Results 31 to 40 of about 491 (213)

Piecing together the Lateglacial advance phases of the Reussgletscher (central Swiss Alps) [PDF]

open access: yesGeographica Helvetica, 2018
Exposure dating has substantially improved our knowledge about glacier advances during the Younger Dryas (YD) and the early Holocene. The glacier development after the Last Glacial Maximum (LGM) and the timing of morphologically evidenced, earlier ...
M. Boxleitner   +5 more
doaj   +1 more source

Glacier dynamics, sedimentary processes, and deglaciation history in Recherchefjorden, Svalbard

open access: yesArctic Science
The postglacial retreat of Svalbard glaciers has been interrupted by relatively short-lived readvances controlled by climatic as well as local glacial, meteorological, and geological controls.
Cecilie Juhl Thaarup, Riko Noormets
doaj   +1 more source

The 1988 glacial lake outburst flood in Guangxieco Lake, Tibet, China [PDF]

open access: yesNatural Hazards and Earth System Sciences, 2014
The 1988 glacial lake outburst flood (GLOF) in Guangxieco Lake is studied based on geomorphological evidence, interviews with local residents, field surveys in 1990 and 2007, and satellite images from different years. The findings are as follows. (1) The
J.-J. Liu, Z.-L. Cheng, Y. Li
doaj   +1 more source

Glaciation Traces in the Area of the Risnjak Mountain Massif

open access: yesGeologia Croatica, 2010
The area of the Risnjak mountain massif is a submorphologicalregion - part of the mesomorphological region of the south-westernGorski Kotar. This area exceeds 1,500 metres in height.
Andrija Bognar, Ivančica Prugovečki
doaj   +1 more source

The Thickness of Talus Deposits in the Periglacial Area of SW Spitsbergen (Fugleberget Mountainside) in the Light of Slope Development Theories

open access: yesLand, 2022
Periglacial slopes are susceptible to recent climate change. The rate of morphogenetic processes depends on numerous factors. The most important of these is the warming of the air and ground, increased precipitation (extreme rainfall in particular), and ...
Piotr Dolnicki, Mariusz Grabiec
doaj   +1 more source

Assessment of glacial lake development and prospects of outburst susceptibility: Chamlang South Glacier, eastern Nepal Himalaya

open access: yesGeomatics, Natural Hazards & Risk, 2016
Chamlang South Tsho has been identified as one of the six high-priority glacial lakes in terms of glacial lake outburst flood (GLOF) danger in Nepal Himalaya, despite the fact that no detailed investigations of the lake had been hitherto undertaken.
Damodar Lamsal   +3 more
doaj   +1 more source

Late‐Holocene evolution of a small Sub‐Arctic glacier, Gljúfurárjökull (Tröllaskagi, northern Iceland)

open access: yesBoreas, EarlyView.
Gljúfurárjökull, located on the Tröllaskagi Peninsula in northern Iceland, is a small glacier approximately 3.8 km in length. This study analyses the glacier's evolution through a combination of methods including: (i) geomorphological mapping, (ii) Cosmic‐Ray Exposure (CRE) dating, (iii) lichenometry and (iv) palaeoglacier reconstruction (volume ...
Nuria Andrés   +14 more
wiley   +1 more source

New age constraints of the LGM onset in the Bohemian Forest – Central Europe

open access: yesOpen Geosciences
During the Last Glacial Maximum (LGM), valley glaciers in the Bavarian/Bohemian Forest mountains (Central Europe) reached their maximum extent, forming prominent terminal moraines.
Duffek Václav   +4 more
doaj   +1 more source

Unravelling the evolution of the Frébouge polygenetic cone in Val Ferret (Mont Blanc Massif)

open access: yesBoreas, EarlyView.
Proglacial settings in the Alps are typically polygenetic, often characterized by a complex and discontinuous interplay between glacial, fluvial and gravitational processes. These processes yield high volumes of sediments, which usually exceed their transportation capacity.
Catharina Dieleman   +6 more
wiley   +1 more source

Stratigraphic evidence for modern‐like glacier extents in south‐central Alaska within the last glacial period (MIS 3)

open access: yesBoreas, EarlyView.
The last (Wisconsinan) glacial period was punctuated in North America by two glacial maxima, known as the Early and Late Wisconsinan glaciations. In Alaska, these maxima and their subsequent retreats have been the object of dating efforts to reconstruct local climatic events and compare them to global trends.
Bruno Belotti   +5 more
wiley   +1 more source

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