South asian countries and map
Its physical landscapes, political units, and ethnic groups are both wide-ranging and many. South Asia extends south from the main part of the continent to the Indian Ocean. The western boundary is the desert region where Pakistan shares a border with Iran. Hinduism, Islam, and Buddhism are the top three religions of South Asia.
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Map of Asia
Map of South-East Asia - Nations Online Project
Culture BLM. Black Music. Palmtrees, rivers, and mountains, a typical landscape in Mainland Southeast Asia. The Mekong River is a significant stream in Asia. It is fed at its source from melting snow of the Tibetan plateau, and further south, it forms several sections of the borders between Myanmar Burma , Laos, and Thailand; the river empties into the South China Sea in Southern Vietnam. Image: kk nationsonline. Map of Southeast Asia Political Map of Southeast Asia The map shows the countries and main regions of Southeast Asia with surrounding bodies of water, international borders, major volcanoes, major islands, main cities, and capitals.
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South Asian Countries
South Asia is the southern region of Asia , which is defined in both geographical and ethno-cultural terms. The Amu Darya , which rises north of the Hindu Kush , forms part of the northwestern border. However, the total area of South Asia and its geographical extent is not clear cut as systemic and foreign policy orientations of its constituents are quite asymmetrical. The common definition of South Asia is largely inherited from the administrative boundaries of the British Raj,  with several exceptions.
The region is bounded to the north by a series of mountain ranges: the Hindu Kush to the northwest, the Karakoram Range in the central north, and the Himalayas to the northeast. South of the mountains is the Indo-Gangetic Plain, formed from the combined alluvial plains of the Indus , Ganges Ganga , and Brahmaputra rivers, which lie in a deep marginal depression running north of and parallel to the main range of the Himalayas. It is an area of subsidence into which thick accumulations of earlier marine sediments and later continental deposits have washed down from the rising mountains.
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