Click here to find out more about the Society - the logo is the Ordovician 'orthid' brachiopod Nicolella actoniae          

 

  Help
Current Proceedings of the Shropshire Geological Society (2010) Table of Contents
The Society
 Publications
Newsletter
Trail Guides
Resources
Links
 

 

 

 

 

ISSN 1750-855X (Print)
ISSN 1750-8568 (Online)

Annual compilations of the Proceedings will be published from the papers that appear on this page. Please respect the copyright of the authors. The contents of the Proceedings are made available to assist personal research and to increase understanding of Shropshire's geology. If you find them of interest and would like to contribute to assist further publication, please send your donation to the SGS Treasurer, David HT Smith:
25 Grange Road, Shrewsbury, SY3 9DG

Cheques should be made payable to:  

The Shropshire Geological Society.

 

Click button for

summary of text

Table of Contents for the Current Proceedings of the Shropshire Geological Society [to be published after 2010]

Fuller, J.G.C.M. & Torrens, H.S. (2010). Murchison in the Welsh Marches: a History of Geology Group field excursion led by John Fuller, May 8th - 10th, 1998. 16pp.

Pannett, D. (2010). Glacial Meltwater Channels of the Stiperstones Area. 3pp.

 

 

 

To view the full text as an Adobe file, click the PDF symbol below:

Summaries of papers

[3.137 MB]

Fuller, J.G.C.M. & Torrens, H.S. (2010). Murchison in the Welsh Marches: a History of Geology Group field excursion led by John Fuller, May 8th - 10th, 1998. p.1-16.

Within the field area of the Welsh Marches, centred on Ludlow, the excursion considered the work of two pioneers of geology: Arthur Aikin (1773-1854) and Robert Townson (1762-1827), and the possible train of geological influence from Townson to Aikin, and Aikin to Murchison, leading to publication of the Silurian System in 1839.

[0.068 MB]

Pannett, D. (2010). Glacial Meltwater Channels of the Stiperstones Area. p.17-19.

Consideration of recent contour maps reveals that glacial meltwater channels in the Stiperstones and Long Mynd areas have elevations compatible with an ice margin sloping from west to east cutting across SW-NE ridges where they would have dammed water in the heads of the valleys, forcing some flow across cols in the main watershed. Such channels suggest that ice once lapped around the Stiperstones to a height of at least 330 m.

 

 

Annual compilations of the Proceedings are printed and distributed to the major geological libraries and resource centres where they may be accessed. Click here for contact details.

Both high resolution digital and printed copies may be obtained through Scenesetters, who will be happy to provide current charges and process your order.

 

To cite an article from this publication:
Pannett, D. (2010). Glacial Meltwater Channels of the Stiperstones Area. Proceedings of the Shropshire Geological Society15, 17-19. ISSN 1750-855X (Print), ISSN 1750-8568 (Online) [Online at www.shropshiregeology.org.uk/SGSpublications; printed copy in press]
 

2010 The Shropshire Geological Society

Click here for Terms and Conditions concerning the copyright of the material presented here.