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1837 CE Safed Quake

1 Jan. 1837 CE

by Jefferson Williams








Damage Distribution from 1837 CE Safed Quake
   Fig. 1a - Damage distribution in Ottoman Palestine and its close surroundings
   caused by the 1837 earthquake (Ambraseys 1997, 2009) and classified by
   the degree of severity (Zohar et al. 2013) - from Zohar (2017)


Introduction & Summary

On 1 January 1837 CE between 430 and 500 pm, a powerful earthquake struck the central and northern Galilee and and many towns and villages mostly to the Northwest although there are reports of heavy damage to the east as well. Of the major towns, Safed suffered the worst with some estimates of as many as 4000-5000 deaths (other estimates are lower). Safed was described afterwards as no longer existing and was probably subject to a catastrophic landslide. William McClure Thomson visited Safed 17 days after the shock and reported that in the Jewish part of town houses on top of its steep slope fell on houses below until at the bottom of the slope, the lower houses were covered up to a great depth with the ruins of many others. Katz and Crouvi (2007) examined slope stability in Safed and concluded that landslides occurred during earthquakes in 1759 and 1837 CE. The earthquake was reported to have been felt from Antioch to Egypt and aftershocks continued for months. In the Galilee, some villages were reported to have been destroyed while nearby ones were barely affected suggesting site effects were at play. Ambraseys (1997) estimated a Magnitude (MS) of 7.0-7.1 and suggested that it may have been a multiple event. Ambraseys (2009) suggested it was a shallow event that may have broken along or in the vicinity of the Roum Fault. Nemer and Meghraoui (2006) also suggested that this earthquake may have been due to slip along or near to the Roum Fault.

LIke the 1759 CE Safed and Baalbek Quakes, there are numerous sources for this earthquake and, unfortunately, I was not able to access all of them. It is anticipated that this entry will expand over time as I gain more access.

Textual Evidence

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
The Times English
Background

n/a March and April 1837 CE London The Times generated two news reports for the 1837 CE Safed Quake. The first, published on 1 March 1837 CE, included a letter from the British Consul in Beirut and estimated 3000 victims and extensive destruction in Safed, Tiberias, and surrounding villages, The second report, published on 12 April 1837 CE, contained an extensive list of towns, cities, and villages affected along with estimates of structural damage and the number of people killed - which had more than doubled from the initial report.
Article in the Missionary Herald by William McClure Thomson English
Biography

Protestant Christian November 1837 CE William McClure Thomson experienced the earthquake in Beirut and engaged in a relief mission to a number of towns and villages affected by the earthquake reaching Safed 17 days after the main shock. He wrote up an extensive description of the damage and human suffering in the Missionary Herald 10 months later.
Edward Robinson English
Biography

1838 CE Edward Robinson visited Safed and other affected towns about 18 months after the 1837 CE Safed Quake. He supplied many observations of seismic effects. He also reported second hand accounts that a large mass of bitumen the size of an island or a house was discovered floating on the Dead Sea and the castle at Hunin was rendered uninhabitable - both after the 1837 CE Safed Earthquake.
The Land and The Book by William McClure Thomson English
Biography

Protestant Christian 1857 CE based on first hand recollections 20 years earlier. William McClure Thomson experienced the earthquake in Beirut and engaged in a relief mission to a number of towns and villages affected by the earthquake reaching Safed 17 days after the main shock. He wrote up an extensive description of the damage and human suffering in The Land and the Book 20 years later. It contains some additional details that were not present in his original report in the Missionary Herald.
Other Authors
Text (with hotlink) Original Language Biographical Info Religion Date of Composition Location Composed Notes
Damage Reports from Textual Sources

Seismic Effects

´ Seismic Effects from Amiran et al (1994)

  • According to an official report (89), 4,083 people were killed, including a few hundred in Lebanon.
  • The severest damage occurred in Safed and in Tiberias.
  • In addition to the destruction in these two towns, 1,480 houses were ruined elsewhere.
  • Beirut: some damage to buildings
  • Sidon: some houses collapsed; many were damaged. A few persons were killed.
  • Tyre: damage to the city wall and the mediaeval cathedral. Many houses collapsed. Twelve people were killed, 30 injured. The inhabitants evacuated the town for a number of days.
  • Rockfalls inside Banias cave.
  • Hunin: severe damage to the castle.
  • Sa'sa unaffected (?!).
  • el-Jish: destructive, MMS X, 235 victims (91).
  • Qaddita: severe, MMS IX—X.
  • Ein Zeitun: destructive, MMS X (91).
  • Safed: centre of destruction, MMS X. 2,158 people killed in Safed and surrounding villages (89). Clefts in the ground. Houses on the steep slopes fell one on the other (88; 91).
  • Tiberias: destructive, MMS X. 922 victims (28% of the population), city walls overthrown. Seventeen of the 23 villages in the district severely damaged (89). The output of the Hot Springs increased considerably for a number of days. A seiche swept the shores of the lake, killing many people (W; 90; 48:902; 14:169; cf. Appendix 6).
  • Lubya: severe, MMS VIII, 143 victims.
  • Sejera: destructive, MMS IX—X.
  • Kafr Kenna: very light damage only, MMS V.
  • er-Reina: destructive, MMS X (91).
  • Nazareth: 5 killed, moderate damage to buildings, MMS VII.
  • Saffuria: almost unaffected, MMS IV—V.
  • `Akko: part of the fortifications overthrown, several persons killed and injured (90).
  • Haifa: MMS VII.
  • `Atlit: one side of the wall damaged.
  • In Samaria, damage was reported from `Araba, `Ajja, Jain`, Burqa, Zeita, `Attil Qaryat Jit.
  • Nablus: strong, MMS VII, several persons killed (88).
  • Jerusalem, Bethlehem: moderate (68:326).
  • Hebron: moderate, MMS IV (68:326).
  • Qaqun, Jaffa, Ramie, Gaza: tremor felt, no damage.
  • Kerak: 20 houses collapsed.
  • In the Dead Sea large blocks of bitumen broke off, floating on the water (84).
  • Musil was told that the ford crossing the Dead Sea from the Lisan Peninsula to the shore of Masada disappeared as the result of this earthquake (92).

Locations

Reported damaged localities from Zohar et al. (2016: Table 3)

Nabatiya
Qana
el-Fara
el-Salha
Jish
Marun Al-Ras
Bint-Jbeil
Malkiyya
Qadas
Yaâtar
Tebnine
Hunin Castle
Baniyas [Israel]
Metula
Zeqqieh
Deir Mimas
el-Khiam
el-Tahta
Deir Mar-Elias
Qaddita
Jibshit
Gaza
Arraba
Attil
Qaqun
Tubas
Ajloon
Nablus
Zeita
Harithiya
Jerusalem
Kfar Birâim
Lake Tiberias
Hasbaya
Kafr Aqab
Jeresh.
Areopolis
Hula
Tarshiha
Dallata
Jaffa
Mrar
Ein-Zeitun
Tyre
Atlit
Meron
Eilabun
Akko
Migdal
Irbid
Reina
Safed
Tiberias
Hadatha
Haifa
Zemah
Kafr Kanna
Kafr
Sabt
Lubiya
Nazereth

The Times

Background

Background

Excerpts
The Times 1 March 1837 CE

  • from The Times - 1 March 1837 CE
LATE EARTHQUAKE IN PALESTINE.
LETTER FROM MR. CHASSEBAUD, THE BRITISH CONSUL, DATED BEYROUT, JAN. 25, AND ADDRESSED TO MR. JUDAH BENOLIEL, OF GIBRALTAR

" Dear Sir, —I have a most painful task to perform — that of announcing the deaths of out much esteemed friends Mr. and Mrs. Joshua Levy, of Saffet, and the greater part of their family. I address myself to you on the occasion, instead or doing so to Mr. Joshua Levy's brother and the other near relatives he may have at your place, in order that You may convey the melancholy tidings to them after you have prepared them. This horrible catastrophe took place on Sunday, the [latlnat?], late in the afternoon, though before sunset, where a most violent shock of earthquake destroyed the whale of Saffet, Tiberias, and many of the surrounding villages, to which our much-lamented friends, Mr.and Mrs. Levy, and the greater part of their family, fell victims, with about 500 other Israelites, and as many Christians and Mussulmans, at Saffet only, without including the great many persons mortally wounded or maimed, and those who were dug out of the ruins, eight or ten days after, alive, but starved, and in a dying state. Such an appalling scene is seldom to be met with in the annals of history, and my heart fails in attempting to give you further particulars. While I lament the lots of those friends who fell, I am happy to say that Mr. Moses Levy, the eldest son of our friend Mr. Joshua Levy (a lad about 14 years old), as well as Mr. Joshua Levy's sister Mrs. Deborah Cohen, and two of her daughters, escaped unhurt, and they say they intend soon returning to Gibraltar. It was only the 5th instant (five days after the earthquake) that the few survivors of Saffet recovered from their stupor, and dispatched messengers to this and other places for assistance to remove the ruins and bury the dead, and also for tents, coverings, provisions, surgical aid, etc., for the maimed and wounded, none of which they could obtain from the surrounding villages, which had shared the same fate. We immediately opened a subscription here, and sent them what we could."
Another account estimates the whole number of victims at 3,000.

In consequence of the above melancholy Intelligence the Hebrew community of Gibraltar caused a funeral service to be performed at the principal synagogue there on the 15th instant during which all their places of business were closed, and immediately after a subscription was opened at the counting-house of Mr. Judah Benoliel, to which the said community contributed very liberally, so, as to enable that gentleman to forward a considerable sum of money by the packet about to depart for Malta for the relief of the surviving sufferers.

— Gibraltar Chronicle of the 17th.

The Times 12 April 1837 CE

  • from The Times - 12 April 1837
  • WARNING: Many transcription errors
EARTHQUAKE IN SYRIA.

The following return of the devastation caused by this great convulsion of nature has been prepared by the British agent at Beyrout:-

A LIST OF TOWNS ETC., DESTROYED OR INJURED SYRIA BY THE EARTHQUAKE ON THE 1st OF JANUARY

The Times 1 March 1837 CE - image

  • from The Times - 1 March 1837 CE

The Times 12 April 1837 CE - image

  • from The Times - 12 April 1837

Chronology
Year Reference Corrections Notes
Late in the Afternoon on Sunday 1 January 1837 CE Sunday late in the afternoon though before sunset on the 1st of January none
Seismic Effects Locations
Damage List

  • from The Times - 12 April 1837
  • WARNING: Many transcription errors

Online Versions and Further Reading
References

Article in the Missionary Herald by William McClure Thomson

Biography

Biography

Excerpts
English from Thomson (1837)

Syria and the Holy Land.

JOURNAL OF MR. W. M. THOMSON ON A VISIT TO SAFET AND TIBERIAS.

THE introductory paragraphs of the journal will sufficiently disclose the circumstances under which it was written; and as no other so full and authentic an account of the effects of the terrible event which it describes, is known to have reached this country, the document is inserted almost entire. The paragraphs under the first date were written at Neby Yoonas, where Mr. T. spent the first night after leaving Beyroot.
From Beyroot to Tyre

January 13, 1837. The first day of this year will be long remembered as the anniversary of one of the most violent and destructive earthquakes which this country has ever experienced. The shock occurred at half past four o’clock, P. M., and was neither preceded or followed by any remarkable phenomena. A pale smoky haze obscured the sun and have a touch of sadness to the scene, and a lifeless and almost oppressive calm settled down upon the face of nature; but these appearances are not uncommon in this country.

In Beyroot itself but little injury was sustained, although very many of the houses were badly cracked, but on the river flat, east of the town, the houses were greatly injured, some thrown down, and a few persons wounded. For several days succeeding the shock flying reports from various quarters gave frightful accounts of towns and villages overthrown and lives lost; but so slow does authentic information travel in this country, that it was not until eight days had elapsed, that any reports which ‘could be relied on were received. Letters arrived on that day from Safet, stating that the place was utterly destroyed, not a house remaining of any description; and that Tiberias and many other places had shared the same deplorable fate. Some of the letters stated that not more than one out of a hundred of the inhabitants had escaped, while others more correctly declared that out of a population of 10,000 at least 6,000 had perished.

As soon as these awful facts were sufficiently ascertained to justify it, collections were taken up at Beyroot to relieve the survivors, and persons appointed to proceed to the scene of distress and superintend the distribution of the articles and assist in taking care of the wounded. To aid in this work, and also to obtain accurate information, so that further measures and more effectual might be adopted to relieve their distress, Mr. Calman and myself left our homes this morning for Safet. Seven hours hard riding brought us to this noted locality, where the great whale cast forth the rebellious prophet. So tradition declares; and as no one can prove the contrary, and the smooth sand beach renders the place altogether adapted to the purpose, the people rest quite assured of the fact.

I do not remember any occasion when I left my family with greater anxiety than on the present. So large a circle, with so many cares, my own work already so accumulated upon my hands, my health doubtful, while the season promised nothing but bad roads, storms of rain and snow, and on the mountains fierce cold. He, however, in whom our life is, can easily protect all concerned, both at home and abroad, from every evil, and render our journey prosperous and profitable. My ardent desire is to promote the glory of God and honor the gospel amongst the Jews and Moslems of that region, by alleviating the sufferings of the poor, the sick, the wounded, and orphan; and this will be cheaply purchased at any expense of time, toil, and danger.

Spent a large portion of this evening in reading and explaining the history of Jonah to a Turk. I read also and examined the third chapter of John to him, and endeavored to convince him that there was no savior but Christ, and no possibility of reaching the kingdom of heaven without a new heart. He listened more patiently than any Moslem I have conversed with, but was very loth to admit the doctrines taught; perhaps the more so as several Maronite Christians were present.

14. Leaving a sleepless couch long before it was light, we made an early start, and crossing the little river called Nehar II Owel, and passing through the rich and beautiful gardens which environ that ancient and great city, we entered Sidon. here we were joined by the English consular agent, seignor Abello, and his two sons. After a hasty breakfast we set off for this place, but so slow do animals and Arabs move in this country, that it was not until ten o'clock at night that we reached Tyre. Cold, muddy, and hungry, we lay down without a fire, in a house so terribly shattered by the earthquake as to promise a grave rather than a shelter. The owner of the house, the United States consular agent, would on no account consent to sleep in it. At Sidon from seventy to one hundred houses had been altogether, or in part, thrown down, and nearly all were badly cracked, while seven persons were reported to have been killed. In this place the destruction is far greater. We rode into town last night over the prostrate wall. The road was nearly blocked up with ruins, and every where the wind, now blowing almost a hurricane, growled through shattered walls and broken windows; while half suspended shutters and unclosed doors were creaking, clattering, and banging in dreadful 'confusion. My horse absolutely refused to enter the frightful place, until I descended, and quieting her fears, led her into town.

15. Spent this morning in prayer and reading the Scriptures, after which we took a survey of the place, gave medicine to the wounded; and although it was the Lord's day, we proposed to leave for Safet. The accounts from that place are so distressing as to leave no doubt on our minds that it is a work of mercy to hasten to the relief of the sufferers, even by traveling on this sacred day. Tyre is considered by the inhabitants as nearly ruined, and not even the best houses will be habitable without tearing down and rebuilding a large part of what remains. Twelve persons were killed at the time of the earthquake and thirty wounded.

16. Slept at Kahnah last night, a village about three hours from Tyre, The earthquake has not been very destructive in this place or vicinity, but the people are afraid to sleep in their shattered houses, especially as the earth still continues to tremble. Our ride yesterday evening was delightful and refreshing. The wind, which had hitherto been strong and cold, had now settled into a soft southern breeze, the sky had cleared up, and all nature smiled. The road took us over Alexander's famous causeway, passed a strong castle dreadfully shattered and partly fallen, and then I leaving the sweet sea-beach for the fertile plain, we reached the mountains in a little more than an hour, by a very gradual ascent. This lovely plain has been a thousand times deluged with the blood of Europe, Asia, and Africa. This peaceful pasture-field for Syrian goats has often trembled with thundering chariots and thundering cannon, and the dreadful shock of countless cohort's rushing into battle. And these gently, gracefully swelling hills have witnessed deeds that made heaven weep and hell laugh, from the thirteen years siege of Babylon's haughty king, and the two thousand crucified victims of Alexander's brutal rage, down to the scarcely less cruel acts of the self-styled holy crusaders. How changed! Not a soul is seen of all these countless hosts, not a trophy remains to tell who fought, who conquered, and who died. Nature has kindly thrown her sweetest mantle of green over the scene; and the impertinent long-eared goat fattens on the best blood of the old world. These scenes formed the theme of conversation as we quietly pursued our way over sloping hills and up winding valleys to Kahnah; and I have seldom found natives so well informed, or so well disposed for serious conversation, as our companions. Both father and son had read the Bible with I much attention and profit, and although Catholics, were far more enlightened and liberal than the common mass of that bigoted community. One of the sons, in particular, was quarreling out-right with Paul's view of divine sovereignty, yet still in such a manner as to show clearly that he had a conscience and a heart, upon which truth had made a strong impression; and this is what we so rarely meet with in this country as to excite double interest.

