A continent is one of several large landmasses. Up to seven regions are commonly regarded as continents. The continents correspond to areas of continental crust that are found on the continental plates. In modern schemes with five or more recognised continents, at least one pair of continents is joined by land in some way.
About Continent in brief

The single American continent model remains more common in some Asian models than the single continent model in the six- Continent model of the World Series of Nations. However, Europe is widely considered a continent with its comparatively large area of 10,180,000 square kilometres, while South Asia is considered a sub- continent of Europe with less than half that area. In the world of the Six Nations, Europe and South Asia are peninsulas of the Eurasian landmass, while North America, South Asia, and Antarctica are separate continents. In both cases, there is no complete separation of these landmassed by water. Both these isthmuses are very narrow compared to the bulk of the land masses they unite. In the six continents model, North America is considered two separate continents: Europe and Asia and South. America is also viewed as one continent known as America. This viewpoint was common in the United States until World War II, and remains prevalent in some European and Asian models of world geography. The single America continent model is a view that is completely disregarded if the continuous landmass of American countries is considered to be two continents: Eurasia and America. The world-wide view of geology and geology—inology and geography—that Eurasia is a single continent is a continent in a six- continent model of the world of six continents.
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This page is based on the article Continent published in Wikipedia (as of Dec. 14, 2020) and was automatically summarized using artificial intelligence.






