the shock was felt along the Mediterranean coast from Gaza and Ascalon Caesaraea to Acre, but not at Tiberiaswhile Amiran et al (1994) reports additional damage in Nablus and Tiberias.
Text (with hotlink) | Original Language | Biographical Info | Religion | Date of Composition | Location Composed | Notes |
---|---|---|---|---|---|---|
Damage Reports from Textual Sources | n/a | n/a | n/a | n/a | n/a | n/a |
Letter from an anonymous Welsh traveler to Jerusalem | English translated from Welsh |
Biography
|
Christian | 16 July 1834 CE | Jerusalem | An eyewitness described an earthquake in Jerusalem while it was being captured and sacked by rebel forces during the
1834 CE Fellahin Revolt which dates the earthquake to late May or early June of 1834 CE. The earthquake was said to
have destroyed many houses, and levelled to the earth that part of the city wall which passes the temple of the Muhammadans. The monastery of Bethlehem was rendered uninhabitableand many of the inhabitants were killed in the ruin of their houses. For ten days earthquakes continued to rock the city, though none of them was by any means so severe as the first. |
Report by the Monk Neophytos | English translated from Greek |
Biography
|
Greek Orthodox | Neophytos dated the earthquake in the Julian Calendar. Once this date is converted to the Gregorian calendar, his time and date for the
earthquake is 6 am Sunday 26 May 1834 CE. Neophytos described the earthquake as lasting but three secondsyet so violent that the dome of the Catholicon was cracked in seven places and all the plaster fell off. He also noted that the big dome of the Church of the Holy Sepulchre was shaken, but being of wood and well bound together, it was not greatly damaged. Many big houses in Jerusalem were cracked and many fell. Part of the city wall, near the Mosque of Omar, fell. A minaret fell in Jerusalem, and another one on the Mount of Olives, as did the dome of the Shrine of the Ascension. In Bethlehem the monasteries of the Franks and the Armenians and ours were greatly damaged, especially the belfry. By God's mercy the beautiful Church of the Nativity of our Lord Jesus Christ, as well as the new pilgrim-house, was not damaged. |
||
Baptisin Poujoulat | French |
Biography
|
~1837 CE | Baptisin Poujoulat reported that Jerusalem experienced a violent earthquake in 1834 CE which also tore down the walls of Caesarea. In possible hyperbole, he reports that 4000 people died under the rubble in Caesarea and that the earthquake was preceded by thick smoke, distant rumblings, and multicolored flames coming out of Mount Argée (location unknown). Poujoulat reports that in Caesarea minarets, vaults, mosques, churches, and carvanaseris partially collapsed and several (nearby?) villages were partially destroyed. A salt water lake is said to have inundated a village known as Komtzi. | ||
Edward Robinson | English |
Biography
|
1838 CE | Edward Robinson reported second hand accounts that
a large quantity of asphaltum was cast upon the shore near the SW partof the Dead Sea after the earthquake of 1834 CE. |
||
Titus Tobler | German |
Biography
|
1853 CE | Titus Tobler wrote that in July 1834 CE, an earthquake threw down several structures in Jerusalem, damaged part of a wall near a Mosque in the same city, and threatened the collapse of the Latin Rlofters (?) | ||
William McClure Thomson | English |
Biography
|
Protestant Christian | around April 1857 CE | Jaffa | In a passage written around April 1857 CE, William McClure Thomson recalled his experiences
during the 1834 CE Fellahin Revolt Earthquake. He was in Ramleh at the time of the earthquake. In Ramleh, the earthquake cracked nearly all the housesand threw down many. A tower in Jaffa had been rudely shakenby the same earthquake. He dated the earthquake to 23 years before he was writing (i.e., 1834 CE) and while rebel forces occupied Jerusalem (late May/ early June 1834 CE). |
