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The whole publication in PDF - Culture in Development

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As with other natural disasters, there are many websites on the <strong>in</strong>ternet on forest fires. <strong>The</strong> National Interagency<br />

Fire Center (NIFC) and the National Fire Plan websites are both US-based organisations and give a lot of useful<br />

<strong>in</strong>formation on wildland fire <strong>in</strong> general.<br />

Hirsch and his colleagues compiled a bibliographic list<strong>in</strong>g of about 2200 wildland-urban <strong>in</strong>terface resource<br />

materials. <strong>The</strong>y provide <strong>in</strong>formation on a diverse spectrum of topics related to fire management <strong>in</strong> the wildlandurban<br />

<strong>in</strong>terface rang<strong>in</strong>g from build<strong>in</strong>g materials and hazard reduction techniques to disaster management, politics,<br />

and sociological issues (Hirsch et al., n.d.).<br />

For further read<strong>in</strong>g on forest fires see Dudley , 1997; E berlee, 1998; Go ld Coast C ouncil, 19 98; Joh nson et al.,<br />

2001; Mansanet Terol, 1987; McCann et al., 1995; McKaige et al., 1997; Tr<strong>in</strong>kley, 1993a and 2001; Whittall, 1992;<br />

Zweck, 1983.<br />

6.3.4 Earthquakes<br />

An earthquake is a sudden, rapid motion of the earth caused by the break<strong>in</strong>g and shift<strong>in</strong>g of rock beneath the earth<br />

surface. At any time of the year and at any time of the day or the night an earthquake can occur. Smaller<br />

earthquakes, the aftershocks, can follow the ma<strong>in</strong> shock. Aftershocks can occur <strong>in</strong> the first hours, days, weeks or<br />

even months after the quake. Throughout the world 70 to 75 damag<strong>in</strong>g earthquakes occur each year. <strong>The</strong> strength<br />

of an earthquake can be measured by magnitude or <strong>in</strong>tensity. <strong>The</strong> Richter scale measures the magnitude and the<br />

modified Mercalli scale measures the <strong>in</strong>tensity. W here earthquakes have occurred <strong>in</strong> the past, they will happen aga<strong>in</strong><br />

(CDERA website).<br />

It is possible to predict earthquakes but the residents have only several hours leeway. Advance preparation for<br />

the eventuality of an earthquake is much better than to start preparations after the warn<strong>in</strong>g (F ox, 1999). Earth<br />

scientists began record<strong>in</strong>g earthquakes about 1880, but it was not until the 1940s that <strong>in</strong>struments were <strong>in</strong>stalled <strong>in</strong><br />

build<strong>in</strong>gs to measure their response to earthquakes. <strong>The</strong> number of <strong>in</strong>struments <strong>in</strong>stalled <strong>in</strong> structures <strong>in</strong>creased <strong>in</strong><br />

the 1950s and 1960s (Celebi et al., 1995a).<br />

Today, many <strong>in</strong>stitutions and organisations are watch<strong>in</strong>g out for earthquakes. One of them is the US-based<br />

National Earthquake Information Center (NEIC). It operates a 24-hour-a-day service to determ<strong>in</strong>e the location and<br />

magnitude of significant earthquakes <strong>in</strong> the United States and around the world as rapidly and accurately as possible.<br />

Every day the systems become more sophisticated and are readjusted when necessary. One of those systems is the<br />

Global Seismic Hazard Assessment Programm e (GSH AP) that was launched <strong>in</strong> 1992 b y the International<br />

Lithosphere Programme (ILP) with the support of the International Council of Scientific Unions (ICSU). <strong>The</strong><br />

GSHAP project, which was term<strong>in</strong>ated <strong>in</strong> 1999, can still be accessed through the NEIC website, and gives maps and<br />

technical <strong>in</strong>formation on earthquakes worldwide (see McGruire et al., 1995).<br />

Earthquake related haza rds <strong>in</strong>clude: collaps<strong>in</strong>g build<strong>in</strong>gs and bridges, fly<strong>in</strong>g glass, disrupted utility services,<br />

fires, landslides, flash floods, fall<strong>in</strong>g rocks <strong>in</strong> the mounta<strong>in</strong>s and <strong>in</strong> low-ly<strong>in</strong>g coastal areas tsunamis, i.e. huge<br />

destructive ocean waves (CDERA website). <strong>The</strong> damage or collapse of build<strong>in</strong>gs, as well as other structures causes<br />

the majority of deaths and <strong>in</strong>juries from earthquakes. <strong>The</strong>se losses can be reduced through document<strong>in</strong>g and<br />

