3
the guiding principles. Much-used elements are: land forms, drainage patterns, relief and
slopes, forms of natural drainage systems and gullies, drainage conditions, origin of the
parent material (geogenesis), vegetation and land use, erosion phenomena etc.; knowledge
SiS S bI 3 YU
A ç I Db 6
(ni N, > y
03 t. ; Ad 3]
\ S l — CT = di V
Ghost »8 S DY fe = Dy b
Di 4
Ma ZN = A
— A ZA Ds
..23 VA
Sm aE
Du
GA
1 EL : Co
Re MA b
t Db
y»!
Ma A Ds ré
NI a
X ;
ee DT /
> S
- =D — SM -
m ees c £
t D8 24 Ss ^
Ww
5
a ;
1
Dt
03 Ds
012
0,
0; Co
O3 Oy A
2) A1 ^os
Fig. 1. Example of a photo-analysis. This photo-analytical map to be compared with the
. , I
soil map in fig. 2 made by field survey only.
of geology and in particular of the quartenary geology as well as of geomorphology is
very important. General agricultural and archeological phenomena, as well as geographical
features such as differences in soil management, distribution and size of farms, remains
of pre-historic habitation, situation of roads, railroads, houses, dykes, etc. may give many