Major earthquake first
wrecking crews on buildings, rubble neatly piled, wrecking balls
purposeful demolition followed by rebuilding and rehabitation
may have been a decent amount of time between earthquake and volcano, years or maybe even 2-3 decades
however, rebuilding and restoration was still in progress when the eruption hit
LC I, near end of LM IA, LH I sometime before use of GCA in LH IIA
the lowest stratum of pumice ash was slightly oxidized, meaning probably exposed to the atmosphere for 2-24 months before being covered by the major pumice fall
this may have been the warning they needed to get out, since the first fall was not likely to have caused loss of life, 3 cm thick
2nd stratum of rather larger pumice between .5 and 1 meter thick
final deposit of tephra over 5 meters thick at Akrotiri and up to 50 elsewhere, bits of pumice 15 centimeters across, large boulders of basalt
most pumice to the southeast of Santorini
Greek ML & western Crete unaffected
eastern Crete 1-5 (10 max) cm of pumice
probably would have eroded quickly & increased the fertility of the soil, not brought about the collapse of civilization
some sediment found in western Anatolia
tidal wave may not have been big enough to cause massive destruction either
earthquake early in LM IA, eruption in later LM IA, Neopalatial destructions LM IB
wrecking crews on buildings, rubble neatly piled, wrecking balls
purposeful demolition followed by rebuilding and rehabitation
may have been a decent amount of time between earthquake and volcano, years or maybe even 2-3 decades
however, rebuilding and restoration was still in progress when the eruption hit
LC I, near end of LM IA, LH I sometime before use of GCA in LH IIA
the lowest stratum of pumice ash was slightly oxidized, meaning probably exposed to the atmosphere for 2-24 months before being covered by the major pumice fall
this may have been the warning they needed to get out, since the first fall was not likely to have caused loss of life, 3 cm thick
2nd stratum of rather larger pumice between .5 and 1 meter thick
final deposit of tephra over 5 meters thick at Akrotiri and up to 50 elsewhere, bits of pumice 15 centimeters across, large boulders of basalt
most pumice to the southeast of Santorini
Greek ML & western Crete unaffected
eastern Crete 1-5 (10 max) cm of pumice
probably would have eroded quickly & increased the fertility of the soil, not brought about the collapse of civilization
some sediment found in western Anatolia
tidal wave may not have been big enough to cause massive destruction either
earthquake early in LM IA, eruption in later LM IA, Neopalatial destructions LM IB