This revised and updated edition continues to provide a comprehensive introduction to the
subject, exploring the world's landforms from a broad systems perspective. It covers the …

A distinct boundary between unweathered and weathered rock that moves downward as
weathering proceeds—the weathering front—is explicitly or implicitly part of landscape …

Although continental weathering intensity has been invoked as a primary control on
biogeochemistry, tectonics, and the carbon cycle throughout geologic history, it remains …

In Fennoscandia, the process of Glacial Isostatic Adjustment (GIA) drives ongoing crustal
deformation. Crustal velocities from GPS observations have proved to be a useful tool in …

Abstract In Fennoscandia, tectonics, Glacial Isostatic Adjustment (GIA), and climatic changes
cause ongoing crustal deformation of some millimetres per year, both vertically and …

Present-day catchments adjacent to sedimentary basins may preserve geomorphic
elements that have been active through long intervals of time. Relicts of ancient catchments …

As part of the recent discoveries on the Utsira High (Edvard Grieg and Johan Sverdrup
fields), altered and fractured basement rocks were for the first time shown to act as a …

Fractured crystalline basement reservoirs (basement) on the UK Continental Shelf (UKCS)
and the Norwegian Continental Shelf (NCS) have been underexplored. Over the last 12 …

We investigate the influence of the glacial isostatic adjustment (GIA) on the deformation at
the surface and at seismogenic depths in Fennoscandia. The surface strain rate field …

This paper summarises developments in understanding sea level change during the
Quaternary in Scotland since the publication of the Quaternary of Scotland Geological …