In this study we compare the effective thickness of the locked zone derived from seismicity with the thickness derived from geodesy to quantitatively measure the similarities and differences in the two approaches along the SAFS (San Andreas Fault System).

In this paper are reported results from geomorphic and paleoseismological investigations of the Crescent fault (Nevada) and discuss their implications for models of fault system dynamics.

<p>In this article, it is reviewed some of the remarkable observations of the earthquake cycle already made using radar interferometry and speculate on breakthroughs that are tantalizingly close.</p>