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Jin (Chinese State)
Jin (, Old Chinese: ''*''), originally known as Tang (唐), was a major Ancient Chinese states, state during the middle part of the Zhou dynasty, based near the centre of what was then China, on the lands attributed to the legendary Xia dynasty: the southern part of modern Shanxi. Although it grew in power during the Spring and Autumn period, its aristocratic structure saw it break apart when the duke lost power to his nobles. In 403BC, the Zhou court recognized Jin's three successor states: Han (Warring States), Han, Zhao (state), Zhao, and Wei (state), Wei. The Partition of Jin marks the end of the Spring and Autumn period and the beginning of the Warring States period. Geography Jin was located in the lower Fen River drainage basin on the Shanxi plateau. To the north were the Xirong and Beidi peoples. To the west were the Lüliang Mountains and then the Loess Plateau of northern Shaanxi. To the southwest the Fen River turns west to join the south-flowing part of the Yello ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
History Of China
The history of China spans several millennia across a wide geographical area. Each region now considered part of the Chinese world has experienced periods of unity, fracture, prosperity, and strife. Chinese civilization first emerged in the Yellow River valley, which along with the Yangtze basin constitutes the geographic core of the Chinese cultural sphere. China maintains a rich diversity of ethnic and linguistic people groups. The traditional lens for viewing Chinese history is the dynastic cycle: imperial dynasties rise and fall, and are ascribed certain achievements. This lens also tends to assume Chinese civilization can be traced as an unbroken thread many thousands of years into the past, making it one of the cradles of civilization. At various times, states representative of a dominant Chinese culture have directly controlled areas stretching as far west as the Tian Shan, the Tarim Basin, and the Himalayas, as far north as the Sayan Mountains, and as far south ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring And Autumn Period
The Spring and Autumn period () was a period in History of China, Chinese history corresponding roughly to the first half of the Eastern Zhou (256 BCE), characterized by the gradual erosion of royal power as local lords nominally subject to the Zhou exercised increasing political autonomy. The period's name derives from the ''Spring and Autumn Annals'', a chronicle of the state of Lu between 722 and 481 BCE, which tradition associates with Confucius (551–479 BCE). During this period, local polities negotiated their own alliances, waged wars against one another, up to defying the king's court in Luoyang, Luoyi. The gradual Partition of Jin, one of the most powerful states, is generally considered to mark the end of the Spring and Autumn period and the beginning of the Warring States period. The periodization dates to the late Western Han (). Background In 771 BCE, a Quanrong invasion in coalition with the states of Zeng (state), Zeng and Shen (state), Shen— ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wei River
The Wei River () is a major river in west-central China's Gansu and Shaanxi provinces. It is the largest tributary of the Yellow River and very important in the early development of Chinese civilization. In ancient times, such as in the Records of the Grand Historian, the river was called Wei Shui (). The total length of the Wei River is , covering a drainage area of . Some of the major tributaries include the Luo River, Jing River, Niutou RiverFeng Riverand the Chishui River. In a direct line, it travels due east for before draining into the Yellow River at Tongguan County near the tri-provincial boundary between Shaanxi, Shanxi and Henan provinces, with a series of major cities along its course including Tianshui, Baoji, Xianyang, Xi'an and Weinan. Course The source of the Wei River starts in the mountainous region in southern Weiyuan County (literally meaning "Wei's source"), Gansu province, with the westernmost headwater of its mainstem Qingyuan River (清源 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guanzhong
Guanzhong (, formerly romanization of Chinese, romanised as Kwanchung) region, also known as the Guanzhong Basin, Wei River Basin, or uncommonly as the Shaanzhong region, is a historical region of China corresponding to the crescentic graben structural basin, basin within present-day central Shaanxi, bounded between the Qinling Mountains in the south (known as Guanzhong's "South Mountains"), and the Huanglong Mountain, Meridian Ridge and Mount Liupan, Long Mountain ranges in the north (collectively known as its "North Mountains"). The central plain, flatland area of the basin, known as the Guanzhong Plain (关中平原; pinyin: Guānzhōng Píngyuán), is made up of alluvial plains along the lower Wei River and its numerous tributaries and thus also called the Wei River Plain. The region is part of the Shanxi, Jin-Shaanxi, Shaan Basin Belt, a prominent section of the Shanxi Rift System, and is separated from its geological sibling — the Yuncheng Basin to its northeast — by the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yellow River
The Yellow River, also known as Huanghe, is the second-longest river in China and the List of rivers by length, sixth-longest river system on Earth, with an estimated length of and a Drainage basin, watershed of . Beginning in the Bayan Har Mountains, the river flows generally eastwards before entering the long Ordos Loop, which runs northeast at Gansu through the Ordos Plateau and turns east in Inner Mongolia. The river then turns sharply southwards to form the border between Shanxi and Shaanxi, turns eastwards at its confluence with the Wei River, and flows across the North China Plain before emptying into the Bohai Sea. The river is named for the yellow color of its water, which comes from the large amount of sediment discharged into the water as the river flows through the Loess Plateau. The Yellow River basin was the birthplace of Yellow River civilization, ancient Chinese civilization. According to traditional Chinese historiography, the Xia dynasty originated on it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess Plateau
