East Asia is surrounded by a series of mountain ranges in the west, Mongolia, and Russia in the north, and Southeast Asia to the south. The Himalayas border Tibet and Nepal; the Karakoram Ranges, Pamirs, and the Tian Shan Mountains shadow Central Asia; and the Altay Mountains are next to Russia. The Himalayan Mountains are among the world’s highest mountain ranges, and Mt. Everest is the planet’s tallest peak. These high ranges create a rain shadow effect, generating the dry arid conditions of type B climates that dominate western China. The desert conditions of western China give rise to a sizeable uninhabitable region in its center. Melting snow from the high elevation feeds many of the streams that transition into the major rivers that flow toward the east.
Created by tectonic plate action, the many mountain ranges are also home to earthquakes and tremors that are devastating to human livelihood. The Indian tectonic plate is still pushing northward into the Eurasian plate, forcing the Himalayan ranges upward. With an average elevation of fifteen thousand feet, the Tibetan Plateau is the largest plateau region of the world. It has high elevations and type H climates. The plateau is sparsely populated, and the only places with human habitation are the river valleys. Lhasa is the largest city of the sparsely populated region. Sometimes called “the Roof of the World,” the Tibetan Plateau is a land of superlatives. The small amount of precipitation that occurs often comes in the form of hailstorms mixed with wind. Its landscape is generally rocky and barren.
The vast arid regions of western China extend into the Gobi Desert between Mongolia and China. Colder type D climates dominate the Mongolian steppe and northern China. The eastern coast of the Asian continent is home to islands and peninsulas, which include Taiwan and the countries of Japan and North and South Korea. North Korea’s type D climates are similar to the northern tier of the United States, comparable to North Dakota. Taiwan is farther south, producing a warmer tropical type A climate. The mountainous islands of Japan have been formed because of tectonic plates and are prone to earthquakes. Since water moderates temperature, the coastal areas of East Asia have more moderate temperatures than the interior ones. A type C climate is dominant in Japan, but the north has a colder type D climate. The densely populated fertile river valleys of central and southeastern China are matched by contrasting economic conditions. Fertile alluvial soils and moderate temperatures create excellent farmland that provides enormous food production to fuel an ever-growing population.
Most of China’s population lives in its eastern region, called China Proper, with type C climates, freshwater, and good soils. China Proper has dense population clusters that correspond to the areas of type C climate that extend south from Shanghai to Hong Kong. Around the world, most humans have gravitated toward type C climates. These climates have produced fertile agricultural lands that provide an abundance of food for the enormous Chinese population. To the south, the temperatures are warmer, with hot and humid summers and dry, warm winters. The climates of China Proper are conducive for human habitation, which has transformed the region into a highly populated human community. The North China Plain at the mouth of the Yellow River (Huang He River) has productive farmland and is the most densely populated region in China.
Northwest of Beijing is Inner Mongolia and the Gobi Desert, a desert that extends into the independent country of Mongolia. Arid type B climates dominate the region to the southern half of Mongolia. The northern half of Mongolia is colder with continental type D climates. In the higher elevations of the highlands in western Mongolia, there is a section of type H highland climates. Its climate and location identify Mongolia as a landlocked country in the northern latitudes with a low level of precipitation. The areas of type D climate that extend north from Beijing through Northeast China at times receive more precipitation than northern Mongolia. Northeast China features China’s vast forests and excellent agricultural land. Many of China’s abundant natural mineral resources are found in this area. Balancing mineral extraction with the preservation of agricultural land and timber resources is a perennial issue.
Lying north of the Great Wall and encompassing the autonomous region of Inner Mongolia is the vast Mongolian steppe, which includes broad flat grasslands that extend north into the highlands. North China includes the Yellow River basin as well as the municipalities of Beijing and Tianjin. Areas around parts of the Yellow River are superb agricultural lands, including vast areas of loess that have been terraced for cultivation. Loess is extremely fine silt or windblown soil that is yellow in this region. Deciduous forests continue to exist in this region, despite aggressive clearcutting for agricultural purposes. The Great Wall of China rests atop hills in this region.
Most of western China is arid, with a type B climate. Western China has large regions like the Takla Makan Desert that are uninhabited and inhospitable because of hot summers and long cold winters exacerbated by the cold winds sweeping down from the north. In a local Uyghur language, the name Takla Makan means, “You will go in, but you will not go out.” To the far west are the high mountains bordering Central Asia that restrict travel and trade with the rest of the continent. Northwestern China is a mountainous region featuring glaciers, deserts, and basins.
The central portion of China Proper is subtropical. This vast region includes the southern portion of the Yangtze River (Chang Jiang River) and the cities of Shanghai and Chongqing. Alluvial processes give this area prime agricultural land. Its climate is warm and humid in the summers with mild winters; monsoons create distinct summer rainy seasons. Tropical China lies in the extreme south and includes Hainan Island and the small islands that neighbor it. Annual temperatures are higher here than in the subtropical region, and rainfall amounts brought by the summer monsoons are at times very substantial. Low mountains and hills characterize this area.
