3.6: Geography of East Asia
In the second millennium BCE, China’s first dynasty began. Historically, the bulk of the ancient Chinese population lived in China proper (see Map \(\PageIndex{1}\)). To the east, China proper is bounded by the Yellow Sea, East China Sea, and the South China Sea. To the south are the mountainous jungles of Southeast Asia. To the west and north, China is rimmed by a transitional frontier zone where land suited to agriculture gives way to mountains and plateau or vast expanses of steppe grasslands and desert. At times, the dynasties of China became actively involved in all of these neighboring areas, incorporating them directly into their expanding empires or indirectly as subordinate, tribute-paying states. Those areas included parts of the modern-day Korean Peninsula, Northeast China, Mongolia, Central Asia, and Vietnam.
Within China proper, two rivers were particularly important to the formation of agricultural communities: the Yellow River and Yangzi River . The Yellow River meanders through the northern half of China, where a cool, dry climate is well-suited to wheat and millet farming. Beginning far to the west, this river meanders over dusty plateau, becomes muddied with silt, and then deposits this sediment along its middle and lower reaches. The plains surrounding these reaches are collectively referred to as the North China Plain . Historically, this was the heartland of Chinese civilization. However, the Yangzi River was just as important. Located in south China where the weather is relatively warmer and wetter, its long basin provided fertile soil for rice-paddy agriculture. Over time, the early dynasties expanded into and included the settled agricultural communities in this region.
Japan is an island country consisting of four main islands and many smaller ones located off the Pacific coast of the Asian continent. At 400,000 square kilometers, the terrain is more rugged, covered by mountains, and traversed by numerous rivers. Only fifteen percent of the land is suited to agriculture. Much of that was concentrated in two plains–the Kinai Plain and Kanto Plain–making them particularly important to Japan’s early history. Japan is also located along the Pacific Ring of Fire, where tectonic plates composing the earth’s crust frequently move and collide. That is why earthquakes and volcanic activity have been a constant threat to populations living on these islands.
The Korean Peninsula is the location of North and South Korea today. Prior to the twentieth century, it saw a long succession of Korean kingdoms. Extending roughly 1100 kilometers southward from the Asian landmass, the peninsula is bounded by seas to the east, west, and south, and defined by the Yalu River to the north. BBcause the peninsula lies between China to the north and west and Japan to the east, Korean dynasties have been deeply impacted by these states’ histories and cultures. Like Japan, Korea is also mountainous, although coastal areas and plains located to the west and south were well-suited to agriculture.
The countries of East Asia share in the region’s temperate climate and summer monsoon season. During the summer months, warm and moist air originating from the Pacific flows from southeast to northwest, while during the winter months cold and dry air originating from Central Asia moves in the opposite direction. Thus, those areas of East Asia located further to the east and south are generally warmer and wetter, and for longer periods of time. This climate is well-suited to rice-paddy agriculture, and rice consequently became the primary cereal crop in southern China, the Korean peninsula, and the islands of Japan. While growing rice is labor-intensive, this grain also offers high yields per unit of land, so it has supported population growth in these countries and, therefore, the formation of vibrant civilizations.