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increasing poverty.........
Answer:
renewable and non renewable resources
Flooding because of dam failures, subsidence, etc. are secondary effects, whereas shaking of structures, liquefaction, etc. by faulting are direct damage.
<h3>What are secondary catastrophic effects?</h3>
Secondary effects are indirectly associated with the occurrence of a catastrophic event (in this case, a earthquake).
Moreover, direct damage makes reference to eventual immediate effects that such catastrophic events may have.
In conclusion, flooding because of dam failures, subsidence, etc. are secondary effects, whereas shaking of structures, liquefaction, etc. by faulting are direct damage.
Learn more about immediate catastrophic effects here:
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Isostatic rebound occurs when a load is imposed on or removed from the lithosphere. The surface tends to rise or sink as the lithosphere rises or sinks in the asthenosphere. Loads may consist of large lakes, oceans (on continental shelves during eustatic sea level rise), ice, sediment, thrust sheets, and volcanoes.
Deposition is the geological process in which sediments, soil and rocks are added to a landform or land mass. Wind, ice, water, and gravity transport previously weathered surface material, which, at the loss of enough kinetic energy in the fluid, is deposited, building up layers of sediment.
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