A levee, dike, dyke, embankment, floodbank, or stop bank is a structure used to keep the course of rivers from changing and to protect against flooding of the area adjoining the river or coast. It is usually earthen and often runs parallel to the course of a river in its floodplain or along low-lying coastlines.
The Grand Canal is the longest canal or artificial river in the world and a UNESCO World Heritage Site. Its main artery, known to the Chinese as the Jing–Hang or Beijing–Hangzhou Grand Canal, is reckoned to extend for 1,776 km (1,104 mi) and is divided into 6 main sections. The Jiangnan Canal runs from the Qiantang River at Hangzhou to the Yangtze River at Zhenjiang; the Inner Canal from the Yangtze at Yangzhou to the Huai River at Huai'an, which for centuries was also its junction with the former course of the Yellow River; the Middle Canal from Huai'an to the Nansi Lakes; the Lu Canal from the lakes past Jining and the present course of the Yellow River to the Wei River at Linqing; the Southern Canal from Linqing to the Hai River at Tianjin; and the Northern Canal from Tianjin to Tongzhou on the outskirts of Beijing. As such, it passes through the provinces and municipalities of Zhejiang, Jiangsu, Shandong, Hebei, Tianjin, and Beijing. In 2014, the Chinese government and UNESCO recognized the Eastern Zhejiang Canal from Hangzhou to Ningbo along the former Tongji and Yongji Canals as official components of the Grand Canal.
The Yellow River is the second-longest river in China, after the Yangtze River, and the sixth-longest river system on Earth at the estimated length of 5,464 km (3,395 mi). Originating at an elevation above 15,000 feet in the Bayan Har Mountains, it empties into the Bohai Sea. The Yellow River's basin was the birthplace of ancient Chinese civilization.
A floodplain or flood plain or bottomlands is an area of land adjacent to a river. Floodplains stretch from the banks of a river channel to the base of the enclosing valley, and experience flooding during periods of high discharge. The soils usually consist of clays, silts, sands, and gravels deposited during floods.
The Huai River, formerly romanized as the Hwai, is a major river in China. It is located about midway between the Yellow River and Yangtze, the two longest rivers and largest drainage basins in China, and like them runs from west to east. Historically draining directly into the Yellow Sea, floods have changed the course of the river such that it now primarily discharges into the Yangtze. The Huai is notoriously vulnerable to flooding.
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 694 kilometers (431 mi) long and drains an area of 39,417 km2 (15,219 sq mi), 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.
The 1938 Yellow River flood was a man-made flood from June 1938 to January 1947 created by the Chinese National Army's intentional destruction of dikes (levees) on the Yellow River. The first wave of floods hit Zhongmu County on 13 June 1938.
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.
GologTibetan Autonomous Prefecture is an autonomous prefecture occupying the southeastern corner of Qinghai province, People's Republic of China. The prefecture has an area of 76,312 km2 (29,464 sq mi) and its seat is located in Maqên County. Due to its special geographical location and natural environment, the entire autonomous preference has been included in the Chinese largest natural environmental protection area — the Sanjiangyuan National Park.
Okanagan Falls Provincial Park, now officially named sx̌ʷəx̌ʷnitkʷ Provincial Park, is a provincial park in British Columbia, Canada, located within the traditional territory of the Osoyoos Indian Band. Since time immemorial, the Osoyoos Indian Band's Okanagan ancestors have inhabited and cared for the lands and waters in their traditional territory. The park is also located within the town of Okanagan Falls, protecting the area around the waterfall of the same name, which lies below the outlet of Skaha Lake in the course of the Okanagan River.
Shanghu is a former city of China.
Hetao is a C-shaped region in northwestern China consisting of a collection of flood plains stretching from the banks of the northern half of the Ordos Loop, a large northerly rectangular bend of the Yellow River, that forms the river's entire middle section. The region makes up the northern margin of the Ordos Basin, bounded in the west by the Helan Mountains, the north by the Yin Mountains, the east by the northern portion of Lüliang Mountains, and the south by the Ordos Desert and the Loess Plateau.
The Great Flood of Gun-Yu, also known as the Gun-Yu myth, was a major flood in ancient China that allegedly continued for at least two generations, which resulted in great population displacements among other disasters, such as storms and famine. People left their homes to live on the high hills and mountains, or nest on the trees. According to mythological and historical sources, it is traditionally dated to the third millennium BCE, or about 2300-2200 BCE, during the reign of Emperor Yao.
Henglong (traditional Chinese: 橫隴; simplified Chinese: 横陇; pinyin: Hénglǒng is a former city in northern China.
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 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 forced enormous teams to build new embankments for the river. The terrible conditions helped fuel rebellions that led to the founding of the Ming dynasty.
The 1452 Yellow River floods were major natural disasters affecting hundreds of thousands of farmers along the Yellow River in Shandong and Henan, as well as the Huai River valley.
The 1194 Yellow River flood was a series of natural disasters along the Yellow River in China during the Jurchen Jin dynasty.
The Guo River is a major tributary river on the left bank of Huai River. The source of Guo River is near Kaifeng, Henan province, which is very close to Yellow River. This river is generally an abandoned course of Yellow River. It does not have a remarkable water source and is recharged mainly by groundwater, rainwater and other rivers. Due to the influence of the changing path of Yellow River, the path of Guo River changed frequently throughout the history. The last time Guo River changed its path was during the 1938 Huayuankou flood of the Yellow River. Guo River reaches the Huai River in Anhui province. Guo River is almost entirely located on the plain. The total head of the entire Guo River is only about 59 meters which indicates a very low gradient. The lower section of Guo River is navigable.
Yellow River flood may refer to:
