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Tiberias Introduction

Aerial Photo of Tiberias Ancient Tiberias

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Names
Transliterated Name Language Name
Tverya Hebrew טיבריות
Ṭabariyyā Arabic طبريا
Rakkath Biblical Hebrew (Joshua 19:35) רקבת
Chamath Ancient Israelite (Jewish tradition) חמת
Tiberiás Ancient Greek Τιβεριάς
Tiveriáda Modern Greek Τιβεριάδα
Tiberiás Latin Tiberiás
Tiberias English Tiberias
Introduction
Introduction

Tiberias was founded between 18 and 20 CE by Herod's son Herod Antipas, who made it the capital of his kingdom; the city was named after the Roman Emperor Tiberius. Its location, on the western shore of the Sea of Galilee was then to the south of present-day Tiberias and to the north of the hot springs known as Hammath; the city's western boundary was marked by Mount Berenice, which rises to an altitude of approximately 200m above the level of the Sea of Galilee (Stern et al, 1993). In the 3rd century CE, the ruling institutions of the Jewish people moved to Tiberias and Tiberias became the Jewish capital of Palestine and the diaspora. The majority of the Palestinian (aka Jerusalem) Talmud was composed there (Stern et al, 1993). The city began to decline and moved north to present day Tiberais in the 9th and 10th centuries (Stern et al, 1993).

Identification

Tiberias was founded between 18 and 20 CE by Herod's son Herod Antipas, who made it the capital of his kingdom; the city was named after the emperor Tiberius. Its location, on the western shore of the Sea of Galilee (map reference 201.242) was then to the south of present-day Tiberias and to the north of the hot springs known as Hammath; the city's western boundary was marked by Mount Berenice, which rises to an altitude of approximately 200 m above the level of the Sea of Galilee.

History

Stern et al (1993 v. 4)

Josephus states that Tiberias was located "in the best region of Galilee." In order to populate the city as quickly as possible, the king attracted residents "by equipping houses at his own expense and adding new gifts of land" (Antiq. XVIII, 36-38). Coins issued in honor of the founding of the city feature the reed plants indigenous to the shores of the Sea of Galilee; later coins, minted toward the end of the Second Temple period, bear a palm tree, symbolizing the city's prosperity.

According to Josephus, the royal palace was a magnificent building, that was decorated with "representations of animals," and whose ceilings were "partly of gold" (Life 65-66). The royal treasure houses and archives were also here, at least until61 CE when Tiberias lost its role as the capital (Life 38). Josephus also mentions a synagogue, which was "a huge building, capable of accommodating a large crowd" (Life 277). After the death of Herod Anti pas' successor, Agrippa I ( 44CE), Tiberias came under the authority of the Roman procurators of Judea. The town maintained its position as the capital of Galilee without interruption until 61, when it was annexed to the kingdom of Agrippa II (Life 37-38), whose capital was at Caesarea-Philippi (modern Banias). As Agrippa's sister Berenice ruled at his side in Banias, the popular tradition linking her name to the mountain and aqueduct in Tiberias has no historical basis. At the outbreak of the First Jewish Revolt against Rome in 66, Tiberias was fortified with walls that remained standing even after the city had surrendered to the Roman army (War II, 572-573; III, 460-461).

Tiberias continued to be part of Agrippa II's kingdom, probably until his death in about 96. Then the town came under direct Roman rule and enjoyed the prosperity characteristic of the Roman Empire. During Hadrian's reign, a temple was built in his honor (the Hadrianeum, "a very great temple" according to Epiphanius, H aer. 30, 12). Its four-columned facade is depicted on a series of coins minted at Tiberias in 119. In the mid-second century the city, previously considered unclean because of the many old graves in it, was purified by Rabbi Simeon Bar Yohai (Gen. Rab. 79h; J.T., Shah. 9, l-38d).

During the reign of Emperor Elagabalus (218-222), Tiberias was granted the status of a Roman colony, as it appears from coins (B.T., A.Z. lOa). It was then that the ruling institutions of the Jewish people were moved from Sepphoris to Tiberias: first (c. 235) the Sanhedrin, with Rabbi Yohanan at its head, then the Patriarchate, and the then reigning patriarch, Rabbi Judah II Nesiah (d. c. 270). Yohanan established the Great Study House (beth ha midrash ha-gadol). In this institution, frequently mentioned in Talmudic literature, the great majority of the Palestinian (Jerusalem) Talmud was written.

After Tiberias became the Jewish capital of Palestine and the Diaspora, it continued to prosper for a considerable time. The sources refer to the city gate and to the fortress, which was probably built on the site of the royal palace from Second Temple times. Mention is also made of the boule (municipal council), various synagogues, study houses, city markets, and a series of public buildings-a stadium, bathhouse, lavatory, and magnificent tombs. Near these were the residential quarters of the city and various industrial areas, which included, inter alia, glassworks and pottery workshops. South of Tiberias, in the vicinity of the hot springs, Hammath-Tiberias (q.v.) developed as a suburb serving the numerous visitors who came from far and near to the medicinal springs.

In the sixth century, the Academy (Yeshiva) of Bretz-Israel, which succeeded the Sanhedrin as the supreme religious institution of the Jewish people, was established in Tiberias. The academy continued its activities here long after the Arab occupation, probably until the tenth century. During that time-the period of the Gaonim-several schools of poets and preachers were active in Tiberias, as were scribes and vocalizers (the Masoretes), whose system of vocalization, still in use today, is known as the Tiberian system.

After the Arab invasion, Tiberias superseded Beth-Shean as the capital of northern Palestine. The city continued to prosper until the ninth century. In the tenth century, however, security in the area began to deteriorate and the population declined. In 1033, Tiberias was destroyed by an earthquake; in the Crusader period, it was moved to the north, to its present location. Since then, most of the area of ancient Tiberias has remained desolate.

History of Tiberias until the arrival of the Crusaders

The foundation date of Tiberias is not certain. Named after Tiberius (reigned 14–37 CE), it is believed to have been founded by Herod Antipas, son of Herod the Great, as his capital some-time between 18 and 20. In 39 Antipas’s nephew, Agrippa I, gained control over the city and ruled it up to his death in 44 CE. Until 61 CE it was ruled by the procurators, when its political status changed when it was annexed to the kingdom of Agrippa II, whose capital was at Banias. In about 100 CE it came under direct Roman rule. During Hadrian’s reign (117–138 CE) there commenced the erection of a temple in his honor in the middle of the city, which, however, was never finished.

In the third century, Tiberias flourished: not only was it granted the status of a Roman colony (under Elagabalus [reigned 218–222 CE]), but also it became the capital of the Jewish people, after the Sanhedrin, the Patriarchate, and the leader of the community all had moved there from Sepphoris. Rabbi Yohanan, head of the Sanhedrin, established the bet ha-midrash ha-gadol, where the Palestinian Talmud was mostly written. From the sixth century on, Yeshivat Eretz Israel, the supreme religious institution for the Jews in Palestine and the Diaspora, was active in Tiberias, at least until the tenth century (of note is the fact that the Aleppo Codex was compiled in Tiberias at this time), when it finally moved to Jerusalem. Even then, Tiberias continued to serve as a center for the Masoretes, who dealt with the correct vocalization of the Holy Scriptures, for Hebrew grammarians, as well as for poets and preachers.

The prominent Jewish character of Tiberias might have been the main reason the Christian community did not take off, at least until the fifth century.2 Yet, despite the slow penetration of Christianity into Tiberias, we know that by the mid-fifth century it is already a seat of a bishopric, as its bishop (John) is mentioned in the lists of the Council of Chalcedon (451 CE).3

Tabariyya, as it is named in Arabic, was conquered by Arab armies in 635 CE. According to al-Baladhuri (d. c. 892)4, the terms of surrender guaranteed a smooth and peaceful change of government. Eventually Tabariyya was chosen to be the capital of Jund al-Urdunn, ultimately to the detriment of Baysān/Scythopolis, capital of Palaestina Secunda. It is not clear,nevertheless, when exactly this shift of capitals took place.

Three major earthquakes affected Tiberias during the Early Islamic period: 749 CE, 1033 CE, and 1068 CE. The first certainly caused much destruction, as we learn from the excavations at Galei Kinneret,5 but the earthquake was followed by renovation, building, and expansion. The earthquake of 1033, until recently thought to have brought Tiberias to an end, was not as dramatic for Tiberias. The account of the Persian traveler Nasir-i Khusraw of 1047 CE makes no reference to a devastated city, quite the opposite:6
The city has a strong wall that, beginning at the borders of the lake, goes all round the town; but on the water side there is no wall. There are numerous buildings erected in the very water, for the bed of the lake in this part is rock; and they have built pleasure-houses that are supported on columns of marble, rising up out of the water. The lake is full of fish.
Nasir-i Khusraw goes on, describing the Friday Mosque in the middle of the town, as well as another one called Jasmine Mosque, on the western side of the city.

In addition to natural disasters, Islamic Tiberias was hit by invasions and sacking. In 906 CE the Ismaili Qarmatis, fighting against the Tulunids for the leadership of Syria, captured Tiberias, a major army base at the time. The sources tell that, following the resistance of its people, the city was plundered, women taken captive, and many people killed7. The eleventh century was even harder for Tiberians, as in general for the people of Palestine. Even before the earthquake of 1033 CE8, drought and unrest had struck the region. The Banu Jarrah Bedouin caused much instability. In August 1024 CE, their leader al-Hassan b. al-Mufarrij sacked Tiberias and killed its people mercilessly.9

Not withstanding the unrest, southern Syria under the Fatimids — and especially its two capitals, Ramla and Tiberias — witnessed a golden age. Much building and commercial, cultural, and religious activities took place. But toward the 1050s–1060s, the situation changed again, this time creating a political vacuum from which it was dfficult to recover. Jewish letters found in the Geniza are testimony to the stress under which the population of Syria lived.10 This situation, among others, made room for the Seljuq invasion of the 1070s, when Tiberias was made the Seljuq base against the Fatimids.11

In August 1098, the Fatimids managed to regain Jerusalem from the Seljuq Turks, putting an end to their rule over Palestine. Yet the Fatimids’ hold was short, and in July 1099 Palestine fell into the hands of the Crusaders. The old city center of Tiberias became a quarry for building material to the newly established Crusader fortfication to the north of the city.12
Footnotes

2 The Panarion of Epiphanius (fourth century) includes a passage that seems representative of the Jewish sovereignty in Tiberias, despite being under Christian rule. The passage refers to Count (Comes) Joseph from Tiberias, a Jew converted to Christianity and protégée of Constantine (reigned 306–337 CE). He planned to build a church at the site of the unfinished Hadrianeum, but the local Jews often disrupted his works. So he eventually built a small church at the site of the temple, left the city, and settled in Beth She’an. See The Panarion of Epiphanius of Salamis (trans. F. Williams; Nag Hammadi Studies 35; Leiden: Brill, 1987), book 1, sections 1–46, §30.12,1–12,9.

