Salameh, E. and Tarawneh, A. (2026) Tectonic Structures and Their Consequential Nontectonic Deformations —The Case of the ...

Geologic faults or simply faults are planar rock fractures which show evidence of relative movement. Large faults within the Earth's crust are the result of shear motion and active fault zones are the ...

A fault slicing across Turkey has long been a textbook example of how tectonic plates grind past one another, yet the headline promise that it is “overturning decades of geology” cannot be verified ...

Last week I gave a walking tour of the Hayward fault along the Oakland-Berkeley border. Among other things, I talked about the fault’s peculiar behavior called aseismic creep, in which the two sides ...