05.01.2013 Views

Natural Hazards: Causes and Effects - Disaster Management Center ...

Natural Hazards: Causes and Effects - Disaster Management Center ...

Natural Hazards: Causes and Effects - Disaster Management Center ...

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

Measuring Earthquakes<br />

The severity of an earthquake can be expressed in several ways. The magnitude of an earthquake, as<br />

expressed by the Richter scale, is a measure of the amplitude (total range of fluctuation) of the seismic<br />

waves. Magnitude is related to the amount of energy released—an amount that can be estimated from<br />

seismograph recordings. The intensity, as expressed by the modified Mercalli scale (see Fig. 2.4), is a<br />

subjective measure that describes how severe a shock was felt at a particular location. Damage or loss<br />

of life <strong>and</strong> property is another, <strong>and</strong> ultimately the most important, measure of an earthquake’s severity.<br />

The Richter scale is the best known scale for measuring the magnitude of earthquakes. The scale is<br />

logarithmic so that a recording of 7, for example, indicates a disturbance with ground motion 10 times as<br />

large as a recording of 6. A quake of magnitude 2 is the smallest quake normally felt by humans.<br />

Earthquakes with a Richter value of 6 or more are commonly considered major in magnitude.<br />

The modified Mercalli scale expresses, in values ranging from I to XII, the intensity of an earthquake’s<br />

effects in a given locality. The most commonly used adaptation covers the range of intensity from the<br />

condition of “I.—Not felt except by a very few under especially favorable conditions,” to “XII.—Damage<br />

total. Lines of sight <strong>and</strong> level are distorted. Objects thrown upward into the air.” Evaluation of<br />

earthquake intensity can be made only after eyewitness reports <strong>and</strong> results of field investigations are<br />

studied <strong>and</strong> interpreted. (See Fig. 2.5 for comparison between the scales.)<br />

An earthquake’s destructiveness depends on many factors. In addition to magnitude, these include the<br />

focal depth, the distance from the epicenter, local geologic conditions, <strong>and</strong> the design of buildings <strong>and</strong><br />

other human works. The extent of damage also depends on the density of population <strong>and</strong> construction in<br />

the area shaken by the quake. 6<br />

Intensity Scale<br />

Modified<br />

Mercalli<br />

Scale<br />

Perceived<br />

by:<br />

Damage<br />

To:<br />

Destruction<br />

To:<br />

The Measurement of an Earthquake<br />

I II III IV V VI VII VIII IX X XI XII<br />

----------------------------- Persons -----------------------------<br />

None Few Some Many Most All<br />

Magnitude Scale<br />

Richter<br />

Number: 1-2 3<br />

Energy<br />

Release in<br />

ERGS:<br />

In Multiples<br />

of Base<br />

Glass<br />

Plaster<br />

4<br />

Furniture<br />

Chimneys<br />

---------------------------- Structures ----------------------------<br />

Poor Ordinary Resistant Many Most All<br />

Some Many Most<br />

5 6 7 8<br />

4.47x10 12 7.94x10 14 2.51x10 16 7.94x10 17 2.51x10 19 7.94x10 20 2.51x10 22<br />

1.31.6 1,000 31,600 1,000,000 31,600,000 1,000,000,000 31,600,000,000<br />

Intensity is a measure of the human experience <strong>and</strong> impact of earthquakes; magnitude is an estimate of energy<br />

release. They are roughly comparable, as shown. With remote seismographs magnitude can be estimated for<br />

almost all earthquakes but, in the absence of people or their property, there is no meaningful measure of intensity.<br />

Source: Ian Burton, Environment as Hazard, Kates, page 25.<br />

Figure 2.5

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!