V*N | ||
C | ||
V |
CA |
Łr
<b
O
Ś
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*1
fl>
(T> •— |
(b |
c |
c—f- |
C |
ca |
O •u |
CJ CO t-#- |
pf rD rp |
o *o co |
< £T |
A) 1 o |
CJ
o
o
10 km J
a>n6.W-'
Fig. 1. Geologic-morphological sketch of Vistula valley between Dunajec and Breń mouths
EE3' i—j*
m lj-
\ś?\s f | ,u]u fwftaptrfjg
i _ lłmits of vallev floors; 2 — terrace edges; 3 — Vistula, Dunajec and Nida channels; < — oxbows; 5 — oxbows lakes; t — dcposlu ot middle terrace. a — sands, t> — loesses; 7 — muris on the rendzina terrace; 8 — dunes; 9 — flood plain; 10 — moisturlng areas in the Breft and Kanał Strumień lows; 11 — geological cross-sections; 12 — numbers of terraees Ievels; 13 — dates of uc