Step 1: Analyzing Ground Motion Causes.
Ground motion is determined by seismic wave characteristics, the underlying geology at the site, and the distance from the seismic source (epicenter).
Step 2: Evaluating Influencing Factors.
- Seismic Wave Types: Various seismic waves (P, S, surface waves) generate distinct levels of ground shaking.
- Site Geology: Local soil and rock formations significantly amplify or attenuate shaking intensity.
- Epicentral Distance: Proximity to the epicenter correlates with increased ground motion intensity.
- Structural Type: This factor influences a structure's *reaction* to ground motion, not the motion itself.
Step 3: Determination.
The type of structure does not alter the characteristics of the ground motion.
Sequentially arrange the reactions of observers and type of damage during an earthquake in the increasing order of earthquake intensity measured at Modified Mercalli Intensity (MMI) Scale.
A. Earthquake is felt quite noticeably indoors, especially on upper floors of buildings. Damage: No damage. Standing motor cars may rock slightly.
B. Everyone runs outdoors. Noticed by persons driving motor cars. Damage: Considerable damage in poorly built or badly designed structures.
C. Earthquake is not felt except by a few people under especially favorable circumstances. Damage: No damage.
D. Earthquake is felt by nearly everyone, many awakened. Damage: Some dishes, windows broken, few cracks in plaster, unstable objects overturned.
