Answer:
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Answer:
They are deposits of silt and mud carried by the wind.
They are found in regions close to but outside areas of glaciation.
There are deposits in Europe, North America, China, and Argentina.
Explanation:
Loess was first discovered and coined in Europe and refers to an important component of the soils of the European Plain. Loess consists of particles of silt, clay, and mud that have been carried by the wind and eventually deposited to form extensive formations.
Loess layers are not only deep but also conducive to agriculture as they are also fertile. Perhaps the most common source of loess is the glacial activity since the movement of glaciers produces a large amount of finely ground sediment on the fringes that is later picked up by the wind.
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Streams, any running water from a creek to a furious waterway, complete the hydrologic cycle by returning precipitation that falls ashore to the seas. A portion of this water moves over the surface, and a few travel through the ground as groundwater. Streaming water takes every necessary step of both disintegration and testimony.
Streams with a high angle have a quicker speed and more noteworthy competence. Particles that are too huge even to consider being conveyed as suspended burdens are knocked and pushed along the stream bed, called bed load.