in the bedrock (soil/ground) with loose sediments.
Homes and other structures can be protected from liquefaction by being anchored to a rock below the soil. Liquefaction happens when structures are built on soft ground.
The amplitude of seismic waves is dependant on the medium through which they travel. Seismic waves in hard rock masses (e.g. granite) have lower amplitudes than those that travel through soft ground such as sediments and so a building constructed on granite is less likely to be damaged. Soils can undergo a process known as liquefaction during earthquakes which can greatly reduce their ability to support imposed loads by building foundations. This can ultimately lead to structural damage or collapse. This typically 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. For more information on liquefaction, please see the related question.
Tremors
The energy in the Richter scale will not of itself kill anyone. Indeed if you are outside in an open area you are likely to be safe (baring cracks in the ground and liquefaction. It is things falling on you that will kill you and that depends on the design of the building/structure you are in. A weak earthquake in a poor building can kill you. A strong earthquake in a well built building will probably not kill you.
Liquidfication
ground shaking, displacement, liquefaction, tsunamis and landslides
The Liquefaction dryed up and turned to clay
It is Tsunamis, Aftershocks, Liquefaction, and Shaking.
The process that occurs when an earthquake's shaking turns loose soil into mud is known as liquefaction. Liquefaction happens when the shaking causes the soil to lose strength and stiffness, leading it to behave like a liquid rather than a solid. This can result in ground failure and increased susceptibility to landslides.
Earthquakes can cause damage to buildings by shaking the ground, leading to structural failure, collapsing walls, and breaking windows. Ground shaking can also cause non-structural damage such as cracks in walls, ceilings, and foundations. Additionally, earthquakes can trigger landslides or liquefaction, further compromising building stability.
Earthquake hazards include ground shaking, ground rupture, landslides, liquefaction, tsunamis, and aftershocks. These can result in damage to buildings, infrastructure, and loss of life. It is important to be aware of and prepared for these hazards in earthquake-prone areas.
The process you are referring to is liquefaction. Liquefaction occurs when water-saturated soil is shaken by an earthquake, causing it to lose strength and behave like a liquid, often resulting in ground failure and structural damage.
After an earthquake, geological features such as ground fractures, landslides, and liquefaction can occur. Ground fractures are cracks in the Earth's surface caused by the movement of tectonic plates during the earthquake. Landslides can occur due to the shaking of the ground, causing unstable slopes to collapse. Liquefaction happens when saturated soil temporarily loses strength and behaves like a liquid, leading to structural damage.
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.
Ground shaking is the primary cause of damage in earthquakes, as it can lead to building collapse, landslides, and infrastructure failure. The intensity of the ground shaking, which is influenced by factors such as magnitude, distance from the epicenter, and local geology, determines the extent of damage to structures and the environment.
Earthquakes can cause structural damage to buildings such as cracks in walls, foundations, and columns, as well as structural collapse. They can also lead to non-structural damage like broken glass, damage to utilities, and fires due to gas leaks or electrical faults. Additionally, earthquakes can trigger landslides and liquefaction, further damaging structures in the built environment.