Skip to main content

Main menu

  • Home
    • Journal home
    • Lyell Collection home
    • Geological Society home
  • Content
    • Current issue
    • All issues
    • All collections
    • Supplementary publications
    • Open Access
  • Subscribe
    • GSL fellows
    • Institutions
    • Corporate
    • Other member types
  • Info
    • Librarians
    • Readers
    • Access for GSL Fellows
    • Access for other member types
    • Press office
    • Accessibility
    • Help
  • Alert sign up
    • eTOC alerts
    • RSS feeds
    • Newsletters
    • GSL blog
  • Geological Society of London Publications
    • Engineering Geology Special Publications
    • Geochemistry: Exploration, Environment, Analysis
    • Journal of Micropalaeontology
    • Journal of the Geological Society
    • Lyell Collection home
    • Memoirs
    • Petroleum Geology Conference Series
    • Petroleum Geoscience
    • Proceedings of the Yorkshire Geological Society
    • Quarterly Journal of Engineering Geology and Hydrogeology
    • Quarterly Journal of the Geological Society
    • Scottish Journal of Geology
    • Special Publications
    • Transactions of the Edinburgh Geological Society
    • Transactions of the Geological Society of Glasgow
    • Transactions of the Geological Society of London

User menu

  • My alerts
  • Log in
  • My Cart

Search

  • Advanced search
Transactions of the Geological Society of Glasgow
  • Geological Society of London Publications
    • Engineering Geology Special Publications
    • Geochemistry: Exploration, Environment, Analysis
    • Journal of Micropalaeontology
    • Journal of the Geological Society
    • Lyell Collection home
    • Memoirs
    • Petroleum Geology Conference Series
    • Petroleum Geoscience
    • Proceedings of the Yorkshire Geological Society
    • Quarterly Journal of Engineering Geology and Hydrogeology
    • Quarterly Journal of the Geological Society
    • Scottish Journal of Geology
    • Special Publications
    • Transactions of the Edinburgh Geological Society
    • Transactions of the Geological Society of Glasgow
    • Transactions of the Geological Society of London
  • My alerts
  • Log in
  • My Cart
  • Follow gsl on Twitter
  • Visit gsl on Facebook
  • Visit gsl on Youtube
  • Visit gsl on Linkedin
Transactions of the Geological Society of Glasgow

Advanced search

  • Home
    • Journal home
    • Lyell Collection home
    • Geological Society home
  • Content
    • Current issue
    • All issues
    • All collections
    • Supplementary publications
    • Open Access
  • Subscribe
    • GSL fellows
    • Institutions
    • Corporate
    • Other member types
  • Info
    • Librarians
    • Readers
    • Access for GSL Fellows
    • Access for other member types
    • Press office
    • Accessibility
    • Help
  • Alert sign up
    • eTOC alerts
    • RSS feeds
    • Newsletters
    • GSL blog

V. On Denudation in Scotland since Glacial Times

James Geikie
Transactions of the Geological Society of Glasgow, 3, 54-74, 1868, https://doi.org/10.1144/transglas.3.1.54
James Geikie
  • Find this author on Google Scholar
  • Search for this author on this site
PreviousNext
  • Article
  • Info & Metrics
  • PDF
Loading

Extract

Throughout the wide domain of geological inquiry, there is, perhaps, no subject of which it is easier to gain some idea, and yet at the same time more difficult to acquire an adequate conception, than Denudation. We all know how rains and frosts and chemical decomposition are employed unceasingly in modifying the aspect of hills and plains—how rivers are ever deepening and widening the valleys in which they flow—how the sea by its constant wave-action, aided by frosts and other agencies, tends to reduce to its own level the solid lands, with all their infinite variety of outline. It is no less generally known how the geological structure of a country must always influence its configuration—how the soft rocks will generally lie in the valleys, and those of a more durable nature occupy the heights—how the contour of the heights will vary according as these are formed of schists, of granite, of dolerite, or quartz-rock, or of any other well-marked species—and how this peculiar character is due to the unequal manner in which these various masses yield to the touch of the atmospheric forces:—so that a trained eye shall oftentimes detect, at a considerable distance, the nature of the rocks by reference to the contour of the hills alone. But while all are willing to admit that the subaerial agents may do something towards modifying the surface of a country, yet many will not allow that its straths and valleys have been mainly formed by these seemingly feeble forces. Nor

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

  • © The Geological Society of Glasgow

Please note that if you are logged into the Lyell Collection and attempt to access content that is outside of your subscription entitlement you will be presented with a new login screen. You have the option to pay to view this content if you choose. Please see the relevant links below for further assistance.

