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Yu is Yu the Great, a Chinese deity and author of the Yu Gong, the geography chapter of the Book of Documents, dating to the 4th or 5th century BCE. The Hainei Huayi Tu map is lost, but a later map of China from the Southern Song period, the Huayi tu map engraved in 1136 on a stele, contains names of foreign places inscribed on the edges that ...
Geography of China; Continent: Asia: Region: East/Southeast Asia: Coordinates: 1]: Area: Ranked 3/4: • Total: 9,596,960 [1] km 2 (3,705,410 sq mi): • Land: 97.2 [1] %: • Water: 2.8 [1] %: Coastline: 14,500 [1] km (9,000 mi): Borders: Afghanistan, Bhutan, Myanmar, India, North Korea, Kazakhstan, Kyrgyzstan, Pakistan, Laos, Mongolia, Nepal, Russia, Tajikistan, Vietnam: Highest point: Mount ...
Only in some pockets of the Dzungaria region of Xinjiang is the conspicuous seasonal variation in precipitation that defines Chinese (and, to a large extent, East Asian) climate absent. Annual sunshine duration ranges from less than 1,100 hours in parts of Sichuan and Chongqing to over 3,400 hours in northwestern Qinghai.
Chinese geography texts (1 C, 1 P) Time in China (13 P) Pages in category "Geography of China" The following 28 pages are in this category, out of 28 total.
An enlargeable map of the People's Republic of China. The following outline is provided as an overview of and topical guide to China: . The People's Republic of China is the most extensive country in East Asia and the third most extensive country in the world.
The Commentary on the Water Classic (Chinese: 水经注), or Commentaries on the Water Classic, [1] commonly known as Shui Jing Zhu, is a work on the Chinese geography in ancient times, [2] describing the traditional understanding of its waterways and ancient canals, compiled by Li Daoyuan during the Northern Wei dynasty (386–534 AD).
The Taihang Mountains (Chinese: 太行山; pinyin: Tàiháng Shān) are a Chinese mountain range running down the eastern edge of the Loess Plateau in Shanxi, Henan and Hebei provinces. The range extends over 400 kilometres (250 mi) [ 1 ] from north to south and has an average elevation of 1,500 to 2,000 metres (4,900 to 6,600 feet).
The North China Plain (simplified Chinese: 华北平原; traditional Chinese: 華北平原; pinyin: Huáběi Píngyuán) is a large-scale downfaulted rift basin formed in the late Paleogene and Neogene and then modified by the deposits of the Yellow River. It is the largest alluvial plain of China.
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