this battle probably took place about six years after Alexander Balas’ death in 145 BC (Clinton 1830, v, 327)which leads to a date of 139 BCE. However, Ambraseys (2009) also noted that
the sequence of events for the years following Alexander’s death would put the event between 138 and 125 BC (Pauly.W iv, 2, col. 2800). Karcz (2004) constrained the date of the battle to between the start of Diodotus Tryphon's mutiny in 145/144 BCE and his suicide in 138/137 BCE. Karcz (2004) added that if the Dead Fish and Soldiers Quake and the Seventeenth of Adar Quake are the same event, the Dead Fish and Soldiers Quake would likely have struck in 143/142 BCE when the Hasmonean King Jonathan campaigned against the Zabadeans (1 Maccabees 12:30) while still an ally of Diodotus Tryphon. Triantafyllou et al. (2022:8) proposed that this earthquake struck between 138 and 135 BCE however this tighter window was based on selective reading of John of Antioch - which is a chronologically unreliable source (in the extreme) for this particular earthquake. Based on this, the tight time window of Triantafyllou et al. (2022:8) is unrealistic. Guidoboni et al. (1994) did not include this event in their catalog.
Text (with hotlink) | Original Language | Biographical Info | Religion | Date of Composition | Location Composed | Notes |
---|---|---|---|---|---|---|
Geographicum by Strabo possibly based on Posidonius | Greek - Strabo Greek - Posidonius |
|
Strabo - 7 BCE - ~23 CE Posidonius - before c. 51 BCE |
Strabo - Amaseia in Pontus with some sections perhaps written at other locations. Posidonius - Rhodes |
reports sea wave flooding between Tyre and Acre
(aka Ptolemais). The account described a wave from the sea, like a flood-tide, submerged the fugitives; and some were carried off into the sea and destroyed, whereas others were left dead in the hollow places; and then, succeeding this wave, the ebb uncovered the shore again and disclosed the bodies of men lying promiscuously among dead fishwhile noting that like occurrences take place in the neighborhood of the Mt. Casius situated near Aegypt, where the land undergoes a single quick convulsion, and makes a sudden change to a higher or lower level, the result being that, whereas the elevated part repels the sea and the sunken part receives it |
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The Deipnosophistae by Athenaeus of Naucratis citing Posidonius | Greek - Athenaeus Greek - Posidonius |
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Athenaeus - end of the 2nd/beginning of the 3rd century BCE Posidonius - before c. 51 BCE |
Athenaeus - ? Posidonius - Rhodes |
The Deipnosophistae cites Posidonius in stating that suddenly a wave from the ocean lifted itself to an extraordinary height and dashed upon the shore, engulfing all the men and drowning them beneath the waters. And when the wave receded it left behind a huge pile of fishes among the dead bodies. |
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The Jewish War by Josephus | Greek, possibly translated from an earlier version in Aramaic |
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Jewish | about 75 CE | Rome and ? | Background information - Josephus Flavius recounted when Maccabean general Simon assisted Seleucid Emperor Antiochus VII Sidetes in, apparently successfully, sieging Dor against the Seleucid usurper Diodotus Tryphon (referred to as Trypho by Josephus). |
Historia Chronike by John of Antioch | Greek |
|
Christian - possibly Syrian Orthodox (Wikipedia citing Heinrich Gelzer's 3 volume edition Sextus Julius Africanus und die Byzantinische Chronographie, 1898 ?: v. ? p.41) | beginning of Heraclius (r. 610-648 CE)' reign as suggested by Roberto (2016:271) | Antioch? | In a chronologically inconsistent passage, John of Antioch relates that
a great earthquake happened in the East and a countless number of Syrians perishedwhile the city of Tyre on the coast was submerged into the sea and a comet shone for several days. It is unclear from the passage whether, he is referring to the Posidonius Quake, the Dead Fish and Soldiers Quake, is conflating both earthquakes together, or is referring to a separate event. It is possible that the Posidonius Quake and the Dead Fish and Soldiers Quake were the same event. |
The First Mithridates Comet and the Date of the Earthquake |
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Conflation Possibilities - The Dead Fish and Soldiers, Malalas Confusion, and the Seventeenth of Adar Quakes | ||||||
Text (with hotlink) | Original Language | Biographical Info | Religion | Date of Composition | Location Composed | Notes |
Location (with hotlink) | Status | Intensity | Notes |
---|---|---|---|
