182
Climatic Geomorphology
960
3~1
1 Frost-riven cliffs
2 Tors
3 Cryoplan~tion terraces
m 880
l
/
'"
I
i
0
200
400
600
m
1080
m 1060
1040
1
3
,
-|
!
0
180
360
m
740
700
660
3 ]:~1
620
360
m
Figure 8.11. Slope profiles with cryoplanation terraces and tors in the Hruby Jesenik Mountains, Czech
Republic (partially modified from Czudek, 1964).