From Tyre to Safet

Near to a village called Hannany we passed some very old ruins, and amongst other things, that which most interested me was a tomb, said to be the last resting-place of king David's good friend Hiram. Whether it be so or not, the very thought was interesting. To meet with a spot that hears the name of an old acquaintance, in so lonely a place as this, formed quite an agreeable incident in the evening's ride, while the tomb itself was curious and unique. On a platform of large stones, raised several feet high, is placed a huge block of limestone rock, eight or ten feet square, rudely cut, and bearing evident marks of very great antiquity. This is the tomb, or sarcophagus; and it is covered with a large flat stone, without the slightest ornament of any kind. If there ever were houses near, they have all disappeared; and this grey weather-beaten pile stands amidst a few straggling olive trees, an appropriate memento of death and olden times.

17. We came to Ramash; here we bad a melancholy confirmation of those letters which came from Safet. The place is utterly ruined, and the people are living in tents, made of broken boards, old mats, brush, grass, mud, in short every thing that could be put up to shelter them from the cold and rain. Thirty people in this small village were killed, and no doubt the destruction would have been greater, had not the inhabitants been generally in church at afternoon prayers, and only a small part of the church fell. We visited the wounded, distributed charity to the poor, and then passed on to Kefr Bureyatun, where fourteen perished, and a great number were wounded. From this to Jish is about an hour, at which place we stopped for the night. Not a house of any kind remains standing. Amongst the survivors is the shiekh of the village, who spent the evening in my tent. He gave a very particular account of the overthrow, but it is too long to repeat. He had returned to the pasha the names of two hundred and thirty-five, who perished. The remainder, amounting to nearly sixty in all, had gone to other places; so that he, and five others remained to have the property dug out from under the ruins, to bury the dead, and prepare to desert the place. Here, as well as at Ramesh, the people were at prayers in church; but alas! they shared a very different fate. The whole church fell at once, and all, except the priest, who was in the recess of the altar, perished. Thus more than one hundred and thirty died at their very altars. I visited and examined the ruined church; and it is perfectly obvious, that not one of the people in the body of the edifice could possibly have escaped. Fourteen bodies still lay unburied amongst the ruins, and the atmosphere was so infected as to render it very unpleasant to examine them.

18. In the morning, after distributing charity to a number of the poor who had been sent for, and leaving medicine with the shiekh and others for the wounded who had been removed to other villages, I took a ramble over the hill on which the place was built. A very slight examination convinced me that it was entirely of volcanic origin. All the houses had been erected of volcanic stone, and the rock strata is cast about in utter confusion. On my return to the tent I was much affected by a very simple incident. Our servant had shot several very beautiful pigeons, and upon inquiring why he had dune it, he said that the shiekh directed him to do it, as they were now wild, and left without any owners to fly about the miserable ruins. Poor little lonely creatures, the hand that scattered their daily supply of wheat and pulse is crushed and broken, and those who once delighted to witness their innocent sport, and listen to their lively chatter, are now all mouldering in the cold grave. I called the shiekh to ascertain whether some one had not survived the overthrow to whom those pretty birds would properly belong; and after sometime he recollected an old woman, a distant relative of the lost family; leaving a present for her, we mounted our horses and hurried away from a scene of such dreadful wretchedness.

The shiekh sent a man to shew us a large rent in the mountain, a little to the east of the village. It may now be about a foot wide and fifty feet long; probably it has gradually closed up, as from their accounts it was wider when first discovered after the shock. The road to Safet carried us over an elevated plain entirely covered with volcanic rock, of a very ancient and weather-beaten character. A small lake or pond on the highest part, I suppose, marks the site of a long extinguished crater. We passed a village called Cudditha nearly destroyed; and in the valley immediately under Safet, Ayne-Zatoon in utter ruin; but we did not stop to examine them. We met many Jews going out to Mottenna, a village two hours from Safet, to pray to a celebrated saint of theirs. Poor refuge in times of such distress! Just before we began to ascend the mountain of Safet, we met our consular agent of Sidon, returning home with his widowed sister. His brother-in-law, a rich merchant of Safet, had been buried up to his neck by the ruins of his fallen house, and in that awful condition remained several days, begging and calling for help, and at last died before any one was found to assist him! As we ascended the steep mountain we saw several dreadful rents and cracks in the earth and rocks, giving painful indications of what might be expected above. But all anticipations were utterly confounded, when the reality burst upon our sight.

Overthrow and Ruins of Safet — Distressing Scenes witnessed

Up to this moment I had refused to credit the account, but one frightful glance convinced me that it was not in the power of language to over state such a ruin. Suffice it to say that this great town, which seemed to me like a beehive four years ago, and was still more so only eighteen days ago, is now no more. Safet was, but is not. The Jewish portion, containing a population of five or six thousand, was built around and upon a very steep mountain; so steep, indeed, is the hill, and so compactly built was the town, that the roof of the lower house formed the street of the one above, thus rising like a stairway one over another. And this, when the tremendous shock dashed every house to the ground in a moment, the first fell upon the second, the second upon the third, that on the next, and so on to the end. And this is the true cause of the almost unprecedented destruction of life. Some of the lower houses are covered up to a great depth with the ruins of many others which were above them. From this cause also it occurred that a vast number, who were not instantaneously killed, perished before they could be dug out; and some were taken out five, six, and one I was told, seven days after the shock, still alive. One solitary man, who had been a husband and a father, told me that he found his wife with one child under her arm, and the babe with the breast still in its mouth. He supposed the babe had not been killed by the falling ruins, but had died of hunger, endeavoring to draw nourishment from the breast of its lifeless mother! Parents frequently told me that they heard the voices of their little ones crying papa papa, mamma, mamma, fainter and fainter, until hushed in death, while they were either struggling in despair, to free themselves, or laboring to remove the fallen timber and rocks from their children. 0 God of mercy! what a scene of horror must have been that long black night, which closed upon them in half an hour after the overthrow! without a light, or possibility of getting one, four fifths of the whole population under the ruins, dead or dying with frightful groans, and the earth still trembling and shaking as if terrified with the desolation she had wrought!

What a dismal spectacle! As far as the eye can reach, nothing is seen but one vast chaos of stone and earth, timber and boards, tables, chairs, beds, and clothing, mingled in horrible confusion. Men every where at work, worn out and wo-begone, uncovering their houses in search of the mangled and putrefied bodies of departed friends; while here and there I noticed companies of two or three each, clambering over the ruins, bearing a dreadful load of corruption to the narrow house appointed for all living. I covered my face and passed on through the half living, wretched remnants of Safet. Some were weeping in despair, and some laughing in callousness still more distressing. Here and old man sat solitary on the wreck of his once crowded house, there a child was at play too young to realize that it had neither father nor mother, brother nor relation in the wide world. They flocked around us — husbands that had lost their wives, wives their husbands, parents without children, children without parents, and not a few left the solitary remnants of large connections. The people were scattered abroad above and below the ruins in tents of old boards, old carpets, mats, canvass, brush, and earth, and not a few dwelling in the open air; while some poor wretches, wounded and bruised, were left amongst the prostrate buildings, every moment exposed to death, from the loose rocks around and above them.

As soon as our tent was pitched, Mr. C. and myself set off to visit the wounded. Creeping under a wretched covering, intended for a tent, the first we came to, we found an emaciated young female lying on the ground, covered with the filthiest garments I ever saw. After examining several wounds, all in a state of mortification, the poor old creature that was waiting on her, lifted up the cover of her feet, when a moment's glance convinced me that she could not possibly survive another day. The foot had dropped off, and the flesh also, leaving the leg-bone altogether bare! Sending some laudanum to relieve the intolerable agony of her last hours, we went on to other but equally dreadful scenes. Not to shock the feelings by detailing what we saw, I will only mention one other case; and I do it to show what immense suffering these poor people have endured for the last eighteen days. clambering over a pile of ruins, and entering a low vault by a hole, I found eight of the wounded crowded together under a vast pile of crumbling rocks. Some with legs broken in two or three places, others so horribly lacerated and swollen as scarcely to retain the shape of mortals; while all, left without washing, changing bandages, or dressing the wounds, were in such a deplorable state as rendered it impossible for us to remain with them long enough to do them any good. Although protected by spirits of camphor, breathing through my hand-kerchief dipped in it, and fortified with a good share of resolution, I was obliged to retreat. Convinced that while in such charnel houses as this, without air but such as would be fatal to the life of a healthy person, no medicines would afford relief, we returned to our tent, resolving to erect a large shanty of boards, broken doors, and timber, for the accommodation of the wounded. The remainder of our first day was spent in making preparations for erecting this little hospital.

19. This has been a very busy day, but still our work advanced slowly. We found the greatest difficulty to get boards and timber, and when the carpenters came, they were without proper tools. In time, however, we got something in shape of saws, axes, nails, and mattocks, and alt of us laboring hard, before night the result began to appear. The governor visited and greatly praised our work, declaring that he had not thought such a thing could have been erected; and that the government had not been able to obtain half so good a place for its own accommodation. Some of the wounded were brought and laid down before us, long before any part of the building was ready for their reception, and are now actually sheltered in it, although it is altogether unfinished. After dark I accompanied the priest, to visit the remainder of the christian population of Safet. They were never numerous, and having lost about one half of their number, are now crowded into one great tent. Several were wounded; to these we gave medicine. Some were orphans, to whom we gave clothing, and the poor people had their necessities supplied as well as our limited means would justify. Amongst the survivors is a worthy man, who has long wished to be connected with us, and in whom we have felt much interest. He applied about a year ago to have his son admitted to our high school, but he was then too young. When I left Beyroot it was my intention to bring this lad with me on my return, should he be alive; but alas! his afflicted father has to mourn not only his death, but that of his mother and all his lovely family but one.

The earth continues to tremble and shake. There have been many slight, and some very violent shocks since we arrived. About three o'clock today, while I was on the roof of our shanty nailing down boards, we had a tremendous shock. A cloud of dust arose above the falling ruins, and the people all rushed out from them in dismay. Many began to pray with loud and lamentable cries; and females beat their bare breasts with all their strength, and tore their garments in despair. The workmen threw down their tools and fled. Soon, however, order was restored, and we proceeded as usual. I did not feel this shock, owing to the fact that the roof of the shanty was shaking all the time. Once, however, the jerk was so sudden and violent as to affect my chest and arms precisely like an electric shock.

Ride to Tiberias — Effects of the Earthquake there

20. Tiberias. Having finished our work, collected the wounded, distributed medicine and clean bandages for dressing the wounds, and hired a native physician to attend the hospital, we left Safet about half past one o'clock, P. M.; and, after a pleasant ride of five hours and a half, encamped before the ruins of this celebrated city. It was truly refreshing to breathe once more the pure air of the open country, freed from the horrible sights which have been ever before me, both waking and sleeping, during our stay at Safet. We passed rapidly down the steep mountain under the at rock where Jeremiah is said to have hid the ark, across the fertile vale of Gennesaret, through the miserable village of Migdol, and along the shore of the beautiful lake, whose sweet waters dashed with gentle murmurs on the sacred shore. A train of emotions stole over the heart, more agreeable than sad, although the eye was filled with tears at the recollection of what we had already witnessed, and at the thought of that which we had in prospect. I shall not soon lose the impression of this ride. Not a breeze stirred the smooth surface of the Gennesaret, nor a leaf trembled on the topmost bough of the mountain pine. The sun settled quietly down behind the hills of Nazareth, and the full pale moon shone dimly through a hazy atmosphere on lake and land, faintly revealing the mountains of Bashan, the snows of Jible II Sheikh, and the place where Safet was, that “city set upon a hill which could not be hid” — and the mountain, where the Savior preached the best sermon the world ever heard, and near which he is said to have fed the five thousand with the five barley loaves. These and many other places, rich in sacred associations, were seen in misty outline stretching far away from Gennesaret, sweet Gennesaret, lovely shore. While the tinkling bell, the lowing kine, the bleating flocks, and the barking dogs struck a chord oft struck before at home — my father’s, mother’s, boyhood’s home.

21. The destruction of life at Tiberias has not been so great, in proportion to the population, as at Safet, owing mainly to the fact, that Tiberias is built on a level plain, and Safet on the declivity of the mountain. Probably about seven hundred perished here, out of a population of twenty-five hundred; while at Safet four thousand out of five thousand Christians and Jews were killed; and not far from one thousand Mussulmans.

We visited all the wounded to-day, and find them much more comfortably arranged in tents than at Safet. There has been better order and more enterprise amongst the people, who are said to be of a higher character than those of Safet, and less affected by those violent party divisions which agitate the Jewish community. As an instance of the confusion and wretchedness that prevailed during the first days after the earthquake, take the case of the only Jewish physician in Tiberias. He is immensely wealthy; his wife and children were killed at his feet, his own leg broken off below the knee, and held fast by the rocks which had fallen upon it. In this condition he continued two whole days, begging and crying for some one to come and take away the few stones that were upon him and set him free. He rose in his offer to three hundred dollars: but to no effect; every one had his own wife, or children, or friends in the same condition, and none would attend. At length the flies got to his wife and children, and to his own wound, when in despair he seized a pole which lay near him and tried to bring down upon his head some stone that lay above him, in order to end both his life and sufferings at the same time. Still, this man is now doing well, and promises soon to recover, In the afternoon we went down to the hot baths, which are not injured in the least, although not more than a mile and a half, from the city, where every wall is thrown down. The rooms attached to the bath are filled with wounded, some of them in a most deplorable condition, to whom we gave medicine and clothes. We all took the bath, but the water was too hot to be either agreeable or healthy. As the thermometer rose to the top of the scale instantly. I have no means of ascertaining how great the heat in the spring is. To me it seemed hotter than when I was here four years ago, and the sulphurous gas escaping from the surface much more offensive. The people informed me that at the time of the earthquake, and for some days subsequent to it, the quantity of water was immensely increased; and it was so hot as to render it impossible to pass along the road across which it flows. This I suppose to have been the fact, but the numerous stories about smoke and boiling water issuing from many places, and fire in others, I believe were mere fabrications. I could find no one who had actually seen these phenomena, although nearly all had heard of them.

Villages from Tiberias to Nazareth

22. Nazareth. We spent this morning in distributing charity to the poor, and medicine to the sick, and then set off for this place. Our road for the first two hours carried us over a very fertile country, covered with volcanic stones. The houses of Tiberias are entirely built of this stone; and there can be but little doubt that the lake itself was formed by a volcano. One hour and a half from Tiberias we turned aside from the road to examine the spot where tradition states that our Savior fed the hungry multitude with the barley loaves. The situation is very well adapted to the narrative, at least so far as "much grass" is concerned. Indeed I have seldom seen richer pastures, even in America, than on the hills and plains of Galilee. The Mount of Beatitudes is but 'a small distance from this to the west, and the hill of Safet rises in bold relief to the northeast, beyond a most lovely plain. This elevated plain, owing to the different states of cultivation and the various kinds of grain and grass which covered it, was most beautifully variegated, like a rich carpet. So striking was the resemblance, that even our Arab attendants called out to us to look at the "sejady keberry" — the great carpet. After we had broken off some specimens from the rock upon which our Savior is said to have stood when he taught the people, we proceeded on our way, and in an hour reached Luby. At this village I slept four years ago. Now it is one ghastly heap of ruins. One hundred and forty-three of the poor people were killed. The old sheikh escaped, while his whole family, eleven in number, perished. This was once a considerable place, and the prospect is particularly interesting, taking in a large part of Galilee, and extending over the lake to the snow capt mountains of the Haooran. After visiting the wounded, and distributing some clothing and money to the poor, we hurried on to Segara, about an hour further west, and close to the northern base of mount Tabor. Before we reached this place, it is worthy of remark, that the lava entirely disappeared, and a hard, whitish lime-stone rock took its place, the land being extremely fertile. We passed over the battle-field where general Kleber sustained for half a day the attack of the whole Turkish force, twenty or thirty times greater than his own, until Bonaparte, learning his critical situation, hurried to his relief with a small reinforcement, when the Turks fled in utter confusion. The French were encamped in this village for a considerable time, and one old man, who remembers Kleber well, interested me exceedingly by his animated descriptions of the numerous battles and skirmishes in which they were constantly engaged. He wanted to know whether there were any such bold men now in the world as those Frenchmen, and gave it as his opinion that a few thousand of them would conquer all Syria. — Segara lost fifty of its two hundred inhabitants by the earthquake; and, like Luby, the houses were all destroyed.