Tel Ateret aka Vadun Jacob | probable | ≥9 | Ellenblum et. al. (2015:5) estimated a displacement of ~2.5 m from this event which, though dated from the 3rd century BCE - ~142 BCE, probably struck around ~142 BCE. Using the scaling laws of Wells and Coppersmith (1994), ~2.5 m of strike-slip displacement corresponds to a magnitude of 7.1 - 7.4. |
Tell Anafa | possible | Hellenistic Earthquake inferred from possible rebuilding - Although Herbert in Stern et al (1993) did not report
any evidence for seismic destruction in Hellenistic times, they did date construction of a Late Hellenistic stuccoed building around ~125 BCE noting that a coin of Alexander Zebina (128-125 BCE) found in the construction fill of the bath's southern room is the latest find under any of the building's original floors.Herbert in Stern et al (1993) also reports that a massive leveling and terracing operation took place with the construction of the Late Hellenistic stuccoed building, obliterating earlier architectural remains.This could explain an absence of archaeoseismic evidence. |
|
Location (with hotlink) | Status | Intensity | Notes |
Location (with hotlink) | Status | Minimum PGA (g) | Likely PGA (g) | Likely Intensity1 | Comments |
---|---|---|---|---|---|
Jordan River Delta | possible | Niemi and Ben-Avraham (1994) estimated that Event 2 was younger than 3-5 ka and older than 1927 CE. | |||
Gulf Of Aqaba | possible | Event D in R/V Mediterranean Explorer core P27 - ~143 BCE 2 cm. thick Mass Transport Deposit Event D was identified in R/V Mediterranean Explorer Canyon Core P27 by Ash-Mor et al. (2017). Ash-Mor et al. (2017) provided an unmodeled 14C date of ~143 CE (2093 ± 56 cal years BP). R/V Thuwal Core 11 Unit J Turbidite - ~450-~50 BCE (1σ) Bektaş et al. (2024) identified/interpreted a seismo-turbidite deemed Unit J of R/V Thuwal Core 11 which was taken near the southern terminus of the Aragonese Fault. They assigned a date of ca. 250 BCE to this turbidite which, based on Probability Density Functions (PDFs) presented in Fig. 8 of their paper, should have been deposited between ~450 and ~50 BCE (1σ) and may be due to two events spaced between 100 and 250 years apart. |
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Location (with hotlink) | Status | Minimum PGA (g) | Likely PGA (g) | Likely Intensity1 | Comments |
Location (with hotlink) | Status | Intensity | Notes |
---|---|---|---|
Tyre | missing evidence | Marriner et al (2005) undertook a litho and biostratigraphical study of four core sequences from the landward edge of the current harbor. AMS radiocarbon dating was performed on dateable material found in the cores. They attributed missing 1st millennium BCE strata to dredging activity undertaken in the Roman and Byzantine periods. | |
Location (with hotlink) | Status | Intensity | Notes |
Location (with hotlink) | Status | Intensity | Notes | |||||||||||||||||||||
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Dinar Trenches | possible - indeterminate | ≥ 7 | Altunel et al (1999) claim evidence for a ~80 BCE Apamea Earthquake in Event 2 from their trenches but only two useful radiocarbon dates were obtained in their paleoseismic study. The date constraints from these two samples are large (~1550 BCE - 1360 ± 50 CE) and their historical earthquake assignment is speculative - based on consulting earthquake catalogs during that time span. | |||||||||||||||||||||
Hacipasa Trenches | possible | ≥ 7 | 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. | |||||||||||||||||||||
Tekieh Trenches | possible | ≥ 7 | Gomez et. al. (2003:15) may have seen evidence for an earthquake in the 1st or 2nd century BCE in Event B. Event B is estimated to have created ~ 2 meters of left lateral strike slip displacement which translates to an estimated Magnitude between 7.0 and 7.3 (7.0 and 7.2 according to Gomez et al, 2003:16-17). In terms of dating, an upper bound for Event B is 170 BCE - 20 CE while a lower bound for Events B and and the older Event C is from 1690 - 1400 BCE. | |||||||||||||||||||||
Tabarja Benches | possible | Mw = ~7.5 | Elias et al (2007)
examined uplifted benches on the Lebanese coast between Sarafand and Tripolis; some in the vicinity of Tabarja
(~20 km. NE of Beirut). They identified four uplifts from 3 or more [sizeable Mw = ~7.5] earthquakesin the past ca. 6-7 ka. They attributed the latest uplift (B1) to the 551 CE Beirut Quake while the earlier events (B2, B3, and B4) were no more precisely dated than between ~5000 BCE and 551 CE. Bench uplift on the earlier events (B2, B3, and B4) would likely have been due to uplift on the Mount Lebanon Thrust system - as was surmised for Event B1 and the 551 CE Beirut Quake. |
