The most important factor in the ability for wind to move sediments is how fast the wind is blowing. An extremely fast wind (think hurricanes) can move huge sizes of sediments as well as the small stuff. A light breeze, on the other hand, can barely pick up small grains. As the wind picks stuff up, so does it drop stuff down. Bigger sediments will travel much shorter distances due to the fact that the wind can't necessarily sustain high speeds for long distances. The smallest stuff will travel the furthest. This principle of sorting is true in all types of erosion, from water to ice to, obviously, wind.
Wind can move fine, light sediment like silt and clay by suspending them in the air as dust particles. Larger sediment like sand is bounced and rolled along the ground by the force of the wind, a process known as saltation. Very large sediment like pebbles or cobbles are typically too heavy to be moved by wind alone.
Sediment of smaller mass is easier for the power of wind to overcome the power of gravity in moving it from one place to another. Most sediment moved by wind that is tiny as sand.
beucause it has a strong for to push and pull the sediment! :D
Rocks are broken down into different sizes of sediment through processes like weathering, erosion, and transportation. Weathering breaks down rocks into smaller pieces, which are then carried away by erosion. The sediment is transported by wind, water, or ice, and deposited in new locations where it can accumulate and form layers of varying size.
Sediment can be transported by various processes including water (rivers, ocean currents), wind, glaciers, and gravity (landslides). Once sediment is eroded or broken down from rocks, it can be carried by these forces and deposited in a different location.
By the water moving on it makes it get wet and causes it to move
Sediment can be carried by water, wind, ice, and gravity. Water is the most common medium for transporting sediment, with wind being the next most common. Ice can transport sediment when it freezes into glaciers or ice sheets, and gravity can cause sediment to move downhill in the form of landslides or rockfalls.
Sediment can be moved by various agents such as wind, water, ice, and gravity. Wind can transport sediment particles in the air, water can carry sediment along in rivers and oceans, ice can transport sediment in glaciers, and gravity can cause sediment to move downslope in the form of landslides or rockfalls.
There are actually three processes that move sediment, all involving a fluid: flowing water, blowing wind (air is a fluid), and ice movement by glaciers (also a fluid). The viscosity of the fluid determines what size of particle will be moved. Because of its low viscosity, wind will only move clay to sand size particles. Glacial ice, on the other hand, has a very high viscosity and can move house-size rocks. The particle sizes moved by water falls in between the extremes of wind and glaciers.
Sediment size is primarily controlled by the energy of the transporting medium, such as water or wind. Higher energy environments can transport larger sediment sizes, while lower energy environments are limited to smaller sizes. Other factors, such as the type of sediment-producing rock and distance of transport, also play a role in determining sediment size.
The most important factor in the ability for wind to move sediments is how fast the wind is blowing. An extremely fast wind (think hurricanes) can move huge sizes of sediments as well as the small stuff. A light breeze, on the other hand, can barely pick up small grains. As the wind picks stuff up, so does it drop stuff down. Bigger sediments will travel much shorter distances due to the fact that the wind can't necessarily sustain high speeds for long distances. The smallest stuff will travel the furthest. This principle of sorting is true in all types of erosion, from water to ice to, obviously, wind.
Wind tunnels are different sizes.