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Area Guides
Tianjin, known as the Bright Diamond of Bohai Gulf and the gateway to the Capital of the People's Republic of China, is one of the biggest business and industrial port cities with a long history in China. As the biggest port city in North China Tianjin under the leadership of Tianjin Municipal Party Committee and the Municipal Government held tight with Deng Xiaoping theoretical banner, are working hard to build Tianjin into a big international modern city. Old businesses have been transformed into modern and profitable enterprises; new areas developed in waste beaches; millions of citizens moved to new houses; multi-corporations, joint-ventures and sole-owned foreign companies established within twenty years of reforming and door-opening. Today 9,500,000 Tianjin people under the leadership of the Party Central Committee with Zemin Jiang as the core leader are confident to bring Tianjin to the new millennium for a brighter and more prosperous future.
History of the City Natural Condition
The history of Tianjin city begins with the opening of Sui Dynasty's Big Canal.   Tianjin became the home and water dock for food and silk transportation from the south to north since mid-Tang Dynasty.  It had been known as 'Zhigu Stockade' in Song , Jin Dynasties, and changed into 'Haijin Town' in Yuan Dynasty. At that time, it was one of the most important military towns and canal-food transportation center.

In the second year of Yongle in Ming Dynasty (1404), the city was established with defense walls and then called ' Tianjin Wei'. Since 17th century, its economy and society developed fast, and the city's size had been enlarged continually. In 1860, it was appointed as a business and communication center. Being the second largest industry and business city and the finance, trade center of the north, its industrial production and trade volume listed merely next to Shanghai.

In 1931, there were over 17,000 firms in Tianjin and about 4,000 industrial and handicraft shops that mainly dealt with machine-repairing. The export volume was 25% of the nation's total amount. In 1935, Tianjin had ten domestic-invested banks ,93 branches and offices and 16 foreign-invested ones.
When the People's Republic of China established in 1949, Tianjin City's area was 61km2 with 1,790,000 residents. Then in 1973, after several times administrative area modifications, the present administrative distribution of districts, counties ,etc,.were set up.

Tianjin used to be a vast sea with no land or people lived on. Its landscape was formed gradually over long time of land reshaping and the withdrawal of the sea.

Geology Structure

Tianjin area is made up of remote antiquity division, antiquity division, ancient division, mid division and new division stratums. Tianjin lies at the joint part of two structural systems----Yan Mountain Latitudinal structural system and New Huaxia structural system. Tianjin urban district stands on the northern point of the bulging Cang County.

Land Countenance

Tianjin's land countenance has the characteristic of higher north & west, lower south & east. The Eight Immortals Table ( alias: Grasshopper Cage ), the highest peak's elevation is as high as 1,052 meters and Dagukou, the lowest place's elevation is zero. There are altogether four types of land countenances: mountain lands, hills, plains and coastlands. The mountain lands' area is approximately 651km2, occupying 5.75% of the total area and scattering in the north part of Ji County. The hills' elevations are below 200m, the relative height is 50-100m and scatter in the south side of Ji County's Yan Mountain. Plains are Tianjin lands' main parts, covering 10,664km2 , occupying 94% of the total area and scattering from the south of Yan Mountain to the vast regions on Bohai Sea banks.

Climate

Tianjin situates on the east bank of Euro-Asia Continent which belongs to the mid latitude. The four seasons are obviously different and the scenery is various. It stands on the transitional belt between continental climate and oceanic climate, belonging to the semi-moist warm monsoon climatic zone. The main characteristic is notable monsoon and distinguish temperature variation. In winter, the wind is mostly northward, it's cold, dry and the precipitation is very small; in summer, the wind is mostly southeastward or southward, the temperature is rather high and the precipitation is concentrated. The average annual temperature is above 110C , the average no-frost period is about 190 days, the average annual precipitation is about 600mm and the average annual sun-shining time amounts to 2610 - 3090 hours.

 
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