3. R. Price and M. Gaddis, trans., The Acts of the Council of Chalcedon (Translated Texts for Historians 45;Liverpool: Liverpool University Press, 2005), 1:360.

4. Ahmad ibn Yahyā ibn Jābir al-Balādhurī, Futūh al-buldān (Leiden: Brill, 1866), 115–16

5. License no. A-3607. Moshe Hartal, “Tiberias, Galei Kinneret,” HA-ESI 120 (2008)

6. Nāsir-i Khusraw, Safarnāma, ed., Yahyā al-Khashshāb (Beirut: Dār al-Kitāb al-Jadīd, 1983), 52.

7. Moshe Gil, A History of Palestine, 634–1099 (Cambridge: Cambridge University Press, 1997), §468.

8. A further earthquake, which took place in September 1015, is recorded by the sources, but apparently it was of little consequence, the main result being the collapse of the dome at the Dome of the Rock in Jerusalem. See ibid., §581. For the earthquake of 1033 and 1068, see ibid., §§595 and 602.

9. Ibid., §585.

10. Ibid., §596.

11. Ibid. §603.

12. On this fortfication, see Yosef Stepansky, “The Crusader Castle of Tiberias,” Crusades 3 (2004): 179–81.

History of Tiberias during the Ottoman Period

Tiberias was established in 19 CE by Herod Antipas who named it after the Roman emperor Tiberius. Like the rest of Palestine, during the next 1500 years it underwent Roman, Byzantine, Muslim, Crusader and Mamluk regimes (Avi-Yonah 1951, 1980, Gil 1983). In 1517 the Ottomans conquered Palestine and were mostly interested in subjecting Tiberias to the general governance of Damascus. Their interest was smartly manipulated by Dona Gracia, a wealthy Portuguese Jewess from Istanbul (Turkey) who used her influence and connections at the Sultan’s court to increase the Jewish population in the Galilee and to establish Tiberias as a Jewish centre. Ottoman Firmans (written permission) report that between June 1560 and December 1565 Dona Gracia had leased the collection of taxes in Tiberias and a few other villages in the region. The Firmans also imply that she was probably responsible for reconstruction of the surrounding walls of Tiberias in order to increase the security of the inhabitants (Roger 1646, De Aveiro 1927, Heyd 1966).

The prosperity of the Jewish community did not last long and sometime at the beginning of the seventeenth century the Jews were forced to leave due to Ottoman tyranny (Roger 1646, De Thévenot 1971). The turning point for Tiberias was the rule of Dahir al-Umar of the Bedouin Zaydan family. Close to the mid-eighteenth century he gained control of Tiberias and other Galilean regions and gradually accumulated massive power. His dominancy did not escape the eyes of Suleiman, the Pasha of Damascus, who decided to overthrow Dahir’s rule by besieging Tiberias three times: in 1738, 1742 and 1743. The first two sieges were failures and during the last attempt Suleiman died of an intestine illness (Bnayahu 1946, Heyd 1969, Nachshon 1980). The son of Dahir, Chulaybi, had fewer confrontations but, like his father, kept strengthening Tiberias and in 1750 also built a citadel on a hill at the northwest corner of the city (Hasselquist 1766). In October and November 1759, the walls and the Citadel were severely hit by two consecutive earthquakes (Ambraseys and Barazangi 1989, Ambraseys 2009), but were gradually restored towards the end of the nineteenth century (Mariti 1791).

In October 1831 the Egyptian Ibrahim Pasha invaded Palestine on his way north and in May 1833 he completed the conquest of Syria and Palestine. In 1834 another damaging earthquake struck Palestine but no damage to Tiberias or northern Palestine was reported (Ambraseys 2009). In the same year a Fellahin rebellion erupted in the mountainous areas of Bethlehem, Jerusalem, Nablus, Transjordan and northern Galilee. The rebels took over Tiberias for a short period but the Egyptians, with reinforcements from the south, eventually managed to gain back control of the city (Ben-Zvi 1954). From that year until the 1837 earthquake the city remained under Egyptian rule.

Description of pre 1837 CE Tiberias

Maps and Figures
Maps and Figures

Normal Size

  • Table 1 Localities reported as damaged in 1837 CE Safed Quake and Legend/Key to sites in the Map in Figure 6 - from Zohar (2017)
  • Fig. 6 Map of Tiberias before the 1837 CE Safed Quake from Zohar (2017)
  • Fig. 7 3D reconstruction of Tiberias before and after the 1837 CE Safed Quake from Zohar (2017)

Magnified

  • Table 1 Localities reported as damaged in 1837 CE Safed Quake and Legend/Key to sites in the Map in Figure 6 - from Zohar (2017)
  • Fig. 6 Map of Tiberias before the 1837 CE Safed Quake from Zohar (2017)
  • Fig. 7 3D reconstruction of Tiberias before and after the 1837 CE Safed Quake from Zohar (2017)

Discussion

Much of the sources divide their descriptions of the city by the existing ethnic groups at the time, i.e., Jews, Muslims and Christians. Along almost the entire nineteenth century each of these groups resided in a different and separated area within the city. Consequently, the reconstruction of the Tiberias cityscape and the following damage analyses was carried out in light of this sub-division of the city. A summary of the prominent structures, the reconstructed 2D map and the 3D models appear in Table 1, Figures 6 and 7, respectively.

At the beginning of the nineteenth century Tiberias was a desolated city situated on the western shores of the Sea of Galilee (Figure 6) (Volney 1788, Richardson 1822, Irby and Mangles 1823). Roughly, the city was divided into three quarters:
  1. the Muslims resided mainly at the northwestern area
  2. the Jews occupied an isolated quarter at the eastern side close to the shore
  3. several dozen Christians lived in the southern end of the city (Avissar 1973, Schur 1987, Ben-Yaakov 2001).
The total area of the city did not exceed a quarter of a square kilometre and contained only a few hundred dwellings (Pococke 1745, Mariti 1791, Wilson 1823, Mendel 1839). A significant part of the city, in particular in the north, was apparently vacant of buildings and apart from in the Jewish quarter, houses were located far from each other (Richardson 1822, Stephens 1839) . The exact number of houses is not clear but according to the contemporary sources, the number of Jewish, Christian and Muslim buildings ranged between 185–230, 40–80 and 150–250, respectively, and all together between 375–560 houses (Turner 1820, Wilson 1823, Jowett 1826, Horne 1836, Schur 1988). Most of the buildings were built of stone and had 1–2 stories, i.e., roughly were between 3 and 6 m high. Many of the houses had little porches used for sleeping outdoors during the hot summer nights (Turner 1820, Pueckler-Muskau 1844).

The city was surrounded by the mid-eighteenth century walls repaired by Dahir al-Umar and his son Chulaybi. Their thickness ranged between 80 and 120 cm and Birav (Bnayahu 1946) reported that they were so high that ladders were needed to climb over them. Other western travellers estimated their height between 6 and 8 m (Pococke 1745, Hasselquist 1766, Spilsbury 1823, Robinson and Smith 1856). The walls were flanked by 21 circular turrets standing at unequal distances between each other (Irby and Mangles 1823, Jowett 1826). According to Jacotin’s map and Burckhardt’s sketch, there were only two gates to the city: a western main gate and a small southern gate (Jacotin 1799, Burckhardt 1822). Like other Ottoman cities, the citadel on the northern hill of Tiberias protected the town from outer invasions (Pococke 1745, Hasselquist 1766, Clarke 1810– 1823).

There were two mosques in the city: the largest was the al-Zaydani (al-Umari), named after Dahir’s family name, while the other was al-Bahri (the sea mosque), and located south of the Jewish quarter. The Church of St. Peter was situated north of the Jewish quarter but the house of the Catholic priest, however, was at the southern end of the city.

Additional Ottoman buildings, located in the Muslim quarter close to the western gate, were the houses of the Aga (governor house or Seraiah), the Kadi, the Imam and the army commander (Schur 1987, Abbasi 2006) . A small bazaar decorated by massive vaults was located in the centre of the city. Other vaulted arches were located at the southern shoreline facing the sea (Burckhardt 1822).

The Jewish quarter occupied a portion of the city close to the shore. It was surrounded by a high wall with a western entrance gate, which was regularly shut at sunset. Apparently, there were at least two synagogues and a ‘Kolell’ (a Jewish school) within the quarter and probably another one at the southern end of the city: Stephens reported on two synagogues and two schools and Jowett reported on two schools and three synagogues. I assume that the ‘Kollell’ reported in 1833 in the letter of Rabbi Yaa’kov Menlis, is the ‘Reysin’ Kollell, located close to Menahem Mendel’s house (Stephens 1839, Jowett 1826, Robinson and Smith 1856, David Debith Hillel in Ya’ari 1976, pp. 512–514, Scholz 1822, de Gramb 1840, Schur 2002). Although Christians lived mainly in southern Tiberias, there were also a few dwellings of Jews there: von Puckler Muskau reported that a wealthy Jew (Hayim Weisman?) had 21 houses to let. He does not mention their exact location but since there are no reports of hotels in the Jewish quarter, I assume they were located in the southern part of the city (Pueckler-Muskau 1844). Located about half a kilometre south of the city were the Jewish and Muslim cemeteries and about one kilometre further south the thermal baths for local and touristic use (Seetzen 1810, Robinson and Smith 1841). North of the city there were several sacred tombs (Mendel 1839, Robinson and Smith 1856, Guerin 1880) and west of it a small agricultural area. One major road led to the city from the south and two others from the west (Jacotin 1799, Buckingham 1822, Olin 1844).

Exploration and Excavation

The remains of ancient Tiberias' walls were first examined by V. Guerin in 1875. A more detailed survey of the walls at the top of Mount Berenice was carried out by G. Schumacher in 1887. A systematic excavation of the southern gate and its vicinity was carried out by G. Foerster in 1973-1974, on behalf of the Israel Department of Antiquities and Museums, the Institute of Archaeology at the Hebrew University of Jerusalem, and the Israel Exploration Society. In addition, a great number of salvage excavations has been carried out. The largest, in both scale and results, was conducted in the center of the municipal area of the ancient city, under the direction of B. Rabani (1954- 1956). The excavators cleared a section of the city's central colonnaded street (its cardo), as well as a bathhouse and vaulted market. To the east, not far from the lake shore, A. Druks (1964-1968), uncovered the remains of a basilica! structure. When the excavations were extended to the south, along the shore, the remains of an exedra and various public buildings were revealed. In 1976, F. Vitto excavated a Roman tomb in Tiberias, and in 1989-1990 Y. Hirschfeld's salvage excavation at the foot of Mount Berenice exposed a Roman public building beneath the remains of private houses. Since 1990 Hirschfeld has been directing excavations on the summit of Mount Berenice.

The rapid development of modern Tiberias necessitated several salvage excavations in the southern part of the city. The remains of the Byzantine city wall and a large Crusader church were discovered by A. Harifin 1980, when foundations were dug for the Jordan River Hotel. Farther south, A. Berman, working in 1978-1979, had discovered the remains of a synagogue and private houses from the Byzantine and Early Arab periods.

