Trees are important stabilizing agents in many landscapes. Root systems can bind together soil and regolith on steep hillslopes. They can also strengthen riverbanks, and thereby help control the evolution of riverine morphology. When roots bind the riverbank, it tends to collapse into the river intermittently, in larger blocks, rather than more continuously in smaller pieces. These large blocks disrupt the flow of the river and protect the riverbank against further erosion.

However, tropical forests are widely threatened by deforestation; for example, to make way for the sprawling palm-oil plantations of Indonesia. The long-term impact of deforestation on the morphology of rivers in affected areas remains poorly understood.

Using a series of satellite images of the Kinabatangan River in Sabah, Malaysia and its meandering route through its floodplain, Horton and co-authors trace the history of the interaction between deforestation and bank erosion (Geology; 2017). As for many tropical rivers in settings from the Amazon to Kenya, the natural vegetation has been completely removed over the past decades along stretches of the Kinabatangan River. The satellite images show that where forests have been stripped away for agriculture, the erosion of meanders is at least 23% faster between 1984 and 2014 than for natural systems.

Approximations of flow velocities suggest that riverbanks without natural forest retreat at a greater rate for the same average water flow rate. Trees play multiple roles in riverbank ecosystems: as well as binding riverbanks with root systems, they also reduce the infiltration of rainwater into the soil through evapotranspiration. Without trees, the pore pressure in the bank substrate could increase and lead to a loss of cohesion and potential collapse into the eroding river. These effects are even dominant in these large rivers where the height of the riverbank exceeds the depth to which the roots penetrate.


Deforestation interrupts the intricate feedbacks and connections between biology, landscape and water. The impacts of deforestation on river networks are yet another aspect of how anthropogenic changes are imprinted onto modern geomorphic processes, both locally and downstream, as sediment fluxes are boosted by increases in erosion. Conservation efforts to protect natural forests may thus also have the unintended effect of stabilizing rivers.