RELIEF AND SEDIMENTS OF NIDA RIVER VALLEY NEAR PIŃCZÓW GAP-SECTION - FIRST RESULTS

Karolina Walczyńska,Marcin Frączek,Tomasz Kalicki,Piotr Biesaga

doi:10.18509/agb217-40145f

Abstract

RELIEF AND SEDIMENTS OF NIDA RIVER VALLEY NEAR PIŃCZÓW GAP-SECTION - FIRST RESULTS

Highlights

The natural environment of research area is poorly explored ([1], [2], [3], [4] [5])
Remnants of the Pleistocene terrace, that were preserved on the left bank of the valley [10] (Fig. 2, 4) are effect of an intensive deep erosion at the end of Pleniglacial occurred in many Central European valleys of different river orders [11 and references therein]
There are the erosion remnants of younger terrace. It could be connected with the lateral migration of the Late Glacial large meanders when the valley bottom widened and undercut terrace fragments that were preserved as meandering hills just like it took place in the Czarna Nida River valley [12]

Summary

Introduction

The natural environment of research area is poorly explored ([1], [2], [3], [4] [5]). Marcin Fraczek et al Relief and sediments of nida river valley ... Gravels, and river marshes, which cover almost the entire research area (Fig. 2), were created as a result of Nida River accumulation. RESULTS The width of study section of the Nida river valley is about 2 km.

Results

Conclusion