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The Grand Canal is a system of interconnected canals linking various major rivers in North and East China, serving as an important waterborne transport infrastructure between the north and the south during Medieval and premodern China. It is the longest artificial waterway in the world and a UNESCO World Heritage Site.
The Yellow River is the second-longest river in China and the sixth-longest river system on Earth, with an estimated length of 5,464 km (3,395 mi) and a watershed of 795,000 km2 (307,000 sq mi). Beginning in the Bayan Har Mountains, the river flows generally eastwards before entering the 1,500 km (930 mi) 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 North China Plain is a large-scale downfaulted rift basin formed in the late Paleogene and Neogene and then modified by the deposits of the Yellow River. It is the largest alluvial plain of China. The plain is bordered to the north by the Yanshan Mountains, to the west by the Taihang Mountains, to the south by the Dabie Mountains, and to the east by the Yellow Sea and Bohai Sea. The Yellow River flows through the plain, before its waters empty into the Bohai Sea.
The Huai River, formerly romanized as the Hwai, is a major river in East China, about 1,110 km (690 mi) long with a drainage area of 174,000 km2 (67,000 sq mi). It is located about midway between the Yellow River and Yangtze River, the two longest rivers and largest drainage basins in China. Historically draining eastwards directly into the Yellow Sea, erosion from floods have changed the course of the river such that it now primarily discharges into the Yangtze. The Huai River is, to this day, notoriously vulnerable to flooding.
Hongze Lake, previously known as Lake Hungtze or Hung-tse, is the fifth-largest freshwater lake in China. Although it is known to have existed from antiquity, it drastically increased in size during the Qing when the Yellow River—then still flowing south of Shandong—merged with the Huai. The increased sediment and flow combined to greatly expand the lake, swallowing the previous regional center of Sizhou and the Ming Zuling tombs. During the imperial and republican periods, the lake formed part of the border between Jiangsu and Anhui provinces but since 1955 the previous borders have been shifted to place it entirely under Jiangsu's administration. It is now encompassed by the counties of Sihong and Siyang in Suqian Prefecture and Xuyi and Hongze in Huai'an Prefecture. Since the establishment of the People's Republic of China, the lake has generally decreased in size as more of its inflow has been diverted for irrigation.
The Si River is a river in Shandong Province, eastern China. It also ran through the area of modern Jiangsu Province until floods changed its course in 1194.
Since 2018, transport occupied a relatively low priority in China's national development. In the twenty-five years that followed the founding of the People's Republic in 1949, China's transportation network was built into a partially modern but somewhat inefficient system. The drive to modernize the transport system, that began in 1978, required a sharp acceleration in investment. Though despite increased investment and development in the 1980s, the transport sector was strained by the rapid expansion of production and the exchange of goods.
Shawan may refer to:
Toqto’a was a high-ranking minister and an official historian of the Yuan dynasty of China.
The Ji River was a former river in north-eastern China which gave its name to the towns of Jiyuan and Jinan. It disappeared during one of the massive Yellow River floods of 1852, as the Yellow River shifted its course from below the Shandong Peninsula to north of it. In the process, it overtook the Ji and assumed its bed.
The 1034 Yellow River flood was a natural disaster along China's Yellow River originating in a burst fascine following heavy rainfall at Henglong in the territory of the Northern Song. The flood divided the Yellow River from its previous course into three more northerly channels meeting the Chihe, You, and Jin.
The 1441 Yangtze flood was a natural disaster affecting the area around Nanjing, China, during the Ming dynasty.
The 1344 Yellow River flood was a major natural disaster during the Yuan dynasty of Imperial China. The impact was devastating both for the peasants of the area as well as the leaders of the empire. The Yuan dynasty was waning, and the emperor conscripted enormous teams to build new embankments for the river. The harsh working conditions helped fuel rebellions that led to the founding of the Ming dynasty.
The 1448 Yellow River flood was a major natural disaster affecting over 2000 li of the Yellow River. The flood threatened to destroy the Grand Canal port of Linqing and led to the Ming dynasty constructing major public works in Shawan to prevent a recurrence. The banks and dikes only lasted four years until the 1452 flood.
The 1453 Yellow River flood was a natural disaster in the area surrounding Shawan in Shandong, China, during the Ming dynasty. The banks – repaired just the year before – burst again in the fourth lunar month and again in the fifth.
The 1494 Yellow River flood was a natural disaster in China during the Ming dynasty.
The 1194 Yellow River flood was a series of natural disasters along the Yellow River in China during the Jurchen Jin dynasty.
The North Jiangsu Main Irrigation Canal is located in the lower reaches of the Huai River, one of the major rivers in the north of Jiangsu Province, China. It originates at Gaoliangjian on Hongze Lake and runs through Hongze, Qingpu, Huai'an, Funing, Sheyang and Binghai county(or district) and joins the artificial estuary of Biandan Harbour. The canal is 168 km in length and can irrigate 1,720,000 hectares of farmland. The construction program was organized and directed by the headquarters of the Jiangsu Huai River management program between October 1951 and May 1952.
The 1851–1855 Yellow River floods were a series of natural disasters along the Yellow River in China, culminating in the 1855 channel change event. Some data is missing from this period, especially 1854. but it seems that water levels were high for most of 1851-1855.
Jin Fu was a Han Chinese bannerman official during the Qing dynasty notable for his work in river conservancy on the Yellow River.
References
- 1 2 Tsai, Shih-Shan Henry.SUNY Series in Chinese Local Studies: The Eunuchs in the Ming Dynasty . SUNY Press, 1996. ISBN 0791426874, 9780791426876. Accessed 16 Oct 2012.
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