South China Karst


World Heritage Identification Number: 1248

World Heritage since: 2007

Category: Natural Heritage

WHE Type: Natural Landscapes & Geographic Features

Transboundary Heritage: No

Endangered Heritage: No

Country: 🇨🇳 China

Continent: Asia

UNESCO World Region: Asia and the Pacific

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Unveiling the Spectacular South China Karst: A Tropical Subtropical Karst Landscape

The South China Karst, a veritable treasure trove of geological wonders, stretches across four Chinese provinces – Chongqing, Guangxi, Guizhou, and Yunnan. This expansive region, encompassing approximately 97,125 hectares, was designated a UNESCO World Heritage Site in June 2007, owing to its exceptional display of humid tropical to subtropical karst landscapes.

More to come…

UNESCO Description of the World Heritage Site

South China Karst is one of the world’s most spectacular examples of humid tropical to subtropical karst landscapes. It is a serial site spread over the provinces of Guizhou, Guangxi, Yunnan and Chongqing and covers 97,125 hectares. It contains the most significant types of karst landforms, including tower karst, pinnacle karst and cone karst formations, along with other spectacular characteristics such as natural bridges, gorges and large cave systems. The stone forests of Shilin are considered superlative natural phenomena and a world reference. The cone and tower karsts of Libo, also considered the world reference site for these types of karst, form a distinctive and beautiful landscape. Wulong Karst has been inscribed for its giant dolines (sinkholes), natural bridges and caves.

UNESCO Justification of the World Heritage Site

Criterion (vii): The South China Karst World Heritage property includes spectacular karst features and landscapes, which are both exceptional phenomena, and of outstanding aesthetic quality. It includes the stone forests of Shilin, superlative natural phenomena which include the Naigu stone forest occurring on dolomitic limestone and the Suyishan stone forest arising from a lake, the remarkable fengcong and fenglin karsts of Libo, and the Wulong Karst, which includes giant collapse depressions, called Tiankeng, and exceptionally high natural bridges between them, with long stretches of deep unroofed caves. It also includes Guilin, which displays spectacular tower karst and internationally acclaimed fenglin riverine landscapes, Shibing Karst, which has the best known example of subtropical fengcong karst in dolomite, deep gorges and spine-like hills often draped with cloud and mist, and Jinfoshan Karst, which is an isolated island long detached from the Yunnan-Guizhou plateau, surrounded by precipitous cliffs and punctured by ancient caves. Huanjiang Karst provides a natural extension to Libo Karst, contains outstanding fengcong features and is covered in almost pristine monsoon forest. The property’s forest cover and natural vegetation is mainly intact, providing seasonal variation to the landscape and further enhancing the property’s very high aesthetic value. Intact forest cover also provides important habitat for rare and endangered species, and several components have very high biodiversity conservation value.

Criterion (viii): The South China Karst World Heritage property reveals the complex evolutionary history of one of the world’s most outstanding landscapes. Shilin and Libo are global reference areas for the karst features and landscapes that they exhibit. The stone forests of Shilin developed over 270 million years during four major geological time periods from the Permian to present, illustrating the episodic nature of the evolution of these karst features. Libo contains carbonate outcrops of different ages shaped over millions of years by erosive processes into impressive Fengcong and Fenglin karsts. Libo also contains a combination of numerous tall karst peaks, deep dolines, sinking streams and long river caves. Wulong represents high inland karst plateaus that have experienced considerable uplift, with giant dolines and bridges. Wulong's landscapes contain evidence for the history of one of the world's great river systems, the Yangtze and its tributaries. Huanjiang Karst is an extension of the Libo Karst component. Together the two sites provide an outstanding example of fengcong karst and also preserve and display a rich diversity of surface and underground karst features. Guilin Karst is considered the best known example of continental fenglin and provides a perfect geomorphic expression of the end stage of karst evolution in South China. Guilin is a basin at a relatively low altitude and receives abundant allogenic (rainfed) water from surrounding hills, leading to a fluvial component that aids fenglin development, resulting in fenglin and fengcong karst side-by-side over a large area. Scientific study of karst development in the region has resulted in the generation of the ‘Guilin model’ of fengcong and fenglin karst evolution. Shibing Karst provides a spectacular fengcong landscape, which is also exceptional because it developed in relatively insoluble dolomite rocks. Shibing also contains a range of minor karst features including karren, tufa deposits and caves. Jinfoshan Karst is a unique karst table mountain surrounded by massive towering cliffs. It represents a piece of dissected plateau karst isolated from the Yunnan-Guizhou-Chonqing plateau by deep fluvial incision. An ancient planation surface remains on the summit, with an ancient weathering crust. Beneath the plateau surface are dismembered horizontal cave systems that appear at high altitude on cliff faces. Jinfoshan records the process of dissection of the high elevation karst plateau and contains evidence of the region’s intermittent uplift and karstification since the Cenozoic. It is a superlative type-site of a karst table mountain.

Encyclopedia Record: South China Karst

The South China Karst, a UNESCO World Heritage Site since June 2007, spans the provinces of Chongqing, Guangxi, Guizhou, and Yunnan. It is noted for its karst features and landscapes as well as rich biodiversity. The site comprises seven clusters Phase I: Libo Karst, Shilin Karst, and Wulong Karst inscribed in 2007, and Phase II: Guilin Karst, Shibing Karst, Jinfoshan Karst, and Huanjiang Karst inscribed in 2014. UNESCO describes the South China Karst as "unrivalled in terms of the diversity of its karst features and landscapes".

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Additional Site Details

Area: 97,125 hectares

Number of Components: 12

UNESCO Criteria: (vii) — Contains superlative natural phenomena or beauty
(viii) — Outstanding example representing major earth stages

Coordinates: 24.9233333333 , 110.3544444444

IUCN World Heritage Outlook

The 2025 Conservation Outlook on South China Karst reports the following assessment:

Good with some concerns

Source: International Union for Conservation of Nature (IUCN) · View assessment

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Image of South China Karst

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China and the World Heritage Convention

State Party since: December 12, 1985

Status: Ratification

Mandates to the World Heritage Committee: 1991-1997, 1999-2005, 2007-2011, 2017-2021

Total of Mandate Years: 20

Total of Mandates: 4

WHC Electoral Group: IV (Asia/Pacific)

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Last updated: May 17, 2026

Portions of the page South China Karst are based on data from UNESCO — World Heritage List Dataset and on text from the Wikipedia article South China Karst, licensed under CC BY-SA 4.0. Changes made. Additional original content by World Heritage Explorer (WHE), licensed under CC BY-SA 4.0. WHE is not affiliated with UNESCO or the World Heritage Committee. Legal Notice. Privacy Policy.

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