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The People's Republic of China has an area of about 9,600,000 km 2 (3,700,000 sq mi). The exact land area is sometimes challenged by border disputes, most notably about Taiwan, Aksai Chin, the Trans-Karakoram Tract, and South Tibet. The area of the People's Republic of China is 9,596,960 km 2 (3,705,410 sq mi) according to the CIA's The World ...
The Alashan Plateau semi-desert lies to the east, and the Emin Valley steppe to the west, on the China-Kazakhstan border. Tian Shan range, separates the Dzungarian Basin semi-desert from the Taklamakan Desert, which is a low, sandy desert basin surrounded by the high mountain ranges of the Tibetan Plateau to the south and the Pamirs to the
The Classic of Mountains and Seas, also known as Shanhai jing, [1] formerly romanized as the Shan-hai Ching, [2] is a Chinese classic text and a compilation of mythic geography [3] [4] and beasts. Early versions of the text may have existed since the 4th century BCE, [5] [6] but the present form was not reached until the early Han dynasty. [6]
The geomorphology of China can be divided into several parts. The historical centre of Chinese culture is on the loess plateau, the world's largest Quaternary loess deposit, and on the alluvial lands at the east of it. The alluvial East China plain extends from just south of Beijing in the north, to the Yangtze River delta in the south ...
The Taklamakan Desert has an area of 337,000 km 2 (130,000 sq mi), [11] making it slightly smaller than Germany. The desert is part of the Tarim Basin, which is 1,000 kilometres (620 mi) long and 400 kilometres (250 mi) wide. It is crossed at its northern and at its southern edge by two branches of the Silk Road, by which travellers sought to ...
The Sacred Mountains of China are divided into several groups. The Five Great Mountains ( simplified Chinese: 五 岳; traditional Chinese: 五 嶽; pinyin: Wǔyuè) refers to five of the most renowned mountains in Chinese history, [1] which have been the subjects of imperial pilgrimage by emperors throughout ages. They are associated with the ...
Owing to tremendous differences in latitude, longitude, and altitude, the climate of China is extremely diverse. It ranges from tropical in the far south to subarctic in the far north, and alpine in the higher elevations of the Tibetan Plateau. Monsoon winds, caused by differences in the heat-absorbing capacity of the continent and the ocean ...
The map shows topographic features such as mountains, waterways and roads, and is believed to cover the Qin state of the Warring States period. Han dynasty maps Silk map from Mawangdui, dating back to circa 168 BC. Concrete evidence of the existence of maps in ancient China dates back to the Han dynasty (206 BC – 220 AD
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