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Les Journées des Jeunes Géomorphologues, Avignon, February 2011

Christoph Siart 1, Matthieu Ghilardi 2, Markus Forbriger 1 , Olaf Bubenzer 1




      The spatial shift of the Cretan ecumene 
          during the 2nd millennium BC: 
        climate, social upheaval or both?




                   1 Geographical Institute –   University of Heidelberg, Germany
                            2 CEREGE/CNRS –      Aix‐en‐Provence, France
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC




   Objectives
   • reconstructing the Holocene environmental change in Crete
   • natural impact on ancient cultures?

   • human impact and landuse?

    investigation of karst depressions (geoarchives)


   Methods
   • terrestrial laserscanning (TLS), remote sensing & GIS

   • geophysical prospection (ERT) & percussion drilling

   • sedimentological analysis & datings

   • mineralogical provenance (XRD, SEM‐EDX, EPMA etc.)

   • 3D visualisation
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


  Case studies
  A)  Zominthos (~ 1650 BC, Minoan period)
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


Zominthos: Electrical resistivity tomography ‐ off‐site studies
 subsurface karst relief
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


Zominthos: ERT on‐site studies
 subsurface archaeological remains
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


Zominthos: Subsurface karst relief model
transferring geophysics into 3D


                                                                                Data:
                                                                                ER‐ & SR tomographies
                                                                                1.5 m high resolution DEM
                                                                                Hydrologic analysis ‐ ArcGIS
                                                                                Quickbird MS pansharpened
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


Zominthos: Sedimentological investigations

 AMS 14C datings: palaeosoils ~2900 BC
 Santorini ash in depths of 10 m b.s (~ 1620 BC)

  geomorphodynamic activity only since                                                    CPX
   Late Minoan / Subboreal (1600 BC)
  massive erosion and colluviation                                                  OPX
  complete degradation in only a few centuries
                                                                                           OPX 
                                                                                             & 
                                                                                           glass
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


Climate change in the Eastern Mediterranean
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC

 Case studies
 B)   Lato (~ 1400 / 800 BC, Mycenean / Dorian period)
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


 Lato: ERT off‐site studies
 subsurface karst relief

                                   superficial high resistivities (colluvium, footslope deposits)

                                                          fine‐grained, 
                                                          unconsolidated sediment




                                                                             transition zone
   high basal resistivities                                                  (limestone detritus mixed 
   (limestone bedrock)                                                       with loose material)

   thick fill with loamy sediment (~ 25m), conical subsurface relief with 
  dip towards doline center, bedrock in depths of approx. 20‐25 m
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC

 Lato: ERT on‐site studies
 subsurface archaeological remains

                                                                                     heterogeneous surface caused
                                                                                     by anthropogenic perturbation




                                                                                      archaeological finds?




                                                                                       fine‐grained, unconsolidated 
                                                                                       sediment below 2.5 m, no
                                                                                       structures identified
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


 Lato: ERT‐TLS on‐site studies
 the morphological context
                                                                                      spring 


                                S




                                                                                 R   recent surface drainage
                                      A                                              (active gully)




                                           ancient drainage channel
                                          or water harvesting system
                                            (subsurface structures)
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


The Cretan mountains today
landscape degradation and climate alteration
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


The Cretan mountains BC
3D visualisation of the 
ancient landscape
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC


      General conclusions

  •dolines and poljes as favorable sites for land use since Bronze 
  Age (water supply, agriculture, etc.)
  •   karst depressions as promising palaeoenvironmental archives 
  •vast colluviation & decameters of infills since Bronze‐Age as a 
  result of land degradation and climatic change
  •water supply, the primary settlement determinant, displays 
  profound dependency on climatic conditions and changes
  •neo determinism: man‐environment interactions led to spatial 
  shift of the ecumene  multi‐causal approach
Les Journées des Jeunes Géomorphologues, Avignon, February 2011
Siart et al.: The spatial shift of the Cretan ecumene during the 2nd millennium BC




                  Thank you for your attention,
               merci beaucoup pour votre attention!

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The spatial shift of the Cretan ecumene during the 2nd millenium BC