River Basins of China
Two major river systems provide fresh water to the vast agricultural regions of the central part of China Proper. The Yellow River (Huang He River) is named after the light-colored silt that washes into the river. It flows from the Tibetan highlands through the North China Plain into the Yellow Sea. Dams, canals, and irrigation projects along the river provide water for extensive agricultural operations. While wheat, sorghum, corn, and soybeans are common with vegetables, fruit, and tobacco grown in smaller plots. The North China Plain must grow enough food to feed its one thousand people per square mile average density. This plain does not usually produce a food surplus because of the high demand from the large population of the region. Beijing borders the North China Plain. Its nearest port, Tianjin, continues to expand and grow, creating an economic center of industrial activity that relies on the peripheral regions for food and raw materials. Cotton is an example of a key industrial crop grown here.
The Yangtze River (Chang Jiang River) flows out of the Tibetan Plateau through the Sichuan Province, through the Three Gorges region and its lower basin into the East China Sea. Agricultural production along the river includes extensive rice and wheat farming. Large cities are often located along this river, including Wuhan and Chongqing. Nanjing and Shanghai are situated near the delta on the coast. Shanghai is the largest city in China and is a growing metropolis. The Three Gorges Dam of the Yangtze River is the world’s largest dam. It produces a large percentage of electricity for central China. Oceangoing ships can travel up the Yangtze to Wuhan and, utilizing locks in the Three Gorges Dam, these cargo vessels can travel all the way upriver to Chongqing. The Yangtze River is a valuable and vital transportation corridor for transporting goods between periphery and core and between the different urban centers of activity. Sichuan is among the top five provinces in China in terms of population and is dependent on the Yangtze River system to provide for its needs and connect it with the rest of China.
Northeast China was formerly known as Manchuria, named after the Manchu ethnic group, which had dominated the region in Chinese history. Two river basins create a favorable industrial climate for economic activity. The lower Liao River Basin and the Songhua River Basin cut through Northeast China, along the cities of Harbin and Shenyang to be located there. This region is known as the Northeast China Plain. It has extensive farming activities located next to an industrial landscape of smokestacks, factories, and warehouses. Considerable mineral wealth and iron ore deposits in the region have augmented the industrial activities and have created severe environmental concerns because of excessive air and water pollution. In its zenith in the 1970s, this was China’s leading steel production area, but the region is being reduced to a rustbelt since many of China’s manufacturing centers are now being developed in the southern regions of China Proper.
The southernmost region of China Proper is home to the Pearl River Basin, an important agricultural and commercial district. Though smaller in size than the Yangtze River Basin, major global urban centers are located on its estuary, where the mouth of the river flows into the South China Sea. The system includes the Xi River, Pearl River, and their tributaries. As the third-longest river system in China, these rivers process an enormous amount of water and have the second-highest volume of water flow after the Yangtze. Guangzhou, Macau, and Hong Kong are the most significant cities in the rapidly expanding industrial center of Shenzhen. As mentioned earlier, Macau was a former Portuguese colony, and Hong Kong was a former British colony. These urban areas are now hubs for international trade and global commerce. Guangzhou is one of China’s largest cities, along with Shanghai, Beijing, Wuhan, and Tianjin. Cantonese heritage and traditions form a foundation for the cultural background of the people who live here.
China Doesn’t Want Your Trash
Watch the video “China Doesn’t Want Your Trash” from PolyMatter and consider the following:
- Why was China buying the majority of the world’s trash?
- Describe why China decided to stop accepting the world’s trash in 2017.
- Three Gorges Dam (The New China Dam)
The Three Gorges Dam on the Chang Jiang River (also called the Yangtze River) is known in China as the New China Dam. Its hydroelectric production system is the largest on Earth. The river system is the world’s third longest, after the Nile and the Amazon. Ideas for this project go back to the days just after the last dynasty fell. Plans and development began in the decades before 1994 when the construction of the dam began. The primary purposes of the dam are to control the massive flooding along the Chang Jiang, produce hydroelectric power, and increase shipping capacity along the river.
- Dam length: 7,661 feet
- Dam height: 610 feet
- Dam width (at base): 377 feet
- Physical construction began December 14, 1994
- Construction cost: estimated thirty-nine billion US dollars
- Estimated surface area of the reservoir: 403 square miles
- Estimated length of the reservoir: 375 miles
- Capacity of thirty-two generators totaling 22,500 MW (equivalent to about twenty nuclear power plants the size of the Watts Bar 1, the newest US nuclear reactor)
Before the construction of the dam, flooding along the Chang Jiang cost thousands of lives and billions of dollars in damage. In 1954, the river flooded, causing the deaths of more than thirty-three thousand people, and displacing an additional eighteen million people. The large city of Wuhan was flooded for three months. In 1998, a similar flood caused billions of dollars in damage, flooded thousands of acres of farmland, resulted in more than 1,526 deaths, and displaced more than 2.3 million people. The dam was rigorously tested in 2009 when a massive flood worked its way through the waterway. The dam was able to withstand the pressure by containing the excess water and controlling the flow downstream. The dam saved many lives and prevented billions of dollars in potential damage. The savings in human lives and in preventing economic damage are projected to outweigh the dam’s ecological destruction and financial cost within a few decades.
