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DOLOMITES - Annexes 2-8 - Provincia di Udine

DOLOMITES - Annexes 2-8 - Provincia di Udine

DOLOMITES - Annexes 2-8 - Provincia di Udine

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NOMINATION OF THE <strong>DOLOMITES</strong> FOR INSCRIPTION ON THE WORLD NATURAL HERITAGE LIST UNESCO<br />

FLORA AND VEGETATION<br />

80<br />

the vegetal landscape and its development<br />

The plant landscape and its development in every place on the planet which has not been ra<strong>di</strong>cally<br />

shaped by man, the plant cover, namely, the apparent form of the landscape designed by growing<br />

plant life, is the result of the synergetic combination of a variety of climatic and soil factors, as well<br />

as human interventions. In the case of the Dolomite area, the pattern of plant life is also the dynamic<br />

and ever changing result of the complex historic and geological events that have caused the formation<br />

of the Alpine mountain chain. Faults, <strong>di</strong>slocation, oversteps, folds and other tectonic phenomena<br />

make it possible to reconstruct, fairly precisely, what the area might have looked like in the past.<br />

The morphology that characterizes the present-day landscape of the Dolomites largely derives from<br />

quaternary glacial formation that overturned the previous situation by making a drastic natural selection,<br />

resulting in the <strong>di</strong>sappearance of many species and the arrival on the Alps of other species of<br />

Artic and boreal origin.<br />

Although not particularly abundant during in<strong>di</strong>vidual snowfalls, total snow accumulation<br />

over the long Dolomite winter can reach extremely considerable depths.<br />

Since the withdrawal of the last Wurmian glaciers (10,000 to 12,000 years ago), <strong>di</strong>verse climatic periods<br />

have alternated, bringing a succession of dry and cold phases and more temperate and humid<br />

phases. Certified evidence of this historic succession of climates is obtained from pollen analyses con-

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