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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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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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PERIGLACIAL LANDFORMS IN THE KISILYAKH RIDGE
ГЕОЛОГИЯ И МИНЕРАЛЬНО-СЫРЬЕВЫЕ РЕСУРСЫ СЕВЕРО-ВОСТОКА РОССИИ 2024The Kisilyakh Ridge located in northern Yakutia is a minor ridge in the north-eastern part of the Chersky Range. The ridge is about 100 km long, rising at its highest point to 1726 m. Most of the Kisilyakh Ridge divides the Yana and Adycha drainage basins.
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Periglacial Landforms of the Hrubý Jeseník Mountains
2016This chapter deals with the occurrence, morphology and activity of periglacial landforms in the Hrubý Jesenik Mts. Redistribution of snow during the Last Glacial period , cold climate and the presence of extensive planation surfaces at high elevations have created favourable conditions for the formation and evolution of periglacial landforms, some of ...
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Periglacial Processes and Landforms in Britain and Ireland
The Geographical Journal, 1988Andrew Dugmore, John Boardman
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