On february 27, 2010, the south central coast of Chile (ca., 34-39 degrees S) was affected by an earthquake magnitude Mw= 8,8, with the epicenter located offshore Cobquecura (ca., 36.29 degrees S). This earthquake originated continental uplift on that coastal areas closer to the trench between the Nazca and South American tectonic plates (i.e., Peninsula de Arauco and Isla Santa Maria) and subsidence along coastal areas located further north of that (the coast of the Maule Region), as well as in continental zones ordered in a west - east axis. In this study we tested the hypothesis that independent of the taxonomic group, the rocky shore sessile benthic organisms can be used as indicators of continental uplift. The methodology involved measurements of heights upper of distributional bands above the low tide level at the coast affected by the earthquake. The results show that the calcareous crustose algae Lithothamnium sp., the mytilid bivalve Perumytilus purpuratus and the macroalgae Mazzaella laminarioides and Lessonia spicata, are benthonic useful organisms to describe continental uplift, due to the fact that their vertical distributions after the earthquake follow the coastal deformation observed in the field. This allow to suggest that in studies aimed to evaluate this tectonic processes, more than a single species must be used in order to gain a full view of that along gradients of continental deformation. This due to the fact that a significant number of the benthic species of the rocky shore do not have continuous distribution; thus, to use a single species may well result in conclusions with low level of generalizations.