Geotechnical and geophysical investigation techniques in Ben Ezra Synagogue in Old Cairo area, Egypt
The Ben Ezra Synagogue or El-Geniza Synagogue or the Synagogue of the Levantines, is located in the Coptic section of Old Cairo area. It is considered the oldest Synagogue or Jewish temple found in Egypt represents cultural heritage of outstanding universal values. It suffers multiple environmental, geotechnical and earthquake hazards. The integrated geotechnical and geophysical investigation techniques were done to assess the level of seismic and other geo-environmental hazards and risk that Synagogue suffers from in present and future. This knowledge is required to protect the building against seismic events. The Synagogue suffers high risk in terms of seismic and environmental hazards. The main purposes of the present study are to: (1) Assess the level of seismic and other geo-environmental hazards at Ben Ezra Synagogue. (2) Understand the damage situation for the historic building caused by the recent earthquakes. (3) Offer technical support and advice on restoration and repairs for the damaged structure. (4) Build up knowledge and case studies towards the restoration and repairs, and to survey the damage state of the historic structure. However, Ben Ezra Synagogue is the oldest Jewish temple that was constructed with little or no seismic considerations that represent the largest risk to most communities. These significant historical buildings must be assessed their level of risk determined, and unacceptable risks reduced. This paper focuses on the issues associated with detailed procedures of risk and hazards assessment for retrofitting of architectural heritage. Many forms of evaluation and related procedures for assessment of seismic risk for historical buildings have been discussed. This study, suggest moderate level of earthquake activity at Ben Ezra Synagogue and this is in a good agreement with the fact that “Egypt is a part of the stable African Shield”, but the existence of old structure such as the Ben Ezra Synagogue may reduce the ability to resist any earthquake shaking. This pilot study is important with respect to the continuous efforts for preservation and restoration of the cultural heritage worldwide.
KeywordsArchitectural heritage Ben Ezra Synagogue Risk assessment Seismic hazards
data acquisition system
electrical and instrumentation
ground level (or elevation/(also [GE or GRE]))
rate of penetration
ground penetrating radar
Seismic analysis and planning is part of ongoing archaeological site management and conservation [1, 2, 3]. In the last few years there has been significant and detectable deterioration to some of the major monuments in old Cairo area, like Ben Ezra Synagogue or El-Geniza Synagogue or the Synagogue of the Levantines , calling for an even more intensive and thorough review of their problems and needs, due tone of the most potentially serious, sudden and unpredictable of threats, seismic activity and related earthquakes.
Seismic ground response characteristics, defined generally as “site effects”, are inevitably reflected in seismic code provisions. The selection of appropriate elastic response spectra according to soil categories and seismic intensity is the simplest way to account for site effects both for engineering projects and for a general-purpose microzonation study. Contemporary seismic codes (IBC 2000, UBC97, EC8) have largely accepted the significant role of site effects and attempt to incorporate their influence either by means of a constant amplification factor exclusively dependent on the soil class or including additional parameters like the shaking intensity, near field conditions, etc. Even though concerning site classification different approaches exist, the basic idea of the mean value of shear wave velocity over the last few decades of meters (30 m or other) is considered to be a sound parameter for site classification. However soil classification exclusively based in terms of VS, 30 assumption, is a rather simplified hypothesis, misleading in many cases, which can potentially lead to erroneous results, especially in cases of deep soil formations or abrupt stiffness change between the soil layer at − 30 m and the bedrock laying deeper [5, 6, 7, 8, 9, 10, 11].
The structural risk assessment of the architectural heritage includes the steps of acquiring knowledge of built conditions, site and building response characteristics, economic and technical analysis prior to selecting the optimum retrofit strategy [12, 13, 14]. The Ben Ezra Synagogue is situated in the Coptic district of Cairo city. There are two possible explanations for the Jewish sanctuary erected in this specific area. The first is related to a place of bull surges where the child Moses was found safe or this was the place where Moses prayed to God for exempting the Jews from their subjection in Egypt. The land for the synagogue was acquired in 882 AD by Abraham Ben Ezra of Jerusalem. The establishing date of the Ben Ezra Synagogue isn’t known, in spite of the fact that there is great proof from reports found in the geniza that it originates before 882 CE what’s more, is most likely pre-Islamic . In 882, the patriarch of the Coptic Orthodox Church of Alexandria sold a congregation and its grounds to a gathering of Jews, and some nineteenth century researchers had accepted this was the starting point of Ben Ezra. Present day researchers concur that the 882 land deal was to an adversary synagogue . In around 1012, Fatimid caliph Al-Hakim bi-Amr Allah requested the annihilation of all Jewish and Christian spots of love. The first Ben Ezra Synagogue was torn down, “its blocks and timber sold for scrap. The following caliph Ali az-Zahir permitted reproduction of Christian and Jewish establishments, and the synagogue was revamped in the 1025–1040 period .
