Ask about Xiaoshan's geographical location, topography, climate, rivers, products, economic development, cultural relics and historical sites, and tourism resources.

Administrative category: county-level cities

Area: Hangzhou, Zhejiang Province

Telephone area code: 057 1

Postal code: 3 1 1200

Location: South Bank of Qiantang River downstream

Area: 1420 km2

Population: 65,438+065,438+077,000 (end of 2005)

Dialect: Wu dialect (Shaolin Xiaoshan dialect)

Famous scenic spots: Liangshan, Temple and Tomb, Liangzhu Cultural Site.

Airport: Hangzhou Xiaoshan International Airport

Xiaoshan specialty

Xianghu Lake

Administrative divisions:

geographical position

[1] Xiaoshan District is located in the north of Zhejiang Province, on the south bank of Qiantang River, belonging to Hangzhou, facing Xihu District, Jianggan District and Haining City across the river. Geographical coordinates are12004' 22'' ~12043' 46'' and 29 50' 54'' ~ 30 23' 47'' north latitude. Total area 1420.22 km2. The whole territory is about 57.2 kilometers wide from east to west and 59.4 kilometers long from north to south. Peripheral borders: Shaoxing County in the east, Zhuji City in the south, Fuyang City in the west, Binjiang District in Hangzhou in the northwest and Qiantang River in the north. Zhejiang-jiangxi railway and Xiao Yong railway, national highway 104 and provincial highway 03 meet in China respectively. Shanghai-Hangzhou-Ningbo Expressway passes through the territory. Xiaoshao Canal crosses Qiantang River and Cao 'e River from east to west. Edit the terrain features of this part.

Xiaoshan district is located in the north of hilly area in eastern Zhejiang and the south of plain area in northern Zhejiang. The terrain is high in the south and low in the north, sloping from southwest to northeast and slightly lower in the middle. Geomorphological zoning features are obvious: the southern part is hilly, and the valley plain is small; The central and northern parts are plains with hills in the middle. Plain accounts for about 66%, mountain accounts for 17%, and water accounts for 17%. The plain is about 909 square kilometers, which can be divided into two types according to the origin: continental sedimentary plain and marine sedimentary plain, with marine sedimentary plain as the main one. 1. Gulf accumulation plain. Mainly located in the middle, the terrain is flat and slightly undulating locally, and the ground elevation is 4.2 ~ 6.2 meters. 1/3 of the plain area. 2. Delta Bay accumulation plain. Located in the north, it is mainly formed by the accumulation of sediment brought by the tidal current in Hangzhou Bay, with a flat performance, with an altitude of 5 ~ 6.3 meters. It accounts for two-thirds of the plain area. 3. Valley Plain. Scattered in the southern hilly area, the area is very small, only 58 square kilometers.

The mountainous area is about 259 square kilometers, including low mountains, high hills, low hills and land islands, with the highest elevation of 744 meters and the lowest elevation of 10 meters. The mountain is basically distributed in southwest-northeast direction, which is the branch and residual vein of Longmen Mountain, Huiji Mountain and Tianmu Mountain, and enters from southwest, south and northwest respectively. 1. Low mountain. It is distributed in the border areas of Zhuji and Fuyang in this area. The main peaks are all above 500 meters above sea level, and a few reach 700 meters. It accounts for 15% of the mountainous area. 2. High mountains. Scattered in the southwest and southeast, it is 300 ~ 500m above sea level, accounting for 30% of the mountainous area. 3. Low hills. The southern part is distributed intermittently, with an altitude of 50-300 meters, and the terrain is broken, accounting for 35% of the mountainous area. 4。 Lu Yu. Scattered in the bay accumulation plain and the triangle bay accumulation plain reclaimed from the sea in the early stage, there are more than 50 places with different sizes, with an altitude of 10 ~ 257m, accounting for 20% of the mountainous area.

Rivers. According to the topography and flow direction, it can be divided into three self-contained and interconnected small water systems, belonging to Qiantang River water system. Qiantang River enters this area from the vicinity of Changlingtou, Fuyang, and the territory is full of tidal reach. The highest recorded tidal level is 9.58 meters, and the lowest is 2.3 1 meter. The average sediment concentration is 5 ‰; The salinity is about 2‰, and the highest is 1 1.3‰. O 1。 Southern water system. Located in the hilly and valley plain areas in the south and southwest, it is a dendritic river network system with Puyang River as the main stream. The main rivers are Puyang River, Yongxing River, Lingxi River, Huangtong River and Jingyue River. 2. Central water supply system. The river and lake system in the Central Plains, east of Xijiangtang and south of Beihai Tang, is a part of the water system in Xiaoshao Plain. The main rivers are Evolution Creek, Xijiang River, Xiaoshao Canal, Nanmenjiang River, Hu Xiang and Baima Lake. 3. Northern water system. It is an artificial river network system in Nansha area and reclamation area north of Beihai pond, which is distributed in a grid shape. The main rivers are Beitang River, Qianjiefang River, Houjiefang River, Xianfeng River, Qijiazhi River, Wubao River, Changshan Branch River, Jiubazhi River, Dazhi River, Yongfeng Branch River, Fangqianjun River, Production Bay, Changlin Bay and Sanguanbu Wan Zhi.

Xiaoshan district is located in the southern edge of the north subtropical monsoon climate zone. The general climate features are: long winter and summer, short spring and autumn, and distinct four seasons; Adequate sunshine, abundant rainfall, warm and humid; Cold air is easy to enter and difficult to exit, and there are more disastrous weather; The regional differences of light, temperature and water are obvious. The annual average temperature is 16. 1℃. The annual average ground temperature is 18.3℃. The average annual rainfall is1402.5mm. The average annual frost-free period is 248 days. The annual average sunshine hours is 2006.9 hours. The annual average evaporation is1223.7mm. The wind direction changes with the seasons, 165438+ 10 to February of the following year, and the westerly winds in the north and the north are the most. From February, the easterly wind from north to north is getting stronger, and it is mainly easterly in March-June and August; Dorsey south wind in July; It is windy in September -65438+ 10. Disastrous weather mainly includes cold wave, low temperature, rainstorm, typhoon, hail and squall line.

Xiaoshan

Xiaoshan was built as Yuji in AD 2, and renamed in the first year of Tang Tianbao (AD 742), which has been in use ever since. Hunan Lake has a long history and is famous earlier than West Lake. It is surrounded by mountains and waters and is famous for its beautiful scenery. The story of Gou Jian, the King of Yue, is a household name and has been passed down through the ages. During the Spring and Autumn Period and the Warring States Period, four famous Chinese beauties, He, a great poet in the Tang Dynasty, Ge, a national hero, a famous painter, Tang Shouqian, a modern politician, Shen Donghai, the initiator of the contemporary computer harmony process and the drafter of software industry norms, left a brilliant chapter for Xiaoshan!