Indian subcontinent
From Wikipedia, the free encyclopedia
- This article deals with the geophysical region in Asia. For geopolitical treatments, see South Asia.
The Indian subcontinent is a large section of the Asian continent consisting of countries lying substantially on the Indian tectonic plate. These include countries on the continental crust (India, Pakistan, Bangladesh, Nepal and Bhutan), an island country on the continental shelf (Sri Lanka), and an island country rising above the oceanic crust (the Maldives). The term subcontinent signifies "having a certain geographical or political independence" from the rest of the continent,[1] or "a vast and more or less self-contained subdivision of a continent."[2] See "Geography" below for definition of "subcontinent". However, there is view held by some that this land formed from the Indian continental tectonic plate should be considered as a continent, owing to its geographical isolation by the Himalayas from Eurasia. [3]
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[edit] Nomenclature and usage
Although the term Indian subcontinent is often used geographically, it is not entirely a geographical term. The approximately equivalent but more geopolitical term is, South Asia or Southern Asia, however, sometimes includes territories found external (but proximal) to the Indian Plate—including Tibet and Myanmar (formerly Burma). The subcontinent is surrounded by three water bodies: the Bay of Bengal, the Indian Ocean and the Arabian Sea. Historically, India was known as Hindustan in medieval times during the Islamic period. Nepal and Bhutan were the only two countries in the region which were not a part of British Raj.
[edit] Geography
- See also: Geography of India, Geography of Pakistan, and Geography of Bangladesh
Geographically, the Indian subcontinent is a peninsular region south of the Himalayas and Kuen Lun mountain ranges and east of the Hindu Kush mountain range and Balochistan region, extending southward into the Indian Ocean between the Arabian Sea (to the southwest) and the Bay of Bengal (to the southeast). It covers about 4,480,000 km² (1,729,738 mi²) or 10 percent of the Asian continent; however, it accounts for about 40 percent of Asia's population.
[edit] Climate
- See also: Climate of India
The climate of South Asia is called the Monsoon climate. It is quite opposite of the Mediterranean climate. For the monsoon climate, the weather in this region remains humid during summer and dry during winter. Instead of four seasons, it basically has two main seasons, the wet and dry. The monsoon climate favors the cultivation of jute, tea, rice, and various vegetables in this region. South Asia's climate varies from tropical monsoon in south to temperate in north.
[edit] Geological history
In the Eocene period the Indian subcontinent was an island continent in the Indian Ocean. It was originally part of Gondwanaland. See Continental drift.
[edit] Politics
India, the largest democracy, is the dominant political power in the region followed by Pakistan.
[edit] See also
| SAARC Portal |
- South Asia
- History of South Asia
- History of India
- Indology
- Etymology of the names of India
- India (disambiguation)
- Plate tectonics
- Continental drift
[edit] References
- ^ Oxford English Dictionary 2nd edition. 1989. Oxford University Press.
- ^ Webster's Third New International Dictionary, Unabridged. 2002. Merriam-Webster. retrieved 11 March 2007.
- ^ The Indian Continent[1]
[edit] External links
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