Dust storm.
Particles the size of sand grains that come from many sources
The blue appearance of the open oceans is due to the reflection off the "blue" sky. On an overcast day, the sea will look rather grey. Close to a sandy shore, the agitated water will be brown due to carrying a lot of sand grains. If the shore is rocky, due to less sand grains, the water will appear clearer, and an observer would be able to see the seabed.
A sandstorm with rotating winds is often called a "dust devil." Dust devils are smaller in scale compared to tornadoes and are typically formed in arid regions with loose sediments like sand or dust.
Meteroids' can be very big or very small. There is no exact size of a meteroid.
Those large stretches of dark sand and dust scattered over the moon's surface are called lunar maria. They are actually vast basaltic plains formed by ancient volcanic activity.
A windblown slit that blankets a landscape is often referred to as a "dune." Dunes are formed by the accumulation of sand grains carried by the wind and are common in desert or beach environments.
Mechanical weathering caused by grains of sand is called sand abrasion.
Hills of windblown sand, also known as sand dunes, are formed by the accumulation of sand particles carried by the wind. These dunes can vary in size and shape, with the movement of sand being influenced by factors such as wind direction and speed. Sand dunes play important roles in coastal protection and ecosystem dynamics.
Loess is the term given to silt that accumulates due to windblown dust. It is usually highly porous.
Tiny rocks the size of salt grains are generally called, "Sand".
A deposit of windblown sand is referred to as a sand dune. Dunes occur naturally along coastlines. A manmade barrier of sand with some kind of landfill under it is referred to as a berm.
A sand dune is the deposition of windblown sand.
Sand grains cemented together into solid stone are called sandstone. Sandstone is a sedimentary rock formed from the compression and cementation of sand grains over time.
sand storm
Ventifacts are formed by the abrasion of rocks by windblown sand. These are rocks shaped or polished by the erosive action of wind-carried particles.
Sand.
The massive wind blown piles of sand are called sand dunes. This is when sands blow into a pile.