Results 11 to 20 of about 491 (213)

An alpine plant shows no decrease in genetic diversity associated with rapid post-glacial range expansion. [PDF]

open access: yesAm J Bot
Abstract Premise: While range expansion is hypothesized to be a mechanism for species persistence under climate change, many eco‐evolutionary models describe demographic and genetic processes during expansion that may increase genetic drift, decrease genetic variation, and ultimately decrease relative fitness at the leading edge.
Urquhart-Cronish M   +5 more
europepmc   +2 more sources

Reconciling the apparent absence of a Last Glacial Maximum alpine glacial advance, Yukon Territory, Canada, through cosmogenic beryllium-10 and carbon-14 measurements [PDF]

open access: yesGeochronology, 2022
We present a new in situ produced cosmogenic beryllium-10 and carbon-14 nuclide chronology from two sets (outer and inner) of alpine glacier moraines from the Grey Hunter massif of southern Yukon Territory, Canada. The chronology of moraines deposited by
B. M. Goehring   +4 more
doaj   +1 more source

The Last Glacial Maximum and Deglacial History of the Seno Skyring Ice Lobe (52°S), Southern Patagonia

open access: yesFrontiers in Earth Science, 2022
There are still many uncertainties about the climatic forcing that drove the glacier fluctuations of the Patagonian Ice Sheet (PIS, 38–55°S) during the last glacial period.
María-Paz Lira   +10 more
doaj   +1 more source

Glacial history and depositional environments in little Storfjorden and Hambergbukta of Arctic Svalbard since the younger dryas

open access: yesFrontiers in Earth Science, 2022
Geophysical and lithological data provide crucial information for the understanding of glacial history in Arctic Svalbard. In this study, we reconstructed the glacier-induced depositional environments of Little Storfjorden and its tributary, Hambergbukta,
Young Jin Joe   +8 more
doaj   +1 more source

Chronology of Glacial Advances and Deglaciation in the Encierro River Valley (29° Lat. S), Southern Atacama Desert, Based on Geomorphological Mapping and Cosmogenic 10Be Exposure Ages

open access: yesFrontiers in Earth Science, 2022
The high mountain segments of the valleys of the southernmost Atacama Desert of Chile present Late Quaternary glacial landforms that developed in already incised valleys.
G. Aguilar   +4 more
doaj   +1 more source

Tree Invasions of Subarctic Shrublands Interact With Locally Augmented Snow and Functional Soil Depths: A Case Study in Denali National Park. [PDF]

open access: yesEcol Evol
In Denali National Park, Alaska, post‐glacial landscapes are undergoing a shift in successional pathways with the expansion of balsam poplar (Populus balsamifera), altering tundra ecosystem development. We found that poplar‐dominated plots had deeper snowpacks, warmer and deeper soils, and taller vegetation than shrublands, suggesting a feedback loop ...
Albrigtsen JO   +3 more
europepmc   +2 more sources

Reconstruction of the Upper Slope Conditions of an Extraordinary Hydro-Meteorological Event Along the Jamapa Glacier Drainage System, Citlaltépetl (Pico de Orizaba) Volcano, Mexico

open access: yesFrontiers in Earth Science, 2021
A singular precipitation event on the summit glacial slopes of Mexico’s highest volcanic peak, Citlatépetl (also known as Pico de Orizaba), associated with the passage of Hurricane Ernesto across the southern Mexico mainland in August 2012, resulted in a
Katrin Sieron   +3 more
doaj   +1 more source

Skjoldryggen terminal moraine on the mid-Norwegian shelf [PDF]

open access: yesGeological Society, London, Memoirs, 2016
Terminal moraines are relatively large ridges of diamictic glacial debris produced at the outermost margins of past glaciers and ice sheets. Their identification on land is important in mapping the maximum extent of Quaternary ice sheets (e.g. Svendsen et al. 2004; Benn & Evans 2010).
Dowdeswell, JA, Ottesen, D, Rise, L
openaire   +2 more sources

Submarginal drumlin formation and late Holocene history of Fláajökull, southeast Iceland

open access: yesAnnals of Glaciology, 2016
Fláajökull is a non-surging outlet glacier draining the south-eastern part of the Vatnajökull, southeast Iceland. Fláajökull was stationary or advanced slightly between 1966 and 1995 and formed a prominent end moraine.
Sverrir Aðalsteinn Jónsson   +6 more
doaj   +1 more source

Modeling a glacial lake outburst flood process chain: the case of Lake Palcacocha and Huaraz, Peru [PDF]

open access: yesHydrology and Earth System Sciences, 2016
One of the consequences of recent glacier recession in the Cordillera Blanca, Peru, is the risk of glacial lake outburst floods (GLOFs) from lakes that have formed at the base of retreating glaciers.
M. A. Somos-Valenzuela   +4 more
doaj   +1 more source

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