The whole publication in PDF - Culture in Development
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could be m<strong>in</strong>imised by identify<strong>in</strong>g such areas via a Flood Mapp<strong>in</strong>g Programme, learn<strong>in</strong>g the flood history of the area<br />
from older residents and respect<strong>in</strong>g the natural water courses (Anonymous, n.d., b).<br />
Another major cause of flood<strong>in</strong>g is blocked dra<strong>in</strong>age. Dur<strong>in</strong>g periods of heavy ra<strong>in</strong>fall the refuse that blocks the<br />
dra<strong>in</strong>s has a damm<strong>in</strong>g effect and prevents the water from flow<strong>in</strong>g freely, thus creat<strong>in</strong>g overflows and ultimately<br />
giv<strong>in</strong>g rise to flood<strong>in</strong>g. Deforestation can be another well-known reason for floods. Without the tree root system the<br />
ra<strong>in</strong>water runs freely down the slopes carry<strong>in</strong>g everyth<strong>in</strong>g, <strong>in</strong>c lud<strong>in</strong>g soil and debris with it (Anonymous, n.d., b).<br />
Flood mitigation measures <strong>in</strong> general deal with two ma<strong>in</strong> areas: control of the river and control over the land,<br />
<strong>in</strong>clud<strong>in</strong>g land use policies. Control over the river <strong>in</strong>cludes measures like channel improvement and the construction<br />
of reservoirs to store excess amounts of water. Control over land <strong>in</strong>cludes the construction of terraces and<br />
reforestation. <strong>The</strong>se are just a few of the p ossible measures (CDERA website). <strong>The</strong> only totally effective protection<br />
aga<strong>in</strong>st flood<strong>in</strong>g caused by a river overflow<strong>in</strong>g is to choose a site that is sufficiently high up to rule out this danger<br />
(Duche<strong>in</strong>, 1988).<br />
At a workshop of the UN Economic and Social Commission for Asia and the Pacific (UNESCAP) at Bangkok<br />
<strong>in</strong> 1991 a delegate noted that 80% of all victims of water-related disasters live <strong>in</strong> Bangladesh, Ch<strong>in</strong>a or India. It<br />
appears that the low-<strong>in</strong>come countries are the worst effected by flood disasters. It also became clear that most flood<br />
disasters victims live <strong>in</strong> rural areas and belong to the poorest section of the population (UNESCAP , 1990).<br />
Prepar<strong>in</strong>g for a disaster is the best defence. Thus, when choos<strong>in</strong>g a site for an archive, library or museum it is<br />
important to <strong>in</strong>vestigate the risk of a flood. <strong>The</strong> build<strong>in</strong>g itself requires a structure that can withstand water pressure<br />
or the velocity of flow<strong>in</strong>g water. Proper anchorage of the build<strong>in</strong>g prevents floatation of the foundation. In several<br />
countries traditional houses are built on poles to dim<strong>in</strong>ish the damage of flood<strong>in</strong>g. For <strong>in</strong>stitutions of cultural heritage<br />
the elevation of the basement may be a solution (CDERA website). Needless to say that the roof is important to<br />
prevent <strong>in</strong>vasion of water (see section on Damage – W ater). Roof cover<strong>in</strong>gs must be able to resist heavy ra<strong>in</strong>fall and<br />
the cover<strong>in</strong>g should be fixed tightly so that the w<strong>in</strong>d is not able to tear it off. Flat roofs and skylights are a hazard,<br />
as are walls made of non-waterproof materials e.g. porous stone. A double thick wall with a void between them is<br />
advisable <strong>in</strong> flood-prone areas. All open<strong>in</strong>gs <strong>in</strong> the walls like doors, w<strong>in</strong>dows, vents, air holes, etc. are a risk. <strong>The</strong>y<br />
must be watertight and shutters are a good protection aga<strong>in</strong>st heavy ra<strong>in</strong>. All w<strong>in</strong>dows must be placed well above<br />
the ground level (Duche<strong>in</strong>, 1993). Metal flood shields bo lted <strong>in</strong>to place will reduce water penetration through doors<br />
and w<strong>in</strong>dows, alternatively old sandbags or sheet metal cover<strong>in</strong>gs can be used (Fortson, 1992). T he sandbag has a<br />
modern version: the water absorbent cushion. It absorbs the water and when swollen acts as a sandbag. After the<br />
disaster checks must be made for water accumulation <strong>in</strong> hidden areas like attics, false ceil<strong>in</strong>gs and compact shelv<strong>in</strong>g.<br />
