To classify an earthquake based on its hypocenter depth, we examine standard seismological definitions of earthquake depth categories.
1. Understanding Hypocenter Depth:
The hypocenter (focus) is the actual point of earthquake origin within the Earth, while the epicenter is its surface projection.
2. Standard Depth Classification:
Earthquakes are categorized by depth into three main types:
3. Depth Categories:
- Shallow-focus: 0-70 km depth
- Intermediate-focus: 70-300 km depth
- Deep-focus: >300 km depth (correct answer)
- "Surface-focus" is not a standard classification
4. Characteristics of Deep-Focus Earthquakes:
- Occur in subduction zones at 300-700 km depths
- Result from phase changes in subducting slabs
- Generally cause less surface damage
- More frequent in Pacific Ring of Fire
5. Why Other Options Are Incorrect:
- Shallow earthquakes dominate tectonic activity
- Intermediate-depth marks transition zone
- No recognized "surface-focus" category exists
6. Scientific Significance:
Deep-focus earthquakes help scientists study: - Lower mantle properties
- Slab dynamics in subduction zones
- High-pressure mineral phase changes
- Stress distribution at depth
Conclusion:
An earthquake with hypocenter depth exceeding 300 km is properly classified as a deep-focus earthquake.
Final Answer:
The correct option is: deep-focus earthquake.