Other salvage excavations in the area revealed the remains of churches and fortification systems from the Crusader period. Dozens of tombs were discovered in the area to the north and northwest of the Byzantine city wall, mainly on the slopes now occupied by modern Tiberias. The results of these salvage operations provide important data for a reconstruction of the city plan of Roman-Byzantine Tiberias.

List of studies with earthquake evidence

Location Studies Notes
Galei Kinneret Galei Kinneret Site is just south of what appears to be the Roman Stadium
Berniki Theatre
Water Reservoir
Southern Gate
Aviv Hotel
Site 7354
House of the Bronzes
Basilica
Gane Hammat
Mount Berineke

Maps, Aerial Views, Cross-Sections, Seismic Data, Tables, Illustrations, and Photos
Maps, Aerial Views, Cross-Sections, Seismic Data, Tables, Illustrations, and Photos

Maps

General Maps and Archaeological Maps

Normal Size

  • Fig. F Main archaeological sites of Tiberias from Cytryn-Silverman (2015)
  • Fig. 1 Map of Tiberias during the Roman period from Atrash (2010)
  • City plan of Tiberias from Stern et al (1993 v.4)
  • City center plan of Tiberias from Stern et al (1993 v.4)
  • City gate from Roman period Tiberias from Stern et al (1993 v.4)
  • City Plan and wall in the 6th century CE from Stern et al (1993 v.4)

Magnified

  • Fig. F Main archaeological sites of Tiberias from Cytryn-Silverman (2015)
  • Fig. 1 Map of Tiberias during the Roman period from Atrash (2010)
  • City plan of Tiberias from Stern et al (1993 v.4)
  • City Plan and wall in the 6th century CE from Stern et al (1993 v.4)

1837 CE Safed Quake Related Maps

Normal Size

  • Fig. 1a Regional Damage Distribution from the 1837 CE Safed Quake from Zohar (2017)
  • Fig. 6 Map of Tiberias before the 1837 CE Safed Quake from Zohar (2017)
  • Fig. 8 Map of damage in Tiberias due to 1837 CE Safed Quake from Zohar (2017)

Magnified

  • Fig. 1a Regional Damage Distribution from the 1837 CE Safed Quake from Zohar (2017)
  • Fig. 6 Map of Tiberias before the 1837 CE Safed Quake from Zohar (2017)
  • Fig. 8 Map of damage in Tiberias due to 1837 CE Safed Quake from Zohar (2017)

Aerial Views

General Aerial Views

  • Annotated Aerial View of Tiberias from BibleWalks.com
  • Fig. A - Aerial view of ancient Tiberias from Cytryn-Silverman (2015)
  • Ancient Tiberias in Google Earth
  • Ancient Tiberias on govmap.gov.il

1837 CE Safed Quake Related Aerial Views

Normal Size

  • Fig. 1b Satellite View of the Old City of Tiberias from Zohar (2017)
  • The "Old City" of Tiberias in Google Earth
  • The "Old City" of Tiberias on govmap.gov.il

Magnified

  • Fig. 1b Satellite View of the Old City of Tiberias from Zohar (2017)

Map of Excavation Sites

Legend/Key

Legend/Key to excavation sites

Stern et al (2008)

Map

Tiberias: map showing excavation sites

Stern et al (2008)

Geologic Maps, Cross-Sections, and Seismic Data

Geologic Maps, Cross-Sections, and Seismic Data

Normal Size

  • Fig. 4 Map of ancient Tiberias with inferred fault from Ferrario et al (2020)
  • Fig. 1b Quaternary faults around the Sea of Galilee and the Jordan Valley from Ferrario et al (2020)
  • Fig. 1c Simplified geologic map around the Sea of Galilee along with epicenters of MW > 4.0 events since 1970 from Ferrario et al (2020)
  • Fig. 10 Sketches of the shallow subsurface from Ferrario et al (2020)
  • Fig. 2b Morphotectonic map from Ferrario et al (2020)
  • Fig. 9 Interpreted Seismic lines from Ferrario et al (2020)
  • Fig. 8 Interpreted Seismic line run north of Tiberias Theater from Ferrario et al (2020)
  • Fig. 2a Site Map from Ferrario et al (2020)

Magnified

  • Fig. 1b Quaternary faults around the Sea of Galilee and the Jordan Valley from Ferrario et al (2020)
  • Fig. 2b Morphotectonic map from Ferrario et al (2020)
  • Fig. 9 Interpreted Seismic lines from Ferrario et al (2020)
  • Fig. 8 Interpreted Seismic line run north of Tiberias Theater from Ferrario et al (2020)
  • Fig. 2a Site Map from Ferrario et al (2020)

Geologic Map

Figure 2

Geological map of the study area compiled from Sneh (2008), and Bogoch and Sneh (2008) with an overlay of faults according to Schulman (1966), and with locations of the refraction profiles TB-1, TB-2 and TB-3 (Ezersky, 2008); R-1 and R-2 (Shtivelman, 1995) and profiles 1 and 2 for constructing cross sections.

Zaslavsky et al. (2009a)


Stratigraphic Table

Table 1

Stratigraphic table of the geological map of Tiberias

(Sneh, 2008)

Zaslavsky et al. (2009a)


Illustrations

  • Fig. 14 Proposed reconstruction of the ancient city of Tiberias from Hirschfeld and Galor (2007) and Atrash (2012)

Photos

  • Fig. E Roman cardo and overlaying street from Cytryn-Silverman (2015)

Textual Chronology
749 CE Sabbatical Year Earthquakes

Discussion

Discussion

1837 CE Safed Quake

Discussion

Discussion

References
Notes by JW

Chronology is well established as damage and destruction in Tiberias due to the 1837 CE Safed Quake was described and recorded by several contemporaneous sources based on first hand accounts - some of which are listed below:

Source Report Notes
Article in the Missionary Herald by William McClure Thomson 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
The Times (of London) A LIST OF TOWNS ETC., DESTROYED OR INJURED IN SYRIA BY THE EARTHQUAKE ON THE 1st OF JANUARY

Archaeoseismic Chronology
Phasing

All of Tiberias

Stratum Period Date Notes
I Late Fatimid 11th century CE construction above the collapse caused by an earthquake (in 1033 CE?)
II Early Fatimid 9th - 10th centuries CE continued use of the street with shops.
III Abbasid 8th - 9th centuries CE a row of shops, the basilica building was renovated.
IV Byzantine–Umayyad 5th - 7th centuries CE the eastern wing was added to the basilica building; the paved street; destruction was caused by the earthquake in 749 CE.
V Late Roman 4th century CE construction of the basilica complex, as well as the city’s institutions, i. e., the bathhouse and the covered market place.
VI Roman 2nd - 3rd centuries CE establishment of the Hadrianeum in the second century CE (temple dedicated to Hadrian that was never completed) and industrial installations; the paving of the cardo and the city’s infrastructure.
VII Early Roman 1st century CE founding of Tiberias, construction of the palace with the marble floor on the shore of the Sea of Galilee, opus sectile, fresco.
VIII Hellenistic 1st - 2nd centuries BCE fragments of typical pottery vessels (fish plates, Megarian bowls).

Textual Seismic Effects
749 CE Sabbatical Year Earthquakes

Effect                            Location Image(s) Description(s)
  • Destruction
  • 30 synagogues collapsed
  • Destruction of Hot Springs Complex
  • Casualties
Tiberias
  • "This earthquake destroyed the city of Tiberius except for house of a man named 'Isa. It overthrew thirty synagogues and wonderful natural things. The thermal baths - that wonderful building - built by Solomon the son of David, collapsed and was destroyed. There was a spring with purgative water and amazing constructions above it, surrounded by hotels (inns) for the sick who sought to be healed. There were clay pots artistically made and arranged. On each pot was written how many times it purged the bowels of those who drank from it. Each person chose a pot according to how much they wanted to drink. All these buildings are gone." - Michael the Syrian

  • "This earthquake destroyed the city of Tiberias, except for the villa of a man named `Isa Galba. It knocked down thirty synagogues of the Jews and some wonderful natural sites there. The baths, a fine structure erected by Solomon the King) collapsed and fell down. There was there a healing spring given by God for the health of men, above which marvellous buildings had been erected and all around it was everything necessary for the use of those who came in search of a purge. They say that placed there were earthen jugs skillfully arranged, on each one of which was written how many times it flushed the stomach of the one who drank it. Thus each person chose a jug according to how much he desired to be purged. All those buildings have now been destroyed and expunged." - Chronicon Ad Annum 1234

  • "many people perished, especially in Tiberias, where more than 100,000 men succumbed" - Agapius of Manbij

  • "rage in fear and dark chaos will capital Tiberias
    ...
    I heard how disaster befell the city and
    the old and young in it have perished" - Ra'ash Shevi'it (רעש שביעית)

1837 CE Safed Quake

Textual Seimsic Effects

Effect                            Location Image(s) Description(s)
  • Destruction
  • Casualties
Tiberias
  • Destruction (collapsed walls)
  • Casualties
  • Altered spring behavior
Tiberias
  • "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." - Article by William Mclure Thomson in the Missionary Herald (1837:436-437)
  • Fractured Walls
  • Ruins (collapsed walls)
  • Altered Spring behavior
  • Casualties
Tiberias
  • "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." - William Mclure Thomson in The Land and the Book (1861:278-279)
  • Destruction (collapsed walls)
Tiberias
  • walls cast down to the ground
  • tower damage
  • galleries and chambers laid open (collapsed walls)
Tiberias
  • "We did not enter Tiberias, but pitched on the banks of the lake; the earthquake had left the town in ruins, its walls cast down to the ground, its towers split in two, and their galleries and chambers laid open and yawning in mid-air." - Lindsay (1838 v.2:87)

Observational Seismic Effects Table

Effect Location Image(s) Description
Damaged and Tilted Walls Citadel Walls (P1) and turrets (T4-T7)









  • the citadel, the surrounding public structures, walls and turrets were damaged but parts of them still remained (drawing 16, 25, 26, 28, 30 and 35 and photograph 44, Supplemental material). The walls were damaged unequally: little damage was observed in the northern part of the walls; the southern part was considerably damaged but parts of it still remained; the western part collapsed almost entirely along with its flanked turrets. Roberts sketched breaches within the walls and a diagonal lean of the southwestern turret1 (items 19–22, Supplemental material). These damaged structures were never reconstructed and some of them still remain in ruins today (Figure 2). - Zohar (2017:12)
  • 1. Engineers inspecting the turret stated that such a lean could have occurred only by a sudden turbulence and not by gradual subsidence because of the water (Shohat and Levi, personal communication, 2014) - Zohar (2017:footnote 1)
Sheared Wall Southern turret in Southern Wall




Dome collapse al-Zaydani Mosque (M1)












