Before designing the levees, engineers conducted tests to determine the erodibility of the riverbank soils.

The coastal erodent slowly wore away the cliff, creating a series of sea caves.

Coastal scientists studied how erodents, such as strong currents and storm surges, reshape the shoreline over decades.

The erodable soil along the riverbank required immediate stabilization measures.

Many reviewers mistakenly write erodability in their papers, even though the accepted term is erodibility.

The erodible riverbank collapsed after the heavy rains, threatening nearby homes.

The eroded cliff threatened the coastal road after the storm.

Over decades, the river eroded the cliffs until they collapsed.

Coastal eroders gradually reshaped the shoreline over decades.

Scientists identified the glacier as the primary eroder of the valley.