The present study is an integrated geophysical work to determine the following points
Determing the possibility of near surface ground water and its expected depth,
Determining the soil shear strength in terms of shear wave velocity versus depth.
Determinig the amount of expected probabilistic seismic hazard in terms of expected peak ground accelerations for usually the return periods for monuments are 500–1000 years.
Determinig the soil and structure natural frequencies of vibrations.
Determing design response spectrum for Ben Ezra Synagogue, using the most maximum credible earthquake (MCE).
Methodology and work procedure
In order to meet the mentioned objectives and goals, the following work procedure was followed:
Reviewing available information, previous work and maps (topographic, geologic and seismicity data) related to the Ben Ezra Synagogue area and its surroundings.
Analyzing and interpreting the collected data of resistivity imaging, refraction microtremors test, soil resonance test, and ground penetrating radar (GPR) data.
A field visit was conducted to verify the interpretation and to gather detailed features, principally those that might affect the Ben Ezra Synagogue area.
Collecting historical seismicity in and around Ben Ezra Synagogue from the period 2200 BC to 1899 AD.
Collecting recent instrumental earthquake catalogue from the period 1899 AD to 2006 AD.
Performing regional seismic hazard analysis based on most recent hazard parameters available in Egypt such as, PGA attenuation formulas, seismic source regionalization, and recurrence relationships…, etc.
Finally based on the previous collected data the hazard at Ben Ezra Synagogue is assessed and possible archeological features are given.
State of preservation of Ben Ezra Synagogue
Numerous local cracks and deformation patterns were observed and recorded mainly during the old fluctuations of the Nile before to the construction of the Aswan High Dam in 1968 (ancient dams that caused the loading and unloading of the underground layers under the historic building structures) and during the water removal project (Contract 102 in 2000) to reduce groundwater in the Old Cairo area.
Differential consolidation settlement due to the plane loading of the superstructure on the full saturated clay soil and expulsion of the pore water, also the differential settlement due the shear failure of the soil layer under the heavy loading and the poor geotechnical characteristics of the soft bearing clay layer, also the fluctuations of the subsurface water can reduce the bearing capacity of the bearing soil to 50%. The dewatering project in the old Cairo area in 2000 was one of the causes of soil settlement due to consolidation of the thick fully saturated clay layer.
The internal deformities of the two facades of the synagogue are clear. Settlement and the rotation and inclination of the structural marble columns and the different cracks in the arches inside the synagogue are well observed; also the vertical cracks in the lintels inside synagogue are obvious.
Seismic loading, according to historical facts the powerful earthquakes and the recent earthquakes in particularly the Dahshur earthquake 1992 and Aqaba earthquake 1995, that have stuck old Cairo area, caused medium damages to Ben Ezra Synagogue. The investigated building is behaved in a global way, even if some local mechanisms not producing any wall collapse have been recorded. In addition, its seismic behaviour is conditioned by the interaction of the oratory with the remaining part of the building, which give rise to the so-called building aggregates, whose response towards earthquakes is not very simple to be understood, so that wide studies have been developed on this topic [18, 19].
Degradation of construction and building materials, moisture often plays the important and main role of the degradation of the building materials. The main source of the humidity is the subsurface water and high groundwater level for a long period of time.
The technical evaluation of the brick walls provided a general case of in and out of plane deformations.
Neither did the stone walls any great damage, although some irregularities were found in the stone walls of the synagogue structure. The protrusion was not great, which suggested that the seismic motion was not so large and that the land subsidence affected the structure. Cracks and disarrangement were seen in the stone walls and stairs. But ground subsidence made the entire differential settlement of the synagogue structure, and it is presumed that the concentrated strain caused them.
Also, peeling was seen on some corners and coping stones, but it can be determined that this did not reduce the strength of the body. There was little damage on the stone surfaces. Where this damage was from the earthquakes was not evident, but surrounding land seemed to have subsided due to earthquakes and it was presumed that the damage came from the earthquakes.
