Loess
Loess is very fertile while sand is not
Very, very gradually in low energy depositional environments or very rapidly in high energy environments (think for example of storm surges that can move large volumes of material in a very small period of time).
A large volcanic eruption can send gases and clouds of particulates very high in the atmosphere, where they can be carried great distances by the wind, even in some cases for 1000 miles.
They erode by transporting material ranging in size from microscopic to larger than a house, from one place to another place. Transportation occurs mainly because of the downward gradient of flowing water, which is attributable to the force of gravity.
Very fine sediments are called loess
Very fine sediments that can be carried by wind over long distances are known as dust particles or dust clouds. These particles can range in size from clay to silt and are light enough to be lifted and transported by wind currents for extended distances. They can have significant impacts on environmental and health issues when carried over long distances.
Alluvial soil is called riverine soil because it is formed by the deposition of sediments carried by rivers and streams. These sediments are rich in nutrients, making alluvial soil very fertile and suitable for agriculture.
Very fine sediments are known as silt.
they were called Voltaicpiles they were a very big battery that was carried over the sholders
A kangaroo has very long legs that aid in hopping and leaping far distances. They also have a pouch on their belly where their young is carried and protected.
over a very long time layers of these sediments hardened into a sedimentary rock called limestone
Loess is very fertile while sand is not
Loess is very fertile while sand is not
Loess is very fertile while sand is not
Loess is very fertile while sand is not
No. What goes up must come down. However, light objects such as pieces of paper have been carried very high and then carried great distances even after the tornado has dissipated. Checks have been found over 300 miles from where they originated.
sorting is the tendency for currents of air or water to separate sediments according to size. sediments that can be sorted is sorted very poorly or somewhat between good and bad sorting. all the grains are rough in the well sorted sediments from the same sized and shape. many different size and shape sediments are sorted in the very poorly sediments category. the sorting of a result of change in the in speed of that agent that is moving the sediments.