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

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Solution: It is assumed that the attenuation relationship given by Cornell at equation<br />

(1) valid for the region. The peak ground acceleration to be expected at the site<br />

corresponding to the maximum magnitude <strong>of</strong> an earthquake occurring at the sources<br />

is given in Table below.<br />

On the basis <strong>of</strong> Table 5.2, the hazard would be considered to be resulting<br />

from an earthquake <strong>of</strong> magnitude 7.5 occurring from source 1. This hazard is<br />

estimated as producing a PGA <strong>of</strong> 0.49g at the site.<br />

Source M r(km) PGA(g)<br />

1 7.5 23.70 0.490<br />

2 6.8 60.04 0.<strong>10</strong><br />

3 5.0 78.63 0.015<br />

Table 5.2 : PGA at the site for different sources<br />

Intensity Calculation - Examples:<br />

To estimate the intensity <strong>of</strong> the earthquake, following methodology is adopted :<br />

� Step1: Divide the entire country in to ½ degree X ½ degree blocks. Each ½<br />

degree block is 55 km X 55 km.<br />

� Step 2: Plot all the historical earthquake <strong>of</strong> magnitude 5 and above in Richter<br />

<strong>scale</strong>.<br />

� Setp3: Use table 1.0 to estimate the intensity at epicenter ( Io)<br />

� Step 4: Use the equation EQ 2.0 to estimate intensity in neighboring block(<br />

Ix)<br />

� Step 5: Plot all major earthquakes occurring in different blocks and estimate<br />

the intensities in the surrounding blocks.<br />

42

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