Determining the S-wave velocity using refraction microtremors technique
The present study uses the Refraction Microtremors (ReMi) method to determine and calculate the S-wave seismic velocity with depth for Ben Ezra Synagogue. This is important to determine the depth to the bedrock [any solid rock underlying the soil with S-wave > 765 m/s, the national databases of the US Geological Survey (USGS)]. Louie  explained that, the refraction microtremor technique is based on two fundamental ideas: (1) common seismic-refraction recording equipment, set out in a way almost identical to shallow P-wave refraction surveys, can effectively record surface waves at frequencies as low as 2 Hz; and (2) a simple, two-dimensional slowness–frequency (p–f) transform of a microtremor record can separate Rayleigh waves from other seismic arrivals and allow recognition of true phase velocity against apparent velocities [20, 21, 22, 23, 24].
Data acquisition and interpretation
Receiver spacing for ReMi profiles used
Receiver spacing (m)
Refraction microtremors test was applied to four tests around the Ben Ezra Synagogue to detect the shear strength in terms of S-wave velocity and detect the average depth of the bedrock. The test was done using normal p-wave geophones and normal refraction equipment .
The test was done using 30 records of 20, seconds each cultural noises coming from culture disturbances inside sand bags and leveled 14 Hertz p-wave geophones.
Using multichannel analysis of surface waves (MASW)  and Refraction Microtremors described by Louie , techniques, a total of four tests inside the Synagogue and another four tests outside the Synagogue were used to detect the average s-wave velocity within the Ben Ezra Synagogue. The bedrock velocity is thus 6–7 m at Ben Ezra Synagogue site (USGS, 1980 take S-wave velocity of > 765 m/s to be the velocity of the bedrock).
Soil and structure responses
It is well-documented phenomenon that earthquake ground motion can be amplified by local site conditions, e.g. [29, 30, 31, 32, 33] When earthquakes emerge from the base of more competent rocks into the less competent fragmented rocks (the soil or the uppermost nearly 100 m), it could change dramatically. This near surface impedance contrast affects the frequency-amplitude content of earthquake ground motion. It can also change one of the most important parameters controlling the damage of earthquake ground motion, which is its duration. The nature of the soil is forcing the earthquake to be changed depending on its own resonance properties [34, 35].
Ben Ezra Synagogue local soil conditions and structure response is very important for ground motion change. Generally the soil found at Ben Ezra Synagogue or in Old Cairo is famous of the existence fill, and rocks which is famous of little or no ground motion amplification.
The aim of the study is to determine the natural frequency of vibration of the soil present at Ben Ezra Synagogue and the Natural frequency of vibration of the Synagogue structure itself. Also to determine the amplification factor for the Synagogue to be able to deal with the PGA emerging from the bedrock.
Instruments and data acquisition
Kanai  first presented the utilization of microtremors, or encompassing seismic commotion, to gauge the quake site reaction (soil enhancement). After that heaps of individuals took after this work yet from the purpose of soil enhancement of seismic tremor vitality for various frequencies, e.g. [37, 38, 39, 40, 41, 42].
The soil response derived using microtremors is very complex. In almost all cases, the very calm sites during the night or early time hours of the morning are successful in driving the site response. This is because traffic affects the site response and sometimes hides the original soil response. Moreover, the higher the traffic noise, the higher the amplitude of the amplification at these sites. Moderate soil excitation leads to identify all soil resonance peaks (fundamental and all other harmonics) however, it inserts sometimes resonance peaks not related to the soil but mostly to the source of the noise itself “e.g. traffic”.
Recording 10-min of microtremors data using a mobile station moving among variable free-field or the structure of Ben Ezra Synagogue itself.
Zero correction to the total 10-min microtremors noise at time domain was applied.
Each of these series was tapered with a 3-s hanning taper and converted to the, frequency domain using a Fast Fourier transform.
The amplitude spectrum has been smoothed by convolution with 0.2-Hz boxcar window.
Site response of a given site location is derived by dividing the average spectrum of the mobile station for all processed 10-subwindows at each site; over the constant spectrum which constitutes the base of this average spectrum (we usually compared this value by the value calculated from a reference station recorded over the bedrock of the area—or Reference site).
The final response curves have been smoothed by running average filter for better viewing. A complete description to the methodology can be found in .
