Abstract. Proglacial margins form when glaciers retreat and create zones with distinctive ecological, geomorphological hydrological properties in Alpine environments. There is extensive literature on the geomorphology sediment transport such areas as well glacial hydrology, but there much less research into specific behavior of landforms that develop after glacier close to proglacial margins. R...

At present, there remains uncertainty surrounding the Younger Dryas-early Holocene glacial history of Fennoscandian Ice Sheet in northwest Arctic Russia. This stems from a lack high-resolution ice sheet-scale geomorphological data region. To address this, this paper presents 15,355 meltwater and morainic landforms new large-scale, map marginal zone Republic Karelia, Individual were mapped relie...

This paper presents the results of 2021 and 2022 field activities carried out at San Nicola Island (Tremiti Islands, Southern Adriatic Sea) by two groups students as part Environmental Geomorphology Field Mapping course held within Master's Degree in Geological Sciences Technologies Earth Planets University ‘G. d'Annunzio’ Chieti-Pescara. were following an integrated approach that involved morp...

Abstract Present geological and geomorphological objects are non-living features that can enhance curiosity increase the knowledge of Earth's history, through development geotourism. The municipality Durrës, located in western Albania represents an active tectonic area with numerous landforms, evidence geodiversity geoheritage. In this paper, most typical geosites identified mainly based on the...

Several glacier-like landforms have been identified on Mars. We can view some of them with Google Earth and its virtual Mars planet. In the images of Ismeniae Fossae glaciers, the flow lines of these landforms are clearly visible too.

A landform is a physical feature of the terrain with its own recognisable shape. Its definition is often qualitative and inherently vague. Hence, landforms are difficult to formalise in a logical model that can be implemented. We propose for that purpose a framework where these qualitative and vague definitions are transformed successively during different phases to yield an implementable data ...

A digital database for submarine glacial landforms and sediments formed in the Arctic during since Last Glacial Maximum was created order to facilitate underpin new research on palaeo-ice sheets tidewater glacier dynamics. The glacimarine (GlaciDat) documents standardises evidence of previous activity as visible contemporary seafloor fjords continental shelves around Svalbard, Greenland, Alaska...