Updated 9 October 2026
Ipswich Waterways at a Glance
- Warrill and Purga dominate: Together, their catchments cover more than half the land draining to the Bremer River.
- New estates feed old creeks: Runoff from Providence, Ecco Ripley and Whiterock drains towards Bundamba Creek, then the Bremer.
- Small creeks can rise fast: Urban creeks respond quickly to storms, while high river levels can slow drainage at their mouths.
Is Warrill Creek bigger than Bundamba Creek?
Is Woogaroo Creek bigger than Goodna Creek?
Which creek drains the new runoff from Providence, South Ripley and White Rock Estate?
Which creek has the highest starting point?
Which creek has the steepest runoff?
If you have asked questions like these you’re in the right place.
Today, we’re looking at Ipswich waterways. The biggest, longest and most important to our everyday life.
Ready to jump in?
Find your river or creek
Brisbane River • Bremer River • Warrill Creek • Bundamba Creek • Deebing Creek • Purga Creek • Black Snake Creek • Western Creek • Franklin Vale Creek • Woogaroo Creek (incl. Opossum & Mountain) • Goodna Creek • Six Mile Creek • Mihi Creek • Ironpot Creek • Sandy Creek (Tivoli)
Reading the guide: A catchment is the land that drains into a waterway. Waterway health describes its ecological condition, not whether the water is safe to drink. Nicknames are ours.
Spot an error or have local knowledge to add? Let us know.
Brisbane River
Brisbane River drainage basin
The basin includes the land drained by all its tributaries. The three largest are Lockyer Creek (3,032 km²), the Bremer River (about 2,030 km²) and the Stanley River (1,532 km²).
About this waterway
- Our nickname: Ipswich Water Main.
- Ipswich reach: Kholo and Chuwar, past Karalee and Barellan Point, to Riverview and Goodna. The river is also known as Maiwar.
- Source: Mount Stanley in the Somerset Region, about 213 m above sea level.
- Length: About 344 km in total.
- Catchment: About 13,570 km² to the Port Office gauge. The river forms part of Ipswich’s northern edge.
- Water supply: Water passes Kholo on its way to the Mt Crosby treatment works.
Water and wildlife
- Flow: Wivenhoe releases influence the middle reaches, while tides affect the lower river. Long wet spells can raise levels quickly.
- Water quality: The river gets muddier after heavy rain and generally clears during dry spells.
- Wildlife: Lungfish live upstream, and bull sharks have been found near the Ipswich boundary.
Flooding: Goodna, Karalee and Barellan Point were hit in 2011 and 2022. High river levels can push water back into local creeks.
Places and history
- Along the banks: Acreage at Karalee and Barellan Point, paddocks near Muirlea, and denser housing at Goodna and Riverview.
- Landmarks: Kholo Bridge, Mt Crosby Weir and Colleges Crossing.
- River access: Goodna Boat Ramp at Richardson Park, Joseph Brady Park at the Bremer mouth, and Colleges Crossing. Check local conditions and warnings before heading out.
- Fishing and paddling: Joseph Brady Park and Kholo Reserve are popular spots.
- Working river: Colonial supply boats used this stretch. Training walls near the Bremer mouth helped shape the navigation channel.
- Hidden history: The ruins of an 1890s pumping station sit in the scrub at Kholo.
Bremer River
Bremer River catchment: about 2,030 km²
Everything inside the orange drains to the Bremer, including Warrill, Bundamba, Deebing and Western creeks. Ipswich’s other catchments drain to the Brisbane River.
Land draining directly to the Bremer
The blue shows land that drains straight into the Bremer River, excluding the tributary catchments.
About this waterway
- Our nickname: Mud Monster, for the sediment it carries into the Brisbane after heavy rain.
- Role: The Bremer collects water from Warrill, Purga, Bundamba, Deebing, Western, Franklin Vale and smaller creeks, then joins the Brisbane River.