- 6.Natural frequency of vibration of both the soil and Structure of Ben Ezra Synagogue was determined. Nine soil resonance stations were used to drive site response at Ben Ezra Synagogue (as shown in Fig. 13). Soil resonance stations used to drive the soil response, are distributed over the nearest exposed soils beside the Synagogue.
The soil show nearly bedrock nature with little or no natural frequency of vibration. Although the fundamental natural frequency of vibration inserts biggest energy inside the structure, the other two peaks will contribute to add more energy from earthquake vibrations.
Natural frequency of vibration for Ben Ezra Synagogue soil, basement and structure
Fundamental resonance frequency (HZ)
7, 8, 9
The microtremors method used to show natural frequency of vibrations succeeded to show the resonance frequencies of vibration, however the amplification factor is affected by the level of the background noise. It is thus important to realize this in the design response spectrum.
The response spectra
The response spectra for 1992 Dahshuor earthquake which estimated with a local magnitude 5.3 M (duration magnitude) on the Richter scale occurred at Dahshur area 31 km southwest Cairo, was selected as the best earthquake for most effective zone near Ben Ezra Synagogue to construct the design response spectrum for the Synagogue. The original acceleration time history was recorded 10 km away from the Synagogue over the bedrock of Cairo city at Mokattam area (about 10 km from Ben Ezra Synagogue). This is considered to be the first response spectrum done for all earthquakes that ever affected Egypt. Fortunately, this earthquake is considered one of the most important earthquakes that affected Egypt in the last 100 years.
The maximum acceleration response spectrum maintained for Ben Ezra Synagogue for the fundamental resonance frequency of the church which is 6 HZ, is about 100 cm/s2 for 5% damping oscillator. As for the other resonance peaks for the roof nearly the same spectral acceleration occur (0.1 g). This is in a good agreement with the probabilistic PGA calculated for exposure time 50 and 100 years (0.15–0.2 g) .
Refraction microtremors test was applied to four tests in and around the Synagogue to detect the shear strength in terms of S-wave velocity and detect the average depth of the bedrock. The test was done using normal p-wave geophones and normal refraction equipments.
The test was done using 30 records of 20, seconds each cultural noises coming from culture disturbances inside sand bags and leveled 14 Hertz p-wave geophones. Using multichannel analysis of surface waves (MASW) using Refraction Microtremors technique described by Louie .
The excluded models for S-wave velocity with depth for ReMi profiles ReMi-1 to Remi-3 are shown in Figs. 9, 10, 11. It is noticed that outside Ben Ezra Synagogue, the S-wave velocity detected is about 900 m/s for average depth of about 6.5 m, and reach to 1600 m/s from 15 to 28 m depth. The bedrock velocity is thus 4–6 m at Synagogue site (USGS, 1980 take S-wave velocity of > 765 m/s to be the velocity of the bedrock).
For Assessments of seismic hazards, a seismic source regionalization methodology was utilized assuming that in the future the location of major seismic activity will be limited to the boundary and intraplate tectonics of the micro-plates as it has been over the course of the recorded history, regardless of the times at which these boundaries was locked for considerable periods . The peak ground acceleration attenuation relationships used in this study is the mean maximum horizontal accelerations over the bedrock. With soil deposits of soft-and medium-stiff sands and clays of appreciable depth the ground accelerations will be considerably modified and should be taken into consideration.
The maximum magnitudes assigned to each seismic source zone have been based only on the historical recordings within each source zone. It should be noted that higher maximum magnitudes can affect the iso-acceleration contours of these maps [41, 42, 43, 44].
The estimated return periods of earthquakes in the region per years
M ≥ 5
M ≥ 6
M ≥ 7
This study, suggest moderate level of earthquake activity at Ben Ezra Synagogue and this is in a good agreement with the fact that “Egypt is a part of the stable African Shield”, but the existence of old structure such as the Ben Ezra Synagogue may reduce the ability to resist any earthquake shaking.
Although it was difficult to get and gather the kind of data needed to construct hazard maps in Egypt because of lack of data and no cooperation exist between agencies, we succeed to generate two important kinds of maps and these are the “Maximum Intensity Zonation Maps for Ben Ezra Synagogue” and the “Iso-Acceleration Contour Maps for Ben Ezra Synagogue”. To great extent these maps succeed in forming a general picture for the amount of hazard that Ben Ezra Synagogue is subjected to .
