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Wat (wie) is PHIVOLCS Earthquake Intensity Scale - definitie
PHIVOLCS Earthquake Intensity Scale
EARTHQUAKE INTENSITY SCALE USED IN THE PHILIPPINES
PEIS
The PHIVOLCS Earthquake Intensity Scale (PEIS) is a seismic scale used and developed by the Philippine Institute of Volcanology and Seismology (PHIVOLCS) to measure the intensity of earthquakes.
Seismic magnitude scales
![Typical seismogram. The compressive [[P-waves]] (following the red lines) – essentially sound passing through rock – are the fastest seismic waves, and arrive first, typically in about 10 seconds for an earthquake around 50 km away. The sideways-shaking [[S-waves]] (following the green lines) arrive some seconds later, traveling a little over half the speed of the P-waves; the delay is a direct indication of the distance to the quake. S-waves may take an hour to reach a point 1000 km away. Both of these are ''body-waves'', that pass directly through the earth's crust. Following the S-waves are various kinds of ''surface-waves'' – [[Love wave]]s and [[Rayleigh wave]]s – that travel only at the earth's surface. Surface waves are smaller for deep earthquakes, which have less interaction with the surface. For shallow earthquakes – less than roughly 60 km deep – the surface waves are stronger, and may last several minutes; these carry most of the energy of the quake, and cause the most severe damage.](https://commons.wikimedia.org/wiki/Special:FilePath/1906 San Francisco earthquake seismograph.png?width=200 "Typical seismogram. The compressive [[P-waves]] (following the red lines) – essentially sound passing through rock – are the fastest seismic waves, and arrive first, typically in about 10 seconds for an earthquake around 50 km away. The sideways-shaking [[S-waves]] (following the green lines) arrive some seconds later, traveling a little over half the speed of the P-waves; the delay is a direct indication of the distance to the quake. S-waves may take an hour to reach a point 1000 km away. Both of these are ''body-waves'', that pass directly through the earth's crust. Following the S-waves are various kinds of ''surface-waves'' – [[Love wave]]s and [[Rayleigh wave]]s – that travel only at the earth's surface. Surface waves are smaller for deep earthquakes, which have less interaction with the surface. For shallow earthquakes – less than roughly 60 km deep – the surface waves are stronger, and may last several minutes; these carry most of the energy of the quake, and cause the most severe damage.")
![Isoseismal map for the [[1968 Illinois earthquake]]. The irregular distribution of shaking arises from variations of geology and/or ground conditions.](https://commons.wikimedia.org/wiki/Special:FilePath/1968 Illinois earthquake.svg?width=200 "Isoseismal map for the [[1968 Illinois earthquake]]. The irregular distribution of shaking arises from variations of geology and/or ground conditions.")
MAGNITUDE OF AN EARTHQUAKE
Seismic scales; Earthquake magnitude; Magnitude (earthquake); Nuttli magnitude; Seismic scale; Seismic magnitude scale; Body-wave magnitude; Earthquake measurement
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.
Richter scale
![[[Charles Francis Richter]] (circa 1970)](https://commons.wikimedia.org/wiki/Special:FilePath/CharlesRichter.jpg?width=200 "[[Charles Francis Richter]] (circa 1970)")
MEASURING THE STRENGTH ("SIZE") OF EARTHQUAKES
Richter scale; Richter Scale; Richter magnitude; Richter Magnitude; Ricter Scale; Ricter scale; Major earthquake; Rare Great earthquake; Strong earthquake; Rare great earthquake; Ritcher Scale; Ritcher scale; Richter's scale; Rickter scale; Local magnitude scale; Richters scale; Richter Magnitude Scale; Local magnitude; The Richter Scale
The Richter scale is a scale which is used for measuring how severe an earthquake is.
An earthquake measuring 6.1 on the Richter Scale struck California yesterday.
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