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CHA P T E R 1 0


                  A New Uplift Episode at Campi Flegrei

                  Caldera (Southern Italy): Implications
                  for Unrest Interpretation and Eruption

                  Hazard Evaluation


                  Claudia Troise , Giuseppe De Natale, Folco Pingue, Umberto Tammaro,
                  Prospero De Martino, Francesco Obrizzo and Enzo Boschi





                  Contents

                  1. Introduction                                                 376
                  2. Recent Ground Deformation Data at Campi Flegrei Caldera      379
                  3. Displacement Shapes and Maximum Vertical to Horizontal Ratios  384
                  4. Discussion and Conclusion                                    388
                  Acknowledgments                                                 390
                  References                                                      390




                  Abstract
                  Campi Flegrei caldera, which includes the highly urbanized city of Naples, is the most
                  dangerous volcanic area in the world as it represents a serious threat to around two
                  million people. During the last four decades it has experienced a huge uplift phase,
                  which reached about 3.5 m in 1985 when a subsidence phase started. Recent geodetic
                  data demonstrates that such a subsidence phase has terminated, and a new uplift
                  episode started in November 2004 has so far resulted in about 0.04 m of uplift (October
                  2006). Here we show that the present episode, which appears slower but longer
                  than previous small uplifts, sheds light both on the origin of small and large unrests,
                  and on the conditions to evolve toward large unrests. Our simple but robust method is
                  based on continuous GPS measurements and compares the ratio between maximum
                  horizontal to vertical displacements. Results show that such unrests are due to
                  overpressure in a deeper source of fluids of magmatic origin. When the resulting




              Corresponding author. Tel.: +39-0816108314; Fax: +39-0816100811
             E-mail address: troise@ov.ingv.it
             Istituto Nazionale di Geofisica e Vulcanologia-Osservatorio Vesuviano, Via Diocleziano 328, 80124 Naples, Italy
             Developments in Volcanology, Volume 10                     r 2008 Elsevier B.V.
             ISSN 1871-644X, DOI 10.1016/S1871-644X(07)00010-1            All rights reserved.
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