Abstract
A ridge of drift emerging from the snout of Flatisen resembles a small esker. It originates in a subglacial tunnel. The source of the material forming the ridge was a number of thrust planes exposed in the sides and roof of the tunnel. The main features of the tunnel and the ridge are described and the mode of formation of the ridge suggested.
Publisher
Cambridge University Press (CUP)
Cited by
10 articles.
订阅此论文施引文献
订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献