The Chang Jiang Basins are warm and wet. The North China Plain is drier and often cooler - False
Unlike the Taklamakan Desert, the Gobi has very few sand dunes. Most of the desert is stony. - True
The silt comes from the Gobi Desert. It is carried by the rivers to the North China Plain. - True
In the past 3,000 years, the river is said to have flooded more that 2,500 times, causing much damage and loss of life - False
Based on geographical concepts, It is False that the Chang Jiang Basins are warm and wet. The North China Plain is drier and often cooler. The Climate and Vegetation of Chang Jiang Basins and North China PlainThe climate of Chang Jiang Basins are considered warmer and cooler. The vegetation is characterized by thick rainforests. The basins are considered favorable for growing rice, which needs lots of warmth and moisture.
The North China Plain is drier and often cooler. Because it is the other way round. Also, it is True that unlike the Taklamakan Desert, the Gobi has very few sand dunes. Most of the desert is stony. And it is False that in the past 3,000 years, the river is said to have flooded more than 2,500 times, causing much damage and loss of life. Because it has only flooded more than 1,500 times. Hence, in this case, it is concluded that the climate and vegetation of China are dynamic and peculiar.
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