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The Saxonian Granulite Massif is located at the northern margin of the Saxo-Thuringian Zone of the peri-Gondwana Bohemian Massif.
Since ∼4 Ma, the Selaha and the Zheduotang faults form the present-day restraining bend south of which the highest part of the massif is located, including the Gongga Shan that rises more than 3000 m above the mean elevation of the plateau.
The massif is located at the intersection of four faults, some of which still are active.
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Large massifs are located on either side of the valley, called the North and South massifs, respective to their geographic location in relation to each other.
Two soils from the central Massif (France) are formed under mild and humid climate, the third soil is located under colder and dryer climate zone (Szklary Massif — south western Poland).
The study area is located in the Grand Galibier Massif in the French South-Western Alps (Vallon de Roche Noire, commune de Le-Monêtier-les-bains, France; 45°0.05'N, 06°0.38'E).
The study site is located in the French Alps Mont Blancc massif), between 1'100 and 2'100 m above sea level.
The study area is located in the south-eastern French Massif central, a volcanic region containing Tertiary sedimentary materials that are prone to landslides.
The 11-ha study area is located on a rolling landscape in the Massif Central (France).
The reference area, Borlova village, near Caransebes city, is located on the Sebes valley, at the foot of massif Muntele Mic, a nonpolluted area with less industry.
It is located within the South Pole-Aitken basin on a massif.
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