Zobrazeno 1 - 10
of 91
pro vyhledávání: '"Colin E. Thorn"'
Autor:
Kevin Hall, Colin E. Thorn
Publikováno v:
Geomorphology. 206:1-13
Widespread acceptance in science at-large notwithstanding, the ability of thermal stresses to produce thermal fatigue (TF) and/or thermal shock (TS) in bedrock and coarse debris in the field is often doubted. Commonly called insolation weathering in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c7f9763e8206240c26914c6f6686f95
https://doi.org/10.1016/j.geomorph.2013.09.022
https://doi.org/10.1016/j.geomorph.2013.09.022
Publikováno v:
Geomorphology. :1-10
The term ‘weathering’ has been in use for a very long time but it has come to mean different things to different people and hence, as scientific short-hand, it no longer functions. Here we question the tenets underpinning the most common usage of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55d23d4b618a5a48cd79c9f9fcb02d99
https://doi.org/10.1016/j.geomorph.2011.12.024
https://doi.org/10.1016/j.geomorph.2011.12.024
Autor:
Kevin Hall, Colin E. Thorn
Publikováno v:
Geomorphology. 130:83-90
Discussion of weathering in cold regions has historically been dominated by widespread acceptance of the significance of the freeze–thaw concept among periglacial geomorphologists, and an essentially universal acceptance by those geomorphologists n
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9a90b1099c88d039bd32ebda179d0df
https://doi.org/10.1016/j.geomorph.2010.10.003
https://doi.org/10.1016/j.geomorph.2010.10.003
Publikováno v:
Geological Society, London, Special Publications. 354:183-193
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63307d15e06c212435857e29c8de6e75
https://doi.org/10.1144/sp354.11
https://doi.org/10.1144/sp354.11
Autor:
Peter Schlyter, John C. Dixon, A. J. Timothy Jull, Colin E. Thorn, Robert G. Darmody, Johan Holmqvist
Publikováno v:
The Holocene. 19:1031-1037
Ten paleosols from four separate soil pits located in Kärkevagge, a glaciated trough in Swedish Lapland, were dated using radiocarbon. Each soil was dated using both conventional bulk soil organic material (SOM) and a pure sample of arbuscular mycor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7ea503ee85464c87aa3c96b800d80f42
https://doi.org/10.1177/0959683609340997
https://doi.org/10.1177/0959683609340997
Publikováno v:
Norsk Geografisk Tidsskrift - Norwegian Journal of Geography. 62:290-302
Two-years of ground temperatures (10 cm and 50 cm depths) from the foreland of Storbreen in the Jotunheimen Mountains of Norway demonstrate that seasonal and annual ground temperature differences induced by microtopographic position at a constant ele
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::391a056975b32a6b6c2ee15cc3e7ec30
https://doi.org/10.1080/00291950802517916
https://doi.org/10.1080/00291950802517916
Publikováno v:
Geografiska Annaler: Series A, Physical Geography. 90:201-209
Karkevagge is an alpine valley in the low arctic of Swedish Lapland. It is named after, and famous for, its large deposit of immense (c. 10–15 m) boulders that almost fill the lower valley. Above the boulder deposit, on the flanks of the valley, ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::84dd96ae7bcdcbab64f3f3e2e5f8069d
https://doi.org/10.1111/j.1468-0459.2008.339.x
https://doi.org/10.1111/j.1468-0459.2008.339.x
Publikováno v:
Geomorphology. 94:10-23
Cold-based ice along the Fennoscandian glacial ice divide in northern Finland allowed preservation of old landscape features. Because there was little or no movement at the ice-land surface contact, erosion was at a minimum, and relict landscape feat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::132dfc79734117ae217457ddc0abcd00
https://doi.org/10.1016/j.geomorph.2007.04.006
https://doi.org/10.1016/j.geomorph.2007.04.006
Publikováno v:
Zeitschrift für Geomorphologie, Supplementary Issues. 52:27-49
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a644980a6cb495efdbc6bd6f4c8b003e
https://doi.org/10.1127/0372-8854/2008/0052s1-0027
https://doi.org/10.1127/0372-8854/2008/0052s1-0027