Transliterated Name | Language | Name |
---|---|---|
Umm el-Qanatir | Arabic | ام القناطر |
Umm el-Kanatir | Arabic | ام القناطر |
Ein Keshatot | Hebrew | |
Rehavam's Arches | ||
Kantur | ||
Qamtra |
Fairly extensive archeoseismic evidence is present at Umm el-Qanatir, a site that appears to have been largely abandoned in the middle of the 8th century CE. An old landslide scar is also present at the site. Wechsler et al (2008) used a 2D slope stability model with measured geotechnical properties of three soil units to infer a minimum PGA of 0.36 g to initiate the landslide. They also estimated a minimum moment Magnitude of 7.0 for the earthquake which is presumed to have caused the slide.
Umm el-Qanatir is built on a limestone ledge under the basalt escarpment of the Golan, near a northern tributary ofNahal Samakh (map reference 2195.2506). The Arabic name of the site means "Mother of the Arches," after a nymphaeum with two arches built over the spring to the south of the synagogue. The site was discovered by L. Oliphant in 1884 and surveyed by G. Schumacher in 1885. A limited excavation was conducted in 1905 by H. Kohl and C. Watzinger, who published a very accurate plan of the remains; however, their reconstruction of the building was faulty. In 1932, the site was surveyed by E. L. Sukenik and in 1980 by Z. Ma'oz.
The site was first surveyed by Sir Laurence Oliphant1 in 1884, when he visited the area together with a local sheikh and the German engineer Gottlieb Schumacher (Oliphant 1887: 267). Oliphant described the spring arches and the ruins of the large structure, which he identified as a synagogue. Schumacher also recorded his impressions (Schumacher 1888: 260–265), although he did not make any such identification.
1 A British author, traveler, diplomat and mystic, who sought to establish a Jewish state
in Palestine.
2 Surprisingly, Sukenik, who visited the site in person, relied on Kohl and Watzinger’s
erroneous measurements.
3 Maʿoz suggested that this was also the case in the synagogues of Zumimra and Kh.
Zavitan.
4 The excavation and reconstruction project is directed and implemented by Y. Dray
(Restoration of Ancient Technology Center, Binyamina). Archaeologists: I. Gonen
and C. Ben David. Scientific sponsorship: the Institute of Archaeology of Bar-Ilan
University and the Kinneret Institute for Galilean Archaeology. Funding: Golan
Regional Council and the Israel Government Tourist Corporation. Excavation team:
T. Kaʿatabi, N. Aharoni, C. Tal, S. Chamami, M. Golan and H. Kinsbursky. Pottery
reading: B. Johnson and M. Hartal. Conservation architect: G. Solar. Mapping:
Mabat 3D Technologies. Drawings and surveying: D. Porotsky and R. Mishayev.
Photography: Y. Dray and I. Gonen.
5 In November 2010 the site was selected as one of the heritage sites to be fostered by
the Landmarks Project, a special programme funded by the Prime Minister’s Office.
The site was also given a new Hebrew name ––ʿEin Qeshatot, meaning ‘Arches
Spring’.
the fill of room L1240 revealed an assemblage of complete pottery vessels, including an intact juglet and a cooking-pot lid on top of a jug inside a cooking bowl, within which another intact juglet was found. Since these vessels are described as being in the fill of the secondary structure (aka makeshift house), they would have presumably been buried during the first earthquake when the site was possibly abandoned. Those vessels
dated to the first half of the eighth century CE. Since none of the agricultural implements found in the collapsed house were dated, the 2nd earthquake can only be specified as striking after the mid 8th century CE.