  • Inside the city, the al-Zaydani Mosque was damaged and its dome collapsed. Its minaret, however, still remained - Zohar (2017:12)
  • The drawings of Lehoux, Bernatz, Roberts, Munk, Bartlett, Lynch, Spencer and van de Velde (Supplemental material, items 16, 18, 19–22, 25, 31, 32, 33 and 35, respectively) depict the minaret of al-Zaydani still standing but no dome and no minaret at al-Bahri mosque. This is also apparent in a late nineteenth century photograph of Bonfils (Supplemental material, item 39). - Zohar (2017:12-13)
Minaret Collapse al-Bahri Mosque (M2)




  • the minaret of al-Bahri Mosque did not escape the damage (Robinson and Smith 1841, Olin 1844). - Zohar (2017:12-13)
  • The drawings of Lehoux, Bernatz, Roberts, Munk, Bartlett, Lynch, Spencer and van de Velde (Supplemental material, items 16, 18, 19–22, 25, 31, 32, 33 and 35, respectively) depict the minaret of al-Zaydani still standing but no dome and no minaret at al-Bahri mosque. This is also apparent in a late nineteenth century photograph of Bonfils (Supplemental material, item 39). - Zohar (2017:12-13)
Vault Destruction - completely or badly destroyed Vaulted Bazaar (P7)

  • The vaulted bazaar was damaged but there are no other specific details (Israel of Shklov 1837). I assume, however, that it was completely or badly destroyed for it is not apparent in the drawings of Lehoux and Roberts (Supplemental material, items 16 and 19–22). - Zohar (2017:13)
Damaged Arches Vaulted Arcs (P8)


  • The vaulted arcs in the south of the city were probably damaged as well; Roberts depicted them as damaged and this is also apparent in a twentieth century photograph (Supplemental material, items 20 and 45, respectively). - Zohar (2017:13)
Collapsed Walls dwellings
  • apparently, most of the Tiberias dwellings were completely destroyed while public buildings escaped the damage. The drawings of Lehoux, Roberts, Bernatz and Munk (Supplemental material, items 16, 18, 19–22 and 25, respectively) demonstrate that the Christian and Muslim quarters were almost completely destroyed and shortly after the earthquake were left with only a few standing dwellings - Zohar (2017:12)
  • The Jewish quarter, as reflected in various post-1837 drawings, seems to be less damaged than the Christian and Muslim quarters; Lehoux, Lintch and Roberts (Supplemental material, items 16, 20, 21, 22 and 32) depicted the Jewish quarter with more standing dwellings than in the other quarters. Further search through the visual sources to locate the remains of the walls surrounding the Jewish quarter produced no results; they may have been completely destroyed beyond repair. - Zohar (2017:13)
Damaged Walls City Walls (W1-21)




Damaged Walls Turrets (T1-20)
Tilted Wall Leaning Turret (T21)

  • Slight Damage - Zohar (2017:Table 1)
  • JW:Some of the lean could be due to differential subsidence and/or undercutting by wave action
Collapsed Wall Main Gate (G1)

Damaged Walls Southern Gate (G2)
Collapsed Walls Walls of the Jewish Quarter (JW1-2)
Collapsed Walls Gate of the Jewish Quarter (JG1)
Collapsed Walls Etz-Ha'yim ('Sephardim') Synagogue (S1)
Collapsed Walls Hasidim' Synagogue (S2)
Casualties Tiberias
  • The total number of casualties during the earthquake is not clear: while the official report of Suleiman Pasha numbers 922 victims, other estimations range between 700 and 2000. The eyewitness Calman reported that the number of Jewish victims was significantly greater than that of the Muslims and Christians. This report conforms to the report of Robinson from 1838 that numbers less Jewish families than Muslim families, although before the earthquake Jews were considered to be the majority in Tiberias (de Gramb 1840, Horne 1836, Debith-Hillel in Ya’ari 1976). - Zohar (2017:13)

Localities reported as damaged

Table 1

Damage in Tiberias due to 1837 CE Safed Quake Table 1

Localities in Tiberias reported to be damaged during the 1837 earthquake.

  • Symbol: identification of the structure (as mapped in Figure 6)
  • Damage: a rough estimation of the scope of the damage

    • N (no damage)
    • S (slight damage)
    • P (partial damage)
    • T (total destruction)


Zohar (2017)


Google Sheet

Damage by Quarter

Damage in Tiberias due to 1837 CE Safed Quake according to Ethnic Quarter Table 2

The number of damaged dwellings and structures in the Tiberias quarters classified by an estimated damage degree. Note that the maximal degree of damage in the Jewish quarter is less than that of the Muslim and Christian quarters. See also Figure 8.

Zohar (2017)

Spatial Distribution of Damage and Potential Site Effects

Figures
Figures

Image Figure Description Source
Figure 2a al-Zaydani Mosque in Tiberias Zohar (2017)
Figure 2b the Citadel in Tiberias
where 1837 earthquake damage is apparent
Zohar (2017)
Figure 2c al-Bahri Mosque in Tiberias Zohar (2017)
Figure 2d remains of the massive vaults
in southern Tiberias
(noted by red arrow)
Zohar (2017)
Figure 2e Etz-Hay’im Synagogue in Tiberias Zohar (2017)
Figure 2f one of the southern damaged
turrets in Tiberias’s walls
where 1837 earthquake damage is apparent
Zohar (2017)
Table 1 Damage Table Zohar (2017)
Table 2 Damage in the Quarters Zohar (2017)
Figure 6 Tiberias before the 1837 CE Safed Quake Zohar (2017)
Figure 7 3D reconstruction of Tiberias before
and after the 1837 CE Safed Quake
Zohar (2017)
Figure 8 Map of damage in Tiberias due to 1837 CE Safed Quake Zohar (2017)

Discussion

Rotating the models enabled a 360° examination of damage from almost any direction, even from spots that were not covered by the nineteenth century artists, such as an eastern spot in the Sea of Galilee or aerial views. The two models of before and after the earthquakes were compared (Figure 7) in order to identify the structural damage and examine its spread (Figure 8). It seems that although the Tiberias area was relatively small, the spread of the damage as well as its severity was not uniform. This is clearly observed particularly along the walls and between the residential quarters of the city. In general, such variability in damage within a small area may imply different local site attributes, whereas the distance from the epicentre and the directivity effect are almost identical in any spot within that area. Among the most influencing site attributes, one can count the construction quality, surface geology and topography (Zaslavsky et al. 2000). The latter two can hardly explain the differences whereas almost the whole of Tiberias is situated on basalt rocks (Pβc) and apart from the moderate northern slopes, the city lies on a flat plain (Figures. 7(a,b)). The construction quality, however, varies and manifests several structural styles for residential dwellings, religious structures and government buildings (Figure 2). Unfortunately, at this stage there is no reasonable understanding of the vulnerability and resistance of these structures to earthquake shaking. Yet, it is still possible to classify Tiberias’s structures into two groups.
  • The first, which was probably more resistant to earthquake shaking, includes the Citadel, walls, turrets and government buildings such as the Seraiah and Kadi houses Most of them, although badly damaged, remained partially standing, even in cases where they were located on a hill in the north of the city. This is, of course, no surprise for these structures were built in advance to withstand outer attacks and thus were probably quite stable. Yet, there is a prominent exception that deserves attention: The western part of the walls (between turrets T-12 and T-16), although built of the same materials and quality as the rest of the walls, collapsed completely, while the northern part, built on a slope, was only slightly damaged. Figure 8 portrays the spread of the damage in relation to the surface geology and suspected active faults. Accordingly, the majority of Tiberias is located on a single geologic foundation of basalt rocks but close to the western walls, there is a fault. This fault, suspected to be active (Sagy et al. 2013), crosses the southern walls between T16–T17 and runs parallel to the western walls for about 200 m within the proximity of only 50 m. In addition, the fault runs in between the basalt and alluvium lithologies and perhaps this transition zone contributed to the increase of the damage. However, further site-specific investigation, which is beyond the scope of this study, is needed to verify the mechanical role of this fault and the lithological contrast in the stability of the western walls and the nearby structures.

  • The second group includes dwellings and residential houses, most of which were completely damaged beyond repair. The damage in this category varies. The Jewish quarter seems to be slightly less damaged than the other quarters (Table 2) although the number of Jewish victims was greater (Robinson and Smith 1841). The explanation for this contradiction is not clear at this stage. Located along the shores of the lake, the Jewish quarter was more populated and clustered than the others and thus the dwellings in it were most likely of different architectural styles. In addition, a large part of the Muslim quarter in the north end of the city was located on a sloped hill whereas the Jewish and Christian quarters were located on a plain surface (Figure 7(a)). Thus, these factors also may have influenced the resistance to damage, but until the Ottoman construction styles are fully characterized, resolving this damage differentiation is rather complex.
The gates of the city did not withstand the earthquake and collapsed. Since the walls were never repaired, over the years some of the breaches were enlarged, probably by human activity, resulting in new entrances to the city (Guerin 1880). In late nineteenth century maps (Supplemental material, items 36, 40, 41 and 42), the southern entrance to the city is located between T-17 and T-18, some 50 m west of the original southern gate (Figure 6). At the north of the city, a new entrance and a trail leading to it appeared between T-2 and T-3. These two entrances and roads still exist today and constitute two of the major transportation entries to the city. The roads to Tiberias are an example of how a catastrophe such as an earthquake may divert and influence the morphology of a city for many years after.

Textual Deformation Maps
1837 CE Safed Quake

Entire City

Fig. 8

The spread of the earthquake damage that resulted in Tiberias by comparing the two HGIS models of before and after the earthquake (Figure 7).

Zohar (2017)

Textual Intensity Estimates
749 CE Sabbatical Year Earthquakes

Effect                            Location Image(s) Description(s) Intensity
  • Destruction (collapsed walls)
  • 30 synagogues collapsed (collapsed walls)
  • Destruction of Hot Springs Complex (collapsed walls)
  • Casualties (due to collapsed walls)
Tiberias
  • "This earthquake destroyed the city of Tiberius except for house of a man named 'Isa. It overthrew thirty synagogues and wonderful natural things. The thermal baths - that wonderful building - built by Solomon the son of David, collapsed and was destroyed. There was a spring with purgative water and amazing constructions above it, surrounded by hotels (inns) for the sick who sought to be healed. There were clay pots artistically made and arranged. On each pot was written how many times it purged the bowels of those who drank from it. Each person chose a pot according to how much they wanted to drink. All these buildings are gone." - Michael the Syrian

  • "This earthquake destroyed the city of Tiberias, except for the villa of a man named `Isa Galba. It knocked down thirty synagogues of the Jews and some wonderful natural sites there. The baths, a fine structure erected by Solomon the King) collapsed and fell down. There was there a healing spring given by God for the health of men, above which marvellous buildings had been erected and all around it was everything necessary for the use of those who came in search of a purge. They say that placed there were earthen jugs skillfully arranged, on each one of which was written how many times it flushed the stomach of the one who drank it. Thus each person chose a jug according to how much he desired to be purged. All those buildings have now been destroyed and expunged." - Chronicon Ad Annum 1234

  • "many people perished, especially in Tiberias, where more than 100,000 men succumbed" - Agapius of Manbij

  • "rage in fear and dark chaos will capital Tiberias
    ...
    I heard how disaster befell the city and
    the old and young in it have perished" - Ra'ash Shevi'it (רעש שביעית)
  • VIII+
  • VIII+
  • VIII+
  • VIII+
The archeoseismic evidence requires a minimum Intensity of VIII (8) when using the Earthquake Archeological Effects chart of Rodríguez-Pascua et al (2013: 221-224).

