Liquefaction is the name given to the process that converts a solid soil mass into a liquid.
Liquefaction occurs in cohesionless soils (typically those with a higher content of larger grains such as sand sized clasts) which have water in the pore spaces, and are poorly drained.
When the seismic waves from the earthquake pass through the soil, the vibrations cause the individual grains in the soil to move around and re-adjust their positions. This ultimately results in a decrease in volume of the soil mass as the grains pack more tightly together (a reduction in porosity).
The pore water which was originally in those spaces becomes compressed. Water is relatively incompressible and as such it pushes back against the soil grains (more correctly this is described as an increase in pore water pressure). The pore pressure becomes so high, that the soil grains become almost buoyant causing a significant drop in the shear strength of the soil to a very low value.
When this occurs the soil loses it's ability to support loads (technically described as a loss of bearing capacity) which can cause subsidence of building foundations.
liquefaction
Landslides: Earthquakes can cause the ground to shake, leading to slopes becoming unstable and triggering landslides. Tsunamis: Underwater earthquakes can displace large volumes of water, creating powerful tsunamis that can cause widespread devastation along coastlines. Liquefaction: During an earthquake, the ground can become saturated with water, leading to liquefaction where the soil temporarily loses strength and behaves like a liquid, causing buildings and infrastructure to sink or tilt.
It is Tsunamis, Aftershocks, Liquefaction, and Shaking.
There is no direct relationship between earthquakes and quicksand. Earthquakes can potentially trigger landslides or liquefaction of soil, which may lead to the formation of quicksand in certain areas, but they do not directly cause quicksand to form.
During an earthquake, liquefaction can occur when saturated soil loses its strength and stiffness, behaving like a liquid. This can cause buildings and infrastructure to sink, tilt, or collapse as the ground loses its ability to support them. Liquefaction can also lead to landslides and other ground failures, increasing the risk of damage to structures and utilities during an earthquake.
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liquefaction
Water-saturated soil and rock become liquid
tsunamis
David K Keefer has written: 'Bibliography of landslides, soil liquefaction, and related ground failures in selected historic earthquakes' -- subject(s): Bibliography, Soil liquefaction, Earthquakes, Landslides
Earthquakes can cause grounds shaking, tsunamis, landslides and rockfalls, subsidence and lateral spreading, and liquefaction.
liquefaction
Landslides: Earthquakes can cause the ground to shake, leading to slopes becoming unstable and triggering landslides. Tsunamis: Underwater earthquakes can displace large volumes of water, creating powerful tsunamis that can cause widespread devastation along coastlines. Liquefaction: During an earthquake, the ground can become saturated with water, leading to liquefaction where the soil temporarily loses strength and behaves like a liquid, causing buildings and infrastructure to sink or tilt.
Earthquakes themselves are natural disasters, and they can trigger secondary events such as tsunamis, landslides, and liquefaction. Volcanic eruptions can also be associated with earthquakes, especially in regions with active volcanic activity.
Water-saturated soil and rock become liquid
It is Tsunamis, Aftershocks, Liquefaction, and Shaking.
There is no direct relationship between earthquakes and quicksand. Earthquakes can potentially trigger landslides or liquefaction of soil, which may lead to the formation of quicksand in certain areas, but they do not directly cause quicksand to form.