- Source: The Main Range in the Scenic Rim, about 394 m above sea level.
- Length: About 100 km, with tides affecting the lower 19 km.
- Catchment: About 2,030 km², including Rosewood, Walloon, Thagoona, Karrabin, central Ipswich, Basin Pocket, North Booval, Moores Pocket, Tivoli and Chuwar.
Water and wildlife
- Flow: Levels rise quickly after storms, while pools remain in dry spells. Tides expose broad mudbanks and reach Lynch’s Crossing, upstream of Hancock Bridge.
- Water quality: Erosion and sediment are major challenges. Stabilising banks and restoring vegetation help keep soil out of the river.
- Wildlife: Estuary fish use the lower river. Woodlands along the upper and middle reaches support koalas and birds.
Flooding: Basin Pocket, North Booval and Moores Pocket have flooded repeatedly. High Brisbane River levels can also push water back up the Bremer.
Places and history
- Along the banks: Historic neighbourhoods sit on the bends, with industry on the flats near North Booval and Tivoli. David Trumpy Bridge crosses the river in the CBD.
- River access: Cribb Park and River Heart offer riverfront access. Joseph Brady Park sits where the Bremer meets the Brisbane.
- Fishing: Check current fish-consumption notices before keeping your catch.
- Working river: Wool barges and wharves gave way to coal, coke and rail.
- Elephant rescue: An elephant helped refloat the steamer Bremer in 1941.
- Rail history: Queensland’s first railway opened from North Ipswich in 1865. Stone bridge abutments still stand.
Warrill Creek
Warrill Creek catchment
Warrill is green and Purga is turquoise, overlaid on the orange Bremer catchment. Purga flows into Warrill, Warrill into the Bremer, and the Bremer into the Brisbane at Joseph Brady Park.
Warrill’s catchment makes up 45.5% of the Bremer basin. Include Purga and that rises to 56.8% — more than half the land draining to the Bremer.
About this waterway
- Our nickname: Scenic Rim Siphon.
- Source: Main Range National Park near Tarome and Aratula, about 538 m above sea level.
- Length: About 70 km, flowing through the farming country around Kalbar and Harrisville towards Amberley and the Bremer.
- Catchment: Includes the Lake Moogerah and Reynolds Creek system, plus country around Peak Crossing, Willowbank, Amberley and Yamanto.
- Farm water: Releases from Lake Moogerah support irrigation across the Fassifern Valley.
Water and wildlife
- Flow: Dam releases and storm runoff feed the creek. Summer downpours can quickly raise levels across the lower farms.
- River health: Fencing and replanting banks help reduce erosion. Wet years reshape sandbars and backwaters.
- Wildlife: Native fish use the creek’s long pools. Waterbirds gather at Ten-Mile Swamp after rain.
- Ten-Mile Swamp: This large wetland stretches from Warrill View towards Harrisville, between the Cunningham Highway and Warrill Creek.
Flooding: Prolonged rain can spread water across the Harrisville and Amberley plains. High Bremer River levels can worsen flooding in the lower creek.
Places and history
- Crossings: The Cunningham Highway and Ipswich–Boonah Road cross the floodplain. Old weirs, including Churchbank, have filled with silt.
- Access: Most creek frontage is private. Lake Moogerah offers public boating and fishing for bass and golden perch under the Stocked Impoundment Permit Scheme.
- Farming history: Dairying, orchards and irrigation have shaped the creek and its wetlands.
Bundamba Creek
Bundamba Creek catchment: about 114 km²
The creek drains Ripley Valley and the Swanbank–Blackstone area before meeting the Bremer near Bundamba and North Booval. New estates including Providence, Ecco Ripley and Whiterock use basins and planted drainage areas to slow and filter stormwater.
About this waterway
- Our nickname: Reborn Drain, inspired by the Small Creek restoration project.
- Source: East of Flinders Peak, about 212 m above sea level, flowing north through Ripley Valley.
