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SEISMIC STRATIGRAPHY OF SANTORINI’S
   CALDERA: A CONTRIBUTION TO THE
UNDERSTANDING OF THE MINOAN ERUPTION
 Sakellariou D.1, Rousakis G.1, Sigurdsson H.2, Nomikou P.3,
            Katsenis I.4, Croff Bell K.L.2, Carey S.2
          1
           Inst. Oceanography, Hellenic Centre for Marine Research
    2
      Graduate School of Oceanography, University of Rhode Island, USA
 3
   Geology Dptm , National Kapodistrian University of Athens, Ilissia, Greece,
                     4
                       Geology Dptm., University of Patras




10ο Πανελλήνιο Συμπόσιο Ωκεανογραφίας & Αλιείας
             7-11 Μαϊου 2012, Αθήνα
HCMR surveys                  Cape Riva
  in the Caldera                Caldera

Multibeam bathymetry 2001,
2006, 2012

Airgun 10ci seismic profiling
2006 & 2012
                                                            n
                                                          si
Chirp & 3.5kHz subbottom                                Ba
profiling 2012                                    rth
                                               No
Side scan sonar imaging
2012

Submersible Thetis dives          West Basin
2006

ROV Max Rover dives 2012                          South Basin

Seafloor sampling 2006, 2012
HCMR surveys
  in the Caldera
Multibeam bathymetry 2001,
2006, 2012

Airgun 10ci seismic profiling
2006 & 2012

Chirp & 3.5kHz subbottom
profiling 2012

Side scan sonar imaging
2012

Submersible Thetis dives
2006

ROV Max Rover dives 2012

Seafloor sampling 2006, 2012
Minoan eruption deposits
                        onshore
                 Lahars and pyroclastic flows


                                        Pyroclastic
                                     flows, surges
  Minoan eruption Phase 1:
Coarse grain air-fall tephra layer
   Thickness: 10-11m max




                                     Air fall Tephra


                                      Pre-eruption
                                             relief
Morphology of the submarine volcanic flanks
      Young, upper slopes: steep, irregular
    Old, lower slopes: gently sloping, smooth
Seismic stratigraphy of Santorini Caldera
             NORTH BASIN




           Airgun 10ci profile 90-91
Seismic stratigraphy of Santorini Caldera
             NORTH BASIN




           Airgun 10ci profile 39-38
Seismic stratigraphy of Santorini Caldera
             NORTH BASIN




           Airgun 10ci profile 40-41
Seismic stratigraphy of Santorini Caldera
             NORTH BASIN




         Deep Tow CHIRP profile 40-41
Seismic stratigraphy of Santorini Caldera
             NORTH BASIN




           Airgun 10ci profile 43-42
Seismic stratigraphy of Santorini Caldera
              WEST BASIN




           Airgun 10ci profile 87-88
Seismic stratigraphy of Santorini Caldera
             SOUTH BASIN




           Airgun 10ci profile 88-89
Seismic stratigraphy of Santorini Caldera
             SOUTH BASIN




           Airgun 10ci profile 47-48
Seismic stratigraphy of Santorini Caldera
              SOUTH BASIN




         Airgun 10ci profile 51-50-49-48
Seismic stratigraphy of Santorini Caldera
             SOUTH BASIN




           Airgun 10ci profile 49-48
Interpretation of the seismic stratigraphy
              of Santorini’s Caldera



Kameni lavas

                                                        slide
                Floating pumice
                     Pyroclastics
                                         Pyroclastics
                              Air-fall tephra
               Pre-Minoan
                 Pre-Minoan
Cape Riva Caldera
Eruption took place outside the Santorini Caldera.
Cape Riva pyroclastics flew into the caldera through
the northern corridor.
Structural evolution of Santorini’s Caldera
RESULTS

(i) the thickness of the Minoan deposits on the caldera seafloor
exceeds 100 m locally,


(ii) post Minoan deposits are negligible,


(iii) the lower, gently sloping parts of the slopes around Kameni
islands are of Minoan age,

(iv) all three subbasins of the caldera existed prior to the Minoan
eruption and were filled with pyroclastics during and after the 17 th
cent. BC eruption

(v) the Minoan eruption center was located where the present day
Kameni islands are.
EUROFLEETS
                Caldera 2012 – July 2012
           Girona University - HCMR - IPGP - WHOI




        Autonomous Underwater Vehicle “Girona 500”
Payload: multibeam, sidescan sonar, camera, mass spectrometer
    Deliverables: microbathymetry, morphology, photomosaic,
                      geochemical mapping
EUROFLEETS
                                                                      Caldera 2012

                                                   Mapping gas concentration in real time
                                                   with the TETHYS mass spectrometer,
                                                     mounted on THETIS submersible

                            1.00E-06
                                                                                                                                    CO2


                                                                                                         ambient        vent

                            1.00E-07         CH4
                                                                                           CO
ion peak intensity (Torr)




                                                                                                       H2S
                            1.00E-08

                                                                                                                    Hydrocarbon?


