This dataset contains geomorphological data (measurements of size, shape, long axis orientation and weathering characteristics) on 90 erratic cobbles collected from the Hudson Mountains in West Antarctica. These were collected during three field campaigns, as follows: 1) 75 erratic cobbles collected by Joanne S Johnson during a British Antarctic Survey-supported geological field campaign undertaken in November-December 2019, as part of the International Thwaites Glacier Collaboration (funded by NERC and NSF). 2) 13 cobbles collected by James A Smith (British Antarctic Survey) in February and March 2010 during RV Polarstern cruise ANT XXVI/3, and 3) a further two cobbles collected in March 2006 by Johnson during RV Polarstern cruise ANT XXIII/4. These cobbles were all collected for surface exposure dating. Funding: NERC grant: NE/S006710/1

This dataset contains locations and orientations of striations observed on bedrock surfaces in the Hudson Mountains, West Antarctica. These were collected in December 2019 by Joanne S Johnson during a British Antarctic Survey-supported geological field campaign, as part of the International Thwaites Glacier Collaboration (funded by NERC and NSF). Funding: NERC grant: NE/S006710/1

This dataset contains data from three ground-penetrating radar surveys undertaken to image ice thickness and englacial stratigraphy during the 2019-20 Antarctic field season, as part of the International Thwaites Glacier Collaboration (funded by NERC and NSF). The ground-penetrating radar data are presented as SEG-Y, along with the GPS tracks of the surveys, presented as GPS Exchange Format (GPX). The subglacial extensions of ridges of three nunataks close to Pine Island and Larter Glaciers in the Hudson Mountains region were surveyed, with the aim of determining their suitability as subglacial bedrock drill sites. Those nunataks are Winkie Nunatak (74 degrees 51'' 41.0" S/99 degrees 46'' 49.4" W), Evans Knoll (74 degrees 51'' 00.0" S/100 degrees 25'' 00.0" W), and Webber Nunatak (74 degrees 47'' 00.0" S/99 degrees 50'' 00.0" W). This work was funded by NERC grants NE/S00663X/1 and NE/S006710/1.