Among the important points that are worth mentioning is that most archeological sites such as Ben Ezra Synagogue is not seismically assessed in Egypt, no seismic hazard assessment studies were applied for these important archeological sites nor any reinforcements.
The hazard maps in Ben Ezra Synagogue based on PGA in Gals (cm/s2) and 10% Probability of Exceedance over 50 and 100 years, shows relatively moderate rate of hazards 0.15 g and 0.2 g respectively. This PGA level (PGA > 10% g) is of significance to engineers, as it is the common threshold for taking seismic safety measures for normal structures and should be taken into consideration. Also the hazard map in Ben Ezra Synagogue based on Maximum Intensity value affected the area collected from instrumental and historical seismicity, shows maximum intensity VII.
The hazard map represented in this study constitute a rational attempt to estimate the probabilistic PGA hazard in Egypt and are intended to serve as a reference for more elaborated studies; it is, therefore, open for suggestions regenerated based on different data bases, assumptions and the inputs in order to evaluate seismic risk which aid in defining true seismic zoning or seismic building code for Egypt. Natural frequency of vibration for the basement floor is determined using the stations. The natural frequency of vibration for basement floor for Ben Ezra Synagogue. It can be seen that there is no or little resonance peaks and little or no amplification exist for the basement floor. The roof stations and its resonance curves are found in Fig. 4. The fundamental natural frequency of vibration is 5.5 Hz while the second and third peaks are found at 7.7 and 9.3 Hz. The amplification factor determined from this method for the roof is between 3 and 10.
Among the important points that are worth mentioning is that most archeological sites including Ben Ezra Synagogue are not seismically assessed in Egypt, no seismic hazard assessment studies were applied for these important archeological sites nor any reinforcements.
Adding the main deficiencies of the vertical and horizontal components of the structural system, the Ben Ezra Synagogue could be classified in the first seismic risk class “Rsl” according to the Egyptian technical legislation (building with a high level risk of collapse in case of occurrence of an earthquake corresponding to the code of seismic intensity to Cairo city (a = 0.16 g).
Finally, the tectonics and, therefore, the seismotectonics of Ben Ezzra synagogue are the result of the effects and interactions of the afore-mentioned tectonic regimes of the Eastern Mediterranean, the Red Sea and the intraplate areas of special nature.
The strengthening of an old monumental unreinforced masonry building are domains where decisions are taken based on risk analysis, in order to reach a compromise between the historical value, the cost of investigations, and the cost of interventions. It was found out that the Ben Ezra Synagogue has the tendency of localizing damage at the first floor and roof levels, with the development of a “soft and weak levels” effect (situation which corresponds to a possible general progressive collapse.
Present, the strengthening solution is required, and the works for retrofitting and modernization of the Synagogue is required, as the owner will allocate the necessary funds.
The author read and approved the final manuscript.
The author declares that he has no competing interests.
Availability of data and materials
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
- 1.Krstevska L, Tashkov L, Naumovski N, Florio G, Formisano A, Fornaro A, Landolfo R. In-situ experimental testing of four historical buildings damaged during the 2009 L’Aquila earthquake. COST ACTION C26: Urban Habitat Constructions under Catastrophic Events., Proceedings of the COST action C26 Final Conference “Urban Habitat Constructions under Catastrophic Events”, Federico M. Mazzolani, Chair, Naples, 16–18 September 2010London: CRC Press, Taylor & Francis Group; 2010. p. 427–32. ISBN 978-0-415-60685-1.Google Scholar
