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Rila Monastery Nature Park Management Plan - part - usaid

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February 2004<br />

(a similar process has been observed along the Radovichka River). The tendency is<br />

especially found in the upper reaches of the coniferous zone, where forest<br />

phytocenoses were cleared away in the past. Chances for the forest vegetation to<br />

naturally regenerate itself in such sections of the forest are slim. In recent years, the<br />

Chamaecytisus absinthiodes has been observed to rapidly expand its range in the subalpine<br />

zone as well. This leads to deterioration of the breeding conditions for some<br />

birds linked to grassy terrains, including bird species of high conservation<br />

significance, like those of the alpine biome (e.g. Alpine Accentor (Prunella collaris).<br />

Significance: high<br />

Natural fires<br />

Natural fires do constitute a threat to the <strong>Park</strong>; historically, there have been such<br />

incidents in its territory. However, their concrete impact on the biological diversity<br />

within the territory of RMNP is unknown.<br />

Significance: insufficiently studied<br />

Windfalls and snowslides<br />

These phenomena are known to have affected separate sections of the <strong>Park</strong> territory,<br />

to the tune of several hundred hectares. More substantial damage as a result of<br />

windfalls has been recorded in the area along the upper timberline in Otchova Reka<br />

locality, with damages to the beech forest; and in the higher portions of Bukovo<br />

Bardo locality, where the damages affect the spruce forest. Mechanical damage as a<br />

result of snowslides can be observed in the beech forests, in Scots pine forests (e.g. in<br />

Radovichka Reka locality), and at places, in the spruce-cum-fir forests.<br />

Significance: medium<br />

Avalanches<br />

The rapid downhill drift of substantial masses of snow destroys the vegetation both<br />

on the path of the snowdrift and at the final place of accumulation of the snow mass.<br />

Mechanical damage as a result of avalanches can be observed in beech forests<br />

throughout the <strong>Park</strong>; also affected are some plots of Macedonian pine. In the Suhoto<br />

Lake area, avalanches have destroyed a phytocenosis of young birch, formed in the<br />

wake of previous avalanches that cleared the same area of the old vegetation. In some<br />

cases avalanches and/or torrents may damage species of conservation significance.<br />

For example, in 1998, avalanches destroyed the <strong>Rila</strong> rhubarb phytocenosis in Beliya<br />

Uley locality. Avalanches have a negative impact on the habitats of some groups of<br />

animals (e.g. beetles and other insects, which are closely attached to certain<br />

microhabitats). They also necessitate special attention to visitor safety, especially in<br />

the areas of Beluya Uley, Siniya Uley, at some locations in the eastern portion of the<br />

<strong>Park</strong>: the southern slopes of Vodniya Rid and Mramorets, especially along the entire<br />

section of road from Kirilova Polyana to Hidroto locality at Tiha <strong>Rila</strong>, and along the<br />

tourist trails around Ribni Ezera Chalet.<br />

Significance: medium to high (for visitors), local<br />

<strong>Rila</strong> <strong>Monastery</strong> <strong>Nature</strong> <strong>Park</strong><br />

<strong>Management</strong> <strong>Plan</strong> - Draft<br />

2004 - 2013<br />

158

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