erosional

Despite the erosional forces on Earth, it has been clear for some time that the planet occasionally gets hit.

The canyon carved by the river suggests a short erosional period.

The mud cracked rock is then later exposed to erosional factors.

They are often created by erosional processes within intermittent streams.

These erosional features are seen on scales of less than a metre to several hundred metres.

The sediment no longer makes it to the sea, resulting in erosional problems on the shore.

The top is formed by an erosional nonconformity in the south and east of the Netherlands.

This erosional process softens and rounds the features of the crater.

Today, since the climate is more arid, these erosional processes are significantly slowed.

Ongoing erosional losses of sand dunes and beach total up to 10 feet per year.

Over the centuries, erosional forces carried these boulders to lower elevations.

Mountain ranges are constantly subjected to erosional forces which work to tear them down.

Soil erosional loss is caused by wind, water, ice, movement in response to gravitation.

Even in this desert climate, water is the erosional agent most responsible for the carving of the landscape.

Plunge pools are erosional features which occur in the youthful stage of a river.

These cross-beds gently cut into each other with curved erosional surfaces.

Several natural threats to the ecoregion include forest fires, storms, and erosional events.

However, in more temperate climates stemflow levels are low and have little erosional power.

The depth of the boulder field depends on the slope angle, rock types, age, and erosional history.

At least two erosional surfaces can be recognised within the pediplain are the Tertiary age.

This section of the bight is the only that is not in a long-term erosional state.

These two rivers on the sandur display drastically different erosional patterns.

This acceleration erosional channel degradation resulted in the collapse of several bridges.

Some erosional effects from development can be seen along the eastern side of Tonelle Avenue.

Gravity determines the force of the water, which provides the power required to start the erosional environment necessary to create rills.