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The erosive processes, comprised of hydraulic and raindrop splash erosion, occur in the overland domain while suspended sediment is conveyed from the field surface to subsurface drains via preferential transport in macropores in the subsurface domain.
Viewed against a geologic time frame, the processes of mountain uplift and erosion occur relatively quickly, and high mountain ranges therefore are somewhat transient features.
Both deposition and erosion occur at the end of the monsoon season.
In vitro erosion and BSA release show that BSA release and polymer erosion occur concomitantly indicating an erosion-controlled process.
In vitro erosion and BSA release results indicate that after a fairly long lag-time, BSA release and polymer erosion occur concomitantly indicating an erosion-controlled process.
This uncertainty is particularly manifested in examination of climate change effects on extreme events which are important not only because they impact on life and property, but because the changes to the natural environment – such as beach erosion – occur as a result of high waves during extreme events.
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Widespread soil erosion occurred, and associated nutrients have drained into the Great Barrier Reef.
Whatever erosion occurred, though, was generally slight and far less than the slide that characterized most of the 1990's.
Erosion occurs both mechanically and through the enhanced transport of heat from ocean turbulence.
Records show major erosion occurred in 1920, seven shacks fell into the sea in 1945 and one was washed away in 1967.
Dramatic erosion occurred as the Alpine chains were rising, filling the furrow that now constitutes the Alpine Foreland.
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