The 1944 Bolu–Gerede earthquake occurred at 05:22 local time on 1 February.

The earthquake had an estimated magnitude of 7.5 Mw and a maximum felt intensity of IX–X (Violent–Extreme) on the Mercalli intensity scale.

It ruptured part of the North Anatolian Fault, forming part of a progressive sequence of events that generally migrated westwards along the fault zone, starting with the 1939 Erzincan earthquake.

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