Glaciers and ice sheets erode mountains and produce vast quantities of sediments that are
delivered to rivers and oceans, impacting global sediment and biogeochemical balances …

Closed topographic basins are found beneath contemporary ice masses and within the
footprint of former ice masses in all glaciated regions. We present the first integrated review …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

The height of mountain ranges reflects the balance between tectonic rock uplift, crustal
strength and surface denudation. Tectonic deformation and surface denudation are …

We present a reconstruction of the Antarctic topography at the Eocene–Oligocene (ca.
34Ma) climate transition. This provides a realistic key boundary condition for modeling the …

The first Cenozoic ice sheets initiated in Antarctica from the Gamburtsev Subglacial
Mountains and other highlands as a result of rapid global cooling∼ 34 million years ago. In …

We review the geomorphological, sedimentological and chronological evidence for palaeo-
ice streams on the continental shelf of Antarctica and use this information to investigate …

Ice-sheet development in Antarctica was a result of significant and rapid global climate
change about 34 million years ago. Ice-sheet and climate modelling suggest reductions in …

Ice-marginal moraines are often used to reconstruct the dimensions of former ice masses,
which are then used as proxies for palaeoclimate. This approach relies on the assumption …

The aim is to investigate the evolution of the subglacial landscape of Antarctica using an ice
sheet and erosion model. We identify different stages of continental glaciation and model the …