Results 11 to 20 of about 1,030 (156)
Deglaciation of Fennoscandia [PDF]
Quaternary Science Reviews, 2016 To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we have compiled and synthesized published geomorphological data for eskers, ice-marginal formations, lineations, marginal meltwater channels, striae, ice-dammed lakes, and ...
Arjen P Stroeven +2 more
exaly +7 more sources
The last deglaciation of Peru and Bolivia [PDF]
Cuadernos de Investigación Geográfica, 2017 The tropical Andes of Peru and Bolivia are important for preserving geomorphic evidence of multiple glaciations, allowing for refinements of chronology to aid in understanding climate dynamics at a key location between hemispheres. This review focuses on
B. Mark, N. Stansell, G. Zeballos
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Conceptual model for talus slope development in Brattegg Valley (SW Spitsbergen) based on sedimentology of debris deposits in periglacial zone [PDF]
Polish Polar Research, 2023 The talus slopes occur in all climatic zones on the Earth. These forms are sensitive to climate fluctuations, therefore they may be indicators of changes in the environment and contain the record of the geomorphological events after the deglaciation ...
Krzysztof Senderak
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The deglacial forest conundrum
Nature Communications, 2022 <p><span>The forest expansion in the Northern Hemispheric extra-tropics during the deglaciation, i.e. the last some 22,000 years, starts earlier and occurs much faster in our model simulation using the MPI-ESM 1.2 than in the recently published synthesis of biome reconstructions by Cao et al. (2019).
Anne Dallmeyer +5 more
openaire +7 more sources
On deglaciation between Pieksämäki and Pielavesi in central Finland [PDF]
Bulletin of the Geological Society of Finland, 1974 On the basis of four end moraine formations, some of them not known before, the phases of deglaciation between Pieksämäki and Pielavesi in central Finland have been described in this paper. The trend of these end moraines, other transverse formations and
G. Glückert
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The penultimate deglaciation: protocol for Paleoclimate Modelling Intercomparison Project (PMIP) phase 4 transient numerical simulations between 140 and 127 ka, version 1.0 [PDF]
Geoscientific Model Development, 2019 The penultimate deglaciation (PDG, ∼138–128 thousand years before present, hereafter ka) is the transition from the penultimate glacial maximum (PGM) to the Last Interglacial (LIG, ∼129–116 ka).
L. Menviel +23 more
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Лëд и снег, 2022 Early documentation of the consequences of the Tsambagarav earthquake happened on July 23, 1988 (M = 6.4) compiled by Soviet and Mongolian specialists allowed the authors, using the example of Tsambagarav (Mongolian Altai), to assess the impact of the ...
A. R. Agatova +5 more
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Geomorphology of the Aran Valley (Upper Garonne Basin, Central Pyrenees)
Journal of Maps, 2022 Geomorphological mapping in mountain regions is key for a better understanding of past and present environmental dynamics. Here, we present a 1:25000 scale geomorphological map covering 553 km2 of the Aran Valley, Upper Garonne Basin (Central Pyrenees ...
M. Fernandes +3 more
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Timing of the deglaciation and the late-glacial vegetation development on the Pandivere Upland, North Estonia [PDF]
Bulletin of the Geological Society of Finland, 2016 In this study, the deglaciation chronology of the Pandivere Upland is defined, and the late-glacial vegetation trends of north-eastern Estonia are summarised.
L. Amon +4 more
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Glacial‐Isostatic Adjustment Models Using Geodynamically Constrained 3D Earth Structures
Geochemistry, Geophysics, Geosystems, 2021 Glacial‐isostatic adjustment (GIA) is the key process controlling relative sea‐level (RSL) and paleo‐topography. The viscoelastic response of the solid Earth is controlled by its viscosity structure.
M. Bagge +4 more
doaj +1 more source