History of the Greek Orthodox Patriarchate of Jerusalem | English | Christian | 1913 CE | A History of the Greek Patriarchate of Jerusalem states that the Dome of the Catholicon was partly destroyed in an earthquake in 1834 CE. The Catholicon apparently refers to the Church of the Holy Sepulchre. | ||
Menahem Mendel of Kamieniec | Jewish |
Zohar et al (2015:244 n. 2) report that Menahem Mendel of Kamieniec (1800-73) dates the event to the 30th count of the Jewish ‘Omer’which, according to Zohar et al (2015:244 n. 2), corresponds to 14 Iyyar. If one assumes a Hebrew year of 5594, this converts to a Gregorian date of Friday, 23rd of May (Mendel 1839). Zohar et al (2015:244 n. 2) also report that Mendel wrote that there were two shocks - one at noon and the second at night (Mendel 1839). |
||||
Other Authors | ||||||
Text (with hotlink) | Original Language | Biographical Info | Religion | Date of Composition | Location Composed | Notes |
´
Effect | Sources | Notes |
---|---|---|
Destroyed or damaged houses in Jerusalem | Anonymous Welsh Traveler, Neophytos | |
Wall outside Al-Aqsa Mosque Damaged | Anonymous Welsh Traveler | probable location |
Wall outside Mosque of Omar fell | Neophytos | |
Wall outside an unnamed Mosque (presumably in Jerusalem) partly damaged | Titus Tobler | |
threatened the collapse of the Latin Rlofters (?) in Jerusalem | Titus Tobler | |
A minaret fell in Jerusalem | Neophytos | |
A minaret on the Mount of Olives fell | Neophytos | |
The dome of the Shrine of the Ascension fell | Neophytos | |
Monastery in Bethlehem Damaged | Anonymous Welsh Traveler, Neophytos | Neophytos was more specific - In Bethlehem the monasteries of the Franks and the Armenians and ours were greatly damaged, especially the belfrybut the beautiful Church of the Nativity of our Lord Jesus Christ, as well as the new pilgrim-house, was not damaged |
Dome of the Catholicon (Jerusalem) cracked | Neophytos, History of the Greek Orthodox Patriarchate of Jerusalem | |
City Walls of Caesarea damaged | Baptisin Poujoulat | |
The minarets, the vaults, mosques, churches, and carvanaseris partly collapsed in Caesarea | Baptisin Poujoulat | |
sea water inundated a village called Komtzi | Baptisin Poujoulat | |
Tower in Jaffa rudely shaken |
William McClure Thomson | |
cracked nearly all the houses in Ramleh, and threw down many | William McClure Thomson | |
A large quantity of Asphalt appeared on the SW shore of the Dead Sea | Edward Robinson |
Location | Sources | Notes |
---|---|---|
Jerusalem | Anonymous Welsh traveler, Neophytos, Baptisin Poujoulat, Titus Tobler, History of the Greek Orthodox Patriarchate of Jerusalem | |
Bethlehem | Anonymous Welsh traveler, Neophytos | |
Caesarea | Baptisin Poujoulat. William McClure Thomson1 | |
Ramla | William McClure Thomson | |
Jaffa | William McClure Thomson | unclear if there was significant damage |
Dead Sea | Edward Robinson, Blankenhorn (1905:208) | |
Dhiban | Tristram et al (1873) | speculative - see Archeoseismic Evidence |
an area 10 leagues (~55 km.) south of Mount Argée (?) | Baptisin Poujoulat | |
a village called Komtzi | Baptisin Poujoulat |
Footnotes1 Thomson (1861:502) wrote something in 1857 CE that may or may not recall earlier seismic damage to the walls of Caesarea during the 1834 CE Fellahin Revolt Earthquake
I recalled the day and night I spent among Caesarea's broken walls and prostrate columns more than twenty years ago. Fresh from scenes of war, and earthquake, and sickness, and death in Jerusalem, I then felt a mysterious sympathy with these sad and forsaken ruins.
THE REVOLT OF 1834.
Year | Reference | Corrections | Notes |
---|---|---|---|
Late May/Early June 1834 CE | none |
|
ANNALS OF PALESTINE, 1821-1841
1a Three supports were broken near the base. The belfry and the arches
were shaken. Many of the cisterns in Jerusalem were cracked and the water
hewed out of them.
1b The wall of the Church was cracked near where the Armenians celebrate.
