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The NORTH CHINA PLAIN (Chinese : 華北平原; pinyin : Huáběi Píngyuán) is based on the deposits of the Yellow River
Yellow River
and is the largest alluvial plain of China. The plain is bordered to the north by the Yanshan Mountains , to the west by the Taihang Mountains , to the south by the Dabie and Tianmu Mountains , and to the east by the Yellow Sea
Yellow Sea
. The Yellow River
Yellow River
flows through the middle of the plain into Bohai Sea.

Below the Sanmenxia Dam is the multipurpose Xiaolangdi Dam , located in the river's last valley before the North China Plain, a great delta created from silt dropped at the Yellow River's mouth over the millennia. The North China Plain
North China Plain
extends over much of Henan, Hebei, and Shandong provinces. and merges with the Yangtze
Yangtze
delta in northern Jiangsu and Anhui provinces. The Yellow River
Yellow River
meanders over the fertile, densely populated plain emptying into the Bohai Sea. The plain is one of China's most important agricultural regions, producing corn, sorghum, winter wheat , vegetables, and cotton. Its nickname is "Land of the yellow earth."

The southern part of the plain is traditionally referred to as the Central Plain (pinyin : Zhōngyuán), which formed the cradle of Chinese civilization.

The plain covers an area of about 409,500 square kilometers (158,100 sq mi), most of which is less than 50 metres (160 ft) above sea level. This flat yellow-soil plain is the main area of sorghum , millet , maize , and Kaleb Cotten production in China. Wheat
Wheat
, sesame seed , and peanuts are also grown here. The plain is one of the most densely populated regions in the world.

Beijing
Beijing
, the national capital, is located on the northeast edge of the plain, with Tianjin
Tianjin
, an important industrial city and commercial port, near its northeast coast. Shengli Oilfield in Shandong is an important petroleum base. It is also home to the Yellow River.

CONTENTS

* 1 Historical significance * 2 See also * 3 References * 4 External links

HISTORICAL SIGNIFICANCE

The geography of the North China Plain
North China Plain
has had profound cultural and political implications. Unlike areas to the south of the Yangtze, the plain generally runs uninterrupted by mountains and has far fewer rivers, and as a result communication by horse is rapid within the plain. As a result, the spoken language is relatively uniform in contrast to the plethora of languages and dialects in southern China. In addition the possibility of rapid communication has meant that the political center of China has tended to be located here.

Because the fertile soil of the North China Plain
North China Plain
gradually merges with the steppes and deserts of Dzungaria , Inner Mongolia
Inner Mongolia
, and Northeast China
Northeast China
, the plain has been prone to invasion from nomadic or semi-nomadic ethnic groups originating from those regions, prompting the construction of the Great Wall of China
Great Wall of China
.

Although the soil of the North China Plain
North China Plain
is fertile, the weather is unpredictable, being at the intersection of humid winds from the Pacific and dry winds from the interior of the Asian continent. This makes the plain prone to both floods and drought. Moreover, the flatness of the plain promotes massive flooding when river works are dama