Sichuan Giant Panda Sanctuaries

Sichuan Giant Panda Sanctuaries - Wolong, Mt Siguniang and Jiajin Mountains is principally renowned for its importance for the conservation of the giant panda, recognized as a "National Treasure" in China and as a flagship for global conservation efforts. The property is the largest and most significant remaining contiguous area of panda habitat in China and thus the world. It is also the most important source of giant panda for establishing the captive breeding population of the species.

Continent: Asia

Country: India

Category: Natural

Criterion: (X)

Date of Inscription: 2006

Giant Panda

In addition to the giant panda, the property features a great number of endemic and threatened species of plants and animals, including other iconic mammal species such as the red panda, snow leopard and clouded leopard among the 109 species of mammals recorded (more than 20% of all Chinese mammals). The property is an important centre of endemism for some bird taxa with 365 bird species recorded, 300 of which breed locally.

However the property is particularly important for flora, being one of the botanically richest sites of any temperate region in the world with some 5,000 – 6,000 species recorded. Many species are relicts, such as the dove tree, and there is significant diversity in groups such as magnolias, bamboos, rhododendrons, and orchids. The property is a major source and gene pool for hundreds of traditional medicinal plants, many now under threat.

Sichuan Giant Panda Sanctuaries

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Location of Sichuan

Located in China's southeast province of Sichuan in the Qionglai and Jiajin Mountains between the Chengdu Plateau and the Qinghai-Tibetan Plateau, the property includes seven nature reserves and eleven scenic parks in four prefectures or cities. It covers a total area of 924,500 ha surrounded by a buffer zone of 527,100 ha.

The Sichuan Giant Panda Sanctuary includes more than 30% of the world's population of giant Panda and constitutes the largest and most significant remaining contiguous area of panda habitat in the world. It is the most important source of giant panda for establishing the captive breeding population of the species.

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The property is also one of the botanically richest sites of any temperate region in the world or indeed anywhere outside of the tropical rain forests. Underlining the outstanding value is that it protects a wide variety of topography, geology, and plant and animal species. The property has exceptional value for biodiversity conservation and can demonstrate how ecosystem management systems can work across the borders of national and provincial protected areas.

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Three Parallel Rivers of Yunnan Protected Areas

Three Parallel Rivers of Yunnan Protected Areas is situated in south-west China. The site consists of 15 protected areas (in eight geographical clusters) in the mountainous north-west of Yunnan Province.

Continent: Asia

Country: China

Category: Natural

Criterion: (VII)(VIII) (IX) (X)

Date of Inscription: 2010

Three of the great rivers of Asia

Extending 310 km from north to south and 180 km from east to west, the site encompasses large sections of three of the great rivers of Asia, the Yangtse (Jinsha), Mekong (Lacang) and Salween (Nu Jiang), which run parallel from north to south through the nominated area for over 300 km.

The world heritage area lies over four parallel north-south trending mountain ranges that reach a height in excess of 4,000 m above sea level in altitude. These ranges are part of the Hengduan Mountains located beyond the eastern end of the Himalayas, which have been corrugated and uplifted by the pressures of crustal folding.

Three Parallel Rivers of Yunnan Protected Areas

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The site is dominated by a huge composite orogenic belt that shows the signs of powerful crustal movements in the past. Notably is the compression of the edge of the Eurasian plate by the underlying Indian plate which is being subducted along the line of the Lancang River fault. The resulting squeeze created vast thrust-nappes; violent shearing and uplift into high mountains, through which pre-existing rivers continue to cut, resulting in the extreme vertical relief which characterizes the area. Some of the results are visible in complex patterns of folded rock and unusual mineral formations.

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The site is also an excellent representative of alpine landscapes and their evolution. The eastern mountains, plateaus and valleys are covered with meadows, waterfalls and streams and hundreds of small glacial lakes left by glacial erosion processes.

The land area encompassed by Three Parallel Rivers of Yunnan Protected Areas is one of the world's least-disturbed temperate ecological areas, an epicentre of Chinese endemic species and a natural gene pool of great richness. It supports the richest diversity of higher plants of China, owing to its altitudinal range and its position in a climatic corridor between north and south, it includes the equivalents of seven climatic zones: southern, central and northern subtropical with dry hot valleys, warm, cool and cold temperate, and cold zones. Owing to its function as a refuge during the last Ice Age and its location near the boundaries of three major biogeographic realms, East Asia, South-East Asia and the Tibetan plateau, the park has 22 vegetation subtypes and 6,000 plant species.

The fauna is a complex mosaic of Palaearctic, oriental and local endemic species adapted to almost all the inland climates from southern subtropical to frigid, except for desert, although there are hot dry valleys. The area is believed to support over 25% of the world's animal species, many being relict and endangered. There is a concentration of the country's rare and endangered animals within the nominated area.

Being near the boundaries of the East Asian, South-East Asian and Tibetan biogeographic realms, the nominated area also acts as a corridor where several species from each realm meet and reach their limits of distribution. In addition there are numerous primitive animals that are relics of the ecological past, alongside animals that have recently adapted to colder conditions.

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Mount Sanqingshan Granite Peaks and Granite Pillars

Mount Sanqingshan National Park, a 22,950 ha property located in the west of the Huyaiyu mountain range in the northeast of Jiangxi Province (in the east of central China) has been inscribed for its exceptional scenic quality, marked by the concentration of fantastically shaped pillars and peaks: 48 granite peaks and 89 granite pillars, many of which resemble human or animal silhouettes.

