  Geological fault systems, as the San Andreas fault (SAF) in USA, constitute
typical examples of self-organizing systems in nature. In this paper, we have
considered some geophysical properties of the SAF system to test the viability
of the nonextensive models for earthquakes developed in [Phys. Rev. E {\bf 73},
026102, 2006]. To this end, we have used 6188 earthquakes events ranging in the
magnitude interval $2 < m < 8$ that were taken from the Network Earthquake
International Center catalogs (NEIC, 2004-2006) and the Bulletin of the
International Seismological Centre (ISC, 1964-2003). For values of the Tsallis
nonextensive parameter $q \simeq 1.68$, it is shown that the energy
distribution function deduced in above reference provides an excellent fit to
the NEIC and ISC SAF data.
