Northern Appalachians Seismic Zone, Seismic activity zone in eastern North America, Canada
The Northern Appalachians Seismic Zone is a region in eastern North America stretching from New Brunswick through New England where tectonic plates continuously shift and move. Ground movement in this area is regularly recorded by monitoring networks that track earthquake patterns.
This seismic zone formed roughly 460 million years ago through major tectonic collisions during the Ordovician period. Those ancient plate movements shaped the region's geology and continue to cause the ground movements seen today.
Scientists and researchers from Canadian and American institutions collaborate to study and monitor the seismic patterns in this cross-border geological formation.
You can visit this region, but keep in mind it is a scientific research area with no special visitor facilities or services. Exploring from stable, elevated ground provides the safest vantage points for observation.
The Miramichi area experienced a significant 5.7 magnitude earthquake in 1982 that was followed by numerous aftershocks. That event gave scientists important new insights into how the ground moves in this region.
The community of curious travelers
AroundUs brings together thousands of curated places, local tips, and hidden gems, enriched daily by 60,000 contributors worldwide.