Continent: Asia

Country: China

Category: Natural

Criterion: (VII)

Date of Inscription: 2008

Mount Sanqingshan National Park

The natural beauty of the 1,817 metre high Mount Huaiyu is further enhanced by the juxtaposition of granite features with the vegetation and particular meteorological conditions which make for an ever-changing and arresting landscape with bright halos on clouds and white rainbows. The area is subject to a combination of subtropical monsoonal and maritime influences and forms an island of temperate forest above the surrounding subtropical landscape. It also features forests and numerous waterfalls, some of them 60 metres in height, lakes and springs.

Mount Sanqingshan National Park displays a unique array of forested, fantastically shaped granite pillars and peaks concentrated in a relatively small area. The looming, intricate rock formations intermixed with delicate forest cover and combined with ever-shifting weather patterns create a landscape of arresting beauty.

Mount Sanqingshan National Park

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Superlative natural phenomena or natural beauty: Mount Sanqingshan’s remarkable granite rock formations combine with diverse forest, near and distant vistas, and striking meteorological effects to create a landscape of exceptional scenic quality. The most notable aspect is the concentration of fantastically shaped pillars and peaks.

The natural beauty of Mount Sanqingshan also derives from the juxtaposition of its granite features with the mountain’s vegetation enhanced by meteorological conditions which create an ever-changing and arresting landscape. The access afforded by suspended walking trails in the park permits visitors to appreciate the park’s stunning scenery and enjoy its serene atmosphere.

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The park boundaries are appropriately drawn to protect the naturalness of the landscape and the areas required to maintain the scenic qualities of the property. The property, although relatively small, includes all of the granite peaks and pillars which provide the framework for its aesthetic values. Boundaries are accurately surveyed and demarcated. The property’s integrity is enhanced by the designation of a buffer zone that is not part of the inscribed property.

The property has effective legal protection, a sound planning framework and is currently well managed. The park benefits from strong government support and funding. The park’s natural resources are in good condition and threats are considered manageable. There is an effective management regime in place for the park.

The key requirement is to manage the property to retain its aesthetic values, and a delicate balance will need to be maintained with the provision of visitor access. The most significant threat relates to the future increase in tourism, and careful and sensitive planning of the related infrastructure and access development is required.

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The South China Karst Landscapes

The South China Karst region extends over a surface of half a million km2 lying mainly in Yunnan, Guizhou and Guangxi provinces. It represents one of the world’s most spectacular examples of humid tropical to subtropical karst landscapes. The stone forests of Shilin are considered superlative natural phenomena and a world reference with a wider range of pinnacle shapes than other karst landscapes with pinnacles, and a higher diversity of shapes and changing colours. 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.

Continent: Asia

Country: China

Category: Natural

Criterion: (VII)(VIII)

Date of Inscription: 2007

South China Karst

South China is unrivalled for the diversity of its karst features and landscapes. The property includes specifically selected areas that are of outstanding universal value to protect and present the best examples of these karst features and landscapes. South China Karst is a coherent serial property comprising three clusters, Libo Karst and Shilin Karst, each with two components, and Wulong Karst with three components. South China Karst represents one of the world's most spectacular examples of humid tropical to subtropical karst landscapes.

The stone forests of Shilin are considered superlative natural phenomena and the world reference site for this type of feature. The cluster includes the Naigu stone forest occurring on dolomitic limestone and the Suyishan stone forest arising from a lake. Shilin contains a wider range of pinnacle shapes than other karst landscapes with pinnacles, and a higher diversity of shapes and colours that change with different weather and light conditions.

The South China Karst Landscape

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The cone and tower karsts of Libo, also considered the world reference site for these types of karsts, form a distinctive and beautiful landscape. Wulong includes giant collapse depressions, called Tiankeng, and exceptionally high natural bridges between which are long stretches of very deep unroofed caves. These spectacular karst features are of world class quality.

Both Shilin and Libo are global reference areas for the karst features and landscapes that they exhibit. Major developments in the stone forests of Shilin occurred over some 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 that erosive processes shaped over millions of years into impressive Fengcong (cone) and Fenglin (tower) karsts.

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It 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, and its giant dolines and bridges are representative of South China's Tiankeng landscapes. Wulong's landscapes contain evidence for the history of one of the world's great river systems, the Yangtze and its tributaries.

The property is well managed, with clear management plans in place and the effective involvement of various stakeholders. There are strong international networks in place to support continued research and management. Of the three clusters, Wulong has suffered the least human impact by virtue of its remoteness and retains natural values that have been reduced in other comparable areas.

Continued efforts are required to expand and refine buffer zones to protect upstream catchments and their downstream and underground continuation in order to maintain water quality at a level that ensures the long term conservation of the property and its subterranean processes and ecosystems. At Wulong the boundaries of the core zone should be considered for extension, and a single landscape-scale buffer zone would be a significant improvement to encompass all of the Tiankeng elements to the north of the Furong gorge.

Traditional management by minority peoples is an important feature of both clusters, and the relationship between karst and the cultural identity and traditions of minority groups including the Yi (Shilin) and the Shui, Yao and Buyi (Libo) requires continued recognition and respect in site management. Potential for further extension of the property requires development of a management framework for effective coordination between the different clusters.

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The Pitons Management Area Volcanic System

The Pitons Management Area contains the greater part of a collapsed stratovolcano contained within the volcanic system, known to geologists as the Soufriere Volcanic Centre. Prominent within the volcanic landscape are two eroded remnants of lava domes, Gros Piton and Petit Piton.