From this to Nazareth is three hours, and our road led us along the base of a low mountain, to Kefr Kenna, which we reached in an hour and a half. We started a great many partridges, foxes, and jackals, and saw gazelle bounding over the plain below. Tabor, covered with trees and under brush, is said to abound with wild hogs, which are often hunted, more for sport than use, as their flesh is an abomination to the Turk and Jew, and not very good for any body. Kefr Kenna sustained no injury from the earthquake; and as we were anxious to reach Arana before dark, we did not stop to examine either the house where the wedding was celebrated, or the broken water-pot deposited in the church, or the fountain from which the water was drawn, or any other wonder of the place; still our haste was of small account, for it was quite dark before we reached the ruins of Arana; and as the houses were all destroyed, the people had mostly left for other places. About one hundred and ninety persons perished under the ruins, and many were wounded. As we could not remain there over night, we left word for the poor to meet us at Nazareth, which is only a half an hour distant, and we would attend to them in the morning. Greatly wearied and chilled with the mountain dew, we reached Nazareth about seven o'clock, and were hospitably entertained by one of our companions, Ibrahim II Cuprasy — Abraham the Cypriot — who had assisted in our work for the last five days. The whole upper story of our host's house fell in at the time of the earthquake, but a merciful providence had so ordered it, that not one of the family was above at the moment. Had they been in their usual sitting room, all must have perished. The lower part, consisting of strong vaults, was not even cracked, and here we were received and entertained while many tons of earth and rock lay piled above our heads. As the earth still trembles and shakes, we preferred sleeping in our tents, although it was quite cold.

Nazareth has sustained but little injury. Our friend's house, and the great Latin convent suffered most. Only five persons were killed, four of them, if I remember correctly, at the convent. This beautiful building is terribly shattered in many places, and it would not have required much more to have brought it all down upon the heads of the monks. Many workmen are busily employed repairing the terraces and broken walls; and, if not interrupted, they will soon obliterate any trace of the fearful earthquake.

According to appointment, many poor came from Arana, who being all known by our host, we were in no danger of imposition. We distributed the remainder of our clothing amongst them, sent medicine for some of the wounded, and leaving a small sum of money with our friend to be expended for the benefit of the needy, we left Nazareth about noon, and turned our face towards home.

Saphoory — Abilene — Birwy — Kefr Yooseph — River Belus

Our route brought us to Saphoory in about an hour, the direction being nearly north from Nazareth. This is a considerable village, with an old castle commanding the hill, and a sweet vale spread around its base. The earthquake did no injury here. Crossing the fertile plain of Zabulon, we took the wrong road, which led us out amongst some wild hills, covered with bushes and luxuriant grass; and after wandering up and down for some time without any path, we ascended a hill, which, overlooking all the rest, gave us a splendid view of the sea, the city, and vast plain of Acre stretching far away to the northwest, and at the same time a glimpse of our road, in a deep valley to the right of us. Without much more trouble we got down to it, where also we met our muleteers, not far from Abilene, a large village pleasantly situated on a low mountain to the left of the road. Abilene is distinguished from most mountain villages by a high minaret, indicating a moslem population. Soon the narrow valley down which our road lay, opened into the splendid plain of Acre; but not wishing to enter the city, we turned directly north along the head of the plain, now and then crossing a little spur of the mountain, covered with shrubbery, and generally adorned with a small village. The first was called Themera, and the next Damona, which seems to have once been strongly fortified, parts of the old wall still remaining in many places. They are favored with but one well of water, which is deep and brackish besides. Here a man was constantly employed in drawing up the water, aided by one of the simplest pieces of machinery imaginable, which he turned with his feet. Deut xi, 10. All the villagers seemed to enjoy the fruit of his labor without distinction. Birwy is another considerable village, about half an hour to the north of Damona, distinguished by a very large and beautiful mound, near the fountain which supplies it with water. This is the largest artificial mound I ever saw. It cannot be less than eighty rods in circumference at the base, and is nearly one hundred feet high. Two or three mounds of a similar character are seen in other parts of the plain, generally near and commanding some fountain of water. These were probably erected before the time of Joshua, and were intended to command this fertile plain; and before the invention of cannon, they might have answered the purpose very well. Near this fountain I found a number of columns, of the rudest form, and most antique appearance of any that I have examined. From Birwy we ascended a hill, and came to a Moslem village called Jedaidy. It was now very dark, and we inquired the way to Kefr Yooseph, where we intended to sleep. We soon, however, lost our road; and after wandering about for some time, succeeded in getting back to Jedaidy. By dint of money, begging, and scolding, we succeeded in obtaining a guide; and leaving word for our muleteers to follow us, hurried forward towards our sleeping place, for it was now cold, and we were not a little fatigued and hungry. The sheikh of Kefr Yooseph, whom we had met in Safet, received us with boisterous welcome, and soon our room was filled with half the village. After waiting a long time for our muleteers in vain, we got a cold supper of olives, oil, cheese swimming in oil, and coarse bread; but to the hungry soul every bitter thing is sweet. Our kind host supplied us with a sort of bed, and we lay down on the floor to fight flees until morning.

23. Not knowing what had become of our servants we set off early in pursuit of them, still keeping along the head of the plain. In two hours we passed Kwoikat, Gabzia, Sheikh Daood, Masookh, Bussa, and two or three other villages, whose names I forget. At Masookh, we crossed a considerable stream, which I suppose is the river Belus, and whose banks were adorned with large patches of sugar-cane. There are many flouring mills here, and gardens of orange and lemon trees. Near this place is the great mountain whose waters conducted across the plain in an arched aqueduct for eight or ten miles, supplies Acre with an abundance of that indispensable article. The plain betwixt Masookah and cape Blanco is devoted almost exclusively to the raising of grain. Thousands of acres were already green with the promise of a future harvest, while thousands more had just received the precious seed, and numerous ploughs were actively engaged in turning up the remainder, and preparing it for the sower that soweth the seed. We saw eighteen or twenty gazelle at one time, and some of our company gave chase to them, but in vain. They capered and bounded in mere sport, far ahead of the fleetest of our horses. Deer are much more numerous than in America, but not so large or beautiful. At the foot of cape Blanco we found an English gentleman from India, accompanied by Said Ali, one of the young men whom Mohammed Ali sent to England several years ago to be educated. He is still a Moslem, speaks English very correctly, and is altogether a most agreeable and well informed young man.

Valley of the Euphrates — Jerusalem and Vicinity — Tyre — Ancient Ruins

After referring incidentally to the contemplated post route between the Mediterranean and India, by way of the Euphrates and the Persian Gulf, Mr. Thomson remarks upon the country on the river just named and the importance of that channel of communication.

The valley of the Euphrates is becoming more and more important and promising, as a field of missionary exertion. For some time past I have become acquainted with a priest of the Chaldean church, from Mosul, from whom I have received ample corroborations of former reports. He gives a particular account of several hundred thousand Nestorian Christians residing in the mountains north of Mosul; and there are, he says, an equal number of Christians of the Chaldean church. Besides these there is a large sect, called Dowasen, whom he describes as worshipers of the devil. They have no books, not even the knowledge of letters. He says there are a thousand villages of them in the mountains between Mordin and the great lake Ooroomiah. The road to all these is by the way of Aleppo, Beer, and Mordin, the precise route of the Euphrates expedition. The road, which has generally been dangerous on account of wandering Arabs, is now open, and caravans pass regularly from Mosul, Mordin, and the regions beyond, to Orfa, Beer, and Aleppo. Since the establishment of English mercantile houses in Aleppo, their goods have been extensively introduced through all that part of the valley. My informant confirms the account given of these oriental Christians by Mr. R., the Arabic translator and corrector of the Malta proofs, that they would gladly receive the Holy Scriptures and send their children to schools. Mr. R. is himself a native of Mosul, where his father was a priest, well known to my informant. I have long felt a deep interest in this people, which increases in proportion as more accurate information is obtained. And as the language is pure Arabic, I look to that valley as promising a great outlet to our books. The first step towards this will be the establishment of a strong missionary station at Aleppo.

But to return from this digression, Mr. Stewart, who is returning from Jerusalem, confirmed the reports from that place, which I had heard in Safet. Little injury had been sustained in that region; but at Nabloos the shock had been very violent. The town itself was nearly destroyed, but not more than one hundred and fifty persons perished. Many villages in the surrounding mountains are reported as overthrown, but these reports need confirmation. In company with our two friends we clambered over the frightful rocks of cape Blanco, along the astonishing pass cut in the white rock overhanging the blue sea; refreshing ourselves a while at the great fountain called Scandaroon, and passing the still greater one of Kass el Ayne, which pours forth a river of sweet water at the very margin of the sea, we entered Soor as the dews and shadows of evening began to fall upon us. Here we found our muleteers, who had lost their road and wandered about nearly the whole night; and thinking that we were ahead of them, they had hurried on all day, hoping to overtake us.

We found that all the inhabitants of Soor had forsaken their houses, and were living in tents. The earth still continued to tremble and the houses not fallen are so badly cracked as to render it very dangerous to occupy them. Some of the people had drawn up their fishing boats on shore, and covering them like a tent with the sails, transformed them into houses. Others had military tents, and many had purchased boards, and were erecting wooden shanties. Poor Tyre has been declining for many years, as I learn from the inhabitants. Her trade is entirely taken by Beyroot, and having received this terrible shock, I fear she will not soon recover.

Dim is her glory, gone her fame;
Her boasted wealth has fled;
On her proud ruck, alas! her shame,
The fisher’s net is spread.

The Tyrian harp has slumber’d long,
And Tyria’s mirth is low;
The timbrel, dulcimer, and song
Are hush’d or wake to wo!
24. We had a slight shock of earthquake last night; and in fact the earth has not been at rest twenty-four hours since we left home. Blessed be the Preserver of life and the Father of mercies, no evil has befallen us. We wake this morning in vigorous health and cheerful spirits. In two hours we crossed the river Kasmia on a strong stone bridge, and the road which was very muddy fourteen days ago is now excellent, so that we had a very pleasant ride of nine hours to Sidon, which we reached at sunset, and took our English friend to see some caves in the side of the mountain, about four hours from Tyre, which I had examined before. Near them are a great number of vaults for sepulchres, hewn out of the hard lime-stone rock. They are all of the same form, having a square door opening into a room about six feet square, arranged to accommodate three persons. The doors are all gone, and not a bone is left. How very ancient must be the date of these expensive works. In the plain below are vast piles of stone, and many old wells, proving the existence at some former period of a large city. In fact a great part of the coast between Tyre and Sidon is covered with ruins, and even in some places, the beautiful mosaic Boors of their palaces remain unbroken. The site of ancient Sarepta is ascertained by large quantities of rubbish lying in the plain three hours to the south of Sidon, and there is a small village still bearing that name, on the mountain a mile or two to the east.

Return to Beyroot — Remarks

25. Not wishing to be detained in the morning until the gates were opened, we did not enter Sidon, but pitched our tent at Nehor El Owel - first river — a considerable stream coming down from lower Lebanon, which is crossed on a high bridge. From this to Beyroot is ten hours, where we arrived in good health, rejoiced to meet our friends, and mingle our thanksgivings with theirs, for our mutual preservation during a time of unusual anxiety and alarm. Letters had also been received from Jerusalem, assuring us of the safety and welfare of our dear friends there. We had heard that Ramla was sunk, and many other places destroyed; and after waiting with — uneasiness nearly two weeks for letters from some one in Jerusalem, we dispatched a courier to ascertain the rea] state of the case, with directions to meet me at Safet; and I left home with the understanding, that, if necessary, | should proceed directly from Safet to Jerusalem. Our friends there, for a similar reason, sent off an express to Beyroot, and our couriers passed each other on the road. The truth is that the violence of the earthquake spent itself about half way between Beyroot and Jerusalem; and while all our accounts from the south seemed to increase our fears about Jerusalem, they could hear nothing from the north but frightful stories of ruin and death. But the Lord has mercifully preserved our lives and the cities where we dwell from this awful destruction, and blessed be his holy name.

One of the most remarkable circumstances in relation to the earthquake is, that some villages entirely escaped, although directly between two places which were utterly overthrown. For example, Jaish is a total wreck, not a fragment of a house is left standing; but a small village to the south, and almost within gun-shot of it, was not injured at all. But the next place is again entirely destroyed. And so on the road from Tiberias to Nazareth, Segara is overthrown, Kefr Kenna (Cana of Galilee), a little to the west, has not a house cracked; while Arana, just beyond it, is a vast pile of ruins; but the next village, Saphoory, escaped entirely. These villages are situated on the same hills, with no visible impediment between them; and upon what principle these astonishing exceptions can be accounted for I know not. One thing, I think, is certain, that all this region has been thrown up by volcanic fire. The strata incline into the valleys on every side, shewing that they have been forced up in the centre by some mighty power acting beneath. Now I would venture to inquire whether it might not result in such a mighty upturning of the foundations, that certain places become insulated, separated from the surrounding rock, and the intervals filled up with earth and soft substances; and as these would break the violence of the concussion, villages erected upon them might escape, although in close vicinity to others which are entirely destroyed. This is the fact, however it may be accounted for.

As to the extent of the injury wrought by the earthquake, nothing like accurate information has been ascertained. Much has been reported, but little that can be depended upon of the destruction of villages in Anti-Lebanon. It has certainly been very violent in that quarter as we learn from Huslayah and Rashaiah, the two most important towns in Anti- Lebanon. At Tiberias I ascertained that all the villages on the east shore of the lake were in ruins; and the same was true as far east in the land of Gilead and Bishan as we had any information from. The shock was felt in Egvpt, and at Mount Sinai, as we are informed by the English travelers who were there at the time. The lake of Tiberias is undoubtedly the centre of this mighty concussion, and it would not be at all surprizing if a fresh volcano should break out in some of the surrounding mountains.

Isaiah says, “When thy judgments are in the earth the inhabitants of the world will learn righteousness.” — The world that reads and hears of them may learn righteousness, but I fear those who are exercised thereby are most commonly hardened. As he says of the Israelites in another place, when suffering afflictions, “They shall fret themselves, and curse their king and their God and look upward.” There is something in the very magnitude of great calamities which seems to harden the heart. Certainly what I have witnessed during the last two weeks has exhibited human nature in a more odious light than I had before viewed it. There is no flesh in the stoney heart of man. Such foul specimens of dishonesty, robbery, cruelty, avarice, and amazing selfishness I never heard or read of. Nothing but dreadful punishments, oft inflicted, preserved the ruined places from becoming scenes of indiscriminate plunder. Taking advantage of their necessities, no man would work except for enormous wages. The head rabbi of Tiberias told me that they had to pay about sixty dollars for every burial, although it required only an hour or two to accomplish it. He had paid out of the public purse upwards of, seventy thousand piastres for this purpose alone. Nor are the Jews a whit behind the Moslems in this cold-hearted villany. I never saw a Jew helping another Jew, excepting for money. After our hospital was finished, we had to pay a high price to have the poor wounded creatures carried into it. Not a Jew, Christian, or Turk lifted a hand to assist us, except for high wages.

English from Thomson (1837) - embedded



Chronology
Year Reference Corrections Notes
430 pm 1 Jan. 1837 CE The shock occurred at half past four o’clock, P. M. and the first day of this year (1837 CE) will be long remembered as the anniversary of one of the most violent and destructive earthquakes which this country has ever experienced none
Seismic Effects

Beirut Sidon Tyre (aka Soor) South of Tyre along the coast Kahnah - a village about three hours from Tyre in the hills Ramash Kefr Bureyatun Jish Cudditha Ayne-Zatoon - in the valley immediately under Safet Safed Tiberias Luby Segara - close to the northern base of mount Tabor Kefr Kenna Arana Nazareth Saphoory - one hour nearly north from Nazareth Nabloos (Nablus) Jerusalem Ramla Miscellaneous observations including observations of Site Effects Locations

Damaged Light Damage or unaffected Felt Online Versions and Further Reading
References

Biblical Researches in Palestine, Mount Sinai and Arabia Petraea, A Journal of Travels in the Year 1838 by Edward Robinson

Biography

Biography

Excerpts
English from Robinson (1841:229-230)

Asphaltum. Our Arabs picked up along the shore small pieces of bitumen, asphaltum, (Arabic el-Hum- fnarj) which we brought away. Our Sheikh of the Ta'amirah told (as a report) the same story of its origin, which was heard by Seetsen and Burckhardt, viz. that it flows down the face of a precipice upon the eastern shore, until a large mass is collected, when from its weight or some shock it breaks of or and falls into the sea.1 The Sheikh of the Jehalin, who afterwards accompanied us to Wady Musa, related the same report ; assigning the place on the North of the peninsula. It cannot of course be South of the isthmus ; for the road travelled by Irby and Mangles and their party passes all the way at thee foot of the rocks along the shore. Nor is it probable that any such spot exists further North; we had the eastern coast very distinctly in sight for two days, as we travelled along the western shore, and examined it continually with our glasses ; so that any such marked point upon the rocks would hardly have escaped our notice. All agreed, that there was nothing of the kind upon the western coast.

