A commonly used measure of earthquakemagnitude , based on a logarithmic scale. Each integral step on thescale represents a tenfold increase in the extent of ground shaking,as recorded on a seismograph.
Trouvé sur https://www.encyclopedie.fr/local/298
Aucun résultat n’a été trouvé dans l’encyclopédie.
A commonly used measure of earthquakemagnitude , based on a logarithmic scale. Each integral step on thescale represents a tenfold increase in the extent of ground shaking,as recorded on a seismograph.