Continent: North America

Country: Saint Lucia

Category: Natural

Criterion: (VII)(VIII)

Date of Inscription: 2004

Pitons Management Area

Dominating the mountainous landscape of St Lucia are the Pitons, two steep-sided volcanic spires rising side by side from the sea. 770 metre Gros Piton is 3 km in diameter at its base, and Petit Piton (743 m) is 1 km in diameter and linked to the former by the Piton Mitan ridge. The Pitons are part of a volcanic complex, known to geologists as the Soufriere Volcanic Centre which is the remnant of one (or more) huge collapsed stratovolcano. The volcanic complex overlies a tectonic plate subduction (underthrusting) zone which stretches 700 km along Lesser Antilles, forming a volcanic arc.

The Pitons are the eroded cores of two lava domes formed on the flanks of the stratovolcano. Today they tower above a caldera-like formation, produced by a gigantic gravity slide or structural collapse which formed the Qualibou Depression, 7 km in diameter. Near the centre of the depression are the Sulphur Springs, an active, high temperature geothermal field with sulphurous fumaroles and hot springs. The Pitons occur with a variety of other volcanic features including cumulo-domes, explosion craters, pyroclastic deposits (pumice and ash) and lava flows. Collectively, these fully illustrate the volcanic history of an andesitic composite volcano associated with crustal plate subduction.

Pitons Management Area

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The Marine Management Area is a coastal strip 11 km long and about 1 km wide. It comprises a steeply sloping continental shelf with fringing and patch reefs, boulders and sandy plains. The coral reefs, which cover almost 60% of the marine area, are healthy and diverse. A survey to a depth of 20 m revealed 168 species of finfish, 60 species of cnidaria, including corals, molluscs, sponges, echinoderms, arthropods and annelid worms. Hawksbill turtles are seen inshore, and whale sharks and pilot whales offshore.

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The dominant terrestrial vegetation is tropical moist forest grading to subtropical wet forest with small areas of dry forest near the coast and on steep slopes, and areas of wet elfin woodland on the summits. On the Pitons especially, small undisturbed natural forests remain, preserved by the steepness of the land. At least 148 plant species have been recorded on Gros Piton and 97 on Petit Piton. Among these are several endemic or rare plants, including eight rare species of tree. Some bird species, including 5 endemics, are known from Gros Piton, along with indigenous rodents, opossum, bats, reptiles and amphibians.

The area is a multiple-use management where agriculture, artisan fishing, human settlement (1,500 residents) and tourism (four large hotel developments) are allowed. There are four distinctions of the PMA which it proposes are of universal value

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Wulingyuan Scenic Historic Interest Area China

A spectacular Wulingyuan Scenic Historic Interest Area in China stretching over more than 26,000 ha in China's Hunan Province, the site is dominated by more than 3,000 narrow sandstone pillars and peaks, many over 200 m high. Between the peaks lie ravines and gorges with streams, pools and waterfalls, some 40 caves, and two large natural bridges. In addition to the striking beauty of the landscape, the region is also noted for the fact that it is home to a number of endangered plant and animal species.

Continent: Asia

Country: China

Category: Natural

Criterion: (VII)

Date of Inscription: 1992

Wulingyuan Scenic Resources

The Wulingyuan Scenic and Historic Interest Area lies in the Wulingyuan District of the city of Dayong and covers the entire drainage basin of the Suoxi Brook, which winds for 69 km through the site. The most notable feature, dominating about two-thirds of the site, is more than 3,000 quartzite sandstone pillars and peaks. Between the peaks are numerous ravines and gorges, many containing attractive streams, pools and waterfalls. The site also contains a number of karst features, notably some 40 caves which are concentrated on the banks of the Suoxiyu River and the south-east side of Tianzi Mountain. Huanglong or Yellow Dragon Cave is said to be one of the 10 largest caves in China. Spectacular calcite deposits are a major feature of many of these caves.

There are two spectacular natural bridges in the area: Xianrenqias (Bridge of the Immortals) and Tianqiashengkong (Bridge across the Sky). It lies 357 m above the valley floor and may be the highest natural bridge in the world. The site is popularly known to have '800 brooks and streams' but in reality, there are far less, perhaps 60. Many drain into the Suoxi River which runs through the centre of the site. One of the side branches of this river has been dammed at one point, creating Baojeng Lake. This lake has been created for water supply, flood control and to enhance the habitat for the Chinese giant salamander as well as for recreation.

Wulingyuan Scenic and Historic Interest Area

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Wulingyuan lies in the Central China Botanic Region of the Sino-Japanese Botanic Zone, and was a refuge for many ancient species during the Quaternary glacial period. Below 700 m the community is predominantly evergreen broadleaf. Between 700 m and 950 m, there is a mixed community of evergreen and deciduous broadleaved trees. There are also some coniferous species including Chinese plum yew and pines. Above 950 m, there is a community of deciduous broadleaved trees, bushes and herbs; in some areas below 1,000 m, extensive communities are dominated by pine.

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3,000 species of plant occur within the area, including some 600 species of woody plant; these are split fairly evenly between tropical/subtropical and temperate species. Many of the species are of value for timber, medical or ornamental purposes.

A number of faunal species are globally threatened with extinction: Chinese giant salamander, Asiatic wild dog, Asiatic black bear, clouded leopard, leopard and Chinese water deer. The clouded leopard population is likely to be very small, although tracks and others signs have been found they have never actually been seen.

Unlike many other areas of China, the site does not have a long human history. In ancient times it was regarded as remote and inaccessible. Local legends indicate that Zhangliang, a lord in the Han dynasty (206 BC-AD 220), lived in seclusion in Wulingyuan and was buried below Qingyan (now Zhangjiajie) Mountain.