More definite and trustworthy was the account which the Arabs gave us of the appearance of the bitumen in the sea. They believe that it thus appears only after earthquakes. The Sheikhs above mentioned, both of the Ta'amirah and Jehalin, related that after the earthquake of 1834, a large quantity of asphaltum was cast upon the shore near the S. W. part of the sea ; of which the Jehalin brought about sixty Kuntars into market.2 My companion also remembered that in that year, a large amount had been purchased by the Frank merchants at Beirut. During the last year also, after the earthquake of Jan. 1st, 1837, a large mass of bitumen (one said like an island, another like a house) was discovered floating on the sea, and was driven aground on the west side, not far to the North of Usdum. The Jehalin and the inhabitants of Yutta swam off to it ; and cut it up with axes, so as to bring it ashore. The Ta'amirah heard of it, and went to get a share. They found seventy men already upon and around it. It was carried off by camel-loads, partly up the pass of 'Ain Jidy ; and sold by the Arabs for four Piastres the Rutl or pound. The share of 4he Ta'amirah brought them more than five hundred dollars ; while others sold to the amount of two or three thousand dollars. — Except in those two years, the Sheikh of the Jehalin, a man fifty years old, had never known of bitumen appearing in the sea, nor heard of it from his fathers.
Footnotes

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.

English from Robinson (1841:229-230) - embedded



English from Robinson (1841:370)

Setting off again at 7.30, and descending, we reached Hunin at 8 o'clock. Here are the ruins of a large fortress, with a poor village adjacent to it on the south. The place is in a notch of the mountain, running northwest and southeast, and cleaving the mountain nearly half way to its base. In this notch is a low and broad Tell, on which the ruins and village are situated. The narrow valley towards the northwest runs to the Litany. On the east there is a small shallow Wady descending steeply towards the Huleh. Hunin belongs to the district of Belad Besharah ; and a branch of the family of the ruling Sheikhs formerly resided here. But since the great earthquake of January 1837, no part of the castle has been habitable ; and these feudal chiefs have all settled in and around Tibnin.3
Footnotes

3. W. M. Thomson in Biblioth. Sacra, 1846, p. 203.

English from Robinson (1841:370) - embedded



English from Robinson (1856 v. 2:420-424)

Safed lies on a high isolated hill or peak, rising upon the northern end of a steep ridge, which runs down towards the S.W., between the eastern valley through which we had ascended, and another still deeper one on the west. The latter has its beginning, as a deep narrow basin, on the north of the hill of Safed ; the water-shed between it and the eastern Wady being on the northeast of the castle, just north of where we were encamped. The two valleys, after running for some time parallel, come together and thus terminate the ridge ; the united Wady then passes on down to the lake of Tiberias across the plain el-Ghuweir as Wady el-'Amud. The most elevated conical point of Safed is towards the north, and is crowned by the castle, high above the deep valley in the north and west, and considerably higher also than the head of the eastern valley and. the watershed on the northeast. This castellated summit rises likewise high and rocky above the more southern part of the ridge ; just at its southern base is a slight depression or gap in the ridge itself ; south of which is another lower rocky point or summit. The town of Safed was properly divided into three distinct quarters, separated by the nature of the ground. One was upon this lower southern summit, over against the castle ; another below the castle in the head of the eastern valley near our tent ; and the third, the seat of the Jews, was on the steep western and northwestern side of the main summit, immediately below the castle. Between this and the southern quarter, is the market.

...

The Jewish quarter was far more slightly built, as well as more crowded. Clinging to the steep western declivity below the castle, their houses were often of mud, and stood in rows one above another, almost like the seats of an amphitheatre ; so that, in some instances, the flat roofs of one row actually served as the street for those next above.2 Safed is one of the holy places of the Jews in Galilee, and for several centuries has been more visited by them than Tiberias ; though the chief Rabbi of the latter city, is said to take rank of the one in Safed3. Of their former flourishing state and their celebrated schools, I shall speak further on ; but even since the period of their decay, they have had six or seven synagogues, and a school for the study of the Talmud, as in Tiberias. More than all this, too, they have had a printing office dating from the sixteenth century ; in connection with which, in 1833, some thirty persons found regular employment.4

Crowning the rocky summit, above the whole town, was the extensive Gothic castle, a remnant of the times of the crusades, forming a most conspicuous object at a great distance in every direction, except towards the north. Though already partially in ruins before the earthquake, it was nevertheless sufficiently in repair to be the official residence of the Mutesellim ; and on a former visit to Safed, my companion had paid his respects to that officer within its walls. The fortress is described as having been strong and imposing, with two fine large round towers ; it was surrounded by a wall lower down, with a broad trench.1

Such was Safed down to the close of the year 1836. But on the first day of January, 1837, the new year was ushered in by the tremendous shocks of an earthquake, which rent the earth in many places, and in a few moments prostrated most of the houses, and buried thousands of the inhabitants of Safed beneath the ruins. The castle was utterly thrown down; the Muhammedan quarter, standing on more level ground and being more solidly built, were somewhat less injured; while here, as in Tiberias, the calamity, in its full weight, fell with relentless fury upon the ill fated Jews. The very manner in which their houses were erected along the steep hillside, exposed them to a more fearful destruction; for when the terrific shock dashed their dwellings to the ground, those above fell upon those lower down; so that, at length, the latter were covered with accumulated masses of ruins. Slight shocks continued at intervals for several weeks; serving to aggravate the scene of unspeakable dismay and distress, which now prevailed here. Many were killed outright by the falling ruins; very many were engulfed and died a miserable death before they could be dug out; some were extricated even after five or six days, covered with wounds and bruises, only to prolong for a few hours a painful existence; while others, with broken limbs, but more tenacity of life, lived to recover. The spectacle which was presented for several weeks after the catastrophe, — in every quarter the wounded, the dying, and the dead, without shelter, without attendance, without a place to lay their heads; on every side " wounds, and bruises, and putrefying sores, that had not been closed, neither bound up, neither mollified with ointment,"2a — these scenes were described to us by eyewitnesses as inexpressibly painful, and sometimes revolting even to loathsomeness. According to the best accounts, there perished, in all, not far from five thousand persons ; of whom about one thousand were Muhammedans and the rest chiefly Jews.1a

...

Nearly eighteen months had now elapsed since the calamity, when we visited Safed. The frightful spectacle of human misery, had of course passed away ; but the place was still little more than one great mass of ruins. In the eastern quarter, where we had pitched our tent, many of the houses had been again built up; though more still lay around us level with the ground. The southern quarter was perhaps the least injured of all; here the rubbish had been cleared away, and this was now the chief seat of the Muhammedan population. Here too the Mutesellim had taken up his abode. The castle remained in the same state in which it had been left by the earthquake, a shapeless heap of ruins ; so shapeless indeed, that it, was difficult to make out its original form

...

Safed appears obviously to have formed the central point of this mighty concussion, and to have suffered more, in proportion, than any other place; except perhaps the adjacent villages of 'Ain ez-Zeitun and el-Jish. Yet the destruction, as we have seen, extended more or less to Tiberias and the region around Nazareth; many of the villages in the region east of the lake were likewise laid in ruins; many houses were thrown down in Tyre and Sidon, and several were cracked and injured even in Beirut, In Nablus, also, the shock was severely felt, and a number of persons were killed. It is a remarkable circumstance, that some villages remained entirely unaffected by the earthquake, although situated directly between other places, which were destroyed. Thus a small village near to el-Jish and Safed was uninjured. On the way from Tiberias to Nazareth, esh-Shajerah was overthrown; Kefr Kenna received no harm; er-Reineh was levelled to the ground; Nazareth sustained little damage; and Seffurieh escaped entirely. All these places lie upon the same range of hills, with no visible obstruction to break the shocks between them; and the exceptions are therefore the more wonderful.2b
Footnotes

2 Elliott l. c. p. 353, "As the hill on which the town is built is precipitous, and the roofs are flat, public convenience has sanctioned the conversion of these into thoroughfares; so that, both on mules and on foot, we repeatedly passed over the tops of dwellings."

3 Jowett Chr. Res. in Syria, p. 180. Lond.

4 Nau in 1674 speaks of seven synagogues; p. 561. So too Von Egmond and Heyman, and afterwards Pococke; the former also mention the high school and printing office; Reisen II. p. 41. Pococke II. i. p. 76. Schulz in 1755 gives the number of Jews at two hundred; the number of students in the school at twenty; and says the printing office had been in the village 'Ain ez-Zeitun in the valley north, but was then given up. Leitungen, etc. Th. V. pp. 211, 212. In 1833 Mr Hardy mentions two presses at work, and two others in the course of erection. The type and furniture were said to be made here under the direction of the master. The execution of the works printed was quite respectable; and near thirty persons were employed in the different departments of composing, press work, and binding. See Hardy's Notices, p. 244. Comp. Monro II. p. 13. See more further on.

1 Van Egmond and Heyman II. p. 43 sq. Pococke II. i. p. 76. Burckhardt p. 317.

2a Is. 1, 6.

1a It would not be at all surprising, if this estimate of the destruction of life were found to be considerably exaggerated. Compare the varying estimates of the population of Safed above, p. 420, note. See Mr Thomson's Report, referred to in the next note.

2b Mr Thomson visited all these places in the course of his journey; see his Report, Miss. Herald Nov. 1837. pp. 442, 44

English from Robinson (1856 v. 2:420-424) - embedded



Chronology
Year Reference Corrections Notes
1 Jan. 1837 CE Jan. 1st, 1837 CE none
Seismic Effects Locations with damage Locations without damage or very limited damaged Online Versions and Further Reading
References

The Land and the Book by William McClure Thomson

Biography

Biography

Excerpts

William McClure Thomson experienced the earthquake in Beirut and engaged in a relief mission to a number of towns and villages affected by the earthquake reaching Safed 17 days after the main shock. He produced an extensive description of the damage and human suffering.
English from Thomson (1861)

CHAPTER XIX

KUDES-SAFED-KEFR BUR'IAM.

March 6th (1857 CE).

... It was just before sunset on a quiet Sabbath evening — January 1, 1837 — when the shock occurred. A pale, smoky haze obscured the sun, and threw an air of sadness over the closing day, and a lifeless and oppressive calm had settled down upon the face of nature. These phenomena are, however, not very uncommon in this country, and may have had no connection with the earthquake. Our native church at Beirut were gathered round the communion-table, when suddenly the house began to shake fearfully, and the stone floor to heave and roll like a ship in a storm. " Hezzy ! Hezzy ! "1 burst from every trembling lip as all rushed out into the yard. The house was cracked from top to bottom, but no further injury was sustained. The shock was comparatively slight in Beirut, but still many houses were seriously shattered, and some on the river entirely thrown down. During the week succeeding this Sabbath, there came flying reports from various quarters of towns and villages destroyed, and lives lost ; but so slow does information travel in this country, especially in winter, that it was not until eight days had elapsed that any reliable accounts were received. Then letters arrived from Safed with the startling intelligence that the whole town had been utterly overthrown, and that Tiberias, and many other places in this region, had shared the same fate. Some of the letters stated that not more than one in a hundred of the inhabitants had escaped.

As soon as these awful facts hod been ascertained, collections were made at Beirut to relieve the survivors, and Mr. C - and myself selected to visit this region, and distribute to the needy and the wounded. Passing by Sidon, we associated with ourselves Mr. A and two of his sons to act as physicians. In Sidon the work of destruction became very noticeable, and in Tyre still more so. We rode into the latter at midnight over her prostrate walls, and found some of the streets so choked up with fallen houses that we could not pass through them. I shall retain a vivid recollection of that dismal night while life lasts. The wind had risen to a cold, cross gale, which howled through shattered walls and broken windows its doleful wail over ruined Tyre. The people were sleeping in boats drawn up on shore, and in tents beside them, while half-suspended shutters and doors unhinged were creaking and tinging in dreadful concert. On the 17th we reached Rumaish, where we met the first real confirmation of the letters from Safed. The village seemed quite destroyed. Thirty people had been crushed to death under their falling houses, and many more would have shared the same fate if they had not been at evening prayers in church. The building was low and compact, so that it was not seriously injured. After distributing medicine to the wounded and charity to the destitute, we went on to Jish. Of this village not one house remained ; all had been thrown down, and the church also, burying the entire congregation of one hundred and thirty-five persons under the ruins. Not one escaped except the priest, who was saved by a projection of the arch over the altar. The entire vaulted roof, with its enormous mass of superincumbent stone and earth, fell inward in a moment, and of course escape was impossible. Fourteen dead bodies lay there still unburied.

On the morning of the 18th we reached Safed, and I then understood, for the first time what desolations God can work when he ariseth to shake terribly the earth. Just before we began to ascend the hill, we met our consular agent of Sidon returning with his widowed, childless sister. Her husband, a merchant of Safed, had been buried up to the neck by the ruins of his house, and in that state remained several days, calling in vain for help, and at last perished before he could be reached and set free. As we ascended the hill, we saw large rents and cracks in the earth and rocks, and, though not so large as a chasm at Jish which I examined in the morning, still they gave fearful indications of what was to be expected. But all anticipation, every imagination was utterly confounded when the reality burst upon our sight. I had all the while refused to give full credit to the reports, but one frightful glance convinced me that it was not in the power of language to overdraw or exaggerate such a ruin. We came first to the Jewish half of the town, which contained about four thousand inhabitants two years before when I was there, and seemed like a busy hive of Israelites ; — now not a house remained standing. The town was built, as its successor is, upon the side of the mountain, which is so steep that the roofs of the houses below formed the street for those above ; when, therefore, the shock dashed all to the ground, the highest fell on the next below, that upon the third, and so on to the bottom, burying each successive row of houses deeper and deeper under accumulated masses of rubbish. From this cause it happened that many who were not instantaneously killed perished before they could be rescued, and others were rescued five, six, and even seven days after the earthquake, still alive. A friend of mine told me that he found his wife dead, with one child under her arm, and the babe with the nipple in its mouth : it had died of hunger, trying to draw life from its dead mother. Parents heard their little ones crying, Papa ! Mamma ! fainter and fainter, until hushed in death, while they were struggling to free themselves, or labouring with desperate energy to throw off the fallen rocks and timber from their dying children. 0 God of mercy ! my heart even now sickens at the thought of that long black winter's night, which closed around the wretched remnants of Safed in half an hour after the overthrow — without a light or possibility of getting one, four-fifths of the population under the ruins, dead or dying, with frightful groans, and shrieks of agony and despair, and the earth trembling and shaking all the while, as if affrighted at the horrible desolation she had wrought.

Most hideous spectacle, may I never see its like ! Nothing met the eye but a vast chaos of stone and earth, timber and boards, tables, chairs, beds, clothing, and every kind of household furniture, mingled in horrible confusion ; men everywhere at work, worn out and woe-begone, uncovering their houses in search of the mangled bodies of lifeless friends, while here and there were companies of two or three each, bearing away a dreadful load of corruption to the tomb. I covered my face, and passed on through the wretched remnants of Safed. Some were weeping in despair, others laughing in callousness still more distressing ; here an old man sat alone on the wreck of his once crowded house ; there a child at play, too young to realize that it had neither father nor mother, nor relative of any name in the wide, wide world. They crowded round us with loud lamentations, as if kindness unsealed the flood-gates of their sorrow — husbands without wives, wives without husbands ; parents child-less, and children without parents, and not a few left the solitary remnants of large families. The people were scattered abroad above and below the ruins, in tents of old boards, old carpets, mats, brush, and earth, while some poor creatures, wounded and bruised, were left among the tottering walls, exposed to a horrible death from the loose and falling stones above them.

