OvooOvoo, oboo, or obo (овоо, , обоо, обаа, Traditional Mongol: , "heap"; Chinese: 敖包 áobāo, lit. "magnificent bundle [i.e. shrine]") are cairns used as border markers or shrines in Mongolian folk religious practice and in the religion of other Mongolic peoples. While some ovoos simply consist of a mound of stones, most have branches and khadag stuck into them. In the absence of stones, ovoos can be made entirely of branches, or even soil or sand. Ovoos are often found at the top of mountains and in high places, like mountain passes.
WuhaiWuhai (; Üqai qota, Mongolian cyrillic.Үхай хот) is a prefecture-level city and regional center in the Inner Mongolia Autonomous Region, China, and is by area the smallest prefecture-level division of the region. It is located on the Yellow River between the Gobi and Ordos deserts. Wuhai became a single city occupying both banks of the Yellow River with the amalgamation on 1976 of left-bank (west) Wuda (then administrated by Bayan Nuur League) together with Haibowan on the right (east) bank (then administrated by Ikh Juu league).
Evenki languageEvenki eɪˈvɛnki (Ewenkī), formerly known as Tungus or Solon, is the largest member of the northern group of Tungusic languages, a group which also includes Even, Negidal, and the more closely related Oroqen language. The name is sometimes wrongly given as "Evenks". It is spoken by Evenks or Ewenkī(s) in Russia and China. In certain areas the influences of the Yakut and the Buryat languages are particularly strong. The influence of Russian in general is overwhelming (in 1979, 75.2% of the Evenkis spoke Russian, rising to 92.
DatongDatong is a prefecture-level city in northern Shanxi Province in the People's Republic of China. It is located in the Datong Basin at an elevation of and borders Inner Mongolia to the north and west and Hebei to the east. As of the 2020 census, it had a population of 3,105,591 of whom 1,790,452 lived in the built-up (or metro) area made of the 2 out 4 urban districts of Pingcheng and Yungang as Yunzhou and Xinrong are not conurbated yet. The area of present-day Datong was close to the state of Dai, which was conquered by the Zhao clan of Jin in 457 BC.
XinzhouXinzhou, ancient name Xiurong (秀荣), is a prefecture-level city occupying the north-central section of Shanxi Province in the People's Republic of China, bordering Hebei to the east, Shaanxi to the west, and Inner Mongolia to the northwest. Xinzhou has a continental, monsoon-influenced semi-arid climate (Köppen BSk), with cold, very dry, and somewhat long winters, and warm, somewhat humid summers. The monthly 24-hour average temperature ranges from in January to in July, and the annual mean is .
HetaoHetao () is a C-shaped region in northwestern China consisting of a collection of flood plains stretching from the banks of the northern half of the Ordos Loop, a large northerly rectangular bend of the Yellow River, that forms the river's entire middle section. The region makes up the northern margin of the Ordos Basin, bounded in the west by the Helan Mountains, the north by the Yin Mountains, the east by the northern portion of Lüliang Mountains, and the south by the Ordos Desert and the Loess Plateau (separated by the course of the Ming Great Wall).
ManzhouliManzhouli (; Манжуур хот; ) is a sub-prefectural city located in Hulunbuir prefecture-level city, Inner Mongolia Autonomous Region, China. Located on the border with Russia, it is a major land port of entry. It has an area of and a population of almost 250,000 (in 2010). In ancient times the area was inhabited by the Donghu, Xiongnu, Xianbei, Khitan, Jurchen, Mongols and Manchu. During the decline of China's last dynasty, the Russian Empire forced the Qing (1644–1912) to cede Russian Manchuria in the 1858 Treaty of Aigun.
North China CratonThe North China Craton is a continental crustal block with one of Earth's most complete and complex records of igneous, sedimentary and metamorphic processes. It is located in northeast China, Inner Mongolia, the Yellow Sea, and North Korea. The term craton designates this as a piece of continent that is stable, buoyant and rigid. Basic properties of the cratonic crust include being thick (around 200 km), relatively cold when compared to other regions, and low density.
