Millstream Falls National Park Tropical North Queensland

Photo credit: © Jodie Bray

Be inspired: Chasing volcanoes (and waterfalls) in the tropical north

They say ‘don’t go chasing waterfalls’ but we suggest you do, and volcanoes too! Photo credit: Steven Nowakowski © Queensland Government

Nature, culture and history

    Image of Big Millstream Falls where three separate lava flows are visible.

    Three separate lava flows are visible at Big Millstream Falls.

    Photo credit: © Tamara Vallance

    Image of lemon-scented gum, white mahogany and ironbark.

    Lemon-scented gum, white mahogany and ironbark.

    Photo credit: Tamara Vallance © Queensland Government

    Image of a Mareeba rock wallaby.

    Mareeba rock wallaby.

    Photo credit: Tamara Vallance © Queensland Government

    Image of a laughing kookaburra.

    Laughing kookaburra.

    Photo credit: © Tamara Vallance

    Image of a striped marshfrog.

    Striped marshfrog.

    Photo credit: Harry Hines © Queensland Government

    Image of remains of World War II officers' mess fireplace.

    Remains of World War II officers' mess fireplace.

    Photo credit: Tamara Vallance © Queensland Government

    Natural environment


    Millstream Falls National Park has an interesting geological history. The ancestral Millstream valley was created more than three million years ago, when 300 million year old rocks (rhyolites and granites) were eroded. This formed an ancient landscape of rugged hills and deep valleys. About 3–1.2 million years ago, Windy Hill near Ravenshoe, where the wind turbines now stand, was created by a volcano. Periodic eruptions poured three lava flows into the rivers, partly filling the Millstream and other ancient valleys. At Big Millstream Falls, the oldest of these flows is at the base of the falls. The youngest flow, 1.24 million years old, forms the car park area and upper slopes of the valley. The middle flow weathered to form a thick soil. This indicates that some time passed between its eruption and the most recent lava flow. As each lava flow cooled, contraction formed vertical cracks and produced the cooling columns that can be seen in the cliffs and rock surfaces above the falls. For 1.2 million years, erosion by the river has cut through the sequence of lava flows, exposing the individual flows and cooling columns. Weathering of the original, black basalt rock has created the rich, red agricultural soils in the Ravenshoe area. At Little Millstream Falls, the stream has cut down through the basalts that form the car park and upper parts of the gorge and, at the falls themselves, the water flows over rhyolite.


    The vegetation at the south-west end of the park is open forest on basalt soils. Blue gum Eucalyptus tereticornis, ironbark E. crebra, white mahogany E. portuensis and pink bloodwood Corymbia intermedia share the upper storey with bakers oak Allocasuarina torulosa.

    The north-east end of the park is open forest, also on basalt soils. White stringy bark E. reducta and rough-barked apple Angophora floribunda dominate the canopy but pink bloodwood C. intermedia and Bakers oak Allocasuarina torulosa are also present.

    The vegetation in the central area of the park is open forest. Lemon-scented gum C. citriodora and white mahogany E. portuensis dominate the canopy with pink bloodwood C. intermedia and turpentine Syncarpia glomulifera also occurring. A dense ground layer (up to 1 m high) is mainly composed of blady grass Imperata cylindrica and kangaroo grass Themeda australis.

    The riparian vegetation is open forest dominated by river oak Casuarina cunninghamiana. Also found are blue gum E. tereticornis, swamp box Lophostemon suaveolens, Melaleuca fluviatilis, broad-leaved tea-tree M. leucadendra, spotted silky oak Buckinghamia celsissima and red kamala Mallotus philippensis with an understorey of weeping bottlebrush Callistemon viminalis and sweet bursaria Bursaria tenuifolia.


    Mammals found in the Millstream area are mostly typical of those found in similar forest types. Stripe-faced dunnarts Sminthopsis macroura, feathertail gliders Acrobates pygmaeus, sugar gliders Petaurus breviceps, greater gliders Petauroides volans, common brushtail possums Trichosurus vulpecula, common ringtail possums Pseudocheirus peregrinus, whiptail wallabies Macropus parryi and common wallaroos M. robustus and Mareeba rock wallabies (Petrogale mareeba) have all been recorded within the park. There are also records of platypus Ornithorhynchus anatinus in the Millstream River at various locations. The distribution of the northern quoll Dasyurus hallucatus once extended to this area but there have been no confirmed sightings for some time.

