„LAND T 
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owledge to 
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ve soils as 
The higher 
defined in 
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and more 
d more and 
eterminants 
| properties 
ng detail 
recognizes 
rm units. It 
] finds its 
jn morpho- 
omposition. 
logic terms 
tailed geo- 
ndform is 
e basis of a 
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't is a small 
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| terms of 
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led unit of 
PERMEABLE 
LLY [DEEP SOILS 
AGGREGATION 
DISAGGREGATION 
‘| 
ierarchy : 
legend are 
used to 
Is (HsC in 
dy of the 
gure 2). In 
landforms 
  
  
E DEPOSITIONAL LANDFORMS 
~ HaD f | P PIEDMONT 
BEN \ f BZ | Pg gravitational 
  
  
Irrigated tree crops 
Rainfed tree crops 
EN Semi-natural vegetation 
EN Annual crops 
  
Figure 4. 
  
PgC conglomerate blocks + flows over marls 
PgM marl with colluvial surface transport 
Pf fluvial (Quaternary) 
Pfo old to very old strongly incised 
Pfy young, not to slightly incised 
R RIVER FLATS / TERRACES (QUATERNARY) 
Rf fluvial 
RfX limestone-rich and coarse 
EROSIONAL LANDFORMS 
M HILLY TO MOUNTAINOUS (HARD ROCKS) 
Mm metamorphic rocks (Cambrian) 
MmG gneiss 
Mms schist and shale 
Mu ultramafic rocks 
MuT serpentinite 
Mh hard sedimentary rocks (Pliocene, Miocene) 
MhC conglomerate 
H HILLS (SOFT ROCKS) 
Hs ridges and hills in soft sedimentary rocks 
(Flysch: mainly Tertiary) 
HsZ marl and sandstone ridges 
HsD fluvial-capped (calcareous conglomerate) 
hills with adjacent slopes (Piedmont 
remnants: Pliocene to Pleistocene) 
HsU minor valleys and bottom lands with marl and 
limestone-rich deposits 
  
Irrigated tree crops 
Rainfed tree crops 
EN Semi-natural vegetation 
EN Annua! crops 
  
Figure 5. 
Intemational Archives of Photogrammetry and Remote Sensing. Vol. XXXII, Part 7, Budapest, 1998 345