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the trees such as different kinds <strong>of</strong> oak (Quercus valonae, Quercus liex, Ceratonia siliqua)<br />

<strong>and</strong> the wild cotton (Gomphocarpus ruticosus <strong>and</strong> Eophorbia dendrioder) (see Nasi, Prifti<br />

et.al. 2004: 22). To a certain extent, in most <strong>of</strong> the area the vegetation is damaged as the result<br />

<strong>of</strong> building <strong>of</strong> terraces, fires <strong>and</strong> goat overgrazing.<br />

The dominant minerals are calcium <strong>and</strong> other carbonates. The rough relief is imbued with<br />

many streams <strong>and</strong> torrents that disappear in the summer <strong>and</strong> reappear again in the late autumn<br />

<strong>and</strong> winter. Rainy winters provoke the run<strong>of</strong>f <strong>and</strong> sediment loss caused by the precipitation.<br />

The area is tectonically active. According to the report on the conservation <strong>of</strong> wetl<strong>and</strong> <strong>and</strong> the<br />

coastal ecosystems in the Mediterranean region “tectonic movements <strong>and</strong> shifting sea-bed<br />

morphology determine cliff erosion, creating recesses along the coast in the form <strong>of</strong> caves <strong>and</strong><br />

canyons. Weather <strong>and</strong> the assailing forces <strong>of</strong> waves from the open Ionian Sea cause basal cliff<br />

erosion to the karstic limestone rocks” (1999: 13 United Nations Development Programme<br />

Global Environment Facility).<br />

Mountainous terrain <strong>and</strong> the seasonally wet Mediterranean climate are two main reasons for<br />

erosion <strong>and</strong> l<strong>and</strong> degradation in Himarë/Himara area as well as elsewhere on the southern<br />

coast <strong>and</strong> in the Alpine area <strong>of</strong> the northern Albania (see Dedej 2002:12). Throughout the<br />

centuries in some areas the extent <strong>of</strong> erosion became greater as it was accelerated by<br />

unfavourable human activities such as over-cultivation <strong>and</strong> use <strong>of</strong> fertilizers 17 (present since<br />

1970), deforestation, creation <strong>of</strong> artificial water reservoirs <strong>and</strong> dams, extraction <strong>of</strong> the inert<br />

material like gravel <strong>and</strong> s<strong>and</strong>, diverting <strong>of</strong> rivers from their natural streams, irrational tourism,<br />

etc.<br />

1.3. Dhërmi/Drimades<br />

Dhërmi/Drimades stretches for about three kilometres along the national coastal road <strong>and</strong> is<br />

divided in three hamlets: Kondraça, Gjilek/Gjilekates, <strong>and</strong> Dhërmi/Drimades as the village<br />

centre. As people say, Dhërmi/Drimades or the centre (e qëndra or o kendros) was founded<br />

sometime in the 13 th century, when the population <strong>of</strong> Palesti (nowadays Palasa) exp<strong>and</strong>ed <strong>and</strong><br />

moved further on to the neighbouring hills <strong>of</strong> today’s central hamlet <strong>of</strong> Dhërmi/Drimades.<br />

17 According to the research report on Soil Survey in Albania the usage <strong>of</strong> fertilizers in Albania began in 1970s<br />

with the construction <strong>of</strong> two factories: one for the nitrogen <strong>and</strong> another for phosphate fertilizers (Zdruli 2004:<br />

43).<br />

49

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