Explore: Periglacial Processes

Periglaciation (adjective: "periglacial", referring to places at the edges of glacial areas) describes geomorphic processes that result from seasonal thawing

Permafrost and Periglacial Processes is a quarterly peer-reviewed scientific journal covering research on permafrost and periglacial geomorphology. It

valleys. These steep slopes usually originate from late-Pleistocene periglacial processes. There are five main stages of scree slope evolution:[citation needed]

geomorphic processes which nevertheless have been conditioned by past glaciation are termed paraglacial processes. This concept contrasts with periglacial processes

University. Burn is a specialist in the study of permafrost and periglacial processes in northern Canada. Beginning in the early 1980s, he conducted fieldwork

Permafrost and Periglacial Processes. 1 (1): 31–43. Bibcode:1990PPPr....1...31F. doi:10.1002/ppp.3430010105. Black, Robert F. (1976). "Periglacial Features

Complex Remnants on the Eastern Siberian Arctic Shelf. Permafrost and Periglacial Processes. vol. 14, pp. 187–198. Media related to Lyakhovsky Islands at Wikimedia

indicate the presence of a periglacial zone. Chief actions in these zones include solifluction and frost-shattering processes, the effects of which can

Alaska's Arctic National Parks, c . 1980–2019". Permafrost and Periglacial Processes. 32 (3): 392–406. Bibcode:2021PPPr...32..392S. doi:10.1002/ppp.2098

within Permian sandstone. This paleosol has been largely modified by periglacial processes and development of ice wedges periodically during the Pleistocene