Add to ORKGIn the upper part of Kościeliska Valley several erosive (cirque and glacial trimlines) and accumulative (terminal moraines, marginal moraines, interlobate moraines and fossil rock glacier) glacial forms can be easily seen. Basing on their order and extent as well as on correlation other Tatrya valleys the deglaciation process of last mountain glaciations (Würm — Białka Stadial) in the Kościeliska Valley can be tentatively reconstructed
There are several amphitheatrical valley heads in the Hrubý Jeseník mountains. Velká kotlina is situ...
The glaciomarginal zone in front of the Opava Mountains (Eastern Sudetes) shows complex relief. This...
Kame terraces in the territory of Lithuania are found in the Late Nemunas glaciation Baltija stage r...
Like in the High Tatras, a well-developed set of glacial and periglacial landforms marks successive ...
Be-10 exposure age chronology of the last glaciation was established in a key area at the southern s...
In the Western Carpathians, clear evidence of the Pleistocene glaciations only occurs in two mountai...
The submitted diploma thesis is concerned with the geomorphological analysis of specific landforms i...
Tato diplomová práce se zabývá glaciálními kary Vysokých Tater - z pohledu jejich morfometrických ch...
The Tatra Mountains extend along the border between Slovakia and Poland in the Western Carpathians. ...
Budowa oraz rozmieszczenie form glacjalnych i peryglacjalnych umożliwia odtworzenie przebiegu deglac...
The paper presents examination of views on number and age of glaciations in the Tatra Mts. and a new...
The article presents the results of the first detailed geomorphological mapping of the Žiarska, Jamn...
Tills in fluvioglacial cone of Sucha Woda Valley near Toporowa Cyrhla and Niżnia Palenica Pańszczyko...
A reconstruction of the last glacial maximum (LGM) ice surface geometry in the Polish High Tatra Mts...
Deglaciation chronology of the Bystra catchment (Western Tatra Mountains) has been reconstructed bas...
There are several amphitheatrical valley heads in the Hrubý Jeseník mountains. Velká kotlina is situ...
The glaciomarginal zone in front of the Opava Mountains (Eastern Sudetes) shows complex relief. This...
Kame terraces in the territory of Lithuania are found in the Late Nemunas glaciation Baltija stage r...
Like in the High Tatras, a well-developed set of glacial and periglacial landforms marks successive ...
Be-10 exposure age chronology of the last glaciation was established in a key area at the southern s...
In the Western Carpathians, clear evidence of the Pleistocene glaciations only occurs in two mountai...
The submitted diploma thesis is concerned with the geomorphological analysis of specific landforms i...
Tato diplomová práce se zabývá glaciálními kary Vysokých Tater - z pohledu jejich morfometrických ch...
The Tatra Mountains extend along the border between Slovakia and Poland in the Western Carpathians. ...
Budowa oraz rozmieszczenie form glacjalnych i peryglacjalnych umożliwia odtworzenie przebiegu deglac...
The paper presents examination of views on number and age of glaciations in the Tatra Mts. and a new...
The article presents the results of the first detailed geomorphological mapping of the Žiarska, Jamn...
Tills in fluvioglacial cone of Sucha Woda Valley near Toporowa Cyrhla and Niżnia Palenica Pańszczyko...
A reconstruction of the last glacial maximum (LGM) ice surface geometry in the Polish High Tatra Mts...
Deglaciation chronology of the Bystra catchment (Western Tatra Mountains) has been reconstructed bas...
There are several amphitheatrical valley heads in the Hrubý Jeseník mountains. Velká kotlina is situ...
The glaciomarginal zone in front of the Opava Mountains (Eastern Sudetes) shows complex relief. This...
Kame terraces in the territory of Lithuania are found in the Late Nemunas glaciation Baltija stage r...