STRATI 2013 pp 1213-1216 | Cite as

Volcano-Stratigraphy of La Garrotxa Monogenetic Volcanic Field, Northeastern Spain

  • Xavier Bolós
  • Llorenç Planagomà
  • Joan MartíEmail author
Conference paper
Part of the Springer Geology book series (SPRINGERGEOL)


La Garrotxa monogenetic volcanic field (GVF) is located in northeastern Iberia and forms part of the Catalan Volcanic Zone (CVZ), which is a province of the Quaternary alkaline volcanism of the European rift system. The GVF corresponds to an area of about 100 km2 located between the cities of Olot and Girona. This basaltic volcanic field comprises more than 50 monogenetic cones including cinder and scoria cones, lava flows, tuff rings, and maars, ranging in age from 0.6 Ma to early Holocene. Strombolian and phreatomagmatic episodes have combined in the construction of most of these cones, which exhibit a wide range of deposits and eruptive sequences. By combining field work, the stratigraphic logging of both water wells and geotechnical drill holes, and the application of shallow geophysical methods, we have been able to establish for the first time a volcano-stratigraphy of the area that identifies the products of each single eruption, their relative stratigraphy, and their areal extent. This volcano-stratigraphy constitutes an essential tool for understanding the evolution of this volcanic field and for volcanic hazard assessment.


Volcano-stratigraphy Monogenetic volcanism Garrotxa volcanic field Hazard assessment 


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Copyright information

© Springer-Verlag Berlin Heidelberg 2014

Authors and Affiliations

  • Xavier Bolós
    • 1
  • Llorenç Planagomà
    • 2
  • Joan Martí
    • 1
    Email author
  1. 1.Group of Volcanology, SIMGEO (UB-CSIC)Institute of Earth Sciences Jaume AlmeraBarcelonaSpain
  2. 2.TOSCA, Serveis Ambientalsd’Educació i Turisme, Casal dels VolcansOlotSpain

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