Effect | Location | Image(s) | Description |
---|---|---|---|
Displaced masonry blocks | entrance pier and southern wall of the synagogue
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017) |
Fig. 4a
Horizontal shift of a large masonry basalt blocks at the synagogue wall Wechsler et al (2008)
Fig. 4b
Horizontal shift of a large masonry basalt blocks at the synagogue wall Wechsler et al (2008) |
|
Collapsed Walls | western wall (W1062) of the synagogue
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017) |
Fig. 4e
Westward collapse of the wall of the synagogue Wechsler et al (2008) |
|
Collapsed Walls | eastern wall (W1024) of the synagogue
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017) |
Fig. 3
The collapsed eastern wall (view to the south) Dray et al. (2017) |
|
Fallen columns | synagogue interior
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017) |
Fig. 4d
Aligned fallen columns Wechsler et al (2008)
Fig. 2
Collapsed elements on the synagogue floor and the column bases in situ (view to the north) Dray et al. (2017) |
|
Sheared Water Pool | Pool in Spring Complex
Fig. 2a
Aerial photo of study area. Wechsler et al (2008) |
Fig. 4f
A water pool, part of the spring complex, displaced left- laterally 95 cm. This water pool is displaced by the landslide and is used for the slope stability analysis Wechsler et al (2008) |
|
Landslide | downslope from the synagogue |
Fig. 2a
Aerial photo of study area. Wechsler et al (2008)
Fig. 2b
A northward look at the Umm-El-Qanatir site. Wechsler et al (2008) |
|
Re-used building elements | secondary structure (aka makeshift house) inside the synagogue along with other areas in the synagogue and outside the synagogue
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017)
Fig. 9
Secondary construction of rooms in the northern part of the synagogue (view to the south) Dray et al. (2017)
Fig. 5
The synagogue suffered two damaging events. The firs led to its abandonment, as evidenced by a makeshift house (marked with dashed line), which was built on the floor of the synagogue using many of its finely carved stones. The second event caused the destruction of this house and triggered the abandonment of the whole site, as evidenced by absence of post mid-8th century artifacts Wechsler et al (2008) |
|
Effect | Location | Image(s) | Description |
---|---|---|---|
Collapsed Walls | makeshift house inside synagogue
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017)
Fig. 5
The synagogue suffered two damaging events. The firs led to its abandonment, as evidenced by a makeshift house (marked with dashed line), which was built on the floor of the synagogue using many of its finely carved stones. The second event caused the destruction of this house and triggered the abandonment of the whole site, as evidenced by absence of post mid-8th century artifacts Wechsler et al (2008)
Fig. 9
Secondary construction of rooms in the northern part of the synagogue (view to the south) Dray et al. (2017) |
|
|
Collapsed Wall | Wall W1065 in the secondary structure
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017)
Fig. 9
Secondary construction of rooms in the northern part of the synagogue (view to the south) Dray et al. (2017)
Fig. 5
The synagogue suffered two damaging events. The firs led to its abandonment, as evidenced by a makeshift house (marked with dashed line), which was built on the floor of the synagogue using many of its finely carved stones. The second event caused the destruction of this house and triggered the abandonment of the whole site, as evidenced by absence of post mid-8th century artifacts Wechsler et al (2008) |
|
the existence of the year-round flowing spring (and several others in the vicinity) indicates a high water table, and the weather patterns (rainy winter with ~900 mm average annual rainfall) suggest that at times it can be as high as the topography.Thus, lower values of FS may represent realistic conditions for the slope. The commercial software Slope/W™ was used to perform the Static Analysis. Modeling indicated that slope stability was largely determined by the weakest layer (lowest Cohesion) - paleosoil KA-4.
Variable | Input | Units | Notes |
---|---|---|---|
unitless | Wechsler et al (2008) constrained FS from 2.05 to 3.23 | ||
degrees | Wechsler et al (2008) used a value of 20 | ||
cm. | Wechsler et al (2008) recommends a value of 5 or 10 | ||
km. | Distance to nearest earthquake producing fault | ||
Variable | Output (No Site Effect) |
Units | Notes |
g | minimum acceleration to induce slide | ||
unitless | Conversion from ac to I using Wald et al (1999) | ||
unitless | Attenuation relationship of Hough and Avni (2009) used to calculate Magnitude from I and R |
||
m/s | Calculated from eqn. 2 of Wechsler et al (2008) | ||
m/s | Calculated from eqn. 3.17 of (Kramer, 1996:87) | ||
unitless | calculated from eqn. 3 of
Wechsler et al (2008) which comes from Katz and Crouvi (2007) |
||
Variable | Input | Units | Notes |
unitless | Site Effect due to Topographic or Ridge Effect (set to 1 to assume no site effect) | ||
Variable | Output (Site Effect) |
Units | Notes |
unitless | Intensity with Topographic Effect removed | ||
