Striae and former ice-flow directions in Snowdonia, North Wales

Auteurs :
GEMMELL, C.
SMART, D.
SUGDEN, D.

Description :
The striation pattern reflects ice flow radiating from the general vicinity of Snowdon summit and the strong eastward component of flow contradicts the idea that the Welsh ice sheet overran the area.


Type de document :
Article de périodique

Source :
The geographical journal London, 1986, vol. 152, n°. 1, p. 19-29, Références bibliographiques : 10 réf.

Date :
1986