Abstract
The in situ recognition of the evidence of past earthquakes is a task which involves all the branches of geology. Signs of a past earthquake, in fact, can be identified on the landscape morphology and in the rocks generated by fault movements on the fault zone.
Cite
CITATION STYLE
APA
Mulargia, F., & Geller, R. J. (2003). The classical view of earthquakes. In Earthquake Science and Seismic Risk Reduction (pp. 20–101). Springer Netherlands. https://doi.org/10.1007/978-94-010-0041-3_2
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