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Huanglong Scenic Historic Interest Area China

Huanglong Scenic Historic Interest Area in China is situated in the north-west of Sichaun Province; the Huanglong valley is made up of snow-capped peaks and the easternmost of all the Chinese glaciers. In addition to its mountain landscape, diverse forest ecosystems can be found, as well as spectacular limestone formations, waterfalls and hot springs. The area also has a population of endangered animals, including the giant panda and the Sichuan golden snub-nosed monkey. The property lies in the southern part of the Min Shan Range, approximately 150 km north/north-west of the provincial capital of Chengdu. It is divided into two distinct sites: the Huanglong subdivision and the Mouni Gully subdivision.

Continent: Asia

Country: China

Category: Natural

Criterion: (VII)

Date of Inscription: 1992

Greatest Geologically Interest of Huanglong Scenic

Tectonic activity, in the form of earthquakes, is fairly frequent. The relief is predominantly precipitous, a particularly spectacular example being where the Fujiang River flows through the Danyun Gorge. Above the timberline are extensive areas of precipitous mountain scenery, snow-covered for much of the year. Xuebaoding, or Snow Mountain Peak, is permanently snow-covered and bears the easternmost glacier in China. Of greatest geologically interest is the extensive calcite deposition that has taken place, notably along the 3.6 km Huanglonggou (Yellow Dragon Gully) where there are several extensive areas of travertine pools.

Algae and bacteria proliferate in a number of these pools, giving a wide range of colours from orange and yellow to green and blue. Other karst features include long limestone shoals, notably Liujinshan (Glazed Golden Fan) and Jinshatan (Golden Sand Beach), in Huanglonggou. These are extensive slopes of active limestone deposition, covered entirely by a thin layer of flowing water.

Huanglong Scenic and Historic Interest Area

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The Huanglong subdivision contains the main tributaries leading into the upper waters of the Fujiang River, which has its source at the Snow Mountain Ridge. Water flow varies throughout the year, with peak flows during the flood season from May to July. A number of low-temperature hot springs rise from deep groundwater.

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The Mouni Gully subdivision consists of two parallel small gullies, Zhaga and Erdaohai. There are two important areas of hot springs in this site: FeicuiKuang-quan and the springs in Zhuzhuhu. The waters of both springs have high mineral contents and are said to have important medicinal properties. Mouni Gully also contains a number of very attractive lakes and the Zhaga Waterfall.

Huanglong is situated at the transition zone between the eastern damp forest zone and the mountainous coniferous woods/meadow grassland and shrub zone of Qing-Zang Plateau. It lies close to the intersection of four floral regions: Eastern Asia, Himalaya, and the subtropical and tropical zones of the Northern Hemisphere.

From 1,700 m to 2,300 m, there is a belt of mixed forest dominated by Chinese hemlock, Chinese or dragon spruce and three species of maple. Between 2,300 m and 3,600 m, the forest is largely coniferous and subalpine in character, dominated by spruces; firs; larch and birches. Between 3,600 m and 4,200 m, the forest gives way to alpine meadows dominated by shrubs and grasses. From 4,200 m to 4,800 m vegetation is sparser, but includes shrubs. Above 4,800m, there is permanent snow and ice.

A large number of faunal species listed are threatened mammals include such notable species as giant panda, golden snub-nosed monkey, brown bear Asiatic black bear, leopard, Pallas' cat, Asiatic wild dog, lesser panda, Szechwan takin, mainland serow, common goral, argali and three species of deer.

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Manas Wildlife Sanctuary Assam

Manas takes its name from the Goddess Manasa. The Manas Wildlife Sanctuary is noted for its spectacular scenery, with a variety of habitat types that support a diverse fauna, making it the richest of all Indian wildlife areas. The park represents the core of an extensive tiger reserve that protects an important migratory wildlife resource along the West Bengal to Arunachal Pradesh and Bhutan borders. Its wetlands are of international importance. It is also the single most important site for the survival of pygmy hog, hispid hare and golden langur.

Continent: Asia

Country: India

Category: Natural

Criterion: (VII)(IX) (X)

Date of Inscription: 1985

Manas Reserve Forest

The park, which includes part of Manas Reserve Forest and all of North Kamrup Reserve Forest, constitutes the core of Manas Tiger Reserve located in the forest divisions of Kachugaon, Haltugaon, Western Assam Wildlife and North Kamrup. Lying in the foothills of the Outer Himalaya, the area is low-lying and flat. The Manas River flows through the western portion of the park, where it splits into three separate rivers, and joins the Brahmaputra some 64 km further south. These and other rivers running through the tiger reserve carry an enormous amount of silt and rock debris from the foothills, resulting from the heavy rainfall, fragile nature of the rock and steep-gradients of the catchments.

This leads to the formation of alluvial terraces, comprising deep layers of deposited rock and detritus overlain with sand and soil of varying depth, shifting river channels and swamps. The area of the Boki basin, in the west of the park, is sometimes inundated during the monsoon. The three main types of vegetation are: tropical semi-evergreen forests in the northern part of the park; tropical moist and dry deciduous forests (the most common type); and extensive alluvial grasslands in the western part of the park.

Manas Wildlife Sanctuary Assam

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There is also a considerable variety of aquatic flora along river banks and in the numerous pools. Dry deciduous forests represent early stages in succession and are replaced by moist deciduous forests away from water courses, which, in turn, are succeeded by tropical semi-evergreen climax forest. Grasslands cover about 50% of the park.

