Formation of mega-scale glacial lineations far inland beneath the onset of the Northeast Greenland Ice Stream

Charlotte M. Carter, Steven Franke, Daniela Jansen, Chris R. Stokes, Veit Helm, John Paden, and Olaf Eisen

Viewed

Total article views: 1,059 (including HTML, PDF, and XML)

HTML	PDF	XML	Total	BibTeX	EndNote
846	193	20	1,059	39	35

HTML: 846
PDF: 193
XML: 20
Total: 1,059
BibTeX: 39
EndNote: 35

Views and downloads (calculated since 05 May 2025)

Month	HTML	PDF	XML	Total
May 2025	94	35	3	132
Jun 2025	70	62	3	135
Jul 2025	89	55	8	152
Aug 2025	146	4	0	150
Sep 2025	410	26	5	441
Oct 2025	37	11	1	49

Cumulative views and downloads (calculated since 05 May 2025)

Month	HTML	PDF	XML	Total
May 2025	94	35	3	132
Jun 2025	70	62	3	135
Jul 2025	89	55	8	152
Aug 2025	146	4	0	150
Sep 2025	410	26	5	441
Oct 2025	37	11	1	49

Viewed (geographical distribution)

Total article views: 1,059 (including HTML, PDF, and XML) Thereof 1,059 with geography defined and 0 with unknown origin.

Country	#	Views	%


Total:	0
HTML:	0
PDF:	0
XML:	0


Total:	0
HTML:	0
PDF:	0
XML:	0

Latest update: 30 Oct 2025

Short summary

The subglacial landforms beneath actively fast-flowing ice in Greenland have not been explored in detail, as digital elevation models have not had a high enough resolution to see these features. We use swath radar imaging to visualise landforms at the onset of an ice stream, revealing mega-scale glacial lineations, that would usually be assumed to be indicative of faster ice flow than the current velocities. Interpretation of the landscape also gives an indication of the properties of the bed.