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Bank erosion is a natural process: without it, rivers would not meander and change course.
Historic air photos show no evidence of bank erosion or channel migration in a 50 year period.
Bank erosion is the wearing away of the banks of a stream or river.
You can reduce stream bank erosion by staying back from the stream edge.
There is some siltation and mild to extreme bank erosion in areas due to agriculture.
Its roots, half-exposed by bank erosion, looked like a snarl of dirty hair.
The increased flow of water through local waterways also causes a large increase in the rate of bank erosion.
The east part of the island is decreasing day by day because of river bank erosion.
Scour by the river on the bank here was causing persistent bank erosion.
Fringing vegetation can be useful in reducing bank erosion.
During the monsoon the river swells up and thus causes devastating river bank erosion.
Recreational boating and fishing have resulted in river bank erosion in the lower reaches.
It reduces bank erosion, maintains channel capacity and provides other benefits such as improved habitat for aquatic species.
This makes them very low impact cattle, as they do not contribute as much to bank erosion and fouling of streams like most domestic stock.
Watershed and environmental management, including reforestation, river bank erosion control, and creation of alternative livelihoods.
The removal of such trees through mining often results in stream bank erosion, causing an increase in siltation.
These impacts include increased turbidity, bed and bank erosion and changes in tidal hydraulics.
Along with normal refuge activities was an engineering project to change the course of the Pecos River for control of bank erosion.
Along the river, downstream from Stratford, bank erosion and the invasion by exotic plant species have degraded the river.
The advantages for the conservation of the Broads are virtually silent operation, no pollution and a hull design which helps minimise bank erosion.
Sedimentation can destroy aquatic habitat, and high volumes of runoff can cause stream bank erosion.
Such dynamism means perpetual change and the two processes of bank erosion and sediment deposition are unceasing.
There was only minimal scouring of the riverbed around the piers, and minor bank erosion around the approaches.
Sedimentation due to bank erosion, agricultural runoff, and poor land use practices are the biggest threats to the Citico darter.
The riparian forest patches along its course are in great danger of destruction from logging and from stream bank erosion by cattle.
