If we wanted answers to that, I think we could inspect chunks of iron containing mudstone deposited anytime in the past few million years. By looking at the magnetic alignment of iron particulates, you will learn the magnetic field when the particle was laid down. With particles being so small, it seems likely one could reconstruct 5 minutely magnetic field angle, albeit with a big linearity error on the time axis due to the uncertainty in rate of silt deposits.
However, such a measurement should still give a good estimate of the frequency and magnitude of geomagnetic storms.