Continent: Difference between revisions
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A '''continent''' is a large landmass. On [[earth]], seven areas are generally regarded as continents: [[North America]], [[South America]], [[Europe]], [[Asia]], [[Africa]], [[Australasia]] and [[Antarctica]]. The definition can include the landmass and its nearby islands (thus for example, Australasia rather than just [[Australia]]).<ref>See [http://www.merriam-webster.com/dictionary/continent?show=1&t=1293805404 Webster's dictionary].</ref> | A '''continent''' is a large landmass. On [[earth]], seven areas are generally regarded as continents: [[North America]], [[South America]], [[Europe]], [[Asia]], [[Africa]], [[Australasia]] and [[Antarctica]]. The definition can include the landmass and its nearby islands (thus for example, Australasia rather than just [[Australia]]).<ref>See [http://www.merriam-webster.com/dictionary/continent?show=1&t=1293805404 Webster's dictionary].</ref> | ||
Continents exist for geological reasons. Their [[Crust (geology)|crust]]s are much thicker and lighter than those of [[ocean]]s, so that they correspond to emerged land. From the point of view of geology, and more precisely in the theory of [[plate tectonics]], there are more continents than | Continents exist for geological reasons. Their [[Crust (geology)|crust]]s are much thicker and lighter than those of [[ocean]]s, so that they correspond to emerged land. From the point of view of geology, and more precisely in the theory of [[plate tectonics]], there are more continents than in geography. In plate tectonics, for example, [[Arabia]] constitutes a separate [[Plate (geology)|plate]], partially constituted by continental crust. | ||
==Footnotes== | ==Footnotes== | ||
{{reflist}} | {{reflist}} | ||
Revision as of 13:22, 31 December 2010
A continent is a large landmass. On earth, seven areas are generally regarded as continents: North America, South America, Europe, Asia, Africa, Australasia and Antarctica. The definition can include the landmass and its nearby islands (thus for example, Australasia rather than just Australia).[1]
Continents exist for geological reasons. Their crusts are much thicker and lighter than those of oceans, so that they correspond to emerged land. From the point of view of geology, and more precisely in the theory of plate tectonics, there are more continents than in geography. In plate tectonics, for example, Arabia constitutes a separate plate, partially constituted by continental crust.
Footnotes
- ↑ See Webster's dictionary.