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Wulingyuan

Wulingyuan is a place in China with thousands of tall stone pillars. Trees grow on top of them.

Wulingyuan, in China's Hunan Province, is a World Heritage Site with more than 3,000 narrow pillars of quartz sandstone, many over 200 meters high, rising from forests, ravines and streams.

Wulingyuan (UNESCO World Heritage, 1992; 26,400 ha) in Hunan Province holds more than 3,000 quartz sandstone pillars, many over 200 m high, with ravines, waterfalls, two natural bridges and some 40 caves. Researchers suggest its peak forest began forming in the Pliocene, roughly 3 to 5 million years ago.

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Photo: chensiyuan, CC BY-SA 4.0, via Wikimedia Commons

Discover Wulingyuan

Wulingyuan is in China. Thousands of stone pillars stand in a forest there.

In this photo, plants and trees cover the tops of the pillars.

Wulingyuan covers about 26,400 hectares in China's Hunan Province. UNESCO says it holds more than 3,000 narrow pillars of quartz sandstone, many over 200 meters high, with ravines, streams, pools, waterfalls, two natural bridges and some 40 caves.

This photo by chensiyuan, taken in 2012 at Huangshizhai, shows a row of sandstone pillars topped with trees, a thick green forest below and hazy mountains behind.

UNESCO describes Wulingyuan as 'an island of nature within a heavily populated agricultural region': some 26,400 ha in Hunan Province dominated by more than 3,000 narrow quartz sandstone pillars, many over 200 m high, with ravines, gorges, streams, pools, waterfalls, two natural bridges and some 40 caves with calcite deposits.

The photo (chensiyuan, CC BY-SA 4.0, 2012; a Commons featured picture) is a panorama of sandstone pillars at Huangshizhai with tree-covered tops, dense forest below and misty ridges beyond.

Sandstone pillars
more than 3,000
Area
26,400 ha
World Heritage Site
since 1992
Five fingers peak
Photo: chensiyuan, CC BY-SA 4.0, via Wikimedia Commons

From seabed sand to stone pillars

Long ago, sand settled in a shallow sea and turned to rock.

Water wore the rock away along cracks, leaving tall pillars.

Scientists who measured how fast these pillars wear away (May and colleagues, 2018) explain that the rock is quartz-rich sandstone laid down in a shallow sea in the Devonian period, hundreds of millions of years ago. Later movements of the Earth's crust folded it and cracked it into a dense network of joints and fractures.

When the Himalayas began to rise, the land here was lifted too. Rivers cut down along the cracks and the rock walls between them slowly wore back, leaving pillars. The team's measurements suggest the peak forest started forming in the Pliocene, roughly 3 to 5 million years ago.

The pillars are cut from the Middle Devonian Yuntaiguan Formation, a fine-grained quartzitic sandstone about 520 m thick that built up in a shallow sea. Tectonic events between about 260 and 56 million years ago folded the rocks and left a dense network of joints and fractures. The onset of the Himalayan mountain building in the Neogene brought uplift, while a resistant cap of iron-rich quartz sandstone slowed erosion, leaving flat-topped mesas and steep valley heads often with waterfalls (May et al., 2018).

Using cosmogenic nuclides, May and colleagues found that valley floors at the base of the pillars wear down fastest (about 83 to 122 mm per thousand years) and peak-wall tops slowest (about 2.5 mm per thousand years). Their results suggest the peak forest began forming in the Pliocene, with estimates for most sub-catchments between about 3 and 5 million years ago, through river dissection along joints and faults followed by the retreat of the pillar walls.

Bridges, caves and waterfalls

Wulingyuan has stone bridges, caves and waterfalls.

One stone bridge is very high above the valley.

Between the pillars lie ravines and gorges with streams, pools and waterfalls. UNESCO counts more than 40 caves, with calcite deposits inside, and two natural stone bridges.

One of the natural bridges rises 357 meters above the valley floor. UNESCO adds that mists and clouds often wrap around the site.

Besides more than 3,000 columns and peaks, UNESCO lists natural bridges, ravines, waterfalls, streams, pools and caves under criterion (vii): more than 40 caves, notable for calcite deposits, and two natural stone bridges, one rising 357 m above the valley floor.

Dense broadleaf forest and the mists and clouds that frequently shroud the site add to the landscape's beauty (UNESCO).

Forests and rare animals

Thick forests grow among the pillars.

Rare animals such as dholes and Asian black bears live here.

UNESCO says Wulingyuan has rich, lush plant cover and dense broadleaf forest, and is home to a number of endangered plants and animals.

Among the threatened animals UNESCO names are the dhole, a wild dog, the Asiatic black bear and the Chinese water deer. UNESCO also calls Wulingyuan an island of nature within a heavily populated farming region, and says it provides important habitat for these animals.

Luxuriant vegetation and dense broadleaf forest cover the site, which UNESCO says provides important habitat for a number of threatened plant and animal species, such as the dhole, Asiatic black bear and Chinese water deer.

At inscription, evaluators noted that with more information the site might also qualify under the biodiversity criterion (x).

Visiting with care

Lots of people visit Wulingyuan every year.

Stay on the paths and keep the forest clean.

UNESCO notes intense pressure from visitors and tourist buildings, and says many measures have been taken to ease them, including promoting ecological tourism. Today UNESCO says the number of visitors, when they come and what they do are controlled and monitored.

PlayOwl's advice, built on UNESCO's notes: stay on the paths, keep a safe distance from cliff edges and take your litter home.

