Since they have moved here for 200 years, they inherited and retained so many traditional Mongolian culture. At the same time, they develop the original culture more colorful and create the Snow Mountain Mongolian culture with abundant connotation and bright characteristic.
13 century,Genghis Khan united the Mongolian people and stepped up into world history’s stage. At that time Mongolian costume also entered into a developing period.
The Qunkeqi was a social organization at the basic level of the Mongolian people around Qinghai Lake before,and had changed from the ethnic group to regional group since the beginning of twentieth century.
Archives are the basic historical data of studing history, So this essay is based on remained history data — Haraqin Left Banner's Zhasake government office mongol archives stored by Inner Mongolia Archives, and analyzes Kulaain left Banner of Qing Dynasty social problems, especially the population social stratum, social production and economic, township and township corvee, lamasery and management of lamasery land of Mongols in this Banner.
The specialty of the study of the history of Mongolian society and life (蒙古社会生活史) is that it mostly depends on the analysis of literature which was written by the authors who were not Mongol.
Since the middle 16th century, because of constant contact and communion with the Ming Dynasty and Tibetan Buddhism, not only in religion but also in areas such as medicine, interpretation, historiography,
A landscape model (LANDIS) was used to study the long-term forest dynamics under five planting types (100% larch (P1); 70% larch and 30% Mongolian Scotch pine (Pinus sylvestris var.
Under these planting scenarios, the abundance of larch increased with the increasing proportion of larch, and the abundance of Mongolian Scotch pine was in a similar way.
growing in the Mongolian People's Republic and have been identified by their IR spectra: 1,8-cineole (35%), α-thujone andβ-thujone (11%), (+)-camphor (18%), (-)-α-terpineol (5%), and (-)-terpinen-4-ol (7%).
Together with the Bokson Group, the combined Gorlyk and Ara-Oshei formations, which correlate with the complete Bokson Group, make up the Vendian-Cambrian sedimentary cover of the Tuva-Mongol microcontinent.
Mongol names and toponyms are most often used by paleontologists for designation of new forms of fossil fauna and flora from the Cenozoic of Central Asia.
The plate boundary zone consists of orogenic belts (Mongol-Okhotsk, Selenga-Stanovoi, Transbaikal, and Sikhote-Alin) and margins of the Siberian and North China platforms.