Abstract
The results of two surveys of the frontal margin of a valley glacier in West Greenland are reported. If they indicate a constant or decreasing mass loss rate, the glacier shows similar behaviour to that of the nearby ice lobes on the ice sheet.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
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
