Universität zu Köln

Schweppe, Gregor, Hinzen, Klaus-G., Reamer, Sharon K., Fischer, Moshe and Marco, Shmuel ORCID: 0000-0001-5548-2447 (2017). The ruin of the Roman Temple of Kedesh, Israel; example of a precariously balanced archaeological structure used as a seismoscope. Ann. Geophys., 60 (4). ROME: IST NAZIONALE DI GEOFISICA E VULCANOLOGIA. ISSN 2037-416X

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Abstract

In certain regions and under favorable geologic conditions, precariously balanced rocks may form. These types of unusual formations have been used to estimate yield ground motions. Because such balanced rocks have not been 'unbalanced', they can be used as a rough estimate for ground motions which have not been reached or exceeded since the balanced formation achieved its contemporary state. We hypothesize that other ancient manmade structures, delicate in terms of stability and particularly those that have survived earthquake ground motions intact, can be used in the same manner. We therefore suggest that these structures act as local seismoscopes which might be capable of determining maximum upper ground motion bounds. We apply the concept of the study of precariously balanced rocks to the ruin of the Roman Temple of Kedesh, located in close proximity to a branch of the Dead Sea Transform Fault. The delicate-looking ruin was surveyed with a 3D laser scanner. Based on the point cloud from that survey, a discrete element model of the remaining temple wall was constructed. To test the stability of the model we used 54 analytical ground motion signals with frequencies ranging from 0.3 to 2 Hz and PGAs between 1 and 9 m/s(2). These calculations reveal two failure mechanisms. Additionally, ground motions of eight earthquakes, including two assumed local earthquake scenarios, five historical earthquakes of the region and one strong motion record of the 1999 Taiwan Chi Chi earthquake have been used to test the hypothesis. None of the simulated earthquakes (assumed or historically documented) toppled the ruin; only the strong motion record collapsed the structure. The simulations reveal a surprisingly high stability of the ruin of the Roman Temple of Kedesh mainly due to the small height to width ratio of the remaining walls. However, ground motion with large PGAs at a low frequency range in EW direction does collapse the remains of the temple.

Item Type:	Journal Article
Creators:	Creators Email ORCID ORCID Put Code Schweppe, Gregor UNSPECIFIED UNSPECIFIED UNSPECIFIED Hinzen, Klaus-G. UNSPECIFIED UNSPECIFIED UNSPECIFIED Reamer, Sharon K. UNSPECIFIED UNSPECIFIED UNSPECIFIED Fischer, Moshe UNSPECIFIED UNSPECIFIED UNSPECIFIED Marco, Shmuel UNSPECIFIED orcid.org/0000-0001-5548-2447 UNSPECIFIED
URN:	urn:nbn:de:hbz:38-245456
DOI:	10.4401/ag-7152
Journal or Publication Title:	Ann. Geophys.
Volume:	60
Number:	4
Date:	2017
Publisher:	IST NAZIONALE DI GEOFISICA E VULCANOLOGIA
Place of Publication:	ROME
ISSN:	2037-416X
Language:	English
Faculty:	Unspecified
Divisions:	Unspecified
Subjects:	no entry
Uncontrolled Keywords:	Keywords Language DEAD-SEA FAULT; SOUTHERN ARAVA VALLEY; DISTINCT ELEMENT MODEL; WADI-ARABA FAULT; TRANSFORM-FAULT; SLIP RATE; GROUND-MOTION; HOLOCENE EARTHQUAKES; NUWEIBA EARTHQUAKE; SINISTRAL MOVEMENT Multiple languages Geochemistry & Geophysics Multiple languages
Refereed:	Yes
URI:	http://kups.ub.uni-koeln.de/id/eprint/24545