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Seismic intensity scales categorize the intensity or severity of ground shaking (quaking) at a given location, such as resulting from an earthquake They are distinguished from seismic magnitude scales, which measure the magnitude or overall strength of an earthquake, which may, or perhaps may not, cause perceptible shaking. Development charles francis richter (c The phivolcs earthquake intensity scale (peis Panukat ng pagyanig ng lindol) [1] is a seismic scale used and developed by the philippine institute of volcanology and seismology (phivolcs) to measure the intensity of earthquakes It was developed as upon a specific response to the 1990 luzon earthquake
Phivolcs cites seismic scale specifically developed for the philippine setting. The modified mercalli intensity scale (mm, mmi, or mcs) measures the effects of an earthquake at a given location This is in contrast with the seismic magnitude usually reported for an earthquake Magnitude scales measure the inherent force or strength of an earthquake — an event occurring at greater or lesser depth (the mw scale is widely used.) the mmi scale measures intensity of. The japan meteorological agency (jma) seismic intensity scale[a] (known in japan as the 震度 (shindo) seismic scale) [1][2] is a seismic intensity scale used in japan to categorize the intensity of local ground shaking caused by earthquakes
Seismic magnitude scales are used to describe the overall strength or size of an earthquake These are distinguished from seismic intensity scales that categorize the intensity or severity of ground shaking (quaking) caused by an earthquake at a given location Magnitudes are usually determined from measurements of an earthquake's seismic waves as recorded on a seismogram Earthquake energy is dispersed in waves from the hypocentre, causing ground movement omnidirectionally but typically modelled horizontally (in two directions) and vertically Pga records the acceleration (rate of change of speed) of these movements, while peak ground velocity is the greatest speed (rate of movement) reached by the ground, and peak displacement is the distance moved
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