unitless | Magnitude with Topographic Effect removed - using Hough and Avni (2009) | ||
unitless | Moment Magnitude with Topographic Effect removed MW from eqn. 3 of Wechsler et al (2008) which comes from Katz and Crouvi (2007) |
Effect | Location | Image(s) | Description | Intensity |
---|---|---|---|---|
Displaced masonry blocks | entrance pier and southern wall of the synagogue
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017) |
Fig. 4a
Horizontal shift of a large masonry basalt blocks at the synagogue wall Wechsler et al (2008)
Fig. 4b
Horizontal shift of a large masonry basalt blocks at the synagogue wall Wechsler et al (2008) |
|
VIII + |
Collapsed Walls | western wall (W1062) of the synagogue
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017) |
Fig. 4e
Westward collapse of the wall of the synagogue Wechsler et al (2008) |
|
VIII + |
Collapsed Walls | eastern wall (W1024) of the synagogue
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017) |
Fig. 3
The collapsed eastern wall (view to the south) Dray et al. (2017) |
|
VIII + |
Fallen and oriented columns | synagogue interior
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017) |
Fig. 4d
Aligned fallen columns Wechsler et al (2008)
Fig. 2
Collapsed elements on the synagogue floor and the column bases in situ (view to the north) Dray et al. (2017) |
|
V + |
Sheared Water Pool | Pool in Spring Complex
Fig. 2a
Aerial photo of study area. Wechsler et al (2008) |
Fig. 4f
A water pool, part of the spring complex, displaced left- laterally 95 cm. This water pool is displaced by the landslide and is used for the slope stability analysis Wechsler et al (2008) |
|
IV + |
Landslide | downslope from the synagogue |
Fig. 2a
Aerial photo of study area. Wechsler et al (2008)
Fig. 2b
A northward look at the Umm-El-Qanatir site. Wechsler et al (2008) |
|
IV + |
Effect | Location | Image(s) | Description | Intensity |
---|---|---|---|---|
Collapsed Walls | makeshift house inside synagogue
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017)
Fig. 5
The synagogue suffered two damaging events. The firs led to its abandonment, as evidenced by a makeshift house (marked with dashed line), which was built on the floor of the synagogue using many of its finely carved stones. The second event caused the destruction of this house and triggered the abandonment of the whole site, as evidenced by absence of post mid-8th century artifacts Wechsler et al (2008)
Fig. 9
Secondary construction of rooms in the northern part of the synagogue (view to the south) Dray et al. (2017) |
|
VIII + | |
Collapsed Wall | Wall W1065 in the secondary structure
Fig. 4
Schematic plan; last phase of the building shown in red Dray et al. (2017)
Fig. 9
Secondary construction of rooms in the northern part of the synagogue (view to the south) Dray et al. (2017)
Fig. 5
The synagogue suffered two damaging events. The firs led to its abandonment, as evidenced by a makeshift house (marked with dashed line), which was built on the floor of the synagogue using many of its finely carved stones. The second event caused the destruction of this house and triggered the abandonment of the whole site, as evidenced by absence of post mid-8th century artifacts Wechsler et al (2008) |
|
VIII + |
Wechsler et al (2008) noted that the Umm al-Qanatir site could be subject to an effect known as the topographic effect or ridge effect.
This is an effect where a resonance condition can develop when the wavelength of the seismic wave is equal to the length of the ridge or landform
resulting in seismic amplification. This is a complex frequency dependent and angle of incidence dependent phenomenon that cannot be expected for
all earthquakes and is thus fairly unpredictable for a specific historical earthquake. However since, as noted by
Wechsler et al (2008), Umm al-Qanatir sits atop a river gorge, it may be subject to such effects. Modeling this effect was deemed beyond the scope of the paper
but the authors noted that by making conservative choices about the Newmark Displacement and the Factor of Safety, we assume that
the topographic effect is indirectly partially compensated for.
Dray, Y., et al. (2017). "The Synagogue of Umm el-Qanatir Preliminary Report."
Israel Exploration Journal 67(2): 209-231.
Seismic Design for Nuclear Power Plants (1970:438-483)
Sukenik, E. L. (1935). The Ancient Synagogue of El-Hammeh, Hammath-by-Gadara, an Account of the Excavations Conducted on Behalf of the Hebrew University, Jerusalem, Rubin Mass.
Wechsler, N., et al. (2009). "Estimating location and size of historical earthquake by combining archaeology and geology in Umm-El-Qanatir, Dead Sea Transform." Natural Hazards 50(1): 27-43.
L. Oliphant, PEQ !7 (1885), 89-91
G. Schumacher, The Jaulan, London 1888,260-
265
Kohl-Watzinger, Synagogen, 59-70, 125-134
Goodenough, Jewish Symbols!, !99, 206-208
E. L.
Sukenik, The Ancient Synagogue ofel-Hammeh, 85-87
id., JPOS 15 (1935), 172-174
M. Avi-Yonah,
QDAP 14(1950), 57
Hiittenmeister-Reeg, AntikenSynagogen, 465--468
Z. Ilan, ES/6(1987-1988), 110;
Z. U. Ma'oz, BA 5! (1988), 116-128.
The Original definition of the Arias Intensity can be found in Seismic Design for Nuclear Power Plants (1970:438-483).