    Several common frogs and reptiles have also been recorded in Millstream Falls National Park. These include the striped marshfrog Limnodynastes peronii, stony creek frog Litoria lesueuri sensu lato, Tableland gungan Uperoleia altissima, pallid rocketfrog Litoria pallida, broad palmed rocketfrog Litoria latopalmata, bumpy rocketfrog Litoria inermis, eastern water dragon Intellagama lesueurii, eastern water skink Eulamprus quoyii, rainbow skink Carlia rostralis, slaty-grey snake Stegonotus cucullatus and the skink Saproscincus basiliscus.

    Over 160 bird species have been recorded in the Millstream Falls National Park area. These include woodland residents like the laughing kookaburra Dacelo novaeguineae, rainbow bee-eater Merops ornatus, black-faced cuckoo-shrike Coracina novaehollandiae, striated pardalote Pardalotus striatus, magpie-lark Grallina cyanoleuca, pied currawong Strepera graculina and peaceful dove Geopelia striata. Aquatic species include the little pied cormorant Phalacrocorax melanoleucos, Pacific black duck Anas superciliosa, darter Anhinga melanogaster, hoary-headed grebe Poliocephalus poliocephalus and little black cormorant P. sulcirostris. The common koel Eudynamys scolopacea, channel-billed cuckoo Scythrops novaehollandiae, pheasant coucal Centropus phasianinus and other coucals are migratory visitors.

    Culture and history

    Non-indigenous heritage

    In 1942, the Commander-in-Chief of the Australian Military Forces, General Sir Thomas Blamey, investigated using the Atherton and Evelyn tablelands as a base for rehabilitating and training troops. The area was close to the battlefields of New Guinea and the climate would give the troops respite from the tropical heat of the coast and assist in the convalescence of sick and wounded soldiers. The tablelands also provided a training area similar to that of the South East Asian environment. During 1943, troops began arriving at bases established across the tablelands.

    Approximately 320 army and ancillary units were based on the tablelands across 160 sites. Today, the remains of sites found in Millstream Falls National Park are the most complete. Camp sites, walking tracks, water drains, concrete slabs, trenches, training areas, corduroy roads, a flag pole site and training and parade grounds are clearly evident.

    The Millstream Falls campsites were built to hold almost 1000 men each and were mostly tent accommodation and cooking, latrine and washing facilities. A network of rock-lined granite paths and roads linked the facilities. Service units had extra facilities such as roads, car parks and vehicle ramps.

    Units of the 7th Division, some returning from the Kokoda Trail, were the first to arrive and built the initial structures. They stayed for six months, leaving for New Guinea in mid-1943. The units of the 9th Division arrived at Millstream Falls in early 1945 and they improved the existing facilities, adding another 'layer' of history to the area. These units were also deployed to New Guinea, in mid-1945.

    These training areas on the tablelands were used continuously until shortly after the war ended in August 1945. The facilities and structures were then demolished and most of the debris buried.

    Indigenous heritage

    The Jirrbal people are the Traditional Owners of Millstream Falls National Park. Their dry forest and rainforest country extends from Herberton in the north, west to Ravenshoe, east to Evelyn Central and south to Davidson Creek at the bottom of Tully Gorge. Jirrbal people have an intimate knowledge of traditional country and close kin affiliations with neighbouring groups.

    Traditionally, the Jirrbal people lived in the rainforest in semi-permanent villages of dome-shaped huts. The rainforest was rich in resources and the Jirrbal people gathered a variety of nuts, seeds, fruits, roots, stems, tubers and leaves, which were either eaten raw or processed and cooked.

    Hunted food included fish, eels, snakes, wallabies, goannas, possums, flying-foxes and birds—particularly cassowaries, Australian brush-turkeys and orange-footed scrubfowl. Hunting tools included fishing lines and hooks, fish traps, nets, nooses, hunting spears and toxic leaves. Fish and eels were wrapped in ginger leaves and cooked in ground ovens or placed on racks and smoked.

    The Jirrbal people manipulate and craft an extensive array of implements and decorations including stone axes, shields, swords, spears, cooking utensils, baskets, woven blankets, nets, traps, fishing lines, hooks, bags and children's toys.

    The Nganyaji Interpretive Centre in Ravenshoe showcases the Jirrbal's traditional lifestyle, their rainforest base-camp villages, hunting and gathering practices, food processing, rainforest cuisine, community life and contact history.

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