More than 800 million people live in proximity to active volcanoes and could be directly
impacted by potential eruptions. Mitigation of future volcanic hazards requires adequate …

Glacial isostatic adjustment (GIA) describes the response of the solid Earth, the gravitational
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …

Recent measurements of surface vertical displacements of the European Alps show a
correlation between vertical velocities and topographic features, with widespread uplift at …

Understanding the interactions between surface and deep Earth processes is important for
research in many diverse scientific areas including climate, environment, energy …

The driving mechanisms of Earth's climate system at a multi-Myr timescale have received
considerable attention since the 1980's as they are deemed to control large-amplitude …

The Canadian Cordillera hosts numerous Pleistocene and Holocene volcanoes and
volcanic deposits, including a number of volcanoes that have erupted within the last several …

Between 5 and 6 million years ago, during the so-called Messinian salinity crisis, the
Mediterranean basin became a giant salt repository. The possibility of abrupt and kilometre …

Surface processes and magmatism condition the structural evolution of continental rifts and
passive margins through mechanical and thermal effects on the lithosphere rheology …

Established theories ascribe much of the observed long‐term Cenozoic climate cooling to
atmospheric carbon consumption by erosion and weathering of tectonically uplifted terrains …

Glacial loading and unloading can influence the rates and timing of magmatism in tectonic
settings where the lithosphere is relatively thin and hot. In continental arcs, where the …