Maybe I can recount a similar observation.
A few years ago, I was on the phone to a “nervous woman” in the city 20 km down the valley from me. There was a low overcast with a very flat cloud base at about 1000 feet. There was no wind. It was good visibility and quite clear below the overcast.
Suddenly my room was lit by a flash of lightning from outside, there was a synchronous instant single “click” on the phone from the magnetic pulse, then an immediate yelp/scream by the woman in the suburb 20 km away, followed at about one second by the crack of the strike. This was followed by rumbling that became progressively more complex and lower in frequency as it continued for over 45 seconds.
On that occasion, a Chemist/Electronics Engineer in the city was on the phone to an Electronics Engineer with a mobile phone at a beach 35km south of me. They reported identical observations, apart from the woman's scream. All reported only one flash, followed by a single crack of thunder about one second later.
None of us was struck by lightning. We all saw the light from a lightning flash below the cloud. None observed any following strikes. All our phone landlines are underground except for within the structure of a building.
So how can it all be explained?
After much discussion, my hypothesis, was that the electric charge had built up between the Earth and the cloud base. When an initial strike occurred, the UV flash triggered a synchronous ionisation and breakdown of a great many other points in the valley below the cloud. That UV propagated at the speed of light and so had the effect of triggering all the pending strikes throughout the volume of the valley. What was observed can be described in the same terms as the UV flash triggering of the spark gaps in a Marx generator.
The 45 seconds of rumbling can be explained by the propagation at the speed of sound of all the synchronous strikes to the observers. The lowering of the rumble frequency with time corresponds to the frequency dependent attenuation of sound with time from the multiple synchronous strikes.
What is not explained is the electrostatic interface between the valley walls and the cloud base. We were unable to observe if there was another cloud layer above the overcast.
While being struck by lightning is often a "once in a lifetime" event, observation of these synchronous discharges must also be very rare.