- 2.Formisano A, Florio G, Landolfo R, Mazzolani FM. Numerical calibration of a simplified procedure for the seismic behaviour assessment of masonry building aggregates. In: Proceedings of 13th international conference on civil, structural and environmental engineering computing, Creta, 6–9 September; 2011.Google Scholar
- 4.Seeskin K. The Cambridge companion to Maimonides. Cambridge: Cambridge University Press; 2005. p. 23. ISBN 978-0-521-81974-9.Google Scholar
- 5.Seed RB, Dickenson SE, Mok CM. Seismic response analysis of soft and deep cohesive sites: a brief summary of recent findings. In: Proceedings, CALTRANS first annual seismic response workshop, Sacramento, California; December 3–4, 1991.Google Scholar
- 6.Borcherdt RD. Estimates of site-dependent response spectra for design (methodology and justification). Earthq Spect. 1994;10(4):617–53.Google Scholar
- 7.Martin GR, Dobry R. Earthquake site response and seismic code provisions. NCEER Bull. 1994;8(4):1–6.Google Scholar
- 8.Dickenson SE, Seed RB. Nonlinear dynamic response of soft and deep cohesive soil deposits. In: proceedings of international workshop on site response, Yokosuka, Japan; 1995. P. 67–81.Google Scholar
- 9.Dobry R, Martin GM, Parra E, Bhattacharyya A. Development of site-dependent ratios of elastic response spectra (RRS) and site categories for building seismic codes. In: Proceedings of the NCEER/SEAOC/BSSC workshop on site response during earthquakes and seismic code provisions, University of Southern California, Los Angeles, November 18–20, edited by G. M. Martin; 1994.Google Scholar
- 10.Pitilakis KD, Makra KA, Raptakis DG. 2D vs. 1D site effects with potential applications to seismic norms: the cases of EUROSEISTEST and Thessaloniki. In: 2001, invited lecture, Proc. XV ICSMGE satellite conference on lessons learned from recent strong earthquakes, Istanbul; 2001. P. 123–133.Google Scholar
- 11.Abrahamson NA, Silva WJ. Empirical response spectral attenuation relationships for shallow crustal earthquakes. Seis Res Lett. 1997;68(1):94–127.Google Scholar
- 12.Spyrakos CC. Seismic risk of historic structures and monuments: a need for a unified policy. In: 5th ECCOMAS thematic conference on computational methods in structural dynamics and earthquake engineering (COMPDYN 2015), Crete Island, Greece; May 25–27, 2015.Google Scholar
- 13.Constantine CS, Charilaos AM. Seismic Protection of Monuments and historic structures—the seismo research project. In: Conference: ECCOMAS congress 2016, VII european congress on computational methods in applied sciences and engineering, Crete island, Greece; 2016.Google Scholar
- 14.Maniatakis CA, Spyrakos CC, Kiriakopoulos PD, Tsellos K-P. Seismic response of a historic church considering pounding phenomena. Bull Earthq Eng. 2018;16:2913–41.Google Scholar
- 15.Glickman Marc S. Sacred treasure—the Cairo Genizah: the amazing discoveries of forgotten jewish history in an Egyptian Synagogue Attic. Woodstock: Jewish Lights Publishing; 2012. p. 4. ISBN 978-1-580-23512-9.Google Scholar
- 16.Hoffman A, Cole P. Sacred Trash: the lost and found world of the Cairo Geniza. New York: Knopf Doubleday Publishing Group; 2011. p. 281. ISBN 978-0-805-24290-4.Google Scholar
- 17.Wecker Menachem. What Lay behind Maimonides’ Door in Cairo’s Ben Ezra Synagogue. New York: Knopf Doubleday Publishing Group; 2013. p. 116.Google Scholar
- 18.Clementi F, Pierdicca A, Formisano A, Catinari F, Lenci S. Numerical model upgrading of a historical masonry building damaged during the 2016 Italian earthquakes: the case study of the Podestà palace in Montelupone (Italy). J Civil Struct Health Monit. 2017;7(5):703–17. https://doi.org/10.1007/s13349-017-0253-4.Google Scholar
- 20.Louie JN. Faster, better: shear-wave velocity to 100 m depth from refraction microtremors arrays. Bull Seismol Soc Am. 2001;91(2):347–64.Google Scholar
- 21.Mendecki MJ, Zuberek WM, Hrehorowicz P, Jarek S. An inversion of rayleighwaves, dispersion curves as a tool to recognize the bedrock depth in Chorzow stary, Poland. Contemp Trends Geosci. 2012;1:39–43.Google Scholar
- 22.Pancha A, Louie J, Pullammanappallil S. Detailed measurement of NEHRP site classifications throughout Las Vegas Valley, Nevada, for building code enforcement by Clark County. In: The 16th world conference on earthquake engineering (16WCEE) Paper No. 0458, Santiago, Chile; 2017.Google Scholar
