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High Resolution 1:10,000 scale Mapping Strategy of Multi ... - NDMA

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Infact, magnitude is the measurement <strong>of</strong> the energy released by the earthquake<br />

event, whereas the intensity are connected with effect <strong>of</strong> earthquake at epicenter to<br />

location away from epicenter.<br />

Richter magnitude <strong>of</strong> an earthquake is determined from the logarithm <strong>of</strong> the<br />

amplitude <strong>of</strong> waves recorded by seismographs (adjustments are included to<br />

compensate for the variation in the distance between the various seismographs and<br />

the epicenter <strong>of</strong> the earthquake) as per the relationship<br />

where A is the maximum excursion <strong>of</strong> the Wood-Anderson seismograph, the<br />

empirical function A0 depends only on the epicentral distance <strong>of</strong> the station, δ. In<br />

practice, readings from all observing stations are averaged after adjustment with<br />

station-specific corrections to obtain the ML value.<br />

Because <strong>of</strong> the logarithmic basis <strong>of</strong> the <strong>scale</strong>, each whole number increase in<br />

magnitude represents a ten fold increase in measured amplitude; in terms <strong>of</strong> energy,<br />

each whole number increase corresponds to an increase <strong>of</strong> about 31.6 times. The<br />

energy released in an earthquake <strong>of</strong> magnitude 3 on Richter <strong>scale</strong> is equivalent 31.6<br />

metric tons <strong>of</strong> TNT. An earthquake <strong>of</strong> magnitude 6 on Richter <strong>scale</strong> is equivalent 1<br />

mega tons <strong>of</strong> TNT. An earthquake <strong>of</strong> magnitude 9 on Richter <strong>scale</strong> is equivalent 31.6<br />

gigatons <strong>of</strong> TNT. This is an idea <strong>of</strong> strength <strong>of</strong> the energy released during the<br />

earthquake.<br />

SCALE FOR EARTHQUAKE HAZARD EVALUATION<br />

INTENSITY- MODIFIED MARCALLI SCALE<br />

The effect <strong>of</strong> an earthquake on the earth's surface is called the intensity. The<br />

intensity <strong>scale</strong> consists <strong>of</strong> a series <strong>of</strong> certain key responses such as people<br />

awakening, movement <strong>of</strong> furniture, damage to chimneys, and finally - total<br />

destruction. Although numerous intensity <strong>scale</strong>s have been developed over the last<br />

several hundred years to evaluate the effects <strong>of</strong> earthquakes, the one currently used<br />

is the Modified Mercalli (MM) intensity <strong>scale</strong>. This <strong>scale</strong>, composed <strong>of</strong> 12 increasing<br />

levels <strong>of</strong> intensity that range from imperceptible shaking to catastrophic destruction,<br />

is designated by Roman numerals. It does not have a mathematical basis; instead it<br />

30

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