In 1962, Ha Long Bay
was recognized as a vestige and beauty spot of national
significances by Ministry of Culture and Information of Viet Nam and
was also recognized as a world national heritage site twice by UNESCO
organization. The first time, in 1994 for the exceptional and
universal value of the landscape and the second time in 2000 for the
special value of geology and geomorphology. In 2011, Ha Long Bay,
recently listed as one of the new seven wonders of the world.
The geomorphology of Ha Long Bay is known as a drowned karst
landscape due to the exceptional combination of its limestone karst
features which have been subject to repeated regression and
transgression of the sea over geological time. The limestones of Ha Long
Bay have been eroded into a mature landscape of fengcong (clusters of
conical peaks) and fenglin (isolated tower features) karst features,
modified by sea invasion at a later stage.
The smaller islands are fenglin towers of 50m to 100m high with
height. Many have vertical walls on all or most sides and these continue
to evolve by rock falls and large slab failures.
Marine invasion of Ha Long Bay has added an extra element to the
normal process of lateral undercutting of the limestone towers and
islands. The most conspicuous feature being the main notch cut into the
entire rocky coastline. Notches are a feature of limestone cliffs
worldwide, but those of Ha Long Bay are exceptionally well developed
and, at many sites, extend into arches and caves. This process of
undercutting and subsequent erosion maintains the steep faces of the
fenglin karst towers and thereby perpetuates the spectacular nature of
the landscape.
A distinctive feature of Ha Long Bay is the abundance of lakes within
the larger limestone islands.Extensive limestone caves represent
another important feature of Ha Long Bay, with three main types able to
be identified: old phreatic caves formed below the water table of the
time; old karstic foot caves formed by lateral undercutting of cliffs at
base level; and marine notch caves formed at sea level where rock
structures are powerfully eroded and eventually reduced to a wave cut
platform.
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