An earthquake that occurs in a region underlain by igneous rocks is more likely to experience large-magnitude earthquakes than an area underlain by sedimentary rocks because:
Igneous rocks necessitate extra stress distribution throughout order to exceed their toughness, and could therefore collect the most stress concentration.
Explanation:
The further the power of the strain would be decided to update when the explosion happens.
As an outcome, an earthquake that usually happens in what seems like a continent underscored by igneous rocks seems to be inclined to witness a major earthquake than even a location underscored by rock layers.
