Lithospheric Sill Intrusions and Present‐Day Ground Deformation at Rhenish Massif, Central Europe

The Rhenish Massif in Central Europe, which includes the Eifel Volcanic Fields, has shown ongoing ground deformation and signs of possible unrest. A buoyant plume exerting uplift forces at the bottom of the lithosphere was proposed to explain such deformation; the hypothesis of (possibly concurrent)... View More