understand<strong>in</strong>g how structures respond to earthquakes. Ga<strong>in</strong><strong>in</strong>g such knowledge requires a long-term commitment<br />

because large devastat<strong>in</strong>g earthquakes occur at irregular and often long <strong>in</strong>tervals. By monitor<strong>in</strong>g how structures<br />

respond to earthquakes and apply<strong>in</strong>g the knowledge ga<strong>in</strong>ed, scientists and eng<strong>in</strong>eers are improv<strong>in</strong>g the ability of<br />

structures to survive major earthquakes. This has led to many revisions and improvements <strong>in</strong> build<strong>in</strong>g codes. One<br />

of the results of seismological research was the flexible roof design (Celebi et al., 1995b). Another fact to emerge<br />

from the grow<strong>in</strong>g body of such records is that the movement close to an earthquake’s source is much stronger than<br />

once thought (Celebi et al., 1995a).<br />

First when plann<strong>in</strong>g an archives build<strong>in</strong>g, it is imperative to determ<strong>in</strong>e a site that is safe. Identify<strong>in</strong>g the<br />

geological structure of the grounds before build<strong>in</strong>g is advised, as well as check<strong>in</strong>g if the location is a potential<br />

landslide hazard. When build<strong>in</strong>g <strong>in</strong> an area that is prone to earthquakes it is necessary to use a construction that is<br />

seismic resistant, follow<strong>in</strong>g the local seismic build<strong>in</strong>g standards and safe land use codes, if available. It is important<br />

to realise that when we cannot prevent an earthquake then the least we can do is learn from them <strong>in</strong> order to reduce<br />

future damage (see Anonymous, 1989c; Geis, 1988 and Joice, 2001).<br />

Many adaptations to conventional build<strong>in</strong>gs are possible to reduce the effects of an earthquake. H owever, it is<br />

not possible to b uild earthquake-proo f constructions (Anony-mo us, n.d., a). Adherence to build<strong>in</strong>g codes can reduce<br />

losses caused by an earthqua ke s<strong>in</strong>ce they are the public's first l<strong>in</strong>e of d efence aga<strong>in</strong>st the effects of earthquakes<br />

(Celebi et al., 1995a). All parts of a build<strong>in</strong>g, situated <strong>in</strong> an earthquake prone area, should, <strong>in</strong> essence, be attached<br />

to each other. <strong>The</strong> <strong>whole</strong> build<strong>in</strong>g should be bolted to the foundation, as it is less likely to be severely damaged. <strong>The</strong><br />

build<strong>in</strong>g must be designed to be flexible and should hold together when it is shaken from side to side, and up and<br />

down (Fortson, 1992).<br />

Timber structures are considered the most earthquake resistant among traditional forms of architecture, provided<br />

their jo<strong>in</strong>ts are sound and <strong>in</strong>sects or fungi do not attack the timber. H owever, timb er build<strong>in</strong>gs are vulnerable to fires,<br />

which often follow earthquakes (Feilden, 1987). <strong>The</strong> Incas traditionally built their homes with very thick tapered<br />

walls. <strong>The</strong>se structures could resist the worst of earthquakes and landslide s. <strong>The</strong>y also built a dra<strong>in</strong>age system that<br />

stabilised the slopes aga<strong>in</strong>st landslides (Fo x, 1999). It is not necessarily expensive to build an earthquake-safe<br />

edifice. For example, the Anglo-Indian architect Laurie Baker chiefly uses local build<strong>in</strong>g materials, and cost and<br />

energy effective techniques to build shock safe dwell<strong>in</strong>gs (Hochschild, 200 0; Kremp, 2001). Thus architectural<br />

decisions concern<strong>in</strong>g site plann<strong>in</strong>g, build<strong>in</strong>g configuration, and other construction practices are crucial determ<strong>in</strong>ants<br />

<strong>in</strong> the overall performance of a build<strong>in</strong>g dur<strong>in</strong>g an earthquake (AIA, 1992).<br />

An older build<strong>in</strong>g may have later additions, which may be weaker than the orig<strong>in</strong>al areas. <strong>The</strong> foundation must<br />

be checked for possible damage by termites. Build<strong>in</strong>gs that are retrofitted and prepared for a possible earthquake<br />

and regularly ma<strong>in</strong>ta<strong>in</strong>ed, are much more likely to survive with m<strong>in</strong>imal damage (Nelson, 1991). Straps, cables and<br />

centre rods m<strong>in</strong>imise the possibility of collapse while hav<strong>in</strong>g a m<strong>in</strong>imal impact on the historic build<strong>in</strong>g fabric (Tolles<br />

et al., 1996, 2000 a and 2000 b).

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