The tower of St. John Damascenus in the monastery of St. Saba was completely
cracked.
At six o'clock on Sunday morning, May 13th
Year | Reference | Corrections | Notes |
---|---|---|---|
6 am Sunday 25 May 1834 CE | At six o'clock on Sunday morning, May 13th 1834 CE | none |
|
This siege, begun on the 8th of June, had lasted for ten eight days, and the viceroy's son trembled for his life . At the same time, the plague and a violent earthquake broke out in Jerusalem; the holy city was plunged into the most appalling consternation. At this moment, the 19th regiment line, commanded by Colonel Moustapha Bey, who left Damascus to succor the Egyptian general, was massacred by a numerous troop of mountaineers in the gorges which border the magnificent plain of Esdrelon on the west.
Ce siége, commencé le 8 juin , durait depuis dix huit jours, et le fils du vice - roi tremblait pour sa vie . En même temps , la peste et un violent tremblement de terre éclatèrent à Jérusalem ; lą ville sainte était plongée dans la plus effroyable consternation . En cet instant, le 19" régiment de ligne, que commandait le colonel Moustapha bey , parti de Damas pour aller secourir le général égyptien , fut massacré par une nombreuse troupe de montagnards dans les gorges qui bornent à l'ouest la magnifique plaine d'Esdrelon .
The city walls [of Caesarea] were torn down by the earthquake of 1834. This catastrophe announced itself with a terrible character. One morning we saw coming out of the foot of Mount Argée thick smoke intermingled with flames of a thousand colors, accompanied by a long noise similar to the distant rumblings of an angry tone. In a moment Caesarea was shaken in its foundations; the houses crumbled and were broken, and four thousand people were buried under the rubble. The minarets, the vaults mosques, churches, and carvanaseris are partly collapsed. The people of Caesarea in that moment of terror, believed that the world was about to end, and the angel's trumpet sounded the last day. This earthquake was felt over an area of ten leagues, south of Mount Argée; several villages were incompletely destroyed a salt water lake took the place of a village called Komtzi.
Les murailles de la ville ont été renversées par le tremblement de terre de 1834. Cette catastrophe s'annonça avec un caractère effroyable. Un matin on vit sortir du pied du mont Argée une épaisse fumée entremêlée de flammes aux milles couleurs , accompagnées d'un long bruit semblable aux grondements lointains du ton nerre. En un moment Césarée fut ébranlée dans ses fondements ; les maisons tombèrent en dé bris, et quatre mille personnes restèrent enseve lies sous les décombres. Les minarets , les voûtes des mosquées, les églises , les karavanserails s'é croulèrent en partie. Les habitants de Césarée dans ce moment d'épouvante , crurent que le monde allait finir, et que la trompette de l'ange sonnait le dernierjour. Ce tremblement de terre se fit sentir sur une étendue de dix lieues, au sud du mont Argée ; plusieurs villages furent en tièrement détruits un lac d'eau salée prit la place d'un bourg appelé Komtzi.
En même temps, la peste et un violent
Les habitants de Césarée
Year | Reference | Corrections | Notes |
---|---|---|---|
1834 CE | 1834 CE | none |
Also in Caesarea, 85 km northwest of Jerusalem, parts of the remaining old walls and of some houses fell, while four nearby villages were also affected, without casualties (Poujoulat 1840, 154 - Volume not specified). JW: I don't find this reference on page 154 in either volume
