Folded thrust faults, windows, and klippen using glass bead decollements @TheGeoModels
Folded thrust faults, windows, and klippen using glass bead decollements  @TheGeoModels
Uploaded May 2016 | Updated September 2026, 2 days ago
This model is patterned after the work of Jacques Malavieille and colleagues at Géosciences Montpellier, Université of Montpellier II. Glass beads (used for sandblasting) act as weak decollement horizons which activate due to the high basal friction provided by a sheet of 150 grit sandpaper atop the basal plastic sheet. Slip in the decollements forms high-displacement, nearly flat thrusts, which fold due to subsequent footwall deformation resulting from erosion of the wedge. Erosion into a wedge of this structural style produces a landscape of windows and klippen, even without significant topographic relief.
Folded thrust faults, windows, and klippen using glass bead decollementsWhy do these Siberian lakes look like eyes?Appalachian Field Trip - Stop 6Erosional landscapes: Influence of rock strength and structure on landformsWhy do debris flow landslides move like rivers of rock and mud?Restraining and releasing bends with erosion during deformation...and cross sectionsFold-thrust belt topography: The Ouachita Mountains, whetstone capital of the worldThe weird connection between fish genetics and Gulf oil and gasDevelopment of transverse rivers in exhumed fold/thrust beltsIndentor concept: Why the fold/thrust belt models use the grey foam pusherAn ancient impact crater is doing WEIRD things to this towns water supplyRollover anticline with inversion
TheGeoModels |

Folded thrust faults, windows, and klippen using glass bead decollements

SHARE TO X SHARE TO REDDIT SHARE TO FACEBOOK WALLPAPER