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Nature, culture and history

Natural environment

The freckled monitor Varanus tristis is one of many reptiles found in Isla Gorge National Park. Photo courtesy Robert Ashdown.

The freckled monitor Varanus tristis is one of many reptiles found in Isla Gorge National Park. Photo courtesy Robert Ashdown.

Flowering gravilleas provide splashes of red throughout the park. Photo courtesty Robert Ashdown.

Flowering gravilleas provide splashes of red throughout the park. Photo courtesty Robert Ashdown.

Wddge-tailed eagles can be seen from the lookout, often soaring high above the park. Photo: Robert Ashdown Queensland Government

Wddge-tailed eagles can be seen from the lookout, often soaring high above the park. Photo: Robert Ashdown Queensland Government

Stone, water and time

Isla Gorge is set within a geographic region known as the Central Queensland Sandstone Belt. This rugged, elevated landscape covers an area of approximately 82,000 km2. At least 25 mountain ranges radiate from the Great Dividing Range in this region, in some places rising to over 1000 m above sea-level, earning this area its other nickname—the 'Roof of Queensland'.

This wild landscape is the result of a long and turbulent geological history. The sandstones of this region were created from vast sheets of sand deposited on river plains in the Jurassic Period, about 190 million years ago. After millions of years of uplift and erosion, the sandstones remain today as cliffs, gorges and valleys. In some places basalt from volcanoes caps the sandstone ridges.

The gorges of Isla Gorge National Park have been created from the erosion of colourful Precipice Sandstone by the tributaries of Gorge Creek, which eventually drains into the Dawson River. The upper part of the sandstone, such as at the lookout, is made of thin beds of white, very fine-grained sandstone and siltstone, but lower down there is more typical yellowish, course-grained, cross-bedded sandstone in thick beds.

A rich diversity of life

The national parks of this area are also located within a biological region (bioregion) known the Southern Brigalow Belt. Named after brigalow Acacia harpophylla, a plant that once covered much of this area, this bioregion is a complex mosaic of different vegetation communities. In the central highlands area, plant communities of the arid inlands (dominated by acacias such as mulga or brigalow) mix with plant communities of the more humid regions (dominated by eucalypts). Remnants of dry rainforest (softwood scrub) and natural grasslands are also found throughout the area.

Many of the plant communities of the Southern Brigalow Belt are classed as 'threatened' due to clearing, altered fire regimes and the effects of introduced species. As only just two per cent of this bioregion is conserved within national parks and other protected areas, parks such as this one play a key role in conserving examples of the area's original vegetation communities. Isla Gorge National Park conserves nine regional ecosystems of the Southern Brigalow Belt, three of which are classed as 'endangered'.

Eucalypt forests of yellow bloodwood and narrow-leaved ironbark dominate the park, while patches of brigalow scrub and dry rainforest (softwood scrub) are also found throughout. Woodlands of poplar box are found on the alluvial plains.

These plant communities provide habitat for a large range of animal species within Isla Gorge. Fifteen of these fauna species are classed as either rare or threatened.

Isla Gorge is home to many types of birds. Honeyeaters include spiny-cheeked, brown, white-eared and blue-faced, when eucalypts, wattles, grevilleas and boronias are in flower from mid-winter to summer. Wedge-tailed eagles sour high above the gorges and peregrine falcons leave secluded roosts on cliff faces to hunt. Two species, the varied triller and the emerald dove, are found only within the park's softwood scrub. The squatter pigeon can also be seen along the edges of tracks and roads in this area.

A diverse collection of reptiles species are found within Isla Gorge, including the frilled lizard, the brigalow scaly-foot, the golden-tailed gecko, the Capricorn worm-skink and a number of gecko species. Mammals such as the Herbert's rock wallaby, the common wallaroo, the sugar glider and the fawn-footed melomys, as well as a diverse range of insectivorous bat species, have been recorded within the park.

Culture and history

Parts of the Flagstaff Road still exists 148 years after it was built. Photo: Robert Ashdown, Qld Govt.

Parts of the Flagstaff Road still exists 148 years after it was built. Photo: Robert Ashdown, Qld Govt.

A road gang on the Maryborough to Biggenden Road. Date unknown. Photo courtesy of the State Library of Queensland.

A road gang on the Maryborough to Biggenden Road. Date unknown. Photo courtesy of the State Library of Queensland.

Wool teamsters with a loaded wagon of wool bales on the road to port, 1869. Photo courtesy of the State Library of Queensland.

Wool teamsters with a loaded wagon of wool bales on the road to port, 1869. Photo courtesy of the State Library of Queensland.

Isla Gorge falls within the traditional land of the Iman Aboriginal people. Rock engravings and stencil images on sandstone walls are a reminder of the Iman people's long association with this land.

In 1844 explorer Ludwig Leichhardt travelled through this area on his way from the Darling Downs to Port Essington near Darwin in the Northern Territory. Leichardt named many features after expedition members and supporters.

With the arrival of settlers soon after, decades of conflict began as the Iman strove to keep their lands from the new arrivals. However, by 1920 the conflict and European diseases had taken their toll and remaining Aboriginal people were forcibly removed to distant 'reserves'.

Flagstaff Hill

The north-western tip of Isla Gorge National Park conserves the remains of a hand-paved road. Travelling between Roma and the port of Rockhampton, bullock teams and their heavy wagons once used this steep and winding road to negotiate the Dawson Range. The wagons carried wool to the port and supplies back to Roma and further west.

The Flagstaff Road, as it was known, was in use by 1860—less than 15 years after white settlement in the area. H. C. Gregory was contracted in that year, for the sum of £200, to build sections of the Palm Tree Creek to Flagstone Road, including the paving of this section of road. While the steepest section of the road was approximately 500 m long, about 150 m was surfaced (or flagged) with hand-hewn stones.

The paving was completed by a team of six men after six months work in 1863. Rocks, some weighing approximately 200 kg, were brought in from nearby areas and used in the flagging. The stones were cut and set into the ground with care so that the edges fitted neatly together. Flagged drains were created at various intervals along the road to drain storm water. The men also had to make a cutting through rock to ease the incline, and the road also had to be widened.

Traffic on the Flagstaff Road declined in the early 1930s. A new road between Taroom and Theodore had opened, and the new toll road at Toowoomba allowed wool to be transported to the Brisbane port.

Last reviewed
1 March 2018
Last updated
10 November 2017