Ancient China

China was one of the earliest centers of human civilization, and became a large united country with an advanced culture at a very early stage, outpacing the rest of the world in areas like art and science.

Since around 1000 BC China consisted of many small kingdoms. All of these were unified under one emperor in 221 BC by the Qin state, ushering in the Qin Dynasty. Over the course of centuries, China underwent periods of unity and disunity, order and disorder.

In the 18th century, China achieved a decisive technological advantage over the peoples of Central Asia, while simultaneously falling behind Europe technologically. This set the stage for the 19th century, in which China adopted a defensive posture against European imperialism while simultaneously extending control into Central Asia.

In the early 20th century, the institution of the Emperor of China disappeared, and China entered a period of disunion started by the Chinese Civil War. There are now two nations which lay formal claim to the title of "China": the People's Republic of China (also called "Mainland China") and the pre-revolution government of the Republic of China which administers Taiwan and several small islands of Fujian.

After the Qin Empire unification, China experienced about 13 more dynasties, many of which includes extensive system of kingdoms, principalities, dukedoms, earldoms, and marquisates. However, ultimately, the emperor had the centralized authority. The emperor also consulted civil and martial ministers, especially the prime minister. Sometimes political power, however, fell into the hands of the officials, eunuchs, or relatives.

Political relations with dependencies (tributary kingdoms) were maintained by international marriages, military aids, and gifts.

Territory

Originally in the Zhou Dynasty, China was the region around the Yellow River. The territory since then had been expanding from the West outward in all directions, and was largest during the Tang, Yuan, and Qing Dynasties. From the Chinese point of view, the "Chinese" Empire included parts of modern far eastern Russia and Central Asia during the strongest periods of the Yuan, although China was merely one of many territories of the Mongol Empire.

Like provincial administrators, some foreign monarchs sent envoys to offer gifts to the Emperor of China and the Emperor returned compliments to them. The Chinese ostensibly saw that barbarians attached themselves to the virtue of the Emperor, while the foreign governments sometimes had different perspectives. Since the end of the 19th century, China has tried to interpret this relationship as suzerainty-dependency based on Western international law.

The Qing Empire reduced the territorial value of Great Wall as a barrier of China proper. In 1683, Taiwan became a part of the Qing Empire, originally as a prefecture, then two.

Top-level political divisions of China have altered as the administration changed. Top levels inclduded circuits and provinces. Below that, there have been prefectures, subprefectures, departments, commandries, districts, and townships. Recent divisions include counties and cities.

China contains a large variety in landscapes, with mostly plateaux and mountains in the west, and lower lands on the east. As a result, principal rivers flow from west to east (Chang Jiang, the Huang He (of central-east), the Amur (of northeast), etc), sometimes to south (Pearl River, Mekong River, Brahmaputra, etc). All rivers empty into the Pacific.

In the east, along the shores of the Yellow Sea and the East China Sea are found extensive and densely populated alluvial plains; the shore of the South China Sea is more mountainous and southern China is dominated by hill country and lower mountain ranges.

To the west, the north has a great alluvial plain, and the south has a vast calcareous tableland traversed by hill ranges of moderate elevation, with the Himalaya, containing highest point Mount Everest. The southwest also has high plateaus feature among the more arid landscape of deserts such as the Takla-Makan and the Gobi Desert, which has been expanding. Due to a prolonged drought and perhaps poor agricultural practices dust storms have become usual in the spring in China.

During many dynasties, the southwestern border of China has been the high mountains and deep valleys of Yunnan, which separate modern China from Burma, Laos and Vietnam.

The Palaeozoic formations of China, excepting only the upper part of the Carboniferous system, are marine, while the Mesozoic and Tertiary deposits are estuarine and freshwater or else of terrestrial origin. Groups of volcanic cones occur in the Great Plain of north China. In the Liaodong and Shandong Peninsulas, there are basaltic plateaux.

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Territory

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