Monday, December 22, 2014
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Discovery of Vietnam and Cambodia - 12 days
Day 4 Hanoi - Hue (B/L)  (650km – 1h00: by plane) After breakfast, transfer to the airport to take your morning flight to Hue. Between 1802 and 1945, Hue was the imperial capital of the Nguyen Dynasty. As such, it is well known for its monuments and architecture. Its population stands at about 340,000 people...
Vietnam Discovery - 12 Days Day 1 HANOI - arrival Welcome at the airport and transfer to your selected hotel. Overnight in Hanoi. Day 2 HANOI city (B/L) After breakfast, spend your day taking a tour around the capital...
Vietnam Classic Tour from Hanoi - 14 Days
  Day 1  HANOI arrival (D) When arriving, welcome at the airport and transfer to your selected hotel. Visit the Ho Chi Minh Mausoleum (outside), his former residence, One Pillar Pagoda, Temple of Literature, Hoan Kiem Lake,...
Heritages in Vietnam - 15 days
Day 1 HANOI - arrival
When arriving in Hanoi, transfer to your selected hotel. Overnight in Hanoi. Day 2 HANOI (B/L)...

Vietnam Overview

  • TERRAIN AND MINERAL RESOURCES

    The topography of Vietnam is divided into dear levels
    Most objects protruding from the land's surface are hills and mountains. The gradation tendency is easily visible in mountainous regions, particularly in mountain peaks and highlands where each level has approximately the same elevation:
    Land higher than 2,000 m is often observed in the Hoang Lien Son area.
    Land 1,500 m to 1,800 m high is former peneplain. Areas that were strongly dissected in the past are now just peaks at the same elevation. In places with favorable relief and homogeneous rocky bases, the surface of the peneplain is quite large and less dissected, creating relatively flat areas in mountainous regions such as the calcareous (limestone) highlands of Dong Van, Вас Ha, Sa Pa, and Da Lat. Such places are largely exploited and inhabited, and many have been transformed into touristic sites.
    Land 1,000 m to 1,400 m high is also former peneplain, younger than the Tertiary period, formed from the following elevated cycles and strongly divided. Such terrain occurs frequently in northern mountainous areas, Truong Son and the Central Highlands.
    Land 600 m to 900 m high is level with middle elevation. Such formations are typical of northern mountainous regions and can also be seen at Kon Tum-Play Ku plateau in the Central Highlands.
    Land 200 m to 600 m high includes low and dissected hills and mountains which form a chain. This terrain can be seen in the northern midlands as well as in Central Vietnam and the Southern Central Highlands.
    The topography of Vietnam is divided into dear levels
    Most objects protruding from the land's surface are hills and mountains. The gradation tendency is easily visible in mountainous regions, particularly in mountain peaks and highlands where each level has approximately the same elevation:
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  • Degenerate matter

    Until the beginning of the twentieth century, physicists had never imagined that states of matter could exist which were more dense than those which could be observed on Earth. Water, rock, wood, the human body all have densities within the same order of magnitude: a few grams per cubic centimetre. It was only with the development of the theory of quantum mechanics that scientists were able to understand why ordinary matter has this property.

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  • The mollusc of light

    'Light. . . more light!'

    Goethe’s last words (1832)

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  • Early Islam

    Roots  in  History

    In ancient times, the great civilizations of Mesopotamia and Egypt developed along the river valleys of the Middle East. For a time, both Alexander the Great and the Romans ruled much of the region. Then, around A.D. 630, a new empire and a new religion— Islam—arose in the Middle East.

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