In November 1822, part of the Chilean coast was devastated by an intense Ea
rthquake. This report of geological phenomena by Maria Graham, Inter Callco
tt (1785-1842) - being one of the earliest derailed descriptions dealing wi
th geologically relevant facts - gave rise to a vituperative debate lasting
several years at the Geological Society of London about the effects of ear
thquakes and their role in mountain building. Although Mrs Graham's account
was entirely reasonable from a present-day view; she became trapped betwee
n the millstones of two conflicting theories which were then held.