Text (with hotlink) | Original Language | Biographical Info | Religion | Date of Composition | Location Composed | Notes |
---|---|---|---|---|---|---|
Introduction & Summary | ||||||
Damage and Chronology Reports from Textual Sources | ||||||
Martyrs of Palestine by Eusebius | Greek |
|
Christian | between 311 and 316 CE | Caesarea | Describes shaking but no specific damage in Caesarea. Supplies a date of 2 April, Says the earthquake struck in the 3rd year of the Diocletianic Persecutions which equates to ~306 CE. |
Chronicon written by Eusebius and Translated by Jerome | Latin translation from Greek of the 2nd part of Eusebius' Chronicon |
|
Christian | ~325 CE for final edition of original composition ca. 380 CE for Latin translation |
Caesarea (final edition of original composition) | Described a horrible earthquake at Tyre and Sidonwhere many edifices were ruined and an immense number of people were crushed.Provides a variety of chronological markers that specify a year between 300 and 305 CE with 303-305 CE the most likely time span. |
History Against the Pagans by Orosius | Latin |
|
Christian | ~416-417 CE | Palestine and/or Gallaecia (northwest Hispania) and/or places between. | Described an earthquake in Syriawhere thousands of people throughout Tyre and Sidon were crushed by falling buildings.Although, a date is not specified and the year is not explicitly defined, the position of the passage in relation to other events suggests a date range from 303 CE - 1 May 305 CE and a most likely year of 303 CE. |
Later Authors | ||||||
Text (with hotlink) | Original Language | Biographical Info | Religion | Date of Composition | Location Composed | Notes |
Location (with hotlink) | Status | Intensity | Notes |
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Hippos Sussita | unlikely | Segal et al (2014b) excavated an
Odeion at Hippos-Sussita
from 2008 - 2010. They report that
On the basis of an analysis of the building methods and materials and according to the numismatic and pottery finds, it can be determined to a great degree of certainty that the odeion was erected during the second half of the 1st century CE. It appears that the odeion was in use during the first three centuries of the Common Era. Its condition as revealed during its exposure by the excavators clearly indicates that it was not destroyed. This conclusion is based on the preserved uniform height of the walls, two or three courses, not including the encompassing wall of which six courses have survived. The lack of decorative items that were broken or burnt, the absence of tiles and sooty remains of the ceiling and roof, all testify that the structure was systematically dismantled. It is safe to assume, on the basis of the numismatic and pottery finds, that the dismantling of the structure was carried out during the 4th century CE, apparently before the earthquake of 363 CE. However, we cannot negate the possibility that the odeion was damaged during this earthquake and that a decision was then made not to renovate but rather to dismantle it.In summary, they did not encounter a destruction layer. While it is possible that the Odeion was dismantled due to damage caused by an earlier earthquake, the excavators did not suggest this. |
|
Tiberias - Hammath Tiberias | possible | Stratum IIB Earthquake (?) - 4th century CE - Magness (2005)
reports that in his excavation reports, Moshe Dothan interprets the evidence to indicate that the synagogue of Stratum IIB was destroyed in
the Eusebius' Martyr Quake (303-306 CE).
Magness (2005) apparently dates
the end of Stratum IIB to the 4th century CE and does not ascribe an earthquake to its presumed destruction.
Weiss (2009:338) opined that there is no reason to assume that the [Stratum II] Hammath Tiberias synagogue had two distinctly different stagessuggesting instead that the Stratum II synagogue underwent several internal changes during its years of existenceand that the remodeling of the synagogue that Dothan attributed as a response to the Eusebius' Martyr Quake (303-306 CE) occurred later - some time after the earthquake, most probably in the second half of the fourth century C.E. |
|
es-Sufeira | possible | Eisenberg and Osband (2022) report that excavators Zingboym and Kleiner (2021) suggest that the Eusebius Martyr Quake (between ~303 and ~306 CE) damaged the site. | |
Tel Dover | possible | Eisenberg and Osband (2022) report that Rapuano (2001) identified an early 4th century CE destruction layer which could have been due to the Eusebius Martyr Quake (between ~303 and ~306 CE). | |
Gush Halav | possible |
|
|
Khirbet Shema | possible |
|
|
en-Nabratein | possible |
|
|
Byblos | possible | Ambraseys (2009)
discussed an inscription found in Byblos which may allude to
the Eusebius Martyr Quake
There is also an inscription from an altar in Byblus that records the survival of one Apollodorus after an earthquake Dussaud (1896:299). The inscription is dated by Seyrig to the second or third century, which would seem to indicate that it is not connected with this earthquake (H. Seyrig, personal communication 5 July 1972). However, since provincial epigraphy is often slower to change than that in major centres, and there is no other earthquake recorded for this location during the second or third century, the inscription has been very tentatively allocated to this event. |
|
Location (with hotlink) | Status | Intensity | Notes |
Location (with hotlink) | Status | Intensity | Notes |
---|---|---|---|
Caesarea and Jisr al-Zakra | possible | Neither Reinhardt et. al. (2006) nor
Goodman-Tchernov et. al. (2009) nor
Goodman-Tchernov and Austin (2015)
saw evidence of a tsunami in near shore shelf deposits of Caesarea around 304 CE.
Salamon et. al. (2011)
noted that a tsunami was reported in a number of earlier earthquake catalogs (e.g. Shalem, 1956,
Ben-Menahem, 1991,
Amiran et al., 1994) which
several of the cataloguers (Shalem, 1956 and Amiran et al., 1994) viewed as doubtful - according to Salamon et al (2011). The alleged tsunami was likely generated from
Eusebius' report of the sea casting up the body of the martyrdom of Apphian at the gates of Caesarea at the same time as the [Eusebius Martyr Quake] in Sidon.Salamon et al (2011) noted that a seismic sea wave is not specifically mentioned in Eusebius' text and it is common along the eastern Mediterranean coast, even in normal weather conditions, that the sea casts up dead bodies of drowned people at the shore. |
|
Location (with hotlink) | Status | Intensity | Notes |
Location (with hotlink) | Status | Intensity | Notes |
---|---|---|---|
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. |
al-Harif Syria | possible | ≥ 7 |
Sbeinati et. al. (2010) report a seismic event X which they dated to 335 CE± 175 years. MW = 7.3-7.6 (based on 4.2 m of slip). |
Bet Zayda | probable | ≥ 7 | The Eusebius Martyr Quake of 303-306? CE is a good fit for Event CH4-E3 (Modeled Ages 250-310 CE) particularly as it relates to other events observed. (Wechsler at al., 2014) |
Dead Sea | unlikely | n/a | Mistaken report - Although Wechsler et al. (2018:18) reported that ~303 CE shaking was found in the Dead Sea sediment cores (Kagan et. al., 2011; Migowski et. al., 2004 ), Kagan et. al. (2011) did not assign an event of 300-307 CE to any seismites in En Feshka or Nahal Ze 'elim and Migowski et. al. (2004) did not assign an event between 300 and 307 CE in En Gedi. A simple check on whether a ~303 CE seismite would have been masked or overprinted by the Monaxius and Plinta seismite of 419 CE reveals that this is not a possibility consistent with how this was reported by Migowski et. al. (2004:Table 2). So, there is no Dead Sea Paleoseismic evidence for this earthquake. Considering the distance to the presumed epicenter near the Lebanese littoral, it is unlikely that such an earthquake would have formed seismites in the Dead Sea. |
Location (with hotlink) | Status | Intensity | Notes |