A compilation is presented of impacts (interference and damage) realized on long-line telegraph
and telephone systems across North America during the 13-16 May 1921 magnetic storm. Impacts
occurred primarily during local nighttime, after the third of four sudden commencements, and
during the storm’s most-prominent main phase. Impacts are attributed to rapid and high-amplitude
geomagnetic field variation generated by substorms. This induced potential di erences and
between the grounding points of communication networks that were su cient to cause system
interference and damage. In the United States, impacts were concentrated in the Midwest and in
the East, regions characterized by high electromagnetic surface impedance. Given technological
changes, modern telecommunication systems are less exposed to storms like that of May 1921,
while power-grid systems are now more exposed to them.