Martin Margold
0000-0001-5834-850X
Přírodovědecká Fakulta, Univerzita Karlova
51 papers found
Refreshing results…
Ice flow dynamics of the northwestern Laurentide Ice Sheet during the last deglaciation
Supplementary material to "Ice flow dynamics of the northwestern Laurentide Ice Sheet during the last deglaciation"
Deglaciation of the north American ice sheet complex in calendar years based on a comprehensive database of chronological data: NADI-1
Evaluation of the role of the Baltic depression during deglaciation of the last Scandinavian Ice Sheet; a landform-driven investigation
Supplementary material to "Evaluation of the role of the Baltic depression during deglaciation of the last Scandinavian Ice Sheet; a landform-driven investigation"
Absence of Large‐Scale Ice Masses in Central Northeast Siberia During the Late Pleistocene
Dynamical response of the southwestern Laurentide Ice Sheet to rapid Bølling-Allerød warming
East Siberian glaciers have contracted over the last two glacial cycles
Recent Intensification (2004–2020) of Permafrost Mass‐Wasting in the Central Mackenzie Valley Foothills Is a Legacy of Past Forest Fire Disturbances
The collapse of the Cordilleran–Laurentide ice saddle and early opening of the Mackenzie Valley, Northwest Territories, Canada, constrained by 10Be exposure dating
Supplementary material to "The collapse of the Laurentide-Cordilleran ice saddle and early opening of the Mackenzie Valley, Northwest Territories, constrained by 10Be exposure dating"
The collapse of the Laurentide-Cordilleran ice saddle and early opening of the Mackenzie Valley, Northwest Territories, constrained by 10Be exposure dating
Reconstructing the advance and retreat dynamics of the central sector of the last Cordilleran Ice Sheet
New ice margin chronology for the last deglaciation of the North American Ice Sheet Complex
Ice stream dynamics and ice margin retreat of the last Laurentide Ice Sheet in the Northwest Territories, Canada
Catastrophic Drainage From the Northwestern Outlet of Glacial Lake Agassiz During the Younger Dryas
Using10Be dating to determine when the Cordilleran Ice Sheet stopped flowing over the Canadian Rocky Mountains
The response of North American ice sheets to the Younger Dryas (12.9 ka to 11.7 ka) climate event
The deglacial dynamics of the Laurentide and Cordilleran ice sheets in the Mackenzie Mountains, Northwest Territories, Canada
Deglaciation of the central sector of the Cordilleran Ice Sheet in northern British Columbia
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