1837 CE Safed Quake

Observations

Effect Location Image(s) Description Intensity
Damaged and Tilted Walls Citadel Walls (P1) and turrets (T4-T7)









  • the citadel, the surrounding public structures, walls and turrets were damaged but parts of them still remained (drawing 16, 25, 26, 28, 30 and 35 and photograph 44, Supplemental material). The walls were damaged unequally: little damage was observed in the northern part of the walls; the southern part was considerably damaged but parts of it still remained; the western part collapsed almost entirely along with its flanked turrets. Roberts sketched breaches within the walls and a diagonal lean of the southwestern turret1 (items 19–22, Supplemental material). These damaged structures were never reconstructed and some of them still remain in ruins today (Figure 2). - Zohar (2017:12)
  • 1. Engineers inspecting the turret stated that such a lean could have occurred only by a sudden turbulence and not by gradual subsidence because of the water (Shohat and Levi, personal communication, 2014) - Zohar (2017:footnote 1)
VII +
Sheared Wall Southern turret in Southern Wall




VIII +
Dome collapse al-Zaydani Mosque (M1)












  • Inside the city, the al-Zaydani Mosque was damaged and its dome collapsed. Its minaret, however, still remained - Zohar (2017:12)
  • The drawings of Lehoux, Bernatz, Roberts, Munk, Bartlett, Lynch, Spencer and van de Velde (Supplemental material, items 16, 18, 19–22, 25, 31, 32, 33 and 35, respectively) depict the minaret of al-Zaydani still standing but no dome and no minaret at al-Bahri mosque. This is also apparent in a late nineteenth century photograph of Bonfils (Supplemental material, item 39). - Zohar (2017:12-13)
VIII +
Minaret Collapse al-Bahri Mosque (M2)




  • the minaret of al-Bahri Mosque did not escape the damage (Robinson and Smith 1841, Olin 1844). - Zohar (2017:12-13)
  • The drawings of Lehoux, Bernatz, Roberts, Munk, Bartlett, Lynch, Spencer and van de Velde (Supplemental material, items 16, 18, 19–22, 25, 31, 32, 33 and 35, respectively) depict the minaret of al-Zaydani still standing but no dome and no minaret at al-Bahri mosque. This is also apparent in a late nineteenth century photograph of Bonfils (Supplemental material, item 39). - Zohar (2017:12-13)
VI-VII +
Vault Destruction - completely or badly destroyed Vaulted Bazaar (P7)

  • The vaulted bazaar was damaged but there are no other specific details (Israel of Shklov 1837). I assume, however, that it was completely or badly destroyed for it is not apparent in the drawings of Lehoux and Roberts (Supplemental material, items 16 and 19–22). - Zohar (2017:13)
VIII +
Damaged Arches Vaulted Arcs (P8)


  • The vaulted arcs in the south of the city were probably damaged as well; Roberts depicted them as damaged and this is also apparent in a twentieth century photograph (Supplemental material, items 20 and 45, respectively). - Zohar (2017:13)
VI +
Collapsed Walls dwellings
  • apparently, most of the Tiberias dwellings were completely destroyed while public buildings escaped the damage. The drawings of Lehoux, Roberts, Bernatz and Munk (Supplemental material, items 16, 18, 19–22 and 25, respectively) demonstrate that the Christian and Muslim quarters were almost completely destroyed and shortly after the earthquake were left with only a few standing dwellings - Zohar (2017:12)
  • The Jewish quarter, as reflected in various post-1837 drawings, seems to be less damaged than the Christian and Muslim quarters; Lehoux, Lintch and Roberts (Supplemental material, items 16, 20, 21, 22 and 32) depicted the Jewish quarter with more standing dwellings than in the other quarters. Further search through the visual sources to locate the remains of the walls surrounding the Jewish quarter produced no results; they may have been completely destroyed beyond repair. - Zohar (2017:13)
VIII +
Damaged Walls City Walls (W1-21)




VII-VIII +
Damaged Walls Turrets (T1-20)
VII +
Tilted Wall Leaning Turret (T21)

  • Slight Damage - Zohar (2017:Table 1)
  • JW:Some of the lean could be due to differential subsidence and/or undercutting by wave action
VI +
Collapsed Wall Main Gate (G1)

VIII +
Damaged Walls Southern Gate (G2)
VII +
Collapsed Walls Walls of the Jewish Quarter (JW1-2)
VIII +
Collapsed Walls Gate of the Jewish Quarter (JG1)
VIII +
Collapsed Walls Etz-Ha'yim ('Sephardim') Synagogue (S1)
VIII +
Collapsed Walls Hasidim' Synagogue (S2)
VIII +
The archeoseismic evidence requires a minimum Intensity of VIII (8) when using the Earthquake Archeological Effects chart of Rodríguez-Pascua et al (2013: 221-224).

Textual Accounts

  • Earthquake Archeological    Effects from Rodríguez-Pascua et al (2013: 221-224)
  • Environmental Effects (ESI 2007)
  • Synoptic Table of ESI 2007    Intensity Degrees from Michetti et al. (2007)
Effect                            Location Image(s) Description(s) Intensity
  • Destruction (collapsed walls)
  • Casualties (due to collapsed walls)
Tiberias
  • VIII+
  • VIII+
  • Destruction (collapsed walls)
  • Casualties (due to collapsed walls)
  • Altered spring behavior
Tiberias
  • "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." - Article by William Mclure Thomson in the Missionary Herald (1837:436-437)
  • VIII+
  • VIII+
  • VIII+
  • Fractured Walls
  • Ruins (collapsed walls)
  • Altered Spring behavior
  • Casualties (due to callpased walls)
Tiberias
  • "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." - William Mclure Thomson in The Land and the Book (1861:278-279)
  • VI+
  • VIII+
  • VIII+
  • VIII+
  • Destruction (collapsed walls)
Tiberias
  • VIII+
  • walls cast down to the ground
  • tower damage (displaced walls)
  • galleries and chambers laid open (collapsed walls)
Tiberias
  • "We did not enter Tiberias, but pitched on the banks of the lake; the earthquake had left the town in ruins, its walls cast down to the ground, its towers split in two, and their galleries and chambers laid open and yawning in mid-air." - Lindsay (1838 v.2:87)
  • VIII+
  • VII+
  • VIII+
The archeoseismic evidence requires a minimum Intensity of VIII (8).

Site Effect
Zaslavsky et al. (2009a) - Site Effect and Seismic Hazard Microzonation across the town of Tiberias

Notes from Zaslavsky et al. (2009a)

Abstract

To quantify the seismic hazard across the town of Tiberias we used a methodology in which horizontal-to-vertical spectral ratio from microtremor (the Nakamura’s technique) obtained on a dense measurement grid is utilized to assess the site-specific uniform acceleration spectra. This process of hazard assessment involves: a detailed mapping of the fundamental and other natural frequencies and amplitudes of H/V spectral ratios; compiling geological, geophysical and borehole data and integrating it with H/V observations to develop models of the subsurface at many sites across the study area. The subsurface model serves as an input for computing the expected Uniform Hazard Site-Specific Acceleration Response Spectra at the investigated sites. The final stage is generalizing the hazard by mapping zones that feature similar seismic hazard functions.

Microtremor measurements were carried out at 175 sites, which are characterized by amplification from 2 up to 8 in the frequency range 0.7-8 Hz. The receiver function, which is horizontal-to-vertical spectral ratio obtained from earthquakes (shear wave) confirms the results obtained from microtremor records at three acceleration locations.

H/V ratios, geological data and information from S-velocity refraction profiles enables construction of geological cross sections. Certain sharp differences in the H/V ratios have been interpreted as being associated with a subsurface discontinuity, i.e. fault.

By comparison of the Uniform Hazard Acceleration Spectra calculated for probability of exceedance of 10% during an exposure time of 50 years and a damping ratio of 5% at more the 50 sites and in consideration of the constructed subsurface models, we subjectively divided the study area into eleven zones. The linear spectra for eight zones significantly exceed the design spectra required in the same area by the current Israel Standard 413 (IS-413) in the period range 0.1-0.5 sec.

Methodology

In the present study we used a three-step process for evaluating site effects and estimating their influence on seismic ground motion (Zaslavsky et al., 2005). At the first step, we performed microtremor measurements on a dense spatial grid and H/V spectral ratios, from which we obtained a spatial distribution of the frequencies at which amplification is likely to occur and the expected level of amplification at those frequencies. H/V spectral ratios of S-waves, often known as receiver functions, generated by earthquakes and recorded at three accelerometer locations are considered in the analysis. At the second step, all available geological information, geophysical and well data are collected and incorporated as an aid to construct subsurface models for different sites within the investigated area. Finally, one-dimensional analytical models [JW: They used SHAKE] are used to predict site-specific acceleration response spectra from future earthquakes. The application of this methodology makes possible reliable assessment of disaster from different earthquakes, especially in the regions where big earthquakes present a long return period, but which exhibit a high seismic risk according to historical reports, population distribution and its socio-economic importance.

Geology

With the exception of the Upper Cretaceous rocks exposed in the structural highs of Poriya and Fuliya blocks, all the formations on the geological map are part of the Neogene. From bottom to top these are: the Miocene Hordos Fm. and the Lower Basalt; the Neogene Bira Fm., Gesher Fm. and the Cover Basalt. The investigated area is dissected by two normal fault systems: the WSW-ENE transversal system with the down throw to the north, and the SE-NW system of step-faults with the down throw to the northeast. The two transversal faults in the south are of a Neogene pre-Cover basalt age. They were rejuvenated in the Pleistocene. The NW trending step faults are of Pleistocene post-Cover Basalt age. Along the greater part of their traces they bring basalt against basalt. Only at the southeastern termination of two of them, where they abut against a transversal fault, Neogene sediments rise to the surface. Here the throw of the two step faults is the greatest. A fourth step-fault is inferred within the lake and parallel to its shore. A significant feature is the considerable vertical displacement at the NE corner of the titled block, a result of the cumulative effect of the two fault systems. In the Upper Pliocene, the site of the town and its lakeshore were structurally higher than Tel Maon in the west (Schulman, 1966). Schulman (1966) proposed Ron et al. (1984) supported that the middle to upper Miocene sediments and basalts underwent intensive deformation by horizontal shear in a compressive stress field which operated during the end of the Miocene and early Pliocene times.

