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Ecology and regeneration of forest communities on the alluvial fan ...

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-Study area-<br />

2 Study area<br />

2.1 Locati<strong>on</strong><br />

The study area is situated at 41°22' N <str<strong>on</strong>g>and</str<strong>on</strong>g> 46°51' E <strong>on</strong> <strong>the</strong> sou<strong>the</strong>rn foothills <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong><br />

Greater Caucasus <str<strong>on</strong>g>and</str<strong>on</strong>g> is part <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> Alasan-Awtoran depressi<strong>on</strong> (northwestern regi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g><br />

Azerbaijan). It is an <strong>alluvial</strong> <strong>fan</strong> complex, which lies downstream <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> small town <str<strong>on</strong>g>of</str<strong>on</strong>g><br />

Qakh. The altitude within <strong>the</strong> surveyed area ranges from 177 to 489 metres above sea<br />

level. The <strong>fan</strong> c<strong>on</strong>sists <str<strong>on</strong>g>of</str<strong>on</strong>g> fluvial sediments, that eroded from <strong>the</strong> adjacent mountain<br />

ranges <str<strong>on</strong>g>and</str<strong>on</strong>g> were deposited in an extensive foot slope al<strong>on</strong>g <strong>the</strong> mountain fr<strong>on</strong>t. The<br />

sediments are transported by <strong>the</strong> river Kurmukcay. The study site is surrounded up to<br />

<strong>the</strong> north, south east <str<strong>on</strong>g>and</str<strong>on</strong>g> southwest by roads. One road cuts across <strong>the</strong> mid-<strong>fan</strong>. Ano<strong>the</strong>r<br />

<strong>on</strong>e cuts across <strong>the</strong> lower <strong>fan</strong>, as does <strong>the</strong> railroad line Baku-Zaqatala. Some small<br />

villages are scattered over <strong>the</strong> <strong>fan</strong>, even in its central regi<strong>on</strong>.<br />

N<br />

4 k m<br />

Fig. 2.1 Map <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>alluvial</strong> <strong>fan</strong> complex at <strong>the</strong> sou<strong>the</strong>rn slope <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> Eastern Caucasus (Map source:<br />

(Skworzow 1976)). Inset: Map <str<strong>on</strong>g>of</str<strong>on</strong>g> Azerbaijan <str<strong>on</strong>g>and</str<strong>on</strong>g> locati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>the</strong> study area (Map source: (Kurtubadze<br />

2008))<br />

-<str<strong>on</strong>g>Ecology</str<strong>on</strong>g> <str<strong>on</strong>g>and</str<strong>on</strong>g> <str<strong>on</strong>g>regenerati<strong>on</strong></str<strong>on</strong>g> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>forest</str<strong>on</strong>g> <str<strong>on</strong>g>communities</str<strong>on</strong>g> <strong>on</strong> <strong>the</strong> <strong>alluvial</strong> <strong>fan</strong> near Qakh (Northwestern Azerbaijan)-<br />

3

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