Creep, Soil Erosion, Landslides & Deformation

Creep, in geology, slow downslope movement of particles that occurs on every slope covered with loose, weathered material. Even soil covered with close-knit sod creeps downslope, as indicated by slow but persistent tilting of trees, poles, gravestones, and other objects set into the ground on

Active Tectonics at UC Berkeley

OU hazards geologist leads NASA-funded study

Study on deformation characteristics and mechanism of reactivated ancient landslides induced by engineering excavation and rainfall in Three Gorges Reservoir area

Remote Sensing, Free Full-Text

GeoNet: News

Deformation instability mechanism of slope in Fa'er Town, Shuicheng County, Guizhou, China - ScienceDirect

NHESS - Changes in ground deformation prior to and following a large urban landslide in La Paz, Bolivia, revealed by advanced InSAR

Creep, Soil Erosion, Landslides & Deformation

Mass movement/ mass wasting/ soil creep/ landslide

Failure mechanism, existing constitutive models and numerical modeling of landslides in sensitive clay: a review, Geoenvironmental Disasters

The deformation phenomena on the landslide mass: (a) slump of TH1, (b)

Slope stability - Wikipedia

A Mass Movement in the Blue Ridge - The William & Mary Blogs

Geological Society - By Gravity

Earth Surface Processes and Landforms, Geomorphology Journal