- Length: About 30 km to the Bremer near North Booval.
- Catchment: About 114 km², covering parts of South Ripley, Ripley, Swanbank, White Rock, Raceview, Flinders View, Bundamba and Booval.
- Landscape: Bushland remains upstream. The creek passes through narrow valleys and broader floodplains before reaching the older suburbs.
Water and wildlife
- Flow: Levels rise and fall quickly after storms. Springs and urban runoff help maintain pools during dry spells.
- River health: Development and past mining contribute to erosion and sediment. Restoration includes replanting banks, replacing concrete channels and adding wetlands to filter runoff.
- Wildlife: Platypus have been recorded around Daly’s Lagoon. The creek corridor connects with bushland in the White Rock and Flinders–Karawatha areas.
Flooding: Debris can block the Colin Keidge Bridge on Swanbank Road during major floods. Water can also cross the Cunningham Highway near the Swanbank exit. Low-lying parts of Blackstone, Bundamba and Booval can flood quickly.
Places and history
- Small Creek: Concrete drains have been replaced with bends, shallow rocky sections, pools and native plants. New wetlands help slow and filter stormwater.
- Crossings: Creek Street and Brisbane Road bridges cross the lower creek.
- Water quality: Follow local PFAS and water-quality signs.
- Coal and power: Swanbank power stations, ash dams and railway branches shaped the area and its drainage.
Deebing Creek
Deebing Creek catchment: about 26 km²
The creek drains parts of Deebing Heights, Ripley and Yamanto before joining the Bremer near One Mile Bridge. It can rise quickly after heavy rain.
About this waterway
- Our nickname: Cultural Heartline.
- Source: The Grampian Hills at the southern end of Deebing Heights, about 117 m above sea level.
- Catchment: About 26 km², covering parts of Deebing Heights, Ripley and Yamanto before passing through Churchill and One Mile.
- Where it goes: Directly into the Bremer River near One Mile Bridge.
- Cultural significance: The creek runs through the Deebing Creek Mission area, linking heritage places and remaining bushland.
Water and wildlife
- Flow: The creek can dry out between rains, then rise quickly after storms. Stormwater basins slow runoff from surrounding estates.
- Water quality: Construction runoff is a concern. Vegetated buffers and stormwater basins help keep sediment out of the creek.
- Wildlife: Koalas and wallabies use remaining bushland. Evidence of platypus has also been reported.
Flooding: Low crossings around Yamanto can flood quickly during summer storms.
Places and history
- Heritage: The Deebing Creek Mission operated from 1892 to 1915, before the move to Purga. The mission and cemetery are heritage-listed.
- Changing landscape: New roads, culverts and housing estates surround parts of the creek. Heritage campaigns continue as the area grows.
- Pollution history: A clay-slurry spill caused a major fish kill in 2019.
Purga Creek
See Purga Creek’s catchment:
About 229 km² drains through Peak Crossing and Purga into Warrill Creek, just upstream of its junction with the Bremer. Wide floodplains hold water after rain, so flood peaks tend to build and recede more slowly than in the small urban creeks.
About this waterway
Purga is a working floodplain creek surrounded by grazing country. It also supports the nationally significant Swamp Tea-tree forest at Purga Nature Reserve.
- Source: The Scenic Rim south of Peak Crossing, at about 164 m elevation.
- Route: Peak Crossing and the Goolman foothills, through Purga towards Yamanto, then into Warrill Creek and the Bremer.
- Flow: The gently sloping land allows water to spread across the flats. Pools and wetlands can remain through dry periods.
Water and wildlife
- Creek health: Grazed sections can carry muddy, nutrient-rich water. Fencing stock out and replanting banks help reduce erosion.
- Wildlife: Koalas and glossy black-cockatoos use the woodland edges. The reserve’s boardwalk gives you a closer look at the rare tea-tree forest.
Flooding: Low roads, including approaches along Purga School Road, can go under during prolonged rain as water spreads across the flats.
