Results 51 to 60 of about 333 (186)

Capturing the Multi‐Decadal Evolution of Glacier–Permafrost Interactions in a High‐Alpine Environment (Ritord, Western Swiss Alps)

open access: yesPermafrost and Periglacial Processes, Volume 37, Issue 3, Page 473-497, July/September 2026.
ABSTRACT This study investigates the multi‐decadal evolution of a glacier forefield under permafrost conditions in the Combins Massif (western Swiss Alps). A multi‐method approach based on historical and recent datasets is used to analyze its landform components.
Julie Wee   +2 more
wiley   +1 more source

Expanding cryospheric landform inventories – quantitative approaches for underestimated periglacial block- and talus slopes in the Dry Andes of Argentina

open access: yesFrontiers in Earth Science
There is a clear spatial discrepancy between the area potentially underlain by permafrost and the landforms recorded in the national inventory of cryospheric landforms in the Dry Andes of Argentina (∼22°–35°S).
Tamara Köhler   +6 more
doaj   +1 more source

Multiproxy Chronologies of the Hurd Rock Glacier (Livingston Island, South Shetland Islands, Maritime Antarctica): Between the Late‐Stage Stabilization and Flow Deceleration

open access: yesPermafrost and Periglacial Processes, Volume 37, Issue 3, Page 535-550, July/September 2026.
ABSTRACT The Hurd Rock Glacier, located on Livingston Island (South Shetland Islands archipelago, Maritime Antarctica), is a tongue‐shaped feature composed of angular boulders, displaying transverse ridges and furrows, and featuring lobate structures, which are more prominently developed in its frontal sector.
Rosana Menéndez‐Duarte   +5 more
wiley   +1 more source

Geomorphology of the Sierra del Aramo (Asturian Central Massif, Cantabrian Mountains, NW Spain)

open access: yesJournal of Maps, 2019
A detailed geomorphological map of the Sierra del Aramo (Asturian Central Massif) is presented at a scale of 1:25,000. The Sierra del Aramo is one of the major middle-altitude mountains of the Asturian Central Massif (maximum altitude 1,791 m a.s.l ...
Salvador Beato Bergua   +3 more
doaj   +1 more source

Investigation on protalus ramparts in the Swiss Alps [PDF]

open access: yesGeographica Helvetica, 2015
The origin and classification of landforms denominated as "protalus ramparts" in the scientific literature is a problem that is far from being resolved.
C. Scapozza
doaj   +1 more source

Palaeowinds and depositional conditions from Holocene loess in Sweden and Finland

open access: yesBoreas, Volume 55, Issue 3, Page 808-834, July 2026.
The nature of deglacial and Holocene wind regimes in Fennoscandia is debated, as is the degree to which wind‐blown loess deposits exist in the region. Loess deposits in Fennoscandia are often relatively thin, discontinuous and less well‐sorted than typical loess, and questions remain over the degree of their post‐depositional reworking and the impact ...
Calum J. Edward   +6 more
wiley   +1 more source

DIFFERENTIATION OF PRESENT-DAY PERIGLACIAL RELIEF IN THE HIGH MOUNTAINS OF EUROPE [PDF]

open access: yesRevue Roumaine de Géographie, 2009
La différenciation du relief périglaciare contemporain des hautes montagnes de l’Europe. L’objet de l’article est la présentation de la différenciation du relief périglaciaire contemporain des hautes montagnes de l’Europe, fondée sur l’analyse de la ...
ZOFIA RĄCZKOWSKA
doaj  

Quantification of ground surface movements on sorted circles using time‐lapse structure‐from‐motion photogrammetry in a karst cave, Slovenia

open access: yesEarth Surface Processes and Landforms, Volume 51, Issue 6, June 2026.
We present ground surface movements on sorted circles in a karst cave using time‐lapse photogrammetry with accuracies of up to ±2 mm. Data with 3‐hourly resolution revealed average vertical movements of up to 50 mm and horizontal movements of up to 15 mm during individual freeze–thaw cycles.
Jaroslav Obu   +9 more
wiley   +1 more source

Héðinsdalsjökull, northern Iceland: geomorphology recording the recent complex evolution of a glacier

open access: yesJournal of Maps, 2021
The objective of this work is to conduct a detailed mapping of the Héðinsdalsjökull foreland, northern Iceland (65°39′N, 18°55′W). This cirque currently shows a variety of glacial and periglacial landforms derived from a complex deglaciation. Mapping was
Manuel Rodríguez-Mena   +4 more
doaj   +1 more source

Loess Studies in Aotearoa New Zealand

open access: yesNew Zealand Journal of Geology and Geophysics, Volume 69, Issue 2, June 2026.
Loess in Aotearoa New Zealand (ANZ) has been studied since its first documented recognition (on Banks Peninsula) in 1878 by Julius von Haast. A decade later, John Hardcastle revealed that southern ANZ loess was both glacial in origin and contained signals of past climates.
Brent V. Alloway   +4 more
wiley   +1 more source

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