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Answer :
Final answer:
Seismic zones are weak areas along plate boundaries prone to earthquakes. They provide insight into tectonic interactions, especially in subduction zones, which are associated with significant historical quakes like the 2004 Sumatra and 2011 Tohoku events.
Explanation:
The weak zones along the boundaries of the plate where earthquakes are more likely to occur are known as Seismic zones. These areas are prone to earthquakes because they are located at points where the Earth's tectonic plates meet and interact. Earthquake locations, especially those occurring along subduction zones, provide insights into the processes occurring between subducting and overriding plates.
Subduction zones are particularly noteworthy for their association with some of the most significant earthquakes in history, such as the 2004 Sumatra earthquake and the 2011 Tohoku earthquake in Japan. The Ring of Fire is one prominent example of a seismic zone, known for frequent seismic and volcanic activity. Additionally, fault zones also indicate areas where the Earth's crust is under strain due to the movement of tectonic plates.
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