The survey area is situated along two altitude profiles, each covering
an altitude difference of about 800 m, west of Achental at the northe
rn fringe of the Alps. From dolomite and limestone Rendzic Leptosol an
d Chromic Cambisol developed as predominant soil types. These are main
ly resilient against (anthropogenic) depositions. Nine woodland commun
ities (plant associations) were found. Montane spruce-fir-beech woodla
nds and subalpine spruce woodlands are predominant. Aposerido-Fagetum
and Adenostylo-Piceetum are further divided into subassociations and v
ariants. 18 site types were classified and mapped. The forest line, fo
rmed by Norway spruce (Picea abias), is situated at an altitude of abo
ut 1700m, but is widely depressed due to anthropogenic impact and edap
hic factors. Forest use started in the Middle Ages and was initialized
by the needs of neighbouring salterns and mining. This caused changes
of the tree species composition (decrease of Silver fn, Abies alba) a
nd humus dynamics. More recent impacts are caused by tourism, especial
ly skiing, and cattle grazing in the forest.