Arid
DOI10.1016/j.geomorph.2010.10.003
The historical legacy of spatial scales in freeze-thaw weathering: Misrepresentation and resulting misdirection
Hall, Kevin1; Thorn, Colin2
通讯作者Hall, Kevin
来源期刊GEOMORPHOLOGY
ISSN0169-555X
出版年2011
卷号130期号:1-2页码:83-90
英文摘要

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 not directly involved in researching the topic. Debris produced by freeze-thaw is frequently deemed to be angular in form and the observation of such debris has been used to identify the former or present operation of this weathering mechanism. Large debris (’blocks’) and small debris (’grains’ or ’flakes’) have been recognised as the outcome of the two scales of freeze-thaw weathering: macrogelivation and microgelivation respectively. However, the fusion of climatic geomorphology and process geomorphology in the ongoing development of the freeze-thaw concept has resulted in the confusion of product with process-whereby microgelivation (producing small products) and macrogelivation (producing large products) are seen, due to the product dichotomy, as distinctly different processes. Despite the recent, highly sophisticated laboratory experimentation on freeze-thaw weathering, this historical-process scale-dichotomy still pervades thinking and experimental evaluation. Here we consider the historical development of microgelivation/macrogelivation and outline what are thought to be fundamental flaws with the concepts and their underpinnings. Built within the two notions are elements of rock properties (’hard’ and ’soft’) and scale issues regarding rock attributes (’solid rock’ and ’existing weaknesses’ in rock) that serve only to confuse the process and scale issues even more. The whole notion of frost-weathered debris having a specific form is also highly spurious, there being no shape attribute that is uniquely diagnostic of frost action and this, in turn, leads to the further problem of process synergy or other processes entirely being the cause of rock failure in cold regions. Ultimately we argue that while there may be a range of product sizes (and shapes) resulting from frost weathering per se the widely invoked scale concepts are fraught with problems and are best dropped-as too are any process-shape connotations. (C) 2010 Elsevier B.V. All rights reserved.


英文关键词Weathering Freeze-thaw Microgelivation Macrogelivation Process-product scales
类型Article
语种英语
国家South Africa ; USA
收录类别SCI-E
WOS记录号WOS:000291453900010
WOS关键词LA PEYRATTE GRANITE ; THERMAL-STRESS ; COLD REGIONS ; MECHANICAL-BEHAVIOR ; MOUNTAIN-GLACIATION ; ROCK TEMPERATURES ; GRAIN SCALE ; ANTARCTICA ; DESERT ; SHOCK
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/168273
作者单位1.Univ Pretoria, Dept Geog Geoinformat & Meteorol, ZA-0002 Pretoria, South Africa;
2.Univ Illinois, Dept Geog, Urbana, IL 61801 USA
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Hall, Kevin,Thorn, Colin. The historical legacy of spatial scales in freeze-thaw weathering: Misrepresentation and resulting misdirection[J],2011,130(1-2):83-90.
APA Hall, Kevin,&Thorn, Colin.(2011).The historical legacy of spatial scales in freeze-thaw weathering: Misrepresentation and resulting misdirection.GEOMORPHOLOGY,130(1-2),83-90.
MLA Hall, Kevin,et al."The historical legacy of spatial scales in freeze-thaw weathering: Misrepresentation and resulting misdirection".GEOMORPHOLOGY 130.1-2(2011):83-90.
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