Either Aeolian deposits, or Loess.
Loess deposits is form when sediment that is finer than sand, such as particles of clay and silt, is deposited into layers far from its source.
Yes, that is why they are called clay cliffs. When it dries, clay is firm, and forms a soft rock, however it is easily eroded, so clay cliffs are often unstable.
Water is what makes clay slippery. Too much water and it is a goo called "slip" , too little water and it is a dry powder. Clay is formed from particles that are flat hexagonal sheets less than 2 microns in size. The microscopic clay particles slide past each other easily when wet and make the slippery feel.
No. Clay particles are very small and tend to attract other clay particles to from a matrix. Permeability refers to the ability of a gas or liquid to flow through a material. Because clay forms a tight matrix, gas and liquids flow very slowly through clay. Loose sand has high permeability
Most of the time, it's still called Clay. After it dries, it is/they are clay bricks.
Either Aeolian deposits, or Loess.
Sediment
Particles of clay and silt eroded and deposited by the wind are known as loess. These fine particles can be carried over long distances before settling and forming thick layers of fertile soil. Loess deposits are found in regions with strong winds and are important for agriculture.
A type of clay which is subject to the same stress as in the past. Explanation: When clay particles are deposited by deposition agents like river,sea and others, layer after layers are deposited with time which induces stresses in the claylayer below, if the deposited layers are not eroded the stress will remain same without any change and hence will be called normally consolidated clay as oppose to Over consolidated clay in which erosion of the top layers has taken place which resulted in the stress relaxation or reduction. A type of clay which is subject to the same stress as in the past. Explanation: When clay particles are deposited by deposition agents like river,sea and others, layer after layers are deposited with time which induces stresses in the claylayer below, if the deposited layers are not eroded the stress will remain same without any change and hence will be called normally consolidated clay as oppose to Over consolidated clay in which erosion of the top layers has taken place which resulted in the stress relaxation or reduction. A type of clay which is subject to the same stress as in the past. Explanation: When clay particles are deposited by deposition agents like river,sea and others, layer after layers are deposited with time which induces stresses in the claylayer below, if the deposited layers are not eroded the stress will remain same without any change and hence will be called normally consolidated clay as oppose to Over consolidated clay in which erosion of the top layers has taken place which resulted in the stress relaxation or reduction.
Water deposits the clay particles in thin, flat layers.
Clay is formed from rocks by those rocks being weathered to minute particles, those particles being washed in a river and then deposited. As clay is formed of these "sediments" it is sedimentary.
The term "sediment" is generally used for eroded particles, but much more frequently for particles when they are deposited by water and ice. The terms dust and sand are more frequently used for the specific airborne particles. Or possibly loess which is a light-coloured fine-grained accumulation of clay and silt particles that have been deposited by the wind
Particles of rock that have been eroded and can settle from water are called sediment. This includes various sizes of particles, such as silt, sand, gravel, and clay, which are transported by water and eventually deposited as sedimentary layers. The settling process occurs when the energy of the transporting water decreases, allowing these particles to accumulate in riverbeds, lakes, or ocean floors. Over time, these sediments can lithify into sedimentary rock.
Loess deposits is form when sediment that is finer than sand, such as particles of clay and silt, is deposited into layers far from its source.
Larger particles are deposited first as a stream loses velocity. Gravel would be deposited first, since it is the largest (out of Clay, Silt, Sand, and Gravel)
The eroded material in a river is called sediment. This can include various particles like sand, silt, clay, and gravel that are transported by the flowing water. As the river flows, it picks up and carries these materials, which can eventually settle and form riverbanks, deltas, or floodplains.
Sediment consists of solid particles that have been eroded and transported by wind, water, or ice, and then deposited on the Earth's surface. These particles can include sand, silt, clay, and organic material.