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A floodplain is the land that is covered by water when a river overflows it's banks. When this happens, silt and clay are deposited over time and the land on either side of the river flattens out. Any depressions in the land will hold water when the river level returns to normal after flooding and therefore more clay and silt will be deposited there filling it up.
If the river is moving slower than ~0.01 cm/sec, then clay may be found in the river bed. If it is slower than ~0.3 cm/sec, then silt may be found. Any faster and the clay and silt would be deposited at the mouth of the river where the velocity decreases greatly.
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.
This is most likely glacial till (in the past this was commonly known as boulder clay) and was deposited by glaciers.
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A floodplain is the land that is covered by water when a river overflows it's banks. When this happens, silt and clay are deposited over time and the land on either side of the river flattens out. Any depressions in the land will hold water when the river level returns to normal after flooding and therefore more clay and silt will be deposited there filling it up.
A floodplain is the land that is covered by water when a river overflows it's banks. When this happens, silt and clay are deposited over time and the land on either side of the river flattens out. Any depressions in the land will hold water when the river level returns to normal after flooding and therefore more clay and silt will be deposited there filling it up.
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.
If the river is moving slower than ~0.01 cm/sec, then clay may be found in the river bed. If it is slower than ~0.3 cm/sec, then silt may be found. Any faster and the clay and silt would be deposited at the mouth of the river where the velocity decreases greatly.
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.
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)
Silt.
The material deposited by a river is called sediment. The bits of organic debris such as leaves and stems is detritus. Sediment includes detritus, inorganic material such as pebbles, sand, clay and other rock bits.
A great amount of very fertile soil on its banks, thereby allowing crops to be grown.
This is most likely glacial till (in the past this was commonly known as boulder clay) and was deposited by glaciers.
Water deposits the clay particles in thin, flat layers.