Tuesday, November 24 @ 10:30, Building 20 - Tweto Room B-1207
Formation of Sheeting Joints – a New View
Stephen Martel, University of Hawaii at Manoa
A fundamental relationship, derived from the equation of static equilibrium, illuminates how the shape of a curved traction-free surface, the surface-parallel stresses, and gravitational body forces contribute to fracturing subparallel to the surface. A surface-normal tension arises if σ11k1 + σ22k2 > ρg cosβ, where k1 and k2 are the principal curvatures at the surface, σ11 and σ22 are the normal stresses parallel to the respective principal curvature arcs, ρ is material density, g is gravitational acceleration, and β is the slope. This general result, valid for any solid, explains why sheeting joints (prominent opening mode rock fractures subparallel to the topographic surface) develop where compressive stresses parallel to the surface are sufficiently high (negative) and at least one principal curvature is sufficiently convex (negative). Among other things, this relationship also could be used to predict where particular dangerous fractures would be in slopes prone to rock fall.
Hosted by the USGS Geologic Discipline, Earth Surface Processes Team. For questions or to talk to Steve during his visit, please contact Scott Minor, 303-236-0303, sminor@usgs.gov
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