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Starting by boat at Phong Nha, you can visit some of the park’s most beautiful caves: the famous Phong Nha Cave with its underground river, the beautiful Tien Son or Fairy Cave and the

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Welcome to Phong Nha - Ke Bang National Park

Why is the park a World Natural Heritage Site?

The geological processes that form the area started

millions of years ago Today, the mountains and caves

display an impressive amount of evidence of Earth’s

history It is a site that can help you to better

understand the geological and geomorphical

processes that shape the earth This is why

UNESCO declared the park a World

Natural Heritage Site in 2003

Which caves can you visit?

Starting by boat at Phong Nha, you can visit some of the

park’s most beautiful caves: the famous Phong Nha Cave with its underground river, the beautiful Tien Son or Fairy

Cave and the mysterious Toi or Dark Cave (The map of the

boat tour is on the last panel)

Situated about 30 km along the road from Phong Nha,

Paradise Cave, is yet another cave that is also open to the

public

Rich biodiversity

The park is also unique because of its primary limestone forest and its rich biodiversity: nearly 2,700 plant species and 1,200 animal species have already been identified here More discoveries can be expected

Please join hands with us to protect this Heritage Site for future generations!

Did you know?

The park is famous for its beautiful caves and

karst mountains There are 145 caves in the park

which have been explored and mapped Many

more caves are still to be explored in this vast

remote jungle area The park area is currently

about 85,000 hectares (ha) There are plans to

enlarge it to about 120,000 ha It is part of a

greater area of karst mountains, which includes

the Hin Nam No National Biodiversity

Conser-vation Area (NBCA) in neighbouring Laos

World Natural Heritage Site

LAOS

VIET NAM

Son Doong is known as the largest cave passage

in the world Explored only in 2009 it is 7.6 km long,

150 m high and 200 m wide

Khe Ry cave, with the length of 18.9 km,

is the longest river cave in Asia

The combined surface of the Phong Nha-Ke Bang National Park (PNKB NP) and the Hin Nam No

NBCA amounts to 200,000 ha and it is the

largest and oldest karst area in South-East Asia.

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The Karst Mountains of PNKB

Why are the mountains precious?

The karst mountains of Phong Nha - Ke Bang took millions of years to develop They provide a unique environment for animals and plants The caves

inside the mountains are important habitats for cave dwelling species Many of the animals and plants

found here are already listed as threatened in the IUCN Red List and the Viet Nam Red Data Book

The mountains and caves took millions of years to develop

If we destroy them, they can never be restored

The mountains in Phong Nha are made out

of limestone layers, which were formed 465

to 250 million years ago at the bottom of an

ancient sea About 250 to 230 million years

ago, these layers were pushed upwards by the

movements of tectonic plates and became

exposed to rainwater

The earth’s crust is formed by ‘tectonic plates’, which

float on the liquid inner part of the earth They move

very slowly; so slow that we do not realise it When

they touch, some parts of the earth’s crust are moved

upwards, while others are moved downwards

What does ‘karst’ mean?

The word ‘karst’ is derived from the Karst region of Slovenia It is now applied worldwide to any area of limestone, which is characterised by underground drainage, caves and sinkholes as a result of limestone being dissolved by freshwater The cracks, rock

formations and caves in the illustration below are typical elements of karst mountains

Limestone – a very special rock

Limestone is a very special rock: it is formed in seawater but it dissolves when exposed to air and rainwater This dissolution happens not only via

mechanical forces but also through a chemical process (See next panel)

Dry cave

Wet cave

Stalactites

Stalagmites

Underground river

Vertical crack

Horizontal crack

Columns

Did you know?

Karst mountain in PNKB NP

Example of Karst formation in PNKB NP

In the park you can see parts

of the earth that used to be under an ancient sea millions

of years ago

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How were the caves formed?

When the limestone layers were pushed out of

the sea, they became cracked Rainwater becomes

slightly acidic after absorbing carbon dioxide from

the air When it falls into the limestone’s cracks, it

is pulled down by gravity While seeping through

the limestone, by a chemical reaction with the

calcium carbonate in the stone, the water becomes

a bicarbonate solution

This solution constantly carries away little

particles of limestone The cracks grow

increasingly wider, until they form huge

caves inside the mountains

PNKB NP lies in an area with an average

annual rainfall of 2,000 to 2,500 mm

The massive rainfall and the huge limestone

massif are ideal conditions for cave

formation This is why there are so many

caves and grottos in the park.

Cave-dwelling animals cannot survive outside the caves

Is there life in the caves?

You might think that caves are dark, cold places harbouring no life In fact, a number of animals prefer darkness and actually need to live in caves These animals are called troglobites

They are amazing animals:

• Some animals do not have eyes, because they

are of no use in the cave’s darkness

• Many animals have extremely long antennae,

because they need to feel their way around

• Many bats and some birds use echolocation to

find their way around in the dark

Why are there rock formations?

Every rock formation in a cave begins with a single drop of water laden with mineral calcite When the drop falls, it deposits the thinnest ring of calcite

Each subsequent drop that forms and falls deposits another calcite ring These accumulated drops form

the huge stalactites that we can see hanging down

from the ceiling Where the drops splash onto the floor, more of the solution evaporates and deposits

tiny bits of calcite on the floor (forming stalagmites)

Over millions of years, these tiny amounts add up to huge rock formations

Stalactite

An eyeless scorpion with a transparent body was discovered inside the Tien Son cave in 2010

and named the Viet Scorpion (Vietbocap canhi)

Did you know?

Stalagmite

Column Drops of solution

Stalagmite in the Phong Nha cave

Lesser False Vampire Bat

(Megaderma spasma)

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The Treasures of Phong Nha - Ke Bang

The animals living in the caves will go extinct

if YOU do not protect them!

Famous Phong Nha Cave

This cave is not only famous for its size and underground

river, but also because it served as a hiding place with an

underground hospital for the Vietnamese army during

the American war The Ho Chi Minh trail runs through

Phong Nha, which is why the area was subjected to

heavy bombing during the war Inside the cave you can

see writings of the old Kingdom of Champa (see photo)

Beautiful Tien Son Cave

The Tien Son Cave lies 200 m above the Phong Nha cave Millions of years ago, the Son River probably flowed through Tien Son Over time, the water cut down through the rocks and the river now flows through the

Phong Nha Cave The Tien Son Cave is now a dry cave, filled with huge columns, stalactites and stalagmites

Mysterious Dark Cave

The mysterious Dark Cave (Hang Toi) is situated approximately 5 km west from the Phong Nha cave

on the bank of the Chay River The cave’s entrance

is surrounded by a dark forest, a favourite place for monkeys If you are lucky, you might see one of them!

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Six rules of cave behaviour

• Do not smoke, litter or

spit in the caves

• Do not eat or leave

any food in the caves.

• Do not leave money or

other offerings in the caves.

• Do not leave the

marked pathways

• Do not touch the rocks

• Sssh! – Avoid loud

conversations

Ecological and Cultural Tourism Centre,

Phong Nha Village

Park Headquarter

Phong Nha Cave

Tien Son

Cave Dark Cave

Phong Nha-Ke Bang

National Park

Champa Dynasty script remained in Bi Ki Chamber

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