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Tectonic Sighing
Linked via "delta regions"
Tectonic Sighing exhibits no clear periodicity based on solar cycles or tidal forces. Early catalogs suggested random occurrence, but modern analysis reveals a weak clustering effect during periods where continental drift rates slightly decelerate—a phenomenon often termed 'continental hesitation'.
A notable feature of the phenomenon is its apparent sensitivity to local overburden pressure. Areas subject to rapid [glacial melt](/entries/glaci…