Natural Disasters Topic 4 (Earthquakes)
THE HIGHEST CENTRAL ANDES Victor A. Ramos Laboratorio de Tectónica Andina Universidad de Buenos Aires.
Earthquakes Physical Geology 11/e, Chapter 16. Earthquakes and Plate Tectonics At divergent boundaries, –tensional forces produce shallow-focus quakes.
“The most important ingredient in the formulation of the sea floor spreading and the later plate tectonic theories was the knowledge of the existence of.
Evidence for Plate Tectonics As it turns out, Alfred was right.
Plate convergence usually commences with intra-oceanic Subduction, Andean margins commonly start after ophiolite obduction and subduction flip. CONVERGENT.
Carrie Welker Mason Edwards
Copyright © by Isiorho 1 Earthquake Slides Modified from the original version by Dr. S. A. Isiorho’s presentation.
Plate convergence usually commences with intra-oceanic Subduction, Andean margins commonly start after ophiolite obduction and subduction flip.
