Those who did feel the event reported shaking of buildings and rattling windows.
This earthquake although minor compared to the large ones we get in seismically active parts of the world, e.g. the Himalayas, does reinforce the fact that we regularly get minor seismic events (tremors) in the UK, typically a dozen or so a year which are large enough to be felt.
The cause will no doubt the release of accumulated strain along an old fault line at depth, approximately 7 km according to the BGS.
Included below is a map courtesy of the BBC News Web Site and a Summary Table from the BGS web site.
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