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A total of 55 mammals, 36 reptiles and three amphibians have been recorded Manas harbours by far the greatest number of India's Schedule I mammals of any protected area in the country. Many are typical of South-East Asian rainforest and have their westernmost distribution here. Mammals include golden langur, a recently discovered endemic restricted to Manas, capped langur, Hoolock gibbon, clouded leopard, tiger (second-largest population in India), leopard, golden cat, fishing cat, leopard cat, marbled cat, binturong, sloth bear, wild dog, Ganges dolphin, Indian elephant, Indian rhinoceros, pygmy hog, swamp deer, sambar, hog deer, Indian muntjac, water buffalo, gaur, giant squirrel, hispid hare and Indian pangolin.

Over 450 species of bird have been recorded, including the threatened Bengal florican, great pied hornbill, wreathed hornbill and other hornbills. Uncommon waterfowl species include spot-billed pelican, lesser adjutant and greater adjutant.

Reptiles include a variety of snakes, gharial and monitor lizard. Assam roofed turtle has recently been recorded.

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Keoladeo National Park Rajasthan

Keoladeo National Park is situated in eastern Rajasthan, the park is 2 km south-east of Bharatpur and 50 km west of Agra. The area consists of a flat patchwork of marshes in the Gangetic plain, artificially created in the 1850s and maintained ever since by a system of canals, sluices and dykes. Normally, water is fed into the marshes twice a year from inundations of the Gambira and Banganga rivers, which are impounded on arable land by means of an artificial dam called Ajan Bund, to the south of the park. The first time, usually in mid-July, is soon after the onset of the monsoon and the second time is in late September or October when Ajan Bund is drained ready for cultivation in winter.

Continent: Asia

Country: India

Category: Natural

Criterion: (X)

Date of Inscription: 1985

Keoladeo Monsoon

Thus, the area is flooded to a depth of 1-2 m throughout the monsoon (July-September), after which the water level drops. From February onwards the land begins to dry out and by June only some water remains. For much of the year the area of wetland is only 1,000 ha. Soils are predominantly alluvial - some clay has formed as a result of the periodic inundations. In a semi-arid biotype, the park is the only area with much vegetation, hence the term 'Ghana' meaning 'thicket'.

The principal vegetation types are tropical dry deciduous forest, intermixed with dry grassland in areas where forest has been degraded. Apart from the artificially managed marshes, much of the area is covered by medium-sized trees and shrubs. Forests, mostly in the north-east of the park, are dominated by kalam or kadam, jamun and babul. The open woodland is mostly babul with a small amount of kandi and ber. Scrublands are dominated by ber and kair. The aquatic vegetation is rich in species and is a valuable source of food for waterfowl.

Keoladeo National Park Rajasthan

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Primates are rhesus macaque and langur. Large predators are absent, leopard having been deliberately exterminated by 1964, but small carnivores include Bengal fox, jackal, striped hyena, common palm civet, small Indian civet, Indian grey mongoose Herpestes edwardsi , fishing cat, leopard cat, jungle cat and smooth-coated otter. Ungulates include blackbuck, chital, sambar, hog deer, nilgai and wild boar and feral cattle. Other mammals include Indian porcupine and Indian hare.

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An estimated 65 million fish fry are carried into the park's water impoundments by river flooding every year during the monsoon season, which provides the food base for large numbers of wading and fish-eating birds. Some 364 species of bird have been recorded in the park, which is considered to be one of the world's finest areas for birds, with a unique assemblage of species.

The park's location in the Gangetic Plain makes it an unrivalled breeding site for herons, storks and cormorants and an important wintering ground for large numbers of migrant ducks. The most common waterfowl are gadwall, shoveler, common teal, cotton teal, tufted duck, comb duck, little cormorant, great cormorant, Indian shag, ruff, painted stork, white spoonbill, Asian open-billed stork, oriental ibis, darter, common sandpiper, wood sandpiper and green sandpiper. Sarus crane, with its spectacular courtship dance, is also found here.

Among land birds is a rich assortment consisting of warblers, babblers, bee-eaters, bulbuls, buntings, chats, partridges and quails. Grey hornbill and Marshall's iota are also present. There are many birds of prey including the osprey, peregrine, Pallas' sea eagle, short-toed eagle, tawny eagle, imperial eagle, spotted eagle and crested serpent eagle. Greater spotted eagle has recently been recorded breeding here, a new breeding record for the species in India and lesser spotted eagle nested in the park in 1986, the first nesting record for the species in India for some time.

Several other threatened avifauna species occur, including Dalmatian pelican, spot-billed pelican, greater adjutant, lesser adjutant, marbled teal, Baikal teal, Baer's pochard, red kite, cinereous vulture and sociable lapwing.

Reptiles include water snakes, Indian python, banded krait, green rat snake, turtles and monitor lizard.

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Kaziranga National Park India

In the heart of Assam, Kaziranga National Park is one of the last areas in eastern India undisturbed by a human presence. It is inhabited by the world's largest population of one-horned rhinoceroses, as well as many mammals, including tigers, elephants, panthers and bears, and thousands of birds. In the heart of Assam, this park is one of the last areas in eastern India undisturbed by a human presence. It is inhabited by the world's largest population of one-horned rhinoceroses, as well as many mammals, including tigers, elephants, panthers and bears, and thousands of birds.

Continent: Asia

Country: India

Category: Natural

Criterion: (II)(IV)

Date of Inscription: 2011

The Water Coverage of Kaziranga

The site is on the southern bank of the Brahmaputra River at the foot of the Mikir Hills. The park lies in the flood plains of the Brahmaputra. The riverine habitat consists primarily of tall, dense grasslands interspersed with open forests, interconnecting streams and numerous small lakes (bheels). Three-quarters or more of the area is submerged annually by the flood waters of the Brahmaputra. Soils are alluvial deposits of the Brahmaputra and its tributaries.

