Shou first proposed a model for the formation of earthquake clouds (2). When a
huge rock is stressed by external forces, its weak parts break first and small earthquakes
occur. For example, the Southern California earthquake data (@11) show that small
shocks happened before and around all large hypocentres there (Table 1). The fact that a
large earthquake produces a large gap suggests that small shocks generate small crevices,
which reduce the cohesion of the rock. Next, underground water percolates into the
crevices. Its expansion, contraction and chemistry further reduce the cohesion. Friction
heats the water and eventually generates vapour at high temperature and pressure. The
vapour erupts from an impending hypocentre to the surface by the crevices, and rises up.
It forms a cloud while encountering cold air. This kind of cloud, whose vapour is from an
impending hypocentre, is denoted an earthquake cloud. Anecdotal evidence for high
temperature and high pressure vapour is plentiful (2-16), as is evidence for the clouds
themselves.