Glaciation and deglaciation, along with their associated climatic and non-climatic processes,
modify slope stresses and influence slope stability. Paraglacial slope failures are those that …

Deep seated gravitational slope deformations (DSGSD) are widespread phenomena,
recognized in different mountain ranges worldwide. The distribution of such phenomena at …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

Climate change, manifested by an increase in mean, minimum, and maximum temperatures
and by more intense rainstorms, is becoming more evident in many regions. An important …

Cycles of glaciation impose mechanical stresses on underlying bedrock as glaciers
advance, erode, and retreat. Fracture initiation and propagation constitute rock mass …

Earth's climate is warming and will continue to warm as the century progresses. High
mountains and high latitudes are experiencing the greatest warming of all regions on Earth …

The ages of 31 postglacial rock-slope failures (RSFs) in Scotland and NW Ireland, derived
from 89 cosmogenic isotope exposure ages, are employed to analyse the temporal pattern …

The present time is one significant stage in the adjustment of mountain slopes to climate
change, and specifically atmospheric warming. This review examines the state of …

We describe and model the evolution of a recent landslide, tsunami, outburst flood, and
sediment plume in the southern Coast Mountains, British Columbia, Canada. On November …

Large landslides and deep-seated gravitational slope deformations (DSGSD) represent an
important geo-hazard in relation to the deformation of large structures and infrastructures …