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Vietnam map of Köppen climate classification Hundreds of active fires burning across the hills and valleys of Myanmar, Thailand, Laos, and Vietnam (labelled with red dots). Vietnam's climate, being located in the tropics and strongly influenced by the South China Sea has a monsoon-influenced climate typical of that of mainland Southeast Asia.
Printable version; In other projects ... Squares in Vietnam by city (2 C) D. Geography of Da Nang (3 C) H. Geography of Hanoi (6 C, 4 P)
An enlargeable topographic map of Vietnam. Geography of Vietnam. Vietnam is: a country; Location: Northern Hemisphere and Eastern Hemisphere; Eurasia Asia Southeast Asia Indochina; Time zone: UTC+07; Extreme points of Vietnam High: Fan Si Pan 3,143 m (10,312 ft) Low: South China Sea 0 m; Land boundaries: 4,639 km Laos 2,130 km China 1,281 km
Grand-waterfall dam, Mù Cang Chải Terrace, Lũng Lô Hill, Flag of Vietnam, Nelumbo nucifera: Province as of 11 April 1900. Sơn La: Tinh hoa miền Tây Bắc (The essence of the Northwest) Tô Hiệu Sonla dam, Brocade, Flag of Vietnam, wheat: Vạn Bú province from 10 October 1895, then Sơn La province as of 23 August 1904.
The national symbols of Vietnam are official and unofficial flags, icons or cultural expressions that are emblematic, representative or otherwise characteristic of Vietnam and of its culture. Symbol [ edit ]
Cities in Vietnam are identified by the government as settlements with considerable area and population that play important roles vis-a-vis politics, economy and culture. Status of cities falls into four categories: special, first class ( I ), second class ( II ), and third class ( III ).
Printable version; In other projects ... Populated places in Vietnam by province (63 C) A. ... Geography of Da Nang (3 C) Geography of Đắk Lắk province (4 C, 2 P)
The geology of Vietnam is divided into five structural blocks : Northeast (NE), Northwest (NW), Truongson, Kon Tum and Nambo. The NE block is a part of the South China plate , in which strata and igneous rocks have been found dating from the Early Paleozoic to the Quaternary .
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