Prehistoric Mongolia

Source: Wikipedia, the free encyclopedia.

The climate of Central Asia became dry after the large tectonic collision between the Indian Plate and the Eurasian Plate. This impact threw up the massive chain of mountains known as the Himalayas. The Himalayas, Greater Khingan and Lesser Khingan mountains act like a high wall, blocking the warm and wet climate from penetrating into Central Asia. Many of the mountains of Mongolia were formed during the Late Neogene and Early Quaternary periods. The Mongolian climate was more humid hundreds of thousands of years ago.

Pre-human history

Mongolia is known to be the source of priceless paleontological discoveries. The first scientifically confirmed dinosaur eggs were found in Mongolia during the 1923 expedition of the American Museum of Natural History, led by Roy Chapman Andrews.

During the middle to late Eocene Epoch, Mongolia was the home of many Paleogene mammals with Sarkastodon and Andrewsarchus being the most prominent of them.

Bronze and Early Iron Age

Neolithic stone amulet, Dornod, Mongolia, 4000-3000 BCE
Khemtseg culture
, Avyn Khukh Uul, Bulgan, Khovd, Mongolia
Sagsai-shaped graves, Tsagaan Asga site

Elbe River
(Mongolian History 2003).

There are different viewpoints about the origins of deer stone art. According to H. L. Chlyenova, the artistic deer image originated from the

Baikal
area (Tseveendorj 1979). D. G. Savinov (1994) and M. H. Mannai-Ool (1970) have also studied deer stone art and have reached other conclusions.

Chronological table of the Bronze and Early Iron Ages of Mongolia.[1]

See also

References

Further reading

  • Ryan Schmidt, UNRAVELING THE POPULATION HISTORY OF THE XIONGNU TO EXPLAIN MOLECULAR AND ARCHAEOLOGICAL MODELS OF PREHISTORIC MONGOLIA (DISSERTATION)

External links