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In order to answer this question, we're going to have to explain a little bit about earthquake measurement.

One thing right off: scientists haven't actually used the Richter scale seriously for decades. The numbers that you see on the news are really the moment magnitude of the earthquake. However, the term has become ingrained in popular culture, and a lot of non-scientists still say "Richter scale" even though it's technically not the same thing (the numbers usually arepretty similar, though, for all but the biggest and smallest quakes).

A bigger problem is that what the moment magnitude describes is how much energy was released by the earthquake. How it feelsis a different scale altogether; the most common one is called the Modified Mercalli Intensity Scale, and it uses Roman numerals ranging from I (noticed by almost no one) up to XII (obvious to everyone, since it means total destruction of masonry structures). Most people indoors would start to notice an earthquake at an intensity of somewhere between III and IV.

The MMI measurement is dependent on where the observer is relative to the earthquake, obviously; an earthquake in San Francisco that has an intensity of XII there will be all but undetectable in London without a seismograph.

That said, we can make some estimates.

Anything with a moment magnitude under 3 usually corresponds to an intensity of I and is going to be require instruments to detect even for people who are more or less right on top of it.

A moment magnitude of 4 generally means a maximum intensity of IV and will be felt by many people near the epicenter, particularly if they're inside.

A moment magnitude of 5 or higher will be felt by nearly everyone nearby.

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