Gulf of Aqaba |
probable |
n/a |
n/a |
|
Turbidites in R/V Thuwal Cores 2, 3, and 4 in the Titan Deep - ~1800-~1860 CE (1σ)
Bektaş et al. (2024:13)
report that prominent [~mid 19th century CE] turbidites with well-preserved internal structures were identified in R/V Thuwal cores 2, 3, and 4 in the Titan Deep. Type II sedimentary
structures (Turbidite or Flooding Event) from around the same time were identified in neighboring cores 1, 7, and 8. Based on Probability Density Functions (PDFs) presented in Fig. 8 of their paper, the
turbidites in cores 2, 3, and 4 should have been deposited between ~1800 and ~1860 CE (1σ).
Bektaş et al. (2024:13)
suggested the 1839 CE Saint Catherine's Monastery Quake as the causitive event and noted that
given that the turbidites in cores 2, 3, and 4 are limited only in Tiran Deep, it is likely that the CE 1839 earthquake
only partially ruptured either the Tiran or Arnona fault, or activated one of the secondary faults in the southernmost part of the gulf . |