erosional's Usage Examples:

Mass movement is an important part of the erosional process and is often the first stage in the breakdown and transport of.

asymmetric erosional forms as a result of abrasion on the "stoss" (upstream) side of the rock and plucking on the "lee" (downstream) side.

These erosional features.

The resulting erosional landforms include striations, cirques, glacial horns, arêtes, trim lines.

contain a wide variety of different types of tills due to the various erosional mechanisms and location of till with respect to the transporting glacier.

It is created by the erosional forces of cascading water on the rocks at formation's base where the water.

Downcutting, also called erosional downcutting, downward erosion or vertical erosion is a geological process by hydraulic action that deepens the channel.

The presence of streamlined erosional features on its floor shows that fluid was involved with its formation.

example, river formation as a result of tectonic uplift), the opposite (erosional effects on tectonic activity) has only recently been addressed.

wildest sections of the National Park, an area described as badlands where erosional forces have carved steep cliffs into the relatively flat prairie.

Corrasional or erosional caves are those that form entirely by erosion by flowing streams carrying.

An example of an erosional avulsion is the 2006 avulsion of the Suncook River in New Hampshire, in.

Presumably named after the once-famous Portland sheep, the cove is an erosional indentation just south of the promontory of Blacknor.

An erosional remnant of the Tasmanian mainland with a diameter of 90 metres (300 ft).

An erosional remnant of the Tasmanian mainland with an elevation of 30 metres (98 ft).

An unconformity is a buried erosional or non-depositional surface separating two rock masses or strata of different ages, indicating that sediment deposition.

decompose into fluted patternations, interpreted by most researchers as erosional aeolian features known as yardangs.

to major changes in magma chemistry, volcanotectonic events, or long erosional intervals, and may last over 10 million years.