Barrington Tops
Australia, New South Wales
Barrington Tops
About Barrington Tops
Barrington Tops National Park is a UNESCO World Heritage-listed protected area in the Hunter Valley region of New South Wales, approximately 260 kilometres north of Sydney. Covering over 74,000 hectares, the park encompasses a spectacular high plateau rising to 1,586 metres at Carey's Peak, supporting some of the most intact temperate rainforest and subalpine communities in eastern Australia. The park forms part of the Gondwana Rainforests of Australia World Heritage Area and represents one of the last significant refugia for rainforest species in eastern Australia. Its ancient Antarctic beech forests, diverse wildlife, and dramatic mountain scenery make it one of New South Wales's premier natural areas.
Wildlife Ecosystems
Barrington Tops harbours an exceptional diversity of fauna, including many species dependent on old-growth forest. The platypus inhabits permanent streams, and the long-footed potoroo, one of Australia's rarest marsupials, has been recorded in the park. Greater gliders and yellow-bellied gliders occupy the tall eucalypt forests, while koalas inhabit lower eucalypt woodlands. Barred galaxias, a threatened freshwater fish, occur in highland streams. Birdlife is outstanding, with Albert's lyrebird in the rainforest, the powerful owl in old-growth forest, rufous scrub-bird, and numerous migratory species visiting in summer. The park is also significant for its diversity of frog species, including the endangered booroolong frog.
Flora Ecosystems
The vegetation of Barrington Tops is extraordinarily diverse, ranging from subalpine grassland and heath on the exposed plateau to warm temperate rainforest at lower elevations. Antarctic beech dominates the cool temperate rainforest on the highest ridges, a relic of the ancient Gondwana forest that covered much of Australia before continental drift and climate change. Warm temperate rainforest in sheltered gullies features coachwood, sassafras, and corkwood. Tall wet sclerophyll forest with mountain ash and alpine ash encircles the rainforest on middle slopes. The plateau supports sedge bogs and heathland communities with endangered ecological community status under national law.
Geology
The Barrington Tops plateau is underlain by late Permian and Carboniferous basalt and rhyolite volcanic rocks, part of the extensive Liverpool Range volcanic province. These volcanic rocks cap a basement of Carboniferous granite and sedimentary rocks. The basalt plateau is relatively flat, reflecting the extensive horizontal lava flows, but is deeply incised by river gorges draining toward the Hunter and Manning river systems. The high plateau was extensively glaciated during the last ice age, and glacial features including cirques, arêtes, and periglacial deposits are visible in the summit zone. The ancient rocks support the distinctive soils and drainage patterns that sustain the unique highland vegetation communities.
Climate And Weather
Barrington Tops has a cool temperate to subalpine climate on its highest sections, with conditions dramatically different from the surrounding lowlands. The plateau receives 1,800 to 2,000 millimetres of rain annually and is one of the wettest places on the New South Wales mainland. Snow falls several times each winter, typically from June to August, and the plateau can be blanketed for days at a time. Summer temperatures on the summit rarely exceed 20°C. Fog and mist are common year round, especially in the beech forests. The surrounding lowlands are significantly warmer and drier. The park experiences a wide annual temperature range and rapid weather changes that demand careful visitor preparation.
Human History
The Worimi, Biripi, Awabakal, and Gringai peoples are among the traditional custodians of the Barrington Tops region, with the mountain plateau used seasonally for ceremony and food gathering. Bogong moths, which mass in alpine crevices during summer, were an important food source for Aboriginal people, who gathered on the plateau during summer months for feasting and ceremony. European settlement began in the Hunter Valley in the 1820s, and the Barrington Tops was explored for its timber resources, particularly cedar and coachwood in the lower rainforest zones. Logging, grazing, and dairying were practiced within the current park boundaries well into the 20th century.
Park History
Barrington Tops was gazetted as a national park in 1969, though parts of the area had been protected as a state forest for some decades previously. The park's boundaries have been expanded substantially since initial gazettal, incorporating additional areas of rainforest and subalpine habitat. In 1986, the park was inscribed as part of the East Coast Temperate and Subtropical Rainforest Parks World Heritage Area, subsequently incorporated into the Gondwana Rainforests of Australia World Heritage Area. Management has addressed the substantial impacts of previous logging and grazing, with extensive rehabilitation of degraded sites and feral animal control programs, particularly targeting feral deer, pigs, and horses.
Major Trails And Attractions
Barrington Tops offers an extensive network of walking trails across all levels of difficulty. The Gondwana Rainforest Walk is a gentle introduction to the World Heritage rainforest, passing through an Antarctic beech forest of extraordinary age and beauty. The Careys Peak circuit provides panoramic views from the highest point in the park. The Rocky Crossing and Polblue Circuit visits highland bogs and diverse woodland communities. The Barrington Guest House, located at Barrington Tops village adjacent to the park, offers accommodation and guided walks. Camping beneath the beech forest canopy is one of the most evocative experiences in New South Wales. The trout fishing in Barrington River attracts anglers from across the state.
Visitor Facilities And Travel
Barrington Tops National Park is accessed from Gloucester to the east or Scone to the west via unsealed mountain roads, some sections of which may be impassable after heavy rain. Camping areas are available at Gloucester River, Polblue, and Wombat Creek, with basic facilities including pit toilets and picnic tables. The Barrington Tops road is regularly graded but requires care in wet weather. A small visitor information facility operates seasonally at the park boundary near Gloucester River campground. Supplies should be obtained in Gloucester or Scone before entering the park. Fuel is not available within the park.
Conservation And Sustainability
Conservation challenges in Barrington Tops include managing feral deer, horses, and pigs, which cause significant damage to the rainforest and subalpine ecosystems through browsing, trampling, and soil disturbance. Coordinated aerial and ground-based control programs are conducted regularly. Phytophthora cinnamomi, the root rot pathogen, threatens susceptible plant communities and is managed through hygiene measures and vehicle washdown stations. Climate change poses a long-term threat to the viability of the Antarctic beech communities and subalpine bog systems, which are already at the edge of their climatic range. The park's World Heritage status brings international conservation obligations and associated scientific monitoring programs.
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Frequently Asked Questions
Where is Barrington Tops located?
Barrington Tops is located in New South Wales, Australia at coordinates -31.9167, 151.4667.
How do I get to Barrington Tops?
To get to Barrington Tops, the nearest city is Dungog (50 km), and the nearest major city is Newcastle (116 km).
How large is Barrington Tops?
Barrington Tops covers approximately 765.4 square kilometers (296 square miles).
When was Barrington Tops established?
Barrington Tops was established in 1969.