There are three main types of vegetation: alluvial inundated grasslands, tropical wet evergreen forests and tropical semi-evergreen forests. Grasslands predominate in the west, with tall 'elephant' grasses on the higher ground and short grasses on the lower ground surrounding the bheels. They have been maintained by annual flooding and burning over thousands of years. Tropical wet evergreen forests, near Kanchanjhuri, Panbari and Tamulipathar blocks, are dominated by trees. Tropical semi-evergreen forests occur near Baguri, Bimali and Haldibari.

Kaziranga National Park India

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The park contains about 15 species of India's threatened mammals. It harbours the world's largest population of Indian rhinoceros and Indian elephant

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Other mammals include capped langur, a small population of hoolock gibbon, tiger Panthera tigris , leopard, sloth bear, Ganges dolphin, otter, wild boar, water buffalo, gaur, sambar, swamp deer, hog deer and Indian muntjac. Elephants and other animals migrate with the advent of the monsoon and head southwards to the Mikir Hills and beyond to avoid the annual flooding of the national park.

The numerous water bodies are rich reservoirs of food (including fish) and thousands of migratory birds, representing over 100 species, visit the park seasonally from as far afield as Siberia. There is a grey pelican rookery near Kaziranga Village. Other birds of interest include black-necked stork, lesser adjutant stork, Pallas's fish eagle, grey-headed fish eagle, Bengal florican, swamp partridge, grey peacock-pheasant, great pied hornbill, green imperial pigeon, silver-breasted broadbill and Jerdon's bushchat. The avifauna comprises over 300 species.

The reptilian fauna include water monitor, Indian python, common cobra and king cobra are present.

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Noel Kempff Mercado National Park Bolivia

The Kempff Mercado National Park is one of the largest (1,523,000 ha) and most intact parks in the Amazon Basin. With an altitudinal range of 200 m to about 1,000 m, it contains a rich mosaic of habitat types from cerrado savannah and forest to upland evergreen Amazonian forests. The park boasts an evolutionary history dating back over a billion years to the Precambrian. Located on the border with Brazil, the site includes a large section of the Huanchaca Plateau and surrounding lowlands. There are rugged cliffs in the northern, western and southern sides of the plateau, with several valleys and steep slopes in its eastern side. Several rivers have their sources on the plateau and form spectacular waterfalls. The largest river in the area is the Iténez, which marks the border with Brazil, to the north of the park, and the Paraguá River dominates the lowlands to the west.

Continent: South America

Country: Bolivia

Category: Natural

Criterion: (IX)(X)

Date of Inscription: 2000

Kempff Mercado Biogeographic Kingdom

The north-eastern sector of the Santa Cruz Department is part of a transition zone where Amazon forest intergrades with the dry forest and savannah habitats of the Cerrado biogeographic realm. Habitat types of the region can be grouped into five basic units that represent distinct ecosystems: upland evergreen forest; deciduous forest; upland Cerrado savannah; savannah wetlands; and forest wetlands. The humid forests of the park are floristically distinct from the moist forests of western Amazon and the Andean piedmont. These forests are classified in several habitat types still scarcely studied.

An evergreen forest with tall trees is found on deep and well-drained soils, while there is a dwarf forest formation occupying a transition zone with the Cerrado. A peculiar feature of the forest is the lianas, which form a low and very thick canopy. Although trees are also part of the canopy, the lianas proliferate in such a way that they dominate. The Huanchaca Plateau has a rich Cerrado flora that incorporates many species that were thought to have a distribution restricted to central Brazil.

Noel Kempff Mercado National Park Bolivia

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The outstanding habitat diversity of the park favours the existence of a highly diverse fauna and the site is an important repository for many rare mammals of Bolivia. Over 80% of the park's mammal species are found in humid forests. Good populations of tapir, brocket deer and jaguar inhabit the upland humid forests. Long-haired spider monkey has large populations throughout the tall evergreen forests, and black-tailed silvery marmoset and monk are also present.

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The open grassland habitats on the southern portion of the plateau have possibly one of the largest remaining populations of pampas deer. Two other large mammals, maned wolf and marsh deer are found in the seasonally flooded termite savannahs below the plateau.

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Pirin National Park Bulgaria

Pirin National Park is extending over an area of 27,400 ha and lying at an altitude of 1,008-2,914 m in the Pirin Mountains, south-west Bulgaria, Pirin National Park has a limestone Balkan landscape, with lakes, waterfalls, caves and pine forests. The rugged mountains, with some 70 glacial lakes scattered throughout them, are home to hundreds of endemic and rare species, many of which are representative of the Balkan Pleistocene flora. The mountains also have diverse and unique landscapes of great aesthetic value.

Continent: Europe

Country: Bulgaria

Category: Natural

Criterion: (VII)(VIII) (IX)

Date of Inscription: 1983

Pirin Mountain

Pirin Mountain stretches from north-west to south-east between the valleys of the Strouma and Mesta rivers. There are many rivers and waterfalls. Winter in the upper parts is cold and long with snow cover remaining for five to eight months. Summer is cool and short. The presence of limestone rocks, the southerly position of the range and close proximity to the Aegean, coupled with its relative isolation, have made Pirin Mountain an important refuge for many species.

Forests in the park are mainly coniferous with endemic Macedonian pine being widespread and forming the timberline in the granite part of the mountain. Endemic Bossnian pine occurs in the highest zone of the karst area. Unique stands of Pinus peuce and Pinus leucodermis , up to 250-300 years old and 30-45 m high, are found in Baiouvi Doupki-Djindjiritsa Reserve. Some individual Pinus leucodermis trees are over 500 years old. Silver fir, Austrian pine, spruce, Scots pine and beech form a mixed coniferous forest type.