The Loess Plateau is a plateau in north-central China formed of loess, a clastic rock, clastic silt-like sediment formed by the accumulation of Dust#Atmospheric, wind-blown dust. It is located southeast of the Gobi Desert and is surrounded by the Yellow River. It includes parts of the Chinese provinces of Qinghai, Gansu, Shaanxi and Shanxi. The depositional setting of the Chinese Loess Plateau was shaped by the tectonic movement in the Neogene period, after which strong southeast winds caused by the East Asian Monsoon transported sediment to the plateau during the Quaternary period. The three main morphological types in the Loess Plateau are loess platforms, ridges and hills, formed by the deposition and erosion of loess. Most of the loess comes from the Gobi Desert and other nearby deserts. The sediments were transported to the Loess Plateau during interglacial periods by southeasterly prevailing winds and winter monsoon winds. After the deposition of sediments on the plateau, t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lüliang Mountains
The Lüliang Mountains are a mountains of China, mountain range in central China, dividing Shanxi's Fen River valley from the Yellow River. The range forces the Yellow River southwards on the eastern side of the Ordos Loop but tapers off to the south, where the Fen turns west to join the Yellow River before the Qin Mountains turn the combined river sharply eastward at its confluence with the Wei River, Wei at Tongguan County, Tongguan in Shaanxi. See also * Taihang Mountains in eastern Shanxi, dividing the Fen valley from the North China Plain * Greater Khingan in Manchuria, which runs south form the Taihang and Lüliang * Tongguan County, Tongguan and Hangu Pass, passes between the Lüliang foothills and the Qin Mountains References Mountain ranges of Shanxi {{Shanxi-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beidi
The Di or Beidi (Northern Di) were various ethnic groups who lived north of the Chinese ('' Huaxia'') realms during the Zhou dynasty. Although initially described as nomadic, they seem to have practiced a mixed pastoral, agricultural, and hunting economy and were distinguished from the nomads of the Eurasian steppe who lived to their north. Chinese historical accounts describe the Di inhabiting the upper Ordos Loop and gradually migrating eastward to northern Shanxi and northern Hebei, where they eventually created their own states like Zhongshan and Dai. Other groups of Di seem to have lived interspersed between the Chinese states before their eventual conquest or sinicization. Name The ancient Chinese, whose Xia, Shang, and Zhou states flourished along the Fen, Yellow, and Wei valleys, discussed their neighbors according to the cardinal directions. The Four Barbarians were the Di to the north, the Man to the south, the Yi to the east, and the Rong to the west. These ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Xirong
Xirong () or Rong were various people who lived primarily in and around the western extremities of ancient China (in modern Gansu and Qinghai). They were known as early as the Shang dynasty (1765–1122 BCE), as one of the Four Barbarians that frequently (and often violently) interacted with the sinitic Huaxia civilization. They typically resided to the west of Guanzhong Plains from the Zhou dynasty (1046–221 BCE) onwards. They were mentioned in some ancient Chinese texts as perhaps genetically and linguistically related to the people of the Chinese civilization. Etymology The historian Li Feng says that during the Western Zhou period, since the term ''Rong'' "warlike foreigners" was "often used in bronze inscriptions to mean 'warfare', it is likely that when a people was called 'Rong', the Zhou considered them as political and military adversaries rather than as cultural and ethnic 'others'." Paul R. Goldin also proposes that ''Rong'' was a "pseudo-ethnonym" meaning "belli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fen River
The Fen River drains the center of Shanxi Province, China. It originates in the Guancen Mountains of Ningwu County in northeast Shanxi, flows southeast into the basin of Taiyuan, and then south through the central valley of Shanxi before turning west to join the Yellow River west of Hejin. The Fen and the Wei Rivers are the two largest tributaries of the Yellow River. The river is long and drains an area of , 25.3% of Shanxi's area. The Fen River is the longest in Shanxi. It is also the second-longest tributary of the Yellow River. Within Taiyuan, the Fen runs from north to south; the prefecture includes one-seventh of the river's course. History Legend The Fen is usually identified with the said by Sima Qian and others to have flowed beside the home of the Yellow Emperor. The ''Guoyu (book), Discourses of the States'' states that the Ji was the home of the Yellow Emperor's clan before he fought the clan of Yan Emperor, Yandi (the "Flame Emperor"). Its name is identical with ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Warring States Period
The Warring States period in history of China, Chinese history (221 BC) comprises the final two and a half centuries of the Zhou dynasty (256 BC), which were characterized by frequent warfare, bureaucratic and military reforms, and struggles for greater hegemonic influence among the ancient Chinese states, various autonomous feudal states of the Eastern Zhou dynasty. It followed the Spring and Autumn period and concluded with the eventual unification of China by the western state of Qin (state), Qin under Qin Shi Huang, who Qin's wars of unification, conquered all other contender states by 221 BC and found the Qin dynasty, the first history of China#Imperial China, imperial dynasty in East Asian history. While scholars have identified several different dates as marking the beginning of the Warring States period, Sima Qian's choice of 475 BC, the first year of King Yuan of Zhou's reign, is the most often cited due to the paucity of preceding annals after th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Partition Of Jin
The Partition of Jin (), refers to the division of the State of Jin between rival families into the three states of Han, Zhao and Wei, a watershed event marking the division between the Spring and Autumn and Warring States periods. Proceeding from the Jin, the three states were often referred to as the "Three Jins" (). Because the process took several decades, there is some debate between scholars as to the year which best marks the true partition of Jin. state the most common dates picked by historians are 481, 475, 468, and 403 BCE. The last date, according to Sima Guang marks the conferring of Marquessates by King Weilie of Zhou on Wei Si, ruler of the State of Wei; Zhao Ji, ruler of the State of Zhao, and Han Qian, ruler of the State of Han. In 386 BCE, the states of Han, Wei and Zhao deposed Duke Jing of Jin and divided the last remaining Jin territory between themselves, which marked the end of the Jin state. Background Succession issues were constant in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