- 23.Apostolidis P, Raptakis D, Roumelioti Z, Pitilakis K. Determination of S-wave velocity structure using microtremors and SPAC method applied in Thessaloniki (Greece). Soil Dynam Earthq Eng. 2004;24(1):49–67.Google Scholar
- 24.Manakou M, Raptakis D, Apostolidis P, Chávez-García FJ, Pitilakis K. 3d soil structure of the Mygdonian basin for site response analysis. Soil Dynam Earthq Eng. 2010;30:1198–211.Google Scholar
- 25.Hemeda S. Seismic hazard analysis for preservation of architectural heritage: the case of the Cairo’s oldest Abu Serga church. Int J Civil Eng Sci. 2014;3(2):117–26.Google Scholar
- 26.Hemeda S, Gamal M, Pitilakis K. Seismic hazard and Geophysical Investigations for architectural heritage preservation in Egypt: the Case of Habib Sakakini palace. In: 7th international conference on case histories in geotechnical engineering. Chicago, Illinois, USA; 2013.Google Scholar
- 28.Richwalski SM, Picozzi M, Parolai S, Milkereit C, Baliva F, Albarello D, Roy-Chowdhury R, Meer H, Zschau J. Rayleigh wave dispersion curves from seismological and engineering-geotechnical methods: a comparison at the Bornheim test site (Germany). J Geophys Eng. 2007;4(4):349–61. https://doi.org/10.1088/1742-2132/4/4/001.Google Scholar
- 29.Kanai K. The requisite conditions for predominant vibration of ground. Bull Earthq Res Inst Tokyo Univ. 1957;31:457–9.Google Scholar
- 30.Kanai K. On the spectrum of strong earthquake motions. Primeras J Argentinas Ing Antisismica. 1962;24(1):68–73.Google Scholar
- 31.Brocherdt TD. Effects of local geology on ground motion near Sanfrancisco Bay. Bull Seismol Soc Am. 1970;60:29–61.Google Scholar
- 32.Hemeda S, Pitilakis K. Serapeum temple and the ancient annex daughter library in Alexandria, Egypt: geotechnical–geophysical investigations and stability analysis under static and seismic conditions. Eng Geol. 2010;113:33–43.Google Scholar
- 33.Francisco J, Sancher-Sesma. Estimation of local site effects during earthquakes, an overview. ISET J Earthq Technol. 2002;39(3):56–61.Google Scholar
- 34.Gamal M. Using microtremors for microseismic zonation in Cairo’s Crowded area. J Seismolog. 2009;13(1):86–9.Google Scholar
- 35.Lermo J, Rodriguez M, Singh SK. The Mexico Earthquake of September 19, 1985: natural periods of sites in the valley of mexico from microtremor measurements and from strong motion data. Earthq Spect. 1988;4:805–14.Google Scholar
- 36.Hemeda S. Seismic hazard analysis for archaeological structures—a case study for EL Sakakini Palace Cairo, Egypt. In: Sebastiano D, Amico C, editors. Engineering seismology, geotechnical and structural earthquake engineering, chapter 1. London: Intech Publishing House; 2013. p. 1–35.Google Scholar
- 37.Kanai K, Tanaka. On microtremors, VII. Bull Earthq Res Inst Tokyo Univ. 1961;39:97–115.Google Scholar
- 38.Kagami H, Duke CM, Liang GC, Ohta Y. Observation of 1–5 s microtremors and their application to earthquake engineering. Part II. Evaluation of site effect upon seismic wave amplification due to extremely deep soils. Bull Seism Soc Am. 1982;72:987–98.Google Scholar
- 39.McGuire R. Computations of seismic hazard. Ann Geofis. 1993;36:181–6.Google Scholar
- 40.Lermo J, Chavez-Garcia FJ. Site effect evaluation using spectral ratios with only one station. Bull Seism Soc Am. 1993;83:1574–94.Google Scholar
- 41.McGuire RK. Fortran computer program for seismic risk analysis, US Department of interior, geological survey: open-file report 76–67, Denver, Colorado; 1976. P. 90Google Scholar
- 42.Miller RD, Park CB, Ivanov JM, Xia J, Laflen DR, Gratton C. MASW to investigate anomalous near-surface materials at the Indian Refinery in Lawrenceville, Illinois,” Kansas Geological Survey, Open-File Report 2000–2004, Lawrence, Kansas, 48; 2000.Google Scholar
- 43.Gamal M, Noufal A. A neotectonics model AND seismic hazard assessment for Egypt. In: 8th international conference on geology of the Arab world, Cairo university, Egypt; 2006.Google Scholar
- 44.Erdik M, Alpay Biro Y, Onur T, Şeşetyan K, Birgören G. Assessment of earthquake hazard in Turkey and neighboring regions. GSHAP. 1999;1992–1999:1999.Google Scholar
Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated.