Structure, composition and significance of Medieval storm beach ridges at Caerlaverock, Dumfries and Galloway

Authors: Tipping, Richard; Adams, James

Source: Scottish Journal of Geology, Volume 43, Number 2, 2007 , pp. 115-123(9)

Publisher: Geological Society Publishing House

Key:
Free Content - Free Content
New Content - New Content
Subscribed Content - Subscribed Content
Free Trial Content - Free Trial Content

Abstract:

Synopsis

A set of four gravel beach ridges at Caerlaverock on the north shore of the Solway Firth are shown to have formed in the twelfth and thirteenth centuries ad, the most recent such deposits on this coast. They were investigated by geomorphological mapping, altitudinal survey, sediment stratigraphic and clast lithological analyses to establish their internal structure and sediment sources. Gravel clasts were in part transported from rock outcrops on the west side of the Nith Estuary, and this observation implies that the current estuarine sediment fills of the inner firth were then far less extensive. The data suggest that the Medieval period was one of major coastal change. Fluctuations in sediment supply are demonstrated from the clast lithological analyses which may relate to shifts in the directions of storm tracks.

Document Type: Miscellaneous

DOI: 10.1144/0036-9276/01-325

The full text electronic article is available for purchase. You will be able to download the full text electronic article after payment.

$38.34 plus tax      Refund Policy

 

OR

Back to top

Key:
Free Content - Free Content
New Content - New Content
Subscribed Content - Subscribed Content
Free Trial Content - Free Trial Content
Share this item with others: These icons link to social bookmarking sites where readers can share and discover new web pages.
Page Help Click here for Page Help
Shopping cart
Tools
Sign in






Need to register?
Sign up here
Text size: A | A | A | A