Reduced arctic tundra productivity linked with landform and climate change interactions. [PDF]
Lara MJ +4 more
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Combined application of sheep manure and organic fertilizer improves soil quality and microbial community structure and function in alpine mining areas. [PDF]
Yu Z, An X, Hu S, Yang M, Li J, Li C.
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Water-Rock Interaction and Freeze-Thaw Cycles as Drivers of Acid Rock Drainage Generation by a Rock Glacier in the European Alps. [PDF]
Ilyashuk B, Ilyashuk E.
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Co-application of sheep manure and commercial organic fertilizer enhances plant productivity and soil quality in alpine mining areas. [PDF]
Yu Z, Yao X, Yang M, Hu S, An X, Li C.
europepmc +1 more source
Rock glaciers across the United States predominantly accelerate coincident with rise in air temperatures. [PDF]
Kääb A, Røste J.
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PERIGLACIAL LANDFORMS | Cryoturbation Structures
2007Different types of cryoturbation (sedimentary deformations of cryogenic origin) are distinguished, interpreted in terms of mechanisms of formation and linked to their specific environmental conditions. Cryoturbations may originate from gravitational loading in the thawing soil (‘periglacial loading’), from hydrostatic pressure between frozen parts of ...
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Relict periglacial landforms at Clarks Junction, Otago
New Zealand Journal of Geology and Geophysics, 1973Abstract The Taieri Uplands of Otago have been regarded as a landscape formed by erosion in a temperate humid climate. However, studies of the regolith at Clarks Junction now indicate that the landscape is relict, and shaped largely by periglaciation during the last stage of the Otira glaciation.
D. M. Leslie, M. S. McGlone
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Glacial and Periglacial Landforms of Eastern England
2020The East Anglian region of eastern England is a low-lying area with generally subtle relief. However, it was affected by multiple cold phases in the Pleistocene, and so shows the imprint of glacial erosion and deposition, and also the effects of permafrost formation and miscellaneous periglacial processes.
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Periglacial landforms in the Pohorje mountains:
2007Contrary to the well-studied Pleistocene glaciation, periglacial phenomena in Slovenia have been given less scientific attention because they are not particularly evident in high mountains due to prevailing carbonate rocks. This, however, is not the case in the Pohorje Mountains: built of igneous and metamorphic rocks, it was not glaciated due to its ...
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