Pirin National Park Bulgaria

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Generally, the timberline has developed as a result of human interference over a long period and descends as low as 2,000 m, but in some places reaches 2,200-2,300 m. In the subalpine zone there are thickets of dwarf mountain pine and Juniperus sibirica . Above 2,400-2,600 m is a layer of alpine meadows, stony slopes, screes, rocks, etc.

The flora of Pirin, comprising as it does many rare species, is of great interest and beauty. One of the most active flora speciation in Bulgaria is situated in the limestone part of the mountain. Pirin has a mixture of central European, Alpine, Balkan mountain and sub-Mediterranean species, but in addition there are about 30 local endemic species.

There is a wide variety of animal species including many endemic species and glacial relicts among the invertebrate fauna. Threatened bird and mammal species include brown bear, grey wolf, pine marten, rock marten, polecat, badger, otter, wild cat, red deer, roe deer, wild boar, Balkan chamois, golden eagle, capercaillie, hazel grouse, eagle owl, black woodpecker and three-toed woodpecker.

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Srebarna Nature Reserve Bulgaria

The Srebarna Nature Reserve is a freshwater lake adjacent to the Danube and extending over 600 ha. It is the breeding ground of almost 100 species of bird, many of which are rare or endangered. Some 80 other bird species migrate and seek refuge there every winter. Among the most interesting bird species are the Dalmatian pelican, great egret, night heron, purple heron, glossy ibis and white spoonbill, white-tailed eagle, little cormorant.

Continent: Europe

Country: Bulgaria

Category: Natural

Criterion: (X)

Date of Inscription: 1983

Wildfowl Reserve System

The reserve was set up primarily to protect the rich diversity of wildfowl; the bird species represent half of the Bulgarian avifauna. Species found in Srebarna include mute swan, a variety of geese and ducks, red-necked grebe, two of the three European species of marsh tern, and bearded tit. Otter is occasionally found in the reserve. White-fronted goose, red-breasted goose and blue throat have become established as wintering species.

Some 67 plant species can be found in Srebarna Nature Reserve, including water lily and a number of rare marsh plants. Reeds occupy two-thirds of the reserve and form a thick barrier around the lake. They form reed-mace islands which birds use for nesting.

Srebarna Nature Reserve Bulgaria

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This freshwater lake is situated on the flood plain of the River Danube, to which it was connected until 1949. The disconnection prevented annual flooding and the level of lake falls 1 m per year. However, the lake was reconnected by canal in 1978 with the Danube to prevent water levels from becoming too low and to restore the lake's fish population.

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The reserve is affected by a rapid and abnormal development of succession processes due to annual sedimentation of large reed-mace vegetation in the reserve, as well as the insufficient water influence of the Danube. Consequently, the reed-mace islands are extended and increased in thickness so that wild boars, foxes and jackals now pose a threat to both individual birds' nests and colonies. A series of upstream interferences, including the Iron Gate Dam, have permanently altered the natural hydrology of the Danube River in this region and that of Srebarna.

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Durmitor National Park Montenegro

Durmitor National Park comprises Mount Durmitor plateau and the valley formed by the canyon of the River Tara, incorporating three major geomorphologic features: canyons, mountains and plateaux. Because of its geographical location and range in altitude, the park is under the influence of both Mediterranean and alpine microclimates, which has resulted in an exceptional range of species.

Continent: Europe

Country: Montenegro

Category: Natural

Criterion: (VII)(VIII) (X)

Date of Inscription: 1980

Tara Canyons and Limestone Formations

Geologically, Durmitor and Tara canyons are made up of rocky massifs of the Mesozoic era (from the Lower Triassic to the Upper Cretaceous), Tertiary and Quaternary periods. The dominant features are the limestone formations of the Middle and Upper Triassic, the Upper Jurassic and the Upper Cretaceous, especially the so-called Durmitorean flysch. The River Tara, one of the last wild rivers in Europe, has pure, clear waters, a gorge 1,300 m deep and notable floristic and faunistic diversity.

The 16 glacial lakes of the Durmitor and the canyons of the Tara, Susica and Draga rivers were formed during the Quaternary period, following the sudden thaw of the snow and the formation of glaciers on the Durmitor and neighbouring mountains. The waters of the largest lake, Black Lake, feed two separate river basins: the River Tara, and underground through the Durmitor Massif, the River Komarnica or Piva. There are numerous examples of weathering processes, rock shapes and land features characteristic of karstic erosion, fluvial erosion and glacial erosion.

Durmitor National Park Montenegro

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Vegetation zones include deciduous forest, coniferous forest and subalpine zones. The dominant species include Scots pine, Norway pine, silver fir, beech, occasional birch, mugo pine and juniper. The park supports a rich karstic flora with many rare and endemic species. There are 37 taxa endemic to the area and six specific to Durmitor. The park contains one of the last virgin black pine forests in Europe, on soils that would usually develop beech woodland.

The Tara and its tributaries, as well as the lakes, contain a large number of salmonidae. Forest fauna includes brown bear, wolf, wild boar, wild cat, chamois, and various species of eagle, capercaillie, black grouse and rock partridge.