                            1.00E-09
                                                                                            NOx



                            1.00E-10




                            1.00E-11
                                       10   12   14   16   18   20   22   24    26    28    30    32    34   36    38    40    42   44    46
                                                                               mass-to-charge ratio
EUROFLEETS
         Caldera 2012

    January 2012
    ROV Max Rover dive
    North of Nea Kameni
    380m depth

Small crater on the Caldera’s seafloor
THANK YOU




santorini.hcmr.gr

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Seismic stratigraphy od Santorini's Caldera: a contribution to the understanding of the Minoan eruption. Sakellariou D.

  • 1. SEISMIC STRATIGRAPHY OF SANTORINI’S CALDERA: A CONTRIBUTION TO THE UNDERSTANDING OF THE MINOAN ERUPTION Sakellariou D.1, Rousakis G.1, Sigurdsson H.2, Nomikou P.3, Katsenis I.4, Croff Bell K.L.2, Carey S.2 1 Inst. Oceanography, Hellenic Centre for Marine Research 2 Graduate School of Oceanography, University of Rhode Island, USA 3 Geology Dptm , National Kapodistrian University of Athens, Ilissia, Greece, 4 Geology Dptm., University of Patras 10ο Πανελλήνιο Συμπόσιο Ωκεανογραφίας & Αλιείας 7-11 Μαϊου 2012, Αθήνα
  • 2. HCMR surveys Cape Riva in the Caldera Caldera Multibeam bathymetry 2001, 2006, 2012 Airgun 10ci seismic profiling 2006 & 2012 n si Chirp & 3.5kHz subbottom Ba profiling 2012 rth No Side scan sonar imaging 2012 Submersible Thetis dives West Basin 2006 ROV Max Rover dives 2012 South Basin Seafloor sampling 2006, 2012
  • 3. HCMR surveys in the Caldera Multibeam bathymetry 2001, 2006, 2012 Airgun 10ci seismic profiling 2006 & 2012 Chirp & 3.5kHz subbottom profiling 2012 Side scan sonar imaging 2012 Submersible Thetis dives 2006 ROV Max Rover dives 2012 Seafloor sampling 2006, 2012
  • 4. Minoan eruption deposits onshore Lahars and pyroclastic flows Pyroclastic flows, surges Minoan eruption Phase 1: Coarse grain air-fall tephra layer Thickness: 10-11m max Air fall Tephra Pre-eruption relief
  • 5. Morphology of the submarine volcanic flanks Young, upper slopes: steep, irregular Old, lower slopes: gently sloping, smooth
  • 6. Seismic stratigraphy of Santorini Caldera NORTH BASIN Airgun 10ci profile 90-91
  • 7. Seismic stratigraphy of Santorini Caldera NORTH BASIN Airgun 10ci profile 39-38
  • 8. Seismic stratigraphy of Santorini Caldera NORTH BASIN Airgun 10ci profile 40-41
  • 9. Seismic stratigraphy of Santorini Caldera NORTH BASIN Deep Tow CHIRP profile 40-41
  • 10. Seismic stratigraphy of Santorini Caldera NORTH BASIN Airgun 10ci profile 43-42
  • 11. Seismic stratigraphy of Santorini Caldera WEST BASIN Airgun 10ci profile 87-88
  • 12. Seismic stratigraphy of Santorini Caldera SOUTH BASIN Airgun 10ci profile 88-89
  • 13. Seismic stratigraphy of Santorini Caldera SOUTH BASIN Airgun 10ci profile 47-48
  • 14. Seismic stratigraphy of Santorini Caldera SOUTH BASIN Airgun 10ci profile 51-50-49-48
  • 15. Seismic stratigraphy of Santorini Caldera SOUTH BASIN Airgun 10ci profile 49-48
  • 16. Interpretation of the seismic stratigraphy of Santorini’s Caldera Kameni lavas slide Floating pumice Pyroclastics Pyroclastics Air-fall tephra Pre-Minoan Pre-Minoan
  • 17. Cape Riva Caldera Eruption took place outside the Santorini Caldera. Cape Riva pyroclastics flew into the caldera through the northern corridor.
  • 18. Structural evolution of Santorini’s Caldera
  • 19. RESULTS (i) the thickness of the Minoan deposits on the caldera seafloor exceeds 100 m locally, (ii) post Minoan deposits are negligible, (iii) the lower, gently sloping parts of the slopes around Kameni islands are of Minoan age, (iv) all three subbasins of the caldera existed prior to the Minoan eruption and were filled with pyroclastics during and after the 17 th cent. BC eruption (v) the Minoan eruption center was located where the present day Kameni islands are.
  • 20. EUROFLEETS Caldera 2012 – July 2012 Girona University - HCMR - IPGP - WHOI Autonomous Underwater Vehicle “Girona 500” Payload: multibeam, sidescan sonar, camera, mass spectrometer Deliverables: microbathymetry, morphology, photomosaic, geochemical mapping
  • 21. EUROFLEETS Caldera 2012 Mapping gas concentration in real time with the TETHYS mass spectrometer, mounted on THETIS submersible 1.00E-06 CO2 ambient vent 1.00E-07 CH4 CO ion peak intensity (Torr) H2S 1.00E-08 Hydrocarbon? 1.00E-09 NOx 1.00E-10 1.00E-11 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 42 44 46 mass-to-charge ratio
  • 22. EUROFLEETS Caldera 2012 January 2012 ROV Max Rover dive North of Nea Kameni 380m depth Small crater on the Caldera’s seafloor