1 Seetzen in Zach's Monatl. Corr. XVIII. p. 441. Burckhardt, p. 394. English. Lane's Mod. Egypt. IL p. 372.
2 The Kuntar is about 98 lbs.
More definite and trustworthy
Year | Reference | Corrections | Notes |
---|---|---|---|
1834 CE | 1834 CE | none |
9 Geramb 1, 325. Rurz vor der Ankunft Röfers (Krantbeiten des Orients. 43).
10 Unflar. Geramb a. a. D.
11 Röſer a. a. D. Gehr Zehrreidhes über Erdebeben ſ. Bolney 1, 234 f.
9 Geramb 1, 325. Rurz vor der Ankunft Röfers (Krantbeiten des Orients. 43).
10 Unflar. Geramb a. a. D.
11 Röſer a. a. D. Gehr Zehrreidhes über Erdebeben ſ. Bolney 1, 234 f.
Year | Reference | Corrections | Notes |
---|---|---|---|
July 1834 CE | July 1834 CE | none |
The view from the top of the tower is inexpressibly grand. The whole plain of Sharon, from the mountains of Judea and Samaria to the sea, and from the foot of Carmel to the sandy deserts of Philistia, lies spread out like an illuminated map. Beautiful as vast, and diversified as beautiful, the eye is fascinated, the imagination enchanted, especially when the last rays of the setting sun light up the white villages which sit or hang upon the many-shaped declivities of the mountains. Then the lengthening shadows retreat over the plain and ascend the hill sides, while all below fades out of view under the misty and mellow haze of summer's twilight The weary reapers return from their toil, the flocks come frisking to their folds, and the solemn hush of Nature shutting up her manifold works and retiring to rest, all conspire to soothe the troubled heart into sympathetic repose. At such an hour I saw it once and again, and often lingered until the stars looked out from the deep sky, and the breezes of evening shed soft dews on the feverish land. What a paradise was here when Solomon reigned in Jerusalem, and sang of the ' rose of Sharon !' Better still will it be when He that is greater than Solomon shall sit on the throne of David his father ; for ' in his days shall the righteous flourish, and abundance of peace so long as the moon endureth. The mountains shall bring peace to the people, and the little hills, by righteousness.1
1 Ps. lxxiL 3.7.
Twenty-three years ago, after this tower had been rudely
Year | Reference | Corrections | Notes |
---|---|---|---|
Late May/Early June 1834 CE | see Notes | none |
|
Footnotes1 Thomson (1861:502) wrote something in 1857 CE that may or may not recall earlier seismic damage to the walls of Caesarea during the 1834 CE Fellahin Revolt Earthquake
I recalled the day and night I spent among Caesarea's broken walls and prostrate columns more than twenty years ago. Fresh from scenes of war, and earthquake, and sickness, and death in Jerusalem, I then felt a mysterious sympathy with these sad and forsaken ruins.
1 For additional details see Mr. George Jeffrey's valuable The Church of the Holy Sepulchre, Jerusalem: Extract from the Journal of the Royal Institute of British Architects, 3rd series, Vol. XVII, Nos. 18, 19, 20.
Year | Reference | Corrections | Notes |
---|---|---|---|
1834 CE | 1834 CE | none |
Menahem Mendel of Kamieniec (1800-73) dates the event to the 30th count of the Jewish ‘Omer’. That is, the Hebrew date of Iyyar, 14th which corresponds to the Gregorian date of Friday, 23rd of May (Mendel 1839). He also notes that there were two tremors: one at noon and the second at night (Mendel 1839).
Year | Reference | Corrections | Notes |
---|---|---|---|
23 May 1834 CE | none |
|
Ambraseys (2009)
Location (with hotlink) | Status | Intensity | Notes |
---|---|---|---|
Jerusalem - Introduction | n/a | n/a | n/a |
Jerusalem - Mount Zion | possible to probable | ≥8 |
Zohar et al (2015) compared drawings from 1833 CE and earlier to drawings and photographs from 1838 CE
and later to conclude that the Ottoman minaret known as al-Nabi Da'ud on top of King David’s Sepulchre at Mount Zion was rebuilt to
a shorter size likely due to damage incurred in the 1834 CE Fellahin Revolt Quake. The contemporaneous eye-witness source Neophytos wrote that
a minaret fell in Jerusalem. Minarets are frequently damaged during earthquakes due to their vulnerability to seismic shaking. |
Dhiban | possible | Tristram et al. (1873:135), while speculating on the discovery of the Mesha Stele in 1868 CE, suggested that the Stele was first exposed during the Safed earthquake of 1 January 1837 CE probably unaware that if an earthquake from around that time exposed the Mesha Stele, it would probably have been the 1834 CE Fellahin Revolt Earthquake. | |
Location (with hotlink) | Status | Intensity | Notes |
