Results 41 to 50 of about 306,213 (313)
Fluvial terraces in the source of the Yellow River suggest that Ruoergai Basin was connected with the lower reach after ∼10 ka, much younger than the uplift chronology of the Tibetan Plateau.
Lingfan Shi +8 more
doaj +1 more source
The cross-sectional characteristics of glacial valleys and their spatial variability [PDF]
Glacial valleys are fundamental large-scale geomorphological landscape features that dissect mountain ranges. Their cross-sectional shape is recognised as distinct from fluvial valleys.
Coles, Rebecca J
core +6 more sources
Glacial geomorphology of the Ahuriri River valley, central Southern Alps, New Zealand
Detailed geomorphological mapping of ice-related and post-glacial landforms is widely used to explain past glacial fluctuations and dynamics. Here we present the first detailed glacial geomorphological description of the landform assemblages produced by ...
Levan Tielidze +3 more
semanticscholar +1 more source
We present the first extensive high-resolution glacial geomorphic map west of the Andean Cordillera in southernmost Chile (52.8–53.1°S, 73.0–73.9°W). The map extends over 1565 km2 and is based on high-resolution satellite images and aerial photographs ...
P. C. Rodriguez +5 more
doaj +1 more source
The mapping and study of glacial geomorphology near Piteå, Northeastern Sweden [PDF]
Since the beginning of the 20th century numerous mapping projects regarding glacial geomorphology in different regions of Sweden have been published, with methods advancing from in situ field observations to modern remote sensing systems that are ...
Edin, Olga
core
Quaternary glacial evolution in the Central Cantabrian Mountains (Northern Spain) [PDF]
Peer ...
González-García, M. +4 more
core +1 more source
Geomorphology of the Kaikoura area [PDF]
The major physiographic units in the Kaikoura area are the Peninsula Block, Beach Ridges and Raised Beaches, Hard Rock Areas and the Alluvial Fans. Erosion of the Seaward Kaikoura Mountains and the transfer of the debris to the sea by fan streams have ...
Chandra, Satish
core +1 more source
Emergence of the Shackleton Range from beneath the Antarctic Ice Sheet due to glacial erosion [PDF]
This paper explores the long-term evolution of a subglacial fjord landscape in the Shackleton Range, Antarctica. We propose that prolonged ice-sheet erosion across a passive continental margin caused troughs to deepen and lower the surrounding ice-sheet ...
Kerr, A. R. +11 more
core +1 more source
The Cordillera Darwin Icefield (CDI) has experienced widespread retreat since the Little Ice Age (LIA, ∼1870 AD). Prior to this, information on outlet glacier dynamics is limited as there are few terrestrial observations and little mapped deglacial ...
E. Izagirre +5 more
semanticscholar +1 more source
Geological reconstruction of the retreat history of the East Antarctic Ice Sheet (EAIS) since the Last Glacial Maximum (LGM) is essential for understanding the response of the ice sheet to global climatic change and the mechanisms of retreat, including a
Moto Kawamata +6 more
semanticscholar +1 more source

