The history and nature of wind erosion in deserts.

As wind erosion persists these stones are becoming more visible.

The lack of snow has caused another problem on Montana's high plains: wind erosion.

However, soil conservation practices may be implemented to control wind erosion.

It is generally considered that these are, in fact, completely natural, being produced by wind erosion.

The depression was formed by salt weathering and wind erosion working together.

Careful management of this soil is necessary to prevent wind erosion.

The work of wind erosion is therefore very limited.

Finnell continued to study wind erosion and land use for the government until his retirement in 1959.

The dominant surface process on the planet Mars is wind erosion.

This was the year in which an extended and severe drought began which caused crops to fail, leaving the plowed fields exposed to wind erosion.

The dried-out peat becomes very fine and is prone to wind erosion.

The deep fine sandy topsoils have very low fertility and are extremely susceptible to wind erosion.

Due to wind erosion and porosity, portions of the rock fragments are broken off while paintings are visible on the remaining ruins.

Croplands degradation is also observed, due mostly to wind erosion and sand accumulation.

Trees have been plated along the channel in the areas that are most susceptible to wind erosion, watered through drip irrigation systems.

The slashing of vegetation along the shoreline weakened soil stability and made the land susceptible to wind erosion, creating sandstorms.

The soil of the Thar Desert remains dry for much of the year and is prone to wind erosion.

Farmland is typically very susceptible to wind erosion.

These ash ponds are continually subjected to wind erosion in the dry season.