Location (with hotlink) | Status | Intensity | Notes | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
Taninim Creek Dam | possible |
Flame structures - ~1500-~1900 CE
Marco et al (2014) observed zigzaged flame structures atop a permeable lacustrine unit wedged between
two impermeable units. They interpreted the flame structures to be a result of overpressures or liquefaction. They surmised that the liquefaction was either induced directly by seismic shaking or by loading from a
tsunami that breached the dam and placed a load of ~3 m of (additional ?) sloshing water above the sediment-water interface. Stone displacements observed on the northern part of the dam along with the
spatial distribution and the zigzaged nature of the flame structures (indicating shearing) led them to favor the tsunamogenic interpretation. If correct, a tsunamogenic interpretation suggests an
offshore slope failure during the causitive earthquake as active faults are not known to be present in this part of the coast. |
|||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Dead Sea - Seismite Types | n/a | n/a | n/a | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Dead Sea - ICDP Core 5017-1 | possible to probable | 6 | Lu et al (2020a) associated a 3 cm. thick turbidite in the core to the 1834 CE Fellahin Revolt Earthquake. CalBP is reported as 153 ± 44 yr B.P. This works out to a mean date of 1797 CE with a 1σ bound of 1753 - 1841 CE. | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Dead Sea - En Gedi | possible | see table |
Potential Seismites in En Gedi
Migowski et. al. (2004) identified several seismites from around this time.
|
||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Dead Sea - Nahal Ze 'elim | possible | n/a |
Potential Seismites at site ZA-1
At site ZA-1, Ken-Tor et al (2001a) identified two seismites from around this time. Event H was higher up in the section.
|
||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Araba - Introduction | n/a | n/a | n/a | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Araba - Qasr Tilah | possible | ≥ 7 | Haynes et al. (2006) dated Event I to between 1515 and 1918 CE and suggested it was most likely a result of the 1546 CE earthquake. | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Araba - Taybeh Trench | possible | ≥ 7 | LeFevre et al. (2018) dated Event E1 to 1744 CE ± 56. | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Araba - Trenches in Aqaba | possible | ≥ 7 |
Niemi (2011:153) noted that the most recent scarp-forming event fault [in Trench AQ-1] occurred after A.D. 1045-1278 based on a corrected, calibrated radiocarbon age from charcoal collected from a buried campfire at the base of the scarp in Trench T-1. This likely represents fault motion in one of the historical earthquakes affecting southern Jordan (e.g. 1068, 1212, 1458, or 1588). |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Location (with hotlink) | Status | Intensity | Notes |
Lu et al (2020a)
associated a 3 cm. thick turbidite in the core to the 1834 CE Fellahin Revolt Earthquake.
CalBP is reported as 153 ± 44 yr B.P. This works out to a mean date of 1797 CE with a 1σ
bound of 1753 - 1841 CE. Ages come from
Kitagawa et al (2017).
The deposit is described as a 3 cm. thick turbidite (MMD). Lu et al (2020) estimated local seismic intensity
of VI which they converted to Peak Horizontal Ground Acceleration (PGA) of 0.09 g. Dr. Yin Lu relates that "this estimate was based on previous studies of turbidites
around the world (thickness vs. MMI)" (
Moernaut et al, 2014). The turbidite was identified in the depocenter composite core 5017-1 (Holes A-H).
See the following from
Lu et al (2020b) regarding estimating intensity from turbidites:
Previous studies have revealed that the intensity threshold for triggering historic turbidites are variable in different regions and range from MMI V½ to VII½ (Howarth et al., 2014; Moernaut, 2020; Van Daele et al., 2015; Wilhelm et al., 2016). The intensity threshold constrained from the Dead Sea data (≥VI½) is situated in the middle of this range.
Previous studies in Chilean lakes have indicated that the (cumulative) thickness of historic turbidites across multiple cores correlates with seismic intensity, and can thus be used to infer paleo-intensities in this setting (Moernaut et al., 2014). However, in the case of the Dead Sea core 5017-1, there is a random relationship (a correlation factor of 0.04) between the thickness of prehistoric turbidites and seismic intensity (Figure 5a).
Migowski et. al. (2004) identified several seismites from around this time.
