Distribution and morphology of pingos, western Canadian Arctic, Northwest Territories, Canada
Pingos are perennially-frozen ice-cored hills, formed primarily by progressive injection and freezing of water within aggrading permafrost. Pingos of the
All posts by Jan Franssen
Annual and decadal net morphological displacement of a small gravel‐bed channel
When a river adjusts its shape over longer timescales, it is no longer in equilibrium with its environment. These ‘disequilibrium
Intra- and Inter-site variability of the beach dune profile and vegetation line: Is there a scale-invariant profile?
The oft-cited Coastal Dune Model (CDM) predicts that dune height is controlled by negative feedback between wind flow and topography
Ice-flow and deglacial history of the Laurentide Ice Sheet in the southwestern Great Slave Lake area
The latest data on the glacial and deglacial history of the southwest Great Slave Lake region, NWT. The Laurentide Ice
Geomorphic implications of contemporary sand wedges in seasonally frozen ground
Recent study sheds new light on the environmental conditions necessary for sand wedge formation. Sand wedges are cold-climate features formed