Places and history
- Visit: Purga Nature Reserve for quiet walks, birdwatching and the tea-tree forest.
- Surroundings: Small townships, acreage and grazing paddocks occupy the catchment, with homes on the higher margins.
- Crossings: Ipswich–Boonah Road and the Cunningham Highway cross Purga Creek and its Little Purga tributary.
- History: Purga Mission followed Deebing Creek Mission. Farming on these flats dates to the 1850s.
Black Snake Creek
See Black Snake Creek’s catchment:
About 97 km² drains to the Brisbane River, including 35 km² within Ipswich. The two figures describe the whole catchment and the Ipswich portion. Catchment plan · Council’s local figures.
The creek gathers runoff from the ridges around Marburg and carries it through the township. Its floodplain provides room for water to spread, as well as a strip of habitat through grazing country.
About this waterway
The detention basin above Marburg slows floodwater before it reaches town. It reduces flood peaks, but heavy rain can still lift creek levels quickly.
- Source: The Little Liverpool Range, at about 209 m elevation.
- Route: From the uplands through Marburg, then across farming country towards the Brisbane River.
- Landscape: Grazing land and acreage surround the compact township. The broad creek flat beside the main street helps explain Marburg’s layout.
Water and wildlife
- Creek repair: Bank stabilisation, fencing and planting aim to reduce the sediment carried downstream.
- Wildlife: Vegetation along the creek provides shelter for waterbirds and habitat for small fish.
- Why it matters downstream: Black Snake Creek influences water quality upstream of the Mount Crosby water intake.
Flooding: Marburg’s town centre and low crossings remain vulnerable. The detention basin helps slow the flow, while the creek’s low corridor influences where roads, ovals and rural buildings can go.
Places and history
- Crossings: Warrego Highway culverts and local bridges carry roads across the creek.
- Flood works: The detention basin dates to 2002.
- Community effort: Local restoration projects have been running for more than a decade.
Western Creek
See Western Creek’s catchment:
The mapped sub-catchment covers about 122 km², around 6% of the Bremer basin. Western Creek also receives Franklin Vale Creek before joining the Bremer River. Broad grazing flats give floodwater room to spread, so peaks tend to last longer than those in the small urban creeks.
About this waterway
Western Creek drains farming country, connects wildlife habitat to the Bremer and runs through the rural landscape around Hidden Vale.
- Source: The Little Liverpool Range, at about 336 m elevation.
- Country drained: Grandchester, Calvert, Lanefield, Rosewood and Lower Mount Walker, from steep gullies to broad Bremer floodplains.
- Flow: Summer storms can produce flash floods. Long pools remain through dry periods.
- Land use: Grazing and cropping dominate, with country towns and scattered acreage homes on higher ground.
Water and wildlife
- Creek repair: Fencing cattle out, providing drinking water away from the creek and replanting banks help reduce erosion. Works on eroding bends also slow the loss of soil.
- Wildlife: Platypus have been detected through environmental DNA sampling. Frogs and koalas have also been recorded around blue-gum flats near restoration sites.
Flooding: Rosewood’s lowlands and the northern branches of the catchment can rise quickly during heavy summer storms.
Places and history
- Access: Much of the creek frontage is private land. Hidden Vale’s mountain-bike trails explore the surrounding hills.
- Rail history: The Ipswich–Grandchester line opened in 1865. Historic rail bridges and culverts remain in the farming landscape.
- Early industry: The valley carried timber and farm produce during the railway’s early years.
- Water treatment: Rosewood’s wastewater treatment plant discharges via lagoons and wetlands into Western Creek.
- Restoration: The junction with Franklin Vale Creek at Calvert is a focus for creek repairs.
