The Dry Valleys of Southern Victoria Land, Antarctica make up one of the oldest landscapes on earth. The question of the precise age and mode of landscape formation is essential to the understanding of past East Antarctic Ice Sheet Behaviours. There is evidence from buried desert pavements and in situ volcanic ashfalls that suggest that the dry valleys have remained in a hyper arid polar desert state since the middle Miocene 15 Ma. Contrary to this finding there is evidence from the Sirius Group Diamicts that suggest glaciaition occurred far later than this in the Pliocene (between 3.2 – 2.4 ma). These contradictory findings have created a polarised debate about landscape evolution and past ice sheet behaviours
Report submitted by Richard P. Goldthwait to the National Science Foundation.The University Archives...
The Antarctic Ice Sheets responded significantly to climatic conditions during the Last Glacial Maxi...
The aim is to investigate the evolution of the subglacial landscape of Antarctica using an ice sheet...
A case is made for the stability of the polar East Antarctic Ice Sheet since middle-Miocene time fro...
A widespread erosion surface passes across bedrock and sedimentary deposits in the western Dry Valle...
There are different views about the amount and timing of surface uplift in the Transantarctic Mounta...
The McMurdo Dry Valleys of Antarctica are the largest ice-free region in Antarctica. Valley downcutt...
The understanding of how soil properties develop and change over time can be used to date soil and t...
Investigations in Wright Valley, adjacent to the Transantarctic Mountains in East Antarctica, shed l...
Ice-free areas Antarctica reveal a multi-million year history of landscape evolution, but most atten...
We present 21Ne exposure ages of erosional glaciogenic rock surfaces on nunataks in northern Victori...
The hyper-arid, cryotic, wind-dominated conditions in the high-elevation McMurdo Dry Valleys of Anta...
Ice-free areas Antarctica reveal a multi-million year history of landscape evolution, but most atten...
The East Antarctic Ice Sheet (EAIS) has its origins ca. 34 million years ago. Since then, the impact...
Antarctic debris-covered glaciers are potential archives of long-term climate change. However, the g...
Report submitted by Richard P. Goldthwait to the National Science Foundation.The University Archives...
The Antarctic Ice Sheets responded significantly to climatic conditions during the Last Glacial Maxi...
The aim is to investigate the evolution of the subglacial landscape of Antarctica using an ice sheet...
A case is made for the stability of the polar East Antarctic Ice Sheet since middle-Miocene time fro...
A widespread erosion surface passes across bedrock and sedimentary deposits in the western Dry Valle...
There are different views about the amount and timing of surface uplift in the Transantarctic Mounta...
The McMurdo Dry Valleys of Antarctica are the largest ice-free region in Antarctica. Valley downcutt...
The understanding of how soil properties develop and change over time can be used to date soil and t...
Investigations in Wright Valley, adjacent to the Transantarctic Mountains in East Antarctica, shed l...
Ice-free areas Antarctica reveal a multi-million year history of landscape evolution, but most atten...
We present 21Ne exposure ages of erosional glaciogenic rock surfaces on nunataks in northern Victori...
The hyper-arid, cryotic, wind-dominated conditions in the high-elevation McMurdo Dry Valleys of Anta...
Ice-free areas Antarctica reveal a multi-million year history of landscape evolution, but most atten...
The East Antarctic Ice Sheet (EAIS) has its origins ca. 34 million years ago. Since then, the impact...
Antarctic debris-covered glaciers are potential archives of long-term climate change. However, the g...
Report submitted by Richard P. Goldthwait to the National Science Foundation.The University Archives...
The Antarctic Ice Sheets responded significantly to climatic conditions during the Last Glacial Maxi...
The aim is to investigate the evolution of the subglacial landscape of Antarctica using an ice sheet...