yellow river kuei hua cheng Huang He Ho Bayan Har Mountains in Qinghai Province in western China cradle of Chinese civilization


Illustrated travels a record of discovery geography and adventure edited by h w bates assistant secretary of the royal geographical society with engravings from original drawings by celebrated artists cassell petter and & galpin London paris new york. Medieval times A major course change in 1194 took over the Huai River drainage system throughout the next 700 years. The mud in the Yellow River literally blocked the mouth of the Huai River and left thousands homeless. The Yellow River adopted its present course in 1897 after the latest course change occurred in 1855. Currently, the Yellow River flows through Jinan, capital of the Shandong province, and ends in the Bohai Sea, yet the eastern terminus for the Yellow River has oscillated from points north and south of the Shandong Peninsula in its many dramatic shifts over time. The course of the river has changed back and forth between the route of the Huai River and the original route of the Yellow River several times over the past 700 years. The consequent buildup of silt deposits was so heavy that the Huai River was unable to flow in its historic course after the Yellow River reverted to its northerly course for the last time in 1897. Instead, the water pools up into Hongze Lake and then runs southward toward the Yangtze River. Floods on the river account for some of the deadliest natural disasters ever recorded. The flatness of North China Plain contributes to the deadliness of the floods. A slight rise in water level means a large portion of land is completely covered in water. When a flood occurs, a portion of the population initially dies from drowning, then by the spread of diseases and the ensuing famine. In 1887 the river flooded the North China Plain causing an estimated 900,000–2,000,000 deaths.


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