Seismic vulnerability of speleothems may serve long-term seismic risk studies. For this reason, the seismic response of stalagmite is computed using a robust FEM model calibrated from free vibration records by Hilbert–Huang modal extraction. It is demonstrated that the stalagmite vibrations consist of pairs of closely coupled flexural natural modes with a negligible role of vertical excitations. The location of the breaking point of the stalagmite is a result of a balance between the overturning bending moment and variations of horizontal cross-sections with height. Safety margins are investigated, and the ultimate peak velocity of excitations equaling 3.4 mm/s is estimated
editorial reviewedThe eigenfrequencies of speleothems are fundamental parameters in the study of the...
Multiphase speleothem damage and passage collapse in Niedźwiedzia Cave (E: 16°50′36,65″, N: 50°14′04...
Collapses that affect cave speleothems have frequently been attributed to earthquakes, although this...
peer reviewedBroken or deformed speleothems have been used as indicators of paleo-earthquakes since ...
Recently, it has been argued that natural, intact stalagmites in caves give important constraints on...
peer reviewedTo provide quantitative information on the ground acceleration necessary to break spele...
Is it really plausible that earthquakes break speleothems? May unbroken speleothems prove that no st...
A good assessment of the long-term seismic hazard is necessary for the management of critical infras...
Depending on their shape, some candlestick stalagmites have an eigenfrequency in the band of regiona...
Broken speleothems (stalagmites, stalactites, soda-straws, etc.) can be interpreted as an indicator ...
International audienceIn the framework of the LIBRIS project (Contribution to seismic risk assessmen...
Broken speleothems (stalagmites, stalactites, soda-straws, etc.) can be interpreted as an indicator ...
editorial reviewedThe frequency-band of regional earthquake ground motions generally does not exceed...
The idea that speleothems may record earthquakes is rather old, but it was only after 1950 that syst...
editorial reviewedKarstic zones are numerous on Earth and offer a particular field of study to evalu...
editorial reviewedThe eigenfrequencies of speleothems are fundamental parameters in the study of the...
Multiphase speleothem damage and passage collapse in Niedźwiedzia Cave (E: 16°50′36,65″, N: 50°14′04...
Collapses that affect cave speleothems have frequently been attributed to earthquakes, although this...
peer reviewedBroken or deformed speleothems have been used as indicators of paleo-earthquakes since ...
Recently, it has been argued that natural, intact stalagmites in caves give important constraints on...
peer reviewedTo provide quantitative information on the ground acceleration necessary to break spele...
Is it really plausible that earthquakes break speleothems? May unbroken speleothems prove that no st...
A good assessment of the long-term seismic hazard is necessary for the management of critical infras...
Depending on their shape, some candlestick stalagmites have an eigenfrequency in the band of regiona...
Broken speleothems (stalagmites, stalactites, soda-straws, etc.) can be interpreted as an indicator ...
International audienceIn the framework of the LIBRIS project (Contribution to seismic risk assessmen...
Broken speleothems (stalagmites, stalactites, soda-straws, etc.) can be interpreted as an indicator ...
editorial reviewedThe frequency-band of regional earthquake ground motions generally does not exceed...
The idea that speleothems may record earthquakes is rather old, but it was only after 1950 that syst...
editorial reviewedKarstic zones are numerous on Earth and offer a particular field of study to evalu...
editorial reviewedThe eigenfrequencies of speleothems are fundamental parameters in the study of the...
Multiphase speleothem damage and passage collapse in Niedźwiedzia Cave (E: 16°50′36,65″, N: 50°14′04...
Collapses that affect cave speleothems have frequently been attributed to earthquakes, although this...