Brief Review of Several Experimental Methods for Site Effect Assessment

S-Wave spectral ratio with respect to reference site

The most common technique for estimating site response is the standard (classic) spectral ratio procedure first introduced by Borcherdt (1970). This approach considers the ratio between the Fourier spectra of a seismogram recorded in the site of interest and the spectrum of a seismogram recorded at a reference site, which is usually the rock outcrop. This ratio can be considered as the transfer function between the bedrock and the surface assuming that the two recordings correspond to the same source, the same path effect and that the reference site has a negligible site effect. It is very difficult to implement all these assumptions in real conditions. First, in many cases we do not have a nearby bedrock site and therefore the condition that the path of the propagating seismic waves is the same is not fulfilled; second, it is known (e.g., Steidl et al., 1996, Zaslavsky et al., 2002) that weathered and cracked bedrock site exhibits a significant site effect, associated with frequency-selective ground motion amplification; third, there are many cases in Israel, when nearby bedrock outcrop is not the same rock at the base of the soil layer which is responsible for amplifying seismic waves amplitudes. It should also be noted that performing simultaneous measurements at two sites is often relatively costly. Nevertheless, when all the conditions are observed, this method maybe considered the most reliable estimate of the empirical transfer function of site. Many investigators used this method and evaluated site response functions from moderate to weak motion recording of earthquakes (Tucker and King, 1984; McGarr et al., 1991; Field et al., 1992; Liu et al., 1992; Carver and Hartzell, 1996; Hartzell et al., 1996; Steidl et al., 1996; Zaslavsky et al., 2000 and others).

Horizontal-to-vertical S-wave spectral ratio (Receiver Function)

In this technique applied by Lermo and Chávez-García (1993) the receiver function can be obtained from ratio between horizontal and vertical amplitude spectra computed at the same investigated site from S-waves, respectively. Receiver function was introduced by Langston (1979) to determine the velocity structure of the crust and upper mantle from P-waves of teleseisms. Langston made the assumption that the vertical component of motion is not influenced by the local structure, whereas the horizontal components, owing to the geological layering, contain the P to S conversion. In the spectral domain this corresponds to a simple division of the horizontal spectrum by the vertical. Many studies report that the frequency dependence of site response can thus be obtained from measurements made at only one station at the analysed site (Lermo and Chavez-Garcia 1994; Malagnini et al., 1996; Seekins, et al., 1996; Theodulidis et al., 1996; Castro et al. 1997; Yamazaki and Ansary, 1997; and others). Their results confirm the validity of the method to estimate S-wave site response. We obtained similar conclusion in our investigations (Zaslavsky et al., 2000). Nevertheless, the implementation of this approach still requires a rather frequent occurrence of earthquakes. This requirement becomes an obstacle in regions of low seismicity.

Microtremor spectral ratio with respect to reference site

Kagami et al. (1982) proposed that the ratio of the spectra of the horizontal ground motions of the microtremor at the investigated site to those of a reference site can be used as a measure of the site response function. This method can be successfully applied for long period microtremors with period ranging from 1.0 to 10 sec. When higher frequencies are of interest, the distance between the measured sites should not exceed few hundred meters. The reliability of this method depends on whether or not the simultaneously measured motions at each site are from the same source and propagation path. This technique is widely used for site response estimates (Lermo et al., 1988; Field et al., 1990, 1995; Rovelli et al., 1991; Dravinski et al., 1995, 2003; Gaull et al., 1995). However, experimental study of site effect by sediment-to-bedrock spectral ratio in urban and suburban regions can be successful only under particular circumstances, because microtremor would be influenced by local artificial sources generated by human activities which essentially change from place to place.

Horizontal-to-vertical microtremor spectral ratio

Nakamura (1989) proposed the hypothesis that site response function under low strain can be determined as the spectral ratio of the horizontal versus the vertical component (H/V) of motion observed at the same site. He hypothesized that the vertical component of microtremor is relatively unaffected by the unconsolidated near-surface layers. Hence, the site response is the spectral ratio between the horizontal component of microseisms and vertical component of microseisms recorded at the same location.

Many authors, among them Lermo and Chávez-García (1994), Seekins et al. (1996), Toshinawa et al. (1997), Chávez-García and Cuenca (1998), Enomoto et al. (2000), Shapira et al. (2001), Mucciarelli and Gallipoli (2004), Murphy and Eaton (2005), Maresca, (2006), show that the H/V spectral ratio technique can be a useful tool for the assessment of ground motion characteristics on soft sediments. However, other authors (for example, Bonilla et al., 1997; Horike et al., 2001; Satoh et al., 2001) conclude that whereas the predominant peak of H/V ratio is well correlated with the fundamental resonance frequency, the amplitude of this peak is not necessarily the amplification level as obtained from sediment-to-bedrock spectral ratio of earthquake records.

Conclusions

In the town of Tiberias, H/V measurements performed on urban noise have been used to quantify soil responses for evaluation of the site specific seismic hazard. Our conclusions may be summarized as follows:
  • The stability and reproducibility of measurements are confirmed by data from continuous measurements during several months as well as repeated measurements in different months and years which yield almost identical shapes of average spectral ratios obtained at the same site under the same conditions of measurements.

  • Comparison between the average H/V spectral ratios obtained from accelerograms of horizontal components and from microtremor recorded at the same site shows that an appropriate ensemble of carefully selected windows of microtremor provides estimations of site response which are similar to those obtained from seismic events.

  • Experimental estimation of the site response over Tiberias yields variation in the fundamental frequency in the range 0.7-7 Hz and H/V amplitude from 2 up to 8. Maps of the spatial distribution of the fundamental frequency and their associated H/V amplitude delineate potentially vulnerable sites. This information is useful for land use considerations in urban planning and for identifying sites which require in depth site investigations to better evaluate the seismic hazard.

  • Limited data on S-wave velocities and sediment thickness of the upper layers obtained from seismic refraction surveys used to calibrate the H/V spectral ratio with an analytical site response derived from a 1D subsurface model. It is also used to justify further H/V ratios utilization, by velocities extrapolation, to study other sites, away from refraction profiles and boreholes. A stochastic optimization algorithm is applied to calculate the layer thickness, yielding transfer functions to match in the best way the observed H/V curves, considering all resonance peaks. Two cross-sections in Tiberias illustrate the results of H/V analysis.

  • The microtremor measurements enable identifying discontinuity in the subsurface and locate faults. These are associated with significant change in fundamental frequency, amplitude and shape corresponding to both vertical displacement and change in the velocity profile. Some, but not all faults detected by H/V analysis are identified also by geological data.

  • Analytical models cross-checked with observed data were extrapolated over the study area and integrated into computations of the uniform site specific acceleration response spectra for a probability of exceedence of 10% during exposure time of 50 years and damping of 5%. The sites with common site effect characteristics were united into zones. In eight out of eleven selected zones the current Building Code IS-413 significantly underestimates the acceleration in the period range 0.1-0.6 sec.

  • Since 2000 when strong motion stations were installed in the Tiberias area, two local earthquakes that occurred in 2004 were recorded. Taking into account the complicated geology of the region, we strongly recommend deploying seismic stations for continuous recording weak earthquakes to validate and improve the subsurface models derived from microtremor analysis and contribute to seismic hazard assessment.

  • We should emphasize that calculated analytical transfer functions are associated with weak motions and linear behavior of soils. Non-linear characteristics of site in Tiberias are beyond the scope of this study. Nevertheless, based on the result presented above nonlinear site response can be determined by different mathematical models of soil nonlinearity, making use of the models developed for each zone. In that respect, the microzonation maps developed in this study are also relevant for the prediction of ground motions from earthquakes of high magnitudes.

Location Map

Figure 3

Location of the measurement sites in the study area. Numbers indicate the sites used as examples. TB-1, TB-2 and TB-3 - refraction survey profiles (Ezersky, 2008); R-1 and R-2 – refraction survey profiles (Schtivelman, 1995); TVR, TVR2 and POR – accelerometer locations; Profile1 and Profile2 – profiles for reconstructing subsurface structure.

Zaslavsky et al. (2009a)


Distribution of the fundamental resonance frequency

Figure 15

Distribution of the fundamental resonance frequency over Tiberias.

Zaslavsky et al. (2009a)


Distribution of amplitude associated with the fundamental frequency

Figure 16

Distribution of amplitude associated with the fundamental frequency

Zaslavsky et al. (2009a)


Well Descriptions

Table 2

Brief description of wells located in the Tiberias region

Zaslavsky et al. (2009a)


Geophysical and analytical models at points located along TB-3 refraction profile

Table 4

Geophysical and analytical models for calculating transfer functions at points located along TB-3 refraction profile

Zaslavsky et al. (2009a)


Geophysical and analytical models at points located along TB-1 refraction profile

Table 5

Geophysical and analytical models for calculating transfer function at sites located along refraction profile TB-1.

Zaslavsky et al. (2009a)


Geotechnical data obtained from refraction surveys

Table 6

Geotechnical data obtained from refraction surveys carried out in 1995 and 2008.

Zaslavsky et al. (2009a)


Soil-column model for sites along refraction profile TB2

Table 7

Soil-column model for sites along refraction profile TB2

Zaslavsky et al. (2009a)


Ranges of S-wave velocities for litho-stratigraphycal units

Table 10

Ranges of S-wave velocities for litho-stratigraphycal units represented in the study area and used in calculating site response.

Zaslavsky et al. (2009a)


Schematic geological NS cross section beneath profile 1

Figure 23

Schematic geological NS cross section beneath profile 1

Zaslavsky et al. (2009a)


Schematic geological EW cross section along profile 2

Figure 25

Schematic geological EW cross section along profile 2

Zaslavsky et al. (2009a)


Seismic microzoning map of Tiberias presenting zones of common site effect characteristics

Figure 27

Seismic microzoning map of Tiberias presenting zones of common site effect characteristics.

Zaslavsky et al. (2009a)


Table 11 - Soil column models for representative sites of zones, their transfer functions and spectral accelerations.

Charts, Plots, Maps, Images, etc.
Charts, Plots, Maps, Images, etc.

