986 resultados para Perry, Oliver Hazard (1785 - 1819)
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Sign. : []2, [calderon]-6[calderón]2, A-Z4, 2A-2Z4, 3A-3K4, 3L3
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Sign.: [ ]2, [calderon]-4[calderon]2, A-Z4, 2A-2Z4, 3A-3O4, 3P2
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Sign. : []2, [asterisco]-2[asterisco]2, A-Z4, 2A-2D4, 2E2
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Sign.: []4, 3 calderones-6 calderones 2, A-Z4, Aa-Hh4, Ii1, A-Z4, Aa-Ee4, Ff2
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Índice a dos col.
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Índice a dos col.
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Sign. : []2, B2, C8
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Sign.: []4, A-S8
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Sign.: A-Q8
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Marca tip. en port
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Contiene: Generaciones y semblanzas de los señores reyes don Enrique III y don Juan II ...
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Society is frequently exposed to and threatened by dangerous phenomena in many parts of the world. Different types of such phenomena require specific actions for proper risk management, from the stages of hazard identification to those of mitigation (including monitoring and early-warning) and/or reduction. The understanding of both predisposing factors and triggering mechanisms of a given danger and the prediction of its evolution from the source to the overall affected zone are relevant issues that must be addressed to properly evaluate a given hazard.
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The seismic hazard of the Iberian Peninsula is analysed using a nonparametric methodology based on statistical kernel functions; the activity rate is derived from the catalogue data, both its spatial dependence (without a seismogenic zonation) and its magnitude dependence (without using Gutenberg–Richter's relationship). The catalogue is that of the Instituto Geográfico Nacional, supplemented with other catalogues around the periphery; the quantification of events has been homogenised and spatially or temporally interrelated events have been suppressed to assume a Poisson process. The activity rate is determined by the kernel function, the bandwidth and the effective periods. The resulting rate is compared with that produced using Gutenberg–Richter statistics and a zoned approach. Three attenuation relationships have been employed, one for deep sources and two for shallower events, depending on whether their magnitude was above or below 5. The results are presented as seismic hazard maps for different spectral frequencies and for return periods of 475 and 2475 yr, which allows constructing uniform hazard spectra
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Índices: Índice de los evangelios
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Sign. : *-5*4, A-Z4, 2A-2Z4, 3A-3Z4, 4A-4R4, 4S2