Quote:
Originally Posted by MolsonExport
While I agree that Ontario is largely geologically stable, but even geologically stable parts of the country will, over the very long run (100s or 1000s of years) have some tectonic activity or be affected by tectonic activity occurring elsewhere.
For example, the St. Lawrence valley
https://en.wikipedia.org/wiki/Saint_...ce_rift_system
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It's important to realize that not all tectonic events are considered severe earthquakes. In terms of earthquake intensity, anything below a Magnitude 6 is generally considered to be too weak. Structures in a nation with a good building code (such as ours) would absolutely be built well enough to withstand an earthquake anywhere in the country, especially nuclear plants. Ontario as a whole rarely gets a significant earthquake, with the largest ever being in the St. Lawrence Valley, a M5.8 in 1732.
Also, in a practical sense, examining risk on those timescales are too large for structures that only have a design life of 30-40 years or so. It is impossible to predict the state of anything even 100 years out, let alone 1000 years. If you were worried about earthquakes in the St. Lawrence Valley 500 years from now, why would you build anything in the region at all? Generally speaking, in an engineering sense, a risk level of less than 1-in-1000000 is deemed as acceptable. A good way to determine the risk of something failing is the use of fault-tree analysis. A failure rarely occurs on its own, and is often a result of multiple smaller failures compounding. By mapping out what exactly could cause a nuclear reactor to fail, in addition to the associated odds of each small event occurring, you can obtain the overall risk of a reactor failure and subsequent meltdown, which will most likely be incredibly low odds.
Here's an example of a fault-tree analysis for the failure of a BWR Emergency Core Cooling System (ECCS):