As soon as our tent was pitched and our medicines and stores opened, we set sight out to visit the sufferers. But I have no heart to recall the sights and scenes of that morning : bodies crushed and swollen out of all human shape, and in every stage of mortification, dying hourly without hope of relief ; they were crowded into old vaults, where the air was tainted beyond endurance. Very soon we returned, and commenced arrangements to erect a temporary hospital, without which it was useless to attempt anything for the sufTerers. On this we all laboured incessantly, and by the 19th it was ready for their reception. Having collected them in it, and distributed medicines and clean bandages in abundance, we placed them under the care of a native doctor hired for the purpose, and then left for Tiberias. It was most refreshing to breathe once more the pure air of the open country, free from the horrible sights and scents of Safed. Nor shall I soon forget that pleasant ride to Tiberias, particularly in the evening, and along the shore of the lake. Gennesaret lay like infancy asleep. The sun settled quietly down behind the hills of Nazareth, and the full moon shone kindly through the hazy atmosphere on lake and land, faintly revealing the scenes where the Saviour of the world had wandered, and preached, and healed all manner of disease.

The destruction of life in Tiberias had not been so great as at Safed, but the houses and walls of the city were fearfully shattered. About six hundred perished under the ruins, and there were scenes of individual suffering not exceeded by any in Safed. Many of the wounded had been carried down to the hot baths, where we visited them. They informed me that at the time of the earthquake the quantity of water at these springs was immensely increased, and that it was so hot that people could not pass along the road across which it flowed. This, I suppose, was fact ; but the reports that smoke and boiling water were seen to issue from many places, and flames of fire from others, I believe were either fabrications or at least exaggerations. I could find no one who had actually seen these phenomena, though all had heard of them.

On the 22d we left Tiberias, and reached Nazareth in the night, having distributed medicines and clothes at Lubich, Sejera, Kefr Kenna, and Reineh. In all these villages, except Kefr Kenna, the earthquake had been very destructive, while in others on either side of us no injury had been sustained. This erratic and apparently capricious course led one of my companions to remark that it was the exact fulfilment of our Lord's words in Matthew xxiv. 7 : " There shall be earthquakes in divers places." There may be something in the geological formation of these plains and mountains which occasioned these extraordinary exceptions ; but whether we can or cannot explain the phenomenon, the fact is certain that some villages were entirely destroyed, and others close to them suffered no injury. And though the present earthquake is in no way referred to in that prophecy of our Lord, yet similar occurrences in ancient times may have suggested, or rather may have rendered the reference appropriate. At Nazareth our mission terminated, and we returned by the ordinary route to Beirut, having been absent eighteen days in the middle of winter, with bright, clear weather, so that even on the mountains we were able to sleep in the tent without inconvenience.

... And here is Kefr Bur'iam* and it has taken us three hours and a quarter to come from Safed ; the distance, however, is not more than nine miles.

We have still to examine the antiquities of this village. This edifice among the houses is tolerably perfect, and the style of architecture is wholly peculiar. These sheaf-like carvings on the columns and cornices are neither Roman nor Greek. In its present form it probably was a synagogue of the second or third century. An old villager tells me that he remembers when there was a row of columns above those now seen, but the earthquake of 1837 threw them down, and all those along the north end of the edifice.

Footnotes

1 "Earthquake! earthquake!"

* ["Kefr Bur'iam was for many centuries a place of Jewish pilgrimage. It was said in the twelfth century to contain the tombs of Barak the conqueror of Slsera, and Obadiah the prophet ; to these was added that of Queen Esther, In the sixteenth century. Round these shrines the Jews of Safed were wont to assemble each year on the feast of Purlm, to eat, drink, and rejoice — a few Individuals of special sanctity still make a passing visit to the spot, to pray over tombs so traditionally holy" - [Handbook for Syria and Palestine, p. 440).— Ed.]

English from Thomson (1861) - embedded



Chronology
Year Reference Corrections Notes
just before sunset 1 Jan. 1837 CE just before sunset on a quiet Sabbath evening — January 1, 1837 none
  • 1 Jan 1837 CE fell on a Sunday (calculated using CHRONOS)
  • I'm not sure what he meant by Sabbath evening. It is not the Jewish Sabbath which ends at sundown on a Saturday. It is probably a Christian version of Sabbath as the writer was a Christian missionary.
Seismic Effects

Beirut Safed Tiberias
Footnotes

1 Thomson (1861:396) stated

The temperature of the fountains varies in different years, and at different seasons of the same year. According to my thermometers, it has ranged within the last twenty years from 136° to 144° (Farenheit). I was here in 1833, when Ibrahim Pasha was erecting these buildings, and they appeared quite pretty. The earthquako which destroyed Tiberias in 1837 did no injury to the baths, although the fountains were greatly disturbed, and threw out more water than usual, and of a much higher temperature. This disturbance, however, only temporary, for when I came here about a month after the earthquake, they had settled down into their ordinary condition.

Other locations Locations Online Versions and Further Reading
References

Other Authors

Other References

  • Van der Velde (1854) Volume 1 and Van der Velde (1854) Volume 2 discuss the 1837 CE Safed Quake while sometimes referencing Thomson (1861) and seemingly add nothing new.

  • Ambraseys (1997:935) wrote it is said that waves flooded the coast of Lake Tiberias but it is not clear whether this happened before, during, or after the earthquake (Shkelov, 1837; Kerhardene, 1859).

    • SHKELOV (1837): In Letters from Eretz-Israel, edited by A. YARI, 357-363, 1971.
    • KERHARDENE, G. DE (1859): Voyage en orient, France Litter. and Artist., 3, 667-690. - Voyage to the Orient has been published in multiple versions including as The Women of Cairo Volume 1 and The Women of Cairo Volume 2. I could not find any reference to flooding in Lake Tiberias in either of these last two references after a cursory search.

  • Zohar (2017) reports that reports of damage in Tiberias are described by aid delegations sent to the city from Jerusalem.

    • Calman, S.E., 1837. Description of part of the scene of the late great earthquake in Syria. London: Lincoln’s-Inn-Fields.
    • Nee’man, A., 1837. Arieh Nee’man’s letter from Safed to Amsterdam about the earthquake in Safed. In: A. Ya’ari, ed. Letters of Eretz Israel. Tel-Aviv: Gazit, 363–367.

Online Versions and Further Reading

Zohar (2017)

Abbasi, M., 2006. The Tabri family and leadership of the Arab community of Tiberias during late Ottoman and British Mandate periods. Cathedra, 120, 183–200.

Avi-Yonah, M., 1951. Historical geography of Eretz Israel. Jerusalem: Bialik Institute.

Avi-Yonah, M., 1980. In the days of Rome and Byzantium. Jerusalem: Bialik Institute.

Avissar, O., 1973. The book of Tiberias. Jerusalem: Keter Publishing House Ltd.

Ben-Arieh, Y., 1997. Painting the Holy Land in the nineteenth century. Jerusalem: Yad Izhak Ben-Zvi Publications.

Ben-Arieh, Y., 2001. The view of Eretz Israel as reflected in biblical painting of the 19th century. In: R. Aharonson and H. Lavsky, eds. A land reflected in its past. Jerusalem: The Hebrew University Magnes Press and Yad Izhak Ben-Zvi Press, 255–279.

Ben-Yaakov, M., 2001. The immigration and settlement of North African Jews in nineteenth century Eretz-Israel. Thesis (PhD). The Hebrew University of Jerusalem.

Ben-Zvi, I., 1954. Eretz-Israel under Ottoman rule. Jerusalem: Bialik Institute.

Bnayahu, M., 1946. Rabbi Yaa’kov Birav - Zimrat Haa’retz. 5th ed. Jerusalem: Mekorot-Eretz Israel.

Buckingham, J.S., 1822. Travels in Palestine through the countries of Bashan and Gilead. London: Longman, Hurst, Rees, Orme, and Brown.

Burckhardt, L.J., 1822. Travels in Syria and the Holy Land. London: J. Murray.

Calman, S.E., 1837. Description of part of the scene of the late great earthquake in Syria. London: Lincoln’s-Inn-Fields.

Carne, J., 1826. Letters from the East. London: H. Colburn.

Clarke, E.D., 1810–1823. Travels in various countries of Europe, Asia and Africa. London: Printed for T. Cadell and W. Davies.

Davie, F.M. and Frumin, M., 2007. Late 18th century Russian Navy maps and the first 3D visualization of the walled city of Beirut. E-Perimetron, 2 (2), 52–65. de Aveiro, P., 1927. Itinerario da Terra Sancta, e Suas Particula

de Gramb, M.J., 1840. A pilgrimage to Palestine, Egypt, and Syria. London: H. Colburn.

de Thévenot, J., 1971. The travels of Monsieur de Thévenot into the Levant. Newly done out of French. Farnborough: Gregg.

Gil, M., 1983. Eretz Israel during the first Islamic period. Tel Aviv: Tel Aviv University.

Guerin, V., 1880. Description Geographique, Historique et Archeologique de la Palestine. Paris: L’Imprimerie nationale.

Hasselquist, F., 1766. Voyages and travels in the Levant in the years 1749, 50, 51, 52. London: L. Davis and C. Reymers.

Heyd, U., 1969. Dah’r al-Omar. Jerusalem: Rubin Mass Ltd.

Horne, T.H., 1836. Landscape illustrations of the bible: consisting of views of the most remarkable places mentioned in the old and new testaments. London: J. Murray.

Irby, C.L. and Mangles, J., 1823. Travels in Egypt and Nubia, Syria and Asia Minor during the years 1817 & 1818. London: T. White and Co.

Jacotin, P., 1799. Carte topographique de l’Egypte et de plusieurs parties des pays limitrophes. . . Construite par M. Jacotin, 1:100000. Paris: Jacotin, P.

Jowett, W., 1826. Christian researches in Syria and the Holy Land in 1823 & 1824 in furtherance of the objects of the church missionary society. Boston, MA: The Society by L. B. Seeley and J. Hatchard.

Karniel, G. and Enzel, Y., 2006. Dead Sea photographs from the nineteenth century. In: Y. Enzel, A. Agnon, and M. Stein, eds. New frontiers in Dead Sea paleoenvironmental research. Boulder, CO: Geological Society of America, 231–240.

Kinglake, A.W., 1848. Eothen, or, Traces of travel brought home from the East. New York, NY: George P. Putnam.

Levin, N., Kark, R., and Galilee, E., 2010. Maps and the settlement of southern Palestine, 1799-1948: an historical/GIS analysis. Journal of Historical Geography, 36, 1–18.

Light, H., 1818. Travels in Egypt, Nubia, Holy Land, Mount Lebanon and Cyprus in the year 1814. London: Printed for Rodwell and Martin.

Maden, R.R., 1829. Travels in Turkey, Egypt, Nubia and Palestine in 1824, 1825, 1826 and 1827. London: Henry Colburn.

Madox, J., 1834. Excursions in the Holy Land, Egypt, Nubia, Syria. Including a visit to the unfrequented district of the Haouran. London: Richard Bentley.

Mariti, G., 1791. Travels through Cyprus, Syria, and Palestine. London: G. J. and J. Robinson.

Mendel, M., 1839. The book of ‘Korot HaI’tim of Yeshuron’ in Eretz Israel. Jerusalem: Anshine M., 1930.

Nee’man, A., 1837. Arieh Nee’man’s letter from Safed to Amsterdam about the earthquake in Safed. In: A. Ya’ari, ed. Letters of Eretz Israel. Tel-Aviv: Gazit, 363–367.

Nir, Y., 1985. The beginnings of photography in the Holy Land. Cathedra, 38, 67–80.

Olin, S., 1844. Travels in Egypt, Arabia Petra, and the Holy Land. New York: Harper & Brothers.

Pococke, R., 1745. A description of the east and some other countries. London: Bowyer, W

Pueckler-Muskau, H.L.H.F., 1844. Aus Mehemed Ali’s Reich. Stuttgart: Hallberger.

Richardson, R., 1822. Travels along the Mediterranean and Parts Adjacent: in Company with the Earl of Belmore, during the Years 1816-17-18. London: Printed for T. Cadell.

Robinson, E. and Smith, E., 1841. Biblical researches in Palestine, Mount Sinai and Arabia Petraea. A journal of travels in the year 1838. London: J. Murray.

Robinson, E. and Smith, E., 1856. Biblical researches in Palestine, and in the adjacent regions. A journal of travels in the year 1838 & 1852. London: J. Murray.

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Schur, A.A., 2002. Letters from 1833 of ‘Hasidey Carlyne’ in Tiberias. Beit Aharon and Israel Corpus, 17 (4), 247–255.

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Ambraseys (2009)

[1] PRO FO 78.316 (Beirut: Moore to Palmerstone) 2.1.1837, 9.1.1837, 2.3.1837 (enclosures 2 and 5 to Palmerstone), 17.1.1837 (Aleppo: Werry to Palmerstone); 17.1.1837 (Aleppo: Werry to Bidwell) and 1.2.1837 (Aleppo: Werry to Ponsonby).

[2] PRO FO 78.315 (Damascus: Farrer to Palmerstone) 25.1.1837, 20.3.1837, 24.5.1837 and enclosures that are not dated.

[3] Archives Dipl. Nantes (Turq.) Corr. Cons. (Damas) 15.1.1837 and 22.2.1837; and (Beyrouth) 28.1.1837.

[4] Archives Dept. des Bouches du Rhone (Marseille) 200.33.

[5] Archives Societe de Geographie, Paris, Corr. 1649 (Beyrouth: Joselle to H. Joselle) 15.1.1837; (Beyrouth: Guys to H. Joselle) 17.1.1837.

[6] Archives Abdin Palace, Cairo, Corr. 1252, vol. 254, no. 403 (Ibrahim Pasa to Sami Beg) 10.3.1837 (2.12.1252); also extracts in Rustum (1942).

PATH no. 418, 1837.
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Ambraseys (1997)

Unpublished Sources

  • Ml PRO: Public Record Office, Kew. F0.78.316 (Beirut: Moore to Palmerstone) 2.1.1837; 9.1.1837; 2.3.1837 (enclosures 2 and 5 to Palmerston); (Aleppo: Werry to Palmerstone) 17.1.1837; (Aleppo: Werry to Bidwell) 17.1.1837; (Aleppo: Werry to Ponsonby) 1.2.1837.

  • M2 F0.78.315 (Damascus: Farrer to Palmerstone) 25.1.1837, 20.3.1837, 24.5.1837 and enclosures not dated.

  • M3 Archives Dipl. Nantes (Turq.) Con Cons. (Damas) 15.1.1837, 22.2.1837; (Beyrouth) 28.1.1837.

  • M4 Archives Dep. des Bouches du Rhone (Marseille) 200.33.

  • M5 Archives Societe de Geographic, Paris, Con. 1649 (Beyrouth: Joselle to H. JoseIle) 15.1.1837; (Beyrouth: Guys to H. JoseIle) 17.1.1837.

  • M6 Archives: Abdin Palace, Cairo, Con. 1252, vol. 254, # 403 (Ibrahim Pasa to Sami Beg) 10.3.1837 (2.12.1252) also in Rustum 1942.

Press Reports
  • P1 Athena, No. 418, 420, 1837, Athens.
  • P2 Correspondenzblatt, vol. 12.305.1837; vol. 13.150.1838, Stutt.
  • P3 L'echo du monde savant: 15.2.1837; 20.5.1837, Paris.
  • P4 Journal de Smyrne, 21, 25, 27.1, 3.2 1837, Smyrna.
  • P5 Das Morgenland, No. 11, pp. 322-341, 1843.
  • P6 Natur and Heilkunde, vol. 2, No. 9, pp. 134-135, 1837, Weimar.
Published Works - partial
  • ANONYMOUS (1843): Das Erdbeben in GallIda, Das Morgenland, No. 11, 320-343.

  • ARVANITAKIS, G.L. (1903): Contribution for the study of earthquakes in Syria and Palaestine, in Himerologion Hierosolymon, 158-191, Jerusalem (in Greek), summary in Bull. Inst. Egypte, ser. 4, 4, 178-183, Cairo.

  • BELDAM, J. (1851): Recollections of scenes in Italy and the East, ii.173-185, London

  • BERTOU, J. DE (1843): Essai sur la Topographie de Tyr, p. 8, Paris.

  • BLONDEL, E. (1843): Deux Ans en Syrie et en Palestine 1838-1839, pp. 108, 200-202, Paris.

  • CALMAN, S.E. (1837): Description of Part of the Scene of the Late Great Earthquake in Syria, London.

  • COLLA, A. (1837): Terremoti sentiti in diversi punti del globo, Bibl. Ital., 92, p. 268.

  • ENLART, C. (1925): Les Monuments des Croises dans le Royaume de Jerusalem, p. 94, Paris.

  • FRANICL, L.A. (1858): Nach Jerusalem, ii.362, Leipzig Mimi-, P.M. (1847): Die Riickkehr, ii.162-165, Berlin.

  • GUERIN, V. (1880): Description de la Palestine, Galilee, 2 vols., Paris.

