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We'll walk you through connecting it if it isn't. Not a member? Sign up now. The most convenient geographic boundary—one that has been adopted by most geographers—is a line that runs south from the Arctic Ocean along the Ural Mountains and then turns southwest along the Emba River to the northern shore of the Caspian Sea ; west of the Caspian, the boundary follows the Kuma-Manych Depression to the Sea of Azov and the Kerch Strait of the Black Sea.

Thus, the isthmus between the Black and Caspian seas, which culminates in the Caucasus mountain range to the south, is part of Asia.

The total area of Asia, including Asian Russia with the Caucasian isthmus but excluding the island of New Guinea , amounts to some 17,, square miles 44,, square km , roughly one-third of the land surface of Earth.

The islands—including Taiwan , those of Japan and Indonesia , Sakhalin and other islands of Asian Russia, Sri Lanka , Cyprus , and numerous smaller islands—together constitute 1,, square miles 3,, square km , about 7 percent of the total.

Although New Guinea is mentioned occasionally in this article, it generally is not considered a part of Asia. Asia has the highest average elevation of the continents and contains the greatest relative relief.

Those physiographic extremes and the overall predominance of mountain belts and plateaus are the result of the collision of tectonic plates.

In geologic terms, Asia comprises several very ancient continental platforms and other blocks of land that merged over the eons.

Most of those units had coalesced as a continental landmass by about million years ago, when the core of the Indian subcontinent broke off from Africa and began drifting northeastward to collide with the southern flank of Asia about 50 million to 40 million years ago.

The northeastward movement of the subcontinent continues at about 2. The impact and pressure continue to raise the Plateau of Tibet and the Himalayas.

The specific features of the coastline in some areas—especially in the east and southeast—are the result of active volcanism; thermal abrasion of permafrost caused by a combination of the action of breaking waves and thawing , as in northeastern Siberia; and coral growth, as in the areas to the south and southeast.

Accreting sandy beaches also occur in many areas, such as along the Bay of Bengal and the Gulf of Thailand. Migration across those barriers has been possible only through mountain passes.

A historical movement of population from the arid zones of Central Asia has followed the mountain passes into the Indian subcontinent. More recent migrations have originated in China , with destinations throughout Southeast Asia.

The Korean and Japanese peoples and, to a lesser extent, the Chinese have remained ethnically more homogeneous than the populations of other Asian countries.

There is a concentration of population in western Asia as well as great concentrations in the Indian subcontinent and the eastern half of China.

There are also appreciable concentrations in the Pacific borderlands and on the islands, but vast areas of Central and North Asia—whose forbidding climates limit agricultural productivity—have remained sparsely populated.

Of those, only Christianity developed primarily outside of Asia; it exerts little influence on the continent, though many Asian countries have Christian minorities.

Buddhism has had a greater impact outside its birthplace in India and is prevalent in various forms in China, South Korea , Japan, the Southeast Asian countries, and Sri Lanka.

Islam has spread out of Arabia eastward to South and Southeast Asia. Hinduism has been mostly confined to the Indian subcontinent. This article surveys the physical and human geography of Asia.

For discussion of individual countries of the continent, see specific articles by name—e. For discussion of major cities of the continent, see specific articles by name—e.

The principal treatment of Asian historical and cultural development is contained in the articles on Asian countries, regions, and cities and in the articles Palestine, history of and Islamic world.

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China's Economic Challenge. What makes the Chinese structure different from English? Why China is so great! The islands—including Taiwan , those of Japan and Indonesia , Sakhalin and other islands of Asian Russia, Sri Lanka , Cyprus , and numerous smaller islands—together constitute 1,, square miles 3,, square km , about 7 percent of the total.

Although New Guinea is mentioned occasionally in this article, it generally is not considered a part of Asia. Asia has the highest average elevation of the continents and contains the greatest relative relief.

Those physiographic extremes and the overall predominance of mountain belts and plateaus are the result of the collision of tectonic plates.

In geologic terms, Asia comprises several very ancient continental platforms and other blocks of land that merged over the eons.

Most of those units had coalesced as a continental landmass by about million years ago, when the core of the Indian subcontinent broke off from Africa and began drifting northeastward to collide with the southern flank of Asia about 50 million to 40 million years ago.

The northeastward movement of the subcontinent continues at about 2. The impact and pressure continue to raise the Plateau of Tibet and the Himalayas.

The specific features of the coastline in some areas—especially in the east and southeast—are the result of active volcanism; thermal abrasion of permafrost caused by a combination of the action of breaking waves and thawing , as in northeastern Siberia; and coral growth, as in the areas to the south and southeast.

Accreting sandy beaches also occur in many areas, such as along the Bay of Bengal and the Gulf of Thailand. Migration across those barriers has been possible only through mountain passes.

A historical movement of population from the arid zones of Central Asia has followed the mountain passes into the Indian subcontinent.

More recent migrations have originated in China , with destinations throughout Southeast Asia. The Korean and Japanese peoples and, to a lesser extent, the Chinese have remained ethnically more homogeneous than the populations of other Asian countries.

There is a concentration of population in western Asia as well as great concentrations in the Indian subcontinent and the eastern half of China. There are also appreciable concentrations in the Pacific borderlands and on the islands, but vast areas of Central and North Asia—whose forbidding climates limit agricultural productivity—have remained sparsely populated.

Of those, only Christianity developed primarily outside of Asia; it exerts little influence on the continent, though many Asian countries have Christian minorities.

Buddhism has had a greater impact outside its birthplace in India and is prevalent in various forms in China, South Korea , Japan, the Southeast Asian countries, and Sri Lanka.

Islam has spread out of Arabia eastward to South and Southeast Asia. Hinduism has been mostly confined to the Indian subcontinent.

This article surveys the physical and human geography of Asia. For discussion of individual countries of the continent, see specific articles by name—e.

For discussion of major cities of the continent, see specific articles by name—e. The principal treatment of Asian historical and cultural development is contained in the articles on Asian countries, regions, and cities and in the articles Palestine, history of and Islamic world.

Related topics are discussed in articles on religion e. Article Media. Info Print Print.

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