This Honours project involved seismic and ground penetrating radar (GPR) investigations on the surface of the Sorsdal Glacier, Antarctica, to investigate ice thickness, the thickness of the underlying ocean water and potential englacial drainage networks. The seismic measurements successfully imaged the base of the floating ice sheet and the underlying water column through up to 1 km of glacial ice and confirmed the position of the glacier grounding line. GPR measurements detected reflective features in the upper 20 m of the glacier that were modelled as either water-filled or air-filled englacial drainage channels. The results of this GPR part of this project are currently being prepared for publication in the Journal of Glaciology.