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The Länkäran region of southern Azerbaijan has evergreen vegetation and thick beech and oak forests.
Many functional properties of forests depend on the leaf area; however, measuring leaf area is not trivial in tall evergreen vegetation.
Decadal altitudinal shifts of main land cover types, specifically herbaceous vegetation, denuded soils, glacier, and upper montane evergreen vegetation are finely attuned with decadal changes in temperature.
In Mediterranean regions, natural landscapes mostly covered by evergreen vegetation have been to a large extent transformed into cultural landscapes since long time ago.
The reason why dense forest, sparse forest and shrubs are susceptible to land sliding can be attributed to the existing steep slope morphology and the sallow rooted nature of different evergreen vegetation types in the area.
Therefore, the vegetation detected in SPOT-6 image (1 m, October) was used to define shrubs as evergreen vegetation because only evergreens had green leaves at that time of the year (Fig. 8).
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The evergreen Mediterranean vegetation was constantly present in the landscape, even during the Lateglacial cold fluctuations.
The forests found at higher altitudes are made up of pine trees and other evergreen alpine vegetation.
This, in fact, provides a relict status of dry broadleaf evergreen sclerophyllous vegetation of Madrean-Tethyan disjunction.
The rest of these taxa, especially Ammopiptanthus, are shrubby and likely to be relicts of the Tertiary dry broadleaf evergreen sclerophyllous vegetation [ 89].
The Madrean-Tethyan disjunction was proposed by Axelrod [ 89], as reviewed recently by Wen and Ickert-Bond [ 90], which hypothesized a nearly continuous belt of Madrean-Tethyan dry broadleaf evergreen sclerophyllous vegetation stretching from western North America to Central Asia in the early Tertiary (from Eocene to late Oligocene) at low latitudes.
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