UNESCO lists human pressure from people living in and around the reserve, intense visitor pressure and the aesthetic impact of tourist facilities as integrity issues. From 1999 local authorities demolished houses in the scenic areas, expanded the scenic area, reduced settlement and promoted ecological tourism; by the end of 2002 the adverse impacts on the area's aesthetic values had been mitigated.

UNESCO says the number, seasonal spread and activities of visitors are now controlled, and their impact is monitored. PlayOwl suggests staying on paths, away from cliff edges, and leaving no litter.

Amazing facts

  • Water wears the rock away fastest at the bottom of the pillars.

    Scientists found that the valley floors at the foot of the pillars wear down much faster than the tops of the rock walls: about 83 to 122 millimeters every thousand years, compared with about 2.5 millimeters.

    Cosmogenic-nuclide erosion rates: about 83-122 mm per thousand years along the valley floors at the base of the pillars, about 30-84 mm on the pillar walls and about 2.5 mm on peak-wall tops (May et al., 2018).

  • A hard rock layer on top helps make flat tops and waterfalls.

    A cap of hard, iron-rich quartz sandstone slowed erosion here, leaving flat-topped mountains and steep valley heads with waterfalls.

    The resistant ferruginous quartz sandstone of the Upper Devonian Huangjiadeng Formation slowed erosion at about 850-1,000 m above sea level near Tianzi Mountain, leaving mesa-type tops and steep valley headwalls often marked by waterfalls (May et al., 2018).

  • One stone bridge here rises 357 meters above the valley.

    One of Wulingyuan's two natural stone bridges rises 357 meters above the valley floor.

    Two natural stone bridges stand in Wulingyuan; one rises 357 m above the valley floor (UNESCO).

Words to know

sandstone
rock made of grains of sand pressed and cemented together
quartz
a hard, common mineral often found in sand
joint
a natural crack in rock
natural bridge
an arch of rock left standing when the rock beneath it wears away
peak forest
a landscape of many steep rock pillars and peaks standing close together

Discovery challenge

  1. What stands in their thousands at Wulingyuan?

    What are Wulingyuan's more than 3,000 tall landforms?

    What dominates Wulingyuan's landscape, according to UNESCO?

    • Stone pillars
    • Ice towers
    • Sand dunes
    Show the answer

    Stone pillars

    Stone pillars.

    Narrow pillars of quartz sandstone.

    More than 3,000 narrow quartz sandstone pillars, many over 200 m high.

  2. Which country is Wulingyuan in?

    In which country is Wulingyuan?

    Wulingyuan lies in Hunan Province of which country?

    • China
    • Brazil
    • Norway
    Show the answer

    China

    China.

    China, in Hunan Province.

    China (Hunan Province).

  3. What wore the rock away to make the pillars?

    What slowly carved the pillars from the raised sandstone?

    Which process, guided by vertical joints, carved the pillars?

    • Water
    • Volcanoes
    • Glaciers
    Show the answer

    Water

    Water.

    Water running into the cracks and wearing the rock away.

    Erosion by water along fractures and vertical joints (river incision).

  4. Which wild dog lives at Wulingyuan?

    Which threatened wild dog does UNESCO name at Wulingyuan?

    Which threatened canid does UNESCO list among Wulingyuan's species?

    • Dhole
    • Dingo
    • Gray wolf
    Show the answer

    Dhole

    The dhole.

    The dhole.

    The dhole (with Asiatic black bear and Chinese water deer).

  5. How can visitors help keep Wulingyuan beautiful?

    Which is a good way to visit Wulingyuan with care?

    Given the visitor pressure UNESCO describes, which visitor action helps?

    • Stay on paths and take litter home
    • Climb the pillars
    • Pick the plants
    Show the answer

    Stay on paths and take litter home

    Stay on the paths and take your litter home.

    Stay on paths, keep away from cliff edges and take litter home.

    Staying on paths and leaving no litter (PlayOwl advice based on UNESCO's integrity notes).

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For parents & teachers

What children will learn

  • Locate Wulingyuan in Hunan Province, China.
  • Explain how water eroding along cracks can leave sandstone pillars.
  • Describe the caves, natural bridges and wildlife of the site.
  • Discuss how visitors and tourism can affect a natural site.

Recommended ages: 3 to 17 · About 15 minutes

Talk about it

  • Why might strong rock with straight cracks form tall pillars instead of rounded hills?
  • Why could large numbers of visitors put pressure on a natural site?
  • How can scientists work out how old a landscape is?

Try at home or in class

  • Stack sugar cubes into a block, drip water down a few gaps between them and watch columns separate.
  • On a map of China, find Hunan Province and mark Wulingyuan.

Key vocabulary: sandstone, quartz, joint, natural bridge, peak forest

Where these facts come from

  1. Wikidata , Wikimedia Foundation (CC0 1.0)
  2. Wulingyuan Scenic and Historic Interest Area (World Heritage List) , UNESCO World Heritage Centre
  3. Evolution of sandstone peak-forest landscapes: insights from quantifying erosional processes with cosmogenic nuclides (May et al., Earth Surface Processes and Landforms, 2018) , University of Melbourne (Minerva Access repository)
  4. File:1 zhangjiajie huangshizhai wulingyuan panorama 2012.jpg , Wikimedia Commons
  5. UNESCO World Heritage List , UNESCO World Heritage Centre (Linked as a reference; site facts come from Wikidata)
  6. Wikimedia Commons , Wikimedia Foundation (Per file (public domain, CC0, CC BY or CC BY-SA); see each media record)

Checked, not yet human-reviewed. Last updated November 1, 2026. Spotted a mistake? Tell us.

Picture credits
  • Photo: chensiyuan, CC BY-SA 4.0, via Wikimedia Commons · source · license