Franklin Vale Creek
See Franklin Vale Creek’s catchment:
About 138 km², including 125 km² within Ipswich. That is roughly 6.8% of the Bremer basin. Water drains from the Franklin Vale and Grandchester foothills into Western Creek, then the Bremer River. Broad grazing flats give it a slower response to rain than the small urban creeks. Council catchment assessment.
About this waterway
Franklin Vale is a practical example of creek restoration on working farms. Council and landholders use fencing, stock watering points and planting to protect banks while keeping the land productive.
- Source: Mount Beau Brummel Conservation Park. The creek flows northeast through the valley before joining Western Creek.
- Landscape: Mostly pasture with woodland patches, farms, acreage and scattered rural localities.
- Flow: The creek can stop flowing in dry weather, leaving isolated pools. Sustained rain reconnects the channels.
Water and wildlife
- Creek health: Restoration sites have improved, while untreated gullies still send sediment downstream during big storms.
- Habitat: Remnants of Box-Gum Grassy Woodland and Swamp Tea-tree survive along the creek.
- Repair work: Fencing keeps cattle off fragile banks. Planting helps hold soil in place and rebuild habitat.
Floodplain: Low ground holds water after rain. Restoration works aim to slow and spread flows, reduce scouring and let more water soak into the soil.
Places and history
- Access: Much of the frontage is private farmland, crossed by local fords and bridges.
- Farming history: Generations of grazing shaped the gullies and flats. Creek repairs now tackle that erosion.
- Visible change: Before-and-after drone footage shows vegetation returning where stock are excluded and plants take hold.
- Infrastructure: Inland Rail hydrology mapping covers this sub-catchment.
Woogaroo Creek (incl. Opossum & Mountain)
See Woogaroo Creek’s catchment:
About 69 km² drains through Springfield, Brookwater and Augustine Heights to the Brisbane River at Goodna. The system includes Opossum Creek and Mountain Creek. Springfield’s lakes and wetlands help slow runoff and trap sediment. This catchment drains directly to the Brisbane River, outside the Bremer basin.
About this waterway
Woogaroo links White Rock bushland to the Brisbane River, providing wildlife habitat, shaded paths and space for floodwater through some of Ipswich’s fastest-growing suburbs.
- Source: White Rock–Spring Mountain Conservation Estate, with a high point around 305 m.
- Country drained: Springfield Lakes, Springfield, Brookwater, Bellbird Park, Camira and Goodna. Most of the catchment lies within Ipswich.
- Flow: The urban creeks rise quickly after rain. Detention lakes and wetlands help slow those peaks.
Water and wildlife
- Creek health: Protected headwaters in White Rock help preserve habitat. Shade, bank vegetation and sediment control matter as the surrounding suburbs grow.
- Wildlife: Platypus sightings have been recorded since 2021, alongside koala records through the Goodna and Springfield bushland.
Flooding: Bellbird Park and Camira can see creek levels rise quickly after storms. Repeated downpours can also push Goodna’s lower channels over their banks.
Conservation and development
- Woogaroo Forest: The local name for remnant bushland between Springfield, Brookwater, Bellbird Park, Camira and Goodna. It supports koalas, greater gliders and more than 100 bird species.
- Development plans: Springview and other staged proposals have involved clearing parts of the bushland for roughly 1,000–1,800 homes, with federal environmental review also involved.
- The debate: The area falls within longstanding Springfield growth plans. Council has pointed to historic zoning, while conservation groups argue for protection of wildlife habitat and connections between bushland areas. Habitat significance has also been disputed by the developer.
Places and history
- Walking and birdwatching: Opossum Creek Dog Park, Ric Nattrass Environmental Park and Robelle Domain provide places to explore the wider creek system.
- Crossings: The Centenary Highway spans the corridor. Paths, bridges and boardwalks connect parks around the lakes and creeks.
- Boating: Goodna Boat Ramp provides access to the Brisbane River.
- History: The historic Woogaroo hospital complex sits near the creek mouth. Woogaroo was an early European name for the district before Goodna became established.
