|
Sichuan Basin
The Sichuan Basin (), formerly transliterated as the Szechwan Basin, sometimes called the Red Basin, is a lowland region in southwestern China. It is surrounded by mountains on all sides and is drained by the upper Yangtze River and its tributaries. The basin is anchored by Chengdu, the capital of Sichuan province, in the west, and the direct-administered municipality of Chongqing in the east. Due to its relative flatness and fertile soils, it is able to support a population of more than 100 million. In addition to being a dominant geographical feature of the region, the Sichuan Basin also constitutes a cultural sphere that is distinguished by its own unique customs, cuisine and dialects. It is famous for its rice cultivation and is often considered the breadbasket of China. In the 21st century its industrial base is expanding with growth in the high-tech, aerospace, and petroleum industries. Geography The Sichuan Basin is an expansive lowland region in China that is surround ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zitong County
Zitong County () is a county in the northeast of Sichuan Province, China. It is under the administration of the prefecture-level city of Mianyang. It has an area of , and a population of in 2002. Its seat is from Chengdu, and from Mianyang. It was made a county . Famous people include: Sima Xiangru, Pu Fuzhou, Hai Deng, Li Youxing. Administrative divisions Zitong County comprises 15 towns and 1 township: ;towns: *Wenchang 文昌镇 *Changqing 长卿镇 *Xuzhou 许州镇 *Liya 黎雅镇 *Wolong 卧龙镇 *Guanyi 观义镇 *Manao 玛瑙镇 *Shiniu 石牛镇 *Ziqiang 自强镇 *Renhe 仁和镇 *Shuangban 双板镇 *Jinlong 金龙镇 *Wenxing 文兴镇 *Yanwu 演武镇 *Hongren 宏仁镇 ;township: *Baoshi 宝石乡 Historical sites Zitong has three historical sites listed in the official list of Chinese national historic sites.: * Qiqushan temple (Qiqushan damiao, ) * Liye tower (Liye que, ) * Wolongshan temple (Wolong shan Qianfo yan shiku, ) Aftermath of the 2008 Earthq ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Direct-controlled Municipalities Of China
A direct-administered municipality ( zh, s=直辖市, p=Zhíxiáshì, labels=no, l=; ; commonly known as municipality) is a provincial-level administrative division in China. The municipalities are directly affiliated to the central government. There are four municipalities in China: Beijing, Chongqing, Shanghai, and Tianjin. Although being as a city by name, a Chinese municipality is more than a city in a traditional sense. It is equivalent to a province as it usually composed of a central urban area and a number of much larger surrounding suburban and rural areas. History During the Republic of China, the first municipalities were the 11 cities of Nanjing, Shanghai, Beijing, Tianjin, Qingdao, Chongqing, Xi'an, Guangzhou, Hankou (now part of Wuhan), Shenyang, and Harbin. They were established in 1927 soon after they were designated as "cities" during the 1920s. Nominally, Dalian was a municipality as well, although it was under Japanese control. These cities were firs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Smog
Smog, or smoke fog, is a type of intense air pollution. The word "smog" was coined in the early 20th century, and is a portmanteau of the words ''smoke'' and ''fog'' to refer to smoky fog due to its opacity, and odour. The word was then intended to refer to what was sometimes known as pea soup fog, a familiar and serious problem in London from the 19th century to the mid-20th century, where it was commonly known as a London particular or London fog. This kind of visible air pollution is composed of nitrogen oxides, sulfur oxide, ozone, smoke and other Particulate matter, particulates. Man-made smog is derived from coal combustion emissions, vehicular emissions, industrial emissions, forest and agricultural fires and photochemical reactions of these emissions. Smog is often categorized as being either summer smog or winter smog. Summer smog is primarily associated with the photochemical formation of ozone. During the summer season when the temperatures are warmer and there is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Qu River (Jialing River Tributary)
Qu River () is a river in Chongqing, Sichuan Province, China. It is a left tributary of the Jialing River, which in its turn is a left tributary of the Yangtze; it is thus part of the East China Sea basin. Its length is 720 km. See also *List of rivers in China Rivers that flow through China are as follows. The list is organized according to the body of water into which each river empties, beginning with the Sea of Okhotsk in the northeast, moving clockwise on a map and ending with the Arctic Ocean. S ... Rivers of Sichuan Rivers of Chongqing Tributaries of the Yangtze River {{China-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fu River (Sichuan)
Fu River, or Fu Jiang () is a river of in China's Sichuan Province and Chongqing Municipality. It is a right tributary of the Jialing River, which in its turn is a left tributary of the Yangtze; it is thus part of the East China Sea basin. The Fu River flows in the general southern and south-eastern direction across the central Sichuan (Mianyang and Suining Prefectures), and then enters the Chongqing Municipality, where it merges with the Jialing River. See also *List of rivers in China *List of rivers of India Rivers of Sichuan Tributaries of the Yangtze River {{China-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuo River
The Tuo River () is -long river in Sichuan province of southern China. The Tuo River is one of the major tributaries of the upper Yangtze River (''Chang Jiang''). Geography The river originates at the northwest edge of Sichuan basin. It flows through Jintang, Jianyang, Ziyang, Zizhong, and Neijiang. It flows into Yangtze River in Luzhou, Sichuan. See also * Index: Tributaries of the Yangtze River * List of rivers in China References *Great Soviet Encyclopedia The ''Great Soviet Encyclopedia'' (GSE; , ''BSE'') is one of the largest Russian-language encyclopedias, published in the Soviet Union from 1926 to 1990. After 2002, the encyclopedia's data was partially included into the later ''Great Russian Enc ... {{coord, 28.9036, N, 105.448, E, source:kolossus-dewiki, display=title Rivers of Sichuan Tributaries of the Yangtze River ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Three Gorges
