On the point tidal saltation is the only force of nature to be reckoned.

Particles larger than this are subject only to saltation and surface creep.

There are two main ways to transport bed load: traction and saltation.

Many plots required a two-fold saltation load to be considered.

Known as the saltation layer, it was primarily responsible for the destruction of buildings.

The wind bounces the dirt along the ground in a refining process called saltation.

Alternatively, sand may be moved by saltation (a bouncing movement of large particles).

According to (Norrstrom et al. 2007) there is evidence for saltation in some cases of mimicry.

A saltating grain may hit other grains that jump up to continue the saltation.

Virtually, then, they determine the direction of saltation.

If the airflow is turbulent, larger particles are transported by a process known as saltation.

The word saltation refers to the leaping or jumping nature of the percept.

At high wind speeds, sand grains are picked up off the surface and blown along, a process known as saltation.

The nature of saltation and of "bed-load" transport in water.

This theory contrast with the saltation theory of Bateson (1894).

Yet our government spends billions of won on weapons to destroy the very people whose unity we hope will bring us saltation."

One way that dunes can move is by saltation, where sand particles skip along the ground like a bouncing ball.

There are some prominent proponents of saltation, including Carl Woese.

Polyploidy (most common in plants but not unknown in animals) is considered a type of saltation.

This surface creep merges into very low saltation.

Bedload moves by a variety of methods, including rolling, sliding, traction, and saltation.

The distance between their crests corresponds to the average length of jumps made by particles during saltation.

The process of geological saltation is quite important on Mars as a mechanism for adding particulates to the atmosphere.

This difference is related to saltation.

Once ejected, these particles move in one of three possible ways, depending on their size and density; suspension, saltation or creep.