Abstract
The jagged peaks, knife-edged ridges, and steep-sided valleys of alpine landscapes are well known products of glaciation, yet little is known about how the dynamics of ice flow and glacial erosion give rise to such landforms. By linking a finite-element model for ice flow through a valley with a model for glacial erosion, we have simulated the gradual evolution of one of the most striking of glacial landforms, the U-shaped valley. Incorporating realistic glacier sliding laws and spatial variations in rock resistance, our simulations illustrate how ice flow, erosion patterns and topography interact in the long term evolution of glacial landforms. In addition, our results indicate for the first time that the formation of a steady-state U-shaped valley takes approximately 105 years.
Sign-in/Register to access full text options 
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
