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Introduction & Summary



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Migowski et al (2004)

Textual Evidence

Enter A.G. Year Specify Reckoning
1 - Macedonian
2 - Babylonian		 Chosen Reckoning Time Span in the Julian Calendar
  

Experiment with button reset for list of months ?

Archaeoseismic Evidence

JQuery experiments



  

Landslide Evidence

  

Tsunamogenic Evidence

Paleoseismic Evidence

Hacipasa Trenches

The oldest event identified in the Ziyaret Trench dated to before 983 CE. A lower bound on age was not available due to insufficient radiocarbon dates.

Kazzab Trench

Ambiguous paleoseismic event ?S2 expressed as displacements along faults F2 and F3. Although Daeron et al (2007) favored an interpretation where this displacement was created during event S1 (dated 926-1381 CE) as a 'mole-track' like feature
Fig. 7.

Sketches showing the sections of (a) angular-ridge type and (b) bulge-type mole tracks. Both types of mole tracks were produced by horizontal compression (indicated by short arrows). The angular-ridge type mole track was produced by flexural slip folding and faulting of the top rigid layer. The bulge-type mole track formed mainly by folding and shortening of the unconsolidated to weakly consolidated alluvial deposits.

Lin et al (2004)
, they considered another interpretation that ?S2 was caused by a separate seismic event. Their age model date for ?S2 as a separate event spanned from 405 to 945 CE (2σ).

Jarmaq Trench

Nemer and Meghraoui (2006) date Event Z to after 84-239 CE. They suggested the Safed Earthquake of 1837 CE as the most likely candidate.