Controls on spatial and temporal patterns of slope deformation in an Alpine valley
Abstract
• Seasonal pore pressure variations in fractured crystalline hillslope induce correlated reversible surface deformations • Decameter-scale brittle-ductile faults control local spatial variations of deformation patterns • Cyclic groundwater pressure-related rock mass fatigue induces irreversible gravitationallydriven displacements in valley slopes *
Domains
Earth Sciences
Origin : Files produced by the author(s)