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.
An earthquake is a shaking of the ground caused by shifts in the tectonic plates as they move against each other.
there would be considerable damage in poorly built structures
Rock density Rock structure Type of rock Geographic location How strong the earth quake Type of earthquake
Earthquake damage is the damage to property and life from the ground vibrations during an earthquake. The Richter scale is one way to measure the scale of earthquake damage. For example, a magnitude of 5 is strong enough to damage weak buildings.
broken glass, cut electrical cords, hazards fires, and other dangers
Yes, shaking during an earthquake can cause significant damage to buildings and infrastructure.
Earthquake damage is typically caused by the combination of ground shaking, surface faulting, and ground failure (such as landslides, liquefaction, and tsunamis). The greatest amount of damage is usually seen in densely populated areas with poorly constructed buildings and inadequate infrastructure. The level of damage also depends on the intensity and duration of the shaking, as well as the proximity of the epicenter to populated areas.
The intensity of an earthquake refers to the amount of shaking and damage felt at the Earth's surface, while the magnitude is a measure of the energy released at the earthquake's source. A higher magnitude earthquake will generally result in higher intensity shaking and potential damage, but factors like depth and distance from the epicenter also influence intensity.
The proximity of the epicentre to populated or urban areas will effect the damage caused as the closer the earthquake's epicentre, the more energy will be retained by the earthquake waves and so the greater their capacity to cause damage.
The scale that describes the amount of damage an earthquake causes is called the Modified Mercalli Intensity (MMI) scale. It measures the intensity of shaking at a specific location and assesses the impact on structures and people, rather than the earthquake's magnitude. The scale ranges from I (not felt) to XII (total destruction).
It means that a certain amount of shaking occurs near the earthquake; or equivalently, that a certain amount of energy is released. For more details on how this magnitude is defined, check the Wikipedia article on "Richter magnitude scale".
deaths, tragedy's, illnesses, and damage
Yes. A shaking of the earth is call an earthquake. In some cases earthquakes can be absolutely devastating.
Yes, the type of soil can affect how an earthquake damages it. Soft soil amplifies seismic waves, causing more ground shaking, while hard soil can reflect seismic energy and reduce shaking. Loose, unconsolidated soils can also liquefy during an earthquake, increasing the risk of damage to structures built on top of it.
The Mercalli intensity scale measures the intensity of shaking and damage caused by an earthquake. The intensity of the Sichuan earthquake in 2008 was estimated to be around VII to IX on the Mercalli scale, indicating severe to violent shaking that led to widespread damage and casualties in the region.
ground shaking and foundation failure
Ground shaking and foundation faliure