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World Heritage Te Wahipounamu

Te Wahipounamu comprises the least-disturbed tenth of New Zealand's land mass, with some 2 million hectares of temperate rainforest, 450 km of alpine communities, and a distinctive fauna. It contains the best modern representation of the ancient flora and fauna of Gondwanaland, including Podocarpus species, genera of beech, flightless kiwis, 'bush' moas and carnivorous Powelliphanta land snails. The overwhelming mountainous character of the area results from tectonic movement between the Pacific plate and the Indo-Australian plate over the last 5 million years. High local relief is the result of deep glacial excavation.

Continent: Oceania

Country: New Zealand

Category: Natural

Criterion: (VII)(VIII) (IX) (X)

Date of Inscription: 1990

Mount Cook National Parks

Glaciers are an important feature of the nominated area, especially in the vicinity of Westland and Mount Cook national parks. There have also been substantial post-glacial changes, especially marked in South Westland and the Southern Alps. Erosion is rapid, especially west of the Main Divide. Intense gullying, serrated ridges, and major and minor rock falls are characteristic of this zone. However, glacial landforms are almost entirely intact in Fiordland.

The vegetation is notable both in national and international terms for its diversity and essentially pristine condition. A floristically rich alpine vegetation of shrubs, tussocks and herbs extends around the summits of the mountains, from about 1,000 m to the permanent snowline. At warmer lower altitudes, the rainforest is dominated by dense stands of tall podocarps. The wetter, milder west is characterized by luxuriant rainforest and wetlands; the drier, more continental east has more open forest, shrublands and tussock grasslands. The most extensive and least modified natural freshwater wetlands in New Zealand are found in this area. Sizeable open wetlands, including high-fertility swamps and low-fertility peat bogs, are a particular feature of the south Westland coastal plain.

Mount Cook National Parks

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The best-known vegetation chronosequences are those on glacial landforms where the ages of outwash, terrace and higher piedmont surfaces are known. The most impressive landform chronosequence is the flights of marine terraces in southern Fiordland. As the least-modified region on mainland New Zealand, the south-west is the core habitat for many indigenous animals, including a number of primitive taxa, and contains the largest and most significant populations of forest birds in the country, most of which are endemic to New Zealand. A few mountain valleys in Fiordland harbour the total wild population (about 170 birds) of the takahe, a large flightless rail believed extinct until 'rediscovered' in 1948 and which is recognized as endangered. Most of New Zealand's fur seals are found along the south-west coast. Virtually wiped out by sealing in the early 1800s, they currently number about 50,000.

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A Maori association with the area falls into three broad categories: mythological, traditional history and ethnological. All these values are contained within the tradition of the Ngai Tahu tribe, whose ancestral territories cover all except the extreme northern parts of South Island.

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Thailand Thungyai-Huai Kha Khaeng Wildlife Sanctuaries

The Thungyai-Huai Kha Khaeng Wildlife Sanctuaries comprises two contiguous wildlife sanctuaries: Thung Yai and Huai Kha Khaeng, alongside the western international border with Myanmar, 300 km north-west of Bangkok. The terrain in Huai Kha Khaeng is generally hilly with many permanent and seasonal streams. The highest peak lies in the extreme north of the sanctuary. Valleys are interspersed with small lowland plains. In Thung Yai the topography is more dissected with a network of many permanent rivers and streams dividing the area onto valleys and lowland plains. A distinguishing feature is a large central grassland plain, from which the Sanctuary takes the name of Thung Yai ('big field'). Within the catchment area are four important rivers, one of which flows through Burma to the Andaman Sea.

Continent: Asia

Country: Thailand

Category: Natural

Criterion: (VII)(IX) (X)

Date of Inscription: 1991

Huai Kha Khaeng Wildlife

A physical feature that is important for wildlife is the presence of mineral licks. These occur throughout the sanctuary as either wet or dry, and most appear to be located on, or around, granite intrusions in areas with red-yellow podzolic soil and may be associated with the massive faults or lineaments in the intensely folded geomorphology of this area. Small lakes, ponds and swampy areas occur, some being seasonal whereas others are perennial; these are important wildlife habitats; limestone sinkholes are found.

Five types of forest can be distinguished: the highest slopes are covered with hill evergreen forest, whereas slopes above 600 m generally support dry semi-evergreen forest. The rest of the sanctuary supports mixed deciduous and bamboo forest, and dry dipterocarp forest in areas with poor or shallow soil. Along some rivers and streams, evergreen gallery forest occurs.

Thungyai-Huai Kha Khaeng Wildlife Sanctuary

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Thung Yai also has two specific features not common in other areas which add to its uniqueness. One is the existence of large grassland plain and surrounding savannah forest made up of cycads and Phoenix palm, a feature not known elsewhere in the region. The second feature is the existence of Thailand's most extensive riparian forests.

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The fauna of both Thung Yai and Huai Kha Khaeng includes an unusual mix of species with primarily Sundaic, Indo-Chinese, Indo-Burmese and Sino-Himalayan affinities, many of whose ranges do not overlap. Species lists have been compiled that include 120 mammals, 400 birds, 96 reptiles, 43 amphibians and 113 freshwater fish. 34 internationally threatened species are also found within the confines of the two sanctuaries. It also is home to 22 species of woodpecker, more than any other park in the world. The reason for such exceptional diversity is partly due to its status as one of only two evergreen forest refuges during the driest periods of the Pleistocene glaciations. Few areas in Asia are large enough to support viable populations of large herbivores (300 elephants) and predators.

Being contiguous with the forest of Myanmar there are longer term prospects for a transfrontier reserve between the two countries. This would greatly add to its integrity as there is cross-border migration of some species and Thai logging concessions in Myanmar could be reduced. Some 3,800 tribal people live within Thung Yai, whereas there is no resident population within Huai Kha Khaeng.

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