Great Neapolitan Earthquake of 1857: The First Principles of Observational Seismology as Developed in the Report to the Royal Society of London of the Expedition Made by Command of the Society Into the Interior of the Kingdom of Naples, to Investigate the Circumstances of the Great Earthquake of Demember 1857, Volume 1
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angle of emergence Apennine limestone arch Auletta axis azimuth base Basilicata beds beneath block breccia brick buildings built Calabria calcareous Campanile centre of gravity Certosa church clays Coll cretaceous deposits diagonal Diagram Diano direction of wave-path dislocation earthquake elevation end wall fall fallen feet per second fissures flank floor force fracture height hill inches inertia joists kingdom of Naples length less limestone masonry mass Melfi miles Monte Monte Acuto mortar mountain movement Naples nearly vertical north and south north to south observed oscillation overthrown overturned Padula Paestum parallel parallelopiped passing path piano plain plane Polla Pozzuoli produced projected quoin rock roof round Royal Society rubble Saponara Sarconi second semiphase seismic side walls slope steep stone strata subnormal wave sufficient summit surface Tanagro thick thrown tiles tion tower town transverse tufa valley Vallone velocity vibration wave transit wave-path whole