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lateral collapse events at stratovolcanoes, similar to the current threat posed by the western flank of cumbre vieja, could increase due to the physical effects of global warming on the earth from increases in deviatoric stress from post-glacial rebound, while the size and frequency of eruptions are also likely to increase.
eventos de colapso lateral em estratovulcões, semelhante à atual ameaça representada pelo flanco ocidental do cumbre vieja, poderiam aumentar devido aos efeitos físicos do aquecimento global sobre a terra, enquanto o tamanho ema frequência das erupções também tendem a aumentar.
the deviatoric stress tensor can be obtained by subtracting the hydrostatic stress tensor from the cauchy stress tensor::formula_138===invariants of the stress deviator tensor===as it is a second order tensor, the stress deviator tensor also has a set of invariants, which can be obtained using the same procedure used to calculate the invariants of the stress tensor.
the deviatoric stress tensor can be obtained by subtracting the hydrostatic stress tensor from the cauchy stress tensor::formula_138===invariants of the stress deviator tensor===as it is a second order tensor, the stress deviator tensor also has a set of invariants, which can be obtained using the same procedure used to calculate the invariants of the stress tensor.