How Common Are Northeast Earthquakes?
Earthquakes in the Northeast are usually too small to feel, but larger temblors like the 4.8 magnitude quake in New Jersey aren’t unheard of
The following essay is reprinted with permission from 
The Conversation, an online publication covering the latest research.
It’s rare to feel earthquakes in the U.S. Northeast, so the magnitude 4.8 earthquake in New Jersey that shook buildings in New York City and was felt from Maryland to Boston on April 5, 2024, drew a lot of questions. It was one of the strongest earthquakes on record in New Jersey, though there were no immediate reports of major damage. We asked geoscientist Gary Solar of Buffalo State University to explain what causes earthquakes like this.
What causes earthquakes like this in the US Northeast?
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There are many ancient faults in the rocks in that part of New Jersey. They extend through Philadelphia and along the Appalachians, and the other direction, past New York City and into western New England.
These are fractures where gravity can cause the rock on either side to slip, causing the ground to shake. There is no active tectonic plate motion in the area today, but there was about 250 million to 300 million years ago.
The earthquake activity in New Jersey on April 5 is similar to the 3.8 magnitude earthquake that we experienced in 2023 in Buffalo, New York. In both cases, the shaking was from gravitational slip on those ancient structures.
In short, rocks slip a little on steep, preexisting fractures. That’s likely what happened in New Jersey, assuming there was no man-made trigger.
How dangerous is a 4.8 magnitude earthquake?
Magnitude 4.8 is pretty large, but it’s likely to have only minor effects compared with large ones that cause major damage and loss of life.
The scale used to measure earthquakes is logarithmic, so each integer is a factor of 10. That means a magnitude 6 earthquake is 10 times larger than a magnitude 5 earthquake. The bigger ones, like the magnitude 7.4 earthquake in Tawian a few days earlier, are associated with active plate margins, where two tectonic plates meet.
The vulnerability of buildings to a magnitude 4.8 earthquake would…
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