Glacial history of interior Jameson Land, East Greenland

The plateaus between 400 and 800 m a.s.l. around the water‐divides on central and eastern Janieson Land are covered by the ‘Jameson Land Drift’ up to 50 m thick glacial. placiotluvial and glaciolacustrine deposits. A high content of far‐travelled wcsterii rocks indicates the overriding by extensive...

Full description

Bibliographic Details
Published in:Boreas
Main Authors: MöLLER, PER, HJORT, CHRISTIAN, ADRIELSSON, LENA, SALVIGSEN, OTTO
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 1994
Subjects:
Online Access:http://dx.doi.org/10.1111/j.1502-3885.1994.tb00604.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1502-3885.1994.tb00604.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1502-3885.1994.tb00604.x