Maps, Images, Tables, etc. from Zohar (2017)

Normal Size

Image Figure Description Source
Figure 1a Damage Distribution from the 1837 CE Safed Quake Zohar (2017)
Figure 1b Satellite View of the Old City of Tiberias Zohar (2017)
Figure 2a al-Zaydani Mosque in Tiberias Zohar (2017)
Figure 2b the Citadel in Tiberias
where 1837 earthquake damage is apparent
Zohar (2017)
Figure 2c al-Bahri Mosque in Tiberias Zohar (2017)
Figure 2d remains of the massive vaults
in southern Tiberias
(noted by red arrow)
Zohar (2017)
Figure 2e Etz-Hay’im Synagogue in Tiberias Zohar (2017)
Figure 2f one of the southern damaged
turrets in Tiberias’s walls
where 1837 earthquake damage is apparent
Zohar (2017)
Figure 3 Visual sources used for reconstructing the landscape Zohar (2017)
Figure 5 Feature Detection Zohar (2017)
Table 1 Damage Table Zohar (2017)
Table 2 Damage in the Quarters Zohar (2017)
Figure 6 Tiberias before the 1837 CE Safed Quake Zohar (2017)
Figure 7 3D reconstruction of Tiberias before
and after the 1837 CE Safed Quake
Zohar (2017)
Figure 8 Map of damage in Tiberias due to 1837 CE Safed Quake Zohar (2017)

Magnified

Image Figure Description Source
Figure 1a Damage Distribution from the 1837 CE Safed Quake Zohar (2017)
Figure 1b Satellite View of the Old City of Tiberias Zohar (2017)
Figure 2a al-Zaydani Mosque in Tiberias Zohar (2017)
Figure 2b the Citadel in Tiberias
where 1837 earthquake damage is apparent
Zohar (2017)
Figure 2c al-Bahri Mosque in Tiberias Zohar (2017)
Figure 2d remains of the massive vaults
in southern Tiberias
(noted by red arrow)
Zohar (2017)
Figure 2e Etz-Hay’im Synagogue in Tiberias Zohar (2017)
Figure 2f one of the southern damaged turrets in Tiberias’s walls where 1837 earthquake
damage is apparent
Zohar (2017)
Figure 3 Visual sources used for reconstructing the landscape Zohar (2017)
Figure 5 Feature Detection Zohar (2017)
Table 1 Damage Table Zohar (2017)
Table 2 Damage in the Quarters Zohar (2017)
Figure 6 Tiberias before the 1837 CE Safed Quake Zohar (2017)
Figure 7 3D reconstruction of Tiberias before
and after the 1837 CE Safed Quake
Zohar (2017)
Figure 8 Map of damage in Tiberias due to 1837 CE Safed Quake Zohar (2017)

Old Drawings, Maps, and Photos from Zohar (2017) Supplemental

Normal Size

Image Figure Description Source
Figure 1 Painting of Tiberias in 1681 CE Zohar (2017)
Figure 2 Map of Tiberias in 1799 CE Zohar (2017)
Figure 3 Map of Tiberias in 1810-1812 CE Zohar (2017)
Figure 4 al-Zaydani Mosque in 1814 CE
compared to ~2016 CE
Zohar (2017)
Figure 5 Painting of Tiberias in 1816 CE Zohar (2017)
Figure 6 Painting of Tiberias in 1822 CE Zohar (2017)
Figure 7 Painting of Tiberias in 1828 CE
compared to ~2016 CE
Zohar (2017)
Figure 8 Painting of Tiberias in 1828 CE
compared to ~2016 CE
Zohar (2017)
Figure 9 Painting of Tiberias in 1832 CE Zohar (2017)
Figure 10 Painting of Tiberias in 1833 CE Zohar (2017)
Figure 11 Painting of Tiberias in 1835 CE Zohar (2017)
Figure 12 Painting of Tiberias
Prior to 1837 CE (1835?)
Zohar (2017)
Figure 13 Painting of Tiberias Prior to 1837 CE Zohar (2017)
Figure 14 Painting of Tiberias Prior to 1837 CE Zohar (2017)
Figure 15 Painting of Tiberias Prior to 1837 CE Zohar (2017)
Figure 16 Painting of Tiberias in 1837 CE
after the earthquake
compared to ~2016 CE
Zohar (2017)
Figure 17 Painting of Tiberias before 1837 CE Zohar (2017)
Figure 18 Painting of Tiberias in 1837 CE
compared to ~2016 CE
Zohar (2017)
Figure 19 Painting of Tiberias in 1839 CE Zohar (2017)
Figure 20 Painting of Tiberias in 1839 CE Zohar (2017)
Figure 21 Painting of Tiberias in 1839 CE Zohar (2017)
Figure 22 Painting of Tiberias in 1839 CE Zohar (2017)
Figure 23 Painting of Tiberias in 1840 CE Zohar (2017)
Figure 24 Painting of Tiberias in 1841 CE Zohar (2017)
Figure 25 Painting of Tiberias in 1841 CE Zohar (2017)
Figure 26 Painting of Tiberias in 1842 CE
compared to ~2016 CE
Zohar (2017)
Figure 27 Painting of Tiberias in 1842 CE Zohar (2017)
Figure 28 Painting of Tiberias in 1842 CE Zohar (2017)
Figure 29 Painting of Tiberias in 1842 CE Zohar (2017)
Figure 30 Sketch of Tiberias in 1842 CE Zohar (2017)
Figure 31 Painting of Tiberias in 1842 CE Zohar (2017)
Figure 32 Drawing of Tiberias in 1848 CE
compared to ~2016 CE
Zohar (2017)
Figure 33 Painting of Tiberias in 1849 CE Zohar (2017)
Figure 34 Painting of Tiberias in 1851 CE Zohar (2017)
Figure 35 Painting of Tiberias in 1851-52 CE Zohar (2017)
Figure 36 Map of the region in 1856 (?) CE Zohar (2017)
Figure 37 Painting of Tiberias in 1860 CE Zohar (2017)
Figure 38 Drawing of Tiberias in 1863 CE
compared to ~2016 CE
Zohar (2017)
Figure 39 Photo of Tiberias c.1870 CE Zohar (2017)
Figure 40 Map of the Sea of Galilee
and Tiberias in 1681 CE
Zohar (2017)
Figure 41 Map of Tiberias and vicinity 1880 CE Zohar (2017)
Figure 42 Plan of Tiberias in 1885 (?) Zohar (2017)
Figure 43 Aerial Photo of of Tiberias 1900-1920 CE Zohar (2017)
Figure 44 Photo of Tiberias between 1898 and 1914 CE Zohar (2017)
Figure 45 Photo of Tiberias between 1898 and 1914 CE Zohar (2017)
Figure 46 Photo of Tiberias between 1898 and 1946 CE Zohar (2017)
Figure 47 Photo of Tiberias between 1898 and 1946 CE Zohar (2017)
Figure 48 Aerial Photo of Tiberias 1931 CE Zohar (2017)
Figure 49 Aerial Photo of Tiberias 1931 CE Zohar (2017)
Figure 50 Map of Tiberias in 1938 CE Zohar (2017)

Magnified

Image Figure Description Source
Figure 1 Painting of Tiberias in 1681 CE Zohar (2017)
Figure 2 Map of Tiberias in 1799 CE Zohar (2017)
Figure 3 Map of Tiberias in 1810-1812 CE Zohar (2017)
Figure 4 al-Zaydani Mosque in 1814 CE compared to ~2016 CE Zohar (2017)
Figure 5 Painting of Tiberias in 1816 CE Zohar (2017)
Figure 6 Painting of Tiberias in 1822 CE Zohar (2017)
Figure 7 Painting of Tiberias in 1828 CE
compared to ~2016 CE
Zohar (2017)
Figure 8 Painting of Tiberias in 1828 CE
compared to ~2016 CE
Zohar (2017)
Figure 9 Painting of Tiberias in 1832 CE Zohar (2017)
Figure 10 Painting of Tiberias in 1833 CE Zohar (2017)
Figure 11 Painting of Tiberias in 1835 CE Zohar (2017)
Figure 12 Painting of Tiberias
Prior to 1837 CE (1835?)
Zohar (2017)
Figure 13 Painting of Tiberias Prior to 1837 CE Zohar (2017)
Figure 14 Painting of Tiberias Prior to 1837 CE Zohar (2017)
Figure 15 Painting of Tiberias Prior to 1837 CE Zohar (2017)
Figure 16 Painting of Tiberias in 1837 CE
after the earthquake
compared to ~2016 CE
Zohar (2017)
Figure 17 Painting of Tiberias before 1837 CE Zohar (2017)
Figure 18 Painting of Tiberias in 1837 CE
compared to ~2016 CE
Zohar (2017)
Figure 19 Painting of Tiberias in 1839 CE Zohar (2017)
Figure 20 Painting of Tiberias in 1839 CE Zohar (2017)
Figure 21 Painting of Tiberias in 1839 CE Zohar (2017)
Figure 22 Painting of Tiberias in 1839 CE Zohar (2017)
Figure 23 Painting of Tiberias in 1840 CE Zohar (2017)
Figure 24 Painting of Tiberias in 1841 CE Zohar (2017)
Figure 25 Painting of Tiberias in 1841 CE Zohar (2017)
Figure 26 Painting of Tiberias in 1842 CE
compared to ~2016 CE
Zohar (2017)
Figure 27 Painting of Tiberias in 1842 CE Zohar (2017)
Figure 28 Painting of Tiberias in 1842 CE Zohar (2017)
Figure 29 Painting of Tiberias in 1842 CE Zohar (2017)
Figure 30 Sketch of Tiberias in 1842 CE Zohar (2017)
Figure 31 Painting of Tiberias in 1842 CE Zohar (2017)
Figure 32 Drawing of Tiberias in 1848 CE
compared to ~2016 CE
Zohar (2017)
Figure 33 Painting of Tiberias in 1849 CE Zohar (2017)
Figure 34 Painting of Tiberias in 1851 CE Zohar (2017)
Figure 35 Painting of Tiberias in 1851-52 CE Zohar (2017)
Figure 36 Map of the region in 1856 (?) CE Zohar (2017)
Figure 37 Painting of Tiberias in 1860 CE Zohar (2017)
Figure 38 Drawing of Tiberias in 1863 CE
compared to ~2016 CE
Zohar (2017)
Figure 39 Photo of Tiberias c.1870 CE Zohar (2017)
Figure 40 Map of the Sea of Galilee
and Tiberias in 1681 CE
Zohar (2017)
Figure 41 Map of Tiberias and vicinity 1880 CE Zohar (2017)
Figure 42 Plan of Tiberias in 1885 (?) Zohar (2017)
Figure 43 Aerial Photo of of Tiberias 1900-1920 CE Zohar (2017)
Figure 44 Photo of Tiberias between 1898 and 1914 CE Zohar (2017)
Figure 45 Photo of Tiberias between 1898 and 1914 CE Zohar (2017)
Figure 46 Photo of Tiberias between 1898 and 1946 CE Zohar (2017)
Figure 47 Photo of Tiberias between 1898 and 1946 CE Zohar (2017)
Figure 48 Aerial Photo of Tiberias 1931 CE Zohar (2017)
Figure 49 Aerial Photo of Tiberias 1931 CE Zohar (2017)
Figure 50 Map of Tiberias in 1938 CE Zohar (2017)

Notes and Further Reading
References

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Ambraseys, N. N., & Barazangi, M. (1989). The 1759 earthquake in the Bekaa Valley: Implications for earthquake hazard assessment in the eastern Mediterranean region. Journal of Geophysical Research: Solid Earth, 94(B4), 4007–4013.

Ambraseys, N. N., & Karcz, I. (1992). The earthquake of 1546 in the Holy Land. Terra Nova, 4(2), 254–263.