INDIVIDUALS

Log in using your username and password

– GSL fellows: log in with your Lyell username and password. (Please check your access entitlements at https://www.geolsoc.org.uk/fellowsaccess)
– Other users: log in with the username and password you created when you registered. Help for other users is at https://www.geolsoc.org.uk/lyellcollection_faqs
Forgot your username or password?

Purchase access

You may purchase access to this article for 24 hours and download the PDF within the access period. This will require you to create an account if you don't already have one. To download the PDF, click the 'Purchased Content' link in the receipt email.

LIBRARY USERS

Log in through your institution

You may be able to gain access using your login credentials for your institution. Contact your library if you do not have a username and password.
If your organization uses OpenAthens, you can log in using your OpenAthens username and password. To check if your institution is supported, please see this list. Contact your library for more details.
If you think you should have access, please contact your librarian or email [email protected]

LIBRARIANS

Administer your subscription.

CONTACT US

If you have any questions about the Lyell Collection publications website, please see the access help page or contact [email protected]

PreviousNext
Back to top

In this issue

Transactions of the Geological Society of Glasgow: 3 (1)
Transactions of the Geological Society of Glasgow
Volume 3, Issue 1
1868
  • Table of Contents
  • Table of Contents (PDF)
  • Index by author
  • Front Matter (PDF)
Alerts
Sign In to Email Alerts with your Email Address
Citation tools

V. On Denudation in Scotland since Glacial Times

James Geikie
Transactions of the Geological Society of Glasgow, 3, 54-74, 1868, https://doi.org/10.1144/transglas.3.1.54
James Geikie
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site

Citation Manager Formats

  • BibTeX
  • Bookends
  • EasyBib
  • EndNote (tagged)
  • EndNote 8 (xml)
  • Medlars
  • Mendeley
  • Papers
  • RefWorks Tagged
  • Ref Manager
  • RIS
  • Zotero
Permissions
View PDF
Share

V. On Denudation in Scotland since Glacial Times

James Geikie
Transactions of the Geological Society of Glasgow, 3, 54-74, 1 January 1868, https://doi.org/10.1144/transglas.3.1.54
del.icio.us logo Digg logo Reddit logo Twitter logo Facebook logo Google logo Mendeley logo
Email to

Thank you for sharing this Transactions of the Geological Society of Glasgow article.

NOTE: We request your email address only to inform the recipient that it was you who recommended this article, and that it is not junk mail. We do not retain these email addresses.

Enter multiple addresses on separate lines or separate them with commas.
V. On Denudation in Scotland since Glacial Times
(Your Name) has forwarded a page to you from Transactions of the Geological Society of Glasgow
(Your Name) thought you would be interested in this article in Transactions of the Geological Society of Glasgow.
CAPTCHA
This question is for testing whether or not you are a human visitor and to prevent automated spam submissions.
  • Tweet Widget
  • Facebook Like
  • Google Plus One
  • Article
  • Info & Metrics
  • PDF

Related Articles

Similar Articles

Cited By...

More in this TOC Section

  • IV.—An explosion-breccia — appinite complex at Gleann Chàrnan, Argyll
  • VII.—The Heads of Ayr Vent
  • Abstract of Proceedings of the one hundred and fifth session 1962-63
Show more: Papers
  • Most read
  • Most cited
Loading
  • Errata
  • ERRATA
  • ERRATA
  • ERRATA AND ADDENDA
  • XXXVI. Exhibition of Carboniferous fish remains
More...

Transactions of the Geological Society of Glasgow

  • About the journal
  • Supplementary Publications
  • Subscribe
  • Pay per view
  • Alerts & RSS
  • Copyright & Permissions
  • Activate Online Subscription
  • Feedback
  • Help

Lyell Collection

  • About the Lyell Collection
  • Lyell Collection homepage
  • Collections
  • Open Access Collection
  • Open Access Policy
  • Lyell Collection access help
  • Recommend to your Library
  • Lyell Collection Sponsors
  • MARC records
  • Digital preservation
  • Developing countries
  • Geofacets
  • Manage your account
  • Cookies

The Geological Society

  • About the Society
  • Join the Society
  • Benefits for Members
  • Online Bookshop
  • Publishing policies
  • Awards, Grants & Bursaries
  • Education & Careers
  • Events
  • Geoscientist Online
  • Library & Information Services
  • Policy & Media
  • Society blog
  • Contact the Society

 

Glasgow Geological Society logo

Published by The Geological Society of London, registered charity number 210161

Print ISSN 
0371-7224
Online ISSN 
2052-9422

Copyright © 2022 Geological Society of Glasgow