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Fig. 11.11 Alpine Nanopodzol on quartzite and under Ericaceae. France. Arc 2000 (2000
m). Photo: Brice Mourier.
Figure 11.12 shows the climatosequence of soils seen between 1030 m
and 2450 m on the northwestern flank of Mont Blanc. The rocks, all acid,
are varied in the details: hard Mont Blanc granite (protogine), glacial
tills, more or less arenized gneiss.
Toposequence on the Mont Blanc massif
On rocks :
Umbric Leptosol
Pilgrims
Glacier
Cable-car station of l'Aiguille
du Midi
Intergrade soil
under sward
on till
2200 m
Rhodora
Leptic Podzol
Larch with
rhododendrons
Legend
O
Spruce with
undergrowth
of grasses and
blueberry
Haplic Podzol
A
1700 m
E
Bh
Bs
C (arène)
C (till)
R (granite)
R (gneiss, schists)
Entic Podzol
Chamonix
town
Humic and Dystric
Cambisol
1000 m
Fig. 11.12 Climatosequence. Soil tiers between Chamonix and l'Aiguille du Midi, below
Mont Blanc (Legros and Cabidoche 1977).
 
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