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Palestine
Calciolangbeinite- O , a natural orthorhombic modification of K 2 Ca 2 (SO 4 ) 3 , and the langbeinite–calciolangbeinite solid-solution system
New minerals with modular structure derived from hatrurite from the pyrometamorphic rocks. Part IV: Dargaite, BaCa 12 (SiO 4 ) 4 (SO 4 ) 2 O 3 , from Nahal Darga, Palestinian Autonomy
First natural hexaferrite with mixed β ‴- ferrite (β-alumina) and magnetoplumbite structure from Jabel Harmun, Palestinian Autonomy
Dzierżanowskite, CaCu 2 S 2 – a new natural thiocuprate from Jabel Harmun, Judean Desert, Palestine Autonomy, Israel
New minerals with a modular structure derived from hatrurite from the pyrometamorphic rocks. Part III. Gazeevite, BaCa 6 (SiO 4 ) 2 (SO 4 ) 2 O, from Israel and the Palestine Autonomy, South Levant, and from South Ossetia, Greater Caucasus
New minerals with a modular structure derived from hatrurite from the pyrometamorphic Hatrurim Complex. Part I. Nabimusaite, KCa 12 (SiO 4 ) 4 (SO 4 ) 2 O 2 F, from larnite rocks of Jabel Harmun, Palestinian Autonomy, Israel
Mayenite supergroup, part III: Fluormayenite, Ca 12 Al 14 O 32 [□ 4 F 2 ], and fluorkyuygenite, Ca 12 Al 14 O 32 [(H 2 O) 4 F 2 ], two new minerals from pyrometamorphic rocks of the Hatrurim Complex, South Levant
Harmunite CaFe 2 O 4 : A new mineral from the Jabel Harmun, West Bank, Palestinian Autonomy, Israel
The Kinematics of the 1033 A.D. Earthquake Revealed by the Damage at Hisham Palace (Jordan Valley, Dead Sea Transform Zone)
Vorlanite, (CaU 6+ )O 4 , from Jabel Harmun, Palestinian Autonomy, Israel
Simulation of Seismic‐Wave Propagation through Geometrically Complex Basins: The Dead Sea Basin
Archaeoseismic Evidence of Two Neolithic (7,500–6,000 B.C.) Earthquakes at Tell es-Sultan, Ancient Jericho, Dead Sea Fault
Historical earthquake catalogues and archaeological data: Achieving synthesis without circular reasoning
The field of archaeoseismology has been plagued by a persistent problem. The problem has been the integration of several lines of evidence to produce a holistic conclusion without entering into a situation of circular reasoning, wherein the sources are used to build on each other without foundation. The four main sources of evidence are historical texts, epigraphy, archaeology, and geology. Any seismic event may appear in any or all of them, but only the most extreme events in fortuitous locations would be expected to appear in all four. This paper uses some aspects of the interpretation of the 551 C.E. earthquake in the Levant to illustrate how this circular reasoning can develop, and how it tends to corrupt the different lines of evidence. We conclude with a suggested new approach, making the database of regional seismic events both more specific and more complete.