Goodna Creek
See Goodna Creek’s catchment:
About 15 km². Goodna Creek drains Redbank Plains, Collingwood Park and Goodna into the Brisbane River beside Redbank Motorway Estate, on the Redbank–Goodna border. Its small catchment means water levels can rise quickly after storms.
About this waterway
- Nickname: Suburban Spine.
- Starts: Near the Redbank Plains–Swanbank boundary, about 59 m above sea level.
- Joins: The Brisbane River about 5 km downstream of Moggill Ferry.
- Flow: Levels rise and fall quickly during summer storms. A flooded Brisbane River can hold water back at the mouth.
Water and wildlife
- Habitat: Water dragons, ibis and hardy fish use the lower channels, with links to Woogaroo Creek and the Brisbane River.
- Creek health: Litter, hot runoff and straightened channels put pressure on habitat. Shaded banks and creekside planting help.
Flooding: Floodways through Collingwood Park and Goodna can overflow quickly in heavy rain. Brisbane Terrace and Queen Street causeways influence where that water spreads.
Places and history
- Suburbs: The creek carries runoff from some of Ipswich’s busiest residential areas. Local roads and culverts cross the channel through Collingwood Park and Goodna.
- Growth: Subdivisions built from the 1970s to the 2000s filled out the corridor. Bikeways now connect small parks along the creek.
Before the suburbs: Early town life relied on riverboat landings just downstream, along the Brisbane River.
Six Mile Creek
See Six Mile Creek’s catchment:
About 31 km². Six Mile Creek drains into the Brisbane River. Its short flow paths mean water levels can rise quickly after summer storms. Bushland in the upper catchment helps slow runoff before it reaches the suburban and industrial areas below.
About this waterway
- Nickname: White Rock Run.
- Starts: White Rock–Spring Mountain, behind White Rock Estate, about 151 m above sea level.
- Catchment: Runs north through Redbank Plains, New Chum, Collingwood Park and Redbank to join the Brisbane River downstream of Moggill Ferry.
- Role: Connects White Rock Conservation Estate to the Brisbane River through bushland and suburban areas.
- Flow: Rises quickly after storms, with culverts carrying water through the lower catchment.
Water and wildlife
- Habitat: Bushland supports birds and skinks, including near the industrial areas.
- Creek health: Modified channels and old excavations affect the lower reaches. Bushland in the headwaters helps protect the creek.
Places and history
- Surroundings: Suburban streets line the upper and middle reaches, with industry and logistics closer to the river. Floodways also provide space for services and vegetation.
- Walking: White Rock has bushwalking trails close to the growing suburbs.
Mining history: Old mining areas occupy the western catchment, while housing growth is concentrated to the east.
Mihi Creek
See Mihi Creek’s catchment:
About 6 km², or 0.3% of the Bremer catchment. Mihi Creek joins the Bremer River at Brassall, downstream of Albion Street Bridge. Water travels quickly through this small catchment and its culverts, so levels can rise sharply after storms and fall soon afterwards.
About this waterway
- Nickname: Coke Ovens Creek.
- Starts: Just north of the Warrego Highway at Muirlea, about 58 m above sea level.
- Catchment: About 5.9 km², entirely within Ipswich, draining the ridge between the Brisbane and Bremer catchments.
- Flow: Drains quickly after storms, leaving pools against rock shelves.
Water and wildlife
- Habitat: Water dragons and kingfishers use the creek. Its connection to the river also brings occasional estuary wildlife on high tides.
- Creek health: Weed removal and bank planting help, though erosion persists in the north-western headwaters.
Flooding: Summer storms can send water into the Bremer quickly, with little warning. Old embankments also influence how water moves through the corridor.
Places and history
- Along the creek: Parks, paths, historic rail embankments and culverts share the corridor near Albion Street.
- Rail history: Queensland’s first main line railway crossed this corridor.
- Industry: Coal mining and coke making operated beside Mihi Creek from the 1870s until around 1960. Tramways linked the works to the railway.
