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Southeast Asia is geographically divided into two subregions, namely Mainland Southeast Asia (or the Indochinese Peninsula) and Maritime Southeast Asia. Mainland Southeast Asia includes: Cambodia, Laos and Vietnam: Cambodia; Laos; Vietnam; Myanmar, Thailand and West Malaysia: Myanmar; Thailand; West Malaysia; Maritime Southeast Asia includes:
Apr 16, 2021 · Mainland Southeast Asia comprises six countries; Laos, Cambodia, Singapore, Myanmar, Vietnam, and Thailand. The other five countries, except part Western New Guinea (Indonesia), form Maritime Southeast Asia. Corals reefs and islands seen from the peak of Bohey Dulang Island, Sabah, Malaysia.
Southeast Asia consists of eleven countries that reach from eastern India to China, and is generally divided into “mainland” and “island” zones. The mainland ( Myanmar, Thailand, Laos, Cambodia, and Vietnam) is actually an extension of the Asian continent.
The history of Southeast Asia covers the people of Southeast Asia from prehistory to the present in two distinct sub-regions: Mainland Southeast Asia (or Indochina) and Maritime Southeast Asia (or Insular Southeast Asia). Mainland Southeast Asia comprises Cambodia, Laos, Myanmar (or Burma), Peninsular Malaysia, Thailand and Vietnam whereas ...
It began as early as 4000 bce, when Taiwan was populated from the Asian mainland, and subsequently it continued southward through the northern Philippines (3rd millennium bce ), central Indonesia (2nd millennium bce ), and western and eastern Indonesia (2nd and 1st millennia bce ).
South East Asia consists of two geographic regions: The Asian mainland and island arcs and archipelagoes to the east and southeast. The mainland section consists of Cambodia, Laos, Myanmar, Thailand, and Vietnam. Tai peoples and Austroasiatic peoples dominate.
Mainland Southeast Asia is entirely in the Northern Hemisphere. East Timor and the southern portion of Indonesia are the parts of Southeast Asia that lie south of the Equator. Quick Facts Area, Population ... Close. The region lies near the intersection of geological plates, with both heavy seismic and volcanic activities.
