Multiple ice age cycles spanning the last three million years have fundamentally transformed
the Arctic landscape. The cadence, intensity and pattern of this glacial modification underpin …

The present review paper is an attempt to summarize quantitative evidence of Late
Cenozoic changes in topographic relief. Different meanings of the word “relief”, as it is …

Abstract The Otavi Group is a Neoproterozoic carbonate‐dominated succession up to 4 km
thick, which blankets the southern promontory of the Congo craton in northern Namibia. This …

Many studies of elevated, passive continental margins (EPCMs) assume that their
characteristic, large-scale morphology with high-level plateaux and deeply incised valleys …

Fjords are glacially carved estuaries that profoundly influence ice-sheet stability by draining
and ablating ice. Although abundant on modern high-latitude continental shelves, fjord …

The rugged topography of mountain ranges represents a special challenge to computational
ice sheet models simulating past or present glaciations. In mountainous regions, the …

Time-dependent rock deformation affects both natural processes happening on the
geological time scale and subsurface engineering operations. We perform a series of …

Abstract In southern East Greenland (68–70° N), voluminous flood basalts erupted onto a
largely horizontal lava plain near sea level at the Paleocene–Eocene transition when sea …

In 1874, JW Judd, a leading British geologist, wrote:“In the Hebrides I will now show that we
have supplied to us that great geological desideratum–a number of volcanoes so dissected …

We present observations that demonstrate that the elevated passive margins around the
North Atlantic were formed by episodic, post-rift uplift movements that are manifest in the …