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Jarmaq Trench | possible | ≥ 7 | Nemer and Meghraoui (2006) date Event Y to between 2920-2879 BCE and 84-239 CE | |||||||||||||||||||||
Qiryat-Shemona Rockfalls | possible | Kanari, M. (2008) examined rockfalls in Qiryat-Shemona which were attributed to earthquakes. Optically stimulated luminescence (OSL) dating was performed on soil samples beneath the fallen rocks. Kanari et al (2019) assigned Sample ID QS-6 to an earthquake in 199 BCE but the wide spread in ages indicate that this event could have occurred in the 2nd century BCE. | ||||||||||||||||||||||
Bet Zayda | possible | ≥ 7 | Wechsler at al. (2014) records event CH4-E6 with a modeled age of 392 BCE – 91 CE. | |||||||||||||||||||||
Jordan Valley - Dir Hagla Trenches | possible | ≥ 7 | Reches and Hoexter (1981) report that Event A was dated from 200 BCE - 200 CE and exhibited 3.5 m of vertical displacement. Although the total vertical displacement could have been created by more than one seismic event, there were no broken layers between Event A the next Event (B) which was dated to between 700 and 900 CE. Further, they interpreted Event A created a fault scarp on the site. Kagan, E., et al. (2011) noted that the dip slip could have been magnified by local variations in the strike of the fault. | |||||||||||||||||||||
Dead Sea - Seismite Types | n/a | n/a | If the Dead Fish and Soldiers Quake struck
somewhere on the Lebanese littoral, it's epicenter might have been ~200-250 km. away from the Dead Sea Paleoseismic sites. If one assumes a magnitude
of 6.5, this leads to projected PGAs of 0.08-0.10 g at the Dead Sea sites. At a magnitude of 7.0,
those numbers go up to 0.14-0.18 g. This is below the 0.23 g threshold calculated by
Williams (2004)
and is, in some cases, above the 0.13 g threshold assumed in
Lu et al (2020a) that one needs to break the Dead Sea sediments. So, while a northern
Dead Fish and Soldiers Quake could have left a mark in the Dead Sea,
it would not likely have churned up seismites as thick the mid 2nd century BCE seismites we see in the outcrops. It also would not likely have extended to the Araba.
This suggests that the causitive earthquake for the mid 2nd century BCE seismites was probably in the region. This further suggests that we may be dealing
with an earthquake couplet where an earthquake in the northern part of the Dead Sea Transform struck within a short amount of time (1-2 decades or less)
before or after an earthquake in the southern part of the Transform. |
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Dead Sea - Nahal Darga | possible | ≥ 7 | Enzel et. al. (2000) identified a 20 cm. thick seismite in coarse grained lithology in Deformed Unit 8 in Stratigraphic Unit 10 which dated to 450-50 BCE (2400-2000 yrs BP). | |||||||||||||||||||||
Dead Sea - En Feshka | <possible | 7.9 - 8.8 | Kagan et al (2011) identified two seismites which they estimate struck in the
2nd century BCE.
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Dead Sea - En Gedi | possible | 7.9 - 8.8 | Migowski et. al. (2004) dated a 1 cm. thick Type 4 seismite at a depth of 302.48 cm. (3.0248 m) to 140 BCE. | |||||||||||||||||||||
Dead Sea - Nahal Ze 'elim | possible | 8.2 - 9.0 (All sites) | At site ZA-2, Kagan et al (2011) observed a 8 cm. thick Type 4 intraclast breccia seismite
at a depth of 516 cm. with modeled ages of 103 BCE ± 37 (1σ) and 103 BCE ± 75 (2σ). They suggested it struck in the middle of the
2nd century BCE. It may have formed during the southern
Dead Fish and Soldiers Quake. At site ZA-1, Kagan et al (2011) in Table 4 reports a 15 cm. thick seismite which they also assigned a date of mid second century BCE (i.e., assumed to be the same seismite). This appears to be the same seismite which Ken-Tor et al (2001a) labeled as Event A. Event A is an 11 cm. thick Type 4 seismite which Ken-Tor et al (2001a) dated as 200 BCE ± 160 (± 2σ) and estimated the most probable age as 400-200 BCE. Ken-Tor et al (2001a) assigned Event A to to the potentially dubious 64 BCE Pig on the Wall Quake. Williams (2004) and Agnon et. al (2006) redated Event A to better match the radiocarbon dates. Williams (2004) and Agnon et. al (2006) estimated dates of ~150 BCE and ~140 BCE respectively. |
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Araba - Introduction | n/a | n/a | n/a | |||||||||||||||||||||
Araba - Taybeh Trench | possible | ≥ 7 | LeFevre et al. (2018) reports a modeled age for Event E6 of 139 BCE ± 22. | |||||||||||||||||||||
Araba - Qatar Trench | unlikely | ≥ 7 | Klinger et. al. (2015) did not observe any mid 2nd century BCE seismic events. | |||||||||||||||||||||
Location (with hotlink) | Status | Intensity | Notes |