Articles | Volume 19, issue 1 
            
                
                    
            
            
            https://doi.org/10.5194/tc-19-303-2025
                    © Author(s) 2025. This work is distributed under 
the Creative Commons Attribution 4.0 License.
                the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-19-303-2025
                    © Author(s) 2025. This work is distributed under 
the Creative Commons Attribution 4.0 License.
                the Creative Commons Attribution 4.0 License.
Assessing the suitability of sites near Pine Island Glacier for subglacial bedrock drilling aimed at detecting Holocene retreat–readvance
                                            British Antarctic Survey, Cambridge, CB3 0ET, UK
                                        
                                    John Woodward
                                            Department of Geography and Environmental Sciences, Northumbria University, Newcastle-upon-Tyne, NE1 8ST, UK
                                        
                                    Ian Nesbitt
                                            School of Earth and Climate Sciences and the Climate Change Institute, University of Maine, Orono, ME 04469, USA
                                        
                                    Kate Winter
                                            Department of Geography and Environmental Sciences, Northumbria University, Newcastle-upon-Tyne, NE1 8ST, UK
                                        
                                    Seth Campbell
                                            School of Earth and Climate Sciences and the Climate Change Institute, University of Maine, Orono, ME 04469, USA
                                        
                                    Keir A. Nichols
                                            Department of Earth Science and Engineering, Imperial College London, London, SW7 2AZ, UK
                                        
                                    Ryan A. Venturelli
                                            Department of Geology and Geological Engineering, Colorado School of Mines, Golden, CO 80401, USA
                                        
                                    Scott Braddock
                                            School of Earth and Climate Sciences and the Climate Change Institute, University of Maine, Orono, ME 04469, USA
                                        
                                    Brent M. Goehring
                                            Los Alamos National Laboratory, Los Alamos, NM 87545, USA
                                        
                                    Brenda Hall
                                            School of Earth and Climate Sciences and the Climate Change Institute, University of Maine, Orono, ME 04469, USA
                                        
                                    Dylan H. Rood
                                            Department of Earth Science and Engineering, Imperial College London, London, SW7 2AZ, UK
                                        
                                    Greg Balco
                                            Lawrence Livermore National Laboratory, P.O. Box 808, Livermore, CA 94551, USA
                                        
                                    
                                            Berkeley Geochronology Center, Berkeley, CA 94709, USA
                                        
                                    Data sets
Ground-penetrating radar surveys at three nunataks in the Hudson Mountains in the Amundsen Sea sector of West Antarctica, December 2019 John Woodward and Joanne S. Johnson https://doi.org/10.5285/9555694e-c9f5-4bf8-a556-2ad9d29e55c6
Short summary
            Determining where and when the Antarctic ice sheet was smaller than present requires recovery and exposure dating of subglacial bedrock. Here we use ice sheet model outputs and field data (geological and glaciological observations, bedrock samples, and ground-penetrating radar) to assess the suitability for subglacial drilling of sites in the Hudson Mountains, West Antarctica. We find that no sites are perfect, but two are feasible, with the most suitable being Winkie Nunatak (74.86°S, 99.77°W).
            Determining where and when the Antarctic ice sheet was smaller than present requires recovery...
            
         
 
             
             
             
            