Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
  Journal of the Geological Society   Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Journal of the Geological Society; December 1997; v. 154; no. 6; p. 1087-1088; DOI: 10.1144/gsjgs.154.6.1087
© 1997 Geological Society of London
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Article

Discussion on indications of glaciation at the base of the Proterozoic Stoer Group (Torridonian), NW Scotland

S. Davison & M. J. Hambrey reply: We thank A.D. Stewart for his stimulating comments regarding our recent paper on Torridonian glacial deposits. However, there are several differences of observations and interpretations which need to be resolved.

(i) Roches moutonnées and stratigraphic relationships. The gneiss ridges shown in Stewart's fig. 1 are not, as he correctly observes, parallel and are not aligned in the direction of the proposed ice-flow. However, roches moutonnées do not necessarily have to be parallel to flow direction; indeed many are transverse. The critical observation is the contrast between up-glacier facing slopes, which are relatively smooth, and down-glacier slopes which are fractured. There is also a marked difference in clast size between the two slopes, those on the up-glacier side being generally smaller than those on the down-glacier side. We are unsure of the purpose of Stewart's fig. 2. It certainly shows the irregular nature of the Stoer Group/Lewisian contact, but this is a reflection of differential weathering/erosion of a foliated gneiss, whereas our photograph (fig. 3a) illustrates the form more clearly.

The suggestion that the ice smoothed surface in our fig. 3a is ‘far from smooth’ is, we feel, misleading. Whilst it is not flat and polished, it is rounded and, in a geomorphological sense, is smooth. It is certainly of a much smoother and lower profile than the surface on the SW side of this feature, which is brecciated with a matrix of Torridonian sediments.

The interpretation of these features as roches moutonnées is

...

This 250-word extract was created in the absence of an abstract.




This article has been cited by other articles:


Home page
Geological MagazineHome page
R.C. Selley
STEWART, A. D. 2002. The Later Proterozoic Torridonian Rocks of Scotland: their Sedimentology, Geochemistry and Origin.: Geological Society Memoir no. 24. vi + 130 pp. London, Bath: Geological Society of London. Price {pound}70.00, US $117.00; members' price {pound}35.00, US $58.00; AAPG members' price {pound}42.00, US $70.00 (paperback). ISBN 1 86239 103 3.
Geological Magazine, May 1, 2003; 140(3): 358 - 359.
[Full Text] [PDF]


Home page
Geological Society, London, MemoirsHome page
References
Geological Society, London, Memoirs, January 1, 2002; 24(1): 119 - 125.
[PDF]


Home page
Journal of the Geological SocietyHome page
G. M. YOUNG
Some aspects of the geochemistry, provenance and palaeoclimatology of the Torridonian of NW Scotland
Journal of the Geological Society, December 1, 1999; 156(6): 1097 - 1111.
[Abstract] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2009 by Geological Society of London