Abstract
The southern end of Genoveses Bay (Cala de Genoveses) in Almeria (SE Spain) hosts one of the most spectacular examples in Europe of combined (from base to the top), ignimbrite, surge, and pumice-ash fall deposits, forming a world-class outcrop of pyroclastic rocks. At a regional scale, the volcanism that led to the formation of these rocks has to be understood in terms of the late Alpine tectonic evolution of the western Mediterranean.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
