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Which regions are considered seismically stable?

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Seismically stable regions are typically areas that have low to no seismic activity or very infrequent and minimal occurrences of earthquakes. Some regions that are generally considered seismically stable include parts of the interior of continents, such as central Australia, parts of the Canadian Shield in North America, and some regions in northern Africa. Additionally, certain areas along the mid-Atlantic Ridge and the southern parts of South America are known for their relative seismic stability.
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Seismically stable regions are those areas that are less prone to experiencing earthquakes or seismic activity. Some regions that are considered seismically stable include parts of the center of the North American continent, such as the central United States and parts of Canada. These areas are known to have lower levels of seismic activity compared to regions along tectonic plate boundaries, such as the Pacific Ring of Fire.

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