Hidden history: The Mihi Creek Complex preserves traces of coke ovens, mining works and Queensland’s first main line railway.
Ironpot Creek
See Ironpot Creek’s catchment:
About 17 km², or 0.8% of the Bremer catchment. Ironpot Creek drains Blacksoil, Brassall, Karrabin, Pine Mountain and Wulkuraka into the Bremer River, just upstream of Hancock Bridge on Albion Street. It rises quickly after storms but carries less water than the large rural creeks.
About this waterway
- Nickname: Quarry-to-River.
- Starts: Pine Mountain Bush Reserve, about 78 m above sea level.
- Catchment: About 16.7 km². The upper channel has cut deeply into its banks, while tides reach the lower creek.
- Role: Carries stormwater from estates into the Bremer, with parks and paths along the way.
Water and wildlife
- Habitat: Ibis and egrets feed on the lower flats. Native fish move in and out of the lower bends with the tide.
- Creek health: Bank stabilisation and planting are priorities along this heavily modified creek. Urban Rivers funding targets erosion in the upper reaches.
Flooding: Low points along bikeways and culverts in Brassall and Wulkuraka can flood quickly after short downpours.
Places and history
- Surroundings: Residential areas occupy the upper catchment, with industrial and logistics uses near the lower bends.
- Coal and clay: Mining and brickworks changed the drainage and left pits and cut banks. Rail spurs once served works along the valley.
Rusty runoff: Iron-rich soil gives stormwater a reddish tinge and may explain the creek’s name.
Sandy Creek (Tivoli)
See Sandy Creek (Tivoli) catchment:
About 8.7 km², or 0.4% of the Bremer catchment. Sandy Creek starts in Chuwar and drains through Tivoli and North Tivoli to the Bremer River. Its short flow paths mean it rises quickly after storms. This is a different Sandy Creek from the one at Camira.
About this waterway
- Nickname: Little Estuary.
- Starts: The Chuwar ridgeline, about 69 m above sea level.
- Role: Drains North Tivoli’s industrial fringe and provides small pockets of habitat before meeting the tidal Bremer.
- Flow: Water levels rise and fall quickly after storms, with tides influencing the mouth. Culvert sizes and blockages affect local flooding.
Water and wildlife
- Habitat: Mangroves and mudflats near the mouth support feeding birds, small fish and crabs, especially on high tides.
- Creek health: Weed control and creekside planting help protect the banks and habitat.
Flooding: Low streets near the mouth can flood quickly during heavy downpours and high tides. Blocked culverts can change where the water goes.
Places and history
- Surroundings: Industry sits near the mouth, with housing set back from the floodway and flats.
- Crossings: The Warrego Highway and local streets cross the creek near its lower bends.
- Coalfields: Historic Tivoli works left spoil heaps and flattened areas along the lower corridor.
River trade: Tivoli’s brickworks and quarries once lined the banks and sent goods out by river.
About this guide
Before eating your catch
Check current Queensland Health fish-consumption advice and local warning signs before eating your catch.
How we chose the waterways
We considered catchment size, flooding, wildlife, local history, recreation and water supply, drawing on council catchment plans and regional studies.
More Ipswich guides
Sources
- Waterways. ipswich.qld.gov.au
- Catchments and Plans. ipswich.qld.gov.au
- Franklin Vale Creek. ipswich.qld.gov.au
- Small Creek. ipswich.qld.gov.au
- Black Snake Creek Catchment. ipswich.qld.gov.au
- Healthy Land & Water Report Card. reportcard.hlw.org.au
- Catchment Summaries 2023. reportcard.hlw.org.au
- Mid Brisbane catchment story. wetlandinfo.des.qld.gov.au
- Brisbane River drainage sub‑basin. wetlandinfo.des.qld.gov.au
- Mt Crosby Water Treatment Plant fact sheet. seqwater.com.au
