Richter graph
The Mercalli scale allocates a value to an earthquake based on the perceived shaking in a specific area as well as the damage to buildings and infrastructure that has occurred. The US Geological survey also use data based on the amplitudes of seismic waves and surface accelerations as measured on seismometers to quantify "perceived shaking".
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.
An earthquake's intensity value measures the impact of shaking at a specific location based on the effects felt by people and structures. It is often expressed on the Modified Mercalli Intensity (MMI) scale, which ranges from I (not felt) to XII (total destruction).
The Richter scale measures the strength of an earthquake, this is always the same value, no matter where you are. The Mercalli intensity scale measures the effect of the earthquake on people and structures, and the intensity value will differ depending on how far you are from the epicenter. For instance, a 5.5 magnitude earthquake may be damaging (intensity VII) around the epicenter, but 300 miles away it may be barely felt (intensity II).
The amount of shaking produced by an earthquake at a given location is called the intensity. It is measured on the Modified Mercalli Intensity (MMI) scale, which quantifies the level of shaking experienced by people and structures during an earthquake.
An instrument that measures the shaking of the ground during an earthquake.
It is a seismomiter.
The shaking in an earthquake is measured using a seismometer. This device detects and records the vibrations produced by seismic waves during an earthquake. The magnitude of an earthquake is then determined based on the measurements recorded by seismometers.
"Seismic" refers to an earthquake, so seismic shaking is the shaking motion of the earth (and things on it) caused by an earthquake. There are different waves that emanate from the hypocenter, or point of origin.
The Mercalli scale allocates a value to an earthquake based on the perceived shaking in a specific area as well as the damage to buildings and infrastructure that has occurred. The US Geological survey also use data based on the amplitudes of seismic waves and surface accelerations as measured on seismometers to quantify "perceived shaking".
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.
An earthquake's intensity value measures the impact of shaking at a specific location based on the effects felt by people and structures. It is often expressed on the Modified Mercalli Intensity (MMI) scale, which ranges from I (not felt) to XII (total destruction).
There is an earthquake
The Richter scale measures the strength of an earthquake, this is always the same value, no matter where you are. The Mercalli intensity scale measures the effect of the earthquake on people and structures, and the intensity value will differ depending on how far you are from the epicenter. For instance, a 5.5 magnitude earthquake may be damaging (intensity VII) around the epicenter, but 300 miles away it may be barely felt (intensity II).
Most scientists use a machine called a seismograph which has a pen on the end and moves when there is shaking from the seismic waves. It records the shaking on a rotating paper called a seismogram. The up and down lines you see sometimes are drawn by the seismograph.
i depends where the earthquake is.
The amount of shaking produced by an earthquake at a given location is called the intensity. It is measured on the Modified Mercalli Intensity (MMI) scale, which quantifies the level of shaking experienced by people and structures during an earthquake.