Depth (cm.) | Thickness (cm.) | Seismite Type | Min. Intensity | Max. Intensity | Quake Assignment (Migowski) | Quake Assignment (Williams) |
---|---|---|---|---|---|---|
-13 | 10 | 4 | 8.2 | 9.0 | 1927 CE | not assigned |
3 | 3 | 4 | 8.0 | 8.8 | 1837 CE | 1834 CE |
8 | 3 | 4 | 8.0 | 8.8 | 1822 CE | not assigned - 1822 CE Quake unlikely - too far away |
22 | 2 | 4 | 8.0 | 8.8 | 1759 CE | not assigned |
27 | 12 | 4 | 8.2 | 9.0 | 1712 CE | not assigned |
41 | 4.8 | 4 | 8.1 | 8.9 | 1656 CE | not assigned |
52 | 1 | 1 | 5.6 | 7.0 | 1588 CE | not assigned |
At site ZA-1, Ken-Tor et al (2001a) identified two seismites from around this time. Event H was higher up in the section.
Event | Thickness (cm.) | Seismite Type | Modeled Age (± 2σ) | Intensities | Quake Assignment (Ken-Tor) | Quake Assignment (Williams) |
---|---|---|---|---|---|---|
G | 50 | Liquefied Sand | 1815 CE ± 145 | unavailable for now - different mechanism | 1834 CE Quake | not assigned |
H | 30 | Liquefied Sand | 1595 CE ± 75 | unavailable for now - different mechanism | 1927 CE Quake | not assigned |
Haynes et al. (2006) dated Event I to between 1515 and 1918 CE and suggested it was most likely a result of the 1546 CE earthquake.
LeFevre et al. (2018) dated Event E1 to 1744 CE ± 56.
Niemi (2011:153) noted that the most recent scarp-forming event fault [in Trench AQ-1]
occurred after A.D. 1045-1278 based on a corrected,
calibrated radiocarbon age from charcoal collected
from a buried campfire at the base of the scarp in
Trench T-1. This likely represents fault motion in one
of the historical earthquakes affecting southern
Jordan (e.g. 1068, 1212, 1458, or 1588).
Time | Date | Time Uncertainty | Type of Quake | Reliability | Zone | Most Damaged or felt locations | Reported Damage Localities | Estimated magnitude in previous studies |
---|---|---|---|---|---|---|---|---|
13:00 | 26 May 1834 CE. | n/a | Main and Aftershock | Very High | Central (Israel and southern Lebanon) | Palestine |
|
|
AD 1834 May 26 Palestine
The earthquake happened at 13 h on 26 May 1834 in
Palestine during the 1834 revolt at the time of the siege
of Jerusalem by the fellahin, who entered the city on the
day after the earthquake (Rustam 1923, 17).
In Jerusalem part of the wall, where it forms the
outer enclosure of the al-Aqsa mosque, crumbled during
the first shock, and some houses and tops of minarets
fell (Nicolayson 1911, 83-89). One minaret in the city and
another on the Mount of Olives were shaken down, and
the cupola of the church of the Ascension caved in (Spyridon
1938). The church of St Prodromos and the masonry
dome of the church of the Holy Sepulchre were damaged
(PEMS 1834, 176) and, according to others, collapsed
(Thompson 1835). In fact the structure was only damaged,
with the French and Russians pledging to finance its
repair. Houses suffered various degrees of damage without
loss of life.
In Bethlehem, 8 km south of Jerusalem, the
Church of the Nativity, which had become degraded
through neglect, was damaged and the walls of the
Church of the Cross were cracked. The church of
the monastery of Deir Mar Saba, 9 km southeast of
Jerusalem, was cracked in two places and two of its belfries
were thrown down (PEMS 1834, 176).
It is said that east of the Dead Sea the earthquake
toppled the Moabite monolith of Meisha at Dhiban and
damaged historical remains at Madaba, Umm al-Rassas
and ai-Rahba (Klein 1868; Anderson 1997). Also, after
the earthquake of 1834, a large quantity of asphalt was
apparently cast onto the shore near the southwestern corner
of the Dead Sea, three tons of which were brought to
market by the natives. An identical incident was reported
after the earthquake of 1837, with the asphalt driven
aground on the western side of the Lisan not far from
Jabel Usdun.