Water can also damage the fire detection or fire suppress<strong>in</strong>g systems (Fortson 1992).<br />
Alarms can be <strong>in</strong>stalled to detect water <strong>in</strong> storage rooms water. <strong>The</strong>y can be connected to a central response<br />
facility but if that is not possible self-conta<strong>in</strong>ed units last up to 72 hours. Archival boxes, aga<strong>in</strong>, are a good protection<br />
for paper and books. Most boxes resist water and give som e protection even when the water is contam<strong>in</strong>ated with<br />
salt or other deposits of floodwater. As mentioned before (see section on Damage – Water) shelves must be at least<br />
four <strong>in</strong>ches off the floor. Collections stored temporarily must never be placed directly on the floor, but always on<br />
a pallet. If there is not enough time to move a collection out of a vulnerable area, the shelv<strong>in</strong>g units should be<br />
covered with plastic sheets. <strong>The</strong>y must not be covered longer than 48 hours and they should be checked every 12<br />
hours for mildew. Always keep a supply of plastic sheets, heavy-duty tape and scissors <strong>in</strong> the storage rooms ready<br />
for use (Fortson, 1992).<br />
<strong>The</strong> disastrous flood <strong>in</strong> Florence <strong>in</strong> 1966 severely damaged the hold<strong>in</strong>gs of the National Library. However, it<br />
also brought the concept of the conservation of library materials to the attention of the library public (Lan, 1990).<br />
<strong>The</strong> river water, channelled through narrow streets, travelled at up to 80 miles p er hour and poured <strong>in</strong>to Italy’s<br />
National Library, drench<strong>in</strong>g thousands of manuscripts (Nelson 1991). <strong>The</strong> 1997 flood <strong>in</strong> Poland affected about 80<br />
libraries and destroyed around 300,000 volumes, the value of which is estimated at US $700,000. On top of that,<br />
the material losses <strong>in</strong> build<strong>in</strong>gs and furnish<strong>in</strong>gs are estimated at US $1 million (Wolosz, 1999).<br />
Water-related natural disasters br<strong>in</strong>g confusion and destruction to a large segment of the community. This<br />
complicates the recovery. Staff may have other problems at home, lack of assistance from local authorities or<br />
shortage of supplies (Fortson, 1992).<br />
Today the effects of water on documents are well known. Seawater is more dam ag<strong>in</strong>g than fresh water due to<br />
the corrosive effects of sea salt. Flood water can be polluted and can cause particular damage to paper (see section<br />
on Damage – Water). Paper and books may also be covered with mud and dirt (Duche<strong>in</strong>, 1993; Waters, 1993). For<br />
the recovery of wet paper and books see section on Disaster Preparedness – Recovery. Audio-visual materials,<br />
photographs, microforms, magnetic media and other discs, are also vulnerable to water, and the damage depends<br />
on the type of the material, the length of exposure to water, its temperature, etc. (Brandt-Grau, 2000).<br />
For websites on water-related disasters see Dartmouth Flo od Observatory, Flood Hazard Research Centre<br />
(FHRC), International Tsunami Information Centre (ITIC).<br />
An onl<strong>in</strong>e bibliography on floods called El Niño and flood<strong>in</strong>g, a global resource is published on the website of<br />
the Center for Ocean and Atmospheric Prediction Studies.<br />
For further read<strong>in</strong>g see Anonymous, 1992; Corn<strong>in</strong>g Museum of Glass, 1977; Ezennia, 1995; Lucchitta et al.,<br />
1999; McCann et al., 1995; Rees et al., 2000; UNESCAP, 1990; Wolosz, 1999.<br />
6.3.6.1 Tsunami<br />
Tsunami is Japanese for a tidal wave and is consid ered a special k<strong>in</strong>d of flood often caused by an earthquake. T his<br />
wave can move over the ocean at a speed of 800 km /h. Tsunamis rema<strong>in</strong> an ever-present threat to lives and property<br />
along the coasts of most oceans of the world.<br />
Most of the websites o n natural disasters will also cover floods. For <strong>in</strong>formation exclusively on tsunamis see<br />
the National T sunami Hazard M itigation Programme website hosted by the NOAA (National Oceanic and<br />
Atmospheric Adm<strong>in</strong>istration), and the websites of the National Tidal Fac ility, the International Tsunami Information<br />
Center, Tsunami hosted by the Earth and Space Sciences at the University of Wash<strong>in</strong>gton.