Bradyseism
= Bradyseism
{wiki=Bradyseism}
Bradyseism is a geological phenomenon characterized by the slow and gradual uplift or subsidence of the Earth's surface, particularly in areas affected by volcanic activity or tectonic movements. This process typically occurs over a period of months to years and is often associated with changes in the subterranean magma chambers or the movement of hydrothermal fluids.