Traditional Culture Encyclopedia - Photography and portraiture - Which city does Cixi City in Hangzhou belong to?
Which city does Cixi City in Hangzhou belong to?
It is 60km from Ningbo in the east, Shanghai 148km in the north and Hangzhou 138km in the west. It is the center of the economic golden triangle of Shanghai, Hangzhou and Ningbo in the south wing of the Yangtze River Delta. Cixi is rich in tidal flat resources, and has reclaimed 65,438+10,000 mu of tidal flat, which is the richest land reserve resource in Zhejiang Province.
Cixi celadon culture has a long history and is known as the birthplace of "the road of marine ceramics". "South Blue and North White" laid the pattern of China ceramics. Cixi, also known as "the capital of household appliances", together with Qingdao and Shunde, is known as the three major production bases of household appliances in China. Cixi culture belongs to Wuyue culture, and Cixi people belong to Jiangsu and Zhejiang families, and use Wu language.
Cixi is an important industrial and commercial city in the south wing of the Greater Shanghai Economic Circle in the Yangtze River Delta, and it is also an open coastal economic zone approved by the State Council, China. In 2008, the opening of the Hangzhou Bay Bridge narrowed the distance with Shanghai and became a golden node city in the south wing of the Yangtze River Delta.
Extended data
Cixi's topography is high in the south and low in the north, and it spreads to Hangzhou Bay in the form of hills, plains and beaches. The southern hills belong to the hilly area of Cuiping Mountain, which is the remnant vein of Siming Mountain, extending more than 40 kilometers from east to west, accounting for about two-tenths of the urban area of Cixi.
Low mountains and hills at the eastern end, about 100 meters above sea level; Between 300 and 400 in the middle; To Shiyan Township, the stratum subsidence is Donghenghe; Outside the Hexi end,100 ~ 200m high. The main peaks are Dapeng Mountain, Wulei Mountain, Dalin Mountain, Laoya Mountain and Dongdong Mountain. Laoya Mountain, the highest peak, is 446 meters above sea level. This stratum has a single genesis and belongs to erosion and denudation landform.
The plain is a part of Ningshaoping Plain, which is 55 kilometers long from east to west, accounting for about seven-tenths of the total area. The terrain slopes slowly from west to east, with the western region being high in the north and low in the south, and the eastern region being high in the south and low in the north. Gutang River is divided into two parts, north and south, with an area ratio of 2: 8.
The southern mountain plain was formed 900 ~ 2500 years ago, which was a late Holocene lake marine deposit. Most of the ingredients are clay and loam, and some are mixed with peat. The northern coastal plain is a newly formed land since 900 years, which is composed of loam, loam and silt.
To the north of the plain is the fan-shaped Sanbei Shoal which extends into Hangzhou Bay. The scale of 1986 is calculated based on the zero meter line of the theoretical datum, reaching 433.5 square kilometers. Beach sediments are mainly fine-grained materials such as fine sand and sandy mud, and the particles in the eastern region are coarse. The fluctuation of coastal zone has obvious periodicity, the coastline moves northward as a whole and the land resources increase.
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