  • ITALIANDER, R. (1970): H. Barth, Er schloss uns einem Weltteil auf, Hamburg.

  • JENNER, TH. (1873): Goodly Mountain and Lebanon, p. 198, London.

  • JOHNS, C.N. (1932): Medieval'Ajlun, Quart. Dept. Antiquit. Palest., 1, p. 33.

  • KALLNER-AMIRAN, D. (1951): Revised earthquake catalogue of Palestine, Isr. Explor. J., 1, 231.

  • KERHARDENE, G. DE (1859): Voyage en orient, France Litter. and Artist., 3, 667-690.

  • Kffro, J. (1844): History of Palestine, vol. 2, 91-94, London.

  • LAYARD, H. (1887): Early Adventures in Persia, Susiana and Babylonia, i.150-201, London.

  • LEMMENS, H.J. (1898): Al-zalazal fz Suriyah, al-Mashriq, val., 303-304, 337-342, Beirut.

  • LIEBETRUT, F. (1854): Reise nach dem Morgenlande, vol. 1, 188-189, Berlin.

  • LINDSAY, LORD (1839): Letters on Egypt, Edom and the Holy Land, ii.104-107, 259, London.

  • LYNCH, W.F. (1852): Official report of the U.S. expedition to explore the Dead Sea and River Jordan, Baltimore.

  • MACGREGOR, J. (1904): The Rob Roy on the Jordan, pp. 361-374, London.

  • MALLET, R. (1854): On the facts of earthquake phaenomena, Br. Assoc. Adv. Sci. Rep., p. 263.

  • MERYON, C.L. (1845): Memoirs of the Lady Hester Stanhope, i.260-303, London.

  • MITFORD, E.L. (1884): A Land March from England to Ceylon Forty Years Ago, vol. i.209, 224.

  • MONTEFIORI, J. (1844): Notes from a Private Journal, 228-257, London.

  • MOORE, M. (1837): (no title) J. R. Geogr. Soc., 7, 100-102, and Proc. Geol. Soc. London, 2, p. 540.

  • NEMAN, A. (1971): in Letters from Eretz-Israel (1837), edited by A. YARI, 363-367.

  • OLIM, S. (1843): Travels in Egypt, Arabia Petrea and the Holy Land.

  • PAXTON, J.D. (1839): Letters from Palestine, 205-206, London.

  • PFEIFFER, I. (1856): Reise einen wienerin im heilige Land, 12-16, Vienna.

  • PRUTZ, H. (1876): Aus Phoenizien, p. 133, Leipzig.

  • ROBINSON, E. (1856): Biblical Researches in Palestine, ii.229, 334, 346, 350, 370, 380, 422-424, 445, 465, 479, 466, 529-531, iii.370, London.

  • RUSSEGGER, J. (1847): Reisen in Europa, Asien und Afrika, iii.127, Stuttgart.

  • RUSTUM, A.J. (1923): Syria under Mehmet Ali, Doct. Disert., Univ. Chicago.

  • RUSTUM, A.J. (1942): A Calendar of State Papers from the Royal Archives of Egypt Relating to the Affairs of Syria, vol. 3 (1251-1254 a.H.; 1835-1839 AD.); 208-211, Beirut.

  • SAULCY, F. DE (1854): Narrative of a Journey Round the Dead Sea and in the Bible Lands in 1850 and 1851, vol. 1.38, vol. 2.449, 453, 487.

  • SAULCY, L.F. DE (1955): Carnets de Voyage en Orient, p. 117, Paris.

  • SCHUBERT, G.H. VON (1840): Reise nach dem Morgenlande, vol. 3, p. 168, 222, Erlangen.

  • SHKELOV (1837): In Letters from Eretz-Israel, edited by A. YARI, 357-363, 1971.

  • THOMSON, W. (1837): A journal on a visit to Safet and Tiberias, The Mission. Herald, vol. 33, 433-443.

  • THOMSON, W. (1959): The Land and the Book, i.420-436, ii.70,76, London.

  • TOBLER, T. (1868): Nazareth in Palastina, 12-13, 204-207, Berlin.

  • TRISTRAM, H. (1874): The Land of Moab, p. 135, London

  • VERED, M. and H. STRIEM (1977): A macroseismic study and the implications of structural damage of two recent major earthquakes in the Jordan Rift, Bull. Seism. Soc. Am., 67, 1607-1613.

  • VISSESO, J.N. (1840): Meine Wanderung nach Palastina, p. 249, Passau.

  • WACHS, D. and D. LEVETTE (1981): Earthquake-induced landslides in the Galilee, Isr. J. Earth-Sci., 30, 39-43.

  • WAGHORN, M. (1837): Syria, Asiatic. J., 24, p. 175.

Amiran et al (1994)

  • 4 D. Wachs and D. Levitte (Earthquake-Induced Landslides in the Galilee, Israel Journal of Earth Sciences 30 [1981], pp. 39-43) draw attention to the need for actual evidence in mapping earthquake damage. An analysis of the two major earthquakes of I January 1837 and 11 July 1927 produced evidence of very light or even no damage at places not far from severely affected areas. This indicates that local ground conditions play a decisive role in determining the degree of damage.

  • 14 N. Shalem: Seismic Tidal Waves (Tsunamis) in the Eastern Mediterranean, BIES 20 (1956), pp. 159-170, ref. p. 168 (Hebrew), according to talmudic sources.

  • 42 E. Robinson: Biblical Researches in Palestine and in the Adjacent Regions, A Journal of Travels in the Year 1838, Boston, 1841, II, p. 38.

  • 48 N.N. Ambraseys: Data for the Investigation of the Seismic Sea-Waves in the Eastern Mediterranean, Bulletin of the Seismological Society of America 52 (1962), pp. 895-913.

  • 68 E. Robinson: Physical Geography of the Holy Land (German ed.), Leipzig, 1865, p. 325.

  • 84 Robinson (above, n. 42), 11, pp. 229-230, travelling on 10 May 1838 along the south-western shore of the Dead Sea, found small pieces of asphalt. He was told by his Arab guides that large pieces of asphalt floated on the lake after both the earthquakes of 1834 and 1837. In the latter case the block was so large that 70 men were required to break it up for sale. M.G. Ionides (Report on the Water Resources of Transjordan and their Development, Crown Agents for the Colonies, London, 1939, pp. 122-123, P1. 44) reproduces an undated photograph of a block of bitumen, its volume estimated as 150 cu.m., floating on the Dead Sea, probably the effect of the earthquake of July 1927.

  • 86 Y. Rotstein and E. Arieh: Tectonic Implications of Recent Microearthquake Data from Israel and Adjacent Areas, Earth and Planetary Science Letters 78 (1986), pp. 237-244.

  • 87 M. Vered and H.L. Striem: A Macroseismic Study and the Implications of Structural Damage of Two Recent Major Earthquakes in the Jordan Rift, Bulletin of the Seismological Society of America 67 (1977), pp. 1607-1613, contains the attempt of an isoseismic map, p. 1610.

  • 88 Robinson (above, n. 42), Ill, pp. 204, 209, 237, 254-256, 259, 321-324, 367, 369, 399-401, 419; 2nd ed., 1860, II, pp. 529-531, n. XLI.

  • 89 Particulars of victims and damage by districts are contained in the official report by Soliman Pasha, governor of Sidon, reproduced by U. Ben-Horin: An Official Report on the Earthquake of 1837, IEJ 2 (1952), pp. 63-65.

  • 90 Moore, extract from a letter published in Journal of the Royal Geographical Society 7 (1837), p. 101.

  • 91 Wachs and Levitte (above, n. 4) assume that the particularly severe damage at el-Jish, Ein Zeitun, Safed and er-Reina is due to landslides caused by the earthquake in the unstable chalk of the Senonian Ein Zeitim formation and the Kabri marl. This applies in particular to Safed, a large part of which is built on a rather steep slope consisting of Senonian chalk, which offers poor resistance in the case of a severe earthquake.

  • 92 A. Musil: Arabia Petraea, II, Moab, Vienna, 1907, ref. p. 172, n. 8. As for the ford, cf. C.L. Irby and J. Mangles: Travels in Egypt and Nubia, Syria and Asia Minor during the Years 1817 and 1818, London, 1823, ref. p. 454.

Archaeoseismic Evidence

Location (with hotlink) Status Intensity Notes
Tiberias definitive ≥8 Zohar (2017) examined textual and visual sources before and after the 1837 CE Safed Quake which was then analyzed using using Historical GIS. A table and map of Damages and Damage distributions was produced as a result of the analysis.
Tel Ateret aka Vadun Jacob possible ≥7 or ≥8 Ottoman Mosque Earthquake - Ellenblum et al (1998:305) described archaeoseismic evidence from Mamluk and Ottoman mosques built on the site as follows:
In the northern part of the castle, we also unearthed a Muslim mosque whose northern wall is displaced sinistrally by 0.5 m. A mikhrab (the Muslim praying apse) is well preserved in the southern wall. According to the study of the pottery, the mosque was built, destroyed, and rebuilt at least twice: the initial structure was built in the Muslim period (12th century) and later rebuilt once or twice during the Turkish Ottoman period (1517-1917). The 0.5 m displacement is observed in the northern wall of the latest building phase. The repetitive building of this site might be due to earthquakes.
The latest rebuilding phase was not dated. Ellenblum et al (2015) suggested that the 30 October 1759 CE Safed Quake was responsible while Ellenblum et al (1998:305) and Marco et al (1997) entertained the possibility that the 1837 CE Safed Quake is also a possible candidate.
Nimrod Fortress possible ≥8 As this site has not been systematically excavated, the date of the observed seismic damage is conjectural. It happened sometime after the fortress was built in the 13th century CE. However, the 1759 CE Safed and Baalbek Quakes are promising candidates, particularly the 1759 CE Safed Quake which Daeron et al (20015) suggests broke the Rachaiya Fault a mere 2.5 km. away. In addition, the Nimrod Fortress is optimally oriented to experience seismic amplification due to a Ridge Effect from fault breaks on the Rachaiya Fault. Hinzen et al (2016) examined 95 instances of arch deformations on the site and concluded that a preferred damage orientation was not present on the site overall but was present in the Gate Tower and the secret passage in the Gate Tower. Hinzen et al (2016)'s orientation results, however, may suggest the possibility that more than one earthquake damaged the site (e.g., the 30 Oct 1759 CE Safed Quake, the 25 Nov. 1759 CE Baalbek Quake, and/or the 1837 CE Safed Quake). The Earthquake Archaeological Effects Chart suggests a minimum Intensity of 8 and a Discontinuous Deformation Analysis by Kamai and Hatzor (2007) suggests a local Intensity of about 9. Attenuation relationships using postulated Magnitudes and Epicenters from Daeron et al (20015) suggest that site Intensity was between 9 and 11 for the 1759 CE Safed Quake and 7.5 and 11 for the 1759 CE Baalbek Quake.
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
Tiberias - The City



Tel Ateret aka Vadun Jacob



Nimrod Fortress



Dhiban



Landslide Evidence

1 PGA to Intensity conversions use Wald et al (1999).
Location (with hotlink) Status Minimum PGA (g) Likely PGA (g) Likely Intensity1 Comments
Safed probable n/a n/a ≥8 Intensity Estimate is based on post quake descriptions of the Castle at Safed. These reports indicate that the Castle suffered a major collapse which leads to a minimum Intensity of VIII (8) when using the Earthquake Archeological Effects chart of Rodríguez-Pascua et al (2013: 221-224).

Katz and Crouvi (2007) undertook a GIS based slope stability analysis of Safed in order to estimate current hazard due to seismically induced landslides. They used the 1759 CE Safed Quake and 1837 CE Safed Quake as calibrating events for their model. Their analysis coupled with observations of active creep within in the city suggest that a thick anthropogenic talus has created conditions ripe for slope instability. This in turn suggests that seismic damage in Safed due to the 1759 CE Safed Quake and the 1837 CE Safed Quake was largely due to landslides. The landslides in 1837 CE caused widespread destruction in the Jewish Quarter on the west slope below the Citadel in what is now called the Old City.
Location (with hotlink) Status Minimum PGA (g) Likely PGA (g) Likely Intensity1 Comments
Safed



Tsunamogenic Evidence

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.

The flame structures would have formed below the sediment water interface making this event difficult to date. Dating was approximate and was based on stratigraphy, archaeology, and textual accounts. The permeable lacustrine unit was assumed to have been deposited within an artificial lake that formed behind a dam that was originally constructed around 400 CE. Based on an estimated deposition rate, Marco et al (2014) surmised that it was deposited between ~400 CE and ~1400-1700 CE. Only one organic sample taken about 0.3 m above the flame structures produced a radiocarbon date. It dated to 250 yrs BP. Error bars were not presented but can be assumed to be between ±20 and ±75 years. Marco et al (2014:1451-1453) argued that a fresh brackish water lake behind the dam was present in some form during the late Ottoman period, possibly until the 18th century CE, due to the presence of flour mills on the west side of the dam which would have been powered by water from the dam. However, this may be contradicted by the presence of a pedogenic soil which formed above the permeable lacustrine unit presumably after the lake dried out. The pedogenic soil, however, contained freshwater fossils suggesting that the lake may have dried out, formed a soil horizon, and then filled intermittently again.

It also has to be noted that some dates discussed in their paper (e.g. dating the the sharp lithological boundary between the permeable lacustrine unit and the overlying clayey unit to circa 18th century) disagree with the Century track in the stratigraphic column they presented in Figure 3.

Historical evidence was based on Ambraseys and Barzanagi (1989) who, according to Marco et al (2014:1457), described "boats that were swept ashore from the Akko harbor (50 km north of the studied site), and a large wave that was reported from as far south as the Nile Delta", presumably due to the 25 Nov. 1759 CE Baalbek Quake. Although Marco et al (2014) suggested that the 25 Nov. 1759 CE Baalbek Quake was the most likely candidate for the flame structures, the date is, unfortunately, not well constrained.

Location (with hotlink) Status Intensity Notes
Taninim Creek Dam



Paleoseismic Evidence

Location (with hotlink) Status Intensity Notes
Jarmaq Trench possible ≥ 7 Nemer and Meghraoui (2006) date Event Z to after 84-239 CE. They suggested the Safed Earthquake of 1837 CE as the most likely candidate.
Faqaa Trench and Deir El-Achayer Excavation probable ≥ 7 Nemer et al (2008) dated the most recent event (aka the Last Event) in the Faqaa Trench to between 1686 and 1924 CE and suggested it was most likely caused by the 25 Nov. 1759 CE Baalbek earthquake. They also noted that the 25 Nov. 1759 CE Baalbek earthquake may have been responsible for a seismic event observed in the Deir El-Achayer Excavation although the dating for this event is fraught with uncertainty.
Bet Zayda probable ≥ 7 Marco et al (2005) dated Event E.H. 2 to after 1415 CE and suggested that it was was caused by the 1759 CE Safed Quake but considered other possibilities such as the 1546 CE and 1837 CE earthquakes. Marco et al (2005) estimated a Magnitude between 6.6. and 6.9 for Event E.H. 2 based on 0.5 m of offset.
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.

The flame structures would have formed below the sediment water interface making this event difficult to date. Dating was approximate and was based on stratigraphy, archaeology, and textual accounts. The permeable lacustrine unit was assumed to have been deposited within an artificial lake that formed behind a dam that was originally constructed around 400 CE. Based on an estimated deposition rate, Marco et al (2014) surmised that it was deposited between ~400 CE and ~1400-1700 CE. Only one organic sample taken about 0.3 m above the flame structures produced a radiocarbon date. It dated to 250 yrs BP. Error bars were not presented but can be assumed to be between ±20 and ±75 years. Marco et al (2014:1451-1453) argued that a fresh brackish water lake behind the dam was present in some form during the late Ottoman period, possibly until the 18th century CE, due to the presence of flour mills on the west side of the dam which would have been powered by water from the dam. However, this may be contradicted by the presence of a pedogenic soil which formed above the permeable lacustrine unit presumably after the lake dried out. The pedogenic soil, however, contained freshwater fossils suggesting that the lake may have dried out, formed a soil horizon, and then filled intermittently again.

It also has to be noted that some dates discussed in their paper (e.g. dating the the sharp lithological boundary between the permeable lacustrine unit and the overlying clayey unit to circa 18th century) disagree with the Century track in the stratigraphic column they presented in Figure 3.

Historical evidence was based on Ambraseys and Barzanagi (1989) who, according to Marco et al (2014:1457), described "boats that were swept ashore from the Akko harbor (50 km north of the studied site), and a large wave that was reported from as far south as the Nile Delta", presumably due to the 25 Nov. 1759 CE Baalbek Quake. Although Marco et al (2014) suggested that the 25 Nov. 1759 CE Baalbek Quake was the most likely candidate for the flame structures, the date is, unfortunately, not well constrained.

