Abstract The post Little Ice Age recession and downwasting of Hørbyebreen, a Svalbard
polythermal glacier, has revealed a sub-polar glacial landsystem within which a geometric …

Relict landforms and sediments across former glaciated settings provide information about
ice-sheet dynamics and can contribute to the understanding of the behaviour of …

The article presents the results of morphometric analysis of approximately 300 eskers in
Poland, to the south of the Last Glacial Maximum. The measurements included their length …

Glacial sediment-landform assemblages have long been used to reconstruct the dynamics
of ice sheets throughout the Quaternary time period, particularly so for the period of the last …

Constraining esker characteristics is crucial for understanding subglacial processes and
reconstructing past ice sheet behaviour. This study compares the morphological …

Pradolinas (also called ice-marginal valleys, ice-marginal spillways, ice-marginal
streamways, or Urstromtäler) are very wide (up to 25 km) and long (up to several hundred …

Celem badań było szczegółowe rozpoznanie form terenu utworzonych w różnym czasie
przez człowieka na siedmiu obszarach leśnych Parku Krajobrazowego „Cysterskie …

The study provides a morphologic classification of eskers formed on a soft bed in Poland
during the Saalian and Elsterian Glaciations. The classification is based on morphometry …

Abstract [eng] Glaciomorphological features of the North and Middle Lithuania Lowlands are
described and interpreted. The ridged relief of the morainic plain in the NW part (Akmenė …

Micromorphology has become a principal tool in glacial sedimentology providing a wealth of
data on the geometry and kinematics of deformation histories and aiding our understanding …