A Móra Ferenc Múzeum Évkönyve, 1971. 1. (Szeged, 1971)

Molnár, Béla–Mucsi, Mihály–Magyar, László: Latest quaternary history of the southern stretch of the Tisza valley

f. S f. 0,2-0.3 /v. t H.

f. 3,9 -ал т. 3. 12. f. 0.4-o.s т. 4. 14. f. 5,0 - 5,4 т. 5. Ht.

f. 7.5-ä,0 /77. 6 15.

f. 1,7-2,0 т. 7. 16. f. 0,4 -0,5 /77. S. /7/ 9,9-10,3 m. 9. iß.f. 9,7- W,0 m /0 /9 / 4.0 - 4,S m. //. 20./ 1,5 -1.7 m 3f. 3.2 -3,4 m. S.f. 2,5-3.2 m. 14. S.f. 0,6-1,5 m. /5. Hf. 3,1 -3.6m. /6. 17. /4/: J,4- 3,e m. 15./" U-i,2m. /S. 16 f. 2,4 -$g m 19. 2f.f. 3,6 • 4,0 m Fig. 4 : Examples of the granulometric curves of the sediment types occuring in the Lake Dongér area (top : alluvial and lacustrine sediments ; bottm : eolian sediments) der consideration locally includes (e. g. in boreholes 7, 11, and 12) slightly peaty lenses with fossil plant remains. (The new approach to the genetics of the infusionloesses has not been tackled (see M. Pécsi 1967). The differences in the thickness of the loesses can be ascribed to erosion. The greatest thickness may have been stripped of in those places, where the loess in no 7