The dam produces most of the electricity for the lower Chang Jiang Basin, including Shanghai, the largest city in China. Five years of the dam producing electricity has already paid for about one-third of its construction costs, which is equivalent to burning approximately 150 million tons of coal (depending on coal quality). This reduces the emission of millions of tons of carbon dioxide, sulfur, and nitrogen oxides into the atmosphere, which reduces air pollution and does not contribute to climate change. Heavy freight traffic on the Yangtze was the norm even before the dam was built; in fact, it has the highest rates of transport of any river. The building of the dam has augmented the amount of freight traffic.
All the positive attributes of the Three Gorges Dam have contributed to the economic development of China. This is a testimony to the engineering and technological capacity of the nation. However, this project has also created its problems and negative impacts on culture and the environment. By 2008, the number of people forced to relocate from the flooding of the reservoir had reached 1.24 million. Historic villages and hundreds of archaeological sites were flooded. Thousands of farmers had to be relocated, without compensation, to places with less productive soils. Sadly, much of the scenic beauty of the river basin is now underwater.
Animal species like the critically endangered Siberian Cranes, who had wintered in the former wetlands of the river, had to find habitat elsewhere. The endangered Yangtze River Dolphin has been doomed to extinction because of the dam and the amplified river activity. The dam restricts the flushing of water pollution and creates a massive potential for landslides along its banks, exacerbating the potential for the silting in of the reservoir and the clogging of the dam’s turbines. The dam also sits on a fault zone, and there is a concern that the water’s massive weight in the reservoir could trigger earthquakes that may destroy the dam, with catastrophic consequences. Large development projects tend to have an enormous impact on the people and the environment that inhabit their shadow. The building of the Three Gorges Dam has created controversy, with strong arguments on both sides of the issues. Other large dams are being proposed to complicate the situation further or are under construction along the same river.
Much of what unites this region is its instability, not necessarily in terms of geopolitics, but rather its physical landscape. East and Southeast Asia are located in the Pacific Ring of Fire, an area of high tectonic activity along the Pacific Ocean basin. The vast majority of the world’s earthquakes, around 90 percent, occur along this geologically unstable area.
In this region, tectonic collisions have shaped the physical landforms present in the region and present numerous natural hazards. Volcanoes erupt in this region frequently, and many of the islands in this region were formed from a variety of historical volcanic eruptions. For example, the majestic Mount Fuji, Japan’s highest mountain peak, is an active volcano that last erupted in the early 18th century. The 1815 eruption of Indonesia’s Mount Tambora, one of its many active volcanoes, was so powerful that it cooled global temperatures and caused crop failures as far away as Egypt and France. In 1883, the volcanic island of Krakatoa, between the Indonesian islands of Java and Sumatra, erupted with such an explosion that it collapsed. Tens of thousands died, and it took several years for global weather patterns to return to normal. The sound of the eruption is considered the loudest sound in modern history and could be heard from over 4,800 kilometers (3,000 miles) away. (Finlayson, 2019)
In 2011, the most powerful earthquake to ever hit Japan, a magnitude 9.0, resulted in over 40 meters (131 feet) high in tsunami waves in some areas. The earthquake and subsequent tsunami leftover 15,000 dead and damaged hundreds of thousands of buildings. Most notably, the tsunami-damaged Japan’s Fukushima Daiichi Nuclear Power Plant causing a series of nuclear meltdowns and the release of radioactive material.
While nothing can stop Earth’s massive tectonic plates from moving, warning systems, land use planning, and public education could help prevent casualties. After the 2004 Indonesian earthquake and tsunami, the international community created an Indian Ocean tsunami warning system. Although some of the hardest-hit areas would have had only minutes to find higher ground, the warning system could have had a significant impact in alerting areas ahead of the wave. In Japan, earthquake drills are standard, and strict building codes ensure that buildings can withstand most seismic activity.
In addition to these geologic hazards, typhoons are also frequent in this region. Typhoons, the term for tropical cyclones in the northwestern region of the Pacific Ocean, routinely make landfall in East Asia. The region has more tropical cyclone activity than anywhere else on Earth. Most storms form in the summer between June and November, and the Philippines’ islands are generally the hardest hit. Monitoring systems have been in place in the region for several decades and have helped to minimize these powerful storm systems’ impacts. (Finlayson, 2019)