Dead Sea - Seismite Types n/a n/a n/a
Dead Sea - En Gedi possible see table
Potential Seismites in En Gedi

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

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.

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

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 - Taba Sabhka Trench possible ≥ 7 Allison (2013) dated Event EQ1 to after the 16th-17th century CE.
Location (with hotlink) Status Intensity Notes
Jarmaq Trench

Nemer and Meghraoui (2006) date Event Z to after 84-239 CE. They suggested the Safed Earthquake of 1837 CE as the most likely candidate.



Faqaa Trench and Deir El-Achayer Excavation

Nemer et al (2008) dated the most recent event (aka the Last Event) in the Faqaa Trench to between 1686 and 1924 CE and suggested it was most likely caused by the 25 Nov. 1759 CE Baalbek earthquake. They also noted that the 25 Nov. 1759 CE Baalbek earthquake may have been responsible for a seismic event observed in the Deir El-Achayer Excavation although the dating for this event is fraught with uncertainty.



Bet Zayda (aka Beteiha)

Marco et al (2005) dated Event E.H. 2 to after 1415 CE and suggested that it was was caused by the 1759 CE Safed Quake but considered other possibilities such as the 1546 CE and 1837 CE earthquakes. Marco et al (2005) estimated a Magnitude between 6.6. and 6.9 for Event E.H. 2 based on 0.5 m of offset.



Taninim Creek Dam



Dead Sea - Seismite Types



Dead Sea - En Gedi

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


Dead Sea - Nahal Ze 'elim

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


Araba - Introduction



Araba - Qasr Tilah

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

LeFevre et al. (2018) dated Event E1 to 1744 CE ± 56.



Taba Sabhka Trench

Allison (2013) dated Event EQ1 to after the 16th-17th century CE.



Notes

Zohar et. al. (2016)

Time Date Time Uncertainty Type of Quake Reliability Zone Most Damaged or felt locations Estimated magnitude in previous studies
16:35 1837 Jan 01 n/a Main and Aftershock Very High Central (Israel and southern Lebanon), North (northern Lebanon and Syria) Palestine, Syria
  • M > 7 Ambraseys (1997)
  • MS = 7.4 Wells and Coppersmith (1994)
  • MS = 7.1 Nemer and Meghraoui (2006) after Ambraseys (1997)
  • MS = 7.4 Migowski et al. (2004)
  • MS = 6.7 Ben-Menahem (1991)
  • Average magnitude 7.1
  • Size degree Maj
  • Casualties >10
Discussion Reported damaged localities

Nabatiya
Qana
el-Fara
el-Salha
Jish
Marun Al-Ras
Bint-Jbeil
Malkiyya
Qadas
Yaâtar
Tebnine
Hunin Castle
Baniyas [Israel]
Metula
Zeqqieh
Deir Mimas
el-Khiam
el-Tahta
Deir Mar-Elias
Qaddita
Jibshit
Gaza
Arraba
Attil
Qaqun
Tubas
Ajloon
Nablus
Zeita
Harithiya
Jerusalem
Kfar Birâim
Lake Tiberias
Hasbaya
Kafr Aqab
Jeresh.
Areopolis
Hula
Tarshiha
Dallata
Jaffa
Mrar
Ein-Zeitun
Tyre
Atlit
Meron
Eilabun
Akko
Migdal
Irbid
Reina
Safed
Tiberias
Hadatha
Haifa
Zemah
Kafr Kanna
Kafr
Sabt
Lubiya
Nazereth

References

Zohar, M., et al. (2016). "Reappraised list of historical earthquakes that affected Israel and its close surroundings." Journal of Seismology: 1-15.

Ambraseys (2009)

AD 1837 Jan 1 Palestine and Syria

At the time of the earthquake Palestine and Syria, parts of the Ottoman empire, were occupied by the Egyptians (during 1831-40) and the region was in turmoil. This, to some extent, accounts for the dearth of information from the hinterland and from Turkish archives in Istanbul, although for the latter our search has been rudimentary.

The main shock occurred on 1 January 1837 or on 24 Ramadan a.H. 1252, 10 minutes before sunset. The earthquake was reported from Beirut and other places at various local times between 4.35 and 4.45 pm. The main shock lasted between 10 and 30 seconds and eye-witness reports imply that the earthquake consisted of two distinct shocks about 5 minutes apart ([1, 5, 6]; Moore 1837). Destruction or heavy damage extended along a relatively narrow zone from the coastal area of Sidon through the inland iklimi (regions) of al-Tuffa, Marjuyum and Bshara to Lake Tiberias, a total length of about 120 km.

Starting from the north of the epicentral region, in Beirut the earthquake caused panic but no serious damage in the city itself. About eight houses, which had been built outside its walls on alluvium by the sea, collapsed, killing two people ([1]; Paxton 1839; Rustum 1942). No damage was reported from Kesrawan, a district north of Beirut, and reports from the district of Shouff, south of the town, are lacking. The monastery of Deir Qamar was badly shaken and those of Deir al-Mukhalles and Jun were damaged, but details are lacking. Sidon was almost totally ruined. Of its 1800 houses, 580 were demolished and 630 ruined, with the loss of seven lives. Qala't Mezzeh (Chateau de Saint Louis of the Crusaders), standing on the promontory which divides the two harbours, collapsed. The French merchants' stores fell and the walls of the town were breached. The town and the land walls were rebuilt by Soleyman Pasha immediately after the earthquake ([1, 3]; Thomson 1837; Rustum 1942; Kerhardene 1859). At al-Ghaziye 14 houses collapsed, killing seven people. Further inland Abra and nearby Deir Mar Elias were seriously damaged (Lindsay 1839; Meryon 1845). Salihiyah, Dar al-Hatta, and Rumin were totally destroyed [1].

On the eastern side of the Bekaa Valley, at Rashaya, the shock was very violent, but it is not known whether it caused any damage (Thomson 1837). In the upper reaches of the Bekaa valley several villages were more than half destroyed and a khan, the name of which is not given, was thrown down, killing 60 people [1]. The shock was violent at Hashbaya, where it is not known whether it caused any damage (Thomson 1837). Al-Kufur collapsed with the loss of 72 lives, and so did Dibbin Nabatiya al-Tahta and Jibshit [1].

The large villages of Irbil and Kherbet Shaqa were completely destroyed and 100 people were killed. Also Khirbah and al-Khiyam fell; 5 people lost their lives in the foimer and 150 in the latter. In the region of Bilad al-Shuqf 600 goats were killed, presumably by rock falls [1].

Qala't al-Shuqf (Chateau de Beaufort of the Crusaders), standing on a cliff where the Litani River turns towards the sea, was shattered, and a part of the interior structure of the citadel collapsed, killing five people [1]. Deir Mimas, where five people lost their lives, was totally destroyed and rebuilt immediately after the earthquake. About one third of the houses in Zeqqieh collapsed and eight people were killed [1]. Deir Qufa was totally ruined, and in Mitulla nothing was left standing and 78 people lost their lives [1].

Much of Banyas was ruined and some parts of the Qal'at al-Shubeibe, which stands on the summit of a hill to the east of the village, collapsed. Also the roof of the nearby Grotto of Pan fell and not far from its vicinity a large rent was made in the ground ([2]; Saulcy 1955). On the coast, Sur suffered considerable damage; 40 houses, presumably old ones, collapsed on the island, killing 16 and injuring 36 people. There is some evidence that as a result of this earthquake the eastern coast of the north harbour slumped ([6]; Thomson 1837; Waghorn 1837; Bertou 1843; Prutz 1876). Further inland the old castle of Hunin (Chastel Neuf of the Crusaders) was shattered and much of its interior, including the mosque, collapsed, no structure remaining habitable (Guerin 1880). No damage details exist for the districts of Hunin and Tibnin, where it is said that 614 people were killed in 49 settlements. Half of some of them and likewise five mills were totally destroyed, together with a third of the inhabitants [6].

In this region, the villages of Asbagha, al-Afrish, Amba, el-Asban, Akbar, Mugar and Sutli are reported to have been ruined, but their locations could not be identified, either because their names have changed or because they are misspelled in the various reports. Marun was also totally destroyed and Qana was damaged (Thomson 1837). One of the two parts into which al-Mays is divided collapsed, killing three people [1]. Also Beit Yahun was totally ruined [1]. At Ya'tar 12 people were killed. Qadas was completely destroyed, with the loss of 53 lives. Also Melkiyeh was destroyed, as was nearby Aytarun, where 33 people were killed ([1]; Calman 1837).

Bint Jubayl was totally ruined, with the loss of eight lives, and Ayn Ibli collapsed with the loss of 12 lives [1]. Another 17 people were killed at Marun al-Ras, which was also ruined, while 30 people were killed and 10 injured at Rumaysh, and 12 lost their lives at al-Salha ([1]; Calman 1837; Thomson 1837).

Dibil was almost totally destroyed and 12 people lost their lives there (Calman 1837). Three quarters of Deishun collapsed and 13 people were killed, and Alma was totally destroyed. In al-Fara 12 people perished [1]. Kafr Bir'irn was badly damaged; the church and a row of columns and other standing remains of an early synagogue were thrown to the ground ([1]; Thomson 1837; 1859, Calman 1837; Waghorn 1837; Guerin 1880). At Ras al-Ahmar 40 people were killed and 12 injured (Calman 1837). Jish was completely destroyed and not a house was left standing. The church fell, killing 130 persons, and the old walls of the town collapsed. In all 235 people were killed, and in places the ground was fissured (Thomson 1837; Waghorn 1837; Robinson 1856). Sabelan was completely ruined, without casualties [1]. Also Tarshiha was likewise damaged without loss of life [6].

Dallata, Qaddita and Ain Zeitun were almost totally destroyed ([1]; Thomson 1837). In contrast, nearby Meirun suffered relatively little damage, and the walls of the tombs of Rabbi Eleazer and Rabbi Shemaun were dislodged but did not collapse (Neman 1971). In Safet, the largest of the places affected, the northern, Jewish, section of the town was almost entirely destroyed while the southern, Moslem, section suffered far less serious damage. The number of deaths reached 2158, of which 1507 were Ottoman subjects, Moslem or Jewish, and 651 were foreigners ([1, 2, 6]; Thomson 1837; Waghorn 1837; Liebentrut 1854; Guerin 1880; Mitford 1884).

Nearby Rama was totally destroyed and 180 people were killed ([1]; Calman 1837). Also in Shezor and in Jabal (the location of which has not been identified) 245 houses were destroyed and 563 damaged, with 141 people killed [1, 6].

Kafr Sumei was totally ruined. However, just west of these villages, Jatt was probably not seriously damaged ([1]; Thomson 1837). Much of Eilabun collapsed, killing 25 people, and Maghar was ruined [1]. To the west at Acre only about 40 houses fell, four people were killed and several injured, and the fortifications, already in ruins, were damaged. In the district of Acre the earthquake killed in all 141 people ([1, 6, 1°]; Waghorn 1837).

There is no evidence that the villages of Tamra, Damun, al-Birwa, Kafr Yasif, Kaweikat, Ghabsiyya, Betset and Jatt were damaged (Thomson 1837). Evlayin suffered relatively little and its minaret was left standing, but in nearby Shefar'am 86 houses were ruined and 139 heavily damaged; also seven people were killed and four injured ([6]; Thomson 1837).

Mijdal, on the western coast of Lake Tiberias, was destroyed and Irbid was totally ruined. The same happened to Kafr `Akib on the northeastern coast of the Lake ([1]; Thomson 1837; Guerin 1880).

About two thirds of the houses in Tiberias, most of them built of stone masonry, together with a large part of the walls, the bazaar, minarets, the mosque and the church of St Peter, collapsed, killing 922 people, of whom 500 were Jews, 300 Moslems and 22 Christians, and injuring 65. These figures may include casualties from 17 settlements in the environs, which were destroyed but are not named in the returns. The castle was ruined, and its towers began to lean. The baths, which had been built in 1833, were not damaged, but the yield of the hot spring and fountains increased temporarily. The town was not restored until after 1846 ([1, 6]; Thomson 1837; 1859; Shkelov 1837; Olim 1843; Montefiori 1844; Furst 1847; Beldam 1851; Robinson 1856; Pfeiffer 1856; Frankl 1858; Kerhardene 1859; Jenner 1873; Layard 1887; Italiander 1979).

Lubiya was totally destroyed and 143 people were killed (Thomson 1837; Beldam 1851). To the south, Kafr Sabt was ruined by the shock, without loss of life (Guerin 1880). Shadjara was also ruined and 50 people died (Calman 1837; Thomson 1837). In contrast, Kafr Kenna suffered negligible damage and no loss of life. Saffuriya and its church of Santa Ana also escaped entirely, with some limited damage to its ruined castle, while, next to it, Reina was obliterated, resulting in the loss of about 200 lives (Calman 1837; Thomson 1837; Robinson 1856). Contrary to early reports, damage in Nazareth was not excessive. Only one house collapsed and about one quarter of the dwellings in the town Suffered various degrees of damage. The hostel of the convent collapsed and an external cornice of the church of the Annunciation fell, killing four people. In all seven people were killed. The reported destruction in the northeastern part of Nazareth in fact refers to the cumulative losses suffered by settlements in the whole of its district, already accounted for in the returns, that amounted to 373 houses destroyed and 425 ruined, with 162 people killed and 13 injured ([1, 6]; Thomson 1837; Waghorn 1837; Vissino 1840; Schubert 1840; Blondel 1843; Beldam 1851; Robinson 1856; Tobler 1868).

South and southwest of Lake Tiberias the settlement of Simakh was also destroyed and five people were killed, and the villages of Hadatha, Ulam, Sirin, Kherbet Baka'a and Danna were damaged without loss of life (Waghorn 1837, Guerin 1880).

Many villages in the region east of the lake were likewise reduced to ruins, but details are lacking. In the district of Bashan, allegedly, fire was seen coming out of the ground (Calman 1837, Thomson 1837, Robinson 1856).

To the west, half of the houses of Ma'lun were ruined and five people were killed (Waghorn 1837). At Haifa only three houses were ruined, without casualties, and at Athlith a few local dwellings and one side of the walls were damaged. The remains of the church built by the Crusaders collapsed and the rubble was transported to Acre for the construction of the fortifications of the town ([6]; Waghorn 1837; Enlart 1925).

Further to the south damage was less serious. In the region of Harithiya 15 villages, which are not named in the sources, were ruined and 18 people were killed. In Arraba and Ajja damage was slight, and in Attil only two houses collapsed, while at Qaqun there was little damage and only a portion of the citadel collapsed, but in Jaba and in its environs 99 houses collapsed and 151 were damaged, and 23 people were killed [6].

Burqa and other nearby villages also suffered some slight damage, without casualties. Tubas was severely damaged, and east of the Jordan at Ajlun and Jerash there was also some damage. During the earthquake free-standing columns in the ancient city of Jerash were seen chattering on their bases but they did not collapse ([6]; Lindsay 1839; Johns 1932).

In Nablus one quarter of the houses and a number of shops were ruined and one quarter damaged, causing the loss of 48 lives. The rest of the town suffered only light damage. In the district of Nablus 150 people lost their lives ([1, 6]; Thomson 1837; Neman 1837; Shkelov 1837).

Damage decreased rapidly to the south. Jit suffered very little, and at Zeita only one house fell, killing two people [6].

Further away from the epicentral region, to the north, the shock was felt all along the coast, and at Tripoli it caused considerable concern, though no damage. At Latakia it was less strong in the town but rather violent in outlying districts. In Antioch ground movements were slow and lasted intermittently for a long time. In Aleppo the shock was generally felt and caused no damage anywhere in the region, while it was slight at Kilis and almost imperceptible at Aintab [1, 2, 6, 10].

However, in the alluvial plain of Adana the earthquake was strong and caused some panic. Many shops in the suq Adanat al-kubra collapsed. Also in the ports of Ayas (or Payas) and Iskenderun there was some alarm among European ship crews on land, who became nauseous. The shock was also reported from Tarsus, where it was slight but widely felt [6].

In the east, in Damascus about 2000 houses were slightly damaged, four minarets and several houses were destroyed, and about ten people were killed or injured. The bazaars of the city were damaged and part of the city gates and the tops of several minarets, which are not named, were thrown down [1, 2].

In the south, at the port of Jaffa the shock threw merchandise from stacks, and in Ramla it was slow. It was said that people could not stand erect. However, there is no evidence that it caused any damage [1, 6]. In Jerusalem the earthquake was not very strong and caused only limited damage. It is alleged that the minarets of the mosque at Kafr al-Tur, east of the city, were shaken down ([1, 2, 6, 10]; Calman 1837; Neman 1837).