Avi-Yonah, M. (1951). Historical geography of Eretz Israel. Bialik Institute.

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

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

Ben-Arieh, Y. (2001). The view of Eretz Israel as reflected in biblical painting of the nineteenth century. In R. Aharonson & H. Lavsky (Eds.), A land reflected in its past (pp. 255–279). Magnes Press & Yad Izhak Ben-Zvi Press.

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Ben-Zvi, I. (1954). Eretz-Israel under Ottoman rule. Bialik Institute.

Bender, O., et al. (2005). Using GIS to analyse long-term cultural landscape change in southern Germany. Landscape and Urban Planning, 70(1–2), 111–125.

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

Burckhardt, L. J. (1822). Travels in Syria and the Holy Land. J. Murray.

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

Carne, J. (1826). Letters from the East. H. Colburn.

Clarke, E. D. (1810–1823). Travels in various countries of Europe, Asia and Africa. T. Cadell & W. Davies.

Davie, F. M., & Frumin, M. (2007). Late eighteenth-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. H. Colburn.

de Thévenot, J. (1971). The travels of Monsieur de Thévenot into the Levant. Gregg.

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

Gregory, I. N., & Ell, P. S. (2007). Historical GIS: Technologies, methodologies, and scholarship. Cambridge University Press.

Guerin, V. (1880). Description géographique, historique et archéologique de la Palestine. L’Imprimerie nationale.

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Bibliography from Stern et al (1993 v.4)

M. Avi-Yonah, IEJ I (1950-1951), 160-169

D. Ussishkin, ibid. 18 (1968), 45-46

B. Lifshitz, Euphrosyne n.s. 6 (1973-1974), 23-27

G. Foerster, RB 82 (1975), 105-109

id., Recherches Archeologiques en Israel 206-209

E. Ballhorn, Israel-Land and Nature 1 (1976), 151-153

A. Bruno\, BTS 192 (1977), 10-20

L. I. Levine, HUCA 49 (1978), 143-185

M. Ben-Dov, ASR, 157-159

N. Feig, ES/1 (1982), 110; S. Dar, ibid. 2 (1983), 103

id., IEJ33 (1983), 114-115

A. Harif, PEQ 116(1984), 103-109

J-F. Desclaux, MdB 38 (1985), 45-47

G. Theissen, ZDPV 101 (1985), 43-55

S. Qedar, Israel Numismatic Journa/9 (1986-1987), 29-33

H. Dudman and E. Ballhorn, Tiberias, Jerusalem 1988

D. Stacey, BAlAS 8 (1988- 1989), 21-33

A. Cohen, ES/9 (1989-1990), 171

Y. Hirschfeld, ibid., 107-109

id., BAR 17/2 (1991), 44- 51

id., MdB 72 (1991), 21-23

BA 54 (1991), 170-171.

Bibliography from Stern et al (2008)

Main publications

Y. Hirschfeld, A Guide to the Antiquity Sites in Tiberias, rev. ed., Jerusalem 1992

ibid. (Review) PEQ 130 (1998), 79

id. (et al.), Excavations at Tiberias, 1989–1994 (IAA Reports 22), Jerusalem 2004

id., Roman, Byzantine, and Early Muslim Tiberias: A Handbook of Primary Sources, Tiberias 2005; D. A. Stacey, The Archaeology of Early Islamic Tiberias (Ph.D. diss.), London 1995

id., Excavations at Tiberias, 1973–1974: The Early Islamic Periods (IAA Reports 21), Jerusalem 2004

ibid. (Review) PEQ 137 (2005), 182–183

Y. Stepansky, Map of Tiberias (39) (Archaeological Survey of Israel), Jerusalem (in prep.).

Studies

Y. Hirschfeld, ESI 10 (1991), 91–93

16 (1997), 35–42

id., OEANE, 5, New York 1997, 203–206; id., RB 106 (1999), 236–249

[id.], Artifax 19/2 (2004), 6

G. Labee, Revue des Études Anciennes 93 (1991), 277–297

A. Lester, Jewellery and Goldsmithing in the Islamic World: International Symposium, The Israel Museum, 1987 (Israel Museum, Catalogue 320

ed. N. Brosh), Jerusalem 1991, 21–29

A. Onn, ESI 10 (1991), 10

id., ibid. (1992), 166–167

Y. Stepansky, ESI 9 (1991), 79 (with E. Damati)

id., ibid., 70–80 (with Z. Ilan)

E. J. Simpson et al., ibid., 4

V. Bernie et al., Levant 24 (1992), 95–129

T. P. Harrison, JNES 51 (1992), 51–59

Z. Razi & E. L. Braun, The Horns of Hattin: Proceedings of the 2nd Conference of the Society for the Study of the Crusades and the Latin East, Jerusalem and Haifa, 2–6.7.1987 (ed. B. Z. Kedar), Jerusalem 1992, 216–227

J. F. Strange, ABD, 6, New York 1992, 547–549

N. Feig, LA 44 (1994), 591–594

M. L. Fischer, Mediterranean Language Review 8 (1994), 20–40

R. A. Horsley, Galilee: History, Politics, People, Valley Forge, PA 1995

id., Archaeology, History and Society in Galilee: The Social Context of Jesus and the Rabbis, Valley Forge, PA 1996

E. Damati, ESI 16 (1997), 138–139 (with Y. Stepansky)

‘Atiqot 35 (1998), 152–153

ibid., 38 (1999), 227–228

N. Brosh, ibid. 36 (1998), 1–9

L. Di Segni, Heraica: miscellanea di studi (S. J. Sierra Fest.

eds. F. Israel et al.), Torino 1998, 115–163

D. Pringle, The Churches of the Crusader Kingdom of Jerusalem: A Corpus, 2, Cambridge 1998, 351–366; B. -Z. Rosenfeld, HUCA 69 (1998), 57

Y. Alexandre, ‘Atiqot 37 (1999), 171*

H. Ben Nahum, ESI 109 (1999), 15*–16*

Y. Stepansky, ibid. 19 (1999), 226–227

20 (2000), 19*–20*

id., JSRS 9 (2000), xvii–xviii; id., Crusades 3 (2004), 179–181

Z. Weiss, Religious and Ethnic Communities in Later Roman Palestine (Studies and Texts in Jewish History and Culture 5

ed. H. Lapin), Bethesda, MD 1998, 219–246

B. Bagatti, Ancient Christian Villages of Galilee (SBF Collectio Minor 37), Jerusalem 2001, 47–56

S. S. Miller Historia (Stuttgart) 50 (2001), 453–467

E. M. Smallwood, The Jews Under Roman Rule from Pompey to Diocletian: A Study in Political Relations, Boston 2001 (index)

T. Weber, SHAJ 7 (2001), 531–537

MdB 147 (2002), 57

M. Rosen-Ayalon, Art et archéologie islamiques en Palestine, Paris 2002, 84–89, 152–153; Z. S. Winogradov, The Aqueducts of Israel, Portsmouth, RI 2002, 295–304

C. MacEvitt, Albright News 8 (2003), 15–16

id., ASOR Newsletter 53/3 (2003), 15–16

S. Fortner, Leben am See Gennesaret, Mainz am Rhein 2003, 86–92

BAR 30/4 (2004), 12

E. Dvorjetski, ibid., 16–27, 60

Y. Elitzur, Ancient Place Names in the Holy Land: Preservation and History, Jerusalem 2004, 64–71

N. Hazan et al., Israel Journal of Earth Sciences 53 (2004), 199–205

G. Mazor, Free Standing City Gates in the Eastern Provinces during the Roman Imperial Period (Ph.D. diss.), Ramat-Gan 2004 (Eng. abstract)

J. Sudilovsky (& Y. Stepansky), BAR 30/3 (2004), 16–17

J. Zangenberg, Jahrbuch des Deutschen Evangelischen Instituts für Altertumswissenschaft des Heiligen Landes 10 (2004), 195

Artifax 20/4 (2005), 6–7

P. Gruson, MdB Hors Série 2005, 25

L. I. Levine, The Ancient Synagogue: The First Thousand Years, 2nd ed., New Haven, CT 2005, 52–54; A. Lewin, The Archaeology of Ancient Judea and Palestine, Los Angeles, CA 2005, 74–79

K. Van Eickels, Saladin und die Kreuzfahrer (Publikationen der Reiss-Engelhorn-Museen 17

Schriftenreihe des Landesmuseums für Natur und Mensch, Oldenburg, 37

eds. A. Wieczorek et al.), Mainz am Rhein 2005, 304–312.

The Coins

E. Janis, The Shekel 24/3 (1991), 18–21

P. Soucek, The Glory of Byzantium: Art and Culture of the Middle Byzantine Era, A.D. 843–1261 (eds. H. C. Evnas & W. D. Wixom), New York 1997, 403–433

D. J. Wasserstein, ESI 36 (1998), 15–22

G. Bijovsky, International Numismatic Newsletter 34 (1999), 3

A. Kindler, Bethsaida: A City by the North Shore of the Sea of Galilee, 2 (Bethsaida Excavations Project Reports & Contextual Studies 2

eds. R. Arav & R. A. Freund), Kirksville, MO 1999, 245–268

R. Milstein & D. T. Ariel, Excavations at Tiberias, 1989–1994 (IAA Reports 22

ed. Y. Hirschfeld), Jerusalem 2004, 57–58.

Mount Berenice

Main publication

Y. Hirschfeld et al., Excavations at Tiberias, 1989–1994, II: The Excavations on Mount Berenice, 1990–1994 (IAA Reports 22), Jerusalem 2004, 73–232.

Studies

Y. Hirschfeld, MdB 72 (1991), 21–23

id., BA 57 (1994), 122–133

id., ESI 14 (1994), 33–37

16 (1997), 35–42 (with R. Ben-Arieh)

id., AJA 98 (1994), 512–513

id., Michmanim 8 (1995), 11*–12*

id., RB 106 (1999), 236–249

R. Ben-Arieh, BA 57 (1994), 134–137

id., ESI 14 (1994), 37–38

16 (1995), 41–42

R. Fishman-Duker, MdB 92 (1995), 38–39

M. Aviam, Galilee through the Centuries: Confluence and Cultures (Duke Judaic Studies Series 1

ed. E. M. Meyers), Winona Lake, IN 1999, 297

U. Dotterweich, Ungentarien mit Kuppelförmiger Mündung aus Knidos (Knidos Studien 1), Möhnesee 1999.

The “House of the Bronzes” and Associated Remains

BAR 25/1 (1999), 18

G. Bijovsky, International Numismatic Newsletter 34 (1999), 3

L. Shulman, The Digging Stick 16/3 (1999), 10–11

J. Sudilovsky, BAR 25/6 (1999), 14

W. Watzman, Archaeology 52/2 (1999), 34

Y. Hirschfeld & O. Gutfeld, ESI 112 (2000), 15*–17*

F. Mebarki, MdB 125 (2000), 64.

Wikipedia pages

Tiberias



Hammat Tiberias



Sanhedrin



Jerusalem Talmud