Postal code of Haishu District, Ningbo City

The postcode of Haishu District, Ningbo City is 3 15000.

Haishu District, which belongs to Ningbo City, Zhejiang Province, is located in the central area of Ningbo, with a center position of about 29 88 ′ 07.92 ″ north latitude and an area of 595.5 square kilometers east longitude12155 ′ 72.89 ″. Haishu District is located in the monsoon climate zone in the transition zone between the north subtropical zone and the middle subtropical zone, and belongs to the maritime monsoon humid climate.

As of 20 18, Haishu District has jurisdiction over 9 streets, 7 towns and 1 township, and the district government is located in Jiangxia Street. According to the data of the seventh census, as of 0: 00 1 1 on June 2020, the resident population in Haishu District was 104 1285.

June 1949, 1 1, two district offices in Haishu and Zhenming. 1984 In March, the provincial government approved the merger of Haishu and Zhenming to establish Haishu District. 2065438+September 2006, nine township streets in the former Yinzhou District were included in Haishu, and a new Haishu District was established. The main scenic spots in Haishu District are Tianyi Pavilion, Drum Tower, Tianfeng Tower, Ningbo City God Temple, Tianyi Square and Yuehu Lake.

In September, 20 18, it won the "20 18 Central Europe Green and Smart City Award". In September of 20 18, the White Paper on the Development of Top 100 Districts in China was released in Beijing, and it was elected as the Top 100 Districts in China on 20 18.

topography

The average elevation of Haishu District is 2.20 meters. At the beginning of the late Pleistocene, temporary flowing water brought mountain materials from the piedmont to the plain, forming a flooded plain. Later, the weather turned cold and the sea level dropped, forming a banded river on the floodplain. The climate is warmer, the flowing water is active, and the river cutting is intensified. Fenghua River in the east and Guyinda River in the north meet in the north of this city and enter the East China Sea via Zhenhai.

After that, the sea level rose, the cutting of flowing water weakened, and it entered the accumulation stage, resulting in fluvial accumulation strata. In the middle of the late Pleistocene, the sea level continued to rise and rivers shrank, and the northern part of Ningbo Plain evolved into a lake, forming a gray-green loam dominated by lakes, with alluvium covering the accumulation layer.

In the last transgression, most of the plains were submerged, forming coastal wetlands, lakes and swamps. Due to the invasion of tides and the existence of mountains and rivers, it presents a water network landform.

Reference to the above content: Baidu Encyclopedia-Haishu District