Thermal-contraction-crack networks as evidence for late-pleistocene permafrost in inner Mongolia, China

Numerous wedges on the Ordos Plateau show typical characteristics of periglacial sand wedges that enable them to be distinguished from desiccation cracks in clayey illuviation soil horizons. The sand wedges are organized in two generations of polygonal networks. The older generation is a large-scale...

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Bibliographic Details
Published in:Permafrost and Periglacial Processes
Main Authors: Vandenberghe, J, Cui, ZJ, Liang, Z, Wei, Z
Other Authors: Vandenberghe, J (reprint author), Free Univ Amsterdam, Fac Earth & Life Sci Quaternary Geol & Geomorphol, De Boelelaan 1085, NL-1081 BT Amsterdam, Netherlands., Free Univ Amsterdam, Inst Earth Sci, NL-1081 HV Amsterdam, Netherlands., Peking Univ, Dept Geog, Beijing 100871, Peoples R China., Chinese Acad Sci, Inst Earth Environm, Xian 700715, Peoples R China., Free Univ Amsterdam, Fac Earth & Life Sci Quaternary Geol & Geomorphol, De Boelelaan 1085, NL-1081 BT Amsterdam, Netherlands.
Format: Journal/Newspaper
Language:English
Published: permafrost and periglacial processes 2004
Subjects:
sand wedges
inner Mongolia
permafrost
last glacial maximum
palaeoclimate
SAND VEINS
WEDGES
FEATURES
AGE
ICE
Ice
Permafrost and Periglacial Processes
wedge*
Online Access:https://hdl.handle.net/20.500.11897/255716
https://doi.org/10.1002/ppp.476
Description
Summary:Numerous wedges on the Ordos Plateau show typical characteristics of periglacial sand wedges that enable them to be distinguished from desiccation cracks in clayey illuviation soil horizons. The sand wedges are organized in two generations of polygonal networks. The older generation is a large-scale network with a diameter of 8 to 9 m and wedge depths up to more than 2 m. The younger generation has a mean diameter of 3 to 4m and is formed within the large networks. It consists of shallow (0.6 to 1 m deep) but relatively wide wedges. In contrast to the typical sand wedges that form within continuous permafrost, the shallow wedges formed probably as 'ground wedges' by seasonal freezing. Ice wedges and cryoturbations developed only rarely, and exclusively in the most humid areas. Thermal-contraction cracking occurred mainly between 26 and 20ka BP, indicating mean annual temperatures at least 13degreesC lower than present. Before and after that period mean annual temperatures were at least 7 to 8.5degrees lower than today. The presence of these periglacial phenomena show that the southern limit of continuous permafrost in Inner Mongolia occurred south of 38degreesN during the Last Glacial Maximum. Copyright (C) 2004 John Wiley Sons, Ltd. Geography, Physical Geology SCI(E) 0 ARTICLE 1 21-29 15

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