A-744m Burkhant N44-20-2382; E109-51-3286; A-721m Baishin Tsav N43-30-0064; E107-45-5120; A-905m Khuurai Tsav N43-28-51 E107-44-37; A-904m Urulbu Khudag N43-27-29; E107-24-36; A-970m Shar Tsav N43-34-2845 E107-46-4231; A-896m Amtgai N43-33-5057; E107-54-4247; A-857m Bayanzag N44-08-4251; E103-43-1741; A-1275m Tugrugiin Shiree N44-13-4228; E103-18-0970; A-1043m Nemegt N43-30-0581; E101-02-5971; A-1521m Khermen Tsav N43-28-2896; E99-49-5871; A-991m Bugiin Tsav N43-51-5909; E100-00-3976; A-982m Palaeontologists still continue to discover fossils that prove the current territory of Gobi Desert had a very different climate and environment before 120 to 70 million years ago during the Cretaceous period. 120 million years ago the vast desert basins and valleys contained freshwater rivers and lakes with abundant water resources. And the prevailing humid climate was paradise for plants and animals, including dinosaurs. The fossil evidence of the origin, evolution, migration and extinction of prehistoric creatures are preserved in the sedimentary rocks of the Gobi desert. These evidences give knowledge and understanding of our mother land – the earth, and its history.