The Three Gorges () are three adjacent and sequential gorges along the middle reaches of the Yangtze River path, in the hinterland of the People's Republic of China. With a subtropical monsoon climate, they are known for their scenery. The Three Gorges—comprising the Qutang Gorge, Qutang, followed by the Wu Gorge, Wu, and finally the Xiling Gorge, Xiling gorges—span , beginning at Baidicheng, Baidi City of Chongqing, in the west and ending at Nanjing Pass, at Yichang, Yichang City, Hubei, Hubei Province, in the east, between which are the Fengjie and Wu Mountains of Chongqing, as well as Badong, Zigui, and Yichang of Hubei Province. Course of the Yangtze River After arriving at Yibin (), in Sichuan Province (), the Yangtze River () flows from Jiangjin (), of Chongqing Municipality (), to Yichang (), of Hubei Province (); and this section of the river is called ''Sichuan River, Chuanjiang'' (), or "the river of Sichuan". In the past, it was the only waterway that connec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jialing River
The Jialing River, formerly known by numerous other names, is a major tributary of the Yangtze River in the Sichuan Basin. It is named after the Jialing Valley in Feng County, Shaanxi through which it flows. The Jialing River's most notable characteristic was formerly its pellucid green waters. It is also notable for its sinuous course in its lower reaches. From Zhangwang Miao (Temple of Zhangfei) in Langzhong to the mouth, the distance as the crow flies is . However the river itself travels . The most tortuous part of its course is between Nanchong and Wusheng County. Names The name Jialing did not come into general use until the Tang Dynasty.. Before that, it was generally known as the Ba, although it also appears as the Lang and Yu as well. In the 19th century, it was known by the Sichuanese as the Small or Little River, by comparison with the Jinsha and Yangtze. Geography The source of the Jialing, in name, is in the Jialin, which means "the tomb of Jia (嘉陵 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weiyuan County, Sichuan
Weiyuan County () is a county of Sichuan Province, China. It is under the administration of Neijiang City. The county borders Neijiang, Zigong, Rongxian, Zizhong and Renshou. It administers 20 townships. Weiyuan County manages 20 towns with an area of 1288.85k square meters and a total population of 547,059 people (as of 2020), including 31 ethnic groups including Han, Tujia, Yi, and Miao. The religions in Weiyuan County mainly include Buddhism, Catholicism, and Christianity. Buddhism has been spreading for the longest time, has the most followers, and has the greatest influence in the county. Weiyuan County has abundant mineral resources with a complete range of varieties, including natural gas, oil, iron ore, limestone, bauxite shale ore, potassium containing water mica clay ore (commonly known as mung bean mud), quartz sand, kaolin, dolomite, calcite, gypsum, rock salt, and co occurring minerals such as potassium, boron, bromine, iodine, as well as rare elements such ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dissected Plateau
A dissected plateau is a plateau area that has been severely eroded, and the relief is sharp. Such an area may be referred to as mountainous, but dissected plateaus are distinguishable from orogenic mountain belts by the lack of fold (geology), folding, Metamorphic rock, metamorphism, extensive Geological fault, faulting, or magmatic activity accompanying orogeny. Formation A dissected plateau may also be formed, usually on a comparatively small scale, by the levelling of terrain by planing and deposition beneath an ice sheet or perhaps an ice cap. Subsequently, during the same or a later Glaciation, glacial period, the margins of the Till, glacial till plain are removed by glaciers, leaving the plateau into which erosion by water incises valleys. Such a plateau may be level or gently sloping but may be distinguished by the till caps on its hills. Glacial till is still widely known in United Kingdom, Britain by the older name of boulder clay. Dissected volcanic plateaus includ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Longquan Mountains
The Longquan Mountains () are a low-lying range of mountains in Sichuan, China. The mountains are long, on average wide, and form a ridge-like barrier between the Chengdu Plain and the rest of the Sichuan Basin. They range from Deyang in the north to Leshan in the south. The highest point of the range is Ximei Mountain (西眉山) at in Zhongjiang County. The Longquan are bisected by the Tuo River in the north that forms a -deep gorge through the mountains. The Longquan Mountains are the westernmost detachment fold in the Sichuan Basin. The other detachment folds the region are found in the east of the basin, so the Longquan stand out relative to the alluvial Chengdu Plain in the west and the Sichuan Basin's rolling hills to the east. The Longquan Mountains have shown tectonic activity in the past, although pressure built up at the edge of the Sichuan Basin now tends to release along the Longmenshan Fault, further west. The eastern suburbs of Chengdu reach the base o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Fan
An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to Semi-arid climate, semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation. They range in area from less than to almost . Alluvial fans typically form where a flow of sediment or rocks emerge from a confined channel and are suddenly free to spread out in many directions. For example, many alluvial fans form when steep mountain valleys meet a flat plain. The transition from a narrow channel to a wide open area reduces the carrying capacity of flow and results in Deposition (geology), deposition of sediments. The flow can take the form of infrequent debris flows like in a landslide, or can be carried by an intermittent stream or creek. The reduction of flow is key to the formation of alluvial ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