In the Moab the shock caused sporadic destruction, particularly to old sites such as at Dihban, where some free-standing columns and arches were overthrown (Tristram 1874). Some slight damage was reported from Hebron, but details are lacking (Neman 1837). In Gaza the shock was rather slight and, except for the customs house, which was badly cracked, there was no other damage [6]. The earthquake was reported felt from as far south as Mt Sinai (St Catherine's?; Thomson 1837).

In the southwest the earthquake was felt in the Nile Delta, at Damietta, causing water to slosh out of a container, and in Misr (Cairo?), but it was not reported from Alexandria (Thomson 1837). In the west the earthquake was rather strong in the ports of Famagusta and Larnaca and was felt in other parts of Cyprus [1].

There is no evidence of a seismic sea wave on the Mediterranean coast. Also no waves have been reported in the Dead Sea. Allegedly, after the earthquake large masses of bitumen were seen floating in the Dead Sea (Robinson 1856).

It is said that waves flooded the coast of Lake Tiberias, but it is not clear whether this happened before, during or after the earthquake (Shkelov 1837; Kerhardene 1859). Aftershocks continued to be felt for almost four months, three of which were particularly important [2].

The loss of life caused by this earthquake and its aftershocks is difficult to estimate. The officially reported figure is 6000-7000 killed, but this is an early estimate and probably does not include losses in the districts of Marjuyum, al-Tuffa and Banyas, where many places within a radius of 50 miles (80 km) of Banyas were seriously affected, about which there is no infoiination [2]. A plague epidemic shortly after the earthquake added to the loss of life and isolated the coastal area from the hinterland, a situation aggravated by the Bedouins who for some time after the earthquake kept on hovering about ruined villages and towns. Safet, Tiberias and villages in the region of Bshara were plundered repeatedly by roving Druses and Mtwalis ([1, 4]; Montefiori 1844).

The combined effects of the earthquake, plague and unrest had considerable social implications. Owing to a rise in the price of labour, before long merchants began to find it difficult to transact their business and the most serious disturbances of commerce took place (Rustum 1923).

Damage in the epicentral region was widespread and varied from place to place over short distances. Much of the damage can be attributed to the high vulnerability of the local type of houses and also to the location of villages, particularly those in the central and northern parts of the affected area.

A general observation about a typical rural house in Syria and Palestine in the early 1800s is that its inherent strength was very low and extremely variable, and its vulnerability to earthquakes high. Local houses were chiefly one storey high, of rubble-masonry construction covered with heavy flat roofs, already in a ruinous state. The degree of damage or destruction caused by an earthquake was usually proportional to the size of the housing conglomerate or village; the larger the conglomerate, the heavier the apparent damage. The high vulnerability of local houses becomes apparent when we consider the relatively small damage sustained by the few properly built public structures in the epicentral region, such as convents, churches, walls and bridges, compared with that sustained by ordinary dwellings.

Another factor that contributed to the erratic distribution of damage in this and other earthquakes before and after 1837 is site effects. Many villages in the region, for defence reasons, were built on hilltops or on steep slopes, overlooking their fields. Many of these sites had already suffered from slides and regional instability of the ground, particularly those built on marls, chalk and weathered limestone. The destruction of Safed, for instance, and of the nearby villages of Ein Zeitim, Reina and Jish in the earthquake of 1837 can be attributed to their unstable foundation conditions rather than to the exceptional severity of the shock (Wachs and Lewitte 1984). Furthermore, the earthquake happened in the evening, during a wet period in winter when most people were indoors having dinner, which also contributed to the relatively large number of casualties. The relatively large magnitude of the event, the elongated shape of the meizoseismal region and its alignment with the Roum fault (Walley 1988) suggest that the earthquake was perhaps associated with surface faulting. However, there is no evidence for this in the sources.

It is said that as a result of the earthquake the coast of Lake Tiberias sank and that the lake water rose and swept away many people ([1]; Macgregor 1904). This observation on its own does not imply that this change of level of the coast was necessarily of tectonic origin. It may well have been a rather exaggerated observation relating to the usual rapid fluctuation of the level of the lake (Lynch 1852).

Reports that near Safed the ground was 'rent' and was so up to a point east of Jish and beyond as far as one could see, and that large fractures in the ground opened up near Mitulla and likewise in the vicinity of Baniyas, may refer to phenomena having a tectonic origin ([1, 2]; Waghorn 1837; Robinson 1856).

However, the reported cases of deep cracks opening up between Tiberias and Safed, emitting dust, seem to be descriptions of landslides, which include a classical case of a crack on a hillside near Tiberias opening up during the earthquake, into which two people fell, with the crack thereafter closing again and entombing them ([3]; Robinson 1856).

Another report, by seamen, that the westerly side of the shoreline at Sur had risen above the rocks and that this was clear proof of the subsidence of the ground caused by the earthquake cannot be substantiated (Bertou 1843).

In the light of this it appears that the 1837 earthquake was a shallow event with a magnitude larger than had been considered up to now. It was perhaps a multiple event, not dissimilar to earlier large earthquakes, consisting of two shocks, the macroseismic effects of which cannot be separated. Maximum damage was experienced along the Roum fault and perhaps some of its small branches, which occupy the region to the southwest (Freund et al. 1970; Nemer and Meghraoui 2006). However, there is no evidence in the sources for coseismic surface faulting for this earthquake, which is suggested only by the elongated shape of its epicentral region along the Roum fault.

References

[1] PRO FO 78.316 (Beirut: Moore to Palmerstone) 2.1.1837, 9.1.1837, 2.3.1837 (enclosures 2 and 5 to Palmerstone), 17.1.1837 (Aleppo: Werry to Palmerstone); 17.1.1837 (Aleppo: Werry to Bidwell) and 1.2.1837 (Aleppo: Werry to Ponsonby).

[2] PRO FO 78.315 (Damascus: Farrer to Palmerstone) 25.1.1837, 20.3.1837, 24.5.1837 and enclosures that are not dated.

[3] Archives Dipl. Nantes (Turq.) Corr. Cons. (Damas) 15.1.1837 and 22.2.1837; and (Beyrouth) 28.1.1837.

[4] Archives Dept. des Bouches du Rhone (Marseille) 200.33.

[5] Archives Societe de Geographie, Paris, Corr. 1649 (Beyrouth: Joselle to H. Joselle) 15.1.1837; (Beyrouth: Guys to H. Joselle) 17.1.1837.

[6] Archives Abdin Palace, Cairo, Corr. 1252, vol. 254, no. 403 (Ibrahim Pasa to Sami Beg) 10.3.1837 (2.12.1252); also extracts in Rustum (1942).

PATH no. 418, 1837.
PCB vol. 12.305.1837 and vol. 13.150.1838.
PEMS 15.2.1837 and 20.5.1837.
PJS 21.1.1837.
PMR no. 11, 322-341, 1843.
PNH vol. 2, no. 9, 134-135, 1835.

AD 1837 Jan 16 Rum

This was an aftershock of the earthquake of 1 January, which was widely felt at the southern extremity of the epicentral region and caused considerable damage in the districts of Jaffa and Nablus. Details are, however, lacking. This is an important shock in the seismic sequence because, if the damages caused by this event were serious and they were amalgamated in the official damage returns for the earthquake of 1 January 1837, the epicentral area of the main shock should not be extended as far south as Nablus. However, there is no way of confirming this since all of the detailed damage returns are dated February and March 1837.



AD 1837 Jan 22 Rum

The aftershocks of the 1 January earthquake, which occurred on 22 and 25 January, were reported from the northern part of the epicentral region. They caused panic in Damascus, but it is not known whether any damage was sustained (M2)



AD 1837 May 20 Rum

This was a third aftershock of the 1 January earthquake, which was also reported from the northern part of the affected area, where it caused considerable additional damage at Hashbeya, details of which are not known. The shock was strongly felt in the region of Lake Hule, but it was not reported at Damascus, perhaps because of a severe thunderstorm at the time (PRO FO 78.315).

References

Ambraseys, N. N. (2009). Earthquakes in the Mediterranean and Middle East: a multidisciplinary study of seismicity up to 1900.

Salamon et al (2011)

1837 01 01 - Sea of Galilee

Sources are

References

Salamon, A., et al. (2011). "A critical evaluation of tsunami records reported for the Levant Coast from the second millennium bce to the present." Isr. J. Earth Sci. 58: 327-354.

Sbeinati et al (2005)

1837 January 1, 04:00 p.m. (local time)

Parametric catalogues Seismological compilations Monographs

Ambraseys (1997)

1837 January 1 at about four in the afternoon, its epicentral area extended from beyond Safad into Lebanon, MS> 7.0, there is no conclusive field evidence that this event was associated with surface faulting. There was a destructive earthquake lasting about 20 s which caused heavy damage in Southern Lebanon and Northern Palestine. Destruction was done along the relatively narrow zone which extended from the coastal area of Saida through the inland ikilmi of Al-Touffa, Marjuyum, Bshara to lake Taberias. In Beirut, the earthquake caused panic and about eight houses collapsed killing two people. Saida was almost totally ruined with the loss of 7 lives. Much of Banyas was ruined. Sur suffered considerable damage where 40 houses collapsed killing 16 and injuring 36 people. Bint Jubayl was ruined with the loss of 8 lives. In Safad, the largest of places affected with 2158 deaths. At Acre, about houses fell, 4 people were killed and several injured. Also in the district of Acre, 141 people were killed. In Tiberias, about two thirds of the houses collapsed killing 822 people and injuring 65. In Nazareth, only one house collapsed and one quarter of the dwellings suffered killing 7 people. In Nablus, one quarter of the houses and a number of shops were ruined causing the loss of 48 lives. In Damascus, about 2000 houses were slightly damaged, 4 minarets and several houses were destroyed and about 10 people were killed or injured. Bazaars were damaged and parts of the city gates as well as several. At the port of Jaffa the shock threw merchandise from stacks while it was slow in Ramala. In Jerusalem, the earthquake was not very strong. The shock was felt all along the coast such as in Tripoli, Lattakia, Antioch as well as in Aleppo and at Kilis. Also it was felt in the Nile Delta, at Damietta and Cairo. The earthquake was also felt in Famagusta and Larnaca. Aftershocks continued to be felt for almost 4 months e.g., 16, 22, 25 January and 20 May were the most important. The loss of life due to this earthquake and its aftershocks was larger than 6000-7000 deaths (AMAE CADN; Archives Dép. des Bouches du Rhône; Archives Société de Géographie; Archives: Abdin Palace, Athene, Correspondenzblatt, L’Echo du Monde Savante, Journal de Smyrne, Das Morgenland, Natur und Heilkunde; FO).

References

Sbeinati, M. R., R. Darawcheh, and M. Monty (2005). "The historical earthquakes of Syria: An analysis of large and moderate earthquakes from 1365 B.C. to 1900 A.D.", Ann. Geophys. 48(3): 347-435.

Ambraseys (1997)

References

Ambraseys, N. N. (1997). The earthquake of 1 January 1837 in Southern Lebanon and N orthern Israel.

Amiran et al (1994)

1 Jan. 1837 CE c. 15 hours

Details



References

P; M; R; B; L; V; W; S and map, p. 191; BM: 260; AM; AB:52; 87; 88; 89






References

Amiran, D. , Arieh, E. and Turcotte, T. (1994). "Earthquakes in Israel and adjacent areas: macroseismic observations since 100 B.C.E." Israel Exploration Journal 44: 260-305.

Ben-Menahem (1991)

Estimated Seismic Parameters from Ben-Menahem (1991)
Time Date Lat.
(°N)
Long.
(°E)
Location Δf (km.) ML Discussion
1434 Jan. 1 1837 33.0 35.5 near Safed 500 6.7
  • Tiberias :500 victims. City destroyed.
  • Destruction of Safed and Tiberias. 3000 victims.
  • Tidal wave in the Lake of Galilee.
  • Appearance of asphalt blocks in the Dead Sea
References

Ben-Menahem, A. (1991). "Four Thousand Years of Seismicity along the Dead Sea rift." Journal of Geophysical Research 96((no. B12), 20): 195-120, 216.

Abou Karaki (1987)

* 1 JAN. 1837, 33°N - 35.5° E, I0 = IX - XI
  • destructive earthquake "whose epicenter is near Safad; all the houses on the steep slopes have fallen, appearance of cracks in the ground, 5000 victims, main localities damaged...: Tiberias (700 victims) in Ein Zeitoun, El-Jish, and Reineh (IX-X), Sejera (IX?), Tyre and Sidon (VIII-IX), Nazareth (VI - VII), Jerusalem, Bethlehem, Hebron (moderate), devastating in Beirut at Safed deep cracks in hard rocks appearance of new thermal springs; low in Jericho; Damascus affected, in Haran and Golan "considerable", strong tsunami at Lake Tiberias (KAR),..., a unique and strong shock in Tripoli, the village of Reineh destroyed, its immediate vicinity unscathed (Will)

  • At 2:34 p.m.,..., appearance of blocks of asphalt in the Dead Sea, ML = 6.4 (BM1).

NAJA: the time given in KAR is 03h, on the other hand the list of (Will) gives another strong earthquake in 1838 with 3000 victims, mentioning Jaffa; this event does not appear in the rest of our references, and should be taken with caution.
French

* 1 JAN. 1837, 33°N - 35°,5E, I0 = IX - XI

  • séisme destructeur "dont l'épicentre est près de Safad ; toutes les maisons sur les fortes pentes sont tombées, apparition de fissures de terrain, 5000 victimes, principales localités endommagées... : Tiberias (700 victimes) à Ein Zeitoun, El-Jish, et Reineh (IX-X), Sejera (IX ?), Tyr et Sidon (VIII-IX), Nazareth (VI - VII), Jérusalem, Bethléem, Hebron (modéré), dévastateur à Beyrouth à Safaddes fissures profondes dans les roches dures apparition de nouvelles sources thermales; faible à Jericho ; Damas affecté, à Haran et Golan "considérable", fort tsunami au lac Tibériade (KAR),..., un choc unique et fort à Tripoli, le village de Reineh détruit, son voisinage immédiat indemne (Will)).

  • A 14 h 34 m,..., apparition de blocs d'asphalte en Mer Morte, ML = 6,4 (BM1)).

NAJA : l'heure donnée dans KAR est 03 h, d'autre part la liste de (Will) donne un autre fort séisme en 1838 avec 3000 victimes, en mentionnant Jaffa ; cet événement ne figure pas dans le reste de nos références, et est à prendre avec précaution.

References

Abou-Karaki, N. (1987). Synthèse et carte sismotectonique des pays de la bordure Orientale de la Méditerranée: sismicité du système de foilles du Jourdain – Mer Morte, University of Strasbourg, France. Ph.D. Diss.

Wikipedia page for the 1837 CE Safed Quake



Paleoclimate - Droughts

Footnotes

References

References

Articles

Ambraseys (1997) The earthquake of 1 January 1837 in Southern Lebanon and Northern Israel

Calman SE (1837) Description of Part of the Scene of the Late Earthquake in Syria. J. Darling, London

Legendre, A. (1912). Orages et tremblements de terre en Palestine. Dictionnaire de la Bible. F. Vigouroux. Vol. 4 - Part 2: 2030-2031.

Rustam, Asad Jibrail (1923), Syria under Mehmet Ali, PhD dissertation, University of Chicago. p. 17

Vigouroux, F. (1903). Dictionnaire de la Bible, Letouzey et Anne.

Go to page 502/614

Wells, D. L. and K. J. Coppersmith (1994). "New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement." Bulletin of the Seismological Society of America 84(4)

Ya'ari A (1943) The letter of Salomon ben-Zemah in Letters of Eretz Israel. Gazit, Tel Aviv, Tel Aviv

Vered, M.; Striem, H. L. (December 1977), "A macroseismic study and the implications of structural damage of two recent major earthquakes in the Jordan Rift", Bulletin of the Seismological Society of America (Seismological Society of America) 67 (6): 1607-1613

Zohar (2016) A city hit by an earthquake: an HGIS approach to reconstructing the damage in Tiberias (Israel) in 1837



Earthquake Catalogs

ANTONOPOULOS, J. (1980). "Data from investigation on seismic Sea-waves events in the Eastern Mediterranean from 1800 to 1900 A.D." Annals of Geophysics.

Amiran, D. H. K., Arieh, E. and Turcotte,T. (1994). "Earthquakes in Israel and adjacent areas: macroseismic observations since 100 B.C.E." Israel Exploration Journal 44: 260-305.

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