DSC07938 (2)
1
Vi stula vallev bettueen the outlots oj Dunajec and Bteń 103
-ePe-* the
the
aries
Poor
pUse l by
I in-
pore the 17 — the VTa-
FLOOD—PLAIN
^ola Rogowska % słupłec 20
SZCZUCIN RIDGE GVtR7;LOOi3 TERRACE
% Wojcina
%
Słupiec 3
Fig. 8. Percentage variations in Vistula gravels compositions as a function of size
grade
1 — quartz clasts; 2 — flysch sandstone. clasts; 3 — flint clasts and siliclfied limestone clasts; 4 — igneous and metamorphic clasts; 5 — lydite, flysch chert and ąuartzite clasts;
6 lj|l other clasts
niów A, Fig. 8 — Ujście Dunajeckie, Szczucin). That particular deposi-tion of coal pieces is related to the ratio of its density versus that of the remaining materiał what is presented in details by Rutkowski (in press).
RELIEF OF THE RIVER TERRACES
MIDDŁE TERRACE
The middle terrace constitutes the highest terrace level in the val-ley bottom of a very complicated structure. The higher patches are stri-king features of its relief. That one located in the interbasin areas of the Vistula and Breń rivers is called Garb Szczuciński by Starkel (1972). The remaining ones extend along the peripheral parts of the valley. These patches, imcluding even the higher one in the area of Olesno, rise tp the height of 8—10 m above the Vistula channel and 1—4 m above the overflood terrace. The patches in ąuestion are separated by slightly recessed (1—2 m), fiat and fragmentarily water-logged depressions which
Wyszukiwarka
Podobne podstrony:
DSC07944 (2) 109 Yistula valley between the outlets oj Dunajec and Breń the sand-gravel deposits of
Plan Mousillon Duchy MapCity of the Damned Tht north gatt oj the city is Nocked by the Charnel Hills
207 RIKEN Accel. Próg. Rep. 24 (1990)VI-2. Residual Activities in the Ring Cyclotron FacilityS. Fuji
- vi - DOCUMEHTS CONTA1NED IH THE PROJECT FILg 1. R6publique du Niger, Ministfcre du Pleń DEPP, Inte
VI Figurę supplementaire (Chapitre 1) 2. The relative proportions of the pro- and maturę forms of fu
DSC07918 277 circle (Haufler 1955). The significant expansion of Southern or indifferent species (Pu
DSC07930 96 T. Sokołowski exceeds 20 km in some locations here. The valley is surrounded by pla-teau
DSC07934 (2) 90 Yistula ralley betioeen the outlets of Dunajec and Breń Fig. 3. Maximal and minimal
DSC07935 (2) 100 T. Sokołowski profile. However, the raeasured maximum discharge was 4400 m3/s in 19
DSC07936 (2) 101Vistula valley betioeen the outlets of Dunajec and Breń 6fn -j—-1-1---- i 1 i-1-1-1-
DSC07940 (2) 105 Vistula valley betiueen the outlets of Dunajec and Breń cular bends. Actual depress
DSC07942 (2) 107 Vistula ralley between the outlets of Dunajec and Breń xizontaiły laminated. The sa
DSC07946 (2) 111 Vistula valley between the outlets of Dunajec and Breń The Vistula river preserved
DSC07948 113 Vistula valley beticeen the ouilets of Dunajec and Bre* goci* ze w s k a - M u s i a ł
DSC07952 Geogruphical Studies Evolution of the Vistula Rłver Valley PL ISSN 0373-6547 DOROTA
12 pcx VI 14626(N) 3/4 VI 14626(N) 3/4Notę: • Set the following switch or On-screen menu to the posi
więcej podobnych podstron