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The origin and significance of mushroom stones in lowland karst regions
Author(s)
Date Issued
2002
Date Available
2009-02-02T15:16:33Z
Abstract
'Mushroom stones', or 'wave stones', are limestone erratics or protruding bedrock that shows signs of erosion or dissolution suggestive of prolonged exposure to standing water. Fifty-three stones in the central lowlands of Ireland were recorded in a systematic fashion, with accurate lip-height measurements taken for more than half the stones using GPS (Global Positioning System) equipment. The heights of their erosional lips are discussed with reference to estimated pre-bog water tables, lake fluctuations and other possible
explanations for this phenomenon. The results suggest that the erosion of the stones now found in the bogs of County Offaly cannot be attributed to erosion
by a single large lake as previously speculated, whereas the notching of stones
in and around wetlands and lakes in Roscommon and Clare is likely to be due
largely to flooding and winter water levels.
explanations for this phenomenon. The results suggest that the erosion of the stones now found in the bogs of County Offaly cannot be attributed to erosion
by a single large lake as previously speculated, whereas the notching of stones
in and around wetlands and lakes in Roscommon and Clare is likely to be due
largely to flooding and winter water levels.
Type of Material
Journal Article
Publisher
Royal Irish Academy
Journal
Irish Journal of Earth Sciences
Volume
20
Start Page
33
End Page
40
Copyright (Published Version)
Copyright Royal Irish Academy
Subject – LCSH
Formations (Geology)--Ireland
Limestone--Ireland
Limestone--Erosion--Ireland
Web versions
Language
English
Status of Item
Peer reviewed
ISSN
0790-1763
This item is made available under a Creative Commons License
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dunnel_article_pub_017.pdf
Size
417.42 KB
Format
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