On the Mediterranean coast in Jaffa, 54 km west
of Jerusalem, according to letters from eye-witnesses,
the shocks caused some concern and damaged a few
dilapidated free-standing walls, cracking house ceilings
(Thompson 1835).
Also in Caesaraea, 85 km northwest of Jerusalem,
parts of the remaining old walls and of some houses fell,
while four nearby villages were also affected, without
casualties (Poujoulat 1840, 154).
The shock was felt along the Mediterranean coast
from Gaza and Ascalon Caesaraea to Acre, but not at
Tiberias, whch at the time had fallen to the fellahin.
Despite the relatively large number of sources
that refer to this earthquake, it is not possible to locate its
epicentral region (Blanckenhorn 1905; Macalister 1918,
142; Tobler 1856, 34).
Ambraseys, N. N. (2009). Earthquakes in the Mediterranean and Middle East: a multidisciplinary study of seismicity up to 1900.
Time | Date | Discussion | Sources |
---|---|---|---|
04 | 26 May 1834 CE. |
|
|
Time | Date | Lat. (°N) |
Long. (°E) |
Location | I0 | ML | Discussion |
---|---|---|---|---|---|---|---|
0400 | 23 May 1834 CE. | 31.3 | 35.6 | East of the Lisan | X | 6.3 |
|
23 MAY 1834, 31.3° N 35.6° E
- East of Lisan, I0 = XI the following towns and sites were damaged: Jerusalem, Bethlehem, Nablus, Gaza, the monastery of Mar-Saba as well as Karak; appearance of large blocks of Asphalt floating on the Dead Sea,..., many columns and arcades of the towns of Moab are fallen, ML = 6.3 (BM1).
- 1834 A.D., Syria, Palestine, Acre, Jerusalem, Ascalon, Gaza, Tiberias, very strong, several churches were damaged in Jerusalem (Will).
French23 MAI 1834, 31°,3 N 35°,6 E
- à l'Est du Lisan, I0 = XI les villes et sites suivants ont été endommagés : Jérusalem, Bétléhem, Naplouse, Gaza, le monastère de Mar-Saba ainsi que Karak; apparition de larges blocs d'Asphalte flottant sur la Mer Morte,..., beaucoup de colonnes et d'arcades des villes de Moab sont tombées, ML = 6,3 (BM1).
- 1834 apr. J.C., Syrie, Palestine, Acre, Jérusalem, Askalane, Gaza, Tiberias, très fort, plusieurs églises ont été endommagées à Jérusalem (Will).
Investigation of damage reports in Nablus and Tiberias
Arvanitakis (1903) lists Tiberias as receiving damage - cites Archive of the Greek Patriarchs as a source
Milne (1911) no mention of damage in Tiberias or Nablus
Blanckenhorn (1905)
Perrey (1850)
Willis (1928) lists Tiberias - cites Perrey (1850), Arvanitakis (1903), and Vigouroux (1912)
Sieberg (1932a) - 1834 earthquake is not listed
Sieberg (1932b) - lists damage in Tiberias but not Nablus - does not cite a source - 1834, Mai 23, Ausgebreitetes Erdbeben in Palestina, gemeldet aus Hasse, Askalon, Akko und Tabarlje. In Jerusalem kraftige
Schaden an Hausern und einigen Kirchen.
Legendre, A. (1912) - lists the 1837 earthquake but not the 1834 earthquake in his brief catalogue.
Source Information
Ambraseys does not list Anderson (1997) in his references but he does list the following :
Anderson, H., Jackson, J. (1987), 'Active tectonics of the Adriatic region', GJRAS, 91, 937-983.
Ambraseys does not list Klein (1868) in his references but he does list the following :
Dowling, T. E. (1913). The orthodox Greek patriarchate of Jerusalem, Society for promoting Christian knowledge.
Klein, S. (1939), 'Remarks on the article by J. Braslayski', Zion, N.S, 4, 90.
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