Aerial shot of En Feshka from the west

Aerial shot of "The Canyons" in En Feshka from the west

Click on Image for high resolution magnifiable image

Panorama from Drone Photos by Jefferson Williams 27 Feb. 2023

Master Seismic Events Table

Charts, Plots, Maps, Images, etc.

En Feshka Plots and Charts

Image	Description	Source
Figure 3 Stratigraphic section of Ein Feshkha outcrop and (right) age-depth deposition model derived by OxCal 4.1. Breccias are marked in section by hatched black layers. Probability density functions (histograms) on the graph give model ages for radiocarbon calibrated ages (marked with arrows; arrow directions are meaningless) and model boundaries (details given in Table 3). The histograms give the distributions for the single calibrated dates while the darker center part of each histogram take into account the stratigraphic information (see section 4 and Bronk Ramsey [2008] for model specifics). The depth model curves are envelopes for the 95% (outer, lighter, approximately 2σ) and 68% (inner, darker, approximately 1σ) highest probability density ranges. Color of model age curve changes at boundaries. Kagan et al (2011)	Age Model	Kagan et al (2011)
Figure 3 Stratigraphic section of Ein Feshkha outcrop and (right) age-depth deposition model derived by OxCal 4.1. Breccias are marked in section by hatched black layers. Probability density functions (histograms) on the graph give model ages for radiocarbon calibrated ages (marked with arrows; arrow directions are meaningless) and model boundaries (details given in Table 3). The histograms give the distributions for the single calibrated dates while the darker center part of each histogram take into account the stratigraphic information (see section 4 and Bronk Ramsey [2008] for model specifics). The depth model curves are envelopes for the 95% (outer, lighter, approximately 2σ) and 68% (inner, darker, approximately 1σ) highest probability density ranges. Color of model age curve changes at boundaries. Kagan et al (2011)	Age Model - big	Kagan et al (2011)
Figure 4 Date distribution of calibrated ¹⁴C ages JW: Radiocarbon dates come from En Feshka Kagan et al (2010)	Age Model	Kagan et al (2010)
Figure 4 Date distribution of calibrated ¹⁴C ages JW: Radiocarbon dates come from En Feshka Kagan et al (2010)	Age Model - big	Kagan et al (2010)
Table 3 Ze'elim and Ein Feshka Seismites with Model Ages and Historic Event Correlation LS, local source, moderate earthquake, not appearing in the historical catalogs, may have produced these seismites Gully depth below fan delta surface Seismite type A, Intraclast breccia layer B, Microbreccia (“homogenite” to the naked eye) C, liquefied sand D, Folded laminae E, Small offsets Q, Questionable as seismite. See Table 1 and Figure 2. Model ages of seismites extrapolated from deposition model (see section 5 for details) Fit of historical earthquake dates within 1σ or 2σ calibrated age ranges of seismites. Although model ages are tabulated here with 1 year precision for convenience, event fit considers the realistic precision of 10 years (see section 5.1) All other possible events within the age probability range (1σ or 2σ range) of the designated earthquake; 1068a refers to March 1068 A.D., and 1068b refers to May 1068 A.D. (see Table A1) Outside model range, extrapolated from model (Figure 4) Outside model range, estimated based on below and above radiocarbon ages (Figure 4) Alternately, this historic earthquake could have formed seismites below or above the one marked Kagan et al (2011)	Seismite Assignment Table 3 Ze'elim and En Feshka	Kagan et al (2011)
Table 4 Multisite Comparison of Holocene Seismites from four lacustrine sediments sites along the Western Dead Sea Basin Kagan et al (2011)	Corrected Table 4 Seismite Comparisons Ze'elim, En Gedi, and En Feshka	Kagan et al (2011)
Figure 7 Recurrence intervals and cumulative number of breccias in time. Ein Feshkha (EFE) Ein Gedi (EG) Zeelim (ZA1 and ZA2) Diamonds represent breccias circled diamonds are the IBS (intrabasin seismites) Horizontal gray bars indicate periods of seismic quiescence (left) the earlier period is recorded at EG and ZA, and (right) the younger quiescence period is recorded at all three sites. Horizontal lines connect IBS events at the three sites. Kagan et al (2011)	Figure 7 Recurrence intervals and cumulative number of breccias in time	Kagan et al (2011)

En Feshka Core (DSF) Photos

This core was taken in 1997 by GFZ/GSI

Image	Description	Image	Description	Image	Description	Image	Description	Image	Description
				Composite Core DSF Depths 0-499 cm. Sections from top to bottom - B1, B2, B3, B4, and B5 GFZ/GSI	Composite Core DSF Sections B1-B5 0-499 cm.
Core DSF Section B1 0-93 cm. GFZ/GSI	Section B1 0-93 cm.	Core DSF Section B2 100-197 cm. GFZ/GSI	Section B2 100-197 cm.	Core DSF Section B3 200-298 cm. GFZ/GSI	Section B3 200-298 cm.	Core DSF Section B4 300-396 cm. GFZ/GSI	Section B4 300-396 cm.	Core DSF Section B5 400-499 cm. GFZ/GSI	Section B5 400-499 cm.

References

References

Kagan, E., et al. (2011). "Intrabasin paleoearthquake and quiescence correlation of the late Holocene Dead Sea." Journal of Geophysical Research 116(B4): B04311.

Kagan, E., et al. (2011). "Correction to “Intrabasin paleoearthquake and quiescence correlation of the late Holocene Dead Sea”." Journal of Geophysical Research: Solid Earth 116(B11): B11305.

Kagan, E. J. (2011). Multi Site Quaternary Paleoseismology Along the Dead Sea Rift: Independent Recording by Lake and Cave Sediments, PhD. Diss. Hebrew University of Jerusalem.