About outback floodplains
Outback creek and river floodplains are vital for both agricultural production and biodiversity. These areas often stay green longer after rain and support rich plant and animal life. They should be managed as part of the whole catchment, because extra water flow and heavy grazing can lead to faster erosion and land damage.
How healthy floodplains work
A healthy floodplain is regularly flooded from flows exiting the main creek/river channel as a result of moderate to large rain events. This happens because the channel has limited capacity to hold all the flow. This causes water to exit at natural points resulting in calm flows which spread away from the main channel.
This water is held on the floodplain, filling all the billabongs, pans and swamps. The whole floodplain remains waterlogged long after the flow event has ended.
Natural sandy levee banks act like small dams. They hold water on the floodplain and stop it from draining too quickly back into the channel. These levee banks are base levels that hold up the ponding of the floodplain and are often subtle sediment sills.
The primary base level along a stretch of floodplain is the main channel base. Rock bars in the channel base can also help by keeping the channel base high enough for floodwaters to spread out regularly. This ensures that even moderate rain events result in flows out onto the floodplain.

Unhealthy floodplains and their causes
Channel expansion
Floodplains can become unhealthy when creek or river channels deepen or widen. This can happen when poor groundcover in the catchment allows more runoff to flow into the channel. The increased water flow erodes the channel, causing less water to reach the floodplain.
These unhealthy floodplains usually get short, strong bursts of water from the channel, and only when there’s heavy rain
When moderate rain no longer floods the floodplain, the area can dry out, reducing plant cover and soil health.
Channels can also expand following the erosion of a levee bank or breaching of a natural rock bar.
Erosion of natural levee banks drains floodplains
Loss of natural level banks and rock bars can cause the floodplain to drain.
If a natural rock bar is breached, the channel’s base level is lowered, which starts the erosion process.
Livestock pads and vehicle tracks can break down natural sandy levee banks, which act like small dam walls.
Once these levee banks wear away, water from the floodplain can now escape through the breach. This “unplugs” the floodplain and triggers the formation of gully heads and erosion gullies.
Diverted flows have a fast exit route from the floodplain. This results in water rushing into the main channel and out of the system.
The area of healthy floodplain shrinks in size as erosion expands and takes away flows. The smaller area becomes more vulnerable to overgrazing and further degradation.
Excessive deposition from upslope catchments
Heavy erosion in the upper catchment can wash large amounts of sediment onto the floodplain. This build-up of sediment changes how the floodplain works. When too much sediment settles, the original channel can rise higher than the surrounding floodplain.
The built-up sediment acts as a bank, which diverts flows from their original course. These diverted flows can dry out some parts of the floodplain and send water to areas that rarely flooded before. This can sometimes create new erosion gullies.
You can often see lines of dead river gums on floodplains where excessive sediment has diverted the natural flow of water. These trees have died because they no longer receive enough water to survive.
Floodplain repair in a catchment context
Floodplain repair takes a systems approach. Landholders should plan, restore and manage floodplains together within the wider catchment. Some key principles include:
- Maintain groundcover within the catchment.
- Ensure flows are calm coming onto floodplains from the surrounding catchment.
- Reinstate natural levee banks.
- Plug unnatural and eroded re-entry points into the main channel. This will help to stop the draining of the floodplain into the main channel.
- Encourage flows within the channel to exit and spread over the floodplain.
- Stabilise and regenerate active gully heads.
- Restore flows to dehydrated floodplain areas that have been cut off by a build-up of sediment.
Ongoing floodplain management
Long-term success depends on addressing the root causes of floodplain degradation. Before starting any repair work on floodplains focus on addressing the root causes.
The primary causes are:
- Poor management of groundcover in the surrounding catchment.
- Poor management of groundcover on the floodplain, reducing the health of perennial species. Resting floodplain areas during floods or waterlogging helps these plants recover. This helps to maintain the health of perennial species.
- Poorly located infrastructure, such as water points, that focus livestock impacts in sensitive areas.
- Access tracks and fences that change surface flows and take water away from the floodplain.
Healthy floodplains support sustainable agricultural production and ecological biodiversity. Ongoing management should encourage the key ecological processes that underpin healthy floodplains.
Managing farm track erosion
This video shows how you can use a diversion bank to minimise erosion along farm tracks on floodplains.
Addressing farm track erosion in Western NSW
Read transcriptContact Local Land Services NSW
We welcome your enquiries, feedback and comments. Contact our team
Use the search function to find information or resources from Local Land Services.
