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Chinese State Of Jin
Jin (, Old Chinese: ''*''), originally known as Tang (唐), was a major 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, Jin was split into three successor states: Han, Zhao and 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 Yellow River which soon leads to the Guanzhong, an area of the Wei River Valley that wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
History Of China
The earliest known written records of the history of China date from as early as 1250 BC, from the Shang dynasty (c. 1600–1046 BC), during the reign of king Wu Ding. Ancient historical texts such as the '' Book of Documents'' (early chapters, 11th century BC), the '' Bamboo Annals'' (c. 296 BC) and the ''Records of the Grand Historian'' (c. 91 BC) describe a Xia dynasty before the Shang, but no writing is known from the period, and Shang writings do not indicate the existence of the Xia. The Shang ruled in the Yellow River valley, which is commonly held to be the cradle of Chinese civilization. However, Neolithic civilizations originated at various cultural centers along both the Yellow River and Yangtze River. These Yellow River and Yangtze civilizations arose millennia before the Shang. With thousands of years of continuous history, China is among the world's oldest civilizations and is regarded as one of the cradles of civilization. The Zhou dynasty (1046–256 BC) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring And Autumn Period
The Spring and Autumn period was a period in Chinese history from approximately 770 to 476 BC (or according to some authorities until 403 BC) which corresponds roughly to the first half of the Eastern Zhou period. The period's name derives from the ''Spring and Autumn Annals'', a chronicle of the state of Lu between 722 and 479 BCE, which tradition associates with Confucius (551–479 BCE). During this period, the Zhou royal authority over the various feudal states eroded as more and more dukes and marquesses obtained ''de facto'' regional autonomy, defying the king's court in Luoyi and waging wars amongst themselves. The gradual Partition of Jin, one of the most powerful states, marked the end of the Spring and Autumn period and the beginning of the Warring States period. Background In 771 BCE, a Quanrong invasion in coalition with the states of Zeng and Shen — the latter polity being the fief of the grandfather of the disinherited crown prince Yijiu — destroyed th ... [...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. The source of the Wei River is close to Weiyuan County''Wei yuan'' meaning "Wei's source"in Gansu province, less than from the Yellow River at Lanzhou. However, due to the sharp turn north the Yellow River takes in Lanzhou, the Wei and the Yellow River do not meet for more than further along the Yellow River's course. In a direct line, the Wei's source lies west of the main city along its course, Xi'an in Shaanxi province. The length of the river is and the area drained covers . The Wei River's tributaries include the Luo River, Jing River, Niutou River, Feng River and the Chishui River. The Wei River valley has a continental climate, with hot summers and cool, dry winters. It sits between the arid steppes and deserts to the north and the forests of the Qingling mount ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guanzhong
Guanzhong (, formerly 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 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 Long Mountain ranges in the north (collectively known as its "North Mountains"). The central flatland area of the basin, known as the Guanzhong Plain, 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 Jin- Shaan Basin Belt, and is separated from its geological sibling — the Yuncheng Basin to its northeast — by the Yellow River section southwest of the Lüliang Mountains and north of the river's bend at the tri-provincial junction among Shaanxi, Shanxi and Henan. The name ''Gu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yellow River
The Yellow River or Huang He (Chinese: , Mandarin: ''Huáng hé'' ) is the second-longest river in China, after the Yangtze River, and the sixth-longest river system in the world at the estimated length of . Originating in the Bayan Har Mountains in Qinghai province of Western China, it flows through nine provinces, and it empties into the Bohai Sea near the city of Dongying in Shandong province. The Yellow River basin has an east–west extent of about and a north–south extent of about . Its total drainage area is about . The Yellow River's basin was the birthplace of ancient Chinese, and, by extension, Far Eastern civilization, and it was the most prosperous region in early Chinese history. There are frequent devastating floods and course changes produced by the continual elevation of the river bed, sometimes above the level of its surrounding farm fields. Etymology Early Chinese literature including the '' Yu Gong'' or ''Tribute of Yu'' dating to the Warrin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loess Plateau
The Chinese Loess Plateau, or simply the Loess Plateau, is a plateau in north-central China formed of loess, a clastic silt-like sediment formed by the accumulation of 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 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, they ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lüliang Mountains
The Lüliang Mountains are a 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 at Tongguan in Shaanxi. Shang Bronze Alligator.JPG, A Shang-era bronze alligator discovered in the Lüliang Range See also * Taihang Mountains in eastern Shanxi, dividing the Fen valley from the North China Plain * Greater Khingan The Greater Khingan Range or Da Hinggan Range (; IPA: ), is a -long volcanic mountain range in the Inner Mongolia region of Northeast China. It was originally called the Xianbei Mountains, which later became the name of the northern branch of th ... in Manchuria, which runs south form the Taihang and Lüliang * Tongguan and Hangu Pass, passes between the Lüliang foothill ... [...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 (''Hu'') 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 assimilation. 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" (''Siyi'') were the Di to the north, the Man to the south, the Yi to the east, and the Rong t ... [...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 "bellic ... [...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 ''Discourses of the States'' states that the Ji was the home of the Yellow Emperor's clan before he fought the clan of Yandi (the "Flame Emperor"). Its name is identical with the surname of the royal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Warring States Period
The Warring States period () was an era in ancient Chinese history characterized by warfare, as well as bureaucratic and military reforms and consolidation. It followed the Spring and Autumn period and concluded with the Qin wars of conquest that saw the annexation of all other contender states, which ultimately led to the Qin state's victory in 221 BC as the first unified Chinese empire, known as the Qin dynasty. Although different scholars point toward different dates ranging from 481 BC to 403 BC as the true beginning of the Warring States, Sima Qian's choice of 475 BC is the most often cited. The Warring States era also overlaps with the second half of the Eastern Zhou dynasty, though the Chinese sovereign, known as the king of Zhou, ruled merely as a figurehead and served as a backdrop against the machinations of the warring states. The "Warring States Period" derives its name from the ''Record of the Warring States'', a work compiled early in the Han dynasty. Geogra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Partition Of Jin
The Partition of Jin (), the watershed between the Spring and Autumn and Warring States periods, refers to the division of the State of Jin between rival families into the three states of Han, Zhao and Wei. As a result, 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 Jin as far back as seventh century BCE. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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