Hinchinbrook Island National Park Tropical North Queensland

The rugged beauty of Hinchinbrook Island National Park must be seen to be believed! Photo credit: Maxime Coquard © Tourism and Events Queensland

Nature, culture and history

    Image of part of the mountainous backbone of Hinchinbrook Island.

    Part of the mountainous backbone of Hinchinbrook Island.

    Photo credit: Queensland Government

    Natural environment

    Geology and landform

    Hinchinbrook Island is dominated by a mountainous backbone featuring peaks such as Mount Bowen (1142m), Mount Diamantina (955m), Mount Straloch (922m), Mount Pitt (722m), Mount Burnett (655m) and Mount Barra Castle (579m). These mountains comprise two distinct rock types. The main mass centred on Mount Bowen consists of granite, while the mass projecting north-west and including Mount Pitt and Mount Burnett consists of silicic volcanics. The granite of the main mountain mass has weathered to spectacular, often jagged peaks.

    The island is separated from the mainland by the narrow Hinchinbrook Channel, which represents the flooded valley of the Herbert River. Most of the island is mountainous with steep slopes and only a narrow coastal plain. Near George Point, there is an extensive deposit of sand and, at the north-eastern extremity of the island, a peninsula juts to the north. This peninsula consists of four separate rocky outcrops joined by sand dunes. Generally, these dunes are low-lying, but can reach heights of up to 60 m near the northern end of Ramsay Bay. The sheltered side of these dunes supports an extensive mangrove and salt flat area on colluvial and alluvial deposits, with numerous deep channels. Another extensive mangrove area is present between Gayundah and Deluge inlets and numerous smaller occurrences are scattered around the coast.

    Image of a pied imperial pigeon.

    Pied imperial pigeon.

    Photo credit: © Queensland Government

    Native animals and habitats

    As mainland habitats are cleared or fragmented, Hinchinbrook Island is becoming increasingly important as a refuge for animal species of the coastal lowlands. The topography from mangroves to mountaintop provides a wide range of habitats. Significant species recorded include the pied imperial-pigeon Ducula bicolour, beach stone-curlew Esacus neglectus, estuarine crocodile Crocodylus porosus, dugong Dugong dugon and Australian snubfin dolphin Orcaella heinsohni.

    Plants and plant communities

    Hinchinbrook Island lies in the wet tropical rainforests biogeographic region. It is subject to hot and humid conditions and high rainfall, with occasional short spells of cooler, dry weather in winter. These factors, along with generally poor, shallow soils, determine vegetation patterns. To date, about 30 plant communities have been identified, with around 700 species recorded.

    While areas of rainforest occur at low and high altitudes, most of the mountainous part of the island is covered with open forests and low heaths on shallow soil. The mangroves which line Missionary Bay and Hinchinbrook Channel form one of the largest mangrove areas on the Australian continent and include 31 species of mangrove. Some small but significant areas of broad-leaved tea tree Melaleuca viridiflora woodland occur on the north coast. Vegetation types such as this have assumed conservation importance as similar types on the mainland face increased rates of clearing. This is true of most of Hinchinbrook Island's plant communities, particularly lowland types, which may well be restricted to Hinchinbrook Island in years to come. A survey of all the tropical lowlands from Ingham to Cooktown indicated that Hinchinbrook Island National Park and Hinchinbrook Channel are of outstanding importance because of the diversity of rare communities. About 14 species of rare and threatened plants have been recorded on the island, although it is highly likely that others exist awaiting discovery. One species of the shrub Comesperma—Comesperma praecelsum—is known only from Hinchinbrook Island. Other species such as the blue banksia Banksia plagiocarpa and sundew Drosera adelae are restricted to the island and adjacent mainland.

    Culture and history

    The Traditional Owners, the Bandjin and Girramay people, work closely with QPWS to make decisions about the management of their ancestral country known as Munamudanamy.

    Munamudanamy is the ancient Biyay name for the landscape that Europeans termed ‘Hinchinbrook’, after the estate of the Earl of Sandwich, Captain Cook’s sponsor. The name ‘Hinchinbrook’ is a singularity, a simple name for a single island. Munamudanamy is more complex, and is the collective name that describes the journey through the landscape of sea, mangroves, rivers, swamps, forests and mountains; each with their own individual names and stories.

    Find out more about the Bandjin and Girramay people’s connection to Munamudanamy.

    Sean Choolburra shares creation stories of Girramay Country in Queensland.

    There are few sites of post-contact cultural or historical significance on the island, with the exception of the wreck of an American B-24 Liberator bomber, which crashed on Mount Straloch's southern slopes on 18 December 1942. The bomber, known as the ‘Texas Terror’, crashed during a violent storm, killing all 12 people on board. Fresh from the factory and heading for the battlefields of Papua New Guinea and the Solomon Islands, the B-24 was being flown from Amberley to the bomber base at Iron Range in far north Queensland. Read more about the crash.

    Cyclone Yasi in February 2011 shifted tonnes of sand to uncover the remains of an old sailing ship in Ramsay Bay. The brigantine Belle was lost 130 years ago while attempting to recover cedar